('Quingdao Depression, CZ12-1-1',4227,'Hezhou','Carboniferous','Mississippian',NULL,'Lower Carboniferous',323.20,358.90,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',NULL,1,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'2','Intense',1,'Potential reservoir',3180,NULL,'Reef-bank. Dolomites contain abundant dissolved pores and are mainly micritic dolomites. These indicate that there are dolomite reservoirs with good porosity distributed in the lower Triassic and lower Carboniferous of the South Yellow Sea.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.35,122.03,NULL,NULL,NULL,NULL,6.44019698973,115.906526651,10.7994325988,50.715663884,-6.28448,86.1989,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Well WX5-ST1',4228,'Qinglong','Triassic','Lower Triassic','Induan','Scythian',247.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','25','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'2','Intense',1,'Potential reservoir',3180,NULL,'Dolomites with high porosity and high\r\npermeability',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.32,122.54,NULL,NULL,NULL,NULL,4.26139251568,120.015537254,27.7803615144,110.766449588,13.6394,105.106,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Ganjgon, Lower Rupelian',4229,'Asmari','Paleogene','Oligocene','Rupelian','lower Rupelian',30.00,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base','1','Corals','2','Algae','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3181,NULL,'Build-up (main body and flanks). Further down-dip, larger benthic foraminifers (large Nummulites test, Operculina and Neorotalia) packstone-grainstone along with discrete coral patches and coralline red algae',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,30.16,51.46,NULL,NULL,NULL,NULL,22.9368263524,45.3416612962,20.9283599627,47.3365362583,22.549,45.5597,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jowzar',4230,'Asmari','Paleogene','Oligocene','Chattian','lower Chattian',27.50,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,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','2','Algae','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3181,NULL,'Polygenetic conglomerate. Meter-thick bedded to massive limestones rich in coral and coralline\r\nred algae fragments confining to the platform margin.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,30.4,51.22,NULL,NULL,NULL,NULL,23.8933395752,45.6578131447,21.9809819845,47.5269033829,26.4228,48.0942,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lower Monte Baria Reef, Cala Gonone, N Oresei Gulg',4236,'Lower Monte Bardia','Jurassic','Upper Jurassic','Tithonian','upper Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','120','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','3','Below storm wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','40','4','Microbial precipitation','1','Present','2','Intensive',NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3185,NULL,'Carbonate (bioclastic) debris, microbialites and microencrusters, and reef-building organisms (mainly corals and stromatoporoids).\r\nMicroframework -rich(microbialites and microencrusters) facies, with abundant skeletal organismus in place. Corals dominate, followed by stromatoporoids, bivalves (including Rudist diceratids), gastropods (including nerineids), echinoid spines.',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,40.16,9.37,NULL,'196865',NULL,NULL,22.2533512176,21.6107406562,23.9451625524,16.4871126777,34.0583,13.8914,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Core XK-1, Stone Island',4241,'Yinggehai','Neogene','Pliocene','Pliocene','Upper Pliocene',2.60,3.60,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',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','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals','2','Algae','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3194,NULL,'Coral content varies between 25% and 74%.The corals are dominated by Turbinaria and Favia, with colonies mainly displaying massive morphologies. Accessory components are debris of frequent to rare benthic foraminifera, red algae, echinoids, brachiopods. Red algal and coral frame- to bindstone, red algal bindstone, floatstone, and wackestone.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.51,112.2,NULL,NULL,NULL,NULL,16.9846878533,111.768191244,16.2928863978,111.8401123,16.4008,111.945,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Falcona Alta, Malaguide Complex',4240,'Unknown','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',NULL,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','1','Corals','4','Stromatoporoids','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,'2','Intensive','1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3192,NULL,'Mainly bafflestones with clotted microbial\r\ngrainstone to packstone matrix. Reef builders\r\nare ramiform thamnoporid corals and twig-like stromatoporoids both with frequent microborings.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,36.47,-4.28,NULL,'197173',NULL,NULL,36.47,-4.28,-9.12774798041,-52.9528871161,-35.0928,13.2965,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Hönne Reef, Beul near Eisborn. Loc. 4',4239,'Unknown','Devonian','Upper Devonian','Frasnian','early Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',NULL,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','2','Shelf or Platform margin','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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3191,NULL,'Terminal reef limestones with colonial rugose coral, biostrome blocks and with the overlying top-middle Frasnian, post-reefal nodular limestones, with shark and pelagic conodont fauna',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,51.23,7.52,NULL,'197088',NULL,NULL,-20.8405728609,-10.6690851976,-1.04999308975,-67.2329750556,-19.3864,6.33956,'Krause','Kiessling','2021-05-28 15:21:12','2023-03-10 15:49:57'),('Hönne Valley Reef Complex at Asbeck Quarry',4238,'Hagen-Balve','Devonian','Middle Devonian','Givetian','middle-upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','4','More than 500 m thick','600','3','101-1000 m wide',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','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','16',NULL,NULL,NULL,NULL,NULL,NULL,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',3191,NULL,'The Asbeck Quarry exposes a sequence of more\r\nthan 600 meters of reefal limestone.\r\nThere are six major facies sets: \r\n1. limestones with evidence of subaerial exposure (e.g., vadose cements, drying and contraction cracks), 2. laminites without macrofauna (but with\r\nparathuramminid foraminifers and ostracods), 3.\r\nmicrites with few components and irregular\r\nmicrobial fenestrae (“birdseyes” to Stromatactis”), 4. fossiliferous micrites, with various reef builders, gastropods, specialized brachiopods, parathuramminids, and ostracods, 5. sublagoonal limestone, mostly rich in dendroid stromatopores (Amphipora, Stachyodes), and 6. reef-core limestones (boundstones), with large stromatopores in growth position.\r\n\r\n\r\nMudstones to bioclastic wackestones with some\r\ntabulate corals, rare colonial Rugosa, very rare\r\nstromatoporid fragments, some crinoid debris,\r\nostracods, and some mollusk debris.',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,51.393,7.867,NULL,'197084',NULL,NULL,-15.9954827905,-14.7533967612,-0.119187133193,-71.2958213121,-19.4004,6.31756,'Krause','Kiessling','2021-05-28 15:21:12','2023-03-10 15:49:58'),('Core XK-1, Stone Island',4242,'Ledong','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,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','1','Intrashelf/ Intraplatform','2c','Atoll (circular structure)','2','Below fair weather wave base','1','Corals','12','Foraminifera','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3194,NULL,'coral framestone and floatston with minor wackestone and packstone. The corals are dominated by Turbinaria and Favia, with\r\ncolonies mainly displaying massive morphologies. The coral content can reach 100%. Matrix containing some bioclastic debris. Accessory components are debris of frequent to rare benthic foraminifera, red algae, echinoids, rare green algae, brachiopods, bivalves.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.51,112.2,NULL,NULL,NULL,NULL,16.6658863994,112.058711173,16.4381569228,112.081638624,16.51,112.2,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Laga Beach, Ibarangelu',4243,'Unknown','Cretaceous','Lower Cretaceous','Albian','lower Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,110,'Early Cretaceous (early Albian, 111 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','3','101-500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','50',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3195,NULL,'Marls with coral biostromes.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,43.24,-2.39,NULL,NULL,NULL,NULL,31.3108317436,8.4187865529,33.6029647791,4.27979273191,31.8247,4.71445,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kouquan section',4244,'Changshan','Cambrian','Series 3','Guzhangian','Middle-Dresbachian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',NULL,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3196,NULL,'massive micritic limestone and calcareous\r\nmudstone',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,39.59,113.07,NULL,'197283',NULL,NULL,20.7194117892,104.296366428,20.7194117892,104.296366428,-3.7484,140.035,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Sampaguita-1, Reed Bank',4245,'Unknown','Paleogene','Oligocene','Chattian','Chattian-Burdigalian',16.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',NULL,2,'1','Seismic data available ',NULL,NULL,'4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3197,NULL,'Carbonate platform reef',NULL,NULL,NULL,NULL,'Philippines','Asia',NULL,NULL,10.24,116.36,NULL,NULL,NULL,NULL,14.8056840825,113.253588652,11.5930218943,113.919399645,13.4024,117.532,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Sampagita‐1',4246,'Unknown','Neogene','Miocene','Upper Miocene','upper Miocene - Pliocene',2.60,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',NULL,NULL,'4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3197,NULL,'Carbonate platform reef',NULL,NULL,NULL,NULL,'Philippines','Asia',NULL,NULL,10.24,116.36,NULL,NULL,NULL,NULL,11.1129904281,115.621924168,9.88735424624,115.761545941,10.2828,116.337,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Huwaiza-1 well',4247,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome',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','5','Rudists','12','Foraminifera','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3198,NULL,'Very coarse-grained bioclastic rudstone dominated by rudistid debris with abundant of benthonic foraminiferal grainstone in the lagoonal facies.',NULL,NULL,NULL,NULL,'Iraq','Asia',NULL,NULL,31.45,47.49,NULL,NULL,NULL,NULL,11.6023187931,43.890304106,8.28787380926,38.9495160077,8.636,39.0062,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Halfaya-1 wall',4248,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome',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','5','Rudists','12','Foraminifera','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3198,NULL,'Rudistid biostrome with open shelf lagoon facies. Abundant of benthonic foraminiferal packstone, that indicates to open lagoon environment.',NULL,NULL,NULL,NULL,'Iraq','Asia',NULL,NULL,31.38,47.24,NULL,NULL,NULL,NULL,11.5696950514,43.6635224824,8.26695868769,38.723595326,8.60367,38.7814,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Amara -1',4249,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3198,NULL,'Rudistid biostrome with open shelf lagoon facies',NULL,NULL,NULL,NULL,'Iraq','Asia',NULL,NULL,31.48,46.53,NULL,NULL,NULL,NULL,11.773154038,43.0719551362,8.5007957047,38.1497071667,8.8081,38.1957,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Abu Amood -1',4250,'uppermost Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','5','Rudists','12','Foraminifera','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3198,NULL,'Skeletal and non-skeletal carbonate grains, rudistid debris.',NULL,NULL,NULL,NULL,'Iraq','Asia',NULL,NULL,31.49,46.28,NULL,NULL,NULL,NULL,11.8205562492,42.8593669351,8.5592328798,37.9421384511,8.85592,37.9852,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Dujaila -1 well',4251,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','5','Rudists','12','Foraminifera','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3198,NULL,'Skeletal and non-skeletal carbonate grains.',NULL,NULL,NULL,NULL,'Iraq','Asia',NULL,NULL,31.57,46.08,NULL,NULL,NULL,NULL,11.9295511234,42.7024467524,8.67629447243,37.7929491247,8.96526,37.83,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wennan, Xintai area',4252,'Zhangxia, Lower Limestone Member','Cambrian','Series 3','Guzhangian','Marjumian',500.50,504.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',NULL,1,'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','1a','Shallow intra-platform','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3200,NULL,'Sponge–microbial boundstones, containing lithistid sponges (areal percentage, approximately 14%) and microbial components (areal percentage, approximately 39%). The sponges in this section are anthaspidellid demosponges. The microbial components consist mainly of frequently branched columnar stromatolites. Vacant spaces among frameworks formed by a combination of stromatolites and sponges are filled with lime mud and rare bioclasts, including trilobites, chancelloriid sclerites and sponge spicules.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.48,117.46,NULL,NULL,NULL,NULL,24.5492149278,97.9557098779,24.5492149278,97.9557098779,-3.23325,145.405,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Tipperary area, Kordephyton-Jawonya-Wagima',4253,'Tindall Limestone','Cambrian','Series 2','Stage 4','upper Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',NULL,3,'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','1a','Shallow intra-platform',NULL,NULL,'3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3201,NULL,'Microbialite columns with Kordephyton bushes (fan pattern) and sporadic Jawonya and Wagima both attached to column surfaces and immured within columns; vagrant Latouchella accordionata on right margin of central column; intercolumn cavity with geopetal infill.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-13.45,130.2,NULL,NULL,NULL,NULL,5.42869314792,99.554876226,5.42869314792,99.554876226,27.6784,-177.922,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Soudan area, Undilla Sub-basin, locality NTGS4648',4254,'Ranken Limestone','Cambrian','Series 3','Guzhangian','Marjumian',500.50,504.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',NULL,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','3','Ramp or Slope',NULL,NULL,'3','Below storm wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3201,NULL,'Reef fabric comprises mainly explanate and in some cases conical Rankenella, encrusted by more or less distinctly laminated, generally non-skeletal stromatolites. Angulocellularia-type microbial mesoclots and Angulocellularia locally intergrades into Taninia. Stromatolites appear to encrust upper surfaces of Rankenella skeletons, as well as those of other bioclasts such as calciate brachiopods, hyoliths and molluscs.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.49,136.55,NULL,NULL,NULL,NULL,4.82799498343,112.360108444,4.82799498343,112.360108444,25.2066,-176.118,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Yazd locality',4255,'Nayband, Howz-e Khan Member','Triassic','Upper Triassic','Norian','Norian-Rhaetian',201.30,228.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','50',NULL,NULL,NULL,'2','10 - 100 m','60',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3202,NULL,'Small reefs formed by dendroid and ceroid corals and differents droups of sponges. Chambered sphinctozoans and noc-chambered sphinctozoans are the most abundant sponges. One chambered hexactinellid sponges was also found.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,31.49,54.2,NULL,'197554',NULL,NULL,25.2211858224,65.1939935196,21.6954605526,64.5723262292,-12.4274,44.8748,'Krause','Krause','2021-05-28 15:21:12','2022-06-22 20:46:19'),('Dagestan, Shakhdag Massif',4256,'Babadag','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','320',NULL,NULL,NULL,'4','More than 1000 m','1500','1.5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1',NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3203,NULL,'Bioherm buildups, represented by the dense gray and greenish grain limestones with a great amount of corals.',NULL,NULL,NULL,NULL,'Azerbaijan','Europe',NULL,NULL,41.15,48.01,NULL,NULL,NULL,NULL,32.4633491919,57.4150770964,36.1349884064,60.9742005837,36.395,53.0394,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Well YB1 and Well YB2,Yuanba, Cangxi',4257,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,2,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick','140',NULL,NULL,NULL,'4','More than 1000 m',NULL,'3.6',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'2','Intense',2,'Actual reservoir',3204,NULL,'The main reservoir rocks are reef-bank dolomite and dolomitic limestone, which are characterized by\r\nmedium-low porosity and medium-low permeability.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.54,106.07,NULL,NULL,NULL,NULL,-9.68272333377,104.695223691,12.7067161262,123.623002199,3.7442,95.0735,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Le Perthus',4258,'Unknown','Jurassic','Lower Jurassic','Sinemurian','upper Sinemurian',190.80,199.30,19,'late Hettangian - early Aalenian',188,195,'Early Jurassic (Hettangian&Sinemurian, 196 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2','1','Less than 10 m wide',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','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','6','4','Microbial precipitation','1','Present','2','Intensive','1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',3209,NULL,'Coral-microbialite patch reef with fragments of crinoids and dacycladacean algae but profuse\r\nooids.\r\nIncludes Mas de Messier locality. Chondrocoenia clavellate dominant',NULL,NULL,NULL,NULL,'France','Europe',NULL,NULL,43.46,3.15,NULL,NULL,NULL,NULL,24.664724042,22.9622176477,31.0100289354,28.7650753919,32.0435,13.3195,'Krause','Krause','2021-05-28 15:21:12','2022-03-23 16:40:13'),('Wadi Aynouna, near Al Khuraybah',4259,'Jabal Kibrit, Wadi Waqb Member','Neogene','Miocene','Middle Miocene','early Middle Miocene',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','26',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3210,NULL,'Massive bioturbated coralline limestone with low diverse, medium isolated corals heads of Favites, Heliastraea, Tarbellastraea, Porites, Thegioastraea spp. Coralline red algae occur as free-rolling or partly attatched rhodoliths and debris of Lithothamnium and Mesophyllum spp. Red algae play a significant role in construction of\r\nthe reef facies, where they bind and connect coral colonies and other skeletal and non  skeletal constituents into a coherent mass. The bivalves, gastropods and echinoids act as essential rock forming constituents in this lithofacies. Fore-reef sediments mainly gave bioclastic wackestone, algal wackestone, bioclastic packstones, coralline framestone, coralline rudstone and grainstones. Most of these sediments are driven from the reef-core framework. Thin sections show fragments of corals, red algae, benthic foraminifera (miliolids) and ostracods. Most of these fragments were recrystallized due to diagenesis.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.1,35.1,NULL,NULL,NULL,NULL,25.1537399679,32.3932619637,24.5140642172,33.4191927893,26.4158,33.4195,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Al Bada',4260,'Jabal Kibrit, Wadi Waqb Member','Neogene','Miocene','Middle Miocene','lower-middle Miocene',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'4259',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','15','Non-rudist bivalves','41','Corals - bryozoans - (algae) - (bivalves)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3210,NULL,'Massive limestone with low diverse, scattered, small dendroid and massive heads of corals of Heliastraea, Tarbellastraea spp. Microfacies analysis of this facies gave coralline framestone, bioclastic grainstone, bryozoan grainstone, bioclastic wacke/floatstones and bioclastic rudstones. The skeletal grains are dominated by reworked moderately preserved small branched, massive and phaceloid corals, bivalves, gastropods and red algae. Matrix in most back reef is made up of peloidal micrite with abundant organic matter.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.31,35.01,NULL,NULL,NULL,NULL,25.3684039438,32.3206693927,24.7323898362,33.3617742145,26.6308,33.3473,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Station 15, Ash Shaykh Humayd',4261,'Unknown','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','26',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3212,NULL,'MIS5e coral reef terraces, expose reef-edge and\r\nback-reef lagoonal deposits with various stony\r\ncorals, molluscs, echinoids, melobesians, etc.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.05,34.34,NULL,'198563',NULL,NULL,27.9036023673,34.1111240618,27.6742635625,34.1749976984,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Station 6, 12 South of Ra-s Suwayhil as Saghir',4262,'Unknown','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',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','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','13',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3212,NULL,'Large boulders overgrown by reefal carbonates with variety of well-preserved scleractinian corals and molluscs, gastropods. Large mamelon-like aragonite botryoids are found.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.45,34.48,NULL,'198537',NULL,NULL,28.3038262551,34.250106804,28.0725378764,34.3206892529,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Station 20, North of Wadi Tayyib Ism',4263,'Unknown','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,2,'0','Outcropping reef ',NULL,NULL,'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','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3212,NULL,'reefal carbonates with conglomeratic layers sitting on Arabian basement granitoids with abundant scleractinian heads, gastropods, epifaunal and infaunal bivalves.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.35,34.47,NULL,'198579',NULL,NULL,28.2038103538,34.2403279363,27.9726677695,34.3091735547,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Station 27, south of Al Maqnah',4264,'Unknown','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,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','1a','Shallow intra-platform',NULL,NULL,'1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3212,NULL,'Porites-dominated reefs and intervening sandy sediments host abundant and diverse associated fauna which includes large bivalves and gastropods.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.2,34.43,NULL,'198586',NULL,NULL,28.0537463746,34.2006928222,27.8231639791,34.2669944909,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('B reef and J reef, Madura Strait Basin',4265,'Kujung','Paleogene','Oligocene','Chattian','Chattian-Aquitanian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',NULL,2,'1','Seismic data available ',2,'Reef mound','4','More than 500 m thick','825','4','More than 1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','3','Below storm wave base','1','Corals','12','Foraminifera','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',3213,NULL,'Reefal facies, composed of a coral framework, larger foraminifera, red algae, echinoderm plates, and other minor carbonate bioclasts.',NULL,NULL,NULL,NULL,'Indonesia','Asia',NULL,NULL,-7.24,113.13,NULL,NULL,NULL,NULL,-3.87592302985,111.361055874,-8.72580840042,114.674270046,-6.53887,118.005,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('O-1Madura Strait Basin',4266,'Mundu','Neogene','Pliocene','Pliocene','Zanclean',3.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',NULL,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf',NULL,NULL,'12','Foraminifera','12','Foraminifera','71','Foraminifera only, (some corals)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',3213,NULL,'porosity of the Mundu carbonate rock can reach more than 40%. Mundu is composed of bioclastic\r\ngrainstone, wackestone and packstone and has been\r\nintensely bioturbated. ',NULL,NULL,NULL,NULL,'Indonesia','Asia',NULL,NULL,-7.19,113.21,NULL,NULL,NULL,NULL,-6.65206348173,112.792482349,-7.53497714969,112.887347208,-7.30625,114.045,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Blue Mountain Inlier',4267,'Rio Grande Limestone','Cretaceous','Upper Cretaceous','Campanian','upper Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,75,'Late Cretaceous (Late Campanian, 75 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','3','Below storm wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3214,NULL,'Rudists as large bouquets of Biradiolites\r\nmooretownensis yielding tens of thousands of\r\nspecimens',NULL,NULL,NULL,NULL,'Jamaica','North America',NULL,NULL,18.3,-76.35,NULL,'198683',NULL,NULL,14.3900985374,-66.4717145358,16.6589865414,-69.8283116854,19.9637,-66.0609,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Atar Group, unit I-5',4268,'Atar','Ediacaran','Ediacaran','Avalon Assemblage','Neoproterozoic',542.00,999.00,0,'Vendian',605,750,'Early Neoproterozoic (late Tonian. 750 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','41',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation',NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3215,NULL,'Stromatolitic bioherms.',NULL,NULL,NULL,NULL,'Mauritania','Africa',NULL,NULL,20.31,-13.03,NULL,NULL,NULL,NULL,-54.7567787445,-0.542051839931,-54.7567787445,-0.542051839931,-23.4577,87.2119,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Pizzo Croce Limestone',4269,'Unknown','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','10','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','3','Below storm wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12',NULL,NULL,'2','Intensive',NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3220,NULL,'Rudist biostrome/buildups, highenergy shelf-margin rudist patches. Caprinidae-Radiolitidae floatstone grading up into amalgamated beds of angular bioclastic rudstone/grainstone. Alternations of foraminifer/ostracod mudstone/wackestone and bioclastic grainstone/fine-rudstone.',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,38.11,13.19,NULL,NULL,NULL,NULL,28.0822593494,13.9009992307,22.4237186233,12.7034024025,21.2032,13.3435,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wadi Mujib',4270,'Wadi As Sir Limestone','Cretaceous','Upper Cretaceous','Cenomanian','middle Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','3','Below storm wave base','5','Rudists','2','Algae','91','Rudists - corals - algae/microbes - (brachiopods)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11',NULL,NULL,'1','Present','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','2','Intense',0,'No or unknown reservoir potential',3222,NULL,'Peritidal (mudstones with monotypic ostracodes or microbial lamination) and agitated shallow subtidal environments (rudist patch reefs).',NULL,NULL,NULL,NULL,'Jordan','Asia',NULL,NULL,31.27,35.34,NULL,NULL,NULL,NULL,15.9106923343,33.6129570758,11.3975931152,28.6309335118,11.9916,29.3065,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Nallıhan',4271,'Yenipazar (=Nardin), Çeğiköy Reef Member','Cretaceous','Upper Cretaceous','Campanian','Campanian/Maastrichtian',66.00,83.60,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',NULL,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,NULL,'5','Rudists','12','Foraminifera','91','Rudists - corals - algae/microbes - (brachiopods)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','26',NULL,NULL,'2','Intensive','2','Intensive','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3224,NULL,'Patch reefs and locally fringing type\r\nreefs comprise abundant hippurits and other rudists, algae, bryozoans, coelenterate, echinoid, gastropods, ammonoids.',NULL,NULL,NULL,NULL,'Turkey','Asia',NULL,NULL,40.12,31.2,NULL,NULL,NULL,NULL,37.0693484965,31.8094589396,37.3739043318,30.3468464859,30.8172,30.2985,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Bird Road, Miami',4272,'Buckingham, Pinecrest Beds or Formation','Neogene','Pliocene','Pliocene','lower Pliocene',3.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','2c','Atoll (circular structure)','3','Below storm wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','30',NULL,NULL,NULL,NULL,'2','Intensive','3','Pronounced zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3225,NULL,'More biohermal in form, the reef system appeared to have distinct zonation. coral fauna was present, including Diploria sarasotana, Septastrea marylandica, Septastrea crassa, Porites furcata Lamarck, and the hydrocoral Millepora alcicornis, and over three hundred species of mollusks along with several species of echinoids and crustaceans.',NULL,NULL,NULL,NULL,'United States','North America',NULL,NULL,25.43,-80.22,NULL,'146873',NULL,NULL,25.1641649859,-79.3974699317,25.9524887954,-79.2936584418,25.5534,-78.9945,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Tangjiahe ',4273,'Xiannüdong','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3','1','Less than 10 m wide',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','3','Microbes','3','Microbes','93','Microbial micrite - pelmatozoans',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3226,NULL,'The Tangjiahe section contains three levels of reefal buildups that were constructed by aconsortium of archaeocyaths and calcimicrobes in varying proportions. The lowest (oldest) reefal buildup is acalcimicrobial biostrome, possibly in the form of a wide mound with a low relief (unconfirmed due to outcroplimitation), which was formed byEpiphytonwith rare small archaeocyaths, and is sandwiched by flat-pebbleconglomerates. The middle reefal buildup is a high-relief calcimicrobial mound, enclosed by oolites, that was built byintergrownRenalcisandTarthinia.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,32.36,106.29,NULL,NULL,NULL,NULL,-3.84042740035,78.5315278314,-3.84042740035,78.5315278314,27.6128,164.827,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kano-yama limestone, Kanto Mountains',4274,'Unknown','Carboniferous','Pennsylvanian','Gzhelian','Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20','2','10 - 100 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','2','Algae','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','20','4','Microbial precipitation',NULL,NULL,'2','Intensive','2','Medium zonation',NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3228,NULL,'Algal-microbial mound composed of Anthracoporella, Palaeoaplysina, Tubiphytes, Archaeolithoporella, and bryozoans. The limestone is characterized by abundant micrite, implying a low-energy back-reef depositional environment.',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,36.5,138.53,NULL,NULL,NULL,NULL,14.0359988711,144.095839731,14.6032865092,76.3871937958,15.1502,105.022,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Fossil Hill',4275,'Unknown','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','5','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4b','Deep basin (> 200 m)','2','Below fair weather wave base','8','Serpulids, worms, vermetids','15','Non-rudist bivalves','16','Serpulids - bivalves - (microbes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','22',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3231,NULL,'Serpulid build-ups: massive deposits composed of fossil serpulid worm tubes (Annelida: Serpulidae) and bivalve shells.',NULL,NULL,NULL,NULL,'United States','North America',NULL,NULL,33.5,-118.41,NULL,'200653',NULL,NULL,33.4870368913,-118.378842149,33.5,-118.41,33.5,-118.41,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Xikou section',4276,'Jinjiling','Triassic','Lower Triassic','Induan','Induan',251.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','0.2','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','3','Microbes','12','Foraminifera','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3239,NULL,'Lower stromatolite bed, lying on the oolitic grainstone, 0.2 m thick. Columnar stromatolites.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.17,109.19,NULL,NULL,NULL,NULL,-6.69722417725,108.018930782,16.752654929,125.558198254,27.9505,93.4566,'Krause','Krause','2021-05-28 15:21:12','2021-06-13 15:20:44'),('Xikou section',4277,'Longdongchuan','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','95.5','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','6','Calcisponges','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,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',3239,NULL,'Very-thick-bedded sponge framestones and thick-to-very-thick-bedded bioclastic grainstones. Fossils are diverse and abundant and include calcareous sponges, calcareous algae, echinoderms, corals, small foraminifers, fusulinids, brachiopods. Clarkina yini zone. Shallow marine, low- to middle\r\nenergy zone. Coordinates stated in the text, decimal.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.2419,109.376,NULL,NULL,NULL,NULL,-7.65229573803,107.063172386,14.2192250605,126.403999257,6.58408,96.3184,'Krause','Krause','2021-05-28 15:21:12','2021-06-19 18:51:08'),('Mtwara Bay',4278,'Mikindani','Neogene','Miocene','Upper Miocene','lower Messinian',6.00,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8.5','1','Less than 10 m wide',NULL,'2','10 - 100 m','25',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1d','Marginal marine - coastal -  siliciclastic shelf','2','Below fair weather wave base','1','Corals','12','Foraminifera','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','46',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3240,NULL,'Coral bioconstruction with two principal facies:\r\nsiliciclastic sheetstone facies dominated by platy\r\ncolonies, and carbonate mix-platestone facies including a variety of growth forms (platy, tabular-massive, branching and solitary. Tabular-massive corals can reach a size of up to 50 cm across.',NULL,NULL,NULL,NULL,'Tanzania','Africa',NULL,NULL,-10.15,40.11,NULL,NULL,NULL,NULL,-10.8506777461,39.2884578343,-11.3782712953,39.2608973756,-10.5205,39.2601,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kotouč Quarry, Štramberk',4279,'Unknown','Cretaceous','Lower Cretaceous','Berriasian','lower Berriasian',139.80,145.00,22,'late Tithonian - early Valanginian',141,145,'Jurassic/Cretaceous Boundary (145 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','18','2','10 - 100 m wide',NULL,'2','10 - 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','1','Corals','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','25','4','Microbial precipitation','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',3241,NULL,'Coral-microbial bindstone passing locally to poorly sorted pelbiointraclastic packstone. Corals and micro-encrusters (Lithocodium aggregatum and Crescentiella morronensis) form a framework\r\nthat supported the sediment during deposition. Bioclasts belong to trepostome bryozoans\r\n(colonies and isolated zooecias), calcareous sponges, crinoids and gastropods. Ooids and\r\ncalcareous dinoflagellate cysts are rare. Cavities are filled with radiaxial-fibrous calcite cement,\r\nchalcedony and blocky calcite.',NULL,NULL,NULL,NULL,'Czech Republic','Europe',NULL,NULL,49.35,18.06,NULL,'202900',NULL,NULL,31.7052507429,29.7985930723,36.9462232624,31.3258075065,41.3672,24.7928,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jebel Taabest',4280,'Choucht to Agoudim','Jurassic','Lower Jurassic','Pliensbachian','lower Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,185,'Early Jurassic (Pliensbachian, 186.8 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','3','Microbes','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11','4','Microbial precipitation','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3243,NULL,'subtidal lagoon paleoenvironments with olistoliths that show a boundstone to floatstone texture, with solitary and colonial corals, sponges, gastropods, serpulid worms, crinoids, brachiopods, echinoids tests and spines, and occasional chaetetid sponges and microbialites.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.9351,-4.9594,NULL,NULL,NULL,NULL,19.6912835586,4.37936443723,26.8786876572,6.06454873649,26.8378,-1.24771,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Koudiat Ech Chehem',4281,'Maftah 3','Jurassic','Lower Jurassic','Pliensbachian','upper Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,185,'Early Jurassic (Pliensbachian, 186.8 Ma)',NULL,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',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'3','Microbes','3','Microbes','86','Microbes - sponges - crinoids',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3243,NULL,'Giant bioherm made of interlayered boundstones\r\n(pillarstones and mixstones) and crinoidal grainstones and packstones. Environment in the\r\noptimal reef window, at the boundary between shoreface and offshore. Well-lit and diverse communities.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,33.4528,-4.9225,NULL,NULL,NULL,NULL,20.9109494868,5.34301544598,28.00261038,7.2143247342,28.1934,-3.23884,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Mihangaoqiaogaolu section, West Ujimqin Banner',4282,'Amushan','Carboniferous','Pennsylvanian','Gzhelian','Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','110','3','101-1000 m wide',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','2','Algae','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','10','4','Microbial precipitation',NULL,NULL,'2','Intensive','2','Medium zonation','2','Medium zonation','3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3244,NULL,'Reefs are superimposed upon each other in the lower part of the section, but are isolated in the upper part. They developed on and are overlain by\r\nmedium- to thick-bedded skeletal wackestone that contains phylloid algae and Shamovella, foraminifers, echinoderms, bryozoans, Rectangulina, and Epimastopora.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,44.2756,117.887,NULL,NULL,NULL,NULL,47.5013909349,130.225581719,63.7421605139,97.6426369165,38.1015,92.8161,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Cioclovina–Bănita area, MFT2',4283,'Unknown','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',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','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','13','4','Microbial precipitation','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3245,NULL,'Platform margin environment, crest—shallow-water patch reefs. Crustose fabrics, biogenic encrustations and perforations; clotted, agglutinated and dome-shaped microbial microstructures, small cavities; the intra-reef sediment is mostly micritic; scarce geopetal structures; radiaxial- fibrous cements and late diagenetic druse/ mosaic spar occur locally',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,45.28,23.15,NULL,NULL,NULL,NULL,28.6163653184,35.664715173,21.9474947491,29.8969779645,26.5294,27.6449,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gunung Subis',4284,'Subis Limestone','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','390','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'6',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,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',3246,NULL,'Massive and branching corals, coralline red algae, benthic foraminifera, bivalves, gastropods, echinoids, and occasionally bryozoans and sponges. Eight microfacies types and four environments were defined to describe the Subis Limestone: outer talus, inner talus, reef rim, and lagoon.\r\nNine genera of benthic foraminifera.',NULL,NULL,NULL,NULL,'Malaysia','Asia',NULL,NULL,3.48,113.51,NULL,NULL,NULL,NULL,3.87418462232,110.715914039,0.637347006763,114.137892011,3.89912,116.63,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kuh-e Siah section, Borazjan city',4285,'Sarvak','Cretaceous','Lower Cretaceous','Albian','Albian-Cenomanian',93.90,113.00,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3251,NULL,'Angular rudist and coral with minor amounts of echinoids and benthic foraminifera fragments. Middle shelf and ramp environments',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,28.49,51.31,NULL,NULL,NULL,NULL,4.03890263155,47.1630337767,2.42681267861,41.5313382801,3.85718,41.4148,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kuh-e Mond well, Fars Area',4286,'Sarvak','Cretaceous','Lower Cretaceous','Albian','Albian-Cenomanian',93.90,113.00,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','2','Below fair weather wave base','5','Rudists','13','Echinoderms','91','Rudists - corals - algae/microbes - (brachiopods)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3251,NULL,'Bioclastic pelloidal packstone consists mainly of pelloid with small benthic foraminifera, such as textulariids, alveolina, plaealveolina, conical orbitolina, echinoderms and rudist fragments. The pelloidal nature of this facies together with rudist\r\nand echinoid bioclasts indicate shallow open marine environment with good water circulation.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,28.2,51.19,NULL,NULL,NULL,NULL,3.7707320202,47.0099087554,2.16642785075,41.3655133272,3.58611,41.2669,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Northern shore of the Cíjara dam',4287,'Villarta, lower Villarta member','Ediacaran','Ediacaran','Nama Assemblage','upper Ediacaran',541.00,635.00,0,'Vendian',605,540,'Cambrian/Precambrian boundary (541 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m','2000','2',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'2','Below fair weather wave base','3','Microbes','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'3','High production of reefal debris','2','Intense',0,'No or unknown reservoir potential',3253,NULL,'Bioherms, shelly-microbial buildups.The reef-core facies consists of Cloudina-thromboid to stromatoid-thromboid boundstones and floatstones. Due to neomorphism, the calcified\r\nmicrobial communities are heterogeneously preserved, with clotted pseudospar textures\r\noccurring directly encrusting both microsparitic substrates and shelly walls. The\r\nmicrobial framestone is dominated by clotted, peloidal, fenestral textures, and subsidiary\r\nstromatolitic microsparite/sparry textures. Predominant skeletal components are\r\nCloudina carinata, C. hartmanae (probably C. xuanjiangpingensis), Sinotubulites\r\nbaimatuoensis, and rare Protolagena sp.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,39.15,-4.47,NULL,'205645',NULL,NULL,-35.2572473968,-4.53407647451,-35.2572473968,-4.53407647451,-46.7133,107.899,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Phu Pha Sing and Phu Pha Noi hills',4288,'Nam Mahoran','Carboniferous','Pennsylvanian','Kasimovian','Kasimovian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','2','Below fair weather wave base','2','Algae','3','Microbes','26','Phylloid and other platy algae - cements - (microbes)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3255,NULL,'Phylloid algal reef mound association is mainly composed of massive phylloid algal boundstone dominated, up 30% of bioclasts, by cup-shaped phylloid algae with locally common algal-skeletal\r\npackstone and wackestone. Red algae,calcimicrobes, forams, rugose coral, peloids, echinoderms,\r\nbrachiopods,fusulinds, ostracods can be found.',NULL,NULL,NULL,NULL,'Thailand','Asia',NULL,NULL,17.15,101.49,NULL,'205808',NULL,NULL,-21.5730426091,138.499803456,-7.57157865638,78.7146136827,-20.9583,105.043,'Krause','Krause','2021-05-28 15:21:12','2021-06-11 15:46:18'),('Değirmençay, Mersin Province',4289,'Karaisali','Neogene','Miocene','Lower Miocene','Burdigalian-Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','30','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3257,NULL,'Red  algae, coral  and  benthic  foraminifera  bearing reefal limestone.',NULL,NULL,NULL,NULL,'Turkey','Asia',NULL,NULL,36.54,34.3,NULL,NULL,NULL,NULL,35.9936677288,31.0164205054,34.5757968323,33.1651232633,36.0931,34.1275,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lumazhai and Zhongxinzhai locality',4290,'Weining','Carboniferous','Pennsylvanian','Moscovian','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','19','3','101-1000 m wide',NULL,'3','More than 100 m','30',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','2','Algae','3','Microbes','26','Phylloid and other platy algae - cements - (microbes)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','19','4','Microbial precipitation',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3259,NULL,'Skeletal–cement–microbial reef (SCMR-1) in lower part of section\r\nGrey thick-bedded microbial carbonate and phylloid algae boundstone. The substrate is composed of grey thick-bedded wackestone and packstone. Peloids, microbial mat debris, bioclasts constitute most of the volume of the lower part. Bioclasts, including bryozoans, small brachiopod shells, gastropods, ostracods, crinoids, and foraminifera. The substrate becomes clotted wackestone towards\r\nthe mound and the biodiversity decreases. Skeletal grains have micritic envelopes.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.5075,106.233889,NULL,'206265',NULL,NULL,-11.4842550207,120.103224063,5.83659551771,96.7993144835,-13.9059,98.7312,'Krause','Kiessling','2021-05-28 15:21:12','2023-01-04 15:04:29'),('Mahmudia Quarry, Caeracul Mare Hill, sample 114',4291,'Caerace, Tubiphytes-Limestone Member','Triassic','Middle Triassic','Anisian','middle Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,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,NULL,NULL,'3','Microbes','15','Non-rudist bivalves','40','Microbes - mollusks',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','122','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3260,NULL,'Tubiphytes-microbial buildup with bivalves, gastropods, brachiopods, ostracod fauna',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,45.03,29.03,NULL,'197722',NULL,NULL,27.8110331768,44.4592677994,26.4206026153,38.7538618433,17.5736,33.6202,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('South of Al Ain locality',4292,'Asmari','Paleogene','Oligocene','Rupelian','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',NULL,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','110','2','10 - 100 m wide',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)','3','Below storm wave base','1','Corals','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3261,NULL,'Massively bedded floatstone/rudstone is interbedded with packstone to floatstone. Coral and calcisponge clasts of pebble to boulder size are abundant.',NULL,NULL,NULL,NULL,'United Arab Emirates','Asia',NULL,NULL,24.01,55.48,NULL,NULL,NULL,NULL,16.7946723726,48.9428145701,14.5450677765,50.3165613533,17.2778,49.4575,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Finucane-1 wells',4293,'Unknown','Neogene','Miocene','Middle Miocene','late Langhian',13.80,14.80,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick','30','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Carbonate buildups and reef facies consisting largely of skeletal grains including foraminifera, bryozoans, molluscs and corals.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.2,116.44,NULL,NULL,NULL,NULL,-26.272183388,112.062434491,-28.7584063564,112.743205467,-28.2234,111.75,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Finucane-1 wells',4294,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick','30','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.2,116.44,NULL,NULL,NULL,NULL,-25.4604967851,112.561567856,-27.7524563652,113.133630199,-25.8188,113.248,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Picard-1',4295,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.04,117.48,NULL,NULL,NULL,NULL,-26.4402607675,112.976689091,-28.9985131032,113.724130598,-28.1116,112.872,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Picard-1',4296,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','1','Corals','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.04,117.48,NULL,NULL,NULL,NULL,-25.3234147611,113.653102663,-27.613962849,114.246964869,-25.7014,114.346,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('IODP-U1464',4297,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-18.04,118.37,NULL,NULL,NULL,NULL,-25.4584870478,113.938624724,-28.0153402779,114.706613281,-27.1512,113.875,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('IODP-U1464',4298,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. Reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-18.04,118.37,NULL,NULL,NULL,NULL,-24.3414773463,114.605972752,-26.630103419,115.216117321,-24.7366,115.323,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Minilya-1',4299,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-18.32,118.5,NULL,NULL,NULL,NULL,-25.7409003786,114.069344841,-28.2975058517,114.840995483,-27.4363,114,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Minilya-1',4300,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'12','Foraminifera','7','Bryozoans','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-18.32,118.5,NULL,NULL,NULL,NULL,-24.6238925019,114.735502822,-26.9122062402,115.348988514,-25.0212,115.447,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('East Mermaid-1',4301,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.15,119.47,NULL,NULL,NULL,NULL,-24.5882404621,115.113940981,-27.1423874163,115.905633699,-26.3062,115.09,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('East Mermaid-1',4302,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','12','Foraminifera','1','Corals','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.15,119.47,NULL,NULL,NULL,NULL,-23.4714542212,115.771109073,-25.7568569491,116.400256621,-23.8873,116.51,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Barcoo-1',4303,'Unknown','Neogene','Miocene','Lower Miocene','upper Burdigalian',16.00,17.50,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'2000','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','1','Corals','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3264,NULL,'Giant barrier reef system containing carbonate buildups and reef facies.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-15.29,120.3,NULL,NULL,NULL,NULL,-23.6815940386,115.468107331,-26.4586582301,116.411534202,-26.8978,114.624,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Reşiţa–Moldova Nouă zone',4304,'Valea Minişului','Cretaceous','Lower Cretaceous','Aptian','middle Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,120,'Early Cretaceous (early Aptian, 121.8 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','42','2','10 - 100 m wide',NULL,'4','More than 1000 m','1100','1.1',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','29','4','Microbial precipitation','2','Intensive','2','Intensive','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',3265,NULL,'Reef built by platy corals. The coral units are underlain by bioclastic limestones interlayered with thin rudist-chaetetid biostromes, separated by a 15–30 m thick interval of bioclastic limestones and overlain by upper Aptian conglomerates. Mostly dense, rarely sparse, platestones are composed of a low diversity coral assemblage mainly represented by the suborder Microsolenina. Small, branching corals are very rare. The matrix mainly consists of fine bioclastic-peloidal packstones and wackestones. Dominance of microsolenine corals, their flattened morphology, the presence of epibionts on coral undersurfaces and occurrence of red algae Sporolithon rude and Polyastra alba.',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,45.01,21.53,NULL,NULL,NULL,NULL,34.6147957382,33.2196496224,27.0289787133,26.0198938115,24.5123,26.3824,'Krause','Krause','2021-05-28 15:21:12','2021-08-19 17:05:37'),('Brecknock 1',4305,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,3,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','12','Foraminifera','1','Corals','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3264,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. ',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-14.35,121.42,NULL,NULL,NULL,NULL,-21.8160906836,117.200456661,-24.3627588828,118.022851417,-23.5773,117.273,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Brecknock 1',4306,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','12','Foraminifera','1','Corals','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3264,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. ',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-15.29,120.3,NULL,NULL,NULL,NULL,-21.625024075,116.667566156,-23.9073052585,117.304827116,-22.057,117.447,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('MioR-3 - Rowley Shoals',4307,'Unknown','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'250','4308',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Buried late Miocene isolated pinnacles and atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.23,119.07,NULL,NULL,NULL,NULL,-21.3930447602,116.620914975,-23.0511723815,116.962310875,-23.953,116.089,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('MioR-3 - Rowley Shoals, near Cunningham island',4308,'Unknown','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Buried late Miocene isolated pinnacles and atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.48,118.4,NULL,NULL,NULL,NULL,-21.633308334,115.929528583,-23.2922951093,116.262998755,-24.1782,115.379,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('MioR-3 - Rowley Shoals, East of Mermaid Reef',4309,'Unknown','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250','4308',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Buried late Miocene isolated pinnacles and atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.06,119.4,NULL,NULL,NULL,NULL,-21.2276283051,116.962000239,-22.8852422503,117.307144655,-23.7949,116.441,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('MioR-3 - East of Rowley Shoals',4310,'Unknown','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'250','4308',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Buried late Miocene isolated pinnacles and atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-16.59,119.5,NULL,NULL,NULL,NULL,-20.7590303877,117.071641044,-22.4164672603,117.417181002,-23.3288,116.564,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('MioR-3 - East of Rowley Shoals',4311,'Unknown','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250','4308',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Buried late Miocene isolated pinnacles and atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-16.51,120.09,NULL,NULL,NULL,NULL,-20.6867644813,117.677431553,-22.3431087437,118.02977875,-23.2692,117.182,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Saal Quarry',4312,'Unknown','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','90','2','10 - 100 m wide',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','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','31','1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1509,NULL,'Mostly reefal debris',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,48.887,11.941,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('GL1, Tazhong (Katake) Uplift, central Tarim',4313,'Penglaiba','Ordovician','Lower Ordovician',NULL,'lower Ordovician',470.00,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','3','Below storm wave base','2','Algae','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','1','Present',2,'Actual reservoir',3270,NULL,'Hydrocarbon reservoir',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,38.94,85,NULL,NULL,NULL,NULL,-15.0816937201,76.6851446934,-15.0816937201,76.6851446934,-24.5747,129.302,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Z11, Tazhong (Katake) Uplift',4314,'Yingshan','Ordovician','Lower Ordovician',NULL,'lower Ordovician',470.00,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,2,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','2','Below fair weather wave base','15','Non-rudist bivalves','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3270,NULL,'Ostracod-oyster-algae floatstone interbedded with bioclastic limestone',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,39.74,83.08,NULL,NULL,NULL,NULL,-16.3084379898,75.4827409691,-16.3084379898,75.4827409691,-24.5284,127.449,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lumazhai section, Houchang area',4315,'Maping','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','10','2','10 - 100 m wide','20','2','10 - 100 m',NULL,NULL,'3554',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','12','Foraminifera','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3271,NULL,'Patch reef consisting of a simple coral framework and a low biodiversity community. The substrate is composed of bioclastic grainstone and rudstone \r\nFomichevella, phacelloid and with an erect growth habit, form the reef framework. Asexual reproductive budding of Fomichevella is visible. Foraminifers and crinoids are common fossils. The spaces in\r\nthe coral framework are filled with bioclastic wackestonepackstone.\r\nBioclastic grainstone covers the coral patch reef, in which some coral debris are seen.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.5667,106.1,NULL,'211310',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2022-03-24 11:00:20'),('Pippu limestone, NE of the Asahikawa city',4316,'Tosshozan','Triassic','Upper Triassic','Carnian','Carnian',228.00,235.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','1','Corals','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3272,NULL,'Tubiphytes-calcimicrobe rudstone, dominated by Tubiphytes spp. and associated with large echinoderm ossicles. Poorly preserved calcimicrobes, reworked mud grains, micritized clasts and coated or aggregate grains are abundant. Other bioclasts are\r\nSoleporacean, red algae, microproblematica and the sponge Uvanella sp. Serpulids and bryozoan debris are rare. Microbial crusts were observed on a recrystallized framebuilder.',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,43.5,142.27,NULL,NULL,NULL,NULL,26.3797880372,147.471969759,79.5670547811,-147.890685914,44.4978,126.559,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jiwozhai reef',4317,'Dushan','Devonian','Middle Devonian','Givetian','middle Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','5','2','10 - 100 m wide','100',NULL,NULL,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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','35','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3273,NULL,'Patch reef with high biodiversity: stromatoporoids, rugose corals, tabulate corals, chaetetids,\r\nbrachiopods, bryozoans, calcified cyanobacteria and tubeworms.\r\n83 species were mentioned but only 35 are considered reef building',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.5,107.34,NULL,'212695',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Kiessling','2021-05-28 15:21:12','2023-03-10 13:16:53'),('WC55 reef, Belaya River gorge',4318,'Gerpigem','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',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','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3275,NULL,'It comprises mudstones interbedded with thin–medium-bedded bioclastic limestones, with abundant coral and sponge fragments, and plentiful bivalves. These grade upwards into massive reef facies that consist of coral-sponge rudstones in the lower part and platy coral reef limestones in the upper part. The reefs comprise thick biostromes. The bedded\r\ncarbonates consist of lagoonal bioclastic and micritic limestones that grade upward into gastropod and oncoidal limestones.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,44.16,40.1,NULL,'213016',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('WC6a-b, Akhtsu Zone',4319,'Katsirkhskaya','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3275,NULL,'Oxfordian–Tithonian. The principal reef organisms are corals and calcisponges. In the middle part of the succession, the facies consist of lithoclastic and bioclastic grainstones in the southern flank of the anticline and bioclastic packstones with sponges and coral fragments in the northern flank. The upper part of the succession on the southern flank of the anticline consists of intertidal-supratidal bioclastic limestones, abundant fenestral grainstone-packstones and algal packstones.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,43.36,40.02,NULL,'213022',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('WC114 - WC115, Bolyshaya Laba River',4320,'Gerpigem','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','30','2','10 - 100 m wide',NULL,'2','10 - 100 m','50',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3275,NULL,'The mound consists mainly of siliceous sponge-microbialite and microbialite boundstones. It is made up of a cluster of much smaller lenticular bodies or bioherms. The top of the reef succession is capped by thinly-bedded microbialite floatstones and bioclastic limestones.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,44.05,40.56,NULL,'213017',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Shitouzhai section, Ziyun region',4321,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base','6','Calcisponges','12','Foraminifera','88','Green algae - phylloid algae - calcisponges - (corals)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite',NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3276,NULL,'Reef formed largely of calcisponge floatstones and/or framestones. The spaces between the rigid framework formed by the sponges are filled with wackestones and packstones that contain numerous benthic foraminifers (Palaeofusulina, Colaniella, Glomospira), green algae (Dasycladales and Mizzia), and crinoids and bivalve fragments.\r\n\r\nFormation original was Changhsing. \r\nComments from Tian & Wang, 2021:\r\n\r\nReef builders: Frame-building and baffling\r\norganisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, bryozoans, and hydrozoans\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, ostracodes, bivalves, brachiopods,gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic: Fore-reef slope: packstone with\r\nfloatstone and reef breccias\r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella.\r\nReef flat (reef crest): algal-foraminiferal packstone with reef breccia.\r\nReef base: bioclastic packstone to grainstone.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin.\r\n\r\nCoordinates stated in text.\r\n\r\n\r\n\r\n',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.8417,106.0944,NULL,NULL,NULL,NULL,-15.6577408632,105.530130143,6.68779257563,123.248366238,7.24145,97.3327,'Krause','Krause','2021-05-28 15:21:12','2021-06-18 17:36:28'),('Lagonaki Highland and vicinity',4322,'Unknown','Jurassic','Upper Jurassic','Oxfordian','lower-middle Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','2b','Margin of deep basins (shelf margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3278,NULL,'Moderately  thick  reefal carbonates.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,44.03,39.08,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('vicinity of the city of Sochi and northern  Abkhazia',4323,'Unknown','Jurassic','Upper Jurassic','Oxfordian','middle-upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,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','4','Basin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3278,NULL,'Massive carbonate deposition with coral reefs',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,43.01,41.4,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Basins of the rivers Belaja and Laba',4324,'Unknown','Jurassic','Upper Jurassic','Oxfordian','middle Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','2b','Margin of deep basins (shelf margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3278,NULL,'Massive carbonate accumulation',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,44.01,41.59,NULL,NULL,NULL,NULL,32.4641082304,51.4977848812,37.3886980179,54.7300005974,38.2759,47.0304,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Barranco de Losilla',4325,'Zegri/Veleta','Jurassic','Middle Jurassic','Bajocian','Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3.5',NULL,NULL,NULL,'1','Less than 20 m','12',NULL,NULL,0,'Tropical or unknown','4','Basin','4b','Deep basin (> 200 m)','2','Below fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3281,NULL,'Buildup of thin-shelled bivalves',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,37.25,-4.24,NULL,NULL,NULL,NULL,16.64086265,14.9789063445,21.9800145478,11.1139888475,28.0497,5.81673,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Longgang area',4326,'Changhsing','Permian','Lopingian','Changhsingian','late Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',3282,NULL,'Grey dolomitized reefs or dolomitized boundstone\r\nfacies, with an average porosity of 4.0%.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,27.48,105.2,NULL,NULL,NULL,NULL,-13.808382706,104.503236395,8.69445676141,122.62660003,8.44898,95.5994,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Shaghap piggyback basin',4327,'Unknown','Paleogene',NULL,NULL,'Eocene/Oligocene',23.00,56.00,NULL,NULL,NULL,35,'Late Eocene (Priabonian, 35.9 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m','500',NULL,NULL,0,'Tropical or unknown','4','Basin','4b','Deep basin (> 200 m)','2','Below fair weather wave base','2','Algae','1','Corals','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','100','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3283,NULL,'Outcrop with conglomerates and breccias, reefal blocks of branching coralline limestones, siltstones, claystones and calci-mudstones. With small planktonic foraminifers, discocyclinids as well as numerous red algal, coralline algal fragments. Additionally, some echinoids,\r\nbryozoans, bivalve fragments and gastropods are present. Few fragments of Bryozoans are observed in microbialites. Microbial peloids and encrusting filaments form incipient branching structures',NULL,NULL,NULL,NULL,'Armenia','Europe',NULL,NULL,39.52,44.51,NULL,'214574',NULL,NULL,39.6133670816,39.1674560563,37.8892467821,43.1932962485,36.1721,40.7467,'Krause','Krause','2021-05-28 15:21:12','2022-05-24 17:16:00'),('Roztoka (S1)',4328,'Hradiste','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15','4','Microbial precipitation','1','Present','1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3285,NULL,'light-beige, porous, sponge–microbial limestones. There are two main types of microfacies: Sponge–microbial framestones–floatstones and fine-grained bioclastic wackestones–packstones. Depositional environment: low- to moderate-energy mid ramp',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,49.52,20.48,NULL,NULL,NULL,NULL,31.2496826059,33.3886401933,37.2602811346,35.3170033321,41.44,27.3347,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lanckorona',4329,'Unknown','Jurassic','Upper Jurassic','Kimmeridgian','lower Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15','4','Microbial precipitation',NULL,NULL,'1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3285,NULL,'Light-beige, porous, sponge–microbial limestones. There are two main types of microfacies: Sponge–microbial framestones–floatstones and fine-grained bioclastic wackestones–packstones. Depositional environment: low- to moderate-energy mid ramp',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,49.5,19.44,NULL,'215202',NULL,NULL,31.587477213,31.1457673971,36.5641872203,33.484476069,41.5403,26.1257,'Krause','Krause','2021-05-28 15:21:12','2022-08-25 16:57:14'),('Sulow',4330,'Unknown','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15',NULL,NULL,NULL,NULL,'1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3285,NULL,'Light-beige, porous, sponge–microbial limestones. There are two main types of microfacies: Sponge–microbial framestones–floatstones and fine-grained bioclastic wackestones–packstones. Depositional environment: low- to moderate-energy mid ramp',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,49.57,20.06,NULL,'215203',NULL,NULL,31.4771757158,32.382732679,37.0465095831,34.4968926345,41.6557,26.6496,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Esashi limestone',4331,'Heian','Triassic','Middle Triassic','Ladinian','Ladinian-Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','20',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'13','Echinoderms','3','Microbes','86','Microbes - sponges - crinoids','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3286,NULL,'Large echinoderm ossicles, debris of calcimicrobes, debris of bivalves, bryozoans and calcimicrobes indet. Remobilized framebuilders (i.e., recristallized corals and spongiomorphids).',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,44.54,142.21,NULL,NULL,NULL,NULL,7.50628107176,162.286819639,80.7925307788,-143.466112108,45.1778,123.323,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Quarry 23, Dent Peninsula, Sabah',4332,'Togopi','Neogene','Pliocene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',NULL,1,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,'2','10 - 100 m wide',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','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','22',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3287,NULL,'Loosely cemented rubbly reef limestone, with well-preserved and rich fauna of molluscs, echinoids, foraminifera, gastropods and corals in apparent growth positions. ',NULL,NULL,NULL,NULL,'Malaysia','Asia',NULL,NULL,5.15,119.12,NULL,NULL,NULL,NULL,5.63898201179,118.724497227,5.14312577351,118.877039777,5.18036,119.428,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('section J reefs, Ibex area, Millard County, Utah',4333,'Wah Wah','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'11','Siliceous sponges','11','Siliceous sponges','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3288,NULL,'Sponge-Rich Patch Reefs. Two conspicuous 1.5 m and 3 m thick reef intervals, with reefs rich in lithistid sponges.',NULL,NULL,NULL,NULL,'United States','North America',NULL,NULL,38.51,-113.27,NULL,NULL,NULL,NULL,21.4236851738,-117.858685301,21.4236851738,-117.858685301,-5.5443,-83.4703,'Krause','Krause','2021-05-28 15:21:12','2022-06-28 16:53:42'),('Mt. Tului',4334,'Mt. Tului','Jurassic','Upper Jurassic','Oxfordian','late Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','45','2','10 - 100 m wide','100',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',3290,NULL,'Type 1 build-ups developed in the proximal middle ramp and consist of 45 m thick, 100 m wide, coral-stromatoporoid boundstone associated with coral–stromatoporoid rudstone–grainstone. Type 2 build-ups, colonizing deeper environments in the middle ramp, are lens-shaped coral–calcareous sponge–diceratid boundstone including stromatoporoids and chaetetid sponges, 1–2 m thick and 3–4 m wide, associated with bioclastic packstone–grainstone. Type 3 lens-shaped calcareous and siliceous sponge–coral–microbialite boundstone build-ups (1 m thick and a few metres wide) formed in lower energy, distal middle-to-outer ramp settings.',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,40.15,9.35,NULL,NULL,NULL,NULL,21.0650280943,24.2228004707,23.1048407077,18.6979560589,33.3116,14.6388,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gold Point Reef, Nevada',4335,'lower Poleta','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','70',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1791',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','58','Archaeocyaths - microbes (Renalcis, Epiphyton, Girvanella) - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3294,NULL,'Reef built by massive branching archaeocyaths and dense renalcid thickets. ',NULL,NULL,NULL,NULL,'United States','North America',NULL,NULL,37.38,-117.26,NULL,NULL,NULL,NULL,14.3196058988,-154.139091862,14.3196058988,-154.139091862,-7.63991,-101.293,'Krause','Krause','2021-05-28 15:21:12','2021-06-12 14:33:36'),('Wudang, western Yangtze Platform',4336,'Tungtzu','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','0.4','1','Less than 10 m wide',NULL,NULL,NULL,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,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3296,NULL,'The stromatolites are 40 cm thick and flat column shaped, but strongly dolomitized.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,26.61,106.75,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-06-13 15:20:44'),('Letca and Băbeni–Cuciulat',4338,'Cozla','Paleogene','Eocene','Priabonian','Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','55',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1096',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','18','1','Constructor guild','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,'1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3297,NULL,'The reefs occur within a shallow‐water succession composed mostly of bedded limestones, dominated by bioclastic (coralline) packstones. Branching ramose colonies, branching low‐integrated phaceloid, and sheet‐like (foliaceous) corals dominate.\r\nRupelian',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,47.33,23.47,NULL,'220523',NULL,NULL,45.7406075429,17.465831329,43.9566915494,17.6748379203,42.9662,20.7541,'Krause','Krause','2021-06-05 21:20:15','2021-06-13 15:20:44'),('Chenluzhen quarry, Chenluzhen County',4339,'Pingliang','Ordovician','Upper Ordovician','Sandbian','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','40',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','3','Below storm wave base','3','Microbes','1','Corals','61','Microbes (thrombolites) - algae - corals','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3298,NULL,'The reef can be classified as a skeleton–cement reef or a triple hybrid carbonate of skeleton–microbial–abiotic components.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.03,109.1,NULL,'220534',NULL,NULL,34.8924063117,92.3052178995,34.8924063117,92.3052178995,-25.3266,122.507,'Krause','Krause','2021-06-07 16:27:41','2021-06-12 14:20:08'),('Kuh-e Hambast C Section, Abadeh Area',4340,'Elika','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1.6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','11','Siliceous sponges','16','Keratose Sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3299,NULL,'Sponge microbial buildups. Coordinates stated in text',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,30.9,53.22,NULL,NULL,NULL,NULL,-1.53494397363,61.360873559,3.1374130146,60.3458109236,-2.15634,47.5684,'Krause','Krause','2021-06-12 07:59:25','2021-07-21 16:21:05'),('Shahreza section',4341,'Elika','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','20','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','11','Siliceous sponges','16','Keratose Sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3299,NULL,'Sponge-Microbial Mounds and Aragonite Crystal Fan or\r\nBundle Layers. Coordinates stated in text',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,32.12,51.95,NULL,NULL,NULL,NULL,0.191306743866,60.6312367216,4.7586553021,59.4034515753,-1.35907,45.8716,'Krause','Krause','2021-06-12 08:16:36','2021-07-21 16:21:05'),('Puerto Llano section',4342,'Sierra del Pozo, upper member','Cretaceous','Lower Cretaceous','Valanginian','Valanginian',132.90,139.80,23,'late Valanginian - early Aptian',126,135,'Early Cretaceous (Valanginian, 136.4 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','51',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3301,NULL,'Coral assemblage. Coordinates estimated from map',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,37.8527,-2.9123,NULL,'220703',NULL,NULL,19.5803245815,10.2811962583,25.2232214533,7.12396048471,29.5583,5.53286,'Krause','Krause','2021-06-13 15:20:40','2021-06-13 16:37:50'),('Kermanshah, Zagros',4343,'Taleh Zanggg','Paleogene','Paleocene','Danian','middle-late Paleocene',56.00,61.60,27,'Thanetian - Ypresian',53,55,'Paleocene/Eocene Boundary (PETM, 56 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','30','2','10 - 100 m wide',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',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',3302,NULL,'Coordinates estimated from map\r\nTotal thickness of massive limestone is 30 m. Individual reef bodies smaller.\r\nAbundant green algae in overyling facies.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,34.21,46.7,NULL,NULL,NULL,NULL,20.5428382257,41.5463509608,22.8402319195,41.2306754512,20.0629,39.7015,'Kiessling','Kiessling','2021-06-17 11:55:21','2022-04-21 09:46:51'),('Qincaiyuan, Gendan, Tanluzhai, Ziyun, Guizhou',4344,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','110.4',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','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','16','4','Microbial precipitation',NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, bryozoans, and hydrozoans\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nreef dwellers:\r\nEchinoderms, ostracodes, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella.\r\nReef flat: algal-foraminiferal packstone with reef breccia.\r\nReef crest: ancient weathering crust.\r\nReef base: bioclastic packstone.\r\nBack-reef: bioclastic packstone with calcareous algae,gastropods, and foraminifers.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.75,106.1,NULL,NULL,NULL,NULL,-15.4084845079,105.577188696,6.92324909249,123.342542704,2.7186,98.3138,'Krause','Krause','2021-06-17 17:45:02','2021-06-20 13:22:33'),('Bure',4345,'Unknown','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,3,'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','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','36',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3304,NULL,'Coral reef complex. Coordinates estimated from map.',NULL,NULL,NULL,NULL,'France','Europe',NULL,NULL,48.5052,5.3578,NULL,NULL,NULL,NULL,27.2592773102,23.3543700481,33.4141374892,24.052097908,39.396,14.5264,'Krause','Krause','2021-06-17 18:30:19','2021-07-21 16:21:05'),('Sirogojno Melange in the Zlatibor Mountain',4359,'Unknown','Triassic','Upper Triassic','Norian','Sevatian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','6','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','1','Corals','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','43',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',3305,NULL,'Dachstein Limestone forereef block is part of the upper carbonate-clastic Sirogojno Melange. The succession starts with coarse-grained rudstones followed\r\nby meter-sized reefal blocks intercalated in partly layered resedimented grainstones\r\nand packstones with abundant reef-building organisms like calcareous\r\nsponges, corals and encrusting organisms. Inside this part of the succession\r\nopen-marine influenced layers are rare. The succession continues with a partly\r\nturbiditic sequence and chaotic rudstones, densely packed with reef-derived\r\nmaterial like broken reef-building organisms and shallow-water material like\r\ngastropods, bivalves and foraminifers. Grainstones with clear open-marine influence\r\n(e.g., thin-shelled bivalves, crinoids, conodonts) appear in between those\r\nrudstones, in cases lumachelle layers consisting of halobiids were deposited. To\r\nthe end of the succession some layers show turbiditic bedding with mixed shallow-\r\nwater and deep-marine grains and organisms, i.e. filaments and crinoids.\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'Serbia','Europe',NULL,NULL,43.7045,19.8378,NULL,'221271',NULL,NULL,17.3096523934,31.2354195615,14.7727274521,27.42095775,22.1254,19.7781,'Krause','Krause','2021-07-21 16:21:02','2021-07-26 12:58:46'),('Tiechanghe, Tongjiang, Sichuan',4346,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','10',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','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12',NULL,NULL,NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers: Crinoids, brachiopods, gastropods, benthic foraminifera, and calcareous algae.\r\n\r\nRock type and reef-related depositional characteristic: Reef core: sponge framestone and bafflestone\r\nInter-reef: bioclastic packstone\r\nReef flat (reef crest): fine-crystalline dolostone containing bioclasts\r\nBack-reef: bioclastic wackestone to packstone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,32.38,107.11,NULL,'220875',NULL,NULL,-8.72119434334,105.453033395,13.5016225662,124.570860975,13.4063,94.0981,'Krause','Krause','2021-06-18 09:58:47','2021-06-22 16:27:05'),('Dapaichong, Guiyang, Hunan',4347,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'3','101-500 m thick','154.4',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','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','4','Microbial precipitation',NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nreef dwellers: Echinoderms, bivalves, ostracodes, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic: Reef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella.\r\nInter-reef: bioclastic lime dolostone.\r\nReef base: crinoidal packstone to grainstone.\r\nBack-reef: bioclastic dolomitic wackestone to packstone with calcareous algae, ostracodes, and foraminifers.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.75,112.82,NULL,'220876',NULL,NULL,-14.2891922765,111.730615578,6.72582742085,129.434565663,11.0318,102.231,'Krause','Krause','2021-06-18 10:40:12','2021-06-22 17:17:21'),('Xinwuchang, Guiyang, Hunan',4348,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','107',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','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sponges, sclerosponges, bryozoans, and hydrozoans.\r\nBinding organisms: Archaeolithoporella, Tubiphytes, Fenestella and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, bivalves, ostracodes, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic: \r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella.\r\nInter-reef: bioclastic lime dolostone.\r\nReef base: crinoidal packstone to grainstone.\r\nBack-reef: bioclastic dolomitic wackestone to packstone with calcareous algae, ostracodes, and foraminifers.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.65,112.48,NULL,NULL,NULL,NULL,-14.4545259647,111.44504726,6.63024632315,129.12468991,10.7681,102.043,'Krause','Krause','2021-06-18 11:07:34','2021-06-20 13:22:33'),('Gantian’ao, Luodian, Guizhou',4349,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','105.2',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','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders: Frame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponge, bryozoan, and hydrozoan\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, ammonites, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic: Fore-reef slope:\r\nspiculitic-calcispherical cherty wackestone with reef breccias.\r\nReef core: framestone, bafflestone, and bindstone.\r\nReef flat (reef crest): packstone with reef breccia.\r\nReef base: echinodermal packstone to grainstone.\r\nBack-reef: bioclastic packstone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.54,106.91,NULL,NULL,NULL,NULL,-15.5059249541,106.358997932,6.67740351595,124.066568706,7.73067,97.9873,'Krause','Krause','2021-06-18 17:36:25','2021-06-20 13:22:33'),('Xikou, Zhenan, Shaanxi',4350,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','95.5',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','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, and bryozoans.\r\nBinding organisms: Tubiphytes, sclerosponge, and cyanobacteria\r\n\r\nReef dwellers: Echinoderms, ostracodes, bivalves, brachiopods, gastropods, bryozoans, benthic foraminifera, calcareous algae, and single rugose corals\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: less sponge framestone and more bafflestone and sponge-Tubiphytes-cyanobacteria bindstone.\r\nReef flat: bioclastic packstone with reef breccia.\r\nReef base: crinoidal packstone.\r\nReef crest: bioclastic wackestone and micritic limestone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.2419,109.376,NULL,NULL,NULL,NULL,-7.55378149464,107.20471821,14.2857181414,126.567030658,15.2291,95.1542,'Krause','Krause','2021-06-19 19:07:17','2021-06-20 10:08:56'),('Songshan, Wuxi, Jiangsu',4351,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','101',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','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, and bryozoans.\r\nBinding organisms: Tubiphytes, sclerosponge, and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and Waagenophyllum.\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: less sponge framestone and more bafflestone and sponge-Tubiphytes-cyanobacteria bindstone.\r\nReef flat: bioclastic packstone with reef breccia.\r\nReef base: crinoidal packstone.\r\nReef crest: bioclastic wackestone and micritic limestone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform nearby platform margin.\r\n\r\nCoordinates stated in text. ',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.6,120.47,NULL,NULL,NULL,NULL,2.61486608713,114.878710357,25.736273826,105.750920815,19.7833,103.903,'Krause','Krause','2021-06-19 19:22:19','2021-06-20 10:08:29'),('Yanggudong, Xuanhan, Sichuan',4352,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','41.7',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','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, and bryozoans.\r\nBinding organisms: Tubiphytes, sclerosponge, Fenestella, Diplotrypa and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, ostracodes, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: less sponge framestone and more bafflestone and sponge-Tubiphytes-cyanobacteria bindstone.\r\nReef flat: bioclastic packstone with reef breccia.\r\nReef base: crinoidal packstone.\r\nReef crest: bioclastic wackestone to packstone with calcareous algae, gastropods, and foraminifers.\r\nReef base: crinoidal packstone\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.7167,108.3334,NULL,NULL,NULL,NULL,-9.20865837492,106.59731832,12.7939762481,125.605176624,13.48,95.3614,'Krause','Krause','2021-06-19 19:30:31','2021-06-20 10:07:39'),('Honghua, (MC2 well), Kaixian, Chongqing',4353,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','90',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','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12',NULL,NULL,NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders:  Baffling organisms: hypercalcified sphinctozoan and inozoan sponges.\r\nBinding organisms: Tubiphytes and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, brachiopods, gastropods, benthic foraminifera, and calcareous. algae.\r\n\r\nRock type and reef-related depositional characteristic: Reef core: sponge bafflestone and\r\nsponge-Tubiphytes-cyanobacteria bindstone.\r\nReef flat: bioclastic algae-crinoid packstone with reef breccia.\r\nReef crest: crinoidal-algal-foraminiferal wackestone to packstone and micritic dolostone.\r\nReef base: bioclastic packstone.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.53,108.48,NULL,NULL,NULL,NULL,-9.37154575493,106.753994065,12.6025113462,125.725512632,13.4031,95.5784,'Krause','Krause','2021-06-19 20:48:03','2021-06-20 16:02:45'),('Qujiawan, Chenxi, Hunan',4354,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','53.6',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','6','Calcisponges','1','Corals','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders: Frame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges and Waagenophyllum. Binding organisms:\r\nArchaeolithoporella, Tubiphytes, and cyanobacteria\r\n\r\nReef dwellers: Crinoids, ostracodes,brachiopods,  gastropods, benthic foraminifera, and calcareous algae.\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: more sponge bafflestone and less sponge framestone with the encrusting Archaeolithoporella\r\nReef flat: dolomitic bioclastic packstone with crinoids and reef breccia.\r\nReef crest: dolomitic crinoidal-algal-foraminiferal wackestone.\r\nReef base: dolomitic packstone with the clasts of brachiopods, gastropods, and crinoids.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform nearby platform margin\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,28,110.18,NULL,NULL,NULL,NULL,-12.5765883348,108.882467629,9.02477838345,127.105648919,11.4317,98.936,'Krause','Krause','2021-06-19 22:06:20','2021-06-20 10:05:42'),('Daoshiyan, Chenxi, Hunan',4355,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','48',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','6','Calcisponges','1','Corals','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12',NULL,NULL,NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, and Waagenophyllun.\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers:\r\nCrinoids, bryozoans brachiopods, gastropods, benthic foraminifera, and calcareous algae.\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: more sponge bafflestone and less sponge framestone with the encrusting Archaeolithoporella\r\nReef flat: dolomitic bioclastic packstone with crinoids and reef breccia\r\nReef crest: dolomitic crinoidal-algal-foraminiferal wackestone\r\nReef base: dolomitic packstone with the clasts of brachiopods, gastropods, and crinoids.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform nearby platform margin.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,28.07,110.22,NULL,NULL,NULL,NULL,-12.5011177447,108.904216855,9.09374124637,127.14341162,11.509,98.9226,'Krause','Krause','2021-06-20 09:49:05','2021-06-20 10:05:22'),('Xiaoquan, Yizhang, Hunan',4356,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','44.2',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','6','Calcisponges','1','Corals','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12',NULL,NULL,NULL,NULL,NULL,NULL,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',3300,NULL,'Reef builders:Frame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, and rugose coral.\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers: Crinoids, bryozoans, ostracodes, brachiopods, gastropods, benthic foraminifera, and calcareous algae.\r\n\r\nRock type and reef-related depositional characteristic: Reef core: more sponge bafflestone.\r\nand less sponge framestone with the encrusting Archaeolithoporella.\r\nReef flat: dolomitic bioclastic packstone with crinoids and reef breccia.\r\nReef crest: dolomitic crinoidal wackestone.\r\nReef base: dolomitic packstone with the clasts of brachiopods, gastropods, and crinoids.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform nearby platform margin.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.31,112.82,NULL,NULL,NULL,NULL,-14.7180697747,111.832157941,6.28586699337,129.428626362,10.6799,102.5,'Krause','Krause','2021-06-20 10:03:43','2021-06-20 10:04:14');
INSERT INTO `new_r_chart` VALUES ('FS1, Liangping, Chongqing',4357,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'1','Seismic data available ',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)',NULL,NULL,'6','Calcisponges',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'2','Intense',2,'Actual reservoir',3303,NULL,'Reef limestone and reef dolomite: Only developed \r\nin the Changxing Formation, the reef building organisms  are mainly sponges, while foraminiferas, brachiopods, and  other accessory organisms can also be seen. The content of sponges in the framework reef limestone is the highest, and  some of the sponges have been dolomitized, meaning the sponge frameworks are filled with dolomite.\r\n\r\nCoordinates estimated from map.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,30.6053,107.94,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-06-20 13:22:30','2021-06-20 16:02:06'),('well F1, FT1, Fengjie, Chongqing',4358,'Changxing, Chang 2 Member','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'1','Seismic data available ',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','6','Calcisponges',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'2','Intense',1,'Potential reservoir',3303,NULL,'Reef limestone and reef dolomite: Only developed\r\nin the Changxing Formation, the reef building organisms are mainly sponges, while foraminiferas, brachiopods, and other accessory organisms can also be seen. The content of sponges in the framework reef limestone is the highest, and some of the sponges have been dolomitized, meaning the sponge frameworks are filled with dolomite.\r\n\r\nCoordinates estimated from map.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.2913,109.2405,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-06-20 13:53:03','2021-06-20 16:02:19'),('Araetgol section, Yeongwol',4360,'Mungok','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1','1','Less than 10 m wide','1','1','Less than 20 m','1',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','16','Keratose Sponges','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2','3','Binder guild',NULL,NULL,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',3307,NULL,'The thrombolitic mounds are domes up to 100 cm high and 40–60 cm wide embedded within within lime mud and shale (ribbon rock). Analysis of slabs revealed that the mounds consist of cm-scale thrombolitic “clots” and homogeneous micrite with several intraclasts and bioclasts filling the interclot spaces.\r\nTwo types of clots are recognised: keratolite–microbialite and lithistid sponge–microstromatolite clots. Keratose and lithistid sponges rarely occur together in the Mungok reefs.',NULL,NULL,NULL,NULL,'South Korea','Asia',NULL,NULL,37.284,128.43,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2021-07-26 12:58:43','2021-07-26 12:58:47'),('Cortes section',4361,'Unknown','Devonian','Middle Devonian','Eifelian','late Eifelian-Givetian',382.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp',NULL,NULL,'13','Echinoderms','1','Corals','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3308,NULL,'Well-developed reef system, with significant diversity of reefal faunas (crinoids, corals and stromatoporoids). The calciturbidites include frequent fragments of crinoids and common coarse-\r\ngrained calciturbidites. Base of the slope.\r\n\r\nCoordinates estimated from map.',NULL,NULL,NULL,NULL,'Portugal','Europe',NULL,NULL,38.194,-8.08,NULL,NULL,NULL,NULL,-31.8292095473,-6.52160034534,-4.06209759556,-36.0081584502,-40.4652,20.6936,'Krause','Krause','2021-07-28 11:34:27','2021-07-28 11:38:58'),('Auerstedt section, German Basin',4362,'Diemel','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','0.05','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin',NULL,NULL,'16','Keratose Sponges','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3311,NULL,'Microbe-metazoan build-ups. The biocrusts at\r\nthe top of the build-ups consist of encrusting Pla-\r\ncunopsis bivalves and microconchids. Subtidal\r\nshallow marine environment. Coordinates estimated from map.',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,51.0975,11.5872,NULL,NULL,NULL,NULL,30.0937217312,29.7097237517,24.1833172497,24.4721790222,17.2847,19.8937,'Krause','Krause','2021-08-19 17:05:33','2021-08-19 17:33:51'),('Mauer, German Basin',4363,'Diemel','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','0.08','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','1','Above fair weather wave base','16','Keratose Sponges','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3311,NULL,'Microbe-metazoan build-ups ',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,49.3419,8.7992,NULL,NULL,NULL,NULL,27.9661135892,28.2026668292,21.7428340129,23.8706054571,14.9691,18.9056,'Krause','Krause','2021-08-19 17:33:48','2021-08-19 17:34:25'),('Seyweiler',4364,'Diemel','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','0.08','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','1','Above fair weather wave base','16','Keratose Sponges','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3311,NULL,'Microbe-metazoan build-up from is mainly composed of silicied carbonate. Fossils include bivalves and\r\nsponges. ',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,49.161,7.2682,NULL,NULL,NULL,NULL,27.5707482979,27.1454614292,21.0692097501,23.0542801164,14.4305,18.0155,'Krause','Krause','2021-08-19 17:52:46','2021-08-19 17:53:18'),('Libiąż, close to the Silesian–Moravian Gate',4365,'Diplopora Beds','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','0.4','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','1','Above fair weather wave base','16','Keratose Sponges','3','Microbes','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3311,NULL,'Microbe-metazoan build-ups, composed of\r\ncalcite, characterized by planar and sometimes\r\ndomal laminations. Stromatolite-bearing intervals occur in the upper part of the Diplopora Bed. Sponges are abundant and can be clearly rec-\r\nognized based on distinctive features such as\r\nmesh-like fabrics.',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,50.1123,19.3268,NULL,NULL,NULL,NULL,30.4961164605,35.4909326295,26.2392181704,29.5194923515,18.5809,24.9777,'Krause','Krause','2021-08-23 14:37:13','2021-08-27 15:46:15'),('Zakupne, Demkivtsi, Lysohirka (Medobory Hills)',4366,'Ternopil Beds','Neogene','Miocene','Middle Miocene','upper Badenian',13.80,16.00,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3312,NULL,'Biohermal (reefal) limestone. Coralgal reefs.',NULL,NULL,NULL,NULL,'Ukraine','Europe',NULL,NULL,49.1174,26.3361,NULL,'70569',NULL,NULL,48.4551115075,22.8579965192,48.0659131724,25.9895344463,49.5002,25.4964,'Krause','Krause','2021-08-27 15:46:11','2021-10-27 13:57:55'),('core XK-1, Xisha carbonate platform on Shidao Island',4367,'Huangliu','Neogene','Miocene','Upper Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'4','More than 1000 m wide',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','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reef.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,17.9873429721,111.300003983,16.333711529,111.4803614,16.7664,111.648,'Krause','Krause','2021-10-27 13:57:52','2021-10-28 18:27:52'),('core XK-1, Xisha carbonate platform on Shidao Island',4368,'Huangliu','Neogene','Miocene','Upper Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'3','101-1000 m wide',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','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reefs.\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,17.6049442161,111.653959042,16.5022223387,111.769900762,16.7566,112.125,'Krause','Krause','2021-10-27 14:14:24','2021-10-28 18:28:16'),('core XK-1, Xisha carbonate platform on Shidao Island',4369,'Meishan','Neogene','Miocene','Upper Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reefs.\r\n\r\nCoordinated stated in text. ',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,17.9873429721,111.300003983,16.333711529,111.4803614,16.7664,111.648,'Krause','Krause','2021-10-27 14:34:37','2021-10-28 18:28:32'),('core XK-1, Xisha carbonate platform on Shidao Island',4370,'Meishan','Neogene','Miocene','Upper Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reefs.\r\n\r\nCoordinates stated in text. ',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,17.6049442161,111.653959042,16.5022223387,111.769900762,16.7566,112.125,'Krause','Krause','2021-10-28 16:56:59','2021-10-28 18:28:49'),('core XK-1, Xisha carbonate platform on Shidao Island',4371,'Meishan','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reefs in shallow-sea shoal. \r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,18.28723206,110.861983659,16.1863375078,111.170163925,16.7664,111.648,'Krause','Krause','2021-10-28 17:05:04','2021-10-28 18:29:05'),('core XK-1, Xisha carbonate platform on Shidao Island',4372,'Meishan','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reefs.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,18.4810051212,110.540887132,16.0946216046,110.946051079,16.9125,112.172,'Krause','Krause','2021-10-28 18:27:02','2021-10-28 18:29:20'),('core XK-1, Xisha carbonate platform on Shidao Island',4373,'Sanya','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','1','Corals',NULL,NULL,'2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',3313,NULL,'Thick dolomitic reef with some bioclastic limestone in the upper part, alternating reefal and bioclastic limestone in the middle, and brownish breccia and coral reefs in the bottom.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,18.7720917869,110.053978895,15.9586122019,110.608439904,17.0969,112.689,'Krause','Krause','2021-11-09 16:05:11','2021-11-10 12:00:22'),('core XK-1, Xisha carbonate platform on Shidao Island',4374,'Sanya','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1d','Marginal marine - coastal -  siliciclastic shelf','2','Below fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Thick dolomitic reef with some bioclastic limestone in the upper part, alternating reefal and bioclastic limestone in the middle, and brownish breccia and coral reefs in the bottom.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,19.093648234,109.727873512,15.895462965,110.415585944,17.0969,112.689,'Krause','Krause','2021-11-09 16:18:17','2021-11-10 12:00:05'),('Jebel Serdj-Bargou',4375,'Lower Serdj','Cretaceous','Lower Cretaceous','Aptian','upper Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 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','1','Corals','5','Rudists','65','Corals - spongiomorphids - oysters - serpulids',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3314,NULL,'high carbonate productivity with the development of biostromal buildups. The carbonates of this unit show net northward facies and thickness changes. The biota is dominated by corals, orbitolinids,\r\nmiliolids, gastropods and oysters, reflecting the oligophotic conditions on a homoclinal carbonate ramp.',NULL,NULL,NULL,NULL,'Tunisia','Africa',NULL,NULL,36.0833,9.5666,NULL,NULL,NULL,NULL,16.7914731035,18.0610326422,19.9720978007,13.1240956947,19.9274,13.1032,'Krause','Krause','2021-11-10 14:21:47','2021-12-26 22:09:49'),('Cruz',4376,'Higueruelas','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1d','Marginal marine - coastal -  siliciclastic shelf','3','Below storm wave base','1','Corals','12','Foraminifera','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3319,NULL,'Biohermes of different thickness (decimetric to metric) and less lateral continuity are developped, highly colonized by corals, that are associated to oncolitic, bioclastic and oolitic of high energy\r\nfacies, in marginal areas, near the litoral developpment.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,41.3359,-0.8621,NULL,NULL,NULL,NULL,19.4880687057,15.1584554355,25.6092036526,12.4794970106,32.483,8.65899,'Krause','Krause','2021-12-26 22:09:46','2021-12-26 22:10:38'),('Jaulin',4377,'Higueruelas','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1d','Marginal marine - coastal -  siliciclastic shelf','3','Below storm wave base','1','Corals','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3319,NULL,'Within the inner shelf, in agitated subtidal conditions close to the coastal oolitic\r\ndevelopment, coral bioherms (boundstone corals) grow\r\n(coral boundstone) associated with bio-clastic, oolitic and oncolitic high energy facies.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,41.4559,-0.9908,NULL,NULL,NULL,NULL,19.6382626839,15.1222669967,25.7629492707,12.4693703515,32.6346,8.62722,'Krause','Krause','2022-01-04 19:57:25','2022-01-11 13:29:31'),('Anjiazhuang near Feicheng, Shandong',4378,'Zhangxia','Cambrian','Series 3','Drumian','Amgan',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'3','101-500 m thick','110','3','101-1000 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium 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',3320,NULL,'Age should be Drumian, which is not yet in the pulldown menu.\r\nSeveral calcimicrobes identified: Epiphyton, Bacinella, Hedstroemia, Girvanella, Renalcis.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.99,116.77,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,-1.2566,147.887,'Kiessling','Krause','2022-01-11 13:29:28','2022-06-28 17:10:20'),('Qujing',4379,'unknown','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',NULL,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,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3324,NULL,'No comment',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.4513,103.816,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-03-23 16:40:10','2023-03-17 17:45:34'),('Muli reef,  Wenshan-southeast Yunnan',4380,'unknown','Devonian','Lower Devonian',NULL,'Lower Devonian',393.30,419.20,8,'middle Pridolian - middle Pragian',412,400,'Early Devonian (Emsian, 400 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3324,NULL,'Sb-ore deposits',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,23.9887,105.3675,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-03-23 17:22:41','2023-03-17 17:45:34'),('Dongwan section',4383,'Feixianguan','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2.5','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','3','Below storm wave base','16','Keratose Sponges','3','Microbes','42','Microbes - siliceous sponges - (bryozoans) - corals','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3329,NULL,'Microbialite (2.5 m thick) is composed mainly of dendrolite. The basal layer of the microbialite is flat and layered, and its upper part is strongly domed. Shell beds are intercalated between domes. At the top, the dome-shaped microbialite flattens horizontally, and is overlain by muddy limestone. Conodont H. parvus was found in the horizon 0.45 m above the bottom of the microbialite.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,30.47,106.94,NULL,NULL,NULL,NULL,-9.76046411997,106.401097517,13.9975485319,123.350185971,11.7706,95.1194,'Krause','Krause','2022-04-06 16:11:09','2022-04-06 16:17:09'),('Mesa de Roldán + La Molata de las Negras',4381,'unknown','Neogene','Miocene','Upper Miocene','upper Messinian',5.30,6.00,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',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','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3322,NULL,'The reef unit onlaps the erosion surface and consists of small Porites patches that grew dispersed in oolitic shoals together with microbial carbonates. These low-diversity reefs are the last zooxanthellate coral reefs in the Mediterranean basin and constitute the endpoint of decreasing coral diversity in the region during the Miocene due to disconnection from the Indian Ocean and global cooling.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,36.95,-1.8667,NULL,'224629',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-03-24 15:03:36','2022-03-24 15:47:02'),('Djebel Ouarkziz',4382,'Djebel Ouarkziz','Carboniferous','Pennsylvanian','Bashkirian','Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,340,'Middle Mississippian (Early Visean, 338.8Ma)',NULL,3,'0','Outcropping reef ',4,'True reef','1','Less than 10 m thick','4.5','2','10 - 100 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals',NULL,'Brachiopods','2','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','25 or more reef building species','14',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3327,NULL,'Biostrome in shallow-water platform. A diverse set of microfacies have been observed in thin sections. The most abundant one is rudstone; bindstone and packstone are also common. More rarely, grainstone occur, mainly in the upper part of the bed. The identified components are the same as those occurring as macrofauna, plus foraminifers, calcareous algae, ostracods and scarce fragments of molluscs. Frequently, there is recorded the intergrowth of gigantoproductid brachiopods, rugose corals and chaetetid sponges.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,28.21,-9.29,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Siphonodendron','2022-03-28 17:49:17','2022-04-06 16:11:13'),('Xiushui section, SW of Dongling village near Sidu',4384,'Daye','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick','2.5','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','3','Below storm wave base','16','Keratose Sponges','3','Microbes','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3329,NULL,'Microbialite consists of a lower thrombolite (1.5 m thick) and an upper dendrolite (0.5 m thick). Hindeodus parvus conodont is present. the putative keratose sponge consortia were identified\r\nfrom a thin-bedded, spar-cemented oolitic limestone below the basal microbialite unit. It overlies unconformably above the uppermost Changhsingian bioclastic limestone. Above this oolitic limestone layer, the thrombolite is characterized by a clotted texture of reddish sparitic patches embedded in a grey micritic matrix, whereas the overlying dendrolite texture consists of brownish sparitic patches embedded within a yellow micritic matrix (weathering colour). Several shell layers containing microgastropod and bivalve fragments, ostracod tests, and intraclasts occur above the microbialite unit (Fig. 2). Above these shell layers is the succession dominated by micrites interbedded with peloidal wackestones. In the oolitic limestone layer, single ooids are 0.2–0.6 mm in diameter and round to oval in outline, occupying 55–65% of entire petrologic texture, and they are unevenly distributed. These ooids are strongly micritized so that concentric lines or radial structures become vague. Some grains retain outline of bioclast remains, mostly gastropods. The pores between the ooids are normally cemented by sparites and micritic clumps (micrite aggregates) are interspersed occasionally, indicating an intermittent high-energy environment. Light-coloured sparitic structures are rather common and evenly scattered and almost fill the dark-coloured micritic clumps. Some elongated individuals show vermiform shapes, while others are filamentous and branch occasionally. These dot-shaped and filamentous structures form maze-like networks. Single filaments vary in length, ranging from 100 to 500 μm, while their thicknesses are relatively consistent, except for tapering ends. Individual filaments are 10–70 μm (averagely 33 μm) in diameter, with filaments of 20–30 μm in diameter being most frequently occurring (nearly 20%). About 60% filaments are 20–40 μm in diameter. Filament is slightly inflated at the junction when branching, and these filamentous sparitic structures tend to be distributed parallel to the edge of the micritic clumps.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,29.05,114.58,NULL,NULL,NULL,NULL,-9.97012425281,113.280880362,11.9108230644,129.971413686,14.6023,101.449,'Krause','Krause','2022-04-06 17:54:58','2022-04-07 11:17:39'),('Xiushui section, SW of Dongling village near Sidu',4385,'Changxing','Permian','Lopingian','Changhsingian','lower Changhsingian',253.00,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'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,NULL,'6','Calcisponges','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3329,NULL,'Massive reefal carbonates with framestone of\r\nreef-core facies built by calcareous sponges. The matrix of the framestone is micritic, indicating that the wave energy on the reef was not strong.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,29.05,114.58,NULL,NULL,NULL,NULL,-11.0743209366,112.137089694,9.13938248376,131.605562272,14.6023,101.449,'Krause','Krause','2022-04-07 09:49:40','2022-04-07 18:33:30'),('Santa Cesarea Terme',4386,'Torre Specchialaguardia Limestone','Paleogene','Eocene','Priabonian','Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','72',NULL,NULL,NULL,NULL,NULL,'1000','1',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','24',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3331,NULL,'Coral fauna is moderately diversified (only 14 genera) associated with coralline algae and larger foraminifers (mainly dyscocyclinids). Tue sequence is represented by three main fades (from the bottom upwards): \r\n1 - Grainstone-packstone facies (ca. 15 m thick) rich in discocyclinids, nummulitids, scleractinian corals, and bryozoans. Large subglobose coral colonies (Actinacis, Antiguastrea, Astrocoenia, Favites and Agathiphyllia) and sublaminar and globose colonies of bryozoans are typically in life position. The displaced colonies are rare and typically bear no evidence of transport (bush-like colonies of e.g.,Actinacis seem to be only fallen down). Generally colonies preserved in situ are immersed in a bioclastic packstone that, with a sharp contact, passes to a grainstone wich disoriented discocyclinids. At the top of this fades present are also debris ßows with branching corals like Acropora, Stylophora and other large bioclasts. Abundant coralline algae and specimens of pectinids and other molluscs are also associated with this facies.\r\n2 - Bioclastic limestone (rudstones and/or floatsrones) facies (ca. 4S m thick) rich in scleractinians and coraline algae. \r\n3 - Wackestone-mudstone facies (ca. 12 m chick) with planktonic foraminifers, in which are debris-flows composed mainly of larger foraminifers and broken coral colonies.',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,40.05,18.475,NULL,'224871',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-04-07 18:33:27','2022-04-20 16:33:20'),('Line M1507-07',4387,'unknown','Neogene','Miocene','Middle Miocene','mid-Miocene',11.60,13.80,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,1,'1','Seismic data available ',NULL,NULL,'4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','4a','Shallow basin','1','Above fair weather wave base','2','Algae',NULL,NULL,'88','Green algae - phylloid algae - calcisponges - (corals)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3332,NULL,'Biogenetic reefs. The carbonates of biogenic reefs in the Andaman Sea are widely distributed, among which the carbonate platforms in the eastern terraces are mostly developed in fault blocks and volcanoes. The eastern terrace carbonate platform is mostly developed on the fault block and volcanic uplift, and the fault activity on the edge of the platform.',NULL,NULL,NULL,NULL,'Andaman Sea','Indian Ocean',NULL,NULL,11.8,96.5,NULL,NULL,NULL,NULL,13.1129929493,95.0130942229,11.0221883362,95.4699333308,9.80521,97.6727,'Krause','Krause','2022-04-20 16:33:17','2022-04-21 11:39:00'),('Line M1507-20',4388,'unknown','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,1,'1','Seismic data available ',NULL,NULL,'4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','4a','Shallow basin','1','Above fair weather wave base','2','Algae',NULL,NULL,NULL,NULL,'2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3332,NULL,'Biogenic reef carbonates ',NULL,NULL,NULL,NULL,'Andaman Sea','Indian Ocean',NULL,NULL,12.17,96.86,NULL,NULL,NULL,NULL,13.5625545145,95.1658013228,11.3346244932,95.6782853535,10.2112,97.9875,'Krause','Krause','2022-04-21 09:42:30','2022-04-21 11:39:35'),('Line M1507-03',4389,'unknown','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,1,'1','Seismic data available ',NULL,NULL,'4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'40',NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','1','Above fair weather wave base','2','Algae',NULL,NULL,NULL,NULL,'2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3332,NULL,'Biogenic reef carbonates',NULL,NULL,NULL,NULL,'Andaman Sea','Indian Ocean',NULL,NULL,12.5,96.86,NULL,NULL,NULL,NULL,13.8925444663,95.1631503848,11.6646241986,95.6778353509,10.5392,97.9511,'Krause','Krause','2022-04-21 11:32:45','2022-04-21 11:40:02'),('Wadi Araba',4390,'Rod El-Hamal Formation','Carboniferous','Pennsylvanian','Moscovian','upper Moscovian',311.00,315.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','8','1','Less than 10 m wide',NULL,'2','10 - 100 m','42',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','2','Algae','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3333,NULL,'Mounds formed by filamentous microbes and phylloid algae. Phylloid algae are loosely accumulated and supported by micritic encrustations that were formed by filamentous microbes. The filamentous microbes growing perpendicularly to the phylloid algal surfaces produced concentrated areas of peloids-A. The spaces between the phylloid algal-microbial frameworks were filled with concentrated areas of peloids-B (peloid-B aggregations) oriented perpendicular to the phylloid algae surfaces.',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,29.1,32.28,NULL,NULL,NULL,NULL,-37.0445649148,29.3327691729,-35.5300533051,7.08352528472,-34.2506,30.0846,'Krause','Krause','2022-06-20 15:43:27','2022-06-20 17:31:54'),('Ruby Creek- Bornite deposit, Brooks Range',4391,'unknown','Silurian',NULL,NULL,'Ludlow-Gedinnian',410.80,427.40,NULL,NULL,NULL,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'4','More than 500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'3','Microbes','2','Algae',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Intense',1,'Potential reservoir',3334,NULL,'Stratigraphy uncertain.\r\nAge given as Wenlock-Lower Devonian',NULL,NULL,NULL,NULL,'United States','North America',NULL,NULL,67.06306,-156.9469,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-06-20 17:31:50','2022-06-23 15:16:39'),('Test 4',4417,'Test 4','Jurassic','Upper Jurassic','Oxfordian','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,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,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3356,NULL,'Test 4',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,44.55,55.44,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2023-04-04 15:50:09',NULL),('Arroyo Uitpa, Arroyo Ekieps at the foothills of the Serranía de Jarara in the Cocinetas Basin',4392,'Siamaná','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,1,'0','Outcropping reef ',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',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','24',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3335,NULL,'The Arroyo Uitpa paleoenvironment is characterized by patch reefs developed in a shallow lagoon close to the shore-line, while Arroyo Ekieps was a barrier reef system, which offered a wide variety of microhabitats enhanced by the structural complexity of the reef framework. This suggests an increase of bryozoan diversity with higher reef complexity.',NULL,NULL,NULL,NULL,'Colombia','South America',NULL,NULL,12.04,-71.26,NULL,'201392',NULL,NULL,7.51495175157,-69.6046432843,10.7106751354,-68.8258607723,11.1348,-67.6034,'Krause','Krause','2022-06-23 15:16:35','2022-06-23 15:27:49'),('Chenluzhen',4393,'Pingliang Formation','Ordovician','Upper Ordovician','Sandbian','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'15','Non-rudist bivalves','16','Keratose Sponges',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3337,NULL,'Age is roughly identified. Maybe Sandbian?',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.035833,109.170833,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'J.-H.Lee','Krause','2022-06-28 19:22:49','2022-06-29 17:08:18'),('Beiquanzi',4394,'Zhangxia Formation','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','0.3','1','Less than 10 m wide','1.5','1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3338,NULL,'Occurs as patches within Epiphyton-dominant microbial reefs that are >10 m large',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,36.479722,116.924444,NULL,NULL,NULL,NULL,23.9854140172,98.6788601127,23.9854140172,98.6788601127,-0.871239,147.56,'J.-H.Lee','Krause','2022-06-28 21:13:44','2022-07-19 18:20:57'),('Zargar area, Section A',4395,'Lut platform','Paleogene','Eocene','Ypresian','Ypresian',47.80,56.00,27,'Thanetian - Ypresian',53,50,'Early Eocene (Ypresian, 51.9 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'2','10 - 100 m','15','30',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','12','Foraminifera','20','Corals - forams','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3339,NULL,'The sedimentary succession consists of two informal units: the conglomerate unit and calcareous unit (Lower and Upper Units).The conglomerate unit is composed with subangular to rounded pebbles of foraminiferal limestone and red chert. A large number of mollusk fragments, mainly gastropods and bivalves were identified. The calcareous unit is composed of thick limestones (wackestone) bearing foraminifera occurring in the lower one-third part of the unit which passes upward into thick gray limestone containing foraminiferal fauna alveolinids and orbitolitids and continues with very thick coral limestones in the middle part of this unit. The upper one-third of the calcareous unit is composed of well-bedded bioclastic gray to yellow wackestone and biomicrosparite which is characterized by the presence of coralline red algae, Nummulites globulus Leymerie and rare miliolids. It continues with gray micritic limestone (packstone to grainstone) defined by the presence of disc-shaped orthophragminids.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,32.7222,59.2417,NULL,NULL,NULL,NULL,33.0211035139,54.382543926,32.5111702882,58.1888560669,8.84273,57.4834,'Krause','Krause','2022-07-19 17:38:47','2022-07-21 18:07:01'),('Kaboudeh area, section B',4396,'Lut platform','Paleogene','Eocene','Ypresian','Ypresian',47.80,56.00,27,'Thanetian - Ypresian',53,50,'Early Eocene (Ypresian, 51.9 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'40','2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','12','Foraminifera','20','Corals - forams','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','16',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3339,NULL,'Coral dominated macrofacies consting of two units - conglomerate and calcareous units. The conglomerate unit contains with various rock fragments such as cherts, basalt and fossiliferous limestone bearing small Nummulites. It is followed by medium grain sandstone including chert fragments and terrigenous detritus (quartz, feldspar and mica). The lower part of calcareous unit contains the small benthic miliolid foraminifera in a micritic matrix. The middle part consists of a succession of thick bedded and massive reefal limestones (boundstone) containing an autochthonous facies. Other components include encrusting\r\ncoralline red algae and common small Nummulites, frequent rotaliids and miliolids. This part is formed by thick bedswith wavy bedding plans and is characterized by red coralline algal bindstone. It passes upward into upper part of calcareous unit composed of bedded limestone bearing larger foraminifera.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,32.4792,59.5736,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-07-20 16:41:09','2022-07-21 18:07:01'),('Hole 966F',4397,'Unknown','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'2','10 - 100 m','30.5',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals',NULL,NULL,NULL,NULL,'1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3340,NULL,'Coral reef facies near its base and lagoonal facies toward its top. The succession was deposited in an oligotrophic environment and exhibits a general shallowing-upward trend',NULL,NULL,NULL,NULL,'Cyprus','Europe',NULL,NULL,32.6833,33.8167,NULL,NULL,NULL,NULL,31.7196757598,32.2825299183,31.2010117377,33.3728561915,32.4475,33.5491,'Krause','Krause','2022-07-21 18:06:57','2022-07-21 18:07:26'),('Zhongxinzhai section',4398,'Weining','Carboniferous','Pennsylvanian','Kasimovian','Kasimovian',303.70,307.00,13,'Bashkirian - Kasimovian',302,NULL,NULL,NULL,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','45','3','101-1000 m wide',NULL,'3','More than 100 m','200',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','3','Microbes','1','Corals','61','Microbes (thrombolites) - algae - corals','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3344,NULL,'The Zhongxinzhai section (25° 30′ 33.5″ N, 106° 12′\r\n08.0″ E), s 78 m thick with a skeletal–cement–microbial reef (SCMR-3, bed 4) in the upper part.\r\nmicrobial–phylloid algal reef at the base\r\nCement-rich microbial carbonates and colonial\r\nrugose corals (Ivanovia) are the main reef builders in the lower middle part\r\nThe upper part of the reef is mainly constructed by small scale cement-rich microbial boundstone, including phylloid algae, bryozoans, calcisponges, and tube-shape algae',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.509306,106.202222,NULL,'206265',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Kiessling','2022-11-14 01:52:45','2023-01-04 15:04:29'),('Tabaïnout section TB2',4399,'Tizra','Carboniferous','Mississippian','Visean','Brigantian',331.00,336.00,12,'middle Visean - Serpukhovian',329,340,'Middle Mississippian (Early Visean, 338.8Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','100','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3345,NULL,'very thick massive microbial limestones accumulated',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,32.9,-5.8,NULL,NULL,NULL,NULL,-38.3855470246,-14.6666614345,-23.7253573021,-26.7389283513,-21.0167,-4.2806,'Krause','Krause','2023-01-04 15:04:25','2023-01-04 23:04:31'),(' Tiaouinine outcrop (Bou Guergour)',4400,'Tizra','Carboniferous','Mississippian','Serpukhovian','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','50','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3345,NULL,'thicker basal siliciclastic/bioclastic unit',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,32.65,-5.37,NULL,NULL,NULL,NULL,-32.3295612353,-10.4146442101,-24.3458525862,-22.3833899954,-16.7938,-2.08022,'Krause','Krause','2023-01-04 16:34:53','2023-01-04 23:05:22'),('Souk el Had',4401,'Tizra','Carboniferous','Mississippian','Visean','Asbian',336.00,340.00,12,'middle Visean - Serpukhovian',329,340,'Middle Mississippian (Early Visean, 338.8Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'2','Below fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','16',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3345,NULL,'Coral biostromes',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,33.17,-5.31,NULL,NULL,NULL,NULL,-42.6683996916,-17.135922042,-22.7180915211,-31.7109980916,-21.043,-3.7547,'Krause','Kiessling','2023-01-04 17:36:53','2023-03-14 15:39:39'),('Kef en N’sour section',4402,'Tizra','Carboniferous','Mississippian','Visean','Brigantian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','4','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3345,NULL,'Coral biostromes.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,32.75,-5.8,NULL,NULL,NULL,NULL,-38.4825571158,-14.8127151497,-23.8280420259,-26.8584125526,-18.0102,-3.03137,'Krause','Krause','2023-01-04 18:00:13','2023-01-04 23:06:42'),('Tizra Section',4403,'Tizra','Carboniferous','Mississippian','Visean','upper Visean',330.90,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3345,NULL,'Microbial reefs',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,33.32,-5.27,NULL,NULL,NULL,NULL,-40.2556631138,-15.1723377617,-23.3005253366,-28.4720955452,-17.8585,-2.28865,'Krause','Krause','2023-01-04 22:28:38','2023-01-04 23:07:37'),('Akerchi section',4404,'Akerchi','Carboniferous','Mississippian','Serpukhovian','upper Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','4','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3345,NULL,'Coral biostromes',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,33.32,-5.23,NULL,NULL,NULL,NULL,-31.9576235278,-9.74201975424,-23.9678188342,-21.7636223437,-17.8799,-2.26162,'Krause','Krause','2023-01-04 22:59:38','2023-03-10 13:16:52'),('Sunmayu, Stage 4,     Shandong, China',4405,'Zhushadong','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','6','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,'30',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,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,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',3347,NULL,'These reefs are inferred to have formed in a high-energy shoal setting\r\nThe calcimicrobes Kordephyton and Epiphyton and tubiform microbes are dominant at the Sunmayu section. The calcimicrobe Amgaina is locally abundant',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.624,117.997,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-10 13:16:48','2023-03-10 17:18:04'),('Jinhe, Stage 4, Shandong, China',4406,'Zhushadong','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,'30','4405',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,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',3347,NULL,'The calcimicrobes Epiphyton and Kordephyton and tubiform microbes are the main components. Tubiform microbes occur sporadically or as tangled\r\naggregations.\r\nCalcimicrobes occupy a maximum of 30%–78% of thin sections.\r\nThis reefs slightly deeper than 4405',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.078,118.173,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-10 13:24:26','2023-03-10 15:49:58'),('Yanbanzhai coral reef, Guizhou',4407,'Xiaodushan','Carboniferous','Pennsylvanian','Kasimovian','Kasimovian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','5.5','2','10 - 100 m wide',NULL,'2','10 - 100 m','50',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2','1','Constructor guild',NULL,NULL,'1','Present','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',3349,NULL,'Fomichevella framestone.\r\nlate Kasimovian base on fusulinids\r\nThe coral (Fomichevella) framestone is considered to have developed in a platform-margin slope environment.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,10,10,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-10 15:49:54','2023-03-10 17:18:04'),('Maustrenk, Lower Austria',4408,'Leitha Limestone','Neogene','Miocene','Middle Miocene','lower Sarmatian',12.50,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1','1','Less than 10 m wide','1','1','Less than 20 m','1',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','7','Bryozoans','8','Serpulids, worms, vermetids','18','Bryozoans - microbes - (algae) - (crinoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,'1','Present','1','Present','2','Medium 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',3350,NULL,'Sarmatian Bryozoan–serpulid–algal–thrombolite bioherms of up to 50 cm size.\r\nThe buildups are globular, lense-like or columnar in shape and reach more than 50 cm in height and width. Along the outcrop of approx. 20 m 8–9 individual buildups can be observed',NULL,NULL,NULL,NULL,'Austria','Europe',NULL,NULL,48.554,16.7,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-10 17:18:00','2023-03-14 15:39:39'),('Ricklow Quarry, Monyash, Derbyshire',4409,'Monsal Dale','Carboniferous','Mississippian','Visean','Brigantian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','28','3','101-1000 m wide','100','3','More than 100 m','250','20',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,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,'1','Present','2','Medium 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',3352,NULL,'The Ricklow mud mound complex originated during a period of creation of accommodation in an intraplatform middle-ramp dysphotic environment with dispersed food resources. The mud mound complex growth was interrupted by a subaerial exposure due to a relative sea-level fall.',NULL,NULL,NULL,NULL,'United Kingdom','Europe',NULL,NULL,53.192,-1.755,NULL,'229499',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-14 15:39:36','2023-03-15 13:39:41'),('Dunmore boreholes',4410,'Kilbryan Limestone','Carboniferous','Mississippian','Tournaisian','upper Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',NULL,3,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick','120','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'60',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium 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',3353,NULL,'Waulsortian limestones occupy a little more than half the thickness of the sequence in which they lie in the two Dunmore cores. There is no sure way of determining whether individual banks extend from one core to the other, but if they do then they number about 10; if not then the number could rise to about 15. Banks of both flat-lying and clinoform depositional structure are present. Their individual thickness ranges from <1m to about 10m; units up to c.20m occur but as they are of flat-lying structure they may include more than one bank. The banks probably resembled in type and dimensions those seen in natural and quarry exposures in the Loughrea area about 60km away.',NULL,NULL,NULL,NULL,'Ireland','Europe',NULL,NULL,53.62,-8.77,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-15 13:39:37','2023-03-17 15:38:45'),('Vel-ky Lipnik',4411,'unknown','Paleogene','Paleocene','Selandian-Thanetian','early Thanetian',56.00,59.20,27,'Thanetian - Ypresian',53,55,'Paleocene/Eocene Boundary (PETM, 56 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','11','2','10 - 100 m wide','40','3','More than 100 m','200','20','747',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11','1','Constructor guild','2','Intensive','1','Present','1','Low 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',3354,NULL,'The age of this reef complex is contracted\r\ninto the interval 57-58 Ma, i. e. lower part of the\r\nThanetian.\r\nCorals are the main constructors of reef framework. Their surfaces are bearing also encrustings of coralline algae and sessile foraminifers, but their volume portion on the construction of rigid reef buildups is small.\r\n\r\nPeculiarity of this locality consists from the fact that deposits of reef complex are probable in situ on the place of their origin (under the deposits of Early Eocene) and they were not transported into younger deposits as is a\r\nrule in other Paleocene reef deposits of Slovakia.',NULL,NULL,NULL,NULL,'Slovakia','Europe',NULL,NULL,49.3766,20.4967,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-17 15:38:42','2023-03-17 17:45:37'),('Usabide complex, Pyrenees',4412,'unknown','Paleogene','Paleocene','Danian','Selandian',59.20,61.60,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','6','2','10 - 100 m wide','50','3','More than 100 m','110',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',559,NULL,'Growth phase 4. Indicate as early Thanetian, but should be Selandian.\r\nBioconstructions within the Usabide and Legunbe\r\ncomplexes (growth phases 4 and 5) appear as lowrelief, tabular-shaped bodies of variable dimensions.\r\nThe former (Usd-1 and Usd-2 in Fig. 2B) are of\r\nrelatively small size, being between 5 and 7 m thick and 70 and 110 m laterally\r\n',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,42.87,-2.04,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-17 17:45:34','2023-03-17 17:51:58'),('Shouxinghu',4413,'Lazhuglung','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',NULL,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,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3355,NULL,'coral-stromatoporoid patch reefs',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,34.9499,81.4656,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2023-04-03 17:28:33',NULL),('Test1',4414,'Test1','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',NULL,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,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3356,NULL,'Test test test\r\nNochmal 4,59',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,44.55,55.44,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2023-04-03 20:31:41',NULL),('Seer Southern Reef',4418,'Burgasutay','Cambrian','Series 2','Stage 4','Botomian-Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','200','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3357,NULL,'Stage 4\r\n\r\nInteresting example of a large archaeocyathan reef lacking typical kalyptrate structures.\r\n\r\nAnother specific feature of the Seer Reef is its principal composition of solitary archaeocyaths and synsedimentory fibrous calcite cement, enveloping their cups, with subdued calcimicrobal\r\npatches. Mud fillings are restricted to the reef top and some areas of lava breccia development. Such composition indicates higher-energy conditions.',NULL,NULL,NULL,NULL,'Mongolia','Asia',NULL,NULL,48.38,92.85,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-07-10 11:50:41',NULL),('Queensland Plateau, Site 811A',4419,'unknown','Neogene','Miocene','Middle Miocene','mid-Miocene',11.60,13.80,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,1,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3358,NULL,'The Middle Miocene rimmed carbonate platform was dominated by a tropical photozoan skeletal assemblage, including green algae, corals, and large benthic foraminifera. Bryozoans occur as a minor component.\r\nDrowning due to excess heat.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-16.5162,148.1572,NULL,NULL,NULL,NULL,-22.4964479579,145.612237474,-24.3835461809,146.723123768,-25.2574,145.616,'Kiessling','Kiessling','2023-07-28 13:32:40',NULL),('Serdrar reef, Amellago',4420,'unknown','Jurassic','Lower Jurassic','Sinemurian','Sinemurian',190.80,199.30,19,'late Hettangian - early Aalenian',188,190,'Early Jurassic (Sinemurian/Pliensbachian, 190.8 Ma)',NULL,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',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3359,NULL,'A pinnacle coral reef (220 m high), located in an open marine environment on a paleo-rim of a tilted block, drowned during the lattermost Sinemurian (Oxynotumto Raricostatum Chronozones) and progressively capped by lower offshore deposits',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,32.0075,-4.9453,NULL,NULL,NULL,NULL,15.7690873969,3.01960094662,25.9836351535,5.59015314374,26.1733,-3.04318,'Krause','Krause','2023-08-29 15:19:27',NULL),('Castle olistoliths, Jebel Taabest',4421,'unknown','Jurassic','Lower Jurassic','Sinemurian','Sinemurian/Pliensbachian',182.70,199.30,19,'late Hettangian - early Aalenian',188,190,'Early Jurassic (Sinemurian/Pliensbachian, 190.8 Ma)',NULL,3,'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,NULL,'1','Corals','15','Non-rudist bivalves',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3359,NULL,'Coral bioherms',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.9414,-4.9585,NULL,NULL,NULL,NULL,17.7469863041,3.30399404096,27.2127383876,6.1436944933,26.1179,-3.08525,'Krause','Krause','2023-08-29 16:22:03',NULL),('Dades Valley 1',4422,'Choucht','Jurassic','Lower Jurassic','Pliensbachian','upper Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,185,'Early Jurassic (Pliensbachian, 186.8 Ma)',NULL,3,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','15','Non-rudist bivalves',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3359,NULL,'Coral reefs with rare lithiotid bivalves.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.5612,-5.90378,NULL,NULL,NULL,NULL,19.8502410986,3.4533117641,27.121028701,5.1082696411,26.216,-3.23716,'Krause','Krause','2023-08-31 16:02:36',NULL),('Koudiat Ech Chehem',4423,'unknown','Jurassic','Lower Jurassic','Pliensbachian','Domerian',182.70,190.80,19,'late Hettangian - early Aalenian',188,185,'Early Jurassic (Pliensbachian, 186.8 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3359,NULL,'Reef mounds. Giant complex bioherm composed of interlayered boundstones (pillarstones and mixstones) and crinoidal grainstones and packstones. Optimal reef window at the boundary between shoreface and offshore. It is a ca. 100 meter high buildup.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.8243,-6.0905,NULL,NULL,NULL,NULL,20.1567157049,3.47795822649,27.4238833551,5.167183942,26.5225,-3.26219,'Krause','Krause','2023-08-31 17:45:36',NULL),('Coral biostrome',4424,'Djenien Formation','Carboniferous','Mississippian','Serpukhovian','upper Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','10','4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','3b','Deeper slope or outer ramp','2','Below fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3360,NULL,'The biostrome contains a 10 m-thick coral biostrome in its middle unit formed by Siphonodendron, Diphyphyllum and Lithostrotion.Few brachiopods and solitary corals are found as dwellers within the biostrome. The coral biostrome records a quieter setting at the interface of middle and outer ramp settings, as seen in the co-existence of in situ coral growth, input of reworked material, deposition of carbonate mud, and sparitic textures.',NULL,NULL,NULL,NULL,'Algeria','Africa',NULL,NULL,30.99,-2.02,NULL,NULL,NULL,NULL,-36.2382119585,-6.3684716528,-27.5376027662,-21.4735000506,-20.4023,1.78604,'Siphonodendron','Siphonodendron','2023-09-22 15:37:59',NULL),('Hippuritid reef, l-Espa, Pyrenees',4426,'unknown','Cretaceous','Upper Cretaceous','Campanian','upper Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,75,'Late Cretaceous (Late Campanian, 75 Ma)',NULL,3,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick','2.5','1','Less than 10 m wide','6','2','10 - 100 m','20','1',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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','1','Constructor guild',NULL,NULL,NULL,NULL,'3','Pronounced 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',3362,NULL,'This late Campanian reef is exposed along some 20 × 6 m outcrop. Builders are mainly Hippurites radiosus, although other rudists, such as Hippuritella lapeirousei, Hippuritella sp. and Mitrocaprina sp. are also present together with corals. The orientation of 325 specimens of mainly H. radiosus was plotted in stereographic and cartesian projections. Orientations and microfacies permit to differentiate 5 vertically stacked intervals (settings) along the outcrop.\r\n\r\nVertical succession of environments depicts a complete rudist reef progradation',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,42.2207,1.687,NULL,NULL,NULL,NULL,34.7483293082,4.38828235612,36.75291409,2.87183283878,31.7906,2.79329,'Kiessling','Kiessling','2023-10-18 16:07:42',NULL),('Yadana Gas Field',4428,'Upper Burman Limestone','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','95','3','101-1000 m wide','500','4','More than 1000 m','3000','4',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'1','Present',2,'Actual reservoir',3366,NULL,'Upper Burman Limestone Formation, early Miocene in age, that is made up of one single carbonate platform, the top of which corresponds to the gas reservoir of the Yadana Field.\r\nModerate dolomitization has affected the top and flanks of the platform during the depositional hiatus.\r\nData from seismics and four wells.\r\nThe high (28%) average porosity of the reservoir is dominantly related to strong development of microporosity, moldic and vuggy porosity.\r\nSkeletal grains are dominated by non-geniculate coralline algae and large benthic foraminifers (Fig. 3A, B, C). Corals may be common in a few intervals (Fig. 3D). Non-geniculate coralline red algae are dominated by encrusting to branching forms, commonly forming nodules (rhodoliths) (Fig. 3A). The dominant genera are Lithothamnion, Mesophyllum and Sporolithon. Larger benthic foraminiferal association is characterized by Lepidocyclinids, Spiroclypeus, Cycloclypeus commonly displaying flat-shaped morphologies (Fig. 3C). Scleractinian assemblage includes robust branching or massive forms. Subordinate components include echninoderms, bryozoans, green algae and rare planktic foraminifera.',NULL,NULL,NULL,NULL,'Burma','Asia',NULL,NULL,15.123,94.783,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-06-25 14:04:02',NULL),('Gelati, Tertiary Piedmont Basin',4429,'Molare','Paleogene','Oligocene','Chattian','middle Chattian',25.00,27.50,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','10','1','Less than 10 m wide','10','2','10 - 100 m','200',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','1','Corals','2','Algae',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','20','1','Constructor guild','1','Present','1','Present','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',3367,NULL,'Brown mesophotic coral reefs in prodelta setting.\r\nlate middle Chattian according to Sr-isotope stratigraphy.\r\nCoral-bearing beds are in general alternated with clay-rich horizons and along the measured sections they display a variable overall thickness, from about 4.5 m (Cascine section) up to 10.5 m (Valletta section). Four different coral facies have been identified: branching Stylophora floatstone (BSF), Acropora-Stylophora floatstone/rudstone (ASFR), Goniopora/Caulastraea pillarstone (GCP), mixed-coral domestone (MCD); their descriptions and interpretation are reported below and summarized in Table 1.',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,44.546,8.446,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-06-25 15:48:36',NULL),('Nors Stenbrott 1, Gotland',4430,'Tufta','Silurian','Wenlock','Sheinwoodian','Sheinwoodian',430.50,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1','1','Less than 10 m wide','2','1','Less than 20 m','2',NULL,NULL,1,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8','3','Binder guild','1','Present','1','Present','2','Medium 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',3368,NULL,'Lower Sheinwoodian bryostromatolite reef in midst of positive isotope excursion.\r\nBryozoan-stromatolite reef. Some tabulate corals and stromatoproids present.\r\nCoordinates and more details provided by Claussen et al. (2022, Sedimentology):\r\nBryzoans 28-43%, porostromate (0-14%) and spongiostromate microbes (14-46%).\r\nMacroboring and microboring present. Bivalve borings',NULL,NULL,NULL,NULL,'Sweden','Europe',NULL,NULL,57.919167,18.921972,NULL,'226712',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-07-18 14:12:34',NULL),('Hallsarve, Gotland',4431,'Eke','Silurian','Ludlow','Ludfordian','Ludfordian',423.00,425.60,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1','1','Less than 10 m wide','2','1','Less than 20 m','10',NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8','3','Binder guild','1','Present','1','Present','2','Medium 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',3369,NULL,'Bryostromatolite - bryozoans and spongiostromate microbes dominant. Some tabulate corals.\r\nSurrounded by coarse-grained, poorly sorted reef debris.\r\nHigh amount of phosphatic components indicated high nutrient input.',NULL,NULL,NULL,NULL,'Sweden','Europe',NULL,NULL,57.288,18.640111,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-07-18 15:32:28',NULL);

--
-- Table structure for table `number_plot_corals`
--

CREATE TABLE `number_plot_corals` (
  `NAME` varchar(255) DEFAULT NULL,
  `R_NUMBER` int(11) NOT NULL AUTO_INCREMENT,
  `FORMATION` varchar(255) NOT NULL,
  `SYSTEM` varchar(255) DEFAULT NULL,
  `SERIES` varchar(255) DEFAULT NULL,
  `STAGE` varchar(255) DEFAULT NULL,
  `INTERVALL` varchar(255) DEFAULT NULL,
  `MIN_MA` decimal(8,2) DEFAULT NULL,
  `MAX_MA` decimal(8,2) DEFAULT NULL,
  `TIME_SLICE` double DEFAULT NULL,
  `TIME_SLICE_TEXT` varchar(255) DEFAULT NULL,
  `TIME_GPLATES` int(11) DEFAULT NULL,
  `SCOTESE_TIME` int(11) DEFAULT NULL,
  `SCOTESE_INTERVALLS` varchar(255) DEFAULT NULL,
  `TIME` double DEFAULT NULL,
  `RELIABILIT` int(11) DEFAULT NULL,
  `SUBSURFACE` varchar(60) DEFAULT NULL,
  `SUBSURFACE_TEXT` varchar(50) DEFAULT NULL,
  `TYPE` double DEFAULT NULL,
  `TYPE_TEXT` varchar(50) DEFAULT NULL,
  `THICKNESS` varchar(10) DEFAULT NULL,
  `THICKNESS_TEXT` varchar(50) DEFAULT NULL,
  `M_THICK` varchar(10) DEFAULT NULL,
  `WIDTH` varchar(10) DEFAULT NULL,
  `WIDTH_TEXT` varchar(50) DEFAULT NULL,
  `M_WIDTH` varchar(10) DEFAULT NULL,
  `EXTENSION` varchar(10) DEFAULT NULL,
  `EXTENSION_TEXT` varchar(50) DEFAULT NULL,
  `M_EXT` varchar(255) DEFAULT NULL,
  `EXT_BELT` varchar(10) DEFAULT NULL,
  `BELONGING` varchar(10) DEFAULT NULL,
  `TROPICAL` double DEFAULT NULL,
  `TROPICAL_TEXT` varchar(50) DEFAULT NULL,
  `ENVIRONMEN` varchar(255) DEFAULT NULL,
  `ENVIRONMENT_TEXT` varchar(60) DEFAULT NULL,
  `SUBENVIRON` varchar(255) DEFAULT NULL,
  `SUBENVIRONMENT_TEXT` varchar(60) DEFAULT NULL,
  `BATHYMETRY` varchar(3) DEFAULT NULL,
  `BATHYMETRY_TEXT` varchar(60) DEFAULT NULL,
  `BIOTA_MAIN` varchar(3) DEFAULT NULL,
  `BIOTA_MAIN_T` varchar(255) DEFAULT NULL,
  `BIOTA_SEC` varchar(10) DEFAULT NULL,
  `BIOTA_SEC_TEXT` varchar(50) DEFAULT NULL,
  `BIOTA_DETA` varchar(3) DEFAULT NULL,
  `BIOTA_DETA_TEXT` varchar(250) DEFAULT NULL,
  `ALG_TYPE` varchar(3) DEFAULT NULL,
  `ALG_TYPE_TEXT` varchar(50) DEFAULT NULL,
  `P_LMC` varchar(3) DEFAULT NULL,
  `P_ARAG` varchar(3) DEFAULT NULL,
  `P_HMC` varchar(3) DEFAULT NULL,
  `UPWELL` int(1) DEFAULT NULL,
  `UPWELL_TEXT` varchar(10) DEFAULT NULL,
  `CONTROL` int(1) DEFAULT NULL,
  `CONTROL_TEXT` varchar(10) DEFAULT NULL,
  `DIVERSITY` varchar(3) DEFAULT NULL,
  `DIVERSITY_TEXT` varchar(50) DEFAULT NULL,
  `M_SPEC` varchar(10) DEFAULT NULL,
  `GUILD` varchar(3) DEFAULT NULL,
  `GUILD_TEXT` varchar(50) DEFAULT NULL,
  `MACRO_BOR` varchar(3) DEFAULT NULL,
  `MACRO_BOR_TEXT` varchar(50) DEFAULT NULL,
  `MICRO_BOR` varchar(3) DEFAULT NULL,
  `MICRO_BOR_TEXT` varchar(50) DEFAULT NULL,
  `VERT_ZONAT` varchar(10) DEFAULT NULL,
  `VERT_ZONAT_TEXT` varchar(50) DEFAULT NULL,
  `HOR_ZONAT` varchar(10) DEFAULT NULL,
  `HOR_ZONAT_TEXT` varchar(50) DEFAULT NULL,
  `MICRITE` varchar(3) DEFAULT NULL,
  `MICRITE_TEXT` varchar(50) DEFAULT NULL,
  `SPARITE` varchar(3) DEFAULT NULL,
  `SPARITE_TEXT` varchar(50) DEFAULT NULL,
  `DEBRIS` varchar(5) DEFAULT NULL,
  `DEBRIS_TEXT` varchar(50) DEFAULT NULL,
  `DOLOMITE` varchar(3) DEFAULT NULL,
  `DOLOMITE_TEXT` varchar(50) DEFAULT NULL,
  `RESERVOIR` double DEFAULT NULL,
  `RESERVOIR_TEXT` varchar(50) DEFAULT NULL,
  `REF1` double DEFAULT NULL,
  `REF2` double DEFAULT NULL,
  `REMARKS` text DEFAULT NULL,
  `LAT_DEG` double DEFAULT NULL,
  `LON_DEG` double DEFAULT NULL,
  `M_LAT` double DEFAULT NULL,
  `M_LONG` double DEFAULT NULL,
  `COUNTRY` varchar(255) DEFAULT NULL,
  `CONTINENT` varchar(20) DEFAULT NULL,
  `GPLATESID` int(3) DEFAULT NULL,
  `OTHERS` varchar(255) DEFAULT NULL,
  `LATIT` double DEFAULT NULL,
  `LONGIT` double DEFAULT NULL,
  `PBDB` varchar(10) DEFAULT NULL,
  `COLLECTION` varchar(255) DEFAULT NULL,
  `PAL_LAT_old` double DEFAULT NULL,
  `PAL_LONG_old` double DEFAULT NULL,
  `PAL_LAT` double DEFAULT NULL,
  `PAL_LONG` double DEFAULT NULL,
  `PAL_LAT_M` double DEFAULT NULL,
  `PAL_LONG_M` double DEFAULT NULL,
  `PAL_LAT_SCOTESE` float DEFAULT NULL,
  `PAL_LONG_SCOTESE` float DEFAULT NULL,
  `USER` varchar(225) DEFAULT NULL,
  `USER_UPDATE` varchar(255) DEFAULT NULL,
  `DATE` datetime DEFAULT current_timestamp(),
  `DATE_UPDATE` datetime DEFAULT NULL,
  UNIQUE KEY `R_NUMBER` (`R_NUMBER`)
) ENGINE=MyISAM AUTO_INCREMENT=4439 DEFAULT CHARSET=utf8 COLLATE=utf8_general_ci;

--
-- Dumping data for table `number_plot_corals`
--

INSERT INTO `number_plot_corals` VALUES ('Mahlknecht',15,'','Triassic','Middle Triassic','Ladinian','upper Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',231,3,'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','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',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',21,0,'Stratigraphy: Upper Longobardian',46,11,1398469,2326479,'Italy','Europe',344,'',46.5,11.3667,'WAHR','67723',16.8503148294,34.8754569196,16.8503148294,34.8754569196,10.8437350139,23.0385131365,7.90845,22.1236,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monti Cadini, Dolomites',27,'Cassian','Triassic','Upper Triassic','Carnian','lower Carnian',233.00,235.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',225,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',35,68,'Some of the best examples of cryptalgal\r\npatch reefs intercalated in well\r\nbedded arenitic limestones of the uppermost\r\nCassian Formation can be studied along\r\nthe southern slope of the Cadini Mountains\r\nabout 400 m WNW of Forcella Maraia. ',46,12,1359945,2388636,'Italy','Europe',344,'',46.5833,12.25,'','170920',16.8639460607,34.0480776552,16.8639460607,34.0480776552,10.7551602754,21.1979672105,11.7788,20.8909,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lovere',34,'Camorelli','Triassic','Middle Triassic','Anisian','middle Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',243,3,'0','Outcropping reef ',2,'Reef mound','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)','2','Below fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,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',43,0,'Pelsonian to early Illyrian\nBindstones formed by Spongiostromata adn tubiphytes crusts. subordinate binding organisms are worms, prostromates and encrusting foraminifera. \nWidespread micritization.',45,10,1394911,2200168,'Italy','Europe',344,'',45.8167,10.0667,'WAHR','67717',16.0587753856,34.4963650325,16.0587753856,34.4963650325,10.4438098041,24.1996253362,6.62279,22.6089,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Summit Peak, N-Wallowa Mountains, Oregon',48,'Martin Bridge','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',214,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','180','2','10 - 100 m wide','75','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','3','Microbes','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1',NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','23','3','Binder guild','1','Present','1','Present','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',1150,63,'Early Norian. Dachstein-type reef according to G. Stanley (coral-calcareous sponge reef mound)\r\nRCM Edit May 2015: Updated with semi-quantitative data from Martindale et al 2012. This changes the patch reefs from coral-sponge reef mounds to microbial-coral or microbial-red algal true reefs. Several of the patch reefs show subtle vertical and horizontal zonation of the diminutive framework builders although due to the small size of the framework builders, this is difficult to see in outcrop. Summit Point reefs are multiple stacked patch reefs, roughly 5-60m thick with skeletal and oncoidal wackestones to floatstones (oncoids, ooids, and intraclasts or skeletal debris) between reef buildups.',45,-117,2515801,-5521820,'United States','North America',101,'76, 140, 57, 435',45.5,-117.5167,'WAHR','38063',19.961991555,-42.5630247514,20.0677295819,-42.4729557542,27.3822359732,-46.8314088831,19.7899,-53.7103,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lagazuoi',67,'Cassian','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,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',68,0,'',46,12,1366028,2371581,'Italy','Europe',344,'',46.5333,12.0333,'','',16.9223096349,34.0342509161,16.9223096349,34.0342509161,11.1429721533,21.1655266413,12.2857,20.5388,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Latemar, Dolomites',69,'Schlern','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',238,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','700',NULL,NULL,NULL,'4','More than 1000 m',NULL,'15',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','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','20','80',0,'no',1,'yes','3','25 or more reef building species','24','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation','1','Less than 30% micrite','3','More than 25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',143,72,'Was Upper Anisian-lower Ladinian.\nNow most likely upper Anisian (Zühlke et al. 2000).\nTotal buildup 700 m thick.\nEncrusting sponges and baffling red algae also present.\nSome coral colonies\n',46,11,1373706,2333328,'Italy','Europe',344,'1704, 1789',46.3833,11.5833,'WAHR','49932',15.3634363632,35.5053352777,15.3634363632,35.5053352777,10.2327155952,25.3947386738,6.47341,23.6795,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('El Capitan, Texas and McKittric, New Mexico',86,'Yates','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',262,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',1,'yes','3','25 or more reef building species','38','2','Baffler guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation','3','Pronounced zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',193,1368,'Submarine cement expecially important in reef edge and fore reef facies.\n\n34 sponge species according to ref. 1683.\nCollection data from Fagerstrom and Weidlich (1999)\n\nAbstract ref. 1368:\nThe Permian Capitan reef was a predominantly heterotrophic ecosystem strongly differentiated into open surface and cryptic communities. Unlike modern phototrophic coralgal reefs, most of the preservable epibenthos was housed within the cryptos and zonation developed only in the shallow parts of the reef. Contrary to established opinion, most sphinctozoan sponges did not grow upright to form a baffling framework but rather were pendent cryptobionts, as were nodular bryozoans and rare solitary rugose corals and crinoids. Indeed, many members of the cryptos were obligate    cryptobionts. Much of the Middle Capitan reef framework was constructed by a scaffolding of large frondose    bryozoans, with the subsidiary platy sphinctozoan Guadalupia zitteliana. Bathymetrically shallow areas of both the Middle and Upper Capitan reef, however, were characterized by platy sponges. In parts of the Upper Capitan, some platy sponges (Gigantospongia discoforma) reached up to 2 m in diameter and formed the ceilings of huge cavities which supported an extensive cryptos. In the absence of destructive forces (both biotic and physical) prevalent on modern reefs, the relatively fragile Capitan reef remained intact after the death of the constructing organisms. Rigidity was imparted to this community by a postmortem encrustation of Tubiphytes and Archaeolithoporella, together with\nmicrobial micrite. The resultant cavernous framework was partially infilled with sediment and preserved by\nsynsedimentary intergrowth of aragonitic botryoids and Archaeolithoporella. Extensive cement precipitation was\nfavoured by a number of factors including deep anoxia, which generated upwelling waters with elevated alkalinity.\nAlthough the accumulation rate of the Capitan may have been comparable to that of modern coralgal reefs, both the trophic structure and relative contributions of inorganic and organic carbonate were profoundly different. ',31,-104,484890,-3705133,'United States','North America',101,'85, 256,129,1683, 896',31.8728,-104.8583,'WAHR','24203',10.9093474899,-30.3165970674,10.9093474899,-30.3165970674,5.35392397197,-37.2500799735,4.06877,-33.4747,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pössneck',89,'Werrakarbonat','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below 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,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',1,'Potential reservoir',89,128,'Stromatolites, bryozoans, algae',50,11,2157322,2586637,'Germany','Europe',331,'2424',50.6667,11.55,'WAHR','51381',26.8972449814,30.794988017,26.9006445531,30.7954943845,23.3280656582,27.0045295409,16.0326,23.1346,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gela, Sicily',101,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,1,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,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','3','Microbes','3','Microbes',NULL,NULL,'2',NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',100,0,'',37,14,1685632,1384304,'Italy','Europe',344,'',37.0833,14.25,'','172798',NULL,NULL,NULL,NULL,9.00494714432,15.6637443531,16.5027,11.3769,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lattari Mountains',106,'','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','11','Serpulids - algae - microbes',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',105,136,'',40,14,2075278,1605105,'Italy','Europe',344,'215, 2173',40.6167,14.4667,'','172809',21.3770166342,25.3943988132,21.3770166342,25.3943988132,18.9337248588,22.5035037239,25.9701,12.1869,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Demascota well, Nova Scotia',108,'Abenaki','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','9','Tubiphytes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',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',109,456,'According to ref. 456 Stromatolite-Tubiphytes bioherms in deeper neritic enrivonment.\n',43,-60,3678610,-1482119,'Canada','North America',121,'466, 827',43.6908,-60.8317,'WAHR','67976',22.11389992,-3.286199134,22.11389992,-3.286199134,27.7900332898,-4.97501186715,33.6923,-10.0132,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Acadia, Nova Scotia',113,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian/Kimmeridgian',157.30,157.30,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100','108',0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer 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','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,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',112,827,'Thrombolite bioherms without sponges\nFew in situ corals',42,-61,3565168,-1576617,'Canada','North America',121,'',42.8622,-61.9167,'','',21.6944921525,-5.26400346877,21.6944921525,-5.26400346877,27.5176669021,-6.89594482421,33.3703,-11.86,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Swimming Woman, Big Snowy Mts., Montana',121,'Lodgepole','Carboniferous','Mississippian','Tournaisian','Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',358,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'150',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','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','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',116,273,'Bryzoans are dominant macrofossils.\nOther fossil than bryozoans relatively rare.\nCement and micrite are main constituents.\n',46,-109,-542377,-4715064,'United States','North America',101,'370',46.7667,-109.35,'','',-14.6825569324,-53.7596137367,-14.6825569324,-53.7596137367,4.38543343837,-99.2703865876,-7.30442,-43.2951,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bridger Range, Montana',122,'Lodgepole','Carboniferous','Mississippian','Tournaisian','Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',358,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'150','121',0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','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,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',116,370,'',45,-110,-520858,-4875920,'United States','North America',101,'',45.8167,-110.9333,'','',-13.9142046336,-55.0272680136,-13.9142046336,-55.0272680136,4.49812370797,-100.719234023,-7.15992,-44.7483,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cedar Creek, Williston Basin, Montana',123,'Lodgepole','Carboniferous','Mississippian','Tournaisian','Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',358,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','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,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',116,2008,'Abstract ref. 2008:\nBuildups in the Lodgepole Formation were deposited throughout the Kinderhookian to Osagean Williston Basin. The Williston Basin was tectonically active at this\ntime as the depositional axis of the basin was shifting from a northerly connection to the ocean through the Elk Point Basin in Alberta to a westerly connection through\nthe Central Montana Trough. This structural setting provided a range of depositional sites for buildups to develop on shelves, ramps, intrabasinal blocks and around\nintrashelf basins. \n     A textural, compositional and geometric range of buildups record a spectrum of depositional processes from hydrodynamically deposited grainstone shoals to\norganically mediated reefs and mud-dominated mounds. Geometries range from lens-shaped shoals and banks to mounds. Lensoidal buildups are associated with\ncoarser grainstone and packstone textures as well as other shallow water indicators such as ooids and, or, photoautotrophic corals. Mound-shaped geometries\ngenerally are dominated by muddier textures and are associated with deeper-water indicators such as filter feeding organisms with delicate skeletons. \n     A textural spectrum of buildups ranges from mud-dominated with few bryozoans and crinoids, to crinoid, bryozoan grainstones with, and without, coral\nframestones or ooids. Mud dominated buildups are best exemplified by mud mound outcrops in two locations in the Bridger Range in Montana. The coarsest\nbuildups are exemplified by coral, crinoid, bryozoan reefs at two outcrops in the Little Belt Mountains in Montana, and by crinoid, ooid grainstones in the subsurface\nof  Manitoba (Canada), and along the Cedar Creek Anticline in North Dakota and Montana. Mound complexes comprised of a broad mixture of textures from\ngrainstones and organically mediated wackestones and mudstones are known from three outcrops in the Big Snowy Mountains in Montana, and drill cores from\nSaskatchewan (Canada), and Montana and North Dakota. \n     Buildup textures, compositions and depositional styles vary according to paleodepositional location in the Lodgepole sea as a response to hydrodynamic\nvariations, trophic requirements and water qualities. The occurrence of organically mediated buildups is widely distributed: 1) on, or around, intrabasinal blocks and\nbasins, 2) on the basin floor, 3) at the base of, or across the slope/ramp, or 4) near the top of the slope/ramp. Grainstone shoals and sheet sands were deposited on\nthe Lodgepole shelf near the break in shelf slope or high on the ramp. The spectrum of buildups reflects the wide range in environmental variables and the diversity of\nsettings for buildups to develop in the Lodgepole sea. ',46,-104,-927813,-4474587,'United States','North America',101,'',46.2,-104.3667,'','',-18.1041420482,-53.11389716,-18.1041420482,-53.11389716,1.62531046362,-97.1524242219,-10.0975,-41.1996,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wilsons Brook, New Brunswick',124,'','Carboniferous','Mississippian','Visean','Visean',330.90,346.70,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,2,'Cold - water','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','15','Algae - microbes - (encrusting forams) - (rare songes)',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',117,0,'Additional serpulid worm tubes\nHydrothermal vent setting?',45,-64,-1551955,-1178575,'Canada','North America',121,'',45.8506,-64.7139,'','',-34.6655104105,-27.9043612504,-34.6655104105,-27.9043612504,-12.1813365422,-54.8760478626,-14.5831,-14.0399,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Havelock, New Brunswick',125,'','Carboniferous','Mississippian','Visean','Visean',330.90,346.70,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','1','Red algae',NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',117,1517,'',45,-65,-1521997,-1221662,'Canada','North America',121,'',45.9972,-65.3083,'','',-34.338589603,-28.259326716,-34.338589603,-28.259326716,-11.9339569788,-55.2465102378,-14.3616,-14.431,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Westerstein, Harz',131,'','Permian','Lopingian','Changhsingian','Zechstein 2',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',257,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 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','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,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',122,270,'One of the best developed Zechstein reefs.\nBryozoans especially at seperated cliffs (fore reef).',51,11,2269631,2515251,'Germany','Europe',331,'',51.6333,11.0833,'WAHR','75575',27.7814076119,30.2454758825,27.7848026129,30.2459560812,23.9834417803,26.1655946429,16.8526,22.5198,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Römerstein, Harz',132,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','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','2c','Atoll (circular structure)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',122,270,'',51,11,2271736,2526842,'Germany','Europe',331,'2424',51.6167,11.25,'WAHR','51382',27.7867504848,30.3637913448,27.7901464964,30.3642751799,24.0254169983,26.2707259232,16.8703,22.6278,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Schale',133,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'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','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',123,0,'Detailed petrographic analysis by Füchtbauer (1980).\nExtension unknown.\nComplex dolomitisation and dedolomitisation',52,7,2285621,2283775,'Germany','Europe',331,'',52.3333,7.9667,'WAHR','75574',28.0914052628,27.9598081238,28.0947779069,27.9602128389,23.5635672169,23.9808603681,16.9301,20.3863,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Abenra',134,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'300',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','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',124,0,'Bryozoans only inferred by facies similarities',55,9,2669159,2268463,'Denmark','Europe',330,'',55.05,9.4333,'','',30.9243640592,28.337500732,30.9277407686,28.3378777692,26.3293282231,23.2132726317,19.7821,20.3968,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('E-Durham, England',135,'Ford','Permian','Lopingian','Changhsingian','Zechstein 2',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',257,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,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','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','4','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',125,126,'Bryozoans, brachiopods and mollusks described.\nReef data compiled from several localities:\nHylton castle\nClaxheugh Railway Cutting\nRock Cottage\nMaiden Paps South and North\nRyhope Railway Cutting\nTunstall Hills East\nReef core facies: 24084\nReef base: 24085\nReef slope and talus: 24086',54,-1,2439445,1604252,'United Kingdom','Europe',331,'283',54.7833,-1.35,'WAHR','24084',29.6948518697,21.300076401,29.6981289407,21.3002375358,23.0549709453,17.4201657179,17.9505,14.1394,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Liebenstein',136,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20','89',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below 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,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',128,0,'',50,10,2151645,2534744,'Germany','Europe',331,'',50.7667,10.8333,'','',26.9011280423,30.2739628088,26.904523288,30.274453461,23.1684295916,26.5295784811,15.9814,22.6541,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dajiang I, Great Bank of Guizhou',157,'','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',250,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine 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','2','4','Microbial precipitation',NULL,NULL,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',144,225,'Identical to Cambrian Renalcis-Epiphyton bioherms.\n\nOccuring in pre platform carbonates (immediately above P-TR) and in the early platform stage.\n\nAbstract of ref. 1814:\nEarly Triassic framestones were discovered in the interior of an isolated, marine carbonate platform in the Nanpanjiang basin. The framestones occur in two horizons: (1) the lowermost Triassic (Griesbachian), as biostromes as much as 15 m thick, and (2) the upper part of the Lower Triassic (Smithian or Spathian) as isolated domal or inverted conical mounds as much as 1.5 m thick. The mounds and biostromes consist of a rigid calcimicrobial framework enclosing a network of internal cavities, 1 to 3 cm across, filled with peloidal-skeletal sediment. The framework is made of irregular-to-tufted masses of chambered-to-clotted micrite structures referable to Renalcis, a calcified coccoid cyanobacteria. The framework is reinforced by microbial induced micritic crusts as well as marine cement. Metazoan fossils within the framework include gastropods, bivalves, ostracodes, spirorbids, and brachiopods. The Early Triassic is widely considered to have been a global gap in reef and reef mound development. The global reef gap concept has formed the foundation of models of reef evolution and of the reorganization of reef ecosystems after the end-Permian extinction. These models should be revised to account for the existence of Early Triassic calcimicrobial mounds and biostromes discussed herein.',25,106,1752516,10294538,'China','Asia',602,'1814',25.55,106.8667,'WAHR','85070',-14.5196914142,107.12551547,-14.7553712322,106.930848233,8.79804365354,122.844153389,5.80665,98.3741,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kosmatiza, Karawanken',163,'Contrin','Triassic','Middle Triassic','Anisian','upper Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'4',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','9','Tubiphytes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'3','47','50',0,'no',0,'no','2','6 to 24 reef building species','21','3','Binder guild',NULL,NULL,'1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',148,1825,'7 Sphinctozoan species\n2 Inozoan\nPorostromata, Spongiostromata, Solenoporaceans.\n7 Microproblematica.\nTubiphytes very abundant.\nSerpulids\nReef composition: \n14 % Spongiostromata\n4 % Porostromata\n14 % Tubiphytes\n2 % Solenopraceans\n11 % sponges (8 % sphinctoz)\n3 % sessile forams\n1 % bryozoans\n1 % serpulids\n< 1 % corals',46,14,1241650,2507917,'Austria','Europe',301,'',46.45,14.2,'','',13.7914819896,36.4222662095,13.7914819896,36.4222662095,8.72920267986,26.9276651084,5.4313,25.1614,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Moliterno, S-Apennin',175,'Mt. Facito','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','100',NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','2','Algae','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',159,1478,'Lenticular massive buildups 80-100 m thick.\nBoundstone predominantly of encrusting organisms (cyanobacteria, foraminifers), green algae and calcisponges.\nRare corals.\nClassified as spar-cemented organically bound skeletal debris reef.',40,15,437744,2260345,'Italy','Europe',344,'',40.2333,15.8667,'','',10.8781683095,30.9830728573,10.8781683095,30.9830728573,5.03456732837,20.5764490522,0.882946,21.3633,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cerchiara, Brienza, S-Apennin',176,'Mt. Facito','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20','175',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1478,159,'See reef 175 for remarks.',40,15,478803,2259298,'Italy','Europe',344,'',40.4833,15.65,'WAHR','20659',11.1506777182,31.1099311997,11.1506777182,31.1099311997,5.33213722405,20.5413899419,1.18249,21.357,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('N-Calabria, microbe-serpulid reefs',179,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',209,2,'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','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','11','Serpulids - algae - microbes',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',162,2173,'Only small reefal clasts are reported\n\nSerpulid shells surrounded by microbial crusts. Locally corals, calcisponges, solenoporanceans and problematica are present (collection data).\n\nAbstract of ref. 2173:\nMicrobial-serpulid communities are the main reef-builders of most Norian-Rhaetian carbonate platforms of Italy. They represent minor, yet significant communities in the shallow western Tethys, in contrast with the highly diversified sponge- and coral-dominated Dachstein reefs widespread from Eastern Alps to Australia. The microbial-serpulid build-ups are systematically associated with narrow intraplatform troughs and developed on the outer margin-upper slope area under marine conditions unsuitable for the development of coralgal reefs. The development of these settings can be related to transtensional tectonics affecting an elongate belt which was roughly parallel to the Piedmont-Ligurian Ocean spreading axis during the Jurassic. Dysoxic and mesosaline waters are the main cause of the success of the Norian microbial-serpulid build-ups. Whereas, from the late Norian to the Rhaetian, eutrophication and climate change control their distribution. These environments acted during Norian-Rhaetian times as refuges, where opportunitistic organisms could survive and build frameworks during a period otherwise dominated by coralgal reefs.',39,15,1917203,1668921,'Italy','Europe',344,'2599',39.9167,15.8667,'WAHR','38046',14.0304925974,26.9652947726,13.8657057323,27.0324041417,12.2030780063,20.4606148257,18.245,14.0673,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Peace River, Alberta',181,'Pekisko','Carboniferous','Mississippian','Tournaisian','middle Tournasian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',352,3,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick','100','2','10 - 100 m wide','200','3','More than 100 m','400','40',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below 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',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',168,0,'Middle Tournasian (TN2)\nWaulsortian bioherm\nBryzoans are dominant macrofossils.\nCrinoids in apron sediments',56,-117,814946,-4261420,'Canada','North America',121,'',56.25,-117.3,'','',-7.38714307932,-45.8059441025,-7.38714307932,-45.8059441025,14.3781582538,-95.4435392967,4.56922,-38.8486,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grigna',205,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,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','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',190,0,'',45,9,1443468,2163490,'Italy','Europe',344,'',45.9167,9.4,'','',17.7879026974,33.6749690666,17.7879026974,33.6749690666,11.2245307511,21.5806574376,8.235,20.6649,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ufa River, Urals',217,'','Permian','Cisuralian','Kungurian','Kungurian',272.30,283.50,15,'Sakmarian - Kungurian',277,280,'Early Permian (early Kungurian, 280 Ma)',273,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','8',NULL,NULL,NULL,'1','Less than 20 m','12','120',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','3','3','Binder guild',NULL,NULL,NULL,NULL,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',200,326,'Two types:\n1. Stromatolitic 3-5 m vertically, 12 m laterally\n2. mounds (1-1.5 x 2-3 m) with problematic fossil: Sylvaella tubularis.',55,56,4131636,4898515,'Russia','Asia',624,'',55.4167,56.7333,'','',26.6292384494,44.8507383454,26.6292384494,44.8507383454,37.0567515193,34.7724541839,28.437,47.0751,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zhilyanka, Aktyubinsk',218,'','Permian','Cisuralian','Kungurian','Kungurian',272.30,283.50,15,'Sakmarian - Kungurian',277,280,'Early Permian (early Kungurian, 280 Ma)',273,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'3',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,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',201,0,'Cited in Chuvashov (1983).',50,57,3655686,5437578,'Kazakhstan','Asia',301,'',50.2667,57.2167,'','',23.2000414017,49.100667781,23.2000414017,49.100667781,35.1085357039,40.6839800291,24.8647,51.2399,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bolshetirsky, Siberia',232,'','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',525,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','100',NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below 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,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',214,0,'Thickness 80-110 m.\nArchaeocyathids, Microphytolites, Epiphyton, Renalcis and Marcovella as main reef builders.',59,108,-2602264,851772,'Russia','Asia',624,'',59.3333,108.4167,'WAHR','80846',0.642730507789,-66.1614567052,0.642730507789,-66.1614567052,0.642730507789,-66.1614567052,-12.8638,-5.39648,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Srednebotuobinsky, Siberia',233,'','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',525,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','45',NULL,NULL,NULL,'3','More than 100 m',NULL,'45',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,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',214,1405,'Gas field\nLess diverse than 232.\n40-45 m thickness. \nMicrophytolites, Epiphyton, Renalcis as main reef builders.\nNepa-Botuoba anteclise.',61,112,-2712908,505834,'Russia','Asia',624,'',61.6667,112.6667,'WAHR','80847',-0.108127891654,-69.2033827769,-0.108127891654,-69.2033827769,-0.108127891654,-69.2033827769,-14.6444,-8.05076,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dulisminsky, Siberia',234,'','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',525,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,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','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,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',214,0,'Marcovella dominant. Other reef builders are Microphytolites and  Renalcis',58,109,-2430655,911425,'Russia','Asia',624,'',58,109,'WAHR','80848',1.9011070649,-65.6263885143,1.9011070649,-65.6263885143,1.9011070649,-65.6263885143,-11.4973,-5.34925,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Valdeteja II',237,'Valdeteja','Carboniferous','Mississippian','Serpukhovian','Serpukhovian/Bashkirian',315.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',318,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,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)','2','Below fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',217,0,'Zoned with cyanophycean-bindstone at the base and masses of almost monospecific corals at the top.',42,-5,-625791,1249802,'Spain','Europe',304,'',42.9167,-5.3667,'WAHR','76871',-22.0230630218,2.97967535653,-22.0230630218,2.97967535653,-17.3380341315,-15.7569847419,-10.818,7.67584,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Djebel Tebaga II',249,'','Permian',NULL,NULL,'Kazanian/Tartarian',268.80,272.30,15,'Sakmarian - Kungurian',277,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','60','100',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','9','Tubiphytes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','30','70',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',229,278,'East-west trending reef belt\nMainly composed of Archaeolithoporella and Tubiphytes.\nAbstract of ref. 1327:\nTubiphytes and Archaeolithoporella are two important building calcareous algae in Permian reefs, especially in the Upper Murghabian of Jebel Tebaga (Tunisia). Systematics of the two algae (probably blue-green) is reviewed.\nTubiphytes and Archaeolithoporella were previously poorly known in the Upper Permian beds from Jebel Tebaga. These algae, always associated, take a prominent part in the building of the reefs. The analysis of the reefs, 20 m thick and 60 m wide, shows the following biological sequence: a) Prereefal first stage: settling of clay-marly sediments including several calcareous organisms, mainly Calcisponges and Bivalves. b) Second stage: Whole organisms or\nremains are encrusted by a first generation of the stromatolitic algae Archaeolithoporella, which will be colonized in a second time by the blue-green algae Tubiphytes. The former, rapidly attached, show a growth which follow the exact shape of the anfractuosites of Archaeolithoporella laminae. Open spaces and cavities created by the growth of alga assemblages are progressively filled by an internal micritic sediment with pellets. This open space filling by a fine material suggests a growth of Tubiphytes in restricted conditions, where the luminosity is lessen, indicating a sciaphilous alga. c) Third stage: Attachment and proliferation of a second generation of dense Archaeolithoporella.\n    They encrust Tubiphytes and other substrates, growing laterally and vertically. The crusts of Archaeolithoporella are parallel to the substrate at the beginning of the growth, but a few millimeters higher appears a mammillated crust, which gives, at the end of the growth, some nodules with concentric laminations, often trapped in interstitial micritic fills.\n These nodules are called here tebagites. This biologic sequence occurs repeatly from the bottom to the top of the reef. Furthermore, examination of relations between the growth of Archaeolithoporella and the early diagenetic features (cements) allows to establish, in addition to the biologic sequence, a diagenetic sequence summarized as following: -\n    growth of dense micritic laminae. - Growth of clear and dark laminae (i.e. typical stage). - Growth of vesicular laminae filled by fibrous or botryoidal cement. - Stop of algae growth, followed by a filling of the interalgal porosity with a botryoidal cement or an internal peloidal sediment. In conclusion, Tubiphytes and Archaeolithoporella constitute the main building organisms of the studied reefs. Identical assemblages are known from the Lower Permian of Carnic Alps,\nfrom Upper Permian of Yugoslavia and Capitan Reef in U.S.A. as well, under the name of Calcisponges/Algal/Cements\n    Reefs (-CAC, new abbreviation). ',33,10,-632930,2062202,'Tunisia','Africa',715,'1327, 1376',33.4167,10.25,'','',-7.35835444208,18.9171955158,-7.35835444208,18.9171955158,-5.98258901575,11.7281148863,-7.5808,18.5902,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Minamidai, Akiyoshi-dai',258,'','Carboniferous','Mississippian','Serpukhovian','Serpukhovian-Bashkirian',315.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',318,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','35','Chaetetids - corals - cyanoyphyceans - algae - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present',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',238,239,'Millerella yowarensis zone to Pseudostaffella antiqua zone\nUpper Serpukhovian to middle Bashkirian.\nMicrobes/algae always dominating over chaetetids. Maximum chaetetid cover is 27%. Microbes 50-72%, corals max. 8%.\nStratigraphic range of chaetetids from Nagatophyllym satoi Zone (upper Visean) to the Beedina akizoshiensis Zone (upper Moscovian).',34,131,77658,14604452,'Japan','Asia',625,'295, 362, 2166',34.2,131.1667,'WAHR','76321',14.7163449564,127.012310018,14.7163449564,127.012310018,4.64387098066,67.4422367629,4.67475,87.5865,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ryugoho, Akiyoshi-dai',259,'','Carboniferous','Mississippian','Serpukhovian','Serpukhovian-Bashkirian',315.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',318,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,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','3','Microbes','1','Corals','35','Chaetetids - corals - cyanoyphyceans - algae - (bryozoans)',NULL,NULL,'40','40','20',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present',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',240,362,'Reef development from Millerella yowarensis zone (Serpukhovian-early Bashkirian) to Profusulinella beppensis zone (latest Bashkirian).\nStromatolites and tabulate corals as main reef builders.',34,131,1539769,12084787,'Japan','Asia',625,'',34.2167,131.2,'','',14.7297085567,127.042608495,14.7297085567,127.042608495,4.63576919544,67.473510561,4.6873,87.6162,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lake Cumberland, Kentucky',274,'Fort Payne','Carboniferous','Mississippian','Visean','upper Osagean',342.00,346.70,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',343,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15',NULL,NULL,NULL,'4','More than 1000 m','1500','15',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'40','0','60',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',254,368,'Crinoids are dominant macrofossils.\nMaximum thickness 15 m, lateral extension 1500 m at Owens Branch.\nSurrounded by siliciclastic sediments (abandoned delta slope).\nBioherm lithology described as bryozoan-coral-crinoidal wackestone.',36,-85,-3071992,-3569787,'United States','North America',101,'1714, 2410',36.95,-85.0167,'WAHR','76446',-35.1573255396,-54.6572305019,-35.1573255396,-54.6572305019,-14.1252480804,-90.4113447311,-25.8457,-34.1423,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zeitz',288,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 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','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','20','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',1,'Potential reservoir',128,0,'Known only from wells',51,12,2221961,2608929,'Germany','Europe',331,'',51.05,12.1333,'','',27.3500025081,31.1077742143,27.3534045418,31.1082855938,23.8499011217,27.1146039511,16.5155,23.3659,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Heeseberg',304,'','Triassic','Lower Triassic','Induan','Scythian',247.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',249,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',280,0,'Stromatolitic domes only.',52,10,2854584,1695627,'Germany','Europe',331,'',52.0972,10.8833,'','',7.76669674761,20.9566960426,30.0373060766,29.8484850971,24.5408636271,25.7433748756,17.6594,20.7028,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alytus',305,'','Permian','Lopingian','Changhsingian','Zechstein',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','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',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',1,'Potential reservoir',282,0,'Main reference is fig. 5B of ref. 282.',54,24,3000130,3162809,'Lithuania','Europe',301,'',54.4,24.05,'','',32.4883164283,38.1029199598,32.4917469307,38.1036444834,30.8478232307,31.3515261578,22.4217,29.0038,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jonava, Pashulyai',306,'','Permian','Lopingian','Changhsingian','Zechstein',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','70',NULL,NULL,NULL,'4','More than 1000 m',NULL,'500',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','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',282,1413,'70 m thickness.\n470-520 km long reef belt.\nGood porosity.\n\nLower Kazanian - Nauyaakmyanian suite = Werrakalk.',55,24,3092265,3141412,'Lithuania','Europe',301,'',55.0667,24.4167,'','',33.1877282868,38.0890264596,33.1911587833,38.0897500226,31.4904047427,31.0284796127,23.1115,28.8783,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Silale',307,'','Permian','Lopingian','Changhsingian','Zechstein',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','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',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',282,0,'Main reference is fig. 5B of ref. 282.',55,22,3071806,2986771,'Lithuania','Europe',301,'',55.5167,22.1333,'','',33.2081171469,36.445086889,33.2115455166,36.4457460198,30.9864161229,29.5312698669,22.9301,27.3965,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hackberry Draw and Chinaberry Draw, Capitan, Texas',316,'Capitan','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',262,2,'0','Outcropping reef ',1,'True reef','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)','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','90','10',0,'no',1,'yes','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1533,293,'Abstract ref. 1533:\nThe Permian Capitan reef of the Guadalupe Mountains was\n  bound, lithified, and preserved by microbially precipitated micrite. A microbial origin or association is based on the distribution, texture, fossil content, and order of microstratigraphic succession. In samples from the\n  middle Capitan Formation, micrite layers (about 1 cm thick) encrusted the top, sides, and undersides of in situ organisms and also piled above organisms in thick (0.5 to > 3 cm) accumulations, with high angles of repose (up to 90°). Primary encrustations commonly consist of thin, homogeneous, subparallel layers of Archaeolithoporella---interpreted to be\n  a red alga that probably lived in dimly lit cavities. Secondary encrustations (0.5--30 mm thick) contain 10--50 µm diameter peloids and fossil cyanophytes, and are usually bound by thin layers of micrite. Secondary encrustations of gravity-defying peloidal micrites are interpreted as having precipitated within mucilaginous microbial aggregations, probably in dark\n  cavities. The secondary microbial micrites were followed by\n  cavity-filling, aragonitic botryoids. Thin (< 1 mm) layers of clotted micrite were deposited on the first botryoids, probably by microbial biofilms. \n\n  In contrast to samples from the middle Capitan Formation, samples from the upper Capitan Formation taken near the transition from reef to outer shelf are composed of smaller (1--2 mm) framework organisms and are bound by layers of thinner (< 1 mm) primary encrustations. In the upper Capitan Formation samples, dense, clotted micrite forms secondary encrustations (£ 1 mm thick), commonly underneath primary framework.\n  Secondary encrustations are succeeded by more abundant tertiary encrustations (1--4 mm thick) of sparse, clotted micrite with vague dendritic structures. The secondary and tertiary encrustations are interpreted as microbial. The samples from the upper Capitan Formation were deposited in the shallowest part of the reef (< 1 to 10 m deep), and most of the samples from the middle Capitan were deposited in deep water  (10--140 m). The difference in the encrustations and in the overall scale of  the two fabrics is probably related to differences in environmental energy   during deposition.',32,-104,486740,-3748525,'United States','North America',101,'292',32.1667,-104.4333,'WAHR','47714',11.011256408,-29.8544737944,11.011256408,-29.8544737944,5.45785477956,-36.7948202879,4.43781,-32.8287,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Boone County I, Missouri',320,'Burlington Limestone','Carboniferous','Mississippian','Visean','Osagean (Tn3)',342.00,346.70,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',346,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m','100','30',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','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'30','0','70',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',299,369,'Waulsortian mound.\nCrinoids are dominant macrofossils.',39,-92,-2409300,-4123597,'United States','North America',101,'',39,-92.8333,'','',-28.8210750733,-56.3209758917,-28.8210750733,-56.3209758917,-9.22850875212,-94.7640081562,-20.9696,-38.8137,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hasanoglan',331,'','Triassic','Middle Triassic','Anisian','upper Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,3,'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','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,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',305,0,'Mounds\' termed algal bindstone.',40,33,2400680,4601281,'Turkey','Asia',522,'',40.025,33.1917,'WAHR','73816',28.0161307726,49.1910879389,28.0161307726,49.1910879389,18.3327635115,43.4919560336,18.8349,37.7005,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Waulsort',360,'','Carboniferous','Mississippian','Tournaisian','upper Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',347,3,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below 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,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',325,1177,'Bryozoans are dominant macrofossils.\nFilaments of cyanophyceans indicate microbial activity.\nType section of Waulsortian mounds\n\nAbstract of ref. 2157:\nThe biostratigraphy and sedimentology of the late Tournaisian, Waulsortian buildups of the type area, at Waulsort (Belgium), are examined in detail. Four buildups are present. Overall, they span the stratigraphic interval from the  base of the Ivorian stage to the lower part of the Moliniacian stage, ending just below the base of the Viséan.\n\nPetrographic study shows that all Waulsortian Phases are represented, the older buildups being of Phases A and B, whereas the youngest ranges through Phases A to D. The relatively crude Phase classification is refined by correspondence analysis, which shows that the grain types present in the Waulsortian and associated limestones conform closely to the relay (systematic shift of relative importance of grain types) described from other Waulsortian buildups in Belgium.\n A Relay Index, derived from the correspondence analysis and defining the position of each sample in the compositional relay, is plotted on stratigraphic logs of the sections studied to allow detailed comparison with other Waulsortian and peri-Waulsortian sections in the Dinant area for which similar curves already exist. The Waulsort buildups are found to fit closely into the depositional and palaeobathymetric patterns established or suspected in the area. Two shallowing upward sequences seem to be present, separated by an abrupt deepening. The earlier, relatively minor shallowing trend, in the Polygnathus communis carina Zone, is here recorded in buildup facies\n for the first time: previous evidence had come from the laterally equivalent facies. The other shallowing trend, which extends through the Scaliognathus anchoralis Zone and culminates near the base of the Moliniacian stage, is the regional, late Tournaisian regression which had a major influence on the biota of the Waulsortian banks in Belgium and was probably largely responsible for cessation of bank growth over most of the area.',50,4,-1648466,518859,'Belgium','Europe',331,'2157, 2568',50.1667,4.8667,'WAHR','76920',-37.8987188186,-6.86756514279,-37.8987188186,-6.86756514279,-2.04546711671,-48.6383746488,-13.9205,4.50167,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cannington Park, Great Britain',361,'','Carboniferous','Mississippian','Tournaisian','Ivorian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',347,3,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','1','Corals','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',325,372,'Well data only.\nSome small corals are also mentioned',51,-3,-1710483,-53706,'United Kingdom','Europe',331,'',51.15,-3.0667,'','',-37.29276182,-13.2877574447,-37.29276182,-13.2877574447,-3.71160523786,-53.4879536157,-14.6267,-0.733016,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Linney Head, Wales, Great Britain',362,'','Carboniferous','Mississippian','Tournaisian','Ivorian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',347,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,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','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',325,0,'Poor data owing to complete dolomitization.',51,-5,-1680234,-201838,'United Kingdom','Europe',331,'',51.6333,-5.0667,'','',-36.7658879971,-14.828716532,-36.7658879971,-14.828716532,-3.82434744978,-54.824330762,-14.4666,-2.10565,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Podolsk',371,'Akatievo','Carboniferous','Pennsylvanian','Moscovian','upper Moscovian',311.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',308,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','15','Algae - microbes - (encrusting forams) - (rare songes)',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',326,2357,'Ivonovia boundstone lenses, up to 2.5 m thick with dens micritic to micropeloidal masses of supposed microbial origin. Some chaetetids.',55,37,1991939,3459038,'Russia','Asia',624,'',55.3833,37.5333,'WAHR','63384',10.7601830518,27.8700671152,8.83668214222,26.5015570397,13.2760562121,7.53475277127,11.6677,29.1005,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chusovoy, Urals',373,'','Permian','Cisuralian','Kungurian','upper Kungurian',272.30,283.50,15,'Sakmarian - Kungurian',277,280,'Early Permian (early Kungurian, 280 Ma)',272,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'120','217',0,'Tropical or unknown','0',NULL,'','Unknown','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,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',326,0,'',58,57,4454533,4634400,'Russia','Asia',624,'',58.3,57.8333,'','',29.0438988543,42.9434025347,29.0438988543,42.9434025347,38.7143183371,31.6873578383,30.9123,45.2378,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Muleshoe, Sacramento Mts., New Mexico',381,'','Carboniferous','Mississippian','Tournaisian','Ivorian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',346,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'80','0','20',0,'no',1,'yes','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',330,373,'Cement up to 90 % of rock volume.\nBryzoans are dominant macrofossils. Crinoids dominant at base.\nOther mounds in the area:\nLittle Sugarloaf mound\nSan Andres NW mound.\nStratigraphy updated from Lees and Miller (1995)',32,-105,-2123480,-5521475,'United States','North America',101,'579, 1023, 1024',32.8,-105.9167,'WAHR','76459',-21.2779879344,-67.0049440414,-21.2779879344,-67.0049440414,-7.52522701304,-107.037089283,-18.9442,-51.6819,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Klaeng',392,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'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','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',335,0,'Algal boundstones were mentioned but most probably cyanophyceans dominate.',13,101,-91472,10031304,'Thailand','Asia',604,'',13,101.5,'WAHR','67684',-19.5323478095,104.008384207,-19.5323478095,104.008384207,17.0317924523,107.979042773,3.83322,96.442,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Podzamcze+Smolen, Zegarowe',425,'Zegarowe','Jurassic','Upper Jurassic','Oxfordian','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',156,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,'110','423',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','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','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',365,2464,'',50,19,5291437,1781537,'Poland','Europe',301,'',50.4333,19.6167,'WAHR','60852',31.8867956748,32.3814424283,31.8867956748,32.3814424283,37.9390989743,34.2750157043,42.2333,26.4423,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Craven, Lancashire, Great Britain',427,'','Carboniferous','Mississippian','Visean','Chadian',345.00,346.70,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',344,3,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'70','0','30',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,'1','Present',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',366,611,'Chadian age, younger than typical Waulsortian mounds. Below lower Visean unconformity.\nReef knolls.\nBryzoans are dominant macrofossils.\nFenestella, crinoids and stromatactis are common.\nGrivanella and sponges locally abundant.\n\nIncluding Crow Hill, Worsaw, Gerna, Sykes and\nTwiston localities of ref. 2567',53,-2,-1333032,-77849,'United Kingdom','Europe',331,'1315, 2567',53.9,-2.4,'','',-30.0165582312,-8.6455009638,-33.1081934727,-11.1523198967,-2.08056895516,-45.4905507542,-8.78585,-0.504839,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Stebden Hill, Cracoe, Great Britain',428,'','Carboniferous','Mississippian','Visean','Asbian',336.00,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',334,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150',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','7','Bryozoans','36','Bryozoans - sponges - microbes',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','13','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',399,366,'Stebden Hill is type locality for Cracoen type reefs (data in Paleobiology Database)\nFramework composed of microbes, bryozoans, lithistid sponges and solitary rugose corals.',54,-2,-381419,474305,'United Kingdom','Europe',331,'367, 611',54.05,-2.0167,'WAHR','28383',-29.8681846509,-8.38410531365,-29.084899116,-7.90845444616,-3.57979004609,-34.4296199027,-5.725,1.28999,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Halton, Carnforth, Great Britain',429,'','Carboniferous','Mississippian','Visean','upper Asbian',336.00,338.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',333,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'150','428',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','36','Bryozoans - sponges - microbes',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',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',1321,399,'Cracoen type reef.\nFramework composed of microbes, bryozoans, lithistid sponges and bryozoans.',54,-2,-384340,422932,'United Kingdom','Europe',331,'367, 1321',54.1,-2.8,'WAHR','76085',-29.81304818,-8.91325625411,-28.0563670387,-7.84439924439,-3.77147602431,-33.325729817,-5.4549,1.12337,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Isle of Man, Great Britain',430,'','Carboniferous','Mississippian','Visean','Asbian',336.00,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',334,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'150','428',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','36','Bryozoans - sponges - microbes',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',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',399,488,'Cracoen type reefs.',54,-4,-407622,297057,'United Kingdom','Europe',331,'',54.0833,-4.75,'','',-29.7856955419,-10.2309094478,-29.0150299694,-9.74186346219,-4.17939994661,-35.9210422277,-5.93196,-0.309138,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Caldon Low, Derbyshire, Great Britain',431,'','Carboniferous','Mississippian','Visean','Chadian',345.00,346.70,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',344,3,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below 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,'4','Microbial precipitation',NULL,NULL,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',366,1713,'Including Dovedale complex.\nFenestrate bryozoan-sponge spicule buildup. Crinoids restricted to flanks.\nLower ramp setting.',53,-1,-1433041,-19644,'United Kingdom','Europe',331,'1715',53.0667,-1.8333,'','',-30.8516478745,-8.25957790134,-33.9463318846,-10.7624645345,-2.69549924077,-44.8342701313,-9.53013,0.00579706,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cork',434,'','Carboniferous','Mississippian','Tournaisian','Tournaisian/Visean',330.90,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',345,2,'0','Outcropping reef ',3,'Mud mound or bank','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','437',0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below 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','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',371,372,'Waulsortian in Ireland genarally thicker than in type locality.\nBryzoans are dominant macrofossils.',51,-8,-1689711,-439592,'Ireland','Europe',331,'',51.9,-8.4667,'','',-34.5867039079,-15.5221788315,-34.5867039079,-15.5221788315,-5.54305905021,-46.8665699132,-10.8893,-3.77646,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kenmare',435,'','Carboniferous','Mississippian','Tournaisian','Tournaisian/Visean',330.90,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',345,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','437',0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below 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','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',371,372,'',51,-9,-1703414,-515991,'Ireland','Europe',331,'',51.8833,-9.5833,'','',-34.4904752967,-16.350782905,-34.4904752967,-16.350782905,-5.78245255871,-47.5161406725,-13.4158,-4.83848,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-03-17 11:58:58'),('Rathkeale, Shannon Estuary',436,'','Carboniferous','Mississippian','Tournaisian','Tournaisian/Visean',330.90,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',345,2,'0','Outcropping reef ',3,'Mud mound or bank','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','437',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below 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','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',1323,372,'Thickest development of all Waulsortian mounds worldwide.',52,-8,-1611462,-480813,'Ireland','Europe',331,'371',52.5167,-8.9333,'WAHR','76915',-33.9331690837,-15.7467567935,-33.9331690837,-15.7467567935,-5.05468531279,-47.3414221904,-10.3038,-4.12779,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Feltrim Hill, Dublin',437,'','Carboniferous','Mississippian','Tournaisian','Courceyan',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',346,3,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','400',NULL,NULL,NULL,'4','More than 1000 m',NULL,'300',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'80','0','20',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',371,372,'400 m thick Waulsortian facies.\nOutcropping and subsurface.\nOriginal dating Courceyan/Chadian.\nNew data suggest late Courceyan (Tournaisian)',53,-6,-1450541,-335224,'Ireland','Europe',331,'1322',53.5,-6.5,'WAHR','76497',-34.841806897,-15.73578974,-34.841806897,-15.73578974,-2.48875520496,-56.3949783125,-12.8354,-3.40016,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Keel',438,'','Carboniferous','Mississippian','Tournaisian','Tournaisian/Visean',330.90,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',345,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,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','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'90','0','10',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',372,371,'Northern limit of Waulsortian facies in Ireland.',53,-7,-1442691,-429200,'Ireland','Europe',331,'',53.6833,-7.8833,'','',-32.8733005279,-14.7921813301,-32.8733005279,-14.7921813301,-3.74487822436,-47.1341107962,-9.07861,-3.61337,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('San Andres Mts, New Mexico',439,'Lake Valley','Carboniferous','Mississippian','Tournaisian','Ivorian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',347,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50','440',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','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,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',373,1632,'Stratigraphy updated from Lees and Miller (1995)',33,-106,-2043375,-5564214,'United States','North America',101,'',33,-106.6667,'','',-20.6176720693,-66.9804975816,-20.6176720693,-66.9804975816,-6.94872487326,-107.362457505,-18.3524,-51.9919,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Teepee Mound, Sacramento Mts., New Mexico',440,'Lake Valley','Carboniferous','Mississippian','Tournaisian','Ivorian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',347,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 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','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',1,'yes','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,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',374,375,'Other mound in Deadman Branch.\nStratigraphy updated from Lees and Miller (1995)',32,-105,-2118543,-5515591,'United States','North America',101,'1023, 1024, 1352',32.8667,-105.9,'','',-21.2732616345,-66.9319748889,-21.2732616345,-66.9319748889,-7.48592202721,-106.980922232,-18.9077,-51.621,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grapevine Canyon, New Mexico',441,'Lake Valley','Carboniferous','Mississippian','Tournaisian','Ivorian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',347,3,'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','3','Ramp or Slope','3b','Deeper slope or outer ramp','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,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',374,375,'Stratigraphy updated from Lees and Miller (1995)',32,-105,-2139923,-5524469,'United States','North America',101,'1023, 1352',32.6833,-105.85,'','',-21.3638102932,-67.1090258296,-21.3638102932,-67.1090258296,-7.64890733696,-107.075762732,-19.0658,-51.7288,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bishop Cap Hills, Las Cruces, New Mexico',442,'Lake Valley','Carboniferous','Mississippian','Tournaisian','Ivorian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',347,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'2',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','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,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',376,0,'Sponges, Ostracodes and some corals also present.\nNo algae.\nStratigraphy updated from Lees and Miller (1995)',32,-106,-2120356,-5610522,'United States','North America',101,'',32.25,-106.5833,'','',-20.8836921752,-67.7341326928,-20.8836921752,-67.7341326928,-7.54218593146,-107.830131161,-18.9213,-52.5129,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bokan',443,'','Carboniferous','Mississippian','Tournaisian','Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',354,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50','444',1,'Temperate','3','Ramp or Slope','3b','Deeper slope or outer ramp','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','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',377,0,'Bryozoans are dominant macrofossils.',33,67,-5503331,7043462,'Afghanistan','Asia',301,'',33.9167,67.9167,'','',-56.7717456161,94.3276546237,-56.7717456161,94.3276546237,-48.5429665834,62.1286822293,-32.0281,83.8777,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Spina Kada',444,'','Carboniferous','Mississippian','Tournaisian','Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',354,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,1,'Temperate','3','Ramp or Slope','3b','Deeper slope or outer ramp','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','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',377,378,'Bryozoans are dominant macrofossils.\nPosition doubtful',33,66,-5490590,6927980,'Afghanistan','Asia',301,'',33.5,66.8333,'','',-57.4126646801,92.9317134533,-57.4126646801,92.9317134533,-48.5137435439,60.6300029188,-31.8365,82.7297,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Band-e Bayan',445,'','Carboniferous','Mississippian','Tournaisian','Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',354,2,'0','Outcropping reef ',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','3','Ramp or Slope','','Unknown','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','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',377,0,'Village Iraq.\nPosition unclear.',34,65,-5312270,6932723,'Afghanistan','Asia',301,'',34.3333,65.1667,'','',-56.9076508655,90.1034018405,-56.9076508655,90.1034018405,-47.1246324402,59.4041169681,-27.8894,80.4695,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Northern Poland',446,'','Carboniferous','Mississippian','Tournaisian','Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',354,2,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','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',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',372,0,'Debris from breccia encountered in borehole.\nBryzoans are dominant macrofossils.\nM. Paszkowski cited in ref. 372.\nPosition unclear.',53,19,-779692,1271893,'Poland','Europe',301,'',53,19,'','',-32.5642005433,2.33525091984,-32.5642005433,2.33525091984,5.63711338649,-43.5527145915,-7.22006,10.9335,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alexander Island, Antarctica',447,'','Jurassic','Upper Jurassic','Tithonian','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',147,2,'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,2,'Cold - water','4','Basin','4b','Deep basin (> 200 m)','2','Below fair weather wave base','3','Microbes','15','Non-rudist bivalves','40','Microbes - mollusks',NULL,NULL,'20','80','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation','1','Present','1','Present',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',379,0,'Methane-seep limestone with gastropodes, bivalves and microbial crusts.\r\nNot a reef',-71,-68,-8625664,-2029790,'Antarctica','Antarctica',803,'',-71.6167,-68.7,'',NULL,-72.6434482438,-33.9157219231,-72.6434482438,-33.9157219231,-62.7297585072,-32.632379031,-61.7996,-26.1865,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grenora, North Dakota',467,'Ratcliffe','Carboniferous','Mississippian','Visean','Meramecian',336.00,345.00,11,'late Famennian - early Visean',351,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',337,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'15',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','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,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',395,0,'Productive reservoir in 1966',48,-103,370847,-3698219,'United States','North America',101,'',48.6333,-103.9167,'','',-13.5133474663,-45.5001786367,-14.3387724257,-46.4553203736,3.69912124537,-78.8595809092,-0.668371,-37.0326,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sheridan County, Montana',468,'Ratcliffe','Carboniferous','Mississippian','Visean','Meramecian',336.00,345.00,11,'late Famennian - early Visean',351,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',337,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','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,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',395,0,'',48,-104,411653,-3684696,'United States','North America',101,'',48.9333,-104.0833,'','',-13.2872503369,-45.2681848764,-14.1194989786,-46.2156542243,3.9876769227,-78.722210312,2.45406,-33.7579,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lion Creek, Queensland',473,'Lion Creek','Carboniferous','Mississippian','Visean','middle-upper Visean',336.00,345.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m','42','80',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','21','4','Microbial precipitation','1','Present',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',441,1848,'Bioherms are lenticular and consist of thromolites, Renalcis, diverse corals,  and solenoporid algae \nIn latest Visean mounds sponges become important.\nSurrounded by oolitic limestones.\nCore facies is coral boundstone: Siphonodendron, Lithostotion, Multithecopora.\nTyrpanites borings\nLargest reef is 15 m thick.\n\nAbstract of Ref. 1848:\nAlthough skeletal organisms have received most of the emphasis in studies on Phanerozoic reef history, the roles of non-skeletal (non-enzymatic) carbonates (e.g., synsedimentary cements, automicrite, microbialite, etc.) in reef framework construction are becoming increasingly better understood. One problem in understanding the role of non-enzymatic carbonates in reef construction has been the difficulty in recognizing them in reef facies. Whereas skeletal organisms commonly can be recognized and documented in the field, non-enzymatic carbonates may be recognizable only in thin section. This paper describes the application of a new sampling technique that allows the quantitative comparison of skeletal macrofauna and flora with associated non-enzymatic carbonates and other microfaunal/microfloral constituents. The technique involves the point counting of thin sections made from small diameter cores that are systematically recovered from grids and line transects that cover a reasonable area (m2) of reef facies. Small, shallow-water patch reefs are abundant in scattered oolitic intervals in the Lower Carboniferous strata of eastern Australia. The youngest known Carboniferous reefs in eastern Australia occur in uppermost Visean strata (limestone FC5) near the top of the Rockhampton Group, approximately 50 km west-northwest of Rockhampton, Queensland. The largest sampled reef was 15 m thick and 42 m in diameter, with synsedimentary relief above the sea floor of at least 2 m during the primary growth phase. The reef occurs within bioclastic-oolitic grainstones representing a shallow shelf setting and consists of eight common framework microfacies: 1) coral boundstone. 2) bryozoan boundstone. 3) mixed crinoid-bryozoan boundstone. 4) tubular problematica boundstone. 5) sponge-automicrite boundstone. 6) encrusted thrombolite boundstone. 7) mixed automicrite boundstone. and 8) thrombolitic wackestone-packstone. Reef growth was initiated by automicrite-producing biofilms, sponges and a tubular problematic organism. Primary relief building was accomplished by automicrite-dominated frameworks and lithistid sponges, crinoids, and corals. Large cerioid Aphrophyllum coral colonies had a heterogeneous distribution through the reef. The framework of the main relief-bearing portion of the reef consists on average of 44.4 % automicrite and automicrite-bound detritus, excluding automicrite-bound sponge body fossils, and at most 19.6 % skeletal organisms in growth position (minimum of 7.2 %). If sponge body fossils are included as automicrite framework, because they are preserved only as a result of automicrite formation, the percentage of automicrite and bound sediment is 54.9 %. A smaller sampled reef consisting of the same basic facies had 39.5 % automicrite and automicrite-bound sediment in its framework (50.2 % including sponges) and, at most, 33.4 % skeletal organisms in growth position (minimum of 22.7 %). The greater volume of skeletal framework in the small reef reflects a greater proportion of large corals. Of frame-building skeletal organisms, automicrite-preserved lithistid and other sponges and cerioid rugose corals provided the greatest volume. However, crinoid holdfasts were the most widespread skeletal framework components. The dominant framework facies are sponge-automicrite boundstone, encrusted thrombolite boundstone, mixed automicrite boundstone, and coral boundstone. The reefs are similar in overall framework construction and ecological succession to slightly older Visean reefs in eastern Australia and to some of the late Visean reefs of northern England. Surprisingly, framework similarities also exist between the reefs and certain thrombolite-lithistid-coral reefs of the European Jurassic.\n',-23,150,-5623132,14065272,'Australia','Oceania',801,'400, 399',-23.3833,150.4,'WAHR','24197',-20.1732924424,153.145929576,-18.7402231545,152.714641574,-36.5609766298,130.559071191,-36.265,146.648,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-25 17:30:16'),('Altensteig',482,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian/Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',150,2,'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','1c','Epeiric sea','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,'40','10','50',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',405,0,'Tubiphytes relatively important forming reefs up section.\nOther encrusters are serpulida and bryozoans.',48,10,4799341,1241619,'Germany','Europe',331,'',48.0833,10.75,'WAHR','68090',29.0360683069,24.3620321762,29.0360683069,24.3620321762,34.1267089906,26.3469958082,39.9604,18.621,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bolshoi Karatau III',490,'','Carboniferous','Mississippian','Visean','lower Visean',336.00,346.70,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',343,3,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20',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','1','Corals','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,'80','0','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',409,0,'Locality doubtful.\nUppermost lower Visean.\nMentioned is shallow water Waulsortian type mound.\nCoral-crinoid-bryozoan-algal.\n',43,68,1840566,6438035,'Kazakhstan','Asia',301,'',43.5,68.5,'','',-10.8623571428,59.3649799935,-13.2659234166,59.3145262371,25.2365967977,18.4379757526,16.0211,48.7627,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bolshoi Karatau V',492,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','13','Echinoderms','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',409,1662,'Locality doubtful.\nMentioned is shallow water Waulsortian type mound.\nCrinoid-bryozoan-algal mounds are described.',43,69,1893537,6500851,'Kazakhstan','Asia',301,'',43.4167,69.5,'','',-12.8402362489,56.015183954,-12.8402362489,56.015183954,23.5145327122,18.327641732,7.16916,45.541,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Esfandiar',496,'Esfandiar Limestone','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'0','Outcropping reef ',4,'Biostrome','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','','Unknown','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,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',411,2388,'Type locality of Esfandiar Limestone.\nDescribed as algal reef limestone.\nMicrobial biostromes and bioherms according to Pandey and Fürsich (2003)',33,57,4335750,5938762,'Iran','Asia',505,'',33.3,57,'','',28.7558912543,69.6810580644,28.7558912543,69.6810580644,32.1098184582,73.2330878948,-14.3491,43.0314,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rocha, Faro',498,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','30',NULL,NULL,NULL,'3','More than 100 m',NULL,'25',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','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,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',413,412,'Coral-chaetetid-stromatopore-debris reefs.\nSiliceous sponges common\nMiddle ramp position',37,-7,3450216,-280381,'Portugal','Europe',304,'',37.1333,-7.8667,'WAHR','68207',18.2171148163,8.03564593855,18.2171148163,8.03564593855,25.3983586468,4.88270927987,31.4536,0.647167,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jabaloyas',502,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30','501',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','1','Corals','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','90','10',0,'no',0,'no','2','6 to 24 reef building species','7','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium 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',412,1608,'Coral thrombolite.\nMicrobial crusts dominate, but small to medium sized corals and coralline sponges increase up-section.\nSiliceous sponge spicules at base.\n5 coral species described (ref. 2312-2313), one added for microbes, one added for coralline sponges',40,-1,3602922,392934,'Spain','Europe',304,'2312, 2313',40.25,-1.4,'WAHR','34613',18.6908801074,14.2671177086,18.6908801074,14.2671177086,24.9587727234,11.4175798339,31.7543,7.60165,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Arruda dos Vinhos, Serra Isabel level',503,'Abadia','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer 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,NULL,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',413,412,'Serra Isabel level, biostromal.\nOverlying coral limestones.',38,-9,3721995,-301214,'Portugal','Europe',304,'',38.9833,-9.0667,'WAHR','68212',20.2937193186,8.09112544761,20.2937193186,8.09112544761,27.4444198763,5.28327946993,33.5292,0.74604,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tamworth, N.S.W.',554,'Rangari','Carboniferous','Mississippian','Tournaisian','Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',358,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,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',439,440,'Oldest Carboniferous bioherms in Australia.\nPosition doubtful',-31,150,-5234861,14077196,'Australia','Oceania',801,'',-31.1167,150.95,'WAHR','76494',-20.672803732,153.209432773,-20.672803732,153.209432773,-38.3514592884,158.950249574,-34.9896,145.047,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Werris Creek, N.S.W.',557,'Caroda or Merlewood','Carboniferous','Mississippian','Visean','Visean',330.90,346.70,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50','558',1,'Temperate','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',439,440,'',-31,150,-6468217,13420626,'Australia','Oceania',801,'1517',-31.3333,150.6833,'WAHR','76496',-25.7170160468,159.343923816,-25.7170160468,159.343923816,-42.3658144334,137.678854462,-44.2905,151.483,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monto, Queensland',558,'Cannindah Limestone','Carboniferous','Mississippian','Visean','middle-upper Visean',336.00,345.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','245',NULL,NULL,NULL,'4','More than 1000 m','1520','50',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1820,440,'Middle to late Visean Cannindah limestone.\nReef complex 245 m thick and 1520 m in diameter according to ref. 440, but below 100 m after ref. 1820',-24,151,-5758186,14055524,'Australia','Oceania',801,'1517',-24.8833,151.1,'','',-20.8333764423,154.73752286,-19.3782361029,154.30200375,-37.3924907293,132.314554782,-37.4435,148.056,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-25 17:30:08'),('Charlestown, Scotland',559,'','Carboniferous','Mississippian','Visean','Brigantian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',329,3,'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','','Unknown','1','Above fair weather wave base','3','Microbes','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','4','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',442,440,'Composed of filamentous microbes, fenestellid bryozonans, sponges and encrustung forams.\nSimilar mounds to the north are possibly deeper.',56,-3,-127330,349093,'United Kingdom','Europe',331,'',56.05,-3.4833,'','',-27.8539838834,-9.30217789318,-22.679282439,-6.33010050788,-2.23924605639,-29.0594247343,-2.55027,1.48652,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Melvin Field, Alabama',565,'Smackover','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'1','Seismic data available ',1,'True reef','1','Less than 10 m thick','6',NULL,NULL,NULL,'4','More than 1000 m','1600','10',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','1','Corals','21','Tubiphytes - cyanophyceans - corals - (algae) - sponges',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',446,699,'In situ reef, but only 6 m thick. 1.6 km extension\nStromatolite boundstone with coral clasts.\nEncrusting worms, forams, lithistid sponges and red algae.\nEvidence for boring sponges.',32,-88,2228065,-4090745,'United States','North America',101,'',32.2,-88.1333,'','',17.0217867301,-28.4780288879,17.0217867301,-28.4780288879,21.2813581467,-30.7088250061,24.1583,-35.5897,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vocation and Appleton Fields, Alabama',566,'Smackover','Jurassic','Upper Jurassic','Oxfordian','middle Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',158,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','50',NULL,NULL,NULL,'3','More than 100 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','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','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',446,699,'Stromatolites and thrombolites dominate by far. \nQuestionable red algae.\nSituated around isolated basement ridge.\n',31,-87,2102041,-4048020,'United States','North America',101,'2367',31.3167,-87.4667,'','',15.9987476128,-28.2337518437,15.9987476128,-28.2337518437,20.2797610234,-30.3735391276,23.212,-35.0941,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('North Haynesville, Louisiana',567,'Smackover','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'1','Seismic data available ',1,'True reef','1','Less than 10 m thick','4',NULL,NULL,NULL,'4','More than 1000 m',NULL,'40','421',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','21','Tubiphytes - cyanophyceans - corals - (algae) - sponges',NULL,NULL,'20','20','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',446,699,'4 m thick.\nDolomite in pockets.\nStomatolitic boundstone with scattered stromatopores, small Actinastrea and Tubiphytes.',32,-93,2392437,-4539329,'United States','North America',101,'',32.9667,-93.15,'','',19.2322501334,-32.3540112455,19.2322501334,-32.3540112455,23.1830003496,-34.8703657911,25.474,-40.0952,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Marib',568,'','Jurassic','Upper Jurassic',NULL,'Upper Jurassic',145.00,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present','1','Present',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',447,0,'Stromatolites, stromatopores and corals were mentioned from lagoonal facies.',15,45,-1558830,3438648,'Yemen','Asia',503,'',15.4167,45.4167,'','',-21.3195337571,35.198208103,-21.3195337571,35.198208103,-17.7431558862,31.5975017103,-10.0202,29.1841,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bolechowice',608,'','Permian','Lopingian','Changhsingian','Zechstein',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'300',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','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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',482,0,'Stromatolites and solenoporaceans.\nNo detailed description of reef facies.',50,20,2443968,3165319,'Poland','Europe',301,'',50.8,20.5667,'','',28.4229744307,37.0024249187,28.4264038378,37.0031160843,26.7207785363,32.0677090864,18.2619,28.6309,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yuzhny Umet, Kamishin, Volgograd',612,'','Permian','Cisuralian','Sakmarian','Sakmarian/Artinskian',283.50,298.90,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',284,2,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'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','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',486,768,'Pinnacle reefs within shelf deposits.',50,45,3042592,4864083,'Russia','Asia',624,'1415, 1413',50.2833,45.3333,'','',16.7912317624,41.6921979458,16.7912317624,41.6921979458,25.1277342109,24.6992522151,16.8368,40.4454,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Georgetown, Indiana',811,'','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1600','1875',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','1','Corals','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,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',613,0,'Stromatactis network.\nFramework densitiy is lower than in Wabash.\nCorals and bryozoans less than 10 % of total assemblage.',39,-87,-3394965,-5412290,'United States','North America',101,'',39.9667,-87.6333,'','',-30.0411917105,-100.518636099,-30.2233672956,-97.227375308,-30.2233672956,-97.227375308,-23.5632,-54.6954,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Miodobor (Medobory)',825,'','Neogene','Miocene','Middle Miocene','lower Sarmatian',12.50,13.80,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',12,3,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','11','Serpulids - algae - microbes',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species','2','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',617,0,'lower Sarmatian (middle Serravallian)\nBuildups mainly of calcite precipitates\nof microbial and inorganic origins. Skeletal framework represented by serpulid tubes and bryozoan skeletons (in places) is of minor importance. Other biota is taxonomically\nimpoverished but often rich in individuals and comprises few species of bivalves, gastropods, foraminifers and ostracods typical of brackish, semi-marine environment.',49,24,6451669,1883124,'Ukraine','Europe',301,'',49.6667,24,'WAHR','70569',49.1045208285,21.0034467614,49.0716124649,20.9080506998,48.7689500891,23.7835371627,50.0141,22.8357,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jengka Pass, mud-mounds',834,'Copaqabana','Permian','Guadalupian','Wordian','Murgabian/Midian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',265,2,'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','2','Below fair weather wave base','3','Microbes','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,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',623,0,'black or dark-grey wackestone-packstone lenses intercalated with shale\nDeeper marine mud-mounds?',3,102,-3095976,11071077,'Malaysia','Asia',614,'',3.5167,102.6333,'WAHR','75755',-31.4073157105,108.212821235,-31.4073157105,108.212821235,-24.2844460401,102.748164144,-28.1613,109.485,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mlynka',902,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'110','423',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','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','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',655,0,'Well developed Stromatactis structures.',50,19,5258542,1804851,'Poland','Europe',301,'',50.1333,19.7167,'','',31.6326739443,32.5834636327,31.6326739443,32.5834636327,37.6769120987,34.4765034587,41.9444,26.5813,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('La Gándara, Soba Valley',903,'','Cretaceous','Lower Cretaceous','Albian','lower Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,110,'Early Cretaceous (early Albian, 111 Ma)',110,3,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','150',NULL,NULL,NULL,'3','More than 100 m','250','10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','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','2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present','1','Present','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',1716,656,'Ref. 1716:\n150 m thick, 250 m wide platform margin mounds.\n\nRef. 656\nReworked microbialite reefs.\nDemosponges abundant but no functional role in reef building.',43,-3,3888563,164569,'Spain','Europe',304,'',43.2333,-3.5667,'WAHR','56771',31.6089598603,7.47649853541,31.6089598603,7.47649853541,33.8667903807,3.29895510824,32.0934,3.63976,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zhunyi, Guizhou',919,'','Ediacaran','Ediacaran','White Sea Assemblage','Dengying epoch',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',550,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 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','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,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',662,0,'Stromatiolites (Baicalia) as reef builders.',27,106,4192032,-17943604,'China','Asia',602,'',27.6833,106.8333,'','',29.5172291271,53.6290046278,29.5172291271,53.6290046278,29.5172291271,53.6290046278,42.9297,165.164,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jinsha, Guizhou',920,'','Ediacaran','Ediacaran','White Sea Assemblage','Dengying epoch',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',550,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 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','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,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',662,0,'',27,106,4162204,-17905736,'China','Asia',602,'',27.4833,106.2,'','',29.9676054139,54.0783829287,29.9676054139,54.0783829287,29.9676054139,54.0783829287,43.2876,165.817,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tonghaiko, Hubei',921,'','Ediacaran','Ediacaran','White Sea Assemblage','Dengying epoch',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',550,1,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'200',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','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,NULL,NULL,'1','Less than 30% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',662,0,'Subsurface reef with botryoidal structures interpreted as a shallow shelf margin reef complex by Xie et al. (1983).',30,113,4379145,17543742,'China','Asia',602,'',30.1833,113.0333,'','',24.5176928197,49.9581084439,24.5176928197,49.9581084439,24.5176928197,49.9581084439,38.6512,159.654,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dashitou, Zhejiang',922,'','Ediacaran','Ediacaran','White Sea Assemblage','late Xifengshi epoch',542.00,800.00,0,'Vendian',605,690,'Middle Neoproterozoic (late Cryogenian, 690 Ma)',546,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','46',NULL,NULL,NULL,'4','More than 1000 m',NULL,'170',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','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,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',662,0,'Maximum thickness 45.7 m.',28,119,4990276,16474505,'China','Asia',602,'',28.1333,119.5833,'','',28.1333,119.5833,NULL,NULL,28.1333,119.5833,66.9012,157.331,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shiqian, Zhejiang',923,'','Ediacaran','Ediacaran','White Sea Assemblage','late Xifengshi epoch',542.00,800.00,0,'Vendian',605,690,'Middle Neoproterozoic (late Cryogenian, 690 Ma)',546,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'170',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','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,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',662,0,'Xifengshi Formation correlated with Dengying Fm.',27,119,5050343,16420832,'China','Asia',602,'',27.6667,119.75,'','',27.6667,119.75,NULL,NULL,27.6667,119.75,67.3087,156.635,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Xixiang, Shaanxi',926,'Xiannudong','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','16',NULL,NULL,NULL,'3','More than 100 m',NULL,'80',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','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,'1','Constructor guild',NULL,NULL,NULL,NULL,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',662,0,'Three horizons of reef beds.\nSecond beds up to 16 m thick.\nBase with Girvanella and algal stromatolites, upper part with archaeocyathid limestones alternating with algal limestones.\nVery dense packing of archaeocyathids (80-90 %).\n',32,107,2978472,15996451,'China','Asia',602,'',32.9667,107.7833,'','',-6.69422386847,80.0621983677,-8.72818475785,82.6728745303,-8.72818475785,82.6728745303,24.802,162.234,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mian Xiang, Shaanxi',927,'Xiannudong','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','16',NULL,NULL,NULL,'3','More than 100 m',NULL,'80','926',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','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,'1','Constructor guild',NULL,NULL,NULL,NULL,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',662,0,'Three horizons of reef beds.\nSecond beds up to 16 m thick.\nBase with Girvanella and algal stromatolites, upper part with archaeocyathid limestones alternating with algal limestones.\nVery dense packing of archaeocyathids (80-90 %).\n',33,106,3033484,16061012,'China','Asia',602,'',33.1667,106.7167,'','',-6.10016019676,80.7637398637,-8.11728298947,83.3627828701,-8.11728298947,83.3627828701,25.271,163.102,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yutang (Danapo, Limei, Shizishan), Hunan',930,'Qingxudong','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',511,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','140',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','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,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',662,0,'Mostly Epiphyton\r\nOthers are Girvanella and other blue greens.\r\n120-140 m thick, 4-6 km long and 0.2-0.8 km wide.\r\nThree reef buildung cycles.\r\nVertical zonation\r\nEpiphyton patch reefs at base, Epiphyton-Girvanella reefs at top\r\nAge just indicated as Lower Cambrian - but probably Botomian-Toyonian',28,109,3258773,15386548,'China','Asia',602,'',28.43,109.37,'WAHR','80091',-5.48934446265,75.6853423307,-7.622750339,78.2494644337,-7.622750339,78.2494644337,26.6146,157.643,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-02-02 16:33:09'),('Changshan, Zhejiang',931,'Sanjushan','Ordovician','Upper Ordovician','Katian','late Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',446,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','150',NULL,NULL,NULL,'4','More than 1000 m','9000',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','2','Algae','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1','Red algae','20','80','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,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',662,1806,'Algae (possibly red), bryozoans, corals and stromatopores.\r\nFramework of cyanobacterium Trichonophyton and some bryozoans mainly.\r\nReefal complex with massively bedded microbial carbonates, bioclastic and micritic succession, coral-algal and stromatoporoid-algal reefs, dolomitic micrites and massive tabulate coral and algal boundstones (top)\r\nReefs on crinoidal mud mounds.',28,118,-1065064,13797640,'China','Asia',602,'2071',28.8667,118.5833,'',NULL,-8.47771454735,65.1502677123,-8.47771454735,65.1502677123,-8.47771454735,65.1502677123,2.05891,124.13,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shiqian, Guizhou',933,'Xiangshuyuan','Silurian','Llandovery','Aeronian','Aeronian',438.50,440.80,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',437,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','48',NULL,NULL,NULL,'3','More than 100 m',NULL,'80',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes','1','Corals','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,'2','Baffler guild',NULL,NULL,NULL,NULL,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',662,1536,'Total thickness 48 m.\nUp to 36 % algae, around 5 % corals.\nBedded biolithites\n\nXiangshuyuan Fm. according to ref. 1536.',27,108,-445627,14070303,'China','Asia',602,'1662',27.4167,108.2333,'WAHR','80095',3.4430702456,67.9265069864,3.4430702456,67.9265069864,3.4430702456,67.9265069864,8.13217,125.369,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fenggnang, Guizhou',934,'','Silurian','Llandovery','Aeronian','Aeronian',438.50,440.80,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',437,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','48',NULL,NULL,NULL,'3','More than 100 m',NULL,'80','933',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes','1','Corals','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,'2','Baffler guild',NULL,NULL,NULL,NULL,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',662,1662,'Reef builders are algae, corals, bryozoans, sponges and stromatopores.\n48 m thick biolithite level.\nMany and diverse reef attachers: brachiopods, echinoderms, forams, ostracods, trilobites, cephalopods.',28,107,-432891,14153965,'China','Asia',602,'',28,107.7,'','',3.41586623777,68.6777958862,3.41586623777,68.6777958862,3.41586623777,68.6777958862,8.20808,126.123,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cheng-kou, Sichuan',936,'Tianheban','Cambrian','Series 3','Stage 5','late Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',513,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'80',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,'1','Constructor guild',NULL,NULL,NULL,NULL,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',662,0,'',31,108,3002169,15831493,'China','Asia',602,'',31.9667,108.85,'','',-6.82299741791,78.7136750173,-8.88877485165,81.3212220134,-8.88877485165,81.3212220134,24.8849,160.754,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ziyun, Guizhou',944,'','Carboniferous','Mississippian',NULL,'Lower Carboniferous',323.20,358.90,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',345,1,'0','Outcropping reef ',2,'Reef mound','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','3','Microbes','2','Algae','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1','Red algae','30','40','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',662,0,'',25,106,-2174933,10603522,'China','Asia',602,'',25.7333,106.2,'','',-22.0356897689,97.1490003656,-22.0356897689,97.1490003656,-2.41699021067,76.3073740921,-14.5473,98.9851,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shali, Lingyun, Guangxi',949,'Maokou','Permian','Guadalupian','Wordian','Maokouan',265.10,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',265,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'65','326',0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','80','20',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',662,298,'Middle to upper Moakouan',24,106,-1050915,9036773,'China','Asia',602,'2362',24.25,106.8333,'','',-19.7517451722,110.984689138,-17.6317467964,118.557116251,0.85423006295,132.983410709,-6.7281,99.106,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yuping, Guizhou',951,'','Triassic','Middle Triassic','Anisian','Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',240,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','60',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','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,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',662,0,'Red algal-cyanophycean framework.',27,108,2022591,10402274,'China','Asia',602,'',27.2667,108.8333,'','',-8.42332414638,110.890372232,-8.42332414638,110.890372232,20.3113019835,121.882365563,15.3674,97.2905,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vostok Manych, Caucasus',975,'Kumanskaya','Triassic','Lower Triassic','Olenekian','middle-upper Scythian',247.20,250.00,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',247,3,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','50','50',0,'no',0,'no','1','Less than 6 reef building species','2','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',673,0,'Well data.\'Algal\' mounds up to 200 m thick.',45,44,3825149,4090037,'Russia','Asia',624,'',45.5,44.5,'','',31.1006096041,56.448611709,31.2822979643,56.3701272478,33.8777867379,49.4766895489,23.3448,44.1755,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vaygach Island',992,'Varnek','Ordovician','Upper Ordovician','Katian','Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','80',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf',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,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',680,1662,'Microbial reefs\n7-80 m thick.',70,60,-1942245,772297,'Russia','Asia',624,'',70,60,'','',-8.6650505438,-53.822619492,-7.34392988348,-53.9982804173,-7.34392988348,-53.9982804173,-11.2279,4.03323,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('South Tran-Urals',994,'','Ordovician','Upper Ordovician','Katian','Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,'15',NULL,NULL,NULL,NULL,NULL,'100',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',680,0,'Algal buildups.',52,60,-3328199,2315902,'Russia','Asia',624,'',52.5,60.5,'','',-18.8001674111,18.9474735292,-17.6951093709,18.759578658,-17.6951093709,18.759578658,-7.22187,46.6957,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('North Kharyakha, Pechora',1053,'','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'400',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'3','Microbes','4','Stromatoporoids','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,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'1','Present',2,'Actual reservoir',680,661,'Stromatopores, algae and tabulate corals.\nProbably plate 342 or 362.\nAccording to 661 rare macrofauna, many algae.',67,56,1449601,842974,'Russia','Asia',624,'1008, 1009',67.75,56.5,'','',7.61092992531,-6.91386644973,7.61092992531,-6.91386644973,26.4316403647,-75.7730339599,8.63608,7.48144,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Unnamed, Pechora',1055,'Ukhta','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'3','Microbes','4','Stromatoporoids','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,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',680,661,'Stromatropores, tabulate corals and algae.\nProbably plate 370 or 343.\nUkhta time.',65,55,1334301,1051281,'Russia','Asia',624,'1008',65.75,55.5833,'','',6.64627153913,-5.11101205708,6.64627153913,-5.11101205708,26.3116867616,-73.5084646305,7.84819,9.37449,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yasachnoy River, B. Tuonnakh',1060,'','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',680,0,'Microbes only.',63,150,5345842,-2173265,'Russia','Asia',624,'',63.5,150.75,'','',25.8132543494,-14.9919323474,25.8132543494,-14.9919323474,50.9082393194,-52.8513612893,36.3466,-24.4084,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cis-Ural Foredeep',1062,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','4','Stromatoporoids','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',680,0,'Stromatopores and algae?',55,51,1273251,2556824,'Russia','Asia',624,'',55.3333,51.5,'','',-10.9894669429,12.3501025443,-10.9894669429,12.3501025443,24.5584530779,-51.7296627547,5.65956,19,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Saratov',1063,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','9','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','3','Microbes','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'70','0','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',680,1690,'Microbial reefs with  ?rugose corals, ?stromatoporoids and ?tabulate corals occurring in sequence with dolostones, oolites and coglomerates.\n',51,45,602402,2718201,'Russia','Asia',624,'',51.5,45.9167,'','',-15.7914557653,14.0321617348,-15.7914557653,14.0321617348,20.3808361468,-48.6142206736,1.09121,21.2101,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('W-middle Urals',1064,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,2,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)','4','Others',NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',680,0,'Algal buildups?.',55,59,1761305,2801586,'Russia','Asia',624,'',55,59,'','',-7.24491786873,14.4806412443,-7.24491786873,14.4806412443,28.7399562605,-50.632869116,9.63087,20.6502,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kozlayu, Pechora',1065,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,1,'1','Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'80',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)','4','Others',NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',680,1008,'Stromatopores and algae?.',64,57,2217153,1806496,'Russia','Asia',624,'661',64.25,57.5833,'','',-4.3307619775,5.62691322469,-4.3307619775,5.62691322469,28.6676036563,-61.2128779943,11.2952,11.3686,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Polar Urals',1066,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,2,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)','4','Others',NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',680,0,'Algal buildups?\nProbably plate 370.',66,61,2514080,1685095,'Russia','Asia',624,'',66,61.5,'','',-2.14786571258,4.62137114289,-2.14786571258,4.62137114289,30.3084315191,-63.2293666841,13.2843,9.98911,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Selennyakh Range',1067,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',680,0,'Stromatopores and algae?.\nProbably plate 492.',67,140,5626873,-2346193,'Russia','Asia',624,'',67.8333,140.5,'','',10.4341442943,-5.39234912328,10.4341442943,-5.39234912328,53.867315787,-37.3736176978,37.8343,-16.5177,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yasachnoy River, Tuonnakh II',1069,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,2,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)','4','Others',NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',680,0,'Algal buildups?',63,150,6315935,-1971238,'Russia','Asia',624,'',63.5,150.75,'','',16.4322953529,-4.6910781292,16.4322953529,-4.6910781292,57.587429431,-45.832563638,40.9925,-23.1809,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Karachaganak Field',1080,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,1,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,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','15','Algae - microbes - (encrusting forams) - (rare songes)','4','Others',NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite',NULL,NULL,'0','',2,'Actual reservoir',1388,0,'Renalcis-Keega mounds with calcisponges. Plenty of marine cement. Wave resistant structures.',51,50,922313,2936416,'Kazakhstan','Asia',301,'',51.1667,50.8333,'','',-13.3004905438,15.9200548484,-13.3004905438,15.9200548484,23.2499987509,-47.3804901143,3.77119,22.7483,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Karachaganak Field',1086,'','Carboniferous','Mississippian','Tournaisian','Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',354,2,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'50','1080',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','24','Tubiphytes - algae - cyanophyceans - (bryozoans) - (sponges)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',2,'Actual reservoir',1388,0,'Depressed rim platform ramp.\nThrombolite algal mounds.\n\nAbstract ref. 1388:\nFacies analysis and laboratory study has been completed on Upper Devonian to Lower Permian reefs and mounds of southern Kazakstan and Russia. Famennian reefs are composed of Girvanella-Renalcis-sponge-brachiopod boundstone and calcitic cementstone and form reef-rimmed platforms. Tournaisian and Lower Visean carbonates lack an organic margin and form ramps that contain Waulsortian mud mounds rich in crinoids, sponges, and rugose corals. Middle Visean through Serpukhovian carbonates consist of grainstone-rimmed platforms and slopes. Waulsortian mounds located in slope settings are composed of bryozoan-sponge-Tubiphytes-algae boundstone and calcitic cementstone. Bashkirian shelf margins consist of Donezellid-Archaeolithoporella-brachiopod boundstone and aragonitic cementstone. Lower Permian shelf margins and slope mounds are comprised of bryozoan-Tubiphytes-algae boundstone and calcitic cementstone and Palaeoaplysina rudstone. Devonian through Lower Carboniferous reefs and slope mounds are tight due to cementation; dolomitization and karsting enhance porosity in shelf margins and interiors. Middle Carboniferous and Lower Permian slope mounds and margin facies are porous due to exposure related diagenesis.   These data suggest that: 1) following a Late Devonian extinction event, major shifts took place in the composition and spatial distribution of reef and mound biota as carbonate benthos became re-established, and; 2) the distribution of reservoir-grade porosity is strongly influenced by early-marine cementation, dolomitization and meteoric-related diagenetic processes. Corresponding shifts in the morphology of carbonate platforms, and the spatial distribution of potential reservoirs, suggest a strong biotic and abiotic influence on platform architecture and reservoir development. Comparisons with study of Karachaganak and Tengiz fields confirm these observations.',51,50,922313,2936416,'Kazakhstan','Asia',301,'',51.1667,50.8333,'','',-20.7069402521,19.7016545847,-20.7069402521,19.7016545847,20.6584067785,-30.7629752733,6.01402,25.2681,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Orsha Depression S.W.',1107,'','Ediacaran','Ediacaran','Nama Assemblage','Vendian',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',570,2,'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','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)','4','Others','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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',693,0,'',54,29,-8752299,-3023200,'Belarus','Europe',NULL,'',54,29.7,'','',-68.9692978945,-106.72495629,-68.9692978945,-106.72495629,-68.9692978945,-106.72495629,-72.361,7.58803,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mohylev',1108,'','Ediacaran','Ediacaran','Nama Assemblage','Vendian',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',570,2,'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','3','Microbes','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)',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,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',693,0,'',53,30,-9008385,634107,'Belarus','Europe',NULL,'',53.75,30.3833,'','',-69.3654232203,-105.992433802,-69.3654232203,-105.992433802,-69.3654232203,-105.992433802,-72.6949,8.70938,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Orsha',1109,'','Ediacaran','Ediacaran','Nama Assemblage','Vendian',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',570,2,'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','3','Microbes','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)',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,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',693,0,'',54,30,-8944175,664107,'Belarus','Europe',NULL,'',54.5,30.3833,'','',-68.6793533646,-105.145961406,-68.6793533646,-105.145961406,-68.6793533646,-105.145961406,-71.9609,9.21795,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rogachev',1110,'','Ediacaran','Ediacaran','Nama Assemblage','Vendian',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',570,2,'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','3','Microbes','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)',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,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',693,0,'',53,30,-9062878,569304,'Belarus','Europe',NULL,'',53.0833,30.0333,'','',-69.8815227226,-107.344668771,-69.8815227226,-107.344668771,-69.8815227226,-107.344668771,-73.2986,7.50732,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bobruysk',1111,'','Ediacaran','Ediacaran','Nama Assemblage','Vendian',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',570,2,'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','3','Microbes','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',693,0,'',53,29,-9053112,479463,'Belarus','Europe',NULL,NULL,53.1333,29.1667,NULL,NULL,-69.6029297817,-108.621770488,-69.6029297817,-108.621770488,-69.6029297817,-108.621770488,-73.1181,5.80951,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Orsha',1118,'','Devonian','Middle Devonian','Eifelian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',394,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'300',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','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',693,0,'',54,30,-1438684,1639563,'Belarus','Europe',NULL,'',54.5,30.3833,'','',-0.89322545277,-11.5652074004,-0.89322545277,-11.5652074004,14.8379613124,-72.7056331821,-11.0857,15.0623,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bobruysk',1119,'','Devonian','Middle Devonian','Eifelian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',394,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'300','1118',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','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',693,0,'',53,29,-1621653,1719946,'Belarus','Europe',NULL,'',53.1333,29.1667,'','',-2.21129744413,-10.7609930795,-2.21129744413,-10.7609930795,13.8707803327,-71.4634511801,-12.4203,15.8552,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Turov',1120,'','Devonian','Middle Devonian','Eifelian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',394,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'300','1118',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','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',693,0,'',52,27,-1805134,1757081,'Belarus','Europe',NULL,'',52.0667,27.6667,'','',-3.54879878383,-10.3378545924,-3.54879878383,-10.3378545924,12.7518766223,-70.5941785542,-13.7655,16.263,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ozerchin, Pripyat Depression',1123,'','Devonian','Upper Devonian','Famennian','lower Famennian',358.90,372.20,10,'Givetian - early Famennian',375,370,'Late Devonian (early Famennian, 370 Ma)',373,3,'1','Seismic data available ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'300','1121',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','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',693,1208,'Well data only.\nOncolithic reef according to ref. 1208.',53,27,-1111998,1514600,'Belarus','Europe',NULL,'',53.5667,27.7333,'','',-22.7900129275,4.7317693465,-22.7900129275,4.7317693465,11.081054259,-55.1446663925,-7.0637,13.4869,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('NW-Florida',1139,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,1,'1','Seismic data available ',2,'Reef mound','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','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','1','Present','1','Present',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',699,446,'Stromatolite mound.',30,-87,2044106,-4020320,'United States','North America',101,'',30.9167,-87.0833,'','',15.5118856169,-28.0516894469,15.5118856169,-28.0516894469,19.8079451033,-30.1474107038,22.7752,-34.7928,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Miller County, Arkansas',1141,'Smackover','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'1','Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'3',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,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',2,'Actual reservoir',701,0,'Upper Smackover Fm.',33,-94,2467020,-4696242,'United States','North America',101,'',33.3333,-94.9667,'','',20.135232351,-33.7109949486,20.135232351,-33.7109949486,23.9725085347,-36.3441605166,26.203,-41.8846,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hueli, Sorbas Basin',1167,'','Neogene','Miocene','Upper Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',6,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','40',NULL,NULL,NULL,'3','More than 100 m','400',NULL,NULL,1,'Temperate','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below 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','4','3','Binder guild',NULL,NULL,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',724,0,'Halimeda mound, lithified by microbial crusts.\nTermed segment reef. Microbial is primary according to ref. 724.\nUp to 40 m thick and 400 m long.',37,-2,4936150,-288241,'Spain','Europe',304,'',37.05,-2.1333,'WAHR','34472',36.5040003854,-3.16082992582,36.5020084832,-3.16176558623,36.8019373561,-2.21429750036,37.1842,-2.66309,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cozzo Dipilo, Sicily',1271,'','Jurassic','Upper Jurassic','Tithonian','Tithonian-Berriasian',139.80,152.10,22,'late Tithonian - early Valanginian',141,145,'Jurassic/Cretaceous Boundary (145 Ma)',145,2,'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','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,'1','Constructor guild',NULL,NULL,NULL,NULL,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',779,2022,'Cayeuxia type biolithites.\nSurrounding facies is coralgal debris.',37,14,2775790,1148111,'Italy','Europe',344,'',37.95,14.0167,'','',13.6165188193,20.4629864713,13.6165188193,20.4629864713,15.8106510004,19.1188693603,25.7624,15.5624,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Penobscot, Nova Scotia',1341,'Abenaki','Jurassic','Upper Jurassic','Oxfordian','Oxfordian/Kimmeridgian',157.30,157.30,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,1,'1','Seismic data available ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100','108',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,'4','Microbial precipitation',NULL,NULL,NULL,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',827,0,'Thin thrombolithic buildup on low angle ramp.',43,-60,3715705,-1425586,'Canada','North America',121,'',43.95,-60.1667,'','',22.5121673608,-3.68843148773,22.5121673608,-3.68843148773,28.3631488082,-5.2615747128,34.3793,-10.2524,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jebel Madar',1361,'','Cretaceous','Lower Cretaceous','Hauterivian','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',133,2,'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','3','Microbes','1','Corals','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'5','65','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',840,841,'Microbe-coral-stromatoporoid patch reefs.',22,58,-1143002,5075810,'Oman','Asia',503,'',22.4333,58.15,'','',-14.6626766456,52.9417116585,-14.6626766456,52.9417116585,-13.702868709,46.8087286416,-10.4757,44.6612,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wadi Nakhr',1362,'','Cretaceous','Lower Cretaceous','Hauterivian','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',133,2,'0','Outcropping reef ',2,'Reef mound','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','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'5','65','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',840,841,'same facies as 1361.\n4 m thick patch reef formed by small bioherms.',23,57,-1031432,4992789,'Oman','Asia',503,'',23.1667,57.2,'','',-13.782120473,52.1910611959,-13.782120473,52.1910611959,-12.7490812349,46.1630071612,-9.49442,44.0674,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wadi Qurr',1365,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian/Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',150,2,'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','3','Microbes','1','Corals','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,'3','Binder guild',NULL,NULL,NULL,NULL,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',841,0,'Microbe-coral-stromatopore boundstones unit between Wadi Qurr and southern end of Wadi Dayqa.',23,58,-1002853,5038176,'Oman','Asia',503,'',23,58.6667,'','',-16.9285002977,50.2271910843,-16.9285002977,50.2271910843,21.5839409669,76.2395911745,-8.49982,44.0689,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jasper, Alberta',1371,'','Ediacaran','Ediacaran','Nama Assemblage','upper Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',550,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','30',NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','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,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',845,0,'Basal stromatolite mounds up to 30 m thick.\nIndividual mounds closely spaced.\nInter-mound sediments are siltstones and shales.',52,-118,-6279330,-9342203,'Canada','North America',121,'',52.7833,-118.2833,'','',-47.0054577219,157.633220022,-47.0054577219,157.633220022,-47.0054577219,157.633220022,-46.8152,-102.692,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jasper II, Alberta',1372,'','Ediacaran','Ediacaran','Nama Assemblage','upper Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',550,3,'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','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,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',845,0,'Younger mounds (compare reef 1371).\nSmaller and shallower water than in basal mounds.',53,-118,-6274387,-9310852,'Canada','North America',121,'',53,-118.5833,'','',-46.9092410085,158.022126496,-46.9092410085,158.022126496,-46.9092410085,158.022126496,-46.7565,-102.289,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dobbin Bay, Ellesmere Island',1373,'Scoresby Bay','Cambrian','Series 2','Stage 4','Botomian-Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',513,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3','1','Less than 10 m wide','5','1','Less than 20 m','6',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,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',846,0,'Renalcis mounds up to 3 m thick and 6 m wide. 2-15 m water depth\nLate Early Cambrian',79,-72,-3270195,-4011521,'Canada','North America',121,'',79.6972,-72.8,'','',28.4585526871,-87.2152466212,29.3305315398,-83.9021234995,29.3305315398,-83.9021234995,-17.0078,-51.547,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Port au Port, Newfoundland',1375,'Petit Jardin','Cambrian',NULL,NULL,'Menevian',500.50,509.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',504,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','10',NULL,NULL,NULL,'2','10 - 100 m','80','5',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,'1','Present',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',848,1759,'Microbe bioherm on siliciclastic carbonate shelf.\n10 m high, 80 m wide.\nBasal Thrombolite, upper stromatolite zone.\nCape Ann Member',48,-59,-3359017,-4728150,'Canada','North America',121,'',48.4167,-59.25,'','',7.0614308572,-94.3919812402,7.0614308572,-94.3919812402,7.0614308572,-94.3919812402,-36.9626,-68.5012,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('E-Wernecke Mountains, Yukon',1376,'Sekwi','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1','1','Less than 10 m wide','1','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','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,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',849,0,'Bonnia-Olenellus Zone.\nMax. 1 m thick and 3 m long.\n50 % of volume is matrix (Mudstone and sparite).\nArchaeocyaths (10-60 %) and microbes (Renalcis, Epiphyton, Grivanella).',64,-132,-1001171,-6619974,'Canada','North America',121,'',64.25,-132,'','',45.9982943176,-109.211764627,46.7332703233,-106.324545369,46.7332703233,-106.324545369,5.198,-66.1911,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mackenzie Mts., NW Territories',1377,'Rockslide','Cambrian','Series 3','Guzhangian','Marjuman',500.50,504.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',499,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','25',NULL,NULL,NULL,'3','More than 100 m','120',NULL,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,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',850,0,'Age indicated as earliest Late Cambrian (Marjuman)\nRamp-style slope.\nUp to 25 m thick and 120 m wide.\nGirvanella, Epiphyton, Renalcis.',62,-128,2281951,-5714788,'Canada','North America',121,'',62.4167,-128.4167,'WAHR','56525',46.1340156234,-100.632503378,46.1340156234,-100.632503378,46.1340156234,-100.632503378,5.18043,-66.795,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Banff National Park, Alberta',1378,'Waterfowl','Cambrian','Series 3','Guzhangian','Dresbachian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',498,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1','1','Less than 10 m wide','5','1','Less than 20 m','10','60',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','3','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',851,0,'Renalcis-Girvanella framestones.\n0.3-0.6 m thick.\nThicker (0.5-1.2 m) in nearshore position.\n',51,-115,865579,-6951140,'Canada','North America',121,'',51.3,-115.55,'','',37.3377893134,-109.137990493,37.3377893134,-109.137990493,37.3377893134,-109.137990493,0.308004,-77.4967,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Paget Peak, Banff Nat. Prk., Alberta',1379,'','Cambrian','Series 3','Guzhangian','Dresbachian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',498,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','7',NULL,NULL,NULL,'1','Less than 20 m',NULL,'60','1378',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine 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,NULL,NULL,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',851,1141,'Small thrombolite bioherms in deeper lagoon.',51,-115,884013,-6945128,'Canada','North America',121,'',51.3667,-115.75,'','',37.476587919,-109.102422471,37.476587919,-109.102422471,37.476587919,-109.102422471,0.430192,-77.4251,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S Mackenzie Mts., N.W.T.',1392,'Broken Skull','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','123',NULL,NULL,NULL,'4','More than 1000 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','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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',861,0,'Coalesced bioherms.\n123 m thick barrier reef complex.\nFramework composed of Thromoblites and Renalcis.',63,-127,3259131,-5185362,'Canada','North America',121,'',63.1667,-127.8833,'','',41.2759803053,-89.2165622387,41.2759803053,-89.2165622387,41.2759803053,-89.2165622387,7.1391,-62.1782,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S Mackenzie Mts. II, N.W.T.',1393,'','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','300',NULL,NULL,NULL,'4','More than 1000 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','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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',861,0,'300 m thick dolomitized boundstone sequence of thrombolites and Renalcis.',62,-128,3292063,-5234324,'Canada','North America',121,'',62.6667,-128.3333,'','',41.5049375165,-89.8689578085,41.5049375165,-89.8689578085,41.5049375165,-89.8689578085,7.18768,-62.9202,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mount Wilson, Alberta',1394,'Survey Peak','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',478,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m',NULL,'40',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','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,'3','Binder guild',NULL,NULL,NULL,NULL,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',862,0,'Up to 2 m thick and 10-15 m wide patch reefs.\r\nAbove storm wave base, below fair weather wave base. Open marine shelf.',52,-116,1253254,-7060084,'Canada','North America',121,'',52,-116.75,'',NULL,34.1422288979,-102.411288015,34.1422288979,-102.411288015,34.1422288979,-102.411288015,0.878941,-73.5366,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wilcox Pass, Alberta',1395,'Bison Creek','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',488,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'40',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','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,'3','Binder guild',NULL,NULL,NULL,NULL,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',862,1870,'see reef 1394 for remarks.',52,-117,2449796,-6559547,'Canada','North America',121,'',52.2,-117.1667,'WAHR','81296',34.4402336573,-102.254803304,34.4402336573,-102.254803304,34.4402336573,-102.254803304,1.15233,-73.3611,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Boat Harbor, Newfoundland',1402,'Boat Harbor','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'300',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','4','Microbial precipitation',NULL,NULL,NULL,NULL,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',866,1084,'Small thrombolite mounds',51,-55,-2126076,-4237836,'Canada','North America',121,'',51.6333,-55.9167,'WAHR','56149',3.95764231347,-80.3725062537,3.95764231347,-80.3725062537,3.95764231347,-80.3725062537,-32.291,-50.4409,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Eddies Cove West, Newfoundland',1403,'Watts Bight','Cambrian','Furongian','Lawsonian','lower Ibexian',480.00,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',484,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'300','1402',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',866,1084,'See reef 1402.\r\nSuspect tabulate corals reideintified as calcareous algae (Elias et al. 2020, Geology)',50,-57,-2175879,-4359574,'Canada','North America',121,'',50.75,-57.1667,'',NULL,7.60046477895,-86.8643437527,7.60046477895,-86.8643437527,7.60046477895,-86.8643437527,-35.338,-60.3462,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-12-26 22:09:49'),('Port au Port, Newfoundland',1404,'Catoche','Ordovician','Lower Ordovician','Floian','Arenig',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',471,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'200',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,'4','Microbial precipitation',NULL,NULL,NULL,NULL,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',866,0,'Thrombolitic mound with abundant fenestrae.\nJeffersonian-Cassinian regional stages',48,-58,-2784234,-3996477,'Canada','North America',121,'',48.55,-58.7833,'','',-2.42073725837,-85.1990105579,-2.42073725837,-85.1990105579,-2.42073725837,-85.1990105579,-32.3336,-49.3559,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Melville Peninsula, N.W.T.',1405,'','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',449,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','30','3','101-1000 m wide',NULL,'3','More than 100 m','800',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1539,1538,'Microbial pinnacle reef.\r\nWebby checked with Nowlan from Geol. Survey of Canada',65,-87,-41292,-4731416,'Canada','North America',121,'2064',65.5833,-87,'',NULL,-0.0965182430004,-101.52419175,-0.0965182430004,-101.52419175,-0.0965182430004,-101.52419175,-3.06912,-44.1193,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hall Land, Greenland',1406,'Aleqatsiaq Fjord','Ordovician','Upper Ordovician','Hirnantian','Hirnantian',443.40,445.20,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',444,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','50',NULL,NULL,NULL,'3','More than 100 m','200','100','1405',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,'0','50','50',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',867,0,'Graptolithes (Climacograptus inuiti) indicate latest Ordovician, conodonts earliest Llandovery age. ',81,-60,894030,-3280437,'Denmark','Europe',330,'',81.8333,-60.3333,'','',7.49743084161,-89.5859189032,7.49743084161,-89.5859189032,7.49743084161,-89.5859189032,2.56523,-31.8488,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gaspé Peninsula II, Quebec',1409,'West Point','Silurian','Ludlow','Ludfordian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',418,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 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','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,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',870,946,'Stromatactic mounds of Gros Morbe Member of West Point Formation.\nSponges only present as spicules.\nSome echinoderms, favositid corals, stromatopores and bryozoans are present.\nSmall dasycaldaceans present.',48,-65,-3387751,-3319515,'Canada','North America',121,'',48.1667,-65,'WAHR','75966',-19.6624631142,-60.5493677353,-19.6624631142,-60.5493677353,-19.6624631142,-60.5493677353,-26.2842,-30.4064,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Southhampton Island, N.W.T.',1427,'Severn River','Silurian',NULL,NULL,'Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,430,'Early Silurian (late Llandovery, 430 Ma)',434,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2','3','101-1000 m wide','140','3','More than 100 m','280',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',882,1538,'Hansine Lake area.\nBioherm complexes of stromatolite mounds with stromatopores-coral mounds.\nCircular tabulate and rugose coral mounds up to 50 m across, less than 2 m thick.',65,-85,-396091,-4344168,'Canada','North America',121,'1536',65.5833,-85.6667,'','',-5.58865758699,-95.241668233,-5.58865758699,-95.241668233,-5.58865758699,-95.241668233,-2.25968,-40.3561,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pipe Creek, Indiana',1431,'','Silurian','Pridoli','Pridoli','Pridolian',419.20,423.00,8,'middle Pridolian - middle Pragian',412,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',417,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','48','3','101-1000 m wide',NULL,'3','More than 100 m','1800','2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','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','41','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',885,2262,'11 miles SW of Marion, Indiana.\nPossibly older (Ludlov).\n48 m thick and 1.8 km wide.\nSteep flanks. Reef crest with Renalcis-stromatopore-tabulate coral framestone.\nReef flank with bryozoans, stromatactis, stromatopores, corals in pack-, rud-, bind- and framestones.\nHighest porosity in interreef sediments.\nFossil in collection (Miller) were collected from the flank beds of the reef. Five lithologies were recognized: limestone, swirly limestone, dolomite and dolomitic limestone, silty mudstone, and interreef siltstone. 97% of the beds in the measured sections were limestone or swirly limestone. limestone described as white to gray, coarse-grained, and highly fossiliferous. swirly limestone described as argillaceous, characterized by milky while sparry calcite mixed with stringers and blobs of green silt to clay sized particles, medium to coarse-grained gray limestone and echinodermal debris',40,-85,-3480009,-5202388,'United States','North America',101,'',40.4167,-85.8167,'WAHR','6706',-28.4711695041,-73.1677473872,-28.4711695041,-73.1677473872,-28.4711695041,-73.1677473872,-29.1067,-47.631,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Qpsalquitch R., New Brunswick',1434,'','Silurian','Ludlow','Gorstian','Ludlovian',423.00,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',421,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'80',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'10','0','90',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',888,2188,'Subfacies of a reef complex.\nStromatopores and microbial micritic crusts dominate. Associated tabulate corals.',47,-66,-3428111,-3443872,'Canada','North America',121,'',47.5833,-66.5,'WAHR','75932',-20.7576049113,-63.8519926175,-20.7576049113,-63.8519926175,-20.7576049113,-63.8519926175,-25.2682,-33.0354,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Koch Fjord, Peary Land, Greenland',1447,'','Silurian',NULL,NULL,'Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,430,'Early Silurian (late Llandovery, 430 Ma)',433,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1441',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,'80','10','10',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',890,0,'Incipient stage of buildup comlex.',82,-42,681413,-2706968,'Denmark','Europe',330,'',82.5,-42,'','',5.89685682493,-83.1619241621,5.89685682493,-83.1619241621,5.89685682493,-83.1619241621,5.6415,-25.6779,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('White Mountain, McGrath, Alaska',1450,'','Silurian',NULL,NULL,'Pridolian/Pragian',407.60,423.00,8,'middle Pridolian - middle Pragian',412,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',412,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','500',NULL,NULL,NULL,'4','More than 1000 m',NULL,'95',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','6','Calcisponges','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',893,1124,'Nixon Fork terrane.\nStromatolite reef mounds on a carbonate ramp.\nSome aphrosalpingid sphinctozoans associated.\nUp to 500 m thick.\nProbably plate 125.',62,-155,385629,-4829744,'United States','North America',101,'',62.8333,-155.3333,'','',4.777885837,-92.117261802,4.777885837,-92.117261802,30.1384434565,-141.476735574,7.94107,-49.0571,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('N Holitna Basin, Sleetmute, Alaska',1451,'','Silurian',NULL,NULL,'Pridolian/Pragian',407.60,423.00,8,'middle Pridolian - middle Pragian',412,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',416,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'95','1450',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,NULL,NULL,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',893,1124,'Coalescended thrombolite mounds.\nContinuous reef growth from Prodolian to Pragian?\nProbably plate 125.',62,-156,431958,-4901339,'United States','North America',101,'',62.1667,-156,'WAHR','75775',4.94766264318,-92.8341870143,4.94766264318,-92.8341870143,30.5456172084,-142.184715013,8.41956,-49.6198,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Stromberg',1464,'','Devonian','Middle Devonian','Givetian','upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',386,3,'0','Outcropping reef ',4,'Biostrome','3','101-500 m thick','350',NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',907,0,'Descibed as algal-reef limestones.\nStromatolites dominate.\nMassive limestones 300-350 m thick.',49,7,-2590892,728182,'Germany','Europe',331,'',49.95,7.8,'','',-16.9159320869,-13.8020352935,-16.9159320869,-13.8020352935,-0.624365308139,-70.1022855792,-23.0089,8.35682,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rocky Pass, Jasper Basin, Alberta',1466,'Southesk','Devonian','Upper Devonian','Frasnian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',376,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,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',909,935,'Simla interval.\n\nNearby is Cardinal River reef.',52,-117,-947144,-5133666,'Canada','North America',121,'2002',52.8417,-117.2667,'WAHR','83728',-7.86010787092,-59.7064552454,-7.86010787092,-59.7064552454,-0.999922924637,-120.102645645,-9.45231,-46.3462,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mt. Padenteddu, Sardinia',1471,'','Devonian','Lower Devonian','Pragian','Pragian/Emsian',393.30,410.80,9,'late Pragian - Eifelian',395,410,'Early Devonian (Pragian, 409.2 Ma)',407,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','2','Below fair weather wave base','3','Microbes','1','Corals','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,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',912,0,'Stromatactis mound.\nMaximum 100 m thick.\nCorals and other fossils rare in comparison with matrix content.',39,8,-4979161,3017440,'Italy','Europe',344,'',39.0333,8.8667,'WAHR','26128',NULL,NULL,NULL,NULL,-13.7116274462,-25.9187781653,-45.4805,43.0569,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mukhanovo-Yerokhovo depression',1536,'','Devonian','Upper Devonian','Frasnian','Frasnian-Famennian',358.90,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',374,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'3','Microbes','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','4','Others',NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',954,0,'Subsurface data.',53,52,618748,2331564,'Russia','Asia',624,'',53.3333,52.3333,'','',-6.0728575544,10.49559465,-6.0728575544,10.49559465,24.9645647171,-54.9490563957,4.35106,21.0025,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bobrovka, Kama-Kinel Depression',1539,'','Carboniferous','Mississippian','Tournaisian','lower Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',357,3,'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','0',NULL,'','Unknown','2','Below fair weather wave base','3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'1','Present',2,'Actual reservoir',954,1208,'Subsurface data only (seismic and drilling).',53,50,1058816,2738903,'Russia','Asia',624,'',53.1667,50.6667,'','',-19.7507142141,17.8263835925,-19.7507142141,17.8263835925,21.3505446463,-32.7759589438,6.90965,23.4655,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vuktyl-Dzhebol depression E',1540,'','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',375,2,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300',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,'40','0','60',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',2,'Actual reservoir',954,0,'Girvanella main builders of reef core.\nStromatopores and corals important.\noriginal age assignment Frasnian-Famennian. Stromatoporoids probably Frasnian',62,58,1365701,1431922,'Russia','Asia',624,'',62.5,58,'','',6.66191182404,-1.67164769938,6.66191182404,-1.67164769938,27.7139742905,-70.0115793631,8.18905,12.8072,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Al Jawf',1547,'Jauf','Devonian','Lower Devonian','Emsian','Emsian-Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,395,'Early Devonian (late Emsian, 395 Ma)',397,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','5',NULL,NULL,NULL,'1','Less than 20 m','11','10',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','7','Bryozoans','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',956,2158,'Qasr Limestone Member of Jauf Fm. \nMassive mounds composed of \'algae\' and very rare rugose corals.\n1-5 m high and more than 10 m wide.\nAbundant bryozoans. No reef detritus. ',29,39,-6312628,7518012,'Saudi Arabia','Asia',503,'',29.7833,39.8667,'WAHR','80262',-36.1895565069,39.4789194463,-36.1895565069,39.4789194463,-56.1370106051,41.086402517,-47.3616,82.9086,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Frasnes area',1560,'Grands Breux','Devonian','Upper Devonian','Frasnian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',379,3,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','150','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','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',NULL,'4','Microbial precipitation',NULL,NULL,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',839,960,'Reinterpreted as mud mounds by ref. 976\nlower Givetian patch reefs are also present.\nIncludes data from Arche, Nord and Lion quarries.\n',50,4,-2730778,512543,'Belgium','Europe',331,'976, 2565',50.05,4.4667,'','',-22.7776126305,-11.9383967454,-22.7776126305,-11.9383967454,-3.29925646131,-67.5186964092,-22.0886,5.53364,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hamar Lakhdad, Anti-Atlas',1565,'Kess-Kess','Devonian','Lower Devonian','Emsian','lower Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,400,'Early Devonian (Emsian, 400 Ma)',406,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','46',NULL,NULL,NULL,'2','10 - 100 m',NULL,'5',NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','1','Corals','56','Microbes - crinoids - tabulate/rugose corals',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','18','4','Microbial precipitation','1','Present',NULL,NULL,'2','Medium 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',962,1421,'Conical (Kess-Kess) Mud mounds with tabulate corals (8 species of auloporids, 9 species of favositids), crinoids and large stromatactis. No stromatopores.\nMicrobially mediated mud mounds related to hydrothermal venting according to ref. 1421.\nMaximum thickness 46 m.\n\nAbstract of ref. 1627:\nVarious interpretations have been proposed for the origin of peculiar cone-shaped, finely crystalline, Devonian carbonate mounds of the Hamar Lakhdad Ridge, Anti-Atlas, Morocco, ranging from shallow-water reefs to deep-water mud mounds, formed by biogenic and/or hydrodynamic processes. This study is the first integrated sedimentological and geochemical analysis of these structures. The mounds are cone shaped, steep sided, circular to subelliptical in plan view, and exhibit internal crude bedding parallel to the mound\'s outer surface. They occur in a cluster of 48 mounds on top of a volcanic massif. Stable isotope analyses of first-stage isopachous nonluminescent cement have yielded marine values. In contrast, the finely crystalline carbonate that makes up the bulk of the mound and the internally sedimented mud between crusts of early marine cements have significantly lower delta18O values, whereas values of delta13C are similar to those of the early marine cement. Strontium isotope ratios also clearly distinguish the nonluminescent early marine cements from the finely crystalline material. The 87Sr/86Sr values for the former (0.707 934 - 0.709 392) are in or near the Devonian marine range, whereas the ratios for the latter (0.708 515 - 0.709 656) indicate a more radiogenic Sr source. On the basis of their lithology, architecture, isotope geochemistry, and clustered occurrence on top of a volcanic pile, we propose that the finely crystalline material that forms the mounds and the intermound beds was precipitated from hydrothermal fluids, and that accretion of the material was driven by hydrothermal venting.',31,-4,-6003980,1667672,'Morocco','Africa',714,'1627',31.3833,-4.05,'WAHR','63041',-35.0509153918,-6.0943327636,-35.0509153918,-6.0943327636,-32.8312649535,-6.63621253106,-52.713,27.5853,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ras el Kebbar',1566,'','Devonian','Middle Devonian','Givetian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',390,3,'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','3b','Deeper slope or outer 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','2','4','Microbial precipitation',NULL,NULL,NULL,NULL,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',963,2182,'Mud mound with relatively few fossils.\nCommon crinoids and mulluscs.',31,-4,-4748079,699498,'Morocco','Africa',714,'',31.4333,-4.4,'WAHR','74494',-38.6947073056,-7.95400975259,-38.6947073056,-7.95400975259,-43.7013221679,-7.88885304318,-43.9359,16.535,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Oscar Range NW, Canning Basin',1576,'','Devonian','Upper Devonian','Famennian','lower Famennian',358.90,372.20,10,'Givetian - early Famennian',375,370,'Late Devonian (early Famennian, 370 Ma)',372,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'350',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,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',965,966,'Almost exclusively Renalcis and stromatolites (some Sphaerocodium).',-17,124,-4361236,11583025,'Australia','Oceania',801,'967',-17.3833,124.95,'','',-24.3623201921,116.90079613,-24.3623201921,116.90079613,-35.6378071626,151.771831316,-19.2393,115.113,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Windjana Gorge II, Canning Basin',1578,'','Devonian','Upper Devonian','Famennian','lower Famennian',358.90,372.20,10,'Givetian - early Famennian',375,370,'Late Devonian (early Famennian, 370 Ma)',372,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'350','1576',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,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',966,965,'',-17,124,-4372011,11566704,'Australia','Oceania',801,'',-17.45,124.85,'WAHR','83973',-24.4700090876,116.852224671,-24.4700090876,116.852224671,-35.7537010017,151.758253455,-19.3268,115.032,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Horseshoe Range, Canning Basin',1579,'','Devonian','Upper Devonian','Famennian','lower Famennian',358.90,372.20,10,'Givetian - early Famennian',375,370,'Late Devonian (early Famennian, 370 Ma)',372,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'350','1576',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,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',966,965,'',-18,126,-4428727,11702636,'Australia','Oceania',801,'',-18.1667,126.25,'','',-24.3490332037,118.508838828,-24.3490332037,118.508838828,-35.1955025682,153.485591567,-19.7053,116.586,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Allan, Saskatoon, Saskatchewan',1583,'Prairie Evaporite','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',388,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','3','Microbes','13','Echinoderms','56','Microbes - crinoids - tabulate/rugose corals',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',971,917,'Main part of buildup consists of baffled carbonate (algal-crinoid peloidal grainstone).',51,-106,-1991112,-4343672,'Canada','North America',121,'',51.8333,-106.25,'','',-14.9329688376,-60.3948823476,-14.9329688376,-60.3948823476,-9.76243079695,-117.337852855,-19.858,-39.8061,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ferques, Boulonnais',1588,'Blacourt','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',388,2,'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','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','44','Worms - microbes - (forams) - (bryozoans) - (corals)',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,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',977,1688,'Small calcimicrobial reef with serpulids and Trypanopora',50,1,-2760250,300906,'France','Europe',331,'1761',50.75,1.75,'WAHR','71457',-18.3531890532,-17.6530832806,-18.3531890532,-17.6530832806,-3.36731318537,-72.934477704,-24.5058,4.37298,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Miaomen and Zhaijian, Guilin, Guangxi',1608,'Yonghsien','Devonian','Upper Devonian','Famennian','early-middle Famennian',358.90,372.20,10,'Givetian - early Famennian',375,370,'Late Devonian (early Famennian, 370 Ma)',371,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','35',NULL,NULL,NULL,'2','10 - 100 m','50',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','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','2','6 to 24 reef building species','14','3','Binder guild',NULL,NULL,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',990,1330,'Cryptalgal bindstones and Epiphyton-Renalcis cementstones. Some Palaeomicrocodium and Wetheredella. Up to 35 m thick over 50 m wide. \nInter-reef sediments with gastropods, ostracodes and forams indicate a restricted setting.\nMarginal slope facies accoring to ref. 1866.',25,110,-1602658,9950259,'China','Asia',602,'1866, 2382, 2559',25.35,110.1,'WAHR','24254',-18.9413494755,90.8842292059,-18.9413494755,90.8842292059,-11.9669320412,107.451631882,-0.427843,101.422,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Caunes-Minervois, Montagne Noire',1619,'','Devonian','Lower Devonian','Emsian','upper Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,395,'Early Devonian (late Emsian, 395 Ma)',399,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform 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','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,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',1000,1373,'Bryozans and sponges as main consituents.\nCrinoids also abundant.\nAbundant stromatactis (20-40 % of rock volume).\nCommon neptunian dykes.\n\nAbstract of ref. 2175:\nThe Devonian sedimentary succession of the southern flank of the Montagne Noire (France) was deposited along a divergent margin. This paper is a contribution to describe and evaluate biogenic, sedimentary, geochemical and micropalaeontological features as indicators of sea-level changes and global history of the Devonian in this area. Following transgression and shallow-water environments during Early Devonian time (Lochkovian to early Emsian), biogenic mud-rich mounds with stromatactis developed during latest Emsian at the platform margin. The depth of the Devonian sea was increasing and the seafloor passed below the photic zone and the lower limit of storm wave base during the Emsian. Growth and seismic faults affected the mounds and created Neptunian cracks and crevices, quickly filled with sedimentary material (pisoids) and cements (Neptunian dykes and veins). Light and CL-microscopy, and stable isotope geochemistry show that stromatactis, cements of Neptunian dykes, veins and pisoid cortices are early marine, whereas the red finely crystalline material that forms the bulk of the mound has been cemented in the near-surface diagenetic environment, after the early marine cementation of stromatactis and Neptunian dykes and veins, by meteoric or hydrothermal fluids. The sedimentary rocks overlying the stromatactis mounds exhibit regularly condensed iron and manganese-rich layers, interrupted by the Kellwasser hypoxic horizon. These condensed deposits developed up to the Famennian in a context of carbonate gravity sedimentation and became more and more rhythmic and frequent up section. The occurrence and irregular distribution of large-scale submarine mass flows during Frasnian and Famennian times can be related to block faulting on which Lower Devonian stromatactis mounds could have been uplifted by this block faulting to form seamounts. The sea-level fluctuations detected in the southern flank of Montagne Noire are compared to the Devonian eustatic sea-level curve of Johnson et al. (1985). [Johnson, J.G., Klapper, G., Sanberg, C.A., 1985. Devonian eustatic fluctuations in Euramerica. Geol. Soc. Am. Bull. 96, 567_587.]',43,2,-4914334,2939006,'France','Europe',331,'2175',43.3167,2.5,'','',-26.2152921261,3.69973369053,-26.2152921261,3.69973369053,-20.7091946025,-8.45099365546,-44.0441,40.5773,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mt. Peyroux Nappe, Mont. Noire',1620,'','Devonian','Lower Devonian','Emsian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,400,'Early Devonian (Emsian, 400 Ma)',402,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'50','1619',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform 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,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',1000,1373,'',43,2,-4881013,2973810,'France','Europe',331,'',43.5,2.9167,'','',-25.9609790738,3.97374830493,-25.9609790738,3.97374830493,-20.6027826748,-8.09029224596,-43.7849,40.9117,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Timor Valley, New South Wales',1621,'','Devonian','Middle Devonian','Eifelian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',394,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'12',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','1','Corals','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,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1001,0,'Micritic buildup (372) with only minor contribution of corals, stromatopores and microbes.\nCrinoids are abundant.',-31,151,-2659316,17699995,'Australia','Oceania',801,'',-31.4167,151.0833,'WAHR','80380',-26.3874419368,137.642528129,-26.3874419368,137.642528129,-26.2004679941,175.880875713,-17.5863,165.991,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bolshaya Synya River, Pechora',1636,'','Silurian','Wenlock','Sheinwoodian','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','400',NULL,NULL,NULL,'3','More than 100 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'3','Microbes','2','Algae','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','4','Others','10','80','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'1','Present',1,'Potential reservoir',1007,661,'Algae and stromatolites as main reef builders.\nAdditionally bryozoans and crinoids, in places tabulate and rugose corals.\n400 m thick. Height to base ratio is 1:4-5.\nLarge caverns present (paleokarst). ',65,58,950318,180330,'Russia','Asia',624,'',65.1333,58.5,'','',13.9066047693,-46.772454134,13.9066047693,-46.772454134,13.9066047693,-46.772454134,1.46022,3.73524,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bagan, Pechora',1641,'','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick','250',NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1640',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',661,1008,'see reef 1640',66,57,1473884,994952,'Russia','Asia',624,'',66.4667,57.75,'','',7.69931572332,-5.53213954845,7.69931572332,-5.53213954845,27.0932430888,-74.4265409691,8.85622,8.85186,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('South Kharyakha, Pechora',1642,'','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1640',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'2','Medium production of reefal debris','1','Present',2,'Actual reservoir',661,1008,'',66,56,1426799,934705,'Russia','Asia',624,'',66.9167,56.5833,'','',7.39014694371,-6.10276535029,7.39014694371,-6.10276535029,26.5741174517,-74.8548893504,8.49398,8.31243,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kharyakha, Pechora',1643,'','Devonian','Upper Devonian','Frasnian','upper? Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',376,3,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick','380',NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1640',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,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',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'2','Medium production of reefal debris','1','Present',2,'Actual reservoir',661,1008,'Frasnian \'lower reef\' (dolomitized) and early Famennian \'upper reef\' (limestone).\nRare macrofauna (Amphipora).\nMicrogranular silts with spherical algae, forams,\ncyanophyceans, red algae.\nRef. 1394: Various algae, Girvanella, stromatoporoids, corals.\n380 m thick. 6-11 % porosity.',67,56,1430642,906622,'Russia','Asia',624,'680, 1394',67.1667,56.5,'','',7.43474626925,-6.35298257531,7.43474626925,-6.35298257531,26.5093265056,-75.1272258174,8.51444,8.05836,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Komandirshor, Pechora',1644,'Ukhta','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick','250',NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1055',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',661,1008,'Ukhta age.\n250 m thick, 3-4 km wide algal reef.',67,55,1385052,907347,'Russia','Asia',624,'',67.0833,55.6667,'','',7.1009089126,-6.3739295465,7.1009089126,-6.3739295465,26.1981885861,-74.9902168426,8.18016,8.07001,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yuryakha, Pechora',1649,'Ukhta','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1055',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',661,1008,'Ukhta time.',66,55,1344573,947260,'Russia','Asia',624,'',66.6667,55.1667,'','',6.78173068237,-6.0394556891,6.78173068237,-6.0394556891,26.0490557141,-74.5048950972,7.89445,8.43481,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Terekhevey, Pechora',1652,'Sirachoy?','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'1000','1648',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',661,1008,'Sirachoy time?\n100 m thick.',65,55,1334628,1080271,'Russia','Asia',624,'',65.5,55.75,'','',6.63196714818,-4.85036561219,6.63196714818,-4.85036561219,26.4060935735,-73.2389466646,7.85877,9.63602,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dzhyer, Timan',1660,'Ukhta','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'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','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',661,1008,'Ukhta age.\nAlgal reef.',63,55,1223736,1308234,'Russia','Asia',624,'',63.3333,55.1667,'','',5.69319265344,-2.86998185557,5.69319265344,-2.86998185557,26.3507334968,-70.8049163733,7.11192,11.7031,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('South Pashnya, Timan',1661,'','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,1,'1','Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'250','1659',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',661,1008,'Askyn zone.',63,56,1294050,1351506,'Russia','Asia',624,'',63.0833,56.5,'','',6.18263722327,-2.43859270115,6.18263722327,-2.43859270115,26.9709285683,-70.5838847655,7.63982,12.087,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Omra-Soyva, Timan',1662,'','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',2,'Reef mound','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)',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',661,1008,'Ukhta time, atoll structure.',63,55,1251260,1352595,'Russia','Asia',624,'',63,55.8333,'','',5.86954730927,-2.45492324826,5.86954730927,-2.45492324826,26.6773633731,-70.4605774457,7.3266,12.1006,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nibel, Timan',1664,'Ukhta','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',2,'Reef mound','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)',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',661,1008,'Ukhta time.',62,55,1228474,1373001,'Russia','Asia',624,'',62.7833,55.5833,'','',5.69188976172,-2.28561654343,5.69188976172,-2.28561654343,26.581374649,-70.2086364931,7.16567,12.2866,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sredne Makarikha well',1671,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick','140',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','2','Below fair weather wave base','3','Microbes','2','Algae',NULL,NULL,'2','Green algae','0','100','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',661,660,'140 m thickness.',66,58,4667274,3447201,'Russia','Asia',624,'',66.6333,58.8333,'','',32.776488233,33.6853695723,32.776488233,33.6853695723,36.3081930369,5.21410744612,31.2589,30.8748,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shapkina well, Pechora',1672,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick','70',NULL,NULL,NULL,'3','More than 100 m',NULL,'40','1682',1,'Temperate','0',NULL,'','Unknown','2','Below fair weather wave base','3','Microbes','2','Algae','28','Palaeoaplysina - microbes - bryozoans - Tubiphytes - (corals)','2','Green algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',0,661,'Blue-green and red algae, \nPalaeoaplysina, small sessile foraminifera.\nthickness: 50-70 m.',67,54,4540764,3270681,'Russia','Asia',624,'',67.3333,54.1667,'','',31.7596700102,31.7123174191,31.7596700102,31.7123174191,34.7048100187,3.84266235353,30.1727,28.9857,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shapkina well II, Pechora',1673,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'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,'40','1682',0,'Tropical or unknown','0',NULL,'','Unknown','2','Below fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',0,661,'see reef 1672',67,54,4523323,3299223,'Russia','Asia',624,'',67.0833,54.25,'','',31.6262508938,31.9636710129,31.6262508938,31.9636710129,34.6683521416,4.1459950363,30.0483,29.2391,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cheia Valley, Dobrogea',1702,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20','1701',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','2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present','1','Present',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',1015,0,'Thrombolithic bialites and stromatolites dominant. Siliceous sponges only 10-30 % of organisms. \nMicrite often winnowed.\nSparitic or automicritic replacement.\nAtoll-shaped structure.',44,28,4806774,2229662,'Romania','Europe',348,'',44.55,28.3833,'WAHR','68715',28.7936839311,41.3579389622,28.7936839311,41.3579389622,34.4057007524,43.6382986518,37.2451,35.143,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Potoczek',1704,'','Neogene','Miocene','Middle Miocene','Sarmatian',11.60,12.70,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',12,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'80',NULL,2,'Cold - water','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','2','Algae','44','Worms - microbes - (forams) - (bryozoans) - (corals)',NULL,NULL,'40','20','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1002,0,'Reef core composed of thrombolitic and stromatolitic structures.\nOuter portions with sessile forams (Nubecularia), monostromatic red algae (Lithoporella, Titanoderma), serpulids and some encrusting bryozoa.\n',50,22,6573474,1708192,'Poland','Europe',301,'',50.7222,22.2222,'','',50.1147181674,19.1847309666,50.1597652386,19.3116247591,49.9149480731,22.1001090116,51.0655,21.1233,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lysakow',1705,'','Neogene','Miocene','Middle Miocene','Sarmatian',11.60,12.70,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',12,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'80','1704',2,'Cold - water','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','12','Foraminifera','44','Worms - microbes - (forams) - (bryozoans) - (corals)',NULL,NULL,'50','10','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1002,0,'Reef core composed of thrombolitic and stromatolitic structures.\nOuter portions with sessile forams (Nubecularia), monostromatic red algae (Lithoporella, Titanoderma), serpulids and some encrusting bryozoa.\nThick early submarine fibrous cement.\nInternal sediment with peloids.',50,20,6557330,1552911,'Poland','Europe',301,'',50.5903,20.325,'','',49.9361034951,17.3219732097,49.9827166358,17.4467247209,49.8042219557,20.2310665676,50.9207,19.2147,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bol-shaya Kos-yu, Urals',1716,'','Ordovician','Upper Ordovician','Hirnantian','upper Ashgillian',445.20,450.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','110','3','101-1000 m wide','1000','3','More than 100 m','1500','200',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','2','Algae','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1022,1420,'110 m thickness.\nReef complex composed of various algae and microbes together with heliolitids, tabulate and rugose corals and sponge-like organisms.\n',62,58,-2610948,1343397,'Russia','Asia',624,'',62.8333,58.6667,'WAHR','24294',-13.1330452069,-48.0893048726,-10.7572027165,-48.104737229,-10.7572027165,-48.104737229,-15.2295,9.76955,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bad-ya, Kozhym River, Polar Urals',1717,'','Ordovician','Upper Ordovician','Hirnantian','upper Ashgillian',445.20,450.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','260',NULL,NULL,NULL,'4','More than 1000 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','2','Algae','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','15','3','Binder guild',NULL,NULL,NULL,NULL,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',1022,1420,'Small bioherms (3-5 m thick in Caradocian)\n260 m thick dolomitized reef complex.\nBioclasts encrusted by microbes and various algae (red and green).\nPeloidal spongiostromate fabric.\nCorals, problematic hydroids and calcareous\nsponges(?) in small concentrations.\nBlack shale on top of reef.',65,60,-2317470,1175854,'Russia','Asia',624,'',65.4167,60.3333,'WAHR','24298',-11.0959358118,-49.8761665796,-8.84498039376,-50.0155657586,-8.84498039376,-50.0155657586,-13.2591,7.88975,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lec-Elec River, Polar Urals',1718,'','Ordovician','Upper Ordovician','Katian','Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','500',NULL,NULL,NULL,'4','More than 1000 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','2','Algae','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','1','Red algae','10','90','0',0,'no',0,'no','2','6 to 24 reef building species','16','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1022,1420,'Partially dolomitized up to 500 m thick reef complex.\nCavern porosity.\nReef boundstones consist of laminar crusts, microproblematica, algae, tabulate corals and calcareous sponges.\nMicrobial-peloidal crusts very dominant.\nHedstroemia, Garwoodia, Solenopora, dasyclads, tabulate corals, Eoatenipora, stromatoporoids.',67,64,-2001421,1144709,'Russia','Asia',624,'',67.0833,64.5,'WAHR','24299',-8.79761069306,-50.438780785,-7.31967178839,-50.6235302666,-7.31967178839,-50.6235302666,-11.2757,7.44574,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Elusive Mound, Dry Canyon, New Mexico',1719,'','Carboniferous','Mississippian','Tournaisian','upper Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',347,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 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','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'70','0','30',0,'no',1,'yes','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',1024,1023,'Upper ramp setting.\nDeeper ramp to the south.\nOther mounds in the area:\nEastern Marble Canyon\nArt\'s Mound, Indian Wells\nSphinx Mound, Indian Wells\nPhone Line Ridge, Indian Wells',32,-105,-2117678,-5505905,'United States','North America',101,'1352',32.9333,-105.8333,'','',-21.3088649242,-66.8467593684,-21.3088649242,-66.8467593684,-7.47521425833,-106.893825885,-18.9012,-51.5293,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Takachiho, Kyushu',1722,'','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',250,3,'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','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,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',1028,0,'Microbial bindstone-cementstone.\nProbably mound-geometry.\nSome gastropods present.',32,131,3968020,11827473,'Japan','Asia',625,'',32.7444,131.3389,'','',2.29271427024,126.952834274,2.14273933922,126.67855542,24.0243819174,116.810852098,28.7188,108.659,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Salemi, Sicily',1731,'','Neogene','Miocene','Upper Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',6,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','4',NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,'70','10','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present','1','Present',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',1033,2219,'Special type of Messinian build-up. 5 m wide at base.\nMud-supported mound of stacking coalescent botryoidal aggregates in lowest zone.\nAbove zone with microbialites and encrusting bryozoans (Celleporaria) melobesiid algae (Lithoporella) and some nubeculariids and serpulids. \nCoral-microbial build-up surroundig the mound.',37,12,4990691,1173011,'Italy','Europe',344,'',37.8,12.8,'WAHR','69922',36.3066689515,11.5958692458,36.3031289069,11.5926922069,36.8893921528,12.8282259705,37.6121,12.5658,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vasalemma',1735,'Padla','Ordovician','Upper Ordovician','Sandbian','Caradocian',451.00,458.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',453,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','10',NULL,NULL,NULL,'2','10 - 100 m','60',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','0','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1036,0,'Keila stage (Sanbian-Katian)\nFigured but not described.\nMostly micrite but edrioasteroids, corals and bryozans important.',59,24,-4178376,-73941,'Estonia','Europe',NULL,'',59.2667,24.1833,'','',-29.5676677805,-62.4801935528,-28.5820883333,-60.8751708628,-28.5820883333,-60.8751708628,-31.5342,-1.49321,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Boda Mounds 2, north of Gotland',1739,'Klasen','Ordovician','Upper Ordovician','Hirnantian','upper Ashgillian',445.20,450.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,3,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100','1738',0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','4','Others',NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',1036,2672,'More than 100 mounds dominated by algae and stromatolites. 10-25 m thick and 200-800 m in diameter. Mound facies: algal packstone/boundstone interbedded with wackestones, cap and flank facies: packstones and wackestones, sub and supra mound facies: lime mudstones and wackestones.',57,18,-4416073,-394427,'Sweden','Europe',330,'',57.8167,18.9,'WAHR','80782',-28.4102168421,-61.8972191089,-26.9640547995,-60.4818130599,-26.9640547995,-60.4818130599,-30.9472,-3.68136,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Weinberg and Rauhheck, Eifel',1740,'Ahbach','Devonian','Middle Devonian','Eifelian','upper Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',393,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','40',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','2',NULL,'40','20','40',0,'no',0,'no','2','6 to 24 reef building species','6','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1039,0,'Pohler et al. (1999): Stromatactis Mud Mound with stromatoporoids in dolomitized part at top. Shallowing-upward sequence\r\nHallert Member.\r\nCoordinates for Weinberg.\r\n\r\nKoch-Früchtl (1995): Girvanella (cyanobacteria), calcisponges (spicules), fenestillid bryozoans, and Stachyodes are reef builders.\r\nGreen alga Pseudopalaeoporella is present.\r\n20 m thick and up to 1 km in diameter.',50,6,-3241861,815425,'Germany','Europe',331,'',50.315,6.7145,'WAHR','82032',-14.5711609387,-17.8444430842,-14.5711609387,-17.8444430842,-0.145280870574,-73.7703666041,-24.551,8.05007,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),