('Saint-Gaultier, Creuse Valley',3923,'','Jurassic','Middle Jurassic','Bathonian','lower Bathonian',166.10,168.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',166,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species','42',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2770,0,'Peri-reefal environment\ncorallian and reefal limestones and lagoonal facies',46,1,4430113,827570,'France','Europe',331,'',46.6333,1.4167,'WAHR','85965',24.6638145316,22.9215456974,24.6638145316,22.9215456974,29.8543855188,23.0586422717,36.118,11.991,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dnipropetrovsk',3924,'Mandrikovka','Paleogene','Eocene','Priabonian','Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',35,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','','Unknown',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,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',2771,0,'Perireef environment. z and az corals',48,34,6092661,2646420,'Ukraine','Europe',301,'',48.45,34.9833,'WAHR','77068',47.6677829784,28.7521084436,47.6677829784,28.7521084436,46.6173913695,33.9194684888,47.8942,30.4547,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lyubasha Mountain, Lyalintsi',3925,'Slivnitsa','Cretaceous','Lower Cretaceous','Berriasian','Berriasian',139.80,145.00,22,'late Tithonian - early Valanginian',141,140,'Early Cretaceous (Berriasian, 142.4 Ma)',143,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'0','90','10',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','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2772,0,'Stacked coral biostromes. Corals, Tubiphytes, microbial carbonates and Parachaetetes reported ',42,22,2949469,2220766,'Bulgaria','Europe',319,'',42.7667,22.75,'WAHR','87068',26.5028846157,35.7297486824,26.5028846157,35.7297486824,31.3742204781,37.1065871296,24.7808,25.1698,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lyubasha Mountain II, Lyalintsi',3926,'Slivnitsa','Cretaceous','Lower Cretaceous','Valanginian','Valanginian',132.90,139.80,23,'late Valanginian - early Aptian',126,135,'Early Cretaceous (Valanginian, 136.4 Ma)',139,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'0','90','10',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','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2772,0,'see reef 3925',42,22,2949469,2231391,'Bulgaria','Europe',319,'',42.7667,22.75,'WAHR','87070',27.6406766392,35.7211211882,27.6406766392,35.7211211882,31.878367684,36.2378834107,24.144,25.396,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sass da Putia buildup',3927,'Sciliar Dolomite','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',230,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','2','Algae','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1','Red algae','0','90','10',0,'no',0,'no','2','6 to 24 reef building species','10','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'1','Present',0,'No or unknown reservoir potential',2773,0,'megabreccia horizons with Tubiphytes/Bacinella wackestones/packstones, Porostromata bindstones, solenoporacean bafflestones/framestones, sphinctozoan bafflestones/bindstones, coral framestones',46,11,1389607,2345525,'Italy','Europe',344,'',46.6667,11.8833,'WAHR','87098',16.6161181849,35.2040231095,16.6161181849,35.2040231095,10.3658374019,23.544138115,7.84021,22.5136,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baingoin region, Tibet',3928,'Pakong','Jurassic','Upper Jurassic','Oxfordian','Oxfordian/Kimmeridgian',157.30,157.30,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species','21','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2774,0,'Only corals described\nPlatfrom margin reefs indicated\nLate Oxfordian to early Kimmeridgian',31,90,2763731,9447434,'China','Asia',602,'',31.3333,90.15,'WAHR','80571',40.0191564842,100.474307068,40.0191564842,100.474307068,20.0245617556,102.977814767,14.5962,85.594,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Corozal, Puerto Rico',3929,'Coamo','Paleogene','Paleocene','Danian','Danian',61.60,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',64,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','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',NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2775,0,'lenticular fossiliferous limestones, reef and near-reef accumulations\nAge disputed.',18,-66,2364789,-6746436,'United States','North America',101,'',18.3333,-66.3167,'WAHR','87547',18.9555618459,-58.4626182861,18.9555618459,-58.4626182861,21.3510636404,-61.3654322336,17.0928,-61.8998,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gebel Zeit',3930,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae',NULL,NULL,NULL,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',2776,0,'',27,33,3773366,3450122,'Egypt','Africa',715,'',27.9333,33.5,'WAHR','87873',27.92535458,33.4877347472,27.9276248057,33.4912389254,27.9245373513,33.4969296724,27.9309,33.4971,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ras Gemsa',3931,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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',NULL,NULL,NULL,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,NULL,NULL,'0','',0,'No or unknown reservoir potential',2776,0,'scleractinian framestone and/or bafflestone, sandy algal bindstone, sandy bioclastic wackestone',27,33,3736275,3464303,'Egypt','Africa',715,'',27.65,33.5833,'WAHR','87876',27.6420616277,33.5710592821,27.6443298399,33.574556452,27.6412303,33.5801923102,27.6476,33.5804,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chuo-Morioka quarries, central Okinawa',3932,'Sobe','Quarternary','Pleistocene','Pleistocene','lower-middle Pleistocene',0.80,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae',NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species','22','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2777,0,'Upper reef slope',26,127,3571061,13268095,'Japan','Asia',625,'',26.3914,127.7308,'WAHR','87892',26.5876691994,127.493397324,26.6504777995,127.417856628,26.3758802361,127.399914497,26.5119,127.553,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kochinda area, S Okinawa',3933,'Naha','Quarternary','Pleistocene','Pleistocene','lower-middle Pleistocene',0.80,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae',NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species','24','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2777,0,'',26,127,3530512,13284992,'Japan','Asia',625,'',26.0833,127.6833,'WAHR','87984',26.2803067862,127.440198782,26.343366852,127.36284661,26.0686508942,127.345864709,26.2034,127.509,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kikai Island, Ryukyu',3934,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','45',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae',NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species','28','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2777,0,'ESR dating of corals\nKawamine terrace 20-80 m elevation.',28,129,3821320,13356703,'Japan','Asia',625,'',28.3,129.9667,'WAHR','88039',28.3573423762,129.896829019,28.3567111837,129.897597434,28.2854531958,129.889785183,28.3376,129.914,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ovciarsko',3935,'','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 ',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)','1','Above fair weather wave base','2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','40','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',519,0,'reef limestone blocks in Lutetian conglomerates',49,18,6427193,1591016,'Slovakia','Europe',336,'',49.2333,18.6667,'WAHR','88186',45.2028866798,18.5988971282,45.2028866798,18.5988971282,46.0751090727,17.8733111422,40.1426,19.4618,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Isla Coronados + Isla Carmen, Baja California',3936,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,'0','70','30',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2778,2810,'Porites reefs developed on andesite boulders',26,-111,3530512,-11578631,'Mexico','North America',105,'',26.0833,-111.2833,'WAHR','88573',26.055351558,-111.224713269,26.0633374914,-111.241451271,26.0772452128,-111.254846234,26.0812,-111.267,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cape Range',3937,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','19','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2779,0,'Fringing reef',-21,114,-2962806,12120439,'Australia','Oceania',801,'',-21.8,114.1167,'WAHR','88574',-21.8338349862,114.095181754,-21.8241679467,114.101330975,-21.8343281289,114.10285948,-21.8332,114.101,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Red Bluff, Lake Macleod',3938,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','21','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2779,0,'',-24,113,-3261914,11920977,'Australia','Oceania',801,'',-24.05,113.4,'WAHR','88576',-24.083717121,113.377866558,-24.074083776,113.384191645,-24.0842310948,113.385618693,-24.083,113.383,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('East Wallabi Island, Houtman-Abrolhos Islands',3939,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','15',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2779,0,'',-28,113,-3838737,11677572,'Australia','Oceania',801,'',-28.4333,113.7167,'WAHR','88593',-28.4670697666,113.693750705,-28.4574213899,113.700309027,-28.467574574,113.701662524,-28.4664,113.699,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Leander Point',3940,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2779,0,'',-29,114,-3947437,11743886,'Australia','Oceania',801,'',-29.2667,114.9333,'WAHR','88594',-29.3006626764,114.910574898,-29.2909591634,114.917069131,-29.3011320408,114.918524093,-29.3001,114.916,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('N Kikai Island',3941,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','29','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2780,0,'5 reef complexes: ~66, ~64, ~62, ~55 and ~52 ka, Oxygen Isotope Stages 3-4\ncoral framestone, coral bindstone/bafflestone, coral and rhodolith floatstone/bindstone, coral framestone/floatstone, coral floatstone/rudstone',28,130,3825672,13359243,'Japan','Asia',625,'',28.3333,130.0167,'WAHR','88595',28.3420690938,130.005996439,28.3395631712,130.00905487,28.3316512412,130.008174802,28.3375,130.011,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Plimiri, Rhodes Island',3942,'Lindos Acropolis','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m','450',NULL,NULL,1,'Temperate','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','2','Algae','2','Algae','29','Coralline algae only (some corals)','1','Red algae','0','0','100',0,'no',0,'no','1','Less than 6 reef building species','5','3','Binder 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',2782,0,'Titanoderma, Lithophyllum, Tenarea as corallines, Halimeda, Cladocora',35,27,4801937,2715388,'Greece','Europe',338,'',35.9167,27.8333,'WAHR','88773',35.9149278951,27.8202562017,35.9154344429,27.8239831784,35.9131831494,27.8314802657,35.9146,27.831,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ambergris Cay, barrier-reef',3943,'Ambergris Cay Limestone','Quarternary','Pleistocene','Pleistocene','late Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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','10','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2783,0,'Thickness unclear. Reef only partially exposed.\nCoralline algae and Halimeda.\nIncludes isolated patch reefs in coll. 88825\n',18,-87,2469375,-9462906,'Belize','North America',NULL,'',18.1167,-87.8167,'WAHR','88824',18.1140217146,-87.8050112344,18.1147874696,-87.8083507496,18.1234970053,-87.8076184432,18.1184,-87.8064,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Twin Cays, Porites patches',3944,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','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','6','1','Constructor guild','1','Present','1','Present',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',2784,0,'Porites patches in lagoonal environments. Some Halimeda',16,-88,2294229,-9535447,'Belize','North America',NULL,'',16.8167,-88.1,'WAHR','88826',16.8140727622,-88.0885644338,16.814823928,-88.0918316117,16.8235250332,-88.0910703678,16.8185,-88.0898,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tuturinguen Point, Palawan Island',3945,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals',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',2785,0,'',10,118,1396424,13093668,'Philippines','Asia',563,'',10.2,118.9167,'WAHR','88866',10.2086326751,118.909596053,10.2061660766,118.91162595,10.1984211538,118.909757236,10.2001,118.919,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mactan Island',3946,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals',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',2785,0,'Poor description',10,124,1412335,13652111,'Philippines','Asia',563,'',10.3167,124.0167,'WAHR','88867',10.3012850478,124.024516435,10.3056828878,124.022280617,10.2868758285,124.04177028,10.3154,124.026,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Panglao Island, MIS 7',3947,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals',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',2785,0,'Poor description of reef facies',9,123,1312308,13647162,'Philippines','Asia',563,'',9.5833,123.8,'WAHR','88868',9.48630817332,123.844199017,9.4873591507,123.843707489,9.31397152874,124.034789537,9.57182,123.884,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Panglao Island, MIS 5',3948,'','Quarternary','Pleistocene','Pleistocene','late Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals',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',2785,0,'Poor description. Two OI substages recognized by radiometric dating. MIS 5c and 5e',9,123,1307764,13642475,'Philippines','Asia',563,'',9.55,123.75,'WAHR','88869',9.53497280413,123.756682727,9.53925967978,123.754770785,9.51987564598,123.775985693,9.54872,123.759,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Great Inagua Island',3949,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals',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',2786,0,'MIS 7 193-141 ka,',21,-73,2858246,-7851992,'Bahamas','North America',NULL,'',21.0167,-73.6833,'WAHR','88948',20.9833633274,-73.6059550098,20.983730773,-73.6068044347,21.0634280372,-73.5934556085,21.0235,-73.5935,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Great Inagua Island, Devils Point',3950,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals',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',2787,0,'Well developed patch reef',21,-73,2858246,-7855552,'Bahamas','North America',NULL,'',21.0167,-73.7167,'WAHR','89418',21.0115900149,-73.7047934039,21.013050504,-73.7081950581,21.0219075136,-73.7067239209,21.0175,-73.7067,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Papeete, cores P7, P8, Tahiti',3951,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'1','Seismic data available ',1,'True reef','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','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'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',2788,0,'Reef-flat of barrier reef (atoll)',-17,-149,-2390834,-16149603,'French Polynesia','Pacific',983,'',-17.5333,-149.5667,'WAHR','88958',-17.5482976507,-149.530626968,-17.5482976507,-149.530626968,-17.5333,-149.5667,-17.9604,-148.786,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grape Bay, patch reefs',3952,'Rocky Bay','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','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','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',2789,0,'Patch reefs',32,-64,4335879,-6490748,'Bermuda','Atlantic',101,'',32.2667,-64.7667,'WAHR','89150',32.2601975481,-64.7530565539,32.2620558691,-64.7569542956,32.2667,-64.7667,32.267,-64.7559,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kabola Peninsula, Alor Island',3953,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2790,0,'MIS 7',-8,124,-1118872,13760754,'Indonesia','Asia',614,'',-8.1667,124.5333,'WAHR','89160',-8.11467563216,124.489637784,-8.11524761773,124.490117876,-8.18957387584,124.505872487,-8.15253,124.599,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kabola Peninsula, Alor Island',3954,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2790,0,'MIS 5 c, e',-8,124,-1118872,13760754,'Indonesia','Asia',614,'',-8.1667,124.5333,'WAHR','89161',-8.1586997179,124.526586179,-8.16098564153,124.528504541,-8.16924441146,124.530251868,-8.16515,124.541,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Torres Islands, Hiu Island',3955,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2791,0,'terrace at 82 m asl on the W coast and 74 m asl on the E coast, 118-102 ka (Th/U)',-13,166,-1795601,18219110,'Vanuatu','Oceania',827,'',-13.1333,166.55,'WAHR','89163',-13.1559144664,166.580347693,-13.1494525052,166.571675086,-13.1481224745,166.585793799,-13.184,166.553,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Torres Islands, Tegua Island',3956,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2791,0,'terrace at 34 m asl on the E coast of Hiu, 164 ka (Th/U)\nTegua: 180 and 137 ka (Th/U)',-13,166,-1811447,18221032,'Vanuatu','Oceania',827,'',-13.25,166.6167,'WAHR','89164',-13.3973256721,166.81392711,-13.3957052285,166.811755616,-13.3834008387,166.93897412,-13.7066,166.648,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Torres Islands, Loh and Toga Islands',3957,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2791,0,'Loh: terrace at 90-120 m asl, 135 and 122 ka (Th/U)\nToga: terraces at 55 and 76 m asl, 80 and 112-103 ka (Th/U)',-13,166,-1836331,18219773,'Vanuatu','Oceania',827,'',-13.4333,166.6833,'WAHR','89166',-13.4559804569,166.713503226,-13.4494996587,166.704871877,-13.448127606,166.719089753,-13.4841,166.687,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Santo Island, Tomebou',3958,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2791,0,'terrace at 41 m asl near Tomebou, 38-37 ka (Th/U)\nIncludes poorly dated Malo Island reef',-15,167,-2125387,18147886,'Vanuatu','Oceania',827,'',-15.5667,167.0167,'WAHR','89168',-15.5895447903,167.04581343,-15.5830171198,167.037493316,-15.5815400881,167.052426855,-15.6175,167.02,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Malakula Island, Npenanavet, Malua, Walarno',3959,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2792,2793,'1. 66-47 ka (U/Th)\n2. 72 ka (U/Th)',-16,167,-2183960,18140198,'Vanuatu','Oceania',827,'',-16,167.1667,'WAHR','89231',-16.0229185424,167.195600086,-16.016369822,167.187340901,-16.0148455405,167.202420833,-16.0509,167.169,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Malakula Island, Tisman Bay',3960,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2793,0,'98 ka (U/Th)',-16,167,-2224486,18179208,'Vanuatu','Oceania',827,'',-16.3,167.6833,'WAHR','89233',-16.3231714964,167.712100982,-16.3165505473,167.703870096,-16.3148635405,167.719048308,-16.351,167.686,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Malakula Island, Lambubu Bay',3961,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2793,0,'terrace at 60 m, 75 ka (U/Th)',-16,167,-2206482,18152485,'Vanuatu','Oceania',827,'',-16.1667,167.3667,'WAHR','89234',-16.1897166882,167.395534559,-16.1831399444,167.387294086,-16.1815526523,167.402429365,-16.2176,167.369,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Core CR 14, offshore Irabu Island',3962,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','15','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','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,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2794,0,'glacial reef: \nmounded structure in unit 2, 8-24.4 mbsf, 30-22 ka (Th/U)\nsmall-scaled coral reef at a water depth of ~126 m formed during the lowstand stage of MIS 3-2',24,125,3352736,13102377,'Japan','Asia',625,'',24.7361,125.0586,'WAHR','89236',24.7520786333,125.051468098,24.747513177,125.053507943,24.7392843584,125.053264127,24.7388,125.054,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mogadishu coast',3963,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2795,0,'Fringing reef: 31-105 ka (unpublished Th/U dating)',2,45,283491,5042559,'Somalia','Africa',709,'',2.0667,45.3667,'WAHR','89242',2.0614975497,45.3528048009,2.06298420053,45.3567748227,2.05738581327,45.3589510193,2.06332,45.3596,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kisimayo',3964,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2795,0,'',0,42,48014,4729467,'Somalia','Africa',709,'',0.35,42.5333,'WAHR','89243',0.344252655091,42.5197408172,0.345894973314,42.5236148324,0.340720819326,42.5255394676,0.346673,42.5262,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Praslin, La Digue, Curieuse Islands',3965,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2796,0,'coralgal buildups, 2.5 m max. thickness, 1-5 m² in area, Acropora-dominated association, with abundant Leptastrea\n140-120 ka (Th/U) last interglacial stage',-4,55,-591960,6186454,'Seychelles','Africa',NULL,'',-4.3167,55.7333,'WAHR','89247',-4.32222269947,55.7241667288,-4.32064466355,55.7267761676,-4.32664910923,55.7275653577,-4.32056,55.7257,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Toliara, TU S1, S2 cores',3966,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','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,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2797,0,'boreholes on the outer reef flat of the \'Grand Recif\', 250 m behind the reef front in the Toliara area\n124-118 ka',-23,43,-3175701,4601073,'Madagascar','Africa',702,'',-23.4,43.6333,'WAHR','89248',-23.4069694559,43.6262689426,-23.4049781056,43.6282777631,-23.4094804755,43.6262520471,-23.4033,43.6257,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mayotte slope, Indian Ocean',3967,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2797,0,'glacial reef at foreslope of Mayotte',-12,45,-1750328,4943103,'France','Europe',331,'',-12.8,45.15,'WAHR','89249',-12.8068039356,45.1417433557,-12.8048598607,45.1441023388,-12.8,45.15,-12.8034,45.1427,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fagal-Obock-Tadjoura-Sarrey',3968,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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)','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',2798,0,'130-118 ka (Th/U)',12,43,1650642,4759798,'Djibouti','Africa',NULL,'',12.0667,43.4,'WAHR','89257',12.0519825718,43.3825473059,12.0561875727,43.3875337513,12.0667,43.4,12.0634,43.3931,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kahuku Point, Oahu, Hawaii',3969,'Waimanalo','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2799,0,'121-113 ka, last interglacial',21,-158,2938357,-16801658,'United States','North America',101,'',21.6167,-158.0667,'WAHR','89290',21.6019037632,-158.02957316,21.6019037632,-158.02957316,21.6167,-158.0667,21.5943,-158.032,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kaena Point, Oahu, Hawaii',3970,'Waimanalo','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2799,0,'127-115 ka, last interglacial',21,-158,2931686,-16826516,'United States','North America',101,'',21.5667,-158.2667,'WAHR','89292',21.5519124477,-158.229555245,21.5519124477,-158.229555245,21.5667,-158.2667,21.1184,-157.582,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Oahu, Mokapu and Hahaione, Hawaii',3971,'Waimanalo','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',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',2799,0,'',21,-157,2916112,-16776379,'United States','North America',101,'',21.45,-157.7167,'WAHR','89294',21.4351889993,-157.679616954,21.4351889993,-157.679616954,21.45,-157.7167,21.4276,-157.682,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Haleakala Ridge, offshore Maui, Hawaii',3972,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2800,0,'dredge 32 (1555-1705 m depth), reef terrace 1 (shallowest and youngest terrace), 750 ka',20,-155,2815911,-16611895,'United States','North America',101,'',20.7,-155.6833,'WAHR','89410',20.5658677992,-155.351908276,20.5658677992,-155.351908276,20.7,-155.6833,20.5004,-155.377,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Offshore Lanai, Hawaii',3973,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','2','Algae','2','Algae','29','Coralline algae only (some corals)','1','Red algae','0','10','90',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',2801,0,'algal-dominated mounds at fore-reef slope during glacial',20,-156,2811457,-16722652,'United States','North America',101,'',20.6667,-156.7,'WAHR','89415',20.6518492488,-156.66305341,20.6518492488,-156.66305341,20.6667,-156.7,20.6444,-156.666,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lifou, Loyalty Islands, Melanesia',3974,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2802,0,'terrace at 3.5 m, exact locations on Lifou Island unknown',-20,167,-2840418,17829130,'New Caledonia','Pacific',NULL,'',-20.8833,167.2167,'WAHR','89423',-20.9109757483,167.207088549,-20.9030683843,167.209833663,-20.9099383907,167.214631361,-20.9133,167.213,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ouvea, Loyalty Islands, Melanesia',3975,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2802,0,'terrace at 7.5 m, 117 ka (Th/U)',-20,167,-2840418,17829130,'New Caledonia','Pacific',NULL,'',-20.8833,167.2167,'WAHR','89422',-20.9109757483,167.207088549,-20.9030683843,167.209833663,-20.9099383907,167.214631361,-20.9133,167.213,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Beautemps-Beaupre, Loyalty Islands, Melanesia',3976,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2802,0,'terrace at 2m, small island Beautemps-Beaupre WNW of Ouvea, Loyalty Island\n>200 ka (Th/U)',-20,166,-2778012,17747306,'New Caledonia','Pacific',NULL,'',-20.4167,166.1333,'WAHR','89421',-20.4447779969,166.123291943,-20.4367556876,166.126150401,-20.443767213,166.130829007,-20.447,166.129,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Amedee 4 core, off Noumea',3977,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',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','60','40',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2803,0,'coral framestone interbedded with layers of grainstones/packstones rich in molluscs, echinids, foraminifers\nunit 7: 46-52 m, 410-250 ka, MIS 11?\nunit 8: 40-46 m, ~278 ka, MIS 9?',-22,166,-3053840,17627510,'New Caledonia','Pacific',NULL,'',-22.4833,166.4667,'WAHR','89432',-22.6650061148,166.407957755,-22.663009374,166.408600906,-22.7257209956,166.45398522,-22.7554,166.439,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Amedee 4 core, off Noumea',3978,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',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','60','40',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2803,0,'Youngest reef level OIS 5',-22,166,-3053840,17627510,'New Caledonia','Pacific',NULL,'',-22.4833,166.4667,'WAHR','89435',-22.5112551225,166.457634417,-22.5032679563,166.460223535,-22.5102361012,166.46522795,-22.5135,166.464,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ile des Pins',3979,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',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',2804,0,'Ref. 2803 provides middle Pleistocene ages as well (unreliable).',-22,167,-3062717,17722808,'New Caledonia','Pacific',NULL,'',-22.55,167.4167,'WAHR','89436',-22.5776002742,167.407854626,-22.5697145041,167.410380811,-22.5765580339,167.415442963,-22.5799,167.414,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Urelapa Island',3980,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','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',NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2805,0,'glacial reef\nbranching coral facies of Acropora, various small coral buildups including favids and encrusting coralline algae\n\'keep-up\' reef growth mode; medium- to high-energy conditions close to the sea surface (reef crest or upper fore-reef slope)',-15,167,-2132148,18145155,'Vanuatu','Oceania',827,'',-15.6167,167.0167,'WAHR','89441',-15.6395447837,167.04578688,-15.6330171165,167.037474348,-15.631540088,167.052424877,-15.6675,167.02,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Salt Rocks, Little Cayman, Cayman Islands',3981,'Ironshore','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'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','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','80','20',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2806,0,'',19,-80,2675313,-8582622,'United Kingdom','Europe',331,'',19.65,-80.1,'WAHR','89553',19.6459611936,-80.0881648204,19.6471156529,-80.0915461141,19.6559722345,-80.0904410033,19.6513,-80.0895,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tiarei outer ridge, Tahiti',3982,'','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',1,2,'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','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','60','40',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',2807,0,'coralgal frameworks associated with coral rudstone-floatstone and skeletal limestone (unit IIa); sandy packstones/grainstones and volcaniclastic siltstones and sandstones with coral fragments (units IIb-d)',-17,-149,-2381862,-16135260,'French Polynesia','Pacific',983,'',-17.4667,-149.4,'WAHR','89554',-17.8576373771,-148.461000636,-17.8576373771,-148.461000636,-17.4667,-149.4,-18.0208,-148.384,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maraa western transect, Tahiti',3983,'','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',1,2,'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','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,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2807,0,'coralgal frameworks associated with rudstone-floatstones; floatstone-rudstone rich in rhodoliths and coral fragments; sandy skeletal grainstone-packstones',-17,-149,-2422267,-16136661,'French Polynesia','Pacific',983,'',-17.7667,-149.5667,'WAHR','89555',-18.1576319592,-148.628077247,-18.1576319592,-148.628077247,-17.7667,-149.5667,-18.3214,-148.549,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Faaa, Tahiti',3984,'','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',1,2,'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','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','60','40',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',2807,0,'',-17,-149,-2393084,-16154081,'French Polynesia','Pacific',983,'',-17.55,-149.6167,'WAHR','89556',-17.9409296879,-148.678176387,-17.9409296879,-148.678176387,-17.55,-149.6167,-17.9773,-148.836,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mitiaro',3985,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2808,0,'A lower reef unit is also present (middle Pleistocene?)',-19,-157,-2697658,-16888248,'Cook Islands','Pacific',NULL,'',-19.8167,-157.7167,'WAHR','89568',-19.8315109637,-157.681403598,-19.8315109637,-157.681403598,-19.8167,-157.7167,-19.8391,-157.678,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Atiu',3986,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2808,0,'',-19,-158,-2719982,-16920053,'Cook Islands','Pacific',NULL,'',-19.9833,-158.1167,'WAHR','89569',-20.1166221859,-157.799374326,-20.1166221859,-157.799374326,-19.9833,-158.1167,-20.1851,-157.773,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mauke',3987,'','Quarternary','Pleistocene','Pleistocene','middle/late Pleistocene',0.00,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2808,0,'2 reefal units:\nlower unit: 243-204 ka (MIS 7); upper unit: 136-119 ka (MIS 5e)',-20,-157,-2742309,-16825149,'Cook Islands','Pacific',NULL,'',-20.15,-157.3333,'WAHR','89570',-20.2687445089,-157.050707322,-20.2687445089,-157.050707322,-20.15,-157.3333,-20.3288,-157.027,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kish Island, Persian Gulf',3988,'','Quarternary','Pleistocene','Pleistocene','middle/late Pleistocene',0.00,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',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','33','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2809,0,'252-213 (MIS 7) and 148-100 ka (MIS 5) (ESR and Th/U dated)',26,53,3589723,5601528,'Iran','Asia',505,'',26.5333,53.9667,'WAHR','89571',26.4363796107,53.8836729964,26.4351524451,53.8826221724,26.3893489451,53.8990147384,26.4469,53.9031,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Qeshm Island, Persian Gulf',3989,'','Quarternary','Pleistocene','Pleistocene','late Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',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',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',2809,0,'138-115 ka (MIS 5) (ESR and Th/U dated)',26,56,3648846,5820744,'Iran','Asia',505,'',26.9833,56.2167,'WAHR','89572',26.965678106,56.2017530153,26.9707131054,56.2060234912,26.9648027009,56.2080097875,26.972,56.2087,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Punta San Telmo, Baja California',3990,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','80','20',0,'no',0,'no','1','Less than 6 reef building species','5','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2810,0,'reef facies (mainly Porites) above conglomerates with molluscs and corals, sandy near-reef facies',25,-110,3427240,-11591153,'Mexico','North America',105,'',25.3,-110.95,'WAHR','89597',25.272105769,-110.891334541,25.2800761992,-110.908095072,25.2940794166,-110.921174864,25.298,-110.934,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Santa Maria Island, Azores',3991,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','2','Shelf or Platform margin','2c','Atoll (circular structure)','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','1','Less than 6 reef building species','4','3','Binder guild','1','Present','1','Present','1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2811,0,'Red algal biostrome. MIS 5.5\nshallow depths, probably less than 10 m',36,-25,4934563,-2428135,'Portugal','Europe',304,'',36.9667,-25.1,'WAHR','89618',36.9587692529,-25.109651565,36.9610353764,-25.1068939698,36.9667,-25.1,36.9667,-25.1021,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Loma de San Jua, Michoacan',3992,'','Cretaceous','Lower Cretaceous','Aptian','lower Aptian',120.00,125.00,23,'late Valanginian - early Aptian',126,120,'Early Cretaceous (early Aptian, 121.8 Ma)',122,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','9',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','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','14','1','Constructor guild','1','Present','1','Present','2','Medium zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2812,0,'coral boundstone bed, at least 9 m thick, above a rudist (Amphitriscoelus) rudstone bed (see reef 2489',18,-100,390908,-6324430,'Mexico','North America',105,'',18.5167,-100.9333,'WAHR','89846',15.1511860858,-52.7185307264,14.1204907484,-51.4158107761,16.4175534375,-57.338537946,17.7363,-57.4355,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chumbitaro, Guerrero',3993,'Mal Paso','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,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','19','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','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','16','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2812,0,'Late Albian - Early Cenomanian\nThe coral reef (MP 13) is about 19 m thick and\nprimarily composed of medium- to large-sized massive corals and sparsely distributed, medium- to large-sized phaceloid and ramose corals. Non-coral taxa found within this bed\ninclude abundant Pecten roemeri Hill, 1889, Radiolites cf. R. costata Scott, 1990, large nerineids, Mexicaprina alata Filkorn, 2002a, and massive colonies of the stromatoporoid\nActinostromaria sp.',18,-100,1689167,-6707540,'Mexico','North America',105,'',18.4833,-100.7,'WAHR','89857',17.5584676508,-62.3589936865,17.5584676508,-62.3589936865,19.4019962858,-67.2381072155,17.4386,-66.1481,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Godogani',3994,'','Cretaceous','Lower Cretaceous','Hauterivian','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',133,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'70','1971',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','90','0',0,'no',0,'no','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',2813,1184,'coral-stromatoporoid bioherm',42,42,4953869,3565151,'Georgia','Europe',301,'',42.2667,42.7667,'WAHR','89971',34.3444576915,51.8714799153,34.3444576915,51.8714799153,36.2360369233,52.2681665564,35.4962,48.3159,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mukhura, Dzirul Massif',3995,'','Cretaceous','Lower Cretaceous','Hauterivian','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',133,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'70','1971',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'5','95','0',0,'no',0,'no','3','25 or more reef building species','22','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2813,1184,'',42,43,4961422,3602013,'Georgia','Europe',301,'',42.3167,43.1,'WAHR','89974',34.4868424879,52.1228847079,34.4868424879,52.1228847079,36.3576497255,52.541408793,35.5823,48.6064,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Modinakhe',3996,'','Cretaceous','Lower Cretaceous','Hauterivian','Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',133,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'70','1971',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'10','90','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',2813,1184,'',42,42,4982808,3490862,'Georgia','Europe',301,'',42.5333,42.1833,'WAHR','89978',34.4220527053,51.2648308047,34.4220527053,51.2648308047,36.3616308676,51.6591661502,35.6963,47.7435,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bolshoy Zelenchuk River, Ispravnaya, Caucasus',3997,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','12',NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',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,NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species','42','1','Constructor guild','1','Present',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',2814,502,'',44,41,5039330,3861989,'Russia','Asia',624,'',44.0667,41.6,'WAHR','89995',32.7868049293,50.8425151613,32.7868049293,50.8425151613,37.0406308041,54.1606623021,38.2555,46.8215,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zhinvali-Aranisi + Kokh Mountain, Caucasus',3998,'','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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','17','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2814,0,'Kokh Mountain and Dzhvarisubani are unresolved late Oxfordian-Kimmeridgian.\nZhinvali-Aranisi is late Oxfordian',42,44,5026781,4124857,'Georgia','Europe',301,'',42.1,44.7833,'WAHR','90000',31.8839186516,54.9933702161,31.8839186516,54.9933702161,36.5387934193,58.3506447878,36.83,50.3808,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alkhashenda, Ribisa, Valkhokh',3999,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian/Kimmeridgian',157.30,157.30,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','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',2814,0,'unresolved late Oxfordian-Kimmeridgian.',42,43,5014225,4075400,'Georgia','Europe',301,'',42.45,43.7833,'WAHR','90002',32.1566730478,53.2846437782,32.1566730478,53.2846437782,36.0448633528,56.6396335771,36.9172,49.1018,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Korta, Racha Region',4000,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian/Kimmeridgian',157.30,157.30,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3999',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','50','1','Constructor guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2814,0,'unresolved late Oxfordian-Kimmeridgian.\nTaxonomic data from local area, probably oversplitted',42,43,5026781,4028706,'Georgia','Europe',301,'',42.5333,43.4167,'WAHR','90017',32.1032168846,52.9566397621,32.1032168846,52.9566397621,36.0210442202,56.2910889368,36.9529,48.7507,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Belaya-Pshekha Rivers, Caucasus',4001,'Lagonakskaya','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2017',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','18',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2814,0,'Coral reef boundstones, together with coral rudstones and floatstones. Massive and branching corals acted as the main component of vertical reef growth and provided the skeletons on which  abundant  microorganisms  and  microbialites  were    encrusted. The encrusting microorganisms (mainly   microproblematica) are identified as Bacinella-Lithocodium, Iberopora, Koskinobullina, Prismenproblematikum, Tubiphytesand serpulids, and  are heterogeneously distributed. Microbialites    are commonly encrusted. bioclastic  grainstones  have  been  observed in the reef matrix. Growth cavities are commonly developed and filled with early marine isopachous fibrous cement and occluded by blocky calcite cement. Tubiphytes and microbial fabrics overgrown corals.',44,39,5145741,3647919,'Russia','Asia',624,'',44.2167,39.85,'WAHR','90020',32.3352995986,49.4407746321,32.3352995986,49.4407746321,36.7088747394,52.6349825775,38.1893,45.2138,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ferques, Boulonnais',4002,'Ferques','Devonian','Upper Devonian','Frasnian','lower Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',382,3,'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','1c','Epeiric sea',NULL,NULL,'4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,'45','0','55',0,'no',0,'no','3','25 or more reef building species','26','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',2815,0,'Bois Member of the Freques formation. Largely biostromal\nasymmetricus zone',50,1,-2735613,304838,'France','Europe',331,'',50.8333,1.7667,'WAHR','38689',-22.7772982276,-13.9876029707,-22.7772982276,-13.9876029707,-4.0871881035,-69.2395317051,-22.2863,3.50434,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Penaguila, Valencia',4003,'','Paleogene','Eocene','Priabonian','Upper Eocene',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',35,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','15','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','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','2','Medium zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2817,0,'Coral reef developed in HST on top of deep shelf limestone sequence. \r\nBuried coral reef also inferred for between Ibi and Carrasqueta.\r\n\r\ncoralgal buildups interfingering with miliolid-rotaliid limestones. The top shows a thickening-up bedding pattern and consists of packstones and grainstones with exclusively rotaliids and some coral debris. The unit of pebbly rotaliid limestones with coralgal reefs is considered to represent a highstand prograding barrier with fore-reef, reef and interreef subenvironments.',38,0,4913552,-300298,'Spain','Europe',304,'',38.6833,-0.35,'',NULL,35.61908233,-4.37315732004,35.61908233,-4.37315732004,37.4332017848,-0.566951404357,37.2328,-3.40952,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Normandville II, Alberta',4004,'Pekisko','Carboniferous','Mississippian','Tournaisian','middle Tournasian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',357,3,'1','Seismic data available ',3,'Mud mound or bank','1','Less than 10 m thick','10',NULL,NULL,NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'70','0','30',0,'no',0,'no',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',2822,0,'Described as Waulsortian-type mud mounds (bryozoan-crinoidal).\nTwo facies in core: 1. fenestrate bryozoan facies with minor mud. 2. carbonate mud with minor bryozoans.',55,-117,795136,-4300755,'Canada','North America',121,'',55.8333,-117.4167,'FALSCH','0',-7.41693499972,-46.2301939611,-7.41693499972,-46.2301939611,14.1716121316,-95.8229874906,4.36784,-39.2203,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mulu Quarry, Gunung Mulu, Sarawak',4005,'Temburong','Neogene','Miocene','Lower Miocene','early Aquitanian',22.00,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',22,3,'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','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','60','40',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2823,0,'Reefal olistoliths in deepwater Temburong shales developed during backstepping of the platform',4,114,781444,13097662,'Malaysia','Asia',614,'',4.0333,114.9167,'','',4.28138087538,112.168692934,4.53258739722,112.485441513,-0.0212238767739,116.489278053,4.93717,118.442,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tazhong oil field, Tarim',4006,'Lianglitag','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',456,1,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','20','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','1','Red algae','50','30','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',2824,0,'age indicated as early late Ordovician.\nCorals, stromatoporoids, solenoporaceans and calcimicrobes as reef builders.\nLargest oil field in China. oil in reef-flat and grainstones.\nReef facies in well Tazhong-30: Reef mounds are coral framestones coral bafflestones in 10-20 m thick horizons. Mud mounds are up to 30 m thick.',39,84,342914,12502173,'China','Asia',602,'',39.25,84.6667,'','',-4.61406847865,60.6266019359,-4.61406847865,60.6266019359,-4.61406847865,60.6266019359,-32.4487,120.203,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Goznitsa, Lovech',4007,'Smochan','Cretaceous','Lower Cretaceous','Barremian','upper Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',126,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild','1','Present',NULL,NULL,'1','Low 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',2826,2827,'Small biostromes and patch reefs in lagoonal marls, siltstones and sandstones.\n\nThey are built of colonial corals, faceloid and dendroid, adapted to a soft substratum (clayey bottom). They are preserved in the rock in situ, the dimensions of the colonies varying from several centimeters to several tens of centimeters.\nMassive colonies dominate the central parts, and dendroid corals, the peripheries.',43,24,2635077,2247345,'Bulgaria','Europe',319,'',43.15,24.6833,'WAHR','91679',31.5600172617,37.0119886761,31.5600172617,37.0119886761,34.4244036631,35.9389966621,34.2605,32.6923,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Veliko Tarnovo',4008,'Emen','Cretaceous','Lower Cretaceous','Barremian','lower Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',128,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals',NULL,NULL,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',2828,0,'Corals described from underlying marls, siltstones and sandstones (Balgarene Formation).\nReefs in Emen Fm.',43,25,2614948,2313019,'Bulgaria','Europe',319,'',43.0667,25.6167,'WAHR','85417',31.6909762457,37.803426605,31.6909762457,37.803426605,34.5102983309,36.7651445338,22.0443,28.0854,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mare Island',4009,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',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','3','25 or more reef building species','41','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2833,0,'',-21,167,-2927229,17851474,'New Caledonia','Pacific',NULL,'',-21.5333,167.8833,'WAHR','90042',-21.5607232913,167.874096208,-21.552888075,167.87672482,-21.559669763,167.88165242,-21.5631,167.88,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mare Island',4010,'','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',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','3','25 or more reef building species','41','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2833,0,'',-21,167,-2916112,17868441,'New Caledonia','Pacific',NULL,'',-21.45,167.9833,'WAHR','90061',-21.9566058877,167.81435889,-21.9585618025,167.813713446,-22.1345246522,167.944702169,-22.2229,167.904,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Castrojimeno',4011,'Hortezuelos','Cretaceous','Upper Cretaceous','Coniacian','upper Coniacian',86.30,89.80,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',86,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','8','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','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','5','1','Constructor guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2834,0,'segment reefs, spaced and close cluster reefs and close cluster/frame reefs with oligospecific or monospecific rudist assemblages, and bioclastic beds\n5 rudist species (Radiolitidae and Hippuritidae).',41,-3,3919205,-20463,'Spain','Europe',304,'',41.4,-3.8333,'WAHR','91495',34.2472816533,0.893935232648,34.2472816533,0.893935232648,34.4024203587,-1.01984236473,30.8446,-1.22866,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fucheng, Shaanxi',4012,'Xiannudong','Cambrian','Series 2','Stage 3','Atdabanian/Botomian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',519,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','7','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2835,0,'Upper Atdabanian-Lower Botomian\nsix microbial reef complexes; 1.1-12.5 m thick, laterally extensive; irregular archaeocyaths comprise max. 3.7% of the reefs and were not involved in reef construction.\nMostly in inter-reef settings.',32,107,3056063,15903806,'China','Asia',602,'',32.4667,107.2333,'WAHR','91498',-6.6123751032,80.6738618772,-4.532383383,78.1221076725,-4.532383383,78.1221076725,26.5929,164.178,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Novo Selo',4013,'Emen','Cretaceous','Lower Cretaceous','Barremian','lower Barremian',125.00,129.40,23,'late Valanginian - early Aptian',126,125,'Early Cretaceous (Barremian, 127.2 Ma)',128,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,'4008',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals',NULL,NULL,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',2828,2826,'reefal limestones (Emen Formation) separated by lagoonal marls, siltstones and sandstones (Balgarene Formation)',43,25,2621659,2301852,'Bulgaria','Europe',319,'',43.0833,25.3667,'WAHR','91676',31.6501847942,37.5933722296,31.6501847942,37.5933722296,34.4815354288,36.5454097266,34.2372,33.3005,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Derbent, SW Gissar Range',4014,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian/Kimmeridgian',157.30,157.30,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals',NULL,NULL,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',2836,0,'late Oxfordian - lower Kimmeridgian',38,67,5400412,6103758,'Uzbekistan','Asia',301,'',38.2,67.0167,'WAHR','91788',37.2975300856,74.5252617879,37.2975300856,74.5252617879,39.0224968663,79.2837785526,36.0795,71.7128,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kugitang',4015,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian/Kimmeridgian',157.30,157.30,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'0','Outcropping reef ',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,'',37,66,5427573,6149023,'Uzbekistan','Asia',301,'',37.9667,66.7333,'WAHR','91829',36.9827203223,74.4358261655,36.9827203223,74.4358261655,38.7202098273,79.1384013904,35.8065,71.5001,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Flank of theSchulterkofel, Carnic Alps, Ringmauer area',4068,'Grenzland, Upper Pseudoschwagerina Limestone','Carboniferous','Pennsylvanian','Gzhelian','upper Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20','2','10 - 100 m wide','30',NULL,NULL,'100',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','3','Below storm wave base','2','Algae','3','Microbes','49','Algae - microbes - stromatoporoids - (corals) - (bryozoans)','2','Green algae',NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','7',NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',2915,NULL,'',NULL,NULL,NULL,NULL,'Austria','Europe',NULL,NULL,46.35,13.1,NULL,NULL,-11.5635825947,28.7302399619,-11.5635825947,28.7302399619,-7.99909148279,4.01161802865,-11.1606,23.4863,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Son Sastre, Mallorca',4016,'Son Sastre','Paleogene','Oligocene','Rupelian','lower Rupelian',30.00,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',32,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','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','2','6 to 24 reef building species','14','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2837,0,'coral patches and small patch-reefs probably in a lagoonal environment\nSon Satre sandstone and Lutites Fm.',39,2,5264111,-75656,'Spain','Europe',304,'',39.5439,2.9675,'WAHR','92080',37.9143713444,-2.54599445497,37.8641630229,-2.54331907699,38.9204679651,2.10218399466,39.7842,-1.03404,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Guppy Hills, Canning Basin',4017,'Pillara','Devonian','Upper Devonian','Frasnian','lower Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',382,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2838,0,'corals as a mound, 2.5 m wide, in deeper subtidal back-reef environment\nOtherwise only biostromes are devloped',-18,126,-2802536,12991060,'Australia','Oceania',801,'',-18.2167,126.1333,'WAHR','92875',-24.0315856567,114.246213665,-24.0315856567,114.246213665,-31.1040086463,156.734486758,-18.752,127.258,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Napier Range, Canning Basin',4018,'Pillara','Devonian','Upper Devonian','Frasnian','late Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',376,3,'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','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2838,0,'Back-reef environment',-17,124,-2671291,12832556,'Australia','Oceania',801,'',-17.1333,124.7,'WAHR','92885',-23.6341315822,112.390719106,-23.6341315822,112.390719106,-31.5784451568,154.77051535,-18.225,125.506,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dingo Gap, Napier Range, Canning Basin',4019,'Napier','Devonian','Upper Devonian','Frasnian','latest Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',375,3,'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','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','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',2838,0,'sponge/coral bioherms',-17,124,-2671291,12832556,'Australia','Oceania',801,'',-17.1333,124.7,'WAHR','92896',-23.6341315822,112.390719106,-23.6341315822,112.390719106,-31.5784451568,154.77051535,-18.225,125.506,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Neuvelle-les-Champlitte, Franche-Comte',4020,'unknown','Jurassic','Upper Jurassic','Oxfordian','middle Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','2','1','Less than 10 m wide','10','1','Less than 20 m','10',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea',NULL,NULL,'1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','29','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2839,0,'Donacosmilia bioherm (2 m thick and 10 m in diameter), 3 smaller bioherms (30-60 cm thick and 1-2 m in diameter) and flanking marly limestones',47,5,4506998,833960,'France','Europe',331,'',47.5833,5.55,'WAHR','87801',26.4071023683,23.774002969,26.4071023683,23.774002969,32.5527530741,24.4726236246,38.4242,14.8109,'Kiessling','Krause','2021-05-28 15:21:12','2022-06-28 17:15:09'),('Charcenne, Franche-Comte',4021,'','Jurassic','Upper Jurassic','Oxfordian','middle-late Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','2','1','Less than 10 m wide','10','1','Less than 20 m','10',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea',NULL,NULL,'1','Corals',NULL,NULL,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,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2839,0,'small Argovian and Sequanian coral reefs',47,5,4494198,854432,'France','Europe',331,'',47.35,5.7667,'WAHR','93102',26.2224764086,24.00209609,26.2224764086,24.00209609,32.3628948098,24.7091846749,38.2032,15.0207,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mantoche, Franche-Comte',4022,'unknown','Jurassic','Upper Jurassic','Oxfordian','middle Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea',NULL,NULL,'1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','14','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2839,0,'small coral patch reefs',47,5,4500598,831282,'France','Europe',331,'',47.4167,5.5333,'WAHR','93083',26.2436937872,23.8123368065,26.2436937872,23.8123368065,32.3885158373,24.5083597011,38.2572,14.8134,'Kiessling','Krause','2021-05-28 15:21:12','2022-06-28 17:33:32'),('Tuyeh, Alborz Mts.',4023,'Lalun','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',511,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2','1','Less than 10 m wide','5','1','Less than 20 m','20',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','2','Intense',0,'No or unknown reservoir potential',2840,0,'Archaeocyath-stromatolite calyptras in marginal marine setting. No calcimicrobes',36,54,-685578,14177429,'Iran','Asia',505,'',36.45,54.1667,'','',-38.2892391745,57.165906027,-40.6968053255,59.9855415835,-40.6968053255,59.9855415835,-8.41934,159.907,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Salient Mountain, Britisch Columbia',4024,'Byng','Ediacaran','Ediacaran','Nama Assemblage','upper Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',546,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','2','1','Less than 10 m wide','15','1','Less than 20 m','10',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','1','Corals','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',2841,0,'Small mounds and more extensive biostromes of stromatolites and thrombolites containing namacalathus and Cloudina',53,-118,-4976520,-8267714,'Canada','North America',121,'',53.0333,-118.7333,'','',-46.8357809456,158.112952861,-46.8357809456,158.112952861,-46.8357809456,158.112952861,-47.8819,-107.38,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Inaba Cave, Sambosan, Shikoku',4025,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'50','178',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf 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','2','6 to 24 reef building species','15','1','Constructor guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2843,0,'Norian part of reef complex, dominated by sponge-microbial association',33,133,4378746,13498245,'Japan','Asia',625,'',33.4333,133.0833,'FALSCH','0',40.7739076187,145.466330765,40.0305492795,145.070345893,41.3978812714,152.022034192,44.0714,128.234,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Inaba Cave, Sambosan, Shikoku',4026,'','Triassic','Upper Triassic','Norian','Norian-Rhaetian',201.30,228.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',203,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'50','178',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','1','Corals','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','27','1','Constructor guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2843,0,'Norian-Rhaetian part of reef complex. Sponge-coralmicrobial reef.',33,133,4378746,13508244,'Japan','Asia',625,'',33.4361,133.0847,'FALSCH','165294, 165295, 165296, 165297',46.1025846894,148.474542774,45.3659625383,148.03871833,41.132760127,154.273454866,44.9014,131.301,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Amagour mound complex, Anti Atlas',4027,'Issafen','Cambrian','Series 2','Stage 4','lower Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',514,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','60','2','10 - 100 m wide','80','2','10 - 100 m','80',NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2844,0,'Mound complex on grainstones. \nMound cores exhibit microbial (mainly Epiphyton and Renalcis) patches, up to 0.8 m thick and 1 m long, surrounded by massive microsparite bearing scattered shelly debris. Archaeocyaths, both\npreserved in life position and forming parautochthonous accumulations, are dominated by simple forms.\nAbundant stromatactis',29,-8,-6996358,7847364,'Morocco','Africa',714,'',29.7167,-8.9167,'','',-75.4123346275,-29.1662322052,-75.840465975,-36.1871923118,-75.840465975,-36.1871923118,-66.4123,114.165,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aguerd complex, Anti-Atlas',4028,'Issafen','Cambrian','Series 2','Stage 4','upper Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',513,NULL,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','8','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2844,0,'Reef complexes described from Aguerd (W), Tadakoust (middle) and Tamezrar (E). \nAguerd member of Issafen Fm.\nCoordinates for Tadakoust',29,-8,-7007576,7851194,'Morocco','Africa',714,'',29.2708,-8.7722,'','',-75.8708479851,-29.4340929303,-76.2807101295,-36.786403143,-76.2807101295,-36.786403143,-66.6085,115.583,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pamyatno-Sasovskoye oilfield, Zhirnovsk',4029,'Evlanovian-Livnian','Devonian','Upper Devonian','Frasnian','middle-upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',378,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick','200','3','101-1000 m wide','1000','4','More than 1000 m','15000','80','2241',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','1','Red algae','0','10','90',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','2','Intense',2,'Actual reservoir',2845,0,'Intrabasin buildup.\nflat-topped, narrow, and extended reef\nsteep (southeast) foreslope composed of relatively deep-water deposits and more gentle inner (north-west) slope represented by lagoonal deposits.\nUpward increase of the role of stromatoporoids, corals, crinoids, calcareous algae (green and red), and cyanobacteria.\n8% porosity, 10% detritus (fossils), 32% algal, rest is spar (dolomite)',50,45,-82309,2435104,'Russia','Asia',624,'',50.7833,45.15,'','',-4.31871094163,6.41136656897,-4.31871094163,6.41136656897,20.3248054592,-57.4590064232,-2.00662,21.873,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Godavari quarry',4030,'Chandragiri','Ordovician','Upper Ordovician','','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',460,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','35','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','0','60','40',0,'no',0,'no','1','Less than 6 reef building species','4','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2848,0,'Mud mound with common stromatactis, similar to Meiklejohn Peak.\r\nAge poorly constrained',28,85,0,0,'Nepal','Asia',NULL,'',27.59,85.389722,'WAHR','118944',-19.9253282289,96.6761788664,-19.9253282289,96.6761788664,-19.9253282289,96.6761788664,-17.1778,156.444,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Santa Teresiola, Taranto',4031,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','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','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',2851,0,'The bank (or \'open frame reef\') is formed by numerous, contiguous colonies of coral embedded in a sandy matrix up to 1 m high covering a surface of nearly 0.6 km².',40,17,0,0,'Italy','Europe',344,'',40,17,'WAHR','130581',39.9910068315,16.9883000709,39.9935763579,16.9916426855,39.9929775971,17.0003500711,39.9983,16.9982,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kongul Yayla',4032,'Kongul','Carboniferous','Mississippian','Visean','Asbian',336.00,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',332,3,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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',2852,NULL,'',36,32,NULL,NULL,'Turkey','Asia',522,NULL,36.93,32.43,NULL,NULL,-55.9711534141,33.841433751,-55.3069909171,33.5930743334,-33.6763803515,1.26022275738,-31.3578,28.3149,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('NE Taebaek Basin',4033,'Daegi','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',332,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','14',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','4','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2852,0,'Described as siliceous-sponge microbial reefs. Epiphyton dominant, followed by Siliceous sponges, Renalcis and Epiphyton. 170 m thick section with several intervals. Described is only 14 m thick example. Ooids indicate shallow marine deposition. late Stage 5 to middle Guzhangian.',36,32,NULL,NULL,'South Korea','Asia',NULL,NULL,37.09,129,NULL,NULL,-27.1936870372,79.3999619657,-29.9592277698,84.3468123261,-29.9592277698,84.3468123261,5.88783,149.082,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lake Georgetown Spillway',4034,'Edwards','Cretaceous','Lower Cretaceous','Albian','upper Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,100,'Early Cretaceous (late Albian, 102.6 Ma)',332,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3','2','10 - 100 m wide','40',NULL,NULL,'20',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','12','Foraminifera','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',2,'Actual reservoir',2852,0,'Outcrops of rudist-bearing shallow water carbonates. Weakly cemented, circular, flat-topped radiolitid–caprinid–toucasid mounds developed above the toucasid mounds and low relief, often sucrosic-dolomitized mounds.\r\nLow diversity, with each biohermal stage being composed\r\nof one dominant species—caprinids, toucasids, or caprinid–toucasid–\r\nradiolitids, respectively.',36,32,NULL,NULL,'Texas','North America',NULL,NULL,30.4,-97.43,NULL,NULL,37.9493013187,106.85468669,27.9005224704,-53.4647965543,29.8984288833,-59.3610131477,28.7817,-57.9803,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Sant Onofre',4035,'','Neogene','Pliocene','Pliocene','lower Pliocene',3.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','8','Serpulids, worms, vermetids','2','Algae','48','Red algae - vermetids',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','4','1','Constructor guild','2','Intensive','2','Intensive','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',2853,0,'Dendropoma and Spongites are the main builders',NULL,NULL,NULL,NULL,'Spain','Europe',304,NULL,40.7667,0.5833,'Y','153720',40.4101593545,-0.227481261408,40.4113737133,-0.224756615148,40.5763526103,0.557314590707,40.8719,0.193745,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('East Island Wall',4036,'Assoul','Jurassic','Middle Jurassic','Bajocian','Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','20','3','101-1000 m wide',NULL,NULL,NULL,'310',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','13','Echinoderms','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2859,0,'',NULL,NULL,NULL,NULL,'Morocco','Africa',714,NULL,31.59,-5,NULL,NULL,11.0190660285,11.4964211205,16.0580797792,4.43311760204,20.0039058374,3.48358307646,26.9345,-1.16459,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Bonifacio Basin, SE Corsica',4037,'Cala di Labra','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','16',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','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','16',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2860,0,'',NULL,NULL,NULL,NULL,'France','Europe',331,NULL,41.22,9.11,'Y','151413, 151414, 151415',39.5959752714,3.78818668753,39.7835983875,5.22610841007,40.16584893,8.67162396966,42.8944,4.68196,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Rocky Camp Mound',4038,'Taravale','Devonian','Lower Devonian','Emsian','Emsian',393.30,407.60,9,'late Pragian - Eifelian',395,400,'Early Devonian (Emsian, 400 Ma)',400,3,'0','Outcropping reef ',3,'Mud mound or bank','4','More than 500 m thick','600','3','101-1000 m wide','1000','4','More than 1000 m','1000','10',NULL,0,'Tropical or unknown','','Unknown','','Unknown','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','15','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',2861,0,'Micritic components of the mud-mound were predominantly produced in situ by autochthonous algae and/or other skeletalorganisms. Green algae and stromatactis,together with sponge spicules in the lower facies of this mound - “microbial mud-mound” model',NULL,NULL,NULL,NULL,'Australia','Oceania',801,NULL,-37.29,148.1,NULL,NULL,35,145,-32.713065777,133.403248091,-40.0812163812,173.530184425,-21.8441,170.237,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Marsica',4039,'Ellipsactinia Limestones','Jurassic','Upper Jurassic','Tithonian','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','200','2','10 - 100 m wide',NULL,NULL,NULL,NULL,'3',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','6','Calcisponges','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','10',NULL,NULL,'2','Intensive','2','Intensive',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2858,0,'Biota - corals and calcified demosponges. Sedimentary features - grain size, sorting and reworking degree, bioerosion, cement crusts and cavities.',NULL,NULL,NULL,NULL,'Italy','Europe',344,NULL,41.5,13.6,'Y','154046, 154047, 154048',15.4057335468,19.5443542673,16.2589584656,19.2508329428,18.0194179077,22.5046510948,28.9643,17.9525,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Santanyi',4040,'Santanyí Limestone','Neogene','Miocene','Upper Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','30','1','Less than 10 m wide','6',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes',NULL,NULL,'64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2862,0,'',NULL,NULL,NULL,NULL,'Spain','Europe',304,NULL,39.2,3.1,NULL,NULL,38.9234549155,1.07383075073,38.9243571708,1.06805015418,38.7567091323,2.987689051,39.8487,2.07928,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Shuibatang ',4041,'Shihniulan ','Silurian','Llandovery','Aeronian','Aeronian',438.50,440.80,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate','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,NULL,NULL,NULL,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,NULL,NULL,'0','',0,'No or unknown reservoir potential',2863,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',602,NULL,28.43,107.05,NULL,NULL,3.56130282896,69.3803871063,3.56130282896,69.3803871063,3.56130282896,69.3803871063,8.44763,126.805,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gosausee',4072,'Dachstein','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'4','More than 1000 m wide','3500','4','More than 1000 m','5000',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','3','Microbes','1','Corals','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','50','3','Binder guild','1','Present','1','Present','1','Low zonation','3','Pronounced zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2931,NULL,'Probably part of the same reef tract as Gosaukamm reef (Rf #28), however, the Gosausee site is only lower Rhaetian. Also, although the microbialites are volumetrically the most abundant reef builders, corals and sponges are more important in certain zones',NULL,NULL,NULL,NULL,'Austria','Europe',NULL,NULL,47.536521,13.522713,NULL,NULL,26.6940525928,30.3028407271,26.6940525928,30.3028407271,28.7594453052,23.1379116288,32.2211,15.6741,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Seokgaejae pass',4042,'Dumugol','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2864,NULL,'',NULL,NULL,NULL,NULL,'South Korea','Asia',NULL,NULL,36.13,129.1,NULL,NULL,-32.1181267484,91.4960321963,-32.1181267484,91.4960321963,-32.1181267484,91.4960321963,-1.15655,137.253,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Zhangzhai',4043,'Hunghuayuan','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,1,'Temperate','2','Shelf or Platform margin',NULL,NULL,'1','Above fair weather wave base','3','Microbes','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2865,NULL,'The small-scaled reefs are generally domical or lenticular in shape, ranging in height from tens of centimeters to several meters, and in width from less than a meter to more than 10 m. They are chiefly built by benthic microbes, lithistid sponges, the quasi-sponge fossils Calathium as well as bryozoans and are usually surrounded by skeletal/intraclastic grainstones and packstones. Skeletal fragments of ostracods, trilobites, gastropods, brachiopods, nautiloids, and echinoderms are found within the reefs and surrounding sediments. Three reefal types are recognized.',NULL,NULL,NULL,NULL,'China','Asia',602,NULL,27.27,109.02,NULL,'154810',-15.2402706884,89.9607464719,-15.2402706884,89.9607464719,-15.2402706884,89.9607464719,20.2859,141.449,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Zhangzhai Calathium',4044,'Hunghuayuan','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','4.5','1','Less than 10 m wide','12','1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'6','Calcisponges','3','Microbes','14','Sponges - bryozoans - (microbes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2865,NULL,'intraskeletal crypts of a lithistid sponge-Calathium\r\nreef',NULL,NULL,NULL,NULL,'China','Asia',602,NULL,30.1,107.9,NULL,'154810',-13.4766972424,89.8010710917,-13.4766972424,89.8010710917,-13.4766972424,89.8010710917,17.2157,140.821,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Haoshihe',4045,'Jinghe','Ordovician','Middle Ordovician','Darriwilian','Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','3','Microbes','1','Corals','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2866,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',602,NULL,34.37,108.09,NULL,NULL,32.7652716288,95.9046659056,32.7652716288,95.9046659056,32.7652716288,95.9046659056,-22.1343,127.339,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Shigeyasu Mine',4048,'Akiyoshi Limestone','Permian','Guadalupian','Wordian','Murghabian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',NULL,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','11','Siliceous sponges','7','Bryozoans','14','Sponges - bryozoans - (microbes)','1',NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','12','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3002,NULL,'',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,34.18,131.18,NULL,'173376',6.5268806937,127.887449044,6.5268806937,127.887449044,22.524615824,105.891890194,18.2365,110.771,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Nanyigou section',4049,'Lianglitag','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','3','101-500 m thick','178',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','11','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2868,NULL,'Bioclasts are rare in the lower part of the reef. In the middle part of the reef bindstones are common and stromatolitic structures are becoming more abundant than in the lower part- which can be observed especially on weathered rock surfaces. In the top part of the reef thin-bedded micritic mudstones occur with rare bioclasts.',NULL,NULL,NULL,NULL,'China','Asia',602,NULL,40.05,78.5,NULL,'154867',-3.61270627373,53.2963041801,-3.61270627373,53.2963041801,-3.61270627373,53.2963041801,-36.1333,112.152,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Børglum Elv, Peary Land',4051,'Turesø','Ordovician','Upper Ordovician','Katian','late Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,2,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','3','Below storm wave base','3','Microbes','1','Corals','44','Worms - microbes - (forams) - (bryozoans) - (corals)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2867,NULL,'The individual mounds rarely exceed 1m in height. In terms of the rock fabrics, the North Greenland mudmounds show some similarity to the “thromboid”–bryozoan–worm tube association in the thin interval of “Red River reefs”',NULL,NULL,NULL,NULL,'Denmark','Europe',102,NULL,82.33,-30.15,NULL,NULL,7.88366730582,-84.9839396229,7.88366730582,-84.9839396229,7.88366730582,-84.9839396229,3.67154,-27.0766,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Aïn El Bergoug',4052,'','Neogene','Miocene','Upper Miocene','late Tortonian',7.30,9.00,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,'800',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','2','Below fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,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',2876,NULL,'',NULL,NULL,NULL,NULL,'Morocco','Africa',714,NULL,35.5,-9.02,NULL,NULL,34.2539143906,7.61933135528,34.4390609602,-9.99628253301,34.9799592753,-8.84650414539,35.5486,-10.1427,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Vasalemma Nordkalk quarry',4053,'Vasalemma','Ordovician','Upper Ordovician','Sandbian','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15',NULL,NULL,NULL,'4','More than 1000 m','2.300',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'13','Echinoderms','7','Bryozoans','53','Echinoderms - bryozoans - tabulate corals - (lithistids)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2877,NULL,'Hemicosmitenkalk or cystoid limestone - the rock building abundance\r\nof echinoderm (mainly Hemicosmites, Rhombifera) bioclasts\r\nin this limestone',NULL,NULL,NULL,NULL,'Estonia','Europe',NULL,NULL,59.14,24.19,NULL,'87273',-29.0547990973,-61.1310049985,-29.0547990973,-61.1310049985,-29.0547990973,-61.1310049985,-32.1589,-1.54591,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gisliflue-Homberg',4054,'','Jurassic','Middle Jurassic','Bajocian','Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',NULL,2,'1','Seismic data available ',4,'Biostrome','4','More than 500 m thick','800',NULL,NULL,NULL,'4','More than 1000 m',NULL,'4.5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','26','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2875,NULL,'',NULL,NULL,NULL,NULL,'Switzerland','Europe',331,NULL,47.25,8.06,NULL,'162347',26.8374486534,28.0994883559,26.8374486534,28.0994883559,31.1236442073,28.349518978,36.9533,17.6994,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('North Road Section',4055,'Lianglitag','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','30','2','10 - 100 m wide','50',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','1','Corals','56','Microbes - crinoids - tabulate/rugose corals',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2868,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',602,NULL,40.09,78.5,NULL,NULL,-3.59605530213,53.2598625322,-3.59605530213,53.2598625322,-3.59605530213,53.2598625322,-36.0966,112.132,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Microwave  Station',4056,'Lianglitag','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'3','Microbes','1','Corals','61','Microbes (thrombolites) - algae - corals',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','9','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2868,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',602,NULL,40.8,78.49,NULL,NULL,-5.13464111343,29.1807814417,-5.13464111343,29.1807814417,-5.13464111343,29.1807814417,-37.0469,105.2,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Aggtelek',4057,'Steinalm','Triassic','Middle Triassic','Anisian','Anisian-Ladinian',237.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','2','Algae','12','Foraminifera','13','Algae - encrusting forams',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species','26',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2875,NULL,'No comment',NULL,NULL,NULL,NULL,'Hungary','Europe',NULL,NULL,48.5,20.55,NULL,NULL,11.8508212251,40.2155667597,11.8508212251,40.2155667597,14.5900350522,24.9108453414,1.66188,32.0047,'Krause','Krause','2021-05-28 15:21:12','2022-06-22 20:44:12'),('Microwave  Station',4058,'Lianglitag','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,1,'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,'3','Microbes','1','Corals','61','Microbes (thrombolites) - algae - corals',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2868,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',602,NULL,40,78.56,NULL,NULL,-3.59171890362,53.3610118146,-3.59171890362,53.3610118146,-3.59171890362,53.3610118146,-37.8054,105.528,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Aggtelek',4059,'Jenei','Triassic','Middle Triassic','Anisian','Anisian-Ladinian',237.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','3','Below storm wave base','2','Algae','2','Algae',NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','20',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2875,NULL,'',NULL,NULL,NULL,NULL,'Hungary','Europe',NULL,NULL,48.5,20.55,NULL,NULL,11.8508212251,40.2155667597,11.8508212251,40.2155667597,14.5900350522,24.9108453414,2.50634,31.312,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Taebaeksan Basin',4060,'Duwibong','Ordovician','Middle Ordovician','Darriwilian','Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','4','Stromatoporoids','7','Bryozoans','22','Stromatoporoids/sponges - corals - (algae)','2','Green algae',NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2',NULL,NULL,'1','Present','1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2881,NULL,'Stromatoporoids and bryozoans comprise more than 50 areal percent of these frameworks. Cystostroma stromatoporoids -34%, Nicholsonella bryozoans -16%, unidentified tubular organisms - 4% and siliceous sponge <2%.',NULL,NULL,NULL,NULL,'South Korea','Asia',NULL,NULL,37.14,128.94,NULL,NULL,21.8468018521,81.4703322159,21.6093331276,81.2710429105,21.6093331276,81.2710429105,-9.20773,128.153,'Krause','Krause','2021-05-28 15:21:12','2021-07-26 12:25:01'),('Capo Colonna',4061,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','5',NULL,NULL,NULL,NULL,NULL,NULL,'2.5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','15','Non-rudist bivalves','39','Algae - bivalves - (bryozoans) - (siliceous sponges)','1','Red algae',NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species','35',NULL,NULL,'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','1','Present',0,'No or unknown reservoir potential',2882,NULL,'The Capo Colonna deposits include rigid build-ups, rhodolith accumulations, and a maerl bed. The build-ups, identified as a fossil example of the present day Mediterranean coralligenous, are primarily formed by Mesophyllum alternans',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,39.1,17.11,NULL,'166071, 166072, 166073, 166074',39.0910114283,17.0983490547,39.0935796415,17.1016776808,39.0968849744,17.1089387657,39.0983,17.1081,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Maroni',4062,'Koronia Member - Pakhna Formation','Neogene','Miocene','Upper Miocene','Tortonian-Messinian',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)','1','Red algae',NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2891,NULL,'',NULL,NULL,NULL,NULL,'Cyprus','Europe',NULL,NULL,34.45,33.21,NULL,NULL,33.4773383939,31.6529819143,33.480230056,31.6575284453,32.976123571,32.8120387276,34.0556,32.7752,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Ainsa-Jaca Basin',4063,'Arguis','Paleogene','Eocene','Priabonian','Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'3','101-500 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','1','Corals','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)','1','Red algae',NULL,NULL,NULL,0,'no',0,'no','3','25 or more reef building species','44',NULL,NULL,'2','Intensive','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',2893,NULL,'upper part of Arguis Fm\r\nMesophotic reef',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,42.2,-0.38,NULL,'152582',39.1338850831,-4.52137692186,39.1338850831,-4.52137692186,40.9498812584,-0.600243517045,40.8928,-3.5605,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('south Qinling Mountains, Sanlixia, Xunyang',4064,'Yangshan','Permian','Cisuralian','Asselian','Asselian-Sakmarian',290.10,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',294,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','40',NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','2','Below fair weather wave base','3','Microbes','2','Algae','61','Microbes (thrombolites) - algae - corals','4','Others',NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','12','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',2899,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.01,109.21,NULL,NULL,-5.44762078631,126.585235966,-5.44762078631,126.585235966,42.3900348172,129.23461243,-5.04517,92.5407,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('West Barbados',4065,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae',NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species','14',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2900,NULL,'',NULL,NULL,NULL,NULL,'Barbados','North America',NULL,NULL,13.16,-59.38,NULL,'88831',13.1062251021,-59.3123317277,13.1068161894,-59.3130749068,13.16,-59.38,13.1604,-59.3286,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Dunmore',4066,'unknown','Carboniferous','Mississippian','Tournaisian','upper Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','3.2','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','7','Bryozoans','3','Microbes','60','Bryozoans - Pelmatozoans - (microbes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',2908,NULL,'The local trend, which occurs only in the two southern localities (deeper water), expresses differences between the skeletal grain content of the various lithofacies. These differences result partly from increased sensitivity to substrate texture by organism groups suffering southward attenuation (notably gastropods, hyalosteliid sponges, aoujgaliids, Earlandia and kirkbyacean ostracods) and partly from selective colonization, particularly of the transition facies, by tabulate corals and stick/ramose bryozoans. However, the developmental sequence of precursor carbonate muds is the same at all localities, indicating that the mud-making process (probably microbial) was independent of water depth.',NULL,NULL,NULL,NULL,'Ireland','Europe',NULL,NULL,53.38,-8.45,NULL,NULL,-33.1253298072,-15.2413807516,-33.1253298072,-15.2413807516,-4.14364090342,-47.3501090304,-9.41607,-3.91996,'Krause','Kiessling','2021-05-28 15:21:12','2023-03-15 13:39:41'),('Tiandong 10, Kaijiang, east Sichuan',4067,'','Triassic','Lower Triassic','Induan','Induan',251.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,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,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2911,NULL,'?Microbialite',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.1,107.57,NULL,NULL,-8.94860352871,106.961364897,-8.94860352871,106.961364897,14.8704195218,123.874690811,10.9325,95.4949,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('N of Port Sudan, Red Sea coast',4077,'','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,1,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','15','3','101-1000 m wide','550',NULL,NULL,NULL,'700',NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','1','Corals','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','32','2','Baffler guild','2','Intensive','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3008,NULL,'terraces which are exposed in the coastal plain north of the city of Port Sudan, between 19° 54\' N and 21° 50\' N and 36° 51\' E and 37° 17\' E, until near to the border between Sudan and Egypt',NULL,NULL,NULL,NULL,'Sudan','Africa',NULL,NULL,19.54,36.51,NULL,'101414',19.3977448475,36.2963144811,19.3971949003,36.2954903276,19.3059566964,36.4035468966,19.2465,36.1161,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Sharm Al Arab',4078,'','Quarternary','Pleistocene','Pleistocene','late Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'1','Seismic data available ',NULL,NULL,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','3','Below storm wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3009,NULL,'',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,26.57,33.54,NULL,'176527',26.5643272244,33.5313410577,26.5643272244,33.5313410577,26.5612339686,33.5367803743,26.5676,33.5371,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Sharm Al Arab II',4079,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','3','Below storm wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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',3009,NULL,'',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,26.57,33.54,NULL,'176528',26.5183584782,33.4612351936,26.5189262024,33.4621003557,26.4911155401,33.5109988367,26.5488,33.5135,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wadi Gawasis',4080,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','','Unknown','3','Below storm wave base','1','Corals','1','Corals','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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',3009,NULL,'',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,26.33,34.02,NULL,'176529',26.2786239447,33.9411861935,26.2791887551,33.9420518961,26.2507525844,33.9904435238,26.3087,33.9933,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wadi Gawasis II',4081,'','Quarternary','Pleistocene','Pleistocene','late Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','','Unknown','3','Below storm wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3009,NULL,'',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,26.33,34.02,NULL,'176530',26.3243564269,34.0113356915,26.3243564269,34.0113356915,26.3211936361,34.0167186052,26.3276,34.017,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wadi Wizr',4082,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','3','Below storm wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3009,NULL,'',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,25.47,34.29,NULL,'176532',25.4187749966,34.2116625822,25.4193381475,34.2125230605,25.3905511082,34.2594685245,25.4486,34.2629,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wadi Wizr II',4083,'','Quarternary','Pleistocene','Pleistocene','middle Pleistocene',0.10,0.80,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','3','Below storm wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3009,NULL,'',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,25.47,34.29,NULL,'176533',NULL,NULL,25.4193381475,34.2125230605,25.4611712236,34.2866102002,25.4486,34.2629,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Isla Juanilla, Sandino Basin',4084,'Juanilla','Paleogene','Oligocene','Chattian','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',27,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','','Unknown',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','13',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3016,NULL,'',NULL,NULL,NULL,NULL,'Costa Rica','North America',NULL,NULL,10.58,-85.42,NULL,'179809',8.86800411643,-85.6533405436,8.86800411643,-85.6533405436,13.0463026931,-80.4874091395,10.7406,-84.3951,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Monte Postale',4085,'unknown','Paleogene','Eocene','Ypresian','Ypresian',47.80,56.00,27,'Thanetian - Ypresian',53,50,'Early Eocene (Ypresian, 51.9 Ma)',51,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','15','2','10 - 100 m wide','30','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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','22','1','Constructor guild','2','Intensive','2','Intensive',NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3017,NULL,'Diverse corals Actinacis',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,45.35,11.12,NULL,'180311',38.3108461491,8.45360519391,38.3108461491,8.45360519391,39.9593645561,12.3480594542,37.0755,10.2533,'Krause','Kiessling','2021-05-28 15:21:12','2023-01-04 15:04:28'),('Topuk Tepe, near Pinargözü',4086,'Kasımlar','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',214,1,'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,'11','Siliceous sponges',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3020,NULL,'tectonically\r\nisolated carbonate block composed of Dachstein-type limestones with megalodonts and large dendroid corals. At the top of this\r\nsedimentation a reefal fauna is developed with similarities to the cipit fauna. The Topuk Tepe locality is surrounded by reef\r\nboulder bearing shales of Kasımlar Formation.',NULL,NULL,NULL,NULL,'Turkey','Asia',NULL,NULL,37.26,44.08,NULL,NULL,5.57491768489,45.8310963157,5.35457637676,45.861654778,-2.41448043874,38.0359179196,28.2704,31.4031,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Vojsko Plateau',4087,'Bellerophon','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,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','3a','Upper slope or inner ramp','2','Below fair weather wave base','11','Siliceous sponges','8','Serpulids, worms, vermetids','8','Coralline sponges (chaetetids) - microbes - corals','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3021,NULL,'The major biostrome builders are medium-sized coralline sponges, Demospongea and Calcarea, encrusted by smaller sponges, tube worms, sessile foraminifera, calcareous algae - Archaeolithoporella - and Shamovella - Tubiphytes-, all of which are typically covered by microbial crusts. The biostromes are characteristically composed of bafflestone and bindstone, incorporating sporadic framestone.\r\nNarrowbelts of floatstone surround the buildups, and sponge debris is also present in lenseswithin the mud matrix between metazoan bafflestones',NULL,NULL,NULL,NULL,'Slovenia','Europe',NULL,NULL,46.1,13.55,NULL,'183939',10.6700695789,36.2515879092,10.6700695789,36.2515879092,8.24886331102,28.4326710133,3.69203,26.7634,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Akdag locality',4088,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3020,NULL,'',NULL,NULL,NULL,NULL,'Turkey','Asia',NULL,NULL,37.8,30.53,NULL,'183686',9.04896245868,35.9716691423,8.85503872176,36.0162275963,5.80197383438,27.9335857191,10.3909,21.9401,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Yeongwol County, Yeongheung Fm',4089,'Yeongheung','Ordovician','Middle Ordovician','Darriwilian','Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1','1','Less than 10 m wide','1','1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'1a','Shallow intra-platform','3','Below storm wave base','4','Stromatoporoids',NULL,NULL,'75','Stromatoporoids or chaetetids only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3022,NULL,'A fabric composed of peloids up to several tens of micrometers in diameter, micrite, patches of calcite cement, and ghosts of either in-place or dissociated cyst plates and pillars occupies areas where the internal textures of stromatoporoid skeletons are poorly preserved. This fabric commonly grades intowellpreserved stromatoporoid skeletons, or rarely replace the bulk of each\r\nskeleton.\r\nFramework basically just Labechia, rare calcimicrobes and bryozoans',NULL,NULL,NULL,NULL,'South Korea','Asia',NULL,NULL,37.14,128.26,NULL,'184483',21.9608543485,81.7154207905,21.9608543485,81.7154207905,21.9608543485,81.7154207905,-6.25704,132.243,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Well He 3',4090,'Lianglitag','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','3','Below storm wave base','7','Bryozoans','1','Corals','41','Corals - bryozoans - (algae) - (bivalves)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','2','Baffler 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',3023,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,38.46,79.56,NULL,NULL,-3.51599816814,55.0864737108,-3.51599816814,55.0864737108,-3.51599816814,55.0864737108,-37.2447,113.901,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wells Ma 5',4091,'Lianglitag','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,1,'1','Seismic data available ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','7','Bryozoans','1','Corals','18','Bryozoans - microbes - (algae) - (crinoids)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','10','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3023,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,38.36,79.33,NULL,'184490',-3.72127913586,55.1049652613,-3.72127913586,55.1049652613,-3.72127913586,55.1049652613,-37.4116,113.748,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Yadana field, offshore Myanmar',4092,'Upper Burman Limestone','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick','850','4','More than 1000 m wide',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','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3024,NULL,'The Aquitanian marks the onset of renewed volcanic activity associated with the development of fringing\r\ncarbonate reefs during the Burdigalian. The rapid (~6 My) development of these wide (~5e70 km) and\r\nthick (~300e850 m) carbonate platforms has been mainly controlled by the subsidence.',NULL,NULL,NULL,NULL,'Burma (Myanmar)','Asia',NULL,NULL,15.1,94.4,NULL,NULL,11.3621401341,92.0375422188,11.3621401341,92.0375422188,4.68120729728,91.8573420608,8.51312,98.4507,'Krause','Kiessling','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Myrmidon Reef MYR_3',4093,'','Quarternary','Pleistocene','Pleistocene','late Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,1,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,'2','10 - 100 m wide','28',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','3','Microbes','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3025,NULL,'',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-18.15,147.23,NULL,NULL,-18.1833690371,147.215702935,-18.1738348905,147.219787403,-18.1828711451,147.223259823,-18.1847,147.222,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Stanley',4094,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','3b','Deeper slope or outer ramp',NULL,NULL,'2','Algae','1','Corals','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','58',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3025,NULL,'',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.17,148.4,NULL,'184511',-19.2031420365,148.386153001,-19.1936727529,148.390108823,-19.2026102232,148.393739267,-19.2045,148.392,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Heron',4095,'','Quarternary','Pleistocene','Pleistocene','late Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','58',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3025,NULL,'',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-23.26,152.55,NULL,NULL,-23.2830185063,152.541508979,-23.2830185063,152.541508979,-70.6915101198,127.880641711,-23.2938,152.544,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('One Tree',4096,'','Paleogene','Paleocene','Selandian-Thanetian','Upper Paleocene',56.00,59.20,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','58',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3025,NULL,'',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-23.3,152.5,NULL,'184510',-45.0182333752,153.269672221,-45.0182333752,153.269672221,-49.6652478445,151.407828343,-44.3694,151.579,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Fairfax',4097,'','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','58',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3025,NULL,'',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-23.51,152.22,NULL,'184506',-23.5423051154,152.208104244,-23.5330749902,152.211502352,-23.5416641551,152.215818109,-23.5439,152.214,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Precordillera',4098,'La Silla','Ordovician','Lower Ordovician','Tremadocian','early-mid Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','3','Microbes','2','Microbes','15','Rugose corals - microbes - algae','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3026,NULL,'Coralomorph (Amsassia colonies) in thrombolite mounds. Amsassia intpreted as calcareous green alga by Lee et al. (2021).\r\nStromatolites, and particularly thrombolites, are ubiquitous and very common components of the higher-frequency cycles.  Calcarenites are mainly composed of peloids, well-rounded intraclasts, aggregate lime grains, micritized ooids, and a few bioclasts. Bioclasts are very scarce and include rare calcareous algae such as Nuia sp. and scattered fragments of gastropods, trilobites, and nautiloids within the cross-bedded subtidal grainstone-packstone intervals.  Abundant in situ gastropods seem intimately related with domical thrombolites.',NULL,NULL,NULL,NULL,'Argentina','South America',NULL,NULL,-30.16,-58.4,NULL,'8880',-31.4877371732,-173.400594115,-31.4877371732,-173.400594115,-31.4877371732,-173.400594115,-40.5211,-140.02,'Krause','Kiessling','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Portada Covunco',4099,'La Manga','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','12','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','1','Corals','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15','1','Constructor guild','2','Intensive','2','Intensive',NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',3028,NULL,'',NULL,NULL,NULL,NULL,'Argentina','South America',NULL,NULL,-38.47,-70.11,NULL,'184598',-43.8045831536,-37.1589075683,-43.8045831536,-37.1589075683,-40.0569900847,-37.4993867609,-35.5572,-31.9134,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Nanyigou section',4100,'Yijianfang','Ordovician','Middle Ordovician','Darriwilian','Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2','1','Less than 10 m wide','6',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','6','Calcisponges','15','Algae - microbes - (encrusting forams) - (rare songes)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11','4','Microbial precipitation',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',3029,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,40.05,78.5,NULL,'154821',-13.718412382,64.5292892321,-13.718412382,64.5292892321,-13.718412382,64.5292892321,-31.4198,117.416,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Yangmaile',4101,'','Ordovician','Middle Ordovician','Darriwilian','Darriwilian',458.40,467.30,5,'Darriwilian - Ashgillian',452,465,'Middle Ordovician (early Darwillian,465 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'2','Algae',NULL,NULL,'15','Algae - microbes - (encrusting forams) - (rare songes)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2','2','Baffler 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',3029,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,39.57,79.03,NULL,'184658',-13.4893345114,65.1324499252,-13.4893345114,65.1324499252,-13.4893345114,65.1324499252,-31.7017,118.077,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Sidi Mohamed Smaine',4102,'Sidi Mohamed Smaine','Devonian','Middle Devonian','Givetian','Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','3','101-500 m thick','170',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation',NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',3031,NULL,'',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,33.29,-6.59,NULL,'176209',-36.3663689255,-12.276805532,-36.3663689255,-12.276805532,-41.1668433055,-6.98478423855,-36.1792,5.64244,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Barcoo 1',4103,'','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',3032,NULL,'',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-15.22,120.35,NULL,NULL,-26.9093060116,113.824515082,-24.3502323429,115.09122708,-27.30371532,116.145287895,-25.9589,115.199,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Brecknock 1',4104,'','Neogene','Miocene','Lower Miocene','Aquitanian-Burdigalian',16.00,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250','4103',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)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'NA',NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',3032,NULL,'',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-14.35,121.42,NULL,NULL,-24.1548836113,115.853334109,-24.1548836113,115.853334109,-27.262674148,117.033123872,-25.7578,116.014,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lombardina 1',4105,'','Neogene','Miocene','Upper Miocene','Tortonian-Messinian',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,'Barcoo 1',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)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',3032,NULL,'Reef generation 5. Continued growth of islated atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-15.44,121.32,NULL,NULL,-21.0807998672,118.131955692,-21.0807998672,118.131955692,-23.1869652728,118.680106014,-22.8699,118.148,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lynher 1',4106,'','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'20','Barcoo 1',0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',3032,NULL,'',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-15.28,121.5,NULL,NULL,-19.4734696584,119.13722868,-19.4734696584,119.13722868,-21.1264167755,119.502529571,-21.0876,119.148,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('North Scott Reef 1',4107,'','Neogene','Miocene','Upper Miocene','lower Tortonian',9.00,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Barcoo 1',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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',3032,NULL,'Reef generation 4. Reestablishment of reef belts, atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-13.53,121.53,NULL,NULL,-20.6170350806,117.544880056,-20.6170350806,117.544880056,-23.07139082,118.307006768,-22.3492,117.653,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Panaca Hills',4108,'Highland Peak','Cambrian','Series 3','Guzhangian','Middle-Upper Cambrian',485.00,509.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','3','Below storm wave base','3','Microbes',NULL,NULL,'93','Microbial micrite - pelmatozoans',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3034,NULL,'',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,37.8,-114.37,NULL,NULL,30.9550329829,-134.717174022,31.7762474621,-125.053166947,31.7762474621,-125.053166947,-0.905697,-91.8121,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Delamar Mountains, Nopah Fm',4109,'Nopah','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes',NULL,NULL,'93','Microbial micrite - pelmatozoans',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3034,NULL,'',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,37.05,-114.92,NULL,NULL,31.1224635109,-121.934611404,31.1224635109,-121.934611404,31.1224635109,-121.934611404,-1.6139,-91.0619,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Qaidam Basin, Huaitoutala Fm',4110,'Huaitoutala','Carboniferous','Mississippian','Visean','Visean',330.90,346.70,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide','7',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'1','Corals','14','Brachiopods','57','Brachiopods - bryozoans, sponges, corals, Tubiphytes, encrusting forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3035,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,37.33,96.1,NULL,NULL,29.7690094268,125.330924579,29.7690094268,125.330924579,29.6413931569,41.0502934904,-9.31848,52.1343,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wubaiti, (TD021-4, TD021-X7), eastern Sichuan',4111,'Changxing','Permian','Lopingian','Changhsingian','middle-upper Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',252,3,'1','Seismic data available ',1,'True reef','3','101-500 m thick','200','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',3036,NULL,'Comment from Dong at al., 2021: \r\nTD021-4 reef: carbonate ramp-open platform-platform margin shoal-open platform-platform margin reef facies',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.05,108.01,NULL,NULL,NULL,NULL,-10.0236080552,106.329387278,11.8419056024,125.429185034,9.71177,96.0762,'Krause','Krause','2021-05-28 15:21:12','2021-06-20 14:49:22'),('Gyanyima Section, Burang County in Ngari, Tibet',4112,'Gyanyima','Permian','Lopingian','Wuchiapingian','Lopingian',252.20,259.80,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','236',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf',NULL,NULL,'1','Corals','14','Brachiopods','57','Brachiopods - bryozoans, sponges, corals, Tubiphytes, encrusting forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','160','4','Microbial precipitation','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3037,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,30.43,80.41,NULL,'187535',NULL,NULL,-45.0425005044,52.9870407148,-43.0771857117,60.7689024708,-49.9918,59.3984,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Baidar Valley, Crimean Mountains',4113,'Unknown','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,2,'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','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','11','Siliceous sponges','1','Corals','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','21','4','Microbial precipitation','2','Intensive','2','Intensive','3','Pronounced zonation','3','Pronounced zonation','3','More than 60% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3161,NULL,'Trombolites, incrusted Crescentiella morronensis, and Terebella lapilloides, subordinate corals and\r\nsponges, which are interpreted as deep-water\r\n(mainly microbial) bioherms and a new type of forereef apron deposit discovered in limestones\r\nof the Baidar plateau. Such aprons include\r\ngravitation flow sediments. intraclast rudstones\r\nand floatstones with clasts of various reef-builders, as well as sorted grainstones, rudstones, and microbreccias that bear structural signs of unidirectional current and gravitation flow in some places.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,44.26,33.48,NULL,NULL,NULL,NULL,30.6547202708,43.8504114981,34.6135608237,46.695616632,24.0298,33.4893,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('East Point, Anticosti Isl., Quebec',4114,'Menier','Silurian','Llandovery','Telychian','upper Aeronian',438.50,440.80,6,'Rhuddanian-Telychian',435,425,'Middle Silurian (Wenlock, 430.4 Ma)',436,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','10',NULL,NULL,NULL,'1','Less than 20 m',NULL,'60',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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3038,NULL,'',NULL,NULL,NULL,NULL,'Canada','North America',NULL,NULL,49.15,-61.6833,NULL,'153816',NULL,NULL,-22.4567286167,-85.2426693881,-22.4567286167,-85.2426693881,-21.6745,-34.3074,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('near Yushan, Jiangxi',4115,'Xiazhen','Ordovician','Upper Ordovician','Katian','late Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,'25',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',2856,NULL,'',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,28.36,118.2,NULL,NULL,NULL,NULL,-7.9563672365,64.8337042919,-7.9563672365,64.8337042919,2.58226,123.82,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Pavasaris and South Bliudziai',4116,'','Silurian','Pridoli','Pridoli','lower Pridolian',419.20,423.00,8,'middle Pridolian - middle Pragian',412,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',417,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick','40','3','101-1000 m wide','1000','4','More than 1000 m','1500','1.5',NULL,0,'Tropical or unknown','3','Ramp or Slope','','Unknown',NULL,NULL,'4','Stromatoporoids','13','Echinoderms','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3039,NULL,'The Minija Regional Stage forms the lower part\r\nof the Pridoli (Paskevicius 1997). Carbonates of\r\nthe Minija Regional Stage serve as a good example of a\r\ncarbonate ramp system with a stromatoporoid-crinoid-\r\nbrachiopod-dominated carbonate factory. According to the\r\nlithofacies distribution, the ramp can be subdivided into\r\nfive main facies belts...',NULL,NULL,NULL,NULL,'Lithuania','Europe',NULL,NULL,55.13,22.58,NULL,NULL,NULL,NULL,4.13204023279,-38.513670723,4.13204023279,-38.513670723,-14.2353,1.22266,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jablonna',4117,'','Permian','Lopingian','Wuchiapingian','Wuchiapingian',254.10,259.80,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','73','4','More than 1000 m wide','1500',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','7','Bryozoans','14','Brachiopods','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','50','4','Microbial precipitation','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','2','Intense',0,'No or unknown reservoir potential',3040,NULL,'Consists of three separate reef bodies, as established by a 3-D seismic\r\nstudy.',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,52.1,16.1,NULL,NULL,NULL,NULL,26.3501769277,33.1081594389,25.8614108912,28.260574125,18.0085,26.1943,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Bonikowo',4118,'Unknown','Permian','Lopingian','Wuchiapingian','Wuchiapingian',254.10,259.80,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','90','4','More than 1000 m wide','1600','4','More than 1000 m','1600',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','1d','Marginal marine - coastal -  siliciclastic shelf','3','Below storm wave base','7','Bryozoans','12','Foraminifera','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8','4','Microbial precipitation','1','Present','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','10-25% sparite','3','High production of reefal debris','1','Present',2,'Actual reservoir',3041,NULL,'The drillcore section is a mixture of boundstones (microbial and bryozoan), wackestones, packstones\r\nand grainstones, which often co-occur.',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,52.07,16.37,NULL,NULL,NULL,NULL,26.3617122232,33.2958804791,25.9338328642,28.4298279076,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Tebaga of Medenine',4119,'Unknown','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf',NULL,NULL,'12','Foraminifera',NULL,NULL,'71','Foraminifera only, (some corals)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','3','High production of reefal debris','2','Intense',1,'Potential reservoir',3042,NULL,'the northern edge of the Saharan platform. The exposed Permian sequence at Jebel\r\nTebaga of Medenine and Baten Beni Zid consists at least of 850m of marine strata grading to nonmarine red beds. It is made up of local biohermes, thin carbonate beds, bioclastic limestone, sandstone and shale. The main feature of Permian\r\nsequence is the abrupt and complex facies changes due to presence\r\nof obscure and inferred faults. Particularly, presence of the fusulinacean Yabeina at Oum el Afia section suggests that these rocks are younger than those outcropping at Baten Beni Zid.',NULL,NULL,NULL,NULL,'Tunisia','Africa',NULL,NULL,10.11,33.29,NULL,NULL,NULL,NULL,-31.3017941968,25.8930543318,-31.5097393457,24.8305554883,-36.6891,25.2986,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Penglaitan -Tieqiao',4120,'Heshan','Permian','Lopingian','Wuchiapingian','Wuchiapingian',254.10,259.80,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','91',NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','6','Calcisponges',NULL,NULL,'37','Sponges - microbes - Tubiphytes - (worms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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',3045,NULL,'The overlying Heshan Formation, 150 m\r\nin thickness, is composed of black cherty limestone of\r\nbasinal facies in the lower part and white bioclastic carbonate\r\nof sponge reef facies in the upper part. The Late\r\nWuchiapingian reefal carbonates about 91 m in thickness\r\nat the Tieqiao Section are reduced to 10 m in thickness\r\nat the Penglaitan Section.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,23.41,109.19,NULL,'189412',NULL,NULL,-19.1756293374,108.71703405,-2.32274426355,132.471691023,-1.38445,101.964,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gundara valley',4121,'Gundara','Permian','Cisuralian','Kungurian','Kungurian',272.30,283.50,15,'Sakmarian - Kungurian',277,280,'Early Permian (early Kungurian, 280 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','14','Brachiopods','3','Microbes','89','Brachiopods - echinoderms','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','10','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3046,NULL,'Our preferred palaeoenvironmental reconstruction is one of agglutinated\r\nmicrobial reefs to cluster reefs. The microbial reefs are formed by\r\nthe cyanobacterial microbialites Tubiphytes and Archaeolithoporella, with a few large\r\ncavities filled by botryoidal cements and subordinate skeletal elements. The cluster\r\nreefs are made by in-place conical skeletons of Gundaria insolita n. gen. n. sp. that\r\nwere adjacent but not always in contact with the substrate. The Gundaira insolita\r\nwere also able to trap loose sediment, which indicates that the reefs are matrixsupported.\r\nIn-place, pedicle-attached species contributed to the framework and helped\r\ntrap the matrix. These reefs were likely laterally extensive despite their low\r\ntopographic relief, which is consistent with the mostly bedded nature of the Gundara\r\nFormation. The abundance of matrix and the reduced cementation and bioerosion\r\nsuggest muddy depositional environments, which were probably deeper and more\r\nturbid than those of the Safetdara Formation.',NULL,NULL,NULL,NULL,'Tajikistan','Asia',NULL,NULL,38.45,70.53,NULL,'182702',NULL,NULL,18.0762550985,72.3655071928,38.0788532194,59.1910635083,24.5625,70.3551,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Dugway',4122,'Guilmette','Devonian','Upper Devonian','Frasnian','Frasnian-Famennian',358.90,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'4','Stromatoporoids','4','Stromatoporoids','75','Stromatoporoids or chaetetids only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3047,NULL,'In the Dugway Range, the massive, cliff-forming, peloidal, stromatoporoid-\r\nbearing reef facies is intercalated between thick-bedded,\r\ncarbonate-platform rocks of the lower Famennian, upper Guilmette\r\nFormation below and thin-bedded, upper-slope rocks of the Famennian\r\nWest Range Limestone above. The carbonate facies in the\r\nDugway Range represent the southernmost extension of carbonate bank\r\nthat is equivalent to and continuous with the so-called False Birdbear\r\nunit of the upper Jefferson Formation in Idaho, the upper limestone\r\nunit of the Logan Gulch Member of the Three Forks Formation in\r\nMontana, and the Morro Member of the Palliser Formation in Alberta,\r\nCanada. Carbonate-bank facies deposition persisted\r\nin an extensive, north-south–trending belt from the northern Great\r\nBasin into southern Alberta for at least 3 myr until the middle\r\nFamennian lower Palmatolepis marginifera biozone.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,40.01,-113.2,NULL,NULL,NULL,NULL,-16.4843933578,-66.4803722752,-7.88224407127,-125.007572956,-19.3744,-55.0561,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Agrio, Pilmatué Member, Loma Rayoso Area',4123,'Agrio','Cretaceous','Lower Cretaceous','Hauterivian','lower Hauterivian',129.40,132.90,23,'late Valanginian - early Aptian',126,130,'Early Cretaceous (Hauterivian, 131.2 Ma)',NULL,3,'0','Outcropping reef ',4,'True reef','1','10 to 100 m thick','2','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below storm wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','6 to 24 reef building species','3',NULL,NULL,'2','Intensive','2','Intensive','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','3','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',3048,NULL,'Coral biostrome (1.7 m thick) interbedded between two oyster shell beds. Only one coral species identifed, but one oyster and bryozoan species also indicated.\r\nThe biostrome is laterally continuous for more than 600m.\r\nThe studied section belongs to the upper half of the Pilmatué. The coral bed is interpreted as a coral biostrome. It is composed by low ramose coral colonies that did not form a rigid barrier, lacking lateral coalescence and overgrowing.',NULL,NULL,NULL,NULL,'Argentina','South America',NULL,NULL,-37.37,-70.09,NULL,'61589',NULL,NULL,-44.7772155518,-30.8197652922,-40.0399659553,-37.2682924985,-36.7235,-35.9292,'Krause','Kiessling','2021-05-28 15:21:12','2022-08-25 16:59:27'),('Rietoog',4124,'Omkyk Member','Ediacaran','Ediacaran','White Sea Assemblage','Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','20','2','10 - 100 m wide',NULL,'4','More than 1000 m',NULL,'7',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base','8','Serpulids, worms, vermetids','8','Serpulids, worms, vermetids','76','Worms only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3049,NULL,'Omkyk Member of the Kuibis Subgroup of the Nama Group, at the\r\nDriedoornvlagte pinnacle reef complex, near Rietoog. Reef-building by the earliest known skeletal metazoan, the globally distributed Cloudina',NULL,NULL,NULL,NULL,'Namibia','Africa',NULL,NULL,-23.51,16.39,NULL,'113370',NULL,NULL,-45.0509808147,80.7359229995,-45.0509808147,80.7359229995,-39.6523,176.219,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Tangwangzhai',4125,'Unknown','Cambrian',NULL,NULL,'Millardan',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',NULL,1,'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',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3050,NULL,'Two outcrop sections (Tangwangzhai and Laopozhuang sections) in Shandong Province. Microbial components comprise microstromatolites, calcified Girvanella filaments, and Renalcis-like botryoid forms. Microstromatolites, which are one of the most common components of the maze-like structures, mostly exhibit convex-up laminae composed of alternating micrite and microsparite',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,36.3,116.51,NULL,NULL,NULL,NULL,21.7916313692,100.95468066,21.7916313692,100.95468066,-3.4204,144.294,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Tangwangzhai',4126,'Unknown','Cambrian',NULL,NULL,'Millardan',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',NULL,1,'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',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3050,NULL,'Two outcrop sections (Tangwangzhai and Laopozhuang sections, about 20 km distant) in Shandong Province. Microbial components comprise microstromatolites, calcified Girvanella filaments, and Renalcis-like botryoid forms. Microstromatolites, which are one of the most common components of the maze-like structures, mostly exhibit convex-up laminae composed of alternating micrite and microsparite',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,36.34,117.04,NULL,NULL,NULL,NULL,21.5540935049,100.57039812,21.5540935049,100.57039812,-3.04313,144.498,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Fox Cove',4127,'Forteau','Cambrian','Series 2','Stage 4','late Botomian-Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',513,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3','1','Less than 10 m wide','10',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','10','Archaeocyaths','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3052,NULL,'At the Fox Cove locality, a series of archaeocyathan patch reefs of the lower Forteau Formation. Common components of all thin sections include microbial fabrics, carbonate cement, echinoderms, brachiopods, archaeocyaths and trilobites. Grainstone samples often contain\r\nabraded and broken fossil material as well as detrital\r\ngrains; reef samples are characterized by\r\nabundant microbial fabrics with archaeocyathans.',NULL,NULL,NULL,NULL,'Canada','North America',NULL,NULL,51.28,-56.49,NULL,NULL,NULL,NULL,7.66072685038,-98.950844966,7.66072685038,-98.950844966,-40.6385,-74.1598,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Herefordshire',4128,'Unknown','Silurian','Wenlock','Homerian','Homerian',427.40,430.50,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',NULL,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','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3053,NULL,'The central part of the buildup is formed by coral bafflestone, partly overlain\r\nby brachiopod-rich facies III. The buildup is formed by several pillow-shaped units. The transition\r\nto surrounding bedded facies V is gradual. The buildup framework is formed by complete, in situ colonies of rugose and tabulate corals, stromatoporoids and branching bryozoans. The sediment baffled between the framework builders consists of very poorly sorted echinoderm ossicles, brachiopods and rare ?Dimorphosiphon fragments, but the buildup fabric is distinguished by a high (ca 50%) micritic matrix. Allonema and Rothpletzellaare present as crusts and Rothpletzella also as loose\r\naccumulations within the matrix. These are associated with mottled, peloidal-like structures containing\r\nstructures tentatively identified as sponge spicules. The mottled fabrics contain multiple small\r\n(up to 0.4 cm wide) stromatactis-like cavities filled with spar, characterized by sharp basal parts and irregular undulating upper parts. In SEM images, oncoids and Rothpletzella\r\naccumulations floating in the matrix are built by tubes filled with sparitic cement. The tube walls\r\nare 5-6 µm thick, formed by regularly arranged needleshaped calcite crystals oriented perpendicular to the porostromate tube in longitudinal sections and radially in cross sections. In contrast, the mottled, peloidal matrix of facies IV is composed of chaotically arranged microcrystalline calcareous mud containing a high proportion of clay particles and scattered fragments of skeletal grains. The buildup is overlain by nodular wacke- to packstones composed of well-sorted echinoderm,\r\nbrachiopod, gastropod, trilobite and coral fragments (facies V) and onlapping the units represented by\r\nfacies II, III and IV.',NULL,NULL,NULL,NULL,'United Kingdom','Europe',NULL,NULL,52.07,-2.22,NULL,NULL,NULL,NULL,-15.7194414749,-53.4181340163,-15.7194414749,-53.4181340163,-20.7939,-14.8484,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Saaremaa',4129,'Unknown','Silurian',NULL,NULL,'Wenlockian-Ludlovian',423.00,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,'4','More than 1000 m wide','2000','4','More than 1000 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','4','Stromatoporoids','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',3054,NULL,'Due to constant southwards regression and infilling\r\nof the BSB, the lagoonal-littoral facies became increasingly\r\ndominant all over Saaremaa towards the end of Wenlock. At that time, the shoal facies only reached Saaremaa during short transgressions. A series of upwards shallowing cycles with shoal to lagoonallittoral\r\nsediments, often bracketed by discontinuity surfaces, therefore characterizes the Jaagarahu and Rootsiküla stages on Saaremaa',NULL,NULL,NULL,NULL,'Sweden','Europe',NULL,NULL,58.08,20.53,NULL,NULL,NULL,NULL,-1.74496962239,-46.6749704013,-1.74496962239,-46.6749704013,-10.7703,-4.30084,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Saraburi, Siam City Cement quarry along Highway 2',4130,'Khao Khad','Permian','Guadalupian','Wordian','Murgabian/Midian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','12','Foraminifera','13','Algae - encrusting forams','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','33',NULL,NULL,NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3055,NULL,'Peritidal zone deposits consist of dark carbonaceous mudstones-wackestones and dolomitised laminated algal boundstone beds. Secondary Fe-calcite camouflaged the original depositional texture in some parts. Fossils include Schubertella, Girvanella and Gyroporella algae, Hemigordius, Globivalvulina sp. along with other microscopic non-fusuline foraminifera. Peritidal settings were interpreted within Logs 1 and 4 with ages constrained between the late Murgabian to Midian.\r\nPlatform interior contains three sub-environments: lagoon, the outer platform and the higher energy backreef. The low-energy lagoon is comprised of bioturbated skeletal and peloidal wackestones and packstones with localised interbedded shales. The fossil assemblage contained abundant algae including Girvanella, bivalves (including alatoconchids), fusulinids (N. simplex) and microscopic non-fusuline foraminifera (Globivalvulina, Schubertella, Cribogenerina and Textulariida). The lagoonal environment is interpreted for lower Log 4 and upper Log 6 and deposited in the Murgabian with possible extension into the Midian.\r\nThe outer platform sub-environment is a non-parallel bedded bioclastic limestone grading from wackestone through to grainstone with boundstone interbeds. Isolated coral clumps were also observed within the grainstone sections. Inner platform settings were interpreted within Logs 1, 2, 5, 7 and 8. The age of the environment was constrained using the fusuline foraminifera (Neoschwagerina simplex, other Neoschwagerina sp., Neofusulinella, Nankinella, Kahlerina, Armenina). The fossil assemblages gave an age within the Murgabian Stage.\r\nThe higher-energy backreef sub-environment is defined by parallel bedded wackestones and packstones. Backreef settings are interpreted within Logs 5, 6 and 8. Each major fossil group is present in the Highway 21 backreefs: crinoids, fusulinids (Nankinella, Schwagerina, Colania, Neoschwagerina and Gifuella), bivalves (Alatyoconda), non-fusuline foraminif',NULL,NULL,NULL,NULL,'Thailand','Asia',NULL,NULL,14.38,101.07,NULL,NULL,NULL,NULL,-30.5536235087,116.318592952,-6.34918928484,102.543049871,-14.0517,99.8298,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Akiyoshi and Taishaku',4131,'Unknown','Carboniferous','Pennsylvanian','Gzhelian','Gzhelian-Asselian',295.00,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','4','More than 500 m thick','1000',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','2c','Atoll (circular structure)','3','Below storm wave base','2','Algae','7','Bryozoans','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','16','4','Microbial precipitation',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3057,NULL,'Palaeoaplysina–microencruster reef community.  In a reef-core area\r\nof the atoll, the alga Palaeoaplysina acted as a framebuilder and was associated with various binders (e.g., Tubiphytes,Archaeolithoporella, cystoporate bryozoans, and microbialites) and sediment-bafflers such as fenestrate and cryptostomate bryozoans and phylloid algae. In a subtidal environment of the back-reef area, Palaeoaplysina and phylloid algae flourished as sediment-bafflers. A microbial community, including Tubiphytes and sessile foraminifers, was predominant in a very shallow, peritidal environment of the back-reef area.',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,34.5,133.15,NULL,NULL,NULL,NULL,13.7507906599,139.091090935,17.8004597541,73.1113576858,13.8528,100.233,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Longdianshan Hill, Liuzhou',4132,'Long’an','Carboniferous','Mississippian','Tournaisian','upper Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','30','3','101-1000 m wide','150',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','3b','Deeper slope or outer ramp','2','Below fair weather wave base','7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3058,NULL,'The mud banks are composed of a mixture of two basic micro-facies: (1) spiculitic wackestone with diverse fauna includingcryptostome and fenestellid bryozoans, crinoids, ostracodes, andbrachiopods; (2) fine-grained bioclastic wackestone and pack-stone containing crinoids, bryozoans, sponges, brachiopods,ostracodes, and corals. The mud banks developed during a rela-tive sea-level rise in an outer deep platform margin, and died asrelative sea-level fell evidenced from the bioclastic wackestoneand packstone overlying the banks. The mud banks at Longdian-shan are similar to typical Waulsortian mud mounds, as indicatedby the presence of bryozoans, crinoids, and sponges, mud gen-erations and spar-filled cavities',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,24.13,109.18,NULL,NULL,NULL,NULL,-20.2576012828,93.1453988085,-7.07807609082,91.1948522295,-6.54838,98.7928,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gandongzi village and Xiadong village,, Langping, Guangxi',4133,'Du’an','Carboniferous','Mississippian','Visean','upper Visean',330.90,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','30','3','101-1000 m wide',NULL,NULL,NULL,'260',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','16','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3058,NULL,'Reef complex of various reef types stacked. Largest reef is R6, which is 19 m thick.\r\nCumulative thickness is 30 m\r\n\r\nBuilt mainly by the colonial rugose coral Thysanophyllumand the bryozoan Fistulipora, and less frequently by Syringo-pora (tabulate coral) and Lithostrotion (colonial rugose coral). Reef-dwellers include crinoids, brachiopods,solitary rugose corals, cryptostome bryozoans, foraminifers, gastropods, ostracodes, and green algae.Reefal units show four growth stages with the predominantframeworks of Thysanophyllum, Fistulipora, Thysanophyllum,and Fistulipora-Thysanophyllum, intercalated with intraclastic-crinoidal or crinoidal bank facies. The reef-crest is composedof gray thick-bedded algal peloidal packstones, fine bioclasticwackestones interbedded with brachiopod grainstones and pack-stones. The reef was formed at shallow isolated platform marginand died resulting from relative sea-level fall and rise respec-tively, which may be caused by regional rift activities. At Xiadong village, Langping, reef is about 260 m wide and 50 m thick andthe major reef-builders are colonial rugose corals (Diphyphyl-lum, Siphonodendron, and Lithostrotion), and the tabulate coralSyringopora. Reef-dwellers are solitary rugose corals, crinoids,ostracodes, brachiopods, gastropods, bryozoans, and calcareous algae.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,24.31,106.21,NULL,'215258',NULL,NULL,-20.0955708823,97.3863701648,-1.44381478899,78.2727588001,-15.3832,100.249,'Krause','Krause','2021-05-28 15:21:12','2021-06-17 11:55:24'),('Yashui',4134,'Shangsi','Carboniferous','Mississippian','Visean','middle Visean',340.00,345.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2.5–3.9','3','101-1000 m wide','500','3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Margin of shallow basins (platform margin)','2','Below fair weather wave base','1','Corals',NULL,'Brachiopods','2','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','10',NULL,NULL,NULL,NULL,NULL,'Present','3','Medium zonation',NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3058,NULL,'The middle Viséan coral biostrome from the Shangsi For-mation at Yashui, which is variable from 2.5 m to 3.9 m inthickness and more than 500 m in width, is composed mainlyof Kueichouphyllum (solitary rugose coral), Syringopora,and Siphonodendron. Associated fossils include brachiopods,crinoids, foraminifers, calcareous algae, gastropods, bryozoans,and ostracodes. In the biostrome, three growthstages have been distinguished, which in ascending order areKueichouphyllum growth stage, Kueichouphyllum-Syringoporagrowth stage, and Siphonodendron growth stage. The biostromeoccurred at shallow DQGX platform margin with its growthand demise controlled by relative sea-level rise and fall, asevidenced from the increasing of micrites and sparry calcitein the biostrome and its overlying limestone, respectively. Compared with the coral reefs, the coral biostromelacks calcimicrobe encrustation and sparry calcite cementation',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.59,106.45,NULL,NULL,NULL,NULL,-21.2172414108,96.6875137847,-0.977568238686,77.0607251309,-15.6433,98.9293,'Krause','Siphonodendron','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Mengcun and Helü',4135,'Tatang','Carboniferous','Mississippian','Visean','upper Visean',330.90,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','21','3','101-1000 m wide','150',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3058,NULL,'Morphologies of these stromatolites include laminar, wavy-laminar, domal or hemispheroidal, bulbous, and flabellate-growth columns. Individual stromatolites are generally 3–6 cm thick, which can grow upward upto 60 cm thick in the core facies. The core-facies of stromatolite mounds were formed by calcimicrobes, with initially horizontal laminar and tabular growthforms later becoming domal and bulbous forms, and finally flabellate columnar forms indicating a gradual relative sea-level rising. The occurrence of talus breccias under and above themounds suggests that they were located at a deep slope setting.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,23.36,109.22,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,-12.4745,100.098,'Krause','Krause','2021-05-28 15:21:12','2022-08-25 17:28:52'),('Beibuwan',4136,'Dabu','Carboniferous','Pennsylvanian','Bashkirian','upper Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',NULL,3,'0','Outcropping reef ',NULL,NULL,'3','101-500 m thick','300',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,'2','Algae','13','Echinoderms','13','Algae - encrusting forams','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3058,NULL,'One 300 m thick core of the late Bashkirian-middle Kasi-movian red algae reef crops out in the Dabu and Huanglongformations at Beibuwan. It is located at shallow SW plat-form margin. Themain constructors are the red algae Parachaetetes and Ung-darella. Reef-dwellers include crinoids and fusulinids. Fivesimilar growth stages, characterized by Parachaetetes and Ung-darella bindstone, can be identified, which are separated by fourgrowth intermissions dominated by dolostones, and the fifthgrowth stage also has some small growth intermissions.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,21.26,106.45,NULL,NULL,NULL,NULL,-11.4190502644,109.128179398,4.23242759886,97.7140301382,-13.6095,102.293,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Xinzhai and Longjiangdong Langping',4137,'Huanglong','Carboniferous','Pennsylvanian','Bashkirian','upper Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','20','2','10 - 100 m wide','28',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','13','Echinoderms','85','Corals - (phylloid) algae','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3058,NULL,'Coral patch reef, whichis 15 m in width and 20 m in thickness, is composed mainly ofcolonial rugose corals: (Lonsdaleia and Antheria), and Syringo-pora with crinoids filling around them. \r\nLongjiangdong biostromal reef is about28 m wide and 15 m thick, grows on crinoidal banks, and hasthree cyclical growth stages. Diphyphyllumis abundant and accessory organisms are crinoids, brachiopods,calcareous algae, and foraminifers (Fig. 5B). The coral patchreef at Longjiangdong is about 20 m wide and 8 m thick. Themain reef-builders are Thysanophyllum and Lithostrotionella(Petalaxis) (colonial rugose coral) with Caninia (solitary rugosecoral) secondarily incorporated. Thysanophylum and Lithostro-tionella successively occur in the reefs in clusters, and Caniniarandomly grows near the clusters. Reef-dwellers are mainlycrinoids. TheLongjiangdong reefs were formed at shallow SW platform margin, and grew and demised due to relative sea-levelrise and fall, resulting from the increasing micrites and sparrycalcite in the reefs and their overlying limestones, respectively',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,24.49,106.36,NULL,NULL,NULL,NULL,-11.8553243184,105.859489183,4.77473563139,94.5189226926,-12.3537,99.2377,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lianyuan and Lengshuijiang, Hunan Province',4138,'upper Zimenqiao Formation to lower Dabu Formation','Carboniferous','Mississippian','Serpukhovian','Serpukhovian-Bashkirian',315.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',318,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','6','Calcisponges','78','Calcisponges - serpulids - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3058,NULL,'In Lianyuan and Lengshuijiang cities, HunanProvince, the Serpukhovian-middle Bashkirian massive lime-stones (about 5 m thick) from the upper Zimenqiao Formation tolower Dabu Formation contain abundant benthic fossils includ-ing fasciculate colonial rugose corals, fasciculate tabulate corals,and chaetetids. They locally form bounded frameworks whichresemble the contemporaneous reefs in Akiyoshi, Japan. Besides, stromatolites also occurred in Lianyuan-Lengshuijiang areas during this time',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,27.7,111.63,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Yashui',4139,'Baizuo Formation','Carboniferous','Pennsylvanian','Bashkirian','lower Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,320,'Early Pennsylvanian (Bashkirian, 319.2 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','0.3','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'1','Corals',NULL,'Echinoderms','2','Tabulate/rugose corals - crinoids - (microbes inferred)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3058,NULL,'formed by in situ upright fasciculate colonial rugosecorals. Preliminary data indicate that dwellers of this coralboundstone include crinoids, brachiopods, foraminifers, ostra-codes, gastropods, bryozoans, calcareous algae, and solitaryrugose corals. This coral boundstone was located at shal-low SW platform margin during the early Bashkirian, and it grew and died as relative sea-level rose and fell respec-tively, evidenced from increasing micrites and sparry calcite inthe boundstone and its overlying limestone, respectively. Therefore, the Serpukhovian-middle Bashkirian has the poten-tial for reef development, and the discovery of reefs is to be made',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.59,106.45,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Siphonodendron','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Benxi Area, Liaoning',4140,'Unknown','Carboniferous','Pennsylvanian','Moscovian','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'6','Calcisponges','1','Corals','35','Chaetetids - corals - cyanoyphyceans - algae - (bryozoans)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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',3059,NULL,'Benxi Area, Liaoning Chaetetes – coral reef. At the beginning of the Pennsylvanian, a massive south-north transgression occurred in this region. The sedimentary environment changed from fan delta to fiord coast and then into a carbonate platform, and thus several reefs with\r\na nearly east-west trend were built on the nearshore side of the platform. These reefs are relatively small, with thickness of 2–4 m. There are abundant benthic organisms found in these reefs, and the biotic content is up to 60% of the reef volume. Arachnastraea manchurica and\r\nChaetetes penchiensis are the dominant building organisms in these reefs. Their colonial skeletons are tabular in shape with varying thickness. Multithecopora penchiensis is the secondary building organism in the reefs of this region, and it mainly occur in the spaces between Chaetetes and Arachnastraea. There are also such binding organisms in the reef as Archaeolithoporella and Girvanella. The organisms associated with the Chaetetes coral reef are fusulinids, foraminiferans, brachiopods, ostracodas, bryozoans, gastropods and various genera of algae.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,41.18,123.46,NULL,NULL,NULL,NULL,17.7694454471,129.037398182,18.0759519927,66.3857596837,16.9674,93.5622,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Eastern Tianshan, Xinjiang',4141,'Qijiagou','Carboniferous','Pennsylvanian','Moscovian','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'7','Bryozoans','2','Algae','18','Bryozoans - microbes - (algae) - (crinoids)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3059,NULL,'occurred in the Tianshan-Xingan active ocean trough. Coral pach reef, bryozoan-calcareous algae mound',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,43.49,87.36,NULL,NULL,NULL,NULL,22.9161613293,81.1225508994,44.0606192156,59.7553501427,38.4762,65.1336,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Beibuwan Area, Guangxi',4142,'Maping','Carboniferous','Pennsylvanian','Gzhelian','Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',NULL,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,'6','Calcisponges','2','Algae','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3059,NULL,'Parachaetetes and Ungdarella are the main reef-building\r\norganisms. Calcareous green algae are also associated\r\nwith these reefs',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,21.26,106.45,NULL,NULL,NULL,NULL,-13.7082715349,138.421352982,8.11814898394,107.516450224,-13.6095,102.293,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Mineral Mountains, Utah',4143,'Unknown','Triassic','Lower Triassic','Olenekian','middle-upper Scythian',247.20,250.00,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','15',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'6','Calcisponges','3','Microbes','37','Sponges - microbes - Tubiphytes - (worms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3060,NULL,'Early Smithian reef deposits are characterized by more diverse sponge morphologies. The oldest sponges are embedded within\r\nmicrobialites forming reefs, tens of centimetres thick, distributed\r\nthroughout a massive (up to 10m high) microbial carbonate unit.\r\nThese microbialites are composed of centimetre-scale stromatolitic\r\ndomes and thrombolites sealed off by micrite. Complete cup- to\r\nflat-shape and dendroid centimetre-scale sponges are preserved,\r\nresting on micrite matrix or encrusting microbialitic crusts. They\r\nshow an internal re-crystallized spiculitic network and are often partially to completely dissolved and replaced by calcite-cemented\r\ncavities.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,38.36,-112.82,NULL,NULL,NULL,NULL,22.2705927227,-34.4092076494,15.6281392391,-39.04903958,13.7696,-38.5483,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Pahvant Range, Utah',4144,'Unknown','Triassic','Lower Triassic','Olenekian','middle-upper Scythian',247.20,250.00,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20','2','10 - 100 m wide','50',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'6','Calcisponges','8','Serpulids, worms, vermetids','37','Sponges - microbes - Tubiphytes - (worms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3060,NULL,'the oldest reefs consist of small (ca. 5mm) sponges\r\nencrusting thin bivalve shell layers, which probably facilitated\r\ntheir settlement and enhanced their preservation. Although\r\nthese sponges are preserved in life position, their initial essentially\r\nglobular shape now seems compacted. The sponges are associated with small serpulids within a very abundant micritic matrix, and with common echinoderm plates (probably crinoids) locally reworked as bioclastic accumulations in storm-induced deposits. These biostromes, tens of centimetres thick, are formed by alternating gregarious settling and hydraulic reworking. The latter leads to multiple short-term events of hard-part concentrations in a low to moderate energy mid ramp environment.\r\nIsolated sponges are also found within overlying beds, identified\r\nonly by sparse bundles of spicules. Sponges occur a few metres\r\nhigher in recurrent large (ca. 50 m of lateral exposure) lenticular ca. 5-\r\ncm-thick layers, throughout a ca. 20 m-thick stratigraphic interval. These sponges are preserved in situ as lenticular reefs composed of small coalesced spheres (ca. 1 cm in diameter) that resemble lyssacine hexactinellids bound by submillimetre-scale biofilms. Within the lowermost Spathian PR beds, serpulids form small millimetre to centimetre-consortia with abundant ostracods, brachiopods and rare gastropods, alternating\r\nwith tempestite deposits',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,38.86,-112.23,NULL,NULL,NULL,NULL,22.5659662939,-33.7465036836,15.843317161,-38.3787476131,13.973,-37.8798,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Willow Spring locality, Olds Ferry terrane, Blue Mountains Province, northeastern Oregon',4145,'Huntington','Triassic','Upper Triassic','Norian','Norian-Rhaetian',201.30,228.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','100',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin',NULL,NULL,'1','Corals','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3062,NULL,'Upper member of the Huntington Formation (Olds Ferry terrane) at a locality. Corals at the site include a high-growing, dendroid-phaceloid\r\nspecies that acted as either framework or sediment baffles, and a lowgrowing, cerioid, encrusting coral and a sponge that acted as sediment herein named Willow Spring. binders. Together, these organisms produced at least a 10–50 cm high reef-like or reefal framework. Framework mineralogy of sandstones and clast types in the\r\nconglomerate suggest that the source of these Triassic coral-sponge reef faunas was intrabasinal. The occurrence of the same two coral taxa in the Wallowa and Olds Ferry terranes may support the proximity of these two regions in the late Triassic, but the presence of these taxa in other Cordilleran terranes suggests that they are probably cosmopolitan and therefore not good indicators of terrane proximity.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,44.24,-117.14,NULL,NULL,NULL,NULL,18.0123929912,-43.0571031854,28.4997098552,-47.0009227273,18.5329,-53.687,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Paluma Shoals, Halifax Bay',4146,'Unknown','Quarternary','Holocene','Holocene','Holocene',0.00,0.00,34,'Holocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','29',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3064,NULL,'The palaeoecological assemblages of the PSRC are representative of inner-shelf reef communities across the central GBR, which are characterised by mixed assemblages of acroporids (Montipora, and locally abundant Acropora), dendrophyllids (Turbinaria), euphylliids (Euphyllia and Galaxea), and poritids (Goniopora and Porites). The composition of\r\ninner-shelf coral communities distinguishes them from those associated with mid- and outer-shelf reefs, which are predominantly characterised by assemblages of Acropora',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.06,146.3,NULL,NULL,NULL,NULL,-19.06,146.3,-19.06,146.3,-19.06,146.3,'Krause','Krause','2021-05-28 15:21:12','2022-08-09 21:13:27'),('Stadion locality',4147,'Unknown','Neogene','Miocene','Upper Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','10','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','12','Foraminifera','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','67','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3065,NULL,'diverse assemblage that includes corals, foraminifers, coralline algae, bryozoans, and mollusks. In addition, some echinoid spines, serpulid tubes, small brachiopods, and crustacean chelae were found within the sediments or cemented to coral surfaces. low-relief patch reef',NULL,NULL,NULL,NULL,'Indonesia','Asia',NULL,NULL,-0.58,117.12,NULL,NULL,NULL,NULL,0.587337237239,116.186108319,-1.03794487983,116.448018362,-0.213382,119.007,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jiulongshan, Laiwu',4148,'Zhangxia','Cambrian','Series 3','Guzhangian','Marjumian',500.50,504.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1','1','Less than 10 m wide','9',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3066,NULL,'lower part of the Zhangxia Formation (Crepicephalina Zone: Drumian of Cambrian Series 3). The coralomorph-bearing lithistid demosponge-microbial reefs are intercalated within bioclastic wackestone beds. Thin veneers of stromatolites. In places, sheet-like micrite layers and knobshaped stromatolites consisting of vesicular and globular clots pave the\r\nunderlying wackestone. The underlying wackestone was stabilized by microbial consolidation, which then provided suitable substrates for the microbial reefs. Bioclastic wackestone is thus conformably overlain by the basal parts of the microbial reefs.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,36.04,117.79,NULL,NULL,NULL,NULL,23.9292864478,97.9210924625,23.9292864478,97.9210924625,-2.7025,145.082,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Ile de la Grosse Romaine',4149,'Romaine','Ordovician','Lower Ordovician','Floian','Arenig',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',NULL,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','6','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,'3519',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','11','Siliceous sponges','14','Brachiopods','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3067,NULL,'Mostly composed of peritidal and open-shelf carbonates. Well-developed thrombolite mounds occur in the middle part of the Romaine Formation either as small submeter isolated bioherms or as closely spaced buildups forming larger bioherm complexes up to 6 m high and several tens of meters wide.',NULL,NULL,NULL,NULL,'Canada','North America',NULL,NULL,50.16,-63.49,NULL,NULL,NULL,NULL,0.621301507844,-86.8520066001,0.621301507844,-86.8520066001,-29.0582,-50.6491,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Ile à la Chasse',4150,'Romaine','Ordovician','Lower Ordovician','Floian','Arenig',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick','6','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,'3519',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','11','Siliceous sponges','14','Brachiopods','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3067,NULL,'Coalescent metersized thrombolite heads with a distinctive macroscopic clotted appearance exhibiting a cerebroid pattern in plan view and a digitate branching pattern in cross-section. They are flanked by a ripple-laminated to cross-bedded skeletal dolograinstone interpreted as coarse bioclastic haloes or channels separating individual bioherm complexes.',NULL,NULL,NULL,NULL,'Canada','North America',NULL,NULL,50.13,-63.11,NULL,NULL,NULL,NULL,0.455648549068,-86.6709962215,0.455648549068,-86.6709962215,-29.199,-50.4191,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('South end of the Franklin Mountains at El Paso, Texas',4151,'Unknown','Ordovician','Lower Ordovician','Floian','Arenig',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','6','2','10 - 100 m wide','20',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','2','Algae','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3067,NULL,'Small metazoan-microbial reefs, massive, barrel- to lens-shaped bioherms a few meters high and 2–5 meters across. in situ biotic builders are microbialites (mainly thrombolites) and lithistid, calathid, and pulchrilaminid sponges; many are dominated by thrombolites, some are dominated by Calathium, and a few are dominated by lithistid sponges.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,44.51,-73.21,NULL,NULL,NULL,NULL,0.407545983707,-95.5157463195,0.407545983707,-95.5157463195,-30.0133,-60.5521,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Hudson Platform on Southampton Island',4152,'Red Head Rapids','Ordovician','Upper Ordovician','Katian','Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15','3','101-1000 m wide','500',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'6','Calcisponges','3','Microbes','45','Siliceous sponges - calcisponges - microbes - (algae)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3068,NULL,'At the northern end of the Hudson Bay, the massive cores have been loosely described in the past as micritic, algal, or microbial limestones with metazoans. The Red Head Rapids Formation mounds are locally partly  dolomitized. The reefs contain large voids and vugs that are locally filled with bitumen and dead oil, composed of boundstone and cementstone  with various proportions of early calcified sponge tissues, microbial encrusters, synsedimentary cement and small  metazoans. The accretionary mechanisms of the Red Head Rapids Formation were mainly the result of frame building by early calcified sponges and small colonial corals and binding by calcimicrobial elements for the boundstone facies, and of marine cement precipitation near the seafloor for the cementstone facies.',NULL,NULL,NULL,NULL,'Canada','North America',NULL,NULL,64.21,-84.16,NULL,NULL,NULL,NULL,-1.88626321103,-101.159114403,-1.88626321103,-101.159114403,-5.77856,-44.747,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wadi Al-Ain 6',4153,'Hanifa','Jurassic','Upper Jurassic','Oxfordian','late Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','3','101-500 m thick','123.25',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','1a','Shallow intra-platform','3','Below storm wave base','4','Stromatoporoids','1','Corals','22','Stromatoporoids/sponges - corals - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',1,'Potential reservoir',3071,NULL,'Carbonate ramp. Close (~150 km) to large commercial hydrocarbon fields in Saudi Arabia',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,24.03,46.38,NULL,NULL,NULL,NULL,-13.8719705981,39.0512359004,-10.5101137298,36.4714469547,-3.07063,34.1084,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wadi Dirab',4154,'Hanifa','Jurassic','Upper Jurassic','Oxfordian','late Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','3','101-500 m thick','122',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','1a','Shallow intra-platform',NULL,NULL,'1','Corals','6','Calcisponges','22','Stromatoporoids/sponges - corals - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',1,'Potential reservoir',3071,NULL,'Bioturbated spiculitic wackestone/mud-dominated packstone facies. The facies is characterized by crumbly appearance and nodular bedding produced by\r\nbioturbation. Hardground surface encrusted with oysters. Sponge spicules in a micritic matrix. Mud-dominated packstone with sponge spicules, echinoids, and the foraminifera species, Redmondoides lugeoni, Photomicrograph of wackestone with sponge spicules, echinoids and brachiopods',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,24.26,46.34,NULL,NULL,NULL,NULL,-13.3234016386,39.1517087859,-10.2879377759,36.5423987438,-2.84844,34.1782,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jabal Al - Abakkayn',4155,'Hanifa','Jurassic','Upper Jurassic','Oxfordian','late Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','3','101-500 m thick','114',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','1a','Shallow intra-platform','3','Below storm wave base','1','Corals','12','Foraminifera','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',1,'Potential reservoir',3071,NULL,'Coral facies-capped cycles with bioherms',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,24.57,46.11,NULL,NULL,NULL,NULL,-12.9620444357,39.0522388009,-9.91705248302,36.4925769309,-2.47757,34.1291,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Dalmiapuram limestone quarry',4156,'Dalmiapuram','Cretaceous','Lower Cretaceous','Albian','Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','12',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)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3072,NULL,'Ostracods, bryozoans, gastropod fragments. Grey shale with frequent interbeds of fossiliferous grey limestone (the thickness of which increases upwards) and to a minor extent it is composed of a significant admixture of silt-sized siliciclastics. Coral algal limestone.',NULL,NULL,NULL,NULL,'India','Asia',NULL,NULL,10.58,78.56,NULL,NULL,NULL,NULL,-44.300018006,45.2858087275,-44.8597317752,35.588664139,-50.9094,35.8712,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Raghbah',4157,'Hanifa','Jurassic','Upper Jurassic','Oxfordian','late Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','86',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1d','Marginal marine - coastal -  siliciclastic shelf','3','Below storm wave base','1','Corals','12','Foraminifera','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',1,'Potential reservoir',3071,NULL,'Coral buildups. Prominent bench formed by the cross-bedded peloidal-skeletal grainstone facies. Grainstone and bioherm facies that can be traced over relatively long distances',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,25.13,45.57,NULL,NULL,NULL,NULL,-12.271855423,38.7672587838,-9.19663246428,36.3036922484,-1.75722,33.9424,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Brattefors',4158,'Unknown','Ordovician','Middle Ordovician','Dapingian','Middle Ordovician',458.40,470.00,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',3070,NULL,'Limstone reef. Oil samples from the Brattefors quarry are characterized by pyrene concentrations higher than phenanthrene. Oil samples from Brattefors quarry in south central Sweden were heated by volcanic intrusions with high pyrene/phenanthrene ratios and have C29 S/R sterane ratios significantly\r\nbeyond the normal thermodynamic threshold.',NULL,NULL,NULL,NULL,'Sweden','Europe',NULL,NULL,58.2,12.33,NULL,NULL,NULL,NULL,-27.1977355329,-69.2826618554,-27.1977355329,-69.2826618554,-37.6395,-12.4134,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Bernatai',4159,'Unknown','Ordovician','Upper Ordovician','','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',3070,NULL,'Reservoir oil. Limstone reef.',NULL,NULL,NULL,NULL,'Lettland','Europe',NULL,NULL,56.3,21.11,NULL,NULL,NULL,NULL,-30.6956241717,-61.2952349084,-30.6956241717,-61.2952349084,-33.7878,-2.24059,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Adze-6',4160,'Unknown','Ordovician','Upper Ordovician','','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3070,NULL,'Limstone reef.',NULL,NULL,NULL,NULL,'Lettland','Europe',NULL,NULL,57.01,21.36,NULL,NULL,NULL,NULL,-29.9728717735,-61.3238799436,-29.9728717735,-61.3238799436,-33.0662,-2.29789,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Rute-1',4161,'Unknown','Ordovician','Upper Ordovician','','Upper Ordovician',443.40,458.40,5,'Darriwilian - Ashgillian',452,460,'Middle Ordovician (late Darwillian,460 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',3070,NULL,'Limestone reef.',NULL,NULL,NULL,NULL,'Sweden','Europe',NULL,NULL,57.44,18.49,NULL,NULL,NULL,NULL,-29.8568857412,-63.1787689078,-29.8568857412,-63.1787689078,-32.9998,-4.21899,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Nanjiang, Shatan section',4162,'Xiannüdong','Cambrian','Series 2','Stage 3','Atdabanian/Botomian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','110','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3076,NULL,'Microbial reefs containing archaeocyaths, up to 1.5 m thick, are composed of massive to lenticular thrombolites with densely distributed, millimeter- to centimeter-scale darker mesoclots and rare archaeocyaths. These microbial reefs are enclosed by wackestone–packstone, intraclast packstone– grainstone, ooid packstone–grainstone, calcareous shale, and\r\nfine sandstone. The thrombolites are composed mainly of Girvanella, micritic\r\nclumps, and subordinate Epiphyton.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,32.42,106.83,NULL,NULL,NULL,NULL,-4.23555149135,78.2955671442,-4.23555149135,78.2955671442,27.2729,164.478,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('La Désirade Island, Lesser Antilles',4163,'Unknown','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','20',NULL,NULL,NULL,'3','More than 100 m','100',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','1','Corals','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',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',3077,NULL,'The coral layers are dominated by either scattered domal and thick lamellar\r\ncolonies of Diploria spp., in life position or elkhorn Acropora palmata\r\nrepresented by up to 2-m-thick coral patches or coral breccia. An irregular\r\nerosive surface incises up to 2 m depth into the top of Unit 1. Unit\r\n2 consists of the three following layers. Scattered thick lamellar\r\nDiploria sp. and domal Orbicella colonies in life position, columnar Orbicella\r\nspp. patches up to 4 m thick and 100 m long, and rare, scattered\r\nAcropora palmata. Coral patches form bioherms and are surrounded\r\nand overlain by m-thick-bedded, coarse-grained calcarenites\r\nwith clay, and by dm-to-m-thick-bedded and clayey, sand-supported\r\nred breccia. These breccia include pebbles from the substratum, dm-toover-\r\nm-sized coral fragments, and a few bioclasts.',NULL,NULL,NULL,NULL,'France','Europe',NULL,NULL,16.3,-61.07,NULL,'189821',NULL,NULL,16.2857683064,-61.0703850054,16.2940220618,-61.0685944177,16.294,-61.0686,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kampung Lembah Tuwi, near Kangar',4164,'Lower Setul Limestone','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','28.5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3078,NULL,'These dome-shaped microbialites grew directly on skeletal packstones and grainstones with abundant oncoids. Laterally, the massive microbial boundstone grades into surrounding bioclastic limestones. The microbial reefs are mainly composed of cylindrical columnar stromatolites (8- 35 cm wide and 30-105 cm high), with a distinct laminar texture present over the weathered surfaces. Several stromatolites usually occur alongside each other and are packed together, creating a frame-like cluster structure. Interspaces between stromatolites are often filled with Calathium. lithistid sponge-microbial bafflelbindstones that generally lack recognizable lamination and are characterized by in situ sponges',NULL,NULL,NULL,NULL,'Malaysia','Asia',NULL,NULL,6.26,100.11,NULL,NULL,NULL,NULL,3.94526159004,94.2900167064,3.94526159004,94.2900167064,32.0932,144.555,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Blue River, East Greenland',4235,'Kap Stosch','Triassic','Lower Triassic','Induan','Dienerian',251.20,251.80,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','0.2','1','Less than 10 m wide','0.3','1','Less than 20 m','0.5',NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','8','Serpulids, worms, vermetids',NULL,NULL,'76','Worms only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3184,NULL,'The East Greenland bioaccumulations developed within a restricted Boreal mid-paleolatitude seaway, and comprised a monospecific primary framework of microconchid ‘lophophorate’ tubes with shell fragments and phosphatic debris cemented by biogenic\r\ncalcite.\r\nWordie Creek Group',NULL,NULL,NULL,NULL,'Denmark','Europe',NULL,NULL,73.8,-21.5,NULL,'196949',NULL,NULL,43.9125381794,22.7216714117,35.4892990562,13.8384491585,35.4371,4.20078,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Baimiaozi, Jialing River, Beibei',4234,'Feixianguan','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick','1.5','1','Less than 10 m wide','4','1','Less than 20 m','7.5','1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes',NULL,NULL,'64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2','4','Microbial precipitation',NULL,NULL,'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',3183,NULL,'10 microbial mounds\r\nConodont fossils such as Hindeodus parvus?\r\nand Isarcicella staeschei were found in the microbial mounds, and these fossils indicate\r\nthat the age is that of the lower Griesbachian Stage.\r\nThe microbial mounds in this study can be considered to be composed of three facies, namely, a\r\nmound base, mound body, and mound cap.\r\nGrowth below \"normal\" wave base.\r\n',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,29.811944,106.456,NULL,NULL,NULL,NULL,-10.5827744054,105.965965452,13.0738504181,122.963853873,10.9917,95.1605,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jebel Toksine, Dades Valley',4233,'Unknown','Jurassic','Lower Jurassic','Toarcian','(early?) Toarcian',174.10,182.70,19,'late Hettangian - early Aalenian',188,180,'Early Jurassic (Toarcian, 178.4 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','10','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3182,NULL,'Two main intervals dominated by lithiotid\r\nand lithiotid-coral biostromes. Lithiotid intervals are characterized by alternating ooid-, peloid- and skeletal-rich wackestones to grainstones\r\ninterbedded with thick lithiotid and lithiotid-coral rudstones to framestones. Bivalve fauna, rare megalodontids.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.44,-5.54,NULL,NULL,NULL,NULL,18.7013613574,4.77064088268,24.6250614256,4.57829769876,26.0698,-2.88533,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Fath',4232,'Asmari','Paleogene','Oligocene','Chattian','late Chattian',23.00,25.00,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','3','Below storm wave base','1','Corals','2','Algae','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3181,NULL,'Constructed coralgal build-ups.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,30.37,50.49,NULL,NULL,NULL,NULL,24.5249588025,45.520302808,22.7707226289,47.194868811,26.44,47.3904,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Ganjgon, Late Rupelian',4231,'Asmari','Paleogene','Oligocene','Rupelian','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base','1','Corals','2','Algae','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3181,NULL,'Further down-dip, larger benthic foraminifers (large Nummulites test, Operculina and Neorotalia) packstone-grainstone along with discrete coral patches and coralline red algae',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,30.16,51.46,NULL,NULL,NULL,NULL,23.1038260179,45.4434779069,21.104139131,47.4208866251,22.549,45.5597,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Mt. Ishidate2, Befu-Kito area',4165,'Unknown','Triassic','Middle Triassic','Ladinian','late Ladinian - early Carnian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3079,NULL,'Massive limestone slab. sponge-microbialite boundstones. Abundance of sponges. The reef framework represents a relatively low volume and does not exceed\r\n33%. High abundances of Tubiphytes and peloidal and clotted micrite.',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,33.46,134.4,NULL,NULL,NULL,NULL,7.03872564478,134.787936946,31.1194432743,133.213406926,41.083,116.434,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Mt. Ishidate1, Befu-Kito area',4166,'Unknown','Triassic','Upper Triassic','Carnian','Carnian-Norian',208.50,235.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'11','Siliceous sponges','8','Serpulids, worms, vermetids','4','Siliceous sponges - echinoderms - scleractinian corals - worms',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','14',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3079,NULL,'Massive limestone slab.sponge-dominated reefs during the Late Carnian–Norian to Rhaetian?. abundance of Chaetetids, and the presence of Galeanella sp., Microtubus communis, Decapoalina schaeferae, Alpinophragmium perforatum and Actinotubella gusici. significant reef framework (40–60% of the rock volume)',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,33.46,134.4,NULL,NULL,NULL,NULL,34.6239230155,143.730072062,40.8535114007,151.16792882,41.083,116.434,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wajiki area, Anan, Tokushima prefecture',4167,'Unknown','Triassic','Upper Triassic','Carnian','Carnian-Norian',208.50,235.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'11','Siliceous sponges','8','Serpulids, worms, vermetids','4','Siliceous sponges - echinoderms - scleractinian corals - worms','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','14','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3079,NULL,'Reef limestone clasts crop out, along with basaltic clasts and limestone clasts of other facies, in a VCM breccia. This unit is in tectonic contact with recrystallized massive limestone slabs. Reef limestone crops out in VCM breccia. The reef framework volume is relatively low (approximately 30%) but sponges are comparatively abundant (21%) and Tubiphytes are rare. Sponge-dominated reefs.',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,33.52,134.33,NULL,NULL,NULL,NULL,34.6940535226,143.674495926,40.9297212091,151.122101559,41.149,116.366,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Hellnmaria Member',4168,'Notch Peak','Cambrian',NULL,NULL,'Upper Cambrian',485.00,497.00,3,'Franconian - Tremadocian',488,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','3',NULL,NULL,NULL,'4','More than 1000 m',NULL,'20',NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'1','Low production of reefal debris','2','Intense',0,'No or unknown reservoir potential',3080,NULL,'Tightly packed round to sub-round microbialites.Microbialites in zone 1 are stromatolitic, have diameters of between 10 to 30 cm at their longer axes, and are typically 20–40 cm tall. Synoptic relief is about 10–20 cm. The interspace material is an intra-bioclastic grainstone with some minor packstone domains. Allochems, predominantly composed of\r\nintraclasts (50%) and trilobite bioclasts (40%), average 0.5–4 mm in length, appear moderately sorted, sub-rounded, but generally are not\r\nspherical. Some trilobite bioclasts are over 1 cm long. Zone 1 microbialites have a small areal distribution of about 1 km2. Microbialites in zone 2, which cover the majority of the bed,\r\nare also stromatolitic, have diameters that vary from 40 to 70 cm across their longer axes, and have heights that fluctuate from a few dm to about 70 cm. Synoptic relief is about 10–20 cm. The interspace material is an intrabioclastic grainstone with some minor packstone domains. Allochems, predominantly composed of intraclasts (70%) and trilobite bioclasts (20%) average 0.5–2 mm in length, appear well-sorted, well-rounded, and are sub-spherical. These microbialites are chiefly differentiated from those in zone 1 by the presence of a central core composed of mini-stromatolites. Sponges are recognized as spicule networks that typically do not exceed a few cm in size, with many not exceeding 1 cm',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,39.1,-113.3042,NULL,NULL,NULL,NULL,30.7561914349,-119.130915687,30.7561914349,-119.130915687,-3.24291,-88.1097,'Krause','Kiessling','2021-05-28 15:21:12','2023-02-07 16:35:11'),('Fins, Sharqiyah region',4169,'Unknown','Quarternary','Pleistocene','Pleistocene','late Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1.5','2','10 - 100 m wide','20',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7','1','Constructor guild','2','Intensive',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3084,NULL,'The micritic to microspariticmatrix supports fragments of red algae, corals, small bivalves, echinoid with syntaxial overgrowth, monaxon sponge spicules (some made of silica, some made of calcium carbonate) and bryozoans. The vuggy pores of a dissolved coral are partly filled with equant, drusy calcite cement',NULL,NULL,NULL,NULL,'Oman','Asia',NULL,NULL,22.55,59.12,NULL,NULL,NULL,NULL,22.5370273108,59.1083092486,22.5308964415,59.1097460005,22.537,59.1083,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Carysfort Outlier Reef, Florida',4170,'Unknown','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m','500',NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3087,NULL,'Substage 5a reef growth recorded from -15 to -11 m MSL, spanning an age range of 86.2-80.9 ka. Shallow fore- and back-reef facies dominated by the head corals Montastrea annularis and Colpophylia natans,\r\nand the branching coral Acropora palmata.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,25.13,-80.12,NULL,NULL,NULL,NULL,25.127118063,-80.1107568223,25.135974477,-80.1097088565,25.1271,-80.1108,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Chanakhchi section, near the village of Zangakatun',4171,'Unknown','Permian','Lopingian','Changhsingian','upper Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','12','1','Less than 10 m wide','8',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3089,NULL,'Sponge-microbial build-ups, thrombolitic biostromes',NULL,NULL,NULL,NULL,'Armenia','Europe',NULL,NULL,39.5,45.03,NULL,NULL,NULL,NULL,7.42688005671,56.3288525786,15.0559437992,53.0494983391,-4.45225,40.0699,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Vacuum, Lea County, New Mexico',4172,'upper San Andres','Permian','Guadalupian','Roadian','Roadian',268.80,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','53',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','10','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'2','Intense',1,'Potential reservoir',3090,NULL,'a calcisponge-microbialite reef',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,32.79,-103.46,NULL,NULL,NULL,NULL,6.32282756526,-30.6622331242,1.91243363837,-39.1715558944,4.42612,-31.9183,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kamień Pomorski platform - Benice',4173,'Main Dolomite','Permian','Lopingian','Changhsingian','Zechstein',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,1,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick','40',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'3','Microbes','2','Algae','61','Microbes (thrombolites) - algae - corals','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite',NULL,NULL,'2','Intense',1,'Potential reservoir',3091,NULL,'Within the Main Dolomite carbonates of Poland, the most common organosedimentary structures are microbial laminites, stromatolites, and thrombolites, mostly developed in inter- to subtidal facies . The intertidal facies are chiefly composed of planar stromatolites (<50 cm [20 in.] thick) and thrombolites (20 cm[8 in.] thick). Planar stromatolites mainly contain\r\neven laminae that consist of light (muddy)-gray and dark (organic) couplets of microsparitic dolomite and darkgray micritic dolomite (deposited in restricted lagoons and intertidal pools). They commonly contain fenestrae\r\nfilled with sulfate. Micritic organic layers contain algal\r\nremains (Mizzia), ostracods and rare foraminifera, coated\r\ngrains, and peloids, and are built of coccoid-like organomineral\r\nforms and microbial filaments. Oncoids and peloids\r\nformgrainy planar stromatolites (deposited in inner\r\nooid shoals and tidal channels), dolomitic grainstone, and\r\npackstone.',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,53.54,14.54,NULL,NULL,NULL,NULL,30.1123367628,32.0978872801,26.7366027942,26.9186614507,18.1637,25.4895,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Little Cedar Creek, SW Alabama',4174,'Smackover','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick','11','4','More than 1000 m wide','2000','4','More than 1000 m',NULL,'13',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','3a','Upper slope or inner ramp','3','Below storm wave base','3','Microbes','12','Foraminifera','61','Microbes (thrombolites) - algae - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',3093,NULL,'Hydrocarbon-productive microbial and high energy, nearshore carbonate facies were deposited in shallow subtidal water depths in an inner ramp. The buildups are composed of thrombolites. The microbially influenced facies is present throughout the field area, but the thrombolite buildups are restricted\r\nto the southern part of the field. The microbially influenced facies varies in texture from packstone to lime mudstone. The packstone is a reservoir in parts of the field, and the lime mudstone serves as part of the updip lateral seal in the northeastern area of the field. Upper grainstone and packstone reservoir and lower boundstone and packstone reservoir are interbedded with three lime mudstone and dolomudstone to wackestone units (upper peritidal, middle deeper water subtidal, and lower transgressive subtidal) throughout the field. And to the northeast and updip in well permit 13,976, the Smackover section essentially consists of lime mudstone and dolomudstone, supporting the interpretation that the petroleum trap for this field is stratigraphic. The thrombolites consist of clotted peloidal boundstone and include a microfauna of benthic foraminifera, ostracods, bivalves, and microtubules.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,31.15,-86.55,NULL,NULL,NULL,NULL,15.5798228798,-27.523819484,19.9147996759,-29.6138467898,20.9315,-31.9085,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Black Warrior Basin of Alabama',4175,'Tuscumbia Limestone, Meramecian','Carboniferous','Mississippian','Visean','Meramecian',336.00,345.00,11,'late Famennian - early Visean',351,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','37',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','11','Siliceous sponges','3','Microbes','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',3096,NULL,'Sponge-microbial boundstone composed primarily of spiculitic clots embedded in a detrital carbonatematrix The mound was buried by foreshoal grainstone, much of which is brecciated. Upper Tuscumbia bryozoan-crinoid grainstone formed in a mobile shoal that quickly aggraded to sea level. Echinoderm debris, brachiopods and bryozoans are  abundant. Rugose corals, trilobites, ostracods, and sponges are less common',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,33.38,-88.1,NULL,NULL,NULL,NULL,-31.8682342248,-55.2545688573,-15.5769413103,-79.5044861102,-26.5212,-38.3659,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Assoul, High Atlas',4176,'Assoul','Jurassic','Middle Jurassic','Bajocian','middle Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','2','1','Less than 10 m wide','4','1','Less than 20 m','4','2',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3097,NULL,'Microbial mound. Mud mound surrounding by cross-bedded oolitic grainstone. As much as 25% of clastic sediments. Microbialites and sponges and ooids within growth cavities. Inner ramp',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.59,-5.05,NULL,NULL,NULL,NULL,16.0843197778,4.39820547133,20.0314656705,3.44902302834,26.9556,-1.20611,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Assoul coral microbial, High Atlas',4177,'Assoul','Jurassic','Middle Jurassic','Bajocian','middle Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','12','1','Less than 10 m wide','10','1','Less than 20 m',NULL,'2',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','1','Above fair weather wave base','1','Corals','3','Microbes','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3097,NULL,'Coral-microbialsponge reef: scleractinian corals, microbialites,\r\ncalcareous and siliceous sponges. Distal middle to outer ramp',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.59,-5.05,NULL,NULL,NULL,NULL,16.0843197778,4.39820547133,20.0314656705,3.44902302834,26.9556,-1.20611,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Assoul - Molluscan-coralsponge reef, High Atlas',4178,'Assoul','Jurassic','Middle Jurassic','Bajocian','middle Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','6','3','101-1000 m wide','230','3','More than 100 m','300','2',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','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3097,NULL,'Oysters, brachiopods, bivalves, scleractinian corals, calcareous\r\nsponges, and demosponges. Local deposition of marl. Microencrustation by microbialites, bryozoans, and cyanobacteria. Geopetal fabric. Distal middle ramp',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.59,-5.05,NULL,NULL,NULL,NULL,16.0843197778,4.39820547133,20.0314656705,3.44902302834,26.9556,-1.20611,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Hadahid fault',4179,'Nukhul','Neogene','Miocene','Lower Miocene','Aquitanian-Burdigalian',16.00,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','1','Less than 10 m thick','1','3','101-1000 m wide','300',NULL,NULL,NULL,'300',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3100,NULL,'Poorly cemented, structureless carbonate that contains gastropods, coral,\r\nand bivalves. These carbonates are thin (<2 m, laterally discontinuous (up to ca. 300 m wide), and based on the faunal assemblage, are interpreted to have been deposited in small, patch-reef-like buildups',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,28.42,33.25,NULL,NULL,NULL,NULL,25.8566035819,30.0004384556,25.1024811293,32.0543596361,26.7804,31.4579,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Ermenek area, Mut Basin',4180,'Unknown','Neogene','Miocene','Lower Miocene','Burdigalian-Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick','250','4','More than 1000 m wide','1100','4','More than 1000 m','2000','2',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,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',3101,NULL,'Corals mostly consist of Porites and a few Tarabestrella and\r\nFaviidae (hemispherical form). The matrix is composed of\r\nfragments of red algae, echinoderms, some bivalves, and\r\ngastropods. Frequent small and large benthic foraminifera are\r\nfound depending on the position along the depositional profile. Encrusting algae and rhodoliths are binding a matrix composed of large benthic foraminifera and bivalves, coral fragments, and some gastropods. Abundant red-algae debris associated with common bivalves, echinoderms, and large benthic foraminifera such as Heterestegina and Amphistegina. Bryozoan and oyster debris can be frequent in some place. Occasional Porites\r\nand rare gastropods can be found.',NULL,NULL,NULL,NULL,'Turkey','Asia',NULL,NULL,36.41,32.58,NULL,NULL,NULL,NULL,35.8049623449,29.3173875202,34.4586708734,31.4851458102,36.0764,32.3426,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Hantang, Guilin platform',4181,'Yunghsien','Devonian','Upper Devonian','Frasnian','upper Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','34','3','101-1000 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','13','4','Microbial precipitation',NULL,NULL,'1','Present','2','Medium zonation',NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3103,NULL,'Hantang  mounds  represent  a  microbe-dominated  reef-building  community\r\nwith rare skeletal reef builders. The microbial mounds are composed almost exclusively of calcimicrobes, including Renalcis, Rothpletzella, Girvanell, Izhella, Ortonella, Wetheredella and a Stenophycus-like microbe. Mound-building metazoans and metaphytes include receptaculitids, solenoporoid algae, spiculate and stromatoporoid sponges, and massive corals, but the volumes of these skeletal organisms  are low. Synsedimentary cements are volumetrically important in the mounds and supported  and  reinforced the microbial  frameworks. The microbial facies can be divided into five sub-facies. In roughly ascending stratigraphic order, they are:(i) Rothpletzella-receptaculitid fabric; (ii) Rothpletzella boundstone fabric: (iii)stromatolite-thrombolite fabric;(iv) Rothpletzella-encruster fabric; and (v)Renalcis fabric.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.16,110.12,NULL,'191830',NULL,NULL,-15.2630418315,87.8736957798,-14.4142133786,112.03671138,-1.02098,108.136,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Napoleon quarry',4182,'Massie','Silurian','Wenlock','Sheinwoodian','lower Wenlock',430.50,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1','2','10 - 100 m wide','20',NULL,NULL,'20',NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'7','Bryozoans','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation',NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3109,NULL,'Small build-ups composed primarily of micrite and benthic skeletal remains, termed micro-bioherms.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,39.12,-85.18,NULL,NULL,NULL,NULL,-30.9404207259,-85.4395107677,-30.9404207259,-85.4395107677,-25.2365,-53.8254,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Paojianggou, SW Tarim Basin',4183,'upper Azigan','Carboniferous','Pennsylvanian','Moscovian','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','300',NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','2','Baffler guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3110,NULL,'A Beresella-dominated algal mound. Komia bafflestone of the foremound facies further increased the relief of the crinoid bank on the seafloor. The lower part of the mound framework is dominated by Shamovella–Archaeolithoporella boundstone, while the main (upper) mound framework consists predominantly of Beresella boundstone. Grainstone–packstone characterizes the windward mound flank facies. The mound capping facies include a lower skeletal packstone–wackestone and an upper lagoon facies marlstone and black shale. Various algal colonies performed different roles in the formation of the mound. Komia colonies were the mound constructors that baffled higher energy currents and entrapped fine sediment. Archaeolithoporella, Shamovella and possibly microbes (cyanobacteria) acted as the binders to stabilize mud and fine-grained sediment. Beresella colonies were the major framework constructors whose network entrapped the mud to build the mound.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,37.3,76.5,NULL,'191877',NULL,NULL,10.0809606337,79.4243133321,36.0659340664,42.8009999258,21.8232,64.3625,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kasim and Walio',4184,'Kais','Neogene','Miocene','Lower Miocene','Early Miocene',16.00,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'0','',2,'Actual reservoir',3112,NULL,'Carbonate fabrics include skeletal wackestones,\r\nskeletal packstone, framestone, lime mudstone, and\r\nbindstone in order of decreasing occurrences. The\r\nskeletal grains are strongly modified by\r\ndolomitisation, but were originally dominated by\r\ncorals and red algae, echinoderms, large and\r\nplanktonic foraminifera. Lime mud matrix has been\r\nrecrystallised. The widespread occurrence of corals\r\nand red algae is strongly suggestive of deposition in\r\nproximity to reefal buildups.',NULL,NULL,NULL,NULL,'Indonesia','Asia',NULL,NULL,-1.19,131.01,NULL,NULL,NULL,NULL,-10.9459308819,125.753840612,-13.9698779046,126.9949693,-13.5753,132.788,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Bermejo field, NW Oriente Basin',4185,'Napo','Cretaceous','Upper Cretaceous',NULL,'Cenomanian-Santonian',83.60,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,1,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','40',NULL,NULL,NULL,NULL,NULL,'4000','4',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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',3127,NULL,'Carbonate buildup or a patch reef. Dark and rough top surface and irregular edges.\r\nThe dip map of the M1 carbonate buildup exhibits\r\ndark surface areas and irregular edges, suggesting\r\nkarst features and mechanical fractures, respectively.\r\nThe isopach map of the M1 carbonate buildup\r\nis even more complex, suggesting localized carbonate\r\ngrowth and weathering. The high but variable\r\nseismic amplitude of the top surface of the M1 carbonate\r\nbuildup may also suggest weathering. The carbonate buildup can contain bbl of liquid.',NULL,NULL,NULL,NULL,'Ecuador','South America',NULL,NULL,0.11,-77.23,NULL,NULL,NULL,NULL,-4.75831881661,-48.8105423687,-2.21571733053,-54.4796007844,-5.70708,-53.992,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Götzis locality, 10 km SW of Dornbirn, Vorarlberg',4186,'Oehrli','Cretaceous','Lower Cretaceous','Berriasian','upper Berriasian',139.80,145.00,22,'late Tithonian - early Valanginian',141,140,'Early Cretaceous (Berriasian, 142.4 Ma)',NULL,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','4','Basin','4a','Shallow basin','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','22','Stromatoporoids/sponges - corals - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',3128,NULL,'Facies type 6b. Patch reefs are composed of corals, stromatoporoids, and bryozoans.',NULL,NULL,NULL,NULL,'Austria','Europe',NULL,NULL,47.19,9.39,NULL,'192212',NULL,NULL,27.9958204051,24.1294502522,33.5573068975,25.0269696639,34.5247,19.129,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jeddah, Sharm Obhur',4187,'Unknown','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3129,NULL,'A temporarily exposed 6-m succession of raised\r\nreefal limestone terrace. The clayey layer showed higher species richness (65 species) than the limestone layer (18 species), indicating\r\na rapid change in the coral reef environment during\r\nthe deposition of the interval of MIS 5e.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,21.42,39.05,NULL,NULL,NULL,NULL,21.4103164543,39.0397146478,21.4059987733,39.0417802863,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gawadar and Jiwani, Balochistan coast',4188,'Gwadar','Quarternary','Pleistocene','Pleistocene','late Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'4','More than 1000 m',NULL,'1',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','30','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3130,NULL,'The coral colonies were scattered in large patches on about more than 1-km area. The habitat was mostly rocky, composed of sand stones with fine and coarse sand, boulders and mudstone. Thirty coral species were recorded at this site. Many species were found scattered but a considerable proportion was tightly packed. Coral cover was about 33%. Prominent genera were Favia (11%) and Favites (4%).',NULL,NULL,NULL,NULL,'Pakistan','Asia',NULL,NULL,25.04,61.47,NULL,'192909',NULL,NULL,25.042349301,61.4624157868,25.0357222065,61.4664531,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Subeigo section (Thrombolite), Wuhai',4189,'Unknown','Cambrian',NULL,NULL,'Menevian',500.50,509.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','3','Microbes',NULL,NULL,'64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation','2','Intensive',NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3131,NULL,'Thrombolite, characterized by meter-scale lenticular mounds composed of millimeter- to centimeter-scale mesoclots and wackestone matrix. Thrombolite mesoclots are composed of microstromatolites with alternating dark gray and light gray micritic laminae. Bioturbated micrites that occupy spaces between the mesoclots contain trilobite fragments. Three\r\ntypes of bioturbation are recognized.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,39.4,106.52,NULL,NULL,NULL,NULL,23.7257992503,107.883886413,23.7257992503,107.883886413,-7.82034,137.02,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Subeigo section (maceriate), Wuhai',4190,'Unknown','Cambrian','Series 3','Guzhangian','Mayan',497.00,500.50,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3131,NULL,'Maze-like maceriate reef with siliceous sponges and microstromatolites',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,39.4,106.52,NULL,NULL,NULL,NULL,22.9099417327,108.867993606,22.9099417327,108.867993606,-7.82034,137.02,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Yangba section',4191,'Dengying','Ediacaran','Ediacaran','White Sea Assemblage','Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','43','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','17','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite',NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3132,NULL,'Microbial carbonate. Thrombolites, laminites, oncolites and stromatolites dominate. The microbial dolostone reservoirs are low in porosity and permeability.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,32.25,106.53,NULL,NULL,NULL,NULL,25.6509061587,56.3879355619,25.6509061587,56.3879355619,42.9362,166.226,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Katnikova Cave, Nizhnie Sergi',4192,'Unknown','Devonian','Lower Devonian','Lochkovian','Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,415,'Early Devonian (Lochkovian, 415 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','13','Echinoderms','13','Echinoderms','90','Crinoids - Tubiphytes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3135,NULL,'Packstone bed cropping out near the waterline of the Serga River,\r\nwith a high content (60%) of crinoid stem fragments.\r\nThis bed represents the base of a series of 15 thin\r\ngradational members separated by beds of dark calcareous\r\nclay shale. The bed of bioclastic argillaceous\r\nlimestone sedimentologically represents fore-reef proximal\r\ncarbonate debris.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,56.55,59.29,NULL,NULL,NULL,NULL,25.2979505237,-29.9682595477,39.755459414,-88.8549992712,2.28838,15.1201,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Shijiezigou section, Guyuan City',4193,'Beiguoshan','Ordovician','Upper Ordovician','Katian','early Katian',445.20,453.00,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','5','2','10 - 100 m wide','34',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals','2','Algae','55','Tabulate/rugose corals - crinoids - (microbes inferred)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','14','2','Baffler 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',3137,NULL,'Patch reef in an open platform has a variety of corals that are preserved in situ. Reef-dwelling organisms include dasycladaceans, crinoids and gastropods. Other layers of the section are bedded limestones, many of which bear corals and crinoids, while others bear dasycladaceans or only the Dasycladacea genus Vermiporella. It contains abundant and diverse tabulate corals, which form bafflestones',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,36.12,106.36,NULL,'193282',NULL,NULL,36.3881987294,94.8180765383,36.3881987294,94.8180765383,-25.9552,120.899,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Barzok section',4194,'Qom','Paleogene','Oligocene','Rupelian','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',NULL,1,'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','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3139,NULL,'Coral boundstone, formed by in situ fauna as organic patch reefs, in openmarine\r\nsettings.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,33.51,51.09,NULL,NULL,NULL,NULL,33.5514959947,46.4150250439,31.5732980665,49.5980095886,30.1104,47.1921,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gebel Raghawi section',4195,'Risan Aneiza','Cretaceous','Lower Cretaceous','Aptian','middle Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','12','Foraminifera','91','Rudists - corals - algae/microbes - (brachiopods)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3142,NULL,'Toucasia bafflestone, which is dominated by complete valves of requieniid rudists (Toucasia sp.). The inner aragonitic layer of the rudist\r\nshell is replaced by blocky calcite, and the outer foliated layer is calcite. The matrix is mainly lime mudstone with abundant benthic foraminifers, rudist fragments and rare dasyclad algae (Fig. 9c). This facies is dominated by low energy micrite and benthic foraminifers. We interpret it as an isolated biostrome developed in the back-reef environment.',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,30.48,33.27,NULL,'193559',NULL,NULL,4.4544664125,34.5660899502,5.67571912588,28.4680805235,6.66256,29.0128,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Meregh-1',4196,'Mid Somalia High','Jurassic','Upper Jurassic',NULL,'Upper Jurassic',145.00,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'2000',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals','2','Algae','85','Corals - (phylloid) algae',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'2','Intense',1,'Potential reservoir',3144,NULL,'Isolated pinnacle reefs where the limestones are\r\ncommonly fractured, leached and dolomitized with porosities of up to 19%. The reef builders are predominantly coral and algae.',NULL,NULL,NULL,NULL,'Somalia','Africa',NULL,NULL,3.44,47.18,NULL,NULL,NULL,NULL,-31.2621990197,36.5534622655,-27.6726699803,31.6600975923,-20.0025,30.0404,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Stetten',4197,'Korneuburg','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','3','101-500 m thick','460','3','101-1000 m wide','460','3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1d','Marginal marine - coastal -  siliciclastic shelf','3','Below storm wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1','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',3146,NULL,'Shell accumulation comprising about 54,000 shells of the giant oyster Magallana gryphoides',NULL,NULL,NULL,NULL,'Austria','Europe',NULL,NULL,48.22,16.21,NULL,NULL,NULL,NULL,46.9819595762,12.2817190205,47.0806220036,15.9288799688,48.4982,14.9429,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Niau, Tuamotu',4198,'Unknown','Quarternary','Pleistocene','Pleistocene','late Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',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','15','Non-rudist bivalves','15','Non-rudist bivalves','47','Bivalves (mostly oysters) - algae (microbes)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','120',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3147,NULL,'Slightly raised atoll with rich shell mollusc assemblage',NULL,NULL,NULL,NULL,'French Polynesia','Pacific',NULL,NULL,-16.1,-146.2,NULL,NULL,NULL,NULL,-16.1149863467,-146.163665713,-16.1,-146.2,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Zebra River Farm',4199,'Kuibis Subgroup','Ediacaran','Ediacaran','Nama Assemblage','upper Ediacaran',541.00,635.00,0,'Vendian',605,600,'Late Neoproterozoic (middle Ediacaran, 600 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3148,NULL,'Microbial reef buildups. The lower reef occurrence appears as isolated mounding biostromes with poor fabric retention while the upper reef is sheetlike and forms a resistant bedding plane that exposes mounds of thrombolites and associated stromatolites. The mounds exhibit directional elongation and contain skeletal material within the fill between individual microbial buildups.',NULL,NULL,NULL,NULL,'Namibia','Africa',NULL,NULL,-24.31,16.13,NULL,NULL,NULL,NULL,-45.2070193488,81.897989729,-45.2070193488,81.897989729,-40.8339,-147.478,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Panlongdong',4200,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','83.4','3','101-1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Calcisponges','37','Sponges - microbes - Tubiphytes - (worms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','3','High production of reefal debris','2','Intense',1,'Potential reservoir',3149,NULL,'Number of spcies unknown due to dolomitization\r\n\r\nReef flats/caps contain mainly light gray crystal grain dolomites and sparry calcarenite. Reef cores are mostly sponge reef dolomites with the framework filled up by bioclasts and sand cuttings and contain a low content of calcilutite. Reef bases are less dolomitized and largely bioclastic limestones with bioclasts dominated by metacrinus and foraminifera.\r\n\r\nOriginal Interval (Lopingian) was changed belated (Xuesong Tian, Yue Wang). \r\n\r\nCoordinates, environment and subenvironment changed according to Tian-Wang 2021 (see 3th. paper attached)\r\n\r\nReef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, bryozoans, and hydrozoans. Binding organisms: Archaeolithoporella, Tubiphytes, Fenestella, and cyanobacteria.\r\n\r\nReef dwellers:\r\nEchinoderms, ammonites, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals\r\n\r\nRock type and reef-related depositional characteristic:\r\nFore-reef slope: spiculitic-calcispherical cherty wackestone with reef breccias\r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella\r\nReef flat (reef crest): packstone with reef breccia. \r\nReef base: crinoidal packstone to grainstone. \r\nBack-reef: bioclastic dolostone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type: \r\nMetazoan reef at the shallow carbonate platform margin',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.75,108.4667,NULL,'217016',NULL,NULL,-9.49749375411,106.609232442,6.92834012739,128.691777031,8.37834,96.3233,'Krause','Kiessling','2021-05-28 15:21:12','2021-06-22 16:31:22'),('Amu-Darya Basin',4201,'Unknown','Jurassic','Middle Jurassic','Callovian','Callovian-Oxfordian',157.30,166.10,21,'late Bathonian - early Tithonian',151,165,'Middle Jurassic (Callovian, 164.8 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','3a','Upper slope or inner ramp','1','Above fair weather wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3153,NULL,'carbonate ramp, wherein the thickest sedimentary\r\nformations were deposited, and organic reefs, bioclastic shoals, and oolitic shoals\r\nwere mainly developed. Rudists (50%)- ???, coral, red algae, bryozoans, sponges.',NULL,NULL,NULL,NULL,'Turkmenistan','Asia',NULL,NULL,38.32,64.18,NULL,NULL,NULL,NULL,35.8863322549,73.0008958269,39.1130767565,77.6765591535,36.7582,69.7863,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Skelya and Kamyshlak, Kerch Peninsula',4202,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2','1','Less than 10 m wide','2','1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3154,NULL,'Oval, up to 2 m in diameter, bioherm bodies in the Early Chokrakian basin were formed by bryozoan colonies of cheilostomates (Membranipora, Schizoporella, Cellaria, Scrupocellaria, Celleporaria) and cyclostomates (Crisia), red algae (Belokrys, 1986), and calcareous worm tubes.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,45.28,36.17,NULL,'194975',NULL,NULL,45.0397281197,33.3244200419,44.3027987719,35.6728645096,45.7053,35.0807,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Mayak, Kerch Peninsula',4203,'Unknown','Neogene','Miocene','Middle Miocene','Sarmatian',11.60,12.70,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','2','1','Less than 10 m wide','2','1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'7','Bryozoans','15','Non-rudist bivalves','39','Algae - bivalves - (bryozoans) - (siliceous sponges)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','13',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite',NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3154,NULL,'The main reef forming organisms in bioherms  included seven species of Schizoporella\r\n(Schizoporellidae, Cheilostomata) and quite common\r\ncyclostomes Diastopora, Tubulipora, and Pustulipora.\r\nThe majority of the bryozoans have membraniporiform colonies. Vinculariform types are also present. These bioherms occurred at the transition from the upper to lower sublittoral zones.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,45.13,36.07,NULL,'194982',NULL,NULL,44.9178800672,33.3550285768,44.1964311111,35.6046388521,45.5547,34.9819,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lake Tobechik, Kerch Peninsula',4204,'Unknown','Neogene','Miocene','Upper Miocene','lower Tortonian',9.00,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1.5','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','3','Below storm wave base','7','Bryozoans','15','Non-rudist bivalves','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','14',NULL,NULL,NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3154,NULL,'Bryalgal bioherms. The deposits covering bryozoan bioherms contain detrital limestones.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,45.07,36.24,NULL,'194983',NULL,NULL,44.9591974204,33.9254493577,44.2747660939,35.867034261,45.2386,36.0097,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Cape Kop-Takyl',4205,'Unknown','Neogene','Miocene','Middle Miocene','middle Sarmatian',11.80,12.50,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1.5','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'15','Non-rudist bivalves','8','Serpulids, worms, vermetids','16','Serpulids - bivalves - (microbes)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','18','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3154,NULL,'Serpulid-microbialite buildups (nodular\r\ncarbonate bodies). Mollusks assemblage, in addition\r\nto mass Crypromactra and rare poorly preserved\r\nimprints of cardiids, commonly includes gastropods.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,45.04,36.21,NULL,'194984',NULL,NULL,44.8315479066,33.499058572,44.1054149478,35.7411017122,45.4655,35.1241,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Cape Tuzla, Taman and Cape Popov Kamen, Taman Peninsula',4206,'Unknown','Neogene','Miocene','Upper Miocene','Tortonian/Messinian',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'7','Bryozoans','15','Non-rudist bivalves','39','Algae - bivalves - (bryozoans) - (siliceous sponges)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3154,NULL,'Bryozoan bioherms are formed by Membranipora elliptica,  bivalve mollusks (Polititapes abichi)\r\ngastropods that form mass accumulations. Early Maeotian',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,45.11,36.36,NULL,'194985',NULL,NULL,45.0427295173,34.6384920577,44.5184937403,36.0869762426,45.2788,36.1299,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Belaya River',4207,'Unknown','Neogene','Miocene','Middle Miocene','Chokrakian',13.80,15.30,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1.5','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3154,NULL,'bryozoan colonies of cheilostomates (genera\r\nMembranipora, Schizoporella, Cellaria, Scrupocellaria, Celleporaria), cyclostomates and calcareousworm tubes.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,44.46,38.43,NULL,'194987',NULL,NULL,44.1844534916,35.2071409569,43.320422511,37.7671965242,44.899,37.3678,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Chimbulat quarry, Kirov Region',4208,'Nemda','Permian','Guadalupian','Roadian','Roadian',268.80,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'7','Bryozoans','14','Brachiopods','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','33',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3156,NULL,'bed of yellow bioclastic limestone with numerous bryozoan imprints, crinoid columnals, brachiopod and molluskan shells',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,57.24,48.56,NULL,'170190',NULL,NULL,28.3607945238,44.3779347878,37.5000273519,31.4657178838,27.023,42.2313,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Tastuba-Mitrofanovo quarry',4209,'Unknown','Permian','Cisuralian','Sakmarian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'12','Foraminifera','14','Brachiopods','82','Bryozoans - strophomenid brachiopods',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3157,NULL,'The Mitrofanovo and Tastuba Reefs are composed of organic limestones containing large amounts of diverse fossil animals (foraminifers, brachiopods, bryozoans, gastropods, crinoids, bivalves, trilobites). In\r\nthe Tastuba Reef, the records of trilobites are restricted\r\nto the lower member of massive, cavernous limestones. In the Mitrofanovo Reef, they occur throughout the thickness of the sediments.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,55.62,57.92,NULL,'124196',NULL,NULL,25.775120636,43.5730533803,33.9353319729,21.8754207777,26.2425,42.6418,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Reinecke field, west Texas',4210,'Unknown','Carboniferous','Pennsylvanian','Gzhelian','Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',NULL,2,'1','Seismic data available ',NULL,NULL,'4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'7','Bryozoans','13','Echinoderms','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'2','Intense',2,'Actual reservoir',3159,NULL,'Two types of dolomite are observed.One type is stratiform, replaced micrite-rich facies, and is interpreted as early dolomite that recrystallized in hydrothermal brines. The second type crosscuts stratigraphy and depositional facies and has vertically continuous morphologies that trend northwest-southeast. The latter dolomite is interpreted as forming in hydrothermal brines\r\nderived from latest Permian-aged highly evaporated seawater. Lower porosity but much higher permeability.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,32.34,-101.15,NULL,NULL,NULL,NULL,-2.81415320793,-33.5124697983,-5.96989531096,-56.6929644744,-4.90289,-34.8671,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Browse Basin, Unit 4',4211,'Oliver','Neogene','Miocene','Upper Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',NULL,1,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'4','More than 1000 m','6000','6',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3162,NULL,'Internal seismic reflections in the build-ups are highly discontinuous, producing high-variance, circular to sub-circular depressions. The subtle chaotic appearance on the slope suggest the presence\r\nof a debrite. After the generation of this latter debrite, build-ups were onlapped by, and buried under, low-amplitude strata.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-13.39,122.04,NULL,NULL,NULL,NULL,-16.5207099202,120.312894742,-17.7894728872,120.549668011,-17.5303,120.451,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Browse Basin, Unit 3',4212,'Oliver','Neogene','Miocene','Upper Miocene','Tortonian',7.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'4','More than 1000 m','6000','6',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3162,NULL,'Intra-platform seaways were established between build-ups, and evidence exists for large-scale ripples in the southern part of the study\r\narea.Fringing reefs, and build-up interiors\r\ndevelop discontinuous seismic reflections with high-variance, and circular to sub-circular depressions',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-13.39,121.49,NULL,NULL,NULL,NULL,-18.0797378166,118.865256568,-19.9117459621,119.285997035,-17.5205,119.89,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Browse Basin, Unit 2',4213,'Oliver','Neogene','Miocene','Middle Miocene','mid- Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',NULL,NULL,'4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m','27000','27',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3162,NULL,'carbonate build-ups with topographic highs marking focal points of aggradation. In\r\nsuch a setting, topographic lows within build-up interiors are indicative of marine incursions. Patch reefs within the interior lagoon to the east were also drowned. Prolonged aggradation resulted in significant margin retreat on the southeast margins. The barrier reef was then drowned and buried, likely establishing open-ocean conditions across the southeastern part of the study area. Southwest striking\r\nfaults are observed.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-13.36,122.04,NULL,NULL,NULL,NULL,-20.2754839897,118.178326067,-22.6844347134,118.921243677,-22.1224,118.235,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Browse Basin, Unit 1',4214,'Oliver','Neogene','Miocene','Lower Miocene','upper Burdigalian',16.00,17.50,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,1,'1','Seismic data available ',NULL,NULL,'4','More than 500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3162,NULL,'Topography prior to the Miocene initiation of carbonate build-ups shows flat-topped bryozoan\r\nreefs, and a sharp break in slope to the northwest. This break in slope is regularly incised and controls the northwesterly extent of the Miocene carbonate sequence. Circular to sub-circular topographic highs represent carbonate build-ups with a patch-reef morphology.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-13.36,122.04,NULL,NULL,NULL,NULL,-21.7718628696,117.320814736,-24.5415906175,118.295723986,-22.1224,118.235,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Pre-Caspian Basin',4215,'Unknown','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',NULL,2,'1','Seismic data available ',3,'Mud mound or bank','4','More than 500 m thick','2000','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',3163,NULL,'Reef limestone predominately developed with limy mudstone present at the basal part. The platform margin reef (bank) is located in a transition zone between the platform and the deep- or deeper-water slope, with the water depth at and near the wave base, where good circulation of water body is available. This environment provides a strong hydrodynamic force, due to the joint control of wave and tidal, and hence allows grain-dominated bank facies bodies to deposit, with locally present organic reefs formed by substantial in-situ biogroups.',NULL,NULL,NULL,NULL,'Kazakhstan','Asia',NULL,NULL,48.17,55.41,NULL,NULL,NULL,NULL,17.6703416909,63.9700985406,28.4621834182,25.1808555567,21.8986,48.0359,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Muang Long, Sukhothai Zone',4216,'Unknown','Triassic','Middle Triassic','Ladinian','late Ladinian - early Carnian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'12','Foraminifera','3','Microbes','30','Tubiphytes - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','10','4','Microbial precipitation',NULL,NULL,'2','Intensive',NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3165,NULL,'Cement-rich reefal sediments composed of Carniphytes multisiphonatus-microbial boundstone and sparse-allochem grainstone, the latter consisting mainly of fragments of Plexoramea gracilis, are common in this limestone. They suggest open-marine sedimentation on a shallow carbonate platform.',NULL,NULL,NULL,NULL,'Laos','Asia',NULL,NULL,20.58,100.48,NULL,NULL,NULL,NULL,-3.7384190467,93.7731849193,-3.24796867601,99.6648054175,5.39955,83.659,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lysakow bryozoan reef',4217,'unknown','Quarternary','Holocene','Holocene','Holocene',0.00,0.00,34,'Holocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,1,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1','1','Less than 10 m wide','3','1','Less than 20 m','3',NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans','73','Bryozoans only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1','1','Constructor guild','1','Present','1','Present','1','Low zonation',NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3167,NULL,'Bryozoan bioherms attaining up to a few meters in length and one meter in thickness. The bioherms are built up by cyclostomate and cheilostomate bryozoans but the frame-building assemblage is monospecific in places, consisting of Fasciculipora janinae sp. n. Branching colonies of the new species are so\r\nvariable that their isolated fragments might be easily misidentified as belonging to distinct species, or even genera.',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,50.35,21.267,NULL,NULL,NULL,NULL,50.35,21.267,50.35,21.267,50.3758,21.229,'Krause','Krause','2021-05-28 15:21:12','2022-08-09 21:20:41'),('Lop’yu Kyrta, Ilych River',4218,'Valganskaya','Devonian','Lower Devonian','Lochkovian','upper Lochkovian',410.80,419.20,8,'middle Pridolian - middle Pragian',412,415,'Early Devonian (Lochkovian, 415 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin',NULL,NULL,'1','Above fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',1,'Potential reservoir',3170,NULL,'Among Biohermal limestones stromatolitic ones are predominate, coral, Fistulella-microbial,\r\nand stromatoporoid-microbial ones are rarer. The comparison and correlation of transect series allow us to establish the landscapemorphological\r\nzonation of Lop’yu Kyrta buildup, an outer slope and a reef-flat are distinguished.\r\n\r\nValganskaya Fm. is turbiditic with reworked reef clasts. No formation name given for in situ reef facies',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,62.49,58.74,NULL,NULL,NULL,NULL,24.7966500929,-36.5093221005,38.4262323623,-96.3252932777,3.22335,9.24065,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('New Pass, Nevada',4219,'Augusta Mountain','Triassic','Upper Triassic','Carnian','early Carnian',233.00,235.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',NULL,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15','1','10 - 100 m wide','8','2','10 - 100 m','14',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','11','Siliceous sponges','15','Non-rudist bivalves','59','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3169,NULL,'Sponge-Bivalve-Coral reef mound. Sponges dominated the reef mound followed by bivalves, corals and echinoid fragments. The skeletal content within the overall middle ramp environment is low. Micrite comprises 79% while sparry calcite comprises 2%. Radiolarians, and ammonoids dominate this environment. Thus, we categorize this section as the Radiolarian-Ammonoid Biofacies. The sponge reef mound is largely matrix supported with skeletal content.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,39.36,-117.3,NULL,'186862',NULL,NULL,21.0374490389,-39.8777652848,16.9177271746,-48.1550496554,8.30047,-46.9366,'Krause','Kiessling','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lesno Brdo Quarry',4220,'Unknown','Triassic','Upper Triassic','Carnian','Julian',227.00,237.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','66','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','61','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','2','Intense',0,'No or unknown reservoir potential',3171,NULL,'Presence of three facies types: fine-grained\r\nlimestone as a groundmass, blocks and globular masses of sponge-microbialite boundstone, and lens-like aggregations of polychaete (terebellid) tubes. Sponge-microbialite boundstone contains a rather small number of cosmopolitan sponge\r\ntaxa, solenoporacean red algae, microproblematica, bryozoans, and a small proportion of dwelling fauna. Instead, stromatolites represent the main constituent.',NULL,NULL,NULL,NULL,'Slovenia','Europe',NULL,NULL,46,14.19,NULL,'195833',NULL,NULL,14.9004524266,35.4047905135,8.83068023514,24.3454014235,10.5394,21.681,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Eastern Tianshan, Xinjiang',4221,'Yamansu','Carboniferous','Mississippian','Visean','latest Visean',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5','1','Less than 10 m wide',NULL,'4','More than 1000 m','1300','1.3',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','22',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3172,NULL,'The coral fauna is composed of mainly large\r\ndissepimented solitary corals, accompanied by a few colonial forms. In total, 47 species belonging\r\nto 22 genera in the families Adamanophyllidae, Aulophyllidae, Axophyllidae, Amplexidae, Bothrophyllidae, Cyathopsidae, Palaeosmiliidae and Lithostrotionidae were identified. Among these genera, 16 are solitary, and 6 are colonial. In the latter group, 4 genera are massive,\r\nand 2 are fasciculate.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,41.55,93.46,NULL,'195864',NULL,NULL,34.0107337588,120.962929011,33.3397973905,49.0466776566,1.34609,62.393,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Tabynsk, Voskresenka Mount',4222,'Unknown','Carboniferous','Pennsylvanian','Gzhelian','Gzhelian-Asselian',295.00,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','70','2','10 - 100 m wide',NULL,'4','More than 1000 m','1000','1',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','2','Below fair weather wave base','7','Bryozoans','14','Brachiopods','23','Bryozoans - Tubiphytes - phylloid algae - (microbes) - (encrusting forams)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3173,NULL,'Bioherm facies are represented by bryozoan\r\nlimestones (baundstones and rudstones) with\r\nbrachiopods, algae, and ammonoids. They are underlain by layered crinoid limestones (wackestones and grainstones). The rocks contain a foraminiferal assemblage',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,56.27,54,NULL,NULL,NULL,NULL,24.195665994,40.831090102,30.36138697,14.1520617056,21.5112,38.2223,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Dark Canyon brachiopod mound',4223,'Tansill','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1','1','Less than 10 m wide','5.5','1','Less than 20 m','8',NULL,'276',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','14','Brachiopods',NULL,NULL,'89','Brachiopods - echinoderms',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'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','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3174,NULL,'The small bioherm is about 8 m long, 5.5 m wide, and elongate toward the northwest. \r\nBuilt by brachiopod Sestropoma cribriferum',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,32.34,-104.47,NULL,'47542',NULL,NULL,11.180208246,-29.804018347,5.62704694259,-36.7459068973,4.43728,-32.8839,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Marmorbruch Niederehe, Eifel',4224,'Ahrdorf','Devonian','Middle Devonian','Eifelian','middle Eifelian',387.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',394,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','15','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3176,NULL,'Stromatoporoids, tabulate corals and some rugose corals. Mostly reworked reefal debris.\r\nComplex encrustation pattern\r\nZisterzienser Marble previously quarried as building stone.',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,50.313443,6.746123,NULL,NULL,NULL,NULL,-14.5198179844,-17.7488322191,-0.064213865181,-73.702329182,-25.6683,8.71641,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Staryi Oskol, Novovasil’evo area, Orenburg, Ardatovo horizon',4225,'Unknown','Devonian','Middle Devonian','Givetian','upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','85','4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'22.5',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'4','Stromatoporoids','1','Corals','22','Stromatoporoids/sponges - corals - (algae)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3178,NULL,'Stromatopore–coral limestones. Clayey and bituminous limestones with tentaculites, radiolarians, spongioids, ostracodes, pelecypods, and lingules.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,51.77,55.1,NULL,NULL,NULL,NULL,8.32273180896,1.41596805129,28.2953319114,-64.6700981797,4.66706,22.9683,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Rybkino',4226,'Unknown','Devonian','Upper Devonian','Frasnian','late Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','200','3','101-1000 m wide','1400','4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'4','Stromatoporoids','2','Algae','22','Stromatoporoids/sponges - corals - (algae)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3178,NULL,'Biohermal stromatopore limestones, biohermal algal\r\n(Shuguria) limestones;',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,51.51,53.57,NULL,NULL,NULL,NULL,0.78623390519,7.9409234681,25.6511915755,-57.6337305877,3.68275,22.9517,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Quingdao Depression, CZ12-1-1',4227,'Hezhou','Carboniferous','Mississippian',NULL,'Lower Carboniferous',323.20,358.90,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',NULL,1,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'2','Intense',1,'Potential reservoir',3180,NULL,'Reef-bank. Dolomites contain abundant dissolved pores and are mainly micritic dolomites. These indicate that there are dolomite reservoirs with good porosity distributed in the lower Triassic and lower Carboniferous of the South Yellow Sea.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.35,122.03,NULL,NULL,NULL,NULL,6.44019698973,115.906526651,10.7994325988,50.715663884,-6.28448,86.1989,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Well WX5-ST1',4228,'Qinglong','Triassic','Lower Triassic','Induan','Scythian',247.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','25','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'2','Intense',1,'Potential reservoir',3180,NULL,'Dolomites with high porosity and high\r\npermeability',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.32,122.54,NULL,NULL,NULL,NULL,4.26139251568,120.015537254,27.7803615144,110.766449588,13.6394,105.106,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Ganjgon, Lower Rupelian',4229,'Asmari','Paleogene','Oligocene','Rupelian','lower Rupelian',30.00,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base','1','Corals','2','Algae','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3181,NULL,'Build-up (main body and flanks). Further down-dip, larger benthic foraminifers (large Nummulites test, Operculina and Neorotalia) packstone-grainstone along with discrete coral patches and coralline red algae',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,30.16,51.46,NULL,NULL,NULL,NULL,22.9368263524,45.3416612962,20.9283599627,47.3365362583,22.549,45.5597,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jowzar',4230,'Asmari','Paleogene','Oligocene','Chattian','lower Chattian',27.50,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','1','Corals','2','Algae','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3181,NULL,'Polygenetic conglomerate. Meter-thick bedded to massive limestones rich in coral and coralline\r\nred algae fragments confining to the platform margin.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,30.4,51.22,NULL,NULL,NULL,NULL,23.8933395752,45.6578131447,21.9809819845,47.5269033829,26.4228,48.0942,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lower Monte Baria Reef, Cala Gonone, N Oresei Gulg',4236,'Lower Monte Bardia','Jurassic','Upper Jurassic','Tithonian','upper Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','120','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','3','Below storm wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','40','4','Microbial precipitation','1','Present','2','Intensive',NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3185,NULL,'Carbonate (bioclastic) debris, microbialites and microencrusters, and reef-building organisms (mainly corals and stromatoporoids).\r\nMicroframework -rich(microbialites and microencrusters) facies, with abundant skeletal organismus in place. Corals dominate, followed by stromatoporoids, bivalves (including Rudist diceratids), gastropods (including nerineids), echinoid spines.',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,40.16,9.37,NULL,'196865',NULL,NULL,22.2533512176,21.6107406562,23.9451625524,16.4871126777,34.0583,13.8914,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Core XK-1, Stone Island',4241,'Yinggehai','Neogene','Pliocene','Pliocene','Upper Pliocene',2.60,3.60,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',4,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals','2','Algae','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3194,NULL,'Coral content varies between 25% and 74%.The corals are dominated by Turbinaria and Favia, with colonies mainly displaying massive morphologies. Accessory components are debris of frequent to rare benthic foraminifera, red algae, echinoids, brachiopods. Red algal and coral frame- to bindstone, red algal bindstone, floatstone, and wackestone.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.51,112.2,NULL,NULL,NULL,NULL,16.9846878533,111.768191244,16.2928863978,111.8401123,16.4008,111.945,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Falcona Alta, Malaguide Complex',4240,'Unknown','Devonian','Upper Devonian','Frasnian','Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',NULL,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','1','Corals','4','Stromatoporoids','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,'2','Intensive','1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3192,NULL,'Mainly bafflestones with clotted microbial\r\ngrainstone to packstone matrix. Reef builders\r\nare ramiform thamnoporid corals and twig-like stromatoporoids both with frequent microborings.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,36.47,-4.28,NULL,'197173',NULL,NULL,36.47,-4.28,-9.12774798041,-52.9528871161,-35.0928,13.2965,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Hönne Reef, Beul near Eisborn. Loc. 4',4239,'Unknown','Devonian','Upper Devonian','Frasnian','early Frasnian',372.20,382.70,10,'Givetian - early Famennian',375,380,'Late Devonian (early Frasnian, 380 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','2','Below fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3191,NULL,'Terminal reef limestones with colonial rugose coral, biostrome blocks and with the overlying top-middle Frasnian, post-reefal nodular limestones, with shark and pelagic conodont fauna',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,51.23,7.52,NULL,'197088',NULL,NULL,-20.8405728609,-10.6690851976,-1.04999308975,-67.2329750556,-19.3864,6.33956,'Krause','Kiessling','2021-05-28 15:21:12','2023-03-10 15:49:57'),('Hönne Valley Reef Complex at Asbeck Quarry',4238,'Hagen-Balve','Devonian','Middle Devonian','Givetian','middle-upper Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','4','More than 500 m thick','600','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','16',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3191,NULL,'The Asbeck Quarry exposes a sequence of more\r\nthan 600 meters of reefal limestone.\r\nThere are six major facies sets: \r\n1. limestones with evidence of subaerial exposure (e.g., vadose cements, drying and contraction cracks), 2. laminites without macrofauna (but with\r\nparathuramminid foraminifers and ostracods), 3.\r\nmicrites with few components and irregular\r\nmicrobial fenestrae (“birdseyes” to Stromatactis”), 4. fossiliferous micrites, with various reef builders, gastropods, specialized brachiopods, parathuramminids, and ostracods, 5. sublagoonal limestone, mostly rich in dendroid stromatopores (Amphipora, Stachyodes), and 6. reef-core limestones (boundstones), with large stromatopores in growth position.\r\n\r\n\r\nMudstones to bioclastic wackestones with some\r\ntabulate corals, rare colonial Rugosa, very rare\r\nstromatoporid fragments, some crinoid debris,\r\nostracods, and some mollusk debris.',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,51.393,7.867,NULL,'197084',NULL,NULL,-15.9954827905,-14.7533967612,-0.119187133193,-71.2958213121,-19.4004,6.31756,'Krause','Kiessling','2021-05-28 15:21:12','2023-03-10 15:49:58'),('Core XK-1, Stone Island',4242,'Ledong','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','2c','Atoll (circular structure)','2','Below fair weather wave base','1','Corals','12','Foraminifera','85','Corals - (phylloid) algae','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3194,NULL,'coral framestone and floatston with minor wackestone and packstone. The corals are dominated by Turbinaria and Favia, with\r\ncolonies mainly displaying massive morphologies. The coral content can reach 100%. Matrix containing some bioclastic debris. Accessory components are debris of frequent to rare benthic foraminifera, red algae, echinoids, rare green algae, brachiopods, bivalves.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.51,112.2,NULL,NULL,NULL,NULL,16.6658863994,112.058711173,16.4381569228,112.081638624,16.51,112.2,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Laga Beach, Ibarangelu',4243,'Unknown','Cretaceous','Lower Cretaceous','Albian','lower Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,110,'Early Cretaceous (early Albian, 111 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','3','101-500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','50',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3195,NULL,'Marls with coral biostromes.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,43.24,-2.39,NULL,NULL,NULL,NULL,31.3108317436,8.4187865529,33.6029647791,4.27979273191,31.8247,4.71445,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kouquan section',4244,'Changshan','Cambrian','Series 3','Guzhangian','Middle-Dresbachian',494.00,497.00,2,'Middle Cambrian - Dresbachian',502,490,'Late Cambrian (Jiangshanian, 491.8 Ma)',NULL,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3196,NULL,'massive micritic limestone and calcareous\r\nmudstone',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,39.59,113.07,NULL,'197283',NULL,NULL,20.7194117892,104.296366428,20.7194117892,104.296366428,-3.7484,140.035,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Sampaguita-1, Reed Bank',4245,'Unknown','Paleogene','Oligocene','Chattian','Chattian-Burdigalian',16.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',NULL,2,'1','Seismic data available ',NULL,NULL,'4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3197,NULL,'Carbonate platform reef',NULL,NULL,NULL,NULL,'Philippines','Asia',NULL,NULL,10.24,116.36,NULL,NULL,NULL,NULL,14.8056840825,113.253588652,11.5930218943,113.919399645,13.4024,117.532,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Sampagita‐1',4246,'Unknown','Neogene','Miocene','Upper Miocene','upper Miocene - Pliocene',2.60,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',NULL,NULL,'4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3197,NULL,'Carbonate platform reef',NULL,NULL,NULL,NULL,'Philippines','Asia',NULL,NULL,10.24,116.36,NULL,NULL,NULL,NULL,11.1129904281,115.621924168,9.88735424624,115.761545941,10.2828,116.337,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Huwaiza-1 well',4247,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','12','Foraminifera','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3198,NULL,'Very coarse-grained bioclastic rudstone dominated by rudistid debris with abundant of benthonic foraminiferal grainstone in the lagoonal facies.',NULL,NULL,NULL,NULL,'Iraq','Asia',NULL,NULL,31.45,47.49,NULL,NULL,NULL,NULL,11.6023187931,43.890304106,8.28787380926,38.9495160077,8.636,39.0062,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Halfaya-1 wall',4248,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','5','Rudists','12','Foraminifera','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3198,NULL,'Rudistid biostrome with open shelf lagoon facies. Abundant of benthonic foraminiferal packstone, that indicates to open lagoon environment.',NULL,NULL,NULL,NULL,'Iraq','Asia',NULL,NULL,31.38,47.24,NULL,NULL,NULL,NULL,11.5696950514,43.6635224824,8.26695868769,38.723595326,8.60367,38.7814,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Amara -1',4249,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3198,NULL,'Rudistid biostrome with open shelf lagoon facies',NULL,NULL,NULL,NULL,'Iraq','Asia',NULL,NULL,31.48,46.53,NULL,NULL,NULL,NULL,11.773154038,43.0719551362,8.5007957047,38.1497071667,8.8081,38.1957,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Abu Amood -1',4250,'uppermost Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','5','Rudists','12','Foraminifera','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3198,NULL,'Skeletal and non-skeletal carbonate grains, rudistid debris.',NULL,NULL,NULL,NULL,'Iraq','Asia',NULL,NULL,31.49,46.28,NULL,NULL,NULL,NULL,11.8205562492,42.8593669351,8.5592328798,37.9421384511,8.85592,37.9852,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Dujaila -1 well',4251,'Mishrif','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian-Turonian',89.80,100.50,25,'late Cenomanian - early Campanian',91,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','5','Rudists','12','Foraminifera','62','Rudists - stromatoporoids (hydrozoans) - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,'3','High production of reefal debris','0','',2,'Actual reservoir',3198,NULL,'Skeletal and non-skeletal carbonate grains.',NULL,NULL,NULL,NULL,'Iraq','Asia',NULL,NULL,31.57,46.08,NULL,NULL,NULL,NULL,11.9295511234,42.7024467524,8.67629447243,37.7929491247,8.96526,37.83,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wennan, Xintai area',4252,'Zhangxia, Lower Limestone Member','Cambrian','Series 3','Guzhangian','Marjumian',500.50,504.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3200,NULL,'Sponge–microbial boundstones, containing lithistid sponges (areal percentage, approximately 14%) and microbial components (areal percentage, approximately 39%). The sponges in this section are anthaspidellid demosponges. The microbial components consist mainly of frequently branched columnar stromatolites. Vacant spaces among frameworks formed by a combination of stromatolites and sponges are filled with lime mud and rare bioclasts, including trilobites, chancelloriid sclerites and sponge spicules.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.48,117.46,NULL,NULL,NULL,NULL,24.5492149278,97.9557098779,24.5492149278,97.9557098779,-3.23325,145.405,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Tipperary area, Kordephyton-Jawonya-Wagima',4253,'Tindall Limestone','Cambrian','Series 2','Stage 4','upper Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3201,NULL,'Microbialite columns with Kordephyton bushes (fan pattern) and sporadic Jawonya and Wagima both attached to column surfaces and immured within columns; vagrant Latouchella accordionata on right margin of central column; intercolumn cavity with geopetal infill.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-13.45,130.2,NULL,NULL,NULL,NULL,5.42869314792,99.554876226,5.42869314792,99.554876226,27.6784,-177.922,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Soudan area, Undilla Sub-basin, locality NTGS4648',4254,'Ranken Limestone','Cambrian','Series 3','Guzhangian','Marjumian',500.50,504.00,2,'Middle Cambrian - Dresbachian',502,500,'late Middle Cambrian (Guzhangian, 498.8 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope',NULL,NULL,'3','Below storm wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3201,NULL,'Reef fabric comprises mainly explanate and in some cases conical Rankenella, encrusted by more or less distinctly laminated, generally non-skeletal stromatolites. Angulocellularia-type microbial mesoclots and Angulocellularia locally intergrades into Taninia. Stromatolites appear to encrust upper surfaces of Rankenella skeletons, as well as those of other bioclasts such as calciate brachiopods, hyoliths and molluscs.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.49,136.55,NULL,NULL,NULL,NULL,4.82799498343,112.360108444,4.82799498343,112.360108444,25.2066,-176.118,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Yazd locality',4255,'Nayband, Howz-e Khan Member','Triassic','Upper Triassic','Norian','Norian-Rhaetian',201.30,228.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','50',NULL,NULL,NULL,'2','10 - 100 m','60',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3202,NULL,'Small reefs formed by dendroid and ceroid corals and differents droups of sponges. Chambered sphinctozoans and noc-chambered sphinctozoans are the most abundant sponges. One chambered hexactinellid sponges was also found.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,31.49,54.2,NULL,'197554',NULL,NULL,25.2211858224,65.1939935196,21.6954605526,64.5723262292,-12.4274,44.8748,'Krause','Krause','2021-05-28 15:21:12','2022-06-22 20:46:19'),('Dagestan, Shakhdag Massif',4256,'Babadag','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','320',NULL,NULL,NULL,'4','More than 1000 m','1500','1.5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1',NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3203,NULL,'Bioherm buildups, represented by the dense gray and greenish grain limestones with a great amount of corals.',NULL,NULL,NULL,NULL,'Azerbaijan','Europe',NULL,NULL,41.15,48.01,NULL,NULL,NULL,NULL,32.4633491919,57.4150770964,36.1349884064,60.9742005837,36.395,53.0394,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Well YB1 and Well YB2,Yuanba, Cangxi',4257,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,2,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick','140',NULL,NULL,NULL,'4','More than 1000 m',NULL,'3.6',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'2','Intense',2,'Actual reservoir',3204,NULL,'The main reservoir rocks are reef-bank dolomite and dolomitic limestone, which are characterized by\r\nmedium-low porosity and medium-low permeability.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.54,106.07,NULL,NULL,NULL,NULL,-9.68272333377,104.695223691,12.7067161262,123.623002199,3.7442,95.0735,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Le Perthus',4258,'Unknown','Jurassic','Lower Jurassic','Sinemurian','upper Sinemurian',190.80,199.30,19,'late Hettangian - early Aalenian',188,195,'Early Jurassic (Hettangian&Sinemurian, 196 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','6','4','Microbial precipitation','1','Present','2','Intensive','1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',3209,NULL,'Coral-microbialite patch reef with fragments of crinoids and dacycladacean algae but profuse\r\nooids.\r\nIncludes Mas de Messier locality. Chondrocoenia clavellate dominant',NULL,NULL,NULL,NULL,'France','Europe',NULL,NULL,43.46,3.15,NULL,NULL,NULL,NULL,24.664724042,22.9622176477,31.0100289354,28.7650753919,32.0435,13.3195,'Krause','Krause','2021-05-28 15:21:12','2022-03-23 16:40:13'),('Wadi Aynouna, near Al Khuraybah',4259,'Jabal Kibrit, Wadi Waqb Member','Neogene','Miocene','Middle Miocene','early Middle Miocene',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','26',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3210,NULL,'Massive bioturbated coralline limestone with low diverse, medium isolated corals heads of Favites, Heliastraea, Tarbellastraea, Porites, Thegioastraea spp. Coralline red algae occur as free-rolling or partly attatched rhodoliths and debris of Lithothamnium and Mesophyllum spp. Red algae play a significant role in construction of\r\nthe reef facies, where they bind and connect coral colonies and other skeletal and non  skeletal constituents into a coherent mass. The bivalves, gastropods and echinoids act as essential rock forming constituents in this lithofacies. Fore-reef sediments mainly gave bioclastic wackestone, algal wackestone, bioclastic packstones, coralline framestone, coralline rudstone and grainstones. Most of these sediments are driven from the reef-core framework. Thin sections show fragments of corals, red algae, benthic foraminifera (miliolids) and ostracods. Most of these fragments were recrystallized due to diagenesis.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.1,35.1,NULL,NULL,NULL,NULL,25.1537399679,32.3932619637,24.5140642172,33.4191927893,26.4158,33.4195,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Al Bada',4260,'Jabal Kibrit, Wadi Waqb Member','Neogene','Miocene','Middle Miocene','lower-middle Miocene',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'4259',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','15','Non-rudist bivalves','41','Corals - bryozoans - (algae) - (bivalves)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,'1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3210,NULL,'Massive limestone with low diverse, scattered, small dendroid and massive heads of corals of Heliastraea, Tarbellastraea spp. Microfacies analysis of this facies gave coralline framestone, bioclastic grainstone, bryozoan grainstone, bioclastic wacke/floatstones and bioclastic rudstones. The skeletal grains are dominated by reworked moderately preserved small branched, massive and phaceloid corals, bivalves, gastropods and red algae. Matrix in most back reef is made up of peloidal micrite with abundant organic matter.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.31,35.01,NULL,NULL,NULL,NULL,25.3684039438,32.3206693927,24.7323898362,33.3617742145,26.6308,33.3473,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Station 15, Ash Shaykh Humayd',4261,'Unknown','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','26',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3212,NULL,'MIS5e coral reef terraces, expose reef-edge and\r\nback-reef lagoonal deposits with various stony\r\ncorals, molluscs, echinoids, melobesians, etc.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.05,34.34,NULL,'198563',NULL,NULL,27.9036023673,34.1111240618,27.6742635625,34.1749976984,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Station 6, 12 South of Ra-s Suwayhil as Saghir',4262,'Unknown','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','13',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3212,NULL,'Large boulders overgrown by reefal carbonates with variety of well-preserved scleractinian corals and molluscs, gastropods. Large mamelon-like aragonite botryoids are found.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.45,34.48,NULL,'198537',NULL,NULL,28.3038262551,34.250106804,28.0725378764,34.3206892529,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Station 20, North of Wadi Tayyib Ism',4263,'Unknown','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3212,NULL,'reefal carbonates with conglomeratic layers sitting on Arabian basement granitoids with abundant scleractinian heads, gastropods, epifaunal and infaunal bivalves.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.35,34.47,NULL,'198579',NULL,NULL,28.2038103538,34.2403279363,27.9726677695,34.3091735547,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Station 27, south of Al Maqnah',4264,'Unknown','Quarternary','Pleistocene','Pleistocene','Pleistocene',0.00,2.60,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3212,NULL,'Porites-dominated reefs and intervening sandy sediments host abundant and diverse associated fauna which includes large bivalves and gastropods.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,28.2,34.43,NULL,'198586',NULL,NULL,28.0537463746,34.2006928222,27.8231639791,34.2669944909,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('B reef and J reef, Madura Strait Basin',4265,'Kujung','Paleogene','Oligocene','Chattian','Chattian-Aquitanian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',NULL,2,'1','Seismic data available ',2,'Reef mound','4','More than 500 m thick','825','4','More than 1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','3','Below storm wave base','1','Corals','12','Foraminifera','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',3213,NULL,'Reefal facies, composed of a coral framework, larger foraminifera, red algae, echinoderm plates, and other minor carbonate bioclasts.',NULL,NULL,NULL,NULL,'Indonesia','Asia',NULL,NULL,-7.24,113.13,NULL,NULL,NULL,NULL,-3.87592302985,111.361055874,-8.72580840042,114.674270046,-6.53887,118.005,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('O-1Madura Strait Basin',4266,'Mundu','Neogene','Pliocene','Pliocene','Zanclean',3.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',NULL,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf',NULL,NULL,'12','Foraminifera','12','Foraminifera','71','Foraminifera only, (some corals)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',3213,NULL,'porosity of the Mundu carbonate rock can reach more than 40%. Mundu is composed of bioclastic\r\ngrainstone, wackestone and packstone and has been\r\nintensely bioturbated. ',NULL,NULL,NULL,NULL,'Indonesia','Asia',NULL,NULL,-7.19,113.21,NULL,NULL,NULL,NULL,-6.65206348173,112.792482349,-7.53497714969,112.887347208,-7.30625,114.045,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Blue Mountain Inlier',4267,'Rio Grande Limestone','Cretaceous','Upper Cretaceous','Campanian','upper Campanian',72.10,83.60,26,'middle Campanian - Danian/Selandian',75,75,'Late Cretaceous (Late Campanian, 75 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','3','Below storm wave base','5','Rudists','5','Rudists','72','Rudists only (sometimes with microbial encrustations)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3214,NULL,'Rudists as large bouquets of Biradiolites\r\nmooretownensis yielding tens of thousands of\r\nspecimens',NULL,NULL,NULL,NULL,'Jamaica','North America',NULL,NULL,18.3,-76.35,NULL,'198683',NULL,NULL,14.3900985374,-66.4717145358,16.6589865414,-69.8283116854,19.9637,-66.0609,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Atar Group, unit I-5',4268,'Atar','Ediacaran','Ediacaran','Avalon Assemblage','Neoproterozoic',542.00,999.00,0,'Vendian',605,750,'Early Neoproterozoic (late Tonian. 750 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','41',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation',NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3215,NULL,'Stromatolitic bioherms.',NULL,NULL,NULL,NULL,'Mauritania','Africa',NULL,NULL,20.31,-13.03,NULL,NULL,NULL,NULL,-54.7567787445,-0.542051839931,-54.7567787445,-0.542051839931,-23.4577,87.2119,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Pizzo Croce Limestone',4269,'Unknown','Cretaceous','Upper Cretaceous','Cenomanian','Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','10','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','3','Below storm wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12',NULL,NULL,'2','Intensive',NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3220,NULL,'Rudist biostrome/buildups, highenergy shelf-margin rudist patches. Caprinidae-Radiolitidae floatstone grading up into amalgamated beds of angular bioclastic rudstone/grainstone. Alternations of foraminifer/ostracod mudstone/wackestone and bioclastic grainstone/fine-rudstone.',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,38.11,13.19,NULL,NULL,NULL,NULL,28.0822593494,13.9009992307,22.4237186233,12.7034024025,21.2032,13.3435,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Wadi Mujib',4270,'Wadi As Sir Limestone','Cretaceous','Upper Cretaceous','Cenomanian','middle Cenomanian',93.90,100.50,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','3','Below storm wave base','5','Rudists','2','Algae','91','Rudists - corals - algae/microbes - (brachiopods)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11',NULL,NULL,'1','Present','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','2','Intense',0,'No or unknown reservoir potential',3222,NULL,'Peritidal (mudstones with monotypic ostracodes or microbial lamination) and agitated shallow subtidal environments (rudist patch reefs).',NULL,NULL,NULL,NULL,'Jordan','Asia',NULL,NULL,31.27,35.34,NULL,NULL,NULL,NULL,15.9106923343,33.6129570758,11.3975931152,28.6309335118,11.9916,29.3065,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Nallıhan',4271,'Yenipazar (=Nardin), Çeğiköy Reef Member','Cretaceous','Upper Cretaceous','Campanian','Campanian/Maastrichtian',66.00,83.60,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'5','Rudists','12','Foraminifera','91','Rudists - corals - algae/microbes - (brachiopods)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','26',NULL,NULL,'2','Intensive','2','Intensive','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3224,NULL,'Patch reefs and locally fringing type\r\nreefs comprise abundant hippurits and other rudists, algae, bryozoans, coelenterate, echinoid, gastropods, ammonoids.',NULL,NULL,NULL,NULL,'Turkey','Asia',NULL,NULL,40.12,31.2,NULL,NULL,NULL,NULL,37.0693484965,31.8094589396,37.3739043318,30.3468464859,30.8172,30.2985,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Bird Road, Miami',4272,'Buckingham, Pinecrest Beds or Formation','Neogene','Pliocene','Pliocene','lower Pliocene',3.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','2c','Atoll (circular structure)','3','Below storm wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','30',NULL,NULL,NULL,NULL,'2','Intensive','3','Pronounced zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3225,NULL,'More biohermal in form, the reef system appeared to have distinct zonation. coral fauna was present, including Diploria sarasotana, Septastrea marylandica, Septastrea crassa, Porites furcata Lamarck, and the hydrocoral Millepora alcicornis, and over three hundred species of mollusks along with several species of echinoids and crustaceans.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,25.43,-80.22,NULL,'146873',NULL,NULL,25.1641649859,-79.3974699317,25.9524887954,-79.2936584418,25.5534,-78.9945,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Tangjiahe ',4273,'Xiannüdong','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','93','Microbial micrite - pelmatozoans',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite',NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3226,NULL,'The Tangjiahe section contains three levels of reefal buildups that were constructed by aconsortium of archaeocyaths and calcimicrobes in varying proportions. The lowest (oldest) reefal buildup is acalcimicrobial biostrome, possibly in the form of a wide mound with a low relief (unconfirmed due to outcroplimitation), which was formed byEpiphytonwith rare small archaeocyaths, and is sandwiched by flat-pebbleconglomerates. The middle reefal buildup is a high-relief calcimicrobial mound, enclosed by oolites, that was built byintergrownRenalcisandTarthinia.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,32.36,106.29,NULL,NULL,NULL,NULL,-3.84042740035,78.5315278314,-3.84042740035,78.5315278314,27.6128,164.827,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kano-yama limestone, Kanto Mountains',4274,'Unknown','Carboniferous','Pennsylvanian','Gzhelian','Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','20','4','Microbial precipitation',NULL,NULL,'2','Intensive','2','Medium zonation',NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite',NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3228,NULL,'Algal-microbial mound composed of Anthracoporella, Palaeoaplysina, Tubiphytes, Archaeolithoporella, and bryozoans. The limestone is characterized by abundant micrite, implying a low-energy back-reef depositional environment.',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,36.5,138.53,NULL,NULL,NULL,NULL,14.0359988711,144.095839731,14.6032865092,76.3871937958,15.1502,105.022,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Fossil Hill',4275,'Unknown','Quarternary','Pleistocene','Pleistocene','upper Pleistocene',0.00,0.10,33,'Pleistocene',0,1,'Pleistocene - Calabrian - Gelasian',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','5','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4b','Deep basin (> 200 m)','2','Below fair weather wave base','8','Serpulids, worms, vermetids','15','Non-rudist bivalves','16','Serpulids - bivalves - (microbes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','22',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3231,NULL,'Serpulid build-ups: massive deposits composed of fossil serpulid worm tubes (Annelida: Serpulidae) and bivalve shells.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,33.5,-118.41,NULL,'200653',NULL,NULL,33.4870368913,-118.378842149,33.5,-118.41,33.5,-118.41,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Xikou section',4276,'Jinjiling','Triassic','Lower Triassic','Induan','Induan',251.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','0.2','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','3','Microbes','12','Foraminifera','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3239,NULL,'Lower stromatolite bed, lying on the oolitic grainstone, 0.2 m thick. Columnar stromatolites.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.17,109.19,NULL,NULL,NULL,NULL,-6.69722417725,108.018930782,16.752654929,125.558198254,27.9505,93.4566,'Krause','Krause','2021-05-28 15:21:12','2021-06-13 15:20:44'),('Xikou section',4277,'Longdongchuan','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','95.5','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','6','Calcisponges','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3239,NULL,'Very-thick-bedded sponge framestones and thick-to-very-thick-bedded bioclastic grainstones. Fossils are diverse and abundant and include calcareous sponges, calcareous algae, echinoderms, corals, small foraminifers, fusulinids, brachiopods. Clarkina yini zone. Shallow marine, low- to middle\r\nenergy zone. Coordinates stated in the text, decimal.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.2419,109.376,NULL,NULL,NULL,NULL,-7.65229573803,107.063172386,14.2192250605,126.403999257,6.58408,96.3184,'Krause','Krause','2021-05-28 15:21:12','2021-06-19 18:51:08'),('Mtwara Bay',4278,'Mikindani','Neogene','Miocene','Upper Miocene','lower Messinian',6.00,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8.5','1','Less than 10 m wide',NULL,'2','10 - 100 m','25',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1d','Marginal marine - coastal -  siliciclastic shelf','2','Below fair weather wave base','1','Corals','12','Foraminifera','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','46',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3240,NULL,'Coral bioconstruction with two principal facies:\r\nsiliciclastic sheetstone facies dominated by platy\r\ncolonies, and carbonate mix-platestone facies including a variety of growth forms (platy, tabular-massive, branching and solitary. Tabular-massive corals can reach a size of up to 50 cm across.',NULL,NULL,NULL,NULL,'Tanzania','Africa',NULL,NULL,-10.15,40.11,NULL,NULL,NULL,NULL,-10.8506777461,39.2884578343,-11.3782712953,39.2608973756,-10.5205,39.2601,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kotouč Quarry, Štramberk',4279,'Unknown','Cretaceous','Lower Cretaceous','Berriasian','lower Berriasian',139.80,145.00,22,'late Tithonian - early Valanginian',141,145,'Jurassic/Cretaceous Boundary (145 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','18','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','1','Corals','7','Bryozoans','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','25','4','Microbial precipitation','1','Present','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3241,NULL,'Coral-microbial bindstone passing locally to poorly sorted pelbiointraclastic packstone. Corals and micro-encrusters (Lithocodium aggregatum and Crescentiella morronensis) form a framework\r\nthat supported the sediment during deposition. Bioclasts belong to trepostome bryozoans\r\n(colonies and isolated zooecias), calcareous sponges, crinoids and gastropods. Ooids and\r\ncalcareous dinoflagellate cysts are rare. Cavities are filled with radiaxial-fibrous calcite cement,\r\nchalcedony and blocky calcite.',NULL,NULL,NULL,NULL,'Czech Republic','Europe',NULL,NULL,49.35,18.06,NULL,'202900',NULL,NULL,31.7052507429,29.7985930723,36.9462232624,31.3258075065,41.3672,24.7928,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jebel Taabest',4280,'Choucht to Agoudim','Jurassic','Lower Jurassic','Pliensbachian','lower Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,185,'Early Jurassic (Pliensbachian, 186.8 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','3','Microbes','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','11','4','Microbial precipitation','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3243,NULL,'subtidal lagoon paleoenvironments with olistoliths that show a boundstone to floatstone texture, with solitary and colonial corals, sponges, gastropods, serpulid worms, crinoids, brachiopods, echinoids tests and spines, and occasional chaetetid sponges and microbialites.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.9351,-4.9594,NULL,NULL,NULL,NULL,19.6912835586,4.37936443723,26.8786876572,6.06454873649,26.8378,-1.24771,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Koudiat Ech Chehem',4281,'Maftah 3','Jurassic','Lower Jurassic','Pliensbachian','upper Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,185,'Early Jurassic (Pliensbachian, 186.8 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'3','Microbes','3','Microbes','86','Microbes - sponges - crinoids',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3243,NULL,'Giant bioherm made of interlayered boundstones\r\n(pillarstones and mixstones) and crinoidal grainstones and packstones. Environment in the\r\noptimal reef window, at the boundary between shoreface and offshore. Well-lit and diverse communities.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,33.4528,-4.9225,NULL,NULL,NULL,NULL,20.9109494868,5.34301544598,28.00261038,7.2143247342,28.1934,-3.23884,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Mihangaoqiaogaolu section, West Ujimqin Banner',4282,'Amushan','Carboniferous','Pennsylvanian','Gzhelian','Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','110','3','101-1000 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','2','Algae','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','10','4','Microbial precipitation',NULL,NULL,'2','Intensive','2','Medium zonation','2','Medium zonation','3','More than 60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3244,NULL,'Reefs are superimposed upon each other in the lower part of the section, but are isolated in the upper part. They developed on and are overlain by\r\nmedium- to thick-bedded skeletal wackestone that contains phylloid algae and Shamovella, foraminifers, echinoderms, bryozoans, Rectangulina, and Epimastopora.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,44.2756,117.887,NULL,NULL,NULL,NULL,47.5013909349,130.225581719,63.7421605139,97.6426369165,38.1015,92.8161,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Cioclovina–Bănita area, MFT2',4283,'Unknown','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','13','4','Microbial precipitation','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3245,NULL,'Platform margin environment, crest—shallow-water patch reefs. Crustose fabrics, biogenic encrustations and perforations; clotted, agglutinated and dome-shaped microbial microstructures, small cavities; the intra-reef sediment is mostly micritic; scarce geopetal structures; radiaxial- fibrous cements and late diagenetic druse/ mosaic spar occur locally',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,45.28,23.15,NULL,NULL,NULL,NULL,28.6163653184,35.664715173,21.9474947491,29.8969779645,26.5294,27.6449,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gunung Subis',4284,'Subis Limestone','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','390','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'6',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3246,NULL,'Massive and branching corals, coralline red algae, benthic foraminifera, bivalves, gastropods, echinoids, and occasionally bryozoans and sponges. Eight microfacies types and four environments were defined to describe the Subis Limestone: outer talus, inner talus, reef rim, and lagoon.\r\nNine genera of benthic foraminifera.',NULL,NULL,NULL,NULL,'Malaysia','Asia',NULL,NULL,3.48,113.51,NULL,NULL,NULL,NULL,3.87418462232,110.715914039,0.637347006763,114.137892011,3.89912,116.63,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kuh-e Siah section, Borazjan city',4285,'Sarvak','Cretaceous','Lower Cretaceous','Albian','Albian-Cenomanian',93.90,113.00,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','5','Rudists','1','Corals','91','Rudists - corals - algae/microbes - (brachiopods)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3251,NULL,'Angular rudist and coral with minor amounts of echinoids and benthic foraminifera fragments. Middle shelf and ramp environments',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,28.49,51.31,NULL,NULL,NULL,NULL,4.03890263155,47.1630337767,2.42681267861,41.5313382801,3.85718,41.4148,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Kuh-e Mond well, Fars Area',4286,'Sarvak','Cretaceous','Lower Cretaceous','Albian','Albian-Cenomanian',93.90,113.00,24,'late Aptian - middle Cenomanian',107,95,'Mid-Cretaceous (Cenomanian, 97.2 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','2','Below fair weather wave base','5','Rudists','13','Echinoderms','91','Rudists - corals - algae/microbes - (brachiopods)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3251,NULL,'Bioclastic pelloidal packstone consists mainly of pelloid with small benthic foraminifera, such as textulariids, alveolina, plaealveolina, conical orbitolina, echinoderms and rudist fragments. The pelloidal nature of this facies together with rudist\r\nand echinoid bioclasts indicate shallow open marine environment with good water circulation.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,28.2,51.19,NULL,NULL,NULL,NULL,3.7707320202,47.0099087554,2.16642785075,41.3655133272,3.58611,41.2669,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Northern shore of the Cíjara dam',4287,'Villarta, lower Villarta member','Ediacaran','Ediacaran','Nama Assemblage','upper Ediacaran',541.00,635.00,0,'Vendian',605,540,'Cambrian/Precambrian boundary (541 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m','2000','2',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'2','Below fair weather wave base','3','Microbes','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'3','High production of reefal debris','2','Intense',0,'No or unknown reservoir potential',3253,NULL,'Bioherms, shelly-microbial buildups.The reef-core facies consists of Cloudina-thromboid to stromatoid-thromboid boundstones and floatstones. Due to neomorphism, the calcified\r\nmicrobial communities are heterogeneously preserved, with clotted pseudospar textures\r\noccurring directly encrusting both microsparitic substrates and shelly walls. The\r\nmicrobial framestone is dominated by clotted, peloidal, fenestral textures, and subsidiary\r\nstromatolitic microsparite/sparry textures. Predominant skeletal components are\r\nCloudina carinata, C. hartmanae (probably C. xuanjiangpingensis), Sinotubulites\r\nbaimatuoensis, and rare Protolagena sp.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,39.15,-4.47,NULL,'205645',NULL,NULL,-35.2572473968,-4.53407647451,-35.2572473968,-4.53407647451,-46.7133,107.899,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Phu Pha Sing and Phu Pha Noi hills',4288,'Nam Mahoran','Carboniferous','Pennsylvanian','Kasimovian','Kasimovian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','20','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','2','Below fair weather wave base','2','Algae','3','Microbes','26','Phylloid and other platy algae - cements - (microbes)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3255,NULL,'Phylloid algal reef mound association is mainly composed of massive phylloid algal boundstone dominated, up 30% of bioclasts, by cup-shaped phylloid algae with locally common algal-skeletal\r\npackstone and wackestone. Red algae,calcimicrobes, forams, rugose coral, peloids, echinoderms,\r\nbrachiopods,fusulinds, ostracods can be found.',NULL,NULL,NULL,NULL,'Thailand','Asia',NULL,NULL,17.15,101.49,NULL,'205808',NULL,NULL,-21.5730426091,138.499803456,-7.57157865638,78.7146136827,-20.9583,105.043,'Krause','Krause','2021-05-28 15:21:12','2021-06-11 15:46:18'),('Değirmençay, Mersin Province',4289,'Karaisali','Neogene','Miocene','Lower Miocene','Burdigalian-Langhian',13.80,20.40,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','30','2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'2','Algae','1','Corals','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3257,NULL,'Red  algae, coral  and  benthic  foraminifera  bearing reefal limestone.',NULL,NULL,NULL,NULL,'Turkey','Asia',NULL,NULL,36.54,34.3,NULL,NULL,NULL,NULL,35.9936677288,31.0164205054,34.5757968323,33.1651232633,36.0931,34.1275,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lumazhai and Zhongxinzhai locality',4290,'Weining','Carboniferous','Pennsylvanian','Moscovian','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','19','3','101-1000 m wide',NULL,'3','More than 100 m','30',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','2','Algae','3','Microbes','26','Phylloid and other platy algae - cements - (microbes)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','19','4','Microbial precipitation',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3259,NULL,'Skeletal–cement–microbial reef (SCMR-1) in lower part of section\r\nGrey thick-bedded microbial carbonate and phylloid algae boundstone. The substrate is composed of grey thick-bedded wackestone and packstone. Peloids, microbial mat debris, bioclasts constitute most of the volume of the lower part. Bioclasts, including bryozoans, small brachiopod shells, gastropods, ostracods, crinoids, and foraminifera. The substrate becomes clotted wackestone towards\r\nthe mound and the biodiversity decreases. Skeletal grains have micritic envelopes.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.5075,106.233889,NULL,'206265',NULL,NULL,-11.4842550207,120.103224063,5.83659551771,96.7993144835,-13.9059,98.7312,'Krause','Kiessling','2021-05-28 15:21:12','2023-01-04 15:04:29'),('Mahmudia Quarry, Caeracul Mare Hill, sample 114',4291,'Caerace, Tubiphytes-Limestone Member','Triassic','Middle Triassic','Anisian','middle Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'3','Microbes','15','Non-rudist bivalves','40','Microbes - mollusks',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','122','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3260,NULL,'Tubiphytes-microbial buildup with bivalves, gastropods, brachiopods, ostracod fauna',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,45.03,29.03,NULL,'197722',NULL,NULL,27.8110331768,44.4592677994,26.4206026153,38.7538618433,17.5736,33.6202,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('South of Al Ain locality',4292,'Asmari','Paleogene','Oligocene','Rupelian','Rupelian',28.10,33.90,29,'Priabonian - Rupelian',33,30,'Early Oligocene (Rupelian, 31 Ma)',NULL,2,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick','110','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','3','Below storm wave base','1','Corals','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3261,NULL,'Massively bedded floatstone/rudstone is interbedded with packstone to floatstone. Coral and calcisponge clasts of pebble to boulder size are abundant.',NULL,NULL,NULL,NULL,'United Arab Emirates','Asia',NULL,NULL,24.01,55.48,NULL,NULL,NULL,NULL,16.7946723726,48.9428145701,14.5450677765,50.3165613533,17.2778,49.4575,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Finucane-1 wells',4293,'Unknown','Neogene','Miocene','Middle Miocene','late Langhian',13.80,14.80,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick','30','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Carbonate buildups and reef facies consisting largely of skeletal grains including foraminifera, bryozoans, molluscs and corals.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.2,116.44,NULL,NULL,NULL,NULL,-26.272183388,112.062434491,-28.7584063564,112.743205467,-28.2234,111.75,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Finucane-1 wells',4294,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick','30','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.2,116.44,NULL,NULL,NULL,NULL,-25.4604967851,112.561567856,-27.7524563652,113.133630199,-25.8188,113.248,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Picard-1',4295,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.04,117.48,NULL,NULL,NULL,NULL,-26.4402607675,112.976689091,-28.9985131032,113.724130598,-28.1116,112.872,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Picard-1',4296,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','1','Corals','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-19.04,117.48,NULL,NULL,NULL,NULL,-25.3234147611,113.653102663,-27.613962849,114.246964869,-25.7014,114.346,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('IODP-U1464',4297,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-18.04,118.37,NULL,NULL,NULL,NULL,-25.4584870478,113.938624724,-28.0153402779,114.706613281,-27.1512,113.875,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('IODP-U1464',4298,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. Reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-18.04,118.37,NULL,NULL,NULL,NULL,-24.3414773463,114.605972752,-26.630103419,115.216117321,-24.7366,115.323,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Minilya-1',4299,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-18.32,118.5,NULL,NULL,NULL,NULL,-25.7409003786,114.069344841,-28.2975058517,114.840995483,-27.4363,114,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Minilya-1',4300,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'12','Foraminifera','7','Bryozoans','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. The reef was extinguished and buried by shelfal sediments.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-18.32,118.5,NULL,NULL,NULL,NULL,-24.6238925019,114.735502822,-26.9122062402,115.348988514,-25.0212,115.447,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('East Mermaid-1',4301,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','7','Bryozoans','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.15,119.47,NULL,NULL,NULL,NULL,-24.5882404621,115.113940981,-27.1423874163,115.905633699,-26.3062,115.09,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('East Mermaid-1',4302,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','12','Foraminifera','1','Corals','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Giant barrier reef system containing carbonate buildups and reef facies.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.15,119.47,NULL,NULL,NULL,NULL,-23.4714542212,115.771109073,-25.7568569491,116.400256621,-23.8873,116.51,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Barcoo-1',4303,'Unknown','Neogene','Miocene','Lower Miocene','upper Burdigalian',16.00,17.50,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'2000','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','12','Foraminifera','1','Corals','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3264,NULL,'Giant barrier reef system containing carbonate buildups and reef facies.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-15.29,120.3,NULL,NULL,NULL,NULL,-23.6815940386,115.468107331,-26.4586582301,116.411534202,-26.8978,114.624,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Reşiţa–Moldova Nouă zone',4304,'Valea Minişului','Cretaceous','Lower Cretaceous','Aptian','middle Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,120,'Early Cretaceous (early Aptian, 121.8 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','42','2','10 - 100 m wide',NULL,'4','More than 1000 m','1100','1.1',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','29','4','Microbial precipitation','2','Intensive','2','Intensive','2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3265,NULL,'Reef built by platy corals. The coral units are underlain by bioclastic limestones interlayered with thin rudist-chaetetid biostromes, separated by a 15–30 m thick interval of bioclastic limestones and overlain by upper Aptian conglomerates. Mostly dense, rarely sparse, platestones are composed of a low diversity coral assemblage mainly represented by the suborder Microsolenina. Small, branching corals are very rare. The matrix mainly consists of fine bioclastic-peloidal packstones and wackestones. Dominance of microsolenine corals, their flattened morphology, the presence of epibionts on coral undersurfaces and occurrence of red algae Sporolithon rude and Polyastra alba.',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,45.01,21.53,NULL,NULL,NULL,NULL,34.6147957382,33.2196496224,27.0289787133,26.0198938115,24.5123,26.3824,'Krause','Krause','2021-05-28 15:21:12','2021-08-19 17:05:37'),('Brecknock 1',4305,'Unknown','Neogene','Miocene','Middle Miocene','Langhian',13.80,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,3,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','12','Foraminifera','1','Corals','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3264,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. ',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-14.35,121.42,NULL,NULL,NULL,NULL,-21.8160906836,117.200456661,-24.3627588828,118.022851417,-23.5773,117.273,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Brecknock 1',4306,'Unknown','Neogene','Miocene','Middle Miocene','Serravallian',11.60,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'1600','4293',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','12','Foraminifera','1','Corals','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3264,NULL,'Giant barrier reef system containing carbonate buildups and reef facies. ',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-15.29,120.3,NULL,NULL,NULL,NULL,-21.625024075,116.667566156,-23.9073052585,117.304827116,-22.057,117.447,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('MioR-3 - Rowley Shoals',4307,'Unknown','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'250','4308',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Buried late Miocene isolated pinnacles and atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.23,119.07,NULL,NULL,NULL,NULL,-21.3930447602,116.620914975,-23.0511723815,116.962310875,-23.953,116.089,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('MioR-3 - Rowley Shoals, near Cunningham island',4308,'Unknown','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250',NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Buried late Miocene isolated pinnacles and atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.48,118.4,NULL,NULL,NULL,NULL,-21.633308334,115.929528583,-23.2922951093,116.262998755,-24.1782,115.379,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('MioR-3 - Rowley Shoals, East of Mermaid Reef',4309,'Unknown','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250','4308',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Buried late Miocene isolated pinnacles and atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-17.06,119.4,NULL,NULL,NULL,NULL,-21.2276283051,116.962000239,-22.8852422503,117.307144655,-23.7949,116.441,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('MioR-3 - East of Rowley Shoals',4310,'Unknown','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','4','More than 500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'250','4308',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Buried late Miocene isolated pinnacles and atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-16.59,119.5,NULL,NULL,NULL,NULL,-20.7590303877,117.071641044,-22.4164672603,117.417181002,-23.3288,116.564,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('MioR-3 - East of Rowley Shoals',4311,'Unknown','Neogene','Miocene','Upper Miocene','late Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'250','4308',0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3263,NULL,'Buried late Miocene isolated pinnacles and atolls',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-16.51,120.09,NULL,NULL,NULL,NULL,-20.6867644813,117.677431553,-22.3431087437,118.02977875,-23.2692,117.182,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Saal Quarry',4312,'Unknown','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','90','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','31','1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1509,NULL,'Mostly reefal debris',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,48.887,11.941,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('GL1, Tazhong (Katake) Uplift, central Tarim',4313,'Penglaiba','Ordovician','Lower Ordovician',NULL,'lower Ordovician',470.00,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','3','Below storm wave base','2','Algae','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','1','Present',2,'Actual reservoir',3270,NULL,'Hydrocarbon reservoir',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,38.94,85,NULL,NULL,NULL,NULL,-15.0816937201,76.6851446934,-15.0816937201,76.6851446934,-24.5747,129.302,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Z11, Tazhong (Katake) Uplift',4314,'Yingshan','Ordovician','Lower Ordovician',NULL,'lower Ordovician',470.00,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,2,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1a','Shallow intra-platform','2','Below fair weather wave base','15','Non-rudist bivalves','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3270,NULL,'Ostracod-oyster-algae floatstone interbedded with bioclastic limestone',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,39.74,83.08,NULL,NULL,NULL,NULL,-16.3084379898,75.4827409691,-16.3084379898,75.4827409691,-24.5284,127.449,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lumazhai section, Houchang area',4315,'Maping','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','10','2','10 - 100 m wide','20','2','10 - 100 m',NULL,NULL,'3554',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','12','Foraminifera','20','Corals - forams',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3271,NULL,'Patch reef consisting of a simple coral framework and a low biodiversity community. The substrate is composed of bioclastic grainstone and rudstone \r\nFomichevella, phacelloid and with an erect growth habit, form the reef framework. Asexual reproductive budding of Fomichevella is visible. Foraminifers and crinoids are common fossils. The spaces in\r\nthe coral framework are filled with bioclastic wackestonepackstone.\r\nBioclastic grainstone covers the coral patch reef, in which some coral debris are seen.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.5667,106.1,NULL,'211310',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2022-03-24 11:00:20'),('Pippu limestone, NE of the Asahikawa city',4316,'Tosshozan','Triassic','Upper Triassic','Carnian','Carnian',228.00,235.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','1','Corals','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3272,NULL,'Tubiphytes-calcimicrobe rudstone, dominated by Tubiphytes spp. and associated with large echinoderm ossicles. Poorly preserved calcimicrobes, reworked mud grains, micritized clasts and coated or aggregate grains are abundant. Other bioclasts are\r\nSoleporacean, red algae, microproblematica and the sponge Uvanella sp. Serpulids and bryozoan debris are rare. Microbial crusts were observed on a recrystallized framebuilder.',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,43.5,142.27,NULL,NULL,NULL,NULL,26.3797880372,147.471969759,79.5670547811,-147.890685914,44.4978,126.559,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Jiwozhai reef',4317,'Dushan','Devonian','Middle Devonian','Givetian','middle Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','5','2','10 - 100 m wide','100',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','35','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3273,NULL,'Patch reef with high biodiversity: stromatoporoids, rugose corals, tabulate corals, chaetetids,\r\nbrachiopods, bryozoans, calcified cyanobacteria and tubeworms.\r\n83 species were mentioned but only 35 are considered reef building',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.5,107.34,NULL,'212695',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Kiessling','2021-05-28 15:21:12','2023-03-10 13:16:53'),('WC55 reef, Belaya River gorge',4318,'Gerpigem','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3275,NULL,'It comprises mudstones interbedded with thin–medium-bedded bioclastic limestones, with abundant coral and sponge fragments, and plentiful bivalves. These grade upwards into massive reef facies that consist of coral-sponge rudstones in the lower part and platy coral reef limestones in the upper part. The reefs comprise thick biostromes. The bedded\r\ncarbonates consist of lagoonal bioclastic and micritic limestones that grade upward into gastropod and oncoidal limestones.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,44.16,40.1,NULL,'213016',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('WC6a-b, Akhtsu Zone',4319,'Katsirkhskaya','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3275,NULL,'Oxfordian–Tithonian. The principal reef organisms are corals and calcisponges. In the middle part of the succession, the facies consist of lithoclastic and bioclastic grainstones in the southern flank of the anticline and bioclastic packstones with sponges and coral fragments in the northern flank. The upper part of the succession on the southern flank of the anticline consists of intertidal-supratidal bioclastic limestones, abundant fenestral grainstone-packstones and algal packstones.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,43.36,40.02,NULL,'213022',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('WC114 - WC115, Bolyshaya Laba River',4320,'Gerpigem','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','30','2','10 - 100 m wide',NULL,'2','10 - 100 m','50',NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3275,NULL,'The mound consists mainly of siliceous sponge-microbialite and microbialite boundstones. It is made up of a cluster of much smaller lenticular bodies or bioherms. The top of the reef succession is capped by thinly-bedded microbialite floatstones and bioclastic limestones.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,44.05,40.56,NULL,'213017',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Shitouzhai section, Ziyun region',4321,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base','6','Calcisponges','12','Foraminifera','88','Green algae - phylloid algae - calcisponges - (corals)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','9',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite',NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3276,NULL,'Reef formed largely of calcisponge floatstones and/or framestones. The spaces between the rigid framework formed by the sponges are filled with wackestones and packstones that contain numerous benthic foraminifers (Palaeofusulina, Colaniella, Glomospira), green algae (Dasycladales and Mizzia), and crinoids and bivalve fragments.\r\n\r\nFormation original was Changhsing. \r\nComments from Tian & Wang, 2021:\r\n\r\nReef builders: Frame-building and baffling\r\norganisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, bryozoans, and hydrozoans\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, ostracodes, bivalves, brachiopods,gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic: Fore-reef slope: packstone with\r\nfloatstone and reef breccias\r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella.\r\nReef flat (reef crest): algal-foraminiferal packstone with reef breccia.\r\nReef base: bioclastic packstone to grainstone.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin.\r\n\r\nCoordinates stated in text.\r\n\r\n\r\n\r\n',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.8417,106.0944,NULL,NULL,NULL,NULL,-15.6577408632,105.530130143,6.68779257563,123.248366238,7.24145,97.3327,'Krause','Krause','2021-05-28 15:21:12','2021-06-18 17:36:28'),('Lagonaki Highland and vicinity',4322,'Unknown','Jurassic','Upper Jurassic','Oxfordian','lower-middle Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','2b','Margin of deep basins (shelf margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3278,NULL,'Moderately  thick  reefal carbonates.',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,44.03,39.08,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('vicinity of the city of Sochi and northern  Abkhazia',4323,'Unknown','Jurassic','Upper Jurassic','Oxfordian','middle-upper Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3278,NULL,'Massive carbonate deposition with coral reefs',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,43.01,41.4,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Basins of the rivers Belaja and Laba',4324,'Unknown','Jurassic','Upper Jurassic','Oxfordian','middle Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','2b','Margin of deep basins (shelf margin)',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3278,NULL,'Massive carbonate accumulation',NULL,NULL,NULL,NULL,'Russia','Asia',NULL,NULL,44.01,41.59,NULL,NULL,NULL,NULL,32.4641082304,51.4977848812,37.3886980179,54.7300005974,38.2759,47.0304,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Barranco de Losilla',4325,'Zegri/Veleta','Jurassic','Middle Jurassic','Bajocian','Bajocian',168.30,170.30,20,'middle Aalenian - middle Bathonian',166,170,'Middle Jurassic (Bajocian&Bathonian, 168.2)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3.5',NULL,NULL,NULL,'1','Less than 20 m','12',NULL,NULL,0,'Tropical or unknown','4','Basin','4b','Deep basin (> 200 m)','2','Below fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3281,NULL,'Buildup of thin-shelled bivalves',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,37.25,-4.24,NULL,NULL,NULL,NULL,16.64086265,14.9789063445,21.9800145478,11.1139888475,28.0497,5.81673,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Longgang area',4326,'Changhsing','Permian','Lopingian','Changhsingian','late Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'1','Seismic data available ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','3','Below storm wave base',NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',2,'Actual reservoir',3282,NULL,'Grey dolomitized reefs or dolomitized boundstone\r\nfacies, with an average porosity of 4.0%.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,27.48,105.2,NULL,NULL,NULL,NULL,-13.808382706,104.503236395,8.69445676141,122.62660003,8.44898,95.5994,'Krause','Krause','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Shaghap piggyback basin',4327,'Unknown','Paleogene',NULL,NULL,'Eocene/Oligocene',23.00,56.00,NULL,NULL,NULL,35,'Late Eocene (Priabonian, 35.9 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m','500',NULL,NULL,0,'Tropical or unknown','4','Basin','4b','Deep basin (> 200 m)','2','Below fair weather wave base','2','Algae','1','Corals','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','100','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3283,NULL,'Outcrop with conglomerates and breccias, reefal blocks of branching coralline limestones, siltstones, claystones and calci-mudstones. With small planktonic foraminifers, discocyclinids as well as numerous red algal, coralline algal fragments. Additionally, some echinoids,\r\nbryozoans, bivalve fragments and gastropods are present. Few fragments of Bryozoans are observed in microbialites. Microbial peloids and encrusting filaments form incipient branching structures',NULL,NULL,NULL,NULL,'Armenia','Europe',NULL,NULL,39.52,44.51,NULL,'214574',NULL,NULL,39.6133670816,39.1674560563,37.8892467821,43.1932962485,36.1721,40.7467,'Krause','Krause','2021-05-28 15:21:12','2022-05-24 17:16:00'),('Roztoka (S1)',4328,'Hradiste','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15','4','Microbial precipitation','1','Present','1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3285,NULL,'light-beige, porous, sponge–microbial limestones. There are two main types of microfacies: Sponge–microbial framestones–floatstones and fine-grained bioclastic wackestones–packstones. Depositional environment: low- to moderate-energy mid ramp',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,49.52,20.48,NULL,NULL,NULL,NULL,31.2496826059,33.3886401933,37.2602811346,35.3170033321,41.44,27.3347,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Lanckorona',4329,'Unknown','Jurassic','Upper Jurassic','Kimmeridgian','lower Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15','4','Microbial precipitation',NULL,NULL,'1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3285,NULL,'Light-beige, porous, sponge–microbial limestones. There are two main types of microfacies: Sponge–microbial framestones–floatstones and fine-grained bioclastic wackestones–packstones. Depositional environment: low- to moderate-energy mid ramp',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,49.5,19.44,NULL,'215202',NULL,NULL,31.587477213,31.1457673971,36.5641872203,33.484476069,41.5403,26.1257,'Krause','Krause','2021-05-28 15:21:12','2022-08-25 16:57:14'),('Sulow',4330,'Unknown','Jurassic','Upper Jurassic','Oxfordian','Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15',NULL,NULL,NULL,NULL,'1','Present','1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3285,NULL,'Light-beige, porous, sponge–microbial limestones. There are two main types of microfacies: Sponge–microbial framestones–floatstones and fine-grained bioclastic wackestones–packstones. Depositional environment: low- to moderate-energy mid ramp',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,49.57,20.06,NULL,'215203',NULL,NULL,31.4771757158,32.382732679,37.0465095831,34.4968926345,41.6557,26.6496,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Esashi limestone',4331,'Heian','Triassic','Middle Triassic','Ladinian','Ladinian-Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick','20',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp',NULL,NULL,'13','Echinoderms','3','Microbes','86','Microbes - sponges - crinoids','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3286,NULL,'Large echinoderm ossicles, debris of calcimicrobes, debris of bivalves, bryozoans and calcimicrobes indet. Remobilized framebuilders (i.e., recristallized corals and spongiomorphids).',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,44.54,142.21,NULL,NULL,NULL,NULL,7.50628107176,162.286819639,80.7925307788,-143.466112108,45.1778,123.323,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Quarry 23, Dent Peninsula, Sabah',4332,'Togopi','Neogene','Pliocene','Pliocene','Pliocene',2.60,5.30,32,'Tortonian - Gelasian',6,4,'Piacenzian - Zanclean',NULL,1,'0','Outcropping reef ',NULL,NULL,'2','10 to 100 m thick',NULL,'2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','22',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3287,NULL,'Loosely cemented rubbly reef limestone, with well-preserved and rich fauna of molluscs, echinoids, foraminifera, gastropods and corals in apparent growth positions. ',NULL,NULL,NULL,NULL,'Malaysia','Asia',NULL,NULL,5.15,119.12,NULL,NULL,NULL,NULL,5.63898201179,118.724497227,5.14312577351,118.877039777,5.18036,119.428,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('section J reefs, Ibex area, Millard County, Utah',4333,'Wah Wah','Ordovician','Lower Ordovician','Floian','Floian',470.00,477.70,4,'late Early - early Middle Ordovician',472,470,'Early Ordovician (Floian/Dapingianboundary, 470 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'11','Siliceous sponges','11','Siliceous sponges','80','Lithistid sponges - receptaculid algae - microbes - (stromatoporoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','6','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3288,NULL,'Sponge-Rich Patch Reefs. Two conspicuous 1.5 m and 3 m thick reef intervals, with reefs rich in lithistid sponges.',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,38.51,-113.27,NULL,NULL,NULL,NULL,21.4236851738,-117.858685301,21.4236851738,-117.858685301,-5.5443,-83.4703,'Krause','Krause','2021-05-28 15:21:12','2022-06-28 16:53:42'),('Mt. Tului',4334,'Mt. Tului','Jurassic','Upper Jurassic','Oxfordian','late Oxfordian-Kimmeridgian',152.10,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','45','2','10 - 100 m wide','100',NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'4','Microbial precipitation','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',3290,NULL,'Type 1 build-ups developed in the proximal middle ramp and consist of 45 m thick, 100 m wide, coral-stromatoporoid boundstone associated with coral–stromatoporoid rudstone–grainstone. Type 2 build-ups, colonizing deeper environments in the middle ramp, are lens-shaped coral–calcareous sponge–diceratid boundstone including stromatoporoids and chaetetid sponges, 1–2 m thick and 3–4 m wide, associated with bioclastic packstone–grainstone. Type 3 lens-shaped calcareous and siliceous sponge–coral–microbialite boundstone build-ups (1 m thick and a few metres wide) formed in lower energy, distal middle-to-outer ramp settings.',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,40.15,9.35,NULL,NULL,NULL,NULL,21.0650280943,24.2228004707,23.1048407077,18.6979560589,33.3116,14.6388,'Krause','Krause','2021-05-28 15:21:12','2021-05-29 20:32:28'),('Gold Point Reef, Nevada',4335,'lower Poleta','Cambrian','Series 2','Stage 4','Botomian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','70',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1791',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','58','Archaeocyaths - microbes (Renalcis, Epiphyton, Girvanella) - corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3294,NULL,'Reef built by massive branching archaeocyaths and dense renalcid thickets. ',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,37.38,-117.26,NULL,NULL,NULL,NULL,14.3196058988,-154.139091862,14.3196058988,-154.139091862,-7.63991,-101.293,'Krause','Krause','2021-05-28 15:21:12','2021-06-12 14:33:36'),('Wudang, western Yangtze Platform',4336,'Tungtzu','Ordovician','Lower Ordovician','Tremadocian','upper Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','0.4','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','1','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,NULL,NULL,'2','Intense',0,'No or unknown reservoir potential',3296,NULL,'The stromatolites are 40 cm thick and flat column shaped, but strongly dolomitized.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,26.61,106.75,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-05-28 15:21:12','2021-06-13 15:20:44'),('Letca and Băbeni–Cuciulat',4338,'Cozla','Paleogene','Eocene','Priabonian','Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','55',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1096',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','18','1','Constructor guild','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,'1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3297,NULL,'The reefs occur within a shallow‐water succession composed mostly of bedded limestones, dominated by bioclastic (coralline) packstones. Branching ramose colonies, branching low‐integrated phaceloid, and sheet‐like (foliaceous) corals dominate.\r\nRupelian',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,47.33,23.47,NULL,'220523',NULL,NULL,45.7406075429,17.465831329,43.9566915494,17.6748379203,42.9662,20.7541,'Krause','Krause','2021-06-05 21:20:15','2021-06-13 15:20:44'),('Chenluzhen quarry, Chenluzhen County',4339,'Pingliang','Ordovician','Upper Ordovician','Sandbian','Sandbian',453.00,458.40,5,'Darriwilian - Ashgillian',452,450,'Late Ordovician (Sandbian - Katian, 449.1 Ma)',NULL,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','40',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1e','Open-marine shelf','3','Below storm wave base','3','Microbes','1','Corals','61','Microbes (thrombolites) - algae - corals','4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3298,NULL,'The reef can be classified as a skeleton–cement reef or a triple hybrid carbonate of skeleton–microbial–abiotic components.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.03,109.1,NULL,'220534',NULL,NULL,34.8924063117,92.3052178995,34.8924063117,92.3052178995,-25.3266,122.507,'Krause','Krause','2021-06-07 16:27:41','2021-06-12 14:20:08'),('Kuh-e Hambast C Section, Abadeh Area',4340,'Elika','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1.6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','11','Siliceous sponges','16','Keratose Sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3299,NULL,'Sponge microbial buildups. Coordinates stated in text',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,30.9,53.22,NULL,NULL,NULL,NULL,-1.53494397363,61.360873559,3.1374130146,60.3458109236,-2.15634,47.5684,'Krause','Krause','2021-06-12 07:59:25','2021-07-21 16:21:05'),('Shahreza section',4341,'Elika','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','20','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm wave base','11','Siliceous sponges','16','Keratose Sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3299,NULL,'Sponge-Microbial Mounds and Aragonite Crystal Fan or\r\nBundle Layers. Coordinates stated in text',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,32.12,51.95,NULL,NULL,NULL,NULL,0.191306743866,60.6312367216,4.7586553021,59.4034515753,-1.35907,45.8716,'Krause','Krause','2021-06-12 08:16:36','2021-07-21 16:21:05'),('Puerto Llano section',4342,'Sierra del Pozo, upper member','Cretaceous','Lower Cretaceous','Valanginian','Valanginian',132.90,139.80,23,'late Valanginian - early Aptian',126,135,'Early Cretaceous (Valanginian, 136.4 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','2','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','51',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3301,NULL,'Coral assemblage. Coordinates estimated from map',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,37.8527,-2.9123,NULL,'220703',NULL,NULL,19.5803245815,10.2811962583,25.2232214533,7.12396048471,29.5583,5.53286,'Krause','Krause','2021-06-13 15:20:40','2021-06-13 16:37:50'),('Kermanshah, Zagros',4343,'Taleh Zanggg','Paleogene','Paleocene','Danian','middle-late Paleocene',56.00,61.60,27,'Thanetian - Ypresian',53,55,'Paleocene/Eocene Boundary (PETM, 56 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','30','2','10 - 100 m wide',NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3302,NULL,'Coordinates estimated from map\r\nTotal thickness of massive limestone is 30 m. Individual reef bodies smaller.\r\nAbundant green algae in overyling facies.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,34.21,46.7,NULL,NULL,NULL,NULL,20.5428382257,41.5463509608,22.8402319195,41.2306754512,20.0629,39.7015,'Kiessling','Kiessling','2021-06-17 11:55:21','2022-04-21 09:46:51'),('Qincaiyuan, Gendan, Tanluzhai, Ziyun, Guizhou',4344,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','110.4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','16','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, bryozoans, and hydrozoans\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nreef dwellers:\r\nEchinoderms, ostracodes, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella.\r\nReef flat: algal-foraminiferal packstone with reef breccia.\r\nReef crest: ancient weathering crust.\r\nReef base: bioclastic packstone.\r\nBack-reef: bioclastic packstone with calcareous algae,gastropods, and foraminifers.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.75,106.1,NULL,NULL,NULL,NULL,-15.4084845079,105.577188696,6.92324909249,123.342542704,2.7186,98.3138,'Krause','Krause','2021-06-17 17:45:02','2021-06-20 13:22:33'),('Bure',4345,'Unknown','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',NULL,3,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','36',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3304,NULL,'Coral reef complex. Coordinates estimated from map.',NULL,NULL,NULL,NULL,'France','Europe',NULL,NULL,48.5052,5.3578,NULL,NULL,NULL,NULL,27.2592773102,23.3543700481,33.4141374892,24.052097908,39.396,14.5264,'Krause','Krause','2021-06-17 18:30:19','2021-07-21 16:21:05'),('Sirogojno Melange in the Zlatibor Mountain',4359,'Unknown','Triassic','Upper Triassic','Norian','Sevatian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','6','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','1','Corals','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species','43',NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',3305,NULL,'Dachstein Limestone forereef block is part of the upper carbonate-clastic Sirogojno Melange. The succession starts with coarse-grained rudstones followed\r\nby meter-sized reefal blocks intercalated in partly layered resedimented grainstones\r\nand packstones with abundant reef-building organisms like calcareous\r\nsponges, corals and encrusting organisms. Inside this part of the succession\r\nopen-marine influenced layers are rare. The succession continues with a partly\r\nturbiditic sequence and chaotic rudstones, densely packed with reef-derived\r\nmaterial like broken reef-building organisms and shallow-water material like\r\ngastropods, bivalves and foraminifers. Grainstones with clear open-marine influence\r\n(e.g., thin-shelled bivalves, crinoids, conodonts) appear in between those\r\nrudstones, in cases lumachelle layers consisting of halobiids were deposited. To\r\nthe end of the succession some layers show turbiditic bedding with mixed shallow-\r\nwater and deep-marine grains and organisms, i.e. filaments and crinoids.\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'Serbia','Europe',NULL,NULL,43.7045,19.8378,NULL,'221271',NULL,NULL,17.3096523934,31.2354195615,14.7727274521,27.42095775,22.1254,19.7781,'Krause','Krause','2021-07-21 16:21:02','2021-07-26 12:58:46'),('Tiechanghe, Tongjiang, Sichuan',4346,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','10',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers: Crinoids, brachiopods, gastropods, benthic foraminifera, and calcareous algae.\r\n\r\nRock type and reef-related depositional characteristic: Reef core: sponge framestone and bafflestone\r\nInter-reef: bioclastic packstone\r\nReef flat (reef crest): fine-crystalline dolostone containing bioclasts\r\nBack-reef: bioclastic wackestone to packstone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,32.38,107.11,NULL,'220875',NULL,NULL,-8.72119434334,105.453033395,13.5016225662,124.570860975,13.4063,94.0981,'Krause','Krause','2021-06-18 09:58:47','2021-06-22 16:27:05'),('Dapaichong, Guiyang, Hunan',4347,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'3','101-500 m thick','154.4',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nreef dwellers: Echinoderms, bivalves, ostracodes, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic: Reef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella.\r\nInter-reef: bioclastic lime dolostone.\r\nReef base: crinoidal packstone to grainstone.\r\nBack-reef: bioclastic dolomitic wackestone to packstone with calcareous algae, ostracodes, and foraminifers.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.75,112.82,NULL,'220876',NULL,NULL,-14.2891922765,111.730615578,6.72582742085,129.434565663,11.0318,102.231,'Krause','Krause','2021-06-18 10:40:12','2021-06-22 17:17:21'),('Xinwuchang, Guiyang, Hunan',4348,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','107',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sponges, sclerosponges, bryozoans, and hydrozoans.\r\nBinding organisms: Archaeolithoporella, Tubiphytes, Fenestella and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, bivalves, ostracodes, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic: \r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella.\r\nInter-reef: bioclastic lime dolostone.\r\nReef base: crinoidal packstone to grainstone.\r\nBack-reef: bioclastic dolomitic wackestone to packstone with calcareous algae, ostracodes, and foraminifers.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.65,112.48,NULL,NULL,NULL,NULL,-14.4545259647,111.44504726,6.63024632315,129.12468991,10.7681,102.043,'Krause','Krause','2021-06-18 11:07:34','2021-06-20 13:22:33'),('Gantian’ao, Luodian, Guizhou',4349,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','105.2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3300,NULL,'Reef builders: Frame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponge, bryozoan, and hydrozoan\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, ammonites, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic: Fore-reef slope:\r\nspiculitic-calcispherical cherty wackestone with reef breccias.\r\nReef core: framestone, bafflestone, and bindstone.\r\nReef flat (reef crest): packstone with reef breccia.\r\nReef base: echinodermal packstone to grainstone.\r\nBack-reef: bioclastic packstone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type: Metazoan reef at the shallow carbonate platform margin\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.54,106.91,NULL,NULL,NULL,NULL,-15.5059249541,106.358997932,6.67740351595,124.066568706,7.73067,97.9873,'Krause','Krause','2021-06-18 17:36:25','2021-06-20 13:22:33'),('Xikou, Zhenan, Shaanxi',4350,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','95.5',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, and bryozoans.\r\nBinding organisms: Tubiphytes, sclerosponge, and cyanobacteria\r\n\r\nReef dwellers: Echinoderms, ostracodes, bivalves, brachiopods, gastropods, bryozoans, benthic foraminifera, calcareous algae, and single rugose corals\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: less sponge framestone and more bafflestone and sponge-Tubiphytes-cyanobacteria bindstone.\r\nReef flat: bioclastic packstone with reef breccia.\r\nReef base: crinoidal packstone.\r\nReef crest: bioclastic wackestone and micritic limestone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,33.2419,109.376,NULL,NULL,NULL,NULL,-7.55378149464,107.20471821,14.2857181414,126.567030658,15.2291,95.1542,'Krause','Krause','2021-06-19 19:07:17','2021-06-20 10:08:56'),('Songshan, Wuxi, Jiangsu',4351,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','101',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, and bryozoans.\r\nBinding organisms: Tubiphytes, sclerosponge, and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and Waagenophyllum.\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: less sponge framestone and more bafflestone and sponge-Tubiphytes-cyanobacteria bindstone.\r\nReef flat: bioclastic packstone with reef breccia.\r\nReef base: crinoidal packstone.\r\nReef crest: bioclastic wackestone and micritic limestone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform nearby platform margin.\r\n\r\nCoordinates stated in text. ',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.6,120.47,NULL,NULL,NULL,NULL,2.61486608713,114.878710357,25.736273826,105.750920815,19.7833,103.903,'Krause','Krause','2021-06-19 19:22:19','2021-06-20 10:08:29'),('Yanggudong, Xuanhan, Sichuan',4352,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','41.7',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3300,NULL,'Reef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, and bryozoans.\r\nBinding organisms: Tubiphytes, sclerosponge, Fenestella, Diplotrypa and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, ostracodes, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: less sponge framestone and more bafflestone and sponge-Tubiphytes-cyanobacteria bindstone.\r\nReef flat: bioclastic packstone with reef breccia.\r\nReef base: crinoidal packstone.\r\nReef crest: bioclastic wackestone to packstone with calcareous algae, gastropods, and foraminifers.\r\nReef base: crinoidal packstone\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.7167,108.3334,NULL,NULL,NULL,NULL,-9.20865837492,106.59731832,12.7939762481,125.605176624,13.48,95.3614,'Krause','Krause','2021-06-19 19:30:31','2021-06-20 10:07:39'),('Honghua, (MC2 well), Kaixian, Chongqing',4353,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','90',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','12',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3300,NULL,'Reef builders:  Baffling organisms: hypercalcified sphinctozoan and inozoan sponges.\r\nBinding organisms: Tubiphytes and cyanobacteria.\r\n\r\nReef dwellers: Echinoderms, brachiopods, gastropods, benthic foraminifera, and calcareous. algae.\r\n\r\nRock type and reef-related depositional characteristic: Reef core: sponge bafflestone and\r\nsponge-Tubiphytes-cyanobacteria bindstone.\r\nReef flat: bioclastic algae-crinoid packstone with reef breccia.\r\nReef crest: crinoidal-algal-foraminiferal wackestone to packstone and micritic dolostone.\r\nReef base: bioclastic packstone.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.53,108.48,NULL,NULL,NULL,NULL,-9.37154575493,106.753994065,12.6025113462,125.725512632,13.4031,95.5784,'Krause','Krause','2021-06-19 20:48:03','2021-06-20 16:02:45'),('Qujiawan, Chenxi, Hunan',4354,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','53.6',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','1','Corals','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3300,NULL,'Reef builders: Frame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges and Waagenophyllum. Binding organisms:\r\nArchaeolithoporella, Tubiphytes, and cyanobacteria\r\n\r\nReef dwellers: Crinoids, ostracodes,brachiopods,  gastropods, benthic foraminifera, and calcareous algae.\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: more sponge bafflestone and less sponge framestone with the encrusting Archaeolithoporella\r\nReef flat: dolomitic bioclastic packstone with crinoids and reef breccia.\r\nReef crest: dolomitic crinoidal-algal-foraminiferal wackestone.\r\nReef base: dolomitic packstone with the clasts of brachiopods, gastropods, and crinoids.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform nearby platform margin\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,28,110.18,NULL,NULL,NULL,NULL,-12.5765883348,108.882467629,9.02477838345,127.105648919,11.4317,98.936,'Krause','Krause','2021-06-19 22:06:20','2021-06-20 10:05:42');
