('Gascoyne Inlet, SW Devon Island',1742,'Douro-Barlow Inlet','Silurian','Ludlow','Ludfordian','upper Ludlovian',423.00,425.60,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',420,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','50','2','10 - 100 m wide','50','2','10 - 100 m','60','200',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','1','Corals','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,'90','0','10',0,'no',0,'no','2','6 to 24 reef building species','16','2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1042,1135,'No detailed locality description.\nThree types of mounds in area.\nMudmounds\nCoral-skeletal mounds\nCoral-stromatoporoid skeletal mounds\nOnly Mudmounds better preserved: 15 thick, 50 m in width.\nCompound reef mounds up to 50 m thick and 60 m across.\n14 coral species, microbes and possibly stromatoporoids. Collection of Alroy.\n\nAbstract or ref. 1135:\nNear Gascoyne Inlet, the topmost Douro and and lowermost Barlow Inlet Formations record overall upward  shallowing from ramp to shallow shelf conditions. This transitional sequence contains bioherms of various sizes, from small isolated reef mounds 1 to 2 m across to larger, compound reef mounds over 50 m thick and 60 m across, as well as distinctive inter- and pre-reef mound facies. The larger reef mounds show stages intermediate in character between those in sponge-dominated reef mounds of the Douro Formation and in larger stromatoporoid-crinoid-dominated reefs in the Barlow Inlet Formation. Three principal reef mound facies developed in turn. An initial partly lithified lime mudstone, containing scattered corals and apparently relicit sponge-cryptomicrobial fabrics, developed on sheets of oncolitic storm debris in mainly low energy conditions between storm and fairweather wave bases. This lower facies of the reef mounds achieved up to 2 m relief above surrounding burrowed, soft, detrital and carbonate muds. With gradual shallowing, and progressively higher energy conditions above fairweather wave base, middle facies of coral-and crinoid-rich mudstone developed, flanked by coalescing aprons of coarse crinodal debris. The middle facies achieved a maximum relief of 4 m. Detrital and carbonate muds succeeded the grainy flankbeds, as abrupt deepening    restored conditions of low energy below fair-weather wave base. The ensuing upper facies of the reef mounds is more  varied, comprising sparsely fossiliferous and locally fenestral lime mudstones, patchy coral bafflestone and bindstone, coarse encrinites, and substantial culminating stromatoporoid bindstone. Relief of the upper facies was progressively    reduced by onlap of adjacent muds. The reef mounds were ultimately engulfed by these muds, and a laterally discontinuous, biostromal, Stylopleura rudstone caps the sequence. With resumed shallowing, the sea floor again was exposed to more persistently turbulent conditions above fairweather wave base. Large  stromatoporoid-crinoid-dominated reefs formed just above the transitional sequence on topographic highs inherited from the reef mounds, and are flanked by substantial grainy crinoid-rich facies. ',74,-91,283697,-3376213,'Canada','North America',121,'1617',74.7,-91.4167,'WAHR','5790',5.20114668309,-72.3994016712,5.20114668309,-72.3994016712,5.20114668309,-72.3994016712,1.99207,-30.212,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Oj-Muran, Lena River',1745,'','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',518,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'800','1776',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','14','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1044,1045,'Small bioherms composed of either Renalcis and archaeocyaths or Epiphyton.\nIn addition: Girvanella, Markovella, Chabacovia, stromatolites.',61,126,-2254095,-119996,'Russia','Asia',624,'1093, 1413',61.0833,126.2167,'WAHR','9990',5.87625840153,-65.1505394681,5.87625840153,-65.1505394681,5.87625840153,-65.1505394681,-9.92768,-14.7519,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('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'),('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'),('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'),('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'),('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 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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('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'),('Kozhym River, Pechora',2162,'','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 ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','6','Calcisponges','66','Stromatolites-\'sphinctozoans\'-(stromatoporoids, algae, corals)',NULL,NULL,'10','80','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1344,1345,'',65,60,1075042,169543,'Russia','Asia',624,'1420',65.5833,60.4167,'WAHR','80710',22.5719040596,-44.9179518427,22.5719040596,-44.9179518427,22.5719040596,-44.9179518427,7.66012,2.61862,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Finnmark Platform, Barents Sea',2164,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','160',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate','4','Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1346,0,'Microbial boundstones predominate. Packstone matrix with bryozoans, crinoids, Tubiphytes and forams. Stromatactis limestones at base, bryozoan-cement framestones at top.\n160 m interval cored. Buildup flank with up to 45° dip angle.\nCement alone forms around 46 % of buildup volume.\n38 % biogenic particles.\n16 % overall micrite (including microbially induced).',72,29,4283401,2182704,'Norway','Europe',301,'',72.2158,29.635,'','',29.6640937573,20.7080533043,29.6640937573,20.7080533043,29.0325880064,-5.41245027875,27.7228,18.2722,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Finnmark Platform, Barents Sea',2165,'','Permian','Cisuralian','Artinskian','Artinskian',283.50,290.10,15,'Sakmarian - Kungurian',277,285,'Early Permian (Artinskian, 286.8 Ma)',280,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','160',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate','4','Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','3','Microbes','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1346,0,'See reef 2164 for remarks',72,29,4908420,2431081,'Norway','Europe',301,'',72.2158,29.635,'','',30.3448167663,21.2386483091,30.3448167663,21.2386483091,31.7499717864,3.39577104307,31.2289,21.0801,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rübeland, Harz',2186,'','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','80',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1370,0,'Thrombolitic mudstones, spar layers, stromatolites.\nHexactinellid sponges as only macrofossils.\n80 m thick, 260x150 m lateral extension.',51,10,-2242323,797419,'Germany','Europe',331,'',51.7667,10.85,'','',-19.3306812493,-9.05251403861,-19.3306812493,-9.05251403861,0.941058423226,-66.4452988995,-18.3828,8.01051,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('West Edmond Field, Oklahoma',2223,'Frisco','Devonian','Lower Devonian','Lochkovian','Lochkovian-Pragian',407.60,419.20,8,'middle Pridolian - middle Pragian',412,415,'Early Devonian (Lochkovian, 415 Ma)',411,2,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','13','Echinoderms','60','Bryozoans - Pelmatozoans - (microbes)',NULL,NULL,'40','0','60',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',2,'Actual reservoir',1397,0,'Hunton Group\nLow energy mud mound\nOuter ramp setting\nPelmatozoan-bryozoan packstone.\nMudstones in mound core.',35,-97,-5509379,-4375009,'United States','North America',101,'',35.65,-97.5667,'','',-34.002864692,-75.4836139323,-34.002864692,-75.4836139323,-20.1658357468,-133.157591619,-33.9079,-54.2923,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bolshoi Tir, Siberia',2228,'Osinsky','Cambrian','Terreneuvian','Stage 2','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',527,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','90',NULL,NULL,NULL,'4','More than 1000 m',NULL,'90',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1405,1413,'Osinsky horizon.\nNepa-Botuoba anteclise.\nEpiphyton, Renalcis, Marcovella dominant.\nRare archaeocyaths.\n80-90 m thick.\nDimensions 40 x 90 km but reefs probably much smaller.',57,105,-2518261,1115479,'Russia','Asia',624,'',57.5,105.5,'','',1.17293117074,-63.8349457886,1.17293117074,-63.8349457886,1.17293117074,-63.8349457886,-11.5242,-3.37659,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nepa, Siberia',2229,'Osinsky','Cambrian','Terreneuvian','Stage 2','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',527,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'90','2228',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1405,1406,'Oil field.\nOsinsky horizon.\nNepa-Botuoba anteclise.\nEpiphyton, Renalcis, Marcovella dominant.\nRare archaeocyaths.\n95-100 m thick.',58,105,-2558793,1064719,'Russia','Asia',624,'214, 1413',58,105.8333,'','',0.892093614251,-64.285308644,0.892093614251,-64.285308644,0.892093614251,-64.285308644,-11.9506,-3.69928,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Talakan, Siberia',2230,'Bilir','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',519,2,'1','Seismic data available ',4,'Biostrome','2','10 to 100 m thick','55',NULL,NULL,NULL,'3','More than 100 m',NULL,'65',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1408,1413,'Osa horizon.\nGas field.\nCentral part of Nepa-Botuoba anteclise.\nStromatolithic biostrome massif. 50-55 m thick.\n37 x 65 km\nDominated by stromatolites with archaocyaths in climax stage\nPrevisouly dated as lower Tommotian but now assigned to Atadanian ',60,111,-2576107,644809,'Russia','Asia',624,'2561',60.1667,111.6667,'','',3.20310509398,-58.4645667063,3.20310509398,-58.4645667063,3.20310509398,-58.4645667063,-10.2984,-7.46767,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Verchne Kii, Siberia',2231,'','Cambrian','Terreneuvian','Stage 2','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',527,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'90','2228',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1413,1405,'',58,106,-2624611,1010531,'Russia','Asia',624,'',58.6667,106,'','',0.422695351319,-64.7668102831,0.422695351319,-64.7668102831,0.422695351319,-64.7668102831,-12.5635,-3.98228,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kii, Siberia',2232,'','Cambrian','Terreneuvian','Stage 2','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',527,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'90','2228',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',1,'Potential reservoir',1405,214,'',58,105,-2595135,1041552,'Russia','Asia',624,'1413',58.3333,105.8333,'','',0.630605918574,-64.4919984891,0.630605918574,-64.4919984891,0.630605918574,-64.4919984891,-12.2696,-3.79814,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yuktansk, Siberia',2233,'','Cambrian','Terreneuvian','Stage 2','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',527,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'700',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1405,1406,'',59,104,-2708486,1041118,'Russia','Asia',624,'1413',59,104.8333,'','',-0.214814849664,-64.5036987064,-0.214814849664,-64.5036987064,-0.214814849664,-64.5036987064,-13.0605,-3.49193,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Verchne Chon, Siberia',2234,'Usol\'ye','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',520,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'700','2233',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,'3','Binder 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','1','Present',0,'No or unknown reservoir potential',1405,1406,'Osa horizon.\nPreviously dated as lower Tommotian, now assigned to Atadabanian',59,109,-2595309,792152,'Russia','Asia',624,'214, 1413, 2561',59.5833,109.3333,'','',2.96942430579,-57.1754591993,2.96942430579,-57.1754591993,2.96942430579,-57.1754591993,-10.0792,-6.15721,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Markovo, Siberia',2235,'','Cambrian','Terreneuvian','Stage 2','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',527,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'90','2228',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',1,'Potential reservoir',1405,1406,'',57,106,-2439620,1089842,'Russia','Asia',624,'214, 1413',57.1667,106.5,'','',1.76859243274,-64.0531814574,1.76859243274,-64.0531814574,1.76859243274,-64.0531814574,-11.05,-3.80622,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Muratovo, Donbas, Donetz',2236,'','Carboniferous','Mississippian','Serpukhovian','upper Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',320,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick','240',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','2','Algae','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','2','Green algae','20','60','20',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1409,1410,'Donets aulakogene.\nGas field. Reef top in 3000 m. Asymmetric. N slope dipping 1-1.5°, S slope dipping 5-10°.\nEncrusting microbes and algae as main reef builders. Girvanella, Tubiphytes, bryozoans (Fenestellidae).\nRare corals (Lithostrotion).\n220-240 m thickness.\n',48,38,487234,3227027,'Ukraine','Europe',301,'1413, 1525',48.8,38.7333,'','',-11.5353417017,23.9116044827,-11.5353417017,23.9116044827,7.476993031,4.09895815705,3.77729,29.3541,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yuzhny Umet, Volgograd',2238,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','150',NULL,NULL,NULL,'4','More than 1000 m',NULL,'45',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1416,1413,'Eastern slope of Voronezh anteclise.\nAbout 150 m thick including Sakmarian-Artinskian interval.\nMicrobes and Tubiphytes.',50,45,2508084,4570285,'Russia','Asia',624,'1415',50.2833,45.3333,'','',16.4407266701,41.2791479797,16.4407266701,41.2791479797,23.6787965026,19.6332789837,15.225,39.1273,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chukhonastovka, Volgograd',2239,'','Permian','Cisuralian','Sakmarian','Sakmarian-Artinskian',283.50,298.90,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',284,3,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','170',NULL,NULL,NULL,'4','More than 1000 m',NULL,'45','612',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1415,1413,'Sakmarian to lower Artinskian.\n170 m thick (including Asselian interval).\nMicrobes and Tubiphytes.',49,44,2972993,4879106,'Russia','Asia',624,'',49.8333,44.9167,'','',16.2725993955,41.7663511622,16.2725993955,41.7663511622,24.6622948012,24.9633767599,16.3202,40.5336,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chukhonastovka, Volgograd',2240,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','170',NULL,NULL,NULL,'4','More than 1000 m',NULL,'45','2238',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',1415,1413,'see reef 2239.',49,44,2438207,4586100,'Russia','Asia',624,'',49.8333,44.9167,'','',15.9226303468,41.3571321839,15.9226303468,41.3571321839,23.2166704833,19.9013260554,14.7105,39.2268,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tarasovo, Volgograd',2242,'','Devonian','Upper Devonian','Frasnian','middle-upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',378,3,'1','Seismic data available ',1,'True reef','4','More than 500 m thick','600',NULL,NULL,NULL,'4','More than 1000 m',NULL,'80','2241',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','10','90',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','1','Less than 30% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',1417,1413,'See reef 2241',50,44,-114546,2427444,'Russia','Asia',624,'',50.55,44.8,'','',-4.62399360984,6.51387610192,-4.62399360984,6.51387610192,20.0672478936,-57.253205514,-2.30162,22.002,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ilych River, Urals',2244,'','Ordovician','Upper Ordovician','Hirnantian','upper Ashgillian',445.20,450.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','110','3','101-1000 m wide',NULL,'3','More than 100 m',NULL,'550','993',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','1','Corals','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','17','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1420,1022,'Massive structure 1x1.5 km across.\n110 m thick.\nFramework dominated by encrusting Girvanella, Rothpletzella and other microbes.\nSubordinate heliolitids (Plasmoporella, Heliolites, Propora), tabulate and rugose corals and hydroid problematica (Fistulella).',63,58,-2592879,1332088,'Russia','Asia',624,'',63,58.75,'WAHR','24294',-13.0079951459,-48.2089802243,-10.6404100902,-48.2317925694,-10.6404100902,-48.2317925694,-15.109,9.64392,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lec-Elec River, Pechora',2245,'','Silurian','Llandovery','Telychian','upper Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,430,'Early Silurian (late Llandovery, 430 Ma)',430,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','80',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','0','70',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1420,1973,'Patch reefs composed of an alternation of microbial-coral and stromatoporoid boundstones. \n60-80 m thick.\nInterbeds of microbial mudstones with Stromatactis.\nframework dominated by encrusting Girvanella, Garwoodia, Ikella with subordinate stromatoporoids, favositids and bioclastic debris.',67,64,-29741,421886,'Russia','Asia',624,'',67.0833,64.5,'','',4.45016114638,-51.8004059727,4.45016114638,-51.8004059727,4.45016114638,-51.8004059727,-3.68144,4.41341,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bolshaya Usa River, Polar Urals',2246,'Ovinparma','Devonian','Lower Devonian','Lochkovian','upper Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,415,'Early Devonian (Lochkovian, 415 Ma)',413,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','30','2','10 - 100 m wide',NULL,'2','10 - 100 m','110',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'3','Microbes','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','10','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','2','Intense',0,'No or unknown reservoir potential',1420,2268,'Extensively dolomitized.\nAbout 170 m thick.\nStromatolites predominate.\nCalcimicrobes: Girvanella, Renalcis, Ikella.\nStromatoporoids, branching tabulates and rare rugose corals only in lower part of the reef.',67,64,752976,864014,'Russia','Asia',624,'',67.4167,64.5667,'WAHR','24015',26.6304890308,-42.2704874564,26.6304890308,-42.2704874564,39.332860604,-103.301373833,7.17858,3.67815,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Verchnyaya Pechora River',2247,'','Devonian','Lower Devonian','Pragian','Pragian',407.60,410.80,8,'middle Pridolian - middle Pragian',412,410,'Early Devonian (Pragian, 409.2 Ma)',409,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','2','Algae','64','Microbes/stromatolites  - (cements) - (worm tubes)','4','Others','0','60','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1420,2268,'300 m thick buildup (locally up to 1000 m).\nMicrobial associations comprise more than 50 % of all reef boundstones.\nCoalesced small biostromes and bioherms (3 m thick).\n25 species of calcareous algae in whole region\nPlenty of reef debris flows.\nContinuing into Emsian.',61,58,803570,1479515,'Russia','Asia',624,'',61.8333,58.6667,'WAHR','24018',24.6063511628,-31.9968361302,24.6063511628,-31.9968361302,35.7636294722,-92.5595508105,2.65189,11.0609,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lemva River, Pechora, Urals',2248,'','Devonian','Lower Devonian','Pragian','Pragian-Emsian',393.30,410.80,9,'late Pragian - Eifelian',395,410,'Early Devonian (Pragian, 409.2 Ma)',407,2,'0','Outcropping reef ',3,'Mud mound or bank','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'17',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','6','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1420,2268,'Pragian to lower Emsian.\nUp to 1000 m thick reef complex extensively dolomitized.\nAppears to be microbial mound. Ikella, Garwoodia, Ortonella and Girvanelly at base.\nCavernous porosity.',65,61,1019482,1058463,'Russia','Asia',624,'',65.75,61.2,'WAHR','24019',20.3798213346,-30.5347747676,20.3798213346,-30.5347747676,31.8590910543,-91.3894507379,3.86549,9.44487,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lec-Elec River, Pechora',2249,'','Devonian','Lower Devonian','Emsian','Pragian-lower Emsian',393.30,410.80,9,'late Pragian - Eifelian',395,410,'Early Devonian (Pragian, 409.2 Ma)',407,2,'0','Outcropping reef ',2,'Reef mound','4','More than 500 m thick','580',NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','40','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1420,0,'Pragian part is 360 m thick.\nLower Emsian part is 220 m thick.\nWetheredella-Stachyodes boundstones associated with Ikella-Fistulella, and Solenopora-metazoan boundstones.\n',67,64,1211816,917877,'Russia','Asia',624,'',67.0833,64.5,'WAHR','81602',21.4477305878,-32.1858805671,21.4477305878,-32.1858805671,32.4474840862,-93.4934507857,5.1981,8.12039,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Olysya, Bolshaya Nadota River, Urals',2251,'','Carboniferous','Mississippian','Visean','upper Visean-Serpukhovian',323.20,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',326,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','200',NULL,NULL,NULL,'4','More than 1000 m',NULL,'4',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1420,0,'Massive to poorly bedded, recrystallized structure.\n200 m thick. 2 x 4 km across.\nStromatolitic boundstones predominate. \nIrregular cavities with filled by fibrous blocky calcite cements.\nCrinoids, brachiopods, gastropods, bryozoans occur locally.\nReef talus in the east.',64,58,2930285,2596527,'Russia','Asia',624,'',64,58.5,'','',-2.7404641976,15.5979240611,3.02822829809,17.5030401074,25.175619858,-9.36927072619,21.153,23.8349,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Washington Co., Arkansas',2272,'Pitkin','Carboniferous','Mississippian','Serpukhovian','Chesterian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',326,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','50','50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','20','0',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild','1','Present','1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1431,1517,'Early Serpukhovian\n15-20 m thick, 50 m lateral extension.\nType I thrombolitic mounds with about 3 m synoptic relief.\nInterfingering with oolitic and bioclastic grainstones.\nReticulate framework and encrusted metazoans.\nThrombolites-encrusting bryozoans-fenestrate bryozoans (Archimedes dominant)-encrusting forams-spicular alga as main mound builders.\nTyrpanites and acrothoracican barnacle borings according to ref. 1517.',35,-94,-1594493,-3902270,'United States','North America',101,'',35.9167,-94.3333,'WAHR','76852',-23.6273359116,-49.8365235421,-23.6273359116,-49.8365235421,-11.4589033353,-71.3967705422,-13.1208,-37.3786,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Madison Co., Arkansas',2273,'Pitkin','Carboniferous','Mississippian','Serpukhovian','Chesterian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',326,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','50','50','2272',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','20','0',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild','1','Present','1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1431,1517,'See reef 2272.',36,-93,-1611449,-3864836,'United States','North America',101,'',36,-93.9167,'','',-23.8571006926,-49.5519373979,-23.8571006926,-49.5519373979,-11.6038058507,-71.0745847027,-13.2498,-37.0473,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Searcy Co., Arkansas',2274,'Pitkin','Carboniferous','Mississippian','Serpukhovian','Chesterian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',326,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','6',NULL,NULL,NULL,'2','10 - 100 m',NULL,'50','2272',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1431,0,'Type II thrombolitic mounds of ref. 1431.\n6 m synoptic relief.\nThrombolites-encrusting bryozoans-fenestrate bryozoans-encrusting forams-spicular alga as mound builders.\n\nPhylloid algae more common than in type I mounds (reefs. 2272, 2273).',35,-92,-1717823,-3765599,'United States','North America',101,'',35.8167,-92.5333,'WAHR','76853',-24.8765336703,-49.0032103987,-24.8765336703,-49.0032103987,-12.4365977042,-70.2855656005,-14.0429,-36.2113,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Battle Mountain, Nevada',2275,'Harkless','Cambrian','Series 2','Stage 4','upper Botomian - Toyonian',504.50,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',513,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','15','20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','58','Archaeocyaths - microbes (Renalcis, Epiphyton, Girvanella) - corals',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1433,1995,'Dominated by Renalcis and Epiphyton. Proaulopora.\nArchaeocyathids (important taxa only): Mackenziecyathus, Siderocyathus, Keriocyathus, Archaesycon, Molybdocyathus.\n\nAbstract of ref. 1995:\nAbstract: Several new occurrences of archaeocyathan-calcimicrobe-built reefs have been discovered in the upper Harkless Formation (Bonnia-Olenellus Zone) in\nEsmeralda County, Nevada. Initial analyses of the paleoecology of these reefs show that the community structure consisted of several genera of archaeocyaths acting as the framework entity with calcimicrobes acting as the binding entity. Since the reefs are found in the upper Harkless, they are among the youngest known\nmetazoan-built reefs in western North America and represent the last pulse of metazoan reef building prior to their global disappearance in the Middle to Late\nCambrian. The mechanism or mechanisms that contributed to the demise of the metazoan reefs are unknown; therefore, we are studying these reefs in part to test hypotheses concerning the collapse of the Early Cambrian metazoan reef communities. \n\nThese reefs contain the typical assemblage of Early Cambrian reef dwellers such as trilobites, echinoderms, and brachiopods; however, at one locality coralomorphs\nare conspicuously present. These coralomorphs are approximately 12 cm long by 18 cm wide, are found scattered throughout the reefs, and constitute only a small percentage of the reef by volume. The coralomorphs have definite polygonal corallites which do not share walls, and resemble cerioid tabulate corals without obvious tabulae. Septa occur as obscure processes that project into the center of the corallites, dividing the corallites in half. These coralomorphs are similar to the genus Rosellatana, Kobluk, 1984 from the Lower Cambrian Cassiar Mountains of British Columbia. ',41,-116,-1987590,-9240912,'United States','North America',101,'',41.0333,-116.9833,'WAHR','81004',34.1473202567,-132.518514834,34.1473202567,-132.518514834,34.1473202567,-132.518514834,1.19637,-92.7579,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hunyuan, Shanxi',2302,'Gushan-Changshan','Cambrian','Series 3','Guzhangian','Gushanian',497.00,500.50,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',497,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1450,0,'Storm dominated ramp system.\nMounds composed of stromatolites, microbial laminites, oncolites, cyanobacteria (Epiphyton, Girvanella etc.), crinoids, bryozoans.\nUp to 3 m thickness, 0.5 m to 6 m across.\nThrombolitic buildups in Gushan Formation.\nStromatolitc buildups in Changshan Formation.',39,113,5883571,-16082198,'China','Asia',602,'',39.7,113.6667,'','',20.443279721,103.886876808,20.443279721,103.886876808,20.443279721,103.886876808,-5.23364,137.632,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Qinhuangdao, Hebei',2303,'Gushan','Cambrian','Series 3','Guzhangian','Gushanian',497.00,500.50,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',498,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1450,0,'Storm dominated ramp system.\nSee also reef 2302.\nThrombolitic buildups in Gushan Formation.',39,119,5947060,15634995,'China','Asia',602,'',39.9333,119.5833,'','',18.2991865889,99.6328527928,18.2991865889,99.6328527928,18.2991865889,99.6328527928,-1.28692,139.9,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hunyuan, Shanxi',2304,'','Cambrian','Furongian','Lawsonian','Fengshanian',491.00,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',491,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1449,0,'Change from storm dominated ramp-system to epeiric carbonate platform.\nStromatolitic buildup.',39,113,5860529,15966555,'China','Asia',602,'',39.7,113.6667,'','',20.0435278133,103.712647052,20.0435278133,103.712647052,20.0435278133,103.712647052,-9.52079,132.18,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lishi, Shanxi',2305,'','Cambrian','Furongian','Lawsonian','Fengshanian',491.00,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',491,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1449,0,'See reef 2304.',37,111,6071625,-15866699,'China','Asia',602,'',37.5,111.1667,'','',22.9031389901,104.455986252,22.9031389901,104.455986252,22.9031389901,104.455986252,-12.3606,132.964,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bayan Gol, Zavkhan Basin',2308,'Bayan Gol','Cambrian','Terreneuvian','Fortunian','Nemakit-Daldynian',529.00,541.00,1,'Nemakit/Daldynian - Toyonian',520,540,'Cambrian/Precambrian boundary (541 Ma)',535,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','2',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','1','Binder 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',1452,0,'Calcimicrobial domal bioherms, up to 1 m in height and 2 m in diameter. \r\nDominated by Korilophyton. Tarthinia is a minor component.\r\nBioherm stacks as substrate for domal stromatolites.\r\nShould be plate 419.\r\n\r\nAbstract of ref. 1452: The Neoproterozoic-Cambrian succession in the Zavkhan Basin of western Mongolia preserves early Cambrian bioconstructions of Nemakit-Daldynian to Botomian age. As elsewhere (Siberia, Morocco), the Nemakit-Daldynian bioconstructions in the upper Tsagaan Gloom Formation to lower Bayan Gol Formation interval were purely calcimicrobial. Spectacular calcimicrobial \'patch reefs\' of presumed Tommotian age are present in the lower Bayan Gol Formation. In contrast, late Atdabanian-early Botomian bioconstructions are varied and well developed in the upper Salaany Gol Formation including, in addition to calcimicrobial bioherms, Gordonophyton-Razumovskia crusts, radiocyathan-archaeocyathan bioherms and thickets of the ramose archaeocyath Cambrocyathellus.\r\n\r\nThese latter Zavkhan Basin buildups show some ecological and sedimentological features in common with coeval bioconstructions in South Australia, which also developed under a tectonically active regime.',46,96,-1633775,3507531,'Mongolia','Asia',NULL,'',46.7,96.3,'WAHR','22947',1.84921884439,-65.9959237658,1.84921884439,-65.9959237658,1.84921884439,-65.9959237658,-6.24268,5.54393,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-07-23 16:06:01'),('Tayshir, Zavkhan Basin',2309,'Salaagol ??','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',524,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','3',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','1','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1452,0,'Calcimicrobial patch reefs in sandstone.\r\nVery shallow water. Growth up to sea level indicated by flat upper tops.\r\nMounds up to 0.7 m thick and 3 m in diameter.\r\nShould be plate 419.',46,96,-1635979,3523966,'Mongolia','Asia',NULL,'',46.7,96.5167,'WAHR','22948',5.39617349561,-52.4699182028,5.39617349561,-52.4699182028,5.39617349561,-52.4699182028,-3.28235,5.57115,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kotuikan River, Siberia',2311,'Medvezhin','Cambrian','Terreneuvian','Stage 2','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',527,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','2',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1453,0,'Thrombolite boundstone biostrome with Renalcis texture. Individual heads up to 1.2 m high and 2.1 m wide. \nAssociated well-stratified channel grainstones.',70,103,-3954924,226658,'Russia','Asia',624,'',70.6167,103.4833,'WAHR','50431',-9.48408159728,-71.5612304711,-9.48408159728,-71.5612304711,-9.48408159728,-71.5612304711,-24.245,-6.86496,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wadi Arus, Wadi Hajar',2321,'','Jurassic','Upper Jurassic','Tithonian','upper Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',146,3,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,'3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1470,0,'Up to 3 m thick beds consisting of microbialite boulders.\nNo in situ reef described.',14,48,-1962373,3787553,'Yemen','Asia',503,'',14.35,48.3833,'','',-23.0448443784,38.2304196525,-23.0448443784,38.2304196525,-19.8811948163,34.0403741359,-12.829,31.6527,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Marjum Pass, Central Hourse Range',2330,'Marjum','Cambrian','Series 3','Drumian','middle Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',504,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2443,0,'This reef number previously Pen Island Llandovery/Wenlock. More detailed stratigraphy required replacement.\n\nThe mud mounds are thin (<2 m), closely spaced, laterally linked, symmetrical domes composed of massive, fenestral, peloidal\nto clotted microspar with sparse unoriented, poorly sorted skeletal material,\ncalcitized bacterial(?) filaments/tubes and abundant fenestrae and stromatactoid\nstructures.',39,-113,342914,-8268104,'United States','North America',101,'',39.2542,-113.3611,'','',30.9168869951,-132.788698093,31.7006261756,-127.743490579,31.7006261756,-127.743490579,-0.562711,-91.8452,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Curuk Dagh, Antalya',2338,'','Triassic','Lower Triassic','Induan','Induan',251.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',250,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','1','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1476,0,'Stromatolitic microbialites form mounds up to 40 cm thick (LLH type).',36,30,-750333,3044253,'Turkey','Asia',522,'',36.6833,30.4667,'','',-1.07664076423,38.5813210528,-1.07664076423,38.5813210528,-1.97446669355,33.743514772,-10.8419,30.0448,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vedi, Transcaucasia',2339,'','Triassic','Lower Triassic','Induan','Induan',251.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',250,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2',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','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1476,0,'2 m thick domal microbial biolithite, overlain by bedded platy lime mudstones and microbial limestones.',39,45,1630619,4246667,'Armenia','Europe',526,'',39.8333,45,'','',9.01726493783,56.7288450989,9.01726493783,56.7288450989,16.309613066,53.5137265006,1.54652,37.6126,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Abadeh',2340,'','Triassic','Lower Triassic','Induan','Induan',251.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',250,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1477,0,'Several m thick zone of \'algal biolithite\'.\nStromatolites-thrombolites unit.',31,52,1236038,5572511,'Iran','Asia',505,'',31.1,52.6667,'','',-0.782294722603,61.1065817884,-0.782294722603,61.1065817884,3.82705527116,60.0458443672,-3.22541,47.2225,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ponte Arverino, Terni, Umbria',2343,'Monte Cetona','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 ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,'1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1480,0,'Lower member of Monte Cetona Fm.\nThrombolite mounds\nDeeper part of homoclinal ramp.',42,12,2396101,1587887,'Italy','Europe',344,'',42.5667,12.65,'','',23.7156143929,25.8523608942,23.7156143929,25.8523608942,19.9625110961,24.3671024813,28.3412,12.0061,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Épine',2362,'','Jurassic','Upper Jurassic','Oxfordian','upper middle 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','2','10 to 100 m thick','11',NULL,NULL,NULL,'1','Less than 20 m','20',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1490,0,'In situt reefs up to 11 m thick and 20 m across.\nDiverse macro- and microborings.\nHigh species diversity, but low ecological diversity.\n\nAbstract of ref. 1490\nDuring the late middle Oxfordian, patch reefs grew on the northern margin of the Paris Basin. According to the facies analysis of the reef and inter-reef sediments, the environment was a warm, clear and agitated sea with highly episodic sedimentation. The bioherms were a short-lived phenomenon during the third phase of regional reefal development. Sequence stratigraphically, they are associated with a highstand system tract. Volumetrically and trophically dominant organisms were microbes now represented by massive clotted leiolite, \'stalactitic\' hemispheroids with purely thrombolitic texture are restricted to open caves. Corals were of structural, reef-building importance due to their rapid upward growth. The patch reefs are characterised by thickets of ramose corals which developed a very open framework. In the vicinity of these patch reefs, though in hydrodynamically higher-energy environments, grew thickets of more stoutly branched corals. However, they are rarely preserved in situ and are generally represented as abundant coral rubble. The reef taxa are characterised by the notable absence of several groups (e.g. oysters, serpulids, bryozoans, pectinids) occurring at other localities where reefs of similar age developed in similar environmental conditions. The reefs also have strikingly modern aspects to them, in particular the presence of cryptic elements within caves and a sponge-dominated borer association. Dwellers belong to various life-form types although encrusting taxa are exceedingly rare. This may be explained by the presence of soft microbial films on most surfaces. The palaeoecological analysis suggests that the major controls on faunal composition and high diversity were elevated nutrient levels, highly episodic sedimentation and probably seasonal environmental disturbances. Structural and functional aspects of the reef community (grazers trigger framebuilders, borers trigger binders, binders hamper borers) allow ecological comparisons to be made with contemporaneous, as well as Recent, reefs. The unique combination of ecological factors resulted in a specialised, previously undescribed, community which differs from both Tethyan and northern localities in various aspects. These include cavities with cryptofauna, prominence of grazing gastropods and high faunal diversity in a microbially dominated build-up. ',49,4,4852996,707157,'France','Europe',331,'',49.6056,4.4333,'WAHR','11084',28.1548035075,22.3594089078,28.1548035075,22.3594089078,34.3305365186,23.0173333059,40.3824,13.6531,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('H2 1/90 well, Rügen, Baltic Sea',2363,'','Permian','Lopingian','Changhsingian','Zechstein 1 (Werra)',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick','18',NULL,NULL,NULL,'2','10 - 100 m',NULL,'300',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','6','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1495,0,'About 18 m thick stromatolite-bryozoan boundstones with some intercalations of grainstones, packstones and wackestone.\nOne horizon with rudstones.\nBryozoans:\nFenestella\nThamnopora\nAcanthocladia\nStenopora\nProretopora\n\nAbstract ref. 1495:\nIn the deep borehole H2 - 1/90 of \'Petrobaltic\' joint venture situated 20 km eastward from the Island of Rügen a reef of the basal Zechstein (Upper Permian) was discovered. Litho- and biofacies of this reef were investigated by the authors of this paper. New results allow a new palaeogeographic interpretation of some elder boreholes of Rügen Island.',54,14,2688879,2582562,'Germany','Europe',331,'',54.3167,14.0667,'WAHR','10696',30.7968164496,31.5686574429,30.8002219261,31.5691503361,26.8939948742,26.0517869282,19.9857,23.3415,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rhine graben',2364,'','Paleogene',NULL,NULL,'Eocene-Oligocene',23.00,56.00,NULL,NULL,NULL,50,'Early Eocene (Ypresian, 51.9 Ma)',33,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'25',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','1','Red algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1496,0,'Lens shaped stomatolitic bioherms and algal mounds on fan-delta complexes in the early Rhine rift. \nPartialy eroded by vadose circulation.\n',47,7,5951027,343044,'France','Europe',331,'',47.7,7.3833,'','',45.5313970137,1.9193748903,45.5313970137,1.9193748903,46.1027461151,7.078945919,45.7985,3.29009,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Meiklejohn Peak, southern Nevada',2366,'Lower Antelope Valley','Ordovician','Middle Ordovician','Dapingian','Dapingian',467.30,470.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',468,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','76',NULL,NULL,NULL,'3','More than 100 m','300',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','13','Echinoderms',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1498,1499,'Lower Antelope Valley Limestone.\r\n76 m thick, 300 m long mud mound without organic frame.\r\nTraces of Sphaerocodium, Nuia, small ostracods, trilobits, brachiopods and pelmatozoan plates.\r\nRef. 1498 not seen.',37,-116,485945,-8663124,'United States','North America',101,'',37,-116.75,'WAHR','80054',18.689801824,-122.471250027,18.689801824,-122.471250027,18.689801824,-122.471250027,-6.10915,-85.8376,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Verchnyaya Pechora River',2369,'','Devonian','Lower Devonian','Emsian','lower Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,400,'Early Devonian (Emsian, 400 Ma)',406,3,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1420,0,'See reef 2247.',61,58,803570,1479515,'Russia','Asia',624,'',61.8333,58.6667,'','',19.3456500251,-24.2763121878,19.3456500251,-24.2763121878,31.4026835576,-85.2810189899,2.90018,13.2901,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Neuville quarry',2376,'Neuville','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 ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','4','Stromatoporoids','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)',NULL,NULL,'0','30','70',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1508,2183,'Other localities are Croisette quarry and Tapoumont Buildup.\nMud mound\nStromatactis important.\nNeuville formation.\nStromatoporoids + Phillipsastrea, Alveolites and microbes (Renalcis, Epiphyton, Rothpletzella).\nPhillipsastrea in argillaceous limestone at base.\n',50,4,-2714127,476554,'Belgium','Europe',331,'2565',50.3167,4.1333,'WAHR','76638',-22.6299956183,-12.2723562755,-22.6299956183,-12.2723562755,-3.29190457261,-67.8608042992,-21.974,5.18646,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fort Condé, Givet',2379,'','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 ',3,'Mud mound or bank','2','10 to 100 m thick','25',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1515,0,'Mud mound\n15-25 m thick, 30-45 m diameter.\nBedded at base (crinoid rudstones), massive at top.\nRare sponges (siliceous?), no corals.\nStromatactis important.\nEssentially micrite, but stromatactis important.\nLow diversity.',50,4,-2705243,531255,'France','Europe',331,'',50.1333,4.8333,'','',-22.5993601578,-11.7491614188,-22.5993601578,-11.7491614188,-3.06498058128,-67.4327098519,-21.8931,5.70082,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gudman, Rockhampton, Queensland',2381,'Gudman','Carboniferous','Mississippian','Tournaisian','lower Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',357,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','7','1','Less than 10 m wide',NULL,'2','10 - 100 m','50','1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','7','Bryozoans',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1518,1517,'Initiated on oolitic sands.\nDominated by thrombolites. \nCommon worm tubes.\nMicro-encrusters: Claracrusta(?), Wetheredella, Aphralysia, Mitcheldeania, forams.\nCommon crinoid holdfasts, encrusting forams.\nAbundant ramose bryozoans, syringoporoid corals, solitary and rugose corals.\nHard-substrate borings.',-23,150,-4326843,14529484,'Australia','Oceania',801,'',-23.3833,150.4167,'WAHR','36545',-15.2172344787,147.423513251,-15.2172344787,147.423513251,-33.1486474824,151.86843134,-27.696,141.982,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Carlton Shelf, Bonaparte Gulf, Wester',2382,'Ningbing Group','Devonian','Upper Devonian','Famennian','late Famennian',358.90,372.20,11,'late Famennian - early Visean',351,360,'Devono-Carboniferous Boundary (358.9 Ma)',363,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1519,1982,'Several facies zones are developed.\nBasin, marginal-slope, platform with reef-margin, reef-flat and back-reef.\nGroup includes five formations:\nDjilirri Limeston\nKamilili Fm.\nWungabal Limestone\nGarimala Limestone\nButtons Fm.\n\nExcept for Buttons Fm. all formatins part of reef complex. \nThickness of Ninging Group 171-1166 m.',-15,128,-4003352,12141687,'Australia','Oceania',801,'2004, 1517',-15.25,128.5,'','',-20.7305635803,118.766363048,-20.7305635803,118.766363048,-31.6639822633,152.498423868,-16.3606,118.06,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baelen, Verviers',2383,'','Devonian','Upper Devonian','Famennian','upper middle Famennian',358.90,372.20,11,'late Famennian - early Visean',351,360,'Devono-Carboniferous Boundary (358.9 Ma)',365,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','86','Microbes - sponges - crinoids',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1520,1517,'upper middle Famennian; late marginifera Zone\nThe reefs were surrounded by mainly finegrained\nsiliciclastic sediments, but the relatively\ncontinuous export of bioclasts resulted in the\nmixed siliciclastic-carbonate facies, which surrounds\nthe carbonate bodies.',50,5,-1566304,568335,'Belgium','Europe',331,'',50.5833,5.8333,'WAHR','75672',-31.8642140762,-6.89007856465,-31.8642140762,-6.89007856465,-1.26505537414,-61.1818989736,-17.9489,4.90319,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Richelle, Visé area',2384,'','Carboniferous','Mississippian','Visean','upper Visean',330.90,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',332,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','6','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1521,1517,'Informatiin from ref. 1517.\n\nCampine Basin\nboundstone facies \n (1) a thick crust of calcimicrobes and Aphralysia around small solitary corals (Amplexocarinia sp.), and bryozoans;\n(2) peloidal packstones, with thrombolitic outline; and (3) various stromatactoid cavities.',50,5,-684550,1061085,'Belgium','Europe',331,'2568',50.75,5.6667,'','',-32.7991426877,-2.62050201272,-29.3705558995,-0.770497351776,-4.39564777316,-24.7889365159,-7.13005,7.38341,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-25 17:28:31'),('Namur',2385,'','Carboniferous','Mississippian','Visean','middle Visean',340.00,345.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',337,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'3','Pronounced zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1522,1517,'Information from ref. 1517.',50,4,-740706,1013308,'Belgium','Europe',331,'',50.4667,4.85,'WAHR','76656',-33.1553850404,-3.18212846734,-35.662620822,-4.80666823867,-3.99032247615,-35.4662378058,-9.6405,5.01291,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hadnock, Wales, Great Britain',2386,'','Carboniferous','Mississippian','Visean','Arundian',342.00,345.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',342,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','77','Vermetid gastropods -  microbes',NULL,NULL,'10','90','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present','1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1818,1523,'Vermetid gastropods and microbes forming biostromes in marginal marine setting.\nSmall bioherms up to 25 cm in height.\n',51,-2,-1612687,-44490,'United Kingdom','Europe',331,'',51.8333,-2.6833,'WAHR','76720',-32.0806466939,-8.87901937096,-34.6989596191,-10.8775405613,-4.64834252137,-41.6426000271,-9.81688,-0.0549004,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Stack Cleugh, Bewcastle, England',2387,'','Carboniferous','Mississippian','Visean','Arundian',342.00,345.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',342,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m','13',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','77','Vermetid gastropods -  microbes',NULL,NULL,'10','90','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1523,1517,'Vermetid gastropods and stromatolites forming bioherm in marginal marine setting.\n2 m high, 13 m long.',55,-2,-1182767,-124991,'United Kingdom','Europe',331,'',55.0667,-2.6833,'','',-28.847702901,-8.81598932035,-31.4674145079,-10.7468058141,-1.69449823724,-42.9599374643,-6.63517,-0.636769,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bat Mountain, Mojave Desert, California',2389,'Tin Mountain','Carboniferous','Mississippian','Tournaisian','Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',358,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','40',NULL,NULL,NULL,'3','More than 100 m',NULL,'1',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'90','0','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1526,1517,'Core facies: bryozoan grainstone, bryozoan-crinoid wacke-/packstone and bryozoan packstone\nBryozoans are dominant macrofossils.\n\n\nMound core dominated by allochems (fenestrate bryozoans and crinoids).\nPolymuds and spar make up only 40 % by volume.',36,-116,-1080400,-6176185,'United States','North America',101,'',36.3333,-116.5,'','',-11.9949028957,-65.4790155277,-11.9949028957,-65.4790155277,1.77303971133,-111.287174167,-9.29485,-56.2527,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Brentwood, Arkansas',2390,'Bloyd','Carboniferous','Pennsylvanian','Bashkirian','upper Morrowan',315.00,323.20,13,'Bashkirian - Kasimovian',302,320,'Early Pennsylvanian (Bashkirian, 319.2 Ma)',315,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','12','Foraminifera','13','Algae - encrusting forams',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1527,1517,'Locality doubtful.\nBrentwood Member\nInformation from ref. 1517.',36,-94,-700166,-3093672,'United States','North America',101,'',36,-94,'','',-12.2582574428,-34.4531116087,-15.3095330203,-37.5310196628,-13.2700181032,-53.4974978833,-9.31222,-32.3727,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Verkhoyan',2419,'','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 ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'3','Microbes','1','Corals','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,'1','Present',0,'No or unknown reservoir potential',1557,1536,'\'Algae\' colonial corals and stromatoporoids forming reefs and biostromes.\nSequence 900 m thick.\nLocality and compostition unknown.',65,135,3735634,-2849338,'Russia','Asia',624,'1671',65,135,'','',29.1864674157,-75.6829840391,29.1864674157,-75.6829840391,29.1864674157,-75.6829840391,24.9751,-17.4226,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bulleys Lump, Judge Daly Promot., Nunavut',2431,'Bulleys Lump','Ordovician','Lower Ordovician','Tremadocian','middle-upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',481,3,'0','Outcropping reef ',3,'Mud mound or bank','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1400',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,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1574,0,'Member A\nOuter Shelf edge buildup.\nTogether with upper Member B about 1.5 km syndepositional relief.\nFenestral pelmicrite and fenestral pelsparite predominate. Calcimicrobes associated: Halysis, cf. Hedstroemia, Epiphyton, Renalcis, Girvanella. \nUp to 30 % early marine cement.\n\nAbstract of ref. 1574:\nFour Lower Ordovician buildup categories occur in carbonate platform strata in the Canadian Arctic Islands: outer and inner shelf-margin buildups and outer and inner shelf-interior buildups. The outer shelf-margin buildup in the Bulleys Lump Formation consists mainly of calcirnicrobial biolithite and early marine cement, forming a structure that probably had a depositional relief of more than 1.5 km over contiguous basinal chert and mudrock. The length of the outer shelf-margin buildup is probably more than 1400 km, although it is discontinuously exposed. Inner shelf-margin buildups are smaller, mounded structures, attaining thicknesses in excess of 100 m and widths of several kilometres. A representative inner shelf-margin buildup comprises four distinct microbial facies; the stratigraphically lowest and deepest water facies contains up to 4 m-thick thrombolite mounds surrounded by Conophyton-like stromatolitic pinnacles. The two middle facies consist of numerous, aligned ovoidal thrombolites with thromboidal or columnar stromatolitic interiors and stromatolitic margins. Thrombolites were built mainly by benthic microbial communities, but fleshy and locally well-sclerotized sponges were probably important constructors as well. These thrombolites are overlain by the shallowest water and youngest buildup facies, consisting of cerebroform stromatolites and thrombolites, but which lack the distinctive ovoidal thrombolites of the underlying facies. Zoned inner shelf-margin microbial buildups such as these are previously undocumented. Shelf-interior buildups are composed of thrombolites and stromatolites, forming isolated, I to 5 m-high mounds and coalesced mounds in buildups more than 2.0 km wide. The distribution of the four buildup categories implies a shelf-margin embayment in the central part of the Arctic Islands.',80,-69,1016227,-2914320,'Canada','North America',121,'',80.75,-69.25,'','',25.5052732236,-64.8753895932,25.5052732236,-64.8753895932,25.5052732236,-64.8753895932,-7.99414,-39.3674,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bulleys Lump, Judge Daly Promot., Nunavut',2432,'Bulleys Lump','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 ',1,'True reef','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1400',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,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1574,0,'Member B.\r\nSee reef 2431.\r\nIn addition: Enigmatic tubes (two types).',80,-69,1019003,-3137585,'Canada','North America',121,'',80.75,-69.25,'',NULL,15.975388471,-77.2224192159,15.975388471,-77.2224192159,15.975388471,-77.2224192159,-0.930921,-34.1241,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hawker Bay, Grinell Peninsula, Nunavut',2434,'Blanley Bay','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','105',NULL,NULL,NULL,'4','More than 1000 m','50000','1400','2431',0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'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',1574,0,'Inner shelf-margin buildups composed of thrombolitic limestone. \nLargest is at least 100 m thick and 2-3 km in diameter.\nZonation: Lowest are 1 mud mounds with composed thromboids and Conophyton-like stromatolites, then 2 cerebroform stromatolite facies, then 3 thrombolite facies with clotted core and stromatolitic margin, locally encrusted by lithistid sponges 4 large thrombolite facies with a columnar stromatolitic core.\nOuter shelf interior buildups also present (reef. 2347).',76,-96,1464482,-3519474,'Canada','North America',121,'',76.8,-96.25,'','',29.5083759519,-70.6139674021,29.5083759519,-70.6139674021,29.5083759519,-70.6139674021,-5.13356,-45.2137,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Central Ellesmere Island, Nunavut',2435,'Cape Clay','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','77',NULL,NULL,NULL,'4','More than 1000 m',NULL,'1400','2431',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1574,0,'77 m thick outer shelf-interior buildups.\nSee reef 2434 for more remarks.',78,-84,1190156,-3300826,'Canada','North America',121,'',78.25,-84.6667,'','',27.2561528319,-68.5647087597,27.2561528319,-68.5647087597,27.2561528319,-68.5647087597,-7.00422,-43.0051,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Central Ellesmere Island, Nunavut',2436,'Eleanor River','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','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1400','2432',0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1574,0,'Basal Eleanor River Fm.\r\nInner shelf edge buildup.\r\nSee reef 2434 for more remarks.',78,-84,1063259,-3551734,'Canada','North America',121,'',78.25,-84.6667,'',NULL,23.3270154064,-72.1853791976,23.3270154064,-72.1853791976,23.3270154064,-72.1853791976,-4.45048,-40.7434,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('N Judge Daly Prom., Ellesmere I., Nunavut',2438,'Baumann Fiord-Cape Clay','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1400','2431',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,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1574,0,'Inner shelf interior.\nMarginal marine, interbedded with laminated gypsum.',81,-66,1009882,-2828551,'Canada','North America',121,'',81.3333,-66,'','',25.342683447,-64.0397544386,25.342683447,-64.0397544386,25.342683447,-64.0397544386,-7.97132,-38.5882,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Melville Island, NWT',2439,'','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1400','2431',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,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1574,0,'Several formations with inner shelf interior mounds.\nSmall isolated mounds composed of thrombolites and columnar stromatolites.\n',76,-113,1993185,-3592337,'Canada','North America',121,'',76,-113,'','',33.4837515753,-71.1790560252,33.4837515753,-71.1790560252,33.4837515753,-71.1790560252,-1.30449,-46.3879,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Apsley, N.S.W.',2445,'Nubrigyn','Devonian','Lower Devonian','Emsian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,400,'Early Devonian (Emsian, 400 Ma)',402,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'90',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'30','0','70',0,'no',0,'no',NULL,NULL,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',1591,1662,'Allochthonous blocks of \'algal reef\' limestone in deep water Nubrigyn Fm.\nSourced by platform edge 10 km to the west (Garra Fm.).\nUp to 7 km wide and 100+ m thick blocks.\nAlgal, stromatoporoid and coral boundstones, commonly massive.',-32,148,-2903791,17444110,'Australia','Oceania',801,'',-32.6,148.9833,'','',-28.0082195798,132.684638021,-28.0082195798,132.684638021,-36.3894693707,169.731972953,-14.7658,172.88,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Boree, N.S.W.',2446,'Nubrigyn','Devonian','Lower Devonian','Lochkovian','Gedinnian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,415,'Early Devonian (Lochkovian, 415 Ma)',414,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'90',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','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,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',1591,0,'See reef 2245.',-33,148,-2160377,18983492,'Australia','Oceania',801,'',-33.2667,148.9667,'','',-22.3277210257,126.546393023,-22.3277210257,126.546393023,-45.5132083182,141.362466041,-5.34425,175.376,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cerro La Silla, Jáchal, Argentina',2456,'San Juan','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','4',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)','3','Receptaculitids','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','9','3','Binder guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1607,0,'Collection of Miller \nShallow subtidal intrashelf.\nReef-mounds with lithistid sponges, receptaculids (Calathium) and microbialite. Girvanella dominant 20-30 % (up to 70 %) of mound volume.\n4 sponge species are common. \n4 m thick complex of domal bioherms.\nDistinct flanking beds.\nTwo facies types: \nBio-lithoclastic wackestone/packstone\nMicrobial boundstone.\nBorings present in cryptomicrobial structures (early lithification).',-30,-68,-2208751,-8235754,'Argentina','South America',201,'',-30.1667,-68.75,'WAHR','8704',-25.5652159436,-165.841813239,-25.5652159436,-165.841813239,-25.5652159436,-165.841813239,-38.6838,-128.718,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bachu, Tarim',2457,'Lianglitag','Ordovician','Upper Ordovician','Katian','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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,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',1910,1730,'Webby, pers. comm.',39,78,-507083,12545423,'China','Asia',602,'',39.75,78.5,'',NULL,-3.73754162981,53.5696595868,-3.73754162981,53.5696595868,-3.73754162981,53.5696595868,-36.0985,112.651,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cow Head, Newfoundland',2458,'','Ordovician','Lower Ordovician','Floian','Arenigian-Llanvirnian',468.00,472.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',467,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder 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',1609,0,'Cow head Group. Beds 10 and 12.\nRedeposited reefal blocks in deep water limestone.\nShelf margin boundstones, grainstones, packstones, wackestones.\nBoundstones dominated by microbes (Renalcis, Epiphyton, Girvanella) together with archeoscyphid sponges.\nAlga Halysis, some Pulchrilamina-like organisms, Wetheredella-like tubules also present.',49,-57,-2633628,-3899835,'Canada','North America',121,'',49.9167,-57.8167,'WAHR','80771',-1.58741932624,-83.9445473356,-3.99718876503,-84.8172533466,-3.99718876503,-84.8172533466,-30.2462,-45.8327,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Los Navalucillos-Pena Hueca, Toledo',2464,'Los Navalucillos Limestone','Cambrian','Series 2','Stage 3','upper Ovetian',509.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',519,3,'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','2','6 to 24 reef building species','9','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',1614,0,'Abstract ref. 1614:\nWe have studied the carbonates with Archaeocyatha in the outcrop of Los Navalucillos-Pena Hueca (Montes de Toledo occidentales), that belong to Los Navalucillos Limestone. These organic carbonates are, for the most part, of algae activity, and to a smaller extent to that of other organisms. Archaeocyatha and Trilobites. On the whole it is a trans-reef area with small mounds of algae and archaeocyatha, and levels with cups and organic debris accumulations. We described the species: Rotundocyathus salebrosus (Vologdin, 1931); Sibirecyathus disepimentalis Vologdin, 1940b; Afiacyathus alloiteaui Debrenne, 1964; Rasetticyathus iglesiensis DebrenneE, 1971; Inessocyathus spatiosus (Bornemann, 1887); Protopharetra polymorpha Bornemann, 1887; Pycnoidocyathus toledani Perejon, 1976, and Anthomorpha sisovae (Vologdin, 1940a); this association is characteristic of the Upper Ovetiense.',39,-4,-5854138,8730300,'Spain','Europe',304,'',39.6667,-4.6333,'WAHR','81295',-66.3052044965,-4.12640741767,-66.3052044965,-4.12640741767,-66.3052044965,-4.12640741767,-49.8542,109.286,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cheyne Point, Griffith Is., Nunavut',2466,'Douro','Silurian','Ludlow','Ludfordian','upper Ludlow',423.00,425.60,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',420,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','5','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',1617,0,'Abundant heliotids in mud mound flanking beds.\nCollection of Alroy with only 2 coral species indicated.\n\nAbstract of ref. 1617:\nHeliolitine corals occur in Upper Silurian strata of the topmost Douro, lower Barlow Inlet, and lower Somerset Island formations in the Boothia Uplift region. The fauna includes Heliolites (nine species), Propora (two species), the stelliporellid genera Ponollites (three species) and Stelliporella (one species), and the plasmoporid Squameolites (one species). Species present but not previously reported from the region include Heliolites arcuatus Bondarenko, Heliolites uksunayensis Mironova, Stelliporella ilensis Bondarenko, Podollites assitus new species, Podollites parryi new species, Podollites plectilis new species, Propora tubulata (Lonsdale) and an unidentified species of Propora. All species occur in reef and reef-associated facies of open carbonate shelf and ramp settings. In restricted nonreefal carbonate shelf settings, diversity attenuates to a minimum, exemplified by numerically abundant monospecific assemblages of Heliolites uksunayensis. Six of the 16 morphotaxonomic units recognized compare with species reported previously in Silurian faunas of Kazakhstan and Mongolia. Combinations of characters in the species attributed to Podollites support revision of the genus, possibly to include Derivatolites and Tarbagatailites, in a group morphologically intermediate between Stelliporella and Heliolites.',74,-95,381940,-3459468,'Canada','North America',121,'',74.5333,-95.3,'WAHR','5796',5.52735635473,-73.3948069698,5.52735635473,-73.3948069698,5.52735635473,-73.3948069698,2.7265,-30.9537,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maumee, Ohio',2469,'Lockport','Silurian',NULL,NULL,'Wenlock-Ludlow',423.00,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',422,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','2','Intense',0,'No or unknown reservoir potential',1625,0,'Lockport dolomite.\nMicrobialite-coral reef.\nOnly microbes and small Favosites.\nFavosites showing evidence of stress (stress bands, small size).\nHigh sedimentation rates indicated by growth form and in situ preservation. \nNutrient-rich setting.',41,-83,-3454648,-5025191,'United States','North America',101,'',41.5333,-83.8333,'WAHR','79365',-28.4595100371,-82.4449934595,-28.4595100371,-82.4449934595,-28.4595100371,-82.4449934595,-24.9609,-49.1922,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kosyu River, prepolar Urals',2495,'Ustpalnik','Ordovician','Upper Ordovician','Katian','upper Caradocian',451.00,453.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',452,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','1','Corals','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',1661,1662,'Up to 20 m thick dolomitized  \'algal\' , bryozoan, and tabulate [Lichenaria, Eofletcheria, Lessnikovia  ] coral bioherms.\nTabulates up to 50 cm in diameter.',65,59,-2355746,1117488,'Russia','Asia',624,'',65.6333,59.0333,'','',-23.6669084515,-44.5515719622,-14.4773196739,-48.9819295148,-14.4773196739,-48.9819295148,-16.2525,8.92718,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Karaoba, Tsheljabinskaja',2496,'','Ordovician','Upper Ordovician','Katian','Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','15',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1663,1662,'Less than 15 m thick microbial reefs.',53,61,-3231413,2288001,'Russia','Asia',624,'',53.1667,61.2167,'','',-18.3591496655,18.2497022611,-17.2484138945,18.070190587,-17.2484138945,18.070190587,-6.52609,46.3084,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Podmakennaya Tunguska River, Siberia',2497,'Chunya','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','120',NULL,NULL,NULL,'4','More than 1000 m','2000','1300',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','2','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1664,1724,'300 m thick, 200 km wide and 1500 km long stromatolite reef tract.',61,91,-1980219,1741262,'Russia','Asia',624,'1662',61.6667,91.5,'','',-2.78697205788,-25.9424643568,-2.78697205788,-25.9424643568,-2.78697205788,-25.9424643568,-5.3495,17.0981,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Podmakennaya Tunguska River, Siberia',2498,'Chunya','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m','2000','1300','2497',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,'1','Low zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1664,1724,'See reef 2497.',61,95,-1867897,1557480,'Russia','Asia',624,'1662',61.8333,95.4167,'','',-1.1860323778,-26.8919841615,-1.1860323778,-26.8919841615,-1.1860323778,-26.8919841615,-4.39973,15.4919,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Podmakennaya Tunguska River, Siberia',2499,'Chunya','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m','2000','1300','2497',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,'1','Low zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1664,1724,'See reef 2497.',60,98,-1581727,1503849,'Russia','Asia',624,'1662',60.25,98.5,'','',0.882084004093,-26.2163712249,0.882084004093,-26.2163712249,0.882084004093,-26.2163712249,-2.2605,15.0947,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Podmakennaya Tunguska River, Siberia',2500,'Chunya','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m','2000','1300','2497',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,'1','Low zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1664,1724,'See reef 2497.',60,101,-1501526,1372937,'Russia','Asia',624,'1662',60.25,101.1667,'','',2.01507992584,-26.900048364,2.01507992584,-26.900048364,2.01507992584,-26.900048364,-1.59196,13.9522,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Stepnyak, Kazachstan',2505,'Mailisor','Ordovician','Upper Ordovician','Katian','late Caradocian',451.00,453.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',452,3,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','150','4','More than 1000 m wide','1500','4','More than 1000 m','15000','100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','0','100','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1668,1662,'See reef 2503.',52,70,-2451653,7223830,'Kazakhstan','Asia',301,'',52.8333,70.75,'','',-24.0735891412,27.6723714096,-15.4522273383,19.8515207234,-15.4522273383,19.8515207234,-3.44711,49.008,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mailisor Lake, Kazachstan',2506,'','Ordovician','Upper Ordovician','Katian','Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'18',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1669,1668,'Position doubtful.\nAtoll structure.\nCalcimicrobial rim with bryozoans, brachiopods, coral.\nBiostromal \'algae\' in the lagoon.',52,65,-2886486,6889688,'Kazakhstan','Asia',301,'',52.5,65.6667,'','',-15.6562092611,18.8800832581,-14.550711788,18.7209254958,-14.550711788,18.7209254958,-4.40053,48.0918,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lake Alakol, Kazachstan',2507,'Uzunbulak','Ordovician',NULL,NULL,'Darriwilian-Caradocian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',460,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','50',NULL,NULL,NULL,'4','More than 1000 m','1000',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1668,1662,'Reef complexes up to 50 m thick and 1 km across, smaller\n1-1.5 m thick microbial patch reefs at periphery\nSome larger reefs may be present.',46,81,-1793469,8275981,'Kazakhstan','Asia',301,'',46,81.25,'','',-16.1611725272,33.5502044173,-16.1611725272,33.5502044173,-16.1611725272,33.5502044173,-3.95474,57.542,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Selennyakh Range, Indigirkar River',2510,'Taryn-Yuyakhsk','Ordovician',NULL,NULL,'Darriwilian-Caradocian',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,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1671,1662,'Several km long biohermal massifs with \'algae\' and tabulates.',67,141,545255,-1800749,'Russia','Asia',624,'',67.5,141.8333,'','',7.65425903248,-65.3971769192,7.65425903248,-65.3971769192,7.65425903248,-65.3971769192,2.3395,-6.38795,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chorku, Fergana, Tyan Shan, Kirgisia',2515,'Matcha-Kiziltash','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','3','101-500 m thick','400',NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids',NULL,NULL,NULL,NULL,'40','0','60',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1673,0,'Matcha and Kiziltash Formations.\n100-500 m thick microbial atoll-like mudmounds.\nBarrier complex fringin ferganian carbonate platform.\n60 % clotted micrite.\nSparitic flank facies.\nRare stromatoporoids, corals and bryozoans.\nRare Stromatactis',39,70,679975,3088025,'Kyrgyzstan','Asia',NULL,'',39.95,70.6333,'','',11.631685706,40.4010182145,11.631685706,40.4010182145,11.631685706,40.4010182145,8.73367,42.2299,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Selennyakh, Siberia',2523,'','Silurian',NULL,NULL,'Wenlock-Ludlow',423.00,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',422,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'100',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,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',1662,0,'Massive \'algal\' reefs in 500 m thick strata.',67,143,2588448,-4205295,'Russia','Asia',624,'',67.3333,143,'','',16.2574450766,-86.8362812588,16.2574450766,-86.8362812588,16.2574450766,-86.8362812588,21.6372,-26.099,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chorku, Fergana, Tyan Shan, Kirgisia',2524,'','Devonian','Lower Devonian','Lochkovian','Lochkovian-Pragian',407.60,419.20,8,'middle Pridolian - middle Pragian',412,415,'Early Devonian (Lochkovian, 415 Ma)',411,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','3','Microbes',NULL,NULL,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','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1673,0,'See reef 2515.',39,70,1358936,3896233,'Kyrgyzstan','Asia',NULL,'',39.95,70.6333,'','',13.8813183375,47.9760113204,13.8813183375,47.9760113204,23.9012516859,15.4934261866,6.9435,46.8184,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chorku, Fergana, Tyan Shan, Kirgisia',2536,'','Devonian','Lower Devonian','Emsian','Emsian-Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,395,'Early Devonian (late Emsian, 395 Ma)',397,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','3','Microbes',NULL,NULL,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','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1673,0,'See reef 2515.',39,70,1576064,3950787,'Kyrgyzstan','Asia',NULL,'',39.95,70.6333,'','',8.30079871107,53.8421647435,8.30079871107,53.8421647435,25.8828729154,17.0141110046,5.48483,50.9673,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Drewer, Nordrhein-Westfalen',2538,'','Devonian','Upper Devonian','Famennian','upper Famennian',358.90,372.20,11,'late Famennian - early Visean',351,360,'Devono-Carboniferous Boundary (358.9 Ma)',363,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','9',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'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',1685,0,'< 10 m mud mound resting on black shales of annulate horizon.\nBelow storm wave base.',51,8,-1251138,1311733,'Germany','Europe',331,'',51.5,8.3667,'','',-30.4826992391,-5.47366929993,-30.4826992391,-5.47366929993,0.5022817964,-60.6782806484,-16.3356,5.82407,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Salair Range, Siberia',2540,'Malobachat','Devonian','Lower Devonian','Pragian','Pragian',407.60,410.80,8,'middle Pridolian - middle Pragian',412,410,'Early Devonian (Pragian, 409.2 Ma)',409,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','100',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'3','Microbes','1','Corals','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',1676,1662,'\'Algal\'-coral-stromatoporoid reefs.\nUp to 100 m thick.',54,85,5638847,2819093,'Russia','Asia',624,'',54.25,85.5,'WAHR','84388',61.8687731535,-16.081811984,61.8687731535,-16.081811984,41.7484183475,4.10357742519,31.1637,14.1413,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Amur River',2549,'','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 ',NULL,NULL,'3','101-500 m thick','500',NULL,NULL,NULL,'4','More than 1000 m',NULL,'300',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','1','Corals','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',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',1692,1662,'Position doubtful.\n250-800 m thick reef massif, 300 km long, composed of \'algae\', corals, and bryozoans.',53,125,8222062,6351736,'Russia','Asia',624,'',53,125,'','',69.3710037314,91.5279626132,69.3710037314,91.5279626132,73.0126059886,-63.3098084196,42.01,59.7009,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hingganling ranges, Inner Mongolia',2553,'Hoboshan','Devonian','Middle Devonian','Eifelian','upper Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',393,3,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes',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',1694,1662,'Late Eifelian-early Givetian.\n',48,121,7891744,6318445,'China','Asia',602,'',48.8333,121.5,'','',66.0961553957,82.5500411198,66.0961553957,82.5500411198,77.4045306851,-56.529569137,38.3853,55.7537,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hingganling ranges, Inner Mongolia',2554,'Hoboshan','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 ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes',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',1694,1662,'Hoboshan Fm.\nLate Eifelian-early Givetian.',48,121,6114434,6952763,'China','Asia',602,'',48.8333,121.5,'','',60.7471753123,77.7571801545,60.7471753123,77.7571801545,78.7055289857,-42.7293883531,38.1867,57.056,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tom River, Kemerovo',2555,'Peshcherka','Devonian','Upper Devonian','Famennian','lower Famennian',358.90,372.20,10,'Givetian - early Famennian',375,370,'Late Devonian (early Famennian, 370 Ma)',373,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'60',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','4','Stromatoporoids','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','7','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1695,1662,'Calcimicrobial reefs associated locally with stromatoporoids and bryozoans\nReefs terminated by regression.\n',55,85,4994688,2682071,'Russia','Asia',624,'',55.5833,85.9167,'WAHR','84376',19.5026329796,36.5226166811,19.5026329796,36.5226166811,38.0990521107,0.767158987691,31.5113,20.432,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Atasu-Sagentan, Kazachstan',2556,'','Devonian','Upper Devonian','Famennian','Famennian-Tournaisian',346.70,372.20,11,'late Famennian - early Visean',351,360,'Devono-Carboniferous Boundary (358.9 Ma)',360,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'150',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1696,0,'Algal\' reefs associated with terrigenous-volcanogenic sediments.',48,71,2539350,6155750,'Kazakhstan','Asia',301,'',48.5,71.5,'','',-10.4630022659,55.3371368329,-10.4630022659,55.3371368329,28.524879531,16.2424443109,13.0354,44.6932,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baisa, Yangshuo, Guangxi',2557,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',366,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',957,1662,'Microbial mudmound',24,110,-1541389,9966800,'China','Asia',602,'',24.9167,110.25,'','',-18.6158265558,90.549846353,-18.6158265558,90.549846353,-11.7654533849,107.867453263,-0.0170536,101.228,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ustkut, Siberia',2558,'','Ordovician','Middle Ordovician','Darriwilian','Llanvirnian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',464,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1697,1662,'Algal\' bioherms,1-2m high, and locally associated with phosphoritic gravels',56,105,919426,1678100,'Russia','Asia',624,'',56.75,105.6667,'','',11.5439772883,-32.4312588307,11.5439772883,-32.4312588307,11.5439772883,-32.4312588307,11.5205,14.8438,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ustkut, Siberia',2559,'','Ordovician',NULL,NULL,'Darriwilian-Caradocian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',460,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'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',1697,1662,'See reef 2558',56,105,2347942,1546495,'Russia','Asia',624,'',56.75,105.6667,'','',11.5439772883,-32.4312588307,11.5439772883,-32.4312588307,11.5439772883,-32.4312588307,11.5205,14.8438,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Picadilly, Port au Port, Newfoundland',2571,'Table Point','Ordovician','Middle Ordovician','Darriwilian','Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',464,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','35',NULL,NULL,NULL,'3','More than 100 m','150','10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','87','Girvanella - lithistid sponges - sclerosponges',NULL,NULL,'0','80','20',0,'no',0,'no','1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,'1','Present','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',1711,0,'early Llanvirn\n35 m thick, > 150 m wide stromatactis mud mound.\n< 10 km across.\n15-30 % are calcareous algae and invertebrates.\nOnly conspicuopus megafossils are lithistid sponges and sclerosponges (Lapidipanis). Girvanella oncolites and coarse pelmatozoan debris.\nFragmented foreland basin platform. Mounds nucleated on structural highs.',48,-58,-2776419,-4005878,'Canada','North America',121,'',48.5833,-58.9167,'WAHR','80003',-10.6078830759,-89.5592330845,-10.6078830759,-89.5592330845,-10.6078830759,-89.5592330845,-29.0726,-43.203,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Burnt Island, Newfoundland',2572,'Table Point','Ordovician','Middle Ordovician','Dapingian','upper Whiterockian',467.30,469.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',460,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','87','Girvanella - lithistid sponges - sclerosponges',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','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',1711,0,'See also reef 2571.\nEquivalent to early-middle Darriwilian',51,-55,-2468460,-3725535,'Canada','North America',121,'',51.5472,-55.7583,'','',-4.21806795154,-83.6193894203,-4.59957944212,-83.8842554691,-4.59957944212,-83.8842554691,-28.5532,-42.8061,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bay Fiord, Ellesmere Isl., N.W.T.',2573,'Cape Phillips','Silurian',NULL,NULL,'Wenlockian-Ludlovian',423.00,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',422,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','8','1','Less than 10 m wide','12','2','10 - 100 m','40',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','13','Echinoderms','86','Microbes - sponges - crinoids',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,'1','Present','2','Medium zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1712,0,'Two small mud mounds\n5 m thick, 30-40 m wide and 3-8 m thick and > 10 m wide, respectively.\n4 zones:\n- Basal encrinite packstone/grainstone\n- Middle stromatactoid-rich encrinite packstone/grainstone\n- Upper encrinite packstone and stromatoporoid floatstone\n- ostracod-rich mudstone/wackestone.\nCements abundant in first 3 zones.\nCrinoids with micrite rims.',79,-82,542226,-2838266,'Canada','North America',121,'',79.5,-82.75,'','',7.35908355934,-74.0847102744,7.35908355934,-74.0847102744,7.35908355934,-74.0847102744,4.87505,-26.8536,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Draa ez Zemla',2574,'','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 ',3,'Mud mound or bank','1','Less than 10 m thick','5',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','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','1','Red algae','0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,'1','Present','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',1717,0,'Small (5 m thick) mud mounds on inner carbonate ramp.\nCyanobacterial precipitation indicated by clotted micrite fabrics, spar-filled molds, and preserved filaments. \nThin red algal crusts\nRare rudists and corals.',35,5,2578914,604545,'Algeria','Africa',706,'',35.2833,5.7833,'','',25.1322835532,8.41253576063,25.1322835532,8.41253576063,24.2231736628,5.50091482125,21.1999,5.6027,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jebel Mrhila',2575,'','Cretaceous','Upper Cretaceous','Turonian','Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',92,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','6',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','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','1','Red algae','0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation','1','Present','1','Present','2','Medium zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1717,0,'Mud mounds with crestal bioclastic limestone on top.\n4-6 m thick. \nReef 2574 for more remarks.',35,9,2485800,906634,'Tunisia','Africa',715,'',35.35,9.1333,'','',24.1249685966,11.7557769719,24.1249685966,11.7557769719,22.4709896006,8.44035771056,19.9701,8.08284,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gulf of Gabes',2576,'','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,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','1','Red algae','0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation','1','Present','1','Present','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',1717,2348,'Carbonate mud mounds on outer carbonate ramp.',34,11,2311765,1083019,'Tunisia','Africa',715,'',34.5,11.3333,'','',23.301014516,13.0362619456,23.301014516,13.0362619456,22.1685113012,10.0015799643,19.294,10.0872,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Putilovo quarry, St. Petersburg',2580,'Volkhov','Ordovician','Middle Ordovician','Dapingian','Dapingian',467.30,470.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',470,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','4','2','10 - 100 m wide','30','2','10 - 100 m','50',NULL,NULL,2,'Cold - water','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','13','Echinoderms','93','Microbial micrite - pelmatozoans',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation','1','Present',NULL,NULL,'1','Low zonation','2','Medium zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1721,0,'Mud mounds, described from the Volkhovian (earliest Middle Ordovician), east of St Petersburg (Dronov and Federov 1994), are 4 to 5 m high, 30 to 50 m across, dome-shaped, and with a mud core and micritic crust facies; no reported calcimicrobes. A Trypanites-bored discontinuity surface separates the micritic crust from flanking pelmatozoan bioclastic limestones. Pelmatozoans are thought by Dronov and Federov to have grown on the atoll-like micritic rim, as baffles to the inner lagoonal mud core. Palaeomagnetic drift paths (Torsvik et al 1992) suggest the mud mounds grew in cooler temperate shallow seas.',59,30,-5383643,26190,'Russia','Asia',624,'',59.9667,30.6667,'WAHR','61803',-30.0140744555,-59.8403742616,-30.0140744555,-59.8403742616,-30.0140744555,-59.8403742616,-36.5715,0.439923,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Malyi Karatau, Kazachstan',2581,'','Cambrian','Furongian','Lawsonian','Trempealeauan-Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',488,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','20',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1722,1960,'Latest Cambrian-earliest Ordovician Epiphyton-bearing buildups, up to 20 m high, occur on ocean-facing margins of a seamount in Maly Karatau, Kazakhstan, with smaller mounds scattered in the seamount interior (Cook et al 1991).\nThin section with Girvanella, clotted micrite and Epiphyton shown by ref. 1960',42,70,-120705,9644683,'Kazakhstan','Asia',301,'',42.8333,70.5,'','',-28.8175275365,47.2408428814,-28.8175275365,47.2408428814,-28.8175275365,47.2408428814,-19.6639,58.8756,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Southern Franklin Mts., Texas',2583,'José','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,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,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1725,1723,'Submeter scale stromatolitic mounds.',31,-106,242373,-8584927,'United States','North America',101,'',31.7833,-106.4833,'','',19.2761275071,-119.99802322,19.2761275071,-119.99802322,19.2761275071,-119.99802322,-13.4366,-91.0745,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hare Bay, Newfoundland',2584,'Catoche','Ordovician','Lower Ordovician','Floian','Arenig',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',471,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','70',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1726,866,'Equivalent to Catoche Fm.\nMore than 70 m thick continental margin reef complex. \nSuperposed and coalesced thrombolitic mounds.',51,-56,-2499290,-3749214,'Canada','North America',121,'',51.2667,-56.0333,'','',-0.999052782595,-82.2834642258,-0.999052782595,-82.2834642258,-0.999052782595,-82.2834642258,-30.5142,-46.2104,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jefferson, Missouri',2585,'','Ordovician','Lower Ordovician','Floian','Floian',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','2',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','1','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1727,0,'Domed hemispherical and laminar stromatolites up to 2 m across in intertidal Jefferson dolomite.\r\nPosition doubtful.',38,-92,-2053664,-7001236,'United States','North America',101,'',38.5,-92.5,'',NULL,7.33960152531,-109.52975429,7.33960152531,-109.52975429,7.33960152531,-109.52975429,-22.6585,-76.8815,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Syas, St. Petersburg',2586,'','Ordovician','Middle Ordovician','Dapingian','Volkhovian',467.30,470.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',470,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','5',NULL,NULL,NULL,'2','10 - 100 m','50',NULL,NULL,2,'Cold - water','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','13','Echinoderms','93','Microbial micrite - pelmatozoans',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1721,0,'See reef 2580.',59,32,-5423735,155032,'Russia','Asia',624,'',59.8333,32.8333,'','',-30.645467377,-58.8043181432,-30.645467377,-58.8043181432,-30.645467377,-58.8043181432,-36.6197,1.80209,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Elko Co., Nevada',2592,'','Ordovician','Middle Ordovician','Dapingian','Dapingian',467.30,470.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',468,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m','1300',NULL,NULL,0,'Tropical or unknown','4','Basin','4b','Deep basin (> 200 m)','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,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1732,0,'Meikeljohn type mud mound associated with deep basinal environment.\r\n1.3 km long outcrop.',41,-115,190800,-7994798,'United States','North America',101,'',41,-115.8333,'',NULL,19.624350075,-118.285365657,19.624350075,-118.285365657,19.624350075,-118.285365657,-5.45383,-81.8074,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cow Head, Newfoundland',2593,'','Ordovician','Middle Ordovician','Darriwilian','lower Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',466,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'3','Microbes','8','Serpulids, worms, vermetids','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder 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',1609,0,'Cow Head Group.\nBed 14 reefal clasts.\nTube-work dominated clasts are also present.',49,-57,-2633628,-3899835,'Canada','North America',121,'',49.9167,-57.8167,'WAHR','80774',-9.6637793214,-88.3563533101,-9.6637793214,-88.3563533101,-9.6637793214,-88.3563533101,-28.0087,-41.9761,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mirny Creek, Siberia',2596,'','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',453,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1723,0,'Small \'algal\' buildups.',62,114,1779100,914395,'Russia','Asia',624,'',62.5,114,'',NULL,18.0498595242,-51.0634540686,18.0498595242,-51.0634540686,18.0498595242,-51.0634540686,14.4754,8.17806,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aubenas, Ardèche',2629,'Cordon grumeleux','Jurassic','Upper Jurassic','Oxfordian','middle Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',158,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,'30',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','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',1755,0,'Cordon grumeleux\nSubmerged plateau, transitional between Jura shelf and Tethyan basin.\nCryptalgal carbonate bodies. Lime mudstones and wackestones bound by stromatolitic crusts. \nLenticular bodies 0.5 m thick, 1-3 m wide.',44,4,4239163,871771,'France','Europe',331,'',44.6667,4.4333,'','',23.3897590945,23.8024732591,23.3897590945,23.8024732591,29.5357219054,24.413670044,35.4574,14.1219,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Naves, Ardèche',2630,'Cordon grumeleux','Jurassic','Upper Jurassic','Oxfordian','middle Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',158,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'30','2629',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','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',1755,0,'See reef 2629.\nSmall isolated stromatolitic knobs also in lower Kimmeridgian and lower Tithonian. Cryptalgal bodies enriched in radiolarians relative to surrounding deposits.',44,4,4189252,851359,'France','Europe',331,'',44.3333,4.05,'','',22.9974300941,23.6079373077,22.9974300941,23.6079373077,29.1479240794,24.1974989722,35.1052,13.8171,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fincastle, Virginia',2632,'Chepultepec-Stonehenge','Ordovician','Lower Ordovician','Tremadocian','Lower Canadian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',484,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','10',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','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','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',1758,0,'Middle Member of Chepultepec/Stonehenge Fms.\nThrombolitic mounds interbedded with skeletal muds and sands.\nMaximum 10 m thick and 50 m wide mounds composed of stacked bioherms. \nType grainy thrombolites and Girvanella mounds.',37,-79,-2020871,-6727095,'United States','North America',101,'',37.5,-79.8667,'WAHR','80573',4.64641506477,-102.401983096,4.64641506477,-102.401983096,4.64641506477,-102.401983096,-31.5012,-76.3732,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hebron, Virginia',2633,'Chepultepec/Stonehenge','Ordovician','Lower Ordovician','Tremadocian','Lower Canadian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',484,1,'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','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation','1','Present','1','Present','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',1758,0,'Middle Member of Chepultepec/Stonehenge Fms.\nThrombolitic mounds. Type muddy bioherms.\nVermiform fabrics by trapping and binding of lime mud by sponges and algal mats. Microspar cavity-fills interpreted as bioeroded sponge-silt. \nCavities probably formed by bioerosion.',38,-79,-2029226,-6630483,'United States','North America',101,'',38.1333,-79.15,'WAHR','80570',4.6430097981,-101.5497124,4.6430097981,-101.5497124,4.6430097981,-101.5497124,-31.6188,-75.3858,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Avens Bridge, Virginia',2634,'Chepultepec/Stonehenge','Ordovician','Lower Ordovician','Tremadocian','Lower Canadian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',484,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1758,0,'Middle Member of Chepultepec/Stonehenge Fms\nSmall thrombolitic bioherms.\nSee reef 2632 for further remarks.',36,-82,-1902394,-6932800,'United States','North America',101,'',36.6667,-82,'WAHR','80575',5.38985040699,-104.151619145,5.38985040699,-104.151619145,5.38985040699,-104.151619145,-30.506,-78.2545,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Goose Arm, Newfoundland',2635,'Petit Jardin','Cambrian','Series 3','Guzhangian','Middle-Dresbachian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',499,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1759,1855,'Carbonate belt behind platform edge.\nStromatolite and thrombolite mounds occur throughout the section, but do not occupy a specific position in the assemblage.\nEpiphyton-cementstone evident from fig. 85 in James (1983).',49,-57,-3350475,-4591199,'Canada','North America',121,'',49.1,-57.75,'','',6.53489032746,-88.4574678552,6.53489032746,-88.4574678552,6.53489032746,-88.4574678552,-36.4805,-62.3007,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tazewell, Tennessee',2661,'','Cambrian','Series 3','Guzhangian','upper Middle Cambrian',501.00,505.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',502,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,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,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1796,0,'Several small thrombolitic bioherms in subtidal package, with flat pebble conglomerates and bioturbation. \nMinor development in overlying intertidal package.',36,-83,-2771387,-7246135,'United States','North America',101,'',36.45,-83.4833,'','',9.88140387393,-121.162375493,10.5350349916,-116.336237319,10.5350349916,-116.336237319,-27.0215,-91.42,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Flat Gap, Tennessee',2662,'Copper Ridge Dolomite','Cambrian','Series 3','Guzhangian','Dresbachian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',498,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,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,'2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1796,0,'Digitate stromatolite (dendrolite) bioherm interbedded with thrombolites in intertidal Copper Ridge Dolomite.',36,-82,-2828547,-7216165,'United States','North America',101,'',36.35,-82.9333,'','',9.84166027631,-110.742728774,9.84166027631,-110.742728774,9.84166027631,-110.742728774,-28.6843,-87.1945,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('NE Amadeus Basin, N.W.T.',2663,'Shannon','Cambrian','Series 3','Guzhangian','Middle-Upper Cambrian',485.00,509.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',499,2,'0','Outcropping reef ',3,'Mud mound or bank','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','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,'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',1797,0,'Thrombolitic and stromatolitic bioherms.\nSeveral horizons.\n',-23,134,2859782,18729978,'Australia','Oceania',801,'',-23.9167,134.8333,'','',1.49454473941,111.89486295,0.776142768528,117.267223943,0.776142768528,117.267223943,20.3161,-177.249,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('South Australia',2664,'','Cambrian','Series 3','Guzhangian','Middle-Dresbachian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',499,2,'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','','Unknown','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',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',1798,0,'Position doubtful',-32,138,2067104,-19290074,'Australia','Oceania',801,'',-32.1667,138.4167,'','',-0.821965619307,126.507693724,-0.821965619307,126.507693724,-0.821965619307,126.507693724,15.5921,-170.114,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mohawk Valley, New York',2665,'Tribes Hill','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',483,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,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,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1800,0,'Abstract ref. 1800:\nTribes Hill domal thrombolites, termed here microbial reef mounds, occupied the basal part of meter-scale shallowing-upward cycles. They are part of a high-energy facies that a sharp, transgressive surface separates from an underlying low-energy peritidal setting. This erosional surface served as the surface on which one of the reef mounds established itself during initial transgression before further deepening. The others overlie a floor of skeletal grainstone reflecting a high-stand sea-level facies tract. Skeletal grainstone composes the fill between the mounds. One channel and several aggrading hummocks occupy inter-reef mound areas resulting from storm events in a subtidal setting.',42,-75,-1917650,-6045719,'United States','North America',101,'',42.75,-75.5,'','',5.73130209801,-96.2523305215,5.73130209801,-96.2523305215,5.73130209801,-96.2523305215,-31.047,-69.1142,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kalpin, Tarim Platform, Xinjiang',2669,'Shaylik','Cambrian','Series 3','Drumian','early Middle Cambrian',505.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',509,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1807,0,'Basal Middle Cambrian 50 km NE of Kalpin\nLower part of Shaylik Fm. consists of biolithite, leopard limestone, wormkalk and breccioid limestone.\nOverlain by thin-bedded chert-stripped limestone.\nOuter neritic platform setting in high energy environment.',40,79,2722473,13209942,'China','Asia',602,'',40.8333,79.5333,'','',-8.58155740253,64.0040972115,-9.8240730657,65.132296622,-9.8240730657,65.132296622,-15.9532,134.102,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lebanon Co., Pen',2670,'Millbach','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',493,2,'0','Outcropping reef ',NULL,NULL,'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,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1808,0,'',40,-76,-2054408,-6280284,'Lebanon','Asia',508,'',40.4,-76.45,'','',8.13965319024,-101.320023428,8.13965319024,-101.320023428,8.13965319024,-101.320023428,-31.9176,-77.7164,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aligator Creek, Bibb Co., Alabama',2671,'Copper Ridge-Chepultepec','Cambrian','Furongian','Lawsonian','Trempealeauan-Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',488,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,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',1809,0,'',33,-87,-1696277,-7566594,'United States','North America',101,'',33,-87.1667,'','',6.37546192199,-109.69812786,6.37546192199,-109.69812786,6.37546192199,-109.69812786,-28.4929,-84.2654,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Missouri',2672,'Jefferson City Dolomite','Cambrian','Furongian','Lawsonian','Trempealeauan-Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',488,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2',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','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',1727,0,'Domal stromatolites associated with grainstones.\nCollections of Patzkowsky refer to interreef fauna.',38,-92,-809279,-7361665,'United States','North America',101,'',38.5,-92.5,'WAHR','8942',13.1134927323,-107.787271465,13.1134927323,-107.787271465,13.1134927323,-107.787271465,-22.2781,-80.7068,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ellsworth Mts., Antarctica',2673,'Minaret','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',491,1,'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','3','Microbes',NULL,NULL,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,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1073,0,NULL,-79,-81,-1332105,-17537450,'Antarctica','Antarctica',803,'',-79.75,-81,'',NULL,-11.8689002315,156.522378265,-11.8689002315,156.522378265,-11.8689002315,156.522378265,-6.20069,-148.688,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-10 13:16:52'),('Fuzhouwan, Liaoning',2674,'','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 ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes',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',1813,0,'',39,121,5954308,15058585,'China','Asia',602,'',39.3667,121.6667,'','',17.1014823631,98.8384008551,17.1014823631,98.8384008551,17.1014823631,98.8384008551,-1.49513,139.358,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Haletown, Tennessee',2710,'Bangor Limestone','Carboniferous','Mississippian','Serpukhovian','Chesterian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',326,2,'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,'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',1835,0,'Microbial mound growing on grainstones and buried by grainstones.\n\nAbstract 1835:\nCarbonate mounds within the Chesterian (Mississippian) Bangor Limestone in north Alabama and east Tennessee are few in number, but diverse in character. Fourteen known mounds in this area can be assigned to five categories: 1) stromatolitic, 2) mud, 3) bryozoan-crinoid-coral, 4) bryozoan-crinoid, and 5) coral. Stromatolitic and mud mounds are microbial, bryozoan-crinoid-coral mounds are biodetrital, and coral mounds and some bryozoan-crinoid mounds are biohermal (reefal). Three lensoid stromatolites within crinkly-laminated dolomudstone comprise a single mound horizon about 0.5 m thick east of Monteagle, Tennessee. Near Haletown, Tennessee, the Bangor Limestone contains two mud mounds. The largest measures 8.2 m across and contains articulated bivalves and brachiopods, and intact fenestrate bryozoans. The mound\'s upper surface is bored. The mud matrix appears to contain tubular microfossils resembling Renalcis. A single bryozoan-crinoid-coral mound has been identified in Lawrence County, Alabama. It is approximately 25 m wide, up to 1.6 m thick, and had a maximum of 45 cm of synoptic relief. This mound is dominated by in situ colonies of the large rugosan Caninia sp. in a matrix of fenestrate bryozoan and echinoderm debris. A bryozoan-crinoid mound about 0.7 m thick and 1.5 m wide near Blount Springs, Alabama, contains a framework of fenestrate bryozoans and serpulids, spar-filled voids, and skeletal debris dominated by echinoderm ossicles. Bryozoan-crinoid mounds about 2 m thick have been reported from the Bangor-Pennington transition zone east of Monteagle. Five mounds up to 15 m wide and up to 1.5 m thick that are constructed entirely by Caninia sp. are known near Blount Springs and Lacon, Alabama.   Bangor mounds are relatively rare and small, suggesting environmental stress. The mounds we examined are mostly underlain by packstone/grainstone, which suggests that the principal stressor might have been a mobile substrate coupled with periodic smothering. However, the Lawrence County mound is underlain by oolitic grainstone that had first been indurated during a period of early subaerial exposure. Early diagenesis or other stabilization mechanisms probably occurred at the other mound sites as well. ',35,-85,-2208657,-3227067,'United States','North America',101,'',35.0333,-85.5333,'','',-29.8166578569,-45.6746503722,-29.8166578569,-45.6746503722,-16.3376633527,-65.9145290523,-17.7191,-31.6048,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lacon, Alabama',2711,'Bangor Limestone','Carboniferous','Mississippian','Serpukhovian','Chesterian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',326,2,'0','Outcropping reef ',4,'Biostrome','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','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1835,0,'Stromatolitic biostrome.\nSee also reef 2710',34,-86,-2217342,-3375749,'United States','North America',101,'',34.3333,-86.9,'','',-29.4226521884,-47.12868783,-29.4226521884,-47.12868783,-16.3164028845,-67.2939936606,-17.7682,-32.994,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('New York Route 67, Amsterdam, New York',2713,'Tribes Hill','Ordovician','Lower Ordovician','Tremadocian','early-mid Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',485,3,'0','Outcropping reef ',4,'Biostrome','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,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1837,0,'Wolf Hollow Member\nPillow- to dome shaped and biostromal thrombolites in intraclast-echinoderm pack- to grainstone matrix.\nScour-and fill structures.\n\nTribes Hill microbial reef mounds, occupied \nthe basal part of meter-scale shallowing-upward \ncycles.  They are part of a high-energy facies that a \nsharp, transgressive surface separates from an \nunderlying low-energy peritidal setting.  This \nerosional surface served as the surface on which one \nof the reef mounds established itself during initial \ntransgression before further deepening.  The others \noverlie a floor of skeletal grainstone reflecting a \nhigh-stand sea-level facies tract.  Skeletal grainstone \ncomposes the fill between the mounds.  One channel \nand several aggrading hummocks occupy inter-reef \nmound areas resulting from storm events in a subtidal \nsetting.  This study is part of a continuing program of \nTribes Hill sedimentology.',43,-74,-1984379,-5949351,'United States','North America',101,'',43,-74.2833,'','',5.26382859217,-95.4492700787,5.26382859217,-95.4492700787,5.26382859217,-95.4492700787,-31.5613,-68.2129,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Amgar River, S Siberia',2717,'','Cambrian','Series 3','Drumian','Amgan',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',507,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','1','3','Binder 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',1842,1998,'Epiphyton reefs.\nCoalescing small bioherms 0.5-1 m in diameter over at least 50 m extension.',60,131,-1350439,-273497,'Russia','Asia',624,'',60.6333,131.65,'','',11.1154537021,-51.1933057835,11.1154537021,-51.1933057835,11.1154537021,-51.1933057835,-4.45043,-11.3372,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Guerrero',2719,'Olinala','Permian','Guadalupian','Wordian','Wordian-Capitanian',259.80,268.80,16,'Roadian - Changhsingian',261,265,'Middle Permian (Wordian/Capitanian Boundary 265.1 Ma)',265,3,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1844,0,'Ref. 1844:\nThe Upper Permian in South Mexico includes the Olinala Formation in the state of Guerrero. This formation is the youngest Paleozoic sedimentary cover of the Mixteco Terrane. This formation contains the youngest Permian beds reported in Mexico (Woardian, Capitanian). The lower and middle part, containg fosilss of goniatits, of Woardian age, consists of silisiclastic rocks, while the upper part is a carbonate sequence of Late Guadalupean age. The carbonate sequence overlies the siliciclastic sequence by erosional contact. This carbonate sequence is a ramp deposit, the inner shallow ramp deposits are mainly composed of echinoderm debris grainstone-packstones, in which are found, crinoids, pelecypods, gastropods, as well as microfossils such as Parachaetes sp, seaweed (Tubhyfites sp; Tubhyfites obscurus Maslov 1956), boundstones type LLH(C), and organic bank crinoids boundstones and shoal bioclastic grainstones.  The middle ramp is characterized by interbeded finegrained limestones and sandstones. The limestones are bioclastic packstone-wackestones with echinoid fragments (crinoids mainly), bryozoa, pelecypod shells of, brachiopod spines, small Foraminifera (Abadehella ex gr.coniformis) and fusulinids (Codonofusiela extensa Skinner& Wilde, 1955; Rauserella errática, Dumbar 1944, Condofusiella extensa Skinner & Wilde 1955) of Woardian-Capitanian age. The sanstones are litarenites and sub litarenites.  The deep ramp deposits consist of carbonate mud mount of cyanobacterium (Tubiphytes, Aelisaccus), calcareous sponges, Prorichtofenids, and bryozoa, that trap the calcareous mudstone, forming typical stromatactitis. ',17,-99,-938457,-4692008,'Mexico','North America',105,'',17.5,-99,'','',-0.506751790425,-39.2434823923,-0.506751790425,-39.2434823923,-9.80389199038,-47.6323951069,-5.28668,-42.0627,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nagornij-Karabach, Azerbaidzhan',2722,'','Triassic','Lower Triassic','Induan','Scythian',247.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',248,1,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1847,0,'Algal bioherms of Early Triassic age mentioned.',39,46,1700859,4389761,'Azerbaijan','Europe',NULL,'',39.6667,46.8333,'','',-20.0000038534,48.5133922639,10.1222914455,58.2473233188,18.2111786225,55.3942039564,3.51179,38.2413,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Doberlug, Brandenburg',2723,'Zwethau','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',519,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','20',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','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','8','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1849,1850,'Epiphyton predominates. Domal in lower parts, columnar in upper part.\nSome Renalcis, Botomaella and Kordephyton.\nIrregular archaecyaths also important.\nShallow subtidal ramp\nDimensions not given but probably nearly 20 m thick.\n\nAbstract of ref. 1849:\nThe palaeoecology of calcimicrobial communities from the only Gondwana-related Lower Cambrian in Central Europe (eastern Germany, carbonates and siliciclastics) has been studied. Six morphological groups of calcimicrobes are described. Some of them show a significant ability for sediment stabilization and construction of biohermal reef mounds. Other types of calcimicrobes were more common in biostromal thickets. Some of them were capable of populating different environments, growing in different modes and on different substrates. An Epiphyton-archaeocyathan reef mound is described, illustrating the importance of calcimicrobes for mound formation. The fossil communities together with a complex of sedimentary features allow a reconstruction of the depositional history of the environment. Based on comparison with similar Gondwanan Lower Cambrian successions (Sardinia/Italy, Spain) and facies development a model is proposed describing the sedimentary history. Three depositional stages are distinguished: (1) deep subtidal ramp, (2) shallow subtidal ramp, (3) shallow subtidal to intertidal mixed siliciclastic-carbonate ramp with migrating oolitic shoals. In spite of similarities with the deposits in southern Europe, some distinct differences exist with respect to the succession of facies, the completeness of the sections, the fossil spectrum, and the nature of the siliciclastic sediments. For the German Lower Cambrian, a facies development from a low energy deep environment to a high energy shallow environment (partly restricted and with some evaporites) can be reconstructed. As compared with Sardinia and Spain, the depositional environment of the eastern German Lower Cambrian successions was predominantly characterized by low-energy conditions.',51,13,-6287537,-2642591,'Germany','Europe',331,'',51.6333,13.55,'WAHR','24190',-51.6193971172,5.92138989628,-51.6193971172,5.92138989628,-51.6193971172,5.92138989628,-38.3043,107.545,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Last Chance Range, California',2724,'Bonanza King','Cambrian','Series 3','Guzhangian','Marjumian',500.50,504.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',500,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','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','2','3','Binder 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','1','Present',0,'No or unknown reservoir potential',1852,0,'Marjumid Biomere\nPlatform margin slope with Girvanella and Epiphyton boundstone clasts (up to 6 m) stemming from thrombolite mounds on platform edge.\nMicritized grains.\n\'Algal\' boundstones also figured from platform interior but not described.',37,-117,723532,-8779995,'United States','North America',101,'',37.4,-117.7667,'','',34.0892404071,-130.880948306,34.0892404071,-130.880948306,34.0892404071,-130.880948306,0.57732,-94.7247,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Western Utah',2727,'Wheeler Shale','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',505,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m','6',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1855,0,'Small mound (6 m wide) of stromatolites and Renalcis.',39,-113,338292,-8285471,'United States','North America',101,'',39,-113.5,'','',30.8973522813,-133.109679319,31.6843015118,-128.067403566,31.6843015118,-128.067403566,-0.449733,-92.0971,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cow Head, Newfoundland',2741,'Shallow Bay','Cambrian',NULL,NULL,'Steptoan-Sunwaptan',491.00,494.50,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',495,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1870,0,'Trilobite faunas from boulder of shelf-margin buildups analyzed.',49,-57,-2242269,-4442705,'Canada','North America',121,'',49.9167,-57.8333,'WAHR','81269',6.71738869073,-85.6000523907,6.71738869073,-85.6000523907,6.71738869073,-85.6000523907,-35.2554,-59.2066,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Eshelman Quarry, Waterside, Pennsylvania',2743,'Gatesburg','Cambrian','Furongian','Jiangshanian','Steptoean',493.00,494.50,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',496,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','5',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,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1871,0,'Ore Hill Member\nElvinia Zone (=Dresbachian = Steptoan).\nThrombolite reef resting on grainstones. Rare stromatolitic fabrics. Abundant fenestrae.\nAbout 5 m thick.\nSharp contrast between mounds and inter-reef grainstones',40,-78,-2062245,-6332696,'United States','North America',101,'',40.25,-78.4,'WAHR','9264',9.23857487643,-102.940851749,9.23857487643,-102.940851749,9.23857487643,-102.940851749,-30.6686,-79.1973,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Imler Quarry, Bedford, Pennsylvania',2744,'Gatesburg','Cambrian','Furongian','Jiangshanian','Steptoean',493.00,494.50,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',496,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30','2743',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,'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',1871,2328,'See reef 2743\nVery rich trilobite fauna.\nSteptoen stage = Dolgellian',39,-78,-2048709,-6361744,'United States','North America',101,'',39.9833,-78.5,'WAHR','9262',9.11594315129,-103.19295326,9.11594315129,-103.19295326,9.11594315129,-103.19295326,-30.7291,-79.5122,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('IJAMS core, Alabama',2766,'','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,'1','Seismic data available ',2,'Reef mound','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','1c','Epeiric sea','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',1,'Potential reservoir',1890,0,'The micro(bio)herms are composed of an enigmatic tubular organism (resembling Renalcis). These microherms are up to 0.3 m thick and 0.5 m wide. It is suggested that the microherms combined with micritic sediment to form a decameter-scale mound. ',31,-88,2102867,-4115631,'United States','North America',101,'',31.2667,-88.1667,'','',16.1538304438,-28.8372313632,16.1538304438,-28.8372313632,20.3890198115,-31.0029987083,23.2357,-35.7468,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tiewadian, Xian, Shaanxi',2771,'Jinghe','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 ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','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',1723,0,'Webby pers. comm.',34,108,5537556,14371062,'China','Asia',602,'',34.5,108.8333,'',NULL,35.4540659475,92.371612373,35.4540659475,92.371612373,35.4540659475,92.371612373,-23.8898,124.966,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tiewadian, Xian, Shaanxi',2772,'Jinghe','Ordovician','Upper Ordovician','Sandbian','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',459,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','150',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','4','Stromatoporoids','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)',NULL,NULL,'10','80','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',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1723,0,'Webby, 2002:\r\nA series of reef complexes, reefs, and biostromes have been\r\nreported through a carbonate succession 600 m thick at Tiewadian\r\n(Fig. 5) and equivalent sequences of adjoining areas, north of the\r\nWei River, Shaanxi Province (Ye et al., 1995, Ye et al., 1996). They\r\noccur on topographic highs of the rifted, southwestern margin of\r\nthe Ordos Platform (North China Block). At Tiewadian the sequence\r\nincludes a composite, 150-m-thick reef complex composed\r\nof superposed biostromes and reef mounds, a 30-m-thick\r\nbiostrome, and discrete, large to small, lens-shaped reefs, from 5\r\nto 35 m thick. A wide range of frame-builders and binders are\r\nrecorded, though seldom all groups in a single reef or biostrome.\r\nStromatoporoid Forolinia (probably Labechia), and microbes\r\nPhacelophyton, Renalcis, Epiphyton, Trichophyton, and Girvanella,\r\nare the main contributors. Less important are algae Solenopora,\r\nVermiporella, and the corals Lichenaria, Cryptolichenaria, Amsassia,\r\nand Eofletcheria. Some larger reefs exhibit a generalized framework\r\nsuccession: substrate stablization of bioclasts by microbial\r\n(stromatolitic) growth, in places associated with corals or succeeded\r\nby them, and then dominant Forolinia, and/or less common\r\nPhacelophyton, towards the top. Smaller reefs are mainly\r\nstromatolitic. Vermiporella, though recorded by Ye et al. (1996) as\r\na major reef builder, may have had a more limited role in\r\nsediment production.',34,108,5492214,14459030,'China','Asia',602,'',34.9167,108.5667,'',NULL,35.1198870799,92.7779193094,35.1198870799,92.7779193094,35.1198870799,92.7779193094,-23.8581,124.452,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kullsberg, Siljarn District',2782,'Kullsberg','Ordovician','Upper Ordovician','Katian','early Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',453,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','50',NULL,NULL,NULL,'3','More than 100 m','350','20',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','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',1913,1914,'Position?\nKeila age\nEleven carbonate mud mounds are recorded from the Kullsberg Limestone of the Siljarn district in Sweden (Jaanusson 1979; 1982). \nIsolated, on-shelf, stromatactis-bearing mounds, up to 50 m high.',60,14,-4120754,-662780,'Sweden','Europe',330,'2831',60.5,14.5,'WAHR','73411',-26.318212146,-65.0627236095,-26.318212146,-65.0627236095,-26.318212146,-65.0627236095,-29.4034,-7.03415,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sukharikha River, Igarka, Siberia',2798,'Sukharikha','Cambrian','Terreneuvian','Fortunian','Nemakit-Daldynian',529.00,541.00,1,'Nemakit/Daldynian - Toyonian',520,540,'Cambrian/Precambrian boundary (541 Ma)',535,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','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','2','6 to 24 reef building species','6','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',1940,1939,'Age given as Late Vendian but abundant trace fossils indicate Cambrian age.\nMassive dolomitic bioherms composed of Renalcis, Girvanella, Hedstroemia, Proaulopora and Subtifloria\n',67,87,-4188308,960821,'Russia','Asia',624,'',67.25,87.75,'WAHR','80839',-16.2112233787,-76.8947573692,-16.2112233787,-76.8947573692,-16.2112233787,-76.8947573692,-26.9972,2.00554,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sukharikha River, Igarka, Siberia',2799,'Sukharikha','Cambrian','Terreneuvian','Stage 2','lower Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',527,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1939,1940,'Flat and wide (up to 1.5 m) biscuit-like bioherms composed of Renalcis.',67,87,-4188308,960821,'Russia','Asia',624,'',67.25,87.75,'WAHR','80840',-11.4207864533,-65.1943019221,-11.4207864533,-65.1943019221,-11.4207864533,-65.1943019221,-23.7028,0.283547,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Medvezhiya River, Kotuy, Siberia',2800,'Manykay','Cambrian','Terreneuvian','Fortunian','Nemakit-Daldynian',529.00,541.00,1,'Nemakit/Daldynian - Toyonian',520,540,'Cambrian/Precambrian boundary (541 Ma)',535,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,'300',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','5','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1939,0,'Koril member of Manykay Formation (5-10 m thick) traceable in the basins of Kotuy, Medvezhiya, Eriechka, Fomich and Rassokha Rivers.\nLess than 30 cm thick calyptras with uniform composition of calcibionts: Renalcis, Girvanella, Korilophyton and Gemma.',71,103,-4006043,210491,'Russia','Asia',624,'',71,103,'WAHR','50423',-15.3367719596,-83.6652617893,-15.3367719596,-83.6652617893,-15.3367719596,-83.6652617893,-28.5384,-5.21794,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kotuy River, Siberia',2801,'Manykay','Cambrian','Terreneuvian','Fortunian','Nemakit-Daldynian',529.00,541.00,1,'Nemakit/Daldynian - Toyonian',520,540,'Cambrian/Precambrian boundary (541 Ma)',535,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,'300','2800',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1939,0,'Marked solitary bioherm 12 m below Koril Member.\n1.5 m-2 m wide, 0.2 m high consisting of Renalcis and samll columellae of branching stromatolites',69,103,-3811857,324418,'Russia','Asia',624,'',69.25,103.75,'','',-13.7627519035,-82.832386296,-13.7627519035,-82.832386296,-13.7627519035,-82.832386296,-26.7823,-4.98291,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rassokha River, Siberia',2802,'Manykay','Cambrian','Terreneuvian','Fortunian','Nemakit-Daldynian',529.00,541.00,1,'Nemakit/Daldynian - Toyonian',520,540,'Cambrian/Precambrian boundary (541 Ma)',535,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m',NULL,'300','2800',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1939,0,'See reef 2800',71,110,-3890454,-75946,'Russia','Asia',624,'',71.8333,110.75,'','',-14.7102595528,-86.2826955141,-14.7102595528,-86.2826955141,-14.7102595528,-86.2826955141,-28.8164,-8.16962,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Isit, Lena River',2803,'Tolba','Cambrian','Terreneuvian','Fortunian','Nemakit-Daldynian',529.00,541.00,1,'Nemakit/Daldynian - Toyonian',520,540,'Cambrian/Precambrian boundary (541 Ma)',535,2,'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',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','5','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',1939,0,'Isit\' well with Renalcis and Korilophyton\nIn outcrops Renalcis, Subtifloria, Botomaella and Korilophyton.',60,125,-2242134,-63840,'Russia','Asia',624,'',60.8167,125.3333,'WAHR','81109',-2.36903464855,-87.4999773426,-2.36903464855,-87.4999773426,-2.36903464855,-87.4999773426,-17.5016,-13.7005,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bulleys Lump, Judge Daly Promot., Nunavut',2830,'Bulleys Lump','Ordovician','Middle Ordovician','Darriwilian','Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',463,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1400',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,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1574,0,'Upper part of Member B\r\nSee reefs 2431 and 2432',80,-69,995345,-3243164,'Canada','North America',121,'',80.75,-69.25,'',NULL,15.975388471,-77.2224192159,15.975388471,-77.2224192159,15.975388471,-77.2224192159,-0.930921,-34.1241,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Syltefjord, Finmark',2835,'Porsanger Dolomite','Ediacaran','Ediacaran','Avalon Assemblage','Riphean',720.00,850.00,0,'Vendian',605,690,'Middle Neoproterozoic (late Cryogenian, 690 Ma)',680,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1957,0,'Stromatolithic bioherm beneath Varanger tillites.',70,30,-7458537,-2302140,'Norway','Europe',301,'',70.5167,30,'','',-30.4786512499,-116.767383285,-30.4786512499,-116.767383285,-30.4786512499,-116.767383285,-35.4004,-114.718,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nopah Range, California',2836,'Nopah','Cambrian','Furongian','Lawsonian','Trempealeauan',485.40,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',493,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','60',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1958,2142,'Smoky Member of Nopah Formation\nDigitate microbial dolobafflestones, thrombolite heads and columnar stromatolites together with dolograinstone, stromatactoid spar, and pelloidal stuff.\nMicrobial structures repeatedly occurring in 300 m thick seuqence. Cummulative reef thickness about 60m.',36,-116,1412730,-8563714,'United States','North America',101,'',36.0917,-116.15,'','',32.2552948181,-132.242657538,32.2552948181,-132.242657538,32.2552948181,-132.242657538,-0.516142,-96.2458,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fuzhouwan, Lianoning',2837,'','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',492,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1959,0,'Stromatolithic bioherms',39,121,5954344,15060233,'China','Asia',602,'',39.3667,121.65,'','',17.1083076943,98.849867227,17.1083076943,98.849867227,17.1083076943,98.849867227,-1.50646,139.352,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Salvnicke Podhorie, Carpathians',2838,'Bohunice','Jurassic','Middle Jurassic','Bathonian','Bathonian-Callovian',163.50,168.30,21,'late Bathonian - early Tithonian',151,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',164,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','24','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','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','1','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2283,1961,'Typical Stromatactis mound resembling Paleozoic counterparts. Cement is mixture of marine cement and recrystallization spar.\nSome crinoids present.\n\ndense network of Stromatactis and stromatactoid cavities. Peloidal interparticle matrix.',49,18,3954482,2318089,'Slovakia','Europe',336,'',49.0167,18.1833,'FALSCH','0',29.8586391523,33.3921884956,29.8586391523,33.3921884956,35.6098480701,34.8458833113,40.1393,25.6725,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jiaodingshan, Sichuan',2844,'Daduhe','Ordovician','Upper Ordovician','Katian','late Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',445,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1969,0,'Mn-Co deposits in microbial reef complex.\r\nMean Mn concentration is 31.6%\r\nSmall atoll-like reef, 1000 m diameter\r\n3 facies types. Framework-reef complex, reef-flank talus, atoll lagoon.',29,102,601853,14570021,'China','Asia',602,'',29.4167,102.8167,'WAHR','80155',3.3094277372,72.2915644096,3.3094277372,72.2915644096,3.3094277372,72.2915644096,13.7114,131.554,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dawashan, Sichuan',2845,'Daduhe','Ordovician','Upper Ordovician','Katian','late Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',445,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'1',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',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1969,0,'Mn deposit in several pinnacle reefs, ranging 20 to several 100 m in length. \r\nSeveral facies: reef-base bank, reef core, reef-front talus, back-reef algal flat, back-reef fill and reef cap.\r\nCore is massive \'algal\' rhodochrosite.\r\nReef possibly grown in high-productivity environment.',29,103,582121,14554076,'China','Asia',602,'',29.35,103.05,'',NULL,3.17416879264,72.1255287319,3.17416879264,72.1255287319,3.17416879264,72.1255287319,13.5813,131.379,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jinan, Shandong',2856,'Zhangxia','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',504,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','15',NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','6','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',1979,0,'Thrombolite microframes\n\nAbstract ref. 1979:\nMid Cambrian reefs with microframe structure built by calcified microbes, probably cyanobacteria, are well-exposed in the Zhangxia Formation near Jinan in\nShandong Province. Members of the Epiphyton, Renalcis and Girvanella groups are almost solely responsible for a series of extensive biostromes, individually up to 15 m thick, in which metazoans are scarce. These reefs are surrounded by coarse cross-bedded oolite-pisolite, reflecting rapid growth in a high-energy environment.\nThe two main reef lithotypes present are: (1) matrix-rich Tarthinia-Tubomorphophyton thrombolite-dendrolite microclusters, and (2) Gordonophyton-Razumovskia thrombolite microframes. The latter were created by rectilinear arrangement of prostrate and vertical microbial filaments, and the small (millimetric) size of the cavities contributed to framework strength.\nSimilar, but usually less well-preserved, mid-late Cambrian reefs appear to be widespread in Asia and North America. These North China examples establish\nmicrobial microframes as a distinctive reef-structure, and show that frame-building continued during the Cambrian despite archaeocyath demise.\n',36,116,6302125,15413403,'China','Asia',602,'',36.65,116.95,'WAHR','81107',25.442339237,97.7394305845,23.8192993836,98.7255472595,23.8192993836,98.7255472595,-2.65453,144.601,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('South central Pennsylvania',2871,'Ledger','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',505,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','30','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2411,1994,'Abstract ref. 1994:\nLaurentian shelf margin deposits typically are dolomitized or metamorphosed, but the Ledger Fm. contains an exceptionally well preserved microbialite reef complex, riddled with large submarine cavities. The microbialite consists of Renalcis-like shrubs, centimeter-scale domal stromatolites, dense fronds and laminated\nfabrics. Petrographically, the microbialite is expressed as clots of spherulites, stringers, arborescent garlands, and dendritic shrubs. Microbial processes dominated all\necological niches; forming the substrate, colonizing cryptic spaces, coating and encrusting other algae. Cavities within the microbialite formed through a number of previously undescribed processes, at least on the large scale reported here. Organic decay led to the development of stromatactis-like voids on a meter-scale, while syn-depositional slumping and channel formation led to microbial props and folds which resulted in further void generation.  \nThese large cavities were stabilized with multiple generations of radiaxial fibrous and herringbone calcite cements, intercalated with internal sediment. The herringbone calcite cement has depleted carbon isotopic values relative to the radiaxial fibrous cement, even those within the same cavity. This suggests that the herringbone morphology is related to unusual porewater conditions. In this instance I interpret that the herringbone calcite reflects near anoxic porewaters due to large quantities of decaying microbial material nearby. \n\nMarine cement stratigraphy, based on petrography, CL, stable isotopes, and trace element geochemistry, demonstrate that the cavities did not fill simultaneously.\nRather, even adjacent cavities exhibit complex patterns of cementation, encrustation, and cement breakage, indicating that the reef\'s location was in a high energy,\nshelf margin setting where storms and local events impacted each cavity differently. ',40,-78,-2917754,-6588128,'United States','North America',101,'',40.3333,-78.3333,'','',9.53409802858,-115.492698176,10.1136027171,-110.660945365,10.1136027171,-110.660945365,-29.6741,-85.8156,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bappagai Well, Tankhai-Ust-Mil, Siberia',2872,'','Cambrian','Series 3','Guzhangian','Mayan',497.00,500.50,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',503,3,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','320',NULL,NULL,NULL,'4','More than 1000 m','2000',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1996,1997,'Large \'algal\' reef complex underlain by Domanik facies type limestones of Lena-Amgan age.',63,123,-1741605,92165,'Russia','Asia',624,'',63.0333,123.9667,'','',7.39255764943,-48.2842495638,7.39255764943,-48.2842495638,7.39255764943,-48.2842495638,-6.88991,-7.51733,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Amga River II, Yakutiya, Siberia',2876,'','Cambrian','Series 2','Stage 3','Lenian-Amgaian',509.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',510,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'3','Microbes','3','Microbes','7','Archaeocyaths - microbes',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','',0,'No or unknown reservoir potential',1998,0,'See reef 2875',60,130,-1311544,-213495,'Russia','Asia',624,'',60.3,130.6167,'','',7.97998044454,-64.327459857,7.97998044454,-64.327459857,7.97998044454,-64.327459857,-7.88057,-16.8805,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('T-Reef, Gor Uein Terguet, Tindouf Bas., West Sahara',2883,'','Devonian','Middle Devonian','Givetian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',390,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','25',NULL,NULL,NULL,'3','More than 100 m','2000',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'3','Microbes','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'90','0','10',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1687,2488,'Chain of stromatactis mud mounds with steep flanks. \nSome mounds with common rugose corals.\nCrinoids common.\n',26,-11,-5041889,-196582,'Morocco','Africa',714,'',26.65,-11.35,'WAHR','79549',-40.2773271927,-17.7630041478,-40.2773271927,-17.7630041478,-40.3007182015,-17.2389937347,-45.8534,5.9552,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Limonovka, central Urals',2886,'Samsonovskie','Devonian','Upper Devonian','Frasnian','middle(?) Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',379,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','13',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','2','Below fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2003,0,'Steeply flanked mound composed of massive \'algae\' and stromatoporoids (Actinostroma).',55,58,1129284,2252833,'Russia','Asia',624,'',55,58.1333,'','',4.51635712103,5.55004730553,4.51635712103,5.55004730553,28.3857147463,-61.5453708949,6.71641,20.2245,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('La Serre, Montagne Noire',2890,'Roc de Murviel','Carboniferous','Mississippian','Serpukhovian','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',324,2,'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','','Unknown',NULL,NULL,'3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','14','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2435,2009,'Abstract ref. 2009:\n During the Early and Middle Viséan rugose corals again occurred widespread within shallow water marine environments. To some extent they accumulated to form reefal structures. The significance and function of related rugose corals were highly variable. In order to achieve a systematic approach Lower Carboniferous biostromes and biohermes were examined in different geotectonic settings north (Belgium) and south (France: Montagne Noire) of the European Variscian orogenic belt. \n     In the Montagne Noire the Viséan to Namurian sequence is part of large olistoliths originating from an active continental margin. Limestone olistoliths yield different shallow-water communities. Bioherms show a community consisting of calcareous algae, cyanobacteria (e.g. Orthonella), and bryozoans. Accessory brachiopods, corals, molluscs, siliceous sponges, and foraminifers occur. Sporadically there are intercalations of dark, well-bedded pack- and grainstones (part of peri-biohermal facies). Some of the olistoliths yield a rich coral fauna. Most abundant are solitary corals (e.g. Axophyllum), but in some cases colonial forms contributed to the formation of biostromes and small bioherms. They were dominated in changing compositions by Lithostrotionidae, Lonsdaleia and Axophyllum.\nThese small structures seem to be bound to lagoonal or inter-biohermal settings. \n     In Belgium coral biostromes occur throughout the Viséan. Siphonodendron martini occurs in the capping-beds of the cryptalgal-bryozoan Buildup of Bomal\n(Middle Viséan). During the Late Viséan a diverse coral fauna inhabited the microbial mounds of the Campine Basin. From the same interval two biostromes are known form Royseux (northern limb of the Dinant Syncline). These biostromes show important contributions by Lithostrotionidae. \n     In general Late Viséan and Early Namurian coral biostromes and bioherms appear to represent local niches. The reef-building potential seems to be relatively high if rugose corals and encrusting organisms co-occur. ',43,3,-1653172,1293151,'France','Europe',331,'',43.55,3.3333,'WAHR','50810',-27.7578499111,6.69903775765,-27.7578499111,6.69903775765,-13.0019601441,-10.0370205906,-11.8918,12.5759,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sierra de la Estrella, Guadiato',2891,'Sierra del Castillo','Carboniferous','Mississippian','Visean','Brigantian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',327,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','25',NULL,NULL,NULL,'2','10 - 100 m','40',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2010,2434,'Microbial mud mounds between inner and outer ramp setting.\nAsbian-Brigantian\n\nAbstract ref. 2010:\n     In the Guadiato Area sedimentation occurred during the upper Viséan to form the Sierra de la Estrella outcrops which belong to the Sierra del Castillo Unit The\nGuadiato Area is located on the boundary between the Ossa-Morena and Central-Iberian zones, in the south-western Iberian Peninsula, where Lower\nCarboniferous outcrops are numerous. Buildups development has been recognised in most outcrops of the Sierra del Castillo Unit, and they are located at La Casa\nde la Calera, Peñarroya, Sierra Boyera and Sierra de la Estrella. Although the stratigraphical setting of the first three sections has been previously described, their\nbuildup development and morphologies are different to those of Sierra de la Estrella, whose buildups are thicker and more abundant. \n     The stratigraphic succession from Sierra de la Estrella is dated precisely as upper Viséan by means of foraminifers (Zone 15 of Mamet). The main guide taxa are:\nPalaeotextularia (bilaminar), Cribrostomum, Vissariotaxis compressa, Howchinia, \'Monotaxinoides\' sp., Endothyranopsis crassa, and the Microproblematicum\nSaccamminopsis fusulinaeformis. Sediments at Sierra de la Estrella show characteristics of a storm-dominated transitional zone between outer and inner ramp. The\noutstanding feature of this ramp is the development of microbial buildups. They may be called mud-dominated buildups or mud-mounds because they are\nmud-dominated (they show more than 50% of mud). They are regarded as microbial mounds because they are mainly composed of organomicrite and show\ncommon stromatactoid cavities. \n     Two main morphologies have been identified: \n\n     1. Tabular mud-banks; they extend laterally for 1000 m to 1300 m, and are 35-60 m in thickness. \n     2. Domal mud-mounds; they have variable size; they are 2-25 m in thickness and 4- 40 m in diameter.\n\nBuildup types were related to sedimentological conditions; domical mud-mounds were developed in transitional facies between the inner and outer ramp, with\nvariations in the environmental conditions, while tabular mud-banks were developed in more stable conditions in an outer ramp setting. \n     Microbial buildups are interbedded with tempestites and marls. Some siliciclastic beds showing erosion surfaces and hummocky cross-bedding also occur \n     The sedimentological and paleontological characteristics of the Sierra de la Estrella section allow us to recognise two deepening-upward sequences (probably of\n4th order), which are integrated into a major transgressive sequence (belonging to a 3rd order cycle). This glacio-eustatic cycle is recognised in upper Viséan\nthroughout the Guadiato Area, so it could be envisaged that it will influence all outcrops from this epoch within the Ossa-Morena and Central Iberian zones. ',37,-4,-2200552,534637,'Spain','Europe',304,'',37.95,-4.8667,'WAHR','39708',-43.4294853251,-8.48425542803,-38.2410129323,-5.41014332715,-18.0144790464,-31.9459328223,-17.6934,4.10675,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Drake Island, Glacier Bay National Park, Alaska',2929,'Willoughby','Silurian','Ludlow','Gorstian','Ludlow',423.00,427.40,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',421,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m','150',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','6','Calcisponges','66','Stromatolites-\'sphinctozoans\'-(stromatoporoids, algae, corals)',NULL,NULL,'0','40','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,'3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2036,0,'Platform margin reef\n\n\nAbstract ref. 2036:\nIn Glacier Bay, Alaska, Silurian limestones record the development and demise of a stromatolite reef complex in the Alexander terrane. These microbial deposits are of regional and paleontological significance because they contain paleogeographically distinctive biotas and yield important insights into Phanerozoic stromatolites that inhabited normal-marine subtidal environments. Willoughby limestones exposed on Drake Island reveal that stromatolite growth at the platform margin influenced platform dynamics with the protection of peritidal and lagoonal habitats behind a reef-fringed rim, which experienced early lithification by the precipitation of synsedimentary marine cements. Relatively low-energy subtidal conditions in a restricted, shallow-marine lagoon are implied by the peloidal and mollusk-rich wackestones, packstones, and grainstones. At the platform margin, stromatolite boundstones and cementstones capped a reef-like mound by forming a thick microbial-cement crust on a core of outer lagoonal sediments. Well laminated, fenestral mudstones and peloidal wackestones-grainstones have an abrupt lateral contact with the microbial boundstones, indicating their formation in peritidal flats adjacent to the stromatolite reefs. Foreslope breccias consist of clasts derived from shallow subtidal environments on the shelf and at its rim. Cyclic repetition of these deposits indicate that sea level fluctuations and tectonic instability in the Alexander terrane contributed to periodic shedding of shallow-marine detritus to the upper slope, followed by the rebuilding of stromatolite reefs at the platform margin. Culminating stages in the Klakas orogeny induced large-scale, catastrophic collapse of the carbonate platform. Silurian stromatolites characterized by similar habitats and microbial-sponge biotas in southwestern Alaska and the Ural Mountains, Russia, together with paleomagnetic data, detrital zircon evidence, and the timing of late-stage Caledonide events, firmly establish genetic and temporal links of the Alexander terrane with other areas along the Uralian Seaway.',58,-136,908727,-7707262,'United States','North America',101,'',58.6333,-136.2167,'WAHR','79359',11.1735791413,-114.035022491,11.1735791413,-114.035022491,11.1735791413,-114.035022491,-2.69102,-91.5554,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lakeside Mountains, Utah',2933,'','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 ',3,'Mud mound or bank','1','Less than 10 m thick','9',NULL,NULL,NULL,'3','More than 100 m','200',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,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2040,0,'Thrombolitic and stromatolitic mounds (pinch and swell structures).\n\nAbstract ref. 2040:\nStromatolites have been recognized as opportunistic disaster forms following the end-Permian mass extinction. This occurrence was attributed to the partial relaxation of ecological constraints in the aftermath of the mass extinction. A similar pattern occurs in the Great Basin following the Late Ordovician mass extinction in association with a shift to low-diversity, generalized faunas.\n\nMost Late Ordovician-Silurian faunal communities in the Great Basin are diverse and limited to relatively narrow environmental zones. Thin (10-20 cm thick) stromatolites occur throughout the section within inner-shelf tidal-flat facies. After the mass extinction, earliest Silurian (Rhuddanian) communities are broadly distributed with low diversity. Associated stromatolitic and thrombolitic mounds increase in abundance and reach a thickness of 2.5 meters. Bootstrapping analysis suggests the restriction of thick mounds to the post-extinction interval is non-random (probability <0.5%).\n\nThe widespread shelf stromatolites and thrombolites of the early Paleozoic declined, probably because their habitat was disrupted by the evolving Paleozoic Evolutionary Fauna. By mid-Ordovician, stromatolites and thrombolites were small and restricted to marginal, inner-shelf environments. They temporarily regained prominence in the aftermath of the Late Ordovician and end-Permian mass extinctions. In the earliest Silurian, shelf communities were undifferentiated in the long (3-4 MY) aftermath of the mass extinction. Thick stromatolites and thrombolites disappeared when diversity increased and differentiated communities were re-established. This patterns suggests animals that were suppressing stromatolites and thrombolites were reduced or absent after mass extinctions.',40,-112,-1192533,-7475449,'United States','North America',101,'',40.9167,-112.8333,'','',-15.3736656261,-125.876802786,-15.3736656261,-125.876802786,-15.3736656261,-125.876802786,-6.23614,-71.8369,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lost Springs, Nevada',2934,'Union Wash','Triassic','Lower Triassic','Olenekian','Spathian',247.20,251.20,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',246,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,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,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2041,0,'Stromatolitic bioherms.\nNo bioherms in shallow water. \nAbstract of ref. 2041:\nMost of what is known about the biotic recovery from the end-Permian mass extinction has been recovered from strata deposited in shallow-water environments. Yet, properties of the deep-ocean have been invoked as causes for the mass extinction as well as the unusually prolonged biotic recovery from this crisis. A nearshore to shelf transect of the Lower Triassic Virgin/Schnabkaib Limestones of the Moenkopi Formation (southern Nevada) was studied for changes in facies types and biofabrics as well as comparison with the coeval outer slope to deep basin Union Wash Formation (eastern California).\n\nA number of biofabric trends were documented across this transect. Vertical burrows are common in nearshore strata, while horizontal burrows are prevalent in shelf strata. Intervals with relatively high ichnofabric indices (ii 4-5) are more common in shelf than nearshore strata. The most intriguing biofabric trend is the lack of microbial structures, such as stromatolites, in the most nearshore section, with their greatest occurrence found in shelf strata. This anachronistic onshore-offshore trend of stromatolitic development points to offshore and oceanic environments as a likely influence on their formation. Presence of seafloor carbonate cements in coeval slope and deep basin Union Wash strata, implying an offshore presence of water masses supersaturated in calcium carbonate, suggests that unusual ocean chemistry may have played a significant role in the development of Early Triassic shelfal stromatolites. \n',37,-117,699453,-5164712,'United States','North America',101,'',37,-117,'','',22.3681457435,-38.1803837539,22.3681457435,-38.1803837539,16.1729977663,-42.48998498,8.80244,-42.7408,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-16 12:19:55'),('Mfamosing quarry 2',2935,'','Cretaceous','Lower Cretaceous','Albian','Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',107,2,'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','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','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',2042,0,'Stromatolite \'bodies\' in subtidal low energy environment.\nThree horizons in succession.\nSubstantial borings by Lithophaga.',5,8,-1711067,-123867,'Nigeria','Africa',701,'',5.1333,8.5,'','',-7.52899465813,-1.70170936436,-9.20226417607,4.02786473213,-7.52899465813,-1.70170936436,-9.3344,-1.16762,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Adnet',2949,'Adnet','Jurassic','Lower Jurassic','Sinemurian','lower Sinemurian',190.80,199.30,19,'late Hettangian - early Aalenian',188,195,'Early Jurassic (Hettangian&Sinemurian, 196 Ma)',195,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','15','1',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',1,'yes','1','Less than 6 reef building species','2','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2050,2051,'Stromatolitic layer immediately above basal Sinemurian ferromanganese crust.',47,13,4414507,1944161,'Austria','Europe',301,'',47.7,13.1667,'','',31.8620329203,27.3901858985,31.8620329203,27.3901858985,31.9375361903,26.8739049292,32.8773,19.462,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ikebrane, Ajjers Basin',2950,'Assekaifaf','Carboniferous','Mississippian','Visean','upper Visean',330.90,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',332,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m','3','600',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,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2053,0,'Two distinct units of stromatolites. \nCoalesced domes up to 1.5 m thick and 2.5 m in diameter.\nSheltered marine deltaic environment. ',27,9,-4025371,887130,'Algeria','Africa',706,'',27,9.5,'','',-57.2697553994,-6.74677114888,-54.0542429869,-4.6441452921,-36.6390631027,-22.2012266455,-31.8141,7.49323,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-25 17:28:38'),('Ghadames-Fezzan Basin',2951,'Mrar','Carboniferous','Mississippian','Visean','upper Visean',330.90,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',332,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'600','2950',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2053,0,'',28,11,-3901722,1157245,'Libya','Africa',715,'',28.8333,11.3333,'','',-56.7383646156,-2.36090576076,-53.497267557,-0.612451995001,-36.1648694575,-19.2192679778,-30.9404,10.1698,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-25 17:28:44'),('Admiral Bay Fault, Canning Basin',2954,'Goldwyer','Ordovician','Middle Ordovician','Darriwilian','lower Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',466,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick','330',NULL,NULL,NULL,'4','More than 1000 m','1000','16',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','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',2056,0,'Primary reef framework of domical and digitate stromatolites. Flanking deposits are bryozoan and palmatozoan grainstones and packstones.\n\nFrom Webby:\nLocalized stratigraphically within the Goldwyer Formation, of probable early-mid Darriwilian age, and occupy restricted sites immediately adjacent to a major, intra-basinal fault zone (Admiral Bay Fault Zone). Four separate occurrences of these linear-shaped, microbial-dominated reefs are recorded along the main Admiral Bay fault line over a distance of 16 km. They vary from 500 m wide and 330 m thick to 200 m wide and 25 m thick, and at least one is more than 1 km in length. The reefs exhibit a primary reef framework of domical and digitate stromatolites. Flanking deposits are bryozoan and pelmatozoan grainstones, and packstones. The fault system which defines the northeastern margin of the Willara Sub-basin, was apparently active intermittently through Early-Middle Ordovician time. McCracken et al. (1996) suggested that uplift of the footwall side of the main fault produced a narrow, raised, linear belt along the line of the fault, providing suitable shallower depositional conditions for localized reefal growth. The timing of uplift is possibly early Darriwilian. These reefal masses were subsequently fractured by renewed phases of faulting that facilitated movement of mineralizing solutions and extensive alternation of the host rocks, with the emplacement of the Mississippi Valley-type, lead-zinc mineralization.',-18,123,1515446,16624186,'Australia','Oceania',801,'',-18,123,'','',-0.35113193214,98.7713999261,-0.35113193214,98.7713999261,-0.35113193214,98.7713999261,10.0489,153.622,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Victoria Fjord, North Greenland',2955,'Borglum River','Ordovician','Upper Ordovician','Sandbian','Caradocian',451.00,458.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',453,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','90',NULL,NULL,NULL,'3','More than 100 m','200','100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2058,0,'50 to 100 m high mud mounds with irregular fenestrae. Comparable to Meiklejohn Peak mound',81,-45,813618,-3057779,'Denmark','Europe',330,'',81.8333,-45.5,'','',14.2520337726,-75.8649005843,9.75940280116,-83.2502579644,9.75940280116,-83.2502579644,1.94923,-29.8382,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yango-Yakha River, Vaygach Island',2957,'Yugor','Ordovician','Upper Ordovician','Sandbian','Caradocian',451.00,458.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',454,2,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick','3','1','Less than 10 m wide','5','1','Less than 20 m','5',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','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',2061,0,'Small microbial reefs and biostromes dominated by bryozoans.',70,59,-1967522,742115,'Russia','Asia',624,'',70.0833,59.0833,'','',-19.4403019211,-46.0491114074,-13.3460915321,-50.5156170378,-13.3460915321,-50.5156170378,-14.923,6.16378,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Williston Basin, SE Saskatchewan',2959,'Herald','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',445,3,'1','Seismic data available ',1,'True reef','1','Less than 10 m thick','3','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','44','Worms - microbes - (forams) - (bryozoans) - (corals)',NULL,NULL,'80','20','0',0,'no',0,'no',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2063,0,'2.8 m thick reef composed of mottled thrombolitic boundstone with intergrown worm tubes, microbe Ortonella and scattered ramose bryozoans. ',49,-103,-807253,-6608817,'Canada','North America',121,'',49.75,-103.25,'',NULL,-7.01071113704,-118.118618069,-7.01071113704,-118.118618069,-7.01071113704,-118.118618069,-8.47983,-61.3165,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Keisley, northern England',2960,'','Ordovician','Upper Ordovician','Hirnantian','upper Ashgillian',445.20,450.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,3,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,2,'Cold - water','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','0','20',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','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2066,2067,'Mud mound dominated by Girvanella and a rich fauna of brachiopods, trilobites, pelmatozoans, bryozoans etc.',54,-2,-5917209,-1604813,'United Kingdom','Europe',331,'',54.6167,-2.4333,'WAHR','80657',-38.78712652,-74.2861360928,-36.7005380198,-72.132346873,-36.7005380198,-72.132346873,-45.1134,-16.0602,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chair of Kildare, easter',2961,'Kildare Limestone','Ordovician','Upper Ordovician','Hirnantian','Hirnantian',443.40,445.20,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',444,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,2,'Cold - water','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2068,2067,'Only brachiopod fauna in Paleobiology database.',53,-6,-6051651,-1926609,'Ireland','Europe',331,'',53.1667,-6.75,'WAHR','23068',-33.6121698207,-71.234042487,-33.6121698207,-71.234042487,-33.6121698207,-71.234042487,-37.4153,-19.4583,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Woods Gap + Thorn Hill, Tennessee',2969,'Maryville Limestone','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',504,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','35','2','10 - 100 m wide',NULL,'4','More than 1000 m','20000','45',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','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2075,0,'Thickness applies to reef complex. Microbial (Girvanella, Renalcis) reefs often interrupted by emersion surfaces and packstone/grainstone horizons.\nTwo types of boundstones:\nRenalcis-Girvanella\nand\nGirvanella-sponge-Renalcis',36,-83,-2762553,-7290854,'United States','North America',101,'',36.1667,-83.8,'WAHR','24020',9.88551281398,-121.549398552,10.5439804579,-116.723975256,10.5439804579,-116.723975256,-26.847,-91.8002,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zhanjiang, Guangxi',2979,'Yongshien','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',366,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','35','2','10 - 100 m wide','50','3','More than 100 m','180',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,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2084,1866,'In Guangxi, up to 35 m thick and ~50-180m in diameter calcimicrobial Renalcis -Epiphyton mounds of the upper Yongshien Fm. near  Miaomen and Zhaijiang, have their surfaces intersected by sediment-infilled fissures showing contemporaneous erosion (Yu & Shen, 1998). Inter-reef sediments with gastropods, ostracodes and forams indicate a restricted peritidal setting for these reefs. ',22,109,-1316647,10138141,'China','Asia',602,'',22.9,109.7833,'','',-16.6215490672,90.0026656406,-16.6215490672,90.0026656406,-11.8665735819,109.970878245,2.03877,101.379,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('N Holitna Basin, Sleetmute, Alaska',3016,'','Devonian','Lower Devonian','Lochkovian','Lochkovian/Pragian',407.60,419.20,8,'middle Pridolian - middle Pragian',412,415,'Early Devonian (Lochkovian, 415 Ma)',411,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'95','1450',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'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',893,1124,'',62,-156,3117408,-3644915,'United States','North America',101,'',62.1667,-156,'','',4.1155083245,-91.2474815707,4.1155083245,-91.2474815707,28.1011868379,-140.60457934,5.40617,-48.2134,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wangjiaping, Yichang, Hubei',3022,'Tianheban','Cambrian','Series 2','Stage 4','late Botomian-early Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',512,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','2','1','Less than 10 m wide','2','1','Less than 20 m','2',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','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','4','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2127,2360,'Tianheban epoch\n33% archaeocyaths but only one genus\nAbstract of ref. 2127:\nThe limestone of the Tianheban Formation on the Yangtze Gorges belongs to open shelf marine deposit in middle Early Cambrian age. Two distinct types of archaeocyath reefs are preserved - an isolated archaeocyath mud mound, and a patch reef. The reefs are composed of irregular archaeocyathids and calcified microbial microfossils such as Epiphyton, Renalcis, Givanella, etc., belonging to baffling reef mounds. The patch reef succession shows the hydrodynamic changing from low energy to moderately high energy, and then to a low energy environment. ',30,111,2943667,15583975,'China','Asia',602,'',30.6667,111.3,'WAHR','81010',-7.76052013288,76.4166165344,-9.87767984942,79.0339579572,-9.87767984942,79.0339579572,24.2711,158.13,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hwangju District',3031,'Songnim','Ordovician','Lower Ordovician','Floian','Upper Lower Ordovician?',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',476,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','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',2135,0,'Cryptozoon reefs in upper part of Songnim Fm. (Lower Ordovician)',38,125,5056249,14124575,'North Korea','Asia',601,'',38.6667,125.75,'','',17.5089155516,91.3262309921,17.5089155516,91.3262309921,17.5089155516,91.3262309921,-4.11751,134.463,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ch osan',3032,'Montoan Shale','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 ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2135,0,'Girvanella manclurica limestone embedded in shale sequence.',38,125,6214237,-15622512,'North Korea','Asia',601,'',38.9167,125.5,'','',35.8864526101,82.1394567257,30.517600216,84.3114987608,30.517600216,84.3114987608,9.79838,150.367,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kanggye',3033,'Choson Supergroup','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',504,1,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','100',NULL,NULL,NULL,NULL,NULL,NULL,'5',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2135,0,'Middle Cambrian white massive limestone, sometimes oolitic',40,126,5828217,15124377,'North Korea','Asia',601,'',40.9667,126.5833,'','',18.7556871126,91.808456341,16.7215652737,93.4465850622,16.7215652737,93.4465850622,5.99596,144.753,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ch osan',3034,'Fuchoan','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',505,1,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','40',NULL,NULL,NULL,NULL,NULL,NULL,'5',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2135,0,'White massive limestone and oolitic limestone.\n10 species of trilobites',38,125,6080481,14864573,'North Korea','Asia',601,'',38.9167,125.5,'','',20.9654520972,91.7073645269,18.9178056246,93.1713918188,18.9178056246,93.1713918188,4.29433,146.172,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hwangju District',3035,'Songnim','Ordovician','Lower Ordovician',NULL,'Lower Ordovician',470.00,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',480,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2135,0,'',38,125,6008929,14574471,'North Korea','Asia',601,'',38.6667,125.75,'','',16.5109861906,93.2452848441,16.5109861906,93.2452848441,16.5109861906,93.2452848441,-2.9375,136.007,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lost Cabin, Spring Mountains, Nevada',3054,'Moenkopi','Triassic','Lower Triassic','Olenekian','Spathian',247.20,251.20,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',246,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','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,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2143,2184,'Stromatolitic mounds in normal marine environment.\nMaximum thickness 2 m (= syndepositional relief).\nVirgin Member of Moenkopi Fm.\n\nRef 2184: These microbial structures from the Virgin Limestone Member of the Moenkopi Formation have been recently reinvestigated to determine if they represent true reefs. In places microbial mounds occur as isolated patch reefs, although elsewhere they coalesce to form tabular biostromes. These mounds are an agglomeration of smaller subunits that have wavy laminations and thrombolitic textures. Measurements on isolated mounds show that they attained a relief of 1-2 meters above the seafloor. ',36,-115,529534,-5095413,'United States','North America',101,'',36.0833,-115.6667,'','',21.1096848576,-37.4960769189,21.1096848576,-37.4960769189,14.8415349401,-42.008836236,9.1583,-43.9545,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dry Mountain, Last Chance Range, California',3056,'Nopah','Cambrian','Furongian','Lawsonian','Trempealeauan',485.40,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',492,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m',NULL,'100','2836',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2145,0,'',36,-117,1588437,-8498159,'United States','North America',101,'',36.8667,-117.5167,'','',33.5846401385,-132.001322782,33.5846401385,-132.001322782,33.5846401385,-132.001322782,0.56087,-95.4407,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Marmolada, Dolomites',3067,'','Triassic','Middle Triassic','Anisian','latest Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',238,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,'1','Less than 10 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','6','Calcisponges','37','Sponges - microbes - Tubiphytes - (worms)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','7','4','Microbial precipitation',NULL,NULL,'1','Present',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',2155,0,'Cement-rich peloidal boundstones. Low-Mg Cc constituting more than 50% of rock volume. \nCyanobacteria: Ortonella, Cayeuxia, Bavocastria\nSponges: Olangocoelia itti, Deningeria',46,11,1364774,2353634,'Italy','Europe',344,'',46.4333,11.85,'WAHR','67739',15.2213440117,35.636987187,15.2213440117,35.636987187,10.1589846277,25.5732868474,6.3991,23.8561,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Drakht Bid Bala, Mashad, Kopet Dagh',3072,'Mozduran','Jurassic','Upper Jurassic','Oxfordian','Oxfordian/Kimmeridgian',157.30,157.30,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,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','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2168,0,'Patch reefs in open marine facies composed of cyanophyceans and Tubiphytes (forams)\nCommon open marine bioata like bryozoans, brachiopods and minor pelagic fauna associated',36,60,4839317,5924166,'Iran','Asia',505,'',36.5,60.25,'','',33.1157649187,69.8909412024,33.1157649187,69.8909412024,35.3694865116,73.886432399,29.596,69.9051,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Saint-Priest-en-Jarez, Massif-Central',3078,'Saint-Priest-en-Jare','Carboniferous','Pennsylvanian','Gzhelian','lower Stephanian',303.70,307.00,14,'Gzhelian - Asselian',290,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',305,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','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','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2177,0,'= Kasimovian\nSilicified stromatolithic buildups in continental environment',45,4,-412805,1856133,'France','Europe',331,'',45.4667,4.3667,'WAHR','63148',-2.29964807344,16.647115552,-2.29964807344,16.647115552,-2.28352061705,-0.627486121266,-4.00617,16.4925,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Southern Nishiyama',3085,'Omi Limestone','Carboniferous','Pennsylvanian','Bashkirian','middle Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,320,'Early Pennsylvanian (Bashkirian, 319.2 Ma)',315,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','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','4','3','Binder guild','1','Present',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',2181,0,'Stromatolite-like laminar boundstones interpreted as reef-crest boundstone. Skeletal microbes?\n\nMicrobial bindstones with Donezella in lagoonal facies.',36,137,1557904,12755184,'Japan','Asia',625,'',36.9958,137.7667,'WAHR','24134',16.5801688561,134.961097661,16.5801688561,134.961097661,1.62106822422,72.2621274834,8.70984,94.9656,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('SW Virginia',3096,'Nolichucky','Cambrian','Furongian','Jiangshanian','lower Upper Cambrian',491.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',498,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1','1','Less than 10 m wide','2','1','Less than 20 m','10','10',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','0','',0,'No or unknown reservoir potential',2194,0,'Bioherms are 30 cm to 1.5 m high and range from club-shaped heads 30 cm to 2 m in diameter to coalescent forms 10 m wide. Bioherms consist of branching digitate stromatolite columns (1 cm wide, 2 to 4 cm high), lesser sponge and calcareous algae, and interstitial carbonate mudstone and skeletal wackestone.\n\nBioherms overlie flat-pebble breccias that are underlain by ripple-laminated shaly-pellet limestone and interbedded breccia lenses and sheets. Shaly limestones locally overlie fossiliferous marine shale. Bioherms are overlain by ripple-laminated shaly-pellet limestone that also fills interbioherm depressions, and locally by ooid grainstone sheets (up to 8 m thick).',36,-82,-2883428,-7119038,'United States','North America',101,'',36.75,-82,'FALSCH','',8.95351805716,-107.126738216,8.95351805716,-107.126738216,8.95351805716,-107.126738216,-29.7504,-83.9458,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hanwang, Sichuan',3126,'Hanwang','Triassic','Upper Triassic','Carnian','upper Carnian',228.00,230.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',219,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','50','2','10 - 100 m wide',NULL,'2','10 - 100 m','100','25','8',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','43','Siliceous sponges - serpulids - (bivalves) - (calcisponges) - (microbes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2213,0,'> 90% micrite. Microbial origin of micrite suspeceted due to cloudy, clotted and peloidal textures.\nThickness ratio of mounds to inter-mound sediments about 5:1.\n',31,104,3744343,10322263,'China','Asia',602,'',31.4722,104.1458,'FALSCH','',13.879397167,111.221059769,13.879397167,111.221059769,44.4141183439,112.531249567,28.9831,90.7082,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tabuska River-Ufa River',3129,'Kulamat','Devonian','Lower Devonian','Lochkovian','upper Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,415,'Early Devonian (Lochkovian, 415 Ma)',413,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','4','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)',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,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2216,0,'Position not clear.\n\'Algal\'-bryozoan reefs from uppermost Lochkovian (pesavis zone) to lower Pragian (sulcatus-kindley) zone.\nHigh brachiopod diversity.\nSee reef 3130 for Pragian part.',56,59,346836,2079511,'Russia','Asia',624,'',56.4167,59.0833,'WAHR','81662',25.1858600785,-29.8189818238,25.1858600785,-29.8189818238,39.6608222699,-88.6629019256,2.37021,13.9297,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tabuska River-Ufa River',3130,'Kulamat','Devonian','Lower Devonian','Pragian','lower Pragian',407.60,410.80,8,'middle Pridolian - middle Pragian',412,410,'Early Devonian (Pragian, 409.2 Ma)',410,3,'0','Outcropping reef ',1,'True reef','4','More than 500 m thick','1000','4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)',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,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2216,0,'500-1500 m thick reef limestone succession  (=Serginsk reef), approximately equivalent to Koneprusy limestones of Czechia',56,59,346836,2079511,'Russia','Asia',624,'',56.4167,59.0833,'WAHR','81663',25.2798484155,-26.064218276,25.2798484155,-26.064218276,37.5483750721,-86.1773108166,2.00417,16.4473,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Skaz, Nizhnyaya Shemakha River, Urals',3133,'Afonin','Devonian','Middle Devonian','Eifelian','middle Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',394,3,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','40','3','101-1000 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','3','Microbes','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)',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',2216,0,'Ivdelinia acutolobalta zone (=costatus to kockelianus zones).\nMassive reefal limestones bordered by deep-water cherts (tectonic boundary).',56,59,739309,2097531,'Russia','Asia',624,'',56.2833,59.3,'','',15.1150522493,-7.97498178543,15.1150522493,-7.97498178543,31.0734434935,-75.2140128971,4.86286,18.8901,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bol-shaya Nadota Carbonate Complex',3145,'','Carboniferous','Mississippian','Visean','upper Visean-Serpukhovian',323.20,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',326,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','15','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'3','Microbes','2','Algae','61','Microbes (thrombolites) - algae - corals','4','Others','0','50','50',0,'no',0,'no','2','6 to 24 reef building species','9','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite',NULL,NULL,'1','Present',0,'No or unknown reservoir potential',2227,0,'',65,60,3161002,2472330,'Russia','Asia',624,'',65.65,60.9833,'WAHR','13278',-1.03072417935,14.6413829415,4.73376778654,16.5373278168,26.5460502691,-10.9247676556,22.8816,22.841,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nixon Gulch, Horseshoe Hills, Montana',3146,'Snowy Range','Cambrian','Furongian','Jiangshanian','Steptoean',493.00,494.50,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',496,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','6','4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','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',2229,0,'= Dresbachian\nThrombolitic boundstone colums composed of micritic limestone with clotted fabric and colonies of Epiphyton. \nLinear structure parallel to shoreline in intrashelf basin below fair weather wave base, aboutn 50 km wide and 250 km long',46,-111,797874,-6794600,'United States','North America',101,'',46.1667,-111.1667,'WAHR','242',32.3927980584,-111.314474684,32.3927980584,-111.314474684,32.3927980584,-111.314474684,-6.29623,-80.7591,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Swamp Lake, Absaroka Range, Wyoming',3147,'Snowy Range','Cambrian','Furongian','Jiangshanian','Steptoean',493.00,494.50,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',496,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','9','4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250','3146',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','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',2229,0,'See reef 3146',44,-109,685578,-6877939,'United States','North America',101,'',44.8333,-109.9167,'FALSCH','',31.0620176011,-112.349165788,31.0620176011,-112.349165788,31.0620176011,-112.349165788,-7.302,-82.0064,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Eagle Mountain, California',3148,'Carrara','Cambrian','Series 3','Drumian','lower Middle Cambrian',505.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',509,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','6','2','10 - 100 m wide','100','2','10 - 100 m','150',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,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2230,0,'Thrombolite bioherms in Jangle Limestone Member. Some probalbe Renalcis',36,-116,581449,-8925034,'United States','North America',101,'',36.2083,-116.375,'','',31.0018632396,-142.251972443,31.932967971,-135.587320346,31.932967971,-135.587320346,0.606756,-97.0843,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Apuane Alps, Tuscany',3150,'Massiccio Limestone','Jurassic','Lower Jurassic','Hettangian','Hettangian?',199.30,201.30,19,'late Hettangian - early Aalenian',188,195,'Early Jurassic (Hettangian&Sinemurian, 196 Ma)',198,1,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'3','Microbes','1','Corals','61','Microbes (thrombolites) - algae - corals',NULL,NULL,'0','80','20',0,'no',0,'no',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2233,0,'Small microbial(?) mounds with corals and crinoids within shoal complexes.',44,10,4211213,1502986,'Italy','Europe',344,'',44,10.25,'','',27.874340379,25.9043542408,27.874340379,25.9043542408,23.8521868195,26.0346609445,30.8752,12.8914,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Waukesha County, Wisconsin',3169,'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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'70','1851',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'70','0','30',0,'no',0,'no','2','6 to 24 reef building species','11','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2250,0,'Very fossiliferous. This is a typical Wenlockian carbonate mud mound community, in which the core contains mostly carbonate mud, sometimes with Stromatactis-like structures, and echinoderm debris and the flank beds are echinoderm-dominated. Skeletal grains in the flank beds which contain this community can be either moldic or dolomite-replaced, and the texture ranges from non-cherty, porous dolowackestone to dolopackstone, with some grainstone present also in the flank facies, to crystalline dolomudstones and sparse dolowaxkestone to dolopackstone, with some grainstone present also in the flank facies, to crystalline dolomudstones and sparse dolowackestones in the cores. Skeletal grains show the full range from well to poorly sorted, and some graded bedding is present in the inclined beds of the echinoderm facies. Corals, which tend to surround the mound core, are sometimes overturned (Philcox, 1970), and in any case, are not abundant enough to form an organic framework. As noted by Witzke (1981b, 1987b), the general absence of skeletal boundstone fabrics precludes interpretation as an organic-framework reef, but the presence of apparent penecontemporaneous cave and fissure-fills in the core, often with thick trilobite or nautiloid concentrations, plus wedge-shaped debris flows in some facies, suggests that the mounds were rigid features, possibly resulting from submarine cementation processes (Witzke, 1987a). Dolomitized botryoidal and fibrous marine cembents are present. Sedimentary features are consistent with episodic high-energy conditions, such as would result from storm action in depths generally at or slightly below fair weather wave base.',43,-88,-3057394,-5315148,'United States','North America',101,'',43,-88.3333,'WAHR','13353',-26.9483889586,-89.7938784966,-26.9483889586,-89.7938784966,-26.9483889586,-89.7938784966,-21.4529,-51.9119,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('St. Francois Mountain, Washington Co., Missouri',3172,'Bonneterre','Cambrian','Furongian','Jiangshanian','upper Dresbachian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',498,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2254,0,'Bioherm located around a small epicontinental sea island.\r\nCollection of Patzkowsky describes fauna from inter-reef.',37,-90,-1723150,-7557915,'United States','North America',101,'',37.8333,-90.6833,'WAHR','9625',15.6061571902,-113.487323511,15.6061571902,-113.487323511,15.6061571902,-113.487323511,-22.348,-87.7397,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Goodsir Creek, Cornwallis Island, Nunavut',3175,'Douro','Silurian','Ludlow','Ludfordian','upper Ludlow',423.00,425.60,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',420,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'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','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1617,0,'',75,-93,534852,-3464348,'Canada','North America',121,'',75.05,-93.7,'WAHR','5797',5.78122028152,-72.7764580818,5.78122028152,-72.7764580818,5.78122028152,-72.7764580818,2.67868,-30.2891,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Griffin Inlet, Devon Island, Nunavut',3176,'Douro','Silurian','Ludlow','Ludfordian','upper Ludlow',423.00,425.60,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',420,3,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',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',1617,0,'Collections of Alroy include Dragleybeck Inlet.\nA total of 5 coral species identified. + microbes',75,-92,548558,-3286445,'Canada','North America',121,'',75.0833,-92.05,'WAHR','5793',5.61804703982,-72.380464543,5.61804703982,-72.380464543,5.61804703982,-72.380464543,2.35678,-30.009,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mount Irish, Lincoln Co., Nevada',3180,'Guilmette','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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'3','Microbes','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','11','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',2263,0,'the bioherm facies is sometimes described as a calcilutite in the measured section descriptions.\nCollection of Miller',37,-115,-2206198,-6455218,'United States','North America',101,'',37.6667,-115.3333,'WAHR','7117',-17.372593873,-71.9178077983,-17.372593873,-71.9178077983,-12.1980208453,-130.979721825,-20.3522,-58.1873,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lida Wash, Esmeralda Co., Nevada',3181,'Harkless','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 ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','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','5','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',2264,0,'Collection of Patzkowsky\nBonnia-Olenellus zones\nLaterally adjacent to and interfingering with the \nbiostromal limestone is an archaeocyathan-rich biosparite indicating rewroking and deposition as lenses along side the bistromal growths. The siltstones/shales above and below the biostrome are lacking archaeocyathan.\nThe assemblage is found in a biostromal limestone with a boundstone fabric in which micrite mud surrounds the fossils. the formation consists of interbedded sandstone and shales with occasional bedded and/or lenticular limestone.',37,-117,-2256188,-9738371,'United States','North America',101,'',37.5167,-117.5333,'WAHR','7787',28.662423266,-144.079444046,28.662423266,-144.079444046,28.662423266,-144.079444046,-0.278366,-98.5359,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jefferson and Madison counties, Montana',3182,'Sappington','Carboniferous','Mississippian','Tournaisian','lower Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',359,3,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'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','3','4','Microbial precipitation',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',2265,0,'',46,-112,-493444,-4987659,'United States','North America',101,'',46,-112,'WAHR','8606',-8.84548164789,-56.2495590492,-8.84548164789,-56.2495590492,5.16142766139,-101.100728834,-4.24659,-47.8919,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-25 16:49:29'),('Urspring, Bavaria',3193,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','25','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species','33','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2273,0,'Upper Oxfordian to lower Kimmeridgian. \nplanula to platynota zones\nMalm beta and gamma\nMost data from Oxfordian (27 siliceous sponge species).',49,11,5014225,1204240,'Germany','Europe',331,'',49.7333,11.2167,'WAHR','25411',29.8103201035,26.3440469713,29.8103201035,26.3440469713,35.5335119416,27.6454601085,41.0378,19.203,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sierra del Cuera, Asturia',3216,'Valdeteja','Carboniferous','Pennsylvanian','Bashkirian','upper Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',313,3,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','10','90','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',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2290,0,'Upper to middle slope with boundstone types B and C.\nC: Donezella, phylloid and ungdarellid algae, Girvanella and Ortonella\nB: Bryozoans, Sponges, Girvanella and Ortonella\nLower slope with boundstone type A: Bryozoans and sponges.\nHere type C.',43,-4,-644479,1253903,'Spain','Europe',304,'',43.3667,-4.7667,'WAHR','76872',-17.1694062295,5.45710317793,-17.1694062295,5.45710317793,-18.1833799906,-11.3744000511,-9.04632,9.22869,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sierra del Cuera, Asturia',3217,'Picos de Europa','Carboniferous','Pennsylvanian','Moscovian','lower Moscovian',310.00,315.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',310,3,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,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',2290,0,'Uppermost slope boundstone (Type C) with peloidal fabric, and diverse skeletal assemblages. Primary cavities filled bz radial and radiaxial fibrous cement',43,-4,-644479,1253903,'Spain','Europe',304,'',43.3667,-4.7667,'FALSCH','0',-8.80241778004,9.30159514145,-10.3384528265,8.56828303585,-10.7839829843,-11.5407825765,-7.2667,10.3705,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sierra del Cuera, Asturia',3218,'Valdeteja','Carboniferous','Pennsylvanian','Bashkirian','upper Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',313,3,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','36','Bryozoans - sponges - microbes',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'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',2290,0,'Middle and lower slope boundstones (types A and B), see reef 3216 for further remarks.',43,-4,-647219,1254991,'Spain','Europe',304,'',43.3667,-4.7667,'FALSCH','0',-17.1694062295,5.45710317793,-17.1694062295,5.45710317793,-18.1833799906,-11.3744000511,-9.04632,9.22869,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Domkirken, Jameson Land, Greenland',3223,'Wordie Creek','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',250,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2','1','Less than 10 m wide','4','1','Less than 20 m','4',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,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2296,0,'Stromatolithic reefs developed 20 m and 80 m above the base of the formation. Individual domes up to 70 cm in height forming a 1.5 m high and 4 m wide limestone lense resting on calcirudit of fragmented stromatolite heads and thick-shelled Promyalina',72,-24,4249954,593957,'Denmark','Europe',330,'',72.2167,-24.3167,'','',42.2084107857,22.0436888296,42.0010864104,22.0526359959,33.7126592385,13.4271766354,29.5272,13.0386,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shakhtesai Subzone, Axial Zone, Pamirs',3247,'Chichkautek','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 ',NULL,NULL,'3','101-500 m thick','150','2','10 - 100 m wide',NULL,'4','More than 1000 m',NULL,'110',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','19',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2314,0,'',37,74,3480009,8152841,'Tajikistan','Asia',301,'',37.7833,74.25,'WAHR','34645',53.3554118143,83.2723772486,53.3554118143,83.2723772486,20.0300050732,89.034111923,35.2344,59.2381,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kiya River Section, Siberia',3250,'Usa','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)',512,3,'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','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','3','25 or more reef building species','94','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',1220,0,'',55,88,-3175833,2053034,'Russia','Asia',624,'',55.5167,88.0167,'WAHR','56760',-1.98231325753,-43.8679225959,-1.01321004458,-39.6971894847,-1.01321004458,-39.6971894847,-9.67703,7.65428,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shannon County, Missouri',3270,'Eminence','Cambrian','Furongian','Lawsonian','Trempealeauan',485.40,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',492,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','5',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,'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',2331,0,'',37,-91,-1000392,-7445989,'United States','North America',101,'',37.6389,-91.1222,'WAHR','8699',16.03218428,-119.305983098,16.03218428,-119.305983098,16.03218428,-119.305983098,-20.8139,-91.6085,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Clear Creek, Wind River Mountains, Wyoming',3271,'DuNoir Limestone','Cambrian','Series 3','Guzhangian','Dresbachian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',499,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2329,0,'',43,-109,-342914,-7290156,'United States','North America',101,'',43.2897,-109.8319,'WAHR','8957',34.3505877047,-116.331087749,34.3505877047,-116.331087749,34.3505877047,-116.331087749,-3.5477,-85.5153,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Flörsheim, Mainz',3283,'Upper Cerithium beds','Paleogene','Oligocene','Chattian','late Chattian',23.00,25.00,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',24,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','25','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','1','3','Binder 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',2340,0,'Salinity controlled environment.\nCyanophycean crust limestone (Cladophorites)',50,8,6458330,509651,'Germany','Europe',331,'',50.0167,8.4167,'WAHR','70002',47.9930715205,3.62540377694,48.0988489517,3.79622922828,48.7630146741,8.37432527034,49.8954,5.91855,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Oppenheim/Nierstein, Quarry, Mainz',3284,'Middle Cerithium beds','Paleogene','Oligocene','Chattian','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',26,3,'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,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'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','1','3','Binder guild','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',2344,0,'',49,8,6429145,502767,'Germany','Europe',331,'',49.85,8.35,'FALSCH','0',47.8241616305,3.57588903395,47.8241616305,3.57588903395,48.5390075829,8.31066189222,49.6407,5.62398,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cody, Indian Pass Triangle, Wyoming',3294,'Gypsum Spring','Jurassic','Middle Jurassic','Bajocian','Bajocian-Bathonian',166.10,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',167,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1','1','Less than 10 m wide','3','1','Less than 20 m','3',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2352,2353,'Thrombolite patch reefs in mixed carbonate-evaporitic sequence (restricted inner ramp setting).\nPart of abstract of ref. 2353: The observed buildups are approximately 3 meters across and 1 meter thick. Each buildup is composed of circular \'heads\' of layered microbialite with an internal clotted texture (i.e. thrombolite). Individual heads are approximately 0.5 meters in diameter and 0.25 meters thick. Environmental interpretations of these microbial buildups suggest that they developed in shallow water (< 1 meter water depth).\nAs many Jurassic thrombolite reefs discussed in the literature have been interpreted to have developed in deep-water settings, examination of these well-exposed Wyoming reefs provides important contributions to extend the distribution of thrombolite reefs into shallow-water environments. ',44,-109,3703514,-4979122,'United States','North America',101,'',44.5333,-109.05,'','',34.5683602643,-37.4222044261,34.5683602643,-37.4222044261,37.2356663416,-41.1506077202,35.9239,-48.6679,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Arrow Canyon Range, Clark Co., Nevada',3300,'unknown','Cambrian',NULL,NULL,'Millardan',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',492,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15','1','Less than 10 m wide','50','1','Less than 20 m','50','8',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform',NULL,NULL,NULL,NULL,'3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2359,0,'Reef from old Trempelauan\r\n\r\nLithistid sponges prevailint (Lee pers. comm. 2023)\r\n\r\nA sponge-microbialite reef horizon occurs in the upper Cambrian (Millardan) strata of the Arrow Canyon Range, Clark County, Nevada. This horizon represents one of the few metazoan reefs occurring between the extinction of the Archaeocyathids at the end of the early Cambrian and the proliferation of Calathium-sponge-microbialite reefs in the late early Ordovician.\r\n\r\nGood exposures of the reefs occur discontinuously on the western slopes of the Arrow Canyon Range. Uneven dolomitization obscures some reef structures while creating patches of well-preserved reef rock that are up to 15 m thick by 50 m wide. Some dolomitic intervals between reef mounds reveal faint reef-like textures and structures, therefore the shape and extent of the original reef(s) is uncertain. The interval may have extended into the overlying dolostone and the original reef may have formed distinct mounds larger than 50 m wide, or a single continuous biostrome over the 8 km exposure. \r\n\r\nThe reef(s) show an ecological succession from basal-domal stromatolites (0.5 m wide, 1 m tall) to digitate stromatolites (5-20 cm wide, 10-20 cm high), a core of sponge-thromolite reef (3-7 m thick), and a cap layer of columnar stromatolites (20 cm w., 1-2 m h.) with attached and detrital sponges between the columns. Sponges in the core have thin walls (1-2 mm), and are broadly conical to bowl-like in shape, (5-10 cm w/h). They form a closely packed framework that is in-situ with pendent microbialites; Renalcis and Epiphyton. \r\n\r\nAge determination is currently supported by 4 conodont collections from strata underlying the reef through the reef core. Strata below the reef have Proconodontus muelleri and are assigned to that zone. Eoconodontus notchpeakensis occurs in the stromatolitic base and indicates the E. notchpeakensis Subzone of the Eoconodontus Zone. Palaeobotryllus taylori, also from the Eoconodontus Zone, occurs in the core.',36,-114,1369151,-8294308,'United States','North America',101,'',36.5833,-114.9,'',NULL,30.9039186096,-122.416123283,30.9039186096,-122.416123283,30.9039186096,-122.416123283,-1.67019,-91.5257,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-10 13:16:52'),('Maldeota, Mussoorie Hills, Uttar Pradesh',3301,'Krol','Cambrian','Terreneuvian','Fortunian','Nemakit-Daldynian',529.00,541.00,1,'Nemakit/Daldynian - Toyonian',520,540,'Cambrian/Precambrian boundary (541 Ma)',535,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'3','Microbes','4','Stromatoporoids','7','Archaeocyaths - microbes',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2361,0,'Basal Cambrian of uppermost Krol Formation with small patch reef in irregular lenses.\nTwo species of stromatoporoid-grade sponges and on possible calcimicrobe',30,78,-294915,17394573,'India','Asia',501,'',30.35,78.1333,'WAHR','63045',-14.3191217429,68.7997153723,-14.3191217429,68.7997153723,-14.3191217429,68.7997153723,-6.23068,169.001,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Northern Bustamante Canyon, Nuevo Leon',3313,'Cupido','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 ',3,'Mud mound or bank','2','10 to 100 m thick','20','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','45','Siliceous sponges - calcisponges - microbes - (algae)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2366,0,'Type 2\nLower Cupido Formation.\nSponge-microbial mud mounds on outer ramp setting\nMicrobes, siliceous sponges,  calcisponges, coralline algae',26,-100,1232693,-6069193,'Mexico','North America',105,'',26.5333,-100.5333,'','',20.2189875387,-47.2840356857,20.2189875387,-47.2840356857,23.5059850714,-53.2304254475,24.8894,-54.0743,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Piedra Santa Range, Neuquén Basin',3329,'Los Molles','Jurassic','Lower Jurassic','Toarcian','(early?) Toarcian',174.10,182.70,19,'late Hettangian - early Aalenian',188,180,'Early Jurassic (Toarcian, 178.4 Ma)',182,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15','2','10 - 100 m wide','40','2','10 - 100 m','60',NULL,NULL,2,'Cold - water','4','Basin','4b','Deep basin (> 200 m)','2','Below fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2385,0,'Stromatolithic bioherms with worm tubes enclosed in shales and silts. Part of deepening upward sequence.\nDepth estimated several 100 m.',-39,-70,-5492866,-2676945,'Argentina','South America',201,'',-39.3539,-70.5122,'','',-40.3950958242,-35.3877521266,-40.3950958242,-35.3877521266,-35.8280479051,-36.2430449257,-37.6915,-30.5315,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dajiang II, Great Bank of Guizhou',3333,'','Triassic','Lower Triassic','Olenekian','Smithian-Spathian',247.20,251.20,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',248,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2',NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','3','Binder 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',144,225,'',25,106,1752516,10294538,'China','Asia',602,'1814',25.55,106.8667,'WAHR','85071',-12.7672985953,108.278471689,-12.7672985953,108.278471689,14.0627392524,120.714571638,8.48601,97.7749,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Driedoornmlakte, Zaris Subbasin',3339,'Kuibis Subgroup','Ediacaran','Ediacaran','Nama Assemblage','middle Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',555,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',2392,2441,'Coalesced thrombolite mounds with stromatolithic cover',-24,16,-5251679,-15618045,'Namibia','Africa',NULL,'',-24.8667,16.6333,'WAHR','51737',-44.6903017217,82.607814406,-44.6903017217,82.607814406,-44.6903017217,82.607814406,-41.4435,-177.876,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nopah Range, California',3340,'Bonanza King','Cambrian','Furongian','Paibian','latest Marjumian-Steptoan',493.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',498,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','8','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2393,0,'',36,-116,569115,-8892364,'United States','North America',101,'',36.0833,-116.1667,'WAHR','44745',32.3573991023,-131.616052837,32.3573991023,-131.616052837,32.3573991023,-131.616052837,-3.3053,-92.8634,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mohawk Hill, California',3341,'Bonanza King','Cambrian','Furongian','Jiangshanian','lower Steptoan',493.00,494.50,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',497,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','8','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2393,0,'',35,-115,526629,-8838916,'United States','North America',101,'',35.4917,-115.5583,'WAHR','44746',30.9918592782,-124.353377083,30.9918592782,-124.353377083,30.9918592782,-124.353377083,-3.61495,-91.65,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Delamare Mountains, California',3342,'Bonanza King','Cambrian','Furongian','Paibian','latest Marjumian-Steptoan',493.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',498,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','5','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2393,0,'',37,-114,329200,-8668573,'United States','North America',101,'',37.1667,-114.25,'WAHR','44747',31.4768548833,-129.657200726,31.4768548833,-129.657200726,31.4768548833,-129.657200726,0.0313572,-93.7347,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mons Glacier, British Columbia',3354,'Mistaya','Cambrian','Furongian','Lawsonian','Sunwaptan',491.00,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',492,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','6','1','Less than 10 m wide','10','1','Less than 20 m','15',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2405,1141,'Thrombolitic mounds, \'patch reefs\' on coarse skeletal grainstones',51,-117,2426751,-6558919,'Canada','North America',121,'2700',51.8667,-117.1333,'WAHR','81301',38.8314031985,-110.956198072,38.8314031985,-110.956198072,38.8314031985,-110.956198072,1.36889,-77.6194,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sasso Piatto, Dolomites',3355,'Wengen-Cassian','Triassic','Middle Triassic','Ladinian','late Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',231,3,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'3','Microbes','6','Calcisponges','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2406,0,'Cipit boulders interpreted as reworked blocks from mud mounds.\n21% cements, 6% fossils, rest is 49% automicrite, 10% allomicrite and 14% microspar',46,11,1369151,2313154,'Italy','Europe',344,'',46.5,11.7333,'WAHR','45434',16.6278436467,34.9998383015,16.6278436467,34.9998383015,10.6904151736,23.242539243,7.76295,22.3318,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Arzo, Lugano',3370,'Broccatello','Jurassic','Lower Jurassic','Sinemurian','lower Sinemurian',190.80,199.30,19,'late Hettangian - early Aalenian',188,195,'Early Jurassic (Hettangian&Sinemurian, 196 Ma)',194,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,'1','Less than 10 m wide',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','11','Siliceous sponges','45','Siliceous sponges - calcisponges - microbes - (algae)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2420,0,'Red stromatactis limestone, massive, inclosed in mound-shaped \'biohermal Broccatello\' rich in brachipods and calcareous sponges, some solitary corals, common crinoids.\nSeveral meters thick, origianal thickness estimated to be 50 m.',45,8,4481392,1580841,'Switzerland','Europe',331,'',45.8667,8.9333,'WAHR','48131',19.4469160863,24.6090634242,19.4469160863,24.6090634242,27.1575583365,28.125637513,33.2765,15.3972,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Morte Mérie, Balazuc, Ardeche',3371,'','Jurassic','Middle Jurassic','Bathonian','upper Bathonian',166.10,168.30,21,'late Bathonian - early Tithonian',151,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',165,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2421,0,'Ref. 2421: One kilometre further south of the MM1 site, the lowermost Sinemurian bioclastic limestones are unconformably overlain by an upper Bathonian, 1-m-thick bed of pure micritic bearing Stromatactis-like features, and capped by large oncolites (referred to as \'Snuff boxes\'- Elmi, 1990) , in addition to brachiopods and belemnite rostra. This bed is interpreted as a low-relief mud-mound deposited on the Middle Jurassic depositional slope in quite deep-water environments. \n',44,4,4198289,868067,'France','Europe',331,'',44.5,4.3667,'','',23.1234900472,25.6975351685,23.1234900472,25.6975351685,28.2705820656,25.9316108242,34.2153,14.7791,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Anna Quarry, Illinois',3385,'Ste. Genevieve Limestone','Carboniferous','Mississippian','Serpukhovian','lower Chesterian',334.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',332,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','4','1','Less than 10 m wide',NULL,'1','Less than 20 m','12',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species','10','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2431,0,'Lowermost Chesterian (Asbian-Brigantian) microbial mounds. Bryozoans boundstone (laterally grading into microbial-serpulid-bryozoan boundstone) at windward side of mound. and overlain by solenoporacean boundstones.',37,-89,-1505449,-3517772,'United States','North America',101,'',37.45,-89.2333,'WAHR','76724',-26.6716401731,-47.0271013997,-26.6716401731,-47.0271013997,-12.467295004,-69.4637745484,-14.5345,-33.5059,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Buncombe quarry, Johnson Co., Illinois',3386,'Kikaid Limestone','Carboniferous','Mississippian','Serpukhovian','Arnsbergian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',321,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2431,0,'Fenestrate bryozoan (Archimedes, Fenestella) mud-mound in Cave Hill Member of the Kinkaid Limestone (upper Chesterian).\nSponge spicules becoming more abundant upwards',37,-88,-1539496,-3504922,'United States','North America',101,'',37.4667,-88.9667,'WAHR','76725',-22.5547552871,-40.1486049383,-26.1313339948,-45.6177573296,-12.7826205712,-66.9195189397,-14.2203,-32.8101,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grafton, Jersey Co., Illinois',3387,'Choteau Limestone','Carboniferous','Mississippian','Tournaisian','upper Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',351,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','0','20',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2431,0,'Small possible mounds at Chautauqua and Mason Hollow.\nFenestellid bryozoan-crinoidal wackestone core. Sponge spicules, brachiopods and small solitary corals present but rare.',38,-90,-2628368,-3992117,'United States','North America',101,'',38.9667,-90.4333,'','',-30.4674772991,-55.3108060629,-30.4674772991,-55.3108060629,-10.2596464342,-93.1862024617,-22.0016,-37.1431,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Noel, McDonald Co., Missouri',3388,'Compton Limestone','Carboniferous','Mississippian','Tournaisian','upper Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',351,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','9','1','Less than 10 m wide',NULL,'2','10 - 100 m','80',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2431,0,'Wackestone buildups with common fenestellid bryozoand fragments. Spar-filled cavities relatively common. Clotted texture.',36,-94,-2588099,-4350225,'United States','North America',101,'',36.5333,-94.4833,'FALSCH','0',-28.7696023051,-59.5044169903,-28.7696023051,-59.5044169903,-10.538431973,-97.2647700565,-22.2589,-41.4754,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Broughton field, Hamilton Co., Illinois',3391,'Ullin Limestone','Carboniferous','Mississippian','Visean','Arundian',342.00,345.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',341,3,'1','Seismic data available ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',2432,0,'Waulsortian type mud mounds in Ullin Limestone',37,-88,-1607557,-3446205,'United States','North America',101,'',37.9333,-88.45,'','',-28.5565265056,-49.4166976808,-29.9890818339,-52.180342486,-11.2951089796,-80.9269422081,-17.3714,-35.2429,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Swartkloofberg, Witputs Subbasin',3399,'Schwarzrand Subgroup','Ediacaran','Ediacaran','Nama Assemblage','upper Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',544,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','1','Corals','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2441,0,'Pinnacle reefs, fifty to 70 m wide\nat their base and up to 50m high, associated with drowning\nAbundan Namacalathus',-28,18,-5176949,-15511357,'Namibia','Africa',NULL,'',-28.5833,18,'WAHR','51738',-42.9684077716,87.4781203352,-42.9684077716,87.4781203352,-42.9684077716,87.4781203352,-40.0699,-173.039,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mukhaizna-11 well, South Oman Salt Basin',3400,'Birba','Ediacaran','Ediacaran','Nama Assemblage','upper Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',544,3,'1','Seismic data available ',3,'Mud mound or bank','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','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','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2442,0,'Thrombolitic bioherms with Cloudina and Namcalathus.\r\nPaper focussed on extinction of the two genera',18,54,-1259997,16105389,'Oman','Asia',503,'',18.75,54.5,'WAHR','51739',-5.83384285538,42.8092619386,-5.83384285538,42.8092619386,-5.83384285538,42.8092619386,4.15781,143.177,'Kiessling','Krause','2021-05-28 15:21:12','2022-06-28 17:40:31'),('Kiya River Section, Siberia',3401,'Ust\'kundat','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',524,2,'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','2','6 to 24 reef building species','6',NULL,NULL,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,'',55,88,-3175833,2053034,'Russia','Asia',624,'1221',55.5167,88.0167,'WAHR','56740',-4.36735330259,-55.7206788355,-4.36735330259,-55.7206788355,-4.36735330259,-55.7206788355,-13.533,6.47143,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Septatrypa Mound, El Borj, Khenifra, Meseta',3405,'Serie a facies flysch','Silurian','Pridoli','Pridoli','lower Pridolian',419.20,423.00,8,'middle Pridolian - middle Pragian',412,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',418,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15','1','Less than 10 m wide','30','2','10 - 100 m','70',NULL,NULL,2,'Cold - water','4','Basin','','Unknown','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',2452,0,'Cold seep mound packed with brachiopod Septatrypa\nAge based on finds of Ozarcodina remscheidensis eosteinhornensis.',33,-5,-8843089,1384770,'Morocco','Africa',714,'',33.0669,-5.6033,'WAHR','58097',-42.125001355,-10.8901645615,-42.125001355,-10.8901645615,-42.125001355,-10.8901645615,-67.1494,24.4758,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Top of Iberg, vent mound, Harz',3406,'','Carboniferous','Mississippian','Visean','latest Visean',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',328,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2','1','Less than 10 m wide','10','1','Less than 20 m','10',NULL,NULL,2,'Cold - water','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','2','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2453,2452,'Microbial limestone with thrombolite and botroyoidal cement. Brachiopod floatstones. Very negative isotope values indicate cold-seep setting. ',51,10,-315487,1367028,'Germany','Europe',331,'',51.8269,10.2431,'WAHR','62875',-31.1738013544,0.432843261921,-25.6538585404,3.09323956953,-1.90846593778,-19.9643039651,-4.6585,10.352,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tantes Mound, Pyrenees',3407,'Calcaire de l\'Iraty','Carboniferous','Pennsylvanian','Moscovian','lower Moscovian',310.00,315.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',310,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,2,'Cold - water','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2452,0,'Age indicated as Namurian E-G by conodonts.\nMound surrounded by shales. Interpreted as cold-seep mound',42,0,-836206,1584538,'France','Europe',331,'',42.7183,-0.3028,'','',-10.8826150761,11.9354687386,-12.4207462953,11.2137200558,-12.7888542421,-8.82988950053,-9.39357,12.9548,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vadi-Bala, Tapsa River basin, Tuva',3416,'Il\'chir','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 ',2,'Reef mound',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','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','30','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',2462,0,'Two reefal bands:\n1. Limestones, dolomitized, massive, archaeeocyathit-algal, white, gray or cherry-red, and also limestone breccias and bioherms with archaeocyathids, which are evenly distributed through the band.\n\n2. Tuffs, tuffites, and more rarely dacite porphyries of dirty-brown, gray or greenish-gray color, with lenses of algal and archaeocyathid-algal-limestones, massive and dolomitized.',51,94,-2318953,2444626,'Russia','Asia',624,'',51.8833,94.4167,'WAHR','51431',2.58338950139,-45.8211760023,2.58338950139,-45.8211760023,2.58338950139,-45.8211760023,-6.33806,4.66906,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Drab-Beavertown, Blair County, Pennsylvania',3425,'Gatesburg','Cambrian','Furongian','Lawsonian','lowermost Sunwaptan',491.00,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',494,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'30','2743',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,'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',2470,0,'Microbial reefs, rich in trilobites',40,-78,-2062245,-6300054,'United States','North America',101,'',40.3833,-78.2,'WAHR','62077',10.1209480491,-107.308422438,10.1209480491,-107.308422438,10.1209480491,-107.308422438,-30.2193,-83.1999,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nzala, High Atlas',3444,'Idikel','Jurassic','Lower Jurassic','Sinemurian','upper Sinemurian',190.80,199.30,19,'late Hettangian - early Aalenian',188,195,'Early Jurassic (Hettangian&Sinemurian, 196 Ma)',191,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2486,0,'Mud mound in upper member of Idikel Fm.\nLower part of upper Sinemurian.',32,-4,3361185,-670313,'Morocco','Africa',714,'',32.41,-4.55,'WAHR','68164',15.9236599921,3.53933377445,15.9236599921,3.53933377445,26.073649636,6.16387351502,25.0547,-6.41192,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chargey-lès-Port',3449,'','Jurassic','Middle Jurassic','Bajocian','lower Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',170,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','12','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,'100','340',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2490,0,'Coral-microbialite reefs with up to 70% microbialite.\n7 reef units. Four basal bioherm, three upper biostrome',47,5,4660159,1151328,'France','Europe',331,'',47.7333,5.9833,'WAHR','66947',26.8906400889,26.4369507931,26.8906400889,26.4369507931,31.2281113624,26.6192405852,37.2399,15.8737,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S2 Gold Point, Esmeralda Co., Nevada',3462,'Harkless','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)',512,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'1','Less than 20 m','5',NULL,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','1','Less than 6 reef building species','4','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',2495,0,'Archaecyath bioherms with Renalcis and coralomorphs.\nComposition: \n7% archaeocyaths\n24% Renalcis\n4.5% coralomorphs (calcitic)\n36% lime mud\n12.6% cement\n10% quartz sand',37,-117,-2237989,-9699977,'United States','North America',101,'',37.35,-117.2833,'WAHR','63883',32.1524172841,-141.414575343,32.5043684244,-138.515084581,32.5043684244,-138.515084581,2.30769,-96.9005,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yatton, Bristol, England',3463,'Clifton Down Limestone','Carboniferous','Mississippian','Visean','upper Holkerian',340.00,341.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',337,3,'1','Seismic data available ',4,'Biostrome','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,'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',2496,0,'Thrombolite-Ortonella reefs, originally deposited as biostromes. In beds up to a meter in thickness. Mound-like structures also present. \n\nThis comprising the sites: Yatton, Backwell, Flax Bourton and Avon Gorge.\n\nRestricted lagoonal setting inferred.',51,-2,-726668,443609,'United Kingdom','Europe',331,'',51.3833,-2.8167,'','',-28.7629489009,-6.62559798086,-34.1788177292,-10.0865716746,-5.93863009485,-37.5434331804,-9.17582,0.514313,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chipping Sodbury, Bristol, England',3464,'Clifton Down Limestone','Carboniferous','Mississippian','Visean','upper Holkerian',340.00,341.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',337,3,'1','Seismic data available ',4,'Biostrome','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,'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',2496,0,'This comprising sites: Wick and Chippind Sodbury\nSee also reef 3463',51,-2,-699275,465881,'United Kingdom','Europe',331,'',51.5333,-2.4167,'FALSCH','0',-28.607777115,-6.34512927326,-34.0372078845,-9.77968802324,-5.70115555447,-37.3745659629,-8.98693,0.738342,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cerros de la Proveedora, Sonora',3466,'Buelna','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',511,3,'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','1','Less than 6 reef building species','5','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','',1,'Potential reservoir',1070,0,'cryptalgal boundstones and oncoidal wackestone-packstone and ooid grainstone\nprobably formed subtidally above storm wavebase\ntrilobites and echinoderms reported to be present, but not listed',30,-112,-2844067,-10089239,'Mexico','North America',105,'',30.7,-112.2667,'WAHR','62870',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'),('Artavaggio II, Southern Alps',3477,'Riva di Solto Shale','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','11','Serpulids - algae - microbes',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1027,0,'',45,9,2936076,1581750,'Italy','Europe',344,'',45.9417,9.5722,'WAHR','67731',21.4140088421,28.7685527937,24.1848066675,27.7415155236,21.3290639828,22.870040792,29.2772,12.7293,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sierra de Cazorla (RGCHSP), Andalucia',3486,'','Jurassic','Upper Jurassic','Oxfordian','middle/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','1','Less than 10 m thick','4','1','Less than 10 m wide',NULL,'1','Less than 20 m','10',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2507,0,'',37,-2,3387619,-10463,'Spain','Europe',304,'',37.9167,-2.9167,'WAHR','68306',16.6159641757,13.7761063936,16.6159641757,13.7761063936,23.4863625812,10.4033235571,29.8202,5.73745,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('La Grosse Romaine Island, Quebec',3519,'Romaine','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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',2516,0,'Sainte-Genevieve member dolomitic,stromatolitic lithified wackestone small anthaspidellid bioherms',50,-63,-2507479,-4101419,'Canada','North America',121,'',50.2667,-63.8167,'WAHR','66131',0.829970335893,-86.9594880369,0.829970335893,-86.9594880369,0.829970335893,-86.9594880369,-29.3111,-51.8349,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Goodsir Creek, Cornwallis Island, Nunavut',3524,'Barlow Inlet','Silurian','Ludlow','Ludfordian','Ludfordian',423.00,425.60,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',420,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','','Unknown',NULL,NULL,'3','Microbes','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2521,0,'small mudmound and flanking crinoidal packstone',74,-93,548558,-3452988,'Canada','North America',121,'',74.8167,-93.4,'WAHR','64729',5.53834275854,-72.8156406457,5.53834275854,-72.8156406457,5.53834275854,-72.8156406457,2.47877,-30.4326,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Washington County, Missouri',3525,'Gasconde','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',487,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','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',2522,0,'',37,-90,-1068754,-7418564,'United States','North America',101,'',37.9333,-90.7833,'WAHR','64584',11.6831839354,-107.472584849,11.6831839354,-107.472584849,11.6831839354,-107.472584849,-23.7406,-80.6694,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sharyu River section, Chernyshev Ridge',3537,'','Devonian','Upper Devonian','Famennian','lower Famennian',358.90,372.20,10,'Givetian - early Famennian',375,370,'Late Devonian (early Famennian, 370 Ma)',374,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','300',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','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,'1','Present','2','Medium zonation',NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2536,0,'Microbial boundstone, stromatolite boundstone, peloidal limestone, interpreted to having formed under nutrient-rich conditions.\nStarts in upper Frasnian but largely Famennian',66,59,1587144,999075,'Russia','Asia',624,'',66.3333,59.3333,'WAHR','77333',-2.84280461638,3.99262766726,-2.84280461638,3.99262766726,29.4240480807,-63.5854901241,12.4937,9.47366,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('ENE of Xuyong, Sichuan Basin, Guizhou',3552,'Siniulan','Silurian','Llandovery','Aeronian','Aeronian?',438.50,440.80,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',436,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','35','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','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','1','Present',1,'Potential reservoir',2556,0,'Exact position unclear.\nMud mounds with Stramatactis in open shelf environment, deeper water. Mound cores composed of clotter micrite.\nIndividual mound small but composite up to 35 m. Mound tops dolomitized',28,106,82309,14621744,'China','Asia',602,'',28.3333,106,'','',4.31413205464,69.9257215609,4.31413205464,69.9257215609,4.31413205464,69.9257215609,9.26719,127.248,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Microconch reef, S of Liege',3561,'','Devonian','Upper Devonian','Famennian','upper Famennian',358.90,372.20,11,'late Famennian - early Visean',351,360,'Devono-Carboniferous Boundary (358.9 Ma)',363,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2568,0,'The framework of these small domal-shaped reefs was owing to microconchids and calcimicrobes (Garwoodia, Mitcheldeania).',50,5,-1532688,560408,'Belgium','Europe',331,'',50.5,5.5833,'','',-31.9910730182,-7.03952731552,-31.9910730182,-7.03952731552,-1.43442998439,-61.2410230157,-18.1009,4.80296,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Engihoul Quarry, Liege',3562,'Lives','Carboniferous','Mississippian','Visean','Holkerian',340.00,342.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',338,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','2','1','Less than 10 m wide','5','1','Less than 20 m','5',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','4','3','Binder guild',NULL,NULL,'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',2569,2568,'Local stage Livian (approximately Holkerian).\na massive lens (2 m high, 5 m across) composed of massive, dark\ngrey limestone. Microscopically, the\ncentral part of the lens consists of microbe-bryozoan\nboundstones.',50,5,-706124,1053727,'Belgium','Europe',331,'',50.5833,5.4167,'WAHR','76654',-29.0502789262,-0.646133616887,-35.22868016,-4.05902373544,-4.15017016917,-33.2102709432,-8.94328,5.66227,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hohe Warte, Carnic Alps',3565,'Rauchkofel Limestone','Devonian','Lower Devonian','Lochkovian','Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,415,'Early Devonian (Lochkovian, 415 Ma)',413,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','9','2','10 - 100 m wide',NULL,'2','10 - 100 m','80',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','2','Algae',NULL,NULL,'2','Green algae','30','60','10',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2572,0,'Microbial mounds are documented\nin the Lower Devonian Rauchkofel Limestone.\nBaffling organisms, especially calcareous green\nalgae (Hubmann 1994) and ramose-branching\ntabulate corals, predominate.\nThe dimension of the lensshaped body is about 60-80 m in length and 8-10m in height.',46,12,-5464555,4727629,'Austria','Europe',301,'',46.6,12.8667,'','',-22.643566585,15.4646604522,-22.643566585,15.4646604522,46.6,12.8667,-50.2952,57.8639,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Plopis Mountains, Simleu Basin, Salaj',3576,'unknown','Neogene','Miocene','Middle Miocene','Sarmatian',11.60,12.70,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',12,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','10','1','Less than 10 m wide',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','3','Microbes','8','Serpulids, worms, vermetids','44','Worms - microbes - (forams) - (bryozoans) - (corals)',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3576,3577,'serpulid-bryozoan-microbial bioherms 2-10 m thick.',47,22,6187800,1782809,'Romania','Europe',348,'',47.1333,22.6833,'WAHR','70575',46.5398962315,19.8451074488,46.5843796496,19.9656266603,46.3499186549,18.6656084063,46.5952,22.2989,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sierra de la Joya, Lujar',3612,'','Triassic','Middle Triassic','Anisian','Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',240,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20','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','3','Microbes','2','Algae','61','Microbes (thrombolites) - algae - corals','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species','4','3','Binder guild',NULL,NULL,NULL,NULL,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',2608,0,'Upper Anisian?\nMounds in a lagoonal setting\nbafflestones containing dasycladaceans, gastropods, bivalves, echinoderms ... together with solitary corals and branching cyanophytes (core facies), which alternate with Spongiostromata crusts (cap facies)',36,-3,647219,1020859,'Spain','Europe',304,'',34.22,-2.25,'WAHR','73975',16.5450060908,12.1733886806,16.5450060908,12.1733886806,7.33981549123,6.53243109463,1.77388,5.38113,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Road Cebulovica-Kozina',3638,'Trstelj','Paleogene','Paleocene','Selandian-Thanetian','Thanetian',56.00,59.20,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',57,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','21',NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'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,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2620,2624,'Road-cuts along the motorway between Cebulovica and Kozina.\n\nModies of massive bindstone-bafflestones composed of scleractinian corals, crustose coralline algae and encrusting foraminifers - exceeding 20 m in thickness. \n\nRef. 2624: coral-microbialite mud mounds and\nwackestones with thin foralgal crusts',45,13,4919856,1268485,'Slovenia','Europe',328,'',45.8333,13.8833,'','',37.054127213,13.4359322094,37.054127213,13.4359322094,40.0937919633,14.6089709975,36.1442,12.8884,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Poederlee, microbial buildup',3644,'','Carboniferous','Mississippian','Visean','Asbian',336.00,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',334,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','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',NULL,NULL,'0','',0,'No or unknown reservoir potential',2628,0,'Lower Warnantian age\n5 microbial reef mound intervals with microbial boundstone core facies and bioclastic packstone/grainstone flank and top facies',51,4,-692427,998363,'Belgium','Europe',331,'',51.2333,4.8167,'WAHR','76655',-32.3989737496,-3.33238491032,-31.5852886364,-2.87803190522,-4.18845176871,-29.4459607355,-7.55185,5.986,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Popeshall Quarry Buildup, Dublin',3649,'Lane','Carboniferous','Mississippian','Visean','upper Chadian',345.00,346.00,11,'late Famennian - early Visean',351,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',342,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8','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','3','Microbes','2','Algae','61','Microbes (thrombolites) - algae - corals','2','Green algae','20','20','60',0,'no',0,'no','2','6 to 24 reef building species','7','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',2631,0,'Includes Curkeen Hill Quarry Buildup\n\nMassive buildup facies with a bank-like structure, 2 m thick, intercalated with thin grainstone beds, crinoids are the most conspicuous macrofauna, rare solitary corals in the lower part\n\nMilverton carbonate platform\n\nThe buildups developed on the Milverton carbonate platform, whereas the Waulsortian buildups in the S Co. Dublin developed in a deeper ramp setting of the Dublin Basin.',53,-6,-1423691,-435857,'Ireland','Europe',331,'',53.55,-6.1333,'WAHR','76877',-30.2587943475,-11.2160028901,-33.2533578095,-13.7279800464,-3.35345500853,-46.9184743525,-9.35772,-2.61152,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Clonalvy Buildup, Dublin',3650,'Lane','Carboniferous','Mississippian','Visean','upper Chadian',345.00,346.00,11,'late Famennian - early Visean',351,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',342,3,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','2','Algae','61','Microbes (thrombolites) - algae - corals','2','Green algae','20','40','40',0,'no',0,'no','2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2631,0,'massive buildup facies with thin bioclast layers alternating with micritic laminae, bioclast layers with concentrations of kamaenids, ostracods, or Koninckopora.\n\nMilverton carbonate platform',53,-6,-1420964,-440277,'Ireland','Europe',331,'',53.5833,-6.3333,'WAHR','76879',-30.2151733343,-11.3495604634,-33.2081889512,-13.8652114712,-3.36563793246,-47.041439652,-9.34166,-2.73547,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Salmon Hill Buildup, Dublin',3651,'Holmpatrick','Carboniferous','Mississippian','Visean','Arundian',342.00,345.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',341,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','2','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','4','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',2631,0,'3 m massive pale grey micritic rocks, peloidal matrix textures predominate and are locally coated by cryptalgal structures, dasycladacean algae are absent',53,-6,-544446,218731,'Ireland','Europe',331,'',53.5833,-6.2167,'WAHR','76880',-30.2213200527,-11.269771814,-32.8023538163,-13.2968225063,-3.85305790334,-44.2975466285,-8.41156,-2.46605,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hoare-s Rock Buildup, Dublin',3652,'Holmpatrick','Carboniferous','Mississippian','Visean','Holkerian',340.00,342.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',337,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3','1','Less than 10 m wide',NULL,'1','Less than 20 m','10',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'30','0','70',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',2631,0,'buildup sediments in a 3 m high and 10 m wide outcrop, crinoids are the only conspicuous macrofauna, bryozoans relatively common\n\nMilverton carbonate platform',53,-6,-507439,205447,'Ireland','Europe',331,'',53.5667,-6.4,'WAHR','76881',-26.5419786648,-9.04562146109,-32.3134086972,-12.8187909667,-4.58816802398,-41.0607359096,-7.45348,-2.11455,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Milverton Quarry Buildup, Dublin',3653,'Holmpatrick','Carboniferous','Mississippian','Visean','Holkerian',340.00,342.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',337,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','7','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',2631,0,'buildup facies is dominated by peloid-rich matrix textures',53,-6,-547188,227610,'Ireland','Europe',331,'',53.5667,-6.1333,'WAHR','76882',-26.5498444106,-8.8687846709,-32.331258227,-12.632553641,-4.53243810257,-40.9120038025,-7.43633,-1.95575,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Heceta Island, Marble Cove, Alaska',3707,'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 ',3,'Mud mound or bank','1','Less than 10 m thick','10','2','10 - 100 m wide',NULL,'3','More than 100 m','200',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','66','Stromatolites-\'sphinctozoans\'-(stromatoporoids, algae, corals)',NULL,NULL,'20','40','40',0,'no',0,'no','1','Less than 6 reef building species','5','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1102,1650,'stromatolitic mud mound, 10 m thick and 200 m wide',55,-133,699275,-7409719,'United States','North America',101,'',55.7833,-133.4833,'WAHR','79356',6.88822771541,-118.044025651,6.88822771541,-118.044025651,6.88822771541,-118.044025651,-2.78184,-91.8877,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tsakhir-Khalgain-Nuru, Tsogt area',3725,'Tsogt','Devonian','Lower Devonian','Lochkovian','Lochkovian/Pragian',407.60,419.20,8,'middle Pridolian - middle Pragian',412,415,'Early Devonian (Lochkovian, 415 Ma)',412,1,'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','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','5','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2662,0,'Described as algal-coral bioherms, bryozoans common and described',45,96,6681758,2913882,'Mongolia','Asia',NULL,'',45.3333,96.6333,'WAHR','79713',66.6803056428,-45.2353953675,66.6803056428,-45.2353953675,54.0358328046,45.3065131526,43.3242,12.428,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sukharikha River, Siberia',3756,'Krasnoporog','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',520,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,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',1940,2682,'lowermost Atdabanian, bioherms in the back-reef lagoon\ntwo 1 m thick layers of pink lime mudstone with irregularly shaped archaeocyath-calcibiont bioherms',67,87,-4185360,999943,'Russia','Asia',624,'',67.2167,87.0333,'WAHR','80843',-9.43263208062,-56.0516980464,-9.43263208062,-56.0516980464,-9.43263208062,-56.0516980464,-21.2811,-0.496564,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mojero River, Siberia',3757,'Kotuy','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 ',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','12','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,'Previously combined with 1778 as Tommotian/Atdabanian',68,105,-3598492,332027,'Russia','Asia',624,'1043',68.6333,105.15,'WAHR','80870',-5.15806170374,-61.5487711074,-5.15806170374,-61.5487711074,-5.15806170374,-61.5487711074,-19.2088,-7.54299,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kotuy River, Siberia',3758,'Kotuy','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',524,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','2','1','Less than 10 m wide','1','1','Less than 20 m','1',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','7','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2683,0,'archaeocyath-calcimicrobial bioherm, 1.5-2 m thick, 1.2 m in diameter',69,103,-3795173,334392,'Russia','Asia',624,'',69.0167,103.85,'WAHR','80873',-8.18946117615,-70.6011602033,-8.18946117615,-70.6011602033,-8.18946117615,-70.6011602033,-22.696,-6.4067,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kotuy River, Siberia',3759,'Kotuy','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 ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','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','18','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2683,0,'archaeocyath-calcimicrobial bioherms',69,103,-3795173,334392,'Russia','Asia',624,'',69.0167,103.85,'WAHR','80874',-5.75760395127,-61.4587668983,-5.75760395127,-61.4587668983,-5.75760395127,-61.4587668983,-19.7423,-7.23757,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Selinde River (SE Aldan Shield)',3760,'Pestrotsvet','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 ',2,'Reef mound','1','Less than 10 m thick','1','1','Less than 10 m wide','2','1','Less than 20 m','2',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','7','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2684,0,'',57,132,-1546304,-349356,'Russia','Asia',624,'',57.4167,132.55,'WAHR','80876',10.4133628151,-66.9868772444,10.4133628151,-66.9868772444,10.4133628151,-66.9868772444,-6.15325,-17.8885,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ekwi River, Mackenzie Mountains',3762,'Sekwi','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','4','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','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','23','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2686,0,'archaeocyath-microbial bioherms, up to 4 m thick\r\nNevadella zone and Bonnia-Olenellus zone',63,-128,-1682369,-6631601,'Canada','North America',121,NULL,63.75,-128.8,'WAHR','80957',44.6506886094,-110.112725765,45.3776646783,-107.212420318,45.3776646783,-107.212420318,4.14683,-67.2492,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Koolywurtie bioherms, Teppers Knoll, Yorke Penins',3763,'Parara','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',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 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','3','25 or more reef building species','32','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2687,0,'complex of stacked bioherms and flanking beds capped by Girvanella boundstones',-34,137,1723150,-18774299,'Australia','Oceania',801,'',-34.4333,137.9,'WAHR','81016',-2.18477343535,117.505170776,-2.9656415706,120.034386283,-2.9656415706,120.034386283,13.778,-161.187,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ten Miles Creek bioherms, Flinders Ranges',3764,'Wirrealpa','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',512,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','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','5','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',2688,0,'Largest bioherm 3 m thick and 36 m in lenght; Epiphyton framestone core, low-diversity archaeocyathan-radiocyathan biota\r\nIncludes Balcoracana Creek bioherm\r\nNew data suggest that Wirrealpa Limestone ist Stage 4 (Yun et al. 2024).',-31,138,2129890,-18611441,'Australia','Oceania',801,'',-31.2667,138.9167,'WAHR','81025',0.662892677854,115.877820663,-0.18605781056,118.29275995,-0.18605781056,118.29275995,16.9488,-162.056,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hulutao, Liaodong Peninsula, Liaoning',3765,'Jianchang','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 ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,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','2','6 to 24 reef building species','7','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2689,0,'Fragments of archaeocyathids, trilobites and algae form bioreefs',39,121,6341264,-15467076,'China','Asia',602,'',39.25,121.7,'WAHR','81037',24.5314533509,92.1844836237,22.8167049891,93.8386642415,22.8167049891,93.8386642415,4.19939,148.006,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Franklin bioherms, New Jersey',3769,'Leithsville','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 ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',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,'2','Intense',0,'No or unknown reservoir potential',2692,0,'archaeocyath bioherms, dark gray dolomitic bafflestones and interreefal floatstones',41,-74,-6164064,-6788958,'United States','North America',101,'',41.1167,-74.5667,'WAHR','81073',7.02816444146,-118.479936767,7.67436170111,-115.140682922,7.67436170111,-115.140682922,-30.9062,-88.9005,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Caunes-Minervois, Montagne Noire',3771,'Lastours','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 ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,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',2694,0,'archaeocyathan-microbial floatstones, microbial boundstones',43,2,-4850430,9619245,'France','Europe',331,'',43.3167,2.5333,'WAHR','81088',-64.0610861686,5.02743246721,-65.8613997193,3.87607607022,-65.8613997193,3.87607607022,-50.3996,113.571,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('White Owl Lake, Colorado',3772,'Dotsero','Cambrian','Furongian','Lawsonian','Sunwaptan',491.00,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',493,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','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','3','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',2695,0,' stromatolite-microbial-sponge buildup\nGirvanella-Tarthinia-sponge boundstone forms a veneer over the Girvanella stromatolites, thickness of stromatolite bed: 1.5 m',39,-107,-521146,-7617677,'United States','North America',101,'',39.7333,-107.3167,'WAHR','81101',27.954216377,-121.366022479,27.954216377,-121.366022479,27.954216377,-121.366022479,-5.05336,-89.9619,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Diringde reef complex, Kotuy River',3773,'','Cambrian','Series 3','Stage 5','Maentwrogian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',498,2,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2696,0,'outer shelf microbial reef complex\nOnly trilibites described',68,103,-3387619,627788,'Russia','Asia',624,'',68.3833,103.1667,'WAHR','81113',-3.40823166239,-54.1266829502,-3.40823166239,-54.1266829502,-3.40823166239,-54.1266829502,-17.1959,-5.24359,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Krutoy Log, Sukhie Solontsy bioherm, Khakasiya',3774,'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',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 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','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','30','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2697,2698,'The Sukhie Solontsy biohermal massif spreads latitudinally for 8 km as a discontinuous belt of reefal limestones from 1000 to 1200 m in thickness. The Atdabanian strata are 600 m in thickness.',54,90,-2668609,2229125,'Russia','Asia',624,'',54,90.75,'WAHR','81243',-0.459256845887,-46.1387026189,-0.459256845887,-46.1387026189,-0.459256845887,-46.1387026189,-9.27457,5.53472,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Krutoy Log, Sukhie Solontsy bioherm, Khakasiya',3775,'Usa','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 ',2,'Reef mound','2','10 to 100 m thick','45','3','101-1000 m wide',NULL,'4','More than 1000 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','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','22','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,2697,'',54,90,-2668609,2229125,'Russia','Asia',624,'',54,90.75,'WAHR','81316',0.180302775957,-43.5367239907,1.13682207306,-39.2922922225,1.13682207306,-39.2922922225,-7.53668,7.19582,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Krutoy Log, Sukhie Solontsy bioherm, Khakasiya',3776,'Usa','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',512,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','45','3','101-1000 m wide',NULL,'4','More than 1000 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','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,2697,'calcimicrobial-archaeocyathan biostromes and interbiohermal limestones',54,90,-2668609,2229125,'Russia','Asia',624,'',54,90.75,'WAHR','81319',0.180302775957,-43.5367239907,1.13682207306,-39.2922922225,1.13682207306,-39.2922922225,-7.53668,7.19582,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Malaya Tes River, Batenevskiy Ridge, Khakasiya',3777,'Usa','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,'1','Less than 10 m wide',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','2','6 to 24 reef building species','20',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,0,'small calcimicrobial-archaeocyathan bioherms\nSanashtykgol stage',54,90,-2695420,2222047,'Russia','Asia',624,'',54.2333,90.8167,'WAHR','81326',0.0736445366408,-43.7478674788,1.03744874277,-39.5069986917,1.03744874277,-39.5069986917,-7.71085,7.03433,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Srednyaya Mountain, Batenevskiy Ridge, Khakasiya',3778,'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','3','101-500 m thick','135','2','10 - 100 m wide',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','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','24',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,0,'Kameshki stage\nsmall calcimicrobial-archaeocyathan biostromes and interbiostromal beds\nand\nmassive calcimicrobial-archaeocyathan bioherms',54,90,-2695420,2222047,'Russia','Asia',624,'',54.2333,90.8167,'WAHR','81328',-0.566108101787,-46.3497564253,-0.566108101787,-46.3497564253,-0.566108101787,-46.3497564253,-9.45347,5.37786,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kazyr River, Eastern Sayan, Krasnoyarskiy Kray',3779,'Balakhtison','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 ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','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','24','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,0,'Epiphyton limestone!\nBazaikha stage',53,93,-2574670,1934150,'Russia','Asia',624,'',53.7667,93.4833,'WAHR','81334',0.961596537228,-46.9330084661,0.961596537228,-46.9330084661,0.961596537228,-46.9330084661,-8.25907,4.24748,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kaltat River, Torgashino Ridge, Krasnoyarskiy Kray',3780,'Torgashino','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 ',1,'True reef','2','10 to 100 m thick','34','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,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','3','25 or more reef building species','33','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2697,0,'Gordonicyathus howelli zone, upper Bazaikha-lower Torgashino Formation\nmassive light gray reefal limestones',55,92,-2815911,1974008,'Russia','Asia',624,'',55.9667,92.9167,'WAHR','81252',-0.658479596888,-48.4567378971,-0.658479596888,-48.4567378971,-0.658479596888,-48.4567378971,-10.3323,3.43188,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Western Torgashino Ridge, Krasnoyarskiy Kray',3781,'Torgashino','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','34','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,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','9','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,0,'',55,92,-2815911,1974008,'Russia','Asia',624,'',55.9667,92.9167,'WAHR','81433',-0.0172767411831,-45.8547919571,1.01791594886,-41.6161324207,1.01791594886,-41.6161324207,-8.53283,5.07253,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Western Torgashino Ridge, Krasnoyarskiy Kray',3782,'Torgashino','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',512,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','70','2','10 - 100 m wide',NULL,'2','10 - 100 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','2','6 to 24 reef building species','18',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,0,'Obruchev stage\nmassive calcimicrobial-archaeocyathan bioherm. trilobites and archaecyaths described',55,92,-2815911,1974008,'Russia','Asia',624,'',55.9667,92.9167,'WAHR','81434',-0.0172767411831,-45.8547919571,1.01791594886,-41.6161324207,1.01791594886,-41.6161324207,-8.53283,5.07253,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Western Torgashino Ridge, Krasnoyarskiy Kray',3783,'Torgashino','Cambrian','Series 3','Drumian','Amgan',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',509,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,0,'Subreefal trilobites described',55,92,-1437321,2090815,'Russia','Asia',624,'',55.9667,92.9167,'WAHR','81437',1.16439601261,-33.0767174958,1.16439601261,-33.0767174958,1.16439601261,-33.0767174958,-6.09473,9.24302,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Uyar River, Bellykskoye Mountains, Krasnoyarskiy Kr',3784,'Uyar','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',512,3,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','16','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,0,'calcimicrobial-archaeocyathan bioherms',54,91,-2735613,2160606,'Russia','Asia',624,'',54.6,91.35,'WAHR','81440',0.104493481508,-44.2272563376,1.08462910613,-39.9851379957,1.08462910613,-39.9851379957,-7.85044,6.57041,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Malyy Karakol River, Western Sayan, Khakasiya',3785,'Upper Monok','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',NULL,'2','10 - 100 m wide',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','3','25 or more reef building species','39','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,0,'perireefal limestone unit intercalated in sandstones and tuffconglomerates',52,90,-2829282,2271846,'Russia','Asia',624,'',52.8333,90.2667,'WAHR','81443',0.634758240943,-42.424214199,1.55273838798,-38.1645252047,1.55273838798,-38.1645252047,-6.71852,8.08289,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bayan Kol River, Sayan, Tuva',3789,'Bayan Kol','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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','3','25 or more reef building species','25','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,2697,'sandstone-gravelstone-conglomerate unit with restricted reefal limestones (kalyptra, kalyptrate bioherms, biohermal and biostromal beds)',51,93,-2278483,2501162,'Russia','Asia',624,'',51.5833,93.6,'WAHR','81246',2.37841015157,-45.2694671614,2.37841015157,-45.2694671614,2.37841015157,-45.2694671614,-6.31928,5.26044,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bayan Kol River, Sayan, Tuva',3790,'Bayan Kol','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 ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',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',2698,0,'',51,93,-2278483,2501162,'Russia','Asia',624,'',51.5833,93.6,'WAHR','81475',3.0170818337,-42.6643763397,3.94193364506,-38.322270204,3.94193364506,-38.322270204,-4.57459,7.01149,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kadvoy River, Tannu-Ola Mountains, Tuva',3792,'Irbitey','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 ',2,'Reef mound','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',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','10',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2698,2697,'',50,92,-2143411,2585046,'Russia','Asia',624,'',50.95,92.8333,'WAHR','81483',3.03189074697,-41.8689339021,3.92919053923,-37.5260222635,3.92919053923,-37.5260222635,-4.28018,7.75161,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dedebulak bioherms, Ulug-Tau Mountains',3794,'Dedebulak','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)',512,2,'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','0',NULL,'','Unknown',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','17',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2699,0,'bioherms and biostromes\nListed as late Early to early Middle Cambrian. Presence of archaeocyaths suggest late Early Cambrian',40,72,-4172426,4750306,'Kyrgyzstan','Asia',NULL,'',40.4,72.35,'WAHR','81268',-9.25318832344,34.6679552911,-11.6183887141,37.1179638658,-11.6183887141,37.1179638658,-21.5941,49.721,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mount Murchison, Alberta',3795,'Bison Creek','Cambrian','Furongian','Lawsonian','Sunwaptan',491.00,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',492,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','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,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2700,0,'thrombolite buildups, also in Mistaya Fm.',51,-116,2386348,-6544083,'Canada','North America',121,'',51.8833,-116.6667,'WAHR','81299',38.5581568981,-110.837410151,38.5581568981,-110.837410151,38.5581568981,-110.837410151,1.08052,-77.6294,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mount Cory, Alberta',3796,'Bison Creek','Cambrian','Furongian','Lawsonian','Sunwaptan',491.00,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',492,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','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,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2700,0,'stromatolite adn thrombolite buildups\nIncludes Sundance Range\nTrilobites only',51,-115,2305466,-6535575,'Canada','North America',121,'',51.2,-115.65,'WAHR','81302',37.7604877748,-111.447926349,37.7604877748,-111.447926349,37.7604877748,-111.447926349,0.506363,-78.3623,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chedda Cliffs, Lennard Shelf',4070,'','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','3','Below storm wave base','3','Microbes',NULL,NULL,'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,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2926,NULL,'',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.25,124.63,NULL,NULL,-24.4151012786,116.539445036,-24.4151012786,116.539445036,-35.7837378931,151.402770078,-19.1823,114.765,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Hamar Laghdad',3838,'','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',388,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','6','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2730,0,'several small and poorly exposed mounds\nVent deposits excluded',31,-4,-4750388,657687,'Morocco','Africa',714,'',31.3667,-4.05,'WAHR','82033',-38.865641692,-7.62831316523,-38.865641692,-7.62831316523,-43.9920853635,-7.7562940337,-44.0926,16.9006,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pardonet Hill Patch Reef',3887,'Baldonnel','Triassic','Upper Triassic','Carnian','Tuvalian',227.00,237.00,17,'Induan - early Carnian',235,225,'Late Triassic (Carnian/Norian 227 Ma)',221,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','11','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','1','Corals','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','5','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2751,0,'Ref. 2751:Bioclastic accumulations composed of crinoids, brachiopods, molluscs, spongiomorphs and scleractinian corals at Pardonet Hill. These small buildups (~100 to 500 m3) have planar bases and broadly convex tops (3 small reefs). These mounds are interpreted as small patch reefs composed of packstone, bioclastic floatstone/rudstone and carbonate breccia intercalated with mixed siliciclastic carbonate sediments deposited in a shallow subtidal setting. RCM Edit in May 2015. ',56,-123,3559036,-6318725,'Canada','North America',101,'',56.05,-123.0083,'','67003',37.2811720974,-37.0804898953,37.2811720974,-37.0804898953,33.0235951195,-42.9418900953,31.9228,-53.0432,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Elimberrie bioherm, Oscar Range',3897,'Napier','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',370,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','100','3','101-1000 m wide',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','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','4','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',2754,0,'large stromatolite-sponge bioherms, up to 100 m thick and 1 km in diameter',-17,125,-4417280,11564216,'Australia','Oceania',801,'',-17.6833,125.0667,'WAHR','84828',-24.5544225986,117.181912744,-24.5544225986,117.181912744,-35.7470343823,152.142143613,-19.5043,115.303,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Napier Range, Canning Basin',3898,'Napier','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',370,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','5','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',2754,0,'',-17,125,-4404441,11652213,'Australia','Oceania',801,'',-17.4183,125.9783,'WAHR','84829',-23.860962896,117.825714081,-23.860962896,117.825714081,-34.9123157982,152.582249083,-19.0401,116.131,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Casey Falls, McWhae Ridge',3899,'Virgin Hills','Devonian','Upper Devonian','Famennian','Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',370,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','16','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',2754,0,'marginal reef slope, marly limestone, sponges as transported fragments\nIncludes Mt. Pierre locality',-18,126,-4481392,11612718,'Australia','Oceania',801,'',-18.7333,126.0833,'WAHR','84830',-24.9102110476,118.7029056,-24.9102110476,118.7029056,-35.6788611401,153.897093485,-20.2933,116.567,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sass da Putia buildup',3927,'Sciliar Dolomite','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',230,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','2','Algae','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1','Red algae','0','90','10',0,'no',0,'no','2','6 to 24 reef building species','10','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'1','Present',0,'No or unknown reservoir potential',2773,0,'megabreccia horizons with Tubiphytes/Bacinella wackestones/packstones, Porostromata bindstones, solenoporacean bafflestones/framestones, sphinctozoan bafflestones/bindstones, coral framestones',46,11,1389607,2345525,'Italy','Europe',344,'',46.6667,11.8833,'WAHR','87098',16.6161181849,35.2040231095,16.6161181849,35.2040231095,10.3658374019,23.544138115,7.84021,22.5136,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Normandville II, Alberta',4004,'Pekisko','Carboniferous','Mississippian','Tournaisian','middle Tournasian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',357,3,'1','Seismic data available ',3,'Mud mound or bank','1','Less than 10 m thick','10',NULL,NULL,NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown','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,'70','0','30',0,'no',0,'no',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',2822,0,'Described as Waulsortian-type mud mounds (bryozoan-crinoidal).\nTwo facies in core: 1. fenestrate bryozoan facies with minor mud. 2. carbonate mud with minor bryozoans.',55,-117,795136,-4300755,'Canada','North America',121,'',55.8333,-117.4167,'FALSCH','0',-7.41693499972,-46.2301939611,-7.41693499972,-46.2301939611,14.1716121316,-95.8229874906,4.36784,-39.2203,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fucheng, Shaanxi',4012,'Xiannudong','Cambrian','Series 2','Stage 3','Atdabanian/Botomian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',519,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','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','7','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',2835,0,'Upper Atdabanian-Lower Botomian\nsix microbial reef complexes; 1.1-12.5 m thick, laterally extensive; irregular archaeocyaths comprise max. 3.7% of the reefs and were not involved in reef construction.\nMostly in inter-reef settings.',32,107,3056063,15903806,'China','Asia',602,'',32.4667,107.2333,'WAHR','91498',-6.6123751032,80.6738618772,-4.532383383,78.1221076725,-4.532383383,78.1221076725,26.5929,164.178,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Salient Mountain, Britisch Columbia',4024,'Byng','Ediacaran','Ediacaran','Nama Assemblage','upper Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',546,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','2','1','Less than 10 m wide','15','1','Less than 20 m','10',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','1','Corals','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',2841,0,'Small mounds and more extensive biostromes of stromatolites and thrombolites containing namacalathus and Cloudina',53,-118,-4976520,-8267714,'Canada','North America',121,'',53.0333,-118.7333,'','',-46.8357809456,158.112952861,-46.8357809456,158.112952861,-46.8357809456,158.112952861,-47.8819,-107.38,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Amagour mound complex, Anti Atlas',4027,'Issafen','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','60','2','10 - 100 m wide','80','2','10 - 100 m','80',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2844,0,'Mound complex on grainstones. \nMound cores exhibit microbial (mainly Epiphyton and Renalcis) patches, up to 0.8 m thick and 1 m long, surrounded by massive microsparite bearing scattered shelly debris. Archaeocyaths, both\npreserved in life position and forming parautochthonous accumulations, are dominated by simple forms.\nAbundant stromatactis',29,-8,-6996358,7847364,'Morocco','Africa',714,'',29.7167,-8.9167,'','',-75.4123346275,-29.1662322052,-75.840465975,-36.1871923118,-75.840465975,-36.1871923118,-66.4123,114.165,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aguerd complex, Anti-Atlas',4028,'Issafen','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,NULL,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','8','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2844,0,'Reef complexes described from Aguerd (W), Tadakoust (middle) and Tamezrar (E). \nAguerd member of Issafen Fm.\nCoordinates for Tadakoust',29,-8,-7007576,7851194,'Morocco','Africa',714,'',29.2708,-8.7722,'','',-75.8708479851,-29.4340929303,-76.2807101295,-36.786403143,-76.2807101295,-36.786403143,-66.6085,115.583,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pamyatno-Sasovskoye oilfield, Zhirnovsk',4029,'Evlanovian-Livnian','Devonian','Upper Devonian','Frasnian','middle-upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',378,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick','200','3','101-1000 m wide','1000','4','More than 1000 m','15000','80','2241',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','1','Red algae','0','10','90',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','2','Intense',2,'Actual reservoir',2845,0,'Intrabasin buildup.\nflat-topped, narrow, and extended reef\nsteep (southeast) foreslope composed of relatively deep-water deposits and more gentle inner (north-west) slope represented by lagoonal deposits.\nUpward increase of the role of stromatoporoids, corals, crinoids, calcareous algae (green and red), and cyanobacteria.\n8% porosity, 10% detritus (fossils), 32% algal, rest is spar (dolomite)',50,45,-82309,2435104,'Russia','Asia',624,'',50.7833,45.15,'','',-4.31871094163,6.41136656897,-4.31871094163,6.41136656897,20.3248054592,-57.4590064232,-2.00662,21.873,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Godavari quarry',4030,'Chandragiri','Ordovician','Upper Ordovician','','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',460,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','35','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','0','60','40',0,'no',0,'no','1','Less than 6 reef building species','4','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2848,0,'Mud mound with common stromatactis, similar to Meiklejohn Peak.\r\nAge poorly constrained',28,85,0,0,'Nepal','Asia',NULL,'',27.59,85.389722,'WAHR','118944',-19.9253282289,96.6761788664,-19.9253282289,96.6761788664,-19.9253282289,96.6761788664,-17.1778,156.444,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('NE Taebaek Basin',4033,'Daegi','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',332,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','14',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above 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','4','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2852,0,'Described as siliceous-sponge microbial reefs. Epiphyton dominant, followed by Siliceous sponges, Renalcis and Epiphyton. 170 m thick section with several intervals. Described is only 14 m thick example. Ooids indicate shallow marine deposition. late Stage 5 to middle Guzhangian.',36,32,NULL,NULL,'South Korea','Asia',NULL,NULL,37.09,129,NULL,NULL,-27.1936870372,79.3999619657,-29.9592277698,84.3468123261,-29.9592277698,84.3468123261,5.88783,149.082,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('East Island Wall',4036,'Assoul','Jurassic','Middle Jurassic','Bajocian','Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','20','3','101-1000 m wide',NULL,NULL,NULL,'310',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','13','Echinoderms','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2859,0,'',NULL,NULL,NULL,NULL,'Morocco','Africa',714,NULL,31.59,-5,NULL,NULL,11.0190660285,11.4964211205,16.0580797792,4.43311760204,20.0039058374,3.48358307646,26.9345,-1.16459,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Santanyi',4040,'Santanyí Limestone','Neogene','Miocene','Upper Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','30','1','Less than 10 m wide','6',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes',NULL,NULL,'64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2862,0,'',NULL,NULL,NULL,NULL,'Spain','Europe',304,NULL,39.2,3.1,NULL,NULL,38.9234549155,1.07383075073,38.9243571708,1.06805015418,38.7567091323,2.987689051,39.8487,2.07928,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gosausee',4072,'Dachstein','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'4','More than 1000 m wide','3500','4','More than 1000 m','5000',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','3','Microbes','1','Corals','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','50','3','Binder guild','1','Present','1','Present','1','Low zonation','3','Pronounced zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2931,NULL,'Probably part of the same reef tract as Gosaukamm reef (Rf #28), however, the Gosausee site is only lower Rhaetian. Also, although the microbialites are volumetrically the most abundant reef builders, corals and sponges are more important in certain zones',NULL,NULL,NULL,NULL,'Austria','Europe',NULL,NULL,47.536521,13.522713,NULL,NULL,26.6940525928,30.3028407271,26.6940525928,30.3028407271,28.7594453052,23.1379116288,32.2211,15.6741,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Seokgaejae pass',4042,'Dumugol','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2864,NULL,'',NULL,NULL,NULL,NULL,'South Korea','Asia',NULL,NULL,36.13,129.1,NULL,NULL,-32.1181267484,91.4960321963,-32.1181267484,91.4960321963,-32.1181267484,91.4960321963,-1.15655,137.253,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Zhangzhai',4043,'Hunghuayuan','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,1,'Temperate','2','Shelf or Platform margin',NULL,NULL,'1','Above fair weather wave base','3','Microbes','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','5','4','Microbial precipitation',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',2865,NULL,'The small-scaled reefs are generally domical or lenticular in shape, ranging in height from tens of centimeters to several meters, and in width from less than a meter to more than 10 m. They are chiefly built by benthic microbes, lithistid sponges, the quasi-sponge fossils Calathium as well as bryozoans and are usually surrounded by skeletal/intraclastic grainstones and packstones. Skeletal fragments of ostracods, trilobites, gastropods, brachiopods, nautiloids, and echinoderms are found within the reefs and surrounding sediments. Three reefal types are recognized.',NULL,NULL,NULL,NULL,'China','Asia',602,NULL,27.27,109.02,NULL,'154810',-15.2402706884,89.9607464719,-15.2402706884,89.9607464719,-15.2402706884,89.9607464719,20.2859,141.449,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Haoshihe',4045,'Jinghe','Ordovician','Middle Ordovician','Darriwilian','Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','1','Corals','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',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,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2866,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',602,NULL,34.37,108.09,NULL,NULL,32.7652716288,95.9046659056,32.7652716288,95.9046659056,32.7652716288,95.9046659056,-22.1343,127.339,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),