INSERT INTO `reefs` VALUES ('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'),('El Morro del Porc, Centelles',2577,'','Paleogene','Eocene','Priabonian','lower Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',36,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 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','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1718,1855,'Biodetrital mud mound on delta-lobe facies.\nMaximm thickness 2.5 m, extension 120 m.\nPassage into coral patch reef.',41,2,5363321,-84491,'Spain','Europe',304,'',41.7667,2.1667,'WAHR','69710',38.7557849749,-2.07221680387,38.7557849749,-2.07221680387,40.519412593,1.89890040955,40.3721,-1.06308,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sniabar Mound, Wilson Co., Kansas',2578,'','Carboniferous','Pennsylvanian','Kasimovian','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,2,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'120','221',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','2','Algae','2','Algae','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',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','',1,'Potential reservoir',1719,0,'Hertha limestone\nSW (basinward) extension from Uniontown.\nHigh porosity, oil staining.',37,-95,-407965,-3147934,'United States','North America',101,'',37.5833,-95.8667,'','',-2.9218780093,-28.3727900591,-2.9218780093,-28.3727900591,-4.36161885865,-51.4888632094,-3.4203,-28.579,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yedioluk, Anatolia',2579,'','Devonian','Middle Devonian','Givetian','upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',386,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','80',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1720,0,'Reefal debris in platform carbonates. Around 80 m thick section with stromatoporoids (Stromatopora, Stachyodes, Taleastroma), corals (tabulates: Alveolites, Gyrophyllum, Stringophyllum, Thamnopora)',38,36,-4395784,4473373,'Turkey','Asia',522,'',38.55,36.45,'WAHR','27589',-34.810835875,35.7385011638,-34.810835875,35.7385011638,-54.3456722008,43.0355041086,-40.2976,58.6263,'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'),('Ullerntangen, Ringerike',2582,'','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 ',1,'True reef','2','10 to 100 m thick','12','2','10 - 100 m wide','100','3','More than 100 m','350',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','30','10',0,'no',0,'no','2','6 to 24 reef building species','15','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1723,0,'Middle Hirnantian\nAt Ullerntangen the bioclastic limestone sequence with its small mud  mounds is overlain by a very much larger, lens-shaped buildup, at least 350 m in length, 100 m in width, and up to 12 m in thickness.  It was originally interpreted as a reef by Kiaer (1897) but Hanken (1974) has argued that it lacks an organic framework, being largely composed of reworked material.\nNevertheless a remarkably diverse biota is recorded from this structure, including the stromatoporoid Pachystylostroma, rugoans Palaeophyllum,\nCyathophylloides, Tryplasma, tabulatans Saffordophyllum,  Rhabdotetradium, Lyopora, Reuschia, Catenipora, Proheliolites and Plasmpora as well as exhibiting pockets with clusters of cystoids and trimerellid brachiopod specimens.  The comparatively random directions of orientation of many of the coral and stromatoporoid specimens on the present exposed, slightly inclined, surface are not by themselves a certain basis for claiming that these organisms, or a substantial number of them, were not part of an in situ framework. Almost half the muddy matrix is composed of skeletal bioclasts - predominantly representatives of pelmatozoans, brachiopods, bryozoans, algae (Vermiporella, Hedstroemia) and the cyanobacterieum Girvanella.  The upper surface of the mound is cut by deep fissures up to 6 m deep, that imply a period of significant erosion possibly under subaerial conditions, and then they were infilled by sandy pelmatozoan-dominated bioclastic limestone in a subsequent depositional phase.  Finally a further sandstone unit overlaps the mound on its northern margin, and exhibits a very rich brachiopod, bryozoan and gastropod fauna near the mound.  This unit represents the uppermost part of the unnamed formation, and appears to be bounded at its top by a significant unconformity (hiatus) to the overlying Silurian Saelabonn Formation.\n',60,10,-4172568,-914771,'Norway','Europe',301,'',60.1333,10.1333,'','',-23.4987246045,-63.2650555473,-23.4987246045,-63.2650555473,-23.4987246045,-63.2650555473,-28.8019,-9.25712,'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'),('Mojero River, Siberia',2587,'Kotchakan','Ordovician','Middle Ordovician','Dapingian','lower Middle Ordovician',467.30,470.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',471,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','2','Algae','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','3','Receptaculitids','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,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1729,1723,'A lens-shaped, 2.5-m high, buildup with massive microbial-calathiid (Soanites) core and a capping thin layers of digitate stromatolites has been recorded from the lower part of the Chunya stage in the Moiero River section, Siberian Platform (Miagkova et al. 1977), of probable earliest Middle Ordovician age. \n\n',68,104,-505191,1200005,'Russia','Asia',624,'',68,104.5,'','',0.10685585626,-36.0727460585,0.10685585626,-36.0727460585,0.10685585626,-36.0727460585,-1.96325,10.8034,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zhuozishan, Inner Mongolia',2588,'','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 ',2,'Reef mound',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,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1730,0,'Zhou et al 1992 also draw attention to shelf-edge buildups (with a cheirurid-illaenid trilobite biofacies) on that same northern Tarim margin, and on the western and SW margin of the N China Platform (e.g., at Zhuozishan, Inner Mongolia).\r\n',40,112,5127534,15315393,'China','Asia',602,'',40.8667,112.55,'',NULL,22.9489920123,98.7887638241,22.9489920123,98.7887638241,22.9489920123,98.7887638241,-13.7739,125.736,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Tarim Platform',2589,'Yijianfang','Ordovician','Middle Ordovician','Dapingian','lower Middle Ordovician',467.30,470.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',470,2,'0','Outcropping reef ',2,'Reef mound','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',NULL,NULL,NULL,NULL,'6','Calcisponges','11','Siliceous sponges','94','Lithistid sponges - receptaculitid algae','3','Receptaculitids','0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1730,1723,'Small, sausage-shaped, Calathium-dominated buildups, up to 2 m high, are recorded from the Yijianfang Formation (early Middle Ordovician) at the northern margin of the Tarim Platform, NW China  (Zhou et al. 1992).',41,83,894482,12824596,'China','Asia',602,'',41,83,'WAHR','80007',-13.5424654783,69.6562005139,-13.5424654783,69.6562005139,-13.5424654783,69.6562005139,-27.1681,122.668,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Caudete',2590,'','Cretaceous','Lower Cretaceous','Hauterivian','lower Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',135,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','8',NULL,NULL,NULL,'1','Less than 20 m',NULL,'2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'10','80','10',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1731,0,'6-8 m thick mounds.\nBasal dimensions 12-18 m. \nDeveloped on emersion surfaces. \nMicrite matrix. Dm-sized colonies of corals (Microsolenidae, Thamnasteriidae, Stylinidae) and stromatoporoids, spiculate siliceous sponges (Corynella, Barroisia) and chaetetids. Rudists subordinate. Some bryozoans, calcareous algae, enrusting forams and worms.\nLithophagid borings abundant.\nVertical zonation almost absent.',38,-1,3038371,135347,'Spain','Europe',304,'',38.7333,-1.05,'WAHR','34748',21.3542852175,11.6692089557,21.3542852175,11.6692089557,25.7734134762,8.25447735171,29.4696,7.80155,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Larga, Jumilla',2591,'','Cretaceous','Lower Cretaceous','Hauterivian','lower Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',135,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','8',NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'10','80','10',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1731,0,'See reef 2590.',38,-1,3001596,105610,'Spain','Europe',304,'',38.4,-1.2833,'','',21.13959761,11.3328617487,21.13959761,11.3328617487,25.5671247532,7.90046236967,29.2581,7.43939,'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'),('N Tennessee',2594,'','Ordovician','Upper Ordovician','Sandbian','lower-middle Caradocian',452.00,458.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',456,3,'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,'2','Algae','11','Siliceous sponges','79','Siliceous sponges - algae','2','Green algae','0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1735,0,'Several sponge and algal-rich buildups.',36,-85,-3348888,-6209313,'United States','North America',101,'',36.3333,-85,'','',-9.54707945611,-112.531655898,-18.7796346999,-115.821144238,-18.7796346999,-115.821144238,-28.4583,-67.4551,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kalstad, Trondheim',2595,'Kalstad Limestone','Ordovician','Upper Ordovician','Katian','middle-upper Caradocian',451.00,455.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',453,2,'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','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'90','10','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',1736,0,'Limestone mass with corals and ?microbes and associated breccias. Possible remains of shelf-edge reef.',63,10,-3750000,-911795,'Norway','Europe',301,'',63.3833,10.3333,'','',-22.8684080894,-66.9237178712,-24.2074660776,-68.1161358758,-24.2074660776,-68.1161358758,-27.8124,-9.61603,'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'),('Dagpazari patch reef, Mut Basin, Icel',2597,'Mut','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',18,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','15','2','10 - 100 m wide',NULL,'3','More than 100 m','500','10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2546,1737,'Rimmed carbonate platform with large fringing reefs 80-100 m thick and 1-4 sqkm in area. \r\nMicrite rich coral-algal mounds (pinncales) on protected shelf behind the barrier.',36,33,4724519,3146586,'Turkey','Asia',522,'',36.8,33.4667,'','166093',35.9736868966,29.3632664459,36.15636985,29.9615490363,34.6386682772,32.2386511066,36.4634,33.5501,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bonifacio Basin, Corsica',2598,'','Neogene','Miocene','Lower Miocene','Aquitanian-Burdigalian',16.00,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1204,1739,'See reef 1992 for remarks.',41,9,5487416,342582,'France','Europe',331,'',41.4167,9.1667,'','',39.8710889675,4.80444914432,39.8710889675,4.80444914432,40.3137086168,8.63129724656,42.8596,4.84626,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zigui, Hubei',2599,'','Permian','Lopingian','Changhsingian','middle-upper Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',252,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1740,1700,'Two biostromal layers 1.5-2 m thick composed of Waagenophyllum (70 % of volume). Rest is micrite and bioclastics.\nBaffle- to framestones.',31,110,-18986,9153449,'China','Asia',602,'',31,110.6667,'','',-9.65767992667,108.6104977,-9.65767992667,108.6104977,11.7374594984,127.75295079,11.0763,97.9297,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rochefort-Fouras, Charentes',2600,'','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',96,2,'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,'1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1741,0,'Coral reefs with Thamnasteria, Heliastaea, Eugyra, Stylina, Cryptocoenia, Cyathophora, Isastrea, Synhelia.\nSome Holocoenia, Polytremacis, Helladastraea.',45,-1,4270016,232539,'France','Europe',331,'',45.9667,-1.0167,'','',39.1817458576,5.06522497758,39.1817458576,5.06522497758,37.1747690955,3.33428237692,35.0141,0.810297,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Plauen',2601,'','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',96,2,'0','Outcropping reef ',4,'Biostrome','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','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','25',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1742,1741,'Coral reefs(?) in the Pläner facies.\n\nMany colonial coral species:\nMontlivaltia? tourtiensis Bölsche\nLeptophyllia patellata Mich.\nSynhelia gibbosa\nPsammohelia granulata Bölsche\nThamnastraea tenuissima M. Edwards\nThamnastraea conferta M. Edwards\nThamnastaea belgica?\nDimorphastraea parallela Reuss\nAstrocoenia tourtiensis Bölsche,\nLatimaeandra fromenteli Bölsche',51,13,5113241,1251794,'Germany','Europe',331,'',51,13.8333,'WAHR','74193',45.7261259672,17.1288130135,45.7261259672,17.1288130135,43.0592984211,15.5569357535,40.5976,12.8687,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Betlehem',2602,'','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',96,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1741,0,'Coral reefs.\n',31,35,813714,3140975,'Israel','Asia',508,'',31.7,35.2,'','',14.7699715147,33.5637764703,14.7699715147,33.5637764703,10.0176541728,28.3206661579,10.4202,29.08,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chateauneuf, Charentes',2603,'','Cretaceous','Upper Cretaceous','Turonian','Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',91,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','11',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1741,0,'Typical Turonian coral species:\nActinastaea decaphylla\nA. tuberculata\nActinacis haueri\nAstrataea media\nDimorphastrea glomerata\nHydnophora styriaca\nNefophyllia multicincta\nPachyphyllia minor\nPlacosmilia gracilis\nSynastraea agaricites\nValliculastraea spinosa',46,-1,4673025,80620,'France','Europe',331,'',46.9167,-1.9167,'','',40.8738042657,2.80985699873,40.8738042657,2.80985699873,39.5101981525,1.43925630879,36.7839,-0.216391,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Angoulème, Charentes',2604,'','Cretaceous','Upper Cretaceous','Turonian','Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',91,2,'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,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1741,0,'',45,0,4505577,246515,'France','Europe',331,'',45.65,0.1333,'','',39.7869836183,4.85487263663,39.7869836183,4.85487263663,38.2950787294,3.31684841402,35.5169,1.53772,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Homa',2605,'','Cretaceous','Upper Cretaceous','Turonian','Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',91,2,'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','0',NULL,'','Unknown',NULL,NULL,'1','Corals','4','Stromatoporoids','35','Chaetetids - corals - cyanoyphyceans - algae - (bryozoans)',NULL,NULL,'0','80','20',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1741,0,'Small buildups with Actinacis, Phyllocoenia and Chaetetidae.',34,36,1595092,3375985,'Syria','Asia',NULL,'',34.7333,36.7167,'','',17.6489176129,35.4541404651,17.6489176129,35.4541404651,14.9277903144,31.1265885088,13.4506,30.6374,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('San Luis Potosi',2606,'','Cretaceous','Upper Cretaceous','Turonian','Turonian-Coniacian',86.30,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',89,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'100',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','5','Rudists','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'20','80','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',1743,1741,'Locality unknown.\nCoral and hippuritid reef formations.',22,-100,3288077,-7319727,'Mexico','North America',105,'',22,-100,'','',22.8105181955,-68.58923291,22.8105181955,-68.58923291,25.9940455648,-72.2736681417,23.7238,-70.6657,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hidalgo',2607,'','Cretaceous','Upper Cretaceous','Turonian','Turonian-Coniacian',86.30,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',89,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'100',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','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',1743,1741,'Locality unknown\nCoral and hippuritid reef formations.',20,-98,3032539,-7309596,'Mexico','North America',105,'',20.3333,-98.75,'','',20.9791260269,-67.6357989058,20.9791260269,-67.6357989058,24.1294776785,-71.3768218857,21.8306,-69.8597,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Morelos',2608,'','Cretaceous','Upper Cretaceous','Turonian','Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',91,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'100',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','5','Rudists','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'20','80','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',1743,1741,'Locality unknown\nCoral and hippuritid reef formations.',18,-99,2837985,-7431076,'Mexico','North America',105,'',18.75,-99,'','',19.2056837625,-67.3224533171,19.2056837625,-67.3224533171,22.1624159226,-71.1262440947,19.7926,-69.9742,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Guerrero',2609,'','Cretaceous','Upper Cretaceous','Turonian','Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',91,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'100',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'30','70','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',1743,1741,'Locality unknown\nCoral and hippuritid reef formations.',18,-99,2799500,-7533459,'Mexico','North America',105,'',18.25,-99.75,'','',18.8256642505,-68.1495409644,18.8256642505,-68.1495409644,21.8147365385,-71.9856153879,19.4688,-70.8308,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bugarach-Champ Sorel, Corbières',2610,'','Cretaceous','Upper Cretaceous','Turonian','Turonian-Coniacian',86.30,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',89,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1741,0,'Turonian reefs with superimposed lower and middle Coniacian reefs.',42,2,4138138,446538,'France','Europe',331,'',42.8333,2.5,'','',37.5430917956,7.05345578817,37.5430917956,7.05345578817,35.9736436845,5.19912527773,32.8259,3.64334,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('St. Luis et Parahou, Corbieres',2611,'','Cretaceous','Upper Cretaceous','Cenomanian','latest Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',94,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','12',NULL,NULL,NULL,NULL,NULL,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','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2346,1741,'Latest Cenomanian coralline buildups, 12 m thick.',42,2,3682585,636822,'France','Europe',331,'',42.85,2.3167,'','',36.4199547142,8.58978552346,36.4199547142,8.58978552346,34.2207445758,6.51115841798,30.2957,4.46422,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ankotrofotsy-Masiadolo',2612,'','Cretaceous','Upper Cretaceous','Coniacian','Coniacian-Santonian',83.60,89.80,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',391,1741,'Actinastrea, Caryosmilia, Vallimeandra, Dimorphastrea, Thamnoseris, Microsolena and Actinacis as reef builders.',-18,44,-5343452,3143248,'Madagascar','Africa',702,'',-18.6833,44.45,'WAHR','86510',-33.444450775,38.3028593134,-33.444450775,38.3028593134,-35.5961309864,32.1600535461,-37.366,35.1229,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Curacao, Netherland Antilles',2613,'','Cretaceous','Upper Cretaceous','Coniacian','Coniacian-Santonian',83.60,89.80,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1744,1741,'Only hermatypic corals indicated.',12,-69,680002,-5136330,'Netherlands','Europe',331,'',12.25,-69.0833,'','',6.8534118213,-45.1738756247,6.8534118213,-45.1738756247,9.26132173646,-49.3459321715,8.73863,-55.3735,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chichkaya',2614,'','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 ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1745,1741,'Position doubtful.\nReef building corals indicated.',40,45,3270301,4199702,'Armenia','Europe',526,'',40,45.5,'','',39.6216862867,47.9777195375,39.6216862867,47.9777195375,35.9813096863,44.716013412,28.4487,41.2874,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Corbières',2615,'','Cretaceous','Upper Cretaceous','Santonian','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'5',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','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',1781,1741,'Bioherms at\nLa Jouane\nSougraigne\nSt. Louis\nJean-Marie-de Parahou\nLa Bastide de Champs\nLa Fajolle',43,2,4159447,460767,'France','Europe',331,'',43,2.6667,'','',38.2049637667,6.21648915,38.2049637667,6.21648915,37.344141519,4.16039358293,33.1353,4.13175,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Skrapez and Pocuta Reefs, E Serbia',2616,'','Cretaceous','Upper Cretaceous','Coniacian','Coniacian/Santonian',83.60,89.80,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',86,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','0',0,'no',0,'no','3','25 or more reef building species','43','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2610,1741,'Coral reefs.\nLocality unknown.',44,20,3316766,2121104,'Yugoslavia','Europe',307,'',44.0333,20.0333,'WAHR','74560',31.4867482198,21.2604845823,31.4867482198,21.2604845823,32.4196307219,20.9014732412,27.397,19.1541,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pieninski, Carpathians',2617,'','Cretaceous','Upper Cretaceous','Santonian','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1741,0,'',49,20,4045271,2084160,'Poland','Europe',301,'',49.4167,20.1667,'','',46.0709631935,21.3379052975,46.0709631935,21.3379052975,44.1562948791,19.8404015377,32.6962,21.1831,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Padurea Mts.',2618,'Rosia-Bihor','Cretaceous','Upper Cretaceous','Santonian','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1741,0,'Rosia-Bihor Fms.\nCoral bioherms indicated.',46,23,3574231,2263859,'Romania','Europe',348,'',46.25,23.25,'','',43.2363795616,24.85998348,43.2363795616,24.85998348,35.668751312,20.05703884,29.1172,22.6097,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Godogani',2619,'','Cretaceous','Upper Cretaceous','Santonian','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',NULL,NULL,'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,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1746,1741,'Small coral dominated bioherms.',42,42,4322349,3907299,'Georgia','Europe',301,'',42.2667,42.7667,'','',41.3759842696,44.3391836274,41.3759842696,44.3391836274,38.2002102332,41.3724018519,33.755,39.3239,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bordj Cedina, Potinville',2620,'','Cretaceous','Upper Cretaceous','Santonian','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1747,1741,'Coral buildups. No paleontological description.',36,10,2624571,1054301,'Tunisia','Africa',715,'',36.7,10.3833,'','',25.8513659973,12.3778242577,25.8513659973,12.3778242577,25.3310042329,9.78380480111,21.8421,10.3759,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Central Cuba',2621,'','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',77,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1478,1479,'Reef building corals are:\nDiplaraea\nSynastraea\nMulticolumnastraea\nCentrastraea',22,-80,3033964,-6958396,'Cuba','North America',275,'1480, 1471',22.5,-80.5,'','',16.0865247675,-57.8667831889,16.0865247675,-57.8667831889,18.1791729187,-61.0910302767,19.421,-59.3,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Coalcoman',2622,'','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',77,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'40','60','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',1743,1741,'Coral and Hippurites formation.\nColonial and solitary corals.\nLocality unknown.',18,-102,3384131,-9050733,'Mexico','North America',105,'',18.3333,-102.6667,'','',22.4910391198,-78.2270688005,22.4910391198,-78.2270688005,24.6421947511,-81.6227723211,25.5875,-78.338,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mira',2623,'','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',76,2,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1753,1741,'Scattered coral debris.',40,-8,4597986,-857177,'Portugal','Europe',304,'',40.4333,-8.7333,'WAHR','74563',34.2636684232,-5.33127650789,34.2636684232,-5.33127650789,36.1718471878,-7.07989870086,31.8468,-4.83418,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vah Valley',2624,'','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',76,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1752,1741,'Belusa bioherms.',48,17,5114492,1701284,'Slovakia','Europe',336,'',48.8333,17.95,'WAHR','88191',41.6534673446,17.5835401103,41.6534673446,17.5835401103,40.2152978874,16.7794010708,39.159,18.4532,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tremp-Pobla de Segur',2625,'Vallcarga','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',78,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','24','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1968,1741,'Coral assemblage in olistostrome member of Vallcarga Fm.\n36 genera belonging to 2 orders and 9 suborders. Few reef building genera:\nE.g.\nActinastraea\nAstraraea\nHolocoenia\nFungiastaea\n\nColonial forms predominate but mostly of small size (less than 10 cm).\nLarge borings evident on plates',42,0,4742914,34016,'Spain','Europe',304,'',42.25,0.95,'WAHR','67084',34.8603009871,3.73689518649,34.8603009871,3.73689518649,36.8602361564,2.20262394438,32.1898,3.99163,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maastricht',2626,'','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',69,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1741,0,'',50,5,5792373,351763,'Netherlands','Europe',331,'',50.8333,5.7167,'','',46.1585065973,5.8912229784,46.1585065973,5.8912229784,48.1820890394,4.85864921911,43.1072,4.66551,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Libyan Desert',2627,'','Paleogene','Paleocene','Danian','Danian',61.60,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',63,2,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1751,1741,'Reef building and solitary corals.\nPosition changed!',27,24,1951177,2508422,'Egypt','Africa',715,'',27.5,24.5,'WAHR','86950',16.7107057138,21.6492389375,16.7107057138,21.6492389375,19.7441476643,20.4111942442,15.7241,19.336,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hummingbird Creek, Alberta',2628,'Palliser','Devonian','Upper Devonian','Famennian','middle Famennian',358.90,372.20,11,'late Famennian - early Visean',351,370,'Late Devonian (early Famennian, 370 Ma)',368,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','35',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','2','Algae','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','1','Red algae','0','70','30',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','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1754,0,'35 m thick and several km long reef complex.\nStromatoporoid reef with interbedded peloidal and skeletal wackestones, and mudstones.\nLaminar Labechia palliseri and Clathrostroma cf. jukkense prevail. \nSolenporacean algae rare.',52,-116,446669,-4520989,'Canada','North America',121,'',52.8333,-116,'','',-8.9854018817,-52.428613775,-8.9854018817,-52.428613775,4.64001955772,-111.582660594,-8.06406,-43.3811,'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'),('Civetta, Dolomites',2631,'Sciliar Dolomite','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'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','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','17','3','Binder guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation','3','Pronounced zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1756,0,'Sciliar Dolomite and Cassian Dolomite.\n17 reef building taxa discussed.\nSphinctozoans, microbial crusts, Tubiphytes, microbroblematica. Few Solenoporaceans.\nCorals rare but sometime forming patch reefs.\nPrimary pores preserved and sometimes widened, mostly destroyed by abundant fibrous marine cement.\nObservations from non-dolomitzed slope.',46,12,1345746,2369986,'Italy','Europe',344,'',46.4,12.1333,'WAHR','73877',16.3378687023,35.0448971399,16.3378687023,35.0448971399,10.4442222197,23.404475463,7.52308,22.5018,'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'),('Voskhod and Rodnoye, Chornaya River Basin, Crimea',2636,'','Cretaceous','Lower Cretaceous','Berriasian','upper Berriasian',139.80,145.00,22,'late Tithonian - early Valanginian',141,140,'Early Cretaceous (Berriasian, 142.4 Ma)',142,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','6','1','Less than 10 m wide','4','1','Less than 20 m','4','30',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','14','1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1764,2514,'Lower part of boissieri zone of the Berriasian.\nSmall bioherms (3-5 m thick, 4 m wide) of hermatypic corals and algae. Maximum 6 m thick.\nIntermound areas filled with bioclastic grainstones and packstones with fragments of corals and others. \nFramework of massive colonial (massive platy and pacheloid/ramose) corals and Lithocodium. \n\nAbstract ref. 1764:\nA section of Berriasian deposits from the River Belbek area (Southwestern Crimea) containing coral-algal bioherms is described. A detailed lithological and palaeontological description of one of these bioherms is given. Lithological features of Berriasian carbonate rocks are discussed, microfacies analysis of these rocks with there palaeontological remains are carried out. The history of the Berriasian development of the territory will be reconstructed.',44,33,4951011,2909437,'Ukraine','Europe',301,'',44.55,33.7333,'WAHR','22962',30.9876035768,43.4785953301,30.9876035768,43.4785953301,35.2612035455,45.6672578282,37.5972,39.2839,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ayton Farm, North Yorkshire, England',2637,'','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 ',1,'True reef','1','Less than 10 m thick','2','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,'40','545',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','3','1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1765,0,'Solenopora-gastropod facies as pre- and inter-reef sediments. \nReefs as a series of 2m thick isolated structures. \nCoral skeletal volume very high (90%).\nHighly micritized carbonate grains, and high bioerosion through bivalves. \nEffectively monospecific buildup dominated by Thamnasteria concinna. 30-40 cm sized colonies. ',54,0,5339600,197938,'United Kingdom','Europe',331,'',54.3333,-0.5,'WAHR','22784',31.9458632089,17.5685122062,31.9458632089,17.5685122062,38.1953145745,17.9585501538,44.8831,9.07963,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pandora, Gulf of Papua',2638,'','Neogene','Miocene',NULL,'Miocene',5.30,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,1,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',580,1313,'Probably algal mound.',-9,145,-2820832,14911333,'Papua New Guinea','Oceania',615,'',-9.1833,145.0167,'','',-15.8762303129,141.77179771,-15.9370433454,141.739884803,-18.0660245131,142.779398537,-17.9646,142.192,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Lauron, La Nerthe',2639,'Calcaire Blanc Supérior','Cretaceous','Lower Cretaceous','Valanginian','lower Valanginian',132.90,139.80,22,'late Tithonian - early Valanginian',141,135,'Early Cretaceous (Valanginian, 136.4 Ma)',139,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'40','60','0',0,'no',0,'no','1','Less than 6 reef building species','1','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1768,0,'Calcaire Blanc Supérior\nMonopleura clusters',43,5,3950106,754444,'France','Europe',331,'',43.3833,5.2833,'','',24.8731138546,21.8338375032,24.8731138546,21.8338375032,29.9014182335,21.5476246735,34.2652,14.628,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Periquillos, Colima',2640,'','Cretaceous','Upper Cretaceous','Cenomanian','lower Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',98,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1769,1768,'Recumbent rudist lithosome (Immanitas bed)',19,-104,1686815,-7111960,'Mexico','North America',105,'',19.25,-104,'','',19.6906589099,-69.6509074697,19.6906589099,-69.6509074697,22.1579136052,-73.4573341646,20.2632,-73.7103,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Portopalo, Pachino, Sicily',2641,'','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',69,2,'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','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1770,0,'Massive rudist lithosome with prominent domal shape (4 m high, 5 m wide).\nHighly dispersed cylindrical elevator rudists (Hippurites) in an micritic sandy matrix.\nVocanoclastic setting.\n\nAbstract ref. 1770:\nMaastrichtian strata from the Pachino area (SE Sicily) provide a model of association between rudist-coral frameworks and submarine volcanic activity. Two successive carbonate units are distinguished: (a) Coral- rudist bioherms and biostromes developed in a high-energy environment. (b) Hippuritid build-ups and banks overlain by rudist-coral clusters which grew under harsher ecological conditions, in a weaker current regime. At the top of the Maastrichtian sequence, the growth of rudist-coral frameworks ceased as ecological conditions shifted toward restricted environments. The inferred succession reflects a gradual decrease in current strengths and water depths, related to the Maastrichtian regression phase. The frameworks display consistent evolutionary sequences reflecting progressive changes in their biota, structure, and size and shape. Occurrences of rudist-coral frameworks are clearly linked with submarine volcanoes which provided opportunities for their development; they sometimes grew in the vicinity of active-vent centers, a feature reported for the first time in the Upper Cretaceous.',36,15,3450532,1325788,'Italy','Europe',344,'',36.6833,15.1333,'WAHR','74623',24.7281040538,13.1981171568,24.7281040538,13.1981171568,28.446940629,13.2700613165,24.7057,12.797,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Koronia, Helicon Mountains',2642,'','Cretaceous','Lower Cretaceous','Albian','middle Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',107,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','10','1','Constructor guild','1','Present','1','Present','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1771,1772,'Autochthonous reef limestones in ophiolitic conglomerates, sandstones and marls.\nCorals, encrusting algae, sponges. Rudists in the back reef.',38,22,2240406,2049136,'Greece','Europe',338,'1788, 2481',38.3417,22.9667,'WAHR','60368',18.8039378563,23.4870169791,18.8039378563,23.4870169791,19.7194975248,22.1330120711,18.259,20.8231,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Marmeko, Boeotia',2643,'','Cretaceous','Upper Cretaceous','Turonian','Turonian/Coniacian',86.30,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',89,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','4','Stromatoporoids','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,'40','40','20',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor 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',1771,1772,'Clusters and biostromes of Radiolites souvagesi and Vaccinites inferus above coquina horizon.\nChaetetids associated.',38,23,2570815,2121848,'Greece','Europe',338,'',38.4722,23.275,'WAHR','64253',25.316046319,20.8256025957,25.316046319,20.8256025957,23.1921249341,21.2017179743,21.167,19.5917,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kiriaki',2644,'','Cretaceous','Upper Cretaceous','Santonian','Santonian-Campanian',72.10,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',83,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1771,1772,'Vaccinites chaperi and thick-shelled radiolitids.',38,22,2566598,2076126,'Greece','Europe',338,'',38.3444,22.7833,'WAHR','64297',25.829437259,18.9596967233,25.829437259,18.9596967233,26.5655110146,20.7506494751,22.0767,21.4373,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Antikyra',2645,'','Cretaceous','Upper Cretaceous','Maastrichtian','middle Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',68,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no','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',1771,1772,'Clusters of Hippuritella lapeirousei overlain by biomicritic limestones.',38,22,3555668,2027663,'Greece','Europe',338,'',38.3594,22.6289,'WAHR','64302',26.3286056676,17.70375653,26.3286056676,17.70375653,29.5973378499,20.4098778046,25.3797,19.5723,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Moukharemi, Edessa',2646,'','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',75,2,'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,'1','Corals','5','Rudists','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'20','60','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1771,1772,'Massive limestone with coral-rudist float- to rudstones.\nStrongly bored and enrusted by corallinaceans.\nLapeirouseia identified.',40,21,3881779,1977105,'Macedonia','Europe',NULL,'',40.8,21.95,'WAHR','64308',28.3440025645,19.5221007311,28.3440025645,19.5221007311,29.2869679778,22.3878233855,25.0271,21.5475,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jalpan, Querétaro',2647,'El Abra','Cretaceous','Lower Cretaceous','Albian','upper Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,100,'Early Cretaceous (late Albian, 102.6 Ma)',101,3,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'30','70','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1276,1773,'',21,-99,1798534,-6579383,'Mexico','North America',105,'',21.1667,-99.4333,'','',19.3678033945,-57.7947707616,19.3678033945,-57.7947707616,21.3070818836,-63.617200311,20.2109,-62.4664,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vrbovac, Bacevica, Serbia',2648,'Vrbovac Beds','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',69,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1776,1777,'New rudist genus and several new species described. ',43,22,4263386,2000041,'Yugoslavia','Europe',307,'1741',43.7833,22.0833,'WAHR','74558',40.0645823873,21.8327220071,40.0645823873,21.8327220071,41.4351071829,20.7533860593,30.8018,20.0636,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Castelcucco, Veneto',2649,'','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'20',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','2','Algae','2','Algae','29','Coralline algae only (some corals)','1','Red algae','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','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1783,0,'Massive or coarsely bedded rhodolithic biostromes overlain by coarse-grained glauconitic biocalcarenites.\nTide- and wave-dominated delta setting. Biostromes developed on offshore bars.\nSome bryozoans, serpulids and bivalves associated.\nPhosphate indicates plenty of nutrients.',45,11,5720059,916188,'Italy','Europe',344,'',45.8333,11.8667,'','',42.9076330252,8.96135599263,42.9076330252,8.96135599263,43.1055980765,12.6811343698,44.6692,11.0643,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maré, Loyalty Islands, Melanesia',2650,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',4,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','2','Algae','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Intense',1,'Potential reservoir',1782,0,'Dolomitic rhodolite facies (Middle Miocene) with karstic surface.',-21,168,-3339338,17535791,'Pacific','Pacific',NULL,'',-21.5,168,'',NULL,-26.6624750958,166.404352156,-26.6640342862,166.403841979,-28.0403468201,168.06805385,-28.6152,167.245,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lifou, Loyalty Islands, Melanesia',2651,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',4,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','2','Algae','1','Corals',NULL,NULL,'1','Red algae','0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',1782,0,'See reef 2650.\r\n',-20,167,-3255659,17497124,'New Caledonia','Pacific',NULL,'',-20.8333,167.1667,'',NULL,-26.0664463199,165.475183248,-26.0680377942,165.474634613,-27.4772024434,167.10173526,-28.029,166.292,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rurutu, Polynesia',2652,'','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','60',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation',NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',1782,0,'Belongs to France\n60 m high cliffs on northwestern side of the island composed of packstone with big fragments of coral grading into wackestone. Doublet repeated every 30-50 cm. \nbranched corals replaced by massive coral heads in successive layers.',-22,-151,-3335727,-15409872,'Pacific','Pacific',NULL,'',-22.45,-151.35,'','',-25.02365634,-145.23732541,-25.02365634,-145.23732541,-22.45,-151.35,-26.1998,-143.188,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nauru, Pacific',2653,'','Neogene','Miocene','Lower Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','60','40',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',1784,1782,'Coral facies covered by incresing amounts of coralline algae.',0,166,-689755,19939014,'Nauru','Oceania',NULL,'',-0.55,166.9167,'','',-3.95188763664,-179.755892274,-3.95188763664,-179.755892274,-0.55,166.9167,-5.99444,179.746,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nauru, Pacific',2654,'','Neogene','Miocene','Lower Miocene','lower Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',18,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',1784,1782,'',0,166,-600086,19498826,'Nauru','Oceania',NULL,'',-0.55,166.9167,'','',-3.95188763664,-179.755892274,-3.95188763664,-179.755892274,-0.55,166.9167,-5.99444,179.746,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tongatabu, Tonga, Pacific',2655,'','Neogene','Pliocene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1782,0,'',-21,-175,-3191191,-18049141,'Tonga','Oceania',821,'',-21.15,-175.2,'',NULL,-21.932904492,-177.110496858,-21.932904492,-177.110496858,-22.2955103409,-176.672431735,-22.9729,-175.19,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Central Ranges, Trinidad',2656,'','Cretaceous','Lower Cretaceous','Aptian','Aptian',113.00,125.00,23,'late Valanginian - early Aptian',126,120,'Early Cretaceous (early Aptian, 121.8 Ma)',118,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','6','Calcisponges',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','15','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1790,0,'12 genera and 14 species of coral described. \nAll from \'zoogenic\' limestone blocks with worn coral fragments.\nCorals, sponges, echinoderms, pelecypods and nerineid gastropods indicated.',10,-61,-201910,-3417939,'Trinidad and Tobago','North America',201,'',10.4833,-61.2,'WAHR','25536',5.30008458784,-23.7272485663,5.30008458784,-23.7272485663,8.55040106411,-29.470665616,9.55967,-28.8926,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tehucacan, Pueblo',2657,'','Cretaceous','Lower Cretaceous','Valanginian','Valanginian-Hauterivian',129.40,139.80,23,'late Valanginian - early Aptian',126,135,'Early Cretaceous (Valanginian, 136.4 Ma)',136,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1792,1791,'Reef coral fauna',18,-97,303967,-5960675,'Mexico','North America',105,'',18.4667,-97.3833,'','',10.5689717135,-46.0029984979,10.5689717135,-46.0029984979,14.6549980663,-50.2936044172,15.1516,-51.9752,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('El Tigre, Sonora',2658,'Mural Limestone','Cretaceous','Lower Cretaceous','Aptian','Aptian-Albian',100.50,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',112,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1791,0,'Impoverished continuation of the Glen rose reef trend.\nStrong bioerosion evident on plates.',30,-109,3321755,-6985365,'Mexico','North America',105,'',30.5833,-109.2167,'','',29.7506786865,-60.1628311318,29.7506786865,-60.1628311318,31.5676310494,-67.5706940323,31.5537,-66.1999,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lamy, New Mexico',2659,'Carlile Shale','Cretaceous','Upper Cretaceous','Turonian','middle Turonian',89.80,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',91,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','2','2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1793,0,'1.5 m thick coral thicket of ahermatypic coral Archohelia dartoni Wells. \nBlue Hill Shale Member\nZonation by different sedimentation rates and accompanied variations in debris production.\n\nModerately deep cool water coral accumulation. ',35,-105,5146553,-6751072,'United States','North America',101,'',35.4917,-105.8931,'WAHR','23527',36.7432138175,-70.9059204116,36.7432138175,-70.9059204116,39.8192021715,-73.9280025847,38.1038,-72.5863,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vanderbeek, Leon Co., Texas',2660,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian-Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',150,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'55',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','11','Siliceous sponges','1','Corals','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,'1','Present','1','Present','3','Pronounced zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1795,0,'Amoco well\nOutboard reef trend on distally steepened ramp. \n\nTwo major types of reefs may occur both in an outboard an inboard position during latest Kimmeridgian and earliest Tithonian, resp.\nVanderbeck is an outboard reef, Reef is coral dominated at base but  rich in siliceous sponges and microbial crust at top.\n\nData refer to cement-rich coral-sponge-microbial boundstones and skeletal pack-/grainstones.\nBest reservoir quality in shoal grainstone with reefal debris.\n\nIdeal sequence in area\nTop\nmarine shlae\nmarl\nshallow lagoon\ndebris flow\ncoral-calcareous sponge microbiolite reef\nreefal debris\ndebris fan\nshallow outer ramp\nsponge-thrombolite reef\nupper deep marine ramp\ncoral-calcareous algal reef with washover fan\nlagoon.\n\n',31,-96,2206185,-4883254,'United States','North America',101,'',31.2333,-96.2833,'','',18.9556052743,-38.9152302919,18.9556052743,-38.9152302919,24.1648470503,-41.4539493622,25.999,-46.2904,'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'),('Mt. Medvednica',2666,'','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian-Danian',61.60,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',65,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1802,0,'Abstract of ref. 1802:\nThe biolithitic complex with a barrier reef in NE Mt. Medvednica shows the continuity of sedimentation of the Maestrichtian-Palaeocene. The lower part of the reef, which is built up mainly of rudistids, is of Maestrichtian age. The Palaeocene part of the reef is built up mainly of hermatypic corals and solenoporacean algae. The described biolithitic complex belongs to the sedimentation model characteristic for the subduction zone with an island arc system. The boundary Cretaceous-Tertiary is found everywhere in the Dinarides marked by a significant biostratigraphic discontinuity, and in terms of lithostratigraphy, by a continuity or discontinuity depending on geotectonical events. The facies migration occurred in transgressive succession in direction opposite to the subduction.',46,16,4626012,1520002,'Croatia','Europe',308,'',46,16.25,'FALSCH','',35.4046973412,17.1021714595,35.4046973412,17.1021714595,40.3561039852,15.2612584305,34.2407,15.1701,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vapenkova skala, Rozbehy',2667,'','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',69,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','2','Algae','2','Corals only','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1803,0,'Abstract of ref. 1803:\nThe 1st paleontologically confirmed occurrence of Upper Cretaceous sediments in the Little Carpathians was described. A series of strata of carbonate-sandstones through fine grained conglomerates of the Campanian with large Foraminifera of the genera Orbitoides, Pseudosidlerites and Lepidorbitoides was exposed on the southern slope of Vapenkova skala near Rozbehy. Bodies of biohermal reef limestone with corals and Dasycladaceae, probably of the Maastrichtian, were found on the walls of the Campanian strata. The find represents an important connecting link between the Brezova development of the Upper Cretaceous and Senonian sediments found to exist on the floor of the Vienna basin in drillings in the area of Zavod and Studienka. O. tissoti, O. media, P. vidali and L. minima are discussed in detail.',48,17,4925515,1636219,'Slovakia','Europe',336,'',48.5333,17.4167,'','',41.8168981339,16.238254905,41.8168981339,16.238254905,42.2410624279,14.6734083598,36.0437,17.25,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tsagan-Del, Wester',2668,'','Ordovician','Upper Ordovician','Katian','early Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',448,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','14','Brachiopods','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1805,0,'Lenses of reef-like limestones with tabulate corals: Cateniopora and diverse heliolitines.\nMongoliolites paradoxides\n\'Proheliolites\' ex gr. koskolensis\nPropora ex gr. magna\nHalysites proecedens\nDiverse brachiopod fauna associated with corals.',46,100,3383219,4021760,'Mongolia','Asia',NULL,'',46.3333,100.3333,'WAHR','79589',30.6680893153,-37.026967274,32.2627653195,-37.5839228301,32.2627653195,-37.5839228301,27.3039,22.1204,'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'),('Aqra',2675,'Aqra Limestone','Cretaceous','Upper Cretaceous','Maastrichtian','upper Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',66,3,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','2','Algae','47','Bivalves (mostly oysters) - algae (microbes)','1','Red algae','40','30','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','1','Present',1,'Potential reservoir',1817,1816,'Rudists, forams and algae as main reef builders.\nSome corals.\n',36,43,2808729,3996544,'Iraq','Asia',NULL,'',36.7667,43.9167,'','',21.7414154458,40.2317956373,21.7414154458,40.2317956373,23.2710845326,38.7533629534,19.5888,37.5031,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mesaoria Plain',2676,'Nicosia','Neogene','Pliocene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','9',NULL,NULL,NULL,'2','10 - 100 m','50',NULL,NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','1','Corals','8','Serpulids, worms, vermetids','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'30','70','0',0,'no',0,'no','1','Less than 6 reef building species','3','2','Baffler guild','1','Present',NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1821,0,'40 m water depth inferred. \nDominated by ramose Cladocora, but diverse molluscan fauna 38 species in total. Reef builders Cladocora, Ostrea and serpulids\n9 m thick, 50 m wide.\nBase with Ostrea domination.\n\nReef resting on calcareous silts, sandstones and conglomerates.\n\nSimilar structure as Tortonian reefs.\n\nAbstract of Ref. 1821:\nPaleocological analysis of the reef community shows that, apart from corals, it was dominated by epifaunal molluscs. It represents one of the most diverse fossil communities found on Cyprus following the Messinian Salinity Crisis (MSC), with 38 identified species of macrofossils and 8 species of foraminifera. When compared to patch reefs on Cyprus formed just prior to the MSG, this Pliocene reef shows both the biological devastation of the event and the quick and complete recovery of the reefal biodiversity.',35,33,4661789,3182760,'Cyprus','Europe',701,'',35.0961,33.1486,'WAHR','34689',34.6438169589,32.4139169661,34.6443909028,32.4148412504,34.4068011008,32.9725007824,35.0008,33.1104,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Osmundsberget, Dalarne',2677,'Boda 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 ',2,'Reef mound','2','10 to 100 m thick','30',NULL,NULL,NULL,'3','More than 100 m',NULL,'25',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','2','Algae','69','Non-coralline algae only','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present','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',1823,1824,'Up to 30 m thick bioherms of Palaeoporella variabilis (Codiacean, Chlorophyta) and abundant sparite. \nMicritization noted. Open porosity.\nGrowth ceased before end of Hirnantian.',61,15,-4040129,-629974,'Sweden','Europe',330,'',61.1,15.2,'WAHR','2756',-21.6079347372,-61.2290655989,-21.6079347372,-61.2290655989,-21.6079347372,-61.2290655989,-27.2434,-6.80596,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rosseveltveg, Curacao, Netherland Antilles',2678,'','Neogene','Pliocene','Pliocene','Upper Pliocene',2.60,3.60,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',3,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild','1','Present','1','Present','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1827,0,'Two units:\nTop: Acropora palmata dominant\nBase: Stylophora affinis dominant\nMaximum 11 coral species at one locality. \n',12,-68,1637611,-7484959,'Netherlands','Europe',331,'',12.1333,-68.95,'WAHR','41038',11.4233134763,-69.1133787761,11.4209619069,-69.1138821847,11.9652850768,-69.0165745728,12.1428,-68.597,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Salina, Curacao, Netherland Antilles',2679,'','Neogene','Miocene','Upper Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',6,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','10',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1827,0,'10 coral species listed:\nMontastrea limbata most abundant',12,-68,1633136,-7480003,'Netherlands','Europe',331,'',12.1,-68.9,'WAHR','41028',10.6263172125,-69.2125803238,10.6226394033,-69.2132451931,11.7277631813,-69.0122707857,12.1163,-68.1827,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gurabo Adentro',2680,'Cercado','Neogene','Miocene','Upper Miocene','Tortonian/Messinian',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','19',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','14','1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1827,1902,'Up to 14 species indicated from one reef body.\nPorites, Monastrea and Stylophora prevailing.\n38 coral genera (71 species) in total according to ref. 1902.\n19 m thick fringing reefs near edge of gently sloping shelf.',19,-71,2669065,-7613037,'Dominican Republic','North America',254,'603',19.5333,-71.1833,'WAHR','41065',18.6566038372,-71.0710533091,18.6592304535,-71.0713420194,20.1464987864,-70.7804040041,19.5576,-70.2029,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Brazo Seco',2681,'','Neogene','Pliocene','Pliocene','Zanclean',3.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1827,0,'8 dominant coral species indicated. \nPlacocyathus prevailing.',10,-83,1397351,-9141455,'Costa Rica','North America',230,'',10.25,-83.4167,'WAHR','41072',9.89665695335,-83.5492708825,9.89810564247,-83.5498263326,10.679979604,-83.4545879055,10.148,-82.6791,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bowden',2682,'','Neogene','Pliocene','Pliocene','Upper Pliocene',2.60,3.60,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',3,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','2','Below fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','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',1827,2308,'Deep reef (> 20 m) environment.\n9 coral species indicated\nPlacocyathus alveolus strongly predominant.',17,-76,2450832,-8213301,'Jamaica','North America',222,'',17.8833,-76.3167,'WAHR','34539',17.4751556165,-76.1492180092,17.4738411318,-76.1486943253,18.0176022809,-76.0745258334,17.8988,-75.9591,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cerro de Oro, Sonora',2683,'Cerro de Oro','Cretaceous','Lower Cretaceous','Barremian','Barremian-Aptian',113.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',125,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','10',NULL,NULL,NULL,'2','10 - 100 m','100',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'30','70','0',0,'no',0,'no','3','25 or more reef building species','22','1','Constructor guild','1','Present',NULL,NULL,'1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1828,0,'late Barremian-early Aptian\nUppermost Cerro de Oro Fm.\nDescribed as reef-like biohermal structures up to 10 m thick and up to 100 m long.\nCoral boundstones with bivalves and forams.\n21 Coral species described.',29,-110,2160607,-6857784,'Mexico','North America',105,'',29.75,-110.6667,'WAHR','21253',27.820230278,-57.4599123533,27.820230278,-57.4599123533,29.6044051803,-64.3804720745,30.6657,-63.2555,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cerro de Oro, Sonora',2684,'Mural Limestone','Cretaceous','Lower Cretaceous','Aptian','Aptian-Albian',100.50,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',112,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','10',NULL,NULL,NULL,'4','More than 1000 m','700',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'20','70','10',0,'no',0,'no','2','6 to 24 reef building species','21','1','Constructor guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1828,2350,'Late Aptian to middle Albian.\nBiohermal structures of colonial corals, stromatoporoids, rudists and other bivalves and abundant formas. \nUp to 10 m high and 700 m long.\nCorals and stromatoporoids in growth position.\n20 corals described. 1 added for stromatoporoids',29,-110,3261371,-7166363,'Mexico','North America',105,'',29.6,-110.625,'WAHR','21254',29.1616864039,-61.8289592734,29.1616864039,-61.8289592734,30.8924860964,-69.2228220532,30.6268,-66.6196,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lampazos, Sonora',2685,'Espinazo del Diablo','Cretaceous','Lower Cretaceous','Albian','middle Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',107,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20',NULL,NULL,NULL,'3','More than 100 m',NULL,'8',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','5','Rudists','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'20','80','0',0,'no',0,'no','2','6 to 24 reef building species','13','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1828,2005,'Bisbee Group\nThick massive biohermal limestones mentioned at base and top of Espinazo del Diablo Fm.\n12 Coral species described.\nAge assignment corrected by ref. 2005, abstract:\nThe stratigraphy and structure of the Lower Cretaceous (Aptian-Albian) rocks exposed in the area of Lampazos, Sonora, are redefined and correlated to well-known stratigraphic successions of Chihuahua and northeast Mexico (Coahuila and Nuevo Leon). Originally, seven stratigraphic units were proposed for the Cretaceous rocks exposed in the Lampazos area, but in this article only five units (El Aliso, Agua Salada, Lampazos, Espinazo del Diablo, and Los Picachos formations) have been used, and we propose herein to discontinue usage of the other two (Nogal and La Mesa formations). This Aptian-Albian succession of east-central Sonora yields facies and fossil content remarkably similar to coeval sequences in the Gulf of Mexico realm (Chihuahua, Coahuila, and Nuevo Leon). These sections contain abundant microfossils (benthic and planktonic foraminifera, colomiellids, nannoconids, and radiolarians) that permit detailed biostratigraphic determinations. A complete Aptian-lower Albian section (base of K-6 through top of K-15 of the biochronologic scheme of Longoria, 1984) was identified. Abrupt lithic changes through the Aptian-Albian section of Lampazos revealed three major paleoceanographic events having an overall regional marine transgression, including an early Aptian (K-6 to K-7) event, a late Aptian (K-10 to K-11) event, and an early Albian (K-13 to K-14) maximum flooding phase. We used physical and biochronologic data to tie the aforementioned events to geochemically constrained Aptian-Albian oceanic anoxic events (OAEs) in Santa Rosa Canyon of Nuevo Leon.\n\nThe close correlation between the oceanic events in east Sonora (northwest Mexico) and central Nuevo Leon (northeast Mexico) invokes the closer paleogeographic development of the two regions (Begin page 1812) and undoubtedly links the area of Lampazos to a rapid encroachment of the paleo-Gulf of Mexico through north-central Mexico (the Mexican Sea) into northwestern Mexico (Chihuahua trough and Sonoran basin). The early Aptian (biozones K-6 to K-7) transgression has its maximum extension during the early Albian (biozones K-13 to K-14), culminating with the drowning of the carbonate platforms.\n\nThe Lower Cretaceous rocks exposed in the Lampazos area are complexly folded and faulted. The more conspicuous structures are isoclinal and box-shaped folds and thrust faults, mostly oriented north-south and northwest-southeast, having vergences to both the northeast and southwest. A very conspicuous feature is the opposite vergence of thrust faults, either converging or diverging. Two dextral strike-slip faults (northeast-southwest and east-west) separate the area into three large blocks that have different patterns of folds and thrust faults. Also, it is evident that the area was affected by at least two episodes of normal faulting. Furthermore, the structural style of deformation present in the Lampazos succession is remarkably similar to the style of deformation of coeval rocks in northeastern Mexico, especially to the structure of the Chihuahua tectonic belt. The Lampazos succession is paleogeographically and tectonically related to the Chihuahua tectonic belt, and it is considered to be the westernmost extension of the ancestral Gulf of Mexico.\n\nThe fact that the Lampazos succession can be lithocorrelated to known sequences in northeastern Chihuahua (Lucero, Ahumada, and Loma Plata formations) and northeast Mexico (Cupido, San Angel, La Pe±a, and Tamaulipas formations), which are know to be source rocks in exploration wells in Nuevo Leon and Coahuila, makes the Lampazos area of Sonora potentially attractive as an exploration target.\n',29,-109,3154255,-7098674,'Mexico','North America',105,'',29.2,-109.5,'WAHR','21255',29.3671473451,-65.3590595153,29.3671473451,-65.3590595153,31.1737282779,-71.5115420725,30.1913,-70.1126,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Andara + Fuente De, Asturia',2686,'Picos de Europa','Carboniferous','Pennsylvanian','Moscovian','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',309,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','4','Stromatoporoids','88','Green algae - phylloid algae - calcisponges - (corals)','2','Green algae','5','95','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',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',2,2419,'Beresella (paleosiphono-cladal alga) in sparitic matrix dominant.\nBuildups several 10s of m thick together with phylloid algae, chaetetids, sphinctozoans and small rugose corals.\n',43,-4,-671865,1371645,'Spain','Europe',304,'2626',43.2083,-4.7083,'WAHR','46492',-8.96142402067,9.26092374526,-8.96142402067,9.26092374526,-9.26868974438,-11.7045143888,-7.02799,10.5979,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('NE Cantabrian Mts., Castilla y Leon',2687,'Picos de Europa','Carboniferous','Pennsylvanian','Moscovian','Moscovian-Kasimovian',303.70,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',306,2,'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','1a','Shallow intra-platform','2','Below fair weather wave base','2','Algae','11','Siliceous sponges','79','Siliceous sponges - algae','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2,0,'Anthracoporella (dasycladacean alga) dominant. \nSpiculae as evidence for presence of sponges.\nSphintozoans are also present in Lores Limestone',43,-4,-649220,1320053,'Spain','Europe',304,'',43.0833,-4.5,'WAHR','76626',-7.46272568254,10.1539488403,-7.46272568254,10.1539488403,-8.01675829263,-11.5325856968,-6.77902,10.9695,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tende Hantu Mts., Mangkalihat, Borneo',2688,'Tendehantu','Neogene','Miocene','Lower Miocene','Early Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',5,7,'Atoll structure with low energy, slightly restricted platform interior structure, steep southern and eastern coral reef margins and a northwestern margin with a \'step-wise\' appearance.',0,118,321068,13512217,'Indonesia','Asia',614,'',0.8667,118.8833,'','170615',0.688894334869,115.771225511,0.688894334869,115.771225511,-3.72241509198,118.220504983,1.86591,122.137,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Muarawahau, Borneo',2689,'','Paleogene','Oligocene','Rupelian','lower Oligocene',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',31,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',7,0,'Coral and coralline algae bioclastic pack/rudstone to floatstone with abundant fragmented shallow marine bioclasts including recrystallized corals, coralline algae and Nummulites.',1,116,789454,13371407,'Indonesia','Asia',614,'',1.3333,116.8333,'','',3.89506380666,114.711653522,3.89506380666,114.711653522,-2.34885465007,118.48282015,4.12588,121.944,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Muarawahau, Borneo',2690,'','Paleogene','Eocene','Lutetian','Middle Eocene',38.00,47.80,28,'Lutetian - Bartonian',45,45,'early Middle Eocene (Lutetian, 44.5 Ma)',40,2,'0','Outcropping reef ',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','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'40','60','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',7,0,'Coral pack/floatstones in a marly matrix. Ta 3.\r\nBranching corals, oysters, some larger benthic forams and miliolids.\r\nLow energy inner shelf setting.',1,116,1271818,13318127,'Indonesia','Asia',614,'',1.35,116.8333,'',NULL,5.92243341275,115.51364177,5.92243341275,115.51364177,-2.08579922352,118.991457345,8.73284,120.499,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gurung Pengabun, Borneo',2691,'','Paleogene','Oligocene','Rupelian','lower Oligocene',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',31,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',7,0,'Abundant reworked branching nd rounded massive corals inferred to have been derived from a nearby patch reef environment.',1,117,763835,13437720,'Indonesia','Asia',614,'',1,117.3333,'','',3.48608800162,115.152709259,3.48608800162,115.152709259,-2.9032671287,118.714605722,3.89148,122.499,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Batuputih, Mangkalihat, Borneo',2692,'','Paleogene',NULL,NULL,'Oligocene-Miocene',5.30,33.90,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',23,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',1,'Potential reservoir',7,2819,'Coral bafflestones, rudstones and framestones.\r\nPatch reefs on seaward side of platform.\r\nReservoir potential most prominent in platoform interior (re.f 2819).',1,118,386451,13457314,'Indonesia','Asia',614,'',1.4,118.4833,'','170615',1.24860487764,115.40882226,1.24860487764,115.40882226,-3.11881355983,118.032402133,2.36158,121.707,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Teluk-Landas, Mangkalihat, Borneo',2693,'','Neogene','Miocene','Lower Miocene','Early Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',18,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',7,0,'',1,118,221332,13331108,'Indonesia','Asia',614,'',1.0667,118.9167,'',NULL,0.884041076712,115.826303319,0.884041076712,115.826303319,-3.54726852197,118.322882004,2.06837,122.148,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Teluk-Landas, Mangkalihat, Borneo',2694,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50','2693',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',7,576,'',1,118,221332,13331108,'Indonesia','Asia',614,'',1.0667,118.9167,'','',1.74476116579,117.14622275,1.74476116579,117.14622275,-1.31111337947,118.336866186,1.54593,120.622,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Off Tarakan, Borneo',2695,'','Neogene','Pliocene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','12','Foraminifera','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'5','80','15',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',8,7,'Linear delta-front reefs.\nFramestones, floatstones, \nCorals prevailing, larger forams, coralline algae and Halimeda.',3,117,454113,13061037,'Indonesia','Asia',614,'',3.25,117.5833,'','',3.73705133516,117.189454165,3.73643342371,117.189955692,3.05804554302,117.284086842,3.24949,117.926,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Miller Creek, Blanco Co., Texas',2696,'Glen Rose','Cretaceous','Lower Cretaceous','Albian','middle Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',107,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,'4','More than 1000 m','1','5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',12,0,'Nearshore oyster biostrome traced over 35 km2. Around 1 m thick. Clusters up to 1 m in diameter. \nThick-bodied gastropods, mud-burrowing clams and serpulid worm tubes present.',30,-98,2947042,-6041285,'United States','North America',101,'',30.2,-98.3306,'','',27.8994153016,-54.3732741388,27.8994153016,-54.3732741388,29.8857291163,-60.2869807896,28.7462,-59.0332,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lake Austin, Travis Co., Texas',2697,'Glen Rose','Cretaceous','Lower Cretaceous','Albian','middle Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',107,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',12,0,'Monopleurid biostromes in several horizons within the lowe Glen Rose.\nTabular and conical colonies.\nThree species of monopleurids.\nFew Ostrea are associated. ',30,-97,2950883,-5999215,'United States','North America',101,'',30.3167,-97.9333,'','',27.927386613,-53.9643010143,27.927386613,-53.9643010143,29.9189793125,-59.8706073617,28.7744,-58.621,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cibolo Creek, Kendall Co., Texas',2698,'Glen Rose','Cretaceous','Lower Cretaceous','Albian','middle Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',107,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150','1299',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','2','Algae','47','Bivalves (mostly oysters) - algae (microbes)','1','Red algae','30','60','10',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,'1','Low zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',12,0,'Main Caprinid reef trend at shelf edge.\nCoalcomana texana Whitney strongly prevailing. \nSome coralline and dasycladacean algae present. \nCommon living position ',29,-98,2904392,-6091447,'United States','North America',101,'',29.8,-98.65,'WAHR','84749',27.5804065111,-54.7880181424,27.5804065111,-54.7880181424,29.5612947989,-60.7041610321,28.4269,-59.451,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('The Narrows, Blanco River, Hays Co., Texas',2699,'Glen Rose','Cretaceous','Lower Cretaceous','Albian','lower Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,110,'Early Cretaceous (early Albian, 111 Ma)',110,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','5','Rudists',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','13','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',26,12,'Coral reef with rich fauna, older than Glen Rose trend (basal Glen Rose Fm.).\nIncludes Spring Branch-Cranes Mill region, Comal County',29,-98,2915311,-6040979,'United States','North America',101,'2756',29.9833,-98.2,'WAHR','74762',27.6614785172,-54.3102054454,27.6614785172,-54.3102054454,29.648639266,-60.2186725649,28.5083,-58.9695,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kirkfield, Brich Island, Ontario',2700,'Bobcaygeon','Ordovician','Upper Ordovician','Sandbian','Blackriverian',467.30,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',457,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','1','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',38,0,'Small Tetradium microatoll',46,-81,-2472469,-5506595,'Canada','North America',121,'',46.0667,-81.7667,'WAHR','61730',-4.2321983886,-103.959882649,-4.2321983886,-103.959882649,-4.2321983886,-103.959882649,-21.4829,-54.2309,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('North-central Kentucky',2701,'Grant Lake','Ordovician','Upper Ordovician','Katian','lower Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',448,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide','3','1','Less than 20 m','3',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'7','Bryozoans','7','Bryozoans','73','Bryozoans only',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',47,0,'Late Maysvillian-Gamachian bryozoan reef mounds',38,-84,-3168093,-6091850,'United States','North America',101,'',38.25,-84.6667,'','',-24.2630601437,-114.776580269,-25.0778786834,-113.889801005,-25.0778786834,-113.889801005,-25.2808,-57.5748,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Madison, Indiana',2702,'Saluda','Ordovician','Upper Ordovician','Katian','mid-late Richmondian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',446,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'50','50','0',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',1829,1838,'Biostromes dominated by corals Favistina and Tetradium',38,-85,-3066244,-6131173,'United States','North America',101,'',38.7667,-85.4167,'','',-23.5127388143,-115.017257809,-23.5127388143,-115.017257809,-23.5127388143,-115.017257809,-25.1938,-59.8949,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('SE Indiana',2703,'Whitewater','Ordovician','Upper Ordovician','Katian','late Richmondian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',446,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1829,0,'Biostromes dominated by Labechia and locally Tetradium.',38,-85,-3057061,-6121404,'United States','North America',101,'',38.8833,-85.3667,'','',-23.43539467,-114.913080973,-23.43539467,-114.913080973,-23.43539467,-114.913080973,-25.1266,-59.7812,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('New Wells, SE Missouri',2704,'Leeman','Ordovician','Upper Ordovician','Sandbian','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',445,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'1','Corals','2','Algae','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','2','Green algae','60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1830,0,'Small biohermal mounds with solitary corals, green alga Dimorphosiphon and encrusting bryozoans. Borings!',36,-89,-2988589,-6591410,'United States','North America',101,'',36.75,-89.6667,'',NULL,-15.0898768763,-118.228568175,-15.0898768763,-118.228568175,-15.0898768763,-118.228568175,-24.8268,-65.6663,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tripolitania',2705,'Djeffara','Ordovician','Upper Ordovician','Katian','Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','90',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,2,'Cold - water','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','7','2','Baffler guild',NULL,NULL,'1','Present','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',1831,2645,'10-100 m thick bryozoan dominated biostromes (figures suggest reef mounds\nWackestones with bryozoans, some biomicritc seems, intense dolomitization.\nBryozoans mostly vertically oriented with little evidence of dismantling.',29,12,-8470748,6727809,'Libya','Africa',715,'',29.7833,12.2833,'WAHR','75420',-71.2376913379,52.4204996427,-70.5787159942,49.449664261,-70.5787159942,49.449664261,-72.0488,124.45,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Khabt-el Hajar, Anti-Atlas',2706,'','Ordovician','Upper Ordovician','Katian','Ashgillian',445.20,451.00,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',445,2,'1','Seismic data available ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,2,'Cold - water','0',NULL,'','Unknown',NULL,NULL,'7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',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',1833,1831,'Bryozoan biostromes and or \'reef-like\' lenses, also associated with cystoids. ',30,-8,-9784289,1167676,'Morocco','Africa',714,'2065',30,-8.5,'WAHR','80781',-82.5649656311,-17.090428756,-81.3803478648,-15.6003395735,-81.3803478648,-15.6003395735,-86.6386,46.5437,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Balbanyu River, Prepolar Urals',2707,'Yaptikshor','Ordovician','Upper Ordovician','Hirnantian','Hirnantian',443.40,445.20,5,'Darriwilian - Ashgillian',452,445,'Late Ordovician (Hirnantian, 444.5 Ma) ',444,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','50',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',1661,1662,'Dolostones show abundant relict corals and \'algae\' in massive unbedded strata  of the Yaptikshor Fm., which are identified as 50m thick reefs (ibid., p.102, 116): these have a Holorhynchus, Mesofavosites, Paleophyllum  fauna of Hirnantian age, suggesting that  these reefs were like those of the Baltic area.',65,58,-2411414,1096407,'Russia','Asia',624,'',65.5,58,'','',-4.95163595631,-51.1294636447,-4.95163595631,-51.1294636447,-4.95163595631,-51.1294636447,-12.1401,6.04423,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Abadeh',2708,'Qom','Paleogene','Oligocene','Chattian','Upper Oligocene',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',27,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','10',NULL,NULL,NULL,'3','More than 100 m','200',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species','21','1','Constructor guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1834,0,'5-6 m thick patch reefs, lateral extension up to 30 m in shallowing upward sequence of first cycle.\nPorites-Faviidae assemblage.\n\n10 m thick and 200 m long reefs in next cycle.\nPorites-Faviidae assemblage but Porites less abundant than in lower reef. Heavily encrusted by coralline algae. 80-90 % coral coverage. \n\n20 species indicated (Genera: Acanthastrea, Acropora, Agathiphyllia, Antiguastrea, Astreopora, Astrocoenia, Caulastrea, Diploastrea, Favites, Goniopora, Hydnophora, Leptoria, Montastrea, Porites, Stylocoenia, Stylophora). Algae not described. ',31,52,3891772,4985833,'Iran','Asia',505,'',31.5097,52.7333,'WAHR','41076',31.6077875096,48.6280136035,31.6076048294,48.6292521549,29.7082034723,51.2558441754,28.4831,49.7972,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Qom',2709,'Qom','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',18,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1834,0,'Back-arc basin.\nSmall patch reefs at very top of Qom section. \n2-3 m thick some tens of m lateral extension.\nFormed by dome-shaped colonies (mostly faviids) and large Caulastrea thickets.',34,50,4441915,4768587,'Iran','Asia',505,'',34.6431,50.7125,'','',34.6067901952,46.6364284944,34.645392175,47.240656259,33.1398935141,49.4634030541,32.6123,48.8829,'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'),('Peace Reach, Williston Lake, B.C.',2712,'Liard','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',235,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','14','Brachiopods','13','Echinoderms','89','Brachiopods - echinoderms',NULL,NULL,'60','0','40',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','1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1836,2395,'Terebratulid-echinoderm biostromes.\n\nAbstract ref. 1836:\nAbstract: Mesozoic carbonate accumulations are rare in northwestern Pangea. This is due, initially to the demise of many carbonate secreting organisms during the terminal Permian biotic crisis and subsequently, to increased clastic sedimentation resulting from the tectonic development of western North America. Ecological voids resulting from the extinction however resulted in new opportunities for surviving taxa. Terebratulid brachiopod-echinoderm dominated biostromes within the primarily siliciclastic Liard Formation ( Middle Triassic, Ladinian) of northeastern British Columbia provide an example of this.  The Liard biostromes are composed primarily of whole and unabraded terebratulid brachiopods, articulate crinoid elements and cidaroid echinoid spines and interambulacral plates. Many of the terebratulid brachiopods are characterized by the pedicle attachment trace fossil Podichnus. Other organisms which occupied the biostromes include acrotretid and spiriferid brachiopods, bivalves, and gastropods, as well as rare bryozoans, oysters and possibly scleractinian corals.  Sedimentary units deposited on the margins of the biostromes are characterized by an abundance of body fossils (decapod crustaceans, bivalves and ophiuroids) and trace fossils (i.e. Asterosoma, Cylindrichnus, Palaeophycus, Rosselia, Teichichnus and Thalassinoides). This trace fossil assemblage contains a mix of horizontal and vertical deposit feeding organisms, consistent with deposition in a lower shoreface setting. Hiatal surfaces and laterally restricted bioclastic sandstone layers and lenses within these features suggests that frequent turnover of infaunal and epifaunal communities occurred at the edges of the Liard brachiopod-echinoderm biostromes.  Environmental/ecological criteria essential for the development of the Liard biostromes include: a) initial storm-induced concentration of shell material to create islands or zones of comparably stable substrate, thus promoting colonization by crinoids, terebratulid brachiopods, and cidaroid echinoids; b) a temporary decrease in siliciclastic input to the shoreface, allowing biostrome building organisms the chance to colonize these patches of stable substrate, and dominate deposition within the lower shoreface, and c) aerobic conditions in the lower shoreface allowing for a healthy and robust biostrome fauna.',56,-122,3268234,-4444816,'Canada','North America',121,'',56.05,-122.7167,'WAHR','44367',39.5846719872,-35.1806993066,39.5846719872,-35.1806993066,33.1619916288,-38.8109930222,24.0144,-37.2883,'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'),('Jeffersontown, Jefferson Co., Kentucky',2714,'Liberty','Ordovician','Upper Ordovician','Katian','Richmondian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',447,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'55',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'50','30','20',0,'no',0,'no','2','6 to 24 reef building species','13','1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1838,0,'Bardstown Reef, base of Liberty Fm.\nLocality 10 of Browne (1964)\nCoral beds with \nCorals: Favistella alveolata, Foerstephyllum vacuum, Protaraea richmondensis, Streptelasma rusticum, Tetradium approximatum\nUp to 1 m large coral heads\nStromatoporoids: 4 species of Aulacera\nBryozoans: 4 named species, many unidentified forms\ndiverser brachiopods, gastropods, pelecypods, some trilobites and cephalopods.\nCoral hoizons also in Waynesville (below) and Whitewater (above) Fms.',38,-85,-3116465,-6170930,'United States','North America',101,NULL,38.2,-85.5667,'WAHR','24034',-23.9261090663,-115.459676111,-23.9261090663,-115.459676111,-23.9261090663,-115.459676111,-25.5637,-60.3876,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bardstown, Nelson Co., Kentucky',2715,'Liberty','Ordovician','Upper Ordovician','Katian','Richmondian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',447,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'55','2714',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','7','Bryozoans','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','13','1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1838,0,'Reef 2714 for remarks\nLoc. 1 of Browne (1964)',37,-85,-3170270,-6174293,'United States','North America',101,'',37.8,-85.3833,'','',-24.3406038864,-115.564092754,-24.3406038864,-115.564092754,-24.3406038864,-115.564092754,-25.9662,-60.5401,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Montmorency river, Quebec City, Quebec',2716,'Deschambault','Ordovician','Upper Ordovician','Katian','early Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',454,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','6',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild','1','Present',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',1840,0,'Tenton group\r\nBryozoan bafflestone mound\r\nUp to 1.2 m high and 5.8 m wide\r\nNo evidence for asymmetry or mechanical breakdown.\r\n30 % bryozoan coverage\r\nNo encrusters, no zonation. \r\nMatrix burrowed and bored, sometimes affecting bryozoans (evident from fig. 8d in ref. 1840)',46,-71,-2828747,-4675430,'Canada','North America',121,'',46.8833,-71.15,'',NULL,-20.6256971403,-101.10264617,-20.6256971403,-101.10264617,-20.6256971403,-101.10264617,-23.5591,-45.4985,'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'),('Reed North Quarry, Fairborn, Green Co., Ohio',2718,'Brassfield','Silurian','Llandovery','Aeronian','Aeronian',438.50,440.80,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',437,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2','1','Less than 10 m wide','5','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','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','17','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation','2','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1843,2241,'Stromatoporpoids more common on leeward side\n\nRef. 1843:\nThe Early Silurian is a critical time for understanding the evolution of corals and their role as reef-builders. By the middle Early Silurian, corals and stromatoporoids were the primary reef-building organisms. The Brassfield Formation (Llandoverian) in southwestern Ohio consists principally of nearshore bioclastic grainstones and packstones with occasional boundstones and minor shale intervals. Numerous coral-stromatoporoid patch reefs reported from the Brassfield are among the oldest known in the United States. Unlike other Silurian reefs in the U.S., Brassfield reefs are undolomitized and well-preserved. These conditions allow observation of fine-scale morphological details and permit a detailed taxonomic and paleoecologic comparison with other Silurian reef communities.  Fossil material (in situ and from float) was collected from a Brassfield patch reef exposed in the Reed North Quarry, Fairborn, Greene County, Ohio. Approximately 350 fossil specimens were identified during preliminary mapping of at least 72 square meters of the patch reef. In order of abundance, the reef-building organisms include favositids (176 colonies), stromatoporoids (109 specimens), colonial rugosans (37 specimens), halysitids (16 colonies), and solitary rugosans (9 specimens). A few specimens have encrusting crinoid or bryozoan holdfasts. Initial observations indicate that this Brassfield patch reef is consistent with the model of a typical Early Silurian reef.',39,-83,-3411211,-5497915,'United States','North America',101,'',39.8139,-83.9833,'WAHR','22964',-29.9460684846,-103.946697039,-29.9460684846,-103.946697039,-29.9460684846,-103.946697039,-24.4348,-54.036,'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'),('Krzeszowice, Krakow',2720,'','Devonian','Upper Devonian','Famennian','Strunian',358.90,372.20,11,'late Famennian - early Visean',351,360,'Devono-Carboniferous Boundary (358.9 Ma)',362,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','20','80',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',1845,2136,'\'Reef\' series above brachiopod limestones.\nStromatoporoid beds (partly dolomitic) with prevailing Atelodictyon cracoviensis. Tn 1a',50,19,-1083325,1474723,'Poland','Europe',301,'',50.1333,19.6167,'WAHR','77910',-28.7147770507,12.212679331,-28.7147770507,12.212679331,5.01139842076,-55.0182020385,-11.76,21.2969,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yavapai Co., Arizona',2721,'Martin','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','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','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','8','Serpulids, worms, vermetids','3','Microbes','76','Worms only',NULL,NULL,'30','70','0',0,'no',0,'no','1','Less than 6 reef building species','2','2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',1846,0,'Silicified worm tubes of new species: Serpula helicalis form 0.5 m thick bioherm.\nDensely packed helical worm tubes.\nBioherm overlain by dolomitic algal laminites.',34,-112,-3141542,-5954899,'United States','North America',101,'',34.5833,-112.5,'WAHR','6255',-20.9776259043,-73.3166652131,-20.9776259043,-73.3166652131,-18.0022732681,-127.87104325,-22.8282,-59.7975,'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'),('Dieterlen Well, Clark Co., Ohio',2725,'Jeffersonville Limestone','Devonian','Middle Devonian','Eifelian','Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',394,2,'1','Seismic data available ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'50','0','50',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1853,0,'High-energy biostromal facies.\nBoundstone and rudstone containing stromatoporoids, colonial and solitary rugose corals, tabulate corals, crinoids, bryozoans, brachiopods.',38,-85,-5281330,-3240177,'United States','North America',101,'',38.5833,-85.7333,'','',-34.4501627534,-54.6913296347,-34.4501627534,-54.6913296347,-28.0443438253,-108.461930238,-40.6123,-34.2743,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Central Iowa',2726,'Lime Creek','Devonian','Upper Devonian','Frasnian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',376,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1854,0,'Stromatoporoid-rich biostromal units in shallowing-upward sequence of the Lime Creek-Sweetland cycle.',41,-93,-3775643,-4033366,'United States','North America',101,'',41.5,-93.75,'','',-27.120979298,-56.8079984493,-27.120979298,-56.8079984493,-19.6013421615,-110.769814992,-30.5432,-39.1924,'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'),('Vagia, Rhodes',2728,'Kolymbia','Neogene','Pliocene','Pliocene','Upper Pliocene',2.60,3.60,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',3,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m','50',NULL,NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','7','Bryozoans','2','Algae','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1','Red algae','50','10','40',0,'no',0,'no','3','25 or more reef building species','67','2','Baffler guild','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1856,1857,'Bryozoan thickets, predominated by branching Celleporaria palmata.\nMain structure 50x20 m in area. \nAssociated reef builders are coralline algae, serpulids, and numerous other bryozoans (66 species). Associated is also Lophelia.\n40 m water depth estimated.',36,28,4823101,2683816,'Greece','Europe',338,'',36.25,28.1667,'WAHR','71243',36.1717978532,27.585536849,36.1715374623,27.5836505896,36.0302059575,28.0524788911,36.2395,28.2294,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Toquay, Victoria',2729,'Puebla','Neogene','Miocene','Lower Miocene','upper Burdigalian',16.00,17.50,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',17,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,2,'Cold - water','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',NULL,NULL,'90','0','10',0,'no',0,'no','1','Less than 6 reef building species','1','2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1858,0,'Described as rhythmically bedded bryozoan bioherm. alternating bafflestone and packstone layers.\nDense accumulation of Cellepora gambierensis\n15 m thick.\n',-38,144,-6096882,12568009,'Australia','Oceania',801,'',-38.3333,144.3167,'','',-49.2803662204,142.277400181,-46.2483818919,142.408957376,-48.6242305893,144.847068203,-48.2786,142.672,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nurra, NW Sardinia',2730,'','Cretaceous','Upper Cretaceous','Coniacian','Coniacian-Santonian',83.60,89.80,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','4','Stromatoporoids','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'45','40','15',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1859,0,'Rudist limestone associated with bioclastic carbonates containing chaetetids, algae and corals. ',40,8,4202399,681663,'Italy','Europe',344,'',40.5833,8.2167,'','',38.1075253366,8.73023580307,38.1075253366,8.73023580307,34.5397164865,6.49130751558,33.4216,6.26637,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monte Sant-Angelo, Gargano',2731,'','Cretaceous','Upper Cretaceous',NULL,'Turonian-Campanian',72.10,93.90,25,'late Cenomanian - early Campanian',91,90,'Mid-Cretaceous (Turonian , 91.9 Ma)',83,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'45','55','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1859,0,'Matese group.\nBioherms with radiolitids, hippuritids and corals\nRedeposited in slope deposits.\nRef. 1859:\n\'Organogenic structures are present in which rudists are unbroken and partially preserved in growth position. In these structures, mollusc rudstone-bafflestones and mollusc floatstones are arranged in a complex way to form lens-shaped bodies.\'',41,15,3183480,1568234,'Italy','Europe',344,'',41.7,15.9667,'','',31.2394615299,16.3064547683,31.2394615299,16.3064547683,29.0741853722,17.112530391,26.132,15.9994,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grand Cayman, Cayman Islands',2732,'Bluff','Paleogene',NULL,NULL,'Oligocene-Miocene',5.30,33.90,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',23,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1860,0,'Heavily bioeroded \nby Entobia, Trypanites, Gastrochaenolites, Maeandropolydora, Talpina and Caulostrpsis.\nAlgae significantly less affected than corals and bivalves. Also difference among corals: Stylophora most extensively affected.\n38 % average boring in corals',19,-81,2643542,-8680363,'United Kingdom','Europe',331,'',19.3167,-81.1667,'','',18.3638505446,-77.6450273562,18.3645065347,-77.6479415618,21.358566623,-77.039122108,19.7462,-77.2309,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Eastern Ellesmere Island',2733,'Alan Bay-Cape Storm','Silurian','Llandovery','Aeronian','Aeronian-Telychian',433.40,440.80,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',436,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'2000',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,NULL,NULL,'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',1861,0,'Llandovery sequence\nRecrystallized dolostone containing pentamerids, stromatoporoids and tabulate corals.\nProbably shelf margin reef. \n>150 km exposed outcrop.\nProbably part of 2000 km reef tract.',79,-76,740501,-3137015,'Canada','North America',121,'',79.75,-76.5,'','',5.25837035781,-85.2852354439,5.25837035781,-85.2852354439,5.25837035781,-85.2852354439,6.06861,-29.1894,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Eastern Ellesmere Island',2734,'Alan Bay-Cape Storm','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','4','More than 500 m thick','550',NULL,NULL,NULL,'4','More than 1000 m',NULL,'150',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'90','0','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1861,0,'Coral-microbial shelf margin reef tract\n500 m thickness exposed (base covered by glacier).\nNew genus of branching rugose corals prevails (up to 1 m in diameter).\nAdditionally cf. Halysites (up to 50 cm in diameter)\nCorals encrusted by microbialites and lesser radiacial calcite.\nUp to 50 % marine cement locally.\nMicrobialites: clotted or vaguelly laminated micrites, 3-5% calcimicrobes (Renalcis, Epiphyton\', cf. Gammia).\nStromatoporoids, brachiopods, megalodont bivalves and lithistid sponges are accessorial.\n\nAbstract or ref. 1861:\nA recently discovered Silurian reef tract in the high Canadian Arctic has an exposed length of more than 150 km and is locally more than 500 m thick. The reefs occur within a Silurian ramp and rimmed shelf-margin sequence about 2 km thick. Conodont biostratigraphic data indicate that the reefal strata are late Llandovery to Ludlow in age, and reefs are composed largely of coral-microbial boundstone, The corals are mainly digitate rugosans and large halysitids, associated with fewer stromatoporoids and lithistid sponges. However, most of the reefal strata consist of microbialite, which encrusts skeletal metazoans or is massive or thromboidal. Microbialite microstructure consists mainly of clotted micrite or laminated micrite associated with common Renalcis, other calcimicrobes, and locally abundant early marine cements. Other reef rock types include stromatactis-rich lime mudstone, cementstone, zebroid stromatactis-bearing lime mud-stone, crinoidal grainstone, and, rarely, stromatoporoid boundstone. The reefs formed on the shelf margin and prograded basinward in three distinct phases during Wenlock and Ludlow time. Underlying Llandovery, shelf-margin facies are highly dolomitized and may represent an original stromatoporoid boundstone. Overlying late Ludlow to Pridoli carbonates were deposited on a prograding carbonate ramp, dotted with small coral-stromatoporoid and other biostromes, Three periods of Silurian reef growth can be recognized in the Arctic: Llandovery, latest Llandovery-late Ludlow, and late Ludlow-Pridoli. The Llandovery phase was widespread, and large stromatoporoid-coral reefs occupied a variety of depositional settings, including shelf-edge, intrashelf, drowned shelf, and slope. Late Llandovery to late Ludlow reefs were also regionally extensive, but were predominantly coral-microbial boundstone and locally grainstone-rich structures containing accessory metazoan (stromatoporoid-coral) framestone and boundstone. These formed high-relief structures with coarse allochthonous debris aprons. Large stromatoporoid-coral reefs were also present, but these were confined to areas characterized by high rates of siliciclastic sedimentation or to intrashelf areas. Another regional change in reef composition occurred in the latest Ludlow. Initially, reefs were rare and dominated by lithistid sponges and microbialites, but in Pridoli time, they became widespread and were constructed by corals and stromatoporoids, as were their Llandovery ancestors. In addition, the Pridoli reefs did not attain the large sizes of reefs in the two older sequences. The three phases of reef development can be related to important, basinwide sequence boundaries. Microbialite-rich reefs have also been described from northwestern Russia, Alaska, and eastern Canada and are some of the largest reef structures known. Their large size reveals a need to reconsider popular reef evolutionary models, in which skeletal metazoans are regarded as the predominant constructors. Large reef size is implied in these evolutionary models, but, based on this and other reef studies, microbialite-rich reefs equal, and commonly surpass, the dimensions exhibited by coral-stromatoporoid reefs. Considering the microbialite-rich reefs, now known from both the Ordovician acid Silurian, it is clear that benthic microbial communities played a very important role in reef construction through the lower Paleozoic.',79,-74,442255,-2686319,'Canada','North America',121,'',79.7833,-74.2167,'','',7.22720686342,-72.5188602801,7.22720686342,-72.5188602801,7.22720686342,-72.5188602801,4.10332,-25.4951,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Section B, Eastern Ellesmere Island',2735,'Alan Bay-Cape Storm','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','4','More than 500 m thick','550',NULL,NULL,NULL,'4','More than 1000 m',NULL,'150','2734',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'90','0','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1861,0,'See reef 2734',79,-77,461571,-2749277,'Canada','North America',121,'',79.5667,-77.25,'','',7.13501386831,-73.1012577635,7.13501386831,-73.1012577635,7.13501386831,-73.1012577635,4.26191,-26.0598,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Garlo, Breznik',2736,'','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',73,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','30',NULL,NULL,NULL,'3','More than 100 m',NULL,'15',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','5','Rudists','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,'20','70','10',0,'no',0,'no','2','6 to 24 reef building species','15','1','Constructor guild','1','Present','1','Present','2','Medium zonation',NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1863,0,'Previously considered Maastrichtian age. Sr isotopes suggest Campanian!\n\nSeveral localities with Maastrichtian reefs.\nUp to 30 coral species in one subreef facies at Garlo.\nReefal facies commonly 30 m thick containing 9 to 15 coral species. \n\nCorals associated with rudists, chaetetids, octocorals, calcareous algae and bryozoans. ',42,22,4125613,2061817,'Bulgaria','Europe',319,'',42.7833,22.8333,'WAHR','67569',39.0310567354,23.7014694731,39.0310567354,23.7014694731,39.3286141407,22.5272114969,26.8173,22.7462,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dire Dawa',2737,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian?',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'80',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','80','20',0,'no',0,'no','2','6 to 24 reef building species','7','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1865,0,'Only corals and some stromatoporoids described.\nHeavy limestone sereis overlying conglomerate at base.\nGenera:\nActinostroma\nStylina\nStromatopora\nMilleporidium\nSeveral species.\nMacroborings evident from figures.',9,41,-1922966,3142390,'Ethiopia','Africa',715,'',9.6,41.8667,'','',-24.3521097467,32.1599395872,-24.3521097467,32.1599395872,-20.227109627,28.4597001607,-11.5568,26.3118,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Boudame, Harrar',2738,'','Jurassic','Upper Jurassic','Oxfordian','lower Oxfordian?',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',160,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'80','2737',0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','80','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1865,0,'Lusitanian?\nThamnasteria\nActinostromaria',9,41,-1992928,3131768,'Ethiopia','Africa',715,'',9.0833,41.9167,'','',-24.8576161483,32.0303771715,-24.8576161483,32.0303771715,-20.7196095302,28.2847693296,-12.0601,26.1824,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ouihlane, Tafilalet',2739,'Taboumaklouf','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 ',1,'True reef','1','Less than 10 m thick','8',NULL,NULL,NULL,'3','More than 100 m','200',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1868,1867,'Patch reef in lower eiflius zone.\nAlmost entirely built by big globular stromatoporoids and heliolitid corals with up to 0.4 m diameters. \nSome big alveolitids\nDendroid tabulate corals and solitary Rugosa as accessory reef builders.\nUp 8 m thick 200 m extension.\nCovered by marls',31,-4,-6024222,1241531,'Morocco','Africa',714,'',31.1972,-4.9333,'','',-37.3872422739,-7.93458987711,-37.3872422739,-7.93458987711,-40.3995169851,-7.8466325998,-47.0041,19.2896,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ouihlane',2740,'Bou Dib','Devonian','Middle Devonian','Givetian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',390,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8',NULL,NULL,NULL,'2','10 - 100 m','30',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','3','25 or more reef building species','25','1','Constructor guild',NULL,NULL,'1','Present','1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1867,1869,'Only peri-reef section sampled.\n20-30 m extension of reef.\n17 species of rugose corals described. \nAdditionally diverse tabulate corals and stromatoporoids\nSome calcimicrobes (Rothpletzella, Girvanella)\nClastic input terminated reef growth.',31,-4,-4605626,802657,'Morocco','Africa',714,'',31.1972,-4.9333,'WAHR','62894',-38.7436640595,-8.60870812633,-38.7436640595,-8.60870812633,-43.4269624499,-8.48731594685,-44.0125,15.8299,'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'),('Vermont, USA',2742,'Gorge','Cambrian','Furongian','Lawsonian','Sunwaptan-Ibexian',491.00,493.00,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',488,3,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1870,0,'Trilobite fauna from \'shelf-margin\' buildups.',44,-72,-1994757,-5784922,'United States','North America',101,'',44,-72.8333,'','',9.75168813076,-101.866601469,9.75168813076,-101.866601469,9.75168813076,-101.866601469,-32.1,-77.3172,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('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'),('W Coimbra, N Lusitanian Basin',2745,'','Jurassic','Lower Jurassic','Toarcian','Toarcian',174.10,182.70,19,'late Hettangian - early Aalenian',188,180,'Early Jurassic (Toarcian, 178.4 Ma)',179,2,'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','3b','Deeper slope or outer ramp','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',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',1872,0,'',40,-8,4054776,95082,'Portugal','Europe',304,'',40.25,-8.5,'','',23.1237700189,14.3700033892,23.1237700189,14.3700033892,30.1060953572,12.0642490171,31.2644,4.93342,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Casais Verdelho, Arruda, Lusitanian Basin',2746,'Amaral','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'2',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','3','Microbes','61','Microbes (thrombolites) - algae - corals',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','29','1','Constructor guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',412,0,'Several  small coral-microbial crust biostromes',39,-9,3724026,-300476,'Portugal','Europe',304,'',39,-9.0667,'WAHR','68786',20.308342065,8.0997259962,20.308342065,8.0997259962,27.4576753443,5.29472619585,33.5437,0.755984,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Terriente, Celtiberian Range',2747,'','Jurassic','Upper Jurassic','Kimmeridgian','lower Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',154,3,'0','Outcropping reef ',4,'Biostrome','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','1','Corals','1','Corals','22','Stromatoporoids/sponges - corals - (algae)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','35','1','Constructor guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1873,412,'Very rich coral assemblage reported (ref. 2312-2313), but mostly from adjoining marls.',40,-1,3616615,387662,'Spain','Europe',304,'2312, 2313',40.3333,-1.5,'WAHR','34611',18.7992300468,14.2334369339,18.7992300468,14.2334369339,25.0708357194,11.4020192055,31.864,7.56973,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jumara Kachchh',2748,'','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 ',4,'Biostrome','2','10 to 100 m thick',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','11','Siliceous sponges','11','Siliceous sponges',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',421,0,'',23,69,-3042086,3764318,'India','Asia',501,'',23.5,69.0833,'','',-30.4825330451,40.3268879945,-30.4825330451,40.3268879945,-31.0766586547,36.6146951796,-21.4348,33.0287,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Makhtesh Gadol, Negev',2749,'Matmor','Jurassic','Middle Jurassic','Callovian','upper Callovian',163.50,164.50,21,'late Bathonian - early Tithonian',151,165,'Middle Jurassic (Callovian, 164.8 Ma)',162,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','58',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'20','40','40',0,'no',0,'no','3','6 to 24 reef building species','30','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2829,1842,'Afriat et al. (2023): Athleta and lamberti zones\r\nMore than 20 coral genera, diverse stromatoporoids.\r\nA major shift from coral-dominated patch reefs in the lower part of the section to dominating stromatoporoids in the upper part.\r\n\r\nSclerozoan faunas described in detail by Wilson et al. (2008).',30,34,894920,3075025,'Israel','Asia',508,'2830',30.9347,34.975,'WAHR','91903',-2.67529800285,33.0974387812,-2.72190885408,33.0254334641,-0.969094200893,30.7256253771,9.94426,29.3115,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alrota, Estremadura',2750,'','Jurassic','Upper Jurassic','Tithonian','middle? Tithonian',145.00,152.10,21,'late Bathonian - early Tithonian',151,150,'Late Jurassic (Tithonian, 148.6 Ma)',147,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'8',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'30','50','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1874,1875,'Lense-type, meter-sized coral patch reefs, partly rich in oysters, with additional calcisponges, stromatoporoids and others, in siliciclastic-carbonate setting. \nMostly bafflestones',38,-9,3490845,-506989,'Portugal','Europe',304,'1876',38.9794,-9.1281,'WAHR','68238',21.2945640472,6.22469117886,21.2945640472,6.22469117886,28.4181847006,3.75843873143,33.8742,0.373886,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Montejunto, Estremadura',2751,'','Jurassic','Upper Jurassic','Oxfordian','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',156,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,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','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','80','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present','1','Present','3','Pronounced zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1876,1877,'',39,-9,3747290,-290481,'Portugal','Europe',304,'',39.1958,-9.0514,'','',19.9871761493,9.93784902961,19.9871761493,9.93784902961,27.2596672943,6.83273715131,33.2875,1.56758,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Frost, Cotton Valley, Freestone County, East Texas',2752,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian-Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',150,1,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'130',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,'1','Present','1','Present','3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',1878,1795,'',31,-96,2265299,-4876779,'United States','North America',101,'',31.6667,-96.3556,'','',19.3824809193,-38.8124924338,19.3824809193,-38.8124924338,24.5965255759,-41.3740695316,26.4368,-46.2852,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Barreiro, Lusitanian Basin',2753,'','Jurassic','Upper Jurassic','Oxfordian','Late(?) Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',156,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','80','20',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'3','More than 60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1877,1876,'',38,-9,3683241,-323623,'Portugal','Europe',304,'',38.6392,-9.1514,'WAHR','68245',19.5388061445,9.57778681655,19.5388061445,9.57778681655,26.8525202457,6.397715033,32.845,1.15412,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monte Gordo-Castanheira, Vila Franca',2754,'Abadia','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'4',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','3','Pronounced zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',1876,1879,'Taxonomy in ref. 1875 is from Casal da Carrica\nMarly coral biostromes',38,-9,3713569,-297803,'Portugal','Europe',304,'1875',38.9347,-9,'WAHR','34660',20.2261198042,8.1145353856,20.2261198042,8.1145353856,27.3743006438,5.29638220332,33.4613,0.771132,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sobral, Lusitanian Basin, Estremadura',2755,'Sobral','Jurassic','Upper Jurassic','Kimmeridgian','topmost Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',151,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'30','70','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1877,0,'',39,-9,3726240,-305401,'Portugal','Europe',304,'',39,-9.1256,'','',20.3304602393,8.05699129704,20.3304602393,8.05699129704,27.4855250479,5.25378246441,33.5665,0.708304,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Istein, Freiburg, Rhine Valley',2756,'','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 ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'5','75','20',0,'no',0,'no','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','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1880,1881,'',47,7,4677911,1012245,'Germany','Europe',331,'',47.6667,7.5333,'','',26.859672361,25.184121012,26.859672361,25.184121012,32.9707496206,25.9856938127,38.6179,16.5047,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Beuron, Donautal',2757,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'130',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1882,0,'',48,9,4758646,1109245,'Germany','Europe',331,'',48.0667,9,'','',28.0588499872,24.4261030615,28.0588499872,24.4261030615,33.3743926455,25.8481809656,39.4943,17.2846,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hochwanger Steige',2758,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'130','2757',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1882,1883,'',48,9,4820343,1099044,'Germany','Europe',331,'',48.55,9.1167,'WAHR','74063',28.5432306713,24.3459620942,28.5432306713,24.3459620942,33.8624255673,25.8028113827,39.9821,17.3374,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Blaubeuren',2759,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'130','2757',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1882,0,'',48,9,4816192,1154197,'Germany','Europe',331,'',48.4,9.7667,'','',28.5305026347,24.8651336325,28.5305026347,24.8651336325,33.8187356369,26.3496255909,39.866,17.9128,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dohlenfels, Konstein',2760,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',1884,0,'',48,11,4898165,1235412,'Germany','Europe',331,'',48.8333,11.0833,'','',29.2117439744,25.6572969798,29.2117439744,25.6572969798,34.4501391312,27.2428670592,40.3685,19.0013,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mata, Lisboa',2761,'Sobral','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',152,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','10',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','1','Corals','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'80','20','0',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1885,0,'small oyster patch reefs (up to several metres large and 50 cm high) within delta clastics',38,-9,3716622,-304567,'Portugal','Europe',304,'',38.9667,-9.1,'WAHR','68240',20.2916901773,8.05840872782,20.2916901773,8.05840872782,27.4469903205,5.24874730658,33.5277,0.709196,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Consolaçao, S-Peniche',2762,'','Jurassic','Upper Jurassic','Kimmeridgian','lower Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',154,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present','1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1886,0,'Nanogyra very common',39,0,3449094,459264,'Portugal','Europe',304,'',39.3333,-0.2167,'WAHR','67903',17.4703019933,14.7098749514,17.4703019933,14.7098749514,23.6865690892,11.6591465093,30.5162,8.02934,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Consolaçao, S-Peniche',2763,'','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',152,3,'0','Outcropping reef ',1,'True reef','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','15','Non-rudist bivalves','2','Algae','47','Bivalves (mostly oysters) - algae (microbes)','1','Red algae','80','20','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1886,1887,'',39,0,3449094,459264,'Portugal','Europe',304,'',39.3333,-0.2167,'WAHR','67940',17.4703019933,14.7098749514,17.4703019933,14.7098749514,23.6865690892,11.6591465093,30.5162,8.02934,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Santa Cruz',2764,'','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',152,3,'0','Outcropping reef ',1,'True reef','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','15','Non-rudist bivalves','2','Algae','47','Bivalves (mostly oysters) - algae (microbes)','1','Red algae','80','20','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',1888,1887,'',39,0,3421154,448029,'Portugal','Europe',304,'',39.1,-0.25,'WAHR','68232',17.2706666945,14.5805243261,17.2706666945,14.5805243261,23.5091757885,11.4914121483,30.3223,7.87593,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alcobaça',2765,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'7',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1889,0,'',39,0,3465820,498770,'Portugal','Europe',304,'',39.5667,0.15,'WAHR','68220',17.5598694335,15.0830282597,17.5598694335,15.0830282597,23.7179963599,12.0584312723,30.5892,8.44693,'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'),('Banija',2767,'','Paleogene','Paleocene','Danian','lower Paleocene',61.60,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',62,1,'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','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',503,506,'See reef 639',45,16,4555473,1510685,'Croatia','Europe',308,'',45.4333,16.2,'','',35.1347519497,16.3651626521,35.1347519497,16.3651626521,38.6314659906,17.3727914119,34.3517,14.595,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Vigny, Paris Basin',2768,'','Paleogene','Paleocene','Danian','Danian',61.60,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',64,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','80','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1892,0,'Diverse growth shapes of colonial corals:\nlamellar dominant\nmassive \nbranching\n\nAlgae: Lamellar (Melobesiids, Aethelia, chlorophyceans)\nMassive (Solenoporaceans)\nAlgae associated with encrusting foraminifera\n\nAssociated fauna: miliolid forams, bryozoans, worm tubes, pharetronid sponges, bivalves, brachiopods, echinoids.\nClionid borings.\n\nHigh amount of reworked reef clast and grainstones.',49,1,5590480,42407,'France','Europe',331,'',49.0833,1.9333,'WAHR','20816',44.2263412944,1.97366875224,44.2263412944,1.97366875224,47.4489603651,0.91082808446,42.4376,-0.189739,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Colle, Boñar, Cantabria',2769,'La Vid Group','Devonian','Lower Devonian','Emsian','upper Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,395,'Early Devonian (late Emsian, 395 Ma)',399,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1895,2455,'Several biostromal levels predominated by fasciculate rugose corals (Synaptophyllum). Additionally favositids, alveolitids, auloporids and stromatoporoids.\nSome in growth position.\nSynaptophyllum-Atrypa pioneer fauna.',42,-5,-4859832,2398469,'Spain','Europe',304,'',42.8833,-5.25,'WAHR','77390',-25.6468789289,-1.34228740694,-25.6468789289,-1.34228740694,-10.5357414729,-19.3265062579,-43.4775,34.2975,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ossa Morena, Los Santos de Maimona Basin',2770,'Siphonodendron Lst.','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 ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','14','Brachiopods','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','11','2','Baffler guild','1','Present','1','Present','1','Low zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1896,0,'Interpeted as reef flat behind reef crest.\nGrowth controlled by periodic storms.\nRugose corals (Siphonodendron) and a few brachiopod species form 80 % of framework.\nTabulate corals, bryozoans, and algae as minor constituents.\nBoring visible on Fig. 5/2 of ref 1896',38,-6,-2058645,451093,'Spain','Europe',304,'',38.45,-6.3833,'WAHR','34641',-42.2560502248,-9.22311486525,-39.0036133853,-7.25713986215,-16.9602356358,-35.9330222143,-17.2061,3.03919,'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'),('Bidu River, Kerman',2773,'Bahram','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 ',4,'Biostrome','2','10 to 100 m thick','25',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1899,1898,'Well developed coral-stromatoporoid biostromes (probably reefs). 25 m thick.\nAutogenic succession with first branched then massive corals and finally abundant stromatoporoids.\nActinostroma, Stictostroma, Clathrocoilona, Dendrostroma, Hermatoporella and Stachyodes present. \nRugose corals: Hexagonaria, Peneckialla, Disphyllum, Temnophyllum',30,56,-3607338,7376090,'Iran','Asia',505,'1900',30.75,56.8333,'WAHR','62135',-37.1887419463,58.4011605193,-37.1887419463,58.4011605193,-58.9524900461,83.0046162059,-39.5246,87.1491,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Howz-e Dorah, Tabas',2774,'Shishtu','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 ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',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',1900,0,'Biostrome of branching corals.\nOverlying Bahram Fm.',33,57,-3379862,7206508,'Iran','Asia',505,'',33.4,57.2,'WAHR','62152',-34.9469581831,56.6108747296,-34.9469581831,56.6108747296,-56.7440986075,80.1892321675,-38.3346,90.2192,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Phong Nha, Quang Binh',2775,'Cù Bai','Devonian','Upper Devonian','Famennian','latest Famennian',358.90,372.20,11,'late Famennian - early Visean',351,360,'Devono-Carboniferous Boundary (358.9 Ma)',362,3,'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,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','20','40',0,'no',0,'no','2','6 to 24 reef building species','21','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1901,0,'Diverse assemblage of stromatoporoids, rugose and tabulate corals.\nRugose: Cystophrentis, Cobaiphyllum, Amygdalophyllum\nTabulates: Syringopora, Roemeripora\nStromatop.: Labechia, Stylostroma, Platiferostroma, Vietnamostroma, Rossenella, Clavidictyon.\n21 species in total.\nAdditionally diverse foraminifera.',17,106,-1060470,10906072,'Vietnam','Asia',NULL,'',17.45,106.4833,'','',-10.3156548242,92.7480714094,-10.3156548242,92.7480714094,-29.1955161859,99.1049722719,7.11153,105.994,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Panama Canal',2776,'La Boca - Culebra','Neogene','Miocene','Lower Miocene','Burdigalian?',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',18,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more 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',1903,1904,'11 genera and 23 species of corals.\nsmall patch reefs (<100 m3) in Emperador Limestone.\nSr-age 17.6-22 Ma.\nAstrocoenia, Stylophora, Pocillopora, Acropora, Astreopora, Pavona, Leptoseris, Porites, Goniopora, Goniastrea, Montastrea.',9,-79,1218220,-8714842,'Panama','North America',230,'1902, 2482',9.0833,-79.7333,'WAHR','60267',5.7616241145,-79.4476670019,5.76012725266,-79.4472671905,9.0833,-79.7333,8.5262,-77.4089,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Northern Dominican Republic',2777,'Baitoa','Neogene','Miocene','Middle Miocene','Langhian-Serravallian',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',15,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','7','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1905,1902,'Sr age 13-17.6 Ma\r\nImpoverished fauna: 5 genera, 7 species of corals.\r\nStylophora, Pocillopora, Alveopora, Montastrea, Solenastrea',17,-70,2413488,-7602972,'Dominican Republic','North America',254,'',17.6667,-70.6667,'',NULL,16.2666049543,-70.4794395893,16.2666049543,-70.4794395893,17.6667,-70.6667,17.6319,-69.4061,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dominican Republic',2778,'','Paleogene','Oligocene','Chattian','Chattian?',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',26,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1907,1902,'',19,-70,2597686,-7547039,'Dominican Republic','North America',254,'',19.25,-70.5,'','',17.0999633365,-69.7086488325,17.0999633365,-69.7086488325,20.6401568999,-68.7902934711,18.7006,-69.246,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chingiz',2779,'Bestamak','Ordovician','Middle Ordovician','Darriwilian','Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',460,1,'0','Outcropping reef ',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','2c','Atoll (circular structure)',NULL,NULL,'2','Algae','2','Algae',NULL,NULL,'2','Green algae','0','80','20',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',1668,0,'Eastern Chingiz-Tarbagatay volcanic belt.\r\n\r\nReefal facies in a 20 to 100 m-thick sequence of oolitic, sandy, clayey, clotted, massive and brecciated limestones, that crop out in craggy ranges for at least 100 km along strike, with an abundant biota that includes red and green algae, trilobites, brachiopods and gastropods. \r\n\r\n',49,85,-1028123,7439076,'Kazakhstan','Asia',301,'',49.2,85.95,'',NULL,7.81683460815,-18.7456335373,7.81683460815,-18.7456335373,7.81683460815,-18.7456335373,11.3221,29.1193,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Franklin Mts., El Paso, Texas',2780,'Aleman','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',447,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2',NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1908,1909,'Coral biostrome dominated by rugose (Paleophyllum, Cyathophylloides) and tabulate corals.\r\nUp to 2 m thick.\r\nOccurrence in Franklin and Baylor Mts. \r\nUpper Aleman Fm. of Montoya Group. ',31,-106,-2016009,-8234300,'United States','North America',101,'',31.8833,-106.4833,'WAHR','80617',-17.0306068092,-133.467248477,-17.0306068092,-133.467248477,-17.0306068092,-133.467248477,-16.9722,-77.6407,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Beiguoshan, Longxian, Shaanxi',2781,'Beiguoshan','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',448,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','100','150','2511',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'50','30','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1912,1911,'Original age call: Caradocian-Ashgillian\nWebby pers comm.\nAt Beiguoshan the patch reefs are similar [see reef 2511], but are especially dominated by corals and stromatoporoids, and over 20 m thick and 100 m wide (Zhou and Ye 1996). Zhou et al. (1989)  listed representatives of the illaenid-cheirurid trilobite biofacies in the Beiguoshan Formation at Longxian and Taoqupo Formation at Yaoxian (northeast of Dongzhuang). ',34,106,5524357,14593936,'China','Asia',602,'',34.8833,106.85,'','',37.5643686779,94.1265584357,37.5643686779,94.1265584357,37.5643686779,94.1265584357,-27.2701,121.225,'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'),('Tuosuo Lake - Huashixia, Kunlun Mts., Qinghai',2783,'Aqikkule','Permian','Cisuralian','Sakmarian','Longlinian',290.10,295.00,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',277,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'300',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','9','Tubiphytes','2','Algae','24','Tubiphytes - algae - cyanophyceans - (bryozoans) - (sponges)','1','Red algae','10','0','90',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor 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',1915,2220,'Stratigraphy according to ref. 2220\nReef growth starting in Longlinian with Tubiphytes-Archaeolithoporella frame and crinoid bryozoan baffle frame.\nAbstract of ref. 1915:\nThe early Permian reef belt is distributed in the southern side of eastern Kunlun, north area of Qinghai-Tiber Plateau. The core-reef facies of the reef extends from Tuosuo Lake to Huashixia. Lots of reef breccia was found at the southern slope of the core-reef belt, and to the north of the reef belt there is back-reef limestone. Calcisponges, hydrozoa, bryozoa, Tabulozoa, Tubiphytes and red algae are the main frame-building organisms. Archaeolithoporella, laminated blue-green algaes, Tabulozoa and Tubiphytes played a role of binding or encrustating. There are many kinds of epibiont in the reef, including brachiopod, gasteropod, foraminifera, echinoderm and simple coral. The type and the characteristics of the reef- building organisms in eastern Kunlun and Animaqing are basically the same as those in the south of China.',35,98,-3033604,8478680,'China','Asia',602,'',35.1167,98.8333,'','',25.9858755769,107.786923819,25.9858755769,107.786923819,42.6264638466,62.6954995809,12.9633,73.4828,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hydra',2784,'Eros Limestone','Triassic','Middle Triassic','Anisian','middle Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',243,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','120',NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','9','Tubiphytes','2','Algae','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','2','Green algae','0','20','80',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1916,0,'Pelsonian age\n> 100 m reef mounds, predominatnly Tubiphytes and algae\nTubiphytes reefs.\nAlgae, Tubiphytes, sponges, some corals',37,23,-313827,2673676,'Greece','Europe',338,'',37.3333,23.5,'WAHR','73815',3.12360757004,32.26633016,3.12360757004,32.26633016,-0.24111865557,26.9824164724,-5.97238,25.941,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dax, Aquitaine',2785,'','Paleogene','Paleocene','Danian','upper Danian',61.60,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',62,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick','80',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,'1','Present','1','Present',NULL,NULL,'2','Medium zonation','2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1917,0,'Well data from 20 km east of Dax (Bastennes-Lonné).\nCoral-algal barrier reef indicated and dasycladaceans described.\nUp to 80 m thick.\nAcicularia valeti in rock-forming abundance',43,0,4928616,-226581,'France','Europe',331,'',43.6667,-0.85,'','',38.7222847137,-0.230514936139,38.7222847137,-0.230514936139,42.0051824907,-1.68090144215,37.0786,-2.88929,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('NE Tarbes, Aquitaine',2786,'','Paleogene','Paleocene','Danian','upper Danian',61.60,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',62,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'100','2785',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','80','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,'1','Present','1','Present',NULL,NULL,'2','Medium zonation','2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1917,0,'Well data from several wells along l\'Arcos river (Jacque 1, Osmets 1, Laméac 1).\nSee also reef 2785',43,0,4884320,-135350,'France','Europe',331,'',43.35,0.2167,'WAHR','22970',38.4409569367,0.776494341692,38.4409569367,0.776494341692,41.6987271462,-0.636742742659,36.739,-1.93401,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Asher Atlit 1 Borehole,',2787,'','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,'1','Seismic data available ',1,'True reef','3','101-500 m thick','320',NULL,NULL,NULL,NULL,NULL,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','6','Calcisponges','3','Microbes','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',NULL,NULL,'3','Pronounced zonation',NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',1,'Potential reservoir',1920,2209,'The reef facies may correspond to platform rim biolithite reefs, or to ramp-like oolitic shoals and patch reefs. Reef builders include coralline sponges, microbial crusts and sessile foraminifera, various microproblematica (Microtubus, Bacinella) and corals. Back-reef environments are characterized by algal-foraminiferal facies with coated grains, oncoids and foraminifera, and a grapestone facies. \n\nReef facies intercalated with volcanics. Cummulative thickness of reef facies about 340 m.',32,34,168894,3132060,'Israel','Asia',508,'',32.6833,34.9333,'WAHR','67742',4.93533338499,37.8751431863,8.04085406685,37.5976521806,-0.461304530587,30.5495384556,10.3639,26.9929,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cankiri, Ankara',2788,'Bölugdag','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',68,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1921,0,'Maastrichtian reef limestones unconformably covered by basal conglomerates of Paleocene age.\nNo description of reefs',40,33,4536507,2865917,'Turkey','Asia',522,'',40.6,33.6167,'','',37.9624187371,33.0547338251,37.9624187371,33.0547338251,38.580118703,32.0578542199,32.8145,29.2348,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Sungurlu, Ankara',2789,'Kepirtepe','Paleogene','Eocene','Lutetian','Middle Eocene?',38.00,47.80,28,'Lutetian - Bartonian',45,45,'early Middle Eocene (Lutetian, 44.5 Ma)',40,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1921,0,'Biostromal and biohermal limestones near top of Kepirtepe Fm.',40,34,4975035,2914563,'Turkey','Asia',522,'',40.1667,34.3833,'',NULL,39.4164691276,28.8734587769,39.4164691276,28.8734587769,38.7482276234,33.3027529497,38.3596,30.1219,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Djarty-Rabat, SE Pamir, Tadzhikia',2790,'Gurumdy','Jurassic','Lower Jurassic','Sinemurian','Sinemurian',190.80,199.30,19,'late Hettangian - early Aalenian',188,195,'Early Jurassic (Hettangian&Sinemurian, 196 Ma)',195,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1922,2498,'From Flügel manuscript.\nHettangian to lowermost Sinemurian\nCoral reefs?',37,73,4304549,8609863,'Tajikistan','Asia',301,'',37.7833,73.55,'WAHR','67012',50.4595244287,83.5152061969,50.4595244287,83.5152061969,23.744321732,93.8765151391,35.705,67.3307,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('NMA-1 well, Male',2791,'','Quarternary','Pleistocene','Pleistocene','late Pliocene-Pleistocene',0.80,3.60,33,'Pleistocene',0,4,'Piacenzian - Zanclean',1,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1928,1942,'Abstract of ref. 1928:\nAs documented by industrial seismic reflection profiles and well data, the Cenozoic stratigraphic evolution of the Maldive carbonate system shows three distinct intervals characterised by their own specific depositional signatures. Late Palaeocene volcanics generated by the Reunion hotspot filled deeper pull-apart structures and created a flat topography that promoted the onset of the Maldive carbonate system in the early Eocene. Some of the initial structural depressions remained as deep internal seaways surrounded by reefal margins until the late Oligocene. The Eocene-Early Oligocene stratigraphic signature is essentially aggradational and corresponds to a transgressive cycle associated with a second-order sea-level rise. In the mid-Oligocene, a major sea-level fall exposed the neritic carbonate system and restricted sedimentation to the former deep internal basins. During the next transgression, a neritic carbonate system re-established itself on the newly flooded platform and was finally drowned near the Oligocene- Miocene boundary. The main effect of this second-order transgressive cycle was the transformation of the central troughs into one single deep basin in the Neogene, the palaeo- Maldive Inner Sea. When a reef framework was established in the early Miocene near the present location of the platform edge, systematic bank margin progradation toward the central Inner Sea basin became enhanced. This Neogene progradational phase is explained as the response to a long-term sealevel fall associated with a second- order regressive cycle. Finally, the late Pliocene-Pleistocene depositional signature is mainly aggradational and corresponds to the regional modification from flat-topped carbonate banks to atoll physiographies. The \'antecedent karst theory\' suggests that increased karstification was triggered by high-frequency eustatic and climatic changes in the last 3.0 Ma.',4,72,273753,7888563,'Maldives','Asia',NULL,'',4,72.5,'','',3.46674883826,71.9867933685,3.35050606216,71.8733218162,4,72.5,3.27853,72.1108,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hilleste, Hiiumaa Island',2792,'Hilleste','Silurian','Llandovery','Rhuddanian','upper Rhuddanian',440.80,443.40,6,'Rhuddanian-Telychian',435,440,'Early Silurian (early Llandovery, 441.2 Ma)',440,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','2','6 to 24 reef building species','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',1929,1536,'Pachystylostroma ungeri community (reef community) with\nP. ungerni, P. exile, P. hillistense, Forolinia lineata, Clathrodictyon demissum, C. sarvense, Ecclimdictyon pandum and exotic Plectostrom anecopinatum (earliest actinostromatid).',58,22,-2635426,-262384,'Estonia','Europe',NULL,'',58.8667,22.9833,'WAHR','61750',-19.2513302556,-55.2295443234,-19.2513302556,-55.2295443234,-19.2513302556,-55.2295443234,-26.4301,-1.8917,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ventspils, NW-Latvia',2793,'Ventspils','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 ',1,'True reef','2','10 to 100 m thick','38',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1929,1036,'Plexodictyon irregulare community of Nestor (1999).\nP. irregulare, Plectostroma scaniense, Stromatopora clarkei, Parallelopora ornata, Densastroma cf. sociale, Parallelostroma typicum, Lophiostroma schmidti and Ecclimadictyon aff. robustum.\nExtension of reef belt to Lithuania.\nReef interval from 420-458.3 m in Ventspils drill core.',57,21,-1525130,-465029,'Latvia','Europe',NULL,'',57.4167,21.5833,'WAHR','79814',3.3840003275,-43.2057078546,3.3840003275,-43.2057078546,3.3840003275,-43.2057078546,-11.4127,-3.7747,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lativia',2794,'Ventspils','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 ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1929,1036,'',56,25,-1539918,-201999,'Latvia','Europe',NULL,'',56,25,'','',4.10266646551,-40.9635797124,4.10266646551,-40.9635797124,4.10266646551,-40.9635797124,-11.4945,-1.37847,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mâconnais',2795,'','Jurassic','Middle Jurassic','Bajocian','lower Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',171,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','26','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1934,1935,'16 to 19 genera and 17 to 26 species reported from whole region. Zooxanthellate reef corals prevail.\nLocalities indicated by ref. 1932:\nSt Albain, La Salle, Flacé, Blanot, St. martin Belle Roche, Milly-Lamartine (+Ceyzeriat).',46,4,4471015,1128330,'France','Europe',331,'1932, 1933',46.3333,4.6833,'WAHR','38582',25.2991188436,25.9242947082,25.2991188436,25.9242947082,29.652478733,26.0252050655,35.7371,15.0063,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Franche Comté',2796,'','Jurassic','Middle Jurassic','Bajocian','lower Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',171,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1936,1932,'Coral reefs in Propinquans and Humphriesianum zones\nLocalities of Contini, 1970:\nFortey lès Vesoul, Calmoutier, Arcey, Baume les Dames, Deluz.\nOther Localities of ref. 1932:\nDenney, Echenans, Thesy, Pirey',47,6,4661165,1218583,'France','Europe',331,'1933',47.5833,6.4167,'WAHR','38577',26.830501237,26.7986139574,26.830501237,26.7986139574,31.1571661409,26.9938356593,37.1304,16.2621,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bourgogne',2797,'','Jurassic','Middle Jurassic','Bajocian','lower Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',171,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1937,1938,'see reef 2796\nSeveral localities',47,4,4612028,1070866,'France','Europe',331,'1932, 1933',47.5,4.4667,'WAHR','38563',26.3809302456,25.4117805369,26.3809302456,25.4117805369,30.7484102486,25.5315649541,36.8758,14.6415,'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'),('Duplek, Maribor',2804,'','Neogene','Miocene','Middle Miocene','Badenian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','7','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1941,0,'Coral limestone lense within Lithothamnium limestone.\nDescribed as low-diverstiy fauna. Six species in 4 genera.\nFavia melitae\nFavia macdonaldi\nSolenastraea hyades\nTarbellastraea russoi\nTarbellastraea aquitaniensis\nMussismilia vindoboniensis',46,15,5949380,1288900,'Slovenia','Europe',328,'',46.5,15.7167,'WAHR','22969',45.4423467399,12.5422752122,45.4413258372,12.5411334055,44.9305866507,13.2853990645,45.8637,15.2619,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Central Maldives',2805,'','Paleogene','Oligocene','Rupelian','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',31,2,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'Reef data from seismic interpretation. Seismic unit P1.\nOligocene reef tract bordering an interior basin and an open ocean ramp system towards the open Indian Ocean.\n',4,73,-1191454,7007265,'Maldives','Asia',NULL,'',4.0333,73.3333,'','',-6.00480218441,64.0871420282,-6.00480218441,64.0871420282,4.0333,73.3333,-6.0275,65.087,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Northern Maldives',2806,'','Paleogene','Oligocene','Rupelian','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',31,2,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','2805',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'See reef 2805',4,73,-1080031,7021955,'Maldives','Asia',NULL,'',4.8333,73.1667,'','',-5.18950293306,64.0332526143,-5.18950293306,64.0332526143,4.8333,73.1667,-5.21164,65.1315,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Southern Maldives',2807,'','Paleogene','Oligocene','Rupelian','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',31,2,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','2805',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'See reef 2805',3,73,-1299522,6954177,'Maldives','Asia',NULL,'',3.1667,73.1667,'','',-6.83993780562,63.8004019415,-6.83993780562,63.8004019415,3.1667,73.1667,-6.82251,64.7017,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Northern Maldives II',2808,'','Paleogene','Oligocene','Rupelian','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',31,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'See reef 2805',5,73,-998094,7065489,'Maldives','Asia',NULL,'',5.5,73.3333,'','',-4.55218798662,64.2907940724,-4.55218798662,64.2907940724,5.5,73.3333,-4.60952,65.4636,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Central Maldives',2809,'','Paleogene','Oligocene','Chattian','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',26,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'Seismic interval P2. Reefs covered by Early Miocene pelagic limestone.\nSee reef 2805 for further remarks',4,73,-543364,7420416,'Maldives','Asia',NULL,'',4.0333,73.3333,'','',-4.18828865465,65.5770202854,-4.18828865465,65.5770202854,4.0333,73.3333,-4.20469,66.8924,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Northern Maldives',2810,'','Paleogene','Oligocene','Chattian','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',26,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','2809',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'See reefs 2805 and 2809',4,73,-431451,7421046,'Maldives','Asia',NULL,'',4.8333,73.1667,'','',-3.37696115346,65.4801806183,-3.37696115346,65.4801806183,4.8333,73.1667,-3.38768,66.9017,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Southern Maldives',2811,'','Paleogene','Oligocene','Chattian','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',26,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','2809',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'See reefs 2805 and 2809',3,73,-656673,7381065,'Maldives','Asia',NULL,'',3.1667,73.1667,'','',-5.03733982775,65.3359180092,-5.03733982775,65.3359180092,3.1667,73.1667,-5.01542,66.5429,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Northern Maldives',2812,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'Seismic interpretation. N2 seismic interval, starting above base of Middle Miocene\nInterpeted as platform margin reefs.\nProgradation towards basin.',5,72,59084,7687094,'Maldives','Asia',NULL,'',5.3333,72.9167,'','',1.10225528976,68.7485693849,1.10225528976,68.7485693849,5.3333,72.9167,0.875425,70.1232,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Central Maldives',2813,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'See reef 2812',4,72,-121103,7659546,'Maldives','Asia',NULL,'',4,72.8333,'','',-0.227371773355,68.6193730731,-0.227371773355,68.6193730731,4,72.8333,-0.435002,69.8636,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Southern Maldives',2814,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'See reef 2812',2,72,-292666,7649184,'Maldives','Asia',NULL,'',2.75,72.9167,'','',-1.47950357766,68.6593422926,-1.47950357766,68.6593422926,2.75,72.9167,-1.68498,69.7799,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Southern Maldives II',2815,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'See reef 2812',3,73,-212911,7733169,'Maldives','Asia',NULL,'',3.4167,73.5833,'','',-0.835897148032,69.3474722392,-0.835897148032,69.3474722392,3.4167,73.5833,-1.11229,70.5282,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Northern Maldives II',2816,'','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',13,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'See reef 2812',4,73,-65381,7749209,'Maldives','Asia',NULL,'',4.5,73.5833,'','',0.246788456251,69.3839530157,0.246788456251,69.3839530157,4.5,73.5833,-0.0384652,70.6712,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Northern Maldives',2817,'','Neogene',NULL,NULL,'Miocene-Pliocene',2.60,20.00,32,'Tortonian - Gelasian',6,15,'Middle Miocene (Langhian, 14.9 Ma)',5,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'',4,73,333561,8010324,'Maldives','Asia',NULL,'',4.5,73.5833,'','',1.11602660041,70.2267752219,1.11602660041,70.2267752219,4.5,73.5833,0.756922,71.3335,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Southern Maldives',2818,'','Neogene',NULL,NULL,'Miocene-Pliocene',2.60,20.00,32,'Tortonian - Gelasian',6,15,'Middle Miocene (Langhian, 14.9 Ma)',5,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'',3,73,185231,8006411,'Maldives','Asia',NULL,'',3.4167,73.5833,'','',0.033331212349,70.1905846512,0.033331212349,70.1905846512,3.4167,73.5833,-0.319056,71.2078,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Southern Maldives II',2819,'','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'',2,72,99250,7929178,'Maldives','Asia',NULL,'',2.75,72.9167,'','',0.27356619291,70.4054904351,0.27356619291,70.4054904351,2.75,72.9167,-0.0110306,71.1794,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Central Maldives',2820,'','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',7,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1928,0,'',4,72,271079,7925535,'Maldives','Asia',NULL,'',4,72.8333,'','',1.52531608776,70.3549522558,1.52531608776,70.3549522558,4,72.8333,1.2413,71.2124,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Bandung, Java',2821,'Rajamandala','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',1,'True reef','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','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1943,1944,'Abstract ref. 1943:\nOutcrops of the Rajamandala Formation limestone near Bandung offer an excellent opportunity to study the facies -relationships of an Early Tertiary reef, which may serve as a model for Tertiary reef exploration in Indonesia. The limestones are exposed along quarries and natural Outcrops along the road from Bandung to Jakarta. These limestones with thicknesses of approximately 600 meters are dipping 40 to 60 degrees toward the south and are involved in asymmetric folding and thrusting towards the north. \nAlong its ENE-WSW trending strike the limestone exhibits a graded granular limestone facies representing turbidites at the toe of the basin-slope facies, a foraminiferal algal facies with rudstone facies representing a fore-reef facies, a coral-algal baffiestone to boundstone facies (locally quarried and slabbe as commercial marble), representing, reef ramparts, and a possible milliolid limestone facies with isolated patch reefs, representing the lagoonal back reef facies. \n\n\nCORAL DEBRIS RUDSTONE FACIES: \nThis facies consists of angular fragments of corals and other limestones, mostly dark grey, embedded in a limemud matrix, which is generally lighter in color. Fragments, poorly sorted, vary in size up to 30 cm. Matrix contains considerable amounts of large foraminifera mainly Lepidocyclina. This facies represents talus-slope debris of coral fragments from the main reef\n\nCORAL BOUNDSTONE FACIES: \n\n\nIn general this consists of corals in growth position in which the spaces among the coral framework are filled up with muds containing coral debris, large foraminifera, etc. often bound with encrusting red algae. The rocks are light colored and are usually dense, massive, nonbedded to poorly bedded, with no primary porosity. The following sub-facies can be recognized based on the type of corals: \n\n\nMassive Head Corals Boundstone: This facies consists mainly of colonies of massive head corals, such as brain-corals, Meandrina etc. with encrusting red algae. A pack-stone facies, rich in foraminifera, is common in between the coral colonies. Worm tubes are very common in this facies, as well as large shells of gastropods and lamelli-branchia. These rocks are very massive, dense and usually white in color. The carbonates are very pure, containing over 95% calcium carbonate. Recrystallization is fairly. This rock is polished into commercial marble, common. This facies presumably represents the reef crest or reef flat. \n\n\nPlaty Coral Boundstone: This facies consists of platy corals, which are aligned parallel to bedding. Within the framework of these boundstone are pockets of foraminiferal packstone to wackestone. These rocks are mostly massive and poorly bedded, but occasionally show wavy bedding. This facies presumably represents the deeper environment of the reef front. \n\nBranching Coral Bafflestone: This facies consists primarily of branching corals, mostly in growth position, some as broken fragments \' , embedded in a limemud matrix. Typical corals are Porites, Acropora, -RhabdophyIlia etc. (Gerth, 1933). Branching coral facies presumably represent sub-wayebase environments of the reef front. \n\n\nThese three sub-facies are usually intermixed together and cannot be differentiated, but often the platy coral boundstone and especially branching corals bafflestone form\' definite facies development, such as G. Pawon and G. Manik. \n\n\nREEF DEPOSITIONAL ENVIRONMENTS \n\n\nMeasured sections at several localities and their lateral correlations indicates that depositional environments of the reef related sediments can be identified, based on the lateral facies developments, as well as each individual facies. The following depositional environments can be recognized: \n\n\n',-6,107,-941152,12312821,'Indonesia','Asia',614,'',-6.9,107.4,'','',-4.74544285689,104.876399843,-4.74544285689,104.876399843,-7.58233199822,107.830019562,-6.95843,112.203,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('NE-Evvoia',2822,'Xiron','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian-Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',150,2,'0','Outcropping reef ',1,'True reef','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','2b','Margin of deep basins (shelf margin)',NULL,NULL,'4','Stromatoporoids','1','Corals','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'20','30','50',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1945,0,'Only reef debris limestone preserved.\nKimmerdigian-early Tithonian.\nCladocoropsis limestone\nCladocoropsis mirabilis Felix (hydrozoan) and other frame builders (Actinostromaria, Actinostromarianina, Parastromatopora, Milleporidium) and encrusting algae.\nIntergranular pores occluded by organic crusts, fibrous cement and silty-micritic sediment. Up to 20 m thick debris beds. ',38,23,2677136,2150868,'Greece','Europe',338,'',38.9167,23.4167,'WAHR','68163',6.32287408618,21.9055009826,6.32287408618,21.9055009826,13.4436080539,26.3488323625,22.4173,22.9114,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('NE-Evvoia',2823,'Pantokrator','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',209,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1945,0,'Intraformational reef breccias.\nNo further description available',39,23,1410126,2192777,'Greece','Europe',338,'',39,23.3667,'','',9.22329515877,30.3894916952,9.04692910495,30.4375128169,7.82817131926,23.4211329338,14.5586,18.8181,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Nauru Basin, DSDP Leg 61, West Pacific',2824,'','Paleogene','Oligocene','Chattian','Late Oligocene',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',27,2,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'1','Corals','4','Stromatoporoids','63','Corals - hydrozoans',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1946,0,'Reworked skeletal debris dated as late Oligocene based on larger foraminifera.\r\nReef builders: Corals (Porites, Actinastrea?, Seriatopora) Octocorallia (Alcyonoceans), hydrozoans (Axopora). ',7,-165,343792,-16911778,'Pacific','Pacific',NULL,'',7.2361,-165.0306,'',NULL,1.26122307115,-147.506372755,1.26122307115,-147.506372755,7.2361,-165.0306,0.573993,-149.332,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Line Islands, DSDP Leg 17, Site 165, Pacific',2825,'','Cretaceous','Upper Cretaceous','Campanian','Campanian-Maastrichtian',66.00,83.60,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',70,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'5','Rudists','5','Rudists',NULL,NULL,NULL,NULL,'60','40','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',1947,0,'Displaced reef faunas mentioned. \nLarger forams and broken and abraded skeletal fragments of mollusks (including rudists), echinoids and bryozoans within volcaniclastic strata',8,-164,-490455,-14944185,'Pacific','Pacific',NULL,'',8.1764,-164.8583,'','',-14.4965836316,-118.596200042,-14.4965836316,-118.596200042,8.1764,-164.8583,-6.34351,-130.047,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Line Islands, DSDP Leg 33, Site 315',2826,'','Cretaceous','Upper Cretaceous','Campanian','Campanian-Maastrichtian',66.00,83.60,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',70,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'2','Algae','5','Rudists',NULL,NULL,'1','Red algae','15','0','85',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',1948,1947,'Diverse fauna including larger forams (Pseuorbitoides, Asterorbis, Sulcoperculina), coralline algae and rudist fragments',4,-158,-997096,-14167432,'Kiribati','Oceania',NULL,'',4.1708,-158.525,'','',-17.9973917278,-111.731151551,-17.9973917278,-111.731151551,4.1708,-158.525,-11.2796,-118.699,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Line Islands, DSDP Leg 33, Site 316',2827,'','Cretaceous','Upper Cretaceous','Campanian','Campanian-Maastrichtian',66.00,83.60,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',70,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'5','Rudists','5','Rudists',NULL,NULL,NULL,NULL,'60','20','20',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',1948,1947,'see reef 2826',0,-157,-1541158,-13885170,'Kiribati','Oceania',NULL,'',0.0903,-157.1278,'','',-21.9050489314,-109.789467235,-21.9050489314,-109.789467235,0.0903,-157.1278,-15.1587,-116.763,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Line Islands, DSDP Leg 33, Site 318, Pacific',2828,'','Paleogene','Eocene','Priabonian','late Eocene',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',36,2,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1948,0,'Common coral fragments in Core 319-19 together with coralline algae. \nOnly larger foraminifera described in detail.',-14,-146,-2872769,-13285296,'Pacific','Pacific',NULL,'',-14.8222,-146.8583,'','',-24.3397074935,-122.252922775,-24.3397074935,-122.252922775,-14.8222,-146.8583,-22.413,-124.707,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Finlay Mountains, Texas',2829,'Wilkie Ranch','Permian','Cisuralian','Kungurian','Leonardian',270.60,280.00,15,'Sakmarian - Kungurian',277,275,'Early Permian (late Kungurian, 275 Ma)',273,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'9','Tubiphytes','13','Echinoderms','90','Crinoids - Tubiphytes',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1950,0,'3 m thick and 13 wide Tubiphytes-Crinoid bioherms.\nBuildup growth began with the hydrodynamic accumulation of a bioclastic pile that was colonized by a crinoid thicket, which then diversified with abundant brachiopods, bryozoans and solitary rugose corals, and finally matured into boundstones composed of Tubiphytes, laminar algae, and large crinoids.   ',31,-105,441693,-3855665,'United States','North America',101,'',31.25,-105.6167,'','',1.35715296571,-35.4931694636,1.35715296571,-35.4931694636,-0.649321086035,-41.8814401767,4.61834,-33.7275,'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'),('Provence',2831,'','Cretaceous','Lower Cretaceous','Valanginian','lower Valanginian',132.90,139.80,22,'late Tithonian - early Valanginian',141,135,'Early Cretaceous (Valanginian, 136.4 Ma)',139,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'4','Stromatoporoids','1','Corals','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'20','40','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1952,0,'Stromatoporoid-chaetetid biostromes with less common scleractinians ',43,6,4013700,799770,'France','Europe',331,'',43.75,6,'WAHR','74564',25.3431836852,22.3064874393,25.3431836852,22.3064874393,30.3489759176,22.0696064486,34.6522,15.2397,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dietrichshorn, Salzburg',2832,'Lärchberg','Jurassic','Upper Jurassic','Tithonian','Tithonian-Berriasian',139.80,152.10,22,'late Tithonian - early Valanginian',141,145,'Jurassic/Cretaceous Boundary (145 Ma)',145,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','4',NULL,NULL,NULL,'3','More than 100 m','120',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','4','Stromatoporoids','4','Stromatoporoids','75','Stromatoporoids or chaetetids only',NULL,NULL,'50','10','40',0,'no',0,'no','1','Less than 6 reef building species','1','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1953,0,'Monospecific, complex, massive, nodular hydrozoan (Milleporidium) biostrome, up to 4 m thick and more than 120 m in lateral extent\nLerchkogel Member',47,12,3991492,1483958,'Austria','Europe',301,'',47.6167,12.6667,'WAHR','68260',22.7004365493,27.277344012,22.7004365493,27.277344012,23.4909193322,27.4196477135,33.975,21.5622,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Var, Provence',2833,'Calcaires Blancs','Jurassic','Upper Jurassic','Tithonian','Tithonian-Berriasian',139.80,152.10,22,'late Tithonian - early Valanginian',141,145,'Jurassic/Cretaceous Boundary (145 Ma)',145,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','60','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1954,0,'Massive-nodular coral-stromatoporoid bioherms with calcareous algae developed on a tidal-influenced carbonate platform rim',43,6,3990556,835669,'France','Europe',331,'',43.5,6.3333,'FALSCH','0',24.0478454141,22.4052563087,24.0478454141,22.4052563087,29.5897974107,23.4140403532,34.9409,15.0973,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Transsylvania, South Carpathians',2834,'','Cretaceous','Lower Cretaceous','Valanginian','Valanginian',132.90,139.80,23,'late Valanginian - early Aptian',126,135,'Early Cretaceous (Valanginian, 136.4 Ma)',138,1,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','2','Algae','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','1','Red algae','10','10','80',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1955,0,'Massive-nodular stromatoporoids (mainly Actinostromaria) together with thick crustose Lithocodium bindstones mark the outer platform, and biostromal stromatoporoids (mainly Parastromatopora) occur in the large lagoonal facies',45,24,3205801,2367388,'Romania','Europe',348,'',45.5,24.6667,'','',30.6702349056,36.2119856578,30.6702349056,36.2119856578,22.1395669114,30.6460161079,25.4929,28.3888,'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'),('Tafilalt Basin, Anti Atlas',2839,'','Carboniferous','Mississippian','Visean','late Asbian-Brigantian',331.00,338.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',332,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','30',NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','2','Below fair weather wave base','13','Echinoderms','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1962,0,'Complex agglomeration of Lower Carboniferous mud mounds.\nMounds covering an area of 440 km2.\nMaximum height 30 m, Basal diameter up to 300 m.\n4 types:\n1-2: crinoidal wacke-packstones with or without Stromatactis\n3. Allochthonous\n4. Biodetrital grainstone mounds\nMound growth from texanus-zone to bilineatus-zone (Asbian-Brigantian)',30,-7,-2606505,-342032,'Morocco','Africa',714,'',30,-7.5,'WAHR','76759',-44.9615402276,-19.5823247052,-41.0562419604,-16.3945817887,-24.3567839215,-31.3913734663,-21.1657,-4.03378,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Akasaka',2840,'','Permian','Guadalupian','Roadian','Kubergandian',268.80,272.30,15,'Sakmarian - Kungurian',277,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',269,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','13','Echinoderms','6','Calcisponges','86','Microbes - sponges - crinoids',NULL,NULL,'0','30','70',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1963,0,'Crinoid-calcisponge-microbial mounds in a shallow open marine shelf\nParafusulina granum-avenae zone',35,136,1946284,11173027,'Japan','Asia',625,'',35.3667,136.5667,'','',8.29621526603,133.396645624,8.29621526603,133.396645624,20.7264322687,106.589428653,14.7585,115.894,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Akasaka',2841,'','Permian','Guadalupian','Capitanian','Midian',259.80,265.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',262,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1963,0,'Coral patch-reefs, related back-reef and shoals in the Yabeina globosa Zone.',35,136,1946284,11173027,'Japan','Asia',625,'',35.3667,136.5667,'','',2.20886967527,130.519004371,2.20886967527,130.519004371,20.3708591603,115.379343816,21.6087,114.997,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maestrazgo and Aliaga-Penyagolosa Basins',2842,'Llacova','Cretaceous','Lower Cretaceous','Hauterivian','upper Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',131,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m','20',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','20','Corals - forams','1','Red algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','12','1','Constructor guild','2','Intensive','1','Present','2','Medium zonation',NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1965,2412,'Paucispecific crustose microsolenid biostromes with a remarkable amount of encrusting algae and adherent foraminifera (about 10 m in extension) colonized the outer platform margin . In places they are replaced by microsolenid-dominated patch reefs of biohermal character (up to 7 m in diameter) built by crustose and ramose coral morphotypes.\nThe coral bioherms are overlain by requieniid rudist beds in micritic matrix.\nUpper reef of ref. 2412 and 2554',40,0,3219968,245256,'Spain','Europe',304,'2554',40.4667,0.05,'WAHR','56708',22.5179961282,13.3284206748,22.5179961282,13.3284206748,26.8932635879,10.007710246,30.6133,9.59678,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dündarli, Kayseri',2843,'','Paleogene','Paleocene','Danian','Danian',61.60,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',64,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1966,0,'Only coral-algal limestone described',38,35,3738790,3344721,'Turkey','Asia',522,'',38.0889,35.2056,'','',35.1540679798,34.2165131892,35.1540679798,34.2165131892,31.8551492487,30.1081225361,27.0035,31.0703,'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'),('Wairaki Hills, western Southland',2846,'Mangarewa','Permian','Cisuralian','Kungurian','Kazanian',268.80,272.30,15,'Sakmarian - Kungurian',277,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',268,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform',NULL,NULL,NULL,NULL,'1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',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,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1970,0,'Coral-bryozoan bioherm in Upper Coral Bluff Limestone Member. Molluscan shellbeds in limy siltstone to mudstone and brachiopod shellbeds in fine limy tuffaceous sandstone.',-45,167,-3993911,-17563181,'New Zealand','Oceania',806,'',-45.75,167.75,'',NULL,-73.2175522816,-149.477470544,-73.2175522816,-149.477470544,-75.5124012792,166.853289074,-73.1048,-157.889,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wairaki Hills, western Southland',2847,'Hawtel','Permian','Lopingian','Wuchiapingian','Tatarian',254.10,259.80,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',260,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,2,'Cold - water','1','Intrashelf/ Intraplatform',NULL,NULL,'1','Above fair weather wave base','1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',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',1970,0,'Hilton Limestone Member\r\nCoral-bryozoan bioherms in pure to sandy limestone- Primary tuff with fine to coarse sandstone. Fine pebble to massive boulder conglomerate at base',-45,167,-3993911,-17563181,'New Zealand','Oceania',806,'',-45.75,167.75,'',NULL,-84.4455104413,-133.881237002,-84.460246768,-133.869907841,-81.6548906072,163.595264797,-74.9681,-174.711,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Copetdag, Turkmenia',2848,'','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 ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',1974,0,'Late Oxfordian-early Kimmeridgian barrier reef(?).\nLagoonal laminated micrites with abundant brachiopods. ',38,57,5019888,5465114,'Turkmenistan','Asia',NULL,'',38,57.5,'WAHR','96014',33.2934515408,66.8431275943,33.2934515408,66.8431275943,36.0404734722,70.825972312,34.4693,62.822,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Great Balkhan, Turkmenia',2849,'Urumil\'dshanskaya','Jurassic','Middle Jurassic','Callovian','Callovian-Oxfordian',157.30,166.10,21,'late Bathonian - early Tithonian',151,165,'Middle Jurassic (Callovian, 164.8 Ma)',161,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1974,2114,'Barrier(?) reefs in an onshore setting?',39,54,5124846,5074282,'Turkmenistan','Asia',NULL,'',39.8333,54.4167,'','',33.3285907418,64.1404061643,33.3285907418,64.1404061643,37.3988011626,68.0793592496,36.098,59.8758,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Gipsily, Great Balkhan, Turkmenia',2850,'Tashlyderinskij','Jurassic','Upper Jurassic','Oxfordian','upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',156,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','70',NULL,NULL,NULL,NULL,NULL,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',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1974,2114,'Upper reefal formation (see 2849 for lower part).\nRare brachiopods as compared to lower portion.\n',39,54,5124846,5074282,'Turkmenistan','Asia',NULL,'',39.8333,54.4167,'','',33.4528582378,63.8473629295,33.4528582378,63.8473629295,37.3330536906,67.8286313338,35.9953,59.789,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Kugitang',2851,'','Jurassic','Middle Jurassic','Callovian','middle-upper Callovian',163.50,166.10,21,'late Bathonian - early Tithonian',151,165,'Middle Jurassic (Callovian, 164.8 Ma)',162,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1974,2836,'Lowermost reefal interval in Kugitang.\nReef facies associated with endemic brachiopod fauna. \nCoordinates updated May 2010',37,66,5427560,6154017,'Uzbekistan','Asia',301,'',37.9333,66.7667,'WAHR','91828',-17.7466450739,41.2116317694,36.3500873204,76.0408688519,39.870017859,80.8319868997,36.7032,72.2698,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Daluokeng, Gaofeng, Cili Co., Hunan',2852,'Daluokeng','Permian','Lopingian','Changhsingian','lower Changhsingian',253.00,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',253,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'6','Calcisponges','2','Algae','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','4','Others','0','90','10',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1975,2128,'lower Daluokeng Fm.:\nGreyish white massive sponge-algal-microbial framestone, intercalated lenticular beds of wackestones, shell beds containing corals, sponges, forams, calcareous algae and the brachiopods Uncinunellina multicostioidea, Spirigerell ovalioides, S. shuizhtangensis, Ladoliplica zigzagiformis, L. platformia.\nBrachiopds much rarer in underlying coral limestones of the Xiamidong Fm.\n\nReef overlain by thick-bedded wackestones with intraclasts (Member 2) and oolitic limestone (Member 3).\n\nAbstract ref. 2128:\nBafflestones, framestones as well as bindstones are described. According to the function of reef-building, the organisms are classified to frame-builder, bind organisms and clastic-builder, in which main frame-builders are Sphictozoa, Inozoa, Tabulozoa and Hydrozoan, the bind organisms are Archaeolithiporella, Tubiphytes, Tabulozoa and blue-green algae. Four developing stages of the reefs have been distinguished. ',28,110,-340295,9208039,'China','Asia',602,'',28.6333,110.1833,'WAHR','31420',-12.0607010539,108.662536522,-12.3439365792,108.399622007,8.64232740124,127.71727642,8.58499,99.1524,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Blue Pool Bay, Wales',2853,'Hunts Bay Oolite','Carboniferous','Mississippian','Visean','early Asbian',338.00,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',335,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','10',NULL,NULL,NULL,'2','10 - 100 m','25',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','15','1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1976,0,'Abstract of ref. 1976:\nBuildups with a rigid coral framework are generally rare in Lower Carboniferous time. An exception was found in the Hunts Bay\nOolite-Formation at Blue Pool Bay (Gower Peninsula). This bioherm is intercalated in well-bedded oolitic limestones. It is about 25 meters in\nwidth and rises up to 10 meters in thickness. The coral association indicates an Asbian age of the bioherm. The core of the structure consists of\nlarge massive colonies of Lithostrotion and a small number of dendroid colonies (Siphonodendron and Syringopora). Most of the corals are\npreserved in living position. The density of the colonies is high, in many cases they grow upon eachother. Dendroid corals become more\ncommon in the outer core. An increase of colonies, which are upside-down orientated, together with broken colonies and coarse debris\ndescribe the facies of the flanks. The general decrease of the amount of corals and the gradual increase of fragments of colonies in bioclastic\nrudstones to wackestones at the top of the structure characterize the end of the biohermal development. \n\nDue to the appearance of a coral framework and its thickness, the bioherm is wave resistant. It is described as the first ecological coral-reef of\nthe Lower Carboniferous of South Wales. ',51,-4,-746444,368086,'United Kingdom','Europe',331,'',51.55,-4.2,'WAHR','36674',-32.3330570757,-10.0005209563,-32.525838131,-10.1296386094,-6.33784397876,-36.1979677317,-8.69507,0.068657,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cap Guir, Agadir, Maghreb',2854,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','13',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'5','80','15',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1972,2832,'Peninsula north of Agadir\n\nCoral reef with 70% massive and rare branching corals. Other reef builders are stromatoporoids, bryozoans, mollusks and microbialites (laminated stromatolites and peloidal thrombolites) and microencrusters (Bacinella, Tubiphytes, Lithocodium, encrusting forams), rare solenoporeaceans.\nMicrobialites approaching 25% or reef volume.',30,-9,2869215,-993275,'Morocco','Africa',714,'',30.6667,-9.85,'WAHR','68080',16.0501716355,-0.86126011956,16.0501716355,-0.86126011956,22.1247739267,-2.13937020859,28.2336,-7.44124,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cap Guir, Agadir, Maghreb',2855,'','Jurassic','Upper Jurassic','Kimmeridgian','lower Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',154,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','16',NULL,NULL,NULL,'3','More than 100 m','200',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'4','Stromatoporoids','1','Corals','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','50','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present','3','Pronounced zonation',NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1972,2832,'reef mostly built by stromatoporoids (30%), corals (20%) (Stylina tubilifera, Thecosmilia) and chaetetids, rare mollusks and bryozoans. \nAbundant internal reef debris (50%).\n\nMicrobialites especially abundant in colonisation stage approaching 40%. Stromatolites associated with abundant microencrusters: Tubiphytes, Bacinella and Lithocodium. \nVery pronounced succession with stabilisation, colonisation, diversification and domination indicated.',30,-9,2859195,-988459,'Morocco','Africa',714,'',30.6167,-9.7667,'WAHR','68081',15.6547652115,-1.23012401914,15.6547652115,-1.23012401914,21.7825808179,-2.43001703707,27.7539,-6.8426,'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'),('Novonikolayev Oil Field, Dnjeper',2857,'','Carboniferous','Mississippian','Visean','Tournaisian-Early Visean',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',345,2,'1','Seismic data available ',NULL,NULL,'3','101-500 m thick','180',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',2,'Actual reservoir',1980,0,'Several oil-gas bearing reefs in Dniepr-Donets depression mentioned in text, but exact localities not provided:\nBogatoy, Kampan, Machekh, Novonikoleyev, Selyukhov, Belichev.\nData for only two localities found.',48,34,-430930,2426973,'Ukraine','Europe',301,'',48.55,34.35,'','',-30.6306719264,14.6390885159,-30.6306719264,14.6390885159,10.1402676539,-33.8063176593,-4.10862,21.1705,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Bogatoy Oil Field, Dnjeper',2858,'','Carboniferous','Mississippian','Visean','Tournaisian-Early Visean',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',345,2,'1','Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100','2857',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',2,'Actual reservoir',1980,0,'See reef 2857',48,35,-317503,2456911,'Ukraine','Europe',301,'',48.95,35.5167,'','',-29.8056452975,14.9475985358,-29.8056452975,14.9475985358,11.0001421104,-33.693260152,-3.268,21.3833,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Unur, Inner Mongolia',2859,'Unur','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 ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'1','Corals','14','Brachiopods',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1694,0,'Fm. thickness = 117 m.\nReefs with tabulate and rugose corals and brachiopods. Terrigenous clastic sediments interfinger with reef margins.',49,122,7913836,6399710,'China','Asia',602,'',49.25,122.5,'','',71.7801367875,97.3513998941,71.7801367875,97.3513998941,73.6942123646,-56.7875734453,38.837,54.8559,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Inangahua Outlier, Reefton',2860,'Lankey Limestone','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 ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species','9','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1983,1984,'Buller Terrane.\n\nHorizons of bio-rudite in places exceptionally rich in largely transported coral and stromatoporoid colonies. \nNear coastal environment.\n\nAbstract of ref. 2236:\nStudy of 35 systematically collected and 10 semi-random samples (about 100 cm(2) each) from one outcrop of the Lankey Limestone (Emsian) near Reefton, New Zealand indicates that it is a reef framestone built by tabulate (4? spp.) and clonal rugose (one sp.) corals, two species of stromatoporoids, a few bryozoans (2? spp.) and crinoids. The guild structure of the reef community and data on skeleton orientation and growth direction further indicate that there was relatively minor biostratonomic alteration of the original community. Skeletons are either in growth position or tipped, toppled or even overturned, but they have remained in situ. Other clone-rich Lankey Limestone outcrops in the Reefton area support the notion of an upper shelf reef system and stratigraphic and sedimentologic data suggest that it was located near the Gondwana margin at a paleolatitude of about 35 degreesS.',-42,171,-4045804,17538431,'New Zealand','Oceania',806,'1985, 2236',-42.1167,171.8667,'WAHR','25785',-37.7101496951,139.021778518,-37.7101496951,139.021778518,-46.3688952794,-170.580377927,-22.0626,-177.164,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maloichskaya, West Siberia',2861,'unknown','Silurian','Pridoli','Pridoli','Pridoli-Lochkovian',410.80,423.00,8,'middle Pridolian - middle Pragian',412,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',416,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,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',1986,0,'Brecciaform limestones with fragments of \'algae\' and stromatoporoids.\r\nMany reef builders in common with Nyurolka basin:\r\nTabulate corals:\r\nRiphaeolitidae (Riphaelites and Echyroporfa)\r\nFavosites clarus\r\n\r\nRugose corals:\r\nDendrostella bilaterale\r\nD. vulgaris\r\n\r\nand many stromatoporoids',57,79,5118857,3161130,'Russia','Asia',624,'',57,79,'WAHR','81052',52.3832638784,-31.5274458917,52.3832638784,-31.5274458917,38.0582790869,4.93546041665,27.9358,10.6697,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-02-07 16:15:34'),('Gornoi Altai Mts., Siberia',2862,'','Silurian','Pridoli','Pridoli','Ludlow-Gedinnian',410.80,427.40,NULL,NULL,NULL,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',419,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','2521',0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','3','Microbes','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',1986,0,'',51,83,4691099,952168,'Russia','Asia',624,'',51,83,'','',57.1914560333,-38.289953222,57.1914560333,-38.289953222,35.580580087,12.2690182511,34.0503,12.933,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gornoi Altai Mts., Siberia',2863,'unknown','Silurian','Pridoli','Pridoli','Ludlow-Gedinnian',410.80,427.40,NULL,NULL,NULL,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',417,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','2521',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1986,0,NULL,51,83,5870671,3107358,'Russia','Asia',624,'',51.25,83,'',NULL,56.9476496211,-38.3916849346,56.9476496211,-38.3916849346,35.7226116374,12.0158290157,33.8808,12.7115,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Eisriesenwelt, Tennengebirge',4071,'Dachstein','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','5','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','1','Corals','3','Microbes','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2930,NULL,'',NULL,NULL,NULL,NULL,'Austria','Europe',NULL,NULL,47.502222,13.190972,NULL,NULL,20.4101035487,31.7157899005,20.2293451534,31.8018853646,21.9625720362,17.0115043296,25.656,16.7845,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gornoi Altai Mts., Siberia',2864,'unknown','Silurian','Pridoli','Pridoli','Ludlow-Gedinnian',410.80,427.40,NULL,NULL,NULL,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',417,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','2521',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1986,0,NULL,50,84,6005825,3013414,'Russia','Asia',624,'',50.5,84.5,'',NULL,57.8719586788,-39.8346692856,57.8719586788,-39.8346692856,36.0802925898,13.4397694162,35.0838,12.5839,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Salair-Altai, W Siberia',2865,'','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 ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'400','2548',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more 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',1986,0,'Stromatoporoids very diverse:\nActinostroma salairica \nGerronostroma batschatensis \nAmphipora blochini\nA. pinguis\nStachyodes singularia\nStriatopora schandiensis\nAlveolites multispinosus\nCladopora microcellulata\nCoenites bulvankerae\nSyringopora yavorskyi',53,85,6400046,3230953,'Russia','Asia',624,'',53,85.3333,'WAHR','81054',51.0189706811,25.5812829415,51.0189706811,25.5812829415,43.1699252185,-1.4320653247,31.5336,19.8239,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Salair-Altai, W Siberia',2866,'','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 ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'400','2548',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'4','Stromatoporoids','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1986,0,'See reefs 2865 and 2548',51,84,6498398,3370563,'Russia','Asia',624,'',51.5,84.5,'','',60.4363043107,23.9378073151,60.4363043107,23.9378073151,42.6028207235,4.61496617486,31.7306,20.6018,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('SW Kuznesk Basin',2867,'','Devonian','Middle Devonian','Givetian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',385,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1600','1048',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1986,680,'See reef 1036',52,80,4793034,3280782,'Russia','Asia',624,'',52,80.25,'','',36.8753798658,34.3721282525,36.8753798658,34.3721282525,36.7450868325,0.953591320222,29.4012,23.839,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('SW Altai, Kazachstan',2868,'','Devonian','Middle Devonian','Givetian','Givetian-Frasnian',372.20,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',385,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1600','1048',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1986,680,'See reef 1036',49,84,5183884,3374731,'Kazakhstan','Asia',301,'',49.5,84,'','',40.3084729186,34.7501077983,40.3084729186,34.7501077983,39.4057963239,3.7357983535,32.5385,25.5013,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Manchester Plateau, central Jamaica',2869,'Newport','Paleogene','Oligocene','Chattian','latest Oligocene',23.00,25.00,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',23,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','31','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1993,2574,'About 20 genera and >30 coral species\n5-8 M thick.\n\nAge was Lower Miocene. Revised to latest Oligocene in ref. 2574\n\nAbstract of ref. 1993:\nDuring the middle Tertiary, the island of Jamaica was part of a large system of shallow carbonate platforms extending northeast along the Nicaraguan Rise.\nAlthough these platforms undoubtedly supported a rich fauna of marine benthos, the coral communities of this region are poorly known. New exposures in Jamaica,\nhowever, provide a clearer picture of the development of these Tertiary reefs, especially those spanning the Oligocene/Miocene transition, a time of significant\ntaxonomic turnover in Caribbean corals. \n\nRecent bauxite mining on the Manchester Plateau of central Jamaica exposed well-developed (5 - 8 m thick) patch reefs in the Lower Miocene of the Newport\nFormation. Sections through these coral build-ups have been logged and extensively sampled. This material was compared with new data from similarly exposed\nreefs in the Upper Oligocene Brown\'s Town Formation of north central Jamaica. Cluster analysis and ordination of coral occurrences has revealed similarities as well\nas distinct differences between Oligocene and Miocene assemblages.\n\nBoth units contain coral assemblages dominated by massive, branching, or plate-shaped colonies. Coral diversity is also roughly the same in each formation\n(approximately 20 genera and >30 species). There is some turnover of species between the late Oligocene and early Miocene, but perhaps the most significant\ndifference between the sampled assemblages is a change in the relative abundance of certain key taxa. Antiguastrea cellulosa, for instance, is the dominant massive coral in the Upper Oligocene assemblages but is much less common in Lower Miocene faunas.\n\nEcologically and sedimentologically, there appears to be little difference between the coral build-ups in the Brown\'s Town and Newport Formations. This suggests\nthat, in contrast to some other regions in the Caribbean, patch reef communities in Jamaica thrived throughout the Oligocene/Miocene transition. Changes in dominant\ncoral taxa, however, could suggest a complex shift in community structure during this turnover interval. ',18,-77,2464316,-8304666,'Jamaica','North America',222,'',18.0833,-77.25,'WAHR','69725',16.0396784636,-76.0140345072,16.1873404068,-76.0889332824,19.5903852108,-75.3396814691,17.6694,-75.9209,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('North central Jamaica',2870,'Brown\'s Town','Paleogene','Oligocene','Chattian','Upper Oligocene',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',27,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','31','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1993,0,'No evidence for the Oligocene/Miocene reef crisis in Jamaica.',18,-77,2497931,-8296526,'Jamaica','North America',222,'',18.3333,-77.25,'WAHR','69724',16.2893672532,-76.0010509047,16.2908772536,-76.0010096808,19.8211856584,-75.2355954693,17.7978,-75.9766,'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'),('Bysytykh, Yakutiya, Siberia',2873,'','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 ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1997,1998,'Younger part of reef complex',63,117,-2788757,179847,'Russia','Asia',624,'',63.5833,117.4333,'','',2.45550116657,-60.0113300372,2.45550116657,-60.0113300372,2.45550116657,-60.0113300372,-11.9059,-11.0675,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Bysytykh, Yakutiya, Siberia',2874,'','Cambrian','Series 2','Stage 3','Lenian-Amgaian',509.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',512,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1997,1998,'',63,117,-1907669,397287,'Russia','Asia',624,'',63.5833,117.4333,'','',2.45550116657,-60.0113300372,2.45550116657,-60.0113300372,2.45550116657,-60.0113300372,-11.9059,-11.0675,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Amga River II, Yakutiya, Siberia',2875,'','Cambrian','Series 2','Stage 3','Lenian-Amgaian',509.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',512,1,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'10','Archaeocyaths','3','Microbes','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,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1998,0,'Lower part of younger reef complex (late Lenian-Amgaian',60,130,-2056046,-319768,'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'),('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'),('Cellon, Carnic Alps',2877,'Hohe Warte Limestone','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 ',4,'Biostrome','2','10 to 100 m thick','49',NULL,NULL,NULL,'4','More than 1000 m','7000',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'4','Stromatoporoids','13','Echinoderms','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,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1999,2572,'Reef tract extending from Cellon to Seewarte.\nBiostromes composed of encrinites, stromatoporoids and corals.\nTalus breccia mentioned',46,12,-5464038,4740778,'Italy','Europe',344,'',46.6083,12.9333,'WAHR','81664',-19.9576685615,16.3632818668,-19.9576685615,16.3632818668,46.6083,12.9333,-46.3329,55.4835,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cellon, Carnic Alps',2878,'Plattenkalk','Devonian','Lower Devonian','Emsian','Emsian/Eifelian',387.70,407.60,9,'late Pragian - Eifelian',395,395,'Early Devonian (late Emsian, 395 Ma)',397,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','84',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'4','Stromatoporoids','4','Stromatoporoids','75','Stromatoporoids or chaetetids only',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1999,0,'Only reefal breccias encountered.\nLateral equivalent of stromatoporoid reef. ',46,12,-4607679,3900416,'Italy','Europe',344,'',46.6083,12.9333,'','',-24.1083889156,17.475472705,-24.1083889156,17.475472705,46.6083,12.9333,-39.5114,47.8016,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Palgrunde, Carnic Alps',2879,'Plattenkalk','Devonian','Middle Devonian','Givetian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',390,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','58',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1999,0,'stromatoporoid reefs',46,12,-3302311,2709293,'Italy','Europe',344,'',46.6,12.9833,'','',-28.816002525,18.2184931629,-28.816002525,18.2184931629,46.6,12.9833,-32.8712,37.2904,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Oused Marinelli, Carnic Alps',2880,'','Devonian','Upper Devonian','Frasnian','middle Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',379,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','150',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1999,0,'Stromatoporoid-coral reefs\n',46,12,-3299505,2703381,'Italy','Europe',344,'',46.6083,12.9,'','',-32.4168674608,18.4517574281,-32.4168674608,18.4517574281,46.6083,12.9,-28.5394,31.2292,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pueblo Nuevo, Chiapas',2881,'La Quinta','Paleogene','Oligocene','Chattian','Upper Oligocene',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',26,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','42',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species','28','1','Constructor guild','1','Present','1','Present','3','Pronounced zonation','3','Pronounced zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2000,0,'36 + 6 m thick structures superimposed in Oligocene barrier reef tract, separated by peat bed.\r\nCamino Carretero Member of La Quinta Fm. 27 coral species are described; algae are not described. Dominant genera are: Diploastrea, Atiguastrea, Alveopora, Agathiphyllia, Colpopyllia, Favites, Porites. Strongly zoned: algal-Eulepidina shoal at base, branching coral bed, Porites bank, zone with massive corals.',17,-92,2499061,-9685656,'Mexico','North America',105,'',17.1167,-92.8833,'WAHR','31271',16.5538621271,-88.1948053809,16.5545366983,-88.1979173609,19.9714626877,-87.6595958199,17.8022,-87.9073,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gor Loutat, Tindouf Basin, West Sahara',2882,'','Devonian','Middle Devonian','Givetian','middle-upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',387,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','55',NULL,NULL,NULL,'4','More than 1000 m','2000','300','2541',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','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','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1687,2488,'',26,-10,-5062530,-123821,'Morocco','Africa',714,'',26.75,-10.6667,'WAHR','79496',-40.5040497702,-17.0073594893,-40.5040497702,-17.0073594893,-40.8332900071,-16.8247837174,-46.0601,6.79379,'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'),('Gor Uein Terguet, Tindouf Basin, Western Sahara',2884,'','Devonian','Upper Devonian','Frasnian','lower Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',383,3,'0','Outcropping reef ',4,'Biostrome','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,'1','Corals','1','Corals','2','Corals only',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',1687,0,'Thin biostromal developments of thamnoporoid coral beds',26,-11,-5054632,-208217,'Morocco','Africa',714,'',26.5167,-11.4,'WAHR','79558',-42.3740661701,-19.7134986175,-42.3740661701,-19.7134986175,-42.6884201589,-16.2152996757,-41.8012,1.71273,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sturgeon Lake, Alberta',2885,'Leduc','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'1','Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'42',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',2001,0,'',55,-117,-1042780,-4663477,'Canada','North America',121,'',55,-117.35,'','',-6.6109257328,-57.9315430272,-6.6109257328,-57.9315430272,-0.0943847142711,-117.325765911,-10.1864,-42.1167,'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'),('Monte San Angelo, Gargano',2887,'Ostuni','Cretaceous','Upper Cretaceous','Maastrichtian','Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',68,2,'0','Outcropping reef ',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','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'50','50','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2006,0,'From ref. 2006:\nFormed by rudist framestones and bafflestones, the shelf edge-related rudist complexes, unlike the rudist banks, are commonly not well preserved in situ as the main source of the bioclastic sediments (Figure 10). In the Murge region they are clearly associated with (Begin page 1569) the fault systems that form the eastern shelf edge (Borgomano and Philip, 1987), and in the Gargano they occur as megablocks (>103 m3) in base-slope deposits (Figure 11). A detail study of the biogenic components of those bioclastic sands and blocks has shown that they were mainly sourced from rudist associations not found in the inner platform. Combined analyses of a few preserved shelf edge-related rudist complexes and the associated deeper marine sediments have allowed some of their characteristics to be established. They were dominated by recumbents rudists, including caprinids and Sabinia. The diversity, size, and shape of those rudists, commonly associated with rounded and well-sorted bioclastic gravels, suggest that they lived in a high-energy subtidal setting (Figure 10). These shelf edge-related rudist complexes could be considered as reefs (Longman, 1981), defined as carbonate buildups, influenced by organisms, that controlled depositional processes in adjacent zones and were situated on a topographic high.\n\n',41,15,4085246,1453488,'Italy','Europe',344,'',41.7,15.95,'','',31.7367249519,14.4602381714,31.7367249519,14.4602381714,33.292271043,15.7113175141,29.5247,14.5181,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Murge Area',2888,'Altamura','Cretaceous','Upper Cretaceous',NULL,'Coniacian-early Campanian',72.10,89.80,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',85,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1',NULL,NULL,NULL,'1','Less than 20 m','8',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species','1','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2006,0,'From ref. 2006:\nTidal channel-related rudist <bioherms> consist of meter-thick lenses or <bioherms> (Cummings, 1932) dominated by rudists, overlying algal-mud banks having an erosive contact (Figures 7a, 8). The horizontal dimensions of the rudist <bioherms> are less than 10 m. They are stacked in a progradational system and are overlain by algal-mud banks. The rudist communities are monospecific and have bafflestone-framestone structures (Embry and Klovan, 1971). The <bioherms> have filled preexisting depressions cut through the algal-mud banks. It is plausible that they have affinities with tidal channels because (1) they occur in a zone dominated by cryptalgal laminites inferred to have formed in intertidal environments, (2) they have the character of submarine deposits, and (3) they have prograded in depressions over a lag breccia rich in mud and stromatolitic clasts.\n\n',41,17,3060216,1651340,'Italy','Europe',344,'',41,17.1667,'','',30.2331415942,16.4669329007,30.2331415942,16.4669329007,29.281822356,16.6206552264,25.3467,17.1853,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ouachita Thrust Belt, Oklahoma',2889,'Wapanucka','Carboniferous','Pennsylvanian','Bashkirian','Morrowan',315.00,323.20,13,'Bashkirian - Kasimovian',302,320,'Early Pennsylvanian (Bashkirian, 319.2 Ma)',316,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','5',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','2','Algae','11','Siliceous sponges','79','Siliceous sponges - algae','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2007,0,'  The calcareous alga Donezella is composed of thin (typically 70-160 micrometer in diameter) branching segmented tubes, which bifurcate at an angle of 45-90\ndegrees. This calcareous alga is known to baffle sediment and build small (~6 m thick) to large (30-100 m thick) bioherms. Examples of Donezella-dominated\nbioherms are reported from Middle Carboniferous strata of Algeria, the Canadian Arctic Archipelago, Spain, and West Texas. \n     A 5 m thick Donezella - siliceous sponge bioherm from the Wapanucka Formation was studied in detail by microfacies analysis. Due to high dip of the beds, the lateral dimension of the bioherm is not known. \nThe bioherm overlies thin (20 cm), cross-bedded crinoidal-bioclastic packstone to grainstone, and is capped by peloidal packstone to grainstone The bioherm is primarily composed of Donezella boundstone-bafflestone and peloidal wackestone. In situ siliceous sponge bodies are locally preserved in the lower part of the buildup, by encrustation of micritic crusts and the red alga Archaeolithophyllum. Siliceous sponge spicules are common in the lower half of the bioherm and are rare to present throughout the upper half of the bioherm. The presence of siliceous sponge bodies in the lowest part of the buildup strongly suggests that they played a significant role in initial mound accretion. \n     The green calcareous alga Donezella is common to abundant throughout the bioherm. Donezella builds a delicate framework or colony of thalli enclosing constructional pores. These pores are filled with internal sediments, burial calcite cements, dark micritic crusts and peloids with fuzzy outlines. Toward the top of the bioherm Donezella is increasingly surrounded by carbonate mud. Worm tubes with dark, micritic, encrustations are common in Donezella colonies. \n     The calcareous alga Berestovia (or Claracrusta) is present mainly in the lower half of the bioherm, acting as the primary and secondary encruster of siliceous sponges. Berestovia is also the primary encruster of Donezella colonies. The red alga Archaeolithophyllum is locally present as the secondary and tertiary encruster of siliceous sponges in lower part of the bioherm. Broken segments of Archaeolithophyllum and other phylloid algae are increasingly present toward the top of the bioherm, often encrusted by encrusting foraminifera. \n      Ostracod, benthonic, and encrusting foraminifera are rare to present, but are increasingly present toward the top of the bioherm. Brachiopods, ramose bryozoans, crinoids and corals are rare to present, and are scattered irregularly throughout the bioherm. \n     The bioherm shows a subtle vertical community succession from Donezella boundstone to peloidal wackestone in the lower 5/6 of the bioherm to wackestone\nwith scattered Donezella, fragments of phylloid algae, ostracodes and foraminifera toward the top. This succession is interpreted as being due to shallowing. The presence of siliceous sponge bodies, the abundance of siliceous sponge spicules, and the lack of high-energy microfacies in this bioherm indicates initiation and growth in a quiet-water environment below storm-wave base in the open-marine / slope environment seaward of the platform-margin grainstone belt. \n',34,-95,-783087,-3248278,'United States','North America',101,'',34.75,-95.0833,'WAHR','76327',-26.2687684599,-57.399450405,-15.717614792,-39.0619663416,-13.5434494236,-55.0456363269,-9.85211,-33.8251,'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'),('Koscian reef, Bronsko reef, Rensko reef',2892,'Zechstein','Permian','Lopingian','Changhsingian','Zechstein',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','100',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,'2c','Atoll (circular structure)','1','Above fair weather wave base','7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',2,'Actual reservoir',2011,0,'Gas reservoirs\r\n\r\nAbstract ref. 2011:\r\n     The gas saturated Zechstain Limestone Reefs within western and south western direction from Poznan have been recently discovered. These are Papro W reef\r\nnearby Nowy Tomy l Town and Koscian - Bonikowo Kokorzyn reefs located nearby Koscian Town.  Koscian and Papro reefs and Bonikowo Kokorzyn reefs\r\nwere discovered with 2D and 3D seismic respectively.  The reefs were formed in the inner part of Zechstein See about 60-80 km north from the off shore carbonate\r\nplatform. The genesis of the reefs is strongly connected with a local Carboniferous paleo highs called Wolsztyn High (Fig 1). The paleo-highs are formed with\r\ncarboniferous sandstone (Koscian area) or Autunian volcanic rocks (Paproc_W area) and  they were covered by shallow see. In this shallows there were mainly\r\nbryozoan reefs and oolitic-oncoidic carbonates deposited. Additionally, mostly at the top of the reef the stromatolite occurs. Porous reef body, characterised by\r\nthickness of up to  90 m is surrounded by deep basin limestone facie which is deposited as thin (up to 5m thickness) tight mudstone. \r\n     Below this the most important parameters of the reefs are presented: \r\n\r\n     Porosity very good up to 35 % \r\n     Permeability variable 0.1 3000 mD\r\n\r\nPaproc-W Reef, area 4 sqkm, top depth 2450m TVDSS, thickness 50-80 m -The first discovered by 2D seismic Zechstein Limestone Reef in Poland.  All its\r\nthickness is gas saturated. The accumulated gas contains 40 % of hydrocarbons. \r\n\r\n          Koscian Reef ,  area 20 sqkm, top depth 2100m TVDSS, thickness 60 m. Koscian Reef is the largest of all discovered reefs body (Fig.3). \r\n          There is gas-water contact at the depth of 2208m.The resent discoveries allowed to located new Wielichowo and Ruchocice Reefs at NE from\r\n          Koscian Reef. \r\n          Bonikowo Reef, area 9 sqkm, top depth 2260m TVDSS, thickness 90 m. \r\n\r\n     In 1999 several new reefs was discovered i.e. Rensko-Kokorzyn-Bronsko and it seems to be the largest discovered reef, however  shape of the reef was\r\ninterpreted from 3D seismic and wait for the wells drilling.  The reefs saturated  gas contains 81 % of hydrocarbons (80.5 % of methane) and 18 % of nitrogen. \r\n     It is very important to notice that the efficient reef prospecting is possible thanks to 3D seismic survey.  Both 2D and 3D seismic was shot by GEOFIZYKA\r\nToru.  Especially it is worth emphasising that final success is a result of a co-work of many people; geophysicists, geologists  and engineers. Presently, thanks to\r\nexcellent co-operation between POGC - Oil and Gas Zielona Góra and GEOFIZYKA Toru S.A. the exploration of the Zechstein Limestone reefs has become the\r\npriority task for the companies operating in the western Poland',52,16,2479680,2850307,'Poland','Europe',301,'',52.0833,16.6333,'',NULL,29.0080847607,33.9189203491,29.0115043631,33.9195080948,26.2844590984,29.014658899,18.4727,25.7241,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-03-21 14:10:15'),('Marazani & Dodori, Lamu Basin',2893,'Baratumu','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'550',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'30','60','10',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',2013,0,'Lateral equivalent ot Baratumu Fm., which is dated Aquitanian to Burdigalian.\nBut reefs thought to range through whole Miocene.\n\nMararani and Dodori wells of BP/Shell.\nLamu Reefs encountered in five wells but interpreted shelf margin reef trend is 550 km. \nReefs enveloped in shale.\nBiogenes: Bryozoans, corals, sponges, echinoids, ostracods and crustacean limbs.\n',-1,41,-588301,4118660,'Kenya','Africa',709,'',-1.8333,41.0833,'','',-4.3823948604,38.0569786031,-4.3823948604,38.0569786031,-5.48238398663,37.834416795,-2.93345,38.352,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kipinie & Kofia, Lamu Basin',2894,'Baratumu','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'550','2893',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)','1','Red algae','5','60','35',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',2013,0,'See reef 2893',-2,40,-680920,4056327,'Kenya','Africa',709,'',-2.5,40.5333,'','',-5.06212697648,37.5217568981,-5.06212697648,37.5217568981,-6.13838366805,37.2691774064,-3.60398,37.8062,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pate, Lamu Basin',2895,'Baratumu','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'550','2893',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'20','60','20',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',2013,0,'See reef 2893',-2,41,-629600,4108933,'Kenya','Africa',709,'',-2.1333,41,'','',-4.68432459124,37.9807862054,-4.68432459124,37.9807862054,-5.78075002568,37.7450569408,-3.23403,38.2708,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Marazani & Dodori, Lamu Basin',2896,'Baratumu','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',18,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'550',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'30','60','10',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',2013,0,'See reef 2893',-1,41,-432507,4306575,'Kenya','Africa',709,'',-1.8333,41.0833,'','',-4.54762166095,37.9277791621,-3.83862063194,38.533354557,-4.97770159192,38.2973667187,-2.63095,38.8617,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kipinie & Kofia, Lamu Basin',2897,'Baratumu','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',18,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'550','2896',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'30','60','10',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',2013,0,'See reef 2893',-2,40,-525751,4245376,'Kenya','Africa',709,'',-2.5,40.5333,'','',-5.22742698455,37.3925213119,-4.51740256682,37.9973165447,-5.63710232532,37.7366192844,-3.29983,38.314,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pate, Lamu Basin',2898,'Baratumu','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',18,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'550','2896',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'30','60','10',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',2013,0,'',-2,41,-473909,4297336,'Kenya','Africa',709,'',-2.1333,41,'','',-4.84956269136,37.851614105,-4.14041185216,38.4566662005,-5.27659855084,38.2098892781,-2.93129,38.7796,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ngarama Plateau, Mandawa',2899,'Kiturika','Cretaceous','Lower Cretaceous','Aptian','upper Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',114,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','60',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','40','60',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2014,0,'Pure, massive, white reefal limestones, about 60 m thick.\nCoral growths comparatively rare, but algal material abundant.',-9,39,-4574975,2583885,'Tanzania','Africa',709,'',-9.8667,39.1667,'','',-35.8784642617,29.3581081579,-35.8784642617,29.3581081579,-33.0324199256,22.3248278954,-32.8615,20.2625,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lihimalaya',2900,'Kiturika','Cretaceous','Lower Cretaceous','Aptian','upper Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',114,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','8','Serpulids, worms, vermetids',NULL,NULL,NULL,NULL,'10','90','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2014,0,'Loc. WA. 2326 of Aitken.\nWhite limestone, largely reefal with numerous coral heads. \nTwo beds of of detrital limestone with coral heads in the sequence. \nSome worm tubes also seen.',-9,39,-4509992,2654393,'Tanzania','Africa',709,'',-9.3,39.6167,'','',-35.4565404665,30.0758608364,-35.4565404665,30.0758608364,-32.6420535802,23.0445165066,-32.46,20.9721,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mandawa',2901,'','Cretaceous','Lower Cretaceous',NULL,'Necomian-lower Aptian',124.00,140.00,22,'late Tithonian - early Valanginian',141,135,'Early Cretaceous (Valanginian, 136.4 Ma)',125,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','80','20',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2014,0,'White reefal limestone with intercalated sandstones in west and corlliferous limestone in east.\nOnly fossils are colonial corals and algal masses and occasionally some large gastropod casts',-9,39,-4738649,2460122,'Tanzania','Africa',709,'',-9.8667,39.1667,'','',-39.5654941784,26.6750710625,-39.5654941784,26.6750710625,-36.351396688,19.6948284456,-31.8839,18.0917,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Namorado Field, Campos Basin',2902,'Macae','Cretaceous','Lower Cretaceous','Albian','Albian-Cenomanian',93.90,113.00,24,'late Aptian - middle Cenomanian',107,100,'Early Cretaceous (late Albian, 102.6 Ma)',99,2,'1','Seismic data available ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'2','Algae','2','Algae',NULL,NULL,'1','Red algae','0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2016,0,'Reservoir in the overlying Namorado Sandstone only.\nMacae almost entirely composed of limestone. Lower part is massive. \nLimestones are mostly algaic calcarenites interbedded with micrite.\nSparse faunal content interpreted to be due to environmental restriction. ',-22,-40,-4080109,-785512,'Brazil','South America',201,'',-22.45,-40.4167,'','',-25.4159093899,-5.30549938698,-25.4159093899,-5.30549938698,-25.7628628234,-13.8190334173,-28.2195,-12.2768,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S Campos Basin, off Brazil',2903,'Embore','Paleogene',NULL,NULL,'Oligocene-Miocene',5.30,33.90,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',23,1,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'2','Algae','2','Algae',NULL,NULL,'1','Red 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,NULL,NULL,'0','',1,'Potential reservoir',2016,0,'Siri Member of Embore Fm.\nShelf edge limestone with local development of algal reefs with exceptionally high porosity.\nSaturated with immature oil in the southern part of Campos Basin.',-22,-40,-3142047,-3949540,'Brazil','South America',201,'',-22.6667,-40.75,'','',-24.5547588276,-36.557927957,-24.5547588276,-36.557927957,-22.1568571194,-36.656923739,-22.378,-35.8476,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bombay High Field, Indian Ocean',2904,'','Neogene','Miocene','Lower Miocene','Burdigalian-Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',16,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',2,'Actual reservoir',2017,0,'Foraminiferal mound overlying Aquitanian algal mound.',19,71,1980179,7574721,'India','Asia',501,'',19.3333,71.5,'','',14.0064803734,66.7461518481,14.0064803734,66.7461518481,11.9114090703,67.70301566,13.8924,70.0878,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Zambezi Delta Depression',2905,'Grudja','Paleogene','Paleocene','Selandian-Thanetian','Upper Paleocene',56.00,59.20,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',57,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick','150',NULL,NULL,NULL,'4','More than 1000 m','250',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2019,0,'Paleocene 100-150 m thick barrier reef system interrupted by several submarine canyons.\nAdditional archipelago of Paleocene reefs situated on teh outer edge of the shelf',-18,36,-3910419,2821555,'Mozambique','Africa',NULL,'',-18.6667,36.75,'','',-29.0805144678,30.5087588294,-29.0805144678,30.5087588294,-26.3979226763,27.7628991233,-29.9262,28.2331,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Sengo Marin-1 well, Zambezi Delta Dep.',2906,'Grudja','Paleogene','Eocene','Ypresian','early Eocene',47.80,56.00,27,'Thanetian - Ypresian',53,50,'Early Eocene (Ypresian, 51.9 Ma)',50,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'600',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2019,0,'Westward shift or barrier reef zone from late Paleocene to early Eocene',-19,35,-4032906,2644022,'Mozambique','Africa',NULL,'',-19.6667,35.3333,'','',-28.4007118749,29.1626883344,-28.4007118749,29.1626883344,-27.1787191891,27.1733163142,-29.6612,27.1434,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Inhambane',2907,'Grudja','Paleogene','Eocene','Ypresian','lower Eocene',47.80,56.00,27,'Thanetian - Ypresian',53,50,'Early Eocene (Ypresian, 51.9 Ma)',50,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'600','2906',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2019,0,'Location not discussed in text, only indicated in figure as near end of reef tract',-23,35,-4569102,2547444,'Mozambique','Africa',NULL,'',-23.8333,35.3333,'','',-32.5671493191,29.119960969,-32.5671493191,29.119960969,-31.3251251275,26.7035087944,-33.8629,26.8983,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Janguene-1 well',2908,'Cheringoma','Paleogene','Eocene',NULL,'Middle-Late Eocene',33.90,38.00,28,'Lutetian - Bartonian',45,35,'Late Eocene (Priabonian, 35.9 Ma)',37,1,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','450',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,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2019,0,'Shelf margin barrier reef(?) composed of nummulitic limestone and marl.\nTotal reef thickness is 500-600 m.\nProgradational stratification',-20,34,-3784474,2707362,'Mozambique','Africa',NULL,'',-20,34.6667,'','',-25.1558016627,29.6660906357,-25.1558016627,29.6660906357,-26.082697121,29.1500481134,-24.8201,29.0567,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Janguene-1 well',2909,'Cheringoma','Paleogene','Eocene',NULL,'Middle-Late Eocene',33.90,38.00,28,'Lutetian - Bartonian',45,35,'Late Eocene (Priabonian, 35.9 Ma)',37,1,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick','150',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,1,'Temperate','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2019,0,'',-20,34,-3515129,2885241,'Mozambique','Africa',NULL,'',-20,34.6667,'','',-25.1558016627,29.6660906357,-25.1558016627,29.6660906357,-26.082697121,29.1500481134,-24.8201,29.0567,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('S Ruvuma Basin',2910,'','Jurassic','Middle Jurassic',NULL,'Middle Jurassic',163.50,174.10,20,'middle Aalenian - middle Bathonian',166,165,'Middle Jurassic (Callovian, 164.8 Ma)',167,1,'1','Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'80',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2019,0,'Possible Mid-Jurassic reef detected by seismic exploration.\n',-13,40,-4673382,1986612,'Mozambique','Africa',NULL,'',-13.4167,40.8333,'','',-44.6740797074,19.1651957408,-44.6740797074,19.1651957408,-13.4167,40.8333,-32.586,16.9443,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Ruvuma Basin',2911,'','Jurassic','Middle Jurassic',NULL,'Middle Jurassic',163.50,174.10,20,'middle Aalenian - middle Bathonian',166,165,'Middle Jurassic (Callovian, 164.8 Ma)',167,1,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'80','2910',0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2019,0,'See reef 2910',-12,40,-4568846,1972631,'Mozambique','Africa',NULL,'',-12.7,40.3667,'','',-43.8279666639,19.073119496,-43.8279666639,19.073119496,-41.0370530502,13.5138553597,-31.7499,16.7723,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Black Nose, ODP 171B, West Atlantic',2912,'','Cretaceous','Lower Cretaceous','Aptian','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,120,'Early Cretaceous (early Aptian, 121.8 Ma)',123,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'25',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','5','Rudists','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'20','80','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2021,0,'Abstract ref. \n\nBy Barremian-Aptian time, the reef stepped back 40-50 km from the lower Cretaceous margin and formed a long tract of coral-rudist reefs such as the one evident in seismic profiles in the shallow subsurface at the head of Blake Nose (Fig. 3). \n\nThe Aptian reef tract ceased growth during the late Aptian, at which time periplatform debris was no longer delivered to the outer edge of Blake Nose, and the deposition of green and red variegated clays began. ',29,-76,1522433,-3676865,'Atlantic','Atlantic',NULL,'',29.9167,-76.8333,'','',20.6616389037,-27.4008673802,19.4670954728,-26.2162465243,22.7318072563,-31.9715733271,24.7939,-31.0784,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bihor Mountains',2913,'','Jurassic','Upper Jurassic','Tithonian','Tithonian-Berriasian',139.80,152.10,22,'late Tithonian - early Valanginian',141,145,'Jurassic/Cretaceous Boundary (145 Ma)',145,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2023,0,'Allochthonous reefal blocks',46,22,3392574,2245621,'Romania','Europe',348,'',46.45,22.6667,'','',30.3138968789,33.793268313,30.3138968789,33.793268313,23.3330656295,28.9451032535,27.9173,27.5565,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Argentara Massif, Maritime Alps, France-Italian bor',2914,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian/Tithonian',145.00,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',150,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2024,0,'Abstract ref. 2024:\nA finding of a Nerineae fauna in the southeast part of the Argentera massif and in the Tenda pass (Franco-Italian Alps) is reported. The formation is a reef facies of Kimmeridgian-Tithonian age (upper Jurassic). The following forms are represented in the fauna: an unidentified species of Nerinea, Ptygmatis cf. pseudobruntrutana, Phaneroptyxis moreana, and Cryptoplochus cf. subpyramidalis. ',44,6,4259915,1078341,'France','Europe',331,'',44.4167,6.8833,'','',24.7449831217,22.7102996715,24.7449831217,22.7102996715,29.9548942089,24.2430087263,34.379,15.8007,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Malleval, Vercors',2915,'','Cretaceous','Lower Cretaceous','Valanginian','upper Valanginian',132.90,139.80,23,'late Valanginian - early Aptian',126,135,'Early Cretaceous (Valanginian, 136.4 Ma)',137,3,'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,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2025,0,'Abstract ref. 2025 (not seen):\nSedimentary rocks exposed in the vicinity of Malleval (southeast France) include Tithonian (Jurassic), Berriasian, Valanginian, Hauterivian, and Urgonian (all lower Cretaceous) formations. A new outcrop of the upper Valanginian reef facies is reported. The Nant and Gerlette anticlines and the Picotiere syncline, all oriented north-south, are cut by three previously undescribed fracture systems: north-south, north-northwest-south-southeast, and  west-southwest-east-northeast. The late phase of tangential movements in the Subalpine region is probably responsible for westward thrusting along the fractures. ',45,5,4038180,635934,'France','Europe',331,'',45.1333,5.4167,'','',26.6026944215,21.5194770003,26.6026944215,21.5194770003,31.6431502726,21.3207431487,36.0176,14.6614,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Siniscola-Posada, Sardegna',2916,'','Jurassic','Upper Jurassic','Tithonian','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',147,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2026,0,'Abstract ref. 2026:\nOn the eastern coast of Sardinia, in the Siniscola-Posada area, Jurassic rocks are transgressive on the Hercynic basement. The sequence begins with 15 to 50 metres of dolomitic limestones and dolostones, yielding Bathonian and Callovian ammonites. Oxfordian is probably missing. The middle Jurassic dolostones are directly overlaid by Kimmeridgian limestones, 100 m thick. The Beckeri zone is well represented in their upper half, with the index form and several other ammonites and aptichi. The Jurassic sequence ends with Tithonian limestones in reef facies.',40,9,3813387,811740,'Italy','Europe',344,'',40.6,9.6833,'','',22.3535796248,22.1408183692,22.3535796248,22.1408183692,23.9931725483,17.0323850239,34.0276,14.4095,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Eastern Betic Cordillera',2917,'','Jurassic','Upper Jurassic','Tithonian','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',147,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','5','Rudists','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,'20','80','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',2028,0,'Abstract ref. 2028:\nSpecimens of small diceratids from Tithonian (Jurassic) reef deposits of the eastern Betic cordilleras belong to Monnieria or a closely related genus. Their presence suggests analogous reef environments during the Portlandian and Tithonian in southern Spain and the Languedoc region, southern France. ',37,-2,3055318,13458,'Spain','Europe',304,'',37.25,-2.3333,'','',16.6975787633,10.8043463959,16.6975787633,10.8043463959,23.8570764406,7.41204334931,29.7947,4.92116,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Suva Planina, Serbia',2918,'','Jurassic','Upper Jurassic','Tithonian','Tithonian-Berriasian',139.80,152.10,22,'late Tithonian - early Valanginian',141,145,'Jurassic/Cretaceous Boundary (145 Ma)',145,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2029,0,'Abstract ref. 2029:\nReef limestones of the Suva Planina region and similar organic limestones of eastern Serbia, Yugoslavia, represent continuous sedimentation from Tithonian (Jurassic) to Valanginian (Cretaceous) time. Two types can be distinguished--reef deposits and lateral equivalents formed in deeper waters. Transgression was widespread, and deposition of thick sequences of limestone was due to gradual subsidence of the depositional basin during epeirogenic crustal movements. ',42,20,3009470,1852896,'Yugoslavia','Europe',307,'',42,20.6667,'','',8.85250218364,24.9817135719,8.85250218364,24.9817135719,15.5995716056,28.658409202,26.0688,22.7885,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Suva Planina, Serbia',2919,'','Cretaceous','Lower Cretaceous','Berriasian','Berriasian-Valanginian',132.90,145.00,22,'late Tithonian - early Valanginian',141,140,'Early Cretaceous (Berriasian, 142.4 Ma)',140,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2029,0,'See reef 2918',42,20,3009470,1852896,'Yugoslavia','Europe',307,'',42,20.6667,'','',9.31907981419,26.5544783753,9.31907981419,26.5544783753,15.5185059931,28.9530450869,25.41,22.9347,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('SE Crimea',2920,'','Jurassic','Upper Jurassic','Tithonian','Tithonian/Berriasian',139.80,152.10,22,'late Tithonian - early Valanginian',141,145,'Jurassic/Cretaceous Boundary (145 Ma)',145,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',2030,0,'',45,35,5032341,2966606,'Ukraine','Europe',301,'',45,35,'','',32.276938767,43.7426801062,32.276938767,43.7426801062,36.3079221661,46.5477821077,38.495,40.3642,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Crimea Mountains',2921,'','Cretaceous','Lower Cretaceous','Valanginian','upper Valanginian',132.90,139.80,23,'late Valanginian - early Aptian',126,135,'Early Cretaceous (Valanginian, 136.4 Ma)',137,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8','1','Less than 10 m wide','6','2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','10','70','20',0,'no',0,'no','2','6 to 24 reef building species','18','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2031,2636,'algal-coral bioherms, 2.5-8 m thick, 2.5-6 m across, 3-10 m distance between bioherms\n\nAbstract ref. 2031:\nBiostromal structures have been identified in the upper Valanginian and lower Hauterivian (lower Cretaceous) deposits along the Crimean mountains (USSR). The structures have been formed by scleractinians, algae, and rarely by hydrozoans. Reef facies first appeared during the upper Oxfordian (upper Jurassic) and northward migration of some 25-30 km continued until the Hauterivian. The migration was influenced by tectonic movements and uplift of Kimmerian massifs. ',44,34,4930443,2843770,'Ukraine','Europe',301,'',44.8333,34.5,'WAHR','77072',32.4934254617,44.0997630218,32.4934254617,44.0997630218,36.1106786106,45.4419235201,37.5144,40.2138,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sabana Grande, SW Puerto Rico',2922,'Monte Grande','Cretaceous','Upper Cretaceous','Campanian','Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,80,'Late Cretaceous (Early Campanian, 80.8 Ma)',77,2,'0','Outcropping reef ',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','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,'60','40','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2032,2150,'Part of abstract of ref. 2032:\nThe structurally low Yauco basin began to receive volcanic rocks, clastic rocks, olistostromes, and olistoliths in Maastrichtian time. Campanian reefs which had grown on the uplifted Jurassic crust slid northward into the basin. Emplacement of reefal debris and olistoliths was synchronous with volcanism and uplift. These processes suggest proximity to submarine volcanoes, possibly in a deforming forearc basin. Surficial exposures of mantle rocks are probably the result of structural inversion of the basin in response to contraction in the currently active east-trending left-lateral fault system. ',18,-66,2354681,-6815155,'United States','North America',101,'',18.1,-66.9333,'','',12.097920156,-55.7109730282,12.097920156,-55.7109730282,14.1401448127,-59.0173216226,15.0293,-56.9006,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Porcupine Basin, offshore Ireland, Atlantic',2923,'','Neogene','Pliocene','Pliocene','Pliocene-Pleistocene?',0.00,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',1,1,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,2,'Cold - water','4','Basin','4b','Deep basin (> 200 m)','3','Below storm wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2033,0,'Reefs buried under 30 m of sediment. No age control. \n\nAbstract ref. 2033:\nDuring a recent cruise in the Porcupine Basin, off southwest Ireland, we discovered two extensive and hitherto largely unsuspected deep-water reef provinces, including a giant cluster of hundreds of buried mounds. The ring shapes of many reefs suggest that they are caused by an axial fluid expulsion at the sea bed, a transient flow well confined in space and time. We are exploring various hypotheses, but a stimulating avenue for research is opened by a glacially controlled growth pulse and subsequent decay of a shallow layer of gas hydrates as a methane buffer and probably indirectly as a ground for overlying biological communities.',52,-12,6778174,-1121799,'Atlantic','Atlantic',NULL,'',52.3333,-12.75,'','',52.0668330944,-13.2746755422,52.0688421853,-13.2707529614,52.27421652,-12.6570046563,52.3499,-12.9102,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Sendurai, Tamil Nadu',2924,'','Paleogene','Paleocene','Danian','Danian',61.60,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',64,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,'30','50','20',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2034,0,'Maastrichtian or most likely Danian age based on Hercoglossa danicus. \nHowever, Orbitoides minor is also present suggesting Maastrichtian age.\n\nCorals and bryozoans\n\nQuotation from ref. 2034: The common fossils in this limestone are corals, polyzoans, lamellibranchs and gastropods. The corals are mostly compound and are often so massive and abundant that one is tempted to consider the rock a coral limestone. ',11,79,-3835654,6228910,'India','Asia',501,'',11.2333,79.1667,'','',-28.7121639223,61.1944417231,-28.7121639223,61.1944417231,-26.1334539934,56.0262757503,-28.3829,60.1424,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lindi',2925,'','Paleogene','Paleocene','Danian','Paleocene',56.00,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',61,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2035,0,'Chain of reef knolls overlying sandy detrital limestone.\nNo description',-10,39,-2778119,3313605,'Tanzania','Africa',709,'',-10,39.6833,'','',-21.3802385123,33.9957968486,-21.3802385123,33.9957968486,-18.3645120353,31.2747647655,-21.9661,31.2258,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lindi',2926,'','Paleogene','Eocene',NULL,'Middle-Late Eocene',33.90,38.00,28,'Lutetian - Bartonian',45,35,'Late Eocene (Priabonian, 35.9 Ma)',37,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2035,0,'Sandy reef limestone and marls.\nReef facies suggested by ostracodes. No description.',-10,39,-2472039,3429540,'Tanzania','Africa',709,'',-10,39.6833,'','',-15.1222675972,34.7540787206,-15.1222675972,34.7540787206,-16.3945881911,34.992377797,-14.7186,33.96,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lindi',2927,'','Paleogene','Eocene',NULL,'Middle-Late Eocene',33.90,38.00,28,'Lutetian - Bartonian',45,35,'Late Eocene (Priabonian, 35.9 Ma)',37,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2035,0,'See reef 2926',-10,39,-2184258,3579146,'Tanzania','Africa',709,'',-10,39.6833,'','',-15.1222675972,34.7540787206,-15.1222675972,34.7540787206,-16.3945881911,34.992377797,-14.7186,33.96,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kitunda Cliff, Lindi',2928,'','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2035,0,'Massive, mostly sandy reef limestone surrounded by grey buff clay.\nNo description of reef facies. ',-10,39,-1706650,3928170,'Tanzania','Africa',709,'',-10,39.7,'','',-12.7898522903,36.898350598,-12.7898522903,36.898350598,-13.8871111589,36.9284630308,-11.1532,36.9688,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('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'),('Jebel Huwayyah, U.A.E.',2930,'Simsima','Cretaceous','Upper Cretaceous','Maastrichtian','upper Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',67,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m','5',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild','1','Present',NULL,NULL,'2','Medium zonation','1','Low zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2038,2039,'Isolated small patch coral reefs associated with restricted mollusc banks. \n4 coral species described:\n3 Genera:\nSiderastrea\nCunnolites\nAulosmilia',24,55,919207,5107499,'United Arab Emirates','Asia',NULL,'',24.1333,55.8833,'WAHR','67010',8.08372082969,49.428417943,8.08372082969,49.428417943,9.06856198589,47.0666018319,5.61828,46.0932,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jebel Rawdah, U.A.E.',2931,'Simsima','Cretaceous','Upper Cretaceous','Maastrichtian','upper Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',67,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2',NULL,NULL,NULL,'1','Less than 20 m','5',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','7','1','Constructor guild','1','Present',NULL,NULL,'2','Medium zonation','1','Low zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2038,2039,'Small coral patch reefs with \nCunnolites\nAulosmilia\nDiploctenium\nFavites\n7 coral species',25,55,1072459,5119743,'United Arab Emirates','Asia',NULL,'',25.2667,55.95,'WAHR','67009',9.2092452883,49.5766041727,9.2092452883,49.5766041727,10.1822793961,47.2885936494,6.7385,46.2769,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Loudon, Knoxville, Tennessee',2932,'Holston','Ordovician','Upper Ordovician','Sandbian','lower-middle Caradocian',452.00,458.00,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',456,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'40','2463',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',NULL,NULL,'100','0','0',0,'no',0,'no','3','25 or more reef building species','22','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1575,0,'Southwestermost extension of reef tract. See reef 2463 for remarks.',35,-84,-3464924,-6179033,'United States','North America',101,'',35.65,-84.3167,'','',-10.4204895827,-112.631644606,-19.6585595305,-115.827267086,-19.6585595305,-115.827267086,-28.8937,-64.6664,'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'),('Binanga, Karangmumus, Borneo',2936,'Mura-Djawa','Neogene',NULL,NULL,'Mio-Pliocene',2.60,20.00,32,'Tortonian - Gelasian',6,15,'Middle Miocene (Langhian, 14.9 Ma)',5,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2043,0,'Second limestone horizon assigned to the Halbglanz-Kohlengruppe (Mio-Pliocene). \nFringing coral reefs.',0,117,-42732,13047588,'Indonesia','Asia',614,'',-0.3667,117.2667,'','',0.523242481004,115.689414347,0.740629781074,116.063462726,-1.6189603828,116.471841632,-0.176518,118.381,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Binanga, Karangmumus, Borneo',2937,'Sanga-Sanga','Neogene','Miocene','Middle Miocene','mid-Miocene',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',13,1,'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','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'5','95','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2043,0,'Limestone horizon III\nCoral fringning reefs in \'Glanzkohlengruppe\'.\nTogether with small Lepidocyclina and Miogysina polymorpha.',0,117,9781,13162121,'Indonesia','Asia',614,'',-0.3667,117.2667,'','',0.538347866315,115.71573703,0.538347866315,115.71573703,-2.10211878868,116.49245606,-0.0824982,118.774,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Binanga, Karangmumus, Borneo',2938,'Sanga-Sanga','Neogene','Miocene','Lower Miocene','Early Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',20,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2043,0,'Limestone horizons IV and V. About 700 m under horizon III.\r\nLocality W34.\r\nTwo coral beds separated by 40 m of sandstones. \r\n\'Glanzkohlengruppe\'\r\nDated as early Miocene but younger than the oldest Miocene-Oligocene.\r\nFive coral species described, genera:\r\nGoniopora, Cyathoseris, Leptoseris, Metastraea, Symphyllia.',0,117,119361,13354546,'Indonesia','Asia',614,'',-0.4,117.2333,'',NULL,-0.389680669047,113.992556403,-0.389680669047,113.992556403,-4.31871390948,116.222766602,0.424751,120.637,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gunung Badupar, Bontang, Borneo',2939,'Sanga-Sanga','Neogene','Miocene',NULL,'early to middle Miocene',11.60,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',16,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','150',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','11','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2043,576,'Coral fringing reefs.\nBed 6 of Wanner in Felix (1921)\nAge based on larger forams:\nMiogypsina bifida, Lepidocyclina ferreroi, L. glbra, L. angulosa, L. sumatrensis, L. flexuosa, L. acuta, Flosculinella bontangensis, Cycloclypeus communis, Gypsina globulus, Rotalia beccarii, Operculina complanata.\n10 coral species described.\nGenera: Alveopora, Goniaraea, Porites, Madrepora, Seriapora, Pavonia, Caulastraea, Stylophora, Paracyathus',0,117,78989,13167165,'Indonesia','Asia',614,'',0.1333,117.35,'','',0.407768436732,114.699548931,0.407768436732,114.699548931,-3.16245745179,116.619669341,0.775461,120.092,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gunung Badupar, Bontang, Borneo',2940,'Sanga-Sanga','Neogene','Miocene','Lower Miocene','Early Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',21,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2043,0,'See reef 2939',0,117,193982,13358101,'Indonesia','Asia',614,'',0.1333,117.35,'',NULL,0.127647695179,114.16691046,0.127647695179,114.16691046,-3.86222291395,116.522937419,0.967687,120.694,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sankuliran-Bay, Borneo',2941,'Mura-Djawa','Neogene',NULL,NULL,'Mio-Pliocene',2.60,20.00,32,'Tortonian - Gelasian',6,15,'Middle Miocene (Langhian, 14.9 Ma)',5,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','16','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2043,2418,'Coral limestones.\nPoorly dated but probably Mio-Pliocene.\n11 species described from Kabasian locality (ref. 2043). Genera:\nPorites, Goniopora, Cycloseris, Fungia, Trochoseris, Cyathoseris, Siderastraea, Prionastraea, Acanthastaea, Hydnophora, Stylophora\nSekoerau locality is probably identical and has 15 coral species according to ref. 2418.',0,117,139580,13110035,'Indonesia','Asia',614,'',0.95,117.8667,'WAHR','46490',1.82240429602,116.326626885,2.05184719986,116.675525953,-0.338581330402,117.145974209,1.1721,118.905,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Basleo, Timor',2942,'unknown',' 	Permian','Guadalupian',NULL,'Guadalupian',259.80,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',265,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate','0',NULL,'','Unknown',NULL,NULL,'1','Corals','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','3','25 or more reef building species','33','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2044,2047,'Prolific coral faunas, mostly solitary rugosans but also severals favositid, auloporid and trachypsammid tabulates (Favosites, Pachypora).\nBorings indicated on plates and mentioned in plate captions. Probable sponge borings in Trachypsammia.\nMostly reworked coral material in tuffaceous marls.\nCorals obviously associated with abundant siliceous sponges and bryozoans. ',-9,124,-5736379,9868071,'Indonesia','Asia',614,'2048',-9.75,124.5,'','',-49.36356976,109.203424102,-49.36356976,109.203424102,-40.3018626229,107.174543329,-6.9294,123.88,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Obi',2943,'','Neogene','Pliocene','Pliocene','late Pliocene',2.60,3.60,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',3,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2045,0,'Only three species indicated',-1,127,-222402,14334703,'Indonesia','Asia',614,'',-1.5,127.75,'','',-2.31536568294,127.180300583,-2.31768918524,127.178509901,-2.98860888233,130.036513797,-3.35718,128.124,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nikiniki, Timor',2944,'','Neogene','Pliocene','Pliocene','Upper Pliocene',2.60,3.60,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',3,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2045,0,'Reef limestone of Biwak Niki Niki 750 m above sea level. \n63 coral species described from Timor, many of them from Niki Niki.',-9,124,-1867422,13404842,'Indonesia','Asia',614,'',-9.7833,124.5167,'','',-11.3260473068,123.702174235,-11.3310411225,123.699521756,-11.961037272,123.82774774,-9.67637,124.992,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Echo Shoal, Sahul Shelf, offshore',2945,'','Neogene','Pliocene','Pliocene','Pliocene-Pleistocene?',0.00,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',1,1,'1','Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'400',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2046,0,'No age provided.\nReefs only indicated by Geotech Subot System\nReefs buried by at least 100 m of sediments.',-10,126,-1921732,13646685,'Australia','Oceania',801,'',-10.1667,126.8333,'','',-11.5033039505,126.139628407,-11.4932889828,126.144847648,-12.0305851295,126.262466077,-12.0282,126.205,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ashmore Reef, Sahul Shelf, offshore',2946,'','Neogene',NULL,NULL,'Miocene-Pliocene',2.60,20.00,32,'Tortonian - Gelasian',6,15,'Middle Miocene (Langhian, 14.9 Ma)',5,2,'1','Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'400','2945',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2046,0,'Minor corals of Miocene age drilled.\nRefraction studies indicate major reef tract and erosion in Pliocene',-12,123,-2199647,13159393,'Australia','Oceania',801,'',-12.25,123.1667,'','',-17.9136306269,120.076597881,-17.9136306269,120.076597881,-20.0095209706,120.632468918,-19.7353,120.175,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sahul Shelf, offshore',2947,'','Neogene','Pliocene','Pliocene','Pliocene-Pleistocene?',0.00,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',1,1,'1','Seismic data available ',NULL,NULL,'3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'400',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2046,0,'',-11,125,-2033749,13504144,'Australia','Oceania',801,'',-11,125.8333,'','',-12.3353216126,125.133868901,-12.3253167047,125.13913391,-12.8636716242,125.255630486,-12.8565,125.194,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pesco Falcone, Maiella',2948,'Pesco Falcone','Paleogene','Oligocene','Rupelian','lower Rupelian',30.00,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',33,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','2','Intensive','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2049,0,'Coralgal reef along marign of lower Rupelian shallow-water platform prograding over the uppermost slope. \r\nReef builder rarely in situ and stronly bored (Fig. 12B of ref. 2049).',42,14,4944363,1136869,'Italy','Europe',344,'',42.125,14.075,'','214135',37.5875502604,5.19082754193,37.5136281582,5.18535685135,37.9251970622,14.4715376449,39.025,11.993,'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'),('Dolon Pass, N Tien-Shan',2952,'','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 ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2054,0,'Position!\nMassive reefal limestones mentioned. Unknown composition.',41,76,483204,9831332,'Kyrgyzstan','Asia',NULL,'',41.75,76.75,'','',-24.1002690956,47.836575887,-24.1002690956,47.836575887,-24.1002690956,47.836575887,-15.2435,60.6908,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Southern Novaya Zemlya',2953,'Nelidov','Ordovician','Middle Ordovician','Dapingian','Middle Ordovician',458.40,470.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',468,1,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'7','Bryozoans','7','Bryozoans',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2055,0,'Small, meter scale bryozoan reefs (Dianulites).',71,55,-3943308,1211169,'Russia','Asia',624,'',71,55,'','',-19.6818118889,-47.1560953355,-19.6818118889,-47.1560953355,-19.6818118889,-47.1560953355,-20.7388,7.19974,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('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'),('Sarytuma, southern Betpak-Dala Desert, Kazachstan',2956,'Dulankara','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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2062,0,'Mud mound without stromatactis',45,70,-2856843,7959948,'Kazakhstan','Asia',301,'',45,70,'WAHR','80175',-23.6880717801,36.2468596857,-17.1980638147,29.9048780653,-17.1980638147,29.9048780653,-7.74302,56.3618,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Challenger Mound, eastern Porcupine Seabight',4074,'','Quarternary','Pleistocene','Pleistocene','Gelasian',1.80,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,NULL,'3','101-1000 m wide',NULL,'3','More than 100 m','550',NULL,NULL,2,'Cold - water','4','Basin','4a','Shallow basin','2','Below fair weather wave base','1','Corals','12','Foraminifera','20','Corals - forams','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2941,NULL,'',NULL,NULL,NULL,NULL,'Ireland','Europe',NULL,NULL,51.22,-11.43,NULL,'152368',51.0046413037,-11.8601727275,51.0046413037,-11.8601727275,51.1670126568,-11.3633165199,51.227,-11.4871,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('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'),('Maikain, Chingiz-Tarbagatay Zone, Kazachstan',2958,'Angrensor','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,'2','10 to 100 m thick','100',NULL,NULL,NULL,'4','More than 1000 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1668,0,'Reef-like massifs up to 100 m thick, extending up to 20 km',47,81,-1347806,7714605,'Kazakhstan','Asia',301,'',47.3333,81.3333,'','',-16.4470376992,32.1920338523,-10.0242109604,25.8579520057,-10.0242109604,25.8579520057,0.432402,56.0906,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('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'),('Pirgu',2962,'Pirgu','Ordovician','Upper Ordovician','Katian','late Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',446,3,'0','Outcropping reef ',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,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1036,0,'Isolated micritic mounds\nOriginal age call: middle Ashgill',59,24,-4184054,-32879,'Estonia','Europe',NULL,'',59.1333,24.8167,'','',-26.1564849429,-59.0917947417,-26.1564849429,-59.0917947417,-26.1564849429,-59.0917947417,-29.2604,-0.890028,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Porkuni',2963,'Porkuni','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 ',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','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'50','30','20',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2069,0,'Small coral-stromatoporoid-bryozoan reef surrounded by bioclastic pelmatozoan grainstones.\nExtremely high diversity (150 species)',59,26,-4154400,45300,'Estonia','Europe',NULL,'',59.1667,26.1833,'WAHR','80715',-20.307983604,-55.1836407313,-20.307983604,-55.1836407313,-20.307983604,-55.1836407313,-26.8251,-0.318899,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Elgenchak Mts., Yasachnaya River, Yakutia',2964,'Iryudi','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','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'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',2070,0,'Coral-bearing reefal limestones associated with oolitic shoal complexes.',65,152,1127111,-1913900,'Russia','Asia',624,'',65.75,152,'','',11.7191480845,-76.8387851343,12.2712859169,-77.1379155779,12.2712859169,-77.1379155779,8.35547,-11.4364,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jituoshan, Yushan, Jiangxi',2965,'Sanqushan','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 ',2,'Reef mound','3','101-500 m thick','150','4','More than 1000 m wide','1000','4','More than 1000 m','2000',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','1','Red algae','0','100','0',0,'no',0,'no','3','25 or more reef building species','24','1','Constructor 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',2071,1806,'Four successive domical mud mounds.Core with nodular Solenopora masses and micrite clumps (probably microbial).Collection refers to small mounds with corals and stromatoporoids in Wangjiaba section',28,118,-1010990,13779241,'China','Asia',602,'2667',28.5,118.2667,'WAHR','80141, 153816',-8.06957952819,64.9358125311,-8.06957952819,64.9358125311,-8.06957952819,64.9358125311,2.46843,123.921,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Saal Quarry, Regensburg',2966,'Regensburger Grünsandstein','Cretaceous','Upper Cretaceous','Cenomanian','middle Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',96,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','11','Siliceous sponges','11','Siliceous sponges',NULL,NULL,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','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2072,0,'Lithistid sponges (Jerea) forming clusters in clastic deposits.\nLithistid sponge biostromes and mounds in sandstone beds. Mounds of unit 8: up to 1 m thick. Mounds of unit 10: up to 1.3 m thick and 4.4 m wide. 6 sponge morphotypes.',49,12,4844084,1209281,'Germany','Europe',331,'',49.0167,12.3333,'WAHR','74183',43.6007353213,16.3028015894,43.6007353213,16.3028015894,40.9794355584,14.5708633415,38.5387,11.8446,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Saal Quarry, Regensburg',2967,'Regensburger Grünsandstein','Cretaceous','Upper Cretaceous','Cenomanian','late Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',94,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'1','Less than 20 m','4',NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','11','Siliceous sponges','11','Siliceous sponges',NULL,NULL,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',NULL,NULL,'1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2072,0,'See reef 2966.',49,12,4931854,1219690,'Germany','Europe',331,'',49.0167,12.3333,'WAHR','74183',43.6007353213,16.3028015894,43.6007353213,16.3028015894,40.9794355584,14.5708633415,38.5387,11.8446,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Southern House Range, Utah',2968,'Fillmore','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',476,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2','1','Less than 10 m wide','3','2','10 - 100 m','30','1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','11','Siliceous sponges','2','Algae','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)','3','Receptaculitids','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2074,0,'original age call: mid-late Canadian (Ibexian)\nTrending parallel mounds. More than 55 mounds in area. Up to 1.5 m high, 2-3 m wide and 30 m long.\nLithistid sponges, Calathium and microbes (stromatolites, Girvanella, and Tubiphytes(?)).\nIbexian age',39,-113,-158908,-8102834,'United States','North America',101,'',39.0333,-113.3667,'WAHR','61729',21.7082359418,-117.379544188,21.7082359418,-117.379544188,21.7082359418,-117.379544188,-4.91727,-84.1357,'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'),('Khalyya River, Sette Daban Mountains',2970,'Khandyg','Silurian','Llandovery','Telychian','Telychian',433.40,438.50,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',431,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'70','0','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1665,0,'Late Llandovery tabulate corals and stromatoporoid patch reefs from several localities. Corals usually prevailing',62,138,2902256,-1297565,'Russia','Asia',624,'',62.2,138.15,'WAHR','79394',27.3150828329,-73.7527372015,27.3150828329,-73.7527372015,27.3150828329,-73.7527372015,23.1558,-12.5785,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Molong High, New South Wales',2971,'Liscombe Pools Lst.','Silurian','Llandovery','Telychian','late Llandovery',433.40,443.40,6,'Rhuddanian-Telychian',435,430,'Early Silurian (late Llandovery, 430 Ma)',430,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'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',1559,1536,'8-10 m thick Liscombe Pools Lst. locally massive with rich coral-stromatoporoid fauna.',-33,148,1230659,19199883,'Australia','Oceania',801,'',-33.1,148.8667,'','',5.49106902702,117.117226592,5.49106902702,117.117226592,5.49106902702,117.117226592,11.9754,171.953,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lake Timiskaming, Ontario',2972,'','Silurian','Wenlock','Sheinwoodian','Wenlock',427.40,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',426,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2','1','Less than 10 m wide','3','1','Less than 20 m','4',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2076,0,'Small Wenlock patch reefs, 1-2 m thick and 1-4 m diameter, built of syringoporids and clathrodictyid stromatoporoids, with encrusting bryozoans, auloporids and an associated fauna of favositids and colonial rugosans, mark the lake Timiskaming graben structure, halfway between Hudson Bay and southern Ontario, Canada ',46,-79,-3105231,-4440357,'Canada','North America',121,'',46.7167,-79.1,'','',-24.3901550292,-81.9462022668,-24.3901550292,-81.9462022668,-24.3901550292,-81.9462022668,-21.896,-43.8332,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Verkhov, Vishera River, Urals',2973,'','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 ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'60',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1662,0,'Biota and exact position unknown',60,58,656070,639320,'Russia','Asia',624,'',60.5,58,'','',21.0681516077,-39.5565366342,21.0681516077,-39.5565366342,21.0681516077,-39.5565366342,4.53673,6.79909,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Bonnet Plume River, Yukon',2974,'Road River','Devonian','Lower Devonian','Lochkovian','Lochkovian',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,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no',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',2077,0,'',65,-134,-507165,-4310794,'Canada','North America',121,'',65.8333,-134.8833,'','',3.262758033,-83.7945136238,3.262758033,-83.7945136238,18.7874934133,-142.372455419,4.68057,-43.9823,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pic Ararca, Aldudes, Pyrenees',2975,'','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 ',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,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2079,0,'Small bioherm with stromatoporoids and corals',43,-1,-4987623,2694684,'France','Europe',331,'',43.0833,-1.4167,'','',-27.4627185425,1.54877725758,-27.4627185425,1.54877725758,-11.6799660622,-24.6499362021,-42.9813,35.5391,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bir Aidiat, N',2976,'','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,'2','10 to 100 m thick','50',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',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',2080,1687,'',25,-11,-6252889,165477,'Mauritania','Africa',NULL,'',25.3833,-11.95,'','',-40.1355134935,-18.2306428938,-40.1355134935,-18.2306428938,-37.665597668,-18.1885146844,-52.0173,9.50821,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Washington',2977,'','Devonian','Middle Devonian','Eifelian','late Eifelian-Givetian',382.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',391,2,'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,'1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2082,1662,'Position!\nSmall tabulate coral and stromatoporoid patch reefs.',46,-121,-1635244,-5868742,'United States','North America',101,'',46,-121,'','',-14.5409467706,-75.9804292905,-14.5409467706,-75.9804292905,-9.83514031522,-131.724075443,-17.872,-53.7978,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Unknown Locality',2978,'Shigrov-Semiluki','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',380,2,'0','Outcropping reef ',1,'True reef','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','','Unknown','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2083,0,'<2 m thick, early and middle Frasnian (Shigrov and Semiluki group) coral-stromatoporoid-\'algal\' patch reefs, usually in very shallow nearshore waters.',56,25,-1059336,1194742,'Latvia','Europe',NULL,'',56,25,'','',-10.8741483778,-4.96608475057,-10.8741483778,-4.96608475057,10.2633168829,-66.070443431,-9.57866,11.1958,'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'),('Western Victoria Island, NWT',2980,'Blue Fjord','Devonian','Middle Devonian','Eifelian','late Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',393,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2085,0,'',72,-118,-388371,-3216069,'Canada','North America',121,'',72,-118.5,'','',2.76653564703,-55.5970117289,2.76653564703,-55.5970117289,8.66368649341,-114.864005643,-3.7021,-28.9028,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Ha Lang',2981,'Ha Lang','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',388,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'40','0','60',0,'no',0,'no','3','25 or more reef building species','35','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2086,2087,'Coral and stromatoporoid bearing bioherm and reef-related communities cited:\nAmphipora, Stachyodes, Idiostroma, Thamnopora, Crassialveolites, Cliapora, Scoliopora, Dendrostella, Grypophyllum, Macgeea, Thamnophyllum are common',22,106,-514293,11249243,'Vietnam','Asia',NULL,'',22.6833,106.6667,'WAHR','83244',-9.26308684599,88.3345129639,-9.26308684599,88.3345129639,-17.6106263328,112.862250513,2.18455,117.706,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Northeas',2982,'','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,3,'0','Outcropping reef ',1,'True reef','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,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2089,0,'',43,27,2045392,2718632,'Bulgaria','Europe',319,'',43.6667,27,'','',4.68368335773,38.9707095441,4.68368335773,38.9707095441,24.4437558304,38.4883491594,15.7329,32.9591,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Wollmershausen, Jagst',2983,'Muschelkalk','Triassic','Middle Triassic','Anisian','late Illyrian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',238,3,'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','4',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','13','Echinoderms','15','Non-rudist bivalves','92','Bivalves - crinoids',NULL,NULL,'8','0','92',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2090,0,'Terquemid bivalves encrusted by Encrinus lilliformis. \nMicrite around 50 %.\n80% of allochems are Encrinus holdfasts, 15% Encrinus debris and 35% bivalve shells.',49,10,2471433,1806316,'Germany','Europe',331,'',49.1792,10.025,'WAHR','67647',27.9908496973,29.1266328077,27.9908496973,29.1266328077,22.0292289215,24.694447467,15.1597,19.5901,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Oreokastro, Thessaloniki',2984,'','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 ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2091,0,'Massive limestones with corals reported',40,22,-219741,2986253,'Greece','Europe',338,'',40.7333,22.9167,'','',5.43363894962,34.8091144561,5.43363894962,34.8091144561,0.373706372798,28.5354461384,-5.56201,28.8671,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mürztal Alps, Styria',2985,'Lechkogel','Triassic','Upper Triassic','Carnian','Julian',227.00,237.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',224,3,'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','0',NULL,'','Unknown','2','Below fair weather wave base','6','Calcisponges','9','Tubiphytes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','80','20',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',2093,40,'Deeper water mixed siliciclastic-carbonate ramps.\nHighly diverse biota composed of sphinctozoans, inozoans, Tubiphytes, Plexoramea and various red algae',47,15,2504265,2265609,'Austria','Europe',301,'',47.5333,15.6333,'WAHR','60053',15.6122385646,35.7352603423,15.6122385646,35.7352603423,15.7914256051,16.7085320869,14.037,22.219,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),