('Alexandra, Hay River, N.W.T.',1922,'Alexandra','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','45',NULL,NULL,NULL,'4','More than 1000 m',NULL,'48',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'50','0','50',0,'no',0,'no','2','6 to 24 reef building species','12','1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',917,2545,'Barrier reef complex.\n35-45 m thick.\nReef complex #1 of ref. 2545\nRugose corals and stromatoporoids about equally important. Tabulate corals present\nReefs also in Twin Falls and Hay River Fms.',60,-116,-625010,-4164963,'Canada','North America',121,'2738, 2735',60.5,-116.25,'WAHR','81119',-3.95125036067,-53.0608310769,-3.95125036067,-53.0608310769,3.71007385886,-113.308256528),('Carlson Lake, N.W.T.',1923,'','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m',NULL,'55',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',917,0,'Coral-stromatopore patch reefs and biostromes. Maximum thickness 50 m.',62,-123,-90046,-4245470,'Canada','North America',121,'',62.3333,-123.5833,'','',-0.00916951510691,-53.3867983074,-0.00916951510691,-53.3867983074,7.44525889832,-114.616409499),('Celibeta, Jean Marie, N.W.T.',1924,'Jean-Marie','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,377,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',917,2737,'Platform reef chain > 100 km length, 30 km width. Thickness around 100 m.\nJean Marie member of Redknife = Jean Marie Formation',61,-121,-329200,-4356514,'Canada','North America',121,'',61.3333,-121.75,'WAHR','83807',-1.2574809227,-53.8231221184,-1.2574809227,-53.8231221184,6.12733206636,-114.725332),('Arrowhead, Jean Marie, N.W.T.',1925,'Kakisa','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,377,3,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100','1924',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',917,2738,'See reef 1924 for remarks.',61,-122,-251315,-4334621,'Canada','North America',121,'',61.05,-122.5,'WAHR','84005',-1.08860920722,-54.2502420329,-1.08860920722,-54.2502420329,6.1830172513,-115.183794754),('Winnifried Pass, Alberta',1926,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','35',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp',NULL,'','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite',NULL,'','0','',0,'No or unknown reservoir potential',917,1507,'Scattered stromatoporoids and colonial corals.\nMicrite and stromatactis mounds on fore-reef slope.\n35 m thick, 75 m exposed width.\n',53,-119,-749690,-5147335,'Canada','North America',121,'',53.6333,-119.2833,'WAHR','83698',-6.41682338185,-59.7040720328,-6.41682338185,-59.7040720328,0.401303476146,-120.448549549),('Ice Fall Brook Canyon, B. C.',1927,'Southesk','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','90',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','6','Calcisponges','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',917,0,'Stacked mounds with sponges(?), corals and amphiporids.\n90 m total thickness. Individual patch reefs 5-42 m thick.',51,-117,-1036163,-5206185,'Canada','North America',121,'',51.9,-117.0667,'','',-8.4879277264,-60.4261964381,-8.4879277264,-60.4261964381,-1.78150507741,-120.642101751),('Crossfield, Alberta',1928,'Wabamun','Devonian','Upper Devonian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,369,1,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','4','Others','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',917,0,'Famennian patch reef complex.\n150 km length, 3-5 km wide.\nLabechiid stromatopores, algae, gastropods.\nOther references in 917.',51,-114,240987,-4531957,'Canada','North America',121,'',51.8333,-114.1667,'','',-10.4021177389,-52.9334909505,-10.4021177389,-52.9334909505,3.14375898861,-111.456078697),('Crossfield II, Alberta',1929,'Wabamun','Devonian','Upper Devonian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,369,1,1,'Seismic data available ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150','1928',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','4','Others','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',917,0,'See reef 1928 for remarks.',50,-113,97824,-4617126,'Canada','North America',121,'',50.5833,-113.6667,'','',-11.1820322446,-53.9778040212,-11.1820322446,-53.9778040212,2.01047214805,-112.070111215),('Willow Creek, Drumheller, Alberta',1930,'','Cretaceous','Upper Cretaceous','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,68,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','4',NULL,NULL,NULL,'4','More than 1000 m',NULL,'4',NULL,2,'Cold - water',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1151,0,'Oyster reef (biostrome).\nUp to 4 m thick, 4 km wide?\nUnbored and bored oysters\nEstuarine or barrier lagoon.\nOther refs. in ref. 1151.',51,-112,7530391,-6359882,'Canada','North America',121,'',51.5,-112.6667,'','',57.8366403488,-83.7108618835,57.8366403488,-83.7108618835,58.7411728127,-89.9911938864),('Merrill Ranch, Monarch, Alberta',1931,'','Cretaceous','Upper Cretaceous','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,76,1,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,2,'Cold - water',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1151,0,'Lagoonal intertidal setting.\nUp to 4.5 m thick oyster biostrome.\nAdditionally arenaceous forams.\nUnbored!\n',49,-113,7358350,-6657857,'Canada','North America',121,'',49.75,-113.1667,'','',54.9431736151,-81.1939878196,54.9431736151,-81.1939878196,57.0347431384,-85.7279846624),('Milk River, Alberta',1932,'Foremost','Cretaceous','Upper Cretaceous','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,79,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,2,'Cold - water',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1151,0,'Oyster reef\nBack barrier lagoonal setting.\n0.6 -1.3 m thick.',49,-112,7276262,-6671001,'Canada','North America',121,'',49.1667,-112.0833,'','',54.210291147,-80.2505241972,54.210291147,-80.2505241972,56.3193865839,-84.6911660257),('Logan Co., North Dakota',1933,'Fox Hills','Cretaceous','Upper Cretaceous','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,68,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'80',NULL,2,'Cold - water',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1152,1151,'Only locality 5 of ref. 1152 with in situ oysters.\n3 oyster species.\nPlenty of Cliona borings.',46,-99,6705084,-6192999,'United States','North America',101,'',46.2833,-99.6667,'','',50.609335501,-71.8411891442,50.609335501,-71.8411891442,52.045665474,-76.8573004164),('Kemmerer, Wyoming',1934,'Frontier','Cretaceous','Lower Cretaceous','Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,2,'Cold - water',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1153,1151,'Salt marsh or estuarine.\n2 oyster species.\n0.5 m thick.',41,-110,4757492,-6256112,'United States','North America',101,'',41.8333,-110.5,'','',41.7450299969,-62.0803533086,41.7450299969,-62.0803533086,43.6096235547,-68.5154409592),('Green Island Inlier',1935,'','Cretaceous','Upper Cretaceous','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,68,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1154,1155,'Extreme marginal setting.\nbrackish water indicated by other macrofauna, lignite seams.\nRudists accompanied by dasycladaceans and ostracods.\nAll Campanian-Maastrichtian rudist frameworks are more coppices and thickets rather than biostromes or reefs.',18,-78,2577302,-7980016,'Jamaica','North America',222,'',18.3333,-78.2833,'','',18.6189178203,-70.5820798703,18.6189178203,-70.5820798703,20.1227470792,-73.5200006834),('Maldon Inlier',1936,'Guinea Corn','Cretaceous','Upper Cretaceous','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,68,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1155,1154,'Coral reef overlain by 15.6feet of clay-shale; overlain by small rudist biostrome; overlain by 4feet of whitish beds; overlain by small rudist biostromes 5.2feet thick; overlain by 32 inches of low relief, reefal beds of rudists; overlain by 30 feet of soft (siliciclastic) beds; overlain by rudist biostromes\n\n\n',18,-77,2564730,-7931623,'Jamaica','North America',222,'',18.3,-77.8,'WAHR','66456',18.4484925801,-70.1314206564,18.4484925801,-70.1314206564,19.9759161748,-73.0559183861),('Central Inlier',1937,'','Cretaceous','Upper Cretaceous','upper Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,84,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1154,1155,'late Santonian to Maastrichtian rudist frameworks.\nSee reef 1935 for remarks.\nPatch reef with low mounds of radiolitid clusters that were successively overlain by 0.5 m of cobbly limestones with abundant corals, a thin, reddish soil, 0.5m of in-situ rudists, another reddish soil zone, and a highly fragmented zone with radiolitid rudist fragments followed by a small diversity of rudists.\n',18,-77,1634809,-7080247,'Jamaica','North America',222,'',18.0333,-77.25,'','',12.8814361537,-64.4315142852,12.8814361537,-64.4315142852,15.4667861044,-68.1155161745),('Benbow Inlier',1938,'','Cretaceous','Lower Cretaceous','Barremian-Aptian',113.00,129.40,23,'late Valanginian - early Aptian',126,125,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1154,1155,'Only clusters of rudists with a few corals.\nJubilee Limestone.\nCaprotinid biostromes. Some microbial crusts.',18,-77,-751032,-6265940,'Jamaica','North America',222,'1159',18.2667,-77.0333,'','',3.03166557066,-48.8343952641,3.03166557066,-48.8343952641,5.29456535835,-54.2822088331),('San Polo, Matese',1939,'','Cretaceous','Upper Cretaceous','upper Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,95,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'8',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','1','Corals','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'40','50','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1156,1164,'Rudist-coral-red algal patch reefs at platform edge.',41,14,3194867,1439515,'Italy','Europe',344,'',41.4556,14.5083,'WAHR','74197',28.9814976307,13.279165654,28.9814976307,13.279165654,24.6331146242,16.7828178706),('Monte Girifalco, Mt. Carseolani',1940,'','Cretaceous','Upper Cretaceous','Santonian-Campanian',72.10,86.30,25,'late Cenomanian - early Campanian',91,83,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','3',NULL,NULL,NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1157,0,'Upper Santonian-Campanian.\n3-4 m thick sequence of dolomites with radiolitid banks (inter-supratidal).\n8 rudist species.',42,13,3299266,1361507,'Italy','Europe',344,'',42.0167,13.3833,'WAHR','67601',32.0018437726,10.9408378907,32.0018437726,10.9408378907,31.1597756641,14.7603887597),('Ricetto, Mt. Carseolani',1941,'','Cretaceous','Upper Cretaceous','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,'2','10 - 100 m',NULL,'30','1940',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1157,1173,'4-5 m thick biostrome.\nHippurites (3 species) and corals.',42,13,3339669,1337867,'Italy','Europe',344,'',42.25,13.0167,'WAHR','67594',32.8645448231,14.6050856425,32.8645448231,14.6050856425,29.7392951379,15.1406373688),('Monte Grisa, Triest',1942,'','Cretaceous','Upper Cretaceous','Santonian-Campanian',72.10,86.30,25,'late Cenomanian - early Campanian',91,83,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1158,0,'Although 11 rudist species in area (mostly radiolitits) buildups consist of monospecific assemblages (e.g. Katzeria hercegovinaensis).',45,13,3750472,1494833,'Italy','Europe',344,'',45.7,13.7333,'WAHR','34707',35.5969811615,16.7335680315,35.5969811615,16.7335680315,34.5713375226,16.4411015052),('Khenchela',1943,'','Cretaceous','Upper Cretaceous','Santonian-Campanian',72.10,86.30,25,'late Cenomanian - early Campanian',91,83,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species','6','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','1','Less than 30% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1166,1780,'Late Santonian to early Campanian.\nVaccinites bioconstructions.\n5 species described (+ 1 ssp.)',35,7,2555891,724755,'Algeria','Africa',706,'',35.4167,7.0833,'WAHR','34709',25.5117110617,8.49489013187,25.5117110617,8.49489013187,26.2484226343,6.339419701),('Barrio Barrancas, Puerto Rico',1944,'','Cretaceous','Lower Cretaceous','middle Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,107,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','10',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species','1','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1155,0,'Monospecific Caprinuloidea bank.\n10 m thick.\n',18,-66,-939333,-5971739,'United States','North America',101,'',18.1833,-66.3167,'','',-3.57044233641,-49.8425871173,-3.57044233641,-49.8425871173,-1.55806543769,-55.6006791544),('Pointe-à-Pierre, Trinidad',1945,'','Cretaceous','Lower Cretaceous','upper Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,113,2,0,'Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','5','Rudists','5','Rudists',NULL,NULL,NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1155,0,'Exotic flysch block.',10,-61,44612,-3630126,'Trinidad and Tobago','North America',201,'',10.3167,-61.45,'','',5.12536396364,-23.9684367403,5.12536396364,-23.9684367403,8.37662209818,-29.714190508),('Lambs River, Marchmont Inlier',1946,'','Cretaceous','Upper Cretaceous','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,68,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','4','Stromatoporoids','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,'50','40','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1155,0,'Mature coppice phase of Type B (ref. 1155) rudist framework evolution.\nStromatoporoid heads, Titanosarcolites, Biradiolites, Plagioptychus, Radiolites,Torreites  & Antillocaprina rudists, various oysters, Brachiodonte (bivalve), algae\n',18,-77,2555031,-7943876,'Jamaica','North America',222,'',18.2167,-77.8833,'','',18.3929857343,-70.2374289826,18.3929857343,-70.2374289826,19.9150102692,-73.1595355329),('Grünbach, Niederösterreich',1947,'','Cretaceous','Upper Cretaceous','upper Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,84,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','3','Microbes','47','Bivalves (mostly oysters) - algae (microbes)',NULL,NULL,'45','55','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1159,0,'Dendriform Hippurites-Bioherms.\n1- 2 m in diameter and thickness.\nSome microbial crusts around rudists.\nCliona and microbe borings.',47,16,3951096,1729806,'Austria','Europe',301,'',47.8194,16.0111,'','',40.5756533055,17.4437202629,40.5756533055,17.4437202629,37.2669213697,16.2921090781),('Tres Lagunas, Patagonia',1948,'Cotidiano','Cretaceous','Lower Cretaceous','Berriasian-Valanginian',132.90,145.00,22,'late Tithonian - early Valanginian',141,140,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,1,'Temperate',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'20','80','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild','2','Intensive','2','Intensive',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1160,1245,'Thick branching corals and bivalves (Gryphea, Ostrea).',-44,-70,-7037781,-2129296,'Argentina','South America',201,'',-44.8333,-70.8333,'','',-51.9315981219,-36.3479183632,-51.9315981219,-36.3479183632,-47.4036240492,-37.6260792543),('Lago Fontana, Patagonia',1949,'Cotidiano','Jurassic','Upper Jurassic','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,147,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','80','20',0,'no',0,'no','2','6 to 24 reef building species','7','1','Constructor guild','2','Intensive','2','Intensive',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1160,1245,'Coral assemblage in olistostrome member of Vallcarga Fm.\n36 genera belonging to 2 orders and 9 suborders. Few reef building genera:\nE.g.\nActinastraea\nAstraraea\nHolocoenia\nFungiastraea\n\nColonial forms predominate but mostly of small size (less than 10 cm).\nLarge borings evident on plates',-44,-71,-7055151,-2185032,'Argentina','South America',201,'',-44.85,-71.5,'','',-52.5910045483,-37.6236861851,-52.5910045483,-37.6236861851,-48.2823925314,-36.4366967524),('Oberstdorf',1950,'Schrattenkalk','Cretaceous','Lower Cretaceous','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,123,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','4',NULL,NULL,NULL,'2','10 - 100 m','50','5',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'5','75','20',0,'no',0,'no','3','25 or more reef building species','32','1','Constructor guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1159,1492,'Coral-stromatopore bioherms in Schrattenkalk\n(up to 4 m thickness and 50 m width).\nBasement are rudist (requienid) limestones.\nRef. 1159\nChaetetids, stromatopores, and other sclerosponges.\n4 coral species, microbial crusts, corallinacean crusts.\n\nAccording to ref. 1514 thirty coral species present. 98 % colonial forms.\nHigh debris, very rare in situ framestones.',47,10,4447583,912618,'Germany','Europe',331,'1514',47.4167,10.2167,'WAHR','25535',35.139913271,23.2632792635,34.2880647984,23.8196188545,37.704680398,21.8000168874),('Fenoliga, Istria',1951,'','Cretaceous','Upper Cretaceous','Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,93,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','3','Microbes','47','Bivalves (mostly oysters) - algae (microbes)',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1159,1214,'Classified as paucispecific, simple, dendriform\nradiolitid-biostromes by ref. 1159.\nSeveral biostromes, less than 1 m thick.\nSome microbes as binders.',44,13,3629135,1482390,'Croatia','Europe',308,'',44.7667,13.9069,'WAHR','24021',34.072412316,18.1864756777,34.072412316,18.1864756777,29.6006051769,17.5737893374),('Atzlgraben, Brandenberg',1952,'','Cretaceous','Upper Cretaceous','lower Coniacian',86.30,89.80,25,'late Cenomanian - early Campanian',91,88,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15',NULL,NULL,NULL,'3','More than 100 m',NULL,'2',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)','1','Red algae','10','70','20',0,'no',0,'no','3','25 or more reef building species','34','1','Constructor guild','1','Present','1','Present','3','Pronounced zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1956,1159,'Diverse corals (30 species), solenporacean algae, some microbes and rudists.\nMicrosolena quite important (first description from Upper Cretaceous of Alps).\nCoral-rudist-algal mounds (up to 10 m thick) capped by rudist (Vaccinites) biostromes, up to 5 m thick.',47,11,4024851,1406121,'Austria','Europe',301,'1514, 1492',47.5,11.9222,'WAHR','24265',39.2580196758,14.5811902632,39.2580196758,14.5811902632,34.6767685292,17.7389247868),('Brac',1953,'','Cretaceous','Upper Cretaceous','upper Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,95,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','4',NULL,NULL,NULL,'1','Less than 20 m','20',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','1','4','Microbial precipitation',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1159,0,'1 to 4 m thick and 2 to 20 m wide mud mounds with stromatolites and Stromatactis.',43,16,3363076,1669851,'Croatia','Europe',308,'',43.2792,16.7028,'','',30.7302633937,19.8436157978,30.7302633937,19.8436157978,25.5720624294,19.2698718214),('Cuatretonda, Valencia',1954,NULL,'Cretaceous','Upper Cretaceous','lower Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,69,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m','45',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species','5','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1161,0,'Bioherms of mostly small Pironea (3 species).\r\nOne Hippurites sp. Very few corals.\r\n1.2 m max. thickness.\r\nAround 45 m wide complex.',38,0,4335133,-119113,'Spain','Europe',304,'',38.9667,-0.3833,'WAHR','67551',32.1643924455,0.79315369847,32.1643924455,0.79315369847,35.6347627626,-0.54603616579),('La Cadiere',1955,'La Cadière d\'Azur','Cretaceous','Upper Cretaceous','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no','2','6 to 24 reef building species','7','2','Baffler guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2189,1175,'Peri-deltaic environment\nRudist baffestone buildups.\nrelatively diverse fauna of hippuritids, radiolitids and caprinids (7 species).\n',43,5,4184649,727085,'France','Europe',331,'',43.2167,5.7667,'WAHR','67011',38.6601637697,9.06005433849,38.6601637697,9.06005433849,43.2167,5.7667),('Ostuni',1956,'','Cretaceous','Upper Cretaceous','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,77,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1163,1774,'Rudist massive organogenic limestones.\nWith Favus n.gen.',40,17,3936391,1585750,'Italy','Europe',344,'',40.7333,17.55,'WAHR','74801',29.9664150534,16.1882156249,29.9664150534,16.1882156249,29.8490200107,16.7578385795),('Khashm Buwaibiyat',1957,'Aruma','Cretaceous','Upper Cretaceous','upper Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,74,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'4','More than 1000 m',NULL,'90',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species','2','2','Baffler guild','1','Present',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1165,0,'2 m thick prominent biostrome at road.\n2 rudist species dominant (Biradiolites and a new form Eodictyoptychus).\nMatrix is fine bioclastic packstone.\n',25,46,726668,4125562,'Saudi Arabia','Asia',503,'',25.1667,46.8333,'WAHR','34710',8.76968531664,41.6975761424,8.76968531664,41.6975761424,8.41356447678,38.3868909292),('Khashm Tawqi',1958,'Aruma','Cretaceous','Upper Cretaceous','upper Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,74,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'4','More than 1000 m',NULL,'90','1957',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species','3','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1165,0,'see reef 1957 for remarks.',25,46,767752,4157551,'Saudi Arabia','Asia',503,'',25.4333,46.4667,'WAHR','34711',9.07814029634,41.4011031654,9.07814029634,41.4011031654,8.74008255385,38.1112063768),('Stranice',1959,'','Cretaceous','Upper Cretaceous','Campanian-Maastrichtian',66.00,83.60,26,'middle Campanian - Danian/Selandian',75,70,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present','2','Medium zonation',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1167,0,'Hippuritid bioherms (15 m thick) overlying calcarenites with corals and radiolitids.',46,15,4684830,1452863,'Slovenia','Europe',328,'',46.3667,15.4,'WAHR','74510',35.6898417602,17.7633912502,35.6898417602,17.7633912502,38.7498995737,15.6951961438),('Barranc del Racó, Bocairent',1960,NULL,'Cretaceous','Upper Cretaceous','late Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,66,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1169,0,'Rudist thicket with Hippurites, echinoids, colonial (Actinacis, Procladocora) and solitary corals in biomicritic matrix.\r\n2 m thick.',38,0,4311506,-144199,'Spain','Europe',304,'',38.7667,-0.6333,'WAHR','74557',31.9902080108,0.535807616007,31.9902080108,0.535807616007,35.4516084293,-0.804836276778),('Soria',1961,'','Cretaceous','Upper Cretaceous','Coniacian-Santonian',83.60,89.80,25,'late Cenomanian - early Campanian',91,85,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','30','10',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1170,0,'Rudist limestones in unit 4 \n(Ethelia in \'milieux récifaux\').\nUp to 5 m thick.',41,-2,3896193,73119,'Spain','Europe',304,'',41.75,-2.4333,'','',34.4354978981,2.00408068482,34.4354978981,2.00408068482,34.8194169064,0.141040791462),('Dugi Otok Island',1962,'','Cretaceous','Upper Cretaceous','latest Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,94,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1171,0,'Rudist buidlups and biostromes.\nNo description.',43,15,3480497,1565357,'Croatia','Europe',308,'',43.8833,15.2333,'','',31.8475323852,19.2587995619,31.8475323852,19.2587995619,26.5798435067,18.4965867166),('Ruvo di Puglia',1963,'','Cretaceous','Upper Cretaceous','late Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,93,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','5',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1172,0,'Patch reef with radiolitids (2 species) and caprinids (2 species).\nUp to 5 m thick.',41,16,3094473,1596548,'Italy','Europe',344,'',41.1167,16.4833,'WAHR','67617',29.4261547076,17.9901906549,29.4261547076,17.9901906549,25.2960476535,16.3755667143),('Saint-Baudille',1964,'','Jurassic','Upper Jurassic','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,152,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','100','10',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1178,0,'Bioherms with microsolenid corals.\n10-100 m width\n15-20 m thickness.',43,3,4109428,845225,'France','Europe',331,'',43.75,3.75,'','',22.9044747871,21.8553291209,22.9044747871,21.8553291209,28.376373247,22.7707906514),('Orgon',1965,'','Cretaceous','Lower Cretaceous','Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,127,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'40','60','0',0,'no',1,'yes','2','6 to 24 reef building species','14','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1179,813,'Diverse corals.\nActinastrea, tabulogyra, Dimorphocoenia, Columnastrea, Calmophyliopsis, Microsolena, ...\nAssociated are oysters and other bivalves and bryozoans.',43,5,3859892,656271,'France','Europe',331,'2575',43.7833,5.05,'WAHR','64072',28.4377509862,20.9640001771,28.4377509862,20.9640001771,32.0821574125,19.133827104),('Alcabideche',1966,'','Cretaceous','Lower Cretaceous','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,133,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'5','65','30',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1180,0,'Association fo stromatoporoids, Lithocodium aggregatum and diverse coral (thamnasteriids, astrocoenids, microsolenids, calamophylliids, stylinids).\n',38,-9,3276885,-583462,'Portugal','Europe',304,'',38.7347,-9.4194,'','',24.4526390094,5.43197614621,24.4526390094,5.43197614621,28.9998085289,1.86310983392),('Sao Juliao',1967,'','Cretaceous','Lower Cretaceous','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,123,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','3','Microbes','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species','5','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1180,0,'Like reef 1966, but not as diverse (obsolete)\nRudist bioconstruction\nBedoulian age.',38,-9,3302550,-574954,'Portugal','Europe',304,'',38.9403,-9.4083,'WAHR','67544',27.6796112742,4.88084299998,26.9895075116,5.27181067633,30.6615109829,1.12404361192),('Ponta da Rana',1968,'','Cretaceous','Lower Cretaceous','upper Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,101,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','3',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species','6','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite',NULL,'','0','',0,'No or unknown reservoir potential',1180,0,'Bioaccumulations of rudists (toucasiformes and capriniformes): 6 species.\n3 m maximum thickness.',38,-9,3492110,-480589,'Portugal','Europe',304,'',38.6722,-9.3208,'WAHR','67543',28.9270308334,0.877976468784,28.9270308334,0.877976468784,30.9327189864,-3.30238382804),('Ugolka, Carpathians',1969,'','Cretaceous','Lower Cretaceous','Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,127,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','150',NULL,NULL,NULL,'2','10 - 100 m','100','100',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','2','Algae','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','2','Green algae','5','90','5',0,'no',0,'no','3','25 or more reef building species','37','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1181,0,'Urgonian facies 2-150 m thick.\nBiomoirphic limestones with whole skeletons of corals and algae. 24 coral species. 2 chaetetid sp., 11 algal sp.\nCores 5-20 m thick and 5-10 m wide, 8-100 m long.\nUpper sublitoral.',48,23,3437851,2287012,'Ukraine','Europe',301,'',48.3333,23.5,'WAHR','67457',36.2252591334,34.1131794495,36.2252591334,34.1131794495,39.2390441319,33.3263236154),('Boljevac, Arnaut River',1970,'','Cretaceous','Lower Cretaceous','late Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,126,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species','6','2','Baffler guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1182,0,'Rudist biostromes with Toucasia, Matheronia, Monopleura and Requienia.\nVery small coral bioherms in the vicinity.',43,22,2925161,2061022,'Yugoslavia','Europe',307,'',43.9167,22.25,'WAHR','67545',31.7571131087,34.7642028699,31.7571131087,34.7642028699,34.7452188098,33.6354410557),('Mokhorotubani, Dzirul Massif',1971,'','Cretaceous','Lower Cretaceous','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,133,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'70','1971',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','90','0',0,'no',0,'no','3','25 or more reef building species','23','1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',1183,1184,'Massive organogenic limestones.\nExclusively corals (diverse)\nDolomitic.',42,43,4970230,3657834,'Georgia','Europe',301,'',42.3667,43.3167,'WAHR','67511',34.5956231464,52.2779823436,34.5956231464,52.2779823436,36.453495715,52.7125323827),('Shkmeri, Dzirul Massif',1972,'','Cretaceous','Lower Cretaceous','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,133,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','130',NULL,NULL,NULL,'3','More than 100 m',NULL,'70','1971',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','70','20',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1184,1183,'Large organogenic structure (up to 130 m) of bioherm type.\nComposed of corals and chaetetids.\nDiverse corals in spite of poor preservation.',42,43,5014288,3610164,'Georgia','Europe',301,'',42.7167,43.0167,'WAHR','67510',34.8307072848,51.8634841197,34.8307072848,51.8634841197,36.720629963,52.3187086745),('Ali-Goresha area, Dzirul Massif',1973,'','Cretaceous','Lower Cretaceous','early Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,128,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','10',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','5','Rudists','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'10','90','0',0,'no',0,'no','3','25 or more reef building species','29','1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1184,0,'Coral-rudist biostromes of 4-10 m thickness.\nCorals dominant and very diverse.\nRudists mostly requienids and diceratids.',42,43,4967386,3705674,'Georgia','Europe',301,'',42.0833,43.65,'WAHR','67512',35.323065895,53.1556841707,35.323065895,53.1556841707,37.1664691742,52.8503830909),('Manistee County, Michigan',1974,'','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,1,'Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1600','1875',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1185,0,'',44,-86,-3024961,-5096370,'United States','North America',101,'',44.2167,-86.3167,'','',-26.3021918645,-97.9722266225,-26.4261735354,-94.7908599908,-26.4261735354,-94.7908599908),('Barre de la Jaume, Var',1975,'','Cretaceous','Upper Cretaceous','Coniacian',86.30,89.80,25,'late Cenomanian - early Campanian',91,87,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','5','Rudists','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'20','50','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1188,0,'Rudist-coral communities on palaeohigh.\nSmall chaetetid bioherms at base. Surrounded by bioclastic limestones.',43,5,4176009,732163,'France','Europe',331,'',43.15,5.8222,'','',38.3485660798,9.67924560087,38.3485660798,9.67924560087,43.15,5.8222),('Barres de Cuers',1976,'','Jurassic','Middle Jurassic','middle Bathonian',166.10,168.30,20,'middle Aalenian - middle Bathonian',166,166,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','4',NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1189,0,'Small coral bioherms in first limestone formation.\nBryozoans and bivalves associates.\nUp to 4 m thick.',43,6,4113394,1342871,'France','Europe',331,'',43.2667,6.0278,'','',21.9667656694,26.8343834361,21.9667656694,26.8343834361,43.2667,6.0278),('Jebel Ouenza',1977,'','Cretaceous','Lower Cretaceous','upper Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,113,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','13',NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','80','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite',NULL,'','0','',0,'No or unknown reservoir potential',1190,0,'Gargansian stage\ncoral biostromes.\nWith calcisponges (chaetetids?)\nUp to 13 m thick.',35,8,2286364,862402,'Algeria','Africa',706,'',35.95,8.0833,'','',17.198207138,16.8725846301,17.198207138,16.8725846301,20.4107733179,11.9258481084),('Murchas',1978,'','Neogene','Miocene','late Langhian',13.80,14.80,31,'Burdigalian - Serravallian',14,14,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','4',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','1','Corals','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'80','20','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1191,0,'Coral-oyster patch reefs.\nUpt to 3-4 m thick and 18 m wide.\nSiliciclastic ramp setting.\nCorals are Heliastrea, Porites, Tarbellastrea, Mussismilia.\nOyster Hyotissa squarrosa up to 70 % of the reef.\nRare encrusters. Some rhodolites.\n10 % is sparry calcite.',36,-3,4891414,-504231,'Spain','Europe',304,'',36.9333,-3.55,'WAHR','69779',35.3162773301,-5.03917078029,35.3162773301,-5.03917078029,36.3402029167,-3.81383198856),('Sebaa Chioukh Hills, Orania',1979,'','Neogene','Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,6,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m','1000','14',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','5','65','30',0,'no',0,'no','2','6 to 24 reef building species','7','1','Constructor guild',NULL,'',NULL,'',NULL,'','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1196,2584,'6 coral species.\nFauna dominated by Tarbellastrea and Porites.\nSeveral bryozoans',35,-1,4673547,-190024,'Algeria','Africa',706,'',35.1833,-1.3333,'WAHR','69864',34.3498565483,-2.1648017844,34.3478684404,-2.1667778081,34.6257980338,-1.25434863268),('Traras, Orania',1980,'','Neogene','Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,6,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'12','1979',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1196,2584,'More marls and more finger colonies of Porites than in reef 1979.',35,-1,4678012,-209525,'Algeria','Africa',706,'',35.2167,-1.5333,'WAHR','70785',34.3834583175,-2.36274129549,34.3814707386,-2.36471249128,34.6631314671,-1.45196190614),('Ofaqim II',1981,'Ziqlag','Neogene','Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','12',NULL,NULL,NULL,'3','More than 100 m','150','7',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','5','70','25',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1201,0,'12 m thickness. 100-150 m width.\nMassive faviid corals dominant.\nOthers are stylophorids and poritids.\n40-80 % of reefs are coral. Other are corraline algae and encrusting forams. Rare bryozoans.',31,34,3961134,3319264,'Israel','Asia',508,'',31.3167,34.6167,'WAHR','69908',29.4093686504,31.9663026863,29.4069502185,31.9636682307,27.1958862797,33.1735768223),('Wadi Sharm el Qibli',1982,'Rudeis','Neogene','Miocene','Burdigalian-Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,16,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m',NULL,'400','685',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',1,'Potential reservoir',1202,2440,'Massive and branching corals: Stylophora, Tarbellastraea, Montastrea.\nSomewhat protected. Reef slopes with abundant siliceous debris rich in molluscs and coralline algae.\nLoc. Wadi Sharm el Bahari very close.',25,34,3299690,3458414,'Egypt','Africa',715,'',25.5,34.65,'','',23.3173311192,31.8103546841,23.3173311192,31.8103546841,22.5413421038,33.4678975572),('Sharm el Luli',1983,'','Neogene','Miocene','Burdigalian/Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,16,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','75',NULL,NULL,NULL,'2','10 - 100 m',NULL,'400','685',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1202,0,'Three individual prograding reef bodies.\nEach some 25 m thick.\n',24,35,3206557,3507747,'Egypt','Africa',715,'',24.8,35.0167,'WAHR','50927',22.6234489039,32.1845692303,22.6234489039,32.1845692303,21.8315891178,33.8032629102);
INSERT INTO `reefstest` VALUES ('Belus-Peyrehorade',1984,'','Paleogene','Oligocene','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,27,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'20','80','0',0,'no',0,'no','3','25 or more reef building species','60','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1203,2176,'60 coral species.\nLocally Delicate, globular and lamellar morphologies.\nMostly big and massive branched and domal.\n\n',43,-1,5582777,-349745,'France','Europe',331,'',43.5667,-1.1167,'WAHR','70067',41.2225678043,-5.07042487181,41.2225678043,-5.07042487181,42.4779890136,-1.24784546622),('Abese-Estoti + Escornebeou, Aquitain',1985,'','Paleogene','Oligocene','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,27,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,'3','More than 100 m',NULL,'20','1984',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','63','Corals - hydrozoans',NULL,NULL,'5','80','15',0,'no',0,'no','3','25 or more reef building species','82','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1203,2176,'Up to 100 coral species.\n50 massive globular species, 15 branched 10 phaceloid, 6 lamellar.\n3 m thick patch reefs, traceable for 200 m.\nAssociated with hydrozoans. Algae very rare.\nCarbonate ramp.\n\nLe Bois (Escornebeou) locality further west is subreefal envrionment with massive corals (about 25 species in 18 genera).',43,-1,5605228,-343138,'France','Europe',331,'',43.75,-1.05,'WAHR','22968',41.4077942162,-5.01685945573,41.4077942162,-5.01685945573,42.6595261563,-1.17382485155),('Gamachot near Villandraut, Bazadais, Gironde',1986,'','Neogene','Miocene','middle Aquitanian',21.00,22.00,30,'Chattian - Aquitanian',22,22,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1203,2578,'In-place Porites colonizing marls.\nCoral carpet on muddy substrate.\n1 m thick bank interrupted by brackish deposits.\n',44,0,5692850,-279760,'France','Europe',331,'',44.4667,-0.3667,'WAHR','70074',42.464736309,-4.06786142842,42.464736309,-4.06786142842,43.5097195187,-0.523578690392),('St. Martin-d\'Oney',1987,'','Neogene','Miocene','late Aquitanian',22.00,23.00,30,'Chattian - Aquitanian',22,20,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','63','Corals - hydrozoans',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite',NULL,'','0','',0,'No or unknown reservoir potential',1203,0,'Rich coral fauna.\nAdditionally millporids and molluscs.',43,0,5621592,-312735,'France','Europe',331,'',43.8833,-0.7167,'','',41.7940411129,-4.45688414494,41.7940411129,-4.45688414494,42.8990610028,-0.880652737946),('Le Peloua',1988,'','Neogene','Miocene','lower Burdigalian',17.50,20.40,31,'Burdigalian - Serravallian',14,19,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','50','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1203,0,'50 coral species.\nCoral colonies up to 1 m in diameter.\nSmall fringing reefs.',44,0,5844156,-211078,'France','Europe',331,'',44.6333,-0.65,'WAHR','70191',42.5307823781,-4.44709499186,42.8561838229,-4.0501522254,43.7923964771,-0.791404922491),('Ales-Villagreca, Sardegna',1989,'','Neogene','Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,22,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','25',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1204,0,'25 m thick coral bioherms with bryozoans and coralline algae.\nUnderlain by siliciclastic rocks.',39,9,5462227,100141,'Italy','Europe',344,'',39.45,9,'WAHR','85110',38.0039499647,3.07852994147,38.0039499647,3.07852994147,38.5551613716,7.60021602442),('Capo Tindari, Sicily',1990,'','Neogene','Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,22,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1204,0,'Fragmentary coral reef material.\nReef grown on metamorphic basement.',38,15,4749538,1247144,'Italy','Europe',344,'',38.1167,15.0833,'','',35.0644199659,11.4478879211,35.0644199659,11.4478879211,35.0220448533,15.017475347),('Jabal al Akhdar',1991,'','Neogene','Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,22,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite',NULL,'','0','',0,'No or unknown reservoir potential',1204,0,'Reefs with abundant branching corals in recrystallized micritic groundmass.\nAssociated with coralline algal carbonates.',32,21,4002026,1867618,'Libya','Africa',715,'',32.45,21.0667,'','',29.395239396,17.8189730598,29.395239396,17.8189730598,29.2719697833,20.3620058039),('Bonifacio Basin, Corsica',1992,'','Neogene','Miocene','Burdigalian-Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,16,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1204,1739,'Coral-red algal reefs.\nExtensive development of bioherms in Bonifacio Basin.\nFour coral reef episodes.\nlate Aquitanian to Langhian.',41,9,5619599,442078,'France','Europe',331,'',41.4167,9.1667,'','',40.0749134823,5.74985768137,40.0749134823,5.74985768137,40.4326496109,8.7803082752),('Aleria, Corsica',1993,'','Neogene','Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,3,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1204,0,'Coral-algal bioherms with pectinids and echinoids.',42,9,5601888,531645,'France','Europe',331,'',42.1,9.5,'','',40.9907604494,6.6805158274,40.9893146234,6.67783254734,41.2515150728,9.22010698977),('Palmi, Rocca Campana, Calabria',1994,'','Neogene','Miocene','late Tortonian',7.30,9.00,32,'Tortonian - Gelasian',6,8,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','9',NULL,NULL,NULL,'3','More than 100 m',NULL,'40',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild',NULL,'',NULL,'','2','Medium zonation',NULL,'','2','30-60% micrite',NULL,'','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',1205,1204,'Seven coral species in area but only Tarbellastraea and Porites common',38,15,5061301,1460656,'Italy','Europe',344,'2578',38.3833,15.8667,'WAHR','70492',36.0800505491,11.2328887169,36.3880592003,11.9870601148,37.8781611326,15.6789484398),('Central Mallorca',1995,'','Neogene','Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,22,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','12','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,'','2','Algae','2','Algae','29','Coralline algae only (some corals)','1','Red algae','0','0','100',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite',NULL,'','0','',0,'No or unknown reservoir potential',1206,0,'Position doubtful.\nRed algal mounds (12 m thick, tens of m wide).',39,2,5230007,-93077,'Spain','Europe',304,'',39.6667,2.75,'','',38.7528844687,-2.21384650911,38.7528844687,-2.21384650911,38.6257514096,2.31692859409),('Serra de Tramuntana, NW Mallorca',1996,'Sant Elm','Neogene','Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,22,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','16',NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','60','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1206,0,'Up to 16 m thick reefs in medium- to coarse-grained terrigenous fans. One reef (coll. 69929) without terrigenous influx.\nPorites dominates coral fauna. Massive and encrusting corals dominant.\nRed algae abundant.\nMatrix wackestones with coral fragments, serpulids, bryozoans and oysters.',39,3,5258741,-79848,'Spain','Europe',304,'',39.8333,3,'WAHR','69927',38.986912432,-2.08584853375,38.986912432,-2.08584853375,38.7879044816,2.5680659563),('Lisboa',1997,'','Neogene','Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,22,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','50',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','11',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1206,1203,'Less than 50 m thick coral reef (11 species).',38,-9,4979815,-1133086,'Portugal','Europe',304,'1645, 1647',38.6833,-9.2667,'WAHR','92102',36.4516369023,-12.4555574985,36.4516369023,-12.4555574985,37.8759845178,-9.57238679888),('Alacant region',1998,'','Neogene','Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,22,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','60',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','5','65','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1206,0,'40-60 m thick reefs with abundant grainstones and rudstones with red-algae, corals, larger forams, bivalves and miliolids.',38,0,4928061,-319517,'Spain','Europe',304,'',38.25,-0.6667,'','',35.7234000349,-3.13133325409,35.7234000349,-3.13133325409,37.2715773006,-1.09335375752),('Penedés, Barcelona',1999,'','Neogene','Miocene','Burdigalian-Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,16,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m',NULL,'7',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','20','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1633,1206,'24 coral species in total (4 ahermatypic).\nPorites dominant. Other corals are Heliastrea, Tarbellastaea, Mussidae, Faviidae.\nFringing reefs up to 50 m thick and 3-7 km long with well developed prograding reef slopes.\nLarge reef with greatest diversity (12-16 species).',41,1,5439809,596656,'Spain','Europe',304,'1855',41.3167,1.75,'WAHR','70411',39.7963718264,-1.26078328401,39.7963718264,-1.26078328401,40.4661213106,1.46488232356),('Guercif',2000,'','Neogene','Miocene','late Tortonian',7.30,9.00,32,'Tortonian - Gelasian',6,8,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','10',NULL,NULL,NULL,'1','Less than 20 m',NULL,'200',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1206,1195,'Coral reefs up to 10 m, but only 2-4 m thick in average.\nPorites and Tarbellastrea dominate.',34,-3,4548125,-381884,'Morocco','Africa',714,'',34.1833,-3.25,'','',32.9367972005,-4.4697092484,33.1058263623,-4.30492885279,33.5114885932,-3.17192223841),('Zevardi well',2001,'Urtabulak','Jurassic','Upper Jurassic','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,156,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'160','974',0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','70','20',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','1','Present',2,'Actual reservoir',672,2836,'',39,64,5393629,5915464,'Uzbekistan','Asia',301,'',39,64.75,'WAHR','91782',36.8096332666,72.7620156159,36.8096332666,72.7620156159,39.7981366972,77.5984424699),('Cansiglio Platform',2002,'','Cretaceous','Lower Cretaceous','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,123,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','3','Microbes','47','Bivalves (mostly oysters) - algae (microbes)',NULL,NULL,'30','70','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1210,0,'Caprinid patch reef about 1.5 m thick.\nFramework of caprinids with Bacinella and Lithocodium.',46,12,3579755,1303931,'Italy','Europe',344,'',46.0167,12.4167,'WAHR','67614',24.8166335917,28.3346332847,23.4914343221,29.053074067,25.5270319199,23.3471098109),('Cebu City, Cebu',2003,'','Cretaceous','Lower Cretaceous','Barremian-Aptian',113.00,129.40,23,'late Valanginian - early Aptian',126,125,1,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1211,0,'Rudist limestones with Amphitriscoelus.',10,123,1226481,15786090,'Philippines','Asia',563,'',10.4,123.8917,'WAHR','74165',10.4,123.8917,NULL,NULL,-26.3545615596,138.674691453),('Bespelj, Bosnia',2004,'','Cretaceous','Upper Cretaceous','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','5','Rudists','4','Stromatoporoids','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,'40','50','10',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1212,0,'Reworked rudist reef (5 rudist species and 1 hydrozoa).\n',44,17,3491016,1745490,'Bosnia and Herzegovina','Europe',328,'',44.4167,17.2833,'','',32.9411505327,19.284226993,32.9411505327,19.284226993,31.5074794275,20.3596514279),('Kudirkos-Naumestis',2005,'','Permian','Upper Permian','Zechstein',252.20,254.10,16,'Roadian - Changhsingian',261,259,2,1,'Seismic data available ',3,'Mud mound or bank',NULL,NULL,'70',NULL,NULL,NULL,NULL,NULL,NULL,'50','306',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite',NULL,'','1','Present',2,'Actual reservoir',1208,0,'60-70 m thick reefs, distinctly asymmetric. \nOnly core samples available.\nCyanobacteria and Fenestella, Acanthocladia (bryozoans).\n',54,22,3005446,3074329,'Lithuania','Europe',301,'',54.7667,22.8833,'','',32.6256481471,37.20503011,32.6290778508,37.205720138,30.6887332934,30.4757334339),('S-Bakony',2006,'','Cretaceous','Lower Cretaceous','upper Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,101,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','25',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1213,0,'Biostromes, bioherms and small patch reefs.\nSeperate structures reach up to 20-25 m thickness. \nRudists rarely in growth position.',47,17,3477266,1929367,'Hungary','Europe',336,'',47,17.75,'','',34.208239335,25.4732734516,34.208239335,25.4732734516,31.1552759037,21.5864430258),('Ereño',2007,'','Cretaceous','Lower Cretaceous','Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,115,1,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1215,0,'Only thickets and patches in area.\nMaximum thickness of reefal limestone 1.7 m.\n',43,-2,3879600,243787,'Spain','Europe',304,'',43.3667,-2.65,'','',29.2529353597,12.3380047967,29.2529353597,12.3380047967,33.3208994778,8.01547432252),('Akerbouss',2008,'','Cretaceous','Upper Cretaceous','upper Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,95,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','21',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','5','Rudists','4','Stromatoporoids','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,'40','50','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1216,0,'21 m of reefal limestones with rudists, stromatopores, dasycladales and bryozoans.',31,-4,2477689,-416273,'Morocco','Africa',714,'',31.8,-4.2167,'WAHR','67619',23.0440625819,-0.504202400426,23.0440625819,-0.504202400426,21.5735003876,-4.03229417661),('Epidauros',2009,'','Cretaceous','Upper Cretaceous','upper Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,95,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1217,0,'Radiolitid banks overlain by caprinid banks.\nMostly floatstone texturs.',37,23,2462297,2093944,'Greece','Europe',338,'',37.6167,23.15,'WAHR','74198',23.2959145603,20.844429703,23.2959145603,20.844429703,20.1467629662,20.6627077939),('Parandaz Mt.',2010,'','Cretaceous','Upper Cretaceous','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,93,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1218,0,'Rudist limestones with Biradiolites and Eoradiolites.',34,68,2145101,7744570,'Afghanistan','Asia',301,'',34.9167,68.9167,'WAHR','74217',37.7660492383,73.6844365237,37.7660492383,73.6844365237,33.8503772511,69.031827029),('Abu Roash, Cairo',2011,'','Cretaceous','Upper Cretaceous','early Coniacian',86.30,89.80,25,'late Cenomanian - early Campanian',91,88,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','10',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','5','Rudists','1','Corals','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'45','55','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1218,1349,'Rudist dominated biostrome on top of Actaeonella series. Almost 10 m thick.\nRadiolitid Durania arnaudi is dominant. Abundant Ceriopora multiformis are also present.\nAge revised by ref. 1349.\nVery close is milleporid mound of small size.\n\n',30,31,1271395,2856821,'Egypt','Africa',715,'',30.0125,31.075,'WAHR','24082',16.0421672053,29.6831714384,16.0421672053,29.6831714384,14.001465414,26.0150222604),('Kiya River Section, Siberia',2012,'Ust\'kundat-Usa','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,519,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','16',NULL,NULL,NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','134','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1222,1220,'Extremely diverse archaeocyaths.\nDiverse and well preserved calcibionts (Renalcis, Epiphyton, Chabakovia and others).\nBioherms mentioned throughout the section, but not described in detail.\nShould be another plate, but was not rotated.',55,88,-3175833,2053034,'Russia','Asia',624,'1221',55.5167,88.0167,'WAHR','56741',-2.62217101696,-46.4680262626,-2.62217101696,-46.4680262626,-2.62217101696,-46.4680262626),('Abitibi R., Hudson Bay Lowl., Ontario',2013,'Kwatraboahegan','Devonian','Middle Devonian','Emsian-Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,397,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species','37','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1227,1228,'Upper Emsian-early Eifelian\n\'Reefoid\' rocks.\n12 species of stromatopores.\n8 solitary and 9 colonial species of rugose corals\n8 species of tabulate corals.',51,-81,-4074932,-2590802,'Canada','North America',121,'1224',51,-81,'WAHR','40039',-23.4809727445,-51.0205259049,-23.4809727445,-51.0205259049,-14.9848786038,-105.160503621),('Mormon Gap, Utah',2014,'','Carboniferous','Upper Carboniferous','Desmoinesian',307.00,315.20,13,'Bashkirian - Kasimovian',302,307,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'4','More than 1000 m',NULL,'25',NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','12','Foraminifera','38','Palaeoaplysina - corals - tubular forams - bryozoans','2','Green algae','20','70','10',0,'no',0,'no','1','Less than 6 reef building species','5',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1230,0,'Oldest occurrence of Palaeoaplysina.\n2 m thick laterally continuous biostromes\nPalaeoaplysina plates encrusted by tubular forams. Some rugose corals, brachiopods, fenestrate bryozoans and Komia.\n',38,-113,1058625,-4597157,'United States','North America',101,'',38.7333,-113.9333,'WAHR','63144',3.08297469472,-41.9584363938,3.08297469472,-41.9584363938,5.80960476841,-63.2846932587),('Sudak, Crimea',2015,'','Jurassic','Middle/Upper Jurassic','Callovian-Oxfordian',157.30,166.10,21,'late Bathonian - early Tithonian',151,161,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','60',NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1231,1529,'Corals, solenoporaceans (including rodolites), calcareous sponges. Sometimes associated microbes.\nBioherms around 50-60 m thick.\n\nReef growth limited to upper Callovian - lower Oxfordian according to ref. 1529.\nAbstract of ref. 1529.\nRich and various crinoidal assemblages existed at Callovian-Oxfordian time in the Sudak environs on Crimea. 22 species are described: Dolichocrinus aberrans, Eugeniacrinitescaryophilites, E. quenstedti, Pilocrinus moussoni, Cyrtocrinus nutans (order Cyrtocrinida), Millericrinus annulatus, M. convexus, M. echinatus, M. etalloni, M. goupilianus, M. granulosus, M. knorri, M. milleri, M. multipunctatus, M. rotiformis, M. thiollieri (order Millericrinida), Balanocrinus dumortieri, B. subteres, Margocrinus modestus, Chariocrinus? burgundicus, Isocrinus amblyscalaris and \'Pentacrinus\' cingulatissimus (order Pentacrinida). The described species belong to two ecological  types: cirriferous (long-stalked plastic, long-stalked immovable and short-stalked forms) and cirriless (long-stalked and short-stalked). Crinoids occupied four trophic tiers and inhabited four types of the biotopes: interreef depressions, interreef rises, reef slopes and reefs. A certain connection exists between biotope types, trophic tiers of crinoids and their ecological types. Tubular worms, bryozoans, bivalves, sponges and corals were settling on crinoid stalks in a certain sequence during the lifetime of crinoids or after their perishing. Millericrinid stems were damaged by parasites, predators and scavengers. Pentacrinid stems were twisted, depending on the environmental dynamics. Atrophy of cirri is typical for tong-stalked flexible pentacrinids.',44,34,5058355,3237846,'Ukraine','Europe',301,'2814',44.8167,34.9167,'WAHR','67868',30.8649643549,46.4012153807,30.8649643549,46.4012153807,36.2803380782,49.0947960971),('Shtschebetovka, Crimea',2016,'','Jurassic','Middle/Upper Jurassic','Callovian-Oxfordian',157.30,166.10,21,'late Bathonian - early Tithonian',151,161,3,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','200',NULL,NULL,NULL,'3','More than 100 m',NULL,'50','2015',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',1231,1529,'Reef growth limited to upper Callovian - lower Oxfordian according to ref. 1529.\nReef blocks of 1-2 km2 extension and 100-200 m thickness.\nLimestones cloddy, cavernous and recrystallized. Big coral and algal nodules. Cryptobionts like crinoids common. ',44,35,5081825,3253337,'Ukraine','Europe',301,'',44.9333,35.2333,'','',31.0689783327,46.5754105743,31.0689783327,46.5754105743,36.4731620819,49.2979384469),('Fishta, N-Caucasus',2017,'','Jurassic','Upper Jurassic','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,156,3,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'600',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1231,2207,'Algae, corals, calcareous sponges.\nFisht-Shakhdag barrier reef starting here and extending to the ESE (ref. 2207).\n',43,39,5117719,3665487,'Russia','Asia',624,'2814',43.9833,39.9,'WAHR','90019',31.8736298014,50.241934941,31.8736298014,50.241934941,36.8937249046,53.3366014957),('Chegem, Caucasus',2018,'','Jurassic','Upper Jurassic','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,157,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1231,0,'More than 1000 m thick algal-coral-sponge reef.',43,43,5131034,3961559,'Russia','Asia',624,'',43.2,43.1167,'','',32.2712762523,53.1041998318,32.2712762523,53.1041998318,37.0738028885,56.4052078588),('Ardon River, Caucasus',2019,'','Jurassic','Upper Jurassic','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,156,3,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100','2018',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1231,2814,'See reef 2018.',42,44,5119495,4031287,'Russia','Asia',624,'',42.9167,44.1667,'WAHR','89999',32.3861127823,54.0624557153,32.3861127823,54.0624557153,37.1130112755,57.4293167306),('Fawn Lake, Horn Plateau, N.W.T.',2020,'Horn Plateau','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','120','3','101-1000 m wide','600','3','More than 100 m','650',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','20','1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',1233,1600,'Pinnacle reef complex.\nensensis to varcus Zone\n650 m wide - 125 m thick.\nColonial corals (rugose and tabulate) and massive and tubular stromatoporoids surrounded by sand gravel sized crinoid coral sediment. Much of the reef is composed of fragmented reef-derived debris\nSeveral algae and some microbes. Rare bryozoans.\nNot more than 10 % micrite in reef core.\n15 species or rugose corals in framework indicated by ref. 1600. Rugosa as primary frame builders.\n\nAbstract of ref. 1603:\nAgastophyllum eximium gen. et sp. nov., a massive digonphyllid coral, is described from the reef flat and organic reef macrofacies of Vopni and Lerbekmo (1972). Dialeptophyllum vopnii gen. et sp. nov., a solitary kyphophyllid coral, is described from the reef flank macrofacies. Thryptophyllum undafundus gen. et sp. nov. is described from the reef flat and reef flank macrofacies, and is referred to a new subfamily of the named Thrptophyllinae. Agastophyllum eximium and Thryptophyllum undafundus are Giventian, Middle varcus zone age; Dialeptophyllum vopnii is presumed to belong to the same zone, and is certainly Givetian. Four undescribed species of Agastophyllum are reported from late Eifelian strata of Western Canada. Dialeptophyllum vopnii and an unnamed Emsian species from the Nelichen Formation of the Indigirka River drainage area of the northeastern Soviet Union are the only known species of Dialeptophyllum. An early Givetian species from the Rockport Quarry Limestone of Michigan, originally described by Ehlers and Stumm (1949), under the name Spongophyllum romingeri, is transferred to the new genus Thryptophyllum. ',62,-117,-399176,-4080747,'Canada','North America',121,'1603',62.1667,-117.8333,'WAHR','34871',-3.11054630325,-57.9437497619,-3.11054630325,-57.9437497619,2.30354065345,-117.196160051),('Mercy Bay, Banks Island, N.W.T.',2021,'','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','30',NULL,NULL,NULL,'3','More than 100 m',NULL,'100','1456',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','3','Pronounced zonation',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1234,898,'Zonation: Lower bioherm (33 m thick) overlain by two biostrome layers (30 m thick).\n\nBioherm (from base to top): \n- 5 m Coral bindstone and bafflestone.\n-2 m stromatoporoid bindstone\n- 10 m Stromatoporoid framestone and rudstone\nStromatopores dominant in shallower water.',74,-118,641945,-3057644,'Canada','North America',121,'',74.0667,-118.3333,'','',4.42399832317,-42.3505964422,4.42399832317,-42.3505964422,14.393049829,-104.791155399),('Palisades Quarry, Linn Co., Iowa',2022,'','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','30','3','101-1000 m wide',NULL,'4','More than 1000 m','2500',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','13','Echinoderms','1','Corals','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',1235,0,'Crinoid-coelenterate mounds.\nHeavily dolomitized, asymmetrical.\n30 m thick, 2.5 km wide complexes consisting of several mounds.\n',42,-91,-2920570,-5623342,'United States','North America',101,'',42.0333,-91.7333,'','',-27.0031026134,-102.963011106,-27.2431435607,-99.7674791906,-27.2431435607,-99.7674791906),('PDB-04 research well, New Mexico',2023,'','Permian','Middle Permian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,262,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','180',NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','86',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','2','Algae','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1','Red algae','10','70','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1236,0,'Reef dolomitic. Abundant marine cements\nCapitan formation with lower slope facies and upper reef facies (about 180 m thick ).Reef growth interrupted by sandstone bed.\nBiota: Sponges, bryozoans, algae (Archaeolithoporella, algal encrustations, rare stromatolites), Tubiphytes. \nAvarage porosity about 10 % (mostly vuggy). Maximum 25 %, 2 d permeability.\n',32,-103,503697,-3648017,'United States','North America',101,'',32.5042,-103.9194,'','',11.1206067157,-29.305295593,11.1206067157,-29.305295593,5.5700695077,-36.2539393707),('Getty #1 well, Delaware Basin, New Mexico',2024,'','Permian','Middle Permian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,262,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','86',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1236,0,'',32,-103,464464,-3603147,'United States','North America',101,'',32.4333,-103.3333,'','',10.8387755006,-28.8851590828,10.8387755006,-28.8851590828,5.29077548471,-35.8379040939),('Delaware Basin margin E, Texas',2025,'','Permian','Middle Permian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,262,2,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'500','86',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1237,1236,'',31,-102,283038,-3626198,'United States','North America',101,'',31.1667,-102.8333,'','',9.51384571996,-29.0593677281,9.51384571996,-29.0593677281,3.96478535559,-36.0015024356),('Sagara district',2026,'Megami','Neogene','Miocene','early Middle Miocene',13.80,16.00,31,'Burdigalian - Serravallian',14,15,3,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1238,0,'Abstract of ref. 1238:\r\nEight fossil molluscan species, including Cryptopecten yanagawaensis (Nomura and Zinbo) and Turbo    (Marmarostoma) mekamiensis Nishiwada, are described on the basis of material obtained from the late Early to early Middle Miocene Megami and Ebie limestones in the Sagara district, Shizuoka Prefecture, Japan. Cryptopecten yanagawaensis has been recorded from late Early to early Middle Miocene formations in Japan. The occurrence of this species indicates that the reef limestones in the Megami Formation were formed within the Japanese faunal realm in Miocene time. In this paper some comments are made on the origin and sedimentary environments of the limestones in the Megami Formation. ',34,138,4974482,13078349,'Japan','Asia',625,'',34.6667,138.1667,'WAHR','70064',36.4660476652,136.628401789,36.4666139144,136.627684326,34.418211083,136.218610343),('San Juan de la Costa, Baja California',2027,'San Gregorio','Paleogene','Oligocene','Late Oligocene',23.00,28.10,30,'Chattian - Aquitanian',22,27,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,'60',NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','8','Serpulids, worms, vermetids','8','Serpulids, worms, vermetids','76','Worms only',NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species','1','1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1239,0,'Small hemispherical reef structures, up to 2.5 m in width and 1 m in height.\nFormed by Diplochaetetes (worm, not sclerosponges as previously assumed).\nCoastal environment.',24,-110,3316581,-10996663,'Mexico','North America',105,'',24.3333,-110.6667,'WAHR','34858',22.238000294,-101.64584477,22.2382109589,-101.649213168,26.3990008118,-99.9430113984),('Baixo, Porto Santo, E-Atlantic',2028,'','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','12','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1241,0,'Abstract of ref. 1241\nAn ephemeral coral reef developed on the submarine slope of the Porto Santo volcanic complex in Upper Miocene time. Systematic and biogeographical aspects of the fossil Scleractinia at this locality are discussed. ',33,-16,4418075,-1688352,'Atlantic','Atlantic',NULL,'',33.05,-16.3333,'WAHR','70666',31.9876989155,-17.2716825253,31.9876989155,-17.2716825253,33.05,-16.3333),('Havelock Island, Andaman Islands',2029,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','12','Foraminifera','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'10','60','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1242,0,'Abstract of ref. 1242:\nCarbonate rocks are widespread on the Andaman-Nicobar Islands, northern Indian ocean, ranging in age from Early  Miocene to Pleistocene. Lithologically they range from deep water to shallow water calcarenites. Thin section analysis of the limestones showed the following major lithofacies: lithic foraminiferal-algal grainstone-packstone; lithic foraminiferal-algal wackstone-mudstone; volcanoclastic packstone-wackstone/radiolarian cherts; foraminiferal packstone; coralgal boundstone and coarse lithic foraminiferal-algal-molluscan packstone-grainstone. They exhibit sequential changes in their fabrics, biogenic and clastic constituents. Depths of deposition ranged from high energy, shallow neritic (lithic foraminiferal-algal grainstone-packstone facies) at the beginning of Early Miocene to progressively lower bathyal marked successfully by lithic foraminiferal-algal wackstone-mudstone, volcanoclastic packstone-wackstone and radiolarian chert facies. The sudden influx of glass shards and tephras in the later Early Miocene suggests that progressive deepening of the basin occurred contemporaneously with explosive volcanism in    neighboring areas. During this interval of basinal subsidence, the limestones received abundant argillaceous material from subaerial erosion of nearby volcanic terrain. Gradual reduction in the frequency of glass shards and pumice from Middle Miocene (Ongeian Stage) onwards indicates culmination of volcanic eruptions and basinal stability. Gradual shallowing to subtidal and patch reef (coralgal facies) environments began to form from the Middle Miocene onwards at Little Andaman, Havelock, Nicholson and other islands. Deep basinal conditions prevailed during the Late Miocene to Early Pliocene at Neill, Sir Hugh Rose and Car Nicobar Islands. These different conditions may be attributed to    tectonism in the Andaman sea region which occurred during the close of Middle Miocene. Thereafter, younger   limestone facies of Plio-Pleistocene age, reflect a shoaling upwards to probable intertidal conditions due to rapid infilling and vertical uplift of the basin floor. No hydrocarbons were observed in the limestone sequences. The regional stratigraphic and petrographic studies reveal the presence of potential reservoir rocks in the Ongeian-Havelockian limestones of Middle Miocene age on the Andaman-Nicobar Islands. ',12,93,843953,10587890,'India','Asia',501,'',12,93,'','',11.0412070701,91.7213123936,11.0412070701,91.7213123936,8.83899174412,92.2406633175),('Hendrick Field, Winkler Co., Texas',2030,'','Permian','Middle Permian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,262,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','86',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',2,'Actual reservoir',1237,0,'Producing reservoir in back reef facies.',31,-103,367679,-3617544,'United States','North America',101,'',31.75,-103.0833,'','',10.1317677074,-28.9960848585,10.1317677074,-28.9960848585,4.58308454804,-35.9428427456),('Havelock Island, Andaman Islands',2031,'','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150','2031',0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1242,0,'see reef 2029.',12,93,1206203,10370470,'India','Asia',501,'',12,93,'','',11.6020463224,92.4357439013,11.6020463224,92.4357439013,10.1277583437,92.7166364959),('Little Andama Island, Andaman Islands',2032,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150','2029',0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1242,0,'see reef 2029.',10,92,659180,10573419,'India','Asia',501,'',10.75,92.4167,'','',9.77560485712,91.175911579,9.77560485712,91.175911579,7.57823297736,91.6872809611),('Little Andama Island, Andaman Islands',2033,'','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1242,0,'see reef 2029.',10,92,1027399,10344378,'India','Asia',501,'',10.75,92.4167,'','',10.3336237542,91.8961653537,10.3336237542,91.8961653537,8.86185270763,92.1734860722),('Small Nggela Island',2034,'','Neogene','Pliocene','lower Pliocene',3.60,5.30,32,'Tortonian - Gelasian',6,4,3,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1243,0,'Abstract of ref. 1243:\nMost of the sedimentary rocks of Small Nggela are early Miocene in age (dated by nannofossils and foraminifera). In the north, uniform volcaniclastic arenite (the Siota Beds) crops out. Much of the central, western and eastern parts of the island contain diverse strata including pillow lava, calcarenite, volcaniclastic arenite, grit and breccia (the Ghumba Beds). The Siota and Ghumba Beds, which are separated by a 1-1.5 km wide, east-trending ophiolite wedge, are considered to have been deposited in a forearc basin. The ophiolite wedge arrested the northward transport of coarse sediment and was emergent during the late Oligocene and early Miocene. The sediment and the ophiolite wedge are considered to have overlain a southward-descending Benioff zone. Well-bedded laminated arenite lacking basalt and rudite (the Ndandala Sandstone) is present in the south-western part of the island and is probably significantly younger than the underlying Ghumba Beds. A veneer of early-mid Pliocene limsteone (the Florida Limestone), representing a patch reef environment, was deposited upon the Ghumba Beds after they were folded. ',-9,160,-1544902,18027935,'Solomon Islands','Oceania',NULL,'',-9.1333,160.3333,'','',-10.0187616236,163.383257053,-10.0156415348,163.373046954,-10.4247066576,163.520954596),('Silifke',2035,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1246,0,'Abstract of ref. 1246 (part):\nThe Miocene sediments overlying the basement rock units are transgressive and grade into each other vertically and laterally. They are represented by polygenic conglomerates, sandstones, marls and reef limestones. Five planktonic foraminiferal biozones, 3 Burdigalian and 2 Helvetian to Tortonian (?), were defined in these formations. ',36,33,4699718,3189712,'Turkey','Asia',522,'',36.3333,33.9167,'','',35.9732560273,31.2865348641,35.9732560273,31.2865348641,34.9798738042,33.1385496923),('Miaru, Papua New Guinea',2036,'Era','Neogene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3',NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','104','2','Baffler guild','1','Present','1','Present','2','Medium zonation',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1247,0,'50 m thick fossiliferous beds in Era Beds.\nSeveral 2-3 m thick coral horizons, corals often in growth position.\nPulses of clastic sedimentation throughout the reefal interval. ',-8,146,-1659864,15873195,'Papua New Guinea','Oceania',615,'',-8.35,146.2833,'WAHR','42736',-10.2477547152,145.365822707,-10.2453522223,145.366976044,-10.9697471161,145.578803063),('Golden Spike, Alberta',2037,'Leduc','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',1,'True reef','3','101-500 m thick','197',NULL,NULL,NULL,'4','More than 1000 m',NULL,'3',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'10','0','90',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1250,1283,'197 m thick atoll reef (on platform).\nExcellent reservoir. 10 % avg. porosity, 100 md permeability.\nMassive and tabular stromatoporoids, few tabulate corals, encrusting algae.\nExtensive submarine cementation in the fore-reef, less in the reef.',53,-113,-1391666,-4628467,'Canada','North America',121,'1396, 1507',53.45,-113.8667,'','',-9.16840168446,-58.0096450299,-9.16840168446,-58.0096450299,-2.58461730076,-116.737843971),('Uniontown, Bourbon Co., Kansas',2038,'Hertha','Carboniferous','Upper Carboniferous','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,304,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','7',NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','2','Algae','1','Corals','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','20','80','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1257,1719,'Oldest phylloid algal mound complexes\nUp to 7 m thick. \nSome lithostrotionellid and syringoporid corals present but not framework-building.\nphylloid wackestone to mudstone\nAuthochthonous Neosyringopora framsestone\nPhylloid thalli framestone.',37,-94,-427598,-3065999,'United States','North America',101,'',37.85,-94.9833,'','',-3.0528732791,-27.635378746,-3.0528732791,-27.635378746,-4.53413367503,-50.7588617331),('S-Neosho Co., Kansas',2039,'Swope-Dennis','Carboniferous','Upper Carboniferous','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,304,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m',NULL,'80',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','2','Algae','2','Algae','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1257,0,'Sparry algal calcilutite.\nUp to 20 m thcik.\nBethyan Falls Limestone Member of Swope Fm. and\nWinterset Limestone Member of Dennis Formation.',37,-95,-445463,-3105784,'United States','North America',101,'',37.55,-95.2833,'','',-3.18909807233,-27.9933808276,-3.18909807233,-27.9933808276,-4.64990970116,-51.1246434412),('Wyandotte Co., Kansas',2040,'Wyandotte','Carboniferous','Upper Carboniferous','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,304,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','17',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','2','Algae','2','Algae','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',1257,0,'Argentine Limestone Member.\nEastern complex up to 17 m thick. Algal to sparry algal calcilutite.',38,-94,-341049,-2986427,'United States','North America',101,'',38.7667,-94.6167,'','',-2.40970251707,-26.9208288638,-2.40970251707,-26.9208288638,-3.93218253506,-50.0079838671),('Padaukpin, Maymyo, Myanmar',2041,'Padaukpin','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,1,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','9','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',2317,0,'Ref. 2317 cites older papers describing 23 rugose and 21 tabulate coral species. Only eight taxa described in ref. 2317.\nBiostrome mentioned \nrugose and tabulate corals, brachiopods, sponges, bryozoans and microfossils reported',22,96,-2048709,13986041,'Burma','Asia',603,'',22.0833,96.5833,'WAHR','62942',-19.228293496,99.2440713878,-19.228293496,99.2440713878,-47.0305015636,133.810574018),('Yunggrangan, Yogyakarta, Java',2042,'Progo Beds','Neogene','Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,18,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','19','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1258,0,'Locality described as Djunggrangan, NW Jogjakarta.\nBurdigalian age suggested by van Bemmelen (1949).\n36 coral species described from Formation but only 18 described in ref. 1258. ',-7,110,-1055426,12351960,'Indonesia','Asia',614,'',-7.6667,110.0833,'WAHR','34721',-5.21570546636,107.763549043,-6.02910822239,107.568663866,-9.02493450313,109.666744838),('Geger Tjabé, Pankah, Java',2043,'','Neogene','Pliocene','lower Pliocene',3.60,5.30,32,'Tortonian - Gelasian',6,4,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','51',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1258,2414,'Small coral reef with 15 species according to ref. 1258\nUmbrove (1946) cited 51 species in another(?) reef',-7,109,-974557,12114077,'Indonesia','Asia',614,'',-7,109.25,'WAHR','34722',-6.47234645797,108.834910023,-6.47412512026,108.836316156,-7.2943819398,108.927327619),('San Andrés Island, Columbia',2044,'San Andres','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1259,2594,'Abstract of ref. 1259:\nSan Andres is a small coralline island 136 km east of the Caribbean coast of Nicaragua. Surface mapping and paleontologic data indicate reefs have been growing actively in the area at least since early Miocene time. Because of the offlap relations of the ancient reef complexes, accessibility of progressively younger rocks is simplified.\n\nField and laboratory examination of both modern and ancient reef complexes indicates five major bottom facies: (1) forereef flank, (2) reef, (3) backreef platform, (4) backreef lagoon with patch reefs, and (5) shore area. Principal builders of the reefs were Millepora and lime-secreting algae with abundant Acropora, Diploria, Montastrea, and Porites.\n\nFrom X-ray and petrographic studies of the limestones, a sequence of carbonate diagenesis has been determined for the San Andres area. During early stages of diagenesis, sediments initially are cemented by grain welding and aragonite precipitation between grains. This early type of cementation is most common in the supertidal and intertidal zones. Subsequent calcite cementation occurs by dissolution-precipitation after aragonite. After calcite precipitation, no evidence can be found of the preexisting aragonite cement. Although inversion of aragonite to calcite commonly occurs in grain material, dissolution-precipitation seems to be the major process of cementation.\n\nDuring the diagenetic sequence, four responses may be expected: (1) magnesium is removed and high-magnesium calcite stabilizes to low-magnesium calcite, (2) aragonite can stabilize to calcite, (3) aragonite may be dissolved, and (4) sediments may become dolomitized. The time required for any of these reactions is variable and depends on the chemical environment. X-ray analyses indicate that all samples older than middle Pleistocene have stabilized to low-magnesium calcite or dolomite. The result of the diagenetic sequence is the development of a low-magnesium calcite limestone, a dolomite, or a combination of the two.\n\nPorosity in the San Andres area is primary, secondary, or occluded and development depends on exposure of carbonate material to a subaerial environment before mineral stabilization occurs.\n\n',12,-81,1763221,-8944414,'Colombia','South America',226,'',12.5333,-81.7,'WAHR','73792',11.2060601258,-81.0159453525,11.2060601258,-81.0159453525,14.1707154333,-80.4236075757),('San Andrés Island, Columbia',2045,'','Neogene','Miocene','lower-middle Miocene',13.80,16.00,31,'Burdigalian - Serravallian',14,16,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1259,2594,'Principal reef builders:\nMillepora, lime-secreting algae and abundant Acropora, Diploria, Montastrea and Porites.',12,-81,1758317,-8932928,'Colombia','South America',226,'',12.5333,-81.7,'','',11.4959603512,-81.1605558632,11.4959603512,-81.1605558632,13.8807205391,-80.7386132139),('San Andrés Island, Columbia',2046,'','Neogene','Upper Neogene','upper Miocene/Pliocene',2.60,11.60,32,'Tortonian - Gelasian',6,5,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','95','5',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1259,2594,'Seef reef 1258.',12,-81,1737284,-8936924,'Colombia','South America',226,'',12.5333,-81.7,'','',11.9994549361,-81.501146513,11.9994549361,-81.501146513,13.25340779,-81.3334992509),('Trinil, Java',2047,'','Neogene','Pliocene','lower Pliocene',3.60,5.30,32,'Tortonian - Gelasian',6,4,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','11',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','39','1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1260,0,'Probably early Pliocene.\nReef limestone around 11 m thick.\nUp to 39 coral species from a single locality (5 localities mentioned by ref. 1260).',-7,111,-1018688,12341888,'Indonesia','Asia',614,'',-7.3667,111.35,'WAHR','71079',-6.83230948372,110.933731938,-6.83411113558,110.935141725,-7.68808079635,111.023806835),('Abukuma',2048,'Torinosu','Jurassic','Upper Jurassic','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,147,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','60','30',0,'no',0,'no','3','25 or more reef building species','39','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1261,0,'Northernmost extension of Torinosu-Limestone.\n28 scleractinian genera\n4 chaetetid genera\n7 stromatopore-hydrozoan genera\nafter Yabe & Sugiyama (1935).',37,140,7719497,10629119,'Japan','Asia',625,'',37.8333,140.75,'','',62.9801047236,161.223078456,62.9801047236,161.223078456,56.7797649441,162.725119124),('Minami-jima',2049,'Ogasawara Group','Neogene','Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,22,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','9','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1261,0,'Small island opposite Minami-zaki (S-Chichi-jima).\nEulepidina used to assign Aquitanian age.\nCoral limestone by crowded coral stocks, mostly in upright position.\n8 genera mentioned in uncomplete list.',27,142,3202378,16511139,'Japan','Asia',625,'',27.0333,142.25,'WAHR','34874',20.3341382137,138.001433285,20.3341382137,138.001433285,21.5864926158,147.299903888),('Oishi, Kawaguchi Lake',2050,'','Neogene','Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,18,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1261,0,'Northernmost limit of Tertiary reefal limestone in Japan.\nSeveral species of genera Favia, Favites, Hydnophyllia, Maeandra.\nMany coral stocks.',35,138,5082977,13036156,'Japan','Asia',625,'',35.5167,138.7333,'WAHR','34875',38.1828849238,136.434178184,37.6921157745,136.731808502,35.2587497817,136.295438757),('Kikai-shima, Ryukyu Islands',2051,'Riukiu Limestone','Neogene','Pliocene','late Pliocene',2.60,3.60,32,'Tortonian - Gelasian',6,3,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','80',NULL,NULL,NULL,NULL,NULL,NULL,'1100',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','21','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1261,0,'19 coral species listed by ref. 1261.\nRiukiu limestone less than 80 m thick, extending from S Taiwan to Kikai-shima.\nReef limestone in some places only.',28,130,3884819,13221128,'Japan','Asia',625,'',28.3333,130,'WAHR','34877',28.7253327052,129.524952251,28.7266158237,129.52340663,28.2350091509,129.471422304),('Shuri, Okinawa',2052,'','Neogene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1100','2051',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1261,0,'Coralline limestone with massive coral stocks.\nMostly Porites.',26,127,3600201,13155029,'Japan','Asia',625,'',26.2167,127.7167,'','',26.825741256,126.977691059,26.8249590019,126.978627706,26.1856749867,126.940485365),('Monte Grappa, Trento',2053,'','Jurassic','Lower Jurassic','upper Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,184,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','10','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','1','Corals','22','Stromatoporoids/sponges - corals - (algae)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1262,476,'Sponge-coral-stromatoporoid patch reefs with intercalated grainstones.\nComplex up to 15 m and 10a of m wide.\nStylothalamia cf. budaensis\nsolitary and colonial corals\nstromatoporoids\nSolenopora\n',45,11,4303132,1731743,'Italy','Europe',344,'',45.85,11.8,'','',20.6357649624,27.6813090444,20.6357649624,27.6813090444,26.272767168,30.2033566397),('Vealmoor, Horseshoe Atoll, Texas',2054,'','Carboniferous','Upper Carboniferous','Missourian-Virgillian',303.70,307.00,13,'Bashkirian - Kasimovian',302,303,2,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','310',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'','2','Algae','2','Algae',NULL,NULL,'1','Red algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',1263,0,'',32,-101,-623325,-3891053,'United States','North America',101,'',32.5167,-101.5833,'','',-4.60452936552,-35.0732463578,-4.60452936552,-35.0732463578,-5.65212404268,-58.2873630491),('Kelly Snyder, Horshoe Atoll, Texas',2055,'Cisco','Carboniferous','Upper Carboniferous','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,304,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','310',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1263,1399,'Isolated reef mound complex (platform margin).\nSponges-algae-bryozoans\nand phylloid algal boundstones (wackestones)\n 8 % avg. porosity.\n50 m thick.\nSponges were 2nd but unlikely',32,-100,-640081,-3827288,'United States','North America',101,'',32.75,-100.95,'','',-4.71732479037,-34.5002634839,-4.71732479037,-34.5002634839,-5.7986528161,-57.7211614348),('Salt Creek, Horshoe Atoll, Texas',2056,'','Carboniferous','Upper Carboniferous','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,304,3,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','310',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','2','Algae','2','Algae',NULL,NULL,'2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1263,0,'',33,-100,-590233,-3786173,'United States','North America',101,'',33.2667,-100.8333,'','',-4.34730879228,-34.1254006334,-4.34730879228,-34.1254006334,-5.45142791558,-57.3242929233),('Block 372, Baltimore Canyon Trough',2057,'','Cretaceous','Lower Cretaceous','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,123,3,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','4','Stromatoporoids','6','Calcisponges','22','Stromatoporoids/sponges - corals - (algae)',NULL,NULL,'10','60','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1264,0,'Stromatoporoid-sponge-coral boundstones and grainstones (subsurface) just before platform drowning.',38,-72,2667871,-3159680,'Atlantic','Atlantic',NULL,'',38.6167,-72.8667,'','',28.372192513,-21.6895254468,27.1719989962,-20.5487941856,30.5714251684,-26.3773893157),('Liuhua, Pearl River Mouth, South Ch',2058,'Zhujiang','Neogene','Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,21,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','476',NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','1','Corals','22','Stromatoporoids/sponges - corals - (algae)','1','Red algae','0','40','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1264,1389,'Carbonate bank.\n476 m thick. \nPlatform margin reef.\n24 % porosity.',20,115,3536042,12030289,'China','Asia',602,'',20.8,115.6833,'','',23.115151495,113.020272089,23.115151495,113.020272089,19.93219015,113.622477117),('Liuhua, Pearl River Mouth, South China Sea',2059,'','Neogene','Miocene','lower Burdigalian',17.50,20.40,31,'Burdigalian - Serravallian',14,19,3,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'25',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','4','Stromatoporoids','22','Stromatoporoids/sponges - corals - (algae)','1','Red algae','0','20','80',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1264,0,'',20,115,2795607,12269469,'China','Asia',602,'',20.85,115.6333,'','',23.2644610709,112.939693009,22.900312564,113.189497654,20.0057469054,113.698605322),('Emperor Seamount, Pacific',2060,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,1,'Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1265,0,'Abstract of ref. 1265:\nThis paper is a review of the present knowledge of coral reef ecology and paleoecology in the Hawaiian-Emperor\nChain during the last 70 Ma. Research on fossil coral deposits throughout the H-E Chain has played a major role in producing information concerning the subsidence, uplift and drowning of individual islands, as well as the  paleocirculation of the North Pacific Ocean during Tertiary time. The origin of the Hawaiian Islands and seamounts    over the Hawaiian hotspot and their subsequent subsidence and transport by plate motion to the north and northwest are reviewed and new data concerning uplift of the central high Hawaiian Islands caused by lithospheric flexure and the effect of sea level change on the geological evolution of individual islands are presented. The Darwin Point, where atolls drown to form guyots, is redefined in dynamic terms as a function of climate and sea level history. The absence of coral reefs during the first half of Hawaiian history is evidence ...',42,170,4991923,-16958529,'Pacific','Pacific',NULL,'',42,170,'','',38.3611171417,-174.056793984,38.3611171417,-174.056793984,42,170),('Emperor Seamount, Pacific',2061,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,1,'Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1265,0,'See reef 2060',42,170,5077103,17218912,'Pacific','Pacific',NULL,'',42,170,'','',38.9986028129,-178.340060631,38.9980799248,-178.336281293,42,170),('Baixo, Porto Santo, E-Atlantic',2062,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1266,0,'Abstract of ref. 1266:\nEphemeral coral reefs developed in the Miocene on the submarine slopes of the Porto Santo and Madeira volcanic complexes. The paleontology of these reefs is discussed. Danaia calcinata described from Baixo, near Porto Santo by Mayer (1864) as a tabulate coral is identified here as synonymous with Pocillopora madreporacea (Lamarck, 1816).\nCorals: Thamnasteria sp., Stylina aff. girodi Efallon and Stylina sp.',33,-16,4358253,-1765710,'Portugal','Europe',304,'',33.05,-16.3333,'','',31.3334188456,-17.777530212,31.3334188456,-17.777530212,33.05,-16.3333),('Vening Meinesz seamounts, Indian Ocean',2063,'','Cretaceous','Upper Cretaceous','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,68,2,1,'Seismic data available ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,2,'Cold - water',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'','5','Rudists','2','Algae','47','Bivalves (mostly oysters) - algae (microbes)','1','Red algae','50','20','30',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite',NULL,'','0','',0,'No or unknown reservoir potential',1267,0,'Inoceramids and rudists dredged',-11,105,-4901609,8774042,'Indian Ocean','Indian Ocean',NULL,'',-11.3333,105,'','',-36.3453334224,93.1422201016,-36.3453334224,93.1422201016,-11.3333,105),('Gunung Anga, Borneo',2064,'','Paleogene','Oligocene','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,32,2,1,'Seismic data available ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'8',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1268,0,'See reef 3098',-1,115,429957,13320391,'Indonesia','Asia',614,'',-1,115.4333,'','',1.81417964579,112.956117301,1.81417964579,112.956117301,-3.5126393063,116.019960952),('Jaan River, Borneo',2065,'','Paleogene','Oligocene','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,32,2,1,'Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'60',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1268,0,'Sequence 2\nSmall patch reef in coral-rich wackestone-packstone sequence',0,114,425281,13217783,'Indonesia','Asia',614,'',-0.7833,114.5333,'','',2.17034176235,112.101251283,2.17034176235,112.101251283,-2.83205612281,115.39164416),('Jaan River, Borneo',2066,'','Paleogene','Oligocene','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,27,2,1,'Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'60',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1268,0,'Sequence 2\n32 - 29.7 Ma',0,114,18767,13063473,'Indonesia','Asia',614,'',-0.7833,114.5333,'','',0.40692365472,111.84942862,0.40692365472,111.84942862,-4.1666766637,114.481780078),('Lemo River, Borneo',2067,'','Paleogene','Oligocene','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,26,3,1,'Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'60','2066',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','12','Foraminifera','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','80','20',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1268,0,'Sequence 3.\nShelf margin coral boundstones and coral-rich\nlarge foram-coralline algae packstone-grainstone.\nMassive and thick branching corals.',-1,114,-13005,13094954,'Indonesia','Asia',614,'',-1.05,114.7833,'','',0.104568223971,112.054842625,0.104568223971,112.054842625,-4.5263369457,114.547216088),('Kangean Block E, Java Sea',2068,'','Neogene','Miocene','Langhian-Serravallian',11.60,16.00,31,'Burdigalian - Serravallian',14,15,3,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1269,0,'Asymmetrical atoll structure.\nReef growth along northern edge of carbonate platform.',-6,116,-875816,13064550,'Indonesia','Asia',614,'',-6.7833,116.4,'','',-5.35541508374,114.749308504,-5.35486220998,114.74605902,-8.74599036024,115.764205181),('Kangean Block W, Java Sea',2069,'','Neogene','Miocene','Langhian-Serravallian',11.60,16.00,31,'Burdigalian - Serravallian',14,13,3,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'30','2068',0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1269,0,'See reef 2068.',-6,116,-884807,13038145,'Indonesia','Asia',614,'',-6.8333,116.1667,'','',-5.40585038464,114.516723202,-5.40529179015,114.513472679,-8.76843796292,115.525498553),('Ernstbrunn',2070,'','Jurassic','Upper Jurassic','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,147,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','60','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1270,0,'',48,16,3953101,1763651,'Austria','Europe',301,'',48.5,16.3833,'','',30.877946358,27.9438492604,30.877946358,27.9438492604,35.820150118,30.2974860638),('Ile Bizard, Montreal',2071,'Laval','Ordovician','Middle Ordovician','Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,460,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','7','Bryozoans','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1272,0,'Bryozoans (Batostoma) form rigid self supporting framework.',45,-73,-2896141,-4930012,'Canada','North America',121,'',45.4833,-73.9167,'WAHR','80006',-8.15809460366,-100.078922678,-8.15809460366,-100.078922678,-8.15809460366,-100.078922678),('Little Cove, Antigua',2072,'Antigua','Paleogene','Oligocene','early late Oligocene',26.00,28.10,30,'Chattian - Aquitanian',22,27,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','21',NULL,NULL,NULL,'3','More than 100 m','105',NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present',NULL,'','3','Pronounced zonation','2','Medium zonation',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1987,1273,'Patch reef in middle part of Antigua Fm.\nmore than 100 m wide and more than 20 max. thickness.',17,-61,2278996,-6683164,'Antigua and Barbuda','North America',NULL,'',17.0333,-61.6833,'WAHR','34504',15.1940773485,-61.3786658363,15.2469036157,-61.4252722275,18.6960012811,-60.4414382436),('St. John\'s Cathedral, Antigua',2073,'Central Plain Group','Paleogene','Oligocene','middle Oligocene',26.00,32.00,29,'Priabonian - Rupelian',33,27,1,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','14','1','Constructor guild','1','Present',NULL,'','3','Pronounced zonation','1','Low zonation',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1273,1987,'2 m thick coralgal deposit.\nPlaty Porites panamensis and subordinate Goniopora in a skeletal matrix of broken coral, coralline, algae and large Lepidocyclina. \n\nOnly about 12 species of corals contribute significantly to reef construction.',17,-61,2209872,-6673436,'Antigua and Barbuda','North America',NULL,'',17.1167,-61.8333,'WAHR','34503',15.1029454513,-61.8412984861,15.092146923,-61.917200159,18.8782091659,-60.749686968),('Makamby Island',2074,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,1,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1274,0,'',-15,45,-2304104,4758045,'Madagascar','Africa',702,'',-15.7,45.9,'','',-17.1918945359,44.3048452648,-17.1918945359,44.3048452648,-18.3057126016,44.1090338317),('Last Chance Canyon, New Mexico',2075,'San Andres','Permian','Middle Permian','Guadalupian',259.80,272.30,16,'Roadian - Changhsingian',261,265,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','25',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,'50','40','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1275,0,'Upper San Andres Fm.\nReef mounds with 25 m depositional relief.\nBryozoans, brachiopods, calcareous sponges.\nInferred water depth 30-50 m (lower slope).\nOther type is crinoid-bryozoan bafflestone bioherm.',32,-104,517939,-3724240,'United States','North America',101,'',32.2833,-104.7,'','',9.08559450261,-30.7371968645,9.08559450261,-30.7371968645,3.9756133852,-38.5546487665),('Truk, Micronesia',2076,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,3,0,'Outcropping reef ',1,'True reef','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1277,0,'',7,151,544803,17851760,'Micronesia','Oceania',NULL,'',7.3333,151.75,'','',5.23251530106,161.824960726,5.23223625649,161.828302468,7.3333,151.75),('Truk, Micronesia',2077,'','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,0,'Outcropping reef ',1,'True reef','4','More than 500 m thick','1100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1277,0,'Reef growth from 12-14 Ma to recent (with interruptions).\nThickness of reef limestone about 1100 m.',7,151,732558,17281145,'Micronesia','Oceania',NULL,'',7.3333,151.75,'','',5.90282030249,157.97940972,5.87583796165,158.083365925,7.3333,151.75),('Ponape, Microne',2078,'','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,0,'Outcropping reef ',1,'True reef','4','More than 500 m thick','600',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1277,0,'Reef growth from 8 Ma to recent (with interruptions).\nThickness of reef limestone 600-800 m.',6,158,646219,17999527,'Micronesia','Oceania',NULL,'',6.8333,158.1667,'','',5.17909927192,164.355397891,5.1485149431,164.458630552,6.8333,158.1667),('Mayotte, Indian Ocean',2079,'','Neogene','Upper Neogene','Miocene/Pliocene',2.60,20.00,32,'Tortonian - Gelasian',6,5,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1277,0,'',-12,45,-1815453,4827673,'France','Europe',331,'',-12.8333,45.1667,'','',-13.9940137148,43.8262518453,-13.9940137148,43.8262518453,-12.8333,45.1667),('Bora-Bora, Polynesia, Pacific',2080,'','Neogene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,3,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1277,0,'',-16,-151,-2543059,-15860409,'Pacific','Pacific',NULL,'',-16.5,-151.7167,'','',-17.6935072607,-148.873682093,-17.6935072607,-148.873682093,-16.5,-151.7167),('N Purcell Mts., British Columbia',2081,'','Cryogenian','Upper Cryogenian','Hadrynian',541.00,635.00,-1,'Neoproterozoic',770,640,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','45',NULL,NULL,NULL,'3','More than 100 m',NULL,'30',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1278,0,'Stromatolitic dolomitic bioherms up to 45 m thick.\nOff-bank facies.\npre-Ediacaran',51,-117,-6248659,-9558977,'Canada','North America',121,'',51.4167,-117.4,'','',-39.3057692876,154.28465058,-39.3057692876,154.28465058,-39.3057692876,154.28465058),('Perico Hills',2082,'Atocongo','Cretaceous','Lower Cretaceous','Hauterivian-Barremian',125.00,132.90,23,'late Valanginian - early Aptian',126,130,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1279,0,'4.5 m thick silicified coral biostrome.\n\nAbstract of ref. 1279:\nDuring the Hauterivian-Barremian, local coral biostromes, possibly patch reefs, developed within shallow marine lagoons fringing Early Cretaceous volcanoes in Peru. The dominant coral is S. columbaris sp. nov. which is similar to European stylinid species of Late Jurassic and Early Cretaceous age having 6-fold septal plans. The biostrome is part of the Atocongo Formation, Lima Group, exposed at Perico Hill (Cerros Perico) about 95 km south of Lima. Only 2 other lower Cretaceous stylinid corals were described from South America. ',-12,-76,-3556536,-4526985,'Peru','South America',201,'',-12.5333,-76.5,'WAHR','50765',-19.2894887039,-39.0028115245,-19.2894887039,-39.0028115245,-15.0542037122,-43.6799448094),('Serranía de Cocinas, Guajira Peninsula, Columbia',2083,'Jipi','Jurassic','Upper Jurassic','lower Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,154,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','100','3','101-1000 m wide','500','4','More than 1000 m','1000',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','10','1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1280,2112,'Coral-limestone with low diversity anthozoan fauna.\nReefal limestones up to 100 m thick and 500 to 1000 m long interfingering with calcareous shales and sandstones.',11,-71,326238,-4582052,'Colombia','South America',226,'',11.8333,-71.6333,'WAHR','34736',4.11720591868,-38.8361009627,4.11720591868,-38.8361009627,9.45388431433,-40.2824313587),('Norman Wells, N.W.T.',2084,'Ramparts-Kee Scarp','Devonian','Middle Devonian','upper Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,3,1,'Seismic data available ',1,'True reef','3','101-500 m thick','160','4','More than 1000 m wide','8000','4','More than 1000 m','25000',NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','3','Pronounced zonation',NULL,'','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1282,1283,'Average porosity 10 %, permeability around 110 md.\n4 growth stages in 160 m thick reef.\nDiversity not described but all groups (stromatoporoids, tabulate and rugose corals) with different species and growth forms.\n\nRanging into Frasnian\n\nAbstract of ref. 2126:\nThe Middle-Upper Devonian Kee Scarp reef complexes are oil-producing, stromatoporoid-dominated carbonates. Episodic increases in the rate of sea level rise produced multiple cycles of reef growth that exhibit backstepping characteristics. These carbonates have original interskeletal, intraskeletal, and intergranular porosity, mostly occluded by nonferroan, dull luminescent cements. Secondary porosity, represented by micropores of various types, developed during diagenesis by aggrading neomorphism and dissolution. The micropores represent the main reservoir porosity in the Kee Scarp limestone. Micropores in the Kee Scarp limestone can be classified into four categories based on their shapes.',65,-126,294504,-4053074,'Canada','North America',121,'1600, 2126',65.2833,-126.8722,'WAHR','84237',2.94748263624,-53.310768878,2.94748263624,-53.310768878,9.19929760991,-114.586227328),('Redwater, Alberta',2085,'Leduc','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',1,'True reef','3','101-500 m thick','245',NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species','14','1','Constructor guild',NULL,'','1','Present','3','Pronounced zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1283,917,'245 m thick bioherm (atoll structure).\nbest reservoir quality in organic facies of reef margin.\n\nMassive stromatoporoids, tabulate corals, rugose corals, Stachyodes, Amphipora, brachiopods, crinoids.\n\nReef: Massiv stromatoporoids\nReef flat: Skeletal rudstone\nInterior: Amphipora beds\n\n7 % avg. porosity.',53,-113,-1391038,-4558683,'Canada','North America',121,'1762, 1396',53.9167,-113.1667,'WAHR','657',-9.21564147614,-57.3791005615,-9.21564147614,-57.3791005615,-2.4692559531,-116.123761662),('Macrossan, Fly River, Papua New Guinea',2086,'','Paleogene','Eocene','Middle Eocene',38.00,47.80,28,'Lutetian - Bartonian',45,40,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'50',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1285,2277,'Compact coral limestone of Eocene, probably middle Eocene age.\r\nCream-coloured matrix.\r\nAge discounted by Wilson and Rosen (1998). Said the faunas are mostly Neogene or of mixed ages',-6,141,-3891485,13628927,'Papua New Guinea','Oceania',615,'',-6.0833,141.3833,'WAHR','70667',-26.7908630534,131.908944387,-26.7908630534,131.908944387,-30.9918458744,134.079782467),('Palmer River, Papua New Guinea',2087,'','Paleogene','Eocene','Middle Eocene',38.00,47.80,28,'Lutetian - Bartonian',45,40,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'50','2086',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1285,0,'reef 2086 for remarks.',-5,141,-3841833,13692015,'Papua New Guinea','Oceania',615,'',-5.75,141.7167,'',NULL,-26.4235345705,132.237191247,-26.4235345705,132.237191247,-30.6188492286,134.41304904),('Hestnesfjell, Prosanger Fjord',2088,'Porsanger Dolomite','Cryogenian','Lower Cryogenian','Riphean',720.00,850.00,-1,'Neoproterozoic',770,700,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','16',NULL,NULL,NULL,'4','More than 1000 m',NULL,'25',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1286,1957,'Up to 16 m thick laterally extensive stromatolite biostrome.',70,25,-7392805,-2525860,'Norway','Europe',301,'',70.3167,25.4833,'','',-28.9834858836,-117.122803919,-28.9834858836,-117.122803919,-28.9834858836,-117.122803919),('Sarronvarre, Prosanger Fjord',2089,'Porsanger Dolomite','Cryogenian','Lower Cryogenian','Riphean',720.00,850.00,-1,'Neoproterozoic',770,705,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15',NULL,NULL,NULL,'1','Less than 20 m',NULL,'25',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1286,1957,'pre-Varanger stromatolithic reefs on carbonate platform',70,24,-7388019,-2553325,'Norway','Europe',301,'',70.25,24.9667,'','',-28.8112104347,-117.20473371,-28.8112104347,-117.20473371,-28.8112104347,-117.20473371),('Wörschach',2090,'','Paleogene','Paleocene','Danian',61.60,66.00,26,'middle Campanian - Danian/Selandian',75,63,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'100','657',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1287,0,'',47,14,4852958,1366891,'Austria','Europe',301,'',47.5667,14.2,'','',40.5941496808,12.9773154784,40.5941496808,12.9773154784,42.5992194226,11.2912832485),('JA90-23, Eucla Shelf, Great Austr',2091,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,1,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'475',NULL,1,'Temperate',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1288,0,'Abstract of ref. 1288:\nThe southern continental margin of Australia is the largest area of cool-water carbonate shelf deposition on the globe. Interpretation of 5495 km of airgun seismic-reflection data in the western part of the Great Australian Bight indicates that the 700-m-thick Cenozoic section of the offshore Eucla basin was deposited largely as a prograding cool-water, middle- to high-latitude carbonate ramp, characterized by widespread development of broad, low-relief, biogenic (bryozoan[?]-sponge), shelf and upper-slope mounds. The succession also contains a spectacular and extensive (>475 km long) buried middle Miocene barrier reef (the Miocene Little Barrier Reef) parallel to the modern shelf edge. This rimmed carbonate platform margin represents an episode of warm-water sedimentation during a global climatic optimum, probably coupled with strong eastward flow of a proto-Leeuwin Current. The late Miocene eustatic sea-level fall produced an areally restricted debris-apron sequence at the foot of the reef escarpment. The carbonate platform is capped by a Neogene cool-water carbonate ramp succession typified by aggradational to sigmoidal sequences, punctuated by periods of cold(?)-water, sea-floor erosion. Interpretation of this succession in the light of global and local tectonic and oceanographic events illustrates the dominant influence of water temperature on carbonate platform and reef growth throughout the Cenozoic.',-32,127,-5478038,11484312,'Australia','Oceania',801,'',-32.8333,127.5833,'','',-39.7758886437,123.958351411,-39.7758886437,123.958351411,-42.1422748319,125.052289145),('Eucla Shelf E, Great Austr',2092,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,1,1,'Seismic data available ',1,'True reef','3','101-500 m thick','250',NULL,NULL,NULL,'4','More than 1000 m','6500','475','2091',2,'Cold - water',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1288,2020,'See reef 2091.',-33,129,-5498351,11613399,'Australia','Oceania',801,'',-33,129,'','',-39.93852538,125.508333539,-39.93852538,125.508333539,-42.2893117396,126.661571235),('Eucla Shelf W, Great Austr',2093,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,1,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'475','2091',1,'Temperate',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1288,0,'See reef 2091 for remarks.',-33,125,-5538268,11187489,'Australia','Oceania',801,'',-33.3333,125.25,'','',-40.2724808659,121.404173637,-40.2724808659,121.404173637,-42.660607574,122.41119229),('Western Schelf',2094,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1289,1448,'Seismic exploration only.',-4,54,-747266,5795786,'Seychelles','Africa',NULL,'',-4.5,54.5,'','',-5.80525465035,52.6871049664,-5.80525465035,52.6871049664,-7.19995945834,52.9174444354),('Southern Schelf',2095,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1289,1448,'',-5,55,-810579,5933260,'Seychelles','Africa',NULL,'',-5,55.75,'','',-6.27508175901,53.9515216568,-6.27508175901,53.9515216568,-7.70843163102,54.1703057749),('Western Schelf II',2096,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1289,1448,'',-4,54,-699946,5842936,'Seychelles','Africa',NULL,'',-4.1667,54.9167,'','',-5.4621100384,53.0964989353,-5.4621100384,53.0964989353,-6.86963878005,53.3384953441),('Russel Basin',2097,'','Neogene','Oligocene/Miocene','Oligocene/Miocene',5.30,33.90,30,'Chattian - Aquitanian',22,23,2,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1290,0,'Shallow-water reefal calcarenites mentioned. No description.',-8,158,-1700614,18736385,'Solomon Islands','Oceania',NULL,'',-8.25,158.5,'','',-12.6705736551,166.960795012,-12.6660181242,166.963955078,-10.864126926,167.265765579),('Russel Basin',2098,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1290,0,'',-8,158,-1620034,18323005,'Solomon Islands','Oceania',NULL,'',-8.25,158.5,'','',-10.9166038021,168.226089491,-10.9180985266,168.224969098,-11.371118352,167.156983484),('Vanikoro Basin, Vanuatu',2099,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1291,0,'',-11,166,-2225040,19431431,'Vanuatu','Oceania',827,'',-11.8333,166.75,'','',-15.3125398362,173.572707689,-15.3125398362,173.572707689,-14.6359780572,174.939063161),('Vanikoro Basin, Vanuatu',2100,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1291,0,'',-11,166,-2136989,19036499,'Vanuatu','Oceania',827,'',-11.8333,166.75,'','',-13.8694810877,174.645717118,-13.8707370074,174.644745699,-13.8400942047,176.653865005),('Eua Channel, Tonga, Pacific',2101,'','Paleogene','Eocene','Upper Eocene',33.90,38.00,29,'Priabonian - Rupelian',33,36,2,1,'Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1292,0,NULL,-21,-175,-3780798,-15863007,'Tonga','Oceania',821,'',-21.3333,-175,'WAHR','70950',-33.4493210794,171.729710664,-33.4493210794,171.729710664,-35.3743333698,175.745992311),('Klamono, New Guinea',2102,'Kais','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','90',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1293,0,'100-500 m thick pinnacle reefs on carbonate platform.\nInterfingering with basinal shales.\nOil field.\nSalawati Basin.\nEarly to late Miocene.',-1,131,-1764715,14481653,'Indonesia','Asia',614,'',-1.1333,131.4667,'','',-10.8799475022,126.217584289,-10.8799475022,126.217584289,-13.2396188528,128.615537344),('Klamono, New Guinea',2103,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','250',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1293,0,'See reef 2102.',-1,131,-1252721,14596255,'Indonesia','Asia',614,'',-1.1333,131.4667,'','',-8.05296941892,127.836555569,-8.05543752495,127.835123486,-9.74005327212,129.723948428),('Klamono, New Guinea',2104,'','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','150',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1293,0,'See reef 2102.',-1,131,-652412,14629081,'Indonesia','Asia',614,'',-1.1333,131.4667,'','',-5.29942743793,129.339874265,-5.3697220771,129.303798105,-6.41674575018,130.61630147),('Wasian, New Guinea',2105,'Kais','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','90',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1293,0,'Bintuni Basin.\n100 - 500 m thick pinncale reefs on platform carbonates, interfingering with basinal shales.\nOil field.',-1,133,-1917271,14625973,'Indonesia','Asia',614,'',-1.8667,133.3333,'','',-11.5685871111,128.137244272,-11.5685871111,128.137244272,-14.4030923954,130.29703956),('Wasian, New Guinea',2106,'Kais','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','250',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1293,0,'See reef 2105.',-1,133,-1394952,14759612,'Indonesia','Asia',614,'',-1.8667,133.3333,'','',-8.76507779711,129.731114528,-8.7675249049,129.729702526,-10.9287002532,131.365150882),('Wasian, New Guinea',2107,'Kais','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','150',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1293,0,'See reef 2102.',-1,133,-773202,14816887,'Indonesia','Asia',614,'',-1.8667,133.3333,'','',-6.02650857287,131.217470288,-6.09671283865,131.181659214,-7.55534605327,132.278893842),('Madura Basin, Java',2108,'','Paleogene','Oligocene','lower Oligocene',28.10,33.90,29,'Priabonian - Rupelian',33,32,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1294,1293,'Massive reefal limestones grading laterally into sandstones, siltstones and coals.',-7,113,-523079,13270614,'Indonesia','Asia',614,'',-7.5833,113.1667,'','',-2.42474025168,111.671763837,-2.42474025168,111.671763837,-8.22311829672,115.512000092),('Wiriagar, New Guinea',2109,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1293,1309,'See reef 2102.',-2,132,-1436026,14693978,'Indonesia','Asia',614,'',-2.25,132.8833,'','',-9.15414989875,129.280895771,-9.15660223973,129.279485369,-11.1841823846,130.822264335),('Wiriagar, New Guinea',2110,'','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1293,1309,'See reef 2102.',-2,132,-820573,14757851,'Indonesia','Asia',614,'',-2.25,132.8833,'','',-6.41173427775,130.766756567,-6.48196711871,130.730909671,-7.82676819583,131.749260284),('Kerendan, Borneo',2111,'Berai','Paleogene','Oligocene','lower Oligocene',28.10,33.90,29,'Priabonian - Rupelian',33,32,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1293,0,'Pinnacle reef on horst, surrounded by basinal shales.\nProducing gas reservoir.\nNW Kutei Basin.\nBerai Formation (late Rupelian to Chattian).',0,116,585081,13340201,'Indonesia','Asia',614,'',0.0167,116,'','',2.72809200493,113.677496679,2.72809200493,113.677496679,-2.98217437832,117.057682548),('Kerendan, Borneo',2112,'Berai','Paleogene','Oligocene','Upper Oligocene',23.00,28.10,30,'Chattian - Aquitanian',22,27,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1293,0,'See reef 2111.',0,116,153928,13211936,'Indonesia','Asia',614,'',0.0167,116,'','',0.973403831539,113.425550459,0.968562409204,113.422964814,-4.28897045215,116.15249691),('Poleng, Madura Basin, Java',2113,'','Neogene','Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',1294,1293,'Thick limestones, often reefal and highly porous, rarely dolomitized.',-6,112,-892443,12677087,'Indonesia','Asia',614,'685',-6.6667,112.9167,'','',-4.96035266352,110.140342858,-4.96035266352,110.140342858,-8.56991339221,112.731390386),('Ardjuna sub-basin, offshore Java',2114,'','Neogene','Oligocene-Miocene','Chattian-Aquitanian',23.00,28.10,30,'Chattian - Aquitanian',22,23,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1295,1293,'Batu Raju Limestone buildup.\nSeismic exploration only.\nSevere diagenetic modification, but basic coral framework visible in places.',-5,107,-802351,12346220,'Indonesia','Asia',614,'',-5.9167,107.7,'','',-2.6475414721,105.93565319,-2.6475414721,105.93565319,-6.060601575,109.760138627),('W-Bengal Basin',2115,'','Paleogene','Eocene','Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,40,1,1,'Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'600',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1296,1297,'Seismic interpretation only.\nRef. 1297 cites only Paleogene age.\nHydrocarbon prospect.',21,88,-29467,8921928,'India','Asia',501,'',21.4167,88,'','',3.81318741981,76.7777667683,3.81318741981,76.7777667683,0.745628982638,77.6374416968),('Monzhukly, Nebit Dag, Turkmenia',2116,'Tyusmergenskaya','Jurassic','Upper Jurassic','Kimmeridgian-Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,150,1,1,'Seismic data available ',1,'True reef','3','101-500 m thick','250',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1298,1299,'Seismic interpretation only.',39,54,5065788,5120807,'Turkmenistan','Asia',NULL,'2114',39.3167,54.45,'','',34.1294883541,61.896478461,34.1294883541,61.896478461,35.8300617394,66.0010563406),('Monzhukly, Nebit Dag, Turkmenia',2117,'','Cretaceous','Lower Cretaceous','Berriasian',139.80,145.00,22,'late Tithonian - early Valanginian',141,143,1,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1298,1299,'Seismic data only.',39,54,5092068,4832680,'Turkmenistan','Asia',NULL,'1794',39.2833,54.4167,'','',32.6776072671,62.4849691992,32.6776072671,62.4849691992,35.2011709673,65.5504277036),('Monzhukly, Nebit Dag, Turkmenia',2118,'','Cretaceous','Lower Cretaceous','Neocomian',133.00,145.00,23,'late Valanginian - early Aptian',126,140,1,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1298,1299,'Two major reef cycles:\nBerriasian-Hauterivian and\nHautervian-Barremian',39,54,5091029,4712535,'Turkmenistan','Asia',NULL,'1794',39.2833,54.4167,'','',32.4955880896,62.7621670226,32.4955880896,62.7621670226,34.970694376,65.348950361),('CLA-111, Lake Maracaibo',2119,'','Cretaceous','Lower Cretaceous','middle Aptian-Cenomanian',93.90,125.00,24,'late Aptian - middle Cenomanian',107,107,2,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','15','Non-rudist bivalves','5','Rudists','47','Bivalves (mostly oysters) - algae (microbes)',NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite',NULL,'','0','',2,'Actual reservoir',1301,0,'Outer carbonate platform setting.\nPelecypod biostromes with rudists and/or oysters.\nUp to 15 % porosity and 8 md permeability.\nCogollo Group.\nWell data.',9,-71,-251603,-4808084,'Venezuela','South America',201,'',9.75,-71.5,'','',1.42836516062,-37.5477192643,1.42836516062,-37.5477192643,4.87746991802,-44.9735928211),('La Paz Field, Maracaibo',2120,'','Cretaceous','Lower Cretaceous','middle Aptian-Cenomanian',93.90,125.00,24,'late Aptian - middle Cenomanian',107,107,2,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150','2119',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','15','Non-rudist bivalves','5','Rudists',NULL,NULL,NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite',NULL,'','0','',2,'Actual reservoir',1301,0,'see reef 2119',10,-72,-122941,-4862956,'Venezuela','South America',201,'',10.6833,-72,'','',2.2488970564,-38.2113201611,2.2488970564,-38.2113201611,5.70716612927,-45.6281420608),('Mishrif reef trend, off Abu Dhabi',2121,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,94,2,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','1279',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1302,0,'See reef 1223.\nWas Cenomanian/Turonian',25,54,-80306,4964151,'United Arab Emirates','Asia',NULL,'',25.0833,54.9167,'','',3.62388773758,49.3596411272,3.62388773758,49.3596411272,0.0271324175732,43.9598799799),('Mishrif trend, off Abu Dhabi',2122,'','Cretaceous','Upper Cretaceous','Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,94,2,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','1279',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1302,0,'See reef 2123.\nWas Cenomanian/Turonian',24,54,-108688,4919198,'United Arab Emirates','Asia',NULL,'',24.8333,54.5,'','',3.42490507232,48.9518954649,3.42490507232,48.9518954649,-0.154822844844,43.5450127562),('Fateh Field, Mishrif trend, off Abu Dhabi',2123,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,95,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'300','1279',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1302,1385,'Coarse shell beds more common than true reefs.\nLow relief rudist coppices. \nRadiolitids dominate rudist fauna. Caprinids and monopleurids also common. Chondrodonta present.\nCladophyllia (small branching coral) in reef core.\nExtremely high sediment production.\n20-30 % porosity. 50 md permeability in average.',25,54,-34584,4916089,'United Arab Emirates','Asia',NULL,'',25.3667,54.4,'','',3.96557393177,48.9320249507,3.96557393177,48.9320249507,0.386202731523,43.5477212073),('Mishrif reef trend, off Abu Dhabi',2124,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,95,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','1279',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1302,0,'',25,53,-40043,4841368,'United Arab Emirates','Asia',NULL,'',25.25,53.6667,'','',3.93862149869,48.2578509741,3.93862149869,48.2578509741,0.387542460463,42.8745965892),('Mishrif reef trend, off Abu Dhabi',2125,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,94,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','1279',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1302,0,'Was Cenomanian/Turonian',24,53,-118277,4825057,'United Arab Emirates','Asia',NULL,'',24.6667,53.5833,'','',3.37107474988,48.1031121092,3.37107474988,48.1031121092,-0.17293240225,42.6962031284),('Ardengost, Pyreneans',2126,'','Carboniferous','Middle Carboniferous','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,324,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'3',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','35','Chaetetids - corals - cyanoyphyceans - algae - (bryozoans)',NULL,NULL,'60','30','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1304,1826,'Massive limestones with Mudstones, Wackestones, boundstones and some grainstones.\nCrinoids, Bryozoans, chaetetids and massive or branching corals (heterocorals, rugose corals).\nDiverse algae and microbes described.',42,0,-1798738,1143389,'France','Europe',331,'',42.9333,0.4667,'WAHR','76632',-29.2360496677,5.14230215809,-29.2360496677,5.14230215809,-16.7210279815,-16.6550194602),('Mukhroh well, Hais',2127,'','Jurassic','Upper Jurassic','Upper Jurassic',145.00,163.50,21,'late Bathonian - early Tithonian',151,155,1,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1307,0,'A single coral (Stylina lortphilippsi) described from limestone.',11,48,-1877136,3944240,'Somalia','Africa',709,'',11.1667,48.9167,'','',-24.1293096208,40.4355862014,-24.1293096208,40.4355862014,-20.9700516363,36.2866009931),('Mukhroh well, Hais',2128,'','Paleogene','Eocene','Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,40,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1307,0,'Description of some corals only.',11,46,409953,4359847,'Somalia','Africa',709,'',11.1667,46.9167,'WAHR','71064',4.54877738649,40.7667781414,4.54877738649,40.7667781414,11.1667,46.9167),('Geba Geba',2129,'','Paleogene','Eocene','Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,40,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1307,0,'',3,44,-637629,4041897,'Somalia','Africa',709,'',3.5333,44.05,'WAHR','71063',-3.14103310626,38.0800647847,-3.14103310626,38.0800647847,-3.8992169742,38.1973469164),('Dubino',2130,'','Paleogene','Oligocene','Oligocene',23.00,33.90,30,'Chattian - Aquitanian',22,28,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1307,0,'Limestone with diverse corals (11 species described) from one locality. 15 miles SSW of Berbera.',10,44,1074851,4496237,'Somalia','Africa',709,'',10.2333,44.8833,'WAHR','71062',6.64753055107,40.629055695,6.65003799702,40.6310621973,5.25667457767,41.1140929125),('Minkowice, Lublin Basin',2131,'','Carboniferous','Middle Carboniferous','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,324,3,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick','35',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate',4,'Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'60','0','40',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',2821,1308,'Waulsortian type mud mound with crinoids, fenestrate bryozoan debris and abundant stromatactis. \nMicrobes probably important\n35 m thick.\nin central part of Lublin Basin.',51,22,-63076,2147947,'Poland','Europe',301,'',51.2,22.75,'','',-15.8535981309,14.0261055625,-15.8535981309,14.0261055625,1.00466728843,-4.23126921603),('Sengkang, Sulawesi',2132,'Tacipi','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','270',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1312,1311,'Late Miocene knoll reefs in Sengkang Basin.\nGas producing reservoir.\nOutcrops with predominance of Porites, diverse coralline algae, forams.\nMaximum thickness of buildups 270 m.',-4,120,-551231,13343770,'Indonesia','Asia',614,'1310,1447',-4.1333,120.0333,'','',-3.07996709878,119.210708653,-3.07996709878,119.210708653,-4.51314793781,119.470487256),('Northern Bone Region, Sulawesi',2133,'','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50','2132',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1312,1447,'',-4,120,-601045,13357360,'Indonesia','Asia',614,'',-4.5,120.1833,'','',-3.4462038724,119.36165855,-3.4462038724,119.36165855,-4.878229458,119.624486743),('Palonki, Northern Bone, Sulawesi',2134,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'10',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',1,'Potential reservoir',1312,0,'Only middle Miocene coralgal rudstones in Palongki area.',-4,120,-524189,13496843,'Indonesia','Asia',614,'',-4.4667,120.1722,'','',-3.83595864649,118.170393934,-3.83595864649,118.170393934,-6.97024476112,118.746040265),('Iramu, Papua New Guinea',2135,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,1,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'40',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1313,0,'',-7,144,-2147913,15340699,'Papua New Guinea','Oceania',615,'',-7.6167,144.8667,'','',-14.2174165127,141.608037895,-14.2196721836,141.606816849,-16.3143374525,142.57150576),('Bobrovcek, W Tatra',2136,'','Triassic','Upper Triassic','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,202,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1314,2752,'Two biostromal units (together about 5 m thick).\nDiverse corals (including new genus Meandrostylophyllum), sponges, calcarerous algae and other organisms.\nNo in situ organisms?\n',49,19,4237923,1851076,'Slovakia','Europe',336,'',49.15,19.6,'WAHR','67625',24.9226315492,34.7142236163,24.9226315492,34.7142236163,28.5321609389,28.0860503312),('Ojin Seamount, Emperor Chain, Pacific',2137,'','Paleogene','Paleocene','Paleocene',56.00,66.00,27,'Thanetian - Ypresian',53,61,1,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,2,'Cold - water',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1316,556,'Bryozoans and coralline algae werde recovered. Seismic evidence for bioherms.\nBryozoan-algal mounds?',37,170,3891667,-16388853,'Pacific','Pacific',NULL,'1317',37.9833,170.6,'','',23.6302677215,-147.032557623,23.6302677215,-147.032557623,37.9833,170.6),('Koko Seamount, Pacific',2138,'','Neogene','Miocene','Miocene',5.30,23.00,30,'Chattian - Aquitanian',22,20,1,1,'Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1317,601,'Fossil reef corals dated as 25-30 Ma.',35,171,4157778,-17653617,'Pacific','Pacific',NULL,'',35.5,171.75,'','',32.4163471214,-176.890116842,32.4017566486,-176.791284018,35.5,171.75),('Yuryaku Seamount, Pacific',2139,'','Paleogene','Oligocene','lower Oligocene',28.10,33.90,29,'Priabonian - Rupelian',33,32,1,1,'Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1317,0,'Fossil reef corals dated by Sr-isotopes 34 Ma.',33,171,3671696,-17130414,'Pacific','Pacific',NULL,'',33.45,171.6333,'','',26.8093739596,-165.111765493,26.8093739596,-165.111765493,33.45,171.6333),('Kanmu Seamount, Pacific',2140,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,1,'Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1317,0,'Fossil reef corals dated as 21, 27.7 and 33 Ma.\nSee also reef 2141.',32,173,3713700,-17900792,'Pacific','Pacific',NULL,'',32.1167,173.0833,'','',28.346168319,-171.844904004,28.346168319,-171.844904004,32.1167,173.0833),('Kanmu Seamount, Pacific',2141,'','Paleogene','Oligocene','Oligocene',23.00,33.90,29,'Priabonian - Rupelian',33,28,1,1,'Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1317,0,'See reef 2140',32,173,3489118,-17124589,'Pacific','Pacific',NULL,'',32.1167,173.0833,'','',26.196453099,-165.559122472,26.2009268106,-165.569513634,32.1167,173.0833),('SE-Menorca',2142,'','Neogene','Miocene','Tortonian/Messinian',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'35',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1318,0,'Very pronounced debris production.\nReefal unit situated on rhodalgal ramp.\nPorites and Tarbellastrea sp. and abundant red algae.\nN 17 (upper Tortonian, lower Messinian).',39,4,5285416,320206,'Spain','Europe',304,'',39.8333,4.25,'','',39.614517414,2.38444628467,39.6124093683,2.39250211922,39.4256931213,4.15590172955),('SW-Menorca',2143,'','Neogene','Miocene','Tortonian/Messinian',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'35','2142',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1318,0,'see reef 2142.',39,3,5297755,280625,'Spain','Europe',304,'',39.9333,3.8333,'','',39.674803879,1.95645650193,39.673057253,1.96461038981,39.5302047015,3.74351384111),('Tattsfield, Weald, England',2144,'','Jurassic','Upper Jurassic','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,157,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1320,0,'Early marine peloidal cements important for reservoir quality. \nAverage porosity around 8-10 %.\nLower part of reefs with laminar Thamnasteria and digitate Thecosmilia. Upper part with robust branching Thecosmilia and massive Isastrea.\nStromatolitic crusts present.',51,0,4977262,325232,'United Kingdom','Europe',331,'',51.2833,0.0167,'','',29.0616546588,18.7756462947,29.0616546588,18.7756462947,35.2970149199,19.206752718),('Ballykane',2145,'','Carboniferous','Lower Carboniferous','Courceyan/Chadian',346.70,350.00,11,'late Famennian - early Visean',351,345,2,0,'Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','437',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','3','Microbes','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1322,0,'Individual mounds up to 100 m thick. Waulsortian sequence about 200 m thick.\nCorals very rare but present (tabulates, rugose).',53,-7,-1475287,-367864,'Ireland','Europe',331,'',53.3667,-7.0333,'WAHR','76916',-33.6299374469,-14.6795314993,-33.9804624544,-15.077124948,-3.02642170454,-51.1902707709),('Krachoua',2146,'','Jurassic','Middle Jurassic','upper Callovian',163.50,164.50,21,'late Bathonian - early Tithonian',151,162,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'20','80','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1324,2369,'',32,10,2189960,1056558,'Tunisia','Africa',715,'',32.6333,10.8667,'','',8.41285190372,15.6352592154,8.25384894689,15.4941217716,12.8292158215,14.9331044745),('Tenia Island, New Caledonia, Melanesia',2147,'','Neogene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1325,0,'Belongs to France',-22,166,-3422170,17278337,'New Caledonia','Pacific',NULL,'',-22.05,166.0833,'','',-23.6373079894,165.572336148,-23.6353015883,165.572961064,-24.1947844389,165.975264744),('Kangjia-ping, Cili, Hunan',2148,'Changhsing','Permian','Lopingian','lower Changhsingian',253.00,254.10,16,'Roadian - Changhsingian',261,253,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','57','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,'4',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'60','30','10',0,'no',0,'no','3','25 or more reef building species','27','1','Constructor guild',NULL,'','1','Present','1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1326,1700,'Paleofusulina zone according to ref. 1326\nRef. 1700 states Wuchipangian age.\nRugose coral (Waagenophyllum) reef. 40-50 % of rock is formed by corals. Single colonies up to 1 m high.\nAddtionally sphinctozoans, hydrozoans (?), Tubiphytes, Archaeolithoporella, red algae (Parachaetetes, Solenopora), bryozoans. All of them rare in coral reef core.\nReef 35-57 m thick. \nDolomitization only in west. Paleontological data from eastern sections with many sponges',29,110,-208302,9245067,'China','Asia',602,'',29.4,110.9333,'WAHR','24247',-11.1796212464,109.164422438,-11.4597761613,108.896337253,9.41548314187,128.373640223),('Mole Creek, Tasmania',2149,'Den','Ordovician','Upper Ordovician','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,449,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','50','20',0,'no',0,'no','2','6 to 24 reef building species','15','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1328,0,'Original age call: Caradocian-Ashgillian\nSmall coral-stromatopore bioherms in Den Formation (Gordon Group).\nTabulate (favositid, heliolitid, halysitid) corals, rugose (solitary and compound) and diverse stromatopores (10 species assigned to 2 morphotypes) are important.\nSome bioherms dominated by stromatopores, others by corals (mostly tabulates).\nEnvironment characterized as outer platform, but fitting to ramp as well.',-41,146,1101831,19761258,'Australia','Oceania',801,'',-41.55,146.4,'WAHR','24252',5.02919802392,119.766356745,5.02919802392,119.766356745,5.02919802392,119.766356745),('Houshan, Guilin, Guangxi',2150,'Yonghsien','Devonian','Upper Devonian','early Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,383,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','8','1','Less than 10 m wide',NULL,'1','Less than 20 m','30',NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild',NULL,'','1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1329,1866,'Western margin of Guilin platform.\nCoral bafflestone reef behind an algal-stromatoporoid platform margin reef. Composed exclusively of rugose coral Smithiphyllum ( 3 species). Brachiopods as dwellers. Some solenoporacean fragments. \n-> Collection of Miller\n\nCoral bioherm (Smithiphyllum) 8 m thick and 30 m wide. Base is Stromatactis limestone, top is peloidal packstone followed by receptaculid-algal limestone.\n\nRef:. 1866:\nReef complex with \n\'Algal\'-stromatoporoid reef\nreceptaculid-algal reef\nSmithiphyllum bioherm\nalgal mounds\n\n30 m exposed thickness.\nLateral differentiation into back-reef, reef flat and margin, margina fore-slope.\nStachyodes most abundant in reef flat.\nCalcimicrobes prevail in reef-slope: Renalcis, Epiphyton, Rothpletzella\nCavities and veins filled with radiaxial-fibrous calcites',25,110,-1173370,10732529,'China','Asia',602,'',25.2833,110.2333,'WAHR','5769',-15.4144968489,87.819118602,-15.4144968489,87.819118602,-14.3494970032,111.885266175),('Laliderer Tal',2151,'','Triassic','Middle Triassic','upper Anisian',242.00,247.20,17,'Induan - early Carnian',235,239,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1331,0,'Earliest small buildups in Northern Alps.\nHomoclinal ramp setting.',47,11,2315069,1999180,'Austria','Europe',301,'',47.4167,11.4667,'WAHR','45426',15.8932170284,36.4303784251,15.8932170284,36.4303784251,10.681959581,26.1391037272),('Xifeng-Kaiyang, Guizhou',2152,'Doushantuo','Ediacaran','Middle Ediacaran','middle Ediacaran',541.00,635.00,0,'Vendian',605,570,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m','100','40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1333,0,'Phosphatic stromatolitic bioherms: 1 m thick, up to 100 m wide.\n',27,107,4950155,15003755,'China','Asia',602,'',27,107.35,'','',29.8785593793,52.7775748189,29.8785593793,52.7775748189,29.8785593793,52.7775748189),('Maurice Ewing Bank, South Atlantic',2153,'','Cretaceous','Lower Cretaceous','Lower Cretaceous',100.50,145.00,23,'late Valanginian - early Aptian',126,135,1,1,'Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,2,'Cold - water',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1336,0,'Seismic evidence for a succession of carbonate buildups.\nAge Jurassic/Cretaceous, most probably early Cretaceous.',-50,-46,-7310569,123496,'Atlantic','Atlantic',NULL,'',-50.5,-46.8333,'','',-55.4160657927,-4.95113666419,-55.4160657927,-4.95113666419,-52.0384972761,-11.2689808586),('Globocec',2154,'','Jurassic','Lower Jurassic','Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,187,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','7',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'10','90','0',0,'no',0,'no','1','Less than 6 reef building species','1','2','Baffler guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1337,0,'5 m and 7 m thick intervals with rock-forming Cochlearites.',45,14,4138384,1947844,'Slovenia','Europe',328,'',45.8833,14.85,'WAHR','34668',18.8258449228,28.8621493114,18.8258449228,28.8621493114,25.0588897091,32.8986687012),('Inhoca',2155,'','Cretaceous','Upper Cretaceous','Upper Cretaceous',66.00,100.50,26,'middle Campanian - Danian/Selandian',75,70,1,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,2,'Cold - water',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1338,0,'Ostrea bank. Oysters with abundant borings.',-25,32,-5059258,2121828,'Mozambique','Africa',NULL,'',-25.2667,32.3833,'','',-38.4538353087,23.7977498449,-38.4538353087,23.7977498449,-39.1378814985,17.6716596382),('Albenza, Southern Alps',2156,'Calcare di Zu','Triassic','Upper Triassic','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,202,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m','8','1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','1','Corals','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','22','1','Constructor guild',NULL,'','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1340,2280,'3 m thick, 8 m wide patch reef. \nLithocodium and Bacinella bindstone at base. \nThen coral-dominated reef with solenopraceans, tabulozoans, \'sphinctozoans\' and some hydrozoans. \nStongly encrusted by Lithocodium and Bacinella.\nMicritic groundmass.\n\nRef. 1340:\nAlternations of marine and meteoric diagenetic conditions, most probably caused by relative sea level fluctuations, are recorded in an Upper Triassic (Rhaetian) patch reef in the Calcare di Zu Formation, Lombardian Basin. Three main types of cements have been distinguished: 1) isopachous fibrous calcite cement, partially to completely filling mostly secondary solution cavities; 2) radial-fibrous calcite cement in which strongly turbid relics of precursor fibrous cements suggesting a neomorphic origin can be observed, and 3) equant spar calcite found both as a last cement occluding the remaining void space after the cementation by the fibrous cements and as a neomorphic product in corals.\nBoth marine and non-marine internal sediments are present in the patch reef. The marine internal sediments are composed of fecal pellets, peloids, micrite and bioclasts. They could be precedent, successive or contemporaneous to the isopachous marine cement and could have a geopetal disposition or may completely fill cavities. The observations made indicate that a \'peloidal texture\' (a nucleus of anhedral HMC crystals from which fibrous crystals radiate) could result from the introduction of peloids/fine-grained micritic intraclasts into fibrous marine cements during their growth.\nThis texture has not been observed in geopetal infill peloids. Non marine internal sediments are composed of crystal silts and their deposition was preceded by the partial dissolution of the isopachous fibrous cements. ',45,9,2922905,1565103,'Italy','Europe',344,'',45.7722,9.4819,'WAHR','27537',27.5616627174,26.7408761459,27.5616627174,26.7408761459,23.8132295755,25.2057866985),('W-Bengal Basin II',2157,'','Paleogene','Eocene','Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,40,1,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'600','2115',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1297,0,'See reef 2115 for remarks.',21,87,-1070053,8724296,'India','Asia',501,'',21,87.8333,'','',3.42186635516,76.5660183902,3.42186635516,76.5660183902,0.363739944895,77.4095015758),('W-Bengal Basin III',2158,'','Paleogene','Eocene','Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,40,1,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'600','2115',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1297,0,'See reef 2115 for remarks.',20,87,-76163,8717159,'India','Asia',501,'',20.4167,87.4167,'','',2.89848985589,76.0982208062,2.89848985589,76.0982208062,-0.138950519733,76.9202207668),('Annan Seamount, Atlantic Ocean',2159,'','Paleogene','Lower Paleogene','Paleocene/Eocene',33.90,66.00,27,'Thanetian - Ypresian',53,55,1,1,'Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','10','60','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1342,0,'Dredged material with corals, crustose coralline algae, bryozoa, molluscs and larger forams.\n\nAbstract of ref. 1342:\nPhosphatidized bioclastic limestomes of Early Tertiary age were dredged from the crest of a seamount in the equatorial Atlantic. The samples were recovered from water depths of 700-970 m but clearly were deposited in a high-energy reefal environment, thus indicating significant Tertiary subsidence. The vertical movement probably reflects reactivation of an old structural line, the Guinee Fracture Zone, which may have had important effects on the transfer of bottom waters of polar origin between the Sierra Leone and Gambia basins. Examination of foraminiferal limestone coating the shallow water material suggests that deep-water conditions were established on the seamount by Middle Miocene time. All phosphatized samples are covered with a layer of ferromanganese oxides which, from textural and faunal evidence, is Paleocene or Eocene in age and of shallow water origin. Pervasive phosphatiziation of the bioclastic limestones probably was accomplished before the end of the Eocene while the crest of the seamount was near sea level, because Upper Eocene limestone of shallow water facies is unaffected by such radical diagenesis. Phosphatization probably was associated with vigorous upwelling near the seamount and has been taken to an unusually advanced stage, resulting in a phosphorite of high economic grade. P2O5 contents are in the range of 37-41%. The purity of the phosphorites may be related to the intensity of upwelling during the Early Tertiary, but other factors such as the paucity of terrigenous detritus, frequent reworking of the sedimentary capping of the seamount, and a high primary porosity of the limestones may have been important in their formation. The Early Tertiary period of phosphorite deposition on the seamount and in northwest Africa ended before the close of Eocene time in both areas, while shallow water conditions prevailed. The cessation of phosphorite formation probably reflects major changes in the surface circulation of the Atlantic during the Eocene. ',9,-21,794671,-2926929,'Atlantic','Atlantic',NULL,'',9.0236,-21.0403,'','',4.30865872692,-26.4354715169,4.30865872692,-26.4354715169,9.0236,-21.0403),('Annan Seamount, Atlantic Ocean',2160,'','Paleogene','Eocene','Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,40,1,1,'Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1342,0,'Abstract ref. 1342:\nPhosphatidized bioclastic limestomes of Early Tertiary age were dredged from the crest of a seamount in the equatorial Atlantic. The samples were recovered from water depths of 700-970 m but clearly were deposited in a high-energy reefal environment, thus indicating significant Tertiary subsidence. The vertical movement probably reflects reactivation of an old structural line, the Guinee Fracture Zone, which may have had important effects on the transfer of bottom waters of polar origin between the Sierra Leone and Gambia basins. Examination of foraminiferal limestone coating the shallow water material suggests that deep-water conditions were established on the seamount by Middle Miocene time. All phosphatized samples are covered with a layer of ferromanganese oxides which, from textural and faunal evidence, is Paleocene or Eocene in age and of shallow water origin. Pervasive phosphatiziation of the bioclastic limestones probably was accomplished before the end of the Eocene while the crest of the seamount was near sea level, because Upper Eocene limestone of shallow water facies is unaffected by such radical diagenesis. Phosphatization probably was associated with vigorous upwelling near the seamount and has been taken to an unusually advanced stage, resulting in a phosphorite of high economic grade. P2O5 contents are in the range of 37-41%. The purity of the phosphorites may be related to the intensity of upwelling during the Early Tertiary, but other factors such as the paucity of terrigenous detritus, frequent reworking of the sedimentary capping of the seamount, and a high primary porosity of the limestones may have been important in their formation. The Early Tertiary period of phosphorite deposition on the seamount and in northwest Africa ended before the close of Eocene time in both areas, while shallow water conditions prevailed. The cessation of phosphorite formation probably reflects major changes in the surface circulation of the Atlantic during the Eocene.',9,-21,890117,-2885811,'Atlantic','Atlantic',NULL,'',9.0236,-21.0403,'','',5.19655852256,-26.2393418856,5.19655852256,-26.2393418856,9.0236,-21.0403),('Ilych River, Pechora',2161,'','Silurian','Ludlow','Ludlovian',423.00,427.40,7,'Wenlock - early Pridoli',425,421,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','40','3','101-1000 m wide',NULL,'4','More than 1000 m','9000',NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','3','Microbes','66','Stromatolites-\'sphinctozoans\'-(stromatoporoids, algae, corals)',NULL,NULL,'80','10','10',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1344,1345,'Up to 40 m thick, 120 m wide. Up to 500 m thick according to ref. 1420.\nLate Wenlockian microbial mound (70 m) and Ludlovian framework with tabulate and branching rugose corals, stromatoporoids, bryozoans and microbes).\nDiverse stromatolite forming calcified microbes:\nEpiphyton, Girvanella, Wetheredella, Rothpletzella, Hecetaphyton ...\nOnly abundant metazoan are aphrosalpingid sphinctozoan sponges.\nHigh energy platform margin setting.\nRef. 2268: This reef shed vast amounts of allochthonous sediments to the adjacent submarine slope',62,58,796259,446122,'Russia','Asia',624,'1420, 1973, 2268',62.5,58.4167,'WAHR','24017',21.4797960282,-41.6676586853,21.4797960282,-41.6676586853,21.4797960282,-41.6676586853),('Kozhym River, Pechora',2162,'','Silurian','Ludlow','Ludlovian',423.00,427.40,7,'Wenlock - early Pridoli',425,421,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','6','Calcisponges','66','Stromatolites-\'sphinctozoans\'-(stromatoporoids, algae, corals)',NULL,NULL,'10','80','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1344,1345,'',65,60,1075042,169543,'Russia','Asia',624,'1420',65.5833,60.4167,'WAHR','80710',22.5719040596,-44.9179518427,22.5719040596,-44.9179518427,22.5719040596,-44.9179518427),('Niyayu, Pechora',2163,'','Silurian','Ludlow','Ludlovian',423.00,427.40,7,'Wenlock - early Pridoli',425,421,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','360',NULL,NULL,NULL,'4','More than 1000 m',NULL,'13',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'20','70','10',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1344,1345,'360 m thick reef.\nMain framework builders: Fistulella (problematic hydrozoan), stromatoporoids (Clatrodyction, Columnostroma), rugose corals, Spongophylloides, Zelolasma, Aphyllum, Solenopora, Parachaetetes, Renalcis, Epiphyton, Girvanella, Ikella. \n\nRich in brachiopods',66,63,1308092,102712,'Russia','Asia',624,'1420, 1973',66.75,63.8333,'','',23.9674423639,-46.1677444148,23.9674423639,-46.1677444148,23.9674423639,-46.1677444148),('Finnmark Platform, Barents Sea',2164,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','160',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate',4,'Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1346,0,'Microbial boundstones predominate. Packstone matrix with bryozoans, crinoids, Tubiphytes and forams. Stromatactis limestones at base, bryozoan-cement framestones at top.\n160 m interval cored. Buildup flank with up to 45° dip angle.\nCement alone forms around 46 % of buildup volume.\n38 % biogenic particles.\n16 % overall micrite (including microbially induced).',72,29,4283401,2182704,'Norway','Europe',301,'',72.2158,29.635,'','',29.6640937573,20.7080533043,29.6640937573,20.7080533043,29.0325880064,-5.41245027875),('Finnmark Platform, Barents Sea',2165,'','Permian','Lower Permian','Artinskian',283.50,290.10,15,'Sakmarian - Kungurian',277,280,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','160',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate',4,'Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','3','Microbes','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1346,0,'See reef 2164 for remarks',72,29,4908420,2431081,'Norway','Europe',301,'',72.2158,29.635,'','',30.3448167663,21.2386483091,30.3448167663,21.2386483091,31.7499717864,3.39577104307),('Ardmore, Oklahoma',2166,'','Carboniferous','Upper Carboniferous','Morrowan',315.00,323.20,13,'Bashkirian - Kasimovian',302,316,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','14','Brachiopods','14','Brachiopods',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1347,0,'Small patch reef formed by an richthofenoid ancestor.\n',34,-97,-720944,-3450001,'United States','North America',101,'',34.1667,-97.2167,'WAHR','76485',-24.8999773061,-58.7846409291,-15.0142245501,-40.8400797168,-12.6903425021,-56.7349037423),('Lopushna',2167,'','Jurassic','Upper Jurassic','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,153,1,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'250','1713',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1348,1424,'Abstract ref. 1348:\nUpper Jurassic (Oxfordian-Tithonian) reef-bearing carbonates are developed throughout the Ukrainian part of the Carpathian foredeep. These occupy an up to 50-km-wide area in which they attain thicknesses of 500-1000 m, occur at depths ranging between 1 and 7 km, and are covered Early Cretaceous to Miocene sediments. Upper Jurassic strata can be differentiated into reef-core, pre-reef, and back-reef facies.\nReservoir development occurs in the karstified, crestal parts of reefs (e.g., Kakhanovka and Letnya fields) and also in detrital back-reef carbonates (Rudky and Lopushnya fields). The potential of this oil and gas play is not yet exhausted, particularly in the area of back-reef facies development under the Carpathian thrust sheets.\nReservoir prediction is difficult due to insufficient core control and therefore is based on sedimentological log analyses. Different facies types are characterized by consistent well-log parameters, including shale content, primary and secondary carbonate texture, structure of associated lithotypes, etc. Different facies types can be correlated with characteristic log parameters. Nine facies types are recognized according to the scheme of J. L. Wilson. This opens the possibility to construct regional facies maps, to trace in time and space the development of the actual reef belt, and thus to enhance reservoir prediction. Sedimentological log analysis, combined with seismic criteria, proved to be an effective tool in the analysis of carbonate prospects, as evidenced by the discovery o the genetically unique Lopushnya field.\nRegional paleosedimentological reconstructions of the Upper Jurassic basin form the basis for evaluating the remaining hydrocarbon potential of the back-reef facies domain in the Ukrainian part of the Carpathian foredeep and the adjacent Romanian territory.',48,25,5163659,2325701,'Ukraine','Europe',301,'',48.0833,25.3333,'','',31.7814916193,35.9959959021,31.7814916193,35.9959959021,36.3936453641,38.618946782),('Rudky',2168,'','Jurassic','Upper Jurassic','Kimmeridgian-Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,150,1,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'250','1713',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1348,1424,'Gas field.\nOxfordian Rudky reefs and Kimmeridgian-Tithonian (Oparian) barrier reefs.',49,23,5307247,2118477,'Ukraine','Europe',301,'',49.6667,23.75,'','',33.4780340891,32.9280210139,33.4780340891,32.9280210139,37.9869495879,35.9777134959),('Tiout',2169,'Amouslek','Cambrian','Lower Cambrian','lower Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','90',NULL,NULL,NULL,'3','More than 100 m',NULL,'40','1762',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species',NULL,NULL,'',NULL,'',NULL,'','2','Medium zonation',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1351,1444,'The lower Atdabanian Amouslek-Tazzemourt-Tiout\nreef barrier.\nArchaeocyathid-bioherm facies laterally grading into oolitic limestones.\nRelatively diverse archaeocyathid assemblage.\nSeries of small kalyptrae (Individually up to 10 m) in open shelf shales. Tiout Member of Amouslek Fm.\nIncludes data from Tazemmourt section 30°23°N/\n08°48°W.',30,-8,-6951229,7878771,'Morocco','Africa',714,'2534, 2844',30.3833,-8.6833,'WAHR','80878',-74.3514307687,-23.0736276401,-74.3514307687,-23.0736276401,-74.3514307687,-23.0736276401),('Ounein, Lemdad Syncline, High Atlas',2170,'Lemdad','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1351,2571,'Several archaeocyath-microbe bioherm levels.\nRegular volcaniclastic influx\nRadiometric dates available (517 Ma)',30,-8,-6887202,7946843,'Morocco','Africa',714,'2844',30.8,-8.2583,'WAHR','80850',-74.6204562548,-25.5570419189,-75.2126197446,-31.9837157965,-75.2126197446,-31.9837157965),('Kur-Teke, Pamir, Tadzhikistan',2171,'','Permian','Upper Permian','Murgabian-Dzhulfian',265.10,268.80,16,'Roadian - Changhsingian',261,262,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','80',NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','4','Stromatoporoids','2','Algae','8','Coralline sponges (chaetetids) - microbes - corals','4','Others','20','80','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1353,0,'Massive hydrozoan-algal reefal limestones. 35-80 m thickness.\nDiverse rugose corals in Murgabian and Djulfian.',37,74,-1301474,6439091,'Tajikistan','Asia',301,'',37.8333,74.25,'','',23.1993871962,82.261351154,23.1993871962,82.261351154,-17.0628445818,67.9639910778),('Igualada, Ebro Basin',2172,'','Paleogene','Eocene','Lutetian-Bartonian',38.00,47.80,28,'Lutetian - Bartonian',45,40,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','11',NULL,NULL,NULL,'2','10 - 100 m','50',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species','44','1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1354,0,'Fringing reefs interfingering with deltaic deposits.\n43 coral species (35 genera).\nSlightly more than 10 m thick, 50 m wide.',41,1,5105547,-66018,'Spain','Europe',304,'',41.5833,1.6,'WAHR','69638',37.6705004333,-2.53849631016,37.6705004333,-2.53849631016,40.0254168134,1.32660851464),('Luguan, Xinhua, Hunan',2173,'','Devonian','Middle Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,3,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',1355,0,'Restricted platform facies with dominant Amphipora.\n\nAbstract of ref. 1355:\nDevonian reefs in Hunan were developed in the late Givetian and early Frasnian. Most reefs have been discovered in the area of carbonate platform facies and regarded as biostromes or patch reefs. Rare oil shows have been found in these kinds of reefs. Some so-called \'reef mounds\' have abundant oil shows, but they have been considered to have developed only on a few elevated blocks in the area of inter-platform depressional facies. Based on research on reef distribution and characters of sedimentography and paleoecology, this paper proposes that many so-called \'biostromes\' are not layered but instead are narrow along the edges of platforms as barrier reefs. Some \'reef mounds\' are only the upper parts of barrier reefs, which extended towards the depressional facies area and were broken by faults. If this is true, they will be found along the edges of platforms and are not restricted within narrow limits. Because these parts of the reefs are preserved in the black shales and have fine oil shows, great attention should be paid to them in oil exploration.',27,111,-1529801,10658979,'China','Asia',602,'',27.7667,111.1667,'','',-17.3793496042,87.3940099887,-17.3793496042,87.3940099887,-14.6146245822,107.686763271),('Putou, Chengbu, Hunan',2174,'','Devonian','Middle Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',1,'Potential reservoir',1355,0,'Barrier type reef with black shales in fore reef.\nOnly stromatoporoid-coral community observed. Domination stage.\nReef rests directly on black shales, without intercalation of bioclastic limestones.\nFew for reef talus.\nSee reef 2173 for more remarks.',26,110,-1314314,10735907,'China','Asia',602,'',26.3333,110.3,'','',-15.7704772406,87.6536552303,-15.7704772406,87.6536552303,-14.9522947484,109.333894041),('Perán-Carranques, Cantabria',2175,'Candás and Portilla','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,'50','1613',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','3','25 or more reef building species','26','1','Constructor guild','1','Present',NULL,'',NULL,'','3','Pronounced zonation',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1356,1595,'26 reef building taxa described. Corals (especially tabulates) dominant in framework facies. 15 genera of rugose corals (mostly solitary).\nUp to 15 m thick massive reefs in shallowing upward sequence. Proximal carbonate ramp. \nSmall and scarce macroborers evident on plates of ref. 1595.\n\nAbstract of ref. 1595:\nFrom four outcrops of the Portilla Fm. and one outcrop of the Candas Fm. in the W Cantabrian Mountains 17 species and subspecies of solitary and phaceloid rugose corals are described. They belong to 15 different genera. The stratigraphical classification of four of the localities in question as Upper  Givetian is confirmed by means of the identified coral faunas, and this age is also probable for the fifth locality. The rugose coral genera BREVISEPTOSIA n. gen. and SINAXIS n. gen. are erected in this paper; moreover the following 13 new species and subspecies are described and figured: Schindewolfia plena n. sp., Neaxon variabilis n. sp., Catactoechus bonarensis n. sp., Metrionaxon transitorius n. sp., Famennelasma antiquum n. sp., Breviseptosia pulchra n. gen. et n. sp., Sinaxis bulbosa n. gen. et. n. sp., Cyathophyllum (C.) postarduum n. sp., Thamnophyllum caespitosum leonense n. ssp., Acanthophyllum confusum n. sp., Stringophyllum buechelense cantabricum n. ssp., Stringophyllum crassimarginatum n. sp. and Solipetra fontainei n. sp. The number of genera and species of the normally ahermatypic classified small solitary corals without dissepimentarium is unusually great with respect to the  reef facies of the Portilla Formation. A part of them even occurs together with compact flat colonies of back reef corals of the \'reef  meadows\' or even together with large solitary corals. So we have to assume that the \'Portilla environment\' of the investigated localities was characterized by a very narrow-spaced irregular morphological pattern of its sea bottom. ',43,-5,-3429404,1267837,'Spain','Europe',304,'2321',43.5833,-5.7333,'WAHR','27605',-29.0306971649,-1.54663698118,-29.0306971649,-1.54663698118,-9.21243184235,-37.4038844209),('Ardagh Quarry, Kingscourt',2176,'Mullaghfin','Carboniferous','Lower Carboniferous','late Asbian-Brigantian',331.00,338.00,12,'middle Visean - Serpukhovian',329,332,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','95',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'90','0','10',0,'no',0,'no','2','6 to 24 reef building species','16','2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation','3','More than 60% micrite',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1357,0,'95 m thick micritic buildup with abundant brachiopods, bivalves, blastoids - dominated by colonial rugose corals at the top (together with bryozoans, algae, forams).\n74 % colonial, 26 % solitary Rugosa.\n16 species, 10 genera\nFauna similar to, but less fragmented than coeval platform facies.',53,-6,-449329,171258,'Ireland','Europe',331,'',53.9,-6.7167,'WAHR','73468',-29.8789005822,-11.5754901639,-25.7662876536,-8.96942065091,-4.91774913474,-31.5092562712),('Partizansk, South Primorye',2177,'','Jurassic','Lower Jurassic','Hettangian?',199.30,201.30,19,'late Hettangian - early Aalenian',188,198,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'','1','Corals','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','4','Others','0','100','0',0,'no',0,'no','1','Less than 6 reef building species','3',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1359,0,'Hettangian bioconstructions of corals, some algae and sphinctozoans.\nOnly Anabacia and Montlivaltia',43,133,4887400,14140219,'Russia','Asia',624,'',43.1667,133.1667,'WAHR','40404',56.5199404114,165.056836908,56.5199404114,165.056836908,48.5676558673,161.043209148),('Sacharnaja Golova, South Primorye, Sichote-Alin',2178,'','Triassic','Upper Triassic','lower Carnian',233.00,235.00,17,'Induan - early Carnian',235,226,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','9',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1359,131,'Reef-like coral communities with Margarophyllia, Margarosmilia, Pachysolenia, Palaeastraea, Protoheterastrea, Stylophyllopsis, Volzeia.\nSphinctozoan Sollasia',44,134,4301535,14457589,'Russia','Asia',624,'',44.5,134.5,'WAHR','36691',29.0636890967,142.611600088,29.0636890967,142.611600088,79.1741178443,166.701047791),('Hembrillo Canyon, San Andres Mts., New Mexico',2179,'Panther Seep','Carboniferous','Upper Carboniferous','Virgilian-Wolfcampian',290.00,303.70,14,'Gzhelian - Asselian',290,299,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','34','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,'4',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','2','Algae','3','Microbes','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'','1','Present',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',1364,2239,'Maximum thickness 34 m.\nPhylloid algae, coquinoid fusulind lenses, brachiopods and crinoids are present.\nRef. 2239 describes abundant dasycladaceans and tubular forams in addition to phylloids. \nMicrobes concluded from common peloids\nCoated grains!\nTwo horizons with bioherms.\nMassive cementstones form base of buildups.\nUp to 7% porosity',32,-106,-239657,-4247159,'United States','North America',101,'',32.8333,-106.5667,'','',1.17131826251,-36.3678806016,1.17131826251,-36.3678806016,-2.29257680682,-56.9911231948),('Montezuma, New Mexico',2180,'','Carboniferous','Upper Carboniferous','Virgilian',298.90,303.70,13,'Bashkirian - Kasimovian',302,302,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','8',NULL,NULL,NULL,'3','More than 100 m','133',NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','2','Algae',NULL,NULL,'2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1365,0,'Phylloid algal bank complex. 133 m in length, 8 m in height.',35,-105,679249,-4104754,'United States','North America',101,'',35.9667,-105.2833,'WAHR','49835',2.11927439603,-34.2218615745,2.11927439603,-34.2218615745,-1.01483218743,-57.2316886782),('Miller Creek, Meeker, Colorado',2181,'Minturn','Carboniferous','Upper Carboniferous','Desmoinesian',307.00,315.20,13,'Bashkirian - Kasimovian',302,307,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','7',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','2','Below fair weather wave base','2','Algae','3','Microbes','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',1366,0,'Upper Minturn Formation phylloid algal-mound (about 7 m thick).\nHydrocarbon staining of fractures.\nPhylloid-algal packstone/grainstone.\nFibrous submarine cement.\nIvanovia dominant.\nBesides phylloids, Epimastopora is present.\nAt the base also bryozoans, Girvanella and worm tubes as reef builders.\nCement up to 50 % of buildup.',39,-107,867481,-4176754,'United States','North America',101,'',39.9,-107.7667,'','',0.605778828628,-37.7162963161,0.605778828628,-37.7162963161,2.50957040158,-58.4676296231),('Altoona, Kansas',2182,'','Carboniferous','Upper Carboniferous','upper Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,304,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','16','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1367,0,'Bryozoan reef developed south of a tidal channel.\nEncrusting bryozoans (Meekoporella dehiscens) dominant (10-100 %).\n16 species, 7 genera among the 4 common Paleozoic orders.\nTermination of growth by grainstone sedimentation.',37,-95,-425350,-3139196,'United States','North America',101,'',37.5167,-95.7,'WAHR','76892',-3.04732567173,-28.2941620776,-3.04732567173,-28.2941620776,-4.49132487532,-51.4173824453),('L\'Original, Ottwa Valley, Ontario',2183,'Pamelia','Ordovician','Upper Ordovician','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,457,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','5','1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','8','Serpulids, worms, vermetids','3','Microbes','44','Worms - microbes - (forams) - (bryozoans) - (corals)',NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species','2','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1369,0,'Blackriverian tubicolous build-ups.\nDune shaped-mounds composed of Tymbochoos (suspension feeding polychaet). Microbes associated (abundant where abundance of Tymbochoos decreases).  Rare other fossils (bryozoa, bivalves).\n48 mounds in area.\nUp to 5 m length and 0.5 m thickness.\nBuildups on oolites either in intertidal channels or shallow subtidal shoals.',45,-74,-2848317,-4987263,'Canada','North America',121,'',45.6167,-74.7,'WAHR','61432',-7.72339312183,-100.442573355,-15.0113970364,-103.491514322,-15.0113970364,-103.491514322),('Dunrobin, Ottwa Valley, Ontario',2184,'Pamelia','Ordovician','Upper Ordovician','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,457,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','8','Serpulids, worms, vermetids','3','Microbes','44','Worms - microbes - (forams) - (bryozoans) - (corals)',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species','2','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1369,0,'See reef 2183 for remarks.',45,-76,-2810668,-5099219,'Canada','North America',121,'',45.45,-76.0667,'WAHR','61434',-7.27226266276,-101.31069197,-14.6709484621,-104.433096793,-14.6709484621,-104.433096793),('Braeside, Ottwa Valley, Ontario',2185,'Lowville','Ordovician','Upper Ordovician','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,457,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','8','Serpulids, worms, vermetids','3','Microbes','44','Worms - microbes - (forams) - (bryozoans) - (corals)',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species','2','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1369,0,'See reef 2183 for remarks.\nBlackriverian',45,-76,-2794229,-5124529,'Canada','North America',121,'',45.4667,-76.4,'WAHR','61435',-7.11452835221,-101.485429704,-14.535767373,-104.630958707,-14.535767373,-104.630958707),('Rübeland, Harz',2186,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','80',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',4,'Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','4','Microbial precipitation',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1370,0,'Thrombolitic mudstones, spar layers, stromatolites.\nHexactinellid sponges as only macrofossils.\n80 m thick, 260x150 m lateral extension.',51,10,-2242323,797419,'Germany','Europe',331,'',51.7667,10.85,'','',-19.3306812493,-9.05251403861,-19.3306812493,-9.05251403861,0.941058423226,-66.4452988995),('Süchteln-Sittard, Krefeld',2187,'','Devonian','Upper Devonian','Strunian',358.90,372.20,11,'late Famennian - early Visean',351,362,3,1,'Seismic data available ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'20','40','40',0,'no',0,'no','2','6 to 24 reef building species','11','3','Binder guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1372,0,'Youngest stromatoporoid biostromes worldwide.\nShallow inner ramp setting (transition to outer ramp). \nMixed-carbonate-siliciclastic ramp.\nMedium diversity: Five massive growing genera and one branching form. Framestones absent.\nSome Syringopora (tabulate corals).\nRare algae: Girvanella, kamaenid algae, Solenopora.\nTiny tubular borings in some stromatoporoids.',51,6,-1455652,577470,'Germany','Europe',331,'',51.3167,6.4,'','',-31.0569350486,-6.7532132756,-31.0569350486,-6.7532132756,-0.486926567725,-61.4265600734),('Kornelimünster, Aachen',2188,'','Devonian','Upper Devonian','Strunian',358.90,372.20,11,'late Famennian - early Visean',351,362,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50','2187',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','4','Stromatoporoids','2','Algae','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','4','Others','10','40','50',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'','1','Present','2','Medium zonation','1','Low zonation','1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1372,0,'See reef 2187 for remarks.',50,6,-1536501,585899,'Germany','Europe',331,NULL,50.7333,6.1833,'WAHR','84307',-31.6539743867,-6.69493829067,-31.6539743867,-6.69493829067,-1.003692248,-61.1234069617),('Certovy Schody quarry, Koneprusy',2189,'Koneprusy Limestone','Devonian','Lower Devonian','upper Pragian',407.60,410.80,9,'late Pragian - Eifelian',395,408,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','7','Bryozoans','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'80','0','20',0,'no',0,'no','2','6 to 24 reef building species','9','1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1373,1978,'Reef facies form Koneprusy to Menany\n\nHorizontal section described.\nTabulate and rugose corals > bryozoans > stromatoporoids in reef core.\nMicrobes and algae rare.\n\nGuilds: Constructor > baffler > encruster > binder\n\nCollection of Miller contains mostly brachiopod data',49,14,-3736118,3722372,'Czech Republic','Europe',331,'',49.9167,14.1667,'WAHR','12071',-14.7416728689,8.45588716726,-14.7416728689,8.45588716726,-16.0090999435,2.41288700433),('Imperial Redknife well, N.W.T.',2190,'Sulphur Point','Devonian','Middle Devonian','upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,386,3,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'','1','Low zonation',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1380,0,'Large stromatoporoids in wackestone matrix.\nFloatstones, rudstones and framestones.\nCorals (including thamonoporids), digital stromatoporoids (commonly Stachyodes) and pebble to cobble sized bulbous or tabular strom.',60,-119,-429669,-4235461,'Canada','North America',121,'',60.9333,-119.2806,'','',-3.41175516647,-59.3264645371,-3.41175516647,-59.3264645371,1.74909582328,-118.496603666),('Meimeh, Delijan',2191,'Nayband','Triassic','Upper Triassic','Sevatian',208.50,214.00,18,'late Carnian - middle Hettangian',218,205,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','30',NULL,NULL,NULL,'2','10 - 100 m','50','25','75',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','6','Calcisponges','4','Stromatoporoids','70','Spongiomorphids - siliceous sponges - pharetronids- corals',NULL,NULL,'0','100','0',0,'no',1,'yes','3','25 or more reef building species','36','2','Baffler guild','1','Present','1','Present','3','Pronounced zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',9,30,'Inozoid, Sphinctozoid and sclerospongid sponges as main reef builders. \nCorals abundant, bored. Spongiostromata crusts locally abundant.\nStrong internal zonation.\nHexactinellid sponges also present. \n30 m thick patch reefs, up to 50 m in diameter, seperated by bedded sandy limestones and calcareous sandstone.\nShales at base and ?surrounding.\nMarls with Heterastridium lobatum at the very base. Heterastridians also within reef.\nWas Norian/Rhaetian, now exclusively late Norian (Flügel, 2002 and PBDB)',33,51,2899866,5276432,'Iran','Asia',505,'1461',33.6167,51,'WAHR','37961',21.5999022106,59.7351802336,26.238052492,60.2042838777,24.5740946188,63.5799758346),('Kuhbanan, Kerman',2192,'Nayband','Triassic','Upper Triassic','Sevatian',208.50,214.00,18,'late Carnian - middle Hettangian',218,205,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',9,1461,'Biostromal buildups. No Heterastridium.\nIncludes Bulbulu reef\nWas Norian/Rhaetian - late Norian according to PBDB',30,57,3353318,6028956,'Iran','Asia',505,'',30.4667,57.25,'WAHR','37963',22.6516665141,68.3452387524,28.4441603203,68.6461249703,22.5419232013,69.9268813342),('Abu Tartur SE, Kharga Oasis',2193,'Abu Tartur','Paleogene','Paleocene','early Paleocene',61.60,66.00,26,'middle Campanian - Danian/Selandian',75,62,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide','150','3','More than 100 m','300',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','10','1','Constructor guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1378,0,'Buildups with two distinct growth stages.\nPachygyra savii & Astrocoenia kurkurensis form low diversity initial stage.\nStorm layer seperates upper part with Dimorphastrea irradians, Siderastrea sp., Montastrea sp., Leptoria cf. pauca, Leptoria laxa, Astrocoenia aff decaphylla, Astrocoenia spongilla and A. kurkurensis with massive, hemispherical, encrusting and branching growth forms.\nLargest extension of reefs 150x300 m.',25,30,1746238,2696702,'Egypt','Africa',715,'',25.4667,30.05,'WAHR','34684',14.2441969628,26.5956622496,14.2441969628,26.5956622496,17.100035993,25.3344909105),('Mafeking, Manitoba',2194,'Winnipegosis','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','50',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','2','Intense',1,'Potential reservoir',1379,0,'Elk Point Group\n50 m thick strongly dolomitized and recrystallized buildups.\nBoundstones minor constituents of buildups (rims).',52,-100,-2174352,-3977070,'Canada','North America',121,'',52.75,-100.9167,'','',-16.1026992635,-57.0953537901,-16.1026992635,-57.0953537901,-10.3059544946,-113.942255342),('Swan River, Manitoba',2195,'Winnipegosis','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','2','Intense',2,'Actual reservoir',1379,0,'See reef 2194',52,-101,-2228645,-4027598,'Canada','North America',121,'',52.1333,-101.1667,'','',-16.5328837027,-57.5823950891,-16.5328837027,-57.5823950891,-10.816447075,-114.326843519),('Winnipegosis, Manitoba',2196,'Winnipegosis','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species','9','1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','2','Intense',0,'No or unknown reservoir potential',1379,2252,'See reef 2194.',51,-99,-2357795,-3976413,'Canada','North America',121,'',51.5667,-99.8,'WAHR','3635',-17.4683016044,-57.1657913349,-17.4683016044,-57.1657913349,-11.6598488973,-113.747937276),('Mt. Tom, New York',2197,'Onondaga','Devonian','Middle Devonian','lower Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,395,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','13','Echinoderms','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'80','0','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1381,1710,'Edgecliff Member\nRugose coral mound.\nFrom base to top: Acinophyllum, Cylindrophyllum, Acinophyllum, Cylindrophyllum facies.',43,-74,-5071703,-2140815,'United States','North America',101,'',43,-74.6667,'WAHR','79593',-31.2550606519,-44.0840018523,-31.2550606519,-44.0840018523,-23.6184491618,-99.1665808964),('Karatchok Field',2198,'','Cretaceous','Upper Cretaceous','Turonian-Campanian',72.10,93.90,25,'late Cenomanian - early Campanian',91,87,2,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick','140',NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','2','Algae','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)','1','Red algae','45','50','5',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','1','Present',2,'Actual reservoir',1382,0,'Shoal rudist complex anlong structurally controlled platform margin. 10-140 m thickness.\nRed algae, rudists, serpulids, corals.\nAverage porosity: 6.6 % (mostly moldic).',37,42,1792043,3916191,'Syria','Asia',NULL,'',37.25,42.25,'','',20.6536864885,39.9726881329,20.6536864885,39.9726881329,19.2515072101,36.8268060998),('Garzan Field',2199,'','Cretaceous','Upper Cretaceous','lower Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,69,3,1,'Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'80','10','10',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1382,0,'Oyster buildups.\nRare red algae and corals.\nAverage porosity: ca. 11 %.',37,41,2995626,3779883,'Turkey','Asia',522,'',37.8333,41.5,'','',23.0791982729,38.3447375181,23.0791982729,38.3447375181,24.7197531302,36.9433104884),('Berri Field',2200,'','Jurassic','Upper Jurassic','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,153,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','30',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','50','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1383,0,'Coral-stromatoporoid boundstones (bioherms) in high-energy ramp margin shoal.\nBioherms less than 30 m thick.\n10-23% porosity.',27,49,-186506,4283316,'Saudi Arabia','Asia',503,'',27.1167,49.6,'','',-11.5059957952,42.912030498,-11.5059957952,42.912030498,-8.96925278165,40.477248335),('Al Huwaisah Field',2201,'Shuaiba','Cretaceous','Lower Cretaceous','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,123,3,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','100',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','3','Microbes','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'40','40','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','3','Pronounced zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1385,0,'Shuaiba Fm. (early to middle Aptian).\nPronounced vertical zonation: \nTop\nRudist complex: Bound-, packstone\nAlgal-coral complex: Lithocodium-stromatoporoid w/p/b\nBacinella Boundstone.\nBase\n90-100 m thick.\n21 % avg. porosity.',21,56,-1178533,4850661,'Oman','Asia',503,'',21.9667,56.0333,'','',-10.6661491694,51.5025057456,-11.8040229898,51.3892464231,-10.3896575474,44.9197474298),('Fahud Field',2202,'','Cretaceous','Upper Cretaceous','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,97,2,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1385,0,'radiolitid biostromes and rudist rubble packstones.',22,56,-961398,4993504,'Oman','Asia',503,'',22.25,56.5167,'','',0.631984312072,50.4663731665,0.631984312072,50.4663731665,-3.00720799377,44.943766883),('Ras Fanar Field, Gulf of Suez',2203,'Belayim','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,14,3,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick','85',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1','Red algae','30','10','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation',NULL,'',NULL,'',NULL,'','1','Present',2,'Actual reservoir',1386,0,'Restricted carbonate platform. \n85 m thick rhodalgal mound/bank.\nStacked mound complex.\nRhodalgal wacke-, packstones, common bryozoans, molluscs, local coral boundstones.\nRestricted carbonate platform, but ramp type succession.\n20 % avg. porosity.\n',28,33,3636582,3222926,'Egypt','Africa',715,'',28.4,33.1,'','',26.6845323631,30.756029933,26.6845323631,30.756029933,26.0295566759,32.2590405357),('Intisar \'A\' Field',2204,'Sabil','Paleogene','Paleocene','Upper Paleocene',56.00,59.20,27,'Thanetian - Ypresian',53,57,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','160',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite',NULL,'','0','',2,'Actual reservoir',1386,0,'Upper Sabil\n400 m thick succession:\nTop	Coral unit\n	Coralline biomicrite unit\nBase	Algal-foram shoal\n\nTopographic high in epicontinental shelf setting.\nCoral boundstone 110 m thick in central part, > 160 m in the south.\n20 % avg. porosity.',29,20,2686882,1770076,'Libya','Africa',715,'',29.0417,20.7667,'','',19.4679957903,17.5140761985,19.4679957903,17.5140761985,22.7370044224,17.4309427636),('Intisar \'D\' Field',2205,'','Paleogene','Paleocene','Upper Paleocene',56.00,59.20,27,'Thanetian - Ypresian',53,57,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','300',NULL,NULL,NULL,'4','More than 1000 m','5000',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','5','40','55',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',2018,1386,'Homogeneous algal-foram build-up with localized coral growth. Red algae dominant.\n300 m thick.\n22 % avg. porosity.\nAlgal-foraminiferal biomicrites dominant. Containing ref algae with coral debris, echinoderm fragments, bryozoans, encrusitng forams, occasional crinoids. ',28,20,2665565,1789308,'Libya','Africa',715,'',28.9,20.9667,'','',19.3115447032,17.6857305101,19.3115447032,17.6857305101,22.5729477044,17.59804344),('Lho Sukon-A, Sumatra',2206,'Peuta','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','30',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1387,0,'Patch reef. 30 m thick.\n13.2 % avg. porosity.',4,96,298111,11153284,'Indonesia','Asia',614,'',4.8333,96.9167,'','',6.49293708573,94.1075994612,6.49293708573,94.1075994612,2.86828538703,95.7248367453),('NSO-A Field, northern Sumatra Bas.',2207,'Malacca','Neogene','Miocene','Early/Middle Miocene',11.60,23.00,31,'Burdigalian - Serravallian',14,16,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','350','4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1387,0,'N-S trending patch reefs. Atoll type setting.\r\nUp to 350 m thick. 10 x 7 km area with patch reefs.\r\nCorals (finger-type, massive digitate), red algae, molluscs, echinoderms, benthic forams.\r\n23 % avg. porosity.',5,97,505547,10958596,'Indonesia','Asia',614,'',5.2167,97.8167,'',NULL,6.75225423762,95.4234839844,6.75225423762,95.4234839844,3.67401617101,96.6328051586),('Rama Field',2208,'Baturaja','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','200',NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1387,0,'200 m thick skeletal bank (Reef mound)\nDeepening upward\n20 % avg. porosity.',-5,106,-788386,12235639,'Indonesia','Asia',614,'',-5.4403,106.2861,'','',-3.73717797261,103.527099736,-3.73717797261,103.527099736,-5.55586497392,106.789049941),('Bima Field',2209,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick','12',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','12','Foraminifera','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','5','20','75',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1387,0,'Mud dominated skeletal bank.\nMud, benthic forams, mixed skeletal fragments, branching red algae, molluscs, corals.\n12 m thick.\n28 % avg. porosity.',-5,106,-752415,12377979,'Indonesia','Asia',614,'',-5.3667,106.55,'','',-3.66301427863,103.79021692,-3.66301427863,103.79021692,-5.43580301756,107.035186954),('Krisna Field',2210,'Baturaja','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','80',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1387,0,'80 m thick fringing reefs (buildups).\n22.7 % avg. porosity.\n',-5,106,-765972,12352641,'Indonesia','Asia',614,'',-5.4167,106.3167,'','',-3.71351080183,103.557574734,-3.71351080183,103.557574734,-5.52712783213,106.81484375),('Kampung Baru Field, Sulawesi',2211,'Tacipi','Neogene','Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,7,2,1,'Seismic data available ',NULL,NULL,'3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50','2132',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'','2','Medium zonation',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1387,1447,'18 km NE\' Lake Tempe\nReworked corals, red algae, forams\nPeri-reef reservoir\nAbout 200 m thick.\n26 % avg. porosity.',-3,120,-528109,13356098,'Indonesia','Asia',614,'',-3.9667,120.1333,'','',-2.91305941365,119.310079105,-2.91305941365,119.310079105,-4.34549270806,119.568747054),('Parsons Quarry, Tennessee',2212,'Rockhouse','Devonian','Lower Devonian','Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,414,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m','14',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','3','Pronounced zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1390,0,'Rockhouse Limestone.\nMud mounds ranging from 1-3 m in width and 1-14 m in length. Maximum thickness 3 m. \n48 mounds.\nSyndepositional relief around 0.5 m.\n4 distinct growth phases\n4 - Echinoderm-bryozoan mudstone/wackestone\n3 - (thickest part) Encrusting cystoporate bryozoan Buskopora dominant. Low diversity\n2 - echinoderm-bryozoan packstone\n1 - Echinoderm-rich terrigenous mudstone\n\n',35,-88,-6045829,-3405140,'United States','North America',101,'',35.6667,-88.1167,'WAHR','79591',-34.4947517868,-68.0634171845,-34.4947517868,-68.0634171845,-19.9656142878,-127.544722243),('Nam Con Son Basin, offshore',2213,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','300','4','More than 1000 m wide','5000','4','More than 1000 m','10000',NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1391,0,'Position unknown.\nCoral-algal reefs developed on tectonic horsts.\n5-10 km across, >= 300 m thick.\nWell developed talus slopes.',9,107,1101831,11865729,'Vietnam','Asia',NULL,'',9,107,'','',10.4169112904,105.315019302,10.4169112904,105.315019302,8.1601047875,105.741949502),('Nam Con Son Basin, offshore',2214,'','Neogene','Upper Neogene','upper Miocene - Pliocene',2.60,11.60,32,'Tortonian - Gelasian',6,5,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','300',NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',1391,0,'See reef 2213 for remarks.',9,107,1172086,11795630,'Vietnam','Asia',NULL,'',9,107,'','',9.80027486578,106.185366967,9.80027486578,106.185366967,8.54470231619,106.364765519),('Luconia F6 Field, Sarawak',2215,'','Neogene','Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,13,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1389,590,'25 % avg. porosity.',4,112,639958,12542174,'Indonesia','Asia',614,'',4.5833,112.25,'','',5.52930267481,110.622916206,5.52930267481,110.622916206,3.17983229024,112.291279227),('Bombay High Field, Indian Ocean',2216,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','30','70',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',2017,1389,'Mudstone dominated carbonate bank, minor packstones.\nAlgal mound(?) with abunadant micrite containing codiacean algae, forams and corals. Overlain by foraminiferal mound.\nField contains half of Indian oil reservoirs',19,71,1420133,7409294,'India','Asia',501,'',19.3333,71.5,'','',13.1877456696,65.9241516479,13.1877456696,65.9241516479,10.8969214961,67.0093438108),('Sui Field',2217,'Sui','Paleogene','Eocene','lower Eocene',47.80,56.00,27,'Thanetian - Ypresian',53,50,3,1,'Seismic data available ',3,'Mud mound or bank','4','More than 500 m thick','620',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','2','Algae','12','Foraminifera','13','Algae - encrusting forams','1','Red algae','20','20','60',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1389,0,'Mud-dominated skeletal bank.\nAlgal-foram wacke-/packstones\n11 % avg. porosity.\n> 600 m thick.',28,69,656220,6982898,'Pakistan','Asia',501,'',28.5,69.3333,'','',7.38303158906,59.815741212,7.38303158906,59.815741212,6.1715128471,61.7675220515),('Wuolonghe Field, Sichuan',2218,'Maokou','Permian','Lower Permian','Kungurian',272.30,283.50,15,'Sakmarian - Kungurian',277,273,2,0,'Outcropping reef ',4,'Biostrome','3','101-500 m thick','160',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','2','Algae','69','Non-coralline algae only','1','Red algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,'',NULL,'',NULL,'','1','Low zonation','1','Low zonation','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',1393,0,'Skeletal banks in high energy open shelf setting.\nMassively bedded red algal limestones.\n160 m thick. \n0.8 % porosity.\n60-70 % grains.',30,107,-832058,9627369,'China','Asia',602,'',30.3333,107.4167,'','',-7.61980279373,118.841055362,-7.61980279373,118.841055362,11.9644102299,126.552318194),('Allakaevsk-Ishimbay',2219,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'Seismic data available ',1,'True reef','4','More than 500 m thick','600',NULL,NULL,NULL,'4','More than 1000 m',NULL,'240','214',1,'Temperate',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','2','Algae','28','Palaeoaplysina - microbes - bryozoans - Tubiphytes - (corals)','2','Green algae','20','40','40',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1394,1413,'Sponges, calcareous algae, corals, bryozoans and Tubiphytes as reef builders.\n500-600 m vertical relief.\nSteep flanks (dipping 35-70°).\n9 % avg. porosity.',53,56,3399892,4762555,'Russia','Asia',624,'',53.3833,56,'','',23.1846490562,44.1803370933,23.1846490562,44.1803370933,30.9497934994,19.887455315),('Kaybob, Alberta',2220,'Swan Hills','Devonian','Middle Devonian','upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,386,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','77',NULL,NULL,NULL,'3','More than 100 m',NULL,'15',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',2,'Actual reservoir',1395,1582,'Reef mound complex\nDown-dip off platform setting\nWave-resistant framework of massive, hemispheriacal stromatoporoids and tabular strom.\nBioclastic matrix with stromatoporoids, corals, brachiopods. Sometimes encrusted by algae.\n\n77 m thick.\n7.4 % avg. porosity.\n\nRef. 1582: Outer zone dominated by Stachyodes (high energy)\nInner zone with Stromatopora, Actinostroma and possibly Trupetostroma, Taleastroma.\nAmphipora in interior (lagoonal) setting.',54,-116,-1116234,-4675721,'Canada','North America',121,'',54.55,-116.7833,'','',-8.65436356495,-63.2253287246,-8.65436356495,-63.2253287246,-4.13807010186,-121.299971943),('W Pembina Field, Alberta',2221,'Nisku','Devonian','Middle Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,1,'Seismic data available ',1,'True reef','3','101-500 m thick','110',NULL,NULL,NULL,'4','More than 1000 m',NULL,'2',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','1','Red algae','40','30','30',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','3','Pronounced zonation','2','Medium zonation','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1396,891,'Zeta Lake Member\nPinnacle reef\nLower and upper reef zone:\nUpper: \nTop \n- Carbonate sands\n- Solenopora algal crest\n- Robust stromatoporoids, rugose corals, Renalcis\n\nLower\n- Algal-laminated crustose (Renalcis, Rothpletzella, ?Wetheredella)\n- Rugose corals, laminated stromatoporoids.\n\n110 m thick. 1.6 km diameter.\n8 % avg. porosity',53,-115,-1298758,-4729988,'Canada','North America',121,'1487',53.25,-115.6667,'','',-8.41890445792,-58.8145122542,-8.41890445792,-58.8145122542,-2.06767526268,-117.701542333),('Strachan Field, Alberta',2222,'Leduc','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','290','4','More than 1000 m wide','4000','4','More than 1000 m','11000',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','3','Pronounced zonation','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','1','Present',2,'Actual reservoir',2015,1396,'Isolated platform buildup\n11 km x 4 km\nReef core: Massive stromatoporoids and colonial corals in biomicritic matrix\nBack reef: Coarse massive coral and stromatoporoid rudstones\nFor reef: Like back reef but transition to facies with dendroid Stachyodes and rugose corals.\n\n\n290 m thick.\n5 % avg. porosity.',53,-115,-1327643,-4712979,'Canada','North America',121,'',53.2167,-115.25,'','',-8.6411914632,-58.6952652909,-8.6411914632,-58.6952652909,-2.25155230814,-117.529642077),('West Edmond Field, Oklahoma',2223,'Frisco','Devonian','Lower Devonian','Lochkovian-Pragian',407.60,419.20,8,'middle Pridolian - middle Pragian',412,411,2,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','13','Echinoderms','60','Bryozoans - Pelmatozoans - (microbes)',NULL,NULL,'40','0','60',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',2,'Actual reservoir',1397,0,'Hunton Group\nLow energy mud mound\nOuter ramp setting\nPelmatozoan-bryozoan packstone.\nMudstones in mound core.',35,-97,-5509379,-4375009,'United States','North America',101,'',35.65,-97.5667,'','',-34.002864692,-75.4836139323,-34.002864692,-75.4836139323,-20.1658357468,-133.157591619),('Black Lake Field, Loisiana',2224,'Sligo','Cretaceous','Lower Cretaceous','Aptian',113.00,125.00,23,'late Valanginian - early Aptian',126,118,1,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','12',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'30','70','0',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1398,0,'Coalesced caprinid rudist mounds.\nBioclastic reef flank.\nTerminated by regression.\n12 m thick.\n16 % avg. porosity.\n',31,-93,2012095,-5156077,'United States','North America',101,'',31.8667,-93,'','',26.067928223,-41.4777226553,26.067928223,-41.4777226553,28.506053189,-48.1180573601),('Empire Abo Field, New Mexico',2225,'Abo','Permian','Lower Permian','Leonardian',272.30,283.50,15,'Sakmarian - Kungurian',277,273,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','215',NULL,NULL,NULL,'4','More than 1000 m',NULL,'2',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','2','Algae','27','Pharetronid sponges - algae','1','Red algae','0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Intense',2,'Actual reservoir',1399,0,'215 m thick shelf margin reef.\nDolomitic. Rare hydrozoans, sponges, algae, brachiopods.\n6.4 % avg. porosity (fracture).',32,-104,753428,-3536489,'United States','North America',101,'',32.7833,-104.1833,'','',1.93913144674,-33.6244417204,1.93913144674,-33.6244417204,-0.012773911642,-40.0313373717),('Marufo Vega Trail, Big Bend, Texas',2226,'Santa Elena','Cretaceous','Lower Cretaceous','upper Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,101,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','5',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'30','70','0',0,'no',1,'yes','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1401,0,'Thin shelled caprinids dominate. Some gastropods associated. \n2 small bioherms lower 5 m thick, upper 2-3 m thick.\n',29,-102,2956005,-6508392,'United States','North America',101,'',29.2331,-102.9194,'','',27.955282754,-59.0142016387,27.955282754,-59.0142016387,29.8745092914,-65.0165468113),('Mexican Saddlehorn, Arizona',2227,'Mural Limestone','Cretaceous','Lower Cretaceous','lower Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,110,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','5','Rudists','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'20','80','0',0,'no',1,'yes','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1402,1256,'',31,-109,3414499,-6925968,'United States','North America',101,'1401',31.3411,-109.1025,'WAHR','74146',31.349762053,-64.3411053888,31.349762053,-64.3411053888,33.1754528452,-70.5263395716),('Bolshoi Tir, Siberia',2228,'Osinsky','Cambrian','Lower Cambrian','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,527,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','90',NULL,NULL,NULL,'4','More than 1000 m',NULL,'90',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1405,1413,'Osinsky horizon.\nNepa-Botuoba anteclise.\nEpiphyton, Renalcis, Marcovella dominant.\nRare archaeocyaths.\n80-90 m thick.\nDimensions 40 x 90 km but reefs probably much smaller.',57,105,-2518261,1115479,'Russia','Asia',624,'',57.5,105.5,'','',1.17293117074,-63.8349457886,1.17293117074,-63.8349457886,1.17293117074,-63.8349457886),('Nepa, Siberia',2229,'Osinsky','Cambrian','Lower Cambrian','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,527,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'90','2228',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1405,1406,'Oil field.\nOsinsky horizon.\nNepa-Botuoba anteclise.\nEpiphyton, Renalcis, Marcovella dominant.\nRare archaeocyaths.\n95-100 m thick.',58,105,-2558793,1064719,'Russia','Asia',624,'214, 1413',58,105.8333,'','',0.892093614251,-64.285308644,0.892093614251,-64.285308644,0.892093614251,-64.285308644),('Talakan, Siberia',2230,'Bilir','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,519,2,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick','55',NULL,NULL,NULL,'3','More than 100 m',NULL,'65',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1408,1413,'Osa horizon.\nGas field.\nCentral part of Nepa-Botuoba anteclise.\nStromatolithic biostrome massif. 50-55 m thick.\n37 x 65 km\nDominated by stromatolites with archaocyaths in climax stage\nPrevisouly dated as lower Tommotian but now assigned to Atadanian ',60,111,-2576107,644809,'Russia','Asia',624,'2561',60.1667,111.6667,'','',3.20310509398,-58.4645667063,3.20310509398,-58.4645667063,3.20310509398,-58.4645667063),('Verchne Kii, Siberia',2231,'','Cambrian','Lower Cambrian','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,527,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'90','2228',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1413,1405,'',58,106,-2624611,1010531,'Russia','Asia',624,'',58.6667,106,'','',0.422695351319,-64.7668102831,0.422695351319,-64.7668102831,0.422695351319,-64.7668102831),('Kii, Siberia',2232,'','Cambrian','Lower Cambrian','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,527,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'90','2228',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',1,'Potential reservoir',1405,214,'',58,105,-2595135,1041552,'Russia','Asia',624,'1413',58.3333,105.8333,'','',0.630605918574,-64.4919984891,0.630605918574,-64.4919984891,0.630605918574,-64.4919984891),('Yuktansk, Siberia',2233,'','Cambrian','Lower Cambrian','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,527,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'700',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1405,1406,'',59,104,-2708486,1041118,'Russia','Asia',624,'1413',59,104.8333,'','',-0.214814849664,-64.5036987064,-0.214814849664,-64.5036987064,-0.214814849664,-64.5036987064),('Verchne Chon, Siberia',2234,'Usol\'ye','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'700','2233',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1405,1406,'Osa horizon.\nPreviously dated as lower Tommotian, now assigned to Atadabanian',59,109,-2595309,792152,'Russia','Asia',624,'214, 1413, 2561',59.5833,109.3333,'','',2.96942430579,-57.1754591993,2.96942430579,-57.1754591993,2.96942430579,-57.1754591993),('Markovo, Siberia',2235,'','Cambrian','Lower Cambrian','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,527,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'90','2228',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',1,'Potential reservoir',1405,1406,'',57,106,-2439620,1089842,'Russia','Asia',624,'214, 1413',57.1667,106.5,'','',1.76859243274,-64.0531814574,1.76859243274,-64.0531814574,1.76859243274,-64.0531814574),('Muratovo, Donbas, Donetz',2236,'','Carboniferous','Lower Carboniferous','upper Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,320,3,1,'Seismic data available ',1,'True reef','3','101-500 m thick','240',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','2','Algae','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','2','Green algae','20','60','20',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1409,1410,'Donets aulakogene.\nGas field. Reef top in 3000 m. Asymmetric. N slope dipping 1-1.5°, S slope dipping 5-10°.\nEncrusting microbes and algae as main reef builders. Girvanella, Tubiphytes, bryozoans (Fenestellidae).\nRare corals (Lithostrotion).\n220-240 m thickness.\n',48,38,487234,3227027,'Ukraine','Europe',301,'1413, 1525',48.8,38.7333,'','',-11.5353417017,23.9116044827,-11.5353417017,23.9116044827,7.476993031,4.09895815705),('Sirotinsky, Donbas, Donetz',2237,'','Carboniferous','Lower Carboniferous','upper Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,320,3,1,'Seismic data available ',1,'True reef','3','101-500 m thick','240',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50','2236',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','7','Bryozoans','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,'60','30','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','3','High production of reefal debris','1','Present',2,'Actual reservoir',1410,1409,'see reef 2236',48,38,485356,3205654,'Ukraine','Europe',301,'1413, 1525',48.9167,38.5,'','',-11.559430675,23.7163442395,-11.559430675,23.7163442395,7.41284128172,3.91557821667),('Yuzhny Umet, Volgograd',2238,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','150',NULL,NULL,NULL,'4','More than 1000 m',NULL,'45',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1416,1413,'Eastern slope of Voronezh anteclise.\nAbout 150 m thick including Sakmarian-Artinskian interval.\nMicrobes and Tubiphytes.',50,45,2508084,4570285,'Russia','Asia',624,'1415',50.2833,45.3333,'','',16.4407266701,41.2791479797,16.4407266701,41.2791479797,23.6787965026,19.6332789837),('Chukhonastovka, Volgograd',2239,'','Permian','Lower Permian','Sakmarian-Artinskian',283.50,298.90,15,'Sakmarian - Kungurian',277,284,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','170',NULL,NULL,NULL,'4','More than 1000 m',NULL,'45','612',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1415,1413,'Sakmarian to lower Artinskian.\n170 m thick (including Asselian interval).\nMicrobes and Tubiphytes.',49,44,2972993,4879106,'Russia','Asia',624,'',49.8333,44.9167,'','',16.2725993955,41.7663511622,16.2725993955,41.7663511622,24.6622948012,24.9633767599),('Chukhonastovka, Volgograd',2240,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','170',NULL,NULL,NULL,'4','More than 1000 m',NULL,'45','2238',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1415,1413,'see reef 2239.',49,44,2438207,4586100,'Russia','Asia',624,'',49.8333,44.9167,'','',15.9226303468,41.3571321839,15.9226303468,41.3571321839,23.2166704833,19.9013260554),('Kotovo, Volgograd',2241,'','Devonian','Upper Devonian','middle-upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,378,3,1,'Seismic data available ',1,'True reef','4','More than 500 m thick','600',NULL,NULL,NULL,'4','More than 1000 m',NULL,'80',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','1','Red algae','0','10','90',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'','2','Medium zonation','1','Less than 30% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1417,1413,'Large reef complex:\nSouthern part dominated by microbes and algae, northern part with abundant stromatoporoids.\n580 -600 m thick oil field. Top in 2300 m depth.\n\nIzhella, Epiphyton, Issinella, Shuguria, Girvanella, Solenopora and stromatoporoids (Stellepora), bryozoans, corals (Thamnophyllum, Penechiella, Thecostegites, Syringopora).\nAdditionally forams, brachiopods, pelecypods, crinoids.',50,44,-126466,2453594,'Russia','Asia',624,'',50.3,44.8333,'','',-4.72280106605,6.74526885379,-4.72280106605,6.74526885379,20.0456935464,-56.9870963485),('Tarasovo, Volgograd',2242,'','Devonian','Upper Devonian','middle-upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,378,3,1,'Seismic data available ',1,'True reef','4','More than 500 m thick','600',NULL,NULL,NULL,'4','More than 1000 m',NULL,'80','2241',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','10','90',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'','2','Medium zonation','1','Less than 30% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1417,1413,'See reef 2241',50,44,-114546,2427444,'Russia','Asia',624,'',50.55,44.8,'','',-4.62399360984,6.51387610192,-4.62399360984,6.51387610192,20.0672478936,-57.253205514),('Lyubimovka, Saratov',2243,'','Devonian','Middle Devonian','upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,386,3,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1418,1415,'More than 25 reefs in Saratov region.\nreef area 100x200 km. \nMain reef builders are stromatoporoids: Paraamphipora, Stromatopora, Anostylostoma, Parallelopora.\nTabulate corals: Cyclochaetetes, Grassialviolites, Thamnopora\nRugosa: Dasphyllum, Neotrigophyllum, Thamnophyllum, Taneckiella\nAlgae\nAlgae and brachiopods, too.\nOil field',51,47,2396101,1587887,'Russia','Asia',624,'1413',51.3333,47.25,'WAHR','84336',3.5541616394,0.289757674855,3.5541616394,0.289757674855,23.4261077275,-64.0776300609),('Ilych River, Urals',2244,'','Ordovician','Upper Ordovician','upper Ashgillian',445.20,450.00,5,'Darriwilian - Ashgillian',452,445,3,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','110','3','101-1000 m wide',NULL,'3','More than 100 m',NULL,'550','993',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','1','Corals','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','17','1','Constructor guild',NULL,'',NULL,'','1','Low zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1420,1022,'Massive structure 1x1.5 km across.\n110 m thick.\nFramework dominated by encrusting Girvanella, Rothpletzella and other microbes.\nSubordinate heliolitids (Plasmoporella, Heliolites, Propora), tabulate and rugose corals and hydroid problematica (Fistulella).',63,58,-2592879,1332088,'Russia','Asia',624,'',63,58.75,'WAHR','24294',-13.0079951459,-48.2089802243,-10.6404100902,-48.2317925694,-10.6404100902,-48.2317925694),('Lec-Elec River, Pechora',2245,'','Silurian','Llandovery','upper Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,430,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','80',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','0','70',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1420,1973,'Patch reefs composed of an alternation of microbial-coral and stromatoporoid boundstones. \n60-80 m thick.\nInterbeds of microbial mudstones with Stromatactis.\nframework dominated by encrusting Girvanella, Garwoodia, Ikella with subordinate stromatoporoids, favositids and bioclastic debris.',67,64,-29741,421886,'Russia','Asia',624,'',67.0833,64.5,'','',4.45016114638,-51.8004059727,4.45016114638,-51.8004059727,4.45016114638,-51.8004059727),('Bolshaya Usa River, Polar Urals',2246,'Ovinparma','Devonian','Lower Devonian','upper Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,413,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','30','2','10 - 100 m wide',NULL,'2','10 - 100 m','110',NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp',NULL,'','3','Microbes','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','10','3','Binder guild',NULL,'',NULL,'','2','Medium zonation',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','2','Intense',0,'No or unknown reservoir potential',1420,2268,'Extensively dolomitized.\nAbout 170 m thick.\nStromatolites predominate.\nCalcimicrobes: Girvanella, Renalcis, Ikella.\nStromatoporoids, branching tabulates and rare rugose corals only in lower part of the reef.',67,64,752976,864014,'Russia','Asia',624,'',67.4167,64.5667,'WAHR','24015',26.6304890308,-42.2704874564,26.6304890308,-42.2704874564,39.332860604,-103.301373833),('Verchnyaya Pechora River',2247,'','Devonian','Lower Devonian','Pragian',407.60,410.80,8,'middle Pridolian - middle Pragian',412,409,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','2','Algae','64','Microbes/stromatolites  - (cements) - (worm tubes)','4','Others','0','60','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1420,2268,'300 m thick buildup (locally up to 1000 m).\nMicrobial associations comprise more than 50 % of all reef boundstones.\nCoalesced small biostromes and bioherms (3 m thick).\n25 species of calcareous algae in whole region\nPlenty of reef debris flows.\nContinuing into Emsian.',61,58,803570,1479515,'Russia','Asia',624,'',61.8333,58.6667,'WAHR','24018',24.6063511628,-31.9968361302,24.6063511628,-31.9968361302,35.7636294722,-92.5595508105),('Lemva River, Pechora, Urals',2248,'','Devonian','Lower Devonian','Pragian-Emsian',393.30,410.80,9,'late Pragian - Eifelian',395,407,2,0,'Outcropping reef ',3,'Mud mound or bank','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'17',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,'','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','6','3','Binder guild',NULL,'',NULL,'',NULL,'','3','Pronounced zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1420,2268,'Pragian to lower Emsian.\nUp to 1000 m thick reef complex extensively dolomitized.\nAppears to be microbial mound. Ikella, Garwoodia, Ortonella and Girvanelly at base.\nCavernous porosity.',65,61,1019482,1058463,'Russia','Asia',624,'',65.75,61.2,'WAHR','24019',20.3798213346,-30.5347747676,20.3798213346,-30.5347747676,31.8590910543,-91.3894507379),('Lec-Elec River, Pechora',2249,'','Devonian','Lower Devonian','Pragian-lower Emsian',393.30,410.80,9,'late Pragian - Eifelian',395,407,2,0,'Outcropping reef ',2,'Reef mound','4','More than 500 m thick','580',NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','40','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1420,0,'Pragian part is 360 m thick.\nLower Emsian part is 220 m thick.\nWetheredella-Stachyodes boundstones associated with Ikella-Fistulella, and Solenopora-metazoan boundstones.\n',67,64,1211816,917877,'Russia','Asia',624,'',67.0833,64.5,'WAHR','81602',21.4477305878,-32.1858805671,21.4477305878,-32.1858805671,32.4474840862,-93.4934507857),('Shernyadeyta River, Chernyshev Ridge',2250,'','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,375,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','6',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','2','Below fair weather wave base','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1420,0,'Stromatoporoid-microbial mounds and banks.\n200-300 m thick bank with 4-6 m thick bioherms.\nMicrobes and alage: Renalcis, Izhella, Shuguria, Epiphyton, Sphaerocodium, Girvanelly, Chbakovia, Paleomicrocodium, Ortonella and solenoporids.\nVarious isopachos fibrous texture through microbial crusts.\n\n',67,61,1709491,910883,'Russia','Asia',624,'',67.5,61.75,'','',9.47384216821,-6.14135057583,9.47384216821,-6.14135057583,28.4420957286,-75.896829162),('Olysya, Bolshaya Nadota River, Urals',2251,'','Carboniferous','Lower Carboniferous','upper Visean-Serpukhovian',323.20,336.00,12,'middle Visean - Serpukhovian',329,326,2,0,'Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,'4',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1420,0,'Massive to poorly bedded, recrystallized structure.\n200 m thick. 2 x 4 km across.\nStromatolitic boundstones predominate. \nIrregular cavities with filled by fibrous blocky calcite cements.\nCrinoids, brachiopods, gastropods, bryozoans occur locally.\nReef talus in the east.',64,58,2930285,2596527,'Russia','Asia',624,'',64,58.5,'','',-2.7404641976,15.5979240611,3.02822829809,17.5030401074,25.175619858,-9.36927072619),('Kozhym River',2252,'','Permian','Lower Permian','lower Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,292,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'400',NULL,1,'Temperate',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,'','9','Tubiphytes','2','Algae','28','Palaeoaplysina - microbes - bryozoans - Tubiphytes - (corals)','2','Green algae','0','50','50',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',1,'Potential reservoir',1420,661,'see reef 914.',65,59,5163709,3889067,'Russia','Asia',624,'680, 660',65.5,59.8333,'WAHR','75612',32.7395210062,35.4589147852,32.7395210062,35.4589147852,37.6725325198,10.5289845441),('Attawapiskat River, Ontario',2253,'Attawapiskat','Silurian','Llandovery','upper Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,429,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','8',NULL,NULL,NULL,'1','Less than 20 m',NULL,'300','1410',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1423,0,'Outcrop of Attawapiskat Formation.\n8.3 m thick.\nStromatoporoid-coral framework overlain by crinoid-rich caprock or bioclastic packstones/rudstones.\n\nAbstract or ref. 1423:\nOutcrop exposures along the Attawapiskat River in the Hudson Bay Lowlands of northern Ontario clearly reveal the morphology of Silurian (upper Llandoverian) reefs of the Attawapiskat Formation and the relationships between reef cores, flanking beds, and post-reef beds. These relationships indicate that the reefs had a syndepositional relief of at least 8-10 m. The relief of the reefs is indicated by debris-flow lenses encased within flanking beds, a debris-flow fan at the base of a reef, thin reef-flanking beds truncated against a vertical reef face, penecontemporaneous brachiopod beds on the flanks of reefs, and three large slide blocks that apparently slid over the side of a reef. Reefs of the Attawapiskat Formation are largely limestones with a wide range of lithologies. from stromatoporoid-, coral-, and cement-rich boundstones to alga- cement-rich boundstones. Thick, laterally extensive Nuia grainstone beds, a product of widespread Nuia monocultures in supratidal to intertidal ponds, are present above the reefs. The most important diagenetic processes were early marine cementation (predominantly radial-fibrous calcite), shallow burial diagenesis, and pervasive neomorphism. Schematic reconstructions of the depositional history of the Attawapiskat Formation in outcrop, constructed from observations of outcrop relationships, show a stratigraphic succession that was controlled by relative-sea-level changes. Reefs growth was terminated by a relative-sea-level fall, but subsequent minor relative-sea-level fluctuations resulted in alternating deposition of supratidal to shallow subtidal sediments for a short time before the final retreat of the Silurian seas from the Hudson Bay Platform; only supratidal evaporite facies are present in the remainder of the Silurian section above the Attawapiskat Formation.',52,-83,-1947802,-4905968,'Canada','North America',121,'',52.8547,-83.7678,'WAHR','77260',-18.409510263,-93.7594475248,-18.409510263,-93.7594475248,-18.409510263,-93.7594475248),('Attawapiskat River, Ontario',2254,'Attawapiskat','Silurian','Llandovery','upper Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,429,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','8',NULL,NULL,NULL,'1','Less than 20 m',NULL,'300','1410',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','7','Bryozoans','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1423,0,'See 2253 for remarks.',52,-82,-1986750,-4836000,'Canada','North America',121,'',52.9067,-82.6878,'WAHR','77328',-18.5047087418,-93.077517324,-18.5047087418,-93.077517324,-18.5047087418,-93.077517324),('Comeault No. 1, Hudson Bay, Ontario',2255,'','Silurian','Lower Silurian','upper Telychian?',433.40,438.50,6,'Rhuddanian-Telychian',435,429,2,1,'Seismic data available ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'500','1889',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1423,0,'See reef 1889',59,-90,-880400,-4919787,'Canada','North America',121,'',59.6667,-90.8333,'','',-10.768910991,-95.6299395596,-10.768910991,-95.6299395596,-10.768910991,-95.6299395596),('Kaskattama No. 1, Hudson Bay, Ontario',2256,'','Silurian','Lower Silurian','Llandovery-Wenlock',427.40,443.40,6,'Rhuddanian-Telychian',435,428,2,1,'Seismic data available ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'500','1889',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1423,0,'See reef 1889',57,-90,-1192970,-5045774,'Canada','North America',121,'',57.0717,-90.1747,'','',-13.3741192963,-95.298326629,-13.3741192963,-95.298326629,-13.3741192963,-95.298326629),('Puskwuche Point well, Ontario',2257,'','Silurian','Lower Silurian','Llandovery-Wenlock',427.40,443.40,6,'Rhuddanian-Telychian',435,428,2,1,'Seismic data available ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'300','1410',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1423,0,'Abundant in situ corals and stromatoporoids in a dark cross-laminated matrix.',51,-80,-2202308,-4753799,'Canada','North America',121,'',51.775,-80.6583,'','',-19.8729802658,-91.0849420712,-19.8729802658,-91.0849420712,-19.8729802658,-91.0849420712),('Beluga well, Hudson Bay, Ontario',2258,'','Silurian','Lower Silurian','Llandovery-Wenlock',427.40,443.40,6,'Rhuddanian-Telychian',435,428,2,1,'Seismic data available ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'500','1889',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1423,0,'Cuttings only\nRichly fossiliferous limestone with brachiopods, crinoids, corals and stromatoporoids.',59,-88,-1023297,-4838153,'Canada','North America',121,'',59.215,-88.5572,'','',-11.6021874175,-93.7852893217,-11.6021874175,-93.7852893217,-11.6021874175,-93.7852893217),('Nadwornaja',2259,'','Jurassic','Upper Jurassic','Kimmeridgian-Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,150,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250','1713',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1424,1021,'Barrier reef.\nReservoirs in reefs and in back reef.',48,24,5209797,2230913,'Ukraine','Europe',301,'',48.6667,24.5,'','',32.7565368832,33.9410702606,32.7565368832,33.9410702606,37.1863263591,36.9547909501),('Cobreces, Cantabria',2260,'Altamira','Cretaceous','Upper Cretaceous','lower Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,98,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','30',NULL,NULL,NULL,'2','10 - 100 m','14','3',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','4','Stromatoporoids','5','Rudists','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'15','65','20',0,'no',0,'no','2','6 to 24 reef building species','16','1','Constructor guild','1','Present','1','Present','3','Pronounced zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1425,0,'Up to 30 m thick reefal interval.\nFused patch reefs at shelf edge.\nPrimary relief 2-5 m.\n12 species of chaetetids and corals.\nRudists, chaetetid sponges, Archaeolithothamnium and massive to foliose corals as reef builders.\nReef growth terminated by siliclastics.',43,-4,3925616,116736,'Spain','Europe',304,'',43.3833,-4.2167,'WAHR','23537',35.3303476429,2.78193458834,35.3303476429,2.78193458834,34.2997209986,0.324293440537),('Kanchurinsk, Bashkiria',2261,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'240','214',1,'Temperate',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','2','Algae','28','Palaeoaplysina - microbes - bryozoans - Tubiphytes - (corals)','2','Green algae','0','40','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1426,1413,'See reef 214',52,55,3332988,4808827,'Russia','Asia',624,'',52.8167,55.75,'','',22.6850488761,44.5131891143,22.6850488761,44.5131891143,30.5902432059,20.4262137044),('Kanchurinsk, Bashkiria',2262,'','Permian','Lower Permian','Sakmarian-Artinskian',283.50,298.90,15,'Sakmarian - Kungurian',277,284,2,1,'Seismic data available ',1,'True reef','4','More than 500 m thick','750',NULL,NULL,NULL,'4','More than 1000 m',NULL,'240',NULL,1,'Temperate',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','2','Algae','28','Palaeoaplysina - microbes - bryozoans - Tubiphytes - (corals)','2','Green algae','0','40','60',0,'no',0,'no','3','25 or more reef building species','40','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1426,1413,'Gas field.\n> 750 m thick.\nSee reef 214 for additional remarks.',52,55,3829461,5122749,'Russia','Asia',624,'',52.8167,55.75,'','',23.0120189454,44.9839785443,23.0120189454,44.9839785443,32.0284371941,25.6150359501),('Stolyarovsk, Bashkiria',2263,'','Permian','Lower Permian','Sakmarian-Artinskian',283.50,298.90,15,'Sakmarian - Kungurian',277,284,3,1,'Seismic data available ',1,'True reef','4','More than 500 m thick','800',NULL,NULL,NULL,'4','More than 1000 m',NULL,'240','2262',1,'Temperate',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','2','Algae','3','Microbes','28','Palaeoaplysina - microbes - bryozoans - Tubiphytes - (corals)','2','Green algae','0','80','20',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1426,1413,'Oil field.\n800 m thick.\nUpper Sakmarian-Artinskian reef.\nSee reef 214 for additional remarks.',52,55,3829461,5122749,'Russia','Asia',624,'',52.8167,55.75,'','',23.0120189454,44.9839785443,23.0120189454,44.9839785443,32.0284371941,25.6150359501),('Kuganak, Bashkiria',2264,'','Permian','Lower Permian','Asselian-Sakmarian',290.10,298.90,14,'Gzhelian - Asselian',290,294,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'240','214',1,'Temperate',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','2','Algae','28','Palaeoaplysina - microbes - bryozoans - Tubiphytes - (corals)','2','Green algae','20','40','40',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1413,0,'See reef 214.',54,55,3447524,4692159,'Russia','Asia',624,'',54.0167,55.8,'','',23.6766583202,43.7932407464,23.6766583202,43.7932407464,31.711756207,21.3453403772),('Chebenki, Bashkiria',2265,'','Permian','Lower Permian','Asselian-Sakmarian',290.10,298.90,14,'Gzhelian - Asselian',290,294,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'240','214',1,'Temperate',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','2','Algae','28','Palaeoaplysina - microbes - bryozoans - Tubiphytes - (corals)','2','Green algae','20','40','40',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1413,0,'See reef 214.',51,55,3249695,4892433,'Russia','Asia',624,'',51.95,55.7167,'','',22.2066917772,45.3717699714,22.2066917772,45.3717699714,30.8423313801,23.5399561179),('Brynzeny-Gordineshty, Moldavia',2266,'','Neogene','Miocene','upper Tortonian',7.30,9.00,32,'Tortonian - Gelasian',6,7,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','60',NULL,NULL,NULL,'3','More than 100 m',NULL,'90',NULL,2,'Cold - water',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','2','Algae','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','40','0','60',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild','1','Present',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1428,1413,'NW-SE trending reef belt from Brichany in N to Domyaska in S.\n\n60 m thick reef mound.\nMain reef builders are Rhodophyta.\n\nBryozoans and vermetids are less abundant.\nThere are plently of bivalves, foraminifera and echinoderms.',48,27,6302137,2276839,'Moldova','Europe',NULL,'',48.1667,27.3333,'','',47.8923078554,25.1084795787,47.9326130681,25.4121401675,47.5901490885,27.179517196),('Petrikan, Moldavia',2267,'','Neogene','Miocene','middle Sarmatian',11.80,12.50,31,'Burdigalian - Serravallian',14,12,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'400',NULL,2,'Cold - water',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','60','0','40',0,'no',0,'no','2','6 to 24 reef building species','11','2','Baffler guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1429,1413,'Reef belt from Kagul through Kishinev-Kamenka to Ledichev.\nBryozoans predominate:\nMembranipora lapidosa, Nitscheina kischinewensis, Schizoporella eichwaldi, S. tetes, S. variabilis, S. mariae...\nAlgae: Lithophyllum ucrainicum, Melobesia badjii, Jania dnestrovica...\nOthers are bivalves and serpulids.\n\nBase of buildups are bryozoan limestones, middle part with bryozoan-algae-foram (Nubecularia) limestones, upper part with algae-Nubecularia limestone.',47,28,6125638,2342946,'Moldova','Europe',NULL,'',47.0833,28.8333,'','',46.6467786702,25.9348162361,46.6857684526,26.0602338652,46.2096666324,28.5176688303),('Kagul, Moldavia',2268,'','Neogene','Miocene','middle Sarmatian',11.80,12.50,31,'Burdigalian - Serravallian',14,12,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'400','2267',2,'Cold - water',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','60','0','40',0,'no',0,'no','2','6 to 24 reef building species','10','2','Baffler guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1429,1413,'See reef 2267.',45,28,5985802,2324172,'Moldova','Europe',NULL,'',45.9167,28.25,'','',45.4658765297,25.4199923501,45.5053497393,25.5427447406,45.0486275669,27.9208926812),('Kunicha-Kamenka, Moldavia',2269,'','Neogene','Miocene','middle Sarmatian',11.80,12.50,31,'Burdigalian - Serravallian',14,12,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'400','2267',2,'Cold - water',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1429,1413,'See reef 2267.',48,28,6234272,2302229,'Moldova','Europe',NULL,'',48,28.6667,'','',47.5584753083,25.7179200763,47.5976678302,25.8450271102,47.1278273831,28.3721784209),('Letitshev',2270,'','Neogene','Miocene','middle Sarmatian',11.80,12.50,31,'Burdigalian - Serravallian',14,12,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'400','2267',2,'Cold - water',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','60','0','40',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1413,0,'See reef 2267.',49,27,6394379,2176027,'Ukraine','Europe',301,'',49.3667,27.65,'','',48.8978258721,24.6306737901,48.938029222,24.7597496012,48.5039826174,27.4017855678),('Lazo, Moldavia',2271,'','Neogene','Miocene','middle Sarmatian',11.80,12.50,31,'Burdigalian - Serravallian',14,12,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'400','2267',2,'Cold - water',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','60','0','40',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1429,1413,'See reef 2267.',47,28,6182474,2258404,'Moldova','Europe',NULL,'',47.5667,28.0167,'','',47.10866118,25.0986010929,47.1484324029,25.2243300702,46.7006762144,27.72398841),('Washington Co., Arkansas',2272,'Pitkin','Carboniferous','Lower Carboniferous','Chesterian',331.00,336.00,12,'middle Visean - Serpukhovian',329,326,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','50','50',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','20','0',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild','1','Present','1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1431,1517,'Early Serpukhovian\n15-20 m thick, 50 m lateral extension.\nType I thrombolitic mounds with about 3 m synoptic relief.\nInterfingering with oolitic and bioclastic grainstones.\nReticulate framework and encrusted metazoans.\nThrombolites-encrusting bryozoans-fenestrate bryozoans (Archimedes dominant)-encrusting forams-spicular alga as main mound builders.\nTyrpanites and acrothoracican barnacle borings according to ref. 1517.',35,-94,-1594493,-3902270,'United States','North America',101,'',35.9167,-94.3333,'WAHR','76852',-23.6273359116,-49.8365235421,-23.6273359116,-49.8365235421,-11.4589033353,-71.3967705422),('Madison Co., Arkansas',2273,'Pitkin','Carboniferous','Lower Carboniferous','Chesterian',331.00,336.00,12,'middle Visean - Serpukhovian',329,326,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','50','50','2272',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','20','0',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild','1','Present','1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1431,1517,'See reef 2272.',36,-93,-1611449,-3864836,'United States','North America',101,'',36,-93.9167,'','',-23.8571006926,-49.5519373979,-23.8571006926,-49.5519373979,-11.6038058507,-71.0745847027),('Searcy Co., Arkansas',2274,'Pitkin','Carboniferous','Lower Carboniferous','Chesterian',331.00,336.00,12,'middle Visean - Serpukhovian',329,326,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','6',NULL,NULL,NULL,'2','10 - 100 m',NULL,'50','2272',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1431,0,'Type II thrombolitic mounds of ref. 1431.\n6 m synoptic relief.\nThrombolites-encrusting bryozoans-fenestrate bryozoans-encrusting forams-spicular alga as mound builders.\n\nPhylloid algae more common than in type I mounds (reefs. 2272, 2273).',35,-92,-1717823,-3765599,'United States','North America',101,'',35.8167,-92.5333,'WAHR','76853',-24.8765336703,-49.0032103987,-24.8765336703,-49.0032103987,-12.4365977042,-70.2855656005),('Battle Mountain, Nevada',2275,'Harkless','Cambrian','Lower Cambrian','upper Botomian - Toyonian',504.50,514.00,1,'Nemakit/Daldynian - Toyonian',520,513,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','15','20',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','58','Archaeocyaths - microbes (Renalcis, Epiphyton, Girvanella) - corals',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1433,1995,'Dominated by Renalcis and Epiphyton. Proaulopora.\nArchaeocyathids (important taxa only): Mackenziecyathus, Siderocyathus, Keriocyathus, Archaesycon, Molybdocyathus.\n\nAbstract of ref. 1995:\nAbstract: Several new occurrences of archaeocyathan-calcimicrobe-built reefs have been discovered in the upper Harkless Formation (Bonnia-Olenellus Zone) in\nEsmeralda County, Nevada. Initial analyses of the paleoecology of these reefs show that the community structure consisted of several genera of archaeocyaths acting as the framework entity with calcimicrobes acting as the binding entity. Since the reefs are found in the upper Harkless, they are among the youngest known\nmetazoan-built reefs in western North America and represent the last pulse of metazoan reef building prior to their global disappearance in the Middle to Late\nCambrian. The mechanism or mechanisms that contributed to the demise of the metazoan reefs are unknown; therefore, we are studying these reefs in part to test hypotheses concerning the collapse of the Early Cambrian metazoan reef communities. \n\nThese reefs contain the typical assemblage of Early Cambrian reef dwellers such as trilobites, echinoderms, and brachiopods; however, at one locality coralomorphs\nare conspicuously present. These coralomorphs are approximately 12 cm long by 18 cm wide, are found scattered throughout the reefs, and constitute only a small percentage of the reef by volume. The coralomorphs have definite polygonal corallites which do not share walls, and resemble cerioid tabulate corals without obvious tabulae. Septa occur as obscure processes that project into the center of the corallites, dividing the corallites in half. These coralomorphs are similar to the genus Rosellatana, Kobluk, 1984 from the Lower Cambrian Cassiar Mountains of British Columbia. ',41,-116,-1987590,-9240912,'United States','North America',101,'',41.0333,-116.9833,'WAHR','81004',34.1473202567,-132.518514834,34.1473202567,-132.518514834,34.1473202567,-132.518514834),('Wat Thep Nimit Banphot',2276,'','Triassic','Middle/Upper Triassic','Ladinian-Carnian',227.00,242.00,17,'Induan - early Carnian',235,228,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1434,0,'Corals (Montlivaltia, Thecosmilia), calcareous sponges and bryozoans are common. Rare solenoporaceans and dasycladaceans.\nForams rare and not diverse.',13,102,38329,10098822,'Thailand','Asia',604,'',13.625,102.4583,'','',-12.376236686,106.276596864,-12.376236686,106.276596864,24.1953544506,106.042614113),('Chom Bung',2277,'','Permian','Middle Permian','Murghabian',265.10,268.80,16,'Roadian - Changhsingian',261,267,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'4',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','9','Tubiphytes','67','Corals - Tubiphytes - bryozoans',NULL,NULL,'80','0','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite',NULL,'','0','',0,'No or unknown reservoir potential',1435,0,'Tabulate and massive rugose corals (Waagenophyllids) including a new genus.\nTubiphytes common.\nAdditionally fenestellid bryozoans.',13,99,-2874265,8332760,'Thailand','Asia',604,'',13.4167,99.5333,'','',-32.7414142125,97.1226786931,-32.7414142125,97.1226786931,-27.0057050408,99.5512791414),('Wat Samakki Tham',2278,'','Permian','Upper Permian','lower Murghabian',265.10,268.80,16,'Roadian - Changhsingian',261,267,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1436,0,'Black massive limestone with scattered corals.\nTabulata (Protomichelinia, Sinopora)\nRugosa: Solitary, fasciculate (Pseudohuangia) and massive.\nPseudohuangia up to 1 m in diameter.\nCalcareous sponges locally abundant. Some brachiopods.',16,101,-2370085,8463808,'Thailand','Asia',604,'',16.4833,101.7833,'','',-28.5997188054,115.124183655,-28.5997188054,115.124183655,-4.24094564315,101.867904863),('Pha Chan Dai',2279,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,1,0,'Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1437,0,'Gray massive limestones.\nStromatoporoids, Tabulata (Heliolites), massive and solitary Rugosa (Ptenophyllidae).',17,101,162502,11667630,'Thailand','Asia',604,'',17.7194,101.95,'WAHR','82082',-2.48950492136,93.1130154156,-2.48950492136,93.1130154156,-35.6985037698,101.871718279),('Ban Nong Tum',2280,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'18',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1437,0,'grey massive boundstones and packstones with stromatoporoids, chaetetids, corals (tabulata and rugosa), brachiopods, crinoids.\nStromatoporoids diverse.\nTabulata with many genera.\nRugosa solitary, fasciculate and massive.\n\nRecognized taxa (incomplete list):\nThamnopora\nScoliopora\nCaunopora\nAlveolitidae\nHeliolites\nThamnophyllum\nPhillipsastrea',17,102,213830,11632142,'Thailand','Asia',604,'',17.2458,102.0611,'','',-2.13680611948,92.7793818572,-2.13680611948,92.7793818572,-35.6846460385,102.469023759),('Pandan Reservoir',2281,'','Triassic','Upper Triassic','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,211,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','50',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'5','90','5',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1438,0,'Reefal debris\nAbout 50 m thick in well\nCorals, sponges, Ladinella, Tubiphytes, bryozoans, stromatolites.\nCorals:\nRetiophyllia clathrata\nThamnasteriamorpha multisepta n. sp.\nPamiroseris minima n. sp.',1,103,347727,10967169,'Singapore','Asia',NULL,'',1.2972,103.7514,'','',7.91281869946,117.455386539,7.49838281838,117.231629963,4.40450874164,117.227341227),('Khao Thao, Phangnga',2282,'','Triassic','Upper Triassic','Upper Triassic',201.30,237.00,18,'late Carnian - middle Hettangian',218,216,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',1439,0,'Algae are frequent:\nPseudolithocodium, Solenopora, Thaumatoporella\nFasciculate corals poorly preserved.',8,98,517514,10094257,'Thailand','Asia',604,'',8.4278,98.6333,'','',7.65680989473,108.954610859,7.65680989473,108.954610859,6.01132490726,108.063421965),('Klo Tho',2283,'','Jurassic','Upper Jurassic','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,153,1,0,'Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','37','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1440,1659,'Limestone of Ban Phu Kloe with large colonies of corals.\nMore than 35 coral species discovered. 3 new species.\nAmmonites (Virgatosphinctes, Spiticeras) at Mae Sot. \n\nLimestones suggest strong bacterial activity.\nM-sized coral colonies.\n\nCould be Middle Jurassic and duplicate of reef 402. ',16,98,2744452,11596214,'Thailand','Asia',604,'',16.5,98.9,'','',30.6081518327,113.645211795,30.6081518327,113.645211795,27.2950383508,116.303681164),('Ban Ai, Chiang Mai',2284,'','Permian','Middle Permian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,267,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',260,0,'Massive Waagenophyllidae.',19,99,-2887982,9365964,'Thailand','Asia',604,'',19.5333,99.1167,'','',-31.7555833281,89.9678877225,-31.7555833281,89.9678877225,-28.9082153682,92.953188547),('Mae Hong Son',2285,'','Permian','Lower Permian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,266,2,0,'Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1441,2471,'Lower to Middle Permian limestone of mostly reefal appearance in whole region.\nMore details on age and fauna in Flügel (1997), ref. 2471',19,98,-4375983,9051425,'Thailand','Asia',604,'',19.3,98,'WAHR','61752',-32.8331367351,89.9086364939,-32.8331367351,89.9086364939,-29.884702385,93.4793109138),('Guguk Bulat, Sumatra',2286,'','Permian','Middle Permian','Murghabian',265.10,268.80,16,'Roadian - Changhsingian',261,267,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','2','Algae','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','2','Green algae','5','95','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1442,0,'Algae are very abundant (e.g. Ungdarella) but not studied.\nSponges are common. One species especially common: Molengraffia tabulata.\nCorals: very scarce fasciculate tabulates (Aulopora) and scarce solitary rugose, but abundant massive Waagenophyllidae (80 % Wentzelloides, 20 % Ipciphyllum).\n',0,100,-3449292,11423590,'Indonesia','Asia',614,'',-0.55,100.55,'WAHR','75571',-33.2910420621,113.827362254,-33.2910420621,113.827362254,-27.1308947311,106.715269526),('Pha Tok',2287,'Ban Khok Phai','Devonian','Middle Devonian','Givetian - lower Frasnian',382.70,387.70,10,'Givetian - early Famennian',375,385,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'3',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1443,0,'Stromatoporoids very abundant: Stachyodes, Amphipora, Actinostroma, Clathrodictyon, Stromatopora ...\nTabulata common: Thamnopora, Coenites\nRugosa rare and only solitary: Ptenophyllidae',18,101,130938,11692853,'Thailand','Asia',604,'',18.025,101.8514,'WAHR','82099',-2.70414380346,93.3501721286,-2.70414380346,93.3501721286,-35.7306656667,101.479985023),('Nagyvisnyó',2288,'','Carboniferous','Upper Carboniferous','Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,301,1,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','2','Algae','3','Microbes','24','Tubiphytes - algae - cyanophyceans - (bryozoans) - (sponges)','2','Green algae','10','80','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1445,0,'Recrystallized phylloid algae predominate.\nMinor components are Girvanella, Eotuberitina, fragments of Rugosa, bryozoans, brachiopods, Tubiphytes.',48,20,-1169928,3465529,'Hungary','Europe',336,'',48.1667,20.4167,'','',-14.7509313758,33.0603941893,-14.7509313758,33.0603941893,-3.07116599345,3.31943155306),('Quanah, Texas',2289,'Chappel','Carboniferous','Lower Carboniferous','Osagean',346.70,358.90,11,'late Famennian - early Visean',351,345,2,1,'Seismic data available ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','13','Echinoderms','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'30','0','70',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','2','Medium zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1446,0,'Mudstone mound core with 0-65 % crinoids, 0-5 % bryozoans and 0-10 % miscellaneous skeletal grains.\nOther is micrite.\n',34,-99,-2452609,-4941306,'United States','North America',101,'',34.3,-99.75,'','',-25.6928420802,-63.7035561749,-25.6928420802,-63.7035561749,-9.7532460373,-102.113879473),('East Java Sea I',2290,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,21,2,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate',4,'Basin','4a','Shallow basin','2','Below fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',685,0,'Well JS 14-A-1\nType 3 bioherms of ref. 685.\nBasinal lime mud mounds, low growth-ratio.',-6,113,-769053,12971761,'Indonesia','Asia',614,'',-6.4167,113.3,'','',-4.71086344479,110.522843549,-4.71086344479,110.522843549,-8.39456590159,113.156474622),('East Java Sea II',2291,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,21,2,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate',4,'Basin','4a','Shallow basin','2','Below fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',685,0,'Well JS 31A-1\nType 3 bioherms of ref. 685.\nBasinal lime mud mounds, low growth-ratio.',-6,112,-796752,12912406,'Indonesia','Asia',614,'',-6.55,112.7667,'','',-4.84347367843,109.99093334,-4.84347367843,109.99093334,-8.42767313356,112.605149769),('East Java Sea III',2292,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,21,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',685,0,'Type 4 buildup (not drilled).\nSlope pinnacle reef with low growth-ratio.\nAssumed coral boundstones.',-6,113,-823790,12983146,'Indonesia','Asia',614,'',-6.8333,113.4,'','',-5.12760870871,110.621929547,-5.12760870871,110.621929547,-8.82234377767,113.17741077),('East Java Sea IV',2293,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,21,2,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick','95',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,1,'Temperate',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','12','Foraminifera','13','Algae - encrusting forams','1','Red algae','10','20','70',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',685,0,'Type 5 buildup.\nBank-edge foram-algal shoal, high growth-ratio.\nE-W trending.\nAlternation of massive encrusting red algal and foraminiferal debris (with Lepidocyclina and Sphaerogypsina).\nThickness varies between 16 and 100 m.',-6,113,-833263,12938574,'Indonesia','Asia',614,'',-6.85,113,'','',-5.14375698721,110.223154187,-5.14375698721,110.223154187,-8.76534909813,112.779335894),('East Java Sea V',2294,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,21,1,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'2',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',685,0,'Type 6 buildup.\nBank-edge coral reef.\nTabular (high grwoth-ratio) morphology.',-6,113,-750635,12945531,'Indonesia','Asia',614,'',-6.25,113.0667,'','',-4.54384374787,110.290440047,-4.54384374787,110.290440047,-8.18792631844,112.957274496),('East Java Sea I',2295,'','Neogene','Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,19,2,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate',4,'Basin','4a','Shallow basin','2','Below fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',685,0,'see reef 2290.',-6,113,-854725,12721729,'Indonesia','Asia',614,'',-6.4167,113.3,'','',-4.71086344479,110.522843549,-4.71086344479,110.522843549,-8.39456590159,113.156474622),('East Java Sea III',2296,'','Neogene','Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,19,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',685,0,'see reef 2292.',-6,113,-910656,12729584,'Indonesia','Asia',614,'',-6.8333,113.4,'','',-5.12760870871,110.621929547,-5.12760870871,110.621929547,-8.82234377767,113.17741077),('East Java Sea V',2297,'','Neogene','Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,19,2,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,1,'Temperate',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','12','Foraminifera','13','Algae - encrusting forams','1','Red algae','0','80','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',685,0,'See reef 2293.',-6,113,-916690,12684807,'Indonesia','Asia',614,'',-6.85,113,'','',-5.14375698721,110.223154187,-5.14375698721,110.223154187,-8.76534909813,112.779335894),('East Java Sea V',2298,'','Neogene','Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,19,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'2',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',685,0,'See reef 2294.',-6,113,-834139,12696805,'Indonesia','Asia',614,'',-6.25,113.0667,'','',-4.54384374787,110.290440047,-4.54384374787,110.290440047,-8.18792631844,112.957274496),('Parigi A, offshore NW Java',2299,'Parigi','Neogene','Miocene','upper middle Miocene',11.60,13.80,31,'Burdigalian - Serravallian',14,12,3,1,'Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'80',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1295,0,'',-6,107,-852946,12068366,'Indonesia','Asia',614,'',-6,107.4167,'','',-4.66116849889,106.018014374,-4.66116849889,106.018014374,-6.85869179442,106.789116268),('Parigi, offshore NW Java',2300,'Parigi','Neogene','Miocene','upper middle Miocene',11.60,13.80,31,'Burdigalian - Serravallian',14,12,3,1,'Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'80','2299',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1295,0,'',-5,108,-813345,12134988,'Indonesia','Asia',614,'',-5.75,108,'','',-4.40696931719,106.598239113,-4.40696931719,106.598239113,-6.66821484358,107.395743452),('Tidwell Hollow, Alabama',2301,'Chickamauga','Ordovician','Upper Ordovician','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,457,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','60','40','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1733,1734,'Chickamauga Limestone.\r\nDominant bryozoans, nodular Solenopora and demosponge Dystactospongia. Some calathiids.',34,-86,-2941612,-6845250,'United States','North America',101,'1449',34,-86.5,'',NULL,-18.8615136263,-118.204428492,-18.8615136263,-118.204428492,-18.8615136263,-118.204428492),('Hunyuan, Shanxi',2302,'Gushan-Changshan','Cambrian','Upper Cambrian','Gushanian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,497,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1450,0,'Storm dominated ramp system.\nMounds composed of stromatolites, microbial laminites, oncolites, cyanobacteria (Epiphyton, Girvanella etc.), crinoids, bryozoans.\nUp to 3 m thickness, 0.5 m to 6 m across.\nThrombolitic buildups in Gushan Formation.\nStromatolitc buildups in Changshan Formation.',39,113,5883571,-16082198,'China','Asia',602,'',39.7,113.6667,'','',20.443279721,103.886876808,20.443279721,103.886876808,20.443279721,103.886876808),('Qinhuangdao, Hebei',2303,'Gushan','Cambrian','Upper Cambrian','Gushanian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,498,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1450,0,'Storm dominated ramp system.\nSee also reef 2302.\nThrombolitic buildups in Gushan Formation.',39,119,5947060,15634995,'China','Asia',602,'',39.9333,119.5833,'','',18.2991865889,99.6328527928,18.2991865889,99.6328527928,18.2991865889,99.6328527928),('Hunyuan, Shanxi',2304,'','Cambrian','Upper Cambrian','Fengshanian',477.70,485.40,3,'Franconian - Tremadocian',488,491,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1449,0,'Change from storm dominated ramp-system to epeiric carbonate platform.\nStromatolitic buildup.',39,113,5860529,15966555,'China','Asia',602,'',39.7,113.6667,'','',20.0435278133,103.712647052,20.0435278133,103.712647052,20.0435278133,103.712647052),('Lishi, Shanxi',2305,'','Cambrian','Upper Cambrian','Fengshanian',477.70,485.40,3,'Franconian - Tremadocian',488,491,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1449,0,'See reef 2304.',37,111,6071625,-15866699,'China','Asia',602,'',37.5,111.1667,'','',22.9031389901,104.455986252,22.9031389901,104.455986252,22.9031389901,104.455986252),('Planany, Kutná Hora',2306,'','Cretaceous','Upper Cretaceous','lower Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,93,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','19',NULL,'','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1451,0,'Redeposited coral limestones\nMany ahermatypic solitary forms.\n19 species of corals listed.',50,15,5068921,1416093,'Czech Republic','Europe',331,'',50.05,15.0333,'','',45.5723456115,17.4508993613,45.5723456115,17.4508993613,43.2976770134,16.1331237284),('Korycany',2307,'','Cretaceous','Upper Cretaceous','upper Cenomanian',93.90,100.50,25,'late Cenomanian - early Campanian',91,95,3,0,'Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','24',NULL,'','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1451,1471,'24 species of corals listed.\nAll reworked.',50,14,5094346,1369770,'Czech Republic','Europe',331,'',50.2667,14.4833,'WAHR','34737',45.0824349366,17.9002633158,45.0824349366,17.9002633158,42.3798632006,16.232132887),('Bayan Gol, Zavkhan Basin',2308,'Tsagaan Olom - Bayan Gol','Cambrian','Lower Cambrian','Nemakit-Daldynian',529.00,541.00,1,'Nemakit/Daldynian - Toyonian',520,535,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','2',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1452,0,'Calcimicrobial domal bioherms, up to 1 m in height and 2 m in diameter. \nDominated by Korilophyton. Tarthinia is a minor component.\nBioherm stacks as substrate for domal stromatolites.\nShould be plate 419.\n\nAbstract of ref. 1452: The Neoproterozoic-Cambrian succession in the Zavkhan Basin of western Mongolia preserves early Cambrian bioconstructions of Nemakit-Daldynian to Botomian age. As elsewhere (Siberia, Morocco), the Nemakit-Daldynian bioconstructions in the upper Tsagaan Gloom Formation to lower Bayan Gol Formation interval were purely calcimicrobial. Spectacular calcimicrobial \'patch reefs\' of presumed Tommotian age are present in the lower Bayan Gol Formation. In contrast, late Atdabanian-early Botomian bioconstructions are varied and well developed in the upper Salaany Gol Formation including, in addition to calcimicrobial bioherms, Gordonophyton-Razumovskia crusts, radiocyathan-archaeocyathan bioherms and thickets of the ramose archaeocyath Cambrocyathellus.\n\nThese latter Zavkhan Basin buildups show some ecological and sedimentological features in common with coeval bioconstructions in South Australia, which also developed under a tectonically active regime.',46,96,-1633775,3507531,'Mongolia','Asia',NULL,'',46.7,96.3,'WAHR','22947',1.84921884439,-65.9959237658,1.84921884439,-65.9959237658,1.84921884439,-65.9959237658),('Tayshir, Zavkhan Basin',2309,'','Cambrian','Lower Cambrian','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,524,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','3',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','1','3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1452,0,'Calcimicrobial patch reefs in sandstone.\nVery shallow water. Growth up to sea level indicated by flat upper tops.\nMounds up to 0.7 m thick and 3 m in diameter.\nShould be plate 419.',46,96,-1635979,3523966,'Mongolia','Asia',NULL,'',46.7,96.5167,'WAHR','22948',5.39617349561,-52.4699182028,5.39617349561,-52.4699182028,5.39617349561,-52.4699182028),('Salaany Gol, Zavkhan Basin',2310,'Salaany Gol','Cambrian','Lower Cambrian','Atdabanian/Botomian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,515,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','40',NULL,NULL,NULL,'2','10 - 100 m','11','15',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','35','1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1452,0,'40 m thick interval with several mounds.\nIndividual mounds up to 5 m thick and more than 10 m long.\nWell developed cements.\nThree types of bioconstructions:\n- Gordonophyton-Razumovskia crusts supporting a cryptic community of coralomorphs, cribricyaths and archaeocyaths in shelter cavities.\n- radiocyathan-archaeocyathan bioherms. 29 species of archaocyaths, 4 species of calcimicrobes, 2 problematic reef builders.\n- calcimicrobial bioherms with Gordonophyton, Batinevia, Proaulopora and rafts of Razumovskia. Archaeocyaths as debris.\nShould be plate 419.',46,95,-1605924,3473155,'Mongolia','Asia',NULL,'',46.8667,95.8,'WAHR','22940',7.36969001398,-38.623483524,6.47937460461,-42.5244759575,6.47937460461,-42.5244759575),('Kotuikan River, Siberia',2311,'Medvezhin','Cambrian','Lower Cambrian','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,527,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','2',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1453,0,'Thrombolite boundstone biostrome with Renalcis texture. Individual heads up to 1.2 m high and 2.1 m wide. \nAssociated well-stratified channel grainstones.',70,103,-3954924,226658,'Russia','Asia',624,'',70.6167,103.4833,'WAHR','50431',-9.48408159728,-71.5612304711,-9.48408159728,-71.5612304711,-9.48408159728,-71.5612304711),('Wyaralong, Attunga, New South Wales',2312,'Moore Creek Limestone','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','18',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','0','70',0,'no',0,'no','2','6 to 24 reef building species','17','1','Constructor guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1454,1463,'buildup with more 50 % organisms.\nStromatoporoids as principal reef builders. \nAdditionally Alveolites, Heliolites and Favosites.\n6-18 m thickness.',-30,150,-2612854,17681837,'Australia','Oceania',801,'',-30.95,150.8667,'WAHR','24210',-26.0113170544,137.271754364,-26.0113170544,137.271754364,-26.0484431755,175.347844862),('Jurkowice-Budy, Góry Swietokrzyskie',2313,'','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1456,0,'',50,21,-1776329,1451863,'Poland','Europe',301,'',50.6333,21.35,'WAHR','83035',-18.8814338967,13.6397731995,-18.8814338967,13.6397731995,7.40570502284,-66.8206407347),('Denizli Molasse Basin',2314,'Tokca','Paleogene','Oligocene','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','10',NULL,NULL,NULL,'1','Less than 20 m','10',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','15','1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1457,2781,'Reef limestones within a fan-delta sequence.\nIsolated coral mounds, up to 10 m in diameter.\nWas Oligo-Miocene. Age refined by ref. 2781\nÜctepeler Reef Member in the lower Tokca Formation',37,29,4855890,2755140,'Turkey','Asia',522,'',37.75,29.5,'WAHR','88771',36.6585265628,25.120290386,36.6585265628,25.120290386,34.4970340096,28.0117161134),('Cabo Espichel',2315,'','Cretaceous','Lower Cretaceous','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,133,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'100',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',792,0,'Biostrome dominated by a low diversity coral (microsolenid) community.\nRare encrustations of Lithocodium-Bacinella, sponges.\nBorings by Lithophagid bivalves.',38,-9,3231506,-574353,'Portugal','Europe',304,'',38.4333,-9.1833,'','',24.0994060678,5.44447899742,24.0994060678,5.44447899742,28.6464284266,1.86892003697),('Shahmirzad, Elburz',2316,'Mila','Cambrian','Middle/Upper Cambrian','Middle-Upper Cambrian',485.00,509.00,2,'Middle Cambrian - Dresbachian',502,499,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','6','2','10 - 100 m wide','1','2','10 - 100 m','30','1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1501,2165,'Calcareous demosponges (Rankenella) occupy 50 % of the reef volume.\nSponges encrusted by bacteria\nAbstract of ref. 1501:\nMiddle and Late Cambrian reefs were built mainly by cyanobacterial communities. A few reefs with a metazoan as well as an algal component, however, are known from this interval. A Middle Cambrian reef formed primarily by spicular demosponges is described here from the Mila Formation in the Elburz Mountains, northern Iran. The reef is enclosed within calcareous grainstones which contain terminal Middle Cambrian (late Mayan) trilobites. The Mila Formation reef was constructed by sponges of the family Anthaspidellidae and bacterial (algal?) sheaths, and is the earliest metazoan reef to be documented from the interval after the demise of archaeocyath sponges. The reefal community is typical of subsequent reefal communities of Early-Middle Ordovician age. The Ordovician examples differ only by the incorporation of additional metazoan elements.',35,52,-1782428,13720339,'Iran','Asia',505,'',35.7167,52.2222,'WAHR','22821',-43.4632875221,57.6409161831,-50.5213133874,68.1846854164,-50.5213133874,68.1846854164),('Yangshuo, Guilin, Guangxi',2317,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',1462,0,'',24,110,-1114308,10703201,'China','Asia',602,'',24.7833,110.4667,'','',-12.2964002839,85.5824402564,-12.2964002839,85.5824402564,-14.8097292518,109.796687423),('Mortera, Cantabria',2318,'','Cretaceous','Upper Cretaceous','upper Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,84,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','4','Stromatoporoids','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1464,0,'Small bioherms dominated by silicified Millepora.\nBioclastic matrix with bryozoans, some bivalves and abundant foraminifera.\nCunnolites meadows above hydrozoan bioherms',43,-3,4140573,-13808,'Spain','Europe',304,'',43.4167,-3.9833,'WAHR','24250',36.350629631,0.732636707035,36.350629631,0.732636707035,37.0633670088,-1.05836838674),('Nago, Trento',2319,'','Paleogene','Eocene','Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,35,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','12',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','10','60','30',0,'no',0,'no','3','25 or more reef building species','32','3','Binder guild','1','Present',NULL,'','2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1468,1466,'Coral-algal boundstone facies up to 12 m thick.\nEncrusting and rare branching corals (Actinacis rollei >> Plocophyllia bartai = Cereiphyllia tenuis > Astreopora tecta). \nDiverse coralline algae (Mesophyllum, Lithoporella (23 %), Spongites (20 %), Neogoniolithon). Larger forams and bryozoans also common.\nUp to 70 % of Matrix.\nSurrounded by well bedded packstones and algal crust-branch rudstones.',45,10,5435443,860912,'Italy','Europe',344,'',45.8861,10.8847,'WAHR','13354',41.5917838795,7.63698478943,41.5917838795,7.63698478943,41.4315987408,12.1443435179),('Hanstholm',2320,'','Paleogene','Paleocene','Danian',61.60,66.00,26,'middle Campanian - Danian/Selandian',75,63,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'80','870',2,'Cold - water',4,'Basin','4a','Shallow basin','2','Below fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',NULL,NULL,'90','0','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1469,622,'Fragments of arborescent bryozoans abundant (23-45%)\nEncrusting forms also common.',57,8,6531840,561830,'Denmark','Europe',330,'',57.1167,8.6333,'','',52.5055137631,7.2094845752,52.5055137631,7.2094845752,55.5620661546,7.1057036848),('Wadi Arus, Wadi Hajar',2321,'','Jurassic','Upper Jurassic','upper Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,146,3,0,'Outcropping reef ',3,'Mud mound or bank',NULL,NULL,'3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','1','Low zonation',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1470,0,'Up to 3 m thick beds consisting of microbialite boulders.\nNo in situ reef described.',14,48,-1962373,3787553,'Yemen','Asia',503,'',14.35,48.3833,'','',-23.0448443784,38.2304196525,-23.0448443784,38.2304196525,-19.8811948163,34.0403741359),('Gaurdak',2322,'','Jurassic','Upper Jurassic','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,156,3,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species','30','1','Constructor guild','1','Present',NULL,'','3','Pronounced zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1471,1413,'Turan Platform\nIsolated intra-basin dome-like reef\nMain reef builders are: CORALS: Rhipidogyra, Stylina, Cryptocoenia, Cladophyllia, Thecosmilia, Thamnasteria, Microsolena, Calamophyllia. Rarely: Montlivaltia, Actinastrea, Heliocoenia, Stilosmilia, Comoseris, Anabacia.\nRED ALGAE: Solenopora, rarely Marinella, Ungdarella, Melobesia, Petschoria, Donezella, Komia, Lithophyllum.\nCYANOBACTERIA: Girvanella, Ortonella, Renalcis, Rothpletzella, stromatolites.\nSometimes abundant stromatoporoids, chlorophyta, porifera, bryozoans and others.',37,66,5303351,6126185,'Turkmenistan','Asia',NULL,'',37.8167,66.05,'WAHR','85949',36.324883112,74.609996778,36.324883112,74.609996778,39.1276456217,79.424905502),('Brest II',2323,'','Silurian','Upper Silurian','Wenlock/Ludlow',423.00,433.40,7,'Wenlock - early Pridoli',425,422,1,1,'Seismic data available ',4,'Biostrome','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'50','1112',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',693,0,'',52,23,-2028319,-18936,'Belarus','Europe',NULL,'',52.1333,23.6667,'','',-4.02826107682,-40.8924478344,-4.02826107682,-40.8924478344,-4.02826107682,-40.8924478344),('Peribaltic Depresion',2324,'','Silurian','Upper Silurian','Wenlock/Ludlow',423.00,433.40,7,'Wenlock - early Pridoli',425,422,1,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',693,0,'',55,27,-1555658,-33195,'Belarus','Europe',NULL,'',55,27,'','',-0.750257738127,-42.0706902716,-0.750257738127,-42.0706902716,-0.750257738127,-42.0706902716),('Attawapiskat River, Ontario',2325,'','Silurian','Lower Silurian','Llandovery/Wenlock',427.40,443.40,7,'Wenlock - early Pridoli',425,428,1,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'300',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',871,1423,'',52,-83,-2198242,-4475983,'Canada','North America',121,'',52.9211,-83.4261,'','',-18.4171948218,-92.601326788,-18.4171948218,-92.601326788,-18.4171948218,-92.601326788),('Comeault No. 1, Hudson Bay, Ontario',2326,'','Silurian','Upper Silurian','lower Wenlock?',427.40,433.40,7,'Wenlock - early Pridoli',425,427,2,1,'Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'500',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1423,0,'Wenlock portion of reef 2255',59,-90,-1127562,-4506947,'Canada','North America',121,'',59.6667,-90.8333,'','',-10.4504785018,-86.805261857,-10.4504785018,-86.805261857,-10.4504785018,-86.805261857),('Kaskattama No. 1, Hudson Bay, Ontario',2327,'','Silurian','Upper Silurian','Llandovery/Wenlock',427.40,443.40,7,'Wenlock - early Pridoli',425,428,2,1,'Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'500','2326',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1423,0,'',57,-90,-1436899,-4634926,'Canada','North America',121,'',57.0717,-90.1747,'','',-13.3741192963,-95.298326629,-13.3741192963,-95.298326629,-13.3741192963,-95.298326629),('Puskwuche Point well, Ontario',2328,'','Silurian','Upper Silurian','Llandovery/Wenlock',427.40,443.40,7,'Wenlock - early Pridoli',425,428,2,1,'Seismic data available ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'300','2325',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1423,0,'',51,-80,-2447037,-4349991,'Canada','North America',121,'',51.775,-80.6583,'','',-19.8729802658,-91.0849420712,-19.8729802658,-91.0849420712,-19.8729802658,-91.0849420712),('Beluga well, Hudson Bay, Ontario',2329,'','Silurian','Upper Silurian','Llandovery/Wenlock',427.40,443.40,7,'Wenlock - early Pridoli',425,428,2,1,'Seismic data available ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'500','2326',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1423,0,'',59,-88,-1271545,-4425755,'Canada','North America',121,'',59.215,-88.5572,'','',-11.6021874175,-93.7852893217,-11.6021874175,-93.7852893217,-11.6021874175,-93.7852893217),('Marjum Pass, Central Hourse Range',2330,'Marjum','Cambrian','Middle Cambrian','middle Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,504,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',4,'Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2443,0,'This reef number previously Pen Island Llandovery/Wenlock. More detailed stratigraphy required replacement.\n\nThe mud mounds are thin (<2 m), closely spaced, laterally linked, symmetrical domes composed of massive, fenestral, peloidal\nto clotted microspar with sparse unoriented, poorly sorted skeletal material,\ncalcitized bacterial(?) filaments/tubes and abundant fenestrae and stromatactoid\nstructures.',39,-113,342914,-8268104,'United States','North America',101,'',39.2542,-113.3611,'','',30.9168869951,-132.788698093,31.7006261756,-127.743490579,31.7006261756,-127.743490579),('Gascons, Gaspé, Quebec',2331,'','Silurian','Lower Silurian','lower Wenlock',427.40,430.50,7,'Wenlock - early Pridoli',425,427,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',881,946,'Wenlock portion of reef 1425',48,-64,-3382756,-3305842,'Canada','North America',121,'',48.2333,-64.8333,'','',-21.8455092162,-69.0639864025,-21.8455092162,-69.0639864025,-21.8455092162,-69.0639864025),('Marcil Anticline, Gaspé, Quebec',2332,'','Silurian','Lower Silurian','Llandovery/Wenlock',427.40,443.40,7,'Wenlock - early Pridoli',425,428,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20','2331',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',881,946,'Wenlock part of reef 1426',48,-65,-3390248,-3326365,'Canada','North America',121,'',48.1333,-65.0833,'','',-23.8486818074,-80.4493728718,-23.8486818074,-80.4493728718,-23.8486818074,-80.4493728718),('Raanes Peninsula I',2333,'','Carboniferous','Upper Carboniferous','Moscovian/Sakmarian',290.10,315.20,13,'Bashkirian - Kasimovian',302,304,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'8',NULL,1,'Temperate',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','2','Algae','2','Algae','25','Palaeoaplysina - phylloid algae','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'','1','Present',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',174,307,'',78,-85,3694061,-32646,'Canada','North America',121,'',78.3667,-85.9,'','',29.2823191306,0.251723038039,29.2823191306,0.251723038039,26.8315842753,-24.2659712734),('Rama Ride, Banda Sea',2334,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,22,2,1,'Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','90','10',0,'no',0,'no',NULL,'',NULL,NULL,'','1','Present','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1472,0,'Reefal platform.\nDecimeter-sized coral fragments (e.g. Porites pusilla).\nMany larger foraminifera.\n                                                   \n\nAbstract ref. 1472:\n In December 1995 we dredged early Miocene coral-reef carbonates and early/middle Pliocene slope carbonates outcropping on the submerged Rama Ridge. This indicates that some of the Banda Sea Ridges were present during early Miocene times. Subsequent major tectonic subsidence occurred between middle Miocene and early Pliocene times. These results concur with the hypothesis of a relatively recent age for the North Banda Sea basement. ',-5,127,-2216653,13802207,'Indonesia','Asia',614,'',-5.5,127.5,'WAHR','70939',-5.70162389836,125.700162299,-5.70162389836,125.700162299,-5.5,127.5),('W Kopetdag, Turkmenia',2335,'','Cretaceous','Lower Cretaceous','Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,127,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','80','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','3','Pronounced zonation',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1,0,'Urgonian facies.\r\nComplex and large reef systems, perhaps of barrier type.\r\nreef cores, reef slope, inter-reef lagoons.\r\nReefs mainly formed by corals and algae.',38,57,5082890,5061668,'Turkmenistan','Asia',NULL,'',38,57.6667,'','170614',35.6267793992,67.2405139545,35.6267793992,67.2405139545,36.4674932908,67.1580702141),('Simferopol',2336,'','Triassic','Upper Triassic','Norian-Rhaetian',201.30,228.00,18,'late Carnian - middle Hettangian',218,203,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','50',NULL,NULL,NULL,'3','More than 100 m',NULL,'40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'5','95','0',0,'no',0,'no','2','6 to 24 reef building species','16','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1473,0,'Corals (3 species of \'Thecosmilia, 1 Astraeomorpha, 1 Thamnastraea) sponges (4 species), \'hydrozoans\' (3 species), solenoporaneans, spongiostromata, bryozoans.\nUp to 50 m thick.\nNo detailed description.',45,34,4450250,3080868,'Ukraine','Europe',301,'',45,34.1667,'','',36.2210158872,40.3072961729,36.0418430562,40.4211480807,35.8722115425,42.2343637493),('Rovira-Payandé, Columbia',2337,'Payandé','Triassic','Upper Triassic','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,209,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','7','Bryozoans','2','Corals only',NULL,NULL,'30','60','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1475,0,'Hermatypic corals associated with some bryozoans, crinoids and bivalves.',4,-75,-1387575,-4964760,'Colombia','South America',226,'',4.2167,-75.2,'','',-8.74294874625,-35.4543645106,-8.6423960456,-35.4731883331,-2.11568288869,-44.6225303469),('Curuk Dagh, Antalya',2338,'','Triassic','Lower Triassic','Induan',251.20,252.20,17,'Induan - early Carnian',235,250,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','1','3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1476,0,'Stromatolitic microbialites form mounds up to 40 cm thick (LLH type).',36,30,-750333,3044253,'Turkey','Asia',522,'',36.6833,30.4667,'','',-1.07664076423,38.5813210528,-1.07664076423,38.5813210528,-1.97446669355,33.743514772),('Vedi, Transcaucasia',2339,'','Triassic','Lower Triassic','Induan',251.20,252.20,17,'Induan - early Carnian',235,250,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1476,0,'2 m thick domal microbial biolithite, overlain by bedded platy lime mudstones and microbial limestones.',39,45,1630619,4246667,'Armenia','Europe',526,'',39.8333,45,'','',9.01726493783,56.7288450989,9.01726493783,56.7288450989,16.309613066,53.5137265006),('Abadeh',2340,'','Triassic','Lower Triassic','Induan',251.20,252.20,17,'Induan - early Carnian',235,250,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1477,0,'Several m thick zone of \'algal biolithite\'.\nStromatolites-thrombolites unit.',31,52,1236038,5572511,'Iran','Asia',505,'',31.1,52.6667,'','',-0.782294722603,61.1065817884,-0.782294722603,61.1065817884,3.82705527116,60.0458443672),('Kenkeren Ridge, Koryak',2341,'','Triassic','Upper Triassic','late Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,205,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'25',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1359,0,'Scleractinians: Beneckastraea, Distichophyllia, Kuhnastraea, Palaestraea, Retiophyllia, Rhaetiastraea, Stuorezia, Thamnotropis.\n\'Hydroids\', calcareous algae additional framework builders.\n40% endemic corals',59,163,4301535,17770786,'Russia','Asia',624,'',59.75,163.0833,'WAHR','40409',69.4317996514,-102.593884609,69.6525745443,-102.560690944,74.6859954728,-92.7382477479),('Monte Cetona, Chianciano, Tuscany',2342,'Monte Cetona','Triassic','Upper Triassic','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,202,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15',NULL,NULL,NULL,'1','Less than 20 m','30','2',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','8','Serpulids, worms, vermetids','3','Microbes','11','Serpulids - algae - microbes',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1480,0,'Mud Mounds on a homoclinal ramp with mixed carbonate-siliciclastic setting.\nMounds in upper part of Monte Cetona Fm. 4-30 m in length and 4-15 m thick. Serpulid framestone and cyanobacteria bindstone.',43,11,2493587,1558028,'Italy','Europe',344,'',43.0333,11.8333,'','',24.4708937868,25.7651102982,24.4708937868,25.7651102982,20.7173611204,24.2779208871),('Ponte Arverino, Terni, Umbria',2343,'Monte Cetona','Triassic','Upper Triassic','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,202,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'','1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1480,0,'Lower member of Monte Cetona Fm.\nThrombolite mounds\nDeeper part of homoclinal ramp.',42,12,2396101,1587887,'Italy','Europe',344,'',42.5667,12.65,'','',23.7156143929,25.8523608942,23.7156143929,25.8523608942,19.9625110961,24.3671024813),('Monti Simbruini, Filettino, Apennin',2344,'','Triassic','Upper Triassic','Norian-Rhaetian',201.30,228.00,18,'late Carnian - middle Hettangian',218,203,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','30',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','8','Serpulids, worms, vermetids','3','Microbes','11','Serpulids - algae - microbes',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',1480,0,'Carbonate platform complex.\nLower massive portion of the Dolomie di Monte Fiumata succession.\nLenticular shape, up to 30 m thick.\nMostly serpulid framestone, associated with float- and rudstone.',41,13,2287160,1595950,'Italy','Europe',344,'',41.9167,13.3,'WAHR','73881',17.9907566722,26.6343133041,17.8270973703,26.7166307249,14.6713439132,20.7379983758),('Montral, Tarragona',2345,'','Triassic','Middle Triassic','middle Ladinian',237.00,242.00,17,'Induan - early Carnian',235,234,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','2','Algae','69','Non-coralline algae only','2','Green algae','3','97','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1481,0,'Dasycladacean reef (Diplopora annulata group)\nSeveral 10ths of m thick.\nRare corals, sponge spicules, bryozoans.',41,1,1055508,1510196,'Spain','Europe',304,'',41.2903,1.0958,'WAHR','67648',19.1406719066,22.8782986927,19.1406719066,22.8782986927,9.82044359576,14.3994325079),('Lakaftari, Esfahan',2346,'','Cretaceous','Lower Cretaceous','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,123,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',1,'yes','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1482,0,'Monopleurid biostrome associated with Orbitolina-sands\nAbout 20 m thick, > 20 m lateral extension.\nhigher early Aptian.',32,52,3629726,5247059,'Iran','Asia',505,'',32.9667,52,'','',29.76231123,63.953688925,29.6666465536,64.4129783656,31.1967876065,63.2588815372),('Darawiz, Chah Riseh',2347,'Qom','Paleogene','Oligocene/Miocene','Oligocene/Miocene',5.30,33.90,30,'Chattian - Aquitanian',22,23,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','5',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1401,0,'Small coral mound (5 m thick).\nDiverse corals in marly matrix.\nPeri-reef facies with few corals. Packstones with larger forams, red algae, bryozoans, pelecypods.',32,52,4071922,4861650,'Iran','Asia',505,'',32.9667,52.1,'','',32.985339134,48.4437432228,32.985339134,48.4437432228,31.3445134739,50.7044285024),('Salzbrunnen, Bagherabad',2348,'Nayband','Triassic','Upper Triassic','Sevatian',208.50,214.00,18,'late Carnian - middle Hettangian',218,205,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','6','Calcisponges','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',1,'yes','2','6 to 24 reef building species','16','1','Constructor guild','1','Present',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',30,1401,'Uppermost member of Nayband Formation.\nLarge spongiomorphids and diverse massive and dendroid corals (Astreacoenia, Asteromorpha, Retiophyllia).\n14 species of corals described. Personal observations add microbes and spongiomorphids.\nReef sitting on Heterastrid-marls.\nSmall patch reefs with sphinctozoans associated.',33,51,2913189,5383446,'Iran','Asia',505,'',33.1167,51.9833,'WAHR','34635',21.3771730041,60.7403476117,26.1229659809,61.2679478678,24.2423008558,64.5709333068),('Domrud, Mamulan, Zagros',2349,'Talezan','Paleogene','Eocene','early Eocene',47.80,56.00,27,'Thanetian - Ypresian',53,53,1,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',1,'yes','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1401,0,'Corals and algal crusts.\nReef within sandstones and siltstones.',33,47,2677096,4358237,'Iran','Asia',505,'',33.4167,47.9667,'','',22.0418154929,40.9962488433,22.0418154929,40.9962488433,22.113127061,42.8815822714),('Deh Sorkh, Esfahan',2350,'','Cretaceous','Lower Cretaceous','Aptian-Albian',100.50,125.00,24,'late Aptian - middle Cenomanian',107,112,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','1','Corals','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present',NULL,'','2','Medium zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1634,1401,'Toucasiids, Eoradiolites, Caprotinids.\nCorals and rudists at the base (± in situ).\nRudist debris at the top.',32,51,3124147,5385055,'Iran','Asia',505,'1482',32.4,51.6,'','',29.2810119421,61.9157482932,29.2810119421,61.9157482932,30.583823564,59.7898018532),('Kashan',2351,'Qom','Paleogene','Oligocene/Miocene','Oligocene/Miocene',5.30,33.90,30,'Chattian - Aquitanian',22,23,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','6',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','12','Foraminifera','12','Foraminifera','71','Foraminifera only, (some corals)',NULL,NULL,'100','0','0',0,'no',1,'yes','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1401,0,'Encrusting forams biostrome, about 6 m thick.\nUnderlain and overlain by foraminiferal packstones with Lepidocyclina.',33,51,4155409,4798092,'Iran','Asia',505,'',33.65,51.75,'','',33.6535515359,48.0542121465,33.6535515359,48.0542121465,32.028770941,50.3633238988),('Azaran',2352,'Qom','Paleogene','Oligocene/Miocene','Oligocene/Miocene',5.30,33.90,30,'Chattian - Aquitanian',22,23,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','12',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','12','Foraminifera','20','Corals - forams',NULL,NULL,'0','100','0',0,'no',1,'yes','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1401,0,'Large corals (more than 1 m diameter).\n12 m thick reef overlain by coral-foram rudstones\nBase with conglomerates and marls.\nRare algae',33,50,4154102,4721198,'Iran','Asia',505,'',33.7167,50.9667,'','',33.6882319143,47.2680392299,33.6882319143,47.2680392299,32.0978361779,49.5944996957),('Mahallat',2353,'Nayband','Triassic','Upper Triassic','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,210,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',1,'yes','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','3','Pronounced zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1401,30,'Recrystallized reef facies, about 15 m thick.\nCorals dominant (especially on top of reef facies), but sponges common.\nRetiophyllia large (up to 1.5 m diameter).\nReef overlying Loferites. Seperated by quartzite.',33,50,2892883,5206657,'Iran','Asia',505,'',33.95,50.3667,'WAHR','37962',21.7563640721,59.0862348654,21.402057349,59.104585595,21.8773402218,58.2943356211),('Phu Khanh Basin, offshore',2354,'','Neogene','Miocene','upper lower Miocene',16.00,20.40,31,'Burdigalian - Serravallian',14,18,2,1,'Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1483,0,'Seismically detected carbonate buildups.\nDated by sequence stratigraphy.',13,109,1741388,11996315,'Vietnam','Asia',NULL,'',13.5,109.5833,'','',15.2796519887,107.278536328,15.2796519887,107.278536328,12.4594464027,107.880088584),('Bolshoy Balkhan, Turkmenia',2355,'Alikper','Cretaceous','Lower Cretaceous','lower Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,135,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)','1','Red algae','0','80','20',0,'no',0,'no','2','6 to 24 reef building species','14','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',2251,1,'Urgonian facies.\nIsolated patch reefs formed by coral-algal-rudist buildups and some oyster and brachiopod banks in lagoonal facies.\nCollections of Patzkowsky:\n2260-2264',39,54,5062505,4743723,'Turkmenistan','Asia',NULL,'',39,54.5,'WAHR','2263',34.9153790839,63.3716543582,34.9153790839,63.3716543582,35.8557430455,63.9841588518),('Karakum',2356,'','Jurassic','Upper Jurassic','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,157,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','130',NULL,NULL,NULL,'4','More than 1000 m',NULL,'160','974',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation',NULL,'','1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1471,1413,'Gas field.\nBarrier reef.\n130 m thick.\nSee reef 2322 for more remarks.',39,67,5487342,6081167,'Uzbekistan','Asia',301,'',39.0833,67.1333,'WAHR','91786',37.8479242427,74.6921067137,37.8479242427,74.6921067137,40.629304894,79.7671393766),('Lyalyakan & Karasan',2357,'','Jurassic','Upper Jurassic','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,157,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','250',NULL,NULL,NULL,'4','More than 1000 m',NULL,'160','974',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present','3','Pronounced zonation','3','Pronounced zonation','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',1,'Potential reservoir',1471,1413,'250 m thick.\nOutcrop\nSee reef 2322 for more remarks.',38,67,5410923,6147596,'Uzbekistan','Asia',301,'',38.4167,67.1333,'WAHR','91827',37.2797422553,75.1318941464,37.2797422553,75.1318941464,40.020368183,80.1228746679),('Shurtan',2358,'','Jurassic','Upper Jurassic','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,157,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,'160','974',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1471,1413,'Barrier reef.\nGiant gas field.\n200 m thick.\nSee reef 2322 for more remarks.',38,66,5391022,6055613,'Uzbekistan','Asia',301,'',38.5667,66.0833,'WAHR','91783',36.9800461913,74.1538014343,36.9800461913,74.1538014343,39.8244623023,79.063935031),('Urtabulak',2359,'Urtabulak','Jurassic','Upper Jurassic','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,156,3,1,'Seismic data available ',1,'True reef','3','101-500 m thick','265',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','80','10',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1471,2339,'Turan Platform\nIsolated intra-basin dome-like reef\n265 m thick\nGas field.\n20 species of corals alone',39,64,5398040,5868782,'Uzbekistan','Asia',301,'1413',39.1667,64.3333,'WAHR','34859',36.7837822314,72.3087433575,36.7837822314,72.3087433575,39.8185997312,77.1255014304),('Strobl, Salzburg',2360,'Theresienstein','Cretaceous','Upper Cretaceous','Turonian/Coniacian',86.30,93.90,25,'late Cenomanian - early Campanian',91,89,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','25','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'10','80','10',0,'no',0,'no','2','6 to 24 reef building species','17','1','Constructor guild','1','Present',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1486,0,'Up to 11 coral-stromatoporoid biostromes in in 280 m thick crinoidal grainstone sequence. corals and stromatoporoids about equally abundant.\nThickness of individual biostromes up to 4 m. Cummalitive thickness in section 1 about 40 m.',47,13,4007304,1532250,'Austria','Europe',301,'',47.7167,13.4806,'WAHR','27296',39.4866413758,16.1818092541,39.4866413758,16.1818092541,35.8853555338,15.089890417),('Zuune Arts',2361,'','Cambrian','Lower Cambrian','upper Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,517,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15',NULL,NULL,NULL,'1','Less than 20 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','23','3','Binder guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1488,14,'Mixed carbonate-siliciclastic shelf setting.\n\nIndividual bioherms less than 2 m thick and wide. \nUpsection coalesced to form up to 15 m thick complexes.\nSurrounded by grainstones with little archaeocyath debris.\n\nFour types of reef buildups:\nCalcimicrobe boundstones\nCalcimicrobe bafflestones\nRadiocyath-archaeocyath-cribricyath bioherms\n\nArchaeocyaths form up to 20 % of rock volume. 12 species.\n\n1 Radiocyath species\n\n10 calcimicrobe species.',47,96,-1578800,3561755,'Mongolia','Asia',NULL,'',47.15,96.9,'WAHR','63210',6.86582756992,-43.2317782756,6.86582756992,-43.2317782756,6.86582756992,-43.2317782756),('l\'Épine',2362,'','Jurassic','Upper Jurassic','upper middle Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,156,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','11',NULL,NULL,NULL,'1','Less than 20 m','20',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1490,0,'In situt reefs up to 11 m thick and 20 m across.\nDiverse macro- and microborings.\nHigh species diversity, but low ecological diversity.\n\nAbstract of ref. 1490\nDuring the late middle Oxfordian, patch reefs grew on the northern margin of the Paris Basin. According to the facies analysis of the reef and inter-reef sediments, the environment was a warm, clear and agitated sea with highly episodic sedimentation. The bioherms were a short-lived phenomenon during the third phase of regional reefal development. Sequence stratigraphically, they are associated with a highstand system tract. Volumetrically and trophically dominant organisms were microbes now represented by massive clotted leiolite, \'stalactitic\' hemispheroids with purely thrombolitic texture are restricted to open caves. Corals were of structural, reef-building importance due to their rapid upward growth. The patch reefs are characterised by thickets of ramose corals which developed a very open framework. In the vicinity of these patch reefs, though in hydrodynamically higher-energy environments, grew thickets of more stoutly branched corals. However, they are rarely preserved in situ and are generally represented as abundant coral rubble. The reef taxa are characterised by the notable absence of several groups (e.g. oysters, serpulids, bryozoans, pectinids) occurring at other localities where reefs of similar age developed in similar environmental conditions. The reefs also have strikingly modern aspects to them, in particular the presence of cryptic elements within caves and a sponge-dominated borer association. Dwellers belong to various life-form types although encrusting taxa are exceedingly rare. This may be explained by the presence of soft microbial films on most surfaces. The palaeoecological analysis suggests that the major controls on faunal composition and high diversity were elevated nutrient levels, highly episodic sedimentation and probably seasonal environmental disturbances. Structural and functional aspects of the reef community (grazers trigger framebuilders, borers trigger binders, binders hamper borers) allow ecological comparisons to be made with contemporaneous, as well as Recent, reefs. The unique combination of ecological factors resulted in a specialised, previously undescribed, community which differs from both Tethyan and northern localities in various aspects. These include cavities with cryptofauna, prominence of grazing gastropods and high faunal diversity in a microbially dominated build-up. ',49,4,4852996,707157,'France','Europe',331,'',49.6056,4.4333,'WAHR','11084',28.1548035075,22.3594089078,28.1548035075,22.3594089078,34.3305365186,23.0173333059),('H2 1/90 well, Rügen, Baltic Sea',2363,'','Permian','Upper Permian','Zechstein 1 (Werra)',252.20,254.10,16,'Roadian - Changhsingian',261,258,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','18',NULL,NULL,NULL,'2','10 - 100 m',NULL,'300',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','6','3','Binder guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1495,0,'About 18 m thick stromatolite-bryozoan boundstones with some intercalations of grainstones, packstones and wackestone.\nOne horizon with rudstones.\nBryozoans:\nFenestella\nThamnopora\nAcanthocladia\nStenopora\nProretopora\n\nAbstract ref. 1495:\nIn the deep borehole H2 - 1/90 of \'Petrobaltic\' joint venture situated 20 km eastward from the Island of Rügen a reef of the basal Zechstein (Upper Permian) was discovered. Litho- and biofacies of this reef were investigated by the authors of this paper. New results allow a new palaeogeographic interpretation of some elder boreholes of Rügen Island.',54,14,2688879,2582562,'Germany','Europe',331,'',54.3167,14.0667,'WAHR','10696',30.7968164496,31.5686574429,30.8002219261,31.5691503361,26.8939948742,26.0517869282),('Rhine graben',2364,'','Paleogene','Upper Paleogene','Eocene-Oligocene',23.00,56.00,29,'Priabonian - Rupelian',33,33,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'25',NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','1','Red algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1496,0,'Lens shaped stomatolitic bioherms and algal mounds on fan-delta complexes in the early Rhine rift. \nPartialy eroded by vadose circulation.\n',47,7,5951027,343044,'France','Europe',331,'',47.7,7.3833,'','',45.5313970137,1.9193748903,45.5313970137,1.9193748903,46.1027461151,7.078945919),('Cook Reef, Leon Co., Texas',2365,'Haynesville-Cotton Valley','Jurassic','Upper Jurassic','Kimmeridgian-Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,150,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1497,0,'Encase in thick basinal shale of Bossier Fm.\n\nProducing gas reservoir.\nSeismic explaration only.\nAbout 100 m wide and 200 m long.',31,-95,2234965,-4832959,'United States','North America',101,'',31.5,-95.8333,'','',19.0682217579,-38.4350759124,19.0682217579,-38.4350759124,24.3027672684,-40.9638338798),('Meiklejohn Peak, southern Nevada',2366,'Lower Antelope Valley','Ordovician','Middle Ordovician','Dapingian',467.30,470.00,4,'late Early - early Middle Ordovician',472,468,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','76',NULL,NULL,NULL,'3','More than 100 m','300',NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','13','Echinoderms',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1498,1499,'Lower Antelope Valley Limestone.\r\n76 m thick, 300 m long mud mound without organic frame.\r\nTraces of Sphaerocodium, Nuia, small ostracods, trilobits, brachiopods and pelmatozoan plates.\r\nRef. 1498 not seen.',37,-116,485945,-8663124,'United States','North America',101,'',37,-116.75,'WAHR','80054',18.689801824,-122.471250027,18.689801824,-122.471250027,18.689801824,-122.471250027),('Shingle Pass, Sunnyside, Nevada',2367,'','Ordovician','Middle Ordovician','Dapingian',467.30,470.00,4,'late Early - early Middle Ordovician',472,468,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','11','Siliceous sponges','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)','3','Receptaculitids','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1728,1643,'Receptaculid (calathid) algae and possible sponges make up 35 % of the mound. 65 % is micrite.\r\nDiscontinuous outer-shelf belt of scattered to stacked buildups.',38,-115,-35311,-8225875,'United States','North America',101,'1499',38.4333,-115.0167,'',NULL,18.0204455568,-120.504071994,18.0204455568,-120.504071994,18.0204455568,-120.504071994),('Nyalam, Tibet',2368,'','Jurassic','Lower Jurassic','Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,187,2,0,'Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'10','90','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1500,0,'Lithiotis bioherm on Tethyan-Himalaya terrane.\nPossibly plate 501.',28,87,-688509,8137536,'China','Asia',602,'',28.3333,87.5,'','',-37.1820291391,55.7735878611,-37.1820291391,55.7735878611,-38.6026241056,47.175692326),('Verchnyaya Pechora River',2369,'','Devonian','Lower Devonian','lower Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,406,3,0,'Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1420,0,'See reef 2247.',61,58,803570,1479515,'Russia','Asia',624,'',61.8333,58.6667,'','',19.3456500251,-24.2763121878,19.3456500251,-24.2763121878,31.4026835576,-85.2810189899),('Monte Pellegrino, Palermo, Sicily',2370,'','Cretaceous','Lower Cretaceous','Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,115,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','5','Rudists','3','Microbes','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'40','40','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1779,1492,'Densely packed caprinids and radiolitids. \nOverlying rudist debris and coral tufts.\nEncrusters: Lithocodium, Pseudolithothamnium.',38,13,2574213,1227374,'Italy','Europe',344,'',38.1667,13.35,'','',20.652999175,21.0772723549,20.652999175,21.0772723549,20.3065209471,16.9350456601),('Oberwössen, Bavaria',2371,'','Cretaceous','Lower Cretaceous','Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','1','Corals','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'5','90','5',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1492,0,'',47,12,3769924,1533765,'Germany','Europe',331,'',47.7,12.4833,'','',33.6781737868,21.1374295137,33.6781737868,21.1374295137,32.7371746476,17.7283954782),('Argentina Range, Pensacola Mts.,',2372,'','Cambrian','Lower Cambrian','upper Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,513,3,0,'Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','27','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1504,0,'Glacial erratics on King George Island (South Shetland Islands) thought to derive from Argentina Range.\n\nAbstract of ref. 1504:\nTwenty six species of archaeocyaths are described (seven in open nomenclature), including Naimarkcyathus elenae gen. et sp. n. representing a new family Naimarkcyathidae and superfamily Naimarkcyathoidea of the order Archaeocyathida, from the Cambrian limestone erratics in the glacio-marine sediments of the Oligocene Polonez Cove and Early Miocene Cape Melville Formations on King George Island (South Shetland Islands, West Antarctica). They are accompanied by coralomorphs and calcified cyanobacteria. The archaeocyathan assemblage closely resembles allochthonous assemblages from the Weddell Sea and Whichaway Nunataks. Current reconstructions of icestream movement and iceberg drift, and similarities in species composition, suggest the Argentina Range limestones as a source of these erratics. The species Stapicyathus stapipora, Prethmophyllum subacutum, Aporosocyathus mucroporus, \'Mennericyathus\' dissitus, Paranacyathus sarmaticus and Archaeopharetra irregularis are added to the list of common species for Antarctica and Australia. The total list of the common Australian-Antarctic archaeocyaths now include 31 of all of the 52 well defined Antarctic species. The archaeocyaths of King George Island, and Early Cambrian Antarctic archaeocyath assemblages (except these of the Mt. Egerton in the Byrd Glacier area) are of uppermost Botomian age (Syringocnema favus Beds) as in South Australia. This means that archaeocyaths did not reach Antarctica until latest Botomian time. Erratic blocks containing archaeocyaths represent various reef facies similar to the Shackleton Limestone facies and those of South Australia. The occurrence of small shelly fossils (Dailyatia ajax, ? Byronia sp., Halkieria parva, Thambetolepis delicata and Albrunicola bengtsoni) which are typical of the Parara Limestone, of the Syringocnema favus archaeocyathan assemblage, and of Hadimopanella antarctica and certain brachiopods in erratics of different lithologies, suggests a very similar faunal and facies succession for Antarctica and South Australia and therefore, a comparable basin history. ',-82,-50,-2330267,-17755711,'Argentina','South America',201,'',-82,-50,'WAHR','62871',-24.226115015,138.931282004,-24.081443656,142.454928835,-24.081443656,142.454928835),('Kolguev Island, Barents Sea',2373,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate',NULL,NULL,NULL,NULL,NULL,'','2','Algae','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','2','Green algae','40','60','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1505,0,'Algal-bryozoan bioherms detected by drilling.',69,49,4498665,2977514,'Russia','Asia',624,'',69,49,'','',31.3981578042,28.758427624,31.3981578042,28.758427624,33.3652388362,1.23514452822),('Kolguev Island II, Barents Sea',2374,'','Permian','Lower Permian','Sakmarian-Artinskian',283.50,298.90,15,'Sakmarian - Kungurian',277,284,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate',NULL,NULL,NULL,NULL,NULL,'','2','Algae','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','2','Green algae','40','60','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1505,0,'',69,49,5081312,3249792,'Russia','Asia',624,'',69,49,'','',31.8275963982,29.2469275672,31.8275963982,29.2469275672,34.9645610724,6.1242130074),('Fondry des Chiens, Nismes, Couvin',2375,'','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'20','0','80',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation',NULL,'','1','Less than 30% micrite','2','10-25% sparite',NULL,'','0','',0,'No or unknown reservoir potential',1508,0,'Patch reef isolated in lagoonal limestones. \nEntirely built by frame-building organisms (large irregular massiv stromatoporoids predominate).\nMatrix with crinoidal debris and sparry calcite cement. \nNo micrite!\nAlgae absent, some encrusting Rothpletzella.\nThree facies zones.',50,4,-2729345,514672,'Belgium','Europe',331,'',50.05,4.5,'WAHR','84298',-18.0331388762,-15.6951593303,-18.0331388762,-15.6951593303,-2.34640201584,-71.3450621297),('Neuville quarry',2376,'Neuville','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','4','Stromatoporoids','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)',NULL,NULL,'0','30','70',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1508,2183,'Other localities are Croisette quarry and Tapoumont Buildup.\nMud mound\nStromatactis important.\nNeuville formation.\nStromatoporoids + Phillipsastrea, Alveolites and microbes (Renalcis, Epiphyton, Rothpletzella).\nPhillipsastrea in argillaceous limestone at base.\n',50,4,-2714127,476554,'Belgium','Europe',331,'2565',50.3167,4.1333,'WAHR','76638',-22.6299956183,-12.2723562755,-22.6299956183,-12.2723562755,-3.29190457261,-67.8608042992),('Börglum Elv, Peary Land, Greenland',2377,'','Silurian','Lower Silurian','upper Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,429,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'800','1441',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'20','0','80',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1511,0,'Crinoidal calcarenite association of ref. 1511.\nFacies includes stromatoporoid bindstones, chaotic resedimented comglomerates and abundant crinoidal calcarenites.\nReef core with predominantly hemispheric and rarely laminar and irregular stromatoporoid bindstone containing a few tabulate corals.\nLaterally grading into strom. floatstone (50 % strom. in skeletal wackestone matrix). Crinoidal calcarernite forms flank beds.\nNo stromatolites\nVery rare micrite\nNo fenestrae',82,-31,667618,-2548776,'Denmark','Europe',330,'',82.3333,-31.25,'','',6.39811744387,-78.4922181236,6.39811744387,-78.4922181236,6.39811744387,-78.4922181236),('Unda well, Great Bahama Bank',2378,'','Neogene','Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,6,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','2','Intense',0,'No or unknown reservoir potential',2444,2593,'This reef number previously as Börglum Elv, Llandovery/Wenlock slice 7. More precise age assignment required replacement.\n\nTotally dolomitized Messinian reef complex at platform edge\n\n',24,-79,3374404,-8196756,'Bahamas','North America',NULL,'',24.5833,-79.0167,'WAHR','73642',24.1835203586,-77.8772460676,24.1825170639,-77.8745486273,25.2989696601,-77.7094192621),('Fort Condé, Givet',2379,'','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','25',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','2','Medium zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1515,0,'Mud mound\n15-25 m thick, 30-45 m diameter.\nBedded at base (crinoid rudstones), massive at top.\nRare sponges (siliceous?), no corals.\nStromatactis important.\nEssentially micrite, but stromatactis important.\nLow diversity.',50,4,-2705243,531255,'France','Europe',331,'',50.1333,4.8333,'','',-22.5993601578,-11.7491614188,-22.5993601578,-11.7491614188,-3.06498058128,-67.4327098519),('Wadi Hamman',2380,'Shuaiba','Cretaceous','Lower Cretaceous','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,123,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','9',NULL,NULL,NULL,'1','Less than 20 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'30','70','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1516,840,'Three main units:\nc) Wackestone with sparse Glossomyophorus\nb) Caprinid and coral grainstones and subordinate packstones with caprinids and Bacinella ( 9 m thick)\na) Caprinid-dominated packstones and wackestones',23,57,-1016118,5054940,'Oman','Asia',503,'',23.3333,57.7833,'WAHR','67020',-9.6016806959,53.3597920418,-10.7525671319,53.2612228238,23.1224319376,71.4926456894),('Gudman, Rockhampton, Queensland',2381,'Gudman','Carboniferous','Lower Carboniferous','lower Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,357,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','7','1','Less than 10 m wide',NULL,'2','10 - 100 m','50','1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1518,1517,'Initiated on oolitic sands.\nDominated by thrombolites. \nCommon worm tubes.\nMicro-encrusters: Claracrusta(?), Wetheredella, Aphralysia, Mitcheldeania, forams.\nCommon crinoid holdfasts, encrusting forams.\nAbundant ramose bryozoans, syringoporoid corals, solitary and rugose corals.\nHard-substrate borings.',-23,150,-4326843,14529484,'Australia','Oceania',801,'',-23.3833,150.4167,'WAHR','36545',-15.2172344787,147.423513251,-15.2172344787,147.423513251,-33.1486474824,151.86843134),('Carlton Shelf, Bonaparte Gulf, Wester',2382,'Ningbing Group','Devonian','Upper Devonian','late Famennian',358.90,372.20,11,'late Famennian - early Visean',351,363,3,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'','3','Pronounced zonation',NULL,'','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1519,1982,'Several facies zones are developed.\nBasin, marginal-slope, platform with reef-margin, reef-flat and back-reef.\nGroup includes five formations:\nDjilirri Limeston\nKamilili Fm.\nWungabal Limestone\nGarimala Limestone\nButtons Fm.\n\nExcept for Buttons Fm. all formatins part of reef complex. \nThickness of Ninging Group 171-1166 m.',-15,128,-4003352,12141687,'Australia','Oceania',801,'2004, 1517',-15.25,128.5,'','',-20.7305635803,118.766363048,-20.7305635803,118.766363048,-31.6639822633,152.498423868),('Baelen, Verviers',2383,'','Devonian','Upper Devonian','upper middle Famennian',358.90,372.20,11,'late Famennian - early Visean',351,365,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','86','Microbes - sponges - crinoids',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1520,1517,'upper middle Famennian; late marginifera Zone\nThe reefs were surrounded by mainly finegrained\nsiliciclastic sediments, but the relatively\ncontinuous export of bioclasts resulted in the\nmixed siliciclastic-carbonate facies, which surrounds\nthe carbonate bodies.',50,5,-1566304,568335,'Belgium','Europe',331,'',50.5833,5.8333,'WAHR','75672',-31.8642140762,-6.89007856465,-31.8642140762,-6.89007856465,-1.26505537414,-61.1818989736),('Richelle, Visé area',2384,'','Carboniferous','Lower Carboniferous','upper Viséan',330.90,340.00,12,'middle Visean - Serpukhovian',329,332,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','6','4','Microbial precipitation',NULL,'',NULL,'','2','Medium zonation',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1521,1517,'Informatiin from ref. 1517.\n\nCampine Basin\nboundstone facies \n (1) a thick crust of calcimicrobes and Aphralysia around small solitary corals (Amplexocarinia sp.), and bryozoans;\n(2) peloidal packstones, with thrombolitic outline; and (3) various stromatactoid cavities.',50,5,-684550,1061085,'Belgium','Europe',331,'2568',50.75,5.6667,'','',-32.7991426877,-2.62050201272,-29.3705558995,-0.770497351776,-4.39564777316,-24.7889365159),('Namur',2385,'','Carboniferous','Lower Carboniferous','middle Visean',340.00,345.00,12,'middle Visean - Serpukhovian',329,337,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','3','Pronounced zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1522,1517,'Information from ref. 1517.',50,4,-740706,1013308,'Belgium','Europe',331,'',50.4667,4.85,'WAHR','76656',-33.1553850404,-3.18212846734,-35.662620822,-4.80666823867,-3.99032247615,-35.4662378058),('Hadnock, Wales, Great Britain',2386,'','Carboniferous','Lower Carboniferous','Arundian',342.00,345.00,11,'late Famennian - early Visean',351,342,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','77','Vermetid gastropods -  microbes',NULL,NULL,'10','90','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'','1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1818,1523,'Vermetid gastropods and microbes forming biostromes in marginal marine setting.\nSmall bioherms up to 25 cm in height.\n',51,-2,-1612687,-44490,'United Kingdom','Europe',331,'',51.8333,-2.6833,'WAHR','76720',-32.0806466939,-8.87901937096,-34.6989596191,-10.8775405613,-4.64834252137,-41.6426000271),('Stack Cleugh, Bewcastle, England',2387,'','Carboniferous','Lower Carboniferous','Arundian',342.00,345.00,11,'late Famennian - early Visean',351,342,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m','13',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','77','Vermetid gastropods -  microbes',NULL,NULL,'10','90','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1523,1517,'Vermetid gastropods and stromatolites forming bioherm in marginal marine setting.\n2 m high, 13 m long.',55,-2,-1182767,-124991,'United Kingdom','Europe',331,'',55.0667,-2.6833,'','',-28.847702901,-8.81598932035,-31.4674145079,-10.7468058141,-1.69449823724,-42.9599374643),('Hueco Mts., Texas',2388,'La Tuna','Carboniferous','Upper Carboniferous','Morrowan',315.00,323.20,12,'middle Visean - Serpukhovian',329,316,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','2','Green algae','40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'','2','Medium zonation','1','Low zonation','1','Less than 30% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1524,1517,'Information from ref. 1517.',31,-105,-1186373,-5042576,'United States','North America',101,'',31.9167,-105.9167,'','',-18.7999435905,-63.7248412834,-11.481626214,-47.7884817847,-8.59640084481,-63.2869484336),('Bat Mountain, Mojave Desert, California',2389,'Tin Mountain','Carboniferous','Lower Carboniferous','Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,358,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','40',NULL,NULL,NULL,'3','More than 100 m',NULL,'1',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'90','0','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1526,1517,'Core facies: bryozoan grainstone, bryozoan-crinoid wacke-/packstone and bryozoan packstone\nBryozoans are dominant macrofossils.\n\n\nMound core dominated by allochems (fenestrate bryozoans and crinoids).\nPolymuds and spar make up only 40 % by volume.',36,-116,-1080400,-6176185,'United States','North America',101,'',36.3333,-116.5,'','',-11.9949028957,-65.4790155277,-11.9949028957,-65.4790155277,1.77303971133,-111.287174167),('Brentwood, Arkansas',2390,'Bloyd','Carboniferous','Upper Carboniferous','upper Morrowan',315.00,323.20,13,'Bashkirian - Kasimovian',302,315,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','12','Foraminifera','13','Algae - encrusting forams',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1527,1517,'Locality doubtful.\nBrentwood Member\nInformation from ref. 1517.',36,-94,-700166,-3093672,'United States','North America',101,'',36,-94,'','',-12.2582574428,-34.4531116087,-15.3095330203,-37.5310196628,-13.2700181032,-53.4974978833),('Lawrence Co., Alabama',2391,'Bangor Limestone','Carboniferous','Lower Carboniferous','Chesterian',331.00,336.00,12,'middle Visean - Serpukhovian',329,326,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','1','Corals','83','Bryozoans - rugose corals - echinoderms - encrusting forams',NULL,NULL,'80','0','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'','1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1626,1528,'Bangor Limestone\nPennington group\nFenestrate bryozoan buildup.\nBryozoans together with rugose corals, stalked echinoderms, soft-bodied organisms encrusted by foraminifera. \nBiodetrital mound\nMound resting on bored oolitic shoals. \n25 m wide, 1.6 m thick, roughly circular. \n\n',34,-87,-2173758,-3404776,'United States','North America',101,'1517',34.5,-87.3333,'WAHR','76726',-29.0414529864,-47.2446857668,-29.0414529864,-47.2446857668,-15.9798503111,-67.5080905567),('Sausset-les-Pins, Nerthe',2392,'','Neogene','Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,18,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,2,'Cold - water',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present',NULL,'','1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1531,0,'Oyster reef (biostrome?) in a litoral envrionment. \nCrassostrea gryphoides.\nAbout 1 m thick.',43,5,5660309,289472,'France','Europe',331,'',43.3333,5.1167,'','',41.4044915799,1.20127103512,41.781570078,1.74769275965,42.4072415793,4.85300377409),('Häutligen, Münsingen',2393,'','Neogene','Miocene','upper Helvetian',11.60,13.80,31,'Burdigalian - Serravallian',14,13,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1531,0,'Crassostrea gryphoides banks in marls.',46,7,6012379,575768,'Switzerland','Europe',331,'',46.8833,7.5833,'','',45.9398166045,4.98409527083,45.9398166045,4.98409527083,46.2292247409,7.54865399091),('Beni Mellal, High Atlas',2394,'','Jurassic','Lower Jurassic','Sinemurian-Pliensbachian',182.70,199.30,19,'late Hettangian - early Aalenian',188,189,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','15','Non-rudist bivalves','1','Corals','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'10','90','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1530,0,'\'Reefs\' consist of biostrome accumulations of great pelecypods:\nLithiotis, Cochlearites, Opisoma, Durga ... in life position.\nCorals in isolated colonies.',32,-6,3463262,-821007,'Morocco','Africa',714,'',32.3333,-6.2333,'','',18.6692269921,2.58359627732,18.6692269921,2.58359627732,28.215719296,5.51187130887),('Aucors, Aquitaine Basin',2395,'Bourg-des-Maisons','Cretaceous','Upper Cretaceous','upper Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,90,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'150',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1532,0,'Dense and loose aggregates of Durania cornupastoris with Biradiolites lumbricalis and other ratiolitids.\nDebris of Biradiolites led to the accumulation of massive white chalky Anoulême Fm.',45,0,4483428,274100,'France','Europe',331,'',45.4833,0.4667,'WAHR','74224',39.650019181,5.18249917392,39.650019181,5.18249917392,38.1375786427,3.62194742029),('Al-Abiad',2396,'Amman','Cretaceous','Upper Cretaceous','Campanian-Maastrichtian',66.00,83.60,26,'middle Campanian - Danian/Selandian',75,70,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','40',NULL,NULL,NULL,'4','More than 1000 m',NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1534,0,'Only oyster Ambigostrea villei (cited as Lopha villei) present.\nLater unpublished report (web) additionally cites Oscillopha figari and Nicaisolopha nicaisei\nArtulated valves prevalent in lower part. Higher up, shells increasingly broken. \nBorings on both valves.\nUp to 40 m thick.\n\nAbstract of ref. 1534:\nPhosphorite grains were authigenically precipitated within\nprecursor marl and biosiliceous deposits during high water level and\nintense upwelling within the Tethys Ocean to the north of Jordan. With\nfalling sea level, the oyster Lopha villei colonized bathymetric highs in the shallow shelfal environments in east-central Jordan during the uppermost Campanian--Lower Maastrichtian (Late Cretaceous). The oyster bioherms in the epeiric southern shelf of the Tethys formed small basins several hundreds of meters across and about 40--50 m deep. Under these lowstand conditions, oyster shells were shed off the bioherms and deposited as large cross-bedded units on the flanks of the basins. At the same time, precursor phosphatic sediments were reworked and winnowed to form high-grade phosphorite sand. More than 250 million metric tons (250 x 109 kilograms) of phosphorite sand were deposited basinward of the oyster beds. As sea level continued to fall, the oyster bioherms formed partially silled basins with low biological diversity in which marl and/or bituminous marl was deposited. The marls are overlain by the transgressive phosphatic marl and chalk of the Muwaggar Formation, which were deposited under open marine conditions. ',31,36,2222717,3205412,'Jordan','Asia',503,'',31.05,36.0833,'','',16.4455222662,32.8677510282,16.4455222662,32.8677510282,17.2739026154,30.406601367),('Barrett Canyon, Salton Sea, California',2397,'Imperial','Neogene','Pliocene','lower Pliocene',3.60,5.30,32,'Tortonian - Gelasian',6,4,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2','1','Less than 10 m wide','20','3','More than 100 m','500',NULL,NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1535,0,'Siderastrea menhalli bank with patch reefs in sandstones of the Latrania Member. Bank 1-2 m thick, 20 m wide and 500 m long.\nLittle or no evidence of bioerosion.\nPatch reefs with some Porites carrizensis, Siderastrea california and S. fainbanksi dispersed between large S. menhalli colonies.',33,-116,4495580,-11464693,'United States','North America',101,'',33.0167,-116.0667,'WAHR','34853',32.4635742079,-114.323878922,32.4631414976,-114.327083868,33.7870468214,-115.311259695),('Visby, Gotland',2398,'Visby','Silurian','Llandovery','Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,430,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1537,1536,'Small bioherms with halysitid and solitary rugose corals in the Lower Visby Fm.\nEarliest reefs on island.',57,18,-2925654,-441111,'Sweden','Europe',330,'',57.7,18.3667,'WAHR','61758',-14.488001439,-52.5536348406,-14.488001439,-52.5536348406,-14.488001439,-52.5536348406),('Melville Peninsula, N.W.T.',2399,'','Silurian','Llandovery','Rhuddanian',440.80,443.40,6,'Rhuddanian-Telychian',435,442,1,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1539,1538,'Capping framework of favositid coral facies on large pinnacle reefs of Late Ordovician age.',65,-87,-355448,-4396528,'Canada','North America',121,'1536',65.5833,-87,'','',-3.22556043378,-99.5204246601,-3.22556043378,-99.5204246601,-3.22556043378,-99.5204246601),('Mansel Island, N.W.T.',2400,'Ekwan River','Silurian','Llandovery','upper Aeronian',438.50,440.80,6,'Rhuddanian-Telychian',435,436,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1538,1536,'Small stromatoporoid-coral bioherms (< 3 m thick).\nUnderlain and overlain by strat with small stromatolitic bioherms (1-2 m thick) in intertidal hypersaline environments.',62,-80,-991366,-4278789,'Canada','North America',121,'',62,-80,'','',-9.16897421855,-95.2317169396,-9.16897421855,-95.2317169396,-9.16897421855,-95.2317169396),('Prince Alfred Bay, Devon Is., N.W.T.',2401,'Allen Bay','Silurian','Llandovery','upper Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,430,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,'','4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1540,1536,'Stromatoporoid mounds, up to 500 m across.',76,-93,748101,-3682278,'Canada','North America',121,'',76.3333,-93.6667,'','',4.01643531873,-91.7753929593,4.01643531873,-91.7753929593,4.01643531873,-91.7753929593),('Rigby Bay, Devon Is., N.W.T.',2402,'Allen Bay','Silurian','Llandovery','Rhuddanian?',440.80,443.40,6,'Rhuddanian-Telychian',435,441,1,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',1541,1536,'Small dolomitized halysitid bioherms.',74,-90,498474,-3776029,'Canada','North America',121,'',74.5667,-90.05,'','',4.11276359755,-95.539357976,4.11276359755,-95.539357976,4.11276359755,-95.539357976),('Podolia, Demshin',2403,'Fourmanivka','Silurian','Lower Silurian','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,425,2,0,'Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1542,2267,'Small rugosan-stromatoporoid-tabulate bioherms. \nData in collection (M. Foote) from several formations.\nReefs also in Trubchin suite',48,25,-2310538,350064,'Ukraine','Europe',301,'2651',48.5,25.8333,'WAHR','23480',-8.58475107435,-38.5550814736,-8.58475107435,-38.5550814736,-8.58475107435,-38.5550814736),('Aqadyr, Balkash',2404,'Akkan-Alpeis-Zhumak','Silurian','Upper Silurian','upper Wenlock-Ludlow',423.00,430.50,7,'Wenlock - early Pridoli',425,422,2,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'400',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1543,1536,'Reefal beds.\n',48,72,-1348488,7619325,'Kazakhstan','Asia',301,'',48.2667,72.8667,'','',12.9180090602,29.6015212099,12.9180090602,29.6015212099,12.9180090602,29.6015212099),('Logar Syncline, Kabul',2405,'','Silurian','Wenlock','Wenlockian',427.40,433.40,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','50',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1544,0,'50 m thick reef limestone with favositids and halysitids in a primarily clastic sequence.\n',34,69,-4115545,13599589,'Afghanistan','Asia',301,'',34.5,69,'WAHR','79345',-27.5022207612,70.6513375139,-27.5022207612,70.6513375139,-27.5022207612,70.6513375139),('Manchap, Himachal Himalaya',2406,'Manchap','Silurian','Wenlock','Wenlockian',427.40,433.40,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m','5000','80','1795',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','7','Bryozoans','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no','3','25 or more reef building species','16','1','Constructor guild',NULL,'',NULL,'','3','Pronounced zonation','3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1545,0,'Cross bedded sandstone at base\nFrame-bind-bafflestones important\n55 % pack-grainstones\n10 % float/rudstones\nReef builders: \nRugose: Radiastraea, Streptelasmatids, Tryplasma, Ptychophyllum\nTabulates: Favosites, Halysites, Plasmaoporella, Plasmopora, Heliolites\nStromatoporoids (laminar and low domal): not identified.\nBryozoans: Hallopora most common, Coenites, Fenestella\nOthers Girvanella, Vermiporella, solenoproids, probable codiaceans.\n\nSee also reef. 1795.',31,78,-4244275,14515549,'India','Asia',501,'',31.6,78.75,'WAHR','36257',-26.5063076519,80.3171129791,-26.5063076519,80.3171129791,-26.5063076519,80.3171129791),('Roberts Mountains, Nevada',2407,'','Silurian','Middle-Upper Silurian','Wenlockian-Ludlovian',423.00,433.40,7,'Wenlock - early Pridoli',425,422,2,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','4','Stromatoporoids','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Intense',0,'No or unknown reservoir potential',1546,1536,'Massive dolomitic reef, platform margin.',39,-116,-1223791,-7590433,'United States','North America',101,'',39.8333,-116.3333,'','',-19.6285430172,-107.612529172,-19.6285430172,-107.612529172,-19.6285430172,-107.612529172),('Klamath Mts., Northern California',2408,'','Silurian','Ludlow','Ludlovian',423.00,427.40,7,'Wenlock - early Pridoli',425,421,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1536,1547,'Reef debris with halysitids and other corals.\nSiliciclastic-volcanic active plate margin belt.',41,-123,-429504,-7756954,'United States','North America',101,'',41.8333,-123.6667,'WAHR','79733',-15.3976605934,-107.576436277,-15.3976605934,-107.576436277,-15.3976605934,-107.576436277),('Canyon Fiord, Ellesmere Is., N.W.T.',2409,'','Silurian','Ludlow','Ludlovian',423.00,427.40,7,'Wenlock - early Pridoli',425,421,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'','2','Medium zonation',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1548,1536,'Massive shelf margin buildups with slope to basinal Cape Phillips Fm.',80,-81,575488,-2784574,'Canada','North America',121,'1712',80,-81.6667,'','',9.26283986861,-69.2126512871,9.26283986861,-69.2126512871,9.26283986861,-69.2126512871),