INSERT INTO `reefs` VALUES ('La Sentinella, Serra Scoris, Gonnesa, Sardinia',1746,'Matoppa','Cambrian','Series 2','Stage 4','lower Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',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,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',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,-49.8842,114.527,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maria Santa Gloria, Sardinia',1747,'Santa Barbara','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'0','Outcropping reef ',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,NULL,'1','Present',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',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,-49.7373,114.574,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jebel Daf',1748,'','Cambrian',NULL,NULL,'Lower Cambrian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',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,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,-28.6195,152.907,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rio Cannas, Sardinia',1749,'Matoppa','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'0','Outcropping reef ',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,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,-51.8127,127.137,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Matoppa, Sardegna',1750,'Gonnesa','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','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,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,-49.7969,114.51,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Huanghuachang, Yichang, Hubei',1751,'Fenxiang','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',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','','Unknown','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,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,-18.4097854743,92.7556084051,16.5205,143.281,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Xintan, Hubei',1752,'Fenxiang','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',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','','Unknown',NULL,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,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,-17.9961645185,92.9246597432,16.8731,143.562,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Liujiachang, Hubei',1753,'Honghuayuan','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',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',NULL,NULL,NULL,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,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1050,1087,'Lithistid sponge (Archaeoscyphia)-Calathium reefs and bioherms.',30,111,442543,14568943,'China','Asia',602,'',30.0833,111.4833,'',NULL,-16.3999045246,88.7320540673,-16.3999045246,88.7320540673,-16.3999045246,88.7320540673,14.6679,138.984,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('San José de Jáchal, Argentina',1754,'','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,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,-40.4317,-127.158,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Camp San Saba, Texas',1755,'Wilberns','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,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,-17.771,-94.4375,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Las Ermitas, Sierra Morena',1756,'Pedroche','Cambrian','Series 2','Stage 3','lower Atdabian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',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,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,-55.9478,112.929,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alconera, Sierra Morena',1757,'','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',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,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,-56.0142,110.457,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Great Valley, Maryland',1758,'Conococheague Limestone','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,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,-31.326,-79.1915,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Great Valley II, Pennsylvania',1759,'Conococheague Limestone','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,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,-31.4086,-78.9502,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Frederick Valley, Maryland',1760,'Frederick Limestone','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,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,-31.7384,-79.1126,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Frederick Valley, Maryland',1761,'Frederick Limestone','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,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,-31.7384,-79.1126,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Amouslek',1762,'Amouslek','Cambrian','Series 2','Stage 3','Atdabanian/Botomian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',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,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,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,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,-63.9527,113.988,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Point Peak, Llano River, Texas',1763,'Wilberns','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,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.\r\nOuter ramp setting, but well above wave base\r\n(rip-up clasts, hummockies, wave ripples).\r\nAlgal flora relatively diverse (Girvanella, Renalcis, Epiphyton).',30,-99,-595235,-8433294,'United States','North America',101,'',30.6486,-99.3139,'','207469',16.724167612,-120.881757783,16.724167612,-120.881757783,16.724167612,-120.881757783,-17.7974,-94.812,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ketza River, Pelly Mts., Yukon',1764,'','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'0','Outcropping reef ',2,'Reef mound','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,NULL,NULL,'1','Low zonation',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',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,-118.810409111,5.00669,-74.3883,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wilkawillina Gorge, South Australia',1765,'','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',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,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',1.30117543977,114.194401493,1.30117543977,114.194401493,1.30117543977,114.194401493,16.7791,-160.323,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mount Scott Range, South Australia',1766,'','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',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,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',1.47928239683,113.353812564,1.47928239683,113.353812564,1.47928239683,113.353812564,17.1724,-161.122,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Stuart Shelf, South Australia',1767,'Andamooka','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',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,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,-0.545968860397,116.464130545,17.1337,-163.996,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Old Wirrealpa Mine, South Australia',1768,'Upper Wilkawillina','Cambrian','Series 2','Stage 4','upper Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',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,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,-0.072076318232,118.171116252,17.0935,-162.143,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Moorowie Mine, Flinders R., South Australia',1769,'Moorowie','Cambrian','Series 2','Stage 4','upper Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',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,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',1.00310809524,115.843545144,0.152505543536,118.244843859,0.152505543536,118.244843859,17.2865,-162,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Starshot Glacier, Holyoake Range, Antarctica',1770,'','Cambrian',NULL,NULL,'Lower Cambrian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',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,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,-0.579475,-155.062,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Austinville, Virginia',1771,'Shady Dolomite','Cambrian','Series 2','Stage 4','Botomian-Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',513,2,'0','Outcropping reef ',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,-27.2316,-95.0528,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Austinville II, Virginia',1772,'','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',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,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,-28.9903,-90.3485,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Saratoga Springs, New York',1773,'','Cambrian','Furongian','Lawsonian','Trempealeauan',485.40,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',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,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,-31.6665,-81.3058,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Southern San Juan Province, Argentina',1774,'','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,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,-38.8638,-128.068,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('San Juan Province, Argentina',1775,'','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,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,-39.8425,-127.745,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kotuy River, Anabar, Siberia',1776,'','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',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','','Unknown','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',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,-22.0474,-7.78534,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kotuy River II, Siberia',1777,'','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',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','','Unknown','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1067,1045,'',71,103,-4078811,151296,'Russia','Asia',624,'',71.75,103,'','',-7.94050867279,-63.1402763351,-7.94050867279,-63.1402763351,-7.94050867279,-63.1402763351,-22.3623,-8.12614,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mojero River, Siberia',1778,'Kotuy','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',525,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'800','1776',0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',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,-21.6574,-6.29012,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aldan, Siberia',1779,'','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',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','','Unknown','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',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,-17.0588,-8.1999,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Markha-Udachnyy, Siberia',1780,'','Cambrian','Series 2','Stage 3','Tommotian/Atdabanian',514.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',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','','Unknown','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',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,-17.8896,-9.27332,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sheya, Yakutiya, Siberia',1781,'','Cambrian','Series 2','Stage 4','Atdabanian-Botomian',509.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',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','','Unknown','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,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,-11.1933,-10.9686,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aldan IV, Yakutiya, Siberia',1782,'','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'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','','Unknown','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',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,-9.79038,-11.7105,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jebel Aswad',1783,'','Cretaceous','Lower Cretaceous','Barremian','Barremian-early Aptian',113.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',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,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',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,-10.0652,45.9489,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Qarib',1784,'','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',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','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1068,0,'Large isolated block of reef limestone in slope setting.',23,58,2403495,5772340,'Oman','Asia',503,'',23.2028,58.9167,'','',17.3832957525,53.5397925572,17.3832957525,53.5397925572,21.4972215063,57.3658217007,18.8598,55.0713,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Quryat',1785,'','Paleogene','Oligocene','Rupelian','middle Oligocene',26.00,32.00,29,'Priabonian - Rupelian',33,25,'Late Oligocene (Chattian, 25.6 Ma)',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','0',NULL,'','Unknown','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,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,'','',16.3616471953,52.524670384,16.2759306513,52.4462300875,21.3950048846,57.3320246383,16.5902,52.9458,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wu’ai village of Songfan Town',4076,'Upper Sanqushan','Ordovician','Upper Ordovician','Katian','late Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',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','','Unknown','2','Below fair weather wave base','3','Microbes','6','Calcisponges','66','Stromatolites-\'sphinctozoans\'-(stromatoporoids, algae, corals)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3003,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,29,118.32,NULL,'173372',-8.32650476722,65.3717454345,-8.32650476722,65.3717454345,-8.32650476722,65.3717454345,2.20851,124.351,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Quryat',1786,'','Paleogene','Eocene','Priabonian','Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',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,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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,'','',15.0066245956,51.539551607,15.0066245956,51.539551607,21.5299907774,57.4423467144,14.1088,51.0851,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Field, British Columbia',1787,'Cathedral','Cambrian',NULL,NULL,'Albertan',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',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,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,-114.92555271,1.07281,-78.3906,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cerro Calaveras, Sonora',1788,'Puerto Blanco','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,3,'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,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,-1.48997,-102.351,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cerro Rajon, Sonora',1789,'','Cambrian','Series 2','Stage 4','Botomian-Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',513,3,'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,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,-1.64378,-102.188,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cerro Rajon/de la Proveedora, Sonora',1790,'Puerto Blanco','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,3,'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,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,-1.39476,-101.9,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Stewarts Mill, Esmeralda Co., Nevada',1791,'Poleta','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','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,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,-138.51277668,2.44365,-96.8101,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Heritage Range, Ellsworth Mts., Antarctica',1792,'Minaret','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,NULL,'11','Siliceous sponges','3','Microbes',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1108,1073,'Reworked clasts\r\nAntarcticocyathus webersi originally identified as archaeocyath but now revised to be a lithistid sponge: Lee, J.-H., 2022, Limiting the known range of archaeocyath to the middle Cambrian: Antarcticocyathus webersi Debrenne et al. 1984 is a lithistid sponge: Historical Biology, p. 1-5.',-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,-5.38624,-148.834,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-10 13:16:52'),('Heritage Range II, Ellsworth Mts., Antarctica',1793,'Minaret','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',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,NULL,'3','Microbes','11','Siliceous sponges','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,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1073,1108,'Cambrian clasts in Permian tillites.',-79,-81,-1451918,-17422098,'Antarctica','Antarctica',803,'',-79.75,-81.0833,'',NULL,-11.8557867798,156.515317358,-11.8557867798,156.515317358,-11.8557867798,156.515317358,-7.20962,-144.597,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-10 13:16:52'),('Nowshera',1794,'Nowshera','Silurian','Pridoli','Pridoli','Pridolian-Lochkovian',410.80,423.00,8,'middle Pridolian - middle Pragian',412,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',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','0',NULL,'','Unknown',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,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,NULL,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,-36.4235,133.122,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gechang-Muth, Himachal Himalaya',1795,'Takche','Silurian','Wenlock','Sheinwoodian','Wenlockian',427.40,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,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,-29.0757,143.78,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mitchell Quarry, Lisbon, Iowa',1796,'','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',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,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,-20.2829,-55.7734,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hunt Quarry, Cedar Co., Iowa',1797,'','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',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,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,-20.4856,-55.7651,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lapel, Indiana',1798,'','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1600','1875',0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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,-24.3259,-53.3502,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Snäckgärdsbaden-Ireviken, Gotland',1799,'Högklint','Silurian','Wenlock','Sheinwoodian','Sheinwoodian',430.50,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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','','Unknown','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,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,-18.3504,-4.40391,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Holmhällar, Gotland',1800,'Eke-Hamra','Silurian','Ludlow','Gorstian','Gorstian',425.60,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',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','','Unknown','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,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,-12.367,-4.77103,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Korpklint, Gotland',1801,'Visby','Silurian','Wenlock','Sheinwoodian','Sheinwoodian',430.50,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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','','Unknown','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,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,-18.6297,-4.40285,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Klinte, Gotland',1802,'Klinteberg Beds','Silurian','Wenlock','Homerian','Homerian',427.40,430.50,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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','','Unknown','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,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,-15.8726,-4.57663,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baerum',1803,'Rytteräker','Silurian','Llandovery','Aeronian','Aeronian-Telychian',433.40,440.80,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,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,-23.0846,-9.12243,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ringerike',1804,'','Silurian','Wenlock','Sheinwoodian','lower Wenlock',430.50,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,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,-15.067,-9.63391,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Holmestrand',1805,'Steinsfjorden','Silurian','Wenlock','Sheinwoodian','middle Wenlock',430.50,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,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,-18.4756,-9.20243,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Skien',1806,'','Silurian','Wenlock','Sheinwoodian','middle Wenlock',430.50,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,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,-18.8525,-9.46015,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Heröya, Ringerike',1807,'','Silurian','Wenlock','Homerian','upper Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,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,-16.3916,-9.5018,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pusku-Suurekivi, Ridala Peninsula',1808,'Ridala','Silurian','Llandovery','Rhuddanian','Rhuddanian',440.80,443.40,6,'Rhuddanian-Telychian',435,440,'Early Silurian (early Llandovery, 441.2 Ma)',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,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,-26.2879,-1.63872,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('St. John Island, Newfoundland',1809,'','Ordovician','Middle Ordovician','Dapingian','Whiterockian',467.30,470.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',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,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,-29.1331,-44.2897,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Birmingham, Alabama',1810,'Chickamauga','Ordovician','Upper Ordovician','Sandbian','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',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','','Unknown','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,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,-29.2029,-68.4425,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Valcour and Garden Islands, New York',1811,'Day Point','Ordovician','Middle Ordovician','Darriwilian','lower Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',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,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,-28.2612,-55.378,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wool Point, New York',1812,'Day Point','Ordovician','Middle Ordovician','Darriwilian','lower Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',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,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,-28.0669,-55.2148,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Isle La Motte, Vermont',1813,'Day Point','Ordovician','Middle Ordovician','Darriwilian','lower Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',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','','Unknown','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,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,-28.0912,-55.1741,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lake Champlain region, Vermont',1814,'Crown Point','Ordovician','Middle Ordovician','Darriwilian','late Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',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,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,-28.0824,-55.1607,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Isle la Motte/Grand Isle, Vermont',1815,'Crown Point','Ordovician','Middle Ordovician','Darriwilian','upper Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',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,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,-28.6604,-55.587,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('St. Jean, Quebec',1816,'Crown Point','Ordovician','Middle Ordovician','Darriwilian','Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',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,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,-27.8359,-54.9671,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Terrebone, Quebec',1817,'Valcour','Ordovician','Middle Ordovician','Darriwilian','upper Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',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,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,-27.2775,-54.8166,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sinking Springs, Virginia',1818,'','Ordovician','Middle Ordovician','Darriwilian','Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',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','','Unknown','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,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,-30.4543,-64.5555,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Huanghuachang II, Yichang, Hubei',1819,'Honghuayuan','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',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','','Unknown',NULL,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,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,-18.4097854743,92.7556084051,16.5205,143.281,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Liujiachang, Hubei',1820,'Fenxiang','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',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','','Unknown','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,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,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,-18.2352726681,91.9459991625,16.8982,142.559,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lechuguilla, Southern Franklin Mts., Texas',1821,'McKelligon Canyon','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',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,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,-14.7177,-88.0489,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Blanco County, Texas',1822,'Honeycut','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',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','','Unknown','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,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,-21.7602,-87.2666,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Burnet County, Texas',1823,'Honeycut','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',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','','Unknown','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,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,-21.6788,-86.6259,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kindblade Ranch, Wichita Mts., Oklahoma',1824,'Honeycut','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',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','','Unknown','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,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,-19.8258,-82.7192,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Longhorn Mt., Wichita Mts., Oklahoma',1825,'','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',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','','Unknown','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,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,-19.7875,-82.6979,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mill Creek, Arbuckle Mts., Oklahoma',1826,'Kindblade','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',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','','Unknown','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,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,-21.1617,-82.586,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ibex, Confusion Range, Utah',1827,'Fillmore (from B. Kroeger paper, belated)','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',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',NULL,NULL,'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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1091,1087,'Earliest Ordovician reefs in House Limestone. \r\nStromatolites, lithistid sponges, receptaculid algae (Calathium).\r\nSponges and other metazoans are only accessorial.',38,-113,1288619,-7960373,'United States','North America',101,'1089',38.9167,-113.5,'',NULL,27.6086292607,-115.901135391,27.6086292607,-115.901135391,27.6086292607,-115.901135391,-3.92659,-86.494,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ibex, Confusion Range, Utah',1828,'','Ordovician','Middle Ordovician','Darriwilian','Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',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','','Unknown','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,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,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,-5.7026,-81.6888,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Columbia Icefield, Jasper, Alberta',1829,'Kotchakan','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',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','0',NULL,'','Unknown','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,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,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,-102.158557026,1.36717,-73.2461,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Churan, Lena River, Siberia',1830,'Pestrotsvet','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',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','','Unknown','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,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,-13.024,-14.0017,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gonam, Siberia',1831,'Pestrotsvet','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',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','0',NULL,'','Unknown','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',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,-9.25943,-17.8224,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sukharikha River, Igarka, Siberia',1832,'Krasnoporog','Cambrian','Terreneuvian','Stage 2','upper Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',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','','Unknown','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,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,-24.1709,0.582309,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Khara-Ulakh Mts., Siberia',1833,'Tyuser','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',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','','Unknown',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','16','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',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,-23.7738,-15.3297,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Olenyek Uplift, Siberia',1834,'Pestrotsvet','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',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','0',NULL,'','Unknown',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,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,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,-23.7688,-13.8169,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('El Desastre, Fortuna',1835,'','Neogene','Miocene','Upper Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',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','','Unknown','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,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,-1.24072797753,38.4191,-1.9418,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tawuia, Stone Knife River, N.W.T.',1836,'Little Dal Group','Ediacaran','Ediacaran','Avalon Assemblage','Neoproterozoic',542.00,999.00,0,'Vendian',605,750,'Early Neoproterozoic (late Tonian. 750 Ma)',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,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,-158.022629463,8.60478,-160.128,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Disneyland, Mackenzie Mts., N.W.T.',1837,'','Ediacaran','Ediacaran','Avalon Assemblage','Neoproterozoic',542.00,999.00,0,'Vendian',605,750,'Early Neoproterozoic (late Tonian. 750 Ma)',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,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,-157.649638311,8.91743,-159.755,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-16 12:18:53'),('Attems/Plabutsch',1838,'Plabutsch','Devonian','Middle Devonian','Eifelian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',394,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','90',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','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,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,-35.5276,43.7162,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Terrades, Pyrenees',1839,'','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',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,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,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,-49.2584,117.821,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Issafene',1840,'','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','50',NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',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,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,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,-61.8653,117.067,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fanning River, Queensland',1841,'Burdekin','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',388,2,'0','Outcropping reef ',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,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,-10.8613,152.795,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Heceta Island, Alexander Terrane, Alaska',1842,'Heceta','Silurian',NULL,NULL,'Wenlock/Ludlow',423.00,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,NULL,NULL,NULL,'2','Medium zonation','2','30-60% micrite',NULL,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,-2.81909,-91.9059,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Prince of Wales Island, Alaska',1843,'Heceta','Silurian',NULL,NULL,'Wenlock/Ludlow',423.00,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,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,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,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,-2.91553,-91.7844,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('West Keels, Newfoundland',1844,'West Centre Cove','Cambrian','Terreneuvian','Fortunian','pre-Tommotian',529.00,541.00,1,'Nemakit/Daldynian - Toyonian',520,540,'Cambrian/Precambrian boundary (541 Ma)',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,2,'Cold - water','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,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.\r\nBuildups consist of Ladatheca cylindrica.\r\n\r\nAbstract ref. 1103:\r\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,-86.0436,21.4572,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baumann Fjord S, Ellesmere I., N.W.T.',1845,'','Silurian','Wenlock','Sheinwoodian','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','400',NULL,NULL,NULL,'3','More than 100 m',NULL,'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,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,-78.5420126552,4.19625,-29.587,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baumann Fjord N, Ellesmere I., N.W.T.',1846,'','Silurian','Wenlock','Sheinwoodian','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','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,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,-78.2934641921,4.18443,-29.3213,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S Ellesmere Island, N.W.T.',1847,'','Silurian','Ludlow','Ludfordian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',418,2,'0','Outcropping reef ',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,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,-70.5360872635,1.99346,-28.1043,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S Ellesmere Island, N.W.T.',1848,'','Silurian','Pridoli','Pridoli','Pridoli-Lochkovian',410.80,423.00,8,'middle Pridolian - middle Pragian',412,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',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,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,-5.78128,NULL,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S Ellesmere Island II, N.W.T.',1849,'','Silurian','Ludlow','Ludfordian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',418,2,'0','Outcropping reef ',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,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,-70.055569039,1.62417,-27.7559,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Colin Archer Pen., Devon Is., N.W.T.',1850,'','Silurian','Ludlow','Ludfordian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',418,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'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,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,-70.7327487429,2.09149,-28.2738,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Horlick Quarry, Racine, Wisconsin',1851,'Racine','Silurian','Wenlock','Sheinwoodian','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',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','','Unknown','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,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,-21.8784,-51.8158,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grafton, Wisconsin',1852,'','Silurian','Wenlock','Sheinwoodian','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',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','','Unknown','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,NULL,NULL,'2','Medium zonation',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',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,-21.3715,-51.4666,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Amtjärn, Siljan',1853,'Boda Limestone','Ordovician','Upper Ordovician','Hirnantian','Hirnantian',443.40,445.20,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',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','','Unknown','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,NULL,'1','Present','2','Medium zonation',NULL,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,-27.4242,-6.82851,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Crown Point, Elk River, Tennessee',1854,'Carters Limestone','Ordovician','Upper Ordovician','Sandbian','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',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,NULL,NULL,'3','Pronounced zonation',NULL,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,-27.9233,-67.3187,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cap River, Anticosti Isl., Quebec',1855,'Chicotte','Silurian','Llandovery','Telychian','Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,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,-22.1653,-33.9702,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Stine Spur, Coffeyville, Kansas',1856,'','Carboniferous','Pennsylvanian','Moscovian','Desmoinesian',307.00,315.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',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,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,-5.44385,-30.3513,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chickasaw, Arbuckle Mts., Oklahoma',1857,'','Ordovician','Upper Ordovician','Katian','early Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',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,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,-21.8182,-70.3847,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('East Cape R., Ellesmere Isl., N.W.T.',1858,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',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,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,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,-19.731153884,29.7183,1.33513,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('W Ellesmere Isl. I, N.W.T.',1859,'','Permian','Cisuralian','Sakmarian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',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,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,-16.2433389221,31.1008,1.91379,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('W Ellesmere Isl. II, N.W.T.',1860,'','Permian','Cisuralian','Sakmarian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',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,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,-16.7528287636,31.0022,1.36223,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mc Kinley Bay, Ellesmere Isl., N.W.T.',1861,'','Permian','Cisuralian','Sakmarian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',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,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,-15.64640583,31.6935,3.03851,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mc Kinley Bay, Ellesmere Isl., N.W.T.',1862,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',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,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,-19.1041379812,30.1986,2.44491,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Delphi, Indiana',1863,'Louisville','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','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,NULL,NULL,NULL,'3','Pronounced zonation','3','More than 60% micrite',NULL,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,-23.5111,-53.6485,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Red House Branch, Tennessee',1864,'Holston','Ordovician','Upper Ordovician','Sandbian','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',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,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,-29.263,-63.5283,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cedar Springs, Tennessee',1865,'Rockdell','Ordovician','Upper Ordovician','Sandbian','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',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,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,-29.0227,-63.6954,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gate City, Virginia',1866,'Rockdell?','Ordovician','Upper Ordovician','Sandbian','early Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',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,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,-29.2501,-63.1368,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rockdell, Virginia',1867,'Rockdell','Ordovician','Upper Ordovician','Sandbian','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',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','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)','1','Others','70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','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.\r\nOn ramp buildup.\r\nDiverse bryozoans, solenoporaceans present, rare stromatoporoids',36,-82,-3473825,-5934215,'United States','North America',101,'',36.8333,-82.1667,'',NULL,-10.7880403233,-110.52894073,-19.1961183387,-113.473576651,-19.1961183387,-113.473576651,-29.211,-62.5733,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tazewell, Virginia',1868,'Rockdell?','Ordovician','Upper Ordovician','','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',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,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,-28.6346,-59.2651,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Porterfield, Virginia',1869,'Effna Limestone','Ordovician','Upper Ordovician','Sandbian','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',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,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,-29.4904,-62.0434,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Effna, Virginia',1870,'Effna Limestone','Ordovician','Upper Ordovician','Sandbian','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',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,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,-29.5149,-61.7689,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Catawba, Virginia',1871,'','Ordovician','Upper Ordovician','Sandbian','lower Caradocian',453.00,458.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',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,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,-29.7295,-60.7913,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Murat, Virginia',1872,'Murat Limestone','Ordovician','Upper Ordovician','','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',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,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,-29.0623,-57.5335,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Staunton, Virginia',1873,'','Ordovician','Upper Ordovician','','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',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,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,-28.9766,-56.8302,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Garnier Bay, Somerset Isl., N.W.T.',1874,'Douro','Silurian','Ludlow','Gorstian','Ludlovian',423.00,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',421,2,'0','Outcropping reef ',2,'Reef mound','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,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,-75.5550138929,3.34971,-32.4715,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Presque Isle Co. W, Michigan',1875,'','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,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,-20.6255,-49.1667,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Presque Isle Co. E, Michigan',1876,'','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,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,-20.8312,-48.7572,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kuppen, Gotland',1877,'Hemse Beds','Silurian','Ludlow','Gorstian','Gorstian',425.60,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',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,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,-13.2423,-4.53109,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Huashito, Sichuan',1878,'Ningqiang','Silurian','Llandovery','Telychian','upper Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',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','','Unknown','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,NULL,NULL,'2','Medium zonation',NULL,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',1.08053897047,74.5830704781,1.08053897047,74.5830704781,1.08053897047,74.5830704781,5.795,131.613,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shizuizigou, Shaanxi',1879,'Ningqiang','Silurian','Llandovery','Telychian','upper Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',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','','Unknown','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,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',0.79044536627,74.4868283725,0.79044536627,74.4868283725,0.79044536627,74.4868283725,5.49256,131.568,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alpena, Michigan',1880,'','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',388,2,'0','Outcropping reef ',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','','Unknown','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,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,-33.4498,-29.2998,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Williamsville and Buffalo, New York',1881,'Onondaga','Devonian','Middle Devonian','Eifelian','lower Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',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','','Unknown','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,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,-38.2853,-25.8924,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maumee, Ohio',1882,'','Silurian','Ludlow','Ludfordian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',418,2,'0','Outcropping reef ',3,'Mud mound or bank','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,NULL,NULL,'2','Medium zonation','1','Low zonation',NULL,NULL,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,-27.0792,-46.8607,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lime Hills, Holitna Basin, Sleetmute, Alaska',1883,'','Silurian',NULL,NULL,'Pridoli-Pragian',407.60,423.00,8,'middle Pridolian - middle Pragian',412,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',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,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,-142.68574429,13.2886,-51.8939,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Peters Field, St. Clair, Michigan',1884,'','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,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,-23.4162,-49.626,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Frontier Quarry, Lockport, New York',1885,'Lockport','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',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,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,-24.489,-46.6504,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Clarendon, New York',1886,'Lockport','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',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,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,-24.6748,-46.1841,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rapid River, Kalkaska Co., Michigan',1887,'','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,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,-20.7484,-50.0678,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Temiscouta, Quebec',1888,'Lac Croche','Silurian','Ludlow','Ludfordian','Ludlovian-Pridolian',419.20,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',418,2,'0','Outcropping reef ',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,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',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,-26.2319,-33.4906,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pen Island No. 1, Hudson Bay, Ontario',1889,'Attawapiskat','Silurian','Llandovery','Telychian','upper Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,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,-9.25537,-45.5974,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cabot Head, Bruce Peninsula, Ontario',1890,'Manitoulin','Silurian',NULL,NULL,'Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,430,'Early Silurian (late Llandovery, 430 Ma)',433,2,'0','Outcropping reef ',3,'Mud mound or bank','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,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,-21.0571,-48.7175,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grand Rapids, Manitoba',1891,'Atikameg-Cedar Lake','Silurian','Llandovery','Aeronian','Aeronian-Telychian',433.40,440.80,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',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,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,-7.90273,-52.9989,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wahringa Farm, Bakers Swamp, NSW',1892,'','Ordovician','Lower Ordovician','Floian','Arenig',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',471,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','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,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',10.5221184767,130.074824027,10.5221184767,130.074824027,10.5221184767,130.074824027,19.029,-173.384,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dolayba',1893,'','Silurian','Wenlock','Sheinwoodian','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,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,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,-26.8221,11.9634,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Trinity Lake, Jasper, Alberta',1894,'Cathedral','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',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,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,-113.283373332,1.90271,-77.378,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('N Franklin Mts., N.W.T.',1895,'Franklin Mountain','Cambrian','Furongian','Lawsonian','Croixian-Tremadocian',477.70,497.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',488,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,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,-86.4325239111,2.98657,-60.1892,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gayna River, Mackenzie Mts.',1896,'Mount Kindle','Ordovician','Upper Ordovician','','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',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','','Unknown','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,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,-112.452616455,10.9779,-55.0351,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ware, British Columbia',1897,'Skoki','Ordovician','Middle Ordovician','Dapingian','Dapingian',467.30,470.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',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,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,-102.794554005,7.0591,-66.2325,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pine Pass, British Columbia',1898,'Beaverfoot','Ordovician','Upper Ordovician','Katian','early Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',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,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,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,-120.538298297,7.09412,-64.3958,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kingston, Ontario',1899,'Gull River','Ordovician','Upper Ordovician','','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',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,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,-24.7543,-51.3393,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mississauga, Ontario',1900,'Meaford','Ordovician','Upper Ordovician','Katian','Richmondian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',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,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,-24.4069,-54.3592,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gore Bay, Manitoulin Island, Ontario',1901,'Georgian Bay','Ordovician','Upper Ordovician','Katian','Rawtheyan',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',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','','Unknown','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,NULL,NULL,'2','Medium zonation',NULL,NULL,'2','30-60% micrite',NULL,NULL,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,-21.1518,-53.0041,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Eddies Cove West, Newfoundland',1902,'Watts Bight','Ordovician','Lower Ordovician','Tremadocian','upper Ibexian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',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','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',866,1084,'Suspect tabulate corals reideintified as calcareous algae (Elias et al. 2020, Geology)',50,-57,-2541433,-3838303,'Canada','North America',121,'',50.75,-57.1667,'',NULL,7.60046477895,-86.8643437527,7.60046477895,-86.8643437527,7.60046477895,-86.8643437527,-35.338,-60.3462,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-12-26 22:09:49'),('Colonsay, Saskatchewan',1903,'Winnipegosis','Devonian','Middle Devonian','Givetian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',390,3,'0','Outcropping reef ',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','','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',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,-19.9179,-39.5245,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Estevan, Saskatchewan',1904,'Winnipegosis','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',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,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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,-23.1617,-39.9599,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Whitemud, Clearwater R., Alberta',1905,'Keg River','Devonian','Middle Devonian','Eifelian','Middle Devonian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',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','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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,-14.7923,-37.9871,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Evie Bank, British Columbia',1906,'','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',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,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',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,-8.12503,-40.7592,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Keg River Barrier Reef, Pine Point',1907,'Keg River','Devonian','Middle Devonian','Eifelian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',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,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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,-12.1055,-36.6045,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Keg River Barrier Reef, Redfern',1908,'Keg River','Devonian','Middle Devonian','Eifelian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',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,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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,-10.4077,-42.2386,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Presqu-ile Barrier reef, Redfern Lake',1909,'','Devonian','Middle Devonian','Givetian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',390,3,'0','Outcropping reef ',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,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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,-8.57542,-42.2723,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Monkman Lake, British Columbia',1910,'Flume','Devonian','Upper Devonian','Frasnian','early Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',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','0',NULL,'','Unknown',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,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,-6.44712,-46.1145,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mt. Buchanan, British Columbia',1911,'Flume','Devonian','Upper Devonian','Frasnian','early Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',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','','Unknown',NULL,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,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,-7.45815,-46.4541,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Noonday Peak, Alberta',1912,'Cairn','Devonian','Upper Devonian','Frasnian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',379,3,'0','Outcropping reef ',3,'Mud mound or bank','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,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,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,-8.37685,-46.3915,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Forbes Creek, Banff, Alberta',1913,'Peechee','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'0','Outcropping reef ',NULL,NULL,'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,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,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,-10.2115,-47.0751,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rice Brook, Alberta',1914,'Fairholme','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'0','Outcropping reef ',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','','Unknown',NULL,NULL,'1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,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,-9.91857,-47.0161,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Leduc & Acheson, Alberta',1915,'Leduc','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','300',NULL,NULL,NULL,'4','More than 1000 m',NULL,'16',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,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,-12.9267,-42.1038,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bonnie Glen, Alberta',1916,'Leduc','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','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,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,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,-13.6522,-43.1128,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Duhamel, Alberta',1917,'Leduc','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','275',NULL,NULL,NULL,'3','More than 100 m',NULL,'8',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,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,-13.4997,-42.0841,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Westerose South, Alberta',1918,'Leduc','Devonian','Upper Devonian','Frasnian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',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,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,NULL,'1','Low zonation',NULL,NULL,NULL,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,-13.0581,-42.5543,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wizard Lake, Alberta',1919,'Leduc','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','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,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,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,-12.9177,-42.2485,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grosmont, Alberta',1920,'Grosmont','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'0','Outcropping reef ',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,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,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,-8.66084,-39.4554,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grosmont II, Alberta',1921,'Grosmont','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'0','Outcropping reef ',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,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,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,-13.5012,-40.2781,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alexandra, Hay River, N.W.T.',1922,'Alexandra','Devonian','Upper Devonian','Frasnian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',379,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','45',NULL,NULL,NULL,'4','More than 1000 m',NULL,'48',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'50','0','50',0,'no',0,'no','2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',917,2545,'Barrier reef complex.\n35-45 m thick.\nReef complex #1 of ref. 2545\nRugose corals and stromatoporoids about equally important. Tabulate corals present\nReefs also in Twin Falls and Hay River Fms.',60,-116,-625010,-4164963,'Canada','North America',121,'2738, 2735',60.5,-116.25,'WAHR','81119',-3.95125036067,-53.0608310769,-3.95125036067,-53.0608310769,3.71007385886,-113.308256528,-7.15647,-37.4353,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Carlson Lake, N.W.T.',1923,'','Devonian','Upper Devonian','Frasnian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',376,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m',NULL,'55',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',917,0,'Coral-stromatopore patch reefs and biostromes. Maximum thickness 50 m.',62,-123,-90046,-4245470,'Canada','North America',121,'',62.3333,-123.5833,'','',-0.00916951510691,-53.3867983074,-0.00916951510691,-53.3867983074,7.44525889832,-114.616409499,-2.39902,-38.1107,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Celibeta, Jean Marie, N.W.T.',1924,'Jean-Marie','Devonian','Upper Devonian','Frasnian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',377,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',917,2737,'Platform reef chain > 100 km length, 30 km width. Thickness around 100 m.\nJean Marie member of Redknife = Jean Marie Formation',61,-121,-329200,-4356514,'Canada','North America',121,'',61.3333,-121.75,'WAHR','83807',-1.2574809227,-53.8231221184,-1.2574809227,-53.8231221184,6.12733206636,-114.725332,-4.53189,-38.414,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Arrowhead, Jean Marie, N.W.T.',1925,'Kakisa','Devonian','Upper Devonian','Frasnian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',377,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100','1924',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',917,2738,'See reef 1924 for remarks.',61,-122,-251315,-4334621,'Canada','North America',121,'',61.05,-122.5,'WAHR','84005',-1.08860920722,-54.2502420329,-1.08860920722,-54.2502420329,6.1830172513,-115.183794754,-4.39722,-38.8544,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Winnifried Pass, Alberta',1926,'','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','35',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',917,1507,'Scattered stromatoporoids and colonial corals.\nMicrite and stromatactis mounds on fore-reef slope.\n35 m thick, 75 m exposed width.\n',53,-119,-749690,-5147335,'Canada','North America',121,'',53.6333,-119.2833,'WAHR','83698',-6.41682338185,-59.7040720328,-6.41682338185,-59.7040720328,0.401303476146,-120.448549549,-8.00935,-46.3771,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ice Fall Brook Canyon, B. C.',1927,'Southesk','Devonian','Upper Devonian','Frasnian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',376,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','90',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'6','Calcisponges','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',917,0,'Stacked mounds with sponges(?), corals and amphiporids.\n90 m total thickness. Individual patch reefs 5-42 m thick.',51,-117,-1036163,-5206185,'Canada','North America',121,'',51.9,-117.0667,'','',-8.4879277264,-60.4261964381,-8.4879277264,-60.4261964381,-1.78150507741,-120.642101751,-10.0961,-47.0545,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Crossfield, Alberta',1928,'Wabamun','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,1,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','4','Others','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',917,0,'Famennian patch reef complex.\n150 km length, 3-5 km wide.\nLabechiid stromatopores, algae, gastropods.\nOther references in 917.',51,-114,240987,-4531957,'Canada','North America',121,'',51.8333,-114.1667,'','',-10.4021177389,-52.9334909505,-10.4021177389,-52.9334909505,3.14375898861,-111.456078697,-9.56542,-43.4076,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Crossfield II, Alberta',1929,'Wabamun','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',369,1,'1','Seismic data available ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150','1928',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','4','Others','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',917,0,'See reef 1928 for remarks.',50,-113,97824,-4617126,'Canada','North America',121,'',50.5833,-113.6667,'','',-11.1820322446,-53.9778040212,-11.1820322446,-53.9778040212,2.01047214805,-112.070111215,-10.6296,-44.1456,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Willow Creek, Drumheller, Alberta',1930,'','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',68,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','4',NULL,NULL,NULL,'4','More than 1000 m',NULL,'4',NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1151,0,'Oyster reef (biostrome).\nUp to 4 m thick, 4 km wide?\nUnbored and bored oysters\nEstuarine or barrier lagoon.\nOther refs. in ref. 1151.',51,-112,7530391,-6359882,'Canada','North America',121,'',51.5,-112.6667,'','',57.8366403488,-83.7108618835,57.8366403488,-83.7108618835,58.7411728127,-89.9911938864,59.4836,-83.8244,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Merrill Ranch, Monarch, Alberta',1931,'','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',76,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1151,0,'Lagoonal intertidal setting.\nUp to 4.5 m thick oyster biostrome.\nAdditionally arenaceous forams.\nUnbored!\n',49,-113,7358350,-6657857,'Canada','North America',121,'',49.75,-113.1667,'','',54.9431736151,-81.1939878196,54.9431736151,-81.1939878196,57.0347431384,-85.7279846624,57.1294,-76.1137,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Milk River, Alberta',1932,'Foremost','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',79,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1151,0,'Oyster reef\nBack barrier lagoonal setting.\n0.6 -1.3 m thick.',49,-112,7276262,-6671001,'Canada','North America',121,'',49.1667,-112.0833,'','',54.210291147,-80.2505241972,54.210291147,-80.2505241972,56.3193865839,-84.6911660257,56.336,-75.2849,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Logan Co., North Dakota',1933,'Fox Hills','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',68,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'80',NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1152,1151,'Only locality 5 of ref. 1152 with in situ oysters.\n3 oyster species.\nPlenty of Cliona borings.',46,-99,6705084,-6192999,'United States','North America',101,'',46.2833,-99.6667,'','',50.609335501,-71.8411891442,50.609335501,-71.8411891442,52.045665474,-76.8573004164,51.8839,-72.24,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kemmerer, Wyoming',1934,'Frontier','Cretaceous','Lower Cretaceous','Albian','Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',105,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1153,1151,'Salt marsh or estuarine.\n2 oyster species.\n0.5 m thick.',41,-110,4757492,-6256112,'United States','North America',101,'',41.8333,-110.5,'','',41.7450299969,-62.0803533086,41.7450299969,-62.0803533086,43.6096235547,-68.5154409592,42.3855,-68.6567,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Green Island Inlier',1935,'','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',68,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1154,1155,'Extreme marginal setting.\nbrackish water indicated by other macrofauna, lignite seams.\nRudists accompanied by dasycladaceans and ostracods.\nAll Campanian-Maastrichtian rudist frameworks are more coppices and thickets rather than biostromes or reefs.',18,-78,2577302,-7980016,'Jamaica','North America',222,'',18.3333,-78.2833,'','',18.6189178203,-70.5820798703,18.6189178203,-70.5820798703,20.1227470792,-73.5200006834,19.2147,-72.1544,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maldon Inlier',1936,'Guinea Corn','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',68,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1155,1154,'Coral reef overlain by 15.6feet of clay-shale; overlain by small rudist biostrome; overlain by 4feet of whitish beds; overlain by small rudist biostromes 5.2feet thick; overlain by 32 inches of low relief, reefal beds of rudists; overlain by 30 feet of soft (siliciclastic) beds; overlain by rudist biostromes\n\n\n',18,-77,2564730,-7931623,'Jamaica','North America',222,'',18.3,-77.8,'WAHR','66456',18.4484925801,-70.1314206564,18.4484925801,-70.1314206564,19.9759161748,-73.0559183861,19.1124,-71.6796,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Central Inlier',1937,'','Cretaceous','Upper Cretaceous','Santonian','upper Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',84,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1154,1155,'late Santonian to Maastrichtian rudist frameworks.\nSee reef 1935 for remarks.\nPatch reef with low mounds of radiolitid clusters that were successively overlain by 0.5 m of cobbly limestones with abundant corals, a thin, reddish soil, 0.5m of in-situ rudists, another reddish soil zone, and a highly fragmented zone with radiolitid rudist fragments followed by a small diversity of rudists.\n',18,-77,1634809,-7080247,'Jamaica','North America',222,'',18.0333,-77.25,'','',12.8814361537,-64.4315142852,12.8814361537,-64.4315142852,15.4667861044,-68.1155161745,16.6507,-62.6639,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Benbow Inlier',1938,'','Cretaceous','Lower Cretaceous','Barremian','Barremian-Aptian',113.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',125,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1154,1155,'Only clusters of rudists with a few corals.\nJubilee Limestone.\nCaprotinid biostromes. Some microbial crusts.',18,-77,-751032,-6265940,'Jamaica','North America',222,'1159',18.2667,-77.0333,'','',3.03166557066,-48.8343952641,3.03166557066,-48.8343952641,5.29456535835,-54.2822088331,8.62873,-55.1234,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('San Polo, Matese',1939,'','Cretaceous','Upper Cretaceous','Cenomanian','upper Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',95,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'8',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','1','Corals','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'40','50','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1156,1164,'Rudist-coral-red algal patch reefs at platform edge.',41,14,3194867,1439515,'Italy','Europe',344,'',41.4556,14.5083,'WAHR','74197',28.9814976307,13.279165654,28.9814976307,13.279165654,24.6331146242,16.7828178706,24.0071,13.4287,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monte Girifalco, Mt. Carseolani',1940,'','Cretaceous','Upper Cretaceous','Santonian','Santonian-Campanian',72.10,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',83,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','3',NULL,NULL,NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1157,0,'Upper Santonian-Campanian.\n3-4 m thick sequence of dolomites with radiolitid banks (inter-supratidal).\n8 rudist species.',42,13,3299266,1361507,'Italy','Europe',344,'',42.0167,13.3833,'WAHR','67601',32.0018437726,10.9408378907,32.0018437726,10.9408378907,31.1597756641,14.7603887597,27.3575,14.73,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ricetto, Mt. Carseolani',1941,'','Cretaceous','Upper Cretaceous','Santonian','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,'2','10 - 100 m',NULL,'30','1940',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1157,1173,'4-5 m thick biostrome.\nHippurites (3 species) and corals.',42,13,3339669,1337867,'Italy','Europe',344,'',42.25,13.0167,'WAHR','67594',32.8645448231,14.6050856425,32.8645448231,14.6050856425,29.7392951379,15.1406373688,27.1471,13.4155,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monte Grisa, Triest',1942,'','Cretaceous','Upper Cretaceous','Santonian','Santonian-Campanian',72.10,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',83,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1158,0,'Although 11 rudist species in area (mostly radiolitits) buildups consist of monospecific assemblages (e.g. Katzeria hercegovinaensis).',45,13,3750472,1494833,'Italy','Europe',344,'',45.7,13.7333,'WAHR','34707',35.5969811615,16.7335680315,35.5969811615,16.7335680315,34.5713375226,16.4411015052,30.8352,16.1488,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Khenchela',1943,'','Cretaceous','Upper Cretaceous','Santonian','Santonian-Campanian',72.10,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',83,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species','6','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1166,1780,'Late Santonian to early Campanian.\nVaccinites bioconstructions.\n5 species described (+ 1 ssp.)',35,7,2555891,724755,'Algeria','Africa',706,'',35.4167,7.0833,'WAHR','34709',25.5117110617,8.49489013187,25.5117110617,8.49489013187,26.2484226343,6.339419701,21.8949,8.14604,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Barrio Barrancas, Puerto Rico',1944,'','Cretaceous','Lower Cretaceous','Albian','middle Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',107,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','10',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species','1','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1155,0,'Monospecific Caprinuloidea bank.\n10 m thick.\n',18,-66,-939333,-5971739,'United States','North America',101,'',18.1833,-66.3167,'','',-3.57044233641,-49.8425871173,-3.57044233641,-49.8425871173,-1.55806543769,-55.6006791544,0.259582,-54.6669,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pointe-à-Pierre, Trinidad',1945,'','Cretaceous','Lower Cretaceous','Aptian','upper Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',113,2,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','5','Rudists','5','Rudists',NULL,NULL,NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1155,0,'Exotic flysch block.',10,-61,44612,-3630126,'Trinidad and Tobago','North America',201,'',10.3167,-61.45,'','',5.12536396364,-23.9684367403,5.12536396364,-23.9684367403,8.37662209818,-29.714190508,9.38877,-29.1389,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lambs River, Marchmont Inlier',1946,'','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',68,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','4','Stromatoporoids','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,'50','40','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1155,0,'Mature coppice phase of Type B (ref. 1155) rudist framework evolution.\nStromatoporoid heads, Titanosarcolites, Biradiolites, Plagioptychus, Radiolites,Torreites  & Antillocaprina rudists, various oysters, Brachiodonte (bivalve), algae\n',18,-77,2555031,-7943876,'Jamaica','North America',222,'',18.2167,-77.8833,'','',18.3929857343,-70.2374289826,18.3929857343,-70.2374289826,19.9150102692,-73.1595355329,19.0421,-71.7757,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gruenbach, Niederoesterreich',1947,'','Cretaceous','Upper Cretaceous','Santonian','upper Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',84,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','3','Microbes','47','Bivalves (mostly oysters) - algae (microbes)',NULL,NULL,'45','55','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1159,0,'Dendriform Hippurites-Bioherms.\n1- 2 m in diameter and thickness.\nSome microbial crusts around rudists.\nCliona and microbe borings.',47,16,3951096,1729806,'Austria','Europe',301,'',47.8194,16.0111,'','',40.5756533055,17.4437202629,40.5756533055,17.4437202629,37.2669213697,16.2921090781,31.9001,17.5441,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tres Lagunas, Patagonia',1948,'Cotidiano','Cretaceous','Lower Cretaceous','Berriasian','Berriasian-Valanginian',132.90,145.00,22,'late Tithonian - early Valanginian',141,140,'Early Cretaceous (Berriasian, 142.4 Ma)',140,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,1,'Temperate','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'20','80','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild','2','Intensive','2','Intensive',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1160,1245,'Thick branching corals and bivalves (Gryphea, Ostrea).',-44,-70,-7037781,-2129296,'Argentina','South America',201,'',-44.8333,-70.8333,'','',-51.9315981219,-36.3479183632,-51.9315981219,-36.3479183632,-47.4036240492,-37.6260792543,-43.8091,-32.3182,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lago Fontana, Patagonia',1949,'Cotidiano','Jurassic','Upper Jurassic','Tithonian','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',147,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','80','20',0,'no',0,'no','2','6 to 24 reef building species','7','1','Constructor guild','2','Intensive','2','Intensive',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1160,1245,'Coral assemblage in olistostrome member of Vallcarga Fm.\n36 genera belonging to 2 orders and 9 suborders. Few reef building genera:\nE.g.\nActinastraea\nAstraraea\nHolocoenia\nFungiastraea\n\nColonial forms predominate but mostly of small size (less than 10 cm).\nLarge borings evident on plates',-44,-71,-7055151,-2185032,'Argentina','South America',201,'',-44.85,-71.5,'','',-52.5910045483,-37.6236861851,-52.5910045483,-37.6236861851,-48.2823925314,-36.4366967524,-43.0449,-31.5451,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Oberstdorf',1950,'Schrattenkalk','Cretaceous','Lower Cretaceous','Aptian','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,120,'Early Cretaceous (early Aptian, 121.8 Ma)',123,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','4',NULL,NULL,NULL,'2','10 - 100 m','50','5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'5','75','20',0,'no',0,'no','3','25 or more reef building species','32','1','Constructor guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1159,1492,'Coral-stromatopore bioherms in Schrattenkalk\n(up to 4 m thickness and 50 m width).\nBasement are rudist (requienid) limestones.\nRef. 1159\nChaetetids, stromatopores, and other sclerosponges.\n4 coral species, microbial crusts, corallinacean crusts.\n\nAccording to ref. 1514 thirty coral species present. 98 % colonial forms.\nHigh debris, very rare in situ framestones.',47,10,4447583,912618,'Germany','Europe',331,'1514',47.4167,10.2167,'WAHR','25535',35.139913271,23.2632792635,34.2880647984,23.8196188545,37.704680398,21.8000168874,31.5491,21.1869,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fenoliga, Istria',1951,'','Cretaceous','Upper Cretaceous','Turonian','Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',93,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','3','Microbes','47','Bivalves (mostly oysters) - algae (microbes)',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1159,1214,'Classified as paucispecific, simple, dendriform\nradiolitid-biostromes by ref. 1159.\nSeveral biostromes, less than 1 m thick.\nSome microbes as binders.',44,13,3629135,1482390,'Croatia','Europe',308,'',44.7667,13.9069,'WAHR','24021',34.072412316,18.1864756777,34.072412316,18.1864756777,29.6006051769,17.5737893374,28.6424,13.9314,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Atzlgraben, Brandenberg',1952,'','Cretaceous','Upper Cretaceous','Coniacian','lower Coniacian',86.30,89.80,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',88,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15',NULL,NULL,NULL,'3','More than 100 m',NULL,'2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)','1','Red algae','10','70','20',0,'no',0,'no','3','25 or more reef building species','34','1','Constructor guild','1','Present','1','Present','3','Pronounced zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1956,1159,'Diverse corals (30 species), solenporacean algae, some microbes and rudists.\nMicrosolena quite important (first description from Upper Cretaceous of Alps).\nCoral-rudist-algal mounds (up to 10 m thick) capped by rudist (Vaccinites) biostromes, up to 5 m thick.',47,11,4024851,1406121,'Austria','Europe',301,'1514, 1492',47.5,11.9222,'WAHR','24265',39.2580196758,14.5811902632,39.2580196758,14.5811902632,34.6767685292,17.7389247868,32.2257,13.7576,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Brac',1953,'','Cretaceous','Upper Cretaceous','Cenomanian','upper Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',95,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','4',NULL,NULL,NULL,'1','Less than 20 m','20',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','1','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1159,0,'1 to 4 m thick and 2 to 20 m wide mud mounds with stromatolites and Stromatactis.',43,16,3363076,1669851,'Croatia','Europe',308,'',43.2792,16.7028,'','',30.7302633937,19.8436157978,30.7302633937,19.8436157978,25.5720624294,19.2698718214,25.2074,15.7653,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cuatretonda, Valencia',1954,'','Cretaceous','Upper Cretaceous','Maastrichtian','lower Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',69,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m','45',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species','5','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1161,0,'Bioherms of mostly small Pironea (3 species).\r\nOne Hippurites sp. Very few corals.\r\n1.2 m max. thickness.\r\nAround 45 m wide complex.',38,0,4335133,-119113,'Spain','Europe',304,'',38.9667,-0.3833,'WAHR','67551',32.1643924455,0.79315369847,32.1643924455,0.79315369847,35.6347627626,-0.54603616579,30.7945,-0.940908,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('La Cadiere',1955,'La Cadière d\'Azur','Cretaceous','Upper Cretaceous','Santonian','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no','2','6 to 24 reef building species','7','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2189,1175,'Peri-deltaic environment\nRudist baffestone buildups.\nrelatively diverse fauna of hippuritids, radiolitids and caprinids (7 species).\n',43,5,4184649,727085,'France','Europe',331,'',43.2167,5.7667,'WAHR','67011',38.6601637697,9.06005433849,38.6601637697,9.06005433849,43.2167,5.7667,33.3078,6.84157,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ostuni',1956,'','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',77,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1163,1774,'Rudist massive organogenic limestones.\nWith Favus n.gen.',40,17,3936391,1585750,'Italy','Europe',344,'',40.7333,17.55,'WAHR','74801',29.9664150534,16.1882156249,29.9664150534,16.1882156249,29.8490200107,16.7578385795,25.7337,17.9425,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Khashm Buwaibiyat',1957,'Aruma','Cretaceous','Upper Cretaceous','Campanian','upper Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,75,'Late Cretaceous (Late Campanian, 75 Ma)',74,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'4','More than 1000 m',NULL,'90',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species','2','2','Baffler guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1165,0,'2 m thick prominent biostrome at road.\n2 rudist species dominant (Biradiolites and a new form Eodictyoptychus).\nMatrix is fine bioclastic packstone.\n',25,46,726668,4125562,'Saudi Arabia','Asia',503,'',25.1667,46.8333,'WAHR','34710',8.76968531664,41.6975761424,8.76968531664,41.6975761424,8.41356447678,38.3868909292,4.20054,39.414,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Khashm Tawqi',1958,'Aruma','Cretaceous','Upper Cretaceous','Campanian','upper Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,75,'Late Cretaceous (Late Campanian, 75 Ma)',74,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'4','More than 1000 m',NULL,'90','1957',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species','3','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1165,0,'see reef 1957 for remarks.',25,46,767752,4157551,'Saudi Arabia','Asia',503,'',25.4333,46.4667,'WAHR','34711',9.07814029634,41.4011031654,9.07814029634,41.4011031654,8.74008255385,38.1112063768,4.52328,39.1362,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Stranice',1959,'','Cretaceous','Upper Cretaceous','Campanian','Campanian-Maastrichtian',66.00,83.60,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',70,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present','2','Medium zonation',NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1167,0,'Hippuritid bioherms (15 m thick) overlying calcarenites with corals and radiolitids.',46,15,4684830,1452863,'Slovenia','Europe',328,'',46.3667,15.4,'WAHR','74510',35.6898417602,17.7633912502,35.6898417602,17.7633912502,38.7498995737,15.6951961438,32.5129,18.18,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Barranc del Racó, Bocairent',1960,'','Cretaceous','Upper Cretaceous','Maastrichtian','late Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',66,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1169,0,'Rudist thicket with Hippurites, echinoids, colonial (Actinacis, Procladocora) and solitary corals in biomicritic matrix.\r\n2 m thick.',38,0,4311506,-144199,'Spain','Europe',304,'',38.7667,-0.6333,'WAHR','74557',31.9902080108,0.535807616007,31.9902080108,0.535807616007,35.4516084293,-0.804836276778,30.6267,-1.20028,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Soria',1961,'','Cretaceous','Upper Cretaceous','Coniacian','Coniacian-Santonian',83.60,89.80,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','30','10',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1170,0,'Rudist limestones in unit 4 \n(Ethelia in \'milieux récifaux\').\nUp to 5 m thick.',41,-2,3896193,73119,'Spain','Europe',304,'',41.75,-2.4333,'','',34.4354978981,2.00408068482,34.4354978981,2.00408068482,34.8194169064,0.141040791462,31.03,0.13964,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dugi Otok Island',1962,'','Cretaceous','Upper Cretaceous','Cenomanian','latest Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',94,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1171,0,'Rudist buidlups and biostromes.\nNo description.',43,15,3480497,1565357,'Croatia','Europe',308,'',43.8833,15.2333,'','',31.8475323852,19.2587995619,31.8475323852,19.2587995619,26.5798435067,18.4965867166,26.1245,14.8659,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ruvo di Puglia',1963,'','Cretaceous','Upper Cretaceous','Cenomanian','late Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',93,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','5',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1172,0,'Patch reef with radiolitids (2 species) and caprinids (2 species).\nUp to 5 m thick.',41,16,3094473,1596548,'Italy','Europe',344,'',41.1167,16.4833,'WAHR','67617',29.4261547076,17.9901906549,29.4261547076,17.9901906549,25.2960476535,16.3755667143,23.7714,14.615,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Saint-Baudille',1964,'','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',152,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','100','10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1178,0,'Bioherms with microsolenid corals.\n10-100 m width\n15-20 m thickness.',43,3,4109428,845225,'France','Europe',331,'',43.75,3.75,'','',22.9044747871,21.8553291209,22.9044747871,21.8553291209,28.376373247,22.7707906514,34.9505,13.0597,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Orgon',1965,'','Cretaceous','Lower Cretaceous','Barremian','Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',127,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'40','60','0',0,'no',1,'yes','2','6 to 24 reef building species','14','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1179,813,'Diverse corals.\nActinastrea, tabulogyra, Dimorphocoenia, Columnastrea, Calmophyliopsis, Microsolena, ...\nAssociated are oysters and other bivalves and bryozoans.',43,5,3859892,656271,'France','Europe',331,'2575',43.7833,5.05,'WAHR','64072',28.4377509862,20.9640001771,28.4377509862,20.9640001771,32.0821574125,19.133827104,34.1454,15.4665,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alcabideche',1966,'','Cretaceous','Lower Cretaceous','Hauterivian','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',133,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'5','65','30',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1180,0,'Association fo stromatoporoids, Lithocodium aggregatum and diverse coral (thamnasteriids, astrocoenids, microsolenids, calamophylliids, stylinids).\n',38,-9,3276885,-583462,'Portugal','Europe',304,'',38.7347,-9.4194,'','',24.4526390094,5.43197614621,24.4526390094,5.43197614621,28.9998085289,1.86310983392,32.5778,1.10221,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sao Juliao',1967,'','Cretaceous','Lower Cretaceous','Aptian','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,120,'Early Cretaceous (early Aptian, 121.8 Ma)',123,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','3','Microbes','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species','5','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1180,0,'Like reef 1966, but not as diverse (obsolete)\nRudist bioconstruction\nBedoulian age.',38,-9,3302550,-574954,'Portugal','Europe',304,'',38.9403,-9.4083,'WAHR','67544',27.6796112742,4.88084299998,26.9895075116,5.27181067633,30.6615109829,1.12404361192,32.064,2.75312,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ponta da Rana',1968,'','Cretaceous','Lower Cretaceous','Albian','upper Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,100,'Early Cretaceous (late Albian, 102.6 Ma)',101,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','3',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species','6','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',1180,0,'Bioaccumulations of rudists (toucasiformes and capriniformes): 6 species.\n3 m maximum thickness.',38,-9,3492110,-480589,'Portugal','Europe',304,'',38.6722,-9.3208,'WAHR','67543',28.9270308334,0.877976468784,28.9270308334,0.877976468784,30.9327189864,-3.30238382804,29.4018,-2.98615,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ugolka, Carpathians',1969,'','Cretaceous','Lower Cretaceous','Barremian','Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',127,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','150',NULL,NULL,NULL,'2','10 - 100 m','100','100',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','2','Green algae','5','90','5',0,'no',0,'no','3','25 or more reef building species','37','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1181,0,'Urgonian facies 2-150 m thick.\nBiomoirphic limestones with whole skeletons of corals and algae. 24 coral species. 2 chaetetid sp., 11 algal sp.\nCores 5-20 m thick and 5-10 m wide, 8-100 m long.\nUpper sublitoral.',48,23,3437851,2287012,'Ukraine','Europe',301,'',48.3333,23.5,'WAHR','67457',36.2252591334,34.1131794495,36.2252591334,34.1131794495,39.2390441319,33.3263236154,27.2485,29.9379,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Boljevac, Arnaut River',1970,'','Cretaceous','Lower Cretaceous','Barremian','late Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',126,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species','6','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1182,0,'Rudist biostromes with Toucasia, Matheronia, Monopleura and Requienia.\nVery small coral bioherms in the vicinity.',43,22,2925161,2061022,'Yugoslavia','Europe',307,'',43.9167,22.25,'WAHR','67545',31.7571131087,34.7642028699,31.7571131087,34.7642028699,34.7452188098,33.6354410557,24.0955,26.3738,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mokhorotubani, Dzirul Massif',1971,'','Cretaceous','Lower Cretaceous','Hauterivian','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',133,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'70','1971',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','90','0',0,'no',0,'no','3','25 or more reef building species','23','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',1183,1184,'Massive organogenic limestones.\nExclusively corals (diverse)\nDolomitic.',42,43,4970230,3657834,'Georgia','Europe',301,'',42.3667,43.3167,'WAHR','67511',34.5956231464,52.2779823436,34.5956231464,52.2779823436,36.453495715,52.7125323827,35.6557,48.7921,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shkmeri, Dzirul Massif',1972,'','Cretaceous','Lower Cretaceous','Hauterivian','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',133,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','130',NULL,NULL,NULL,'3','More than 100 m',NULL,'70','1971',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','70','20',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1184,1183,'Large organogenic structure (up to 130 m) of bioherm type.\nComposed of corals and chaetetids.\nDiverse corals in spite of poor preservation.',42,43,5014288,3610164,'Georgia','Europe',301,'',42.7167,43.0167,'WAHR','67510',34.8307072848,51.8634841197,34.8307072848,51.8634841197,36.720629963,52.3187086745,35.9687,48.458,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ali-Goresha area, Dzirul Massif',1973,'','Cretaceous','Lower Cretaceous','Barremian','early Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',128,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','10',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','5','Rudists','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'10','90','0',0,'no',0,'no','3','25 or more reef building species','29','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1184,0,'Coral-rudist biostromes of 4-10 m thickness.\nCorals dominant and very diverse.\nRudists mostly requienids and diceratids.',42,43,4967386,3705674,'Georgia','Europe',301,'',42.0833,43.65,'WAHR','67512',35.323065895,53.1556841707,35.323065895,53.1556841707,37.1664691742,52.8503830909,34.7993,49.6551,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Manistee County, Michigan',1974,'','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1600','1875',0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',1185,0,'',44,-86,-3024961,-5096370,'United States','North America',101,'',44.2167,-86.3167,'','',-26.3021918645,-97.9722266225,-26.4261735354,-94.7908599908,-26.4261735354,-94.7908599908,-20.71,-51.1347,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Barre de la Jaume, Var',1975,'','Cretaceous','Upper Cretaceous','Coniacian','Coniacian',86.30,89.80,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',87,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','5','Rudists','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'20','50','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',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',1188,0,'Rudist-coral communities on palaeohigh.\nSmall chaetetid bioherms at base. Surrounded by bioclastic limestones.',43,5,4176009,732163,'France','Europe',331,'',43.15,5.8222,'','',38.3485660798,9.67924560087,38.3485660798,9.67924560087,43.15,5.8222,33.1992,6.67533,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Barres de Cuers',1976,'','Jurassic','Middle Jurassic','Bathonian','middle Bathonian',166.10,168.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',166,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','4',NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1189,0,'Small coral bioherms in first limestone formation.\nBryozoans and bivalves associates.\nUp to 4 m thick.',43,6,4113394,1342871,'France','Europe',331,'',43.2667,6.0278,'','',21.9667656694,26.8343834361,21.9667656694,26.8343834361,43.2667,6.0278,33.1244,16.3751,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jebel Ouenza',1977,'','Cretaceous','Lower Cretaceous','Aptian','upper Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',113,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','13',NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','80','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',1190,0,'Gargansian stage\ncoral biostromes.\nWith calcisponges (chaetetids?)\nUp to 13 m thick.',35,8,2286364,862402,'Algeria','Africa',706,'',35.95,8.0833,'','',17.198207138,16.8725846301,17.198207138,16.8725846301,20.4107733179,11.9258481084,20.7176,12.8149,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Murchas',1978,'','Neogene','Miocene','Middle Miocene','late Langhian',13.80,14.80,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',14,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','4',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','1','Corals','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'80','20','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1191,0,'Coral-oyster patch reefs.\nUpt to 3-4 m thick and 18 m wide.\nSiliciclastic ramp setting.\nCorals are Heliastrea, Porites, Tarbellastrea, Mussismilia.\nOyster Hyotissa squarrosa up to 70 % of the reef.\nRare encrusters. Some rhodolites.\n10 % is sparry calcite.',36,-3,4891414,-504231,'Spain','Europe',304,'',36.9333,-3.55,'WAHR','69779',35.3162773301,-5.03917078029,35.3162773301,-5.03917078029,36.3402029167,-3.81383198856,37.0271,-4.71153,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sebaa Chioukh Hills, Orania',1979,'','Neogene','Miocene','Upper Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',6,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m','1000','14',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','5','65','30',0,'no',0,'no','2','6 to 24 reef building species','7','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1196,2584,'6 coral species.\nFauna dominated by Tarbellastrea and Porites.\nSeveral bryozoans',35,-1,4673547,-190024,'Algeria','Africa',706,'',35.1833,-1.3333,'WAHR','69864',34.3498565483,-2.1648017844,34.3478684404,-2.1667778081,34.6257980338,-1.25434863268,35.0839,-1.56593,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Traras, Orania',1980,'','Neogene','Miocene','Upper Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',6,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'12','1979',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1196,2584,'More marls and more finger colonies of Porites than in reef 1979.',35,-1,4678012,-209525,'Algeria','Africa',706,'',35.2167,-1.5333,'WAHR','70785',34.3834583175,-2.36274129549,34.3814707386,-2.36471249128,34.6631314671,-1.45196190614,35.1186,-1.76535,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ofaqim II',1981,'Ziqlag','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',15,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','12',NULL,NULL,NULL,'3','More than 100 m','150','7',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','5','70','25',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1201,0,'12 m thickness. 100-150 m width.\nMassive faviid corals dominant.\nOthers are stylophorids and poritids.\n40-80 % of reefs are coral. Other are corraline algae and encrusting forams. Rare bryozoans.',31,34,3961134,3319264,'Israel','Asia',508,'',31.3167,34.6167,'WAHR','69908',29.4093686504,31.9663026863,29.4069502185,31.9636682307,27.1958862797,33.1735768223,30.3354,33.3486,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wadi Sharm el Qibli',1982,'Rudeis','Neogene','Miocene','Lower Miocene','Burdigalian-Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',16,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m',NULL,'400','685',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',1,'Potential reservoir',1202,2440,'Massive and branching corals: Stylophora, Tarbellastraea, Montastrea.\nSomewhat protected. Reef slopes with abundant siliceous debris rich in molluscs and coralline algae.\nLoc. Wadi Sharm el Bahari very close.',25,34,3299690,3458414,'Egypt','Africa',715,'',25.5,34.65,'','',23.3173311192,31.8103546841,23.3173311192,31.8103546841,22.5413421038,33.4678975572,24.4569,33.4027,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sharm el Luli',1983,'','Neogene','Miocene','Lower Miocene','Burdigalian/Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',16,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','75',NULL,NULL,NULL,'2','10 - 100 m',NULL,'400','685',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1202,0,'Three individual prograding reef bodies.\nEach some 25 m thick.\n',24,35,3206557,3507747,'Egypt','Africa',715,'',24.8,35.0167,'WAHR','50927',22.6234489039,32.1845692303,22.6234489039,32.1845692303,21.8315891178,33.8032629102,23.7527,33.7565,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Belus-Peyrehorade',1984,'','Paleogene','Oligocene','Chattian','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',27,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'20','80','0',0,'no',0,'no','3','25 or more reef building species','60','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1203,2176,'60 coral species.\nLocally Delicate, globular and lamellar morphologies.\nMostly big and massive branched and domal.\n\n',43,-1,5582777,-349745,'France','Europe',331,'',43.5667,-1.1167,'WAHR','70067',41.2225678043,-5.07042487181,41.2225678043,-5.07042487181,42.4779890136,-1.24784546622,43.1882,-3.54654,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Abese-Estoti + Escornebeou, Aquitain',1985,'','Paleogene','Oligocene','Chattian','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',27,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,'3','More than 100 m',NULL,'20','1984',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','63','Corals - hydrozoans',NULL,NULL,'5','80','15',0,'no',0,'no','3','25 or more reef building species','82','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1203,2176,'Up to 100 coral species.\n50 massive globular species, 15 branched 10 phaceloid, 6 lamellar.\n3 m thick patch reefs, traceable for 200 m.\nAssociated with hydrozoans. Algae very rare.\nCarbonate ramp.\n\nLe Bois (Escornebeou) locality further west is subreefal envrionment with massive corals (about 25 species in 18 genera).',43,-1,5605228,-343138,'France','Europe',331,'',43.75,-1.05,'WAHR','22968',41.4077942162,-5.01685945573,41.4077942162,-5.01685945573,42.6595261563,-1.17382485155,43.3726,-3.48642,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gamachot near Villandraut, Bazadais, Gironde',1986,'','Neogene','Miocene','Lower Miocene','middle Aquitanian',21.00,22.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1203,2578,'In-place Porites colonizing marls.\nCoral carpet on muddy substrate.\n1 m thick bank interrupted by brackish deposits.\n',44,0,5692850,-279760,'France','Europe',331,'',44.4667,-0.3667,'WAHR','70074',42.464736309,-4.06786142842,42.464736309,-4.06786142842,43.5097195187,-0.523578690392,44.362,-2.31364,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('St. Martin-dOney',1987,'','Neogene','Miocene','Lower Miocene','late Aquitanian',22.00,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','63','Corals - hydrozoans',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',1203,0,'Rich coral fauna.\nAdditionally millporids and molluscs.',43,0,5621592,-312735,'France','Europe',331,'',43.8833,-0.7167,'','',41.7940411129,-4.45688414494,41.7940411129,-4.45688414494,42.8990610028,-0.880652737946,43.7101,-2.7729,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Le Peloua',1988,'','Neogene','Miocene','Lower Miocene','lower Burdigalian',17.50,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',19,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','50','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1203,0,'50 coral species.\nCoral colonies up to 1 m in diameter.\nSmall fringing reefs.',44,0,5844156,-211078,'France','Europe',331,'',44.6333,-0.65,'WAHR','70191',42.5307823781,-4.44709499186,42.8561838229,-4.0501522254,43.7923964771,-0.791404922491,44.6499,-2.32481,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ales-Villagreca, Sardegna',1989,'','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','25',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1204,0,'25 m thick coral bioherms with bryozoans and coralline algae.\nUnderlain by siliciclastic rocks.',39,9,5462227,100141,'Italy','Europe',344,'',39.45,9,'WAHR','85110',38.0039499647,3.07852994147,38.0039499647,3.07852994147,38.5551613716,7.60021602442,42.5162,1.92296,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Capo Tindari, Sicily',1990,'','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1204,0,'Fragmentary coral reef material.\nReef grown on metamorphic basement.',38,15,4749538,1247144,'Italy','Europe',344,'',38.1167,15.0833,'','',35.0644199659,11.4478879211,35.0644199659,11.4478879211,35.0220448533,15.017475347,36.8812,13.8978,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jabal al Akhdar',1991,'','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',1204,0,'Reefs with abundant branching corals in recrystallized micritic groundmass.\nAssociated with coralline algal carbonates.',32,21,4002026,1867618,'Libya','Africa',715,'',32.45,21.0667,'','',29.395239396,17.8189730598,29.395239396,17.8189730598,29.2719697833,20.3620058039,31.0863,19.6034,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bonifacio Basin, Corsica',1992,'','Neogene','Miocene','Lower Miocene','Burdigalian-Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',16,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1204,1739,'Coral-red algal reefs.\nExtensive development of bioherms in Bonifacio Basin.\nFour coral reef episodes.\nlate Aquitanian to Langhian.',41,9,5619599,442078,'France','Europe',331,'',41.4167,9.1667,'','',40.0749134823,5.74985768137,40.0749134823,5.74985768137,40.4326496109,8.7803082752,42.9056,5.04918,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aleria, Corsica',1993,'','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',15,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1204,0,'Coral-algal bioherms with pectinids and echinoids.',42,9,5601888,531645,'France','Europe',331,'',42.1,9.5,'','',40.9907604494,6.6805158274,40.9893146234,6.67783254734,41.2515150728,9.22010698977,42.8077,6.20816,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Palmi, Rocca Campana, Calabria',1994,'','Neogene','Miocene','Upper Miocene','late Tortonian',7.30,9.00,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',8,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','9',NULL,NULL,NULL,'3','More than 100 m',NULL,'40',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',1205,1204,'Seven coral species in area but only Tarbellastraea and Porites common',38,15,5061301,1460656,'Italy','Europe',344,'2578',38.3833,15.8667,'WAHR','70492',36.0800505491,11.2328887169,36.3880592003,11.9870601148,37.8781611326,15.6789484398,38.1173,15.5599,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Central Mallorca',1995,'','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','12','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'2','Algae','2','Algae','29','Coralline algae only (some corals)','1','Red algae','0','0','100',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',1206,0,'Position doubtful.\nRed algal mounds (12 m thick, tens of m wide).',39,2,5230007,-93077,'Spain','Europe',304,'',39.6667,2.75,'','',38.7528844687,-2.21384650911,38.7528844687,-2.21384650911,38.6257514096,2.31692859409,40.5653,-0.155035,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Serra de Tramuntana, NW Mallorca',1996,'Sant Elm','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','16',NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','60','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1206,0,'Up to 16 m thick reefs in medium- to coarse-grained terrigenous fans. One reef (coll. 69929) without terrigenous influx.\nPorites dominates coral fauna. Massive and encrusting corals dominant.\nRed algae abundant.\nMatrix wackestones with coral fragments, serpulids, bryozoans and oysters.',39,3,5258741,-79848,'Spain','Europe',304,'',39.8333,3,'WAHR','69927',38.986912432,-2.08584853375,38.986912432,-2.08584853375,38.7879044816,2.5680659563,40.7976,-0.0184898,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lisboa',1997,'','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','50',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','11',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1206,1203,'Less than 50 m thick coral reef (11 species).',38,-9,4979815,-1133086,'Portugal','Europe',304,'1645, 1647',38.6833,-9.2667,'WAHR','92102',36.4516369023,-12.4555574985,36.4516369023,-12.4555574985,37.8759845178,-9.57238679888,38.4405,-11.062,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alacant region',1998,'','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','60',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','5','65','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1206,0,'40-60 m thick reefs with abundant grainstones and rudstones with red-algae, corals, larger forams, bivalves and miliolids.',38,0,4928061,-319517,'Spain','Europe',304,'',38.25,-0.6667,'','',35.7234000349,-3.13133325409,35.7234000349,-3.13133325409,37.2715773006,-1.09335375752,38.1314,-2.4748,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Penedés, Barcelona',1999,'','Neogene','Miocene','Lower Miocene','Burdigalian-Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',16,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m',NULL,'7',NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','20','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1633,1206,'24 coral species in total (4 ahermatypic).\nPorites dominant. Other corals are Heliastrea, Tarbellastaea, Mussidae, Faviidae.\nFringing reefs up to 50 m thick and 3-7 km long with well developed prograding reef slopes.\nLarge reef with greatest diversity (12-16 species).',41,1,5439809,596656,'Spain','Europe',304,'1855',41.3167,1.75,'WAHR','70411',39.7963718264,-1.26078328401,39.7963718264,-1.26078328401,40.4661213106,1.46488232356,41.4023,0.300565,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Guercif',2000,'','Neogene','Miocene','Upper Miocene','late Tortonian',7.30,9.00,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',8,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','10',NULL,NULL,NULL,'1','Less than 20 m',NULL,'200',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1206,1195,'Coral reefs up to 10 m, but only 2-4 m thick in average.\nPorites and Tarbellastrea dominate.',34,-3,4548125,-381884,'Morocco','Africa',714,'',34.1833,-3.25,'','',32.9367972005,-4.4697092484,33.1058263623,-4.30492885279,33.5114885932,-3.17192223841,34.0713,-3.56074,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zevardi well',2001,'Urtabulak','Jurassic','Upper Jurassic','Oxfordian','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',156,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'160','974',0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','70','20',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','1','Present',2,'Actual reservoir',672,2836,'',39,64,5393629,5915464,'Uzbekistan','Asia',301,'',39,64.75,'WAHR','91782',36.8096332666,72.7620156159,36.8096332666,72.7620156159,39.7981366972,77.5984424699,36.8017,69.7092,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cansiglio Platform',2002,'','Cretaceous','Lower Cretaceous','Aptian','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,120,'Early Cretaceous (early Aptian, 121.8 Ma)',123,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','3','Microbes','47','Bivalves (mostly oysters) - algae (microbes)',NULL,NULL,'30','70','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1210,0,'Caprinid patch reef about 1.5 m thick.\nFramework of caprinids with Bacinella and Lithocodium.',46,12,3579755,1303931,'Italy','Europe',344,'',46.0167,12.4167,'WAHR','67614',24.8166335917,28.3346332847,23.4914343221,29.053074067,25.5270319199,23.3471098109,29.5134,21.536,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cebu City, Cebu',2003,'','Cretaceous','Lower Cretaceous','Barremian','Barremian-Aptian',113.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',125,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1211,0,'Rudist limestones with Amphitriscoelus.',10,123,1226481,15786090,'Philippines','Asia',563,'',10.4,123.8917,'WAHR','74165',10.4,123.8917,NULL,NULL,-26.3545615596,138.674691453,3.62962,144.679,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bespelj, Bosnia',2004,'','Cretaceous','Upper Cretaceous','Santonian','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','5','Rudists','4','Stromatoporoids','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,'40','50','10',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1212,0,'Reworked rudist reef (5 rudist species and 1 hydrozoa).\n',44,17,3491016,1745490,'Bosnia and Herzegovina','Europe',328,'',44.4167,17.2833,'','',32.9411505327,19.284226993,32.9411505327,19.284226993,31.5074794275,20.3596514279,28.3859,17.4567,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kudirkos-Naumestis',2005,'','Permian','Lopingian','Changhsingian','Zechstein',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',259,2,'1','Seismic data available ',3,'Mud mound or bank',NULL,NULL,'70',NULL,NULL,NULL,NULL,NULL,NULL,'50','306',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite',NULL,NULL,'1','Present',2,'Actual reservoir',1208,0,'60-70 m thick reefs, distinctly asymmetric. \nOnly core samples available.\nCyanobacteria and Fenestella, Acanthocladia (bryozoans).\n',54,22,3005446,3074329,'Lithuania','Europe',301,'',54.7667,22.8833,'','',32.6256481471,37.20503011,32.6290778508,37.205720138,30.6887332934,30.4757334339,22.4461,28.1721,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S-Bakony',2006,'','Cretaceous','Lower Cretaceous','Albian','upper Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,100,'Early Cretaceous (late Albian, 102.6 Ma)',101,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','25',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1213,0,'Biostromes, bioherms and small patch reefs.\nSeperate structures reach up to 20-25 m thickness. \nRudists rarely in growth position.',47,17,3477266,1929367,'Hungary','Europe',336,'',47,17.75,'','',34.208239335,25.4732734516,34.208239335,25.4732734516,31.1552759037,21.5864430258,27.6119,20.9773,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ereño',2007,'','Cretaceous','Lower Cretaceous','Aptian','Aptian',113.00,125.00,23,'late Valanginian - early Aptian',126,120,'Early Cretaceous (early Aptian, 121.8 Ma)',115,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1215,0,'Only thickets and patches in area.\nMaximum thickness of reefal limestone 1.7 m.\n',43,-2,3879600,243787,'Spain','Europe',304,'',43.3667,-2.65,'','',29.2529353597,12.3380047967,29.2529353597,12.3380047967,33.3208994778,8.01547432252,33.0292,9.61554,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Akerbouss',2008,'','Cretaceous','Upper Cretaceous','Cenomanian','upper Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',95,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','21',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','5','Rudists','4','Stromatoporoids','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,'40','50','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1216,0,'21 m of reefal limestones with rudists, stromatopores, dasycladales and bryozoans.',31,-4,2477689,-416273,'Morocco','Africa',714,'',31.8,-4.2167,'WAHR','67619',23.0440625819,-0.504202400426,23.0440625819,-0.504202400426,21.5735003876,-4.03229417661,18.7591,-4.02137,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Epidauros',2009,'','Cretaceous','Upper Cretaceous','Cenomanian','upper Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',95,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1217,0,'Radiolitid banks overlain by caprinid banks.\nMostly floatstone texturs.',37,23,2462297,2093944,'Greece','Europe',338,'',37.6167,23.15,'WAHR','74198',23.2959145603,20.844429703,23.2959145603,20.844429703,20.1467629662,20.6627077939,18.3547,19.0173,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Parandaz Mt.',2010,'','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',93,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1218,0,'Rudist limestones with Biradiolites and Eoradiolites.',34,68,2145101,7744570,'Afghanistan','Asia',301,'',34.9167,68.9167,'WAHR','74217',37.7660492383,73.6844365237,37.7660492383,73.6844365237,33.8503772511,69.031827029,17.094,70.7517,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Abu Roash, Cairo',2011,'','Cretaceous','Upper Cretaceous','Coniacian','early Coniacian',86.30,89.80,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',88,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','10',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','5','Rudists','1','Corals','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'45','55','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1218,1349,'Rudist dominated biostrome on top of Actaeonella series. Almost 10 m thick.\nRadiolitid Durania arnaudi is dominant. Abundant Ceriopora multiformis are also present.\nAge revised by ref. 1349.\nVery close is milleporid mound of small size.\n\n',30,31,1271395,2856821,'Egypt','Africa',715,'',30.0125,31.075,'WAHR','24082',16.0421672053,29.6831714384,16.0421672053,29.6831714384,14.001465414,26.0150222604,11.7969,26.2372,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kiya River Section, Siberia',2012,'Ust\'kundat-Usa','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',519,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','16',NULL,NULL,NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','134','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1222,1220,'Extremely diverse archaeocyaths.\nDiverse and well preserved calcibionts (Renalcis, Epiphyton, Chabakovia and others).\nBioherms mentioned throughout the section, but not described in detail.\nShould be another plate, but was not rotated.',55,88,-3175833,2053034,'Russia','Asia',624,'1221',55.5167,88.0167,'WAHR','56741',-2.62217101696,-46.4680262626,-2.62217101696,-46.4680262626,-2.62217101696,-46.4680262626,-11.4002,6.06114,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Abitibi R., Hudson Bay Lowl., Ontario',2013,'Kwatraboahegan','Devonian','Lower Devonian','Emsian','Emsian-Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,395,'Early Devonian (late Emsian, 395 Ma)',397,2,'0','Outcropping reef ',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','','Unknown','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species','37','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1227,1228,'Upper Emsian-early Eifelian\n\'Reefoid\' rocks.\n12 species of stromatopores.\n8 solitary and 9 colonial species of rugose corals\n8 species of tabulate corals.',51,-81,-4074932,-2590802,'Canada','North America',121,'1224',51,-81,'WAHR','40039',-23.4809727445,-51.0205259049,-23.4809727445,-51.0205259049,-14.9848786038,-105.160503621,-32.6211,-24.7284,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mormon Gap, Utah',2014,'','Carboniferous','Pennsylvanian','Moscovian','Desmoinesian',307.00,315.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',307,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'4','More than 1000 m',NULL,'25',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','12','Foraminifera','38','Palaeoaplysina - corals - tubular forams - bryozoans','2','Green algae','20','70','10',0,'no',0,'no','1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1230,0,'Oldest occurrence of Palaeoaplysina.\n2 m thick laterally continuous biostromes\nPalaeoaplysina plates encrusted by tubular forams. Some rugose corals, brachiopods, fenestrate bryozoans and Komia.\n',38,-113,1058625,-4597157,'United States','North America',101,'',38.7333,-113.9333,'WAHR','63144',3.08297469472,-41.9584363938,3.08297469472,-41.9584363938,5.80960476841,-63.2846932587,5.22748,-44.1883,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sudak, Crimea',2015,'','Jurassic','Middle Jurassic','Callovian','Callovian-Oxfordian',157.30,166.10,21,'late Bathonian - early Tithonian',151,165,'Middle Jurassic (Callovian, 164.8 Ma)',161,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','60',NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1231,1529,'Corals, solenoporaceans (including rodolites), calcareous sponges. Sometimes associated microbes.\nBioherms around 50-60 m thick.\n\nReef growth limited to upper Callovian - lower Oxfordian according to ref. 1529.\nAbstract of ref. 1529.\nRich and various crinoidal assemblages existed at Callovian-Oxfordian time in the Sudak environs on Crimea. 22 species are described: Dolichocrinus aberrans, Eugeniacrinitescaryophilites, E. quenstedti, Pilocrinus moussoni, Cyrtocrinus nutans (order Cyrtocrinida), Millericrinus annulatus, M. convexus, M. echinatus, M. etalloni, M. goupilianus, M. granulosus, M. knorri, M. milleri, M. multipunctatus, M. rotiformis, M. thiollieri (order Millericrinida), Balanocrinus dumortieri, B. subteres, Margocrinus modestus, Chariocrinus? burgundicus, Isocrinus amblyscalaris and \'Pentacrinus\' cingulatissimus (order Pentacrinida). The described species belong to two ecological  types: cirriferous (long-stalked plastic, long-stalked immovable and short-stalked forms) and cirriless (long-stalked and short-stalked). Crinoids occupied four trophic tiers and inhabited four types of the biotopes: interreef depressions, interreef rises, reef slopes and reefs. A certain connection exists between biotope types, trophic tiers of crinoids and their ecological types. Tubular worms, bryozoans, bivalves, sponges and corals were settling on crinoid stalks in a certain sequence during the lifetime of crinoids or after their perishing. Millericrinid stems were damaged by parasites, predators and scavengers. Pentacrinid stems were twisted, depending on the environmental dynamics. Atrophy of cirri is typical for tong-stalked flexible pentacrinids.',44,34,5058355,3237846,'Ukraine','Europe',301,'2814',44.8167,34.9167,'WAHR','67868',30.8649643549,46.4012153807,30.8649643549,46.4012153807,36.2803380782,49.0947960971,38.2128,40.9438,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shtschebetovka, Crimea',2016,'','Jurassic','Middle Jurassic','Callovian','Callovian-Oxfordian',157.30,166.10,21,'late Bathonian - early Tithonian',151,165,'Middle Jurassic (Callovian, 164.8 Ma)',161,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','200',NULL,NULL,NULL,'3','More than 100 m',NULL,'50','2015',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',1231,1529,'Reef growth limited to upper Callovian - lower Oxfordian according to ref. 1529.\nReef blocks of 1-2 km2 extension and 100-200 m thickness.\nLimestones cloddy, cavernous and recrystallized. Big coral and algal nodules. Cryptobionts like crinoids common. ',44,35,5081825,3253337,'Ukraine','Europe',301,'',44.9333,35.2333,'','',31.0689783327,46.5754105743,31.0689783327,46.5754105743,36.4731620819,49.2979384469,38.3671,41.1989,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fishta, N-Caucasus',2017,'','Jurassic','Upper Jurassic','Oxfordian','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',156,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'600',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1231,2207,'Algae, corals, calcareous sponges.\nFisht-Shakhdag barrier reef starting here and extending to the ESE (ref. 2207).\n',43,39,5117719,3665487,'Russia','Asia',624,'2814',43.9833,39.9,'WAHR','90019',31.8736298014,50.241934941,31.8736298014,50.241934941,36.8937249046,53.3366014957,38.0354,45.5314,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chegem, Caucasus',2018,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1231,0,'More than 1000 m thick algal-coral-sponge reef.',43,43,5131034,3961559,'Russia','Asia',624,'',43.2,43.1167,'','',32.2712762523,53.1041998318,32.2712762523,53.1041998318,37.0738028885,56.4052078588,37.6858,48.6129,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ardon River, Caucasus',2019,'','Jurassic','Upper Jurassic','Oxfordian','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',156,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100','2018',0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1231,2814,'See reef 2018.',42,44,5119495,4031287,'Russia','Asia',624,'',42.9167,44.1667,'WAHR','89999',32.3861127823,54.0624557153,32.3861127823,54.0624557153,37.1130112755,57.4293167306,37.5487,49.6307,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fawn Lake, Horn Plateau, N.W.T.',2020,'Horn Plateau','Devonian','Middle Devonian','Givetian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',390,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','120','3','101-1000 m wide','600','3','More than 100 m','650',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','20','1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',1233,1600,'Pinnacle reef complex.\nensensis to varcus Zone\n650 m wide - 125 m thick.\nColonial corals (rugose and tabulate) and massive and tubular stromatoporoids surrounded by sand gravel sized crinoid coral sediment. Much of the reef is composed of fragmented reef-derived debris\nSeveral algae and some microbes. Rare bryozoans.\nNot more than 10 % micrite in reef core.\n15 species or rugose corals in framework indicated by ref. 1600. Rugosa as primary frame builders.\n\nAbstract of ref. 1603:\nAgastophyllum eximium gen. et sp. nov., a massive digonphyllid coral, is described from the reef flat and organic reef macrofacies of Vopni and Lerbekmo (1972). Dialeptophyllum vopnii gen. et sp. nov., a solitary kyphophyllid coral, is described from the reef flank macrofacies. Thryptophyllum undafundus gen. et sp. nov. is described from the reef flat and reef flank macrofacies, and is referred to a new subfamily of the named Thrptophyllinae. Agastophyllum eximium and Thryptophyllum undafundus are Giventian, Middle varcus zone age; Dialeptophyllum vopnii is presumed to belong to the same zone, and is certainly Givetian. Four undescribed species of Agastophyllum are reported from late Eifelian strata of Western Canada. Dialeptophyllum vopnii and an unnamed Emsian species from the Nelichen Formation of the Indigirka River drainage area of the northeastern Soviet Union are the only known species of Dialeptophyllum. An early Givetian species from the Rockport Quarry Limestone of Michigan, originally described by Ehlers and Stumm (1949), under the name Spongophyllum romingeri, is transferred to the new genus Thryptophyllum. ',62,-117,-399176,-4080747,'Canada','North America',121,'1603',62.1667,-117.8333,'WAHR','34871',-3.11054630325,-57.9437497619,-3.11054630325,-57.9437497619,2.30354065345,-117.196160051,-8.21647,-36.5264,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mercy Bay, Banks Island, N.W.T.',2021,'','Devonian','Upper Devonian','Frasnian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',379,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','30',NULL,NULL,NULL,'3','More than 100 m',NULL,'100','1456',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1234,898,'Zonation: Lower bioherm (33 m thick) overlain by two biostrome layers (30 m thick).\n\nBioherm (from base to top): \n- 5 m Coral bindstone and bafflestone.\n-2 m stromatoporoid bindstone\n- 10 m Stromatoporoid framestone and rudstone\nStromatopores dominant in shallower water.',74,-118,641945,-3057644,'Canada','North America',121,'',74.0667,-118.3333,'','',4.42399832317,-42.3505964422,4.42399832317,-42.3505964422,14.393049829,-104.791155399,2.09329,-27.4603,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Palisades Quarry, Linn Co., Iowa',2022,'','Silurian',NULL,NULL,'Niagaran',433.40,435.00,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','30','3','101-1000 m wide',NULL,'4','More than 1000 m','2500',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','13','Echinoderms','1','Corals','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',1235,0,'Crinoid-coelenterate mounds.\nHeavily dolomitized, asymmetrical.\n30 m thick, 2.5 km wide complexes consisting of several mounds.\n',42,-91,-2920570,-5623342,'United States','North America',101,'',42.0333,-91.7333,'','',-27.0031026134,-102.963011106,-27.2431435607,-99.7674791906,-27.2431435607,-99.7674791906,-20.0129,-55.893,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('PDB-04 research well, New Mexico',2023,'','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',262,3,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','180',NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','86',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','2','Algae','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1','Red algae','10','70','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1236,0,'Reef dolomitic. Abundant marine cements\nCapitan formation with lower slope facies and upper reef facies (about 180 m thick ).Reef growth interrupted by sandstone bed.\nBiota: Sponges, bryozoans, algae (Archaeolithoporella, algal encrustations, rare stromatolites), Tubiphytes. \nAvarage porosity about 10 % (mostly vuggy). Maximum 25 %, 2 d permeability.\n',32,-103,503697,-3648017,'United States','North America',101,'',32.5042,-103.9194,'','',11.1206067157,-29.305295593,11.1206067157,-29.305295593,5.5700695077,-36.2539393707,4.5225,-32.2836,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Getty #1 well, Delaware Basin, New Mexico',2024,'','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',262,3,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','86',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1236,0,'',32,-103,464464,-3603147,'United States','North America',101,'',32.4333,-103.3333,'','',10.8387755006,-28.8851590828,10.8387755006,-28.8851590828,5.29077548471,-35.8379040939,4.22256,-31.883,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Delaware Basin margin E, Texas',2025,'','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',262,2,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'500','86',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1237,1236,'',31,-102,283038,-3626198,'United States','North America',101,'',31.1667,-102.8333,'','',9.51384571996,-29.0593677281,9.51384571996,-29.0593677281,3.96478535559,-36.0015024356,2.90653,-32.1134,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Sagara district',2026,'Megami','Neogene','Miocene','Middle Miocene','early Middle Miocene',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',15,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1238,0,'Abstract of ref. 1238:\r\nEight fossil molluscan species, including Cryptopecten yanagawaensis (Nomura and Zinbo) and Turbo    (Marmarostoma) mekamiensis Nishiwada, are described on the basis of material obtained from the late Early to early Middle Miocene Megami and Ebie limestones in the Sagara district, Shizuoka Prefecture, Japan. Cryptopecten yanagawaensis has been recorded from late Early to early Middle Miocene formations in Japan. The occurrence of this species indicates that the reef limestones in the Megami Formation were formed within the Japanese faunal realm in Miocene time. In this paper some comments are made on the origin and sedimentary environments of the limestones in the Megami Formation. ',34,138,4974482,13078349,'Japan','Asia',625,'',34.6667,138.1667,'WAHR','70064',36.4660476652,136.628401789,36.4666139144,136.627684326,34.418211083,136.218610343,37.5511,135.981,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('San Juan de la Costa, Baja California',2027,'San Gregorio','Paleogene','Oligocene','Chattian','Late Oligocene',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',27,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,'60',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','8','Serpulids, worms, vermetids','8','Serpulids, worms, vermetids','76','Worms only',NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species','1','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1239,0,'Small hemispherical reef structures, up to 2.5 m in width and 1 m in height.\nFormed by Diplochaetetes (worm, not sclerosponges as previously assumed).\nCoastal environment.',24,-110,3316581,-10996663,'Mexico','North America',105,'',24.3333,-110.6667,'WAHR','34858',22.238000294,-101.64584477,22.2382109589,-101.649213168,26.3990008118,-99.9430113984,23.1607,-102.428,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baixo, Porto Santo, E-Atlantic',2028,'','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1241,0,'Abstract of ref. 1241\nAn ephemeral coral reef developed on the submarine slope of the Porto Santo volcanic complex in Upper Miocene time. Systematic and biogeographical aspects of the fossil Scleractinia at this locality are discussed. ',33,-16,4418075,-1688352,'Atlantic','Atlantic',NULL,'',33.05,-16.3333,'WAHR','70666',31.9876989155,-17.2716825253,31.9876989155,-17.2716825253,33.05,-16.3333,33.0518,-16.6607,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Havelock Island, Andaman Islands',2029,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150',NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','12','Foraminifera','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'10','60','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',1242,0,'Abstract of ref. 1242:\nCarbonate rocks are widespread on the Andaman-Nicobar Islands, northern Indian ocean, ranging in age from Early  Miocene to Pleistocene. Lithologically they range from deep water to shallow water calcarenites. Thin section analysis of the limestones showed the following major lithofacies: lithic foraminiferal-algal grainstone-packstone; lithic foraminiferal-algal wackstone-mudstone; volcanoclastic packstone-wackstone/radiolarian cherts; foraminiferal packstone; coralgal boundstone and coarse lithic foraminiferal-algal-molluscan packstone-grainstone. They exhibit sequential changes in their fabrics, biogenic and clastic constituents. Depths of deposition ranged from high energy, shallow neritic (lithic foraminiferal-algal grainstone-packstone facies) at the beginning of Early Miocene to progressively lower bathyal marked successfully by lithic foraminiferal-algal wackstone-mudstone, volcanoclastic packstone-wackstone and radiolarian chert facies. The sudden influx of glass shards and tephras in the later Early Miocene suggests that progressive deepening of the basin occurred contemporaneously with explosive volcanism in    neighboring areas. During this interval of basinal subsidence, the limestones received abundant argillaceous material from subaerial erosion of nearby volcanic terrain. Gradual reduction in the frequency of glass shards and pumice from Middle Miocene (Ongeian Stage) onwards indicates culmination of volcanic eruptions and basinal stability. Gradual shallowing to subtidal and patch reef (coralgal facies) environments began to form from the Middle Miocene onwards at Little Andaman, Havelock, Nicholson and other islands. Deep basinal conditions prevailed during the Late Miocene to Early Pliocene at Neill, Sir Hugh Rose and Car Nicobar Islands. These different conditions may be attributed to    tectonism in the Andaman sea region which occurred during the close of Middle Miocene. Thereafter, younger   limestone facies of Plio-Pleistocene age, reflect a shoaling upwards to probable intertidal conditions due to rapid infilling and vertical uplift of the basin floor. No hydrocarbons were observed in the limestone sequences. The regional stratigraphic and petrographic studies reveal the presence of potential reservoir rocks in the Ongeian-Havelockian limestones of Middle Miocene age on the Andaman-Nicobar Islands. ',12,93,843953,10587890,'India','Asia',501,'',12,93,'','',11.0412070701,91.7213123936,11.0412070701,91.7213123936,8.83899174412,92.2406633175,10.5751,94.0086,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hendrick Field, Winkler Co., Texas',2030,'','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',262,3,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'500','86',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',2,'Actual reservoir',1237,0,'Producing reservoir in back reef facies.',31,-103,367679,-3617544,'United States','North America',101,'',31.75,-103.0833,'',NULL,10.1317677074,-28.9960848585,10.1317677074,-28.9960848585,4.58308454804,-35.9428427456,3.52107,-32.0236,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Havelock Island, Andaman Islands',2031,'','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150','2031',0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1242,0,'see reef 2029.',12,93,1206203,10370470,'India','Asia',501,'',12,93,'','',11.6020463224,92.4357439013,11.6020463224,92.4357439013,10.1277583437,92.7166364959,11.0738,93.247,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Little Andama Island, Andaman Islands',2032,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150','2029',0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',1242,0,'see reef 2029.',10,92,659180,10573419,'India','Asia',501,'',10.75,92.4167,'','',9.77560485712,91.175911579,9.77560485712,91.175911579,7.57823297736,91.6872809611,9.28798,93.5187,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Little Andama Island, Andaman Islands',2033,'','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150',NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1242,0,'see reef 2029.',10,92,1027399,10344378,'India','Asia',501,'',10.75,92.4167,'','',10.3336237542,91.8961653537,10.3336237542,91.8961653537,8.86185270763,92.1734860722,9.80265,92.7151,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Small Nggela Island',2034,'','Neogene','Pliocene','Pliocene','lower Pliocene',3.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1243,0,'Abstract of ref. 1243:\nMost of the sedimentary rocks of Small Nggela are early Miocene in age (dated by nannofossils and foraminifera). In the north, uniform volcaniclastic arenite (the Siota Beds) crops out. Much of the central, western and eastern parts of the island contain diverse strata including pillow lava, calcarenite, volcaniclastic arenite, grit and breccia (the Ghumba Beds). The Siota and Ghumba Beds, which are separated by a 1-1.5 km wide, east-trending ophiolite wedge, are considered to have been deposited in a forearc basin. The ophiolite wedge arrested the northward transport of coarse sediment and was emergent during the late Oligocene and early Miocene. The sediment and the ophiolite wedge are considered to have overlain a southward-descending Benioff zone. Well-bedded laminated arenite lacking basalt and rudite (the Ndandala Sandstone) is present in the south-western part of the island and is probably significantly younger than the underlying Ghumba Beds. A veneer of early-mid Pliocene limsteone (the Florida Limestone), representing a patch reef environment, was deposited upon the Ghumba Beds after they were folded. ',-9,160,-1544902,18027935,'Solomon Islands','Oceania',NULL,'',-9.1333,160.3333,'','',-10.0187616236,163.383257053,-10.0156415348,163.373046954,-10.4247066576,163.520954596,-13.4759,160.696,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Silifke',2035,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1246,0,'Abstract of ref. 1246 (part):\nThe Miocene sediments overlying the basement rock units are transgressive and grade into each other vertically and laterally. They are represented by polygenic conglomerates, sandstones, marls and reef limestones. Five planktonic foraminiferal biozones, 3 Burdigalian and 2 Helvetian to Tortonian (?), were defined in these formations. ',36,33,4699718,3189712,'Turkey','Asia',522,'',36.3333,33.9167,'','',35.9732560273,31.2865348641,35.9732560273,31.2865348641,34.9798738042,33.1385496923,35.8998,33.6458,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Miaru, Papua New Guinea',2036,'Era','Neogene','Pliocene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3',NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','104','2','Baffler guild','1','Present','1','Present','2','Medium zonation',NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1247,0,'50 m thick fossiliferous beds in Era Beds.\nSeveral 2-3 m thick coral horizons, corals often in growth position.\nPulses of clastic sedimentation throughout the reefal interval. ',-8,146,-1659864,15873195,'Papua New Guinea','Oceania',615,'',-8.35,146.2833,'WAHR','42736',-10.2477547152,145.365822707,-10.2453522223,145.366976044,-10.9697471161,145.578803063,-11.1004,145.515,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Golden Spike, Alberta',2037,'Leduc','Devonian','Upper Devonian','Frasnian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',379,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick','197',NULL,NULL,NULL,'4','More than 1000 m',NULL,'3',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','3','Microbes','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'10','0','90',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1250,1283,'197 m thick atoll reef (on platform).\nExcellent reservoir. 10 % avg. porosity, 100 md permeability.\nMassive and tabular stromatoporoids, few tabulate corals, encrusting algae.\nExtensive submarine cementation in the fore-reef, less in the reef.',53,-113,-1391666,-4628467,'Canada','North America',121,'1396, 1507',53.45,-113.8667,'','',-9.16840168446,-58.0096450299,-9.16840168446,-58.0096450299,-2.58461730076,-116.737843971,-12.7423,-41.9971,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Uniontown, Bourbon Co., Kansas',2038,'Hertha','Carboniferous','Pennsylvanian','Kasimovian','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','7',NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','2','Algae','1','Corals','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','20','80','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1257,1719,'Oldest phylloid algal mound complexes\nUp to 7 m thick. \nSome lithostrotionellid and syringoporid corals present but not framework-building.\nphylloid wackestone to mudstone\nAuthochthonous Neosyringopora framsestone\nPhylloid thalli framestone.',37,-94,-427598,-3065999,'United States','North America',101,'',37.85,-94.9833,'','',-3.0528732791,-27.635378746,-3.0528732791,-27.635378746,-4.53413367503,-50.7588617331,-3.57581,-27.846,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S-Neosho Co., Kansas',2039,'Swope-Dennis','Carboniferous','Pennsylvanian','Kasimovian','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m',NULL,'80',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','2','Algae','2','Algae','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1257,0,'Sparry algal calcilutite.\nUp to 20 m thcik.\nBethyan Falls Limestone Member of Swope Fm. and\nWinterset Limestone Member of Dennis Formation.',37,-95,-445463,-3105784,'United States','North America',101,'',37.55,-95.2833,'','',-3.18909807233,-27.9933808276,-3.18909807233,-27.9933808276,-4.64990970116,-51.1246434412,-3.70003,-28.2086,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wyandotte Co., Kansas',2040,'Wyandotte','Carboniferous','Pennsylvanian','Kasimovian','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','17',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','2','Algae','2','Algae','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',1257,0,'Argentine Limestone Member.\nEastern complex up to 17 m thick. Algal to sparry algal calcilutite.',38,-94,-341049,-2986427,'United States','North America',101,'',38.7667,-94.6167,'','',-2.40970251707,-26.9208288638,-2.40970251707,-26.9208288638,-3.93218253506,-50.0079838671,-2.95673,-27.1101,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Padaukpin, Maymyo, Myanmar',2041,'Padaukpin','Devonian','Middle Devonian','Eifelian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',394,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','9','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',2317,0,'Ref. 2317 cites older papers describing 23 rugose and 21 tabulate coral species. Only eight taxa described in ref. 2317.\nBiostrome mentioned \nrugose and tabulate corals, brachiopods, sponges, bryozoans and microfossils reported',22,96,-2048709,13986041,'Burma','Asia',603,'',22.0833,96.5833,'WAHR','62942',-19.228293496,99.2440713878,-19.228293496,99.2440713878,-47.0305015636,133.810574018,-10.0028,131.751,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yunggrangan, Yogyakarta, Java',2042,'Progo Beds','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',18,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','19','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1258,0,'Locality described as Djunggrangan, NW Jogjakarta.\nBurdigalian age suggested by van Bemmelen (1949).\n36 coral species described from Formation but only 18 described in ref. 1258. ',-7,110,-1055426,12351960,'Indonesia','Asia',614,'',-7.6667,110.0833,'WAHR','34721',-5.21570546636,107.763549043,-6.02910822239,107.568663866,-9.02493450313,109.666744838,-7.65192,113.917,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Geger Tjabé, Pankah, Java',2043,'','Neogene','Pliocene','Pliocene','lower Pliocene',3.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','51',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1258,2414,'Small coral reef with 15 species according to ref. 1258\nUmbrove (1946) cited 51 species in another(?) reef',-7,109,-974557,12114077,'Indonesia','Asia',614,'',-7,109.25,'WAHR','34722',-6.47234645797,108.834910023,-6.47412512026,108.836316156,-7.2943819398,108.927327619,-7.18255,109.867,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('San Andrés Island, Columbia',2044,'San Andres','Neogene','Miocene','Lower Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',1259,2594,'Abstract of ref. 1259:\nSan Andres is a small coralline island 136 km east of the Caribbean coast of Nicaragua. Surface mapping and paleontologic data indicate reefs have been growing actively in the area at least since early Miocene time. Because of the offlap relations of the ancient reef complexes, accessibility of progressively younger rocks is simplified.\n\nField and laboratory examination of both modern and ancient reef complexes indicates five major bottom facies: (1) forereef flank, (2) reef, (3) backreef platform, (4) backreef lagoon with patch reefs, and (5) shore area. Principal builders of the reefs were Millepora and lime-secreting algae with abundant Acropora, Diploria, Montastrea, and Porites.\n\nFrom X-ray and petrographic studies of the limestones, a sequence of carbonate diagenesis has been determined for the San Andres area. During early stages of diagenesis, sediments initially are cemented by grain welding and aragonite precipitation between grains. This early type of cementation is most common in the supertidal and intertidal zones. Subsequent calcite cementation occurs by dissolution-precipitation after aragonite. After calcite precipitation, no evidence can be found of the preexisting aragonite cement. Although inversion of aragonite to calcite commonly occurs in grain material, dissolution-precipitation seems to be the major process of cementation.\n\nDuring the diagenetic sequence, four responses may be expected: (1) magnesium is removed and high-magnesium calcite stabilizes to low-magnesium calcite, (2) aragonite can stabilize to calcite, (3) aragonite may be dissolved, and (4) sediments may become dolomitized. The time required for any of these reactions is variable and depends on the chemical environment. X-ray analyses indicate that all samples older than middle Pleistocene have stabilized to low-magnesium calcite or dolomite. The result of the diagenetic sequence is the development of a low-magnesium calcite limestone, a dolomite, or a combination of the two.\n\nPorosity in the San Andres area is primary, secondary, or occluded and development depends on exposure of carbonate material to a subaerial environment before mineral stabilization occurs.\n\n',12,-81,1763221,-8944414,'Colombia','South America',226,'',12.5333,-81.7,'WAHR','73792',11.2060601258,-81.0159453525,11.2060601258,-81.0159453525,14.1707154333,-80.4236075757,12.4271,-80.2452,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('San Andrés Island, Columbia',2045,'','Neogene','Miocene','Middle Miocene','lower-middle Miocene',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',16,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',1259,2594,'Principal reef builders:\nMillepora, lime-secreting algae and abundant Acropora, Diploria, Montastrea and Porites.',12,-81,1758317,-8932928,'Colombia','South America',226,'',12.5333,-81.7,'','',11.4959603512,-81.1605558632,11.4959603512,-81.1605558632,13.8807205391,-80.7386132139,12.5097,-80.4152,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('San Andrés Island, Columbia',2046,'','Neogene','Miocene','Upper Miocene','upper Miocene/Pliocene',2.60,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',5,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','95','5',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',1259,2594,'Seef reef 1258.',12,-81,1737284,-8936924,'Colombia','South America',226,'',12.5333,-81.7,'','',11.9994549361,-81.501146513,11.9994549361,-81.501146513,13.25340779,-81.3334992509,12.5749,-80.8922,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Trinil, Java',2047,'','Neogene','Pliocene','Pliocene','lower Pliocene',3.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','11',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','39','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1260,0,'Probably early Pliocene.\nReef limestone around 11 m thick.\nUp to 39 coral species from a single locality (5 localities mentioned by ref. 1260).',-7,111,-1018688,12341888,'Indonesia','Asia',614,'',-7.3667,111.35,'WAHR','71079',-6.83230948372,110.933731938,-6.83411113558,110.935141725,-7.68808079635,111.023806835,-7.50228,111.975,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Abukuma',2048,'Torinosu','Jurassic','Upper Jurassic','Tithonian','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',147,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','60','30',0,'no',0,'no','3','25 or more reef building species','39','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1261,0,'Northernmost extension of Torinosu-Limestone.\n28 scleractinian genera\n4 chaetetid genera\n7 stromatopore-hydrozoan genera\nafter Yabe & Sugiyama (1935).',37,140,7719497,10629119,'Japan','Asia',625,'',37.8333,140.75,'','',62.9801047236,161.223078456,62.9801047236,161.223078456,56.7797649441,162.725119124,44.8903,143.28,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Minami-jima',2049,'Ogasawara Group','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','9','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1261,0,'Small island opposite Minami-zaki (S-Chichi-jima).\nEulepidina used to assign Aquitanian age.\nCoral limestone by crowded coral stocks, mostly in upright position.\n8 genera mentioned in uncomplete list.',27,142,3202378,16511139,'Japan','Asia',625,'',27.0333,142.25,'WAHR','34874',20.3341382137,138.001433285,20.3341382137,138.001433285,21.5864926158,147.299903888,27.6145,143.806,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Oishi, Kawaguchi Lake',2050,'','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',18,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1261,0,'Northernmost limit of Tertiary reefal limestone in Japan.\nSeveral species of genera Favia, Favites, Hydnophyllia, Maeandra.\nMany coral stocks.',35,138,5082977,13036156,'Japan','Asia',625,'',35.5167,138.7333,'WAHR','34875',38.1828849238,136.434178184,37.6921157745,136.731808502,35.2587497817,136.295438757,39.2303,136.316,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kikai-shima, Ryukyu Islands',2051,'Riukiu Limestone','Neogene','Pliocene','Pliocene','late Pliocene',2.60,3.60,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',3,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','80',NULL,NULL,NULL,NULL,NULL,NULL,'1100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','21','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1261,0,'19 coral species listed by ref. 1261.\nRiukiu limestone less than 80 m thick, extending from S Taiwan to Kikai-shima.\nReef limestone in some places only.',28,130,3884819,13221128,'Japan','Asia',625,'',28.3333,130,'WAHR','34877',28.7253327052,129.524952251,28.7266158237,129.52340663,28.2350091509,129.471422304,28.5946,129.63,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shuri, Okinawa',2052,'','Neogene','Pliocene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1100','2051',0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1261,0,'Coralline limestone with massive coral stocks.\nMostly Porites.',26,127,3600201,13155029,'Japan','Asia',625,'',26.2167,127.7167,'','',26.825741256,126.977691059,26.8249590019,126.978627706,26.1856749867,126.940485365,26.4991,127.298,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monte Grappa, Trento',2053,'','Jurassic','Lower Jurassic','Pliensbachian','upper Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,185,'Early Jurassic (Pliensbachian, 186.8 Ma)',184,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','10','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','1','Corals','22','Stromatoporoids/sponges - corals - (algae)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1262,476,'Sponge-coral-stromatoporoid patch reefs with intercalated grainstones.\nComplex up to 15 m and 10a of m wide.\nStylothalamia cf. budaensis\nsolitary and colonial corals\nstromatoporoids\nSolenopora\n',45,11,4303132,1731743,'Italy','Europe',344,'',45.85,11.8,'','',20.6357649624,27.6813090444,20.6357649624,27.6813090444,26.272767168,30.2033566397,32.2327,20.4925,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vealmoor, Horseshoe Atoll, Texas',2054,'','Carboniferous','Pennsylvanian','Kasimovian','Missourian-Virgillian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',303,2,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','310',0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'2','Algae','2','Algae',NULL,NULL,'1','Red algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1263,0,'',32,-101,-623325,-3891053,'United States','North America',101,'',32.5167,-101.5833,'','',-4.60452936552,-35.0732463578,-4.60452936552,-35.0732463578,-5.65212404268,-58.2873630491,-4.87531,-35.3359,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kelly Snyder, Horshoe Atoll, Texas',2055,'Cisco','Carboniferous','Pennsylvanian','Kasimovian','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','310',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1263,1399,'Isolated reef mound complex (platform margin).\nSponges-algae-bryozoans\nand phylloid algal boundstones (wackestones)\n 8 % avg. porosity.\n50 m thick.\nSponges were 2nd but unlikely',32,-100,-640081,-3827288,'United States','North America',101,'',32.75,-100.95,'','',-4.71732479037,-34.5002634839,-4.71732479037,-34.5002634839,-5.7986528161,-57.7211614348,-5.00761,-34.7669,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Salt Creek, Horshoe Atoll, Texas',2056,'','Carboniferous','Pennsylvanian','Kasimovian','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,3,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','310',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'2','Algae','2','Algae',NULL,NULL,'2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1263,0,'',33,-100,-590233,-3786173,'United States','North America',101,'',33.2667,-100.8333,'','',-4.34730879228,-34.1254006334,-4.34730879228,-34.1254006334,-5.45142791558,-57.3242929233,-4.6506,-34.3794,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Block 372, Baltimore Canyon Trough',2057,'','Cretaceous','Lower Cretaceous','Aptian','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,120,'Early Cretaceous (early Aptian, 121.8 Ma)',123,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','4','Stromatoporoids','6','Calcisponges','22','Stromatoporoids/sponges - corals - (algae)',NULL,NULL,'10','60','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1264,0,'Stromatoporoid-sponge-coral boundstones and grainstones (subsurface) just before platform drowning.',38,-72,2667871,-3159680,'Atlantic','Atlantic',NULL,'',38.6167,-72.8667,'','',28.372192513,-21.6895254468,27.1719989962,-20.5487941856,30.5714251684,-26.3773893157,32.6127,-25.3403,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Liuhua, Pearl River Mouth, South Ch',2058,'Zhujiang','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',21,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick','476',NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','1','Corals','22','Stromatoporoids/sponges - corals - (algae)','1','Red algae','0','40','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1264,1389,'Carbonate bank.\n476 m thick. \nPlatform margin reef.\n24 % porosity.',20,115,3536042,12030289,'China','Asia',602,'',20.8,115.6833,'','',23.115151495,113.020272089,23.115151495,113.020272089,19.93219015,113.622477117,21.6545,115.447,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Liuhua, Pearl River Mouth, South China Sea',2059,'','Neogene','Miocene','Lower Miocene','lower Burdigalian',17.50,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',19,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'25',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','4','Stromatoporoids','22','Stromatoporoids/sponges - corals - (algae)','1','Red algae','0','20','80',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1264,0,'',20,115,2795607,12269469,'China','Asia',602,'',20.85,115.6333,'','',23.2644610709,112.939693009,22.900312564,113.189497654,20.0057469054,113.698605322,21.433,115.29,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Emperor Seamount, Pacific',2060,'','Neogene','Miocene','Lower Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,2,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1265,0,'Abstract of ref. 1265:\nThis paper is a review of the present knowledge of coral reef ecology and paleoecology in the Hawaiian-Emperor\nChain during the last 70 Ma. Research on fossil coral deposits throughout the H-E Chain has played a major role in producing information concerning the subsidence, uplift and drowning of individual islands, as well as the  paleocirculation of the North Pacific Ocean during Tertiary time. The origin of the Hawaiian Islands and seamounts    over the Hawaiian hotspot and their subsequent subsidence and transport by plate motion to the north and northwest are reviewed and new data concerning uplift of the central high Hawaiian Islands caused by lithospheric flexure and the effect of sea level change on the geological evolution of individual islands are presented. The Darwin Point, where atolls drown to form guyots, is redefined in dynamic terms as a function of climate and sea level history. The absence of coral reefs during the first half of Hawaiian history is evidence ...',42,170,4991923,-16958529,'Pacific','Pacific',NULL,'',42,170,'','',38.3611171417,-174.056793984,38.3611171417,-174.056793984,42,170,36.4277,-175.649,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Emperor Seamount, Pacific',2061,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1265,0,'See reef 2060',42,170,5077103,17218912,'Pacific','Pacific',NULL,'',42,170,'','',38.9986028129,-178.340060631,38.9980799248,-178.336281293,42,170,37.4382,-179.092,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baixo, Porto Santo, E-Atlantic',2062,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1266,0,'Abstract of ref. 1266:\nEphemeral coral reefs developed in the Miocene on the submarine slopes of the Porto Santo and Madeira volcanic complexes. The paleontology of these reefs is discussed. Danaia calcinata described from Baixo, near Porto Santo by Mayer (1864) as a tabulate coral is identified here as synonymous with Pocillopora madreporacea (Lamarck, 1816).\nCorals: Thamnasteria sp., Stylina aff. girodi Efallon and Stylina sp.',33,-16,4358253,-1765710,'Portugal','Europe',304,'',33.05,-16.3333,'','',31.3334188456,-17.777530212,31.3334188456,-17.777530212,33.05,-16.3333,32.9757,-16.9198,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vening Meinesz seamounts, Indian Ocean',2063,'','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',68,2,'1','Seismic data available ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,2,'Cold - water','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'5','Rudists','2','Algae','47','Bivalves (mostly oysters) - algae (microbes)','1','Red algae','50','20','30',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',1267,0,'Inoceramids and rudists dredged',-11,105,-4901609,8774042,'Indian Ocean','Indian Ocean',NULL,'',-11.3333,105,'','',-36.3453334224,93.1422201016,-36.3453334224,93.1422201016,-11.3333,105,-37.6177,90.7706,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gunung Anga, Borneo',2064,'','Paleogene','Oligocene','Rupelian','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',32,2,'1','Seismic data available ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'8',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1268,0,'See reef 3098',-1,115,429957,13320391,'Indonesia','Asia',614,'',-1,115.4333,'','',1.81417964579,112.956117301,1.81417964579,112.956117301,-3.5126393063,116.019960952,1.57216,121.003,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jaan River, Borneo',2065,'','Paleogene','Oligocene','Rupelian','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',32,2,'1','Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'60',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1268,0,'Sequence 2\nSmall patch reef in coral-rich wackestone-packstone sequence',0,114,425281,13217783,'Indonesia','Asia',614,'',-0.7833,114.5333,'','',2.17034176235,112.101251283,2.17034176235,112.101251283,-2.83205612281,115.39164416,1.61627,120.078,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jaan River, Borneo',2066,'','Paleogene','Oligocene','Chattian','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',27,2,'1','Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'60',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1268,0,'Sequence 2\n32 - 29.7 Ma',0,114,18767,13063473,'Indonesia','Asia',614,'',-0.7833,114.5333,'','',0.40692365472,111.84942862,0.40692365472,111.84942862,-4.1666766637,114.481780078,0.544982,119.356,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lemo River, Borneo',2067,'','Paleogene','Oligocene','Chattian','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',26,3,'1','Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'60','2066',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','12','Foraminifera','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','80','20',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1268,0,'Sequence 3.\nShelf margin coral boundstones and coral-rich\nlarge foram-coralline algae packstone-grainstone.\nMassive and thick branching corals.',-1,114,-13005,13094954,'Indonesia','Asia',614,'',-1.05,114.7833,'','',0.104568223971,112.054842625,0.104568223971,112.054842625,-4.5263369457,114.547216088,0.317921,119.643,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kangean Block E, Java Sea',2068,'','Neogene','Miocene','Middle Miocene','Langhian-Serravallian',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',15,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1269,0,'Asymmetrical atoll structure.\nReef growth along northern edge of carbonate platform.',-6,116,-875816,13064550,'Indonesia','Asia',614,'',-6.7833,116.4,'','',-5.35541508374,114.749308504,-5.35486220998,114.74605902,-8.74599036024,115.764205181,-6.46712,118.69,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kangean Block W, Java Sea',2069,'','Neogene','Miocene','Middle Miocene','Langhian-Serravallian',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'30','2068',0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1269,0,'See reef 2068.',-6,116,-884807,13038145,'Indonesia','Asia',614,'',-6.8333,116.1667,'','',-5.40585038464,114.516723202,-5.40529179015,114.513472679,-8.76843796292,115.525498553,-6.53409,118.461,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ernstbrunn',2070,'','Jurassic','Upper Jurassic','Tithonian','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',147,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','60','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1270,0,'',48,16,3953101,1763651,'Austria','Europe',301,'',48.5,16.3833,'','',30.877946358,27.9438492604,30.877946358,27.9438492604,35.820150118,30.2974860638,40.1084,23.5754,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ile Bizard, Montreal',2071,'Laval','Ordovician','Middle Ordovician','Darriwilian','Chazyan',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',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','','Unknown',NULL,NULL,'7','Bryozoans','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1272,0,'Bryozoans (Batostoma) form rigid self supporting framework.',45,-73,-2896141,-4930012,'Canada','North America',121,'',45.4833,-73.9167,'WAHR','80006',-8.15809460366,-100.078922678,-8.15809460366,-100.078922678,-8.15809460366,-100.078922678,-27.3349,-55.1465,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Little Cove, Antigua',2072,'Antigua','Paleogene','Oligocene','Chattian','early late Oligocene',26.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',27,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','21',NULL,NULL,NULL,'3','More than 100 m','105',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,'3','Pronounced zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1987,1273,'Patch reef in middle part of Antigua Fm.\nmore than 100 m wide and more than 20 max. thickness.',17,-61,2278996,-6683164,'Antigua and Barbuda','North America',NULL,'',17.0333,-61.6833,'WAHR','34504',15.1940773485,-61.3786658363,15.2469036157,-61.4252722275,18.6960012811,-60.4414382436,16.3617,-60.5236,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('St. Johns Cathedral, Antigua',2073,'Central Plain Group','Paleogene','Oligocene','Rupelian','middle Oligocene',26.00,32.00,29,'Priabonian - Rupelian',33,25,'Late Oligocene (Chattian, 25.6 Ma)',27,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','14','1','Constructor guild','1','Present',NULL,NULL,'3','Pronounced zonation','1','Low zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1273,1987,'2 m thick coralgal deposit.\nPlaty Porites panamensis and subordinate Goniopora in a skeletal matrix of broken coral, coralline, algae and large Lepidocyclina. \n\nOnly about 12 species of corals contribute significantly to reef construction.',17,-61,2209872,-6673436,'Antigua and Barbuda','North America',NULL,'',17.1167,-61.8333,'WAHR','34503',15.1029454513,-61.8412984861,15.092146923,-61.917200159,18.8782091659,-60.749686968,16.2922,-60.7589,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Makamby Island',2074,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1274,0,'',-15,45,-2304104,4758045,'Madagascar','Africa',702,'',-15.7,45.9,'','',-17.1918945359,44.3048452648,-17.1918945359,44.3048452648,-18.3057126016,44.1090338317,-16.3492,44.1738,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Last Chance Canyon, New Mexico',2075,'San Andres',' 	Permian','Guadalupian',NULL,'Guadalupian',259.80,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',265,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','25',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,'50','40','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1275,0,'Upper San Andres Fm.\nReef mounds with 25 m depositional relief.\nBryozoans, brachiopods, calcareous sponges.\nInferred water depth 30-50 m (lower slope).\nOther type is crinoid-bryozoan bafflestone bioherm.',32,-104,517939,-3724240,'United States','North America',101,'',32.2833,-104.7,'','',9.08559450261,-30.7371968645,9.08559450261,-30.7371968645,3.9756133852,-38.5546487665,5.51332,-32.3635,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Truk, Micronesia',2076,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,3,'0','Outcropping reef ',1,'True reef','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1277,0,'',7,151,544803,17851760,'Micronesia','Oceania',NULL,'',7.3333,151.75,'','',5.23251530106,161.824960726,5.23223625649,161.828302468,7.3333,151.75,3.46464,161.749,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Truk, Micronesia',2077,'','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'0','Outcropping reef ',1,'True reef','4','More than 500 m thick','1100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1277,0,'Reef growth from 12-14 Ma to recent (with interruptions).\nThickness of reef limestone about 1100 m.',7,151,732558,17281145,'Micronesia','Oceania',NULL,'',7.3333,151.75,'','',5.90282030249,157.97940972,5.87583796165,158.083365925,7.3333,151.75,4.48382,158.257,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ponape, Microne',2078,'','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'0','Outcropping reef ',1,'True reef','4','More than 500 m thick','600',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1277,0,'Reef growth from 8 Ma to recent (with interruptions).\nThickness of reef limestone 600-800 m.',6,158,646219,17999527,'Micronesia','Oceania',NULL,'',6.8333,158.1667,'','',5.17909927192,164.355397891,5.1485149431,164.458630552,6.8333,158.1667,3.77443,164.621,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mayotte, Indian Ocean',2079,'','Neogene',NULL,NULL,'Miocene/Pliocene',2.60,20.00,32,'Tortonian - Gelasian',6,15,'Middle Miocene (Langhian, 14.9 Ma)',5,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1277,0,'',-12,45,-1815453,4827673,'France','Europe',331,'',-12.8333,45.1667,'','',-13.9940137148,43.8262518453,-13.9940137148,43.8262518453,-12.8333,45.1667,-13.4084,43.6761,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bora-Bora, Polynesia, Pacific',2080,'','Neogene','Pliocene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1277,0,'',-16,-151,-2543059,-15860409,'Pacific','Pacific',NULL,'',-16.5,-151.7167,'','',-17.6935072607,-148.873682093,-17.6935072607,-148.873682093,-16.5,-151.7167,-18.1956,-148.642,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('N Purcell Mts., British Columbia',2081,'','Ediacaran','Ediacaran','Avalon Assemblage','Hadrynian',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',640,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','45',NULL,NULL,NULL,'3','More than 100 m',NULL,'30',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1278,0,'Stromatolitic dolomitic bioherms up to 45 m thick.\nOff-bank facies.\npre-Ediacaran',51,-117,-6248659,-9558977,'Canada','North America',121,'',51.4167,-117.4,'','',-39.3057692876,154.28465058,-39.3057692876,154.28465058,-39.3057692876,154.28465058,-46.6444,-104.823,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Perico Hills',2082,'Atocongo','Cretaceous','Lower Cretaceous','Hauterivian','Hauterivian-Barremian',125.00,132.90,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',130,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1279,0,'4.5 m thick silicified coral biostrome.\n\nAbstract of ref. 1279:\nDuring the Hauterivian-Barremian, local coral biostromes, possibly patch reefs, developed within shallow marine lagoons fringing Early Cretaceous volcanoes in Peru. The dominant coral is S. columbaris sp. nov. which is similar to European stylinid species of Late Jurassic and Early Cretaceous age having 6-fold septal plans. The biostrome is part of the Atocongo Formation, Lima Group, exposed at Perico Hill (Cerros Perico) about 95 km south of Lima. Only 2 other lower Cretaceous stylinid corals were described from South America. ',-12,-76,-3556536,-4526985,'Peru','South America',201,'',-12.5333,-76.5,'WAHR','50765',-19.2894887039,-39.0028115245,-19.2894887039,-39.0028115245,-15.0542037122,-43.6799448094,-12.8022,-43.5394,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Serranía de Cocinas, Guajira Peninsula, Columbia',2083,'Jipi','Jurassic','Upper Jurassic','Kimmeridgian','lower Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',154,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','100','3','101-1000 m wide','500','4','More than 1000 m','1000',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','10','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1280,2112,'Coral-limestone with low diversity anthozoan fauna.\nReefal limestones up to 100 m thick and 500 to 1000 m long interfingering with calcareous shales and sandstones.',11,-71,326238,-4582052,'Colombia','South America',226,'',11.8333,-71.6333,'WAHR','34736',4.11720591868,-38.8361009627,4.11720591868,-38.8361009627,9.45388431433,-40.2824313587,11.2415,-41.5989,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Norman Wells, N.W.T.',2084,'Ramparts-Kee Scarp','Devonian','Middle Devonian','Givetian','upper Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',385,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick','160','4','More than 1000 m wide','8000','4','More than 1000 m','25000',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1282,1283,'Average porosity 10 %, permeability around 110 md.\n4 growth stages in 160 m thick reef.\nDiversity not described but all groups (stromatoporoids, tabulate and rugose corals) with different species and growth forms.\n\nRanging into Frasnian\n\nAbstract of ref. 2126:\nThe Middle-Upper Devonian Kee Scarp reef complexes are oil-producing, stromatoporoid-dominated carbonates. Episodic increases in the rate of sea level rise produced multiple cycles of reef growth that exhibit backstepping characteristics. These carbonates have original interskeletal, intraskeletal, and intergranular porosity, mostly occluded by nonferroan, dull luminescent cements. Secondary porosity, represented by micropores of various types, developed during diagenesis by aggrading neomorphism and dissolution. The micropores represent the main reservoir porosity in the Kee Scarp limestone. Micropores in the Kee Scarp limestone can be classified into four categories based on their shapes.',65,-126,294504,-4053074,'Canada','North America',121,'1600, 2126',65.2833,-126.8722,'WAHR','84237',2.94748263624,-53.310768878,2.94748263624,-53.310768878,9.19929760991,-114.586227328,-1.32714,-36.316,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Redwater, Alberta',2085,'Leduc','Devonian','Upper Devonian','Frasnian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',379,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick','245',NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species','14','1','Constructor guild',NULL,NULL,'1','Present','3','Pronounced zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1283,917,'245 m thick bioherm (atoll structure).\nbest reservoir quality in organic facies of reef margin.\n\nMassive stromatoporoids, tabulate corals, rugose corals, Stachyodes, Amphipora, brachiopods, crinoids.\n\nReef: Massiv stromatoporoids\nReef flat: Skeletal rudstone\nInterior: Amphipora beds\n\n7 % avg. porosity.',53,-113,-1391038,-4558683,'Canada','North America',121,'1762, 1396',53.9167,-113.1667,'WAHR','657',-9.21564147614,-57.3791005615,-9.21564147614,-57.3791005615,-2.4692559531,-116.123761662,-12.7417,-41.3571,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Macrossan, Fly River, Papua New Guinea',2086,'','Paleogene','Eocene','Lutetian','Middle Eocene',38.00,47.80,28,'Lutetian - Bartonian',45,45,'early Middle Eocene (Lutetian, 44.5 Ma)',40,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'50',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1285,2277,'Compact coral limestone of Eocene, probably middle Eocene age.\r\nCream-coloured matrix.\r\nAge discounted by Wilson and Rosen (1998). Said the faunas are mostly Neogene or of mixed ages',-6,141,-3891485,13628927,'Papua New Guinea','Oceania',615,'',-6.0833,141.3833,'WAHR','70667',-26.7908630534,131.908944387,-26.7908630534,131.908944387,-30.9918458744,134.079782467,-29.0242,132.507,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Palmer River, Papua New Guinea',2087,'','Paleogene','Eocene','Lutetian','Middle Eocene',38.00,47.80,28,'Lutetian - Bartonian',45,45,'early Middle Eocene (Lutetian, 44.5 Ma)',40,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'50','2086',0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1285,0,'reef 2086 for remarks.',-5,141,-3841833,13692015,'Papua New Guinea','Oceania',615,'',-5.75,141.7167,'',NULL,-26.4235345705,132.237191247,-26.4235345705,132.237191247,-30.6188492286,134.41304904,-28.6497,132.831,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hestnesfjell, Prosanger Fjord',2088,'Porsanger Dolomite','Ediacaran','Ediacaran','Avalon Assemblage','Riphean',720.00,850.00,0,'Vendian',605,690,'Middle Neoproterozoic (late Cryogenian, 690 Ma)',700,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','16',NULL,NULL,NULL,'4','More than 1000 m',NULL,'25',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1286,1957,'Up to 16 m thick laterally extensive stromatolite biostrome.',70,25,-7392805,-2525860,'Norway','Europe',301,'',70.3167,25.4833,'','',-28.9834858836,-117.122803919,-28.9834858836,-117.122803919,-28.9834858836,-117.122803919,-33.9235,-115.188,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sarronvarre, Prosanger Fjord',2089,'Porsanger Dolomite','Ediacaran','Ediacaran','Avalon Assemblage','Riphean',720.00,850.00,0,'Vendian',605,690,'Middle Neoproterozoic (late Cryogenian, 690 Ma)',705,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15',NULL,NULL,NULL,'1','Less than 20 m',NULL,'25',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1286,1957,'pre-Varanger stromatolithic reefs on carbonate platform',70,24,-7388019,-2553325,'Norway','Europe',301,'',70.25,24.9667,'','',-28.8112104347,-117.20473371,-28.8112104347,-117.20473371,-28.8112104347,-117.20473371,-53.0065,-87.2327,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wörschach',2090,'','Paleogene','Paleocene','Danian','Danian',61.60,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',63,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'100','657',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1287,0,'',47,14,4852958,1366891,'Austria','Europe',301,'',47.5667,14.2,'','',40.5941496808,12.9773154784,40.5941496808,12.9773154784,42.5992194226,11.2912832485,36.6798,13.3506,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('JA90-23, Eucla Shelf, Great Austr',2091,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'475',NULL,1,'Temperate','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1288,0,'Abstract of ref. 1288:\nThe southern continental margin of Australia is the largest area of cool-water carbonate shelf deposition on the globe. Interpretation of 5495 km of airgun seismic-reflection data in the western part of the Great Australian Bight indicates that the 700-m-thick Cenozoic section of the offshore Eucla basin was deposited largely as a prograding cool-water, middle- to high-latitude carbonate ramp, characterized by widespread development of broad, low-relief, biogenic (bryozoan[?]-sponge), shelf and upper-slope mounds. The succession also contains a spectacular and extensive (>475 km long) buried middle Miocene barrier reef (the Miocene Little Barrier Reef) parallel to the modern shelf edge. This rimmed carbonate platform margin represents an episode of warm-water sedimentation during a global climatic optimum, probably coupled with strong eastward flow of a proto-Leeuwin Current. The late Miocene eustatic sea-level fall produced an areally restricted debris-apron sequence at the foot of the reef escarpment. The carbonate platform is capped by a Neogene cool-water carbonate ramp succession typified by aggradational to sigmoidal sequences, punctuated by periods of cold(?)-water, sea-floor erosion. Interpretation of this succession in the light of global and local tectonic and oceanographic events illustrates the dominant influence of water temperature on carbonate platform and reef growth throughout the Cenozoic.',-32,127,-5478038,11484312,'Australia','Oceania',801,'',-32.8333,127.5833,'','',-39.7758886437,123.958351411,-39.7758886437,123.958351411,-42.1422748319,125.052289145,-41.6208,123.72,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Eucla Shelf E, Great Austr',2092,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick','250',NULL,NULL,NULL,'4','More than 1000 m','6500','475','2091',2,'Cold - water','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1288,2020,'See reef 2091.',-33,129,-5498351,11613399,'Australia','Oceania',801,'',-33,129,'','',-39.93852538,125.508333539,-39.93852538,125.508333539,-42.2893117396,126.661571235,-41.8069,125.31,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Eucla Shelf W, Great Austr',2093,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'475','2091',1,'Temperate','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1288,0,'See reef 2091 for remarks.',-33,125,-5538268,11187489,'Australia','Oceania',801,'',-33.3333,125.25,'','',-40.2724808659,121.404173637,-40.2724808659,121.404173637,-42.660607574,122.41119229,-42.0755,121.081,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Western Schelf',2094,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,1,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',1289,1448,'Seismic exploration only.',-4,54,-747266,5795786,'Seychelles','Africa',NULL,'',-4.5,54.5,'','',-5.80525465035,52.6871049664,-5.80525465035,52.6871049664,-7.19995945834,52.9174444354,-5.22618,52.6242,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Southern Schelf',2095,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,1,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',1289,1448,'',-5,55,-810579,5933260,'Seychelles','Africa',NULL,'',-5,55.75,'','',-6.27508175901,53.9515216568,-6.27508175901,53.9515216568,-7.70843163102,54.1703057749,-5.72241,53.8771,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Western Schelf II',2096,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,1,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1289,1448,'',-4,54,-699946,5842936,'Seychelles','Africa',NULL,'',-4.1667,54.9167,'','',-5.4621100384,53.0964989353,-5.4621100384,53.0964989353,-6.86963878005,53.3384953441,-4.89166,53.0403,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Russel Basin',2097,'','Paleogene',NULL,NULL,'Oligocene/Miocene',5.30,33.90,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',23,2,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1290,0,'Shallow-water reefal calcarenites mentioned. No description.',-8,158,-1700614,18736385,'Solomon Islands','Oceania',NULL,'',-8.25,158.5,'','',-12.6705736551,166.960795012,-12.6660181242,166.963955078,-10.864126926,167.265765579,-24.6043,160.208,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Russel Basin',2098,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1290,0,'',-8,158,-1620034,18323005,'Solomon Islands','Oceania',NULL,'',-8.25,158.5,'','',-10.9166038021,168.226089491,-10.9180985266,168.224969098,-11.371118352,167.156983484,-20.5016,159.682,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Vanikoro Basin, Vanuatu',2099,'','Neogene','Miocene','Lower Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,2,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1291,0,'',-11,166,-2225040,19431431,'Vanuatu','Oceania',827,'',-11.8333,166.75,'','',-15.3125398362,173.572707689,-15.3125398362,173.572707689,-14.6359780572,174.939063161,-29.031,168.777,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Vanikoro Basin, Vanuatu',2100,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1291,0,'',-11,166,-2136989,19036499,'Vanuatu','Oceania',827,'',-11.8333,166.75,'','',-13.8694810877,174.645717118,-13.8707370074,174.644745699,-13.8400942047,176.653865005,-24.7634,168.123,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Eua Channel, Tonga, Pacific',2101,'','Paleogene','Eocene','Priabonian','Upper Eocene',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',36,2,'1','Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1292,0,'',-21,-175,-3780798,-15863007,'Tonga','Oceania',821,'',-21.3333,-175,'WAHR','70950',-33.4493210794,171.729710664,-33.4493210794,171.729710664,-35.3743333698,175.745992311,-31.0241,-175.558,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Klamono, New Guinea',2102,'Kais','Neogene','Miocene','Lower Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick','90',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1293,0,'100-500 m thick pinnacle reefs on carbonate platform.\nInterfingering with basinal shales.\nOil field.\nSalawati Basin.\nEarly to late Miocene.',-1,131,-1764715,14481653,'Indonesia','Asia',614,'',-1.1333,131.4667,'','',-10.8799475022,126.217584289,-10.8799475022,126.217584289,-13.2396188528,128.615537344,-12.317,133.729,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Klamono, New Guinea',2103,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick','250',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1293,0,'See reef 2102.',-1,131,-1252721,14596255,'Indonesia','Asia',614,'',-1.1333,131.4667,'','',-8.05296941892,127.836555569,-8.05543752495,127.835123486,-9.74005327212,129.723948428,-9.55528,133.103,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Klamono, New Guinea',2104,'','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick','150',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1293,0,'See reef 2102.',-1,131,-652412,14629081,'Indonesia','Asia',614,'',-1.1333,131.4667,'','',-5.29942743793,129.339874265,-5.3697220771,129.303798105,-6.41674575018,130.61630147,-6.77525,132.522,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Wasian, New Guinea',2105,'Kais','Neogene','Miocene','Lower Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick','90',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1293,0,'Bintuni Basin.\n100 - 500 m thick pinncale reefs on platform carbonates, interfingering with basinal shales.\nOil field.',-1,133,-1917271,14625973,'Indonesia','Asia',614,'',-1.8667,133.3333,'','',-11.5685871111,128.137244272,-11.5685871111,128.137244272,-14.4030923954,130.29703956,-13.4788,135.405,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Wasian, New Guinea',2106,'Kais','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick','250',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1293,0,'See reef 2105.',-1,133,-1394952,14759612,'Indonesia','Asia',614,'',-1.8667,133.3333,'','',-8.76507779711,129.731114528,-8.7675249049,129.729702526,-10.9287002532,131.365150882,-10.6144,134.832,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Wasian, New Guinea',2107,'Kais','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick','150',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1293,0,'See reef 2102.',-1,133,-773202,14816887,'Indonesia','Asia',614,'',-1.8667,133.3333,'','',-6.02650857287,131.217470288,-6.09671283865,131.181659214,-7.55534605327,132.278893842,-7.72514,134.302,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Madura Basin, Java',2108,'','Paleogene','Oligocene','Rupelian','lower Oligocene',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',32,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1294,1293,'Massive reefal limestones grading laterally into sandstones, siltstones and coals.',-7,113,-523079,13270614,'Indonesia','Asia',614,'',-7.5833,113.1667,'','',-2.42474025168,111.671763837,-2.42474025168,111.671763837,-8.22311829672,115.512000092,-5.31859,120.022,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Wiriagar, New Guinea',2109,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1293,1309,'See reef 2102.',-2,132,-1436026,14693978,'Indonesia','Asia',614,'',-2.25,132.8833,'','',-9.15414989875,129.280895771,-9.15660223973,129.279485369,-11.1841823846,130.822264335,-10.9108,134.311,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Wiriagar, New Guinea',2110,'','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1293,1309,'See reef 2102.',-2,132,-820573,14757851,'Indonesia','Asia',614,'',-2.25,132.8833,'','',-6.41173427775,130.766756567,-6.48196711871,130.730909671,-7.82676819583,131.749260284,-8.05284,133.806,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Kerendan, Borneo',2111,'Berai','Paleogene','Oligocene','Rupelian','lower Oligocene',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',32,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1293,0,'Pinnacle reef on horst, surrounded by basinal shales.\nProducing gas reservoir.\nNW Kutei Basin.\nBerai Formation (late Rupelian to Chattian).',0,116,585081,13340201,'Indonesia','Asia',614,'',0.0167,116,'','',2.72809200493,113.677496679,2.72809200493,113.677496679,-2.98217437832,117.057682548,2.6769,121.37,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Kerendan, Borneo',2112,'Berai','Paleogene','Oligocene','Chattian','Upper Oligocene',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',27,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1293,0,'See reef 2111.',0,116,153928,13211936,'Indonesia','Asia',614,'',0.0167,116,'','',0.973403831539,113.425550459,0.968562409204,113.422964814,-4.28897045215,116.15249691,1.55155,120.69,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Poleng, Madura Basin, Java',2113,'','Neogene','Miocene','Lower Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',1294,1293,'Thick limestones, often reefal and highly porous, rarely dolomitized.',-6,112,-892443,12677087,'Indonesia','Asia',614,'685',-6.6667,112.9167,'','',-4.96035266352,110.140342858,-4.96035266352,110.140342858,-8.56991339221,112.731390386,-6.28221,117.048,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ardjuna sub-basin, offshore Java',2114,'','Paleogene','Oligocene','Chattian','Chattian-Aquitanian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',23,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1295,1293,'Batu Raju Limestone buildup.\nSeismic exploration only.\nSevere diagenetic modification, but basic coral framework visible in places.',-5,107,-802351,12346220,'Indonesia','Asia',614,'',-5.9167,107.7,'','',-2.6475414721,105.93565319,-2.6475414721,105.93565319,-6.060601575,109.760138627,-5.54276,113.365,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('W-Bengal Basin',2115,'','Paleogene','Eocene',NULL,'Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,50,'Early Eocene (Ypresian, 51.9 Ma)',40,1,'1','Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'600',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1296,1297,'Seismic interpretation only.\nRef. 1297 cites only Paleogene age.\nHydrocarbon prospect.',21,88,-29467,8921928,'India','Asia',501,'',21.4167,88,'','',3.81318741981,76.7777667683,3.81318741981,76.7777667683,0.745628982638,77.6374416968,-0.854363,78.9155,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Monzhukly, Nebit Dag, Turkmenia',2116,'Tyusmergenskaya','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian-Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',150,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick','250',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1298,1299,'Seismic interpretation only.',39,54,5065788,5120807,'Turkmenistan','Asia',NULL,'2114',39.3167,54.45,'','',34.1294883541,61.896478461,34.1294883541,61.896478461,35.8300617394,66.0010563406,35.399,59.4027,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Monzhukly, Nebit Dag, Turkmenia',2117,'','Cretaceous','Lower Cretaceous','Berriasian','Berriasian',139.80,145.00,22,'late Tithonian - early Valanginian',141,140,'Early Cretaceous (Berriasian, 142.4 Ma)',143,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1298,1299,'Seismic data only.',39,54,5092068,4832680,'Turkmenistan','Asia',NULL,'1794',39.2833,54.4167,'','',32.6776072671,62.4849691992,32.6776072671,62.4849691992,35.2011709673,65.5504277036,34.745,59.0959,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Monzhukly, Nebit Dag, Turkmenia',2118,'','Cretaceous','Lower Cretaceous',NULL,'Neocomian',133.00,145.00,22,'late Tithonian - early Valanginian',141,125,'Early Cretaceous (Barremian, 127.2 Ma)',140,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',1298,1299,'Two major reef cycles:\nBerriasian-Hauterivian and\nHautervian-Barremian',39,54,5091029,4712535,'Turkmenistan','Asia',NULL,'1794',39.2833,54.4167,'','',32.4955880896,62.7621670226,32.4955880896,62.7621670226,34.970694376,65.348950361,34.4778,59.1819,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('CLA-111, Lake Maracaibo',2119,'','Cretaceous','Lower Cretaceous',NULL,'middle Aptian-Cenomanian',93.90,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',107,2,'1','Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','15','Non-rudist bivalves','5','Rudists','47','Bivalves (mostly oysters) - algae (microbes)',NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',2,'Actual reservoir',1301,0,'Outer carbonate platform setting.\nPelecypod biostromes with rudists and/or oysters.\nUp to 15 % porosity and 8 md permeability.\nCogollo Group.\nWell data.',9,-71,-251603,-4808084,'Venezuela','South America',201,'',9.75,-71.5,'','',1.42836516062,-37.5477192643,1.42836516062,-37.5477192643,4.87746991802,-44.9735928211,4.4056,-43.2585,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('La Paz Field, Maracaibo',2120,'','Cretaceous','Lower Cretaceous',NULL,'middle Aptian-Cenomanian',93.90,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',107,2,'1','Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150','2119',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','15','Non-rudist bivalves','5','Rudists',NULL,NULL,NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',2,'Actual reservoir',1301,0,'see reef 2119',10,-72,-122941,-4862956,'Venezuela','South America',201,'',10.6833,-72,'','',2.2488970564,-38.2113201611,2.2488970564,-38.2113201611,5.70716612927,-45.6281420608,5.35706,-43.7161,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mishrif reef trend, off Abu Dhabi',2121,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',94,2,'1','Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','1279',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',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',1302,0,'See reef 1223.\nWas Cenomanian/Turonian',25,54,-80306,4964151,'United Arab Emirates','Asia',NULL,'',25.0833,54.9167,'','',3.62388773758,49.3596411272,3.62388773758,49.3596411272,0.0271324175732,43.9598799799,-0.801004,44.2069,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mishrif trend, off Abu Dhabi',2122,'','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',94,2,'1','Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','1279',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1302,0,'See reef 2123.\nWas Cenomanian/Turonian',24,54,-108688,4919198,'United Arab Emirates','Asia',NULL,'',24.8333,54.5,'','',3.42490507232,48.9518954649,3.42490507232,48.9518954649,-0.154822844844,43.5450127562,-1.00112,43.8004,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fateh Field, Mishrif trend, off Abu Dhabi',2123,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',95,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'300','1279',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1302,1385,'Coarse shell beds more common than true reefs.\nLow relief rudist coppices. \nRadiolitids dominate rudist fauna. Caprinids and monopleurids also common. Chondrodonta present.\nCladophyllia (small branching coral) in reef core.\nExtremely high sediment production.\n20-30 % porosity. 50 md permeability in average.',25,54,-34584,4916089,'United Arab Emirates','Asia',NULL,'',25.3667,54.4,'','',3.96557393177,48.9320249507,3.96557393177,48.9320249507,0.386202731523,43.5477212073,-0.460501,43.7792,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mishrif reef trend, off Abu Dhabi',2124,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',95,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','1279',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1302,0,'',25,53,-40043,4841368,'United Arab Emirates','Asia',NULL,'',25.25,53.6667,'','',3.93862149869,48.2578509741,3.93862149869,48.2578509741,0.387542460463,42.8745965892,-0.488817,43.1067,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mishrif reef trend, off Abu Dhabi',2125,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',94,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','1279',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1302,0,'Was Cenomanian/Turonian',24,53,-118277,4825057,'United Arab Emirates','Asia',NULL,'',24.6667,53.5833,'','',3.37107474988,48.1031121092,3.37107474988,48.1031121092,-0.17293240225,42.6962031284,-1.05659,42.9531,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ardengost, Pyreneans',2126,'','Carboniferous','Mississippian','Serpukhovian','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',324,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'3',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','35','Chaetetids - corals - cyanoyphyceans - algae - (bryozoans)',NULL,NULL,'60','30','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1304,1826,'Massive limestones with Mudstones, Wackestones, boundstones and some grainstones.\nCrinoids, Bryozoans, chaetetids and massive or branching corals (heterocorals, rugose corals).\nDiverse algae and microbes described.',42,0,-1798738,1143389,'France','Europe',331,'',42.9333,0.4667,'WAHR','76632',-29.2360496677,5.14230215809,-29.2360496677,5.14230215809,-16.7210279815,-16.6550194602,-13.4069,11.2157,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mukhroh well, Hais',2127,'','Jurassic','Upper Jurassic',NULL,'Upper Jurassic',145.00,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1307,0,'A single coral (Stylina lortphilippsi) described from limestone.',11,48,-1877136,3944240,'Somalia','Africa',709,'',11.1667,48.9167,'','',-24.1293096208,40.4355862014,-24.1293096208,40.4355862014,-20.9700516363,36.2866009931,-12.7973,33.8892,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mukhroh well, Hais',2128,'','Paleogene','Eocene',NULL,'Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,50,'Early Eocene (Ypresian, 51.9 Ma)',40,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1307,0,'Description of some corals only.',11,46,409953,4359847,'Somalia','Africa',709,'',11.1667,46.9167,'WAHR','71064',4.54877738649,40.7667781414,4.54877738649,40.7667781414,11.1667,46.9167,3.59962,39.4716,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Geba Geba',2129,'','Paleogene','Eocene',NULL,'Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,50,'Early Eocene (Ypresian, 51.9 Ma)',40,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1307,0,'',3,44,-637629,4041897,'Somalia','Africa',709,'',3.5333,44.05,'WAHR','71063',-3.14103310626,38.0800647847,-3.14103310626,38.0800647847,-3.8992169742,38.1973469164,-4.09487,36.7986,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dubino',2130,'','Paleogene','Oligocene','Rupelian','Oligocene',23.00,33.90,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',28,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1307,0,'Limestone with diverse corals (11 species described) from one locality. 15 miles SSW of Berbera.',10,44,1074851,4496237,'Somalia','Africa',709,'',10.2333,44.8833,'WAHR','71062',6.64753055107,40.629055695,6.65003799702,40.6310621973,5.25667457767,41.1140929125,7.78818,40.438,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Minkowice, Lublin Basin',2131,'','Carboniferous','Mississippian','Serpukhovian','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',324,3,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick','35',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate','4','Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'60','0','40',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',2821,1308,'Waulsortian type mud mound with crinoids, fenestrate bryozoan debris and abundant stromatactis. \nMicrobes probably important\n35 m thick.\nin central part of Lublin Basin.',51,22,-63076,2147947,'Poland','Europe',301,'',51.2,22.75,'','',-15.8535981309,14.0261055625,-15.8535981309,14.0261055625,1.00466728843,-4.23126921603,-0.208516,19.6036,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sengkang, Sulawesi',2132,'Tacipi','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick','270',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',2,'Actual reservoir',1312,1311,'Late Miocene knoll reefs in Sengkang Basin.\nGas producing reservoir.\nOutcrops with predominance of Porites, diverse coralline algae, forams.\nMaximum thickness of buildups 270 m.',-4,120,-551231,13343770,'Indonesia','Asia',614,'1310,1447',-4.1333,120.0333,'','',-3.07996709878,119.210708653,-3.07996709878,119.210708653,-4.51314793781,119.470487256,-3.95577,120.892,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Northern Bone Region, Sulawesi',2133,'','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50','2132',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1312,1447,'',-4,120,-601045,13357360,'Indonesia','Asia',614,'',-4.5,120.1833,'','',-3.4462038724,119.36165855,-3.4462038724,119.36165855,-4.878229458,119.624486743,-4.31598,121.057,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Palonki, Northern Bone, Sulawesi',2134,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',1,'Potential reservoir',1312,0,'Only middle Miocene coralgal rudstones in Palongki area.',-4,120,-524189,13496843,'Indonesia','Asia',614,'',-4.4667,120.1722,'','',-3.83595864649,118.170393934,-3.83595864649,118.170393934,-6.97024476112,118.746040265,-3.88116,122.278,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Iramu, Papua New Guinea',2135,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'40',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',1313,0,'',-7,144,-2147913,15340699,'Papua New Guinea','Oceania',615,'',-7.6167,144.8667,'','',-14.2174165127,141.608037895,-14.2196721836,141.606816849,-16.3143374525,142.57150576,-16.2468,142.054,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bobrovcek, W Tatra',2136,'','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1314,2752,'Two biostromal units (together about 5 m thick).\nDiverse corals (including new genus Meandrostylophyllum), sponges, calcarerous algae and other organisms.\nNo in situ organisms?\n',49,19,4237923,1851076,'Slovakia','Europe',336,'',49.15,19.6,'WAHR','67625',24.9226315492,34.7142236163,24.9226315492,34.7142236163,28.5321609389,28.0860503312,29.4042,22.552,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ojin Seamount, Emperor Chain, Pacific',2137,'','Paleogene','Paleocene','Danian','Paleocene',56.00,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',61,1,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,2,'Cold - water','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1316,556,'Bryozoans and coralline algae werde recovered. Seismic evidence for bioherms.\nBryozoan-algal mounds?',37,170,3891667,-16388853,'Pacific','Pacific',NULL,'1317',37.9833,170.6,'','',23.6302677215,-147.032557623,23.6302677215,-147.032557623,37.9833,170.6,27.0422,-158.627,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Koko Seamount, Pacific',2138,'','Neogene','Miocene',NULL,'Miocene',5.30,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,1,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1317,601,'Fossil reef corals dated as 25-30 Ma.',35,171,4157778,-17653617,'Pacific','Pacific',NULL,'',35.5,171.75,'','',32.4163471214,-176.890116842,32.4017566486,-176.791284018,35.5,171.75,30.8396,-177.465,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yuryaku Seamount, Pacific',2139,'','Paleogene','Oligocene','Rupelian','lower Oligocene',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',32,1,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1317,0,'Fossil reef corals dated by Sr-isotopes 34 Ma.',33,171,3671696,-17130414,'Pacific','Pacific',NULL,'',33.45,171.6333,'','',26.8093739596,-165.111765493,26.8093739596,-165.111765493,33.45,171.6333,26.3797,-167.946,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kanmu Seamount, Pacific',2140,'','Neogene','Miocene','Lower Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,2,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1317,0,'Fossil reef corals dated as 21, 27.7 and 33 Ma.\nSee also reef 2141.',32,173,3713700,-17900792,'Pacific','Pacific',NULL,'',32.1167,173.0833,'','',28.346168319,-171.844904004,28.346168319,-171.844904004,32.1167,173.0833,26.4679,-173.157,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kanmu Seamount, Pacific',2141,'','Paleogene','Oligocene','Rupelian','Oligocene',23.00,33.90,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',28,1,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1317,0,'See reef 2140',32,173,3489118,-17124589,'Pacific','Pacific',NULL,'',32.1167,173.0833,'','',26.196453099,-165.559122472,26.2009268106,-165.569513634,32.1167,173.0833,25.2634,-168.163,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('SE-Menorca',2142,'','Neogene','Miocene','Upper Miocene','Tortonian/Messinian',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'35',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',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',1318,0,'Very pronounced debris production.\nReefal unit situated on rhodalgal ramp.\nPorites and Tarbellastrea sp. and abundant red algae.\nN 17 (upper Tortonian, lower Messinian).',39,4,5285416,320206,'Spain','Europe',304,'',39.8333,4.25,'','',39.614517414,2.38444628467,39.6124093683,2.39250211922,39.4256931213,4.15590172955,40.4336,3.29844,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('SW-Menorca',2143,'','Neogene','Miocene','Upper Miocene','Tortonian/Messinian',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'35','2142',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',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',1318,0,'see reef 2142.',39,3,5297755,280625,'Spain','Europe',304,'',39.9333,3.8333,'','',39.674803879,1.95645650193,39.673057253,1.96461038981,39.5302047015,3.74351384111,40.498,2.86628,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tattsfield, Weald, England',2144,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1320,0,'Early marine peloidal cements important for reservoir quality. \nAverage porosity around 8-10 %.\nLower part of reefs with laminar Thamnasteria and digitate Thecosmilia. Upper part with robust branching Thecosmilia and massive Isastrea.\nStromatolitic crusts present.',51,0,4977262,325232,'United Kingdom','Europe',331,'',51.2833,0.0167,'','',29.0616546588,18.7756462947,29.0616546588,18.7756462947,35.2970149199,19.206752718,41.8588,9.77317,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ballykane',2145,'','Carboniferous','Mississippian','Visean','Courceyan/Chadian',346.70,350.00,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',345,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,'300','437',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','3','Microbes','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1322,0,'Individual mounds up to 100 m thick. Waulsortian sequence about 200 m thick.\nCorals very rare but present (tabulates, rugose).',53,-7,-1475287,-367864,'Ireland','Europe',331,'',53.3667,-7.0333,'WAHR','76916',-33.6299374469,-14.6795314993,-33.9804624544,-15.077124948,-3.02642170454,-51.1902707709,-10.9422,-3.37354,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Krachoua',2146,'','Jurassic','Middle Jurassic','Callovian','upper Callovian',163.50,164.50,21,'late Bathonian - early Tithonian',151,165,'Middle Jurassic (Callovian, 164.8 Ma)',162,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'20','80','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1324,2369,'',32,10,2189960,1056558,'Tunisia','Africa',715,'',32.6333,10.8667,'','',8.41285190372,15.6352592154,8.25384894689,15.4941217716,12.8292158215,14.9331044745,21.0042,11.7547,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tenia Island, New Caledonia, Melanesia',2147,'','Neogene','Pliocene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1325,0,'Belongs to France',-22,166,-3422170,17278337,'New Caledonia','Pacific',NULL,'',-22.05,166.0833,'','',-23.6373079894,165.572336148,-23.6353015883,165.572961064,-24.1947844389,165.975264744,-24.4477,165.847,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kangjia-ping, Daluokeng, Cili, Hunan',2148,'Changhsing','Permian','Lopingian','Changhsingian','lower Changhsingian',253.00,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',253,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','57','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,'4',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','1','Corals','96','Rugose corals - microbes - algae','1',NULL,'60','30','10',0,'no',0,'no','3','25 or more reef building species','27','1','Constructor guild',NULL,NULL,'1','Present','1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1326,1700,'Paleofusulina zone according to ref. 1326\r\nRef. 1700 states Wuchipangian age.\r\nRugose coral (Waagenophyllum) reef. 40-50 % of rock is formed by corals. Single colonies up to 1 m high.\r\nAddtionally sphinctozoans, hydrozoans (?), Tubiphytes, Archaeolithoporella, red algae (Parachaetetes, Solenopora), bryozoans. All of them rare in coral reef core.\r\nReef 35-57 m thick. \r\nDolomitization only in west. Paleontological data from eastern sections with many sponges. Red algal–coral community is dominated by solenoporaceans.',29,110,-208302,9245067,'China','Asia',602,'',29.4,110.9333,'WAHR','24247',-11.1796212464,109.164422438,-11.4597761613,108.896337253,9.41548314187,128.373640223,9.59332,99.1881,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-03-28 17:49:20'),('Mole Creek, Tasmania',2149,'Den','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',449,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','50','20',0,'no',0,'no','2','6 to 24 reef building species','15','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1328,0,'Original age call: Caradocian-Ashgillian\nSmall coral-stromatopore bioherms in Den Formation (Gordon Group).\nTabulate (favositid, heliolitid, halysitid) corals, rugose (solitary and compound) and diverse stromatopores (10 species assigned to 2 morphotypes) are important.\nSome bioherms dominated by stromatopores, others by corals (mostly tabulates).\nEnvironment characterized as outer platform, but fitting to ramp as well.',-41,146,1101831,19761258,'Australia','Oceania',801,'',-41.55,146.4,'WAHR','24252',5.02919802392,119.766356745,5.02919802392,119.766356745,5.02919802392,119.766356745,8.75836,178.592,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Houshan, Guilin, Guangxi',2150,'Yonghsien','Devonian','Upper Devonian','Frasnian','early Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',383,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','8','1','Less than 10 m wide',NULL,'1','Less than 20 m','30',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild',NULL,NULL,'1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1329,1866,'Western margin of Guilin platform.\nCoral bafflestone reef behind an algal-stromatoporoid platform margin reef. Composed exclusively of rugose coral Smithiphyllum ( 3 species). Brachiopods as dwellers. Some solenoporacean fragments. \n-> Collection of Miller\n\nCoral bioherm (Smithiphyllum) 8 m thick and 30 m wide. Base is Stromatactis limestone, top is peloidal packstone followed by receptaculid-algal limestone.\n\nRef:. 1866:\nReef complex with \n\'Algal\'-stromatoporoid reef\nreceptaculid-algal reef\nSmithiphyllum bioherm\nalgal mounds\n\n30 m exposed thickness.\nLateral differentiation into back-reef, reef flat and margin, margina fore-slope.\nStachyodes most abundant in reef flat.\nCalcimicrobes prevail in reef-slope: Renalcis, Epiphyton, Rothpletzella\nCavities and veins filled with radiaxial-fibrous calcites',25,110,-1173370,10732529,'China','Asia',602,'',25.2833,110.2333,'WAHR','5769',-15.4144968489,87.819118602,-15.4144968489,87.819118602,-14.3494970032,111.885266175,-1.26525,109.83,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Laliderer Tal',2151,'','Triassic','Middle Triassic','Anisian','upper Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1331,0,'Earliest small buildups in Northern Alps.\nHomoclinal ramp setting.',47,11,2315069,1999180,'Austria','Europe',301,'',47.4167,11.4667,'WAHR','45426',15.8932170284,36.4303784251,15.8932170284,36.4303784251,10.681959581,26.1391037272,7.25877,24.3769,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Xifeng-Kaiyang, Guizhou',2152,'Doushantuo','Ediacaran','Ediacaran','Nama Assemblage','middle Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',570,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m','100','40',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1333,0,'Phosphatic stromatolitic bioherms: 1 m thick, up to 100 m wide.\n',27,107,4950155,15003755,'China','Asia',602,'',27,107.35,'','',29.8785593793,52.7775748189,29.8785593793,52.7775748189,29.8785593793,52.7775748189,43.4366,164.275,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maurice Ewing Bank, South Atlantic',2153,'','Cretaceous','Lower Cretaceous',NULL,'Lower Cretaceous',100.50,145.00,22,'late Tithonian - early Valanginian',141,125,'Early Cretaceous (Barremian, 127.2 Ma)',135,1,'1','Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,2,'Cold - water','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1336,0,'Seismic evidence for a succession of carbonate buildups.\nAge Jurassic/Cretaceous, most probably early Cretaceous.',-50,-46,-7310569,123496,'Atlantic','Atlantic',NULL,'',-50.5,-46.8333,'','',-55.4160657927,-4.95113666419,-55.4160657927,-4.95113666419,-52.0384972761,-11.2689808586,-49.2862,-12.8964,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Globocec',2154,'','Jurassic','Lower Jurassic','Pliensbachian','Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,185,'Early Jurassic (Pliensbachian, 186.8 Ma)',187,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','7',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'10','90','0',0,'no',0,'no','1','Less than 6 reef building species','1','2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1337,0,'5 m and 7 m thick intervals with rock-forming Cochlearites.',45,14,4138384,1947844,'Slovenia','Europe',328,'',45.8833,14.85,'WAHR','34668',18.8258449228,28.8621493114,18.8258449228,28.8621493114,25.0588897091,32.8986687012,30.8249,22.3584,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Inhoca',2155,'','Cretaceous','Upper Cretaceous',NULL,'Upper Cretaceous',66.00,100.50,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',70,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1338,0,'Ostrea bank. Oysters with abundant borings.',-25,32,-5059258,2121828,'Mozambique','Africa',NULL,'',-25.2667,32.3833,'','',-38.4538353087,23.7977498449,-38.4538353087,23.7977498449,-39.1378814985,17.6716596382,-42.7732,20.2657,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Albenza, Southern Alps',2156,'Calcare di Zu','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m','8','1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','1','Corals','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','22','1','Constructor guild',NULL,NULL,'1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1340,2280,'3 m thick, 8 m wide patch reef. \nLithocodium and Bacinella bindstone at base. \nThen coral-dominated reef with solenopraceans, tabulozoans, \'sphinctozoans\' and some hydrozoans. \nStongly encrusted by Lithocodium and Bacinella.\nMicritic groundmass.\n\nRef. 1340:\nAlternations of marine and meteoric diagenetic conditions, most probably caused by relative sea level fluctuations, are recorded in an Upper Triassic (Rhaetian) patch reef in the Calcare di Zu Formation, Lombardian Basin. Three main types of cements have been distinguished: 1) isopachous fibrous calcite cement, partially to completely filling mostly secondary solution cavities; 2) radial-fibrous calcite cement in which strongly turbid relics of precursor fibrous cements suggesting a neomorphic origin can be observed, and 3) equant spar calcite found both as a last cement occluding the remaining void space after the cementation by the fibrous cements and as a neomorphic product in corals.\nBoth marine and non-marine internal sediments are present in the patch reef. The marine internal sediments are composed of fecal pellets, peloids, micrite and bioclasts. They could be precedent, successive or contemporaneous to the isopachous marine cement and could have a geopetal disposition or may completely fill cavities. The observations made indicate that a \'peloidal texture\' (a nucleus of anhedral HMC crystals from which fibrous crystals radiate) could result from the introduction of peloids/fine-grained micritic intraclasts into fibrous marine cements during their growth.\nThis texture has not been observed in geopetal infill peloids. Non marine internal sediments are composed of crystal silts and their deposition was preceded by the partial dissolution of the isopachous fibrous cements. ',45,9,2922905,1565103,'Italy','Europe',344,'',45.7722,9.4819,'WAHR','27537',27.5616627174,26.7408761459,27.5616627174,26.7408761459,23.8132295755,25.2057866985,32.2652,11.7884,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('W-Bengal Basin II',2157,'','Paleogene','Eocene',NULL,'Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,50,'Early Eocene (Ypresian, 51.9 Ma)',40,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'600','2115',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1297,0,'See reef 2115 for remarks.',21,87,-1070053,8724296,'India','Asia',501,'',21,87.8333,'','',3.42186635516,76.5660183902,3.42186635516,76.5660183902,0.363739944895,77.4095015758,-1.22084,78.6635,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('W-Bengal Basin III',2158,'','Paleogene','Eocene',NULL,'Eocene',33.90,56.00,28,'Lutetian - Bartonian',45,50,'Early Eocene (Ypresian, 51.9 Ma)',40,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'600','2115',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',1297,0,'See reef 2115 for remarks.',20,87,-76163,8717159,'India','Asia',501,'',20.4167,87.4167,'','',2.89848985589,76.0982208062,2.89848985589,76.0982208062,-0.138950519733,76.9202207668,4.74991,89.416,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),