('Kap Tyson, Hall Land, Greenland',1441,'Hauge Bjerge','Silurian','Llandovery','Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,433,2,0,'Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',890,1511,'Slope mound.\nSee also reef 1440.',81,-61,602415,-3024633,'Denmark','Europe',330,'',81.3333,-61,'','',4.58038969448,-85.7545471105,4.58038969448,-85.7545471105,4.58038969448,-85.7545471105),('Newman Bugt, Nyeboe Land, Greenland',1442,'Hauge Bjerge','Silurian','Llandovery','Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,433,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1441',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',890,0,'Slope mound.\nSee also reef 1440.',81,-58,592330,-2974544,'Denmark','Europe',330,'',81.4167,-58,'','',4.63051987251,-85.298318186,4.63051987251,-85.298318186,4.63051987251,-85.298318186),('Aphrodite Sö, Wulff Land, Greenland',1443,'Rink Firn','Silurian','Llandovery','Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,433,2,0,'Outcropping reef ',3,'Mud mound or bank','3','101-500 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','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',890,0,'Rink Firn Mounds.\nPlatform margin-deeper ramp buildups.\nStromatactis-rich lime mudstone and stromatopore-coral boundstones.',82,-48,625531,-2810647,'Denmark','Europe',330,'',82,-48.5,'','',5.2568655116,-83.9448100205,5.2568655116,-83.9448100205,5.2568655116,-83.9448100205),('Central Warming Land, Greenland',1444,'Rink Firn','Silurian','Llandovery','Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,433,2,0,'Outcropping reef ',3,'Mud mound or bank','3','101-500 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','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',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',890,0,'See reef 1443 for remarks.',81,-53,631080,-2881085,'Denmark','Europe',330,'',81.9167,-53,'','',5.12623298686,-84.5686234951,5.12623298686,-84.5686234951,5.12623298686,-84.5686234951),('Kap Jefferson, Washington Land, Greenland',1445,'Adams Bjerg','Silurian','Llandovery','Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,433,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 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','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',890,1511,'Platform margin buildup.',80,-67,536305,-3176594,'Denmark','Europe',330,'',80.3333,-67.5,'','',3.75285679541,-86.9337550045,3.75285679541,-86.9337550045,3.75285679541,-86.9337550045),('Kap Quensel, Wulff Land, Greenland',1446,'','Silurian','Llandovery','Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,433,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1441',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'20','0','80',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',890,1511,'Intrashelf buildup.',82,-47,644055,-2784883,'Denmark','Europe',330,'',82.1667,-47,'','',5.44836945219,-83.7601815466,5.44836945219,-83.7601815466,5.44836945219,-83.7601815466),('Koch Fjord, Peary Land, Greenland',1447,'','Silurian','Llandovery','Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,433,2,0,'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,'','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),('Nisku, Bigoray, Alberta',1448,'','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'100','1357',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',891,0,'Nisku reef trend.\nBranching corals dominant.\nInitially below wave base.\nProbably plate 124.',52,-115,-1339744,-4767314,'Canada','North America',121,'838',52.7833,-115.6667,'WAHR','75720',-8.68890466098,-59.1994635633,-8.68890466098,-59.1994635633,-2.42769099866,-117.998752231),('White Man Gap, Canmore, Alberta',1449,'Cairn','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',4,'Biostrome','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','2','Below fair weather wave base','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','20','80',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',892,0,'Bulbous stromatopores, Amphipora floatstone and featureless mudstone.\nMud trapped from intertidal sources in a relatively deep water setting.\nFairholme.\nProbably plate 101.',51,-115,-1216527,-5199682,'Canada','North America',121,'',51.0833,-115.4,'WAHR','75747',-9.80593347932,-60.5085037841,-9.80593347932,-60.5085037841,-3.0797578336,-120.400462634),('White Mountain, McGrath, Alaska',1450,'','Devonian','Lower Devonian','Pridolian/Pragian',407.60,423.00,8,'middle Pridolian - middle Pragian',412,412,2,0,'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,'','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),('N Holitna Basin, Sleetmute, Alaska',1451,'','Devonian','Lower Devonian','Pridolian/Pragian',407.60,423.00,8,'middle Pridolian - middle Pragian',412,416,2,0,'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,'','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),('Squaw Mountain, Ogilvie Mts, Alaska',1452,'Ogilvie','Devonian','Lower Devonian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,402,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','40',NULL,NULL,NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',894,1332,'Probably plate 123.\nOver 40 m thick coral-stromatopore reef complex  overlying Renalcis bioherms.\n50-70 % made of coral framestones, half of them in situ.\nColonial rugosans (Xystriphyllum, Spongophyllum) tabulates (Favosites) and tabular to lamellar stromatopores. Stromatopores often on coral heads.\nMicrobes are Renalcis and Girvanella.',65,-141,419962,-4498804,'United States','North America',101,'1124',65.0667,-141.0833,'','',1.27709471675,-74.406583995,1.27709471675,-74.406583995,10.2838754185,-129.846650059),('Montauk Bluff, Alaska',1453,'Ogilvie','Devonian','Lower Devonian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,402,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',894,1332,'Only foreslope debris is present.',65,-141,441980,-4491423,'United States','North America',101,'',65.1667,-141.4167,'WAHR','75818',1.44935416931,-74.4040346409,1.44935416931,-74.4040346409,10.4560625965,-129.852345796),('Sierra, British Columbia',1454,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'7',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'10','0','90',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'','1','Present',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',895,0,'Base is intensly dolomitized.\nWithin basin facies.\nStromatopores very dominant.\nAlgae and corals rare.',58,-121,-488509,-4492205,'Canada','North America',121,'',58.8167,-121.35,'WAHR','75908',-3.97135200646,-61.621268319,-3.97135200646,-61.621268319,0.764470475949,-120.639086315),('Cripple Creek, Fairholme, Alberta',1455,'Southesk','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',NULL,NULL,'3','101-500 m thick','300',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',897,1594,'Margin of Fairholm reef complex.\n300 m thick reef complex. 30 km wide, > 100 km long.\nStromatoporoids, aphiporids, corals, mollusks.\nCoalescended knoll reefs.',52,-116,-1077571,-5139799,'Canada','North America',121,'',52.1833,-116.1167,'WAHR','83725',-8.80958290646,-59.8555845865,-8.80958290646,-59.8555845865,-1.95693073097,-120.016531043),('Mercy Bay, Banks Island, N.W.T.',1456,'','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','60','2','10 - 100 m wide',NULL,'3','More than 100 m','2000','100',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species','20','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',898,1234,'50 patch reefs, up to 60 m thick and 150 m wide.\nShallow siliciclastic shelf.',73,-117,553437,-3082236,'Canada','North America',121,'1248',73.5,-117,'','',3.79763115807,-42.6109042622,3.79763115807,-42.6109042622,13.724084004,-104.905168641),('Evi Field, Alberta',1457,'Slave Point','Devonian','Middle Devonian','upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,386,3,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','42',NULL,NULL,NULL,'3','More than 100 m',NULL,'30',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',899,0,'42 m maximum thickness. \nIntraplatform to platform margin facies.',56,-116,-988001,-4478760,'Canada','North America',121,'',56.55,-116,'WAHR','71423',-7.61458337025,-61.4424133351,-7.61458337025,-61.4424133351,-2.77716016307,-119.766093008),('Golden Field, Alberta',1458,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,1,'Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',899,1283,'Reef fringing a granitic island.',56,-116,-975049,-4490655,'Canada','North America',121,'',56.5333,-116.25,'WAHR','76065',-7.52578436523,-61.5500824947,-7.52578436523,-61.5500824947,-2.71047157368,-119.888008577),('Normandville, Alberta',1459,'Wabamun','Devonian','Upper Devonian','middle Famennian',358.90,372.20,11,'late Famennian - early Visean',351,368,3,1,'Seismic data available ',2,'Reef mound','1','Less than 10 m thick','10',NULL,NULL,NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','4','Others','0','80','20',0,'no',0,'no','2','6 to 24 reef building species','7','3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',900,1576,'Probably marginifera zone.\n10 m thick stromatopore-algal(?) reefs.\nFive stromatoporoid species.\nLabechiid and other forms.',55,-117,785607,-4302588,'Canada','North America',121,'',55.8333,-117.3833,'WAHR','25262',-7.14272029642,-49.9027136302,-7.14272029642,-49.9027136302,7.33744155488,-110.033468265),('Allstones Creek, Alberta',1460,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'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','1b','Intraplatform basin','2','Below fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',901,0,'Coralline patch reef overlying bryozoan shoals.\nSituated in paleo-channel between platform reefs.\nColonial rugose corals.',52,-116,-1045364,-5147568,'Canada','North America',121,'',52.2806,-116.4778,'WAHR','76070',-8.57237813789,-59.9020910907,-8.57237813789,-59.9020910907,-1.73787145386,-120.118528237),('Hummingbird and Whiterabbit, Alberta',1461,'Fairholme','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',902,0,'Margin of platfrom reef complex.\nMiddle Frasnian, Fairholme.',52,-116,-1080933,-5153794,'Canada','North America',121,'',52.0667,-116.2083,'WAHR','76071',-8.82998408819,-59.9849498767,-8.82998408819,-59.9849498767,-2.00763864217,-120.135710968),('Romberg, Brilon',1462,'','Devonian','Upper Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','500',NULL,NULL,NULL,'4','More than 1000 m',NULL,'18',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'','1','Present','3','Pronounced zonation','3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',903,904,'Stachyodes and Amphipora dominant.\nBiostromal growth of buildup.\nTotal thickness about 500 m.\nTop Iberg-Facies: No subfacies\nDorp-Facies: Lateral zonation\nBase Schwelm-Facies: Tuffitic carbonates.',51,8,-2394956,686795,'Germany','Europe',331,'905',51.3833,8.55,'WAHR','75763',-15.4786574455,-14.2843405899,-15.4786574455,-14.2843405899,0.53059539154,-71.075096378),('Esla, Cantabria',1463,'Nocedo','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','20',NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',906,2321,'Contains all Frasnian collections from area based on Reijers (1972).\nUpper Frasnian biostrome.\nCorals, stromatopores and bryozoans.',42,-5,-3534501,1279815,'Spain','Europe',304,'',42.9,-5.1333,'WAHR','27607',-32.6850260741,-2.02066199701,-32.6850260741,-2.02066199701,-8.92253275309,-46.4117365901),('Stromberg',1464,'','Devonian','Middle Devonian','upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,386,3,0,'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,'','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),('Nikanassin Range, Alberta',1465,'','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',908,0,'Probably plate 124.\nSmall mud mounds at base of large clinoform unit.\nLarger reef complex (Miette) mentioned but not described.',52,-117,-927540,-5133542,'Canada','North America',121,'',52.9333,-117.45,'','',-7.71721952399,-59.6919759688,-7.71721952399,-59.6919759688,-0.857794286337,-120.123198993),('Rocky Pass, Jasper Basin, Alberta',1466,'Southesk','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',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,'3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',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),('Whitehorse, Jasper Basin, Alberta',1467,'','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','30',NULL,NULL,NULL,'2','10 - 100 m',NULL,'100','1466',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',909,935,'30 m thick reef (Simla).\nSituated on Thamnopora-dendroid rugose coral wacke-packstone. \nVaried fauna of stromatopores, dendroid rugose corals and horn corals.\n',52,-117,-916977,-5131654,'Canada','North America',121,'',52.9958,-117.5333,'WAHR','76072',-7.64076072396,-59.6677259368,-7.64076072396,-59.6677259368,-0.777796199081,-120.118318108),('Boule Range, Jasper Basin, Alberta',1468,'','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',909,935,'Probably plate 101.\nSimla reef mounds.',53,-117,-873380,-5124199,'Canada','North America',121,'',53.25,-117.8833,'','',-7.32509701799,-59.5715743671,-7.32509701799,-59.5715743671,-0.448460182994,-120.101895633),('Challis, Lost River Range, Custer Co., Idaho',1469,'Jefferson','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','40','4','More than 1000 m wide','1800','4','More than 1000 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','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','9','2','Baffler guild',NULL,'','1','Present','3','Pronounced zonation',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',910,983,'22-40 m thick. Laterally linked reef mounds.\nStromatopores, tabulate corals, colonial rugose corals.\nMajor role of corals. Bioerosion questionable.',44,-114,-1961722,-5662759,'United States','North America',101,'',44.4,-114.0833,'WAHR','45302',-12.1613207076,-67.9845772011,-12.1613207076,-67.9845772011,-8.75102593274,-124.066123043),('Rosevear Field, Alberta',1470,'Swan Hills','Devonian','Upper Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','65',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','4','Stromatoporoids','4','Stromatoporoids','75','Stromatoporoids or chaetetids only',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','2','Intense',2,'Actual reservoir',911,1624,'Platform Reef\r\nUp to 65m thick, cut by a channel.\r\nThick tabular and massive stromatopores, Amphipora, Stachyodes.\r\nGrain-rich is only reef margin.',53,-116,-1236270,-4715894,'Canada','North America',121,'',53.6667,-116.0833,'',NULL,-8.00441202613,-59.9585782629,-8.00441202613,-59.9585782629,-2.95680595685,-118.617952679),('Mt. Padenteddu, Sardinia',1471,'','Devonian','Lower Devonian','Pragian/Emsian',393.30,410.80,9,'late Pragian - Eifelian',395,407,2,0,'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','1','Shelf/platform interior','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,'','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),('Jayena',1472,'','Neogene','Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,9,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','80','20',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',913,0,'Coastal fringing reef.\r\nStrongly dominated by Porites and Tarbellastraea. Corraline algae are also present.\r\nBorings by bivalves, serpulids and sponges.',36,-3,4923285,-445100,'Spain','Europe',304,NULL,36.95,-3.7528,'WAHR','22978',36.0104369134,-4.96311197783,36.0079725407,-4.96437622026,36.593899295,-3.87283338384),('Monachil, Granada',1473,'','Neogene','Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,9,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50','1472',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','80','20',0,'no',0,'no','1','Less than 6 reef building species','5','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',913,0,'Most complex fan delta reef.\r\nStrongly dominated by Porites and Tarbellastraea. Corraline algae are also present.\r\nBorings by bivalves, serpulids and sponges.',37,-3,4948518,-423213,'Spain','Europe',304,'',37.15,-3.5333,'','147183',36.2063003531,-4.7405631165,36.2037990625,-4.74178462597,36.791002426,-3.65030145243),('Ilora, Granada',1474,'','Neogene','Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,9,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50','1472',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','80','20',0,'no',0,'no','1','Less than 6 reef building species','5','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',913,0,'Coastal fringing reef.\nPorites, Tarbellastraea, Platygyra, Siderastrea. Corraline algae are also present.\nBorings by bivalves, serpulids and sponges.',37,-3,4962114,-445374,'Spain','Europe',304,'',37.2583,-3.7667,'WAHR','22979',36.4271838237,-5.3417281841,36.4253767075,-5.3450715268,36.9023397016,-3.88035262003),('Dewal',1475,'Dewal','Devonian','Upper Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',914,0,'About 100 m thick barrier reef.\nMassive and lamellate stromatopores, massive and solitaire rugose corals, massive and lamellate tabulate corals.',33,67,-4590318,8541505,'Afghanistan','Asia',301,'',33.8333,67.8333,'WAHR','74993',-45.3166019899,74.9424062584,-45.3166019899,74.9424062584,-55.2302889876,103.362467564),('Bokan West',1476,'Cawak','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','43',NULL,NULL,NULL,'3','More than 100 m',NULL,'100','1475',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',914,0,'43 m thick reefal interval.\n',34,67,-4569293,8562761,'Afghanistan','Asia',301,'',34.0167,67.8833,'WAHR','84662',-46.0453359778,76.2912407078,-46.0453359778,76.2912407078,-55.396462478,106.105039241),('Koh-e Zardak',1477,'Sin Ghar','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','27',NULL,NULL,NULL,'3','More than 100 m',NULL,'100','1475',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','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,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',914,988,'27 m thick reef interval.\nGivetian at base',34,68,-4538603,8637316,'Afghanistan','Asia',301,'',34.3833,68.3833,'WAHR','75083',-45.6844550669,76.8922899712,-45.6844550669,76.8922899712,-54.9898419674,106.760711109),('Safedak',1478,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','10',NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',914,0,'10 m thick floatstone interval with stromatopores and tabulate corals.',34,68,-4903690,10338775,'Afghanistan','Asia',301,'',34.3333,68.1667,'WAHR','75081',-40.10555863,71.4055199257,-40.10555863,71.4055199257,-52.0172129604,91.6881190471),('Dewal',1479,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,1,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100','1478',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',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',914,0,'Recrystallized mound structure.',33,67,-4959949,10263831,'Afghanistan','Asia',301,'',33.8667,67.8333,'WAHR','75000',-40.5442938211,70.9877468314,-40.5442938211,70.9877468314,-52.4510402187,91.1571892193),('Grünewiese',1480,'Ihmert','Devonian','Middle Devonian','upper Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,393,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','15',NULL,NULL,NULL,'3','More than 100 m',NULL,'30',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','10','30',0,'no',0,'no','3','25 or more reef building species','52','1','Constructor guild','1','Present','1','Present','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',915,1491,'Grünewiese:\nSmall differentiated bioherm of massive boundstones, and bedded reef debris. Knobby to hemispherical, laminar and encrusting reef builder morphologies. Stromatoporoids, alveolitids and chaetetids prevailing. Occasional solitary rugosans.\n17 species of tabulate corals\n10 species of rugose corals\n7 species of stromatoporoids\n1 species of chaetetids\n10 species of algae and microbes\n1 species of encrusting forams\n6 species of bryozoans\n\nMicrite envelopes.\nRare macroborings (Trypanites).\nDistinct ecological succession.\n\nBredenbruch:\nMassive rugose corals (Hexgonaria) and ramose tabulate and rugose corals.\n15 m thick bioherm.',51,7,-3110123,830562,'Germany','Europe',331,'',51.0667,7.65,'WAHR','25364',-13.5749421013,-17.8000531806,-13.5749421013,-17.8000531806,0.800307708471,-74.0868688316),('Ründerroth',1481,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','17',NULL,NULL,NULL,'3','More than 100 m',NULL,'30','1480',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',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',915,0,'Layered stromatopores, tabulate  and rugose corals.\nStacked biostromes. Sequence is 40 m thick.\nThickest individual biostrome 17 m.',51,7,-3127988,816119,'Germany','Europe',331,'',51.0333,7.3667,'WAHR','77050',-13.7159477395,-17.9171588569,-13.7159477395,-17.9171588569,0.627894359196,-74.142611152),('Menden, Steltenberg and Iserlohn',1482,'Massenkalk','Devonian','Middle Devonian','middle-upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,387,3,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','3','Pronounced zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',915,1371,'Stacked biostromes with different composition.\nBiotic succession in Steltenberg studied by ref. 1371. During diversification stage: Alveolitids (49 %), lamellar stromatoporoids (18 %), rugosa (14 %), thamnopores (4 %), amphipores (2 %), auloporids (4 %), green algae (1 %), Dendrostella (rugosa 2 %) of all fossils.\n',51,7,-2424852,637983,'Germany','Europe',331,'1894',51.4333,7.7833,'WAHR','77073',-15.7198673572,-14.7162184261,-15.7198673572,-14.7162184261,0.149215202587,-71.3679537231),('Dornap',1483,'Massenkalk','Devonian','Middle Devonian','late Givetian-early Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,3,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',915,2286,'Amphipora ramosa and massive stromatoporoids.\nDiverse gastropod fauna associated.',51,7,-2481227,608672,'Germany','Europe',331,'',51.2167,7.0833,'WAHR','28047',-18.9469078104,-11.9684428625,-18.9469078104,-11.9684428625,-1.45061250321,-68.3780840255),('Leroy, Genesee County, New York',1484,'Onondaga','Devonian','Middle Devonian','lower Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,395,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','6',NULL,NULL,NULL,'2','10 - 100 m',NULL,'350',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','7','Bryozoans','53','Echinoderms - bryozoans - tabulate corals - (lithistids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','20','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',916,1226,'6 m thick, 62 m wide patch reef.\nCladopora and other tabulate corals are dominant.\nOther important fossils are crinoids and bryozoans.\n10 collections of Miller.',43,-78,-5004264,-2443303,'United States','North America',101,'1381, 2255',43.0167,-78.0333,'WAHR','9529',-31.0911429152,-46.9548744958,-31.0911429152,-46.9548744958,-23.7765883494,-101.849489163),('Port Colburne, Ontario',1485,'Onondaga','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'350','1484',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','13','Echinoderms','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','10','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',917,2256,'Age in collection of Miller given as Givetian. Unlikely because of lithostratigraphy\nAndoned quarry located 2.7 km west of Port Colborne, Ontario, 0.2 km north of Lake Erie on the west side of Quarry Road.\nBiohermal complex with eight distinct facies ranging from crinoidal grainstones to fissile shales and including wackestones, packestones, and mudstone. Corals predominantly from well bedded, light gray to blue, coral-rich, crinoidal packstones with distinct coral-rich fissile shale interbeds.\n',42,-79,-4999514,-2547173,'Canada','North America',121,'',42.8667,-79.3,'WAHR','9476',-31.1428232413,-48.0504175345,-31.1428232413,-48.0504175345,-23.9547994853,-102.857990583),('Syracuse, New York',1486,'Onondaga','Devonian','Middle Devonian','lower Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,395,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'350','1484',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','13','Echinoderms','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'60','0','40',0,'no',0,'no','3','25 or more reef building species','26','2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation',NULL,'',NULL,'','2','Medium production of reefal debris','0','',1,'Potential reservoir',916,982,'',42,-75,-5054093,-2253479,'United States','North America',101,'1226, 1381',42.9667,-75.9167,'WAHR','9539',-31.2525799787,-45.1543750099,-31.2525799787,-45.1543750099,-23.7334360929,-100.157796165),('Roberts Hill, Albany, New York',1487,'Onondaga','Devonian','Middle Devonian','lower Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,395,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','13','Echinoderms','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'80','0','20',0,'no',0,'no','2','6 to 24 reef building species','20','2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',916,1381,'Edgecliff Member\nRugose coral mound with favositid flanks\nSequence of dominant genera:\nAcinophyllum (synaptophyllum), Cylindrophyllum (Eridophyllum), Cyathocylindrium.\nIncreasing corallite diameter.',42,-73,-5144966,-2074248,'United States','North America',101,'1710',42.5,-73.9167,'WAHR','9553',-31.7656955184,-43.4495576731,-31.7656955184,-43.4495576731,-24.0566089019,-98.5094165686),('Krupanj, Serbia',1488,'Rudine','Carboniferous','Middle Carboniferous','Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,316,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','36','1','Less than 10 m wide','20','2','10 - 100 m','30',NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','4','Stromatoporoids','2','Algae','35','Chaetetids - corals - cyanoyphyceans - algae - (bryozoans)','2','Green algae','10','90','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',918,921,'Chaetetes, solitary corals, green algae form bioherm.\n36 m thick and 20-30 m wide.',44,19,-2207630,2760846,'Yugoslavia','Europe',307,'922',44.4,19.4556,'','',-29.1066170578,24.7642807339,-29.1066170578,24.7642807339,-23.936863172,3.85638728357),('Gradac, Serbia',1489,'Stolice','Carboniferous','Middle Carboniferous','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,309,2,0,'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',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','2','Algae','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','2','Green algae','40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',919,921,'Bryozoans, Donezella, corals.',44,19,-2206968,2757461,'Yugoslavia','Europe',307,'922',44.3833,19.4194,'','',-22.3036781067,26.9742959469,-22.3036781067,26.9742959469,-14.7808267933,2.85505620747),('Obradovici, Serbia',1490,'Stolice','Carboniferous','Middle Carboniferous','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,309,2,0,'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',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','2','Algae','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','2','Green algae','40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',919,921,'',44,19,-2201673,2756660,'Yugoslavia','Europe',307,'922',44.4056,19.3722,'','',-22.2634420042,26.9699988687,-22.2634420042,26.9699988687,-14.7447034821,2.83627414113),('Vis-Bobova, Serbia',1491,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'50','20','30',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',920,921,'Mud mounds? with bryozoans, crinoids and algae.',44,19,-1510257,3110789,'Yugoslavia','Europe',307,'922',44.2681,19.7028,'','',-15.648793336,29.8143210525,-15.648793336,29.8143210525,-8.1599224043,8.79831998628),('Kriva Reka - Sklop, Serbia',1492,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'60','0','40',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',920,921,'',44,19,-1484661,3098954,'Yugoslavia','Europe',307,'922',44.3222,19.4033,'','',-15.4407982972,29.7365197269,-15.4407982972,29.7365197269,-8.01286877576,8.63156962046),('Dvorska, Serbia',1493,'','Permian','Middle Permian','Guadalupian',259.80,272.30,16,'Roadian - Changhsingian',261,265,1,0,'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',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',921,922,'',44,19,-528219,3419644,'Yugoslavia','Europe',307,'',44.4278,19.3917,'','',-3.9850579907,33.9585123916,-3.9850579907,33.9585123916,3.57874605615,26.1778204619),('Vapa, Zlatibor, Serbia',1494,'','Triassic','Upper Triassic','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,209,2,0,'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','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','1','Less than 30% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',923,924,'',43,19,1829096,2367700,'Yugoslavia','Europe',307,'',43.7083,19.8472,'','',14.4103353756,31.9151184081,14.2289691127,31.9797841251,10.9575006228,24.6869681239),('Veliki Krs, Zlatibor, Serbia',1495,'','Triassic','Middle/Upper Triassic','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,228,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','80','20',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present',NULL,'','2','Medium zonation',NULL,'','2','30-60% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',924,923,'Wetterstein patch reefs with calcisponges, dendroid corals, hydrozoa, stromatopores, cyanophycea, tubiphytes.\nGreen (Thaumatoporells) and red (solenoporaceans) algae are also present.',43,19,290197,2949193,'Yugoslavia','Europe',307,'',43.7,19.8583,'','',10.7558706118,34.7212509018,10.7558706118,34.7212509018,5.13856048196,23.9442676894),('Ravanjsko Polje, Zlatibor Mt., Serbia',1496,'','Cretaceous','Upper Cretaceous','Cenomanian/Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,93,2,0,'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',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','4','Stromatoporoids','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'45','50','5',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',925,923,'Diverse stromatoporoid fauna according to ref. 1271.',43,19,3335343,1943211,'Yugoslavia','Europe',307,'1271',43.7333,19.9,'','',30.1545577477,22.0923231268,30.1545577477,22.0923231268,26.7614677911,22.9420537676),('Charlevoix, Michigan',1497,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,'3','More than 100 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','0','70',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',926,1693,'4.5 m thick biostromal beds with 3 zones:\nTop: Lamellar stromatopores\nMiddle: massive stromatopores\nBase: Massive corals',45,-85,-3709925,-3200447,'United States','North America',101,'',45.3,-85.2333,'','',-27.2804516096,-50.6944283605,-27.2804516096,-50.6944283605,-20.1867489963,-105.734170139),('Section-Slide Creeks, Miette, Alberta',1498,'Cairn','Devonian','Upper Devonian','middle-late Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,378,3,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','300',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','4','Stromatoporoids','3','Microbes','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','11','2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','3','Pronounced zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',927,1586,'Middle to upper Frasnian.\nFlume Member, Upper Cairn Member.\nAbout 300 m thick.\nStacked stromatoporoid-amphiporid-algal biostromes.\nNine stromatoporoid species in massive facies of Slide Creek.\n31 % - 66 % of stromat. are disoriented.\n\nAbstract ref. 1588:\nThe size distribution and orientation of massive hemispherical tabulate corals and hemispherical stromatoporoids from the Fossil Hill and Manitoulin Formations on Manitoulin Island (Niagaran and Alexandrian, Ontario (Canada)), and of hemispherical stromatoporoids in the Flume and Upper Cairn Members of the Miette reef complex (Frasnian Alberta) and the Jamesville Member of the Manlius Formation (Helderbergian, New York (USA), was determined. In all 5 sample populations there is no statistically significant difference in the mean size between populations of heads in growth position and those disoriented. The process or processes responsible for disorienting heads evidently did not selectively disorient or remove specific size classes. Such disorientation, associated with little lateral transport of heads, could have been accomplished by infrequent short-lived strong wave and current action (storms), structural or soft substrate instability caused by increasing skeleton size due to growth or bioerosion, or some as yet unknown factor. Size-frequency distributions are potentially of value in separating in-place populations from those that have undergone disorientation or transport by size-selective processes. In a paleoenvironmental study this type of data, in conjunction with other information, such as sedimentological evidence or presence or absence of borers, could then be used to help determine the processes of disorientation and (or) transport. ',53,-117,-901078,-5129666,'Canada','North America',121,'1588',53.0833,-117.6667,'WAHR','28074',-7.52547612981,-59.6392078794,-7.52547612981,-59.6392078794,-0.659096916541,-120.118684689),('Formosa, Ontario',1499,'Amherstburg','Devonian','Lower Devonian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,402,2,0,'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',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species','42','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',928,1223,'Superimposed tabular stromatopores, favositid corals and fasciculate rugose corals.\nRef.: 1224\n18 stromatopore species\n13 rugose coral species (mostly solitary).\n11 tabulate coral species.\nDiverse brachiopod fauna.\nReef trilobites in collection 23102\nSeveral collections of Alroy',44,-81,-4789132,-2706585,'Canada','North America',121,'1224, 1225',44.1333,-81.1833,'WAHR','3845',-30.7387551862,-52.0252505896,-30.7387551862,-52.0252505896,-21.3414668828,-105.711791883),('Cline River, Fairholme, Alberta',1500,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m','30','60','1353',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','2','Algae','2','Algae','69','Non-coralline algae only','3','Receptaculitids','0','100','0',0,'no',0,'no','1','Less than 6 reef building species','1','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',929,0,'Receptaculitid mounds.',53,-118,-832058,-5149663,'Canada','North America',121,'',53.25,-118.5,'WAHR','45304',-7.0164700643,-59.7754058969,-7.0164700643,-59.7754058969,-0.197718108029,-120.372600749),('Montague, New Jersey',1501,'Coeymans','Devonian','Lower Devonian','Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,414,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m','100','400','1502',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','3','Pronounced zonation',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',930,1709,'Patch reef with 4 zones.\nMax. 15 m thick.\nCorals, stromatopores, crinoids, bryozoans, algae.',41,-74,-5822542,-1973668,'United States','North America',101,'',41.3167,-74.7833,'WAHR','45305',-28.0492413844,-56.4131332125,-28.0492413844,-56.4131332125,-14.5786453424,-116.486526029),('Knoxboro, Central New York State',1502,'Coeymans','Devonian','Lower Devonian','late Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,413,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','80',NULL,NULL,NULL,'2','10 - 100 m',NULL,'400',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'70','0','30',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','3','Pronounced zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1427,930,'Biomicrite and biosparite at base.\nInitial colonization and stabilization by Favosites.\nLate Favosites and Tryplasma\n\nIncludes data for Mosquito Point reef and four Munnsville reefs.\n\nOn a global basis, carbonate buildups of Early Devonian age are little known compared to examples from Silurian and later Devonian time, and they may be rare in occurrence. Study of the Knoxboro buildup (a patch reef) and related buildups of the Deansboro Member of the Coeymans Formation (Lower Devonian) from central New York has provided insight into the style and development of buildups of this age. The Knoxboro buildup formed on an open marine carbonate platform, and it exhibits 3 distinct vertical stages of sedimentologic and biologic development. Stage I, initial colonization and substrate stabilization, is recognized by the growth of moderately large favositid tabulate corals on a crinoidal calcarenite substrate. Most tabulates are preserved in growth position. Stage II, growth to mean wave base, is characterized primarily by beds of micrite and biomicrite-biomicrudite with in situ colonies of dendroid\nFavosites and Tryplasma corals. These beds form the core of the buildup. Channels, mostly filled with crinoidal debris, cut into beds formed during Stage II. Stage III diversification, is marked by beds of crinoidal debris which blanket the biomicrite core. Planar tabulate (favositid) corals and stromatoporoids (the latter often encrusting the former) are conspicuous in these uppermost beds. Localized occurrences of articulated crinoid columnals represent crinoid patches that occupied somewhat protected locations in the buildup area. Faunal diversity reaches a maximum in these beds,\nalthough diversity appears to be no greater than that of equivalent non-buildup facies of the Deansboro Member. This tabulate and colonial rugose coral buildup is transitional in form and faunal composition between North American midcontinent Silurian buildups and later buildups of Middle Devonian age. ',42,-75,-5610684,-2042259,'United States','North America',101,'2615',42.9894,-75.5236,'WAHR','24955',-26.5154253116,-57.3853111202,-26.5154253116,-57.3853111202,-12.9496971507,-117.173811691),('Western Maryland',1503,'','Devonian','Lower Devonian','Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,414,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'400','1502',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',930,0,'',39,-79,-5958634,-2411405,'United States','North America',101,'',39.4167,-79.1667,'WAHR','45305',-30.4711703085,-59.8319722928,-30.4711703085,-59.8319722928,-16.6262618333,-119.86166061),('Blue Fjord, Ellesmere Island',1504,'Blue Fjord','Devonian','Lower Devonian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,402,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','100','3','101-1000 m wide','2000','4','More than 1000 m','10000',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species','26','1','Constructor guild',NULL,'','1','Present',NULL,'','3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',931,1503,'100 m thick.\nReef talus (corals), forereef limestones (corals), reef margin (stromatopores), reef flat (grainstones with micritization).\nAlmost no fossils in situ.\n\nAbstract of ref. 1503:\nEarly Devonian limestones of Ellesmere, Bathurst, and smaller islands between them in the Canadian Arctic Archipelago contain a diverse fauna of stromatoporoid sponges. This fauna provides the best evidence in North    America of the early recovery phase of this reef-building group from a diversity low at the Silurian/Devonian boundary, a recovery that lead to its diversity peak in Givetian time. Stromatoporoids from the lower member of the Blue Fiord Formation locally form large reefal masses. Well preserved stromatoporoids also occur less abundantly: 1. in the top of the underlying Eids Formation, 2. in the upper member of the Blue Fiord Formation, 3. in the Disappointment Bay Formation, which is correlative of the upper Blue Fiord, and, 4. in the overlying Bird Fiord Formation, and a correlative unnamed formation, both of which span the Lower/Middle Devonian boundary. The stratigraphic distribution of these stromatoporoids can be accurately determined according to conodont biostratigraphy as spanning the dehiscence to partitus (Emsian to basal Eifelian) conodont zones. Common occurrences of Stromatoporella perannulata, Stictostroma gorriense, Habrostroma proxilaminatum, and Parallelopora campbelli in the arctic fauna and southern Ontario and the adjacent United States, indicate that the Detroit River Group is of similar Emsian age, and that the Eastern Americas realm was open to migration from the Arctic. Similarity of species with the Emsian faunas of Russia, Australia and China suggests the cosmopolitan and equatorial distribution of stromatoporoids in Emsian time and opens possibilities for using the group in correlation. The fauna is therefore important in establishing both the evolution of the order and also its geographic distribution in Early Devonian time. Twenty-five    species (assigned to 22 genera) are described. The species concept used is a broad one and the range of variation in each taxon is documented. New species described are: Gerronostroma septentrionalis, Anostylostroma anfractum,    Pseudoactinodictyon conglutinatum, Stictostroma? nunavutense, Clathrocoilona vexata, Stromatopora hensoni. The morphologic limits of the following genera are considered in the description of species: Plectostroma, Aculatostroma and Atelodictyon, Clathrocoilona, Salairella and Syringostromella. The range of Trupetostroma is extended downward into Emsian strata. ',77,-86,-712972,-1929889,'Canada','North America',121,'',77.25,-86.8333,'WAHR','45306',1.20718696176,-51.7312467976,1.20718696176,-51.7312467976,13.5681044619,-108.847715123),('Cameron Island, N.W.T.',1505,'','Devonian','Middle Devonian','lower Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,395,3,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','4','Stromatoporoids','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','16',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',932,931,'Ref. 1407 lists 14 stromatoporoid species.\nGenera: Anostylostroma, Gerronostroma, Pseudoactinodictyon, Actinostroma, Simplexodictyon, Stromatoporewlla, Clathrocoilona, Stromatopora, Salairella, Parallelopora, Pseudotrupetostroma, Stachyodes, Amphipora.',76,-103,-480736,-2292541,'Canada','North America',121,'1407',76.3667,-103.9667,'WAHR','66955',3.19843257165,-47.2789222729,3.19843257165,-47.2789222729,12.9885159588,-109.718438302),('Prince Patrick, N.W.T.',1506,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'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,'','4','Stromatoporoids','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',933,932,'',76,-117,-115259,-2478033,'Canada','North America',121,'',76.5,-117.3333,'','',5.63394711797,-49.2534417252,5.63394711797,-49.2534417252,14.4454741675,-113.246533755),('Gift Lake Slave Point Field, Alberta',1507,'','Devonian','Middle Devonian','upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,386,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'8',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',934,0,'Reef situated on Precambrian high.\nOnly float- and rudstones.',55,-115,-1080455,-4515242,'Canada','North America',121,'',55.8333,-115.5,'','',-8.31046138969,-61.7724064891,-8.31046138969,-61.7724064891,-3.52283025424,-119.953532009),('Wapiabi, Southesk Cairn, Alberta',1508,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',935,936,'Platform reef - isolated stratified carbonate complex\nStacked stromatoporoid biostromes and bioherms.\nBulbous, hemispheriacal, digitate, lamellar, amphiporid stromatopores and rugose corals and algae.',52,-116,-991160,-5085617,'Canada','North America',121,'',52.9833,-116.4333,'WAHR','83638',-8.19526483257,-59.3021278666,-8.19526483257,-59.3021278666,-1.97778376223,-118.226025314),('Southesk Cairn, Alberta',1509,'Flume','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','325',NULL,NULL,NULL,'4','More than 1000 m',NULL,'76',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'','2','Medium zonation','3','Pronounced zonation',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',935,1594,'325 m thick platform reef complex.\n\nAbstract ref. 1594:\nThe MacKenzie, or northwestern, margin of the Frasnian (Late Devonian) Southesk-Cairn carbonate platform is exposed along the McConnell thrust (Laramide) approximately 45 km east of Jasper, Alberta. Exposure is approximately perpendicular to the platform margin providing an excellent example of bank-to-basin depositional style at the Cairn (Lower Leduc), Peechee (Upper Leduc), Grotto-Arcs (Nisku), and Ronde (Blue Ridge-Graminia) stratigraphic levels. The Southesk-Cairn carbonate complex initiated on a regionally extensive shallow-marine platform of the Flume Formation (latest Givetian to earliest Frasnian). The Flume platform overlies a relatively flat pre-Devonian surface and represents an overall deepening-upward sequence. Local evidence suggests that depositionally produced relief (i.e., stacked biostromes) within the Flume, played a fundamental role in the subsequent localization of the Southesk-Cairn platform margin in the Mount MacKenzie area during Cairn time. The Cairn margin has a transgressive, wedge-shaped profile. It is primarily composed of skeletal grainstones and represents a ramp-style bank-to-basin transition. The Cairn platform phase ended with a brief, but pronounced backstepping event. In contrast, the Peechee margin has a well developed stromatoporoid reef-margin facies, a broad back-reef sand apron and a relatively steeply dipping (about 10 degree ) foreslope facies. The combination of starved sedimentation in the adjacent basin and rapid aggradation of the Peechee reef-margin environment produced up to 200 m of platform-to-basin relief. The Grotto-Arcs strata represent a reef-rimmed margin that developed approximately 3 km bankward of the Peechee margin. The Arcs comprises reef and restricted platform-interior facies, whereas the Grotto represents a distally steepened ramp facies. Black, anoxic sediments of the Perdrix Formation were deposited adjacent to the northern margin of the Southesk-Cairn carbonate platform and represent a starved basin which developed during Cairn through Peechee and possibly Grotto time according to conodont data. The slow sedimentation rate of the Perdrix strata was replaced by an episode of very rapid basin infill by Mount Hawk sediments. Platform to basin relief was reduced and nearly filled next to the MacKenzie margin during the late Grotto and during a pre-Ronde sub-aerial exposure event. The Ronde margin initiated more than 4 km basinward of the underlying Arcs and then prograded an additional 2 km over lower Mount Hawk strata. It was a reef-rimmed margin with a moderately dipping foreslope facies characterized by a prominent slope buildup and an orange siltstone unit which separates it from the lower Mount Hawk Formation. A comparison with other outcropping platform-margins indicates that several factors in addition to regional sea level fluctuations influenced the development of these Late Devonian buildups.',53,-117,-924434,-5126350,'Canada','North America',121,'',53,-117.4167,'','',-7.69672916981,-59.6248013504,-7.69672916981,-59.6248013504,-1.58030725763,-118.665188911),('Flathead Range, Alberta',1510,'Peechee','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',937,0,'Pinnacle reefs',49,-114,-1411367,-5298427,'Canada','North America',121,'',49.4167,-114.5833,'','',-7.28236553347,-66.7501329851,-7.28236553347,-66.7501329851,-4.68839781701,-121.082088837),('Flathead Range II, Alberta',1511,'Peechee','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',937,0,'',49,-114,-1404196,-5289382,'Canada','North America',121,'',49.5167,-114.5667,'WAHR','83746',-7.19057450825,-66.7086835809,-7.19057450825,-66.7086835809,-4.61874871758,-121.009285845),('Cardinal Headwaters, Alberta',1512,'Leduc','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',938,0,'',52,-117,-940892,-5136506,'Canada','North America',121,'',52.85,-117.35,'','',-7.81373404719,-59.7278554419,-7.81373404719,-59.7278554419,-0.960034898299,-120.13441396),('Kiska, Nisku, Alberta',1513,'Nisku','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','25',NULL,NULL,NULL,'3','More than 100 m',NULL,'30',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','1','Low zonation','2','Medium zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',939,1487,'25 m thick.\nWithin Cline Channel, between two reef complexes (Fairholme, Southesk-Cairn).\nVery few stromatopores.',52,-116,-1063068,-5141877,'Canada','North America',121,'',52.2375,-116.2667,'','',-8.70317496735,-59.8636324381,-8.70317496735,-59.8636324381,-1.85559947118,-120.049984455),('Littlehorn, Nisku, Alberta',1514,'','Devonian','Upper Devonian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','30',NULL,NULL,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','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',939,0,'30 m thick.\nWithin Cline Channel, between two reef complexes (Fairholme, Southesk-Cairn).\nVery few stromatopores.',52,-116,-1040839,-5147271,'Canada','North America',121,'',52.3042,-116.5167,'','',-8.53939729438,-59.8960823176,-8.53939729438,-59.8960823176,-1.70443237792,-120.120736142),('Burnt Timber, Fairholme, Alberta',1515,'Cairn','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','150',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','4','Stromatoporoids','2','Algae','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','3','Receptaculitids','10','20','70',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',940,0,'Burnt Timber, Panther River and Scalp Creek \nMargin of Fairholme reef complex.\n150 m thick.\nFlank of toe with Receptaculites.',51,-115,-1185335,-5171933,'Canada','North America',121,'',51.4333,-115.4333,'WAHR','76073',-9.58653906106,-60.2310433885,-9.58653906106,-60.2310433885,-2.80050651818,-120.188161788),('Scalp Creek, Fairholme, Alberta',1516,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','150',NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','1515',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',940,0,'Burnt Timber and Scalp Creek \nMargin of Fairholme reef complex.\n150 m thick.',51,-115,-1136922,-5141811,'Canada','North America',121,'',51.8833,-115.6,'','',-9.24210916339,-59.9193354931,-9.24210916339,-59.9193354931,-3.14796752173,-118.540565017),('Mt. McDougall, Fairholme, Alberta',1517,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 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','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',941,0,'Reefs composed of dendroid colonial corals.\nStromatopores absent.',50,-115,-1256762,-5197688,'Canada','North America',121,'',50.9,-115.0333,'WAHR','76087',-10.1002735581,-60.5241414975,-10.1002735581,-60.5241414975,-4.13292436446,-118.890224544),('Galatea Lakes, Fairholme, Alberta',1518,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 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','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','3','25 or more reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',941,0,'Thickets of digitate and massive colonial rugose and tabulate corals and platy stromatopores, Amphipora.',50,-115,-1244585,-5212548,'Canada','North America',121,'',50.8542,-115.2667,'WAHR','76086',-10.0069708613,-60.6488625668,-10.0069708613,-60.6488625668,-3.30839833873,-120.485783385),('Owen Creek, Southesk Cairn, Alberta',1519,'Cairn','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','170',NULL,NULL,NULL,'4','More than 1000 m',NULL,'300',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',942,2736,'Margin of deep water bank.\nCorals? and stromatoporoids.\n170 m thick, 500 m wide.\nIncludes Job Creek and Obstruction Mountain localities of ref. 2736',52,-116,-1047128,-5178945,'Canada','North America',121,'',52.0458,-116.7333,'WAHR','83643',-8.57594617331,-60.1875607978,-8.57594617331,-60.1875607978,-1.80965382331,-120.391682169),('Fatigue Mountain, Fairholme, Alberta',1520,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',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,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',943,0,'',51,-115,-1201246,-5217104,'Canada','North America',121,'',51.0333,-115.6833,'','',-9.68924125,-60.6540946123,-9.68924125,-60.6540946123,-3.00148547929,-120.568268542),('Smith Bay, Prince of Wales Isl.',1521,'Drake Bay','Devonian','Lower Devonian','Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,414,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','10',NULL,NULL,NULL,'1','Less than 20 m','5',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',944,917,'Stromatoporoids, favositid corals and crinoids.',73,-100,-1371688,-2607966,'Canada','North America',121,'',73.3333,-100,'WAHR','26423',3.60312325979,-69.7856367977,3.60312325979,-69.7856367977,18.1515212078,-126.446350121),('Clearwater Creek, Mackenzie, N.W.T.',1522,'','Devonian','Lower Devonian','Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,414,2,0,'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',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf',NULL,'','1','Corals','13','Echinoderms','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite',NULL,'','0','',0,'No or unknown reservoir potential',945,917,'Probably plate 124.\nCoral-crinoid mounds.',61,-125,-1503065,-4273041,'Canada','North America',121,'',61.7,-125.6333,'','',-2.52984535318,-83.4451733973,-2.52984535318,-83.4451733973,12.9880571533,-142.157437197),('Madeleine River, Gaspe, Quebec',1523,'','Devonian','Lower Devonian','Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,414,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',946,917,'Pinnacle reefs.',49,-65,-4906251,-1224283,'Canada','North America',121,'',49.0833,-65.4167,'','',-18.7830376764,-51.8204920524,-18.7830376764,-51.8204920524,-5.95746007413,-110.985636348),('Cameron Island, N.W.T.',1524,'','Devonian','Lower Devonian','Lower Devonian',393.30,419.20,8,'middle Pridolian - middle Pragian',412,407,1,0,'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,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',932,917,'',76,-103,-1086086,-2248584,'Canada','North America',121,'',76.3667,-103.9667,'','',2.73118096191,-60.3824441482,2.73118096191,-60.3824441482,18.4736665432,-119.318707058),('Melville Island, N.W.T.',1525,'','Devonian','Lower Devonian','Lower Devonian',393.30,419.20,8,'middle Pridolian - middle Pragian',412,407,1,0,'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,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',932,917,'',75,-113,-875679,-2454092,'Canada','North America',121,'',75.85,-113.6,'','',3.57435754464,-62.5974952932,3.57435754464,-62.5974952932,18.0530943325,-122.132412143),('Prince Patrick Island, N.W.T.',1526,'','Devonian','Lower Devonian','Lower Devonian',393.30,419.20,8,'middle Pridolian - middle Pragian',412,407,1,0,'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,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',932,917,'',76,-117,-725367,-2444707,'Canada','North America',121,'',76.5,-117.3333,'','',4.64466386594,-62.8666833844,4.64466386594,-62.8666833844,19.0414863812,-122.649937026),('Eids Fjord, Ellesmere Island, N.W.T.',1527,'','Devonian','Lower Devonian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,402,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','20',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',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',947,0,'20 m high, 750 m long downslope buildup.',77,-86,-733297,-1888662,'Canada','North America',121,'',77.3333,-86.6333,'WAHR','84033',1.27468234806,-51.6655120049,1.27468234806,-51.6655120049,13.6467271671,-108.794320967),('Moose River Arch, Ontario',1528,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',948,917,'Corals, stromatopores and crinoids.',49,-81,-4086711,-2608301,'Canada','North America',121,'',49.8667,-81.2,'','',-24.0319878369,-48.4815272141,-24.0319878369,-48.4815272141,-16.9592565824,-104.280020351),('Carnwath River, N.W.T.',1529,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','9',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',949,917,'9 m thick, 14 m diameter.',67,-127,455512,-3884473,'Canada','North America',121,'',67.1667,-127.5,'','',3.2105655372,-56.5420876346,3.2105655372,-56.5420876346,8.77489991938,-116.993544155),('South Nahanni River, District of Mackenzie',1530,'Nahanni','Devonian','Middle Devonian','middle-upper Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,393,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'100',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species','9',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',950,917,'Probably not reefal.\nMassive stromatopores and corals.',61,-124,-980452,-4326572,'Canada','North America',121,'',61.25,-124.5,'WAHR','619',-3.0038687332,-64.962782142,-3.0038687332,-64.962782142,1.56932771925,-123.306230198),('Deep Bay, N.W.T.',1531,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'60',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',951,917,'Dolomitized platform reef.',61,-117,-510455,-4119769,'Canada','North America',121,'',61.3667,-117,'','',-3.94191634714,-58.2671483893,-3.94191634714,-58.2671483893,1.42656792713,-117.358371491),('Keg River Barrier Reef, Pine Point',1532,'Pine Point','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','215',NULL,NULL,NULL,'4','More than 1000 m',NULL,'900',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',2,'Actual reservoir',952,917,'Barrier reef complex.\n215 m maximum thickness.\nReef development starting in Eifelian (see reef 1907).\nIncludes Keg River, Sulphur Point and Pine Point Fms.',60,-114,-678687,-4088795,'Canada','North America',121,'',60.75,-114.75,'WAHR','84247',-5.15396599001,-57.9554577385,-5.15396599001,-57.9554577385,0.293660950212,-116.827150756),('Yoyo, British Columbia',1533,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'17',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',917,0,'9 km wide and 16.5 km long.',58,-121,-1327057,-4433271,'Canada','North America',121,'',58.9167,-121.5,'','',-5.68389225243,-65.6698160954,-5.68389225243,-65.6698160954,-1.18762820959,-123.586717344),('Wadi Hiru II',1534,'','Neogene','Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,18,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','60',NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',953,0,'Massive, branching and platy coral frameworks encrusted by coralline algae.\nAbout 60 m thick. ',14,48,1568264,4994822,'Yemen','Asia',503,'',14.0833,48.8333,'','',8.56537494279,43.1663431585,9.57562847652,44.1061809277,14.0833,48.8333),('Wadi Hiru',1535,'','Neogene','Miocene','lower Miocene',16.00,23.00,30,'Chattian - Aquitanian',22,20,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',953,0,'Reef dominated by faviid corals, Porites or branching and crustose corraline algae.',14,48,1239001,4762318,'Yemen','Asia',503,'',14.0833,48.8333,'','',9.22506603502,43.7441292265,9.22506603502,43.7441292265,14.0833,48.8333),('Mukhanovo-Yerokhovo depression',1536,'','Devonian','Upper Devonian','Frasnian-Famennian',358.90,382.70,10,'Givetian - early Famennian',375,374,2,1,'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,'','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,'','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),('Mukhanovo-Yerokhovo depression',1537,'','Carboniferous','Lower Carboniferous','Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,353,2,1,'Seismic data available ',NULL,NULL,'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','3a','Upper slope or inner ramp',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',954,0,'',53,52,1174558,2783782,'Russia','Asia',624,'',53.25,52.25,'','',-18.8959404969,18.2702489387,-18.8959404969,18.2702489387,22.2596137181,-32.4719418802),('Nikulino, Kama-Kinel\' Depression',1538,'','Carboniferous','Lower Carboniferous','lower Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,357,3,1,'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',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','1','Present',2,'Actual reservoir',954,1208,'',53,52,1203841,2775625,'Russia','Asia',624,'',53.4167,52.5,'','',-18.6829036702,18.1978990463,-18.6829036702,18.1978990463,22.459735949,-32.5802189924),('Bobrovka, Kama-Kinel\' Depression',1539,'','Carboniferous','Lower Carboniferous','lower Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,357,3,1,'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',NULL,NULL,NULL,NULL,'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,'','3','More than 60% micrite',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),('Vuktyl-Dzhebol depression E',1540,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,375,2,1,'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,'','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),('North Caspian depression W',1541,'','Devonian','Upper Devonian','Frasnian-Famennian',358.90,382.70,10,'Givetian - early Famennian',375,374,2,1,'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,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',954,0,'',50,51,406621,2647017,'Russia','Asia',624,'',50.1667,51.5,'','',-7.87995433774,13.1664309247,-7.87995433774,13.1664309247,23.9728571933,-51.5966672396),('North Caspian depression W',1542,'','Devonian','Upper Devonian','Famennian-Tournaisian',346.70,372.20,11,'late Famennian - early Visean',351,360,2,1,'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,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',954,0,'',50,51,897137,3056380,'Russia','Asia',624,'',50.1667,51.5,'','',-17.7353503562,19.4779088002,-17.7353503562,19.4779088002,22.1835829068,-39.4885653229),('North Caspian depression W',1543,'','Carboniferous','Middle Carboniferous','Visean-Bashkirian',315.20,336.00,12,'middle Visean - Serpukhovian',329,325,1,1,'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,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',954,0,'',50,51,1431774,3727136,'Russia','Asia',624,'',50.1667,51.5,'','',-8.95561750838,26.7559698511,-2.45055316362,28.9268142829,14.3873015614,8.93538396515),('Zapadno Teplov, Peri-Caspian',1544,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'Seismic data available ',2,'Reef mound','4','More than 500 m thick','850',NULL,NULL,NULL,'4','More than 1000 m',NULL,'1000',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','7','Bryozoans','23','Bryozoans - Tubiphytes - phylloid algae - (microbes) - (encrusting forams)','2','Green algae','40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1414,1013,'Gas field, top of reef in 3000 m depth. \n15-17 % avg. porosity.\nMore than 850 m thick (including the Sakmarian to lower Artinskian).\nTubiphytes and bryozoans as main reef builders.\nAdditionally stromatolites, encrusting algae, hydrozoans(?), corals and fusulinids.\nAsymmetric with N slope dipping 3-5°, S slope dipping 25-35°.\n',51,51,2951297,4772091,'Kazakhstan','Asia',301,'1413',51.3333,51.5,'','',19.7942264751,43.6395515833,19.7942264751,43.6395515833,27.5966234895,20.7017949049),('Zapadno Teplov, Peri-Caspian',1545,'','Permian','Lower Permian','Sakmarian-Artinskian',283.50,298.90,15,'Sakmarian - Kungurian',277,284,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1000',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','7','Bryozoans','9','Tubiphytes','23','Bryozoans - Tubiphytes - phylloid algae - (microbes) - (encrusting forams)','2','Green algae','60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1414,1013,'see reef 1544.',51,51,3469645,5054690,'Kazakhstan','Asia',301,'486, 1413, 2820',51.5,51.3333,'','',20.1797281275,43.8820903519,20.1797281275,43.8820903519,29.0165905786,25.619164604),('Arlan Field, Bashkirya',1546,'','Devonian','Upper Devonian','Frasnian-Famennian',358.90,382.70,10,'Givetian - early Famennian',375,374,2,1,'Seismic data available ',2,'Reef mound','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'110',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',954,0,'',55,55,892648,2204174,'Russia','Asia',624,'',55,55,'','',-3.97181531847,9.59806288779,-3.97181531847,9.59806288779,26.6987984347,-56.5993624495),('Al Jawf',1547,'Jauf','Devonian','Lower Devonian','Emsian-Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,397,2,0,'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,'','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),('SE Liuzhou, Guangxi',1548,'','Devonian','Middle Devonian','Emsian-Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,397,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',957,0,'',24,109,-1218903,12294981,'China','Asia',602,'',24.0833,109.9167,'','',-7.15844758581,83.2717343583,-7.15844758581,83.2717343583,-18.1478050183,111.088271601),('W Nanning, Guangxi',1549,'Yujiang','Devonian','Middle Devonian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,399,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite',NULL,'','0','',0,'No or unknown reservoir potential',957,2673,'Polygnathus dehiscens zone\n',22,107,-929414,12499852,'China','Asia',602,'',22.75,107.5,'WAHR','80473',-4.4370163534,84.6329419806,-4.4370163534,84.6329419806,-21.6050228536,112.462046325),('E Nanning, Guangxi',1550,'Yujiang','Devonian','Middle Devonian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,399,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'40',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite',NULL,'','0','',0,'No or unknown reservoir potential',957,2673,'',22,109,-1016036,12351848,'China','Asia',602,'',22.8333,109,'WAHR','80472',-4.82953583189,83.299972637,-4.82953583189,83.299972637,-20.2197139047,112.447035558),('NE Yulin, Guangxi',1551,'','Devonian','Middle Devonian','Emsian-Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,397,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,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','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',957,0,'',22,110,-1074400,12215339,'China','Asia',602,'',22.75,110.3333,'','',-5.96048954492,82.5680297307,-5.96048954492,82.5680297307,-17.715616318,112.473535707),('Liu Jing, Hengxian, Guangxi',1552,'','Devonian','Upper Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',957,0,'Patch reef of in situ massive sromatopores and encrusters.',22,109,-795492,10786606,'China','Asia',602,'',22.6333,109.3667,'','',-11.9963005333,87.2330822171,-11.9963005333,87.2330822171,-14.7056581381,113.252629734),('Liuzhai, Nandan, Guangxi',1553,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'20','939',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,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',957,1392,'Asymmetrical reef.',25,107,-1084747,11022035,'China','Asia',602,'1462',25.25,107.3833,'WAHR','82073',-11.9094385989,88.452464783,-11.9094385989,88.452464783,-17.6291260052,110.083015522),('Yangshuo, Guangxi',1554,'Tangjiwan','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'2',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,'20','10','70',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1866,957,'3 horizons of stromatoporoid framework.\nStromatopora, Actinostroma, Anostylostroma and Columnidictyon make up most part of reefs. Additionally corals, chaetetids, brachiopods.\nParallelopora, Stachyodes common in back-reef\nTwo shallowing-up cycles. \n',24,110,-1125349,10726812,'China','Asia',602,'',24.9167,110.25,'','',-12.363859172,85.815658659,-12.363859172,85.815658659,-15.0350046178,109.718470156),('Xiangzhou, Guangxi',1555,'Tungkangling','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'10','0','90',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',957,0,'',23,109,-969031,10756020,'China','Asia',602,'',23.8333,109.8333,'WAHR','45616',-11.216434815,85.8514769888,-11.216434815,85.8514769888,-15.1088514031,110.904865698),('Kadzielnia, Kielce, Holy Cross Mts.',1556,'Kowala','Devonian','Upper Devonian','early Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,383,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','50',NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',958,1037,'Stromatopores, Alveolites, ramose tabulates, rugosans, brachiopods, crinoids and some sponges.\nBioherm 50 m thick.\nKadzielnia member of Kowala Fm.',50,20,-1798371,1398976,'Poland','Europe',301,'2733',50.85,20.65,'WAHR','62179',-21.9090175522,13.1091100779,-21.9090175522,13.1091100779,5.71425733118,-62.4969671353),('Baubigny, Manche',1557,'Nehou','Devonian','Lower Devonian','upper Pragian',407.60,410.80,9,'late Pragian - Eifelian',395,408,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',959,1581,'15-20 m thick bioherm with stromatopores, corals (only tabulates), bryozoans and algae.\nZonation: Brachiopod layer at base\nGlobulat stromatoporoids and tabulate corals\nMassive stromatoporoids at top.\n',49,-1,-4249037,2525395,'France','Europe',331,'',49.4167,-1.8167,'WAHR','78171',-18.7866676756,-1.48313967206,-18.7866676756,-1.48313967206,-17.2126109916,-2.7870272377),('Couvin, Nisme area',1558,'Jemelle','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'Outcropping reef ',4,'Biostrome','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','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',960,2649,'',50,4,-3370769,707657,'Belgium','Europe',331,'2648',50.0667,4.55,'WAHR','78493',-15.5954071056,-18.7207365216,-15.5954071056,-18.7207365216,-1.40541525202,-74.1911382129),('SE Rochefort',1559,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'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',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',960,0,'',50,5,-3337394,746937,'Belgium','Europe',331,'',50.0833,5.2,'','',-15.3240383051,-18.3915631277,-15.3240383051,-18.3915631277,-1.03779889952,-73.9932167327),('Frasnes area',1560,'Grands Breux','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,0,'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,'','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),('Rochefort',1561,'','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50','1560',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite',NULL,'','0','',0,'No or unknown reservoir potential',960,976,'',50,5,-2684590,553694,'Belgium','Europe',331,'',50.1667,5.2167,'WAHR','76604',-22.4599980095,-11.5271577261,-22.4599980095,-11.5271577261,-2.85379262607,-67.3026468322),('Barvaux',1562,'','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite',NULL,'','0','',0,'No or unknown reservoir potential',960,976,'',50,5,-2651014,561154,'Belgium','Europe',331,'',50.35,5.5,'','',-22.214760528,-11.441603682,-22.214760528,-11.441603682,-2.59764303342,-67.3308038147),('Meggen I',1563,'','Devonian','Middle Devonian','upper Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,393,3,0,'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','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',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',961,915,'Reef core with stramotopores and tabulate corals. Reef flank with tabulate and rugose corals.\nIncludes collections of Bilstein, Lennestadt',51,8,-3081012,851458,'Germany','Europe',331,'',51.1333,8.0833,'WAHR','78403',-13.3467773985,-17.632942807,-13.3467773985,-17.632942807,1.07150633751,-74.0166949535),('Meggen II',1564,'','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',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',961,0,'see reef 1563 for remarks.',51,8,-2444762,674068,'Germany','Europe',331,'',51.1333,8.0833,'','',-15.8529531003,-14.3755001728,-15.8529531003,-14.3755001728,0.1510140362,-71.0141087358),('Hamar Lakhdad, Anti-Atlas',1565,'Kess-Kess','Devonian','Lower Devonian','lower Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,406,3,0,'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,'','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),('Ras el Kebbar',1566,'','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'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,'','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),('Aferdeu el Mrakib, Mader Basin',1567,'','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','250','4','More than 1000 m wide','900','4','More than 1000 m','900','20',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',963,2081,'Largest mound in the area.\nOriginally about 250 m thick. \nCommon tabulate corals and sponges spicules. Additionally rugose corals, brachiopods and crinoids.',30,-4,-4819445,656848,'Morocco','Africa',714,'2182',30.8,-4.5833,'WAHR','74491',-39.2245976852,-8.44356847806,-39.2245976852,-8.44356847806,-43.8851746647,-8.75610267424),('Jebel el Oftal',1568,'','Devonian','Middle Devonian','early Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,395,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','40','2','10 - 100 m wide','100','3','More than 100 m','150','20',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','3','Microbes','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','9','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',963,2081,'Auloporids (Bainbridgia, Remesia, Aulocystis) dominant, followed by striatoporids (Taouzia, Pachystriatopora).\nLessa abundant brachiopods, hexactinellids, bryozoans and rugose corals. Rare calcimicrobes (Rothpletzella)',30,-4,-6046786,1590120,'Morocco','Africa',714,'',30.8667,-4.5333,'WAHR','74492',-37.8123801911,-7.66398429109,-37.8123801911,-7.66398429109,-40.8670363936,-7.96547585047),('Hranice, Moravia',1569,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,381,2,1,'Seismic data available ',2,'Reef mound','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100','1573',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,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',964,0,'Well data.',49,17,-2142870,2614578,'Czech Republic','Europe',331,'',49.5667,17.75,'WAHR','79597',-23.9348993833,12.0308204337,-23.9348993833,12.0308204337,3.47111910982,-62.2538891714),('Hranice II, Moravia',1570,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','4','Stromatoporoids','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,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',964,0,'Well data.',49,17,-3622173,3993915,'Czech Republic','Europe',331,'',49.5667,17.75,'','',-19.2394416484,11.8980154572,-19.2394416484,11.8980154572,6.03571743667,-70.033820618),('Ostrava, Moravia',1571,'','Devonian','Upper Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,2,1,'Seismic data available ',2,'Reef mound','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100','1573',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',964,0,'Well data.',49,18,-2084020,2635500,'Czech Republic','Europe',331,'',49.8333,18.3333,'WAHR','79890',-22.2508368008,12.4127417932,-22.2508368008,12.4127417932,3.89834697947,-63.4412603653),('Moravian Karst',1572,'','Devonian','Upper Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',964,0,'',49,16,-2222649,2559134,'Czech Republic','Europe',331,'',49.3333,16.6667,'WAHR','83232',-23.1920602648,11.6223110474,-23.1920602648,11.6223110474,2.70977904357,-63.5103548621),('Krtiny, Moravia',1573,'','Devonian','Upper Devonian','lower Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,383,3,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','40',NULL,NULL,NULL,'3','More than 100 m',NULL,'100',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species','18','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1593,964,'Borehole.\n40 m thick reef interval interfingering with basinal facies.\nAbundant mainly massive stromatoporoids and tabulate corals preserved in growth position. Algae and foraminifers very common. Bryozoans present.\nAbout 18 species of reef builders.\nCoral stromatopore patch reefs.',50,17,-2116731,2534928,'Czech Republic','Europe',331,'',50.1333,17,'WAHR','83222',-23.6551945101,11.2762790946,-23.6551945101,11.2762790946,-1.2462212775,-35.5196368336),('Windjana Gorge, Canning Basin',1574,'Pillara','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'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','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species','50','1','Constructor guild','1','Present',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',965,966,'Stromatoporoids, corals and cyanophyceans (Renalcis and stromatolites) as main reef builders.\n\nMacroborings evident in stromatoporoids of Geikie Gorge (fig. 129 in James, 1983).\n\nCollection sums up data from whole Canning basin.\nDiversity value includes \'algae\', stromatoporoids, and colonial coral (solitary rugosans excluded)',-17,124,-2736403,12841081,'Australia','Oceania',801,'1552',-17.4833,124.9333,'WAHR','25263',-23.8564091675,112.773406888,-23.8564091675,112.773406888,-31.6038638789,155.25663849),('McWhae Ridge, Canning Basin',1575,'Sadler + Virgin Hills','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'350','1574',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,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',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',965,966,'Ref. 1602:\nDiverse rugose corals in back reef',-18,126,-2856322,12953530,'Australia','Oceania',801,'1552, 1602',-18.7333,126.0833,'WAHR','84826',-24.5184305913,114.442777019,-24.5184305913,114.442777019,-31.4416735725,157.195274524),('Oscar Range NW, Canning Basin',1576,'','Devonian','Upper Devonian','lower Famennian',358.90,372.20,11,'late Famennian - early Visean',351,372,3,0,'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,'','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),('Oscar Range SE, Canning Basin',1577,'Pillara','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'350','1574',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','0','70',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'','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',965,966,'',-18,125,-2785157,12890769,'Australia','Oceania',801,'967, 1552',-18,125.4333,'WAHR','92884',-24.1206948721,113.486049669,-24.1206948721,113.486049669,-31.519304694,156.075316557),('Windjana Gorge II, Canning Basin',1578,'','Devonian','Upper Devonian','lower Famennian',358.90,372.20,11,'late Famennian - early Visean',351,372,3,0,'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,'','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),('Horseshoe Range, Canning Basin',1579,'','Devonian','Upper Devonian','lower Famennian',358.90,372.20,11,'late Famennian - early Visean',351,372,3,0,'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,'','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),('Rainbow Field, Alberta',1580,'Keg River','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','240',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',2,'Actual reservoir',968,969,'Pinnacle reef with stromatopores and corals. Basinward of Presqu\'ile reef.\nUpper Keg River Fm.\nAtoll reef\nVery diverse porosity types.\n240 m thick.\n7.2 % avg. porosity.',58,-119,-648768,-4435111,'Canada','North America',121,'704, 917, 1395',58.5,-119,'','',-5.11189738924,-61.0779291501,-5.11189738924,-61.0779291501,-0.25139790289,-119.889261161),('Shekilie Basin, Alberta',1581,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',970,917,'Pinnacle reef.',59,-119,-572007,-4379833,'Canada','North America',121,'',59.25,-119.25,'','',-4.52345512057,-60.5935844291,-4.52345512057,-60.5935844291,0.418228925565,-119.527599713),('Zama Basin, Alberta',1582,'Keg River','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','120',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','3','High production of reefal debris','0','',2,'Actual reservoir',970,917,'Keg River + Zama Members of Upper Elk Point Group.\nStromatopore-coral rudstones and reef detritus grainstone.\n120 m thick pinnacle reef within intrashelf basin.\n7.2 % avg. porosity.\n',59,-118,-611336,-4365771,'Canada','North America',121,'1395',59.1667,-118.6667,'','',-4.80338089815,-60.459940374,-4.80338089815,-60.459940374,0.168729116929,-119.343610948),('Allan, Saskatoon, Saskatchewan',1583,'Prairie Evaporite','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'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,'','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),('Bell Creek, N.W.T.',1584,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','217',NULL,NULL,NULL,'4','More than 1000 m',NULL,'42',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',972,917,'Platform reef complex of atoll type.\n217 m maximum thickness.',65,-129,398092,-4104152,'Canada','North America',121,'',65.25,-129,'','',2.68082207475,-58.4833965408,2.68082207475,-58.4833965408,7.89133466354,-118.817997474),('Goose River, Alberta',1585,'Beaverhill Lake','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'13',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',973,917,'',54,-116,-1101106,-4652962,'Canada','North America',121,'',54.7833,-116.7,'','',-8.53193137613,-63.0186558234,-8.53193137613,-63.0186558234,-3.97827736717,-121.122847308),('Columbus, Indiana',1586,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'Outcropping reef ',1,'True reef','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','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',974,0,'Calcitic bioherm surrounded by dolomite.\nOnondaga group.\nLayered stromatopores interpreted as shallowest deposits. Coral-foram layer as deeper.',39,-82,-5348752,-2889485,'United States','North America',101,'',39.1333,-82.2333,'','',-34.5033043584,-51.3192206619,-34.5033043584,-51.3192206619,-27.672597582,-105.345426402),('Langenaubach-Breitscheid',1587,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'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','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',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',975,0,'Atoll-type situated on volcanic swell.',50,8,-2493507,710402,'Germany','Europe',331,'',50.65,8.2,'','',-21.1385380717,-9.96574733569,-21.1385380717,-9.96574733569,-1.05845842411,-66.5117961902),('Ferques, Boulonnais',1588,'Blacourt','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'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,'','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),('Conley Field, Texas',1589,'','Carboniferous','Lower Carboniferous','Meramecian',336.00,345.00,12,'middle Visean - Serpukhovian',329,337,2,1,'Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'2',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','13','Echinoderms','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,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',978,0,'Crinoid-bryozoan-spicule sand piles rather than Waulsortian mounds.',34,-99,-1424563,-4414334,'United States','North America',101,'',34.2167,-99.6167,'','',-22.4667973767,-57.8650772103,-22.9123474399,-59.160957196,-8.90558593112,-86.5754054108),('Gaudernbach-Wirbelau',1590,'','Devonian','Upper Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'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','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',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',979,1029,'Plenty of fore reef debris according to ref.\n1025.\n\nAbstract of ref. 979:\nCarbonate rocks of the central Lahn (Germany) syncline were examined and sampled. In general, the development of biostromes begins in the Middle varcus zone of the conodont biostratigraphy after the interruption of the volcanic activity of the Givetian/Adorfian phase. Dendroid stromatoporoids and tabulate corals and sponges or platy stromatoporoids and rugose corals settle on top of the pyroclastic sediments resulting in a stabilisation of the substrate, depending on the bathymetric position. In favoured ecologic positions bioherms could develop, whereas deeper situated biostromes were buried by pyroclastics during the revived volcanism. Allochthonous carbonates are derived from reefs persisting into the Adorf-Stage of the Late Devonian. ',50,8,-2513233,722557,'Germany','Europe',331,'',50.4667,8.2167,'WAHR','77748',-19.2223432797,-10.9109070155,-19.2223432797,-10.9109070155,-1.3062777761,-67.3512159683),('Werdohl and Bredenbruch',1591,'Unterhonsel','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'80','0','20',0,'no',0,'no','3','25 or more reef building species','38','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',980,915,'Rugose and tabulate corals dominate. Rare stromatopores and bryozoans.\nData in Paleobiology Database from Maz (1992). His loc. 6 (Brook in the Laeger). Here stromatoporoids prevail.',51,7,-2444749,649991,'Germany','Europe',331,'1491',51.25,7.8,'WAHR','25369',-15.8625505153,-14.5961480159,-15.8625505153,-14.5961480159,0.0613671208509,-71.2067379513),('Judy Creek, Swan Hills, Alberta',1592,'','Devonian','Middle Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,3,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','66',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present','3','Pronounced zonation','3','Pronounced zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',981,917,'Mostly Amphipora and tabular stromatopores. Some corals and algae.\n66 m thick.\n\n9 % avg. porosity.',54,-115,-1193680,-4626016,'Canada','North America',121,'1283, 1396',54.5,-115.5833,'','',-7.72062676332,-59.1140548038,-7.72062676332,-59.1140548038,-2.49006147161,-117.867065747),('Wyckoff Field, Jasper, Steuben Co., New York',1593,'Onondaga','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','70',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','13','Echinoderms','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',2,'Actual reservoir',982,1710,'70 m thick rugose coral-crinoid pinnacle reef with primary porosity preserved (4-5 %).',42,-77,-5127296,-2405211,'United States','North America',101,'',42.1,-77.5167,'','',-32.037795003,-46.6047867548,-32.037795003,-46.6047867548,-24.6746888929,-101.386138),('Cyclone Field, McKean Co., Pennsylvania',1594,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','60',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','7','Bryozoans','53','Echinoderms - bryozoans - tabulate corals - (lithistids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',982,0,'60 m thick bioherm with primary porosity.\nRugose corals.',41,-78,-5128534,-2528810,'United States','North America',101,'',41.8333,-78.8333,'','',-32.2087093493,-47.7856860469,-32.2087093493,-47.7856860469,-24.9797609524,-102.452335734),('Gara Azzel Matti',1595,'','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','1','Corals','3','Microbes','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'','1','Present',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',984,999,'Several mud mounds arranged in parallel ranges (mud ridges).\r\nSome tabulate corals, small rugose corals (some of them with microborings), scarce bryozoans and Receptaculites.\r\nAbundant stromatactis.',25,0,-5591178,1035489,'Algeria','Africa',706,'1097',25.6167,0.9333,'WAHR','81853',-45.7254498652,-4.55232486533,-45.7254498652,-4.55232486533,-50.6926538289,-11.7582146181),('Gouiret es Soud',1596,'','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'15',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','1','Corals','3','Microbes','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'','1','Present',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',984,999,'see reef 1595.',26,1,-5541950,1087320,'Algeria','Africa',706,'1097',26.0833,1.2667,'',NULL,-45.3628901922,-3.9528160141,-45.3628901922,-3.9528160141,-50.7119485038,-10.882854224),('Oued Ouzdaf',1597,'','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','1','Corals','3','Microbes','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'','1','Present',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',984,999,'see reef 1595.',26,1,-5469432,1096012,'Algeria','Africa',706,'1097',26.6667,1.1667,'WAHR','81854',-44.777585679,-3.8449735707,-44.777585679,-3.8449735707,-50.3314169821,-10.173178453),('Jebel Tamamate',1598,'','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','1','Corals','3','Microbes','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',984,999,'see reef 1595.',26,0,-5521077,1034463,'Algeria','Africa',706,'',26.1667,0.75,'',NULL,-45.1512625043,-4.55113153992,-45.1512625043,-4.55113153992,-50.2711855275,-11.1453959148),('Sirte Basin',1599,'Umm ad Dahiy','Paleogene','Oligocene','Rupelian-Chattian',23.00,33.90,30,'Chattian - Aquitanian',22,28,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','10',NULL,NULL,NULL,'4','More than 1000 m',NULL,'20',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'','1','Present','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','1','Low production of reefal debris','0','',2,'Actual reservoir',1991,0,'See reef 1600',29,18,3658810,1592158,'Libya','Africa',715,'',29.75,18.1333,'FALSCH','0',25.6181386297,14.2899903544,25.6204952372,14.2915406433,25.7722777546,17.0551307188),('Sirte Basin',1600,'Umm ad Dahiy','Paleogene','Oligocene','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','10','3','101-1000 m wide',NULL,'4','More than 1000 m','20000',NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species','25',NULL,'','1','Present','1','Present',NULL,'',NULL,'',NULL,'',NULL,'','1','Low production of reefal debris','0','',2,'Actual reservoir',1991,0,'Age given as Rupelian, but many Chattian and lower Miocene corals are also present.\nRupelian age confirmed by Imam and Galmed (2000).\n\nMain reef builders are Stylophora parvistella\nS. thirsiformis\nMadracis decaphylla\nAstraeopora decaphylla\nMonticulastraea ex gr. daedalea\nAthecastraea maradahensis n.sp.\nActincacis rollei\nAgathiphyllia gregaria\n\nIn lower part of reef rim: Astrocoenia, Tarbellastrea, Dictyoastraea, Anisocoenia, A. maradahensis\n\nIn reef slope: M. ex gr. daedalea, Antiguastraea hufrahensis and Madracis decaphylla\n\nAlgal binding probable but obscured by recrystallization of matrix\n\nTaxonomic data in Paleobiology Database\n\nLow production of bioclasts.',29,18,3317917,1528438,'Libya','Africa',715,'',29.75,18.1333,'WAHR','10964',25.2723134456,14.065507699,25.2723134456,14.065507699,25.4202451057,16.9437335163),('Ain el Khira, Cherrat',1601,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',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,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'','2','Medium zonation',NULL,'','2','30-60% micrite',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',985,986,'Stacked biostromes with stromatopores and tabulate corals.',33,-7,-4409359,252537,'Morocco','Africa',714,'',33.8333,-7.0833,'','176103',-35.6943629103,-12.4153451128,-35.6943629103,-12.4153451128,-40.5389850159,-6.63514689304),('Bou Sif, Tiliouine',1602,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'40','1601',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,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',985,986,'see reef 1601.',33,-6,-4485567,320687,'Morocco','Africa',714,'',33.5,-6.1667,'','',-36.3411467957,-11.7673256393,-36.3411467957,-11.7673256393,-41.3657575533,-6.50614794831),('Mzoudia',1603,'','Devonian','Middle Devonian','Givetian?',382.70,387.70,10,'Givetian - early Famennian',375,388,1,0,'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','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',986,987,'',31,-8,-4591300,41794,'Morocco','Africa',714,'',31.8333,-8.3333,'','',-36.9392729739,-14.7549021807,-36.9392729739,-14.7549021807,-40.578833103,-9.60816564749),('Mechra Benabbou, Doukkala',1604,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,1,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',986,987,'Amphipora dominates.',32,-7,-4521097,130014,'Morocco','Africa',714,'',32.6333,-7.8,'','',-36.4644555926,-13.7743484503,-36.4644555926,-13.7743484503,-40.6023848725,-8.39911883089),('Mechra Benabbou II, Doukkala',1605,'','Devonian','Middle Devonian','Emsian-Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,397,1,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',986,987,'',32,-7,-5741070,1072108,'Morocco','Africa',714,'',32.6333,-7.8,'','',-33.8286469055,-12.5030108789,-33.8286469055,-12.5030108789,-31.8490236932,-7.66035984172),('Safi',1606,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',987,986,'',32,-9,-4479855,-17868,'Morocco','Africa',714,'',32.4167,-9.3,'','',-38.1956299148,-16.5788674194,-38.1956299148,-16.5788674194,-42.3736967968,-7.84137142114),('Leimingdong, Lianyuan, Hunan',1607,'Qiziqiao','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','80',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',1,'Potential reservoir',989,1354,'80 m thick stromatoporoid-coral reef.\nFormerly interpreted as biostrome, but ref. 1354 says they are barrier reefs.',27,111,-1551315,10617336,'China','Asia',602,'',27.8333,111.5833,'WAHR','34988',-15.5063515563,85.5683321711,-15.5063515563,85.5683321711,-14.6594241702,106.481164968),('Miaomen and Zhaijian, Guilin, Guangxi',1608,'Yonghsien','Devonian','Upper Devonian','early-middle Famennian',358.90,372.20,10,'Givetian - early Famennian',375,371,3,0,'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,'','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),('Polar Bear Pass, Bathurst Island',1609,'Stuart Bay','Devonian','Lower Devonian','Lochkovian-Pragian',407.60,419.20,8,'middle Pridolian - middle Pragian',412,411,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50','1610',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,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species','16','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',992,1577,'Allochthonous reef blocks.\nStromatopores, corals (mostly Favosites) and microbes-algae.\nLochkovian according to ref. 1577. \n13 stromatoporoid species reported by ref. 1580.',75,-98,-1277277,-2186482,'Canada','North America',121,'1580',75.75,-98.3333,'WAHR','63277',5.01186006178,-65.0846011309,5.01186006178,-65.0846011309,20.0581665729,-123.556169986),('Moses Robinson Riv., Bathurst Island',1610,'','Devonian','Lower Devonian','Pragian',407.60,410.80,8,'middle Pridolian - middle Pragian',412,409,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 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,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',992,0,'Allochthonous reef blocks.',76,-97,-1260407,-2160692,'Canada','North America',121,'',76,-97.9667,'WAHR','63286',4.11920040936,-61.3511185208,4.11920040936,-61.3511185208,19.1568763831,-120.72846752),('Cheyne River N, Bathurst Island',1611,'','Devonian','Lower Devonian','Pragian',407.60,410.80,8,'middle Pridolian - middle Pragian',412,409,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'50','1610',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,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',992,0,'Allochthonous reef blocks.',76,-97,-1236516,-2144099,'Canada','North America',121,'',76.2333,-97.9833,'WAHR','63287',4.33682838501,-61.2667293273,4.33682838501,-61.2667293273,19.3862737547,-120.683253711),('Arnao, Cantabria',1612,'Moniello','Devonian','Lower-Middle Devonian','Emsian-Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,397,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','140',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','0','70',0,'no',0,'no','2','6 to 24 reef building species','20','1','Constructor guild',NULL,'',NULL,'','3','Pronounced zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',993,1680,'140 m thick buildup.\nRugose corals as stabilizers. Then mostly stromatopores with minor tabulate and rugose corals and cyanophyceans. \nSeveral collections of Miller',43,-5,-4750603,2398489,'Spain','Europe',304,'1895',43.5833,-5.9667,'WAHR','5908',-25.50682702,-1.48559637637,-25.50682702,-1.48559637637,-10.3040627955,-21.5420764528),('Coallajú, Cantabria',1613,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','100',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','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',994,0,'Stacked biostromes, bioherms and reefal debris.\nTotal thickness about 100 m.',43,-6,-3447524,1234697,'Spain','Europe',304,'',43.35,-6.0167,'WAHR','80292',-29.1261092016,-1.88535683493,-29.1261092016,-1.88535683493,-8.91193751198,-37.4851355352),('Ghuk',1614,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','4','Stromatoporoids','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',995,0,'',34,64,-3945027,8415500,'Afghanistan','Asia',301,'',34.1667,64.5,'','',-45.7229946861,72.2869037021,-45.7229946861,72.2869037021,-55.365160053,101.16567568),('Rebat-e-Pai',1615,'','Carboniferous','Lower Carboniferous','lower Visean',336.00,346.70,11,'late Famennian - early Visean',351,343,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',995,0,'',34,61,-4663978,6899809,'Afghanistan','Asia',301,'',34,61.5,'','',-61.3072884332,83.3278271723,-61.4784712233,86.2382827496,-40.4297583323,36.4962565567),('Mustoe, Highland Co., Virginia',1616,'Keyser','Devonian','Lower Devonian','Pridolian-Lochkovian',410.80,423.00,8,'middle Pridolian - middle Pragian',412,416,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','9',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',996,1577,'Upper Limestone Member.\n8.8 m thick bioherm overlain by two biostromes (2.3 m and 1.8 m thick, respectively).',38,-79,-6070550,-2470403,'United States','North America',101,'1578',38.3333,-79.65,'WAHR','79380',-31.117196109,-62.2481883352,-31.117196109,-62.2481883352,-16.1535537614,-123.131215973),('Karawanken, Austria',1617,'','Devonian','Lower Devonian','upper Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,398,3,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'15',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,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',998,2078,'Stromatopores and tabulate corals forming only 10-20 % of rock volume.',46,14,-4654520,4012629,'Austria','Europe',301,'',46.4333,14.5,'WAHR','79573',-23.7081192517,18.3062509781,-23.7081192517,18.3062509781,46.4333,14.5),('Karawanken',1618,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'15',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,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',998,0,'',46,14,-3353688,2817319,'Austria','Europe',301,'',46.4333,14.5,'','',-33.0894018983,19.5088637658,-33.0894018983,19.5088637658,46.4333,14.5),('Caunes-Minervois, Montagne Noire',1619,'','Devonian','Lower Devonian','upper Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,399,2,0,'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,'','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),('Mt. Peyroux Nappe, Mont. Noire',1620,'','Devonian','Lower Devonian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,402,2,0,'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,'','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),('Timor Valley, New South Wales',1621,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'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,'','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),('Timor Valley, New South Wales',1622,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'12',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','1','Corals','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1001,0,'see reef 1621.',-31,151,-3601975,15478441,'Australia','Oceania',801,'',-31.4167,151.0833,'','',-26.4452987242,139.976776455,-26.4452987242,139.976776455,-22.9816351518,178.170488605),('Podeni, Cluj',1623,'Girbova de Sus','Neogene','Miocene','lower Badenian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'20',NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','2','Algae','1','Corals','29','Coralline algae only (some corals)','1','Red algae','0','20','80',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1623,1003,'Rhodalgal reefs with some corals.',46,23,6117174,1871579,'Romania','Europe',348,'',46.4333,23.6333,'WAHR','70056',45.6961641973,20.3631408879,45.6957751661,20.3620872535,45.5111765182,18.9383705932),('Bivolare',1624,'','Neogene','Miocene','lower Badenian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','60','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1003,0,'15 m thick, 50 m long.\nRelatively diversified coral fauna, thickly encrusted by red algae.',43,23,5716056,1981481,'Bulgaria','Europe',319,'',43.5,23.5,'WAHR','70048',42.7614467063,20.3964489236,42.7610579308,20.3954389558,42.4835250208,23.066653756),('Okhrid',1625,'','Neogene','Miocene','upper Badenian',13.80,16.00,31,'Burdigalian - Serravallian',14,12,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','15',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','1','Less than 6 reef building species','3','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1003,0,'15 m thick, 100 m long coral reef.\nAlmost only one species (Tarbellastaea conoidea). Reef front is algal ridge.',43,23,5726068,1957027,'Bulgaria','Europe',319,'',43.5833,23.25,'WAHR','70049',42.8375734347,20.1452047995,42.8371827349,20.1441953312,42.5699478068,22.8227468132),('Kazantip, Crimea',1626,'','Neogene','Miocene','Chersonian',9.00,11.00,32,'Tortonian - Gelasian',6,11,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,2,'Cold - water',2,'Shelf or Platform margin','2c','Atoll (circular structure)','2','Below fair weather wave base','7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'30','70','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1003,1412,'Atoll-like bryozoan reef. Some microbes, algae and Spirorbis.\nStrongly dominated by Membranipora lapidosa.\n1.5 X 2.5 km size. Duration of reef growth 1.5 MA.\nSeveral dozens of bryozoan build-ups on Kerch Peninsula and Taman Peninsula.\nHigh porosity.',45,35,5984806,3112082,'Ukraine','Europe',301,'1413',45.4833,35.8833,'','',45.3858365494,33.742387229,45.3784031677,33.6115935043,44.7114160449,35.5316162409),('Taman Peninsula',1627,'','Neogene','Miocene','Chersonian',9.00,11.00,32,'Tortonian - Gelasian',6,11,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'10',NULL,2,'Cold - water',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans',NULL,NULL,NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1003,1413,'',45,36,5946940,3193160,'Russia','Asia',624,'',45.1667,36.6667,'','',45.0856598529,34.5375065335,45.0792362117,34.4073828459,44.3899083534,36.3005224902),('Marmaro, Chios',1628,'','Permian','Middle Permian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,267,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','14','Brachiopods','6','Calcisponges','57','Brachiopods - bryozoans, sponges, corals, Tubiphytes, encrusting forams',NULL,NULL,'80','20','0',0,'no',0,'no','2','6 to 24 reef building species','7','2','Baffler guild',NULL,'',NULL,'','3','Pronounced zonation','2','Medium zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1004,1375,'Almost monospecific Richthofenia assemblage in the reef core.\nOverlying are sponge (calcisponges, silicisponges) limestones.\nRare organisms are bryozoans, corals, encrusting forams and Tubiphytes.',38,26,-1300941,3528070,'Greece','Europe',338,'',38.55,26.05,'WAHR','75028',11.1608557204,40.8805366296,11.1608557204,40.8805366296,6.58007131542,28.8815959171),('Shipukhin, Altai Mts.',1629,'','Devonian','Lower Devonian','Emsian?',393.30,407.60,9,'late Pragian - Eifelian',395,402,1,0,'Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'3',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'50','20','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1005,1006,'Ring-like shape of reef (1.7 x 3.0 km).\nBase with algal bioherms.\nMassive corals, stromatopores, hydroids (Fistulella) and algae as framework builders in\nmain stage.',49,88,6882923,3193764,'Russia','Asia',624,'',49,88,'','',66.5614247041,17.1277975045,66.5614247041,17.1277975045,45.3341998774,8.37299281039),('Vaygach Island',1630,'','Silurian','Upper Silurian','Pridoli-Lochkovian',410.80,423.00,8,'middle Pridolian - middle Pragian',412,416,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m',NULL,'1200',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',661,1662,'Coral-stromatoporid-algal bioherms up to 20 m\nthickness. First reefs on shaly substratum.\nReefal strata extending into Eifelian.',69,60,551285,593328,'Russia','Asia',624,'',69.8333,60.4167,'','',24.950221549,-45.7818793754,24.950221549,-45.7818793754,38.0366510153,-106.206265865),('Sukhoy Nos, Pay Khoy',1631,'','Devonian','Lower Devonian','Emsian-Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,397,1,1,'Seismic data available ',2,'Reef mound','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',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','2','Algae','3','Microbes',NULL,NULL,'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,'','2','30-60% micrite','3','More than 25% sparite',NULL,'','0','',2,'Actual reservoir',661,0,'Estimated thickness 2000 m.\nPredominantly algal limestones containing abundant incrustations and accumulations of black crystalline anthraxolite among columnar calcite.',69,60,1039089,620846,'Russia','Asia',624,'',69.6667,60.5833,'','',18.9017162616,-29.4827952297,18.9017162616,-29.4827952297,28.4866819614,-92.6900697903),('Zelenet Island',1632,'','Silurian','Wenlock','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','400',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',661,0,'Compact coral-stromatoporoid limestones with banks of large bivalves. Abundant black flint inclusions and occasional interbeds of dolomite. \nReef association 400 m thick.',69,59,1211761,-207333,'Russia','Asia',624,'',69.0833,59.4167,'','',14.7294163196,-50.7765747486,14.7294163196,-50.7765747486,14.7294163196,-50.7765747486),('Dolgii Island',1633,'','Silurian','Upper Silurian','Wenlock-Ludlow',423.00,433.40,7,'Wenlock - early Pridoli',425,422,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50','1632',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',661,1674,'See reef 1632 for remarks.',69,59,1208047,-228889,'Russia','Asia',624,'1662',69.25,59.1333,'','',17.8846223236,-50.1618455736,17.8846223236,-50.1618455736,17.8846223236,-50.1618455736),('Mys Belyy Nos, Pay Khoy',1634,'','Silurian','Upper Silurian','Upper Silurian',419.20,423.00,7,'Wenlock - early Pridoli',425,422,1,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'Several hundred m thick reefs with poorly preserved stromatoporoids, corals and brachiopods.',69,60,1273824,-196318,'Russia','Asia',624,'',69.1667,60.7,'','',24.5432814352,-47.2137716295,24.5432814352,-47.2137716295,24.5432814352,-47.2137716295),('Mys Belyy Nos, Pay Khoy',1635,'','Devonian','Lower Devonian','Lower Devonian',393.30,419.20,8,'middle Pridolian - middle Pragian',412,407,1,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','30',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'Reef marble with poorly preserved fauna of Stromatoporoids, corals and brachipods.\n30 m thick.',69,60,560605,667925,'Russia','Asia',624,'',69.1667,60.7,'WAHR','81605',21.8314856856,-38.0477517052,21.8314856856,-38.0477517052,32.4137306568,-98.6203021446),('Bolshaya Synya River, Pechora',1636,'','Silurian','Wenlock','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,426,2,0,'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','2','Shelf/platform margin',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,'','3','More than 60% micrite',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),('Sredne Makarikha, Pechora',1637,'','Silurian','Ludlow','Ludlovian',423.00,427.40,7,'Wenlock - early Pridoli',425,421,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','120',NULL,NULL,NULL,'4','More than 1000 m',NULL,'20',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,0,'Producing reservoir.\n120 m thick reef limestone.',66,58,1051065,33694,'Russia','Asia',624,'',66.6333,58.8333,'','',21.9875048754,-46.0879056988,21.9875048754,-46.0879056988,21.9875048754,-46.0879056988),('Gamburtsev Uplift, Pechora',1638,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'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,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',1008,661,'Coral-stromatoporoid reef belt.\nAround 100 m thick.',67,59,1590260,857163,'Russia','Asia',624,'',67.8333,59.25,'','',8.6319283771,-6.70019973726,8.6319283771,-6.70019973726,27.4445944552,-76.050315875),('Salyuka-Makarikha, Pechora',1639,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'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,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',1008,661,'see reef 1638.',67,59,1563867,929379,'Russia','Asia',624,'',67.1667,59.0833,'','',8.39611674474,-6.06646392652,8.39611674474,-6.06646392652,27.5000715421,-75.2981532813),('Usa-Makarikha, Pechora',1640,'Ukhta','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'Seismic data available ',3,'Mud mound or bank','3','101-500 m thick','250',NULL,NULL,NULL,'4','More than 1000 m',NULL,'800',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp',NULL,'','2','Algae','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','4','Others',NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'Ukhta age.\n250 m thick reef belt, 3-4 km wide.\nComposed of algal thalli.',66,58,1523523,999372,'Russia','Asia',624,'',66.5,58.6667,'','',8.05990462415,-5.46165062078,8.05990462415,-5.46165062078,27.4496392863,-74.5264204842),('Bagan, Pechora',1641,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'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,'','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,'','3','More than 60% micrite',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),('South Kharyakha, Pechora',1642,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'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,'','3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',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),('Kharyakha, Pechora',1643,'','Devonian','Upper Devonian','upper? Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,376,3,1,'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,'','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,'','3','More than 60% micrite',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),('Komandirshor, Pechora',1644,'Ukhta','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'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,'','3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',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),('Layavozh, Pechora',1645,'Sirachoy','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','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,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'Sirachoy age.\nAbout 100 m thick coral-stromatoporoid reef.',67,55,1375384,847521,'Russia','Asia',624,'',67.5833,55.1333,'','',7.06551824517,-6.91751840152,7.06551824517,-6.91751840152,25.9369320003,-75.5170927514),('Vasilkov, Pechora',1646,'Semiluki-Burega','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'700',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'Semiluki-Burega time.',68,54,1341422,789935,'Russia','Asia',624,'1662',68.0167,54.1333,'','',6.85157337309,-7.45515560029,6.85157337309,-7.45515560029,25.515508516,-75.9512636056),('South Shapkina, Pechora',1647,'Semiluki-Burega','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'700','1646',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'Semiluki-Burega.',67,54,1327139,875879,'Russia','Asia',624,'',67.25,54.4167,'','',6.69621193271,-6.69132571688,6.69621193271,-6.69132571688,25.6980993437,-75.1169051546),('Grubeshor, Pechora',1648,'Sirachoy','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1000',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'Sirachoy time.\nCoral-stromatoporoid reef.',67,54,1344096,893087,'Russia','Asia',624,'',67.1333,54.8333,'','',6.81002054835,-6.52663845049,6.81002054835,-6.52663845049,25.870477348,-75.005930927),('Yuryakha, Pechora',1649,'Ukhta','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'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,'','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,'','3','More than 60% micrite',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),('Sredne Shapkina, Pechora',1650,'Semiluki-Burega','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'700','1646',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'',66,54,1289383,945027,'Russia','Asia',624,'',66.5833,54.1667,'','',6.37975537971,-6.09249376992,6.37975537971,-6.09249376992,25.6621725871,-74.3702480337),('Mutnyy Materik, Pechora',1651,'','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick',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,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'Sirachoy and Semiluki(?) times.',65,55,1315078,1022199,'Russia','Asia',624,'',65.9667,55.0833,'','',6.52262476536,-5.38389945984,6.52262476536,-5.38389945984,26.0864439032,-73.7258419647),('Terekhevey, Pechora',1652,'Sirachoy?','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'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,'','3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',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),('East Luza, Pechora',1653,'Sirachoy','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,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,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'Sirachoy time.\nCoral-stromatoporoid reef.',65,55,1314859,1126382,'Russia','Asia',624,'',65.0667,55.6667,'','',6.46110669195,-4.44803134231,6.46110669195,-4.44803134231,26.4154983688,-72.7537049481),('Sebys, Pechora',1654,'Semiluki-Burega','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'700','1646',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'Semiluki-Burega time.',64,54,1244544,1186946,'Russia','Asia',624,'',64.4167,54.8333,'','',5.91313431821,-3.94644510028,5.91313431821,-3.94644510028,26.1196066884,-71.9962294496),('Yedzhidkyrta, Pechora',1655,'','Devonian','Upper Devonian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,369,1,1,'Seismic data available ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'80','1065',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',1008,661,'',64,57,2225404,1830151,'Russia','Asia',624,'',64.0833,57.9167,'','',-4.2643922063,5.83843493461,-4.2643922063,5.83843493461,28.807122399,-61.0172297264),('Kozlanyur, Pechora',1656,'','Devonian','Upper Devonian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,369,1,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'80','1065',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',1008,661,'',64,57,2193864,1829505,'Russia','Asia',624,'',64,57.4167,'','',-4.49827994206,5.8268145117,-4.49827994206,5.8268145117,28.5853662359,-60.9314479663),('Lebyazh, Pechora',1657,'','Devonian','Upper Devonian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,369,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'80','1065',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1008,661,'',63,57,2193513,1839794,'Russia','Asia',624,'',63.9167,57.5,'','',-4.49852579609,5.91806948849,-4.49852579609,5.91806948849,28.6185271746,-60.8349577957),('Vuktyl, Pechora',1658,'','Devonian','Upper Devonian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,369,1,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',1008,661,'',63,57,2174879,1854016,'Russia','Asia',624,'',63.75,57.3333,'','',-4.63324237387,6.04111516099,-4.63324237387,6.04111516099,28.5380126086,-60.6488505812),('E Savinobor, Timan',1659,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'250',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','1','Present',2,'Actual reservoir',661,1008,'Askyn zone.',63,56,1305090,1299758,'Russia','Asia',624,'',63.55,56.4167,'','',6.29202500062,-2.89654246907,6.29202500062,-2.89654246907,26.8886056618,-71.1008455254),('Dzhyer, Timan',1660,'Ukhta','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'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,'','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,'','3','More than 60% micrite',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),('South Pashnya, Timan',1661,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,1,1,'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,'','3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',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),('Omra-Soyva, Timan',1662,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'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,'','3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',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),('Voyvozh, Timan',1663,'Sirachoy','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,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,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'Sirachoy time barrier reef.',62,55,1204592,1348612,'Russia','Asia',624,'',62.95,55.0833,'','',5.53105835633,-2.51894111673,5.53105835633,-2.51894111673,26.3415027785,-70.3752497284),('Nibel, Timan',1664,'Ukhta','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'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,'','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,'','3','More than 60% micrite',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),('Izkos, Timan',1665,'Sirachoy','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,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,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,1008,'',62,54,1182125,1366977,'Russia','Asia',624,'',62.75,54.8333,'','',5.35688072495,-2.36767219924,5.35688072495,-2.36767219924,26.2414556351,-70.143946012),('Charajha, Pechora',1666,'','Devonian','Upper Devonian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,369,2,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',1010,0,'',66,56,2303294,1566381,'Russia','Asia',624,'',66.4167,56.8333,'','',-3.72881612218,3.51691956745,-3.72881612218,3.51691956745,28.4229008315,-63.6893968793),('Ilych, Timan',1667,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,1,0,'Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'200',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',1,'Potential reservoir',661,0,'',62,56,1299427,1419856,'Russia','Asia',624,'',62.5,56.9167,'','',6.18434760098,-1.82137938756,6.18434760098,-1.82137938756,27.2165460348,-69.9522457816),('Pachga, Timan',1668,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,1,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'200','1667',0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,0,'',61,57,1294964,1505491,'Russia','Asia',624,'',61.75,57.25,'','',6.10516485837,-1.05506460767,6.10516485837,-1.05506460767,27.4436225934,-69.1287358602),('Garevskiy, Timan',1669,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,1,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'200','1667',0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,0,'',61,57,1286367,1551920,'Russia','Asia',624,'',61.3333,57.3333,'','',6.01736171319,-0.643489875462,6.01736171319,-0.643489875462,27.5223101801,-68.6653137863),('Gadinskiy, Timan',1670,'','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,1,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'200','1667',0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,0,'',61,57,1283378,1580168,'Russia','Asia',624,'',61.0833,57.4167,'','',5.98044346529,-0.391610137503,5.98044346529,-0.391610137503,27.5853812437,-68.3887156724),('Sredne Makarikha well',1671,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'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',NULL,NULL,NULL,NULL,'2','Below fair weather wave base','3','Microbes','2','Algae',NULL,NULL,'2','Green algae','0','100','0',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',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),('Shapkina well, Pechora',1672,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'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',NULL,NULL,NULL,NULL,'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,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',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),('Shapkina well II, Pechora',1673,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'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',NULL,NULL,NULL,NULL,'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,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',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),('Khosedayu, Sorokin Arch',1674,'','Carboniferous','Upper Carboniferous','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,309,2,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1011,661,'',67,59,4045960,3085338,'Russia','Asia',624,'',67.0833,59.1667,'','',26.1327963641,25.7904884835,26.1327963641,25.7904884835,29.8299374604,0.948818828882),('Varandey, Sorokin Arch',1675,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','2','Algae','2','Algae',NULL,NULL,'2','Green algae','0','100','0',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',661,3,'About 100 m thickness of reef structures\n(seismic).',68,58,4801773,3185284,'Russia','Asia',624,'',68.8333,58,'','',33.8067761108,31.3293590769,33.8067761108,31.3293590769,36.4448430691,2.45884600383),('Varandey II, Sorokin Arch',1676,'','Permian','Lower Permian','Sakmarian/Artinskian',283.50,298.90,15,'Sakmarian - Kungurian',277,284,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','2','Algae','2','Algae',NULL,NULL,'4','Others','0','100','0',0,'no',0,'no',NULL,'',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',1,'Potential reservoir',661,0,'',68,58,5362468,3466575,'Russia','Asia',624,'',68.8333,58,'','',34.2214155176,31.8496072994,34.2214155176,31.8496072994,38.0391353766,7.39175363688),('South Khyl\'chuyu, Pechora',1677,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',661,0,'',68,55,4632829,3208363,'Russia','Asia',624,'',68.0833,55,'','',32.4758033775,31.2557350061,32.4758033775,31.2557350061,35.2043901307,3.05874371069),('South Khyl\'chuyu, Pechora',1678,'','Carboniferous','Upper Carboniferous','Pennsylvanian',298.90,323.20,13,'Bashkirian - Kasimovian',302,303,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',661,0,'',68,55,3950185,2896452,'Russia','Asia',624,'',68.0833,55,'','',25.370990369,23.9499616378,25.370990369,23.9499616378,28.6353548056,-0.659571342296),('South Khyl\'chuyu, Pechora',1679,'','Carboniferous','Lower Carboniferous','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,324,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',661,0,'',68,55,3054492,2103892,'Russia','Asia',624,'',68.0833,55,'','',7.09852842435,14.3438954798,7.09852842435,14.3438954798,23.1950344773,-10.2807127207),('Korova, Shapkina-Yur\'yakha Arch',1680,'','Carboniferous','Lower Carboniferous','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,324,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',1011,661,'',68,53,2996772,2041297,'Russia','Asia',624,'',68.3333,53.1667,'','',6.65965708371,13.762617317,6.65965708371,13.762617317,22.6102219923,-10.745918785),('Korova, Shapkina-Yur\'yakha Arch',1681,'','Carboniferous','Upper Carboniferous','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,309,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',661,0,'',68,53,3898736,2832093,'Russia','Asia',624,'',68.3333,53.1667,'','',24.9025577675,23.258442992,24.9025577675,23.258442992,28.0110379263,-1.16605714741),('Korova, Shapkina-Yur\'yakha Arch',1682,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150',NULL,1,'Temperate',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',661,0,'',68,53,4586425,3141962,'Russia','Asia',624,'',68.3333,53.1667,'','',32.1034029819,30.5198749579,32.1034029819,30.5198749579,34.612500558,2.54816929744),('Khosedayu, Sorokin Arch',1683,'','Carboniferous','Lower Carboniferous','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,324,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1011,661,'',67,59,3167801,2287195,'Russia','Asia',624,'',67.0833,59.1667,'','',7.97625733511,16.0173310422,7.97625733511,16.0173310422,24.5024458599,-8.80838669547),('Vozey, South Kolva Arch',1684,'','Carboniferous','Lower Carboniferous','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,324,1,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',661,0,'',66,57,3030661,2306403,'Russia','Asia',624,'',66.5,57,'','',6.94654173817,16.1118992981,6.94654173817,16.1118992981,23.5385007787,-8.39886089123),('Vozey, South Kolva Arch',1685,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,1,1,'Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',1,'Potential reservoir',661,0,'',66,57,4583337,3423452,'Russia','Asia',624,'',66.5,57,'','',32.1127528703,33.294640756,32.1127528703,33.294640756,35.5678237592,5.17270440401),('Northern Novaya Zemlya',1686,'','Silurian','Upper Silurian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,418,1,0,'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,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,1536,'',76,66,1801209,-930855,'Russia','Asia',624,'',76.6667,66,'WAHR','23637',24.5409251037,-56.4384649458,24.5409251037,-56.4384649458,24.5409251037,-56.4384649458),('Northern Novaya Zemlya II',1687,'','Silurian','Upper Silurian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,418,1,0,'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,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'',76,68,1884652,-921623,'Russia','Asia',624,'',76.75,68.6667,'','',25.1265023829,-56.6584484453,25.1265023829,-56.6584484453,25.1265023829,-56.6584484453),('Off northern Novaya Zemlya',1688,'','Silurian','Upper Silurian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,418,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'',76,63,1724265,-931544,'Russia','Asia',624,'',76.5,63.6667,'','',24.0303832863,-56.1692924068,24.0303832863,-56.1692924068,24.0303832863,-56.1692924068),('Off northern Novaya Zemlya II',1689,'','Silurian','','Silurian',419.20,443.40,7,'Wenlock - early Pridoli',425,422,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'',77,64,1792586,-1069512,'Russia','Asia',624,'',77.8333,64.1667,'','',15.2521540671,-60.0092783751,15.2521540671,-60.0092783751,15.2521540671,-60.0092783751),('Off northern Novaya Zemlya III',1690,'','Silurian','Upper Silurian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,418,1,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'',77,59,1644875,-1085471,'Russia','Asia',624,'',77.5833,59.1667,'','',22.9243262631,-57.2409901798,22.9243262631,-57.2409901798,22.9243262631,-57.2409901798),('Novaya Zemlya',1691,'','Devonian','Upper Devonian','Upper Devonian',358.90,378.00,10,'Givetian - early Famennian',375,384,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'220','1695',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'',75,61,1868358,20570,'Russia','Asia',624,'',75.5,61.9167,'','',1.25348604588,-4.25142491185,3.70384373044,-6.73203591078,29.9416526379,-76.7290682786),('Novaya Zemlya II',1692,'','Devonian','Upper Devonian','Upper Devonian',358.90,378.00,10,'Givetian - early Famennian',375,384,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'220','1695',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'',75,60,1796212,69014,'Russia','Asia',624,'',75,60.0833,'','',0.639444438116,-3.95011073261,3.1012665821,-6.40786989517,29.5994806609,-76.0467950437),('Novaya Zemlya III',1693,'','Devonian','','Devonian',359.00,419.20,10,'Givetian - early Famennian',375,385,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'220','1695',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'',74,58,1740912,118359,'Russia','Asia',624,'',74.5,58.8333,'','',15.9490887958,-25.2815779215,15.9490887958,-25.2815779215,26.197445285,-93.1860349699),('Novaya Zemlya IV',1694,'','Devonian','','Devonian',359.00,419.20,10,'Givetian - early Famennian',375,385,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'220','1695',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'',74,57,1693395,149089,'Russia','Asia',624,'',74.1667,57.75,'','',15.6332709569,-24.9580600125,15.6332709569,-24.9580600125,26.076111852,-92.7109169362),('Novaya Zemlya V',1695,'','Devonian','','Devonian',359.00,419.20,10,'Givetian - early Famennian',375,385,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'220',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',661,0,'',73,56,1648112,189183,'Russia','Asia',624,'',73.75,56.8333,'','',15.3432435613,-24.5512653147,15.3432435613,-24.5512653147,26.0159520165,-92.1722961661),('Chelnin, Kuybyshev',1696,'','Devonian','Upper Devonian','upper Famennian',358.90,372.20,11,'late Famennian - early Visean',351,363,2,1,'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',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1012,0,'',55,77,3602856,5312641,'Russia','Asia',624,'',55.5,77.5,'','',16.0307654462,39.9428322205,16.0307654462,39.9428322205,33.346335863,0.441777355454),('Zapadno Teplov',1697,'','Carboniferous','Middle Carboniferous','Middle Carboniferous',315.20,323.20,13,'Bashkirian - Kasimovian',302,318,1,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,1,'Temperate',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'','7','Bryozoans','7','Bryozoans',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1013,0,'',51,51,2334662,4411280,'Kazakhstan','Asia',301,'',51.5,51.3333,'','',6.23086143512,31.0632468689,6.23086143512,31.0632468689,11.6837046788,15.2599286371),('Sol\'Iletsa, Peri-Caspian',1698,'','Permian','Lower Permian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,289,2,1,'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','2','Shelf/platform margin',NULL,'','7','Bryozoans','7','Bryozoans',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1013,0,'',51,55,3625851,5252395,'Russia','Asia',624,'',51.1667,55,'','',21.4479126442,45.7915154826,21.4479126442,45.7915154826,30.5907218612,25.9162956914),('Kyzyl-Kjuchevskij',1699,'','Devonian','Upper Devonian','Famennian-Tournaisian',346.70,372.20,11,'late Famennian - early Visean',351,360,2,1,'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,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',19,0,'',55,54,1484579,2651761,'Russia','Asia',624,'',55.3333,54.6667,'','',-13.6300313287,15.6608038524,-13.6300313287,15.6608038524,25.4684426665,-44.324735949),('Yanshan, Guilin, Guangxi',1700,'Donggangling','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','135',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'20','20','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'','1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1014,1866,'Fringing reef. Reef outcrop 2 x 1.6 km.\nGivetian based of Stringocephalus.\n135 m thick reef facies. Reef core 18-20 m.\n2 reef cycles.\nTabular and encrusting stromatopores, bryozoans, Chaetetes, corals.\nBorings by algae.\nChaetetid-stromatoporoid framestone with 70-80 % coverage. ',25,110,-1202571,10733097,'China','Asia',602,'',25.5,110.25,'WAHR','34889',-12.9196721746,85.9970043044,-12.9196721746,85.9970043044,-15.1906441349,109.136178495),('Piatra, Dobrogea',1701,'','Jurassic','Upper Jurassic','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,157,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'20',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','19','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1015,2351,'Coral framestone only at base.\nPlenty of debris.\nBoring lithophagid bivalves dominant.\nBacinella and boring forams present.\nSolenopora, Bacinella, Lithocodium as secondary frame builders.\n16 species of corals described in Roniewicz (1976)',44,28,4776828,2255375,'Romania','Europe',348,'',44.3333,28.6667,'WAHR','35183',28.6780417241,41.6692761428,28.6780417241,41.6692761428,34.272252514,43.9589258598),('Cheia Valley, Dobrogea',1702,'','Jurassic','Upper Jurassic','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,157,2,0,'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,'','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),('Cekirgeaua Valley (Topalu), Dobrogea',1703,'','Jurassic','Upper Jurassic','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,157,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','11','Siliceous sponges','9','Tubiphytes','33','Siliceous sponges - microbes - (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,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1015,2351,'Siliceous sponges and Tubiphytes beds and\nthromolithes interbedded.\nInterpreted as distal ramp.',44,28,4809749,2202208,'Romania','Europe',348,'',44.55,28.0667,'','',28.7021803549,41.1227129515,28.7021803549,41.1227129515,34.3279241877,43.3817183156),('Potoczek',1704,'','Neogene','Miocene','Sarmatian',11.60,12.70,31,'Burdigalian - Serravallian',14,12,3,0,'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,'','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),('Lysakow',1705,'','Neogene','Miocene','Sarmatian',11.60,12.70,31,'Burdigalian - Serravallian',14,12,3,0,'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,'','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),('Arachowa',1706,'','Cretaceous','Lower Cretaceous','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,123,3,0,'Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','5','Rudists','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'10','90','0',0,'no',0,'no','3','25 or more reef building species','51','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1016,0,'Reefal blocks (olistolithes) from the Pelagonikum.\n43 Genera of scleractinian corals, 6 rudist genera, stromatoporoids and lithistid sponges associated.',38,22,2278362,1871319,'Greece','Europe',338,'',38.4167,22.6167,'WAHR','34719',14.5308996042,25.2015435118,13.4267942561,25.2204683295,16.9654866245,24.5639292602),('Pollanten',1707,'','Jurassic','Upper Jurassic','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,156,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'50',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','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,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1017,0,'',49,11,4945924,1253043,'Germany','Europe',331,'',49.15,11.5,'WAHR','68549',29.0668201519,27.5209007917,29.0668201519,27.5209007917,35.1109231192,28.5602987677),('Mt. Ashibetsudake, Hokkaido',1708,'','Cretaceous','Lower Cretaceous','upper Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,113,3,0,'Outcropping reef ',4,'Biostrome','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','1','Corals','5','Rudists','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'20','70','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1018,0,'Coral-rudist-stromatolite wackestone.\n\nAbstract of ref. 1018:\nCarbonate blocks of late Aptian (Lower Cretaceous) age occur in the Lower Yezo Group of central Hokkaido in northeast Japan. The shallow-water carbonates were emplaced by gravity sliding and rock fall into a deep-water flysch basin. Various lithofacies can be distinguished within the blocks including massive wackestone, bedded packstone and micro-oncoid grainstone, containing corals, rudists, an oyster, gastropods, calcareous algae and an orbitolinid foraminifer. \n\nFacies and palaeoecological analyses suggest deposition of low-energy biostromes and sand banks in open lagoonal and restricted environments with local higher-energy shoals and beaches. The presence of calcareous sandstones and abundant insoluble residues in limestones suggest deposition in an attached carbonate platform close to a supply of terrigenous material, rather than deposition upon seamounts within an oceanic setting. A narrow rimmed shelf in tropical--subtropical conditions would have been the depositional environment for these carbonates, which were subsequently deformed into blocks and transported into deep water as a result of the tectonic collapse of the platform. ',43,142,4755462,14675939,'Japan','Asia',625,'',43.2042,142.2167,'WAHR','49990',60.585116288,161.806571917,60.585116288,161.806571917,57.2211799771,160.536972869),('Furano, Hokkaido',1709,'','Cretaceous','Lower Cretaceous','upper Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,113,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1018,0,'Toucasia (requienid rudist) wackestone.\n\nSee also reef 1708',43,142,4778197,14665183,'Japan','Asia',625,'',43.3667,142.3333,'','',60.7503668681,161.968635905,60.7503668681,161.968635905,57.383003535,160.69646914),('Horni Benesov',1710,'','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1019,0,'',49,17,-3588158,3967349,'Czech Republic','Europe',331,'',49.9333,17.6,'WAHR','77037',-18.9634942265,11.6227807758,-18.9634942265,11.6227807758,6.07611824136,-70.4129728393),('Horni Benesov',1711,'','Devonian','Middle Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1019,0,'Diverse tabulate and rugose corals.\nStromatopores not described.',49,17,-2109617,2583935,'Czech Republic','Europe',331,'',49.9333,17.6,'WAHR','77034',-22.3828977092,11.9105705101,-22.3828977092,11.9105705101,3.52696551619,-63.7506647557),('Tishkin-Glubokin',1712,'','Carboniferous','Middle Carboniferous','Serpukhovian-Bashkirian',315.20,330.90,12,'middle Visean - Serpukhovian',329,318,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','210',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1020,0,'Described as barrier reef complex.\nWidth 10-16 km, thickness 170-210 m.\nOil bearing.',48,40,553602,3335660,'Russia','Asia',624,'',48.5,40.3333,'','',-5.7671793586,26.6794835155,-5.7671793586,26.6794835155,5.39124122335,10.383713218),('Kokhanovka, Lvov',1713,'','Jurassic','Upper Jurassic','Kimmeridgian-Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,150,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1021,1424,'',49,23,5329949,2086084,'Ukraine','Europe',301,'',49.9167,23.5,'','',33.6430256912,32.6308431289,33.6430256912,32.6308431289,38.1751324507,35.6848690389),('Letnya, Lvov, U',1714,'','Jurassic','Upper Jurassic','Kimmeridgian-Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,150,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250','1713',0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1021,1424,'See reef 2167',49,23,5280138,2139065,'Ukraine','Europe',301,'1348',49.4167,23.8333,'','',33.2702626001,33.1066514609,33.2702626001,33.1066514609,37.7656968214,36.1402946699),('Gorokhov',1715,'','Silurian','Upper Silurian','Upper Silurian',419.20,423.00,7,'Wenlock - early Pridoli',425,422,2,1,'Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',1021,0,'',50,24,-2157525,146052,'Ukraine','Europe',301,'',50.5,24.6667,'','',2.74388426071,-33.9123412038,2.74388426071,-33.9123412038,2.74388426071,-33.9123412038),('Bol\'shaya Kos\'yu, Urals',1716,'','Ordovician','Upper Ordovician','upper Ashgillian',445.20,450.00,5,'Darriwilian - Ashgillian',452,445,3,0,'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,'','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),('Bad\'ya, Kozhym River, Polar Urals',1717,'','Ordovician','Upper Ordovician','upper Ashgillian',445.20,450.00,5,'Darriwilian - Ashgillian',452,445,3,0,'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,'','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),('Lec-Elec River, Polar Urals',1718,'','Ordovician','Upper Ordovician','Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,2,0,'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,'','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),('Elusive Mound, Dry Canyon, New Mexico',1719,'','Carboniferous','Lower Carboniferous','upper Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,347,3,0,'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,'','3','More than 60% micrite','1','Less than 10% sparite',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),('Artavaggio, Southern Alps',1720,'Dolomia Principale','Triassic','Upper Triassic','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,205,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 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','8','Serpulids, worms, vermetids','3','Microbes','11','Serpulids - algae - microbes',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',1027,0,'Serpulids, microbes, sessil forams, calicsponges(?). Some dasycladaceans.\nSmall patch reefs as olistolithes.\n\nIncludes Riva di Solto shale\n\nAbstract of ref. 1027:\nThe development of peculiar margin facies and abundant talus breccias within the Dolomia Principale inner platform is commonly observed in the Lombardy Basin during the Norian. The organisms building these margins are mainly serpulids, benthic microbes, subordinate porostromata and other encrusting forms; typical margin organisms, as sponges or\ncorals, are extremely rare or absent. The build-ups form narrow rims along the borders of tectonic-controlled intraplatform basins. Regional back-stepping and progradation of the margin facies on the talus breccias produced by the erosion of the reef is commonly observed in the uppermost Dolomia Principale depositional system. Widespread occurrence of serpulids\nand microbial margins in middle-late Norian times is indicative of stressed environmental conditions - fluctuation of salinity and temperature on the inner platform and in the intraplatform basins - controlled by palaeogeographic setting. Physical characteristics allowed the bloom of forms able to develop in a wide range of environmental conditions, such as serpulids.\nIn the Late Norian, major input of fine-grained clastics is recorded. Close to the Norian-Rhaetian boundary, carbonate ramps were regionally restored. Locally, small serpulid and microbial bioconstructions still persist in the lowermost part of the shaly succession, even if they are less abundant with respect to the Dolomia Principale. Patch-reefs generally do not build a platform margin, but represent isolated mounds within shaly deposits. These build-ups occur on the edge of former structural highs; the communities survived the environmental change responsible for the siliciclastic input and locally managed to produce mounds during the deposition of the lower part of the upper depositional system (Riva di Solto Shale).',45,9,2936076,1581750,'Italy','Europe',344,'',45.9417,9.5722,'WAHR','67729',21.4140088421,28.7685527937,24.1848066675,27.7415155236,21.3290639828,22.870040792),('Vello, Southern Alps',1721,'','Triassic','Upper Triassic','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,205,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'50','1720',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','8','Serpulids, worms, vermetids','3','Microbes','11','Serpulids - algae - microbes',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1027,0,'see reef 1720 for remarks.',45,10,2888155,1604473,'Italy','Europe',344,'',45.7583,10.0833,'WAHR','67727',21.019544782,28.8426370848,23.7936536892,27.8354866155,20.9487065546,23.0043795656),('Takachiho, Kyushu',1722,'','Triassic','Lower Triassic','Griesbachian',251.80,252.20,17,'Induan - early Carnian',235,250,3,0,'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,'','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),('Villmar, Lahnmulde',1723,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1029,2646,'Reef-fringed volcanic island',50,8,-2526797,725564,'Germany','Europe',331,'',50.3667,8.1667,'WAHR','75570',-16.4408429286,-13.8603574412,-16.4408429286,-13.8603574412,-0.205550024987,-70.333430086),('Kerpen',1724,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1029,1371,'Stromatopores and tabulate corals.\nRugose corals in nearby Korea quarry.',50,6,-2599310,640154,'Germany','Europe',331,'',50.3167,6.7333,'','',-17.0139554369,-14.6067074428,-17.0139554369,-14.6067074428,-1.00701512688,-70.7773044443),('Operich, Büdesheim',1725,'','Devonian','Upper Devonian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,3,0,'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',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',915,1029,'',50,6,-2619042,634596,'Germany','Europe',331,'',50.2167,6.55,'WAHR','82565',-19.9812117993,-11.7454213588,-19.9812117993,-11.7454213588,-2.31482400242,-67.7718322167),('Arnegg',1726,'','Jurassic','Upper Jurassic','lower Tithonian',145.00,152.10,21,'late Bathonian - early Tithonian',151,149,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','60','2','10 - 100 m wide','250','3','More than 100 m','800',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)',NULL,NULL,'0','90','10',0,'no',0,'no','3','25 or more reef building species','35','1','Constructor guild','1','Present','1','Present','2','Medium zonation',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1030,1029,'Malm zeta\nSiliceous sponges and corals (Thecosmilia, Enallthelia, Thamnasteria).\nDebris rich in crusts and Tubiphytes.\nIncluded in collections are also data from Blumenthau (Bermaringen): Coll. 23903',48,9,4815990,1161171,'Germany','Europe',331,'2266',48.3833,9.85,'WAHR','23887',29.4324727422,23.2889056116,29.4324727422,23.2889056116,34.6436478521,25.1895997186),('Klingenhalde, Gosheim',1727,'','Jurassic','Upper Jurassic','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,157,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','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,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1029,0,'',48,8,4763072,1085678,'Germany','Europe',331,'',48.15,8.7333,'','',27.5556968848,25.8918194128,27.5556968848,25.8918194128,33.6476930396,26.7633194206),('Ludwag',1728,'','Jurassic','Upper Jurassic','lower Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,154,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','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,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1031,1029,'Mounds with steep flanks. \n15-20 m thick, 50-60 m in diameter.\n',49,11,5031036,1187437,'Germany','Europe',331,'',49.9333,11.0667,'','',30.2520099781,25.2453348901,30.2520099781,25.2453348901,35.5130526961,26.8969305411),('Eisenrichterstein, Bad Reichenhall',1729,'','Paleogene','Eocene','lower Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,36,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'25',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species','60','2','Baffler guild','1','Present','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1032,1467,'Upper ramp setting.\nSmall patch reefs with corals, encrusted by red algae.\n16 species of red algae\n2 greens\n42 coral\n\nTaxonomic data in Paleobiology Database',47,12,5577424,1034196,'Germany','Europe',331,'',47.1667,12.8833,'WAHR','10703',42.4413733562,7.15501277761,42.4413733562,7.15501277761,42.7195383475,14.6036470465),('Kirchberg, Neubeuern',1730,'','Paleogene','Eocene','lower Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,36,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'25','1729',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','40','60',0,'no',0,'no','2','6 to 24 reef building species','21','3','Binder guild','1','Present','1','Present','1','Low zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1032,0,'Redeposited blocks.\nDominated by Corallinaceans. \nCorals dominant in lagoonal facies only.\nTaxonomic data in Paleobiology Database',47,12,5896848,755165,'Germany','Europe',331,'',47.2,12.15,'WAHR','10963',42.3986474272,6.48086304981,42.3986474272,6.48086304981,42.817674378,13.9364832297),('Salemi, Sicily',1731,'','Neogene','Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,6,3,0,'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,'','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),('Sirataslar Ridge, Maden',1732,'','Cretaceous','Upper Cretaceous','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,69,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','1','Corals','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'45','55','0',0,'no',0,'no','2','6 to 24 reef building species','9','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1034,0,'reefal limestones consisting abundant rudists, gastropods and corals',40,40,3870126,3829308,'Turkey','Asia',522,'',40.125,40.3028,'WAHR','73590',37.8149631789,39.6329330674,37.8149631789,39.6329330674,38.332546533,38.5839678371),('Cape Ajo, Cantabria',1733,'','Cretaceous','Lower Cretaceous','Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1035,2446,'Corals dominant:\nThecosmilia, Cheilosmilia, Diplogyra, Pseudocoenia, Pentacoenia Hydnophormeandraraea.\n',43,-3,3922241,172211,'Spain','Europe',304,'',43.5,-3.5833,'WAHR','56935',31.8622904043,7.57556057752,31.8622904043,7.57556057752,34.1234967977,3.38739435215),('W-Saaremaa',1734,'Padla','Silurian','Ludlow','lower Ludlovian',425.60,427.40,7,'Wenlock - early Pridoli',425,422,3,0,'Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','4','Stromatoporoids','73','Bryozoans only',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1036,1612,'Stromatopore biostrome belt from Gotland (Hemse Group) to Saaremaa (Padla Formation) to SE-Lithuania (Dubysa Formation).\nPlectostroma, Clathrodictyon, Stromatopora, Syringostromella as main frame-builders.',58,22,-1413262,-488684,'Estonia','Europe',NULL,'',58.2167,22.1,'WAHR','79877',1.51846303858,-45.1488655236,1.51846303858,-45.1488655236,1.51846303858,-45.1488655236),('Vasalemma',1735,'Padla','Ordovician','Upper Ordovician','Caradocian',451.00,458.00,5,'Darriwilian - Ashgillian',452,453,2,0,'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','2','Shelf/platform margin','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,'','2','Medium zonation',NULL,'','3','More than 60% micrite',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),('Undva, Saaremaa',1736,'Padla','Silurian','Wenlock','lower Wenlock',427.40,430.50,7,'Wenlock - early Pridoli',425,427,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1036,1612,'Small bryozoan pioneer bioherm.',58,21,-1386102,-512737,'Estonia','Europe',NULL,'',58.5,21.9667,'','',-2.00705737702,-47.0246638639,-2.00705737702,-47.0246638639,-2.00705737702,-47.0246638639),('Kesselaid Mound, Muhu Island',1737,'','Silurian','Wenlock','lower Wenlock',427.40,430.50,7,'Wenlock - early Pridoli',425,427,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',1036,0,'Dolomitic mound in restricted lagoonal setting.',58,23,-1322759,-451903,'Estonia','Europe',NULL,'',58.5833,23.3333,'','',-1.39643024588,-46.6467278502,-1.39643024588,-46.6467278502,-1.39643024588,-46.6467278502),('Boda Mounds 1, north of Gotland',1738,'','Ordovician','Upper Ordovician','Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,2,1,'Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','7','Bryozoans','2','Algae','18','Bryozoans - microbes - (algae) - (crinoids)','4','Others','60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1036,0,'Boda Mud Mounds with scattered bryozoans, algae,\npelmatozoans, corals.\nInterpreted water depth 50-100 m.',58,19,-4361699,-329320,'Sweden','Europe',330,'',58.3333,19.5,'','',-27.8256145822,-61.715174188,-26.8604422695,-60.7985275464,-26.8604422695,-60.7985275464),('Boda Mounds 2, north of Gotland',1739,'Klasen','Ordovician','Upper Ordovician','upper Ashgillian',445.20,450.00,5,'Darriwilian - Ashgillian',452,445,3,1,'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,'','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),('Weinberg and Rauhheck, Eifel',1740,'','Devonian','Middle Devonian','upper Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,393,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','20',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,'40','20','40',0,'no',0,'no','2','6 to 24 reef building species','6','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1039,0,'Girvanella (cyanobacteria), calcisponges (spicules), fenestillid bryozoans, and Stachyodes are reef builders.\nGreen alga Pseudopalaeoporella is present.\n20 m thick and up to 1 km in diameter.\n',50,6,-3241861,815425,'Germany','Europe',331,'',50.3333,6.5833,'WAHR','82032',-14.5711609387,-17.8444430842,-14.5711609387,-17.8444430842,-0.145280870574,-73.7703666041),('Farafra Oasis',1741,'','Paleogene','Paleocene','upper Thanetian',56.00,59.20,27,'Thanetian - Ypresian',53,56,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','5',NULL,NULL,NULL,'1','Less than 20 m',NULL,'2',NULL,1,'Temperate',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','8','Serpulids, worms, vermetids','8','Serpulids, worms, vermetids','76','Worms only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','3','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1041,0,'Up to 5 m thick mounds, topped by a hardground.\nTube structures. Either worms or vermetid gastropodes.\nTemporary upwelling indicated by phosphate particles.',26,27,2262586,2474351,'Egypt','Africa',715,'',26.4528,27.85,'WAHR','34415',16.4099326963,23.8765085471,16.4099326963,23.8765085471,19.3755399249,23.7427710964),('Gascoyne Inlet, SW Devon Island',1742,'Douro-Barlow Inlet','Silurian','Ludlow','upper Ludlovian',423.00,425.60,7,'Wenlock - early Pridoli',425,420,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','50','2','10 - 100 m wide','50','2','10 - 100 m','60','200',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','3','Microbes','1','Corals','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,'90','0','10',0,'no',0,'no','2','6 to 24 reef building species','16','2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1042,1135,'No detailed locality description.\nThree types of mounds in area.\nMudmounds\nCoral-skeletal mounds\nCoral-stromatoporoid skeletal mounds\nOnly Mudmounds better preserved: 15 thick, 50 m in width.\nCompound reef mounds up to 50 m thick and 60 m across.\n14 coral species, microbes and possibly stromatoporoids. Collection of Alroy.\n\nAbstract or ref. 1135:\nNear Gascoyne Inlet, the topmost Douro and and lowermost Barlow Inlet Formations record overall upward  shallowing from ramp to shallow shelf conditions. This transitional sequence contains bioherms of various sizes, from small isolated reef mounds 1 to 2 m across to larger, compound reef mounds over 50 m thick and 60 m across, as well as distinctive inter- and pre-reef mound facies. The larger reef mounds show stages intermediate in character between those in sponge-dominated reef mounds of the Douro Formation and in larger stromatoporoid-crinoid-dominated reefs in the Barlow Inlet Formation. Three principal reef mound facies developed in turn. An initial partly lithified lime mudstone, containing scattered corals and apparently relicit sponge-cryptomicrobial fabrics, developed on sheets of oncolitic storm debris in mainly low energy conditions between storm and fairweather wave bases. This lower facies of the reef mounds achieved up to 2 m relief above surrounding burrowed, soft, detrital and carbonate muds. With gradual shallowing, and progressively higher energy conditions above fairweather wave base, middle facies of coral-and crinoid-rich mudstone developed, flanked by coalescing aprons of coarse crinodal debris. The middle facies achieved a maximum relief of 4 m. Detrital and carbonate muds succeeded the grainy flankbeds, as abrupt deepening    restored conditions of low energy below fair-weather wave base. The ensuing upper facies of the reef mounds is more  varied, comprising sparsely fossiliferous and locally fenestral lime mudstones, patchy coral bafflestone and bindstone, coarse encrinites, and substantial culminating stromatoporoid bindstone. Relief of the upper facies was progressively    reduced by onlap of adjacent muds. The reef mounds were ultimately engulfed by these muds, and a laterally discontinuous, biostromal, Stylopleura rudstone caps the sequence. With resumed shallowing, the sea floor again was exposed to more persistently turbulent conditions above fairweather wave base. Large  stromatoporoid-crinoid-dominated reefs formed just above the transitional sequence on topographic highs inherited from the reef mounds, and are flanked by substantial grainy crinoid-rich facies. ',74,-91,283697,-3376213,'Canada','North America',121,'1617',74.7,-91.4167,'WAHR','5790',5.20114668309,-72.3994016712,5.20114668309,-72.3994016712,5.20114668309,-72.3994016712),('Klokocov',1743,'Frydek','Cretaceous','Upper Cretaceous','Cenomanian-Santonian',83.60,100.50,25,'late Cenomanian - early Campanian',91,89,1,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','20','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1043,2502,'Subsilesian unit.\nRedeposited from coral thickets in stressed environment.\nCoral fauna strongly dominated by Actinacis remesi Felix (90 % of individuals).\n19 coral genera.',49,17,5041400,1633268,'Czech Republic','Europe',331,'',49.75,17.75,'WAHR','67562',45.5347888714,20.0238993004,45.5347888714,20.0238993004,43.1166230453,18.5853397418),('Kurdejov, Hustopece',1744,'','Paleogene','Eocene','Middle Eocene',38.00,47.80,28,'Lutetian - Bartonian',45,40,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','19','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1043,0,'18 coral genera, slightly dominated by Favia.\r\nRedeposited in slumps (from small patch reefs on intrabasinal highs).',48,16,5995936,1162640,'Czech Republic','Europe',331,'',48.9167,16.75,'WAHR','69514',46.881330532,10.555338244,46.881330532,10.555338244,47.4415910518,16.0458828422),('Oj-Muran, Lena River',1745,'','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,518,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'800','1776',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','14','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1044,1045,'Small bioherms composed of either Renalcis and archaeocyaths or Epiphyton.\nIn addition: Girvanella, Markovella, Chabacovia, stromatolites.',61,126,-2254095,-119996,'Russia','Asia',624,'1093, 1413',61.0833,126.2167,'WAHR','9990',5.87625840153,-65.1505394681,5.87625840153,-65.1505394681,5.87625840153,-65.1505394681),('La Sentinella, Serra Scoris, Gonnesa, Sardinia',1746,'Matoppa','Cambrian','Lower Cambrian','lower Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','35',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','18','3','Binder guild',NULL,'','1','Present',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1046,1048,'Up to 35 m thick bioherm complex. Several 100 m in length.\nTwo bioherm levels\n10-15 % of rocks are formed by archaeocyaths.\nMain constructors: Renalcis and Epiphyton.\nmm-sized irregular borings in archaeocyath walls.\nDiverse microbes and some archaeocyath species',39,8,-5059120,9562801,'Italy','Europe',344,'2570',39.2667,8.4667,'WAHR','76110',NULL,NULL,NULL,NULL,39.2667,8.4667),('Maria Santa Gloria, Sardinia',1747,'Santa Barbara','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'25',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','13','3','Binder guild',NULL,'','1','Present',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1046,1048,'Girvanella is dominating. 10-15 % archaeocyaths.\nPlatform margin reefs',39,8,-5040810,9578860,'Italy','Europe',344,'',39.4167,8.4667,'WAHR','81033',NULL,NULL,NULL,NULL,39.4167,8.4667),('Jebel Daf',1748,'','Cambrian','Lower Cambrian','Lower Cambrian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,515,1,0,'Outcropping reef ',4,'Biostrome','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','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1047,0,'No real buildups.\nStromatolites and archaeocyaths mentioned.',21,39,-3132533,14465120,'Saudi Arabia','Asia',503,'',21.5167,39.5833,'','',-37.1366993334,51.7747126894,-44.8762368525,61.2499081151,-44.8762368525,61.2499081151),('Rio Cannas, Sardinia',1749,'Matoppa','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'25','1747',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,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1048,0,'Termed Girvanella buildup.\nAdditionally archaeocyaths and Epiphyton.',39,8,-5069122,9562083,'Italy','Europe',344,'',38,8.55,'WAHR','81027',NULL,NULL,NULL,NULL,39.2,8.55),('Matoppa, Sardegna',1750,'Gonnesa','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','21','2','Baffler guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1048,2425,'Borings restricted to archaeocyaths.\nBuildup framework of branching irregular archaeocyaths. \nEncrusters Renalcis, Grivanella micrite.',39,8,-5048211,9569149,'Italy','Europe',344,'',39.35,8.43,'WAHR','50195',NULL,NULL,NULL,NULL,39.35,8.4333),('Huanghuachang, Yichang, Hubei',1751,'Fenxiang','Ordovician','Lower Ordovician','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,482,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'50',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','2','Algae','11','Siliceous sponges','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)','3','Receptaculitids','20','80','0',0,'no',0,'no','1','Less than 6 reef building species','3','2','Baffler guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1049,1050,'Small bioherms. 3-4 m in diameter and 0.3-0.4 m thick, bryozoan framestones, sponge bafflestones, Girvanella bindstonesIncluding lithistid sponges and receptaculid alga (or microbe?) Calathium.Ref. 1087: Classified as lime mud and algal reef.90 % lime mud.',30,111,1962020,15153636,'China','Asia',602,'1087, 2667, 2854',30.8667,111.3833,'WAHR','61727',-18.4097854743,92.7556084051,-18.4097854743,92.7556084051,-18.4097854743,92.7556084051),('Xintan, Hubei',1752,'Fenxiang','Ordovician','Lower Ordovician','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'50','1751',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','11','Siliceous sponges','3','Microbes','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','8',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1050,2854,'Abstract ref. 1050:A moderately diverse assemblage of anthaspidellid demosponges has been recovered from reef-bearing carbonate platform deposits of Early Ordovician, Tremadoc to early Arenig age, in Hubei Province. The sponges occur, in part, in the Tremadoc Fenxiang Formation and, in part, in the lower Arenig Honghuayuan Formation at several localities near Yichang, Xintan, and Liujiachang. Archaeoscyphia nana Beresi and Rigby, 1993, Archaeoscyphia pulchra (Bassler, 1927), and Archaeoscyphia minganensis (Billings, 1859) occur with the new genera and species, Jianghania yichangensis and Velellospongia adnata, and the new species Rhopalocoelia sanxiaensis and Anthaspidella lamellata. This is the first reported occurrence of Anthaspidella in Ordovician rocks of China. Great numbers of these species of fossil sponges have been found in Lower Ordovician outcrops, particularly in the eastern Yangtze Gorge area of Hubei Province. ',30,110,2008004,15171402,'China','Asia',602,NULL,30.8833,110.8667,NULL,NULL,-17.9961645185,92.9246597432,-17.9961645185,92.9246597432,-17.9961645185,92.9246597432),('Liujiachang, Hubei',1753,'Honghuayuan','Ordovician','Lower Ordovician','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,475,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m','2','20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','11','Siliceous sponges','2','Algae','94','Lithistid sponges - receptaculitid algae','3','Receptaculitids','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'','3','Pronounced zonation',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1050,1087,'Lithistid sponge (Archaeoscyphia)-Calathium (alga) reefs and bioherms.',30,111,442543,14568943,'China','Asia',602,'',30.0833,111.4833,'',NULL,-16.3999045246,88.7320540673,-16.3999045246,88.7320540673,-16.3999045246,88.7320540673),('San José de Jáchal, Argentina',1754,'','Cambrian','Upper Cambrian','Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,494,1,0,'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,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1051,1066,'Complex of non-emergent microbialitic mounds and ponds on carbonate platform with restricted circulation.',-30,-68,-1923481,-7967145,'Argentina','South America',201,NULL,-30.2833,-68.7167,'',NULL,-29.2528547501,-166.164128955,-29.2528547501,-166.164128955,-29.2528547501,-166.164128955),('Camp San Saba, Texas',1755,'Wilberns','Cambrian','Upper Cambrian','Upper Cambrian',485.00,497.00,2,'Middle Cambrian - Dresbachian',502,495,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','12',NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',1,'yes','1','Less than 6 reef building species',NULL,'3','Binder guild','1','Present',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',1052,1056,'Small (3.75 m thick) algal bioherm with 4 zones.\nDifferent kinds of microbes: Girvanella, Epiphyton, Renalcis and Nuia.\nWith dolomitic burrows.\nSome sponges associated\n\nOwn data indicate almost 15 m thick mound complex.\nRare macroborings. ',31,-99,-1501335,-8671725,'United States','North America',101,'1799',31.0042,-99.2694,'WAHR','81095',16.8918136016,-120.551737314,16.8918136016,-120.551737314,16.8918136016,-120.551737314),('Las Ermitas, Sierra Morena',1756,'Pedroche','Cambrian','Lower Cambrian','lower Atdabian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','5',NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1053,1058,'Microbes and archaocyaths.\n3-5 m thick reef mounds stacked.\nMargin of carbonate-siliciclastic platform.\n\nAbstract ref. 1977:\nA well-preserved coelobiontic biota of early Ovetian age (Early Cambrian; Moreno-Eiris et al. 1995. Paleozoic Cnidaria and Porifera from\nSierra Morena. Field Trip D. In PEREJON A. (ed.). VII International Symposium on Fossil Cnidaria and Porifera, Madrid, 1-68) is found near\nthe city of Córdoba (Ossa-Morena, southern Spain). Cryptic cavities occur at the unconformable boundary between an eroded, andesitic paleotopography, which belongs to the Neoproterozoic San Jerónimo Formation, and the giant reef complex of the Lower Cambrian Pedroche Formation (Zamarreño and Debrenne 1977. Sédimentologie et biologie des constructions organogènes du Cambrien inférieur du Sud de l\'Espagne. Mémoires du BRGM, 89, 49-61. Moreno-Eiris 1988. Los montículos arrecifales de algas y arqueociatos del Cámbrico Inferior de Sierra Morena. Publicaciones Especiales del Boletín Geológico y Minero, 98, 1-127). The cavities exhibit several phases of growth, in some cases tectonically induced. The coelobiontic biota is preserved on the cavities (i) attached to the walls or encrusting previously attached organisms, and (ii) within the sediments that fill the cavities. The biota was diverse and consisted of encrusting, self-supported calcimicrobes, chancelloriids and archaeocyaths, found attached to walls and roofs of the cavities. Other reworked organisms preserved within the cavities are\ntrilobites, brachiopods and hyoliths derived from the overlying open-sea communities.',37,-4,-6053480,8643978,'Spain','Europe',304,'1977, 2650',37.9167,-4.8167,'WAHR','78585',-68.6195106414,-6.48078188144,-68.6195106414,-6.48078188144,-68.6195106414,-6.48078188144),('Alconera, Sierra Morena',1757,'','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,519,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'40','1756',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1053,1058,'Mounds with thrombolites, Stromatactis, microbes and archaeocyaths.\nMicritic.',38,-6,-6060362,8461777,'Spain','Europe',304,'',38.4,-6.4667,'WAHR','81039',-67.787077447,-9.46090954042,-67.787077447,-9.46090954042,-67.787077447,-9.46090954042),('Great Valley, Maryland',1758,'Conococheague Limestone','Cambrian','Upper Cambrian','Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,494,1,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','5',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','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,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1054,0,'Biostromal layers up to 5 m thick.\nThrombolitic bioherms with clotted internal fabric.\nRenalcis and Girvanella important.\nStromatactis-like cavities with laminated mudstone, peloids and fibrous or equant cements.\n\nAbstract ref. 1054:\nUpper Cambrian carbonates in western Maryland are comprised of platform facies (Conococheague Limestone) west of South Mountain and basin facies (Frederick Limestone) east of South Mountain. Conocheague platform carbonates contain interbedded non-cyclic and cyclic facies. Non-cyclic facies consist of cross-stratified grainstones, thrombolitic bioherms, and graded, thin-bedded dolostones. These were deposited in shallow, subtidal shelf lagoons. Cyclic facies are composed of repeated sequences of cross-stratified grainstone: ribbon- rock, wavy, prism-cracked laminite and planar laminated dolostone. The cyclic facies are shallowing-upward cycles produced by lateral progradation of tidal flats over shallow, nearshore subtidal environments. Cyclic and non-cyclic facies are interbedded in the Conococheague in a layer cake fashion, but no higher-order cyclicity can be found. The Frederick Limestone is dominated by monotonously thick sequences of graded, thin-bedded limestones, interbedded with massive peloidal grainstones and beds of breccia up to 10 m thick in the lower Frederick. The breccias contain transported megaclasts of Epiphyton-Girvanella boundstones. The basal Frederick was deposited in a slope-to-basinal setting east of a rimmed shelf. An Epiphyton- Girvanella marginal reef along the shelf edge was the source of the blocks in the breccias. The upper Frederick Limestone formed on a carbonate ramp.\n',39,-77,-2004036,-6437750,'United States','North America',101,'',39.6111,-77.9417,'','',8.43897728473,-102.69015855,8.43897728473,-102.69015855,8.43897728473,-102.69015855),('Great Valley II, Pennsylvania',1759,'Conococheague Limestone','Cambrian','Upper Cambrian','Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,494,1,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10','1758',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,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1054,0,'see reef 1758',39,-77,-2010280,-6412456,'United States','North America',101,'',39.75,-77.7167,'','',8.40554979508,-102.468308921,8.40554979508,-102.468308921,8.40554979508,-102.468308921),('Frederick Valley, Maryland',1760,'Frederick Limestone','Cambrian','Upper Cambrian','Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,494,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',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,'','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1054,0,'Epiphyton-girvanella reefal blocks reworked as clasts in basinal (700-800 m) sediments.\n',39,-77,-2057494,-6415045,'United States','North America',101,'',39.4667,-77.4333,'','',8.0529103374,-102.528722944,8.0529103374,-102.528722944,8.0529103374,-102.528722944),('Frederick Valley, Maryland',1761,'Frederick Limestone','Cambrian','Upper Cambrian','Upper Cambrian',485.00,497.00,2,'Middle Cambrian - Dresbachian',502,497,2,0,'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',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,'','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1054,0,'see reef 1760',39,-77,-3061227,-6587191,'United States','North America',101,'',39.4667,-77.4333,'','',8.0529103374,-102.528722944,8.0529103374,-102.528722944,8.0529103374,-102.528722944),('Amouslek',1762,'Amouslek','Cambrian','Lower Cambrian','Atdabanian/Botomian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,515,2,0,'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','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,'','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,'','2','30-60% micrite','2','10-25% sparite',NULL,'','0','',0,'No or unknown reservoir potential',1350,1055,'',30,-9,-6983299,7825905,'Morocco','Africa',714,'1351, 2534',30.2333,-9.0167,'WAHR','80905',-75.0633662933,-30.5202300823,-74.4138052881,-24.2568141439,-74.4138052881,-24.2568141439),('Point Peak, Llano River, Texas',1763,'Wilberns','Cambrian','Upper Cambrian','Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,494,1,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3b','Deeper slope or outer ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',1,'yes','2','6 to 24 reef building species',NULL,'3','Binder guild',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',1056,0,'Relatively large bioherms: 15 m thick and more than 20 m in diameter. Circular in outline.\nOuter ramp setting, but well above wave base\n(rip-up clasts, hummockies, wave ripples).\nAlgal flora relatively diverse (Girvanella, Renalcis, Epiphyton).',30,-99,-595235,-8433294,'United States','North America',101,'',30.6486,-99.3139,'','',16.724167612,-120.881757783,16.724167612,-120.881757783,16.724167612,-120.881757783),('Ketza River, Pelly Mts., Yukon',1764,'','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','90',NULL,NULL,NULL,'4','More than 1000 m','610','5',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','1','Low zonation',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1059,1100,'Shrimp Lake 1 buildup\nTwo large Archaeocyathid-Renalcis buildups.\nBelow normal, but above storm wave base.\nArchaeocyaths are Pycnoidocyathus and Protopharetra.\nStromatoporoid Altaicyathus is also present.\nUp to 90 m thick and 610 m long.',61,-132,-909397,-6921578,'Canada','North America',121,'',61.5194,-132.325,'WAHR','80948',45.3412778705,-121.561302757,45.9500975093,-118.810409111,45.9500975093,-118.810409111),('Wilkawillina Gorge, South Australia',1765,'','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,519,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','12',NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1060,1061,'Archaeocyath-Renalcis-Boundstone.\nwith areas of Epiphyton-archaeocyath intergrowths.\nOpen shelf environment with cross-bedded bioclastic sand shoals.\nMostly 8-10 in length and 3-5 m in thickness\nbut at Ten Mile Creekmore than 20 m l and 12 m h.\nTo the top (sequence 2) replaced by either Renalcis-dominated or Girvanella-Renalcis-Epiphyton dominated buildups.\nCrusts and calcite-filled cavities are important.\n\nAbstract of ref. 1060:\nCarbonate buildups in the Flinders Ranges of mid-Early Cambrian age grew during a period of high archaeocyath diversity and are of two types: (1) low-energy, archaeocyath-sponge-spicule mud mounds, and (2) high-energy, archaeocyath-calcimicrobe (calcified microbial microfossil) bioherms. Mud mounds are composed of red carbonate mudstone and sparse to abundant archaeocyath floatstone, have a fenestral fabric, display distinct stromatactis, contain abundant sponge spicules and form structures up to 150 m wide and 80 m thick. Bioherms are either red or dark grey limestone and occur as isolated small structures 2-20 m in size surrounded by cross-bedded calcarenites and calcirudites or as complexes of mounds and carbonate sands several hundreds of metres across. Red bioherms comprise masses of white Epiphyton with scattered archaeocyaths and intervening areas of archaeocyath-rich lime mudstone. Grey bioherms are complex intergrowth of arachaeocyaths, encrusting dark grey Renalcis and thick rinds of fibrous calcite cement. The bioherms were prone to synsedimentary fracturing and exhibit large irregular cavities, up to 1.5 m across, lined with fibrous calcite. The buildups are isolated or in contiguous vertical succession. Mud mounds occur along in low-energy, frequently nodular, limestone facies. Individual bioherms and bioherm complexes occur in high-energy onshelf and shelf-margin facies. The two types also form large-scale, shallowing-upward sequences composed of basal (deep water) mud mounds grading upward into archaeocyath-calcimicrobe bioherm complexes and bioherms in cross-bedded carbonate sands. The uppermost sequence is capped by ooid grainstone and/or fenestral to stromolitic mudstone. The calcimicrobe and metazoan association form the two major biotic elements which were to dominate reefs throughout much of subsequent Phanerozoic time. ',-31,138,2131120,-18604303,'Australia','Oceania',801,'',-31.3,138.9125,'WAHR','81170',1.30117543977,114.194401493,1.30117543977,114.194401493,1.30117543977,114.194401493),('Mount Scott Range, South Australia',1766,'','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,519,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','60',NULL,NULL,NULL,'3','More than 100 m',NULL,'50','1765',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1060,1061,'60 m thick, 120 m long buildup in intrashelf depression.\nMostly archaeocyaths and spiculate sponges.',-30,138,2203145,-18649834,'Australia','Oceania',801,'1343',-30.5958,138.3389,'WAHR','81172',1.47928239683,113.353812564,1.47928239683,113.353812564,1.47928239683,113.353812564),('Stuart Shelf, South Australia',1767,'Andamooka','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'10',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','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1060,0,'Different types of boundstones.\nThis is referring to Renalcis-archaeocyath boundstones.',-30,137,2217544,-18767108,'Australia','Oceania',801,'',-30.1667,137.1667,'','',0.376314210944,114.036236347,-0.545968860397,116.464130545,-0.545968860397,116.464130545),('Old Wirrealpa Mine, South Australia',1768,'Upper Wilkawillina','Cambrian','Lower Cambrian','upper Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,513,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','4',NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1060,0,'Closely spaced Renalcis-archaeocyath bioherms (maximum 7 m wide and 4 m high).\nMore cement than fossils and sediment combined.',-31,138,2157187,-18599396,'Australia','Oceania',801,'',-31.1,138.9167,'','',0.781669196467,115.760845418,-0.072076318232,118.171116252,-0.072076318232,118.171116252),('Moorowie Mine, Flinders R., South Australia',1769,'Moorowie','Cambrian','Lower Cambrian','upper Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,513,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'20','1768',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','58','Archaeocyaths - microbes (Renalcis, Epiphyton, Girvanella) - corals',NULL,NULL,'20','0','80',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1062,1502,'Microbe-archaeocyath-coralomorph bioherms in shallow mixed siliciclastic-carbonate sequence (marginal fan).\nOldest known tabulate(?) corals.\nDiversity is relatively high.',-31,139,2178325,-18570500,'Australia','Oceania',801,'',-31,139.1667,'WAHR','79944',1.00310809524,115.843545144,0.152505543536,118.244843859,0.152505543536,118.244843859),('Starshot Glacier, Holyoake Range, Antarctica',1770,'','Cambrian','Lower Cambrian','Lower Cambrian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,515,1,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','50',NULL,NULL,NULL,NULL,NULL,NULL,'10',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,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1063,0,'Up to 50 m thick archaeocyath-microbial reefs.\n(Coalesced small reefs with 2 m size).\nLocally with large growth-framework cavities filled with submarine cements and internal sediments. \n2 groups:\n- Renalcis dominated (rare archaeocyaths).\n- variable composition with Epiphyton.\nMaximum abundance of archaecyaths is 30 %.\n\nAbstract of ref. 1063\nThe Shackleton Limestone formed a carbonate platform that bordered part of the Greater Antarctic craton in middle and late Early Cambrian time. In the Holyoake Range of the central Transantarctic Mountains, this unit records deposition on a stable shelf on which flourished ecological reefs composed of microorganisms and archaeocyathans. Burrow-mottled lime mudstone, wackestone and packstone with patch reefs represent accumulation in shelf areas of relatively low to moderate energy. Thick ooidal grainstone units reflect deposition in higher energy shoals and as sand sheets that were associated with extensive reef complexes. The framework of these reefs was principally the product of micro-organisims, by inference mostly cyanobacteria. Archaeocyathans constitute as much as 30% of some reefs, but commonly they forms less than 10% and are absent from some. On the basis of microbial composition, three reef types and are recognized. The first type is a Renalcis boundstone that lacks archaeocyathans. Within these, abundant upward-directed thalli of Renalcis formed a framework that trapped fine-grained sediment. The second type, which forms the core of some larger reefs, is composed of stroamtoctis-bearing, microbial boundstone. The third, yet most common, reef type is variable in composition. It is characterized by the presence of abundant Epiphyton, but may include archaeocyathans, and the microbial microfossils Girvanella and Renalcis as well as cryptomicrobial clotted micrite. In this type of reef, frame-building organisms typically constructed highly porous structures that had small interparticle and fenestral pores and large growth-framework cavities, as well as rare metre-sized caverns. Within these spaces, Epiphyton and, less commonly Ranalcis, encrusted framework elements, fine-grained sediments accumulated, and pervasive sea-floor cements were precipitated. Boundstone fabrics in the Shackleton Limestone are highly complex, with fabrics analogous to younger, more metazoan-rich reefs, as well as deep-water stromatactis-bearing mud-mounds. The Epiphyton-Girvanella-arachaeocyathan frameworks and stromatactis-bearing boundstone, both of which seemingly first appeared in the middle Early Cambrian, are regarded as the precursors, in structure, composition, and preferred hydrologic setting, of the more extensive reefs and complex framework styles of later Phanerozoic time. \n\n',-81,158,-275331,-18693263,'Antarctica','Antarctica',803,'',-81.9167,158.75,'WAHR','80915',-10.6218470334,108.34009923,-12.1056092223,116.49058591,-12.1056092223,116.49058591),('Austinville, Virginia',1771,'Shady Dolomite','Cambrian','Lower Cambrian','Botomian-Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,513,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','60',NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','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','2','Medium zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1064,1615,'Platform edge Epiphyton/Renalcis boundstones in upper Shady Dolomite Fm.\nBoundstones several m thick forming up to 60 m thick reefal complexes.\n\nReefs in both Botomian (Austinville Member) and Toyonian (Upper Shady Dolomite Member)\n\nAbstract ref. 1615:\nMicrocavities within allochthonous Cambrian Epiphyton algal mounds in the upper Shady Dolomite (Shady Formation) of southwestern Virginia contain a preserved coelobiontic (cavity-dwelling) biota of probable late Early Cambrian age. The microcavities (range from 0.3 mm to 15.0 mm across (mean, 2.0 mm) and are constructed by overgrowth of Epiphyton fronds. Epiphyton dominates the coelobiontic biota, although other algae occur on the cavity roof and walls, including spherical micro-algae (?), crust-forming Girvanella and Cavifera, a probable endolithic alga found only in the fringe cements within microcavities. Globular Foraminifera (?) or foraminifer-like microorganisms, possible brachiopods and cylindrical borings also occur on or in the roofs and walls. Disarticulated, small inarticulate brachiopod valves, sponge spicules and grains bored by endolithic microphytes are in the sediment flooring many microcavities. This indicates that microboring algae or fungi, sponges and inarticulate brachiopods, probably inhabited the microcavities. Traces produced on the surface of the sediment in some microcavities and small spines show that vagrant organisms were moving within or through cavities. Localized areas of Epiphyton have been planed flat, pointing to the presence of an unidentified grazing organism in the microcavities. These mounds occur stratigraphically above archaeocyathid patch reefs in the Shady (Dolomite) Formation. The mounds contain no archaeocyathids. The presence of coelobiontic organisms in Lower Cambrian algal mounds lacking a skeletal framework suggests that coelobiontic organisms were not restricted to skeletal reefs but that at least by the end of the Lower Cambrian they had exploited the cavity habitat in algal mounds.',36,-80,-5988417,-7313428,'United States','North America',101,'',36.8525,-80.9022,'WAHR','24039',7.67518047611,-125.01248543,8.24701011392,-121.689639549,8.24701011392,-121.689639549),('Austinville II, Virginia',1772,'','Cambrian','Middle Cambrian','Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,508,1,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15',NULL,NULL,NULL,'1','Less than 20 m',NULL,'10',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1064,1615,'Up to 15 m thick bioherms, a few m wide. \nMainly consisting of Epiphyton, minor Renalcis and doubtful Girvanella.\nFine calcite cement.\nSee reef 1771 for more remarks.',36,-80,-2984884,-7028401,'United States','North America',101,'',36.8167,-80.8,'','',8.53003127924,-119.423991571,9.16168689371,-114.612375436,9.16168689371,-114.612375436),('Saratoga Springs, New York',1773,'','Cambrian','Upper Cambrian','Trempealeauan',497.00,509.00,3,'Franconian - Tremadocian',488,491,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1065,0,'Stromatolithic and thrombolitic boundstones.\nTwo types of trilobites are found beneath the reef. Both\nare found only in this formation: Saratogia calcifera, and\nDellea landingi',43,-73,-2008980,-5911923,'United States','North America',101,'',43.1,-73.8167,'','',9.61183572232,-106.26475405,9.61183572232,-106.26475405,9.61183572232,-106.26475405),('Southern San Juan Province, Argentina',1774,'','Cambrian','Upper Cambrian','Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,494,1,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'200','1754',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,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1066,0,'Thrombolitic-stromatolithic mounds.',-32,-68,-1696781,-8061351,'Argentina','South America',201,'',-32,-68.6667,'','',-28.2871783339,-167.784132953,-28.2871783339,-167.784132953,-28.2871783339,-167.784132953),('San Juan Province, Argentina',1775,'','Cambrian','Upper Cambrian','Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,494,1,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'200','1754',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,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1066,0,'',-31,-68,-1833684,-8031351,'Argentina','South America',201,'',-31,-68.5,'','',-28.9885883819,-166.956026499,-28.9885883819,-166.956026499,-28.9885883819,-166.956026499),('Kotuy River, Anabar, Siberia',1776,'','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,519,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','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,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1067,1045,'Western edge of the Great Siberian Barrier Reef Complex.\nBituminous basinal sediments to the north, lagoonal, evaporitic sediments to the south.\n',71,102,-4052309,198087,'Russia','Asia',624,'1093',71.3333,102.5,'','',-7.75132183802,-62.7328467928,-7.75132183802,-62.7328467928,-7.75132183802,-62.7328467928),('Kotuy River II, Siberia',1777,'','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,519,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1776',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','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,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1067,1045,'',71,103,-4078811,151296,'Russia','Asia',624,'',71.75,103,'','',-7.94050867279,-63.1402763351,-7.94050867279,-63.1402763351,-7.94050867279,-63.1402763351),('Mojero River, Siberia',1778,'Kotuy','Cambrian','Lower Cambrian','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,525,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'800','1776',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','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,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1067,1045,'',68,104,-3663141,395434,'Russia','Asia',624,'1043',68,104.5,'WAHR','80868',-7.25900459633,-70.1228865881,-7.25900459633,-70.1228865881,-7.25900459633,-70.1228865881),('Aldan, Siberia',1779,'','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,519,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'800','1776',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','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,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1043,1045,'',66,108,-3413139,334304,'Russia','Asia',624,'',66.8333,108.6667,'','',-2.92342542513,-61.4111864758,-2.92342542513,-61.4111864758,-2.92342542513,-61.4111864758),('Markha-Udachnyy, Siberia',1780,'','Cambrian','Lower Cambrian','Tommotian/Atdabanian',514.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,521,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'800','1776',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','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,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1093,1043,'',66,112,-3259237,220707,'Russia','Asia',624,'1045',66.4333,112.4,'','',-2.91224381581,-66.7542542448,-2.91224381581,-66.7542542448,-2.91224381581,-66.7542542448),('Sheya, Yakutiya, Siberia',1781,'','Cambrian','Lower Cambrian','Atdabanian-Botomian',509.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,515,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1776',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','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,'','2','Medium production of reefal debris','0','',1,'Potential reservoir',1997,1045,'Some oil and gas shows in back-reef deposits.\nOlder part of reef complex',62,117,-2700406,212932,'Russia','Asia',624,'1044',62.8667,117.5667,'','',3.10469648381,-59.701655283,3.10469648381,-59.701655283,3.10469648381,-59.701655283),('Aldan IV, Yakutiya, Siberia',1782,'','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'800','1776',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','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,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1997,1045,'Drilling in several locations. Older and younger part.\nBarrier reef complex.',63,123,-2570587,-45780,'Russia','Asia',624,'1044',63,123,'','',4.13686583636,-61.9558481301,5.66279147071,-57.6001564665,5.66279147071,-57.6001564665),('Jebel Aswad',1783,'','Cretaceous','Lower Cretaceous','Barremian-early Aptian',113.00,129.40,23,'late Valanginian - early Aptian',126,125,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','30',NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','3','Microbes','47','Bivalves (mostly oysters) - algae (microbes)',NULL,NULL,'40','40','20',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1068,0,'10-30 thick and 50-150 m long reefal domes. \nbeneath domes intercalation with thick conglomerate containing reef limestone.\nRudists, forams and algae Bacinella and Lithocodium.',23,58,-1053512,5139029,'Oman','Asia',503,'',23.1333,58.6472,'','',-10.6585291904,54.0700407399,-10.6585291904,54.0700407399,23.2770477893,72.1944986422),('Qarib',1784,'','Neogene','Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,22,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1068,0,'Large isolated block of reef limestone in slope setting.',23,58,2403495,5772340,'Oman','Asia',503,'',23.2028,58.9167,'','',17.3832957525,53.5397925572,17.3832957525,53.5397925572,21.4972215063,57.3658217007),('Quryat',1785,'','Paleogene','Oligocene','middle Oligocene',26.00,32.00,30,'Chattian - Aquitanian',22,28,1,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,1,'Temperate',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','2','Algae','12','Foraminifera','13','Algae - encrusting forams','1','Red algae','10','0','90',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1068,0,'Reef-breccia with abundant corallinacean algae and large forams (additionally echinoderms, pelecypods, bryozoans).',23,58,2411455,5769452,'Oman','Asia',503,'',23.2611,58.8972,'','',16.3616471953,52.524670384,16.2759306513,52.4462300875,21.3950048846,57.3320246383),('Wu’ai village of Songfan Town',4076,'Upper Sanqushan','Ordovician','Upper Ordovician','late Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,NULL,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','120',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','2',NULL,'3','Microbes','6',NULL,'66',NULL,'2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2',NULL,'12','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3',NULL,'2',NULL,'1',NULL,'0',NULL,0,NULL,3003,NULL,NULL,NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,29,118.32,NULL,'173372',-8.32650476722,65.3717454345,-8.32650476722,65.3717454345,-8.32650476722,65.3717454345),('Quryat',1786,'','Paleogene','Eocene','Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,35,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1068,0,'Small reef structures along intraplatform megachannel.',23,58,1786176,5555012,'Oman','Asia',503,'',23.25,58.8847,'','',15.0066245956,51.539551607,15.0066245956,51.539551607,21.5299907774,57.4423467144),('Field, British Columbia',1787,'Cathedral','Cambrian','Middle Cambrian','Albertan',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,508,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','215',NULL,NULL,NULL,'4','More than 1000 m','5000','25',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,'','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',1069,1141,'Algal reef (Cathedral Escarpment) with approximately 200 m of syndepositional relief.\nEpiphyton boundstones, submarine cemented.\nMinor contributions from Renalcis, Girvanella and spongiostromata. \n\nAbstract ref. 1554:\nThe Cathedral lithosome was generated by the expansions and contractions of a middle carbonate facies belt, deposited at low latitudes on a young, north-facing, thermally subsiding continental margin. It is bounded above by a quasi-synchronous contact, and below by a strongly diachronous contact that youngs eastward to intercept the upper contact. The outboard limit was controlled by, and partly corresponds to, a platform-bounding, organosedimentary reef established above a subtle, linear uplift at the beginning of the Middle Cambrian. Growth of the lithosome took place in three pulses, each succeeding an episode of abrupt sea level rise. Each of these rises introduced new fauna onto the platform and is interpreted as eustatic. At the beginning of each abrupt rise, the carbonate complex was reduced to a narrow rim. As eustatic rise slowed, the carbonate rim complex began to expand into the sheltered inshore basin above the mud-grade inner detrital sediments (Mount Whyte Formation) of the drowning phase. The facies are peritidial over and near the rim and lime-mud-dominated subtidal inboard. Outward expansion of the complex was limited during the early history of the lithosome, and effectively nil during the late stages. Growth of the Cathedral lithosome was terminated by a pulse by a pulse of sea level rise more pronounced than those preceding. This drowned the carbonate complex and admitted open-sea energy to the inshore basin. Craton-derived inner detrital muds (Stephen Formation) were then spread from the inshore basin, across the former site of the carbonate rim and, for the first time since the beginning of Cathedral deposition, into the offshore basin. A series of lithofacies maps on a palinspastic base illustrates paradoxical aspects of lithostratigraphic nomenclature: in the case of a deeply tongued lithosome like the Cathedral, the name given to a depositional unit commonly depends on the lithofacies of overlying and underlying units.\n\n',51,-116,948280,-6944288,'Canada','North America',121,'1554',51.4167,-116.5,'WAHR','45280',38.2466354872,-114.92555271,38.2466354872,-114.92555271,38.2466354872,-114.92555271),('Cerro Calaveras, Sonora',1788,'Puerto Blanco','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','19',NULL,NULL,NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','22','1','Constructor guild',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',1070,0,'18-19 m thick Renalcis-archaeocyath reefs.\nTypified as type 1 reef with abundant cement.\nAbstract ref. 1070:\n I - Framework reefs occurring at the base of the carbonate interval of the Puerto Blanco Formation. These consist of an archaeocyathan framework with encrusting renal acids and abundant fibrous cements. Cavities are filled with mudstone and contain rare sponge spicules. Cements are well developed upon internal sediments. The archaeocyathan fauna is dominated by colonial Paranacyathus along with Batenevia and Claruscoscinus with taeniae and curved tabulae. A few regular archaeocyaths are present, including Palmericyathus and Aulocricus. Lateral to the reef facies the lime mud sediment contains abundant skeletal fragments of trilobites, echinoderms, Chancelloria, hyoliths, and archaeocyaths. These buildups are interpreted to have formed as wave-resistant, framework reefs in a tidally dominated, shelf-margin setting seaward of a carbonate barrier. II - Girvanella-dominated buildups located in the upper part of the carbonate interval of the Puerto Blanco Formation and associated with oolites. These are built by stacked Girvanella crusts, with an important contribution of Renalcis and a less important presence of Epiphyton. Shelter cavities are filled by mudstone often rich in siltsize quartz. Cements are poorly developed and confined to the intraskeletal cavities. Archaeocyaths are scattered in the Girvanella frame either as isolated individuals or as clusters of solitary or colonial forms. Regular archaeocyaths are here abundant, represented by several taxa with an ethmophylloid inner wall, including Palmericyatbus and Cordilleracyathus. The dominant genus is Aulocricus. Colonial species of Archaeocyathus and Arrythmocricus are well developed. These latter two genera are now recorded from Mexico to northern Canada. The internal and lateral sediment contains a rich fauna represented by trilobites, Chancelloria, echinoderm plates, hyoliths, brachiopods, and helcionellacean mollusks. We interpret these buildups to have formed in a back-shoal setting as isolated patch reefs and laterally continuous biostromes. Samples of float from the Buelna Formation contain cryptalgal boundstones consisting of isolated and rare archeocyathan cups in a homogenous micritic tissue interpreted to have resulted from cyanobacterial activity. There are abundant cavities filled with internal sediments that contains scarce skeletal remains. cements are poorly developed. Marine cements are lacking, possibly because they have been replaced by blocky calcite of meteortic origin. Rather large specimens of Claruscoscinus and Archaeocyathus are present. The bioconstructions probably formed subtidally above storm wavebase. Twenty-two taxa of Archaeocyatha are recognized. Two new genera and eleven new species are described. The fauna from the Puerto Blanco Formation is Botomian in age. The fauna from the Buelna is probably Toyonian. ',30,-112,-2863096,-10133354,'Mexico','North America',105,'',30.2667,-112.0833,'WAHR','62866',30.2917866828,-144.163588022,30.6041852019,-141.236463741,30.6041852019,-141.236463741),('Cerro Rajon, Sonora',1789,'','Cambrian','Lower Cambrian','Botomian-Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,513,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30','1788',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','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','6','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1070,0,'Type 2 buildup dominated by Girvanella.\nSee reef 1070 for more remarks.',30,-111,-2881237,-10107218,'Mexico','North America',105,'',30.45,-111.9333,'WAHR','62865',30.1944864582,-143.929533712,30.510317795,-140.9997784,30.510317795,-140.9997784),('Cerro Rajon/de la Proveedora, Sonora',1790,'Puerto Blanco','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30','1788',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','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,'','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1070,0,'Features from Cerro Rajon.\nType 1 buildup with abundant cement-filled growth-framework cavities. \nRenalcis-archaeocyath reef.\nTwo species of archaeocyaths (Paranacyathus polycladus + Batenevia spinosa) strongly dominant.\nSee reef 1070 for more remarks.',30,-112,-2844067,-10089239,'Mexico','North America',105,'',30.7,-112.2667,'WAHR','62864',30.5183875428,-143.697805735,30.8375524336,-140.773690995,30.8375524336,-140.773690995),('Stewarts Mill, Esmeralda Co., Nevada',1791,'Poleta','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','70',NULL,NULL,NULL,'3','More than 100 m',NULL,'200',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','44','1','Constructor guild',NULL,'',NULL,'','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1071,1045,'Almost 70 m thick reef with distinct community succession.\n31 genera and 43 species of archaeocyaths near the base. Decreasing diversity towards the top (domination stage).\nChange from protected lagoonal to wave-swept setting.',37,-117,-2249330,-9729118,'United States','North America',101,'1573',37.4236,-117.4667,'WAHR','81038',32.3156025511,-141.409003735,32.6676101509,-138.51277668,32.6676101509,-138.51277668),('Heritage Range, Ellsworth Mts., Antarctica',1792,'Minaret','Cambrian','Upper Cambrian','Upper Cambrian',485.00,497.00,2,'Middle Cambrian - Dresbachian',502,497,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','10','Archaeocyaths','10','Archaeocyaths',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1108,1073,'Reworked clasts\nAntarcticocyathus webersi .',-79,-84,-1361678,-17403882,'Antarctica','Antarctica',803,'',-79.4167,-84.8333,'WAHR','81112',-11.1018633852,156.468305245,-11.1018633852,156.468305245,-11.1018633852,156.468305245),('Heritage Range II, Ellsworth Mts., Antarctica',1793,'','Cambrian','Middle Cambrian','Upper Cambrian',485.00,497.00,2,'Middle Cambrian - Dresbachian',502,496,1,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1073,1108,'Cambrian clasts in Permian tillites.',-79,-81,-1451918,-17422098,'Antarctica','Antarctica',803,'',-79.75,-81.0833,'','',-11.8557867798,156.515317358,-11.8557867798,156.515317358,-11.8557867798,156.515317358),('Nowshera',1794,'Nowshera','Silurian-Devonian','','Pridolian-Lochkovian',410.80,423.00,8,'middle Pridolian - middle Pragian',412,416,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','250',NULL,NULL,NULL,NULL,NULL,NULL,'9',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'','3','Pronounced zonation',NULL,'',NULL,'',NULL,'','3','High production of reefal debris','1','Present',1,'Potential reservoir',1075,1081,'Reef belt with numerous individual reefs.\nThickness 80-250 m.\nStromatoporoids, tabulate corals (Heliolites, Thamnopora, Favosites, Alveolites, Cladopora) and rugose corals as reef builders.\nFour different paleogeographic settings discussed. Not decided.\nStromatoporoids dominant. Thamnopora important in relatively quiet water settings.\nAge unclear. \nProbable potential as reservoir.\nReef cited as example for succession in Walker and Alberstadt (1975).',34,72,-5388080,11596852,'Pakistan','Asia',501,'',34.0333,72,'WAHR','79383',-30.3617736601,70.3982149876,-30.3617736601,70.3982149876,-47.4110848836,52.1021917353),('Gechang-Muth, Himachal Himalaya',1795,'Takche','Silurian','Wenlock','Wenlockian',427.40,433.40,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',4,'Biostrome','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','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'80','0','20',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1545,0,'Siliciclastic sequence. Coastal fringing reefs.\nGechang\nCrinoidal limestone at base.\nThamnopora framestones in dolomites.\nTabulates: Thamnopora, Favolistes, Halysites protarea.\nMuth \nCoral framestone with stromatoporoids\nStromatopora, Cyathophyllum, Halysites, Favosites, Propora, Parachaetetes',32,77,-4266753,14391011,'India','Asia',501,'',32.1833,77.9,'WAHR','36259',-26.3697363952,79.2920776615,-26.3697363952,79.2920776615,-26.3697363952,79.2920776615),('Mitchell Quarry, Lisbon, Iowa',1796,'','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','55',NULL,NULL,NULL,'3','More than 100 m','400','40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1078,1235,'Massive core with vugs surrounded by stratified flank deposits.\nStromatopores, corals and abundant crinoids.\nFirst two mostly in living position.\nOther bioherms in the area are Sneckloth, Gerber and Brady.\nMaximum thickness 55 m. 400 m lateral extension.',41,-91,-2956885,-5604593,'United States','North America',101,'',41.9,-91.3833,'','',-27.226747858,-102.751406837,-27.4618115977,-99.5489420712,-27.4618115977,-99.5489420712),('Hunt Quarry, Cedar Co., Iowa',1797,'','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'40','1796',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1078,0,'Plenty of vugs and molds.\nStromatopores and favositid corals (about equally important).\nZaphrentids, heliolitids, diplophyllids and crinoids are also important.\nFenestellid bryozoans and brachiopods present but rare.',41,-91,-2983937,-5599239,'United States','North America',101,'',41.75,-91.2,'','',-27.4176374568,-102.674089032,-27.6508444979,-99.4658701517,-27.6508444979,-99.4658701517),('Lapel, Indiana',1798,'','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1600','1875',0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',1,'Potential reservoir',1079,1131,'Only turbiditc deposits were studied by 1079.\nFlank beds rich in crinoids.\nReassigned to slice 6',40,-85,-3498844,-5250321,'United States','North America',101,'',40.0833,-85.75,'','',-30.377589125,-98.8902864384,-30.5216156907,-95.5863754072,-30.5216156907,-95.5863754072),('Snäckgärdsbaden-Ireviken, Gotland',1799,'Högklint','Silurian','Wenlock','Sheinwoodian',430.50,433.40,7,'Wenlock - early Pridoli',425,427,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','35','2','10 - 100 m wide',NULL,'3','More than 100 m','150','60','809',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','10','50',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present','1','Present','3','Pronounced zonation',NULL,'','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1971,1990,'Position refers to Ireviken\n\nLarge composite reef.\nLayered stromatopores dominate (Coenostroma, Clathrodictyon, Labechia).\nOthers are mostly tabulate corals.\nVisby-Series.\nRef. 1893:\n25 % of matrix is sparite\n20 % micrite\n45 % skeletal sand and debris.\nCalcimicrobes common\n\nAbstract of ref. 1971:\nPatch reefs up to 35 m thick and generally 100-150 m wide, separated by bedded inter-reef sediment, dominate the Högklint Formation (Lower Wenlock) of north-west Gotland. The spacing between adjacent patch reefs is variable, but is commonly 150-350 m. The Högklint is a shallowing sequence, and the patch reefs exhibit a well-developed vertical succession: (1) Axelsro-type patch reefs developed in the underlying Visby Formation; (2) halysitid tabulates capped by laminar stromatoporoids; (3) domical and bulbous stromatoporoids and red algae; (4) cyanobacterial-algal reef crest. The patch reefs expand upwards from an initial bioherm phase with a small base to a laterally extensive biostrome phase. This gives them a thumb-tack appearance. In stage 2 of the bioherm phase, rigid framework development and high reef relief resulted in breakage of angular blocks up to 15 m long, which were incorporated into the reefs or fell into adjacent sediments. Poorly sorted talus haloes (Millingsklint Member) also developed adjacent to stage 2 of the bioherm phase. These include angular blocks and exhibit depositional slopes up to 40° away from the reefs. Stage 3 biostrome development was mainly non-rigid cluster reef, which shed skeletal debris (Domkyrka Member) but few lithified blocks. Stage 4 biostrome development was a reef crest with open to closed frame structure. Storm breakage and overturning produced large blocks with complex cavity fill sequences including double geopetals. Relief during the bioherm phase, indicated by fallen blocks and talus slopes, was up to at least 15 m; during the biostrome phase, it was up to 10 m. ',57,18,-1596208,-654539,'Sweden','Europe',330,'1621, 1893, 1080',57.85,18.4833,'WAHR','13592',-8.37920938826,-49.6680565447,-8.37920938826,-49.6680565447,-8.37920938826,-49.6680565447),('Holmhällar, Gotland',1800,'Eke-Hamra','Silurian','Ludlow','Gorstian',425.60,427.40,7,'Wenlock - early Pridoli',425,422,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','5','2','10 - 100 m wide','450','2','10 - 100 m','500','10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','0','70',0,'no',0,'no','2','6 to 24 reef building species','12','3','Binder guild','1','Present',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1133,821,'Around 5 m thick.\nSubcircular belt 500 m in diameter.\nStromatopores (Plectostroma, Parallelostroma) dominant (50-65 % of reef volume). Others are rugose corals.\nEke beds and Hamra beds',56,18,-1707696,-605138,'Sweden','Europe',330,'1080, 1621',56.925,18.3056,'WAHR','13616',-0.874601823194,-45.4307865237,-0.874601823194,-45.4307865237,-0.874601823194,-45.4307865237),('Korpklint, Gotland',1801,'Visby','Silurian','Wenlock','Sheinwoodian',430.50,433.40,7,'Wenlock - early Pridoli',425,427,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','20','2','10 - 100 m wide','20','2','10 - 100 m',NULL,'60','809',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','10','60',0,'no',0,'no','2','6 to 24 reef building species','21','3','Binder guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1080,821,'Near Visby\nSmall reef, strongly dominated by stromatopores. 20 m thick and wide. Tabulate corals very diverse (16 species dominant), 3 rugose species, 2 stromatoporoids.\nPlenty of reef debris (enriched in crinoids as everywhere on Gotland).\nIncluded is study of Vattenfallet section (ref. 1989) were abundant borings were noted',57,18,-1629966,-646384,'Sweden','Europe',330,'1989, 1990, 2123',57.6,18.25,'WAHR','77411',-8.64335424081,-49.5762319769,-8.64335424081,-49.5762319769,-8.64335424081,-49.5762319769),('Klinte, Gotland',1802,'Klinteberg Beds','Silurian','Ludlow','Homerian',427.40,430.50,7,'Wenlock - early Pridoli',425,423,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','2','Algae','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','1','Red algae','0','30','70',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild','1','Present',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1080,1137,'Relicts of a composite reef.\nPlenty of algae present (\'Sphaerocodium\', Solenopora, Hedstroemia).\nIncludes reefs in Halla beds',57,18,-1656423,-633408,'Sweden','Europe',330,'1621, 2639',57.375,18.2542,'WAHR','13601',-4.23517717346,-47.4530429388,-4.23517717346,-47.4530429388,-4.23517717346,-47.4530429388),('Baerum',1803,'Rytteräker','Silurian','Llandovery','Aeronian-Telychian',433.40,440.80,6,'Rhuddanian-Telychian',435,436,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m',NULL,'15',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',821,1536,'Small lensoid bioherms (6 m length, 2 m thickness). Dominated by Halysitids (tabulate coral) and stromatoporoids.\nOther constructors are favositids, heliolitids and syringoporids.\nGirvanella and bryozoans as binders.\nCollection entered by Foote (1999)',59,10,-2865768,-979467,'Norway','Europe',301,'2247',59.8333,10.2333,'WAHR','14319',-16.9770198813,-58.3411487965,-16.9770198813,-58.3411487965,-16.9770198813,-58.3411487965),('Ringerike',1804,'','Silurian','Wenlock','lower Wenlock',427.40,430.50,7,'Wenlock - early Pridoli',425,427,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','8',NULL,NULL,NULL,'1','Less than 20 m',NULL,'15',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','1','Corals','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',821,1536,'Several bioherms. Individual structures 15 long and 8 m high (maximum).\nDominated by encrusting Girvanella, Rothpletzella, Wetheredella and Halysis. Some Halysitids.\nupper Llandovery bioherms also in area (like 1803).',60,10,-1572648,-1184170,'Norway','Europe',301,'',60.0611,10.2583,'WAHR','79880',-5.20886870932,-52.3127312469,-5.20886870932,-52.3127312469,-5.20886870932,-52.3127312469),('Holmestrand',1805,'Steinsfjorden','Silurian','Wenlock','middle Wenlock',430.50,433.40,7,'Wenlock - early Pridoli',425,426,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','7','Bryozoans','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'90','10','0',0,'no',0,'no','3','25 or more reef building species','82','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',821,2327,'Laterally persistent biostromes with tabulate corals (favositids, heliolitids, Thecia sp. syringoporids), rugose corals, algae, bryozoans, stromatopores, and others.\nSmall bioherms in horizons.\nVery diverse (80 species without algae).',59,10,-1644589,-1156530,'Norway','Europe',301,'',59.4833,10.3,'WAHR','14321',-9.99335133337,-53.9823776925,-9.99335133337,-53.9823776925,-9.99335133337,-53.9823776925),('Skien',1806,'','Silurian','Wenlock','middle Wenlock',430.50,433.40,7,'Wenlock - early Pridoli',425,426,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,'50','1805',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',821,0,'0.5 m high and 2-3 m across.\nSee reef 1805 for more remarks.',59,9,-1697814,-1180152,'Norway','Europe',301,'',59.2,9.6167,'','',-10.4303332866,-54.0875007698,-10.4303332866,-54.0875007698,-10.4303332866,-54.0875007698),('Heröya, Ringerike',1807,'','Silurian','Wenlock','upper Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,424,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'4','More than 1000 m',NULL,'150',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','1','Red algae','60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',821,0,'Thin (1 m) but persistent biostrome, strongly dominated by favositids.',60,10,-1564330,-1182714,'Norway','Europe',301,'',60.1125,10.3306,'','',-7.25360661345,-53.2792375779,-7.25360661345,-53.2792375779,-7.25360661345,-53.2792375779),('Pusku-Suurekivi, Ridala Peninsula',1808,'Ridala','Silurian','Llandovery','Rhuddanian',440.80,443.40,6,'Rhuddanian-Telychian',435,442,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','7',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1082,1536,'Tabulate corals (especially Aulocystis) and stromatopores.\n7 m thick.',58,23,-2615311,-237332,'Estonia','Europe',NULL,'',58.8833,23.5,'WAHR','77386',-19.0664646808,-55.0247187306,-19.0664646808,-55.0247187306,-19.0664646808,-55.0247187306),('St. John Island, Newfoundland',1809,'','Ordovician','Middle Ordovician','Whiterockian',467.30,470.00,4,'late Early - early Middle Ordovician',472,468,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'70','1389',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','11','Siliceous sponges','7','Bryozoans','14','Sponges - bryozoans - (microbes)',NULL,NULL,'50','30','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1083,858,'',50,-57,-2532805,-3837156,'Canada','North America',121,'',50.8167,-57.1667,'','',-4.46879948059,-84.7406952385,-4.46879948059,-84.7406952385,-4.46879948059,-84.7406952385),('Birmingham, Alabama',1810,'Chickamauga','Ordovician','Upper Ordovician','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,457,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','5',NULL,NULL,NULL,'1','Less than 20 m','6','15',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','3','Receptaculitids','70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1085,0,'Largest bioherms 5.3 m thick and 6.1 m long.\r\n47 % bryozoans: nodular, ramose, encrusting, bifoliate.\r\n28 % calathid dasycaldaceans.\r\nOthers are brachiopods, demosponges, solenoporid algae, tabulate corals, Girvanella...',33,-86,-3535370,-6497728,'United States','North America',101,'',33.4167,-86.6667,'WAHR','80602',-19.201631698,-118.726728484,-19.201631698,-118.726728484,-19.201631698,-118.726728484),('Valcour and Garden Islands, New York',1811,'Day Point','Ordovician','Middle Ordovician','lower Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,463,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m','2','2',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1086,0,'Base of Scott Member of Day Point Fm.\nSmall mounds of encrusting trepostome bryozoans and some cyclostomes.\nSome 2 m thick and wide.',44,-73,-3022444,-4916124,'United States','North America',101,'',44.6028,-73.4167,'WAHR','80817',-9.07717236461,-100.316938305,-9.07717236461,-100.316938305,-9.07717236461,-100.316938305),('Wool Point, New York',1812,'Day Point','Ordovician','Middle Ordovician','lower Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,463,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',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','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1086,0,'Upper Scott Member  of Day Point Fm.\nCheiloporella (cyclostome) bryozoan reef.\nCircular colonies up to 3 m in diameter.',44,-73,-2993827,-4908060,'United States','North America',101,'',44.8444,-73.4028,'WAHR','80818',-8.88764708964,-100.164913038,-8.88764708964,-100.164913038,-8.88764708964,-100.164913038),('Isle La Motte, Vermont',1813,'Day Point','Ordovician','Middle Ordovician','lower Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,463,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'2',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild','1','Present',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1086,1587,'Middle Fleury Member of Day Point Fm.\nTabulate corals (Lichenaria) and encrusting bryozoa Batostoma. Corals not in situ.\nOldest coral reef worldwide.\nOverlain by massive bryozoan mounds.',44,-73,-2996252,-4903181,'United States','North America',101,'1622',44.8444,-73.3417,'WAHR','80819',-8.91311562597,-100.129441708,-8.91311562597,-100.129441708,-8.91311562597,-100.129441708),('Lake Champlain region, Vermont',1814,'Crown Point','Ordovician','Middle Ordovician','late Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,460,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','2','Algae','4','Stromatoporoids','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','1','Red algae','20','80','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1086,1587,'Solenopora(?) reef.\nBesides algae, stromatopores and bryozoa important.\nStromatoporoids, tabulate corals, ectoprocts or siliceous sponges also as predominant reef builders in area.\nDivers labechiids and some Pachystylostroma spp. present. Up to seven stromatoporoid species co-occurring.\nTyrpanites borings according to refs. 1621, 1622.\nPrimary aragonitic mineralogy suggested for labechiids by ref. 1653.\n',44,-73,-2994853,-4902218,'United States','North America',101,'1621, 1653',44.8583,-73.3347,'WAHR','63301',-8.90478301324,-100.117110798,-8.90478301324,-100.117110798,-8.90478301324,-100.117110798),('Isle la Motte/Grand Isle, Vermont',1815,'Crown Point','Ordovician','Middle Ordovician','upper Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,460,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'4',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','52','Siliceous sponges - bryozoans - tabulate corals - solenoporaceans - (microbes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1086,1587,'Top of Crown Point Fm.\nZittelella (sponge) makes up up to 50 % of the reefs.\nSponges encrusted by algae (Rothpletzella), bryozoans (Batostoma) and corals (Billingsaria).',44,-73,-3078817,-4920263,'United States','North America',101,'',44.1694,-73.3153,'WAHR','63297',-9.4702357374,-100.515977955,-9.4702357374,-100.515977955,-9.4702357374,-100.515977955),('St. Jean, Quebec',1816,'Crown Point','Ordovician','Middle Ordovician','Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,460,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1086,0,'Largest reef in area (2 m thick, 40 wide) predominated by Billingsaria (tabulate coral). Traces of bryozoa. Other reefs in area with predominance of bryozoa.',45,-73,-2958779,-4893149,'Canada','North America',121,'',45.1583,-73.3292,'WAHR','80829',-8.66424124633,-99.9356647012,-8.66424124633,-99.9356647012,-8.66424124633,-99.9356647012),('Terrebone, Quebec',1817,'Valcour','Ordovician','Middle Ordovician','upper Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,460,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','3','2','10 - 100 m wide','30','3','More than 100 m','200',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','7','Bryozoans','1','Corals','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1086,2057,'Bryozoa (Batostoma) and corals (Billingsaria, Eofletcharia).\nStrong succession \n1. Patches of encrusting Batostoma\n2. Discontinuous layers of sheet-like Billingsaria\n3. Reworked Eofletcheria',45,-73,-2882372,-4900119,'Canada','North America',121,'',45.6958,-73.6167,'WAHR','80831',-8.11089316981,-99.7809637502,-8.11089316981,-99.7809637502,-8.11089316981,-99.7809637502),('Sinking Springs, Virginia',1818,'','Ordovician','Middle Ordovician','Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,460,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1086,0,'Billingsaria and Batostoma as main constituents. Others are stromatopores, Rothpletzella and Girvanella.',37,-79,-3489197,-5690020,'United States','North America',101,'',37.8944,-79.9111,'WAHR','80836',-11.223320737,-108.453608425,-11.223320737,-108.453608425,-11.223320737,-108.453608425),('Huanghuachang II, Yichang, Hubei',1819,'Honghuayuan','Ordovician','Lower Ordovician','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','12',NULL,NULL,NULL,'3','More than 100 m','130',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','7','Bryozoans','7','Bryozoans','73','Bryozoans only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1087,2667,'Batostoma bafflestone reefs and algal-sponge reefsMaximum size: 110 long and 11.5 m thick.Time slice change',30,111,1962020,15153636,'China','Asia',602,'2854',30.8667,111.3833,'WAHR','61728',-18.4097854743,92.7556084051,-18.4097854743,92.7556084051,-18.4097854743,92.7556084051),('Liujiachang, Hubei',1820,'Fenxiang','Ordovician','Lower Ordovician','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m','6',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','6','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1088,0,'Reefs largely composed of bryozoa Batostoma (30% of reef core) and pelmatozoan holdfasts. Others are sponge Archaeoscyphia, \'algae\', and Girvanella.\r\nHigh energy setting.\r\n1-3 m thick, 2-6 m long.',30,111,2017661,15060510,'China','Asia',602,'',30.0833,111.4833,'',NULL,-18.2352726681,91.9459991625,-18.2352726681,91.9459991625,-18.2352726681,91.9459991625),('Lechuguilla, Southern Franklin Mts., Texas',1821,'McKelligon Canyon','Ordovician','Lower Ordovician','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,475,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','6',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','11','Siliceous sponges','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)','3','Receptaculitids','0','100','0',0,'no',1,'yes','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'','1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1089,1090,'Largest mound in area.\r\n6 m thick and 15 m wide. Dominated by mud and 3 skeletal components: Pulchrilamina spinosa (uncertain affinity), lithistid sponge (Archaeoscyphia annulata) and receptaculid alga Calathium.',31,-106,-1304885,-8448725,'United States','North America',101,'1113, 1361, 1401',31.7917,-106.4583,'WAHR','80082',13.4113541682,-121.471421676,13.4113541682,-121.471421676,13.4113541682,-121.471421676),('Blanco County, Texas',1822,'Honeycut','Ordovician','Lower Ordovician','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,475,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'125',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','59','Lithistid sponges - cyanophyceans - pelmatozoans',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1089,0,'Archaeoscyphia Beds\r\nBiostromal unit, persistent but thin.\r\nBesides Archaeoscyphia (lithistid sponge, commonly as chert fragments), Girvanella and pelmatozoan fragments are abundant.',30,-98,-2214911,-8054992,'United States','North America',101,'',30.1667,-98.4167,'WAHR','80088',6.68070609275,-119.234416569,6.68070609275,-119.234416569,6.68070609275,-119.234416569),('Burnet County, Texas',1823,'Honeycut','Ordovician','Lower Ordovician','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,475,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'125','1822',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','59','Lithistid sponges - cyanophyceans - pelmatozoans',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1089,0,'See reef 1822 for remarks.',30,-98,-2186136,-7996899,'United States','North America',101,'',30.75,-98.25,'WAHR','80089',6.88045156387,-118.663867076,6.88045156387,-118.663867076,6.88045156387,-118.663867076),('Kindblade Ranch, Wichita Mts., Oklahoma',1824,'Honeycut','Ordovician','Lower Ordovician','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,475,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',1,'yes','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1089,1361,'See reef 1822 for remarks.',34,-98,-1832747,-7699340,'United States','North America',101,'',34.8333,-98.6333,'WAHR','80090',9.37149582525,-115.379182178,9.37149582525,-115.379182178,9.37149582525,-115.379182178),('Longhorn Mt., Wichita Mts., Oklahoma',1825,'','Ordovician','Lower Ordovician','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,475,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','3',NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','11','Siliceous sponges','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)',NULL,NULL,'0','100','0',0,'no',1,'yes','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1089,1361,'Described as algal sponge mounds.\r\nThickest mound complex: ca. 17 m thick.\r\nIndividual mounds about 3 m.\r\nConsisting of Pulchrilamina, Archaeoscyphia Calathium and Renalcis.\r\nOther localities are Unap Mt. and Kindblade Ranch.',34,-98,-1827087,-7698884,'United States','North America',101,'',34.8667,-98.6667,'WAHR','80092',9.41257874024,-115.365619493,9.41257874024,-115.365619493,9.41257874024,-115.365619493),('Mill Creek, Arbuckle Mts., Oklahoma',1826,'Kindblade','Ordovician','Lower Ordovician','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,475,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','2','Algae','11','Siliceous sponges','45','Siliceous sponges - calcisponges - microbes - (algae)','3','Receptaculitids','0','100','0',0,'no',1,'yes','2','6 to 24 reef building species','6','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1089,1361,'Largest buildup in Arbuckle Mts. is 4 m thick and 17 m wide.\r\nLower mounds: Archaeoscyphia > Calathium > Pulchrilamina > stromatolites.\r\nUpper mounds: Calathium > Archaeoscyphia > stromatolites > Pulchrilamina.',34,-97,-2006013,-7626879,'United States','North America',101,'',34.4167,-97.0833,'WAHR','80097',8.07497344874,-115.029619562,8.07497344874,-115.029619562,8.07497344874,-115.029619562),('Ibex, Confusion Range, Utah',1827,'','Ordovician','Lower Ordovician','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,483,1,0,'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',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','3','Microbes','2','Algae','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)','3','Receptaculitids','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1091,1087,'Earliest Ordovician reefs in House Limestone. \nStromatolites, lithistid sponges, receptaculid algae (Calathium).\nSponges and other metazoans are only accessorial.\n',38,-113,1288619,-7960373,'United States','North America',101,'1089',38.9167,-113.5,'','',27.6086292607,-115.901135391,27.6086292607,-115.901135391,27.6086292607,-115.901135391),('Ibex, Confusion Range, Utah',1828,'','Ordovician','Lower Ordovician','Darriwilian',458.40,467.30,4,'late Early - early Middle Ordovician',472,467,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m','14',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','11','Siliceous sponges','2','Algae','45','Siliceous sponges - calcisponges - microbes - (algae)','3','Receptaculitids','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1091,1087,'Arenigian Wahwah and Juab limestones with conical zittelellid and psarodictyid anthaspidellid sponges.  Also Archaeoscyphia and Calathium.\r\nUp to 14 m in diameter.',38,-113,-156192,-8124582,'United States','North America',101,'1089',38.8667,-113.5,'',NULL,10.2387755587,-123.569332797,10.2387755587,-123.569332797,10.2387755587,-123.569332797),('Columbia Icefield, Jasper, Alberta',1829,'Kotchakan','Ordovician','Lower Ordovician','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,483,1,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'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,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1092,1089,'',52,-117,2479491,-6542747,'Canada','North America',121,'1804',52.3333,-117.5,'','',34.6706497051,-102.158557026,34.6706497051,-102.158557026,34.6706497051,-102.158557026),('Churan, Lena River, Siberia',1830,'Pestrotsvet','Cambrian','Lower Cambrian','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,524,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'20',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',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',1093,0,'Archaeocyath bafflestones with abundant cement. Renalcis also abundant.\nRegularis Zone, Tortuosa Subzone.\nDiscrete mounds.\nRenalcis-rich mounds with archaeocyaths in vicinity.\n\nAbstract of ref. 1830:\nWith the possible exception of some older aggregations of  tubicolous skeletal forms, bioherms in. the Pestrotsvet Formation (Tommotian) of the southeastern Siberian Platform represent Earth\'s earliest metazoan-mediated reefs. They are certainly the earliest known bioconstructions of metazoan-calcimicrobial type. The bioherms are geographically limited to the transitional facies tract of the Siberian Platform, \n  separating restricted lagoonal from deep ramp and slope sediments.\nBioherms are intergrowths of archaeocyaths, calcimicrobes (Renalcis) and rare coralomorphs (Cysticyathus) in lime\nmudstone which was cemented early on the sea poor. They consist of meter-scale mounds occurring either singly or stacked together.\nMounds can be categorized into component domains occupied by associations of lime mud, archaeocyaths, calcimicrobes and \n  cement. Some mounds are simply a conglomeration of such domains, with no discernible pattern of internal distribution, while \n  others possibly show incipient ecological succession. The calcimicrobe Renalcis was the major bioconstructor; it and the \n  synsedimentary cement were the principal contributors to framework construction. Archaeocyaths of themselves rarely \n  produced a framework, except where stereoplasm was abundant. \n  Nevertheless, the archaeocyaths provided substrates for the Renalcis and cement, and facilitated the development of\ninternal cavities.\n  Archaeocyaths appeared, as bioconstructors, in the basal Tommotian sunnaginicus Zone. In the succeeding regularis Zone and thereafter, they flourished throughout the mounds, in some cases forming thickets of large sticklike cups atop mature mounds.\nThe bioconstructional regime established in these Tommotian bioherms prevailed throughout the Early Cambrian reef-building phase, particularly in argillaceous limestone facies. Likewise, the trophic web of this very early Cambrian community remained a  blueprint for shallow wafer, open, marine habitats throughout the epoch.',60,125,-2245834,-46248,'Russia','Asia',624,'',60.7833,125.0167,'WAHR','80802',3.36241382537,-74.1015385446,3.36241382537,-74.1015385446,3.36241382537,-74.1015385446),('Gonam, Siberia',1831,'Pestrotsvet','Cambrian','Lower Cambrian','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,524,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'50',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'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,'','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1093,0,'',57,132,-1594125,-302850,'Russia','Asia',624,'',57,132.25,'WAHR','50419',8.11682652281,-76.4837180284,8.11682652281,-76.4837180284,8.11682652281,-76.4837180284),('Sukharikha River, Igarka, Siberia',1832,'Krasnoporog','Cambrian','Lower Cambrian','upper Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,522,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m',NULL,'40',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2','Shelf/platform margin','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1093,0,'',67,86,-4257258,968489,'Russia','Asia',624,'',67.5,86.5,'WAHR','80841',-11.9582154401,-65.1228623915,-11.9582154401,-65.1228623915,-11.9582154401,-65.1228623915),('Khara-Ulakh Mts., Siberia',1833,'Tyuser','Cambrian','Lower Cambrian','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,524,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','16','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1093,2685,'Mostly domain 1 of ref. 1093.\nArchaeocyaths dominant. Small Renalcis.\nBurrowed mud.\nSome cement.\nlenacius-primigenius Zone.',71,127,-3576020,-652206,'Russia','Asia',624,'',71.5667,127.3667,'WAHR','80950',-6.41787501401,-78.7440311379,-6.41787501401,-78.7440311379,-6.41787501401,-78.7440311379),('Olenyek Uplift, Siberia',1834,'Pestrotsvet','Cambrian','Lower Cambrian','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,524,3,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1093,0,'',71,123,-3596836,-445372,'Russia','Asia',624,'',71.5,123,'','',-6.85954430401,-77.4230420448,-6.85954430401,-77.4230420448,-6.85954430401,-77.4230420448),('El Desastre, Fortuna',1835,'','Neogene','Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,9,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1094,0,'Coral and coralgal framestones about 20 m thick. Reef complex is 70 m thick.',38,-1,5082877,-189981,'Spain','Europe',304,'',38.2167,-1.1333,'WAHR','70514',37.4255356452,-2.76020074995,37.4238121594,-2.76365448909,37.8265375039,-1.24072797753),('Tawuia, Stone Knife River, N.W.T.',1836,'Little Dal Group','Proterozoic','Upper Proterozoic','Neoproterozoic',542.00,999.00,-1,'Neoproterozoic',770,770,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown',4,'Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1095,1096,'Non-stromatolitic reef.\nMicrobes similar to Paleozoic forms like Girvanella and Renalcis.\nReef complex 200 m thick and 800 m wide, but seperated by shaly layers.\nBelow storm wave base?\nAbundant marine cement, no primary micrite.\nReef flank with talus wedges.',64,-129,-6348629,-7546430,'Canada','North America',121,'',64.8167,-129.6833,'','',8.56150843713,-153.299118819,8.58552061585,-158.022629463,8.58552061585,-158.022629463),('Disneyland, Mackenzie Mts., N.W.T.',1837,'','Proterozoic','Upper Proterozoic','Neoproterozoic',542.00,999.00,-1,'Neoproterozoic',770,770,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'100',NULL,0,'Tropical or unknown',4,'Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','1','Less than 30% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1096,0,'',65,-130,-6316170,-7520691,'Canada','North America',121,'',65.05,-130.6833,'','',8.87437360141,-152.925977902,8.8985882701,-157.649638311,8.8985882701,-157.649638311),('Attems/Plabutsch',1838,'Plabutsch','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','90',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'55','5','40',0,'no',0,'no','3','25 or more reef building species','26','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1098,2572,'formerly known as \'Barrandei Limestone\', probably ranging from the Upper Emsian to the Lower Givetian, thickness about 100 m.\nCoral framestones and coral-stromatopore floatstones.\nAlgae and calcimicrobes associated',47,15,-4582584,4113693,'Austria','Europe',301,'',47.1,15.3833,'WAHR','76717',-26.8435482675,19.7946455161,-26.8435482675,19.7946455161,47.1,15.3833),('Terrades, Pyrenees',1839,'','Cambrian','Lower Cambrian','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,519,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20',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','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,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1099,0,'Abstract ref. 1099:\nThe Lower Cambrian outcrops near Terrades (Gerona province, Spanish Pyrenees) are mainly siliciclastic interlayered with some bioclastic limestones or reef mounds. Previous works (Abad, 1987, 1989) allowed us to recognize three stratigraphic sections representative of the bioconstructed levels, as well as their spatial relationship and correlation. Microbial mounds are mainly formed by calcimicrobes (Epiphyton and Renalcis). Archaeocyathans are the secondary elements in these boundstones and the following genera have been identified: Taylorcyathus, Gloriosocyathus, Rasetticyathus, Erismacoscinus, Mennericyathus, Coscinocyathus and Anthomorpha. These mounds are superimposed and can reach up to 20 m in thickness. Small mounds are present over the big calcimicrobial mounds. These are buildups by branched colonial archaeocyathans with a high cups density mainly of Anthomorpha and Erismacoscinus.\nThe skeletal metazoans are surrounded by calcimicrobial elements. Lenticular carbonatic beds are located one\nkm away from the mounds. These beds are bioclastic, nodular and brechoid limestones, interstratified with siliciclastic sediments. The main components in the carbonatic levels are calcimicrobes and archaeocyathans, lacking of building mounds. Sedimentological characteristics suggest a restricted shallow area. Thirty genera of Archaeocyathans have been identified among which nine are new. The Terrades assemblage is typical for the Archaeocyatha Zone VII of the Upper Ovetian (Perejon, 1986 and in press). Some genera are common with Sardinia (i.e. Taylorcyathus, Rasetticyathus, Antoniocoscinus, Porocoscinus) and Morocco (i.e. Inacyathella). The relationship with the folded region of Altai Sayan have been based upon nineteen common genera, i.e. Nalivkinicyathus; and its shares with the Siberian Platform localities sixteen genera, a.o. Gloriosocyathus and Muchattocyathus. ',42,2,-5245013,9645533,'Spain','Europe',304,'',42.3167,2.8333,'WAHR','81291',-64.7119399386,9.22529491709,-64.7119399386,9.22529491709,-64.7119399386,9.22529491709),('Issafene',1840,'','Cambrian','Lower Cambrian','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,514,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','50',NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1100,0,'Trend from Dra to Jbal Irhoud (not found).\nBioherms are complex asociations of mounds. Up to 50 m thick.\n20-30 % archaeocyaths (mainly Agastrocyathus and Halysicyathus).\n20-70 % algae (microbes).',32,-4,-6514582,8526164,'Morocco','Africa',714,'',32.2,-4.3667,'','',-73.9834193965,-12.428407967,-75.1207430136,-17.8887892702,-75.1207430136,-17.8887892702),('Fanning River, Queensland',1841,'Burdekin','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild','1','Present','1','Present',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1101,1334,'Only rugose corals.\nBetter adapted to marginal marine stress.\nAlthough mostly in situ, coral are source of carbonate in the area.\nBorings evident form photographs.\nPosition changed',-19,146,-2265663,15308449,'Australia','Oceania',801,'',-19.75,146.4333,'WAHR','106535',-17.2020876254,131.06786432,-17.2020876254,131.06786432,-19.0344699021,165.579029851),('Heceta Island, Alexander Terrane, Alaska',1842,'Heceta','Silurian','Upper Silurian','Wenlock/Ludlow',423.00,433.40,7,'Wenlock - early Pridoli',425,422,1,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','6','Calcisponges','66','Stromatolites-\'sphinctozoans\'-(stromatoporoids, algae, corals)',NULL,NULL,'20','30','50',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'','2','Medium zonation','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1102,1650,'Recrystallized massive stromatopores, halysitis, solenoporids and Renalcis.\n\nBarrier reef with Epiphyton, other calimicrobes, and aphrosalpingid sponges (sphinctozoans).\n\nAbstract ref. 1650:\nLower to Upper Silurian (upper Llandovery-Ludlow) limestones belonging to the Heceta Formation record several episodes of reef growth in the Alexander terrane of southeastern Alaska. As the oldest carbonates of widespread distribution in the region, the Heceta limestones represent the earliest development of a shallow-marine platform within the Alexander arc and the oldest foundation for reef evolution. The excellent preservation of biostromes, fringing and barrier reefs, and a mud mound in shelf, shelf margin, and slope deposits, respectively, contrasts with the restricted occurrence of many marine sediments that originated within other island arcs. Hence, these deposits provide important insights into the dynamic processes, styles, and bathymetry associated with reef growth in tectonically active oceanic islands. Massive stromatoporoids, corals, and red algae are preserved in fragmental rudstones and represent a fringing reef that formed at the seaward edge of the incipient marine shelf. Accessory constitutents in this  reef include crinoids and the cyanobacterium Girvanella. Small biostromes were contructed by ramose corals and stromatoporoids on oncolitic substrates in backreef or lagoonal environments. These buildups were associated with low-diversity assemblages of brachiopods and with gastropods, amphiporids, calcareous algae and cyanobacteria. Microbial boundstones reflect the widespread encrustation of cyanobacteria and calcified microproblematica on shelly debris as stromatolitic mats that resulted in the development of a stromatactoid-bearing mud mound and a barrier reef complex. Epiphytaceans, other microbes, and aphrosalpingid sponges were the primary framebuilders of the barrier reefs. These buildups attained significant relief at the shelf margin and shed detritus as slumped blocks and debris flows into deep-water sites along the slope. The similarity of these stromatolitic-aphrosalpingid reefs to those from Siluro-Devonian strata of autochthonous southwestern Alaska suggests paleobiogeographic ties of the Alexander terrane to cratonal North America during the Silurian. ',55,-133,692865,-7403462,'United States','North America',101,'',55.7472,-133.4472,'WAHR','79357',6.85653876746,-118.070892432,6.85653876746,-118.070892432,6.85653876746,-118.070892432),('Prince of Wales Island, Alaska',1843,'Heceta','Silurian','Upper Silurian','Wenlock/Ludlow',423.00,433.40,7,'Wenlock - early Pridoli',425,422,1,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,'','3','Microbes','2','Algae','66','Stromatolites-\'sphinctozoans\'-(stromatoporoids, algae, corals)','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,'','2','30-60% micrite','2','10-25% sparite',NULL,'','0','',0,'No or unknown reservoir potential',1102,1345,'Ludlovia association of ref. 1102.\nDiverse microbes and algae.\nOthers are aphrosalpingoid sponges.',55,-133,709439,-7391818,'United States','North America',101,'',55.7917,-133.1833,'WAHR','79355',6.7333523822,-117.976191169,6.7333523822,-117.976191169,6.7333523822,-117.976191169),('West Keels, Newfoundland',1844,'West Centre Cove','Cambrian','Lower Cambrian','pre-Tommotian',529.00,541.00,1,'Nemakit/Daldynian - Toyonian',520,535,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','8','Serpulids, worms, vermetids','8','Serpulids, worms, vermetids','76','Worms only',NULL,NULL,'10','90','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1103,0,'Earliest know Metazoa buildups.\nBuildups consist of Ladatheca cylindrica.\n\nAbstract ref. 1103:\n\'Ladatheca\' cylindrica (Grabau, 1990) was a eurytopic metazoan with a calcareous operculum and an elongate, gently tapering conch up to 15+ cm long and with an apical angle of approximately 0.75-2.0.degree.. This apparent polychaete was geographically widespread in the sub-trilobitic Lower Cambrian of middle latitude, siliciclastic (middle and upper Placentian Series, Avalon Zone) and low latitude, carbonate platform (Tommotian Stage, Siberia(?) and Kazakhstan; and, probably, the upper Meishucunian Stage, southwestern China) sequences. In situ conchs (vertically to steeply inclined, apex down) of \'Ladatheca\' cylindrica are common in deep subtidal, siliciclastic mudstones (Chapel Island Formation) and in a peritidal algal mud mound(?) limestone (West Centre Cove Formation) in southeastern Newfoundland. Closely juxtaposed conchs locally form a worm reef at the top of the West Centre Cove Formation. This structure is older than the oldest archaeocyathan build-ups and is the earliest known metazoan-constructed biostrome. \'Ladatheca\' cylindrica was a dominant element of the sessile benthos prior to its apparent ecological displacement by Coleoloides typicalis Walcott, 1889, in the upper Placentian Series. ',48,-53,-6720330,-3951691,'Canada','North America',121,'',48.6028,-53.4056,'WAHR','80844',-60.6735790943,-120.111519265,-78.8047794033,-98.4491709907,-78.8047794033,-98.4491709907),('Baumann Fjord S, Ellesmere I., N.W.T.',1845,'','Silurian','Wenlock','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','400',NULL,NULL,NULL,'3','More than 100 m',NULL,'60',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','1','Red algae','60','30','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1104,1712,'Reefs 1, 2 of ref. 1104.\nPhase 1 mud mound cored pinnacle reefs.\nAll reefs of phase 1 have 300-400 m minimum thickness and a width of 300-1000 m.\nCoral-microbial boundstone overlain by oolite.\nTabulate corals>rugose corals>algae (Solenopora, Pseudochaetetes), stromatopores and lithistid sponges.\nRenalcis and other microbes very abundant.\nReefs formed basinward of platform margin.\nReef apron about 1 km around pinnacles. Olistolites up to 15 m in diameter.',77,-85,382365,-3048061,'Canada','North America',121,'',77.3667,-85.45,'','',4.75509682415,-78.5420126552,4.75509682415,-78.5420126552,4.75509682415,-78.5420126552),('Baumann Fjord N, Ellesmere I., N.W.T.',1846,'','Silurian','Wenlock','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','350',NULL,NULL,NULL,'3','More than 100 m',NULL,'60','1845',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',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',1104,1712,'reefs 3, 4 of ref.  1104.\nsee reef 1845 for remarks.',77,-84,381789,-3018555,'Canada','North America',121,'',77.55,-84.5667,'WAHR','79384',4.85019285932,-78.2934641921,4.85019285932,-78.2934641921,4.85019285932,-78.2934641921),('S Ellesmere Island, N.W.T.',1847,'','Silurian','Upper Silurian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,418,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','150',NULL,NULL,NULL,'3','More than 100 m','600','150','2734',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',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',1104,1861,'Phase 2 reefs of ref. 1104. Pinncacle reef (mud mound at base).\nMaximum thickness 150 m, 300-600 m wide.\nFasciculate and ceroid rugose corals > lamellar stromatopores > favositids > bryozoans.\nMarine cement up to 30 %.',76,-89,388563,-3192122,'Canada','North America',121,'',76.45,-89.5,'','',6.53966466849,-70.5360872635,6.53966466849,-70.5360872635,6.53966466849,-70.5360872635),('S Ellesmere Island, N.W.T.',1848,'','Devonian','Upper Devonian','Pridoli-Lochkovian',410.80,423.00,8,'middle Pridolian - middle Pragian',412,416,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','150',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1104,0,'seef reef 1847.',76,-89,-1381820,-1949169,'Canada','North America',121,'',76.45,-89.5,'','',5.90341262222,-65.670806678,5.90341262222,-65.670806678,23.383349815,-124.30121552),('S Ellesmere Island II, N.W.T.',1849,'','Silurian','Upper Silurian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,418,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','150',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1104,0,'see reef 1847 for remarks.',76,-87,338512,-3153451,'Canada','North America',121,'',76.4667,-87.3333,'','',6.36744237503,-70.055569039,6.36744237503,-70.055569039,6.36744237503,-70.055569039),('Colin Archer Pen., Devon Is., N.W.T.',1850,'','Silurian','Upper Silurian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,418,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',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',1104,0,'',76,-90,401712,-3210922,'Canada','North America',121,'',76.3833,-90.2833,'','',6.55054056063,-70.7327487429,6.55054056063,-70.7327487429,6.55054056063,-70.7327487429),('Horlick Quarry, Racine, Wisconsin',1851,'Racine','Silurian','Wenlock','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','8',NULL,NULL,NULL,'1','Less than 20 m',NULL,'70',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','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','25','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1105,0,'Reef core is massive crinoid-dominated wackestone with large floating stromatopores. \nSome stromatolites.\n\nOther collections from Patzkowsky refer to nearby quarries with similar fauna.\n \n\nAbstract of ref. 1105:\nThe Racine Formation of southeastern Wisconsin contains a diverse reef fauna of Silurian (Wenlockian) age. A collection of more than 10,000 specimens from this fauna includes 191 species and 38 guilds of reef constructors, binders, bafflers and dwellers. Constructors and binders include stromatoporoids, tabulates, rugosans and bryozoans; bafflers include branching tabulates and dendroid rugosans. Only locally do these groups form a skeletal framework, and for the most part, their remains are separated by reef matrix. Reef dwellers are represented by diverse guilds of brachiopods, gastropods, cephalopods, trilobites and echinoderms, and they also include receptaculitids, sponges, solitary rugosans, bryozoans and bivalves. Tiering within the fauna is well developed and probably extended to a height of 1 m above reef surfaces. This reef fauna exhibits higher species diversity, greater numbers of guilds and more extensive tiering than Silurian level-bottom communities. Relatively few of its taxa, however, are restricted to Silurian reef environments. Constructors, binders and bafflers in the reef fauna have morphologic and taxonomic parallels in level-bottom communities, as do nearly all taxa of reef dwellers. Higher diversity in the reef fauna is not a function of specialized reef guilds and species, but results from packing of more species into the same guilds which are present in level-bottom communities. In this regard, the Silurian reef fauna differs fundamentally from that of today and reflects the generally low grade of ecologic complexity of the Paleozoic evolutionary fauna. ',42,-87,-3093143,-5292011,'United States','North America',101,'',42.7167,-87.8833,'WAHR','13069',-27.3049366007,-89.5142317003,-27.3049366007,-89.5142317003,-27.3049366007,-89.5142317003),('Grafton, Wisconsin',1852,'','Silurian','Wenlock','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','5',NULL,NULL,NULL,'2','10 - 100 m','60','70','1851',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','4','Stromatoporoids','7','Bryozoans','54','Bryozoans - stromatoporoids',NULL,NULL,'30','0','70',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','2','Medium zonation',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1105,0,'Lime Kiln Park Quarry\n\n3-5 m thick, 50-60 m wide. Lacking flank beds.\n62 % stromatopores, 20 % bryozoans.\nOthers are crinoids and very rare rugose corals.\nMicrite abundant in lower part.',43,-87,-3026160,-5266079,'United States','North America',101,'',43.3167,-87.95,'','',-26.7113179319,-89.4020174663,-26.7113179319,-89.4020174663,-26.7113179319,-89.4020174663),('Amtjärn, Siljan',1853,'Boda Limestone','Ordovician','Upper Ordovician','Hirnantian',443.40,445.20,5,'Darriwilian - Ashgillian',452,444,2,0,'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','1','Shelf/platform interior','1','Above fair weather wave base','2','Algae','1','Corals','85','Corals - (phylloid) algae','2','Green algae','40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'','1','Present','2','Medium zonation',NULL,'','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1106,1823,'Described as lense-shaped reefs with slight relief. \nBoda-Limestone.\nReef building fossils: corals and algae.\nOnly Codiacean Palaeoporella variabilis is quantitatively important.\nMore abundant are brachiopods, trilobits, gastropods and bivalves.\nFlank beds rich in pelmatozoans (not from reef).',60,15,-4062396,-636399,'Sweden','Europe',330,'',60.9333,15.05,'WAHR','73465',-21.789558806,-61.219177459,-21.789558806,-61.219177459,-21.789558806,-61.219177459),('Crown Point, Elk River, Tennessee',1854,'Carters Limestone','Ordovician','Upper Ordovician','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,457,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','70','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'','3','Pronounced zonation',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1107,1113,'Carters limestone\r\nWell developed ecological succession.\r\nStromatopores dominant (Stomatocerium only), second are diverse tabulate corals (Lichenaria, Tetradium, Foerstphyllum (=Columnaria), Favistella, Nyctopora and Paleoalvelites.\r\nOthers are bryozoans, diverse algae (Solenopora, Vermiporella, Girvanella ..)',35,-86,-3354151,-6445006,'United States','North America',101,'1723',35.0167,-86.9417,'WAHR','80005',-17.8623460328,-117.77279155,-17.8623460328,-117.77279155,-17.8623460328,-117.77279155),('Cap River, Anticosti Isl., Quebec',1855,'Chicotte','Silurian','Llandovery','Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,430,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,'40','1415',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'20','0','80',0,'no',0,'no','2','6 to 24 reef building species','6','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1110,1038,'Lower Reef Cluster\nLess than 1 m thick and 10-20 m wide.\nLow domical to laminar stromatopores dominate - up to 70 % of reef core (Clathrodictyon, Petridiostroma and Strmatopora).',49,-63,-3037146,-3557773,'Canada','North America',121,'',49.2,-63.0833,'WAHR','25251',-22.7051501179,-80.1272804261,-22.7051501179,-80.1272804261,-22.7051501179,-80.1272804261),('Stine Spur, Coffeyville, Kansas',1856,'','Carboniferous','Upper Carboniferous','Desmoinesian',307.00,315.20,13,'Bashkirian - Kasimovian',302,307,2,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','4','Stromatoporoids','75','Stromatoporoids or chaetetids only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1111,0,'Chaetetid biostrome in situ.\nTypical example of an autobiostrome.',37,-95,-477611,-3161591,'United States','North America',101,'',37.0833,-95.6667,'','',-7.45554667786,-32.0039245691,-7.45554667786,-32.0039245691,-5.88394043034,-53.2650980825),('Chickasaw, Arbuckle Mts., Oklahoma',1857,'','Ordovician','Upper Ordovician','early Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,457,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',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','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1112,0,'1 m high, some m long bryozoan reef (cruststone and bindstone).\r\nProbably several trepostome species, but only Batostoma chazyensis was identified.',34,-96,-2643207,-7325292,'United States','North America',101,'',34.4931,-96.9583,'WAHR','80713',-21.1470678744,-125.736139131,-21.1470678744,-125.736139131,-21.1470678744,-125.736139131),('East Cape R., Ellesmere Isl., N.W.T.',1858,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','10',NULL,NULL,NULL,'1','Less than 20 m',NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','2','Algae','9','Tubiphytes','24','Tubiphytes - algae - cyanophyceans - (bryozoans) - (sponges)','2','Green algae','10','80','10',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1114,0,'Small patch reefs or tabular reefs. Up to 10 m thick.\nShallow shelf.\nPalaeoaplysina strongly dominant (85 %).\nOther algae are dasycladaceans.\nTubiphytes and some bryozoans are important.',80,-81,4554795,412362,'Canada','North America',121,'',80.1333,-81.75,'','',31.801883451,3.57186508125,31.801883451,3.57186508125,28.839798809,-19.731153884),('W Ellesmere Isl. I, N.W.T.',1859,'','Permian','Lower Permian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,289,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','10',NULL,NULL,NULL,'1','Less than 20 m',NULL,'20',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','2','Algae','9','Tubiphytes','24','Tubiphytes - algae - cyanophyceans - (bryozoans) - (sponges)','2','Green algae','0','70','30',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1114,0,'see reef 1858 for remarks.',80,-81,5193846,612508,'Canada','North America',121,'',80.05,-81.3333,'','',32.0929796908,3.84753031547,32.0929796908,3.84753031547,29.9303531035,-16.2433389221),('W Ellesmere Isl. II, N.W.T.',1860,'','Permian','Lower Permian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,289,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,'150',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','2','Algae','9','Tubiphytes','24','Tubiphytes - algae - cyanophyceans - (bryozoans) - (sponges)','2','Green algae','5','75','20',0,'no',0,'no','2','6 to 24 reef building species','6','2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1114,0,'Phylloid boundstone facies.\nEugonophyllum, Neoanchicodium and Ivanovia.\nTubiphytes encrusting phylloids.\nSome bryozoa.\nMounds 15 m thick and 10-50 m wide.',79,-83,5180616,555448,'Canada','North America',121,'',79.6667,-83,'','',31.9914458874,3.29080347101,31.9914458874,3.29080347101,29.7362556507,-16.7528287636),('Mc Kinley Bay, Ellesmere Isl., N.W.T.',1861,'','Permian','Lower Permian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,289,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,'150','1860',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','2','Algae','9','Tubiphytes','24','Tubiphytes - algae - cyanophyceans - (bryozoans) - (sponges)','2','Green algae','5','75','20',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1114,0,'See reef 1860 for remarks.',81,-79,5269194,725572,'Canada','North America',121,'',81.1167,-79.0833,'','',32.6912180119,4.98038718321,32.6912180119,4.98038718321,31.5752240511,-15.64640583),('Mc Kinley Bay, Ellesmere Isl., N.W.T.',1862,'','Permian','Lower Permian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,296,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','2','Algae','9','Tubiphytes','24','Tubiphytes - algae - cyanophyceans - (bryozoans) - (sponges)','2','Green algae','10','70','20',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1114,0,'See reef 1860 for remarks.',81,-79,4618326,524508,'Canada','North America',121,'',81.1167,-79.0833,'','',32.2918714696,4.70049029158,32.2918714696,4.70049029158,30.3741078723,-19.1041379812),('Delphi, Indiana',1863,'Louisville','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','62',NULL,NULL,NULL,'3','More than 100 m',NULL,'1600','1875',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'20','0','80',0,'no',0,'no','2','6 to 24 reef building species','9','1','Constructor guild',NULL,'',NULL,'',NULL,'','3','Pronounced zonation','3','More than 60% micrite',NULL,'','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1115,1126,'62 m thick reef complex.\nFaunal abundance distribution maps.\nStromatopores far more important than favositid corals.',40,-86,-3390632,-5302249,'United States','North America',101,'1131',40.5833,-86.6667,'WAHR','22818',-29.6906407299,-99.4864857544,-29.8488547226,-96.2047285977,-29.8488547226,-96.2047285977),('Red House Branch, Tennessee',1864,'Holston','Ordovician','Upper Ordovician','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,455,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','8',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','7','Bryozoans','3','Microbes','60','Bryozoans - Pelmatozoans - (microbes)',NULL,NULL,'80','0','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1116,1613,'Interpreted as deeper water patch reefs on the proximal slope. 2-10 m in diameter.\r\nStromatactis mounds and cavities common.\r\nBryozoa and no algae.\r\n\r\nAbstract ref. 1116:\r\nInvestigation of extensive skeletal grainstone deposits that comprise much of the Middle Ordovician sequence in East Tennessee revealed 2 distinct carbonate buildup complexes. The Rockdell Formation comprises abundant pelmatozoan-bryozoan grainstones and packstones and lesser deposits of lime wackestone. These deposits represent carbonate sand shoals, consisting of a mixture of in situ and transported skeletal grains, which surround relatively small, isolated to anastomosing, lime-mud mounds. The Rockdell buildup was developed in shallow-water, high-energy conditions on a relatively stable platform. The Holston Formation is dominated by bryozoan-pelmatozoan packstones that surround roughly elliptical masses of bryozoan wackestone/boundstone. The Holston represents a series of lime-mud bryozoan patch-reefs that were surrounded by piles of in situ skeletal sand produced in pelmatozoan-bryozoan thickets. The Holston buildup developed in deeper water on the outer platform or perhaps downslope. Recognition and distinction of these 2 buildups is based on consideration of a number of criteria including:\r\ncolor, overall composition and distribution of flora and fauna; composition and distribution of bryozoan fauna; types and distribution of component lithofacies; and character of associated lime-mud deposits. Distinction of these buildups has major importance in the determination of East Tennessee paleogeography during the Middle Ordovician and also has implications for possible hydrocarbon exploration in these deposits. The criteria applied here may be useful in making distinctions among other carbonate buildups in the geologic record. ',36,-82,-3486706,-6015160,'United States','North America',101,'',36.3333,-82.8333,'WAHR','80594',-19.0166653792,-114.192300827,-19.0166653792,-114.192300827,-19.0166653792,-114.192300827),('Cedar Springs, Tennessee',1865,'Rockdell','Ordovician','Upper Ordovician','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,455,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans','3','Microbes','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1116,1613,'Shallow water mud mounds, mostly formed by hydrodynamic activity and trapping by bryozoans.\r\nSmall 0.3-2 m mounds. Encrusting bryozoans and algae dominant.',36,-83,-3457049,-6041708,'United States','North America',101,'',36.4167,-83.1667,'WAHR','80597',-18.7838896724,-114.358855826,-18.7838896724,-114.358855826,-18.7838896724,-114.358855826),('Gate City, Virginia',1866,'Rockdell?','Ordovician','Upper Ordovician','early Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,457,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','60',NULL,NULL,NULL,'4','More than 1000 m',NULL,'115',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','4','Others','70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1117,0,'Shallow ramp buildup of several stacked biostromes.\n60 m thick, 60 km width.\nAll buildups in the area interpreted as shallow ramp setting.',36,-82,-3485058,-5987785,'United States','North America',101,'',36.4833,-82.6,'','',-10.8006202612,-111.030940651,-19.2589867413,-113.991735872,-19.2589867413,-113.991735872),('Rockdell, Virginia',1867,'Rockdell','Ordovician','Upper Ordovician','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,457,3,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','85','4','More than 1000 m wide','35000','4','More than 1000 m','50000','115','1866',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','4','Others','70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1117,0,'Biostromal 85 m thick and 50 x 35 km laterally.\nOn ramp buildup.',36,-82,-3473825,-5934215,'United States','North America',101,'',36.8333,-82.1667,'','',-10.7880403233,-110.52894073,-19.1961183387,-113.473576651,-19.1961183387,-113.473576651),('Tazewell, Virginia',1868,'Rockdell?','Ordovician','Upper Ordovician','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,453,1,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','35',NULL,NULL,NULL,'4','More than 1000 m',NULL,'115','1866',0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','4','Others','60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1117,0,'On-ramp buildup. Biostromal. 35 m thickness, 45 km diameter.',37,-81,-3479257,-5865059,'United States','North America',101,'',37.1333,-81.5333,'','',-24.7195198742,-113.774786956,-24.7195198742,-113.774786956,-24.7195198742,-113.774786956),('Porterfield, Virginia',1869,'Effna Limestone','Ordovician','Upper Ordovician','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,457,3,0,'Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','250',NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','7','Bryozoans','13','Echinoderms','60','Bryozoans - Pelmatozoans - (microbes)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1117,0,'Marine cement important.\nMostly wackestone with  ramose bryozoans.\nEncrusting bryozoans locally common. Other fossils are pelmatozoans, brachiopods, trilobites, Girvanella and sponge spicules.\n250 m thick, 20 km wide.\nDownslope buildup.\nAll buildups of this type similar to Waulsortian mud mounds in dominance of carbonate mud, low content of frame builders, presence of baffling organisms abundant stromatactis and echinoderm flank beds.\nHigh energy setting for mounds, but surrounded by deep ramp shaly limestone (sometimes anoxic).\nFibrous and blocky cements up to 18 %.\n',36,-81,-3504800,-5870717,'United States','North America',101,'',36.9167,-81.5,'','',-11.0932364628,-110.075451099,-19.453604061,-112.970812119,-19.453604061,-112.970812119),('Effna, Virginia',1870,'Effna Limestone','Ordovician','Upper Ordovician','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,457,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','65','4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250','1869',0,'Tropical or unknown',3,'Ramp or Slope','3b','Deeper slope or outer ramp','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1117,0,'65 m thick, 65 x 25 km laterally.\nElongate form.\nCarbonate sands common.',37,-81,-3505090,-5842851,'United States','North America',101,'',37.05,-81.25,'','',-11.1318398704,-109.833942503,-19.4672307178,-112.716570726,-19.4672307178,-112.716570726),('Catawba, Virginia',1871,'','Ordovician','Upper Ordovician','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,457,1,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','50','4','More than 1000 m wide','1000','4','More than 1000 m','8000',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',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1117,0,'Biostromal downslope buildup.\n160 m thick, 8 x 1 km wide.\nMound-like configuration with domelike mud cores up to 50 m thick.\nAssociated hardground surfaces.',37,-80,-3522887,-5738442,'United States','North America',101,'',37.4167,-80.25,'','',-11.3992455643,-108.982765454,-19.6446095897,-111.80559511,-19.6446095897,-111.80559511),('Murat, Virginia',1872,'Murat Limestone','Ordovician','Upper Ordovician','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,453,1,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','65',NULL,NULL,NULL,'4','More than 1000 m',NULL,'250','1869',0,'Tropical or unknown',3,'Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','7','Bryozoans','7','Bryozoans',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'','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',1117,0,'Well developed core facies.\n65 m thick, 25 km wide.\nAssociated hardground surfaces.',37,-79,-3528168,-5676508,'United States','North America',101,'',37.6667,-79.6667,'','',-25.0285694105,-112.071538216,-25.0285694105,-112.071538216,-25.0285694105,-112.071538216),('Staunton, Virginia',1873,'','Ordovician','Upper Ordovician','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,455,1,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','55',NULL,NULL,NULL,'4','More than 1000 m',NULL,'250','1869',0,'Tropical or unknown',3,'Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','4','Others','60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1117,0,'Three small isolated buildups, locally reefal with abundant bryozoans and calcareous algae.\nDownslope buildup.\n20-55 m thickness, 3-8 km wide.',38,-79,-3513983,-5608889,'United States','North America',101,'',38.0833,-79.0833,'','',-24.8964105593,-111.402259353,-24.8964105593,-111.402259353,-24.8964105593,-111.402259353),('Garnier Bay, Somerset Isl., N.W.T.',1874,'Douro','Silurian','Ludlow','Ludlovian',423.00,427.40,7,'Wenlock - early Pridoli',425,421,2,0,'Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'125','1433',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','11','Siliceous sponges','1','Corals','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,'80','0','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present',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',1118,887,'eight species of corals listed. Two added for sponges, one for bryozoans',73,-92,454141,-3598619,'Canada','North America',121,'2334',73.9167,-92.1667,'WAHR','713',5.45772207355,-75.5550138929,5.45772207355,-75.5550138929,5.45772207355,-75.5550138929),('Presque Isle Co. W, Michigan',1875,'','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1600',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','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,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite',NULL,'','0','',2,'Actual reservoir',1119,1186,'Subsurface data.\nProducing reservoirs.\nPorosity 3.8-19.6 % (8.5 % average).\n',45,-84,-3018036,-4886490,'United States','North America',101,'',45.3167,-84.2333,'','',-25.6478130127,-96.0553841264,-25.7270689292,-92.8920111139,-25.7270689292,-92.8920111139),('Presque Isle Co. E, Michigan',1876,'','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,1,'Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','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,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite',NULL,'','0','',1,'Potential reservoir',1119,0,'see reef 1875 for remarks.',45,-83,-3046293,-4838452,'United States','North America',101,'',45.35,-83.6167,'','',-25.7230982758,-95.5802707488,-25.7911733795,-92.4145868877,-25.7911733795,-92.4145868877),('Kuppen, Gotland',1877,'Hemse Beds','Silurian','Ludlow','Gorstian',425.60,427.40,7,'Wenlock - early Pridoli',425,422,3,0,'Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,'4','More than 1000 m',NULL,'1',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','4','Stromatoporoids','75','Stromatoporoids or chaetetids only',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','7','3','Binder guild','1','Present',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',1120,1584,'Strongly dominated by a single stromatopore species: Clathrodictyon mohicanum (40 %).\nOther forms are Parallelostroma, Stromatopora...\nLow diversity.\nSeveral biostromes 0.5 to 5 m thick and traceable for 1 km. \nRef 1893:\nNearly 50 % coverage of stromatoporoids.\n50 % matrix with 25 % micrite, 5 % sparite and 20 % skeletal sand and debris.\nFaunal list in collections refer to middle biostrome at Kuppen (coll. 34406) and Fakle .',57,18,-1625748,-600446,'Sweden','Europe',330,'1621, 1893, 2302',57.4222,18.9403,'WAHR','34406',-0.290198515738,-45.5858965991,-0.290198515738,-45.5858965991,-0.290198515738,-45.5858965991),('Huashito, Sichuan',1878,'Ningqiang','Silurian','Llandovery','upper Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,429,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','31','2','10 - 100 m wide','80','3','More than 100 m','120','45',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','21','2','Baffler guild',NULL,'',NULL,'','2','Medium zonation',NULL,'','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1121,2174,'Largest bioherm in area.\n30.4 m thick, 120 m long.\nEnclosed in shales. \nReef base: packstones and grainstones.\nReef core: Bafflestones.\nCorals > stromatopores\nbaffler > binder\nSimilar reefs close-by are Qunilingdiwan (Collection 23252) and Shijiaoshan (Coll. 23253)',32,105,-600881,14669447,'China','Asia',602,'',32.6667,105.9667,'WAHR','23248',1.08053897047,74.5830704781,1.08053897047,74.5830704781,1.08053897047,74.5830704781),('Shizuizigou, Shaanxi',1879,'Ningqiang','Silurian','Llandovery','upper Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,429,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'2','10 - 100 m','50',NULL,'1878',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','3','Microbes','2','Algae','61','Microbes (thrombolites) - algae - corals',NULL,NULL,'50','0','50',0,'no',0,'no','1','Less than 6 reef building species','5','3','Binder guild',NULL,'',NULL,'','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1121,2174,'Reef core of thrombolites (baffling and binding). Additionally some red algae, corals (Subalvealites, Heliolites).\nSmall coalesced bioherms (< 1 m in diameter).',32,106,-642315,14666215,'China','Asia',602,'',32.8167,106.2833,'WAHR','23250',0.79044536627,74.4868283725,0.79044536627,74.4868283725,0.79044536627,74.4868283725),('Alpena, Michigan',1880,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','12',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1122,0,'Reefs in Hamilton Group.\nSlopes dipping up to 30-40 °.\nReef builders Favosites, Acervularia and Stromatopora.\n12 m thick.',45,-83,-3801960,-3061397,'United States','North America',101,'',45.05,-83.4333,'','',-27.9126440421,-49.42136787,-27.9126440421,-49.42136787,-20.6018417346,-104.427414585),('Williamsville and Buffalo, New York',1881,'Onondaga','Devonian','Middle Devonian','lower Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,395,3,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','2','Corals only',NULL,NULL,'80','0','20',0,'no',0,'no','3','25 or more reef building species','43','1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1126,1222,'Edgecliff Member of Onondaga Limestone. Predominance of  colonial rugose corals (15-16 species), 10 solitary rugose coral species and 15 tabulate coral species, but only 2 stromatopore species.\nMostly tabulate corals.\nFlank beds dipping 5-10 °.',42,-78,-4991571,-2507953,'United States','North America',101,'1381',42.9833,-78.75,'WAHR','9614',-31.0721108199,-47.5677403888,-31.0721108199,-47.5677403888,-23.8284772452,-102.420731582),('Maumee, Ohio',1882,'','Silurian','Upper Silurian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,418,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','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','4','3','Binder guild',NULL,'',NULL,'','2','Medium zonation','1','Low zonation',NULL,'',NULL,'','1','Low production of reefal debris','2','Intense',0,'No or unknown reservoir potential',1123,2160,'Salina Group.\nStromatolitic mound with Hemispherical stromatolite unit (mound) at base and stromatolitic dolobreccia at top.\nFavosites and microbial mesoclots.\n\nAbstract of ref. 2160:\nA completely dolomitized Silurian reef at Maumee, Ohio, U.S.A., is uncommon among early Paleozoic reefs in that its framework consists of about 95% thrombolite boundstone and 5% corals. The reef lithified syndepositonally, as evidenced by centimeter- to meter-scale growth framework cavities within it that are completely filled with internal sediment. The largest cavities, 2--3.5 m in diameter, are probably the\nlargest ever recorded in a thrombolite reef.\n\nFour main types of components are distinguished in the reef framework: (1) dense bushy mesoclots, (2) dense rounded to subrounded mesoclots, (3) saccate\nmicrostructures, and (4) crusts, mostly structureless, but also containing dense bushy mesoclots. The dense bushy components are abundant; rounded to sub-rounded\nmesoclots less so, and the remaining components are rare. The dense bushy and rounded to subrounded mesoclots are interpreted to represent the calcified remains of what were initially either aggregates of the probable filamentous cyanobacterum Angulocellularia or aggregates of renalcid calcimicrobes, or both, and the saccate mesoclots as the calcimicrobe Renalcis sensu stricto. It is speculated that syndepositonal lithification of the reef framework was accomplished by impregnation of unlithified protomesoclots by micrite to create mesoclots along with the formation of micritic cement around and between mesoclots that served to fuse together successive generations of mesoclots.\n\nThe direction of branching of bushy mesoclots in the reef indicates that unlithified protomesoclots were able to grow upward, laterally, and downward. This ability, along with syndepositional lithification to create mesoclots and to cement them together, enabled the protomesoclots and mesoclots to create reef knobs and, eventually, to roof over spaces that were centimeters to three or more meters in width and height to create growth framework cavities. Features indicative of rapid deposition including graded bedding, poor sorting of bioclasts, and textural inversion are common in internal sediment in meter-size cavities. These features suggest that storms, possibly hurricanes, were at least as important, and probably more so, than \'everyday\' wave energy in transporting sediment into all cavities in the reef, regardless of size.',41,-83,-3459424,-5007890,'United States','North America',101,'',41.5833,-83.65,'','',-27.2276968035,-74.3251162098,-27.2276968035,-74.3251162098,-27.2276968035,-74.3251162098),('Lime Hills, Holitna Basin, Sleetmute, Alaska',1883,'','Devonian','Lower Devonian','Pridoli-Pragian',407.60,423.00,8,'middle Pridolian - middle Pragian',412,412,1,0,'Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','500',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','6','Calcisponges','45','Siliceous sponges - calcisponges - microbes - (algae)',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1124,893,'500 m thick algal reef complex.\nLower part with coalescing mounds (thrombolitic), upper part with layered stromatolitic mudstone to wackestone.\nSponges common in Silurian part of buildup.\nSome dasycladaceans.',61,-156,489537,-4953104,'United States','North America',101,'',61.6667,-156.8333,'','',5.23919035802,-93.4011225022,5.23919035802,-93.4011225022,31.0131425253,-142.68574429),('Peters Field, St. Clair, Michigan',1884,'','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','110',NULL,NULL,NULL,'4','More than 1000 m',NULL,'40',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Medium production of reefal debris','2','Intense',2,'Actual reservoir',1127,1128,'110 m thick, about 2 km long.\nOil field. Several other productive reefs in the area (ref. 1128), e.g. Big Hand, Belle River Mills and Marine City fields.\nReef in Engadine Dolomite.\nStromatopores at base.\nIn reef core: corals, crinoids, stromatopores and bryozoans.\n',42,-82,-3387262,-4876773,'United States','North America',101,'1300',42.7333,-82.65,'','',-28.4298609054,-95.5176041881,-28.4955222697,-92.2716489006,-28.4955222697,-92.2716489006),('Frontier Quarry, Lockport, New York',1885,'Lockport','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','12',NULL,NULL,NULL,'1','Less than 20 m',NULL,'100',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species','22','1','Constructor guild',NULL,'',NULL,'','3','Pronounced zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1129,2253,'Gasport Member of Lockport Fm.\nCollection of Foote\n\nReef sudivided in \nInitial reef facies with delicate branching corals (Halysites, Cladopora) and branching bryozoans (Hallopora). Encrusters Girvanella, trepostome bryozoans and tabulate coral Alveolites.\nReef core facies with umrella-shaped asymmetrically shaped stromatopores and a few favositids.\nReef flank facies with debris of stromatopores, tabulate corals and others.\nReef thicknesses in area: 3-12 m.\nReefs less diverse than Niagaran reefs of Michigan.\nExample for reef succession in Walker and Alberstadt (1975).',43,-78,-3534844,-4537183,'United States','North America',101,'',43.1667,-78.7,'WAHR','13054',-28.5666699066,-92.1948919899,-28.5541916378,-88.9451240564,-28.5541916378,-88.9451240564),('Clarendon, New York',1886,'Lockport','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','10',NULL,NULL,NULL,'1','Less than 20 m',NULL,'100','1885',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','4','Stromatoporoids','7','Bryozoans','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1129,0,'See reef 1885 for remarks.',43,-78,-3560194,-4483755,'United States','North America',101,'',43.2,-78.0667,'','',-28.6037832826,-91.6693403712,-28.5789398925,-88.4187228802,-28.5789398925,-88.4187228802),('Rapid River, Kalkaska Co., Michigan',1887,'','Silurian','Wenlock','Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,426,2,1,'Seismic data available ',1,'True reef','3','101-500 m thick','130',NULL,NULL,NULL,'4','More than 1000 m',NULL,'250','1875',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','4','Stromatoporoids','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,'','2','30-60% micrite',NULL,'','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1130,1186,'Pinnacle reef behind barrier reef complex.\nProducing reservoir.\n100 - 130 m thick and up to 3 km long.\nGeneral pattern in subsurfac pinnacle reefs:#\nStromatopore core overlain by stromatolitic zone.',44,-85,-3032459,-4980907,'United States','North America',101,'',44.75,-85.1333,'','',-26.0280470073,-96.9023456321,-26.1270469996,-93.7283019022,-26.1270469996,-93.7283019022),('Temiscouta, Quebec',1888,'Lac Croche','Silurian','Upper Silurian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,418,2,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','300',NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1134,0,'Skeletal framework of stromatopores and corals, encrusting algae and microbes.\nBarrier reef(?) complex along outer margin of a nearshore siliciclastic bank.',47,-69,-3373466,-3640484,'Canada','North America',121,'',47.5,-69,'','',-20.8698689307,-63.2026372216,-20.8698689307,-63.2026372216,-20.8698689307,-63.2026372216),('Pen Island No. 1, Hudson Bay, Ontario',1889,'Attawapiskat','Silurian','Lower Silurian','upper Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,429,3,1,'Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'500',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','10','50',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1134,1423,'Subsurface data.\nSkeletal framwork of stromatoporoids, corals and skeletal algae. Binding by microbes.',56,-88,-1290434,-4990406,'Canada','North America',121,'',56.7519,-88.7542,'','',-13.8810243415,-95.5376209362,-13.8810243415,-95.5376209362,-13.8810243415,-95.5376209362),('Cabot Head, Bruce Peninsula, Ontario',1890,'Manitoulin','Silurian','Llandovery','Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,433,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,'2',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','7','Bryozoans','1','Corals','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1136,0,'Maximum: 1m thick, 2.5 m wide.\nBryozoan-coral bioherms.\nMostly branching bryozoa, encrusting bryozoa, rugose and tabulate corals.\n\nAbstract or ref. 1136:\nSeveral small, previously undescribed bioherms are present in the shallow shelf dolostones of the Manitoulin  Formation (Llandoverian) at the Cabot Head and Wingfield Basin localities in the northernmost portion of the Bruce Peninsula region of southern Ontario (Canada). The bioherms, commonly associated with carbonate tempestites, range from 0.3 to 1.0 m in height and 0.9 to 2.5 m in width and are composed of bafflestones-floatstones and minor bindstones. The chief components of the bioherms are dolomitized lime mud and branching bryozoans. Bioherm building by bryozoans, although common in the ancient record, represents a great divergence from the mostly accessory frame encrusting role of bryozoans in modern environments. Minor skeletal components of the bioherms include\nechinoderms, rugose and tabulate corals and brachiopods. Laminar encrusting bryozoans exist in the top 10 cm of one of the bioherms. Some of the bioherms show evidence of water agitation that may be the result of current action induced by storm or tidal processes. This evidence includes offlapping debris and abrupt near-vertical margins aligned approximately perpendicular to depositional slope of the basin. The occurrence of the Manitoulin Formation bryozoan bioherms on the Bruce Peninsula stretches the already known Llandoverian reef complex on Manitoulin Island further to the south. The reason why these bioherms did not reach sizes comparable to large Llandoverian or Wenlockian reefs and did not make the shift to a coral-stromatoporoid community is probably related to a complex interaction of internal and external factors such as community development, bathymetry, clasticity, and salinity. ',45,-81,-2941626,-5057238,'Canada','North America',121,'',45.2361,-81.2847,'','',-25.8718828245,-98.2554791019,-25.8718828245,-98.2554791019,-25.8718828245,-98.2554791019),('Grand Rapids, Manitoba',1891,'Atikameg-Cedar Lake','Silurian','Llandovery','Aeronian-Telychian',433.40,440.80,6,'Rhuddanian-Telychian',435,436,2,0,'Outcropping reef ',4,'Biostrome','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','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1138,0,'Dolomitized coral-stromatoporoid biostromes at several levels.\nRelated to sea level.',53,-99,-1129694,-5772730,'Canada','North America',121,'',53.1833,-99.2833,'WAHR','26741',-14.5169298363,-104.58206659,-14.5169298363,-104.58206659,-14.5169298363,-104.58206659),('Wahringa Farm, Bakers Swamp, NSW',1892,'','Ordovician','Lower Ordovician','Arenig',470.00,477.70,4,'late Early - early Middle Ordovician',472,471,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','5',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,'',NULL,'',NULL,'',NULL,'','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1139,1723,'5 m thick microbial mound with Stromatactis and some birdseyes.\nGirvanella dominant (2 species).\nSome bryozoans.\nLarge slumped clast derived its seems from a localized,\nsmall carbonate body that formed on the fringes of an Early Ordovician\nvolcanic island.\n',-32,148,2347672,19349365,'Australia','Oceania',801,'',-32.7833,148.9333,'WAHR','80577',10.5221184767,130.074824027,10.5221184767,130.074824027,10.5221184767,130.074824027),('Dolayba',1893,'','Silurian','Wenlock','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,426,2,0,'Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1140,0,'Patch reef complex.\nTabulate corals and ?\nNot described.',40,29,-2896755,1888253,'Turkey','Asia',522,'',40.9167,29.2333,'WAHR','79354',-10.8368231848,-30.8119888284,-10.8368231848,-30.8119888284,-10.8368231848,-30.8119888284),('Trinity Lake, Jasper, Alberta',1894,'Cathedral','Cambrian','Middle Cambrian','Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,507,2,0,'Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','27','1','Less than 10 m wide','6','2','10 - 100 m','30','100','1787',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,'','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1141,1554,'Composite thrombolite mounds.\nUp to 27 m thick and 30 m wide.\nInner margin of a mud-dominated carbonate complex.\nSee reef 1787 for more remarks.',53,-118,1522447,-6861534,'Canada','North America',121,'',53,-118,'','',38.9398664387,-118.592049637,39.5575211428,-113.283373332,39.5575211428,-113.283373332),('N Franklin Mts., N.W.T.',1895,'Franklin Mountain','Ordovician','Lower Ordovician','Croixian-Tremadocian',477.70,497.00,3,'Franconian - Tremadocian',488,488,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,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,'','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1142,0,'Stromatolitic biostromes and bioherms on Mackenzie carbonate platform.\n',65,-127,2847167,-4868112,'Canada','North America',121,'',65.8333,-127,'','',43.1706810118,-86.4325239111,43.1706810118,-86.4325239111,43.1706810118,-86.4325239111),('Gayna River, Mackenzie Mts.',1896,'Mount Kindle','Ordovician','Upper Ordovician','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,453,2,0,'Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','65',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','20','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1142,0,'40 m thick biostrome or bioherm at headwaters of Gayna River.',64,-130,1917515,-5828119,'Canada','North America',121,'',64.9167,-130.6333,'','',15.0825447812,-112.452616455,15.0825447812,-112.452616455,15.0825447812,-112.452616455),('Ware, British Columbia',1897,'Skoki','Ordovician','Middle Ordovician','Dapingian',467.30,470.00,4,'late Early - early Middle Ordovician',472,470,2,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','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,'','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1142,0,'Small (1 m) stromatolithic mounds on Macdonald Platform.\r\nShelf edge probably also reefal, but destroyed by dolomitization.',57,-125,2140247,-6535536,'Canada','North America',121,'',57.5,-125.6667,'',NULL,30.3973657373,-102.794554005,30.3973657373,-102.794554005,30.3973657373,-102.794554005),('Pine Pass, British Columbia',1898,'Beaverfoot','Ordovician','Upper Ordovician','early Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,453,1,0,'Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,'',NULL,'1','Constructor guild',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1142,0,'Coral bioherm (colonial and solitary).\r\n2.5 m thickness.\r\nWithin Kawka Platform. ',55,-122,1318079,-6944227,'Canada','North America',121,'',55.5,-122.8333,'',NULL,5.91027122093,-120.538298297,5.91027122093,-120.538298297,5.91027122093,-120.538298297),('Kingston, Ontario',1899,'Gull River','Ordovician','Upper Ordovician','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,455,1,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','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,'','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1143,1142,'Small (1 m) stromatolite bioherms.\nUpper Gull River Fm., St. Lawrence Platform.\nVery shallow, near-shore.',44,-76,-2933527,-5174241,'Canada','North America',121,'',44.25,-76.5,'WAHR','80616',-20.3402658708,-106.430990962,-20.3402658708,-106.430990962,-20.3402658708,-106.430990962),('Mississauga, Ontario',1900,'Meaford','Ordovician','Upper Ordovician','Richmondian',445.20,453.00,5,'Darriwilian - Ashgillian',452,447,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m','10',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','7','Bryozoans','13','Echinoderms','60','Bryozoans - Pelmatozoans - (microbes)',NULL,NULL,'60','0','40',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild','1','Present',NULL,'',NULL,'',NULL,'','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1144,0,'20 % bryozoans (Stigmatella, Heterotrypa)\n50-70 % sediment and cement.\nRest brachiopods, pelmatozoans and other.\n5-10 % cavities with microbes, worms and bryozoa.',43,-79,-2864846,-5444071,'Canada','North America',121,'',43.5833,-79.5833,'WAHR','80291',-21.4709012505,-108.321008952,-21.4709012505,-108.321008952,-21.4709012505,-108.321008952),('Gore Bay, Manitoulin Island, Ontario',1901,'Georgian Bay','Ordovician','Upper Ordovician','Rawtheyan',445.20,453.00,5,'Darriwilian - Ashgillian',452,446,3,0,'Outcropping reef ',4,'Biostrome','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','1','Shelf/platform interior','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild',NULL,'',NULL,'','2','Medium zonation',NULL,'','2','30-60% micrite',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',1145,2456,'Coral-stromatoporoid biostrome.\n4 m thick.\nCorals: Tetradium, Columnopora, Cyathophylloides\nStromatopores, Labechia, microbes (Girvanella, Hedstroemia).\nKagawong member of Georgian Bay Fm.',45,-81,-2513394,-5513297,'Canada','North America',121,'',45.75,-81.6667,'WAHR','22960',-18.8681339612,-108.681653642,-18.8681339612,-108.681653642,-18.8681339612,-108.681653642),('Eddies Cove West, Newfoundland',1902,'','Ordovician','Lower Ordovician','upper Ibexian',489.50,500.50,4,'late Early - early Middle Ordovician',472,475,2,0,'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','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,'','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',866,1084,'',50,-57,-2541433,-3838303,'Canada','North America',121,'',50.75,-57.1667,'','',7.60046477895,-86.8643437527,7.60046477895,-86.8643437527,7.60046477895,-86.8643437527),('Colonsay, Saskatchewan',1903,'Winnipegosis','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick','100',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',971,917,'8 reefs. 70-100 m thick.',51,-105,-1998861,-4313088,'Canada','North America',121,'',51.9667,-105.8667,'','',-14.9746063706,-60.1171513832,-14.9746063706,-60.1171513832,-9.75164327911,-117.062548279),('Estevan, Saskatchewan',1904,'Winnipegosis','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,1,'Seismic data available ',1,'True reef','2','10 to 100 m thick','80',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1b','Intraplatform basin',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',2,'Actual reservoir',917,0,'Steep sided pinnacle reefs (subsurface).\nUp to 80 m thick.',49,-103,-2437480,-4311015,'Canada','North America',121,'',49.25,-103,'','',-18.2386387409,-60.30520297,-18.2386387409,-60.30520297,-12.9888734063,-116.598721067),('Whitemud, Clearwater R., Alberta',1905,'Keg River','Devonian','Middle Devonian','Middle Devonian',382.70,387.70,9,'late Pragian - Eifelian',395,391,1,0,'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',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',0,'No or unknown reservoir potential',1146,917,'Dolomitic biohermal mounds (a few meters) ',56,-110,-2152645,-4122695,'Canada','North America',121,'',56.7,-110.0833,'','',-9.76315476195,-58.9656202583,-9.76315476195,-58.9656202583,-4.42148036608,-116.948622215),('Evie Bank, British Columbia',1906,'','Devonian','Middle Devonian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,388,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','260',NULL,NULL,NULL,'4','More than 1000 m',NULL,'35',NULL,0,'Tropical or unknown',3,'Ramp or Slope','3a','Upper slope or inner ramp',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',917,0,'Composite platform reef. 260 m thick.\nBasinward slope NW of Keg River barrier reef.',58,-123,-391223,-4547051,'Canada','North America',121,'',58.8333,-123,'WAHR','82071',-3.28969234889,-62.1371995042,-3.28969234889,-62.1371995042,1.33453621658,-121.2754342),('Keg River Barrier Reef, Pine Point',1907,'Keg River','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','210',NULL,NULL,NULL,'4','More than 1000 m',NULL,'900',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',2,'Actual reservoir',952,917,'See reef 1532 for remarks.',60,-114,-1537141,-4025096,'Canada','North America',121,'',60.75,-114.75,'','',-6.65949746592,-61.9204140694,-6.65949746592,-61.9204140694,-1.58113239794,-119.752564296),('Keg River Barrier Reef, Redfern',1908,'Keg River','Devonian','Middle Devonian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,394,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','210',NULL,NULL,NULL,'4','More than 1000 m',NULL,'900','1907',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',2,'Actual reservoir',917,0,'Reef 1532 for remarks.',57,-123,-1306864,-4658165,'Canada','North America',121,'',57.3333,-123.8333,'','',-5.85425596368,-67.6788191664,-5.85425596368,-67.6788191664,-1.66976274225,-125.534602451),('Presqu\'ile Barrier reef, Redfern Lake',1909,'','Devonian','Middle Devonian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,390,3,0,'Outcropping reef ',1,'True reef','3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,'900','1532',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base',NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',1,'Potential reservoir',917,1600,'Equivalent to Keg River Barrier Reef in subsurface.\nvarcus zone.\nOnly rugosans detected are Lythophyllum sp. (subsurface) and Houershanophyllum and Peripaedium at Mt. Bertha.\nReef 1532 for more remarks.',57,-123,-455567,-4711700,'Canada','North America',121,'',57.3333,-123.8333,'WAHR','84245',-3.84205438684,-63.6025349443,-3.84205438684,-63.6025349443,0.50971489885,-122.603645636),('Monkman Lake, British Columbia',1910,'Flume','Devonian','Upper Devonian','early Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,383,3,0,'Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','24',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,'','4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1147,917,'Several stacked stromatopore bioherms.\nTotal thickness 24 m.\n60-80 m wide.',54,-121,-535318,-5127145,'Canada','North America',121,'',54.7,-121.2833,'','',-4.86093585797,-59.4066239959,-4.86093585797,-59.4066239959,1.9826679198,-120.536252974),('Mt. Buchanan, British Columbia',1911,'Flume','Devonian','Upper Devonian','early Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,383,3,0,'Outcropping reef ',4,'Biostrome','3','101-500 m thick','112',NULL,NULL,NULL,'4','More than 1000 m',NULL,'8',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','4','Stromatoporoids','4','Stromatoporoids','75','Stromatoporoids or chaetetids only',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',1147,917,'112 m thick stromatopore-amphipore biostrome.',53,-120,-674304,-5159228,'Canada','North America',121,'',53.8722,-120.1333,'WAHR','76884',-5.86402898624,-59.7682614257,-5.86402898624,-59.7682614257,0.92236011779,-120.643895594),('Noonday Peak, Alberta',1912,'Cairn','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,0,'Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','6',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','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,'','3','More than 60% micrite','3','More than 25% sparite',NULL,'','0','',0,'No or unknown reservoir potential',917,0,'Small algal(?) bioherms foreslope of Ancient Wall reef complex.\nAbundant zebra structures.\n6 m thick, 10-15 m long.\nIn the vicinity late Frasnian stromatopore bioherm (5-10 m thick).',53,-118,-800024,-5146505,'Canada','North America',121,'',53.4167,-118.7833,'WAHR','75860',-6.78390938913,-59.7268418351,-6.78390938913,-59.7268418351,0.0396038793298,-120.381937006),('Forbes Creek, Banff, Alberta',1913,'Peechee','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',NULL,NULL,'3','101-500 m thick','223',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','2','Intense',0,'No or unknown reservoir potential',917,0,'223 m thickness\nCorals and amphiporids throughout, but intensley dolomitized.',51,-116,-1051967,-5207430,'Canada','North America',121,'',51.8167,-116.9333,'WAHR','76448',-8.60284297671,-60.4492845991,-8.60284297671,-60.4492845991,-1.89852511797,-120.636343964),('Rice Brook, Alberta',1914,'Fairholme','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',2,'Reef mound','3','101-500 m thick','460',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1','Shelf/platform interior',NULL,'','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',0,'No or unknown reservoir potential',917,0,'Margin of platform reef complex.\nTotal thickness 460 m.',52,-117,-1011838,-5203478,'Canada','North America',121,'',52.0333,-117.2667,'','',-8.31126557975,-60.3839886442,-8.31126557975,-60.3839886442,-1.59999101907,-120.644478305),('Leduc & Acheson, Alberta',1915,'Leduc','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','300',NULL,NULL,NULL,'4','More than 1000 m',NULL,'16',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',1,'Potential reservoir',1148,1891,'300 m thick, 16 x 5 km wide.\nStromatoproid fragments and unidentifiable dolomitized corals. some bryozoans. ',53,-113,-1416902,-4638310,'Canada','North America',121,'917',53.25,-113.75,'','',-9.34435782163,-58.1290647964,-9.34435782163,-58.1290647964,-2.78512450917,-116.806106225),('Bonnie Glen, Alberta',1916,'Leduc','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','213','4','More than 1000 m wide','2000','4','More than 1000 m','11600',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',917,0,'213 m thick, 11.6 x 2 km wide.',52,-113,-1516713,-4740649,'Canada','North America',121,'',52.0333,-113.9167,'','',-9.99334737178,-59.1780912172,-9.99334737178,-59.1780912172,-3.68120267627,-117.636672852),('Duhamel, Alberta',1917,'Leduc','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','275',NULL,NULL,NULL,'3','More than 100 m',NULL,'8',NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','3','More than 60% micrite',NULL,'',NULL,'','0','',2,'Actual reservoir',1149,917,'Calcilutites with abundant stromatopores, corals and amphiporids.\n\nAbstract of ref. 2125:\nThe Duhamel reef is an isolated Upper Devonian Leduc Formation limestone bioherm, situated immediately NNE of the Bashaw reef complex in south-central Alberta. Although Duhamel has a relatively small basal area (less than 12 km2), this reef rises some 275 m above the platform facies. From seismic data it is interpreted that there is a raised peripheral reef rim that appears to be elevated about 25 m relative to the interior of the reef. Although late-stage accretionary growth about the periphery of the reef complex may have contributed to its development, the raised rim at Duhamel is interpreted to be principally of secondary origin. Optimal hydrocarbon recovery could be realized if all production wells were drilled into the raised reef rim. The Duhamel example shows that even relatively small Leduc reefs can exhibit raised rims and that these rims may be seismically visible. ',52,-113,-1494960,-4630353,'Canada','North America',121,'2125',52.8833,-113.0167,'','',-9.91708145084,-58.1540118975,-9.91708145084,-58.1540118975,-3.34459487907,-116.680985996),('Westerose South, Alberta',1918,'Leduc','Devonian','Upper Devonian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,379,3,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','214','4','More than 1000 m wide','5200','4','More than 1000 m','14600',NULL,NULL,0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'','1','Low zonation',NULL,'',NULL,'',NULL,'','2','Intense',2,'Actual reservoir',917,1708,'> 214 m thick, 14.6 x 5.2 km wide.\nGas field.\nAbstract ref. 1708:\nThe Westerose field produces hydrocarbon from a dolomitized Upper Devonian reef. The reef is 1.6 km by 5.5 km and up to 214 m thick and is not well differentiated into organic reef margin and reef interior facies. Laterally continuous tidal flat and restricted lagoon sediments, which create vertical permeability barriers with the interiors of other reefs, were not observed. Secondary pore systems dominate porosity. The large vugs and fossil molds are well connected throughout the  reef by a pervasive vertical to subvertical fracture system. The equicrystalline xenotopic dolomite matrix has low porosity (3.2%) and permeability and does not contribute to effective intervug communication. The effect of diagenesis on the depositional fabric has made it difficult to subdivide the reef using depositional facies-reservoir quality relationships. Nonparametric statistical techniques were applied to core data to identify trends in permeability and porosity within the reef. Reef  cores were assigned to flank, margin or interior positions based on reef  morphology, an arbitrarity divided into vertical layers 25 m thick giving a total of 17 layer-position combinations. Horizontal permeability, vertical permeability and porosity increase from reef flank to reef interior and from the upper reef to the base of the cored reef. Cumulative probability plots of horizontal permeability data, grouped by reef  position, each exhibit the characteristics of the log-normal distribution but with a portion of the highest permeability values truncated from the data set. Truncation is due to poor core recovery from the highest permeability regions as well as to the limitations of the permeability measuring procedure on high permeability core. Vertical permeability data are not truncated. Truncation effects must be taken into account when estimating average horizontal permeability. Although significant trends in the magnitude of permeability are present within the reef, the reservoir fluid flow model for the rock volume being drained by a single well is best described as a random arrangement of blocks of differing permeability. Permeability calculated for the oil zone from a pressure build-up test is 1115 mD. When corrected for truncation, the geometric average of the core data from within the producing zone of the pressure test is 760 mD, consistent with the pressure test result; the arithmetic mean of the corrected data set would be much too large. The similarity between the geometric average of the horizontal permeability calculated from the pressure build-up test at Westerose is expected from the disordered arrangement of units of differing permeability. \n\n',52,-114,-1435209,-4686080,'Canada','North America',121,'',52.8333,-114.0667,'','',-9.44192293853,-58.5827813189,-9.44192293853,-58.5827813189,-2.99571304106,-117.213498934),('Wizard Lake, Alberta',1919,'Leduc','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,1,'Seismic data available ',2,'Reef mound','3','101-500 m thick','183','4','More than 1000 m wide','1600','4','More than 1000 m','5300','15','1918',0,'Tropical or unknown',1,'Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,'','4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','0','',2,'Actual reservoir',917,0,'183 m thick, 5.3 x 1.6 km wide.',53,-113,-1415811,-4654168,'Canada','North America',121,'',53.15,-113.9167,'','',-9.32464106608,-58.2708808806,-9.32464106608,-58.2708808806,-2.80242195345,-116.94653091),('Grosmont, Alberta',1920,'Grosmont','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'650',NULL,0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',1,'Potential reservoir',917,0,'Patch reefs forming a complex at a shelf to ramp flexure.\nStromatopores, corals and coralline algae. Amphipora wackestones are also part of patch reefs.\nOther references cited by 917.',58,-116,-832072,-4380702,'Canada','North America',121,'',58,-116.5,'','',-5.29224032587,-55.1815555029,-5.29224032587,-55.1815555029,1.88093855565,-115.019335958),('Grosmont II, Alberta',1921,'Grosmont','Devonian','Upper Devonian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,2,0,'Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'650','1920',0,'Tropical or unknown',2,'Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,'','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,'',NULL,NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'',NULL,'','1','Present',1,'Potential reservoir',917,0,'see reef 1920 for remarks.',54,-111,-1493734,-4433804,'Canada','North America',121,'',54.1667,-111,'','',-10.0545334683,-56.3763565035,-10.0545334683,-56.3763565035,-3.02579829466,-114.951380302),