INSERT INTO `reefs` VALUES ('Daoshiyan, Chenxi, Hunan',4355,'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','48',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','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, and Waagenophyllun.\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers:\r\nCrinoids, bryozoans 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\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,28.07,110.22,NULL,NULL,NULL,NULL,-12.5011177447,108.904216855,9.09374124637,127.14341162,11.509,98.9226,'Krause','Krause','2021-06-20 09:49:05','2021-06-20 10:05:22'),('Xiaoquan, Yizhang, Hunan',4356,'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','44.2',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','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:Frame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, and rugose coral.\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers: Crinoids, bryozoans, ostracodes, brachiopods, gastropods, benthic foraminifera, and calcareous algae.\r\n\r\nRock type and reef-related depositional characteristic: Reef core: more sponge bafflestone.\r\nand less sponge framestone with the encrusting Archaeolithoporella.\r\nReef flat: dolomitic bioclastic packstone with crinoids and reef breccia.\r\nReef crest: dolomitic crinoidal 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\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.31,112.82,NULL,NULL,NULL,NULL,-14.7180697747,111.832157941,6.28586699337,129.428626362,10.6799,102.5,'Krause','Krause','2021-06-20 10:03:43','2021-06-20 10:04:14'),('FS1, Liangping, Chongqing',4357,'Changxing','Permian','Lopingian','Changhsingian','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,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',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,'2','30-60% micrite',NULL,NULL,NULL,NULL,'2','Intense',2,'Actual reservoir',3303,NULL,'Reef limestone and reef dolomite: Only developed \r\nin the Changxing Formation, the reef building organisms  are mainly sponges, while foraminiferas, brachiopods, and  other accessory organisms can also be seen. The content of sponges in the framework reef limestone is the highest, and  some of the sponges have been dolomitized, meaning the sponge frameworks are filled with dolomite.\r\n\r\nCoordinates estimated from map.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,30.6053,107.94,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-06-20 13:22:30','2021-06-20 16:02:06'),('well F1, FT1, Fengjie, Chongqing',4358,'Changxing, Chang 2 Member','Permian','Lopingian','Changhsingian','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,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',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,'2','30-60% micrite',NULL,NULL,NULL,NULL,'2','Intense',1,'Potential reservoir',3303,NULL,'Reef limestone and reef dolomite: Only developed\r\nin the Changxing Formation, the reef building organisms are mainly sponges, while foraminiferas, brachiopods, and other accessory organisms can also be seen. The content of sponges in the framework reef limestone is the highest, and some of the sponges have been dolomitized, meaning the sponge frameworks are filled with dolomite.\r\n\r\nCoordinates estimated from map.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,31.2913,109.2405,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2021-06-20 13:53:03','2021-06-20 16:02:19'),('Araetgol section, Yeongwol',4360,'Mungok','Ordovician','Lower Ordovician','Tremadocian','Tremadocian',477.70,485.40,3,'Franconian - Tremadocian',488,480,'Early Ordovician (Tremadoc, 481.6 Ma)',NULL,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','1','1','Less than 10 m wide','1','1','Less than 20 m','1',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','16','Keratose Sponges','3','Microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','2','3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3307,NULL,'The thrombolitic mounds are domes up to 100 cm high and 40–60 cm wide embedded within within lime mud and shale (ribbon rock). Analysis of slabs revealed that the mounds consist of cm-scale thrombolitic “clots” and homogeneous micrite with several intraclasts and bioclasts filling the interclot spaces.\r\nTwo types of clots are recognised: keratolite–microbialite and lithistid sponge–microstromatolite clots. Keratose and lithistid sponges rarely occur together in the Mungok reefs.',NULL,NULL,NULL,NULL,'South Korea','Asia',NULL,NULL,37.284,128.43,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2021-07-26 12:58:43','2021-07-26 12:58:47'),('Cortes section',4361,'Unknown','Devonian','Middle Devonian','Eifelian','late Eifelian-Givetian',382.70,393.30,9,'late Pragian - Eifelian',395,390,'Middle Devonian (Eifelian, 390.5 Ma)',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','3b','Deeper slope or outer ramp',NULL,NULL,'13','Echinoderms','1','Corals','55','Tabulate/rugose corals - crinoids - (microbes inferred)',NULL,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,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3308,NULL,'Well-developed reef system, with significant diversity of reefal faunas (crinoids, corals and stromatoporoids). The calciturbidites include frequent fragments of crinoids and common coarse-\r\ngrained calciturbidites. Base of the slope.\r\n\r\nCoordinates estimated from map.',NULL,NULL,NULL,NULL,'Portugal','Europe',NULL,NULL,38.194,-8.08,NULL,NULL,NULL,NULL,-31.8292095473,-6.52160034534,-4.06209759556,-36.0081584502,-40.4652,20.6936,'Krause','Krause','2021-07-28 11:34:27','2021-07-28 11:38:58'),('Auerstedt section, German Basin',4362,'Diemel','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','0.05','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin',NULL,NULL,'16','Keratose Sponges','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3311,NULL,'Microbe-metazoan build-ups. The biocrusts at\r\nthe top of the build-ups consist of encrusting Pla-\r\ncunopsis bivalves and microconchids. Subtidal\r\nshallow marine environment. Coordinates estimated from map.',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,51.0975,11.5872,NULL,NULL,NULL,NULL,30.0937217312,29.7097237517,24.1833172497,24.4721790222,17.2847,19.8937,'Krause','Krause','2021-08-19 17:05:33','2021-08-19 17:33:51'),('Mauer, German Basin',4363,'Diemel','Triassic','Middle Triassic','Anisian','late 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','1','Less than 10 m thick','0.08','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','16','Keratose Sponges','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3311,NULL,'Microbe-metazoan build-ups ',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,49.3419,8.7992,NULL,NULL,NULL,NULL,27.9661135892,28.2026668292,21.7428340129,23.8706054571,14.9691,18.9056,'Krause','Krause','2021-08-19 17:33:48','2021-08-19 17:34:25'),('Seyweiler',4364,'Diemel','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','0.08','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','1','Above fair weather wave base','16','Keratose Sponges','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3311,NULL,'Microbe-metazoan build-up from is mainly composed of silicied carbonate. Fossils include bivalves and\r\nsponges. ',NULL,NULL,NULL,NULL,'Germany','Europe',NULL,NULL,49.161,7.2682,NULL,NULL,NULL,NULL,27.5707482979,27.1454614292,21.0692097501,23.0542801164,14.4305,18.0155,'Krause','Krause','2021-08-19 17:52:46','2021-08-19 17:53:18'),('Libiąż, close to the Silesian–Moravian Gate',4365,'Diplopora Beds','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','0.4','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','1','Above fair weather wave base','16','Keratose Sponges','3','Microbes','42','Microbes - siliceous sponges - (bryozoans) - corals',NULL,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','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3311,NULL,'Microbe-metazoan build-ups, composed of\r\ncalcite, characterized by planar and sometimes\r\ndomal laminations. Stromatolite-bearing intervals occur in the upper part of the Diplopora Bed. Sponges are abundant and can be clearly rec-\r\nognized based on distinctive features such as\r\nmesh-like fabrics.',NULL,NULL,NULL,NULL,'Poland','Europe',NULL,NULL,50.1123,19.3268,NULL,NULL,NULL,NULL,30.4961164605,35.4909326295,26.2392181704,29.5194923515,18.5809,24.9777,'Krause','Krause','2021-08-23 14:37:13','2021-08-27 15:46:15'),('Zakupne, Demkivtsi, Lysohirka (Medobory Hills)',4366,'Ternopil Beds','Neogene','Miocene','Middle Miocene','upper Badenian',13.80,16.00,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'2','Algae','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',3312,NULL,'Biohermal (reefal) limestone. Coralgal reefs.',NULL,NULL,NULL,NULL,'Ukraine','Europe',NULL,NULL,49.1174,26.3361,NULL,'70569',NULL,NULL,48.4551115075,22.8579965192,48.0659131724,25.9895344463,49.5002,25.4964,'Krause','Krause','2021-08-27 15:46:11','2021-10-27 13:57:55'),('core XK-1, Xisha carbonate platform on Shidao Island',4367,'Huangliu','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 ',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','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,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reef.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,17.9873429721,111.300003983,16.333711529,111.4803614,16.7664,111.648,'Krause','Krause','2021-10-27 13:57:52','2021-10-28 18:27:52'),('core XK-1, Xisha carbonate platform on Shidao Island',4368,'Huangliu','Neogene','Miocene','Upper Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',NULL,2,'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','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,'1','Less than 6 reef building species','3',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reefs.\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,17.6049442161,111.653959042,16.5022223387,111.769900762,16.7566,112.125,'Krause','Krause','2021-10-27 14:14:24','2021-10-28 18:28:16'),('core XK-1, Xisha carbonate platform on Shidao Island',4369,'Meishan','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 ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reefs.\r\n\r\nCoordinated stated in text. ',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,17.9873429721,111.300003983,16.333711529,111.4803614,16.7664,111.648,'Krause','Krause','2021-10-27 14:34:37','2021-10-28 18:28:32'),('core XK-1, Xisha carbonate platform on Shidao Island',4370,'Meishan','Neogene','Miocene','Upper Miocene','Messinian',5.30,7.30,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',NULL,2,'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','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reefs.\r\n\r\nCoordinates stated in text. ',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,17.6049442161,111.653959042,16.5022223387,111.769900762,16.7566,112.125,'Krause','Krause','2021-10-28 16:56:59','2021-10-28 18:28:49'),('core XK-1, Xisha carbonate platform on Shidao Island',4371,'Meishan','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','3','101-500 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reefs in shallow-sea shoal. \r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,18.28723206,110.861983659,16.1863375078,111.170163925,16.7664,111.648,'Krause','Krause','2021-10-28 17:05:04','2021-10-28 18:29:05'),('core XK-1, Xisha carbonate platform on Shidao Island',4372,'Meishan','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','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','1a','Shallow intra-platform','2','Below fair weather wave base','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Biogenic reefs.\r\n\r\nCoordinates stated in text.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,18.4810051212,110.540887132,16.0946216046,110.946051079,16.9125,112.172,'Krause','Krause','2021-10-28 18:27:02','2021-10-28 18:29:20'),('core XK-1, Xisha carbonate platform on Shidao Island',4373,'Sanya','Neogene','Miocene','Lower Miocene','Burdigalian',16.00,20.40,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','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','3','Below storm wave base','1','Corals',NULL,NULL,'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,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',3313,NULL,'Thick dolomitic reef with some bioclastic limestone in the upper part, alternating reefal and bioclastic limestone in the middle, and brownish breccia and coral reefs in the bottom.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,18.7720917869,110.053978895,15.9586122019,110.608439904,17.0969,112.689,'Krause','Krause','2021-11-09 16:05:11','2021-11-10 12:00:22'),('core XK-1, Xisha carbonate platform on Shidao Island',4374,'Sanya','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,1,'1','Seismic data available ',1,'True reef','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','1d','Marginal marine - coastal -  siliciclastic shelf','2','Below 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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3313,NULL,'Thick dolomitic reef with some bioclastic limestone in the upper part, alternating reefal and bioclastic limestone in the middle, and brownish breccia and coral reefs in the bottom.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,16.8458,112.3472,NULL,NULL,NULL,NULL,19.093648234,109.727873512,15.895462965,110.415585944,17.0969,112.689,'Krause','Krause','2021-11-09 16:18:17','2021-11-10 12:00:05'),('Jebel Serdj-Bargou',4375,'Lower Serdj','Cretaceous','Lower Cretaceous','Aptian','upper Aptian',113.00,125.00,24,'late Aptian - middle Cenomanian',107,115,'Early Cretaceous (late Aptian, 115.8 Ma)',NULL,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,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','1','Corals','5','Rudists','65','Corals - spongiomorphids - oysters - serpulids',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,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3314,NULL,'high carbonate productivity with the development of biostromal buildups. The carbonates of this unit show net northward facies and thickness changes. The biota is dominated by corals, orbitolinids,\r\nmiliolids, gastropods and oysters, reflecting the oligophotic conditions on a homoclinal carbonate ramp.',NULL,NULL,NULL,NULL,'Tunisia','Africa',NULL,NULL,36.0833,9.5666,NULL,NULL,NULL,NULL,16.7914731035,18.0610326422,19.9720978007,13.1240956947,19.9274,13.1032,'Krause','Krause','2021-11-10 14:21:47','2021-12-26 22:09:49'),('Cruz',4376,'Higueruelas','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 ',3,'Mud mound or bank','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','1d','Marginal marine - coastal -  siliciclastic shelf','3','Below storm wave base','1','Corals','12','Foraminifera','41','Corals - bryozoans - (algae) - (bivalves)',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',NULL,NULL,'0','',0,'No or unknown reservoir potential',3319,NULL,'Biohermes of different thickness (decimetric to metric) and less lateral continuity are developped, highly colonized by corals, that are associated to oncolitic, bioclastic and oolitic of high energy\r\nfacies, in marginal areas, near the litoral developpment.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,41.3359,-0.8621,NULL,NULL,NULL,NULL,19.4880687057,15.1584554355,25.6092036526,12.4794970106,32.483,8.65899,'Krause','Krause','2021-12-26 22:09:46','2021-12-26 22:10:38'),('Jaulin',4377,'Higueruelas','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 ',3,'Mud mound or bank','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','1d','Marginal marine - coastal -  siliciclastic shelf','3','Below storm wave base','1','Corals','2','Algae','41','Corals - bryozoans - (algae) - (bivalves)','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','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3319,NULL,'Within the inner shelf, in agitated subtidal conditions close to the coastal oolitic\r\ndevelopment, coral bioherms (boundstone corals) grow\r\n(coral boundstone) associated with bio-clastic, oolitic and oncolitic high energy facies.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,41.4559,-0.9908,NULL,NULL,NULL,NULL,19.6382626839,15.1222669967,25.7629492707,12.4693703515,32.6346,8.62722,'Krause','Krause','2022-01-04 19:57:25','2022-01-11 13:29:31'),('Anjiazhuang near Feicheng, Shandong',4378,'Zhangxia','Cambrian','Series 3','Drumian','Amgan',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,'3','101-500 m thick','110','3','101-1000 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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',3320,NULL,'Age should be Drumian, which is not yet in the pulldown menu.\r\nSeveral calcimicrobes identified: Epiphyton, Bacinella, Hedstroemia, Girvanella, Renalcis.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.99,116.77,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,-1.2566,147.887,'Kiessling','Krause','2022-01-11 13:29:28','2022-06-28 17:10:20'),('Qujing',4379,'unknown','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 ',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','',0,'No or unknown reservoir potential',3324,NULL,'No comment',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.4513,103.816,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-03-23 16:40:10','2023-03-17 17:45:34'),('Muli reef,  Wenshan-southeast Yunnan',4380,'unknown','Devonian','Lower Devonian',NULL,'Lower Devonian',393.30,419.20,8,'middle Pridolian - middle Pragian',412,400,'Early Devonian (Emsian, 400 Ma)',NULL,1,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,'1','Less than 10 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,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3324,NULL,'Sb-ore deposits',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,23.9887,105.3675,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-03-23 17:22:41','2023-03-17 17:45:34'),('Dongwan section',4383,'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 ',1,'True reef','1','Less than 10 m thick','2.5','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','16','Keratose Sponges','3','Microbes','42','Microbes - siliceous sponges - (bryozoans) - corals','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','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3329,NULL,'Microbialite (2.5 m thick) is composed mainly of dendrolite. The basal layer of the microbialite is flat and layered, and its upper part is strongly domed. Shell beds are intercalated between domes. At the top, the dome-shaped microbialite flattens horizontally, and is overlain by muddy limestone. Conodont H. parvus was found in the horizon 0.45 m above the bottom of the microbialite.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,30.47,106.94,NULL,NULL,NULL,NULL,-9.76046411997,106.401097517,13.9975485319,123.350185971,11.7706,95.1194,'Krause','Krause','2022-04-06 16:11:09','2022-04-06 16:17:09'),('Mesa de Roldán + La Molata de las Negras',4381,'unknown','Neogene','Miocene','Upper Miocene','upper Messinian',5.30,6.00,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 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','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3322,NULL,'The reef unit onlaps the erosion surface and consists of small Porites patches that grew dispersed in oolitic shoals together with microbial carbonates. These low-diversity reefs are the last zooxanthellate coral reefs in the Mediterranean basin and constitute the endpoint of decreasing coral diversity in the region during the Miocene due to disconnection from the Indian Ocean and global cooling.',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,36.95,-1.8667,NULL,'224629',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-03-24 15:03:36','2022-03-24 15:47:02'),('Djebel Ouarkziz',4382,'Djebel Ouarkziz','Carboniferous','Pennsylvanian','Bashkirian','Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,340,'Middle Mississippian (Early Visean, 338.8Ma)',NULL,3,'0','Outcropping reef ',4,'True reef','1','Less than 10 m thick','4.5','2','10 - 100 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','1','Corals',NULL,'Brachiopods','2','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','25 or more reef building species','14',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3327,NULL,'Biostrome in shallow-water platform. A diverse set of microfacies have been observed in thin sections. The most abundant one is rudstone; bindstone and packstone are also common. More rarely, grainstone occur, mainly in the upper part of the bed. The identified components are the same as those occurring as macrofauna, plus foraminifers, calcareous algae, ostracods and scarce fragments of molluscs. Frequently, there is recorded the intergrowth of gigantoproductid brachiopods, rugose corals and chaetetid sponges.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,28.21,-9.29,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Siphonodendron','2022-03-28 17:49:17','2022-04-06 16:11:13'),('Xiushui section, SW of Dongling village near Sidu',4384,'Daye','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','2.5','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','16','Keratose Sponges','3','Microbes','42','Microbes - siliceous sponges - (bryozoans) - corals',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,'0','',0,'No or unknown reservoir potential',3329,NULL,'Microbialite consists of a lower thrombolite (1.5 m thick) and an upper dendrolite (0.5 m thick). Hindeodus parvus conodont is present. the putative keratose sponge consortia were identified\r\nfrom a thin-bedded, spar-cemented oolitic limestone below the basal microbialite unit. It overlies unconformably above the uppermost Changhsingian bioclastic limestone. Above this oolitic limestone layer, the thrombolite is characterized by a clotted texture of reddish sparitic patches embedded in a grey micritic matrix, whereas the overlying dendrolite texture consists of brownish sparitic patches embedded within a yellow micritic matrix (weathering colour). Several shell layers containing microgastropod and bivalve fragments, ostracod tests, and intraclasts occur above the microbialite unit (Fig. 2). Above these shell layers is the succession dominated by micrites interbedded with peloidal wackestones. In the oolitic limestone layer, single ooids are 0.2–0.6 mm in diameter and round to oval in outline, occupying 55–65% of entire petrologic texture, and they are unevenly distributed. These ooids are strongly micritized so that concentric lines or radial structures become vague. Some grains retain outline of bioclast remains, mostly gastropods. The pores between the ooids are normally cemented by sparites and micritic clumps (micrite aggregates) are interspersed occasionally, indicating an intermittent high-energy environment. Light-coloured sparitic structures are rather common and evenly scattered and almost fill the dark-coloured micritic clumps. Some elongated individuals show vermiform shapes, while others are filamentous and branch occasionally. These dot-shaped and filamentous structures form maze-like networks. Single filaments vary in length, ranging from 100 to 500 μm, while their thicknesses are relatively consistent, except for tapering ends. Individual filaments are 10–70 μm (averagely 33 μm) in diameter, with filaments of 20–30 μm in diameter being most frequently occurring (nearly 20%). About 60% filaments are 20–40 μm in diameter. Filament is slightly inflated at the junction when branching, and these filamentous sparitic structures tend to be distributed parallel to the edge of the micritic clumps.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,29.05,114.58,NULL,NULL,NULL,NULL,-9.97012425281,113.280880362,11.9108230644,129.971413686,14.6023,101.449,'Krause','Krause','2022-04-06 17:54:58','2022-04-07 11:17:39'),('Xiushui section, SW of Dongling village near Sidu',4385,'Changxing','Permian','Lopingian','Changhsingian','lower Changhsingian',253.00,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',NULL,3,'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,'6','Calcisponges','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,NULL,NULL,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',3329,NULL,'Massive reefal carbonates with framestone of\r\nreef-core facies built by calcareous sponges. The matrix of the framestone is micritic, indicating that the wave energy on the reef was not strong.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,29.05,114.58,NULL,NULL,NULL,NULL,-11.0743209366,112.137089694,9.13938248376,131.605562272,14.6023,101.449,'Krause','Krause','2022-04-07 09:49:40','2022-04-07 18:33:30'),('Santa Cesarea Terme',4386,'Torre Specchialaguardia Limestone','Paleogene','Eocene','Priabonian','Priabonian',33.90,38.00,29,'Priabonian - Rupelian',33,35,'Late Eocene (Priabonian, 35.9 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','72',NULL,NULL,NULL,NULL,NULL,'1000','1',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp',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','24',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',3331,NULL,'Coral fauna is moderately diversified (only 14 genera) associated with coralline algae and larger foraminifers (mainly dyscocyclinids). Tue sequence is represented by three main fades (from the bottom upwards): \r\n1 - Grainstone-packstone facies (ca. 15 m thick) rich in discocyclinids, nummulitids, scleractinian corals, and bryozoans. Large subglobose coral colonies (Actinacis, Antiguastrea, Astrocoenia, Favites and Agathiphyllia) and sublaminar and globose colonies of bryozoans are typically in life position. The displaced colonies are rare and typically bear no evidence of transport (bush-like colonies of e.g.,Actinacis seem to be only fallen down). Generally colonies preserved in situ are immersed in a bioclastic packstone that, with a sharp contact, passes to a grainstone wich disoriented discocyclinids. At the top of this fades present are also debris ßows with branching corals like Acropora, Stylophora and other large bioclasts. Abundant coralline algae and specimens of pectinids and other molluscs are also associated with this facies.\r\n2 - Bioclastic limestone (rudstones and/or floatsrones) facies (ca. 4S m thick) rich in scleractinians and coraline algae. \r\n3 - Wackestone-mudstone facies (ca. 12 m chick) with planktonic foraminifers, in which are debris-flows composed mainly of larger foraminifers and broken coral colonies.',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,40.05,18.475,NULL,'224871',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-04-07 18:33:27','2022-04-20 16:33:20'),('Line M1507-07',4387,'unknown','Neogene','Miocene','Middle Miocene','mid-Miocene',11.60,13.80,31,'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,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','4a','Shallow basin','1','Above fair weather wave base','2','Algae',NULL,NULL,'88','Green algae - phylloid algae - calcisponges - (corals)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3332,NULL,'Biogenetic reefs. The carbonates of biogenic reefs in the Andaman Sea are widely distributed, among which the carbonate platforms in the eastern terraces are mostly developed in fault blocks and volcanoes. The eastern terrace carbonate platform is mostly developed on the fault block and volcanic uplift, and the fault activity on the edge of the platform.',NULL,NULL,NULL,NULL,'Andaman Sea','Indian Ocean',NULL,NULL,11.8,96.5,NULL,NULL,NULL,NULL,13.1129929493,95.0130942229,11.0221883362,95.4699333308,9.80521,97.6727,'Krause','Krause','2022-04-20 16:33:17','2022-04-21 11:39:00'),('Line M1507-20',4388,'unknown','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'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,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','4a','Shallow basin','1','Above fair weather wave base','2','Algae',NULL,NULL,NULL,NULL,'2',NULL,NULL,NULL,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',3332,NULL,'Biogenic reef carbonates ',NULL,NULL,NULL,NULL,'Andaman Sea','Indian Ocean',NULL,NULL,12.17,96.86,NULL,NULL,NULL,NULL,13.5625545145,95.1658013228,11.3346244932,95.6782853535,10.2112,97.9875,'Krause','Krause','2022-04-21 09:42:30','2022-04-21 11:39:35'),('Line M1507-03',4389,'unknown','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'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,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'40',NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','1','Above fair weather wave base','2','Algae',NULL,NULL,NULL,NULL,'2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3332,NULL,'Biogenic reef carbonates',NULL,NULL,NULL,NULL,'Andaman Sea','Indian Ocean',NULL,NULL,12.5,96.86,NULL,NULL,NULL,NULL,13.8925444663,95.1631503848,11.6646241986,95.6778353509,10.5392,97.9511,'Krause','Krause','2022-04-21 11:32:45','2022-04-21 11:40:02'),('Wadi Araba',4390,'Rod El-Hamal Formation','Carboniferous','Pennsylvanian','Moscovian','upper Moscovian',311.00,315.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','8','1','Less than 10 m wide',NULL,'2','10 - 100 m','42',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','2','Algae','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','2',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','1','Less than 10% sparite',NULL,NULL,'1','Present',0,'No or unknown reservoir potential',3333,NULL,'Mounds formed by filamentous microbes and phylloid algae. Phylloid algae are loosely accumulated and supported by micritic encrustations that were formed by filamentous microbes. The filamentous microbes growing perpendicularly to the phylloid algal surfaces produced concentrated areas of peloids-A. The spaces between the phylloid algal-microbial frameworks were filled with concentrated areas of peloids-B (peloid-B aggregations) oriented perpendicular to the phylloid algae surfaces.',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,29.1,32.28,NULL,NULL,NULL,NULL,-37.0445649148,29.3327691729,-35.5300533051,7.08352528472,-34.2506,30.0846,'Krause','Krause','2022-06-20 15:43:27','2022-06-20 17:31:54'),('Ruby Creek- Bornite deposit, Brooks Range',4391,'unknown','Silurian','Pridoli','Pridoli','Ludlow-Gedinnian',410.80,427.40,NULL,NULL,NULL,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',417,1,'0','Outcropping reef ',NULL,NULL,'4','More than 500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'3','Microbes','2','Algae',NULL,NULL,NULL,NULL,NULL,NULL,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',1,'Potential reservoir',3334,NULL,'Stratigraphy uncertain.\r\nAge given as Wenlock-Lower Devonian',NULL,NULL,NULL,NULL,'United States','North America',101,NULL,67.06306,-156.9469,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-06-20 17:31:50','2022-06-23 15:16:39'),('Test 4',4417,'Test 4','Jurassic','Upper Jurassic','Oxfordian','upper 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,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',3356,NULL,'Test 4',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,44.55,55.44,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2023-04-04 15:50:09',NULL),('Arroyo Uitpa, Arroyo Ekieps at the foothills of the Serranía de Jarara in the Cocinetas Basin',4392,'Siamaná','Neogene','Miocene','Lower Miocene','Aquitanian',20.40,23.00,30,'Chattian - Aquitanian',22,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','7','Bryozoans','41','Corals - bryozoans - (algae) - (bivalves)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','24',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3335,NULL,'The Arroyo Uitpa paleoenvironment is characterized by patch reefs developed in a shallow lagoon close to the shore-line, while Arroyo Ekieps was a barrier reef system, which offered a wide variety of microhabitats enhanced by the structural complexity of the reef framework. This suggests an increase of bryozoan diversity with higher reef complexity.',NULL,NULL,NULL,NULL,'Colombia','South America',NULL,NULL,12.04,-71.26,NULL,'201392',NULL,NULL,7.51495175157,-69.6046432843,10.7106751354,-68.8258607723,11.1348,-67.6034,'Krause','Krause','2022-06-23 15:16:35','2022-06-23 15:27:49'),('Chenluzhen',4393,'Pingliang Formation','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','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,'15','Non-rudist bivalves','16','Keratose Sponges',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,'2','30-60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3337,NULL,'Age is roughly identified. Maybe Sandbian?',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.035833,109.170833,NULL,NULL,NULL,NULL,34.8598972721,92.2435657323,34.8598972721,92.2435657323,-25.2687,122.525,'J.-H.Lee','Krause','2022-06-28 19:22:49','2022-06-29 17:08:18'),('Beiquanzi',4394,'Zhangxia Formation','Cambrian','Series 3',NULL,'Middle Cambrian',497.00,509.00,2,'Middle Cambrian - Dresbachian',502,510,'early Middle Cambrian (late Epoch 2, 510 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','0.3','1','Less than 10 m wide','1.5','1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3338,NULL,'Occurs as patches within Epiphyton-dominant microbial reefs that are >10 m large',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,36.479722,116.924444,NULL,NULL,NULL,NULL,23.9854140172,98.6788601127,23.9854140172,98.6788601127,-0.871239,147.56,'J.-H.Lee','Krause','2022-06-28 21:13:44','2022-07-19 18:20:57'),('Zargar area, Section A',4395,'Lut platform','Paleogene','Eocene','Ypresian','Ypresian',47.80,56.00,27,'Thanetian - Ypresian',53,50,'Early Eocene (Ypresian, 51.9 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'2','10 - 100 m','15','30',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','12','Foraminifera','20','Corals - forams','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','15',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',3339,NULL,'The sedimentary succession consists of two informal units: the conglomerate unit and calcareous unit (Lower and Upper Units).The conglomerate unit is composed with subangular to rounded pebbles of foraminiferal limestone and red chert. A large number of mollusk fragments, mainly gastropods and bivalves were identified. The calcareous unit is composed of thick limestones (wackestone) bearing foraminifera occurring in the lower one-third part of the unit which passes upward into thick gray limestone containing foraminiferal fauna alveolinids and orbitolitids and continues with very thick coral limestones in the middle part of this unit. The upper one-third of the calcareous unit is composed of well-bedded bioclastic gray to yellow wackestone and biomicrosparite which is characterized by the presence of coralline red algae, Nummulites globulus Leymerie and rare miliolids. It continues with gray micritic limestone (packstone to grainstone) defined by the presence of disc-shaped orthophragminids.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,32.7222,59.2417,NULL,NULL,NULL,NULL,33.0211035139,54.382543926,32.5111702882,58.1888560669,8.84273,57.4834,'Krause','Krause','2022-07-19 17:38:47','2022-07-21 18:07:01'),('Kaboudeh area, section B',4396,'Lut platform','Paleogene','Eocene','Ypresian','Ypresian',47.80,56.00,27,'Thanetian - Ypresian',53,50,'Early Eocene (Ypresian, 51.9 Ma)',NULL,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'40','2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','12','Foraminifera','20','Corals - forams','1',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',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3339,NULL,'Coral dominated macrofacies consting of two units - conglomerate and calcareous units. The conglomerate unit contains with various rock fragments such as cherts, basalt and fossiliferous limestone bearing small Nummulites. It is followed by medium grain sandstone including chert fragments and terrigenous detritus (quartz, feldspar and mica). The lower part of calcareous unit contains the small benthic miliolid foraminifera in a micritic matrix. The middle part consists of a succession of thick bedded and massive reefal limestones (boundstone) containing an autochthonous facies. Other components include encrusting\r\ncoralline red algae and common small Nummulites, frequent rotaliids and miliolids. This part is formed by thick bedswith wavy bedding plans and is characterized by red coralline algal bindstone. It passes upward into upper part of calcareous unit composed of bedded limestone bearing larger foraminifera.',NULL,NULL,NULL,NULL,'Iran','Asia',NULL,NULL,32.4792,59.5736,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2022-07-20 16:41:09','2022-07-21 18:07:01'),('Hole 966F',4397,'Unknown','Neogene','Miocene','Upper Miocene','Upper Miocene',5.30,11.60,32,'Tortonian - Gelasian',6,5,'latest Miocene (Messinian, 6.3 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'2','10 - 100 m','30.5',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,'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',3340,NULL,'Coral reef facies near its base and lagoonal facies toward its top. The succession was deposited in an oligotrophic environment and exhibits a general shallowing-upward trend',NULL,NULL,NULL,NULL,'Cyprus','Europe',NULL,NULL,32.6833,33.8167,NULL,NULL,NULL,NULL,31.7196757598,32.2825299183,31.2010117377,33.3728561915,32.4475,33.5491,'Krause','Krause','2022-07-21 18:06:57','2022-07-21 18:07:26'),('Zhongxinzhai section',4398,'Weining','Carboniferous','Pennsylvanian','Kasimovian','Kasimovian',303.70,307.00,13,'Bashkirian - Kasimovian',302,315,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',NULL,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','45','3','101-1000 m wide',NULL,'3','More than 100 m','200',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','3','Below storm wave base','3','Microbes','1','Corals','61','Microbes (thrombolites) - algae - corals','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'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',3344,NULL,'The Zhongxinzhai section (25° 30′ 33.5″ N, 106° 12′\r\n08.0″ E), s 78 m thick with a skeletal–cement–microbial reef (SCMR-3, bed 4) in the upper part.\r\nmicrobial–phylloid algal reef at the base\r\nCement-rich microbial carbonates and colonial\r\nrugose corals (Ivanovia) are the main reef builders in the lower middle part\r\nThe upper part of the reef is mainly constructed by small scale cement-rich microbial boundstone, including phylloid algae, bryozoans, calcisponges, and tube-shape algae',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.509306,106.202222,NULL,'206265',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Kiessling','2022-11-14 01:52:45','2023-01-04 15:04:29'),('Tabaïnout section TB2',4399,'Tizra','Carboniferous','Mississippian','Visean','Brigantian',331.00,336.00,12,'middle Visean - Serpukhovian',329,340,'Middle Mississippian (Early Visean, 338.8Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','100','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','2','Below fair weather wave base','3','Microbes',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,'1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3345,NULL,'very thick massive microbial limestones accumulated',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,32.9,-5.8,NULL,NULL,NULL,NULL,-38.3855470246,-14.6666614345,-23.7253573021,-26.7389283513,-21.0167,-4.2806,'Krause','Krause','2023-01-04 15:04:25','2023-01-04 23:04:31'),(' Tiaouinine outcrop (Bou Guergour)',4400,'Tizra','Carboniferous','Mississippian','Serpukhovian','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','50','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','1','Corals',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,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',3345,NULL,'thicker basal siliciclastic/bioclastic unit',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,32.65,-5.37,NULL,NULL,NULL,NULL,-32.3295612353,-10.4146442101,-24.3458525862,-22.3833899954,-16.7938,-2.08022,'Krause','Krause','2023-01-04 16:34:53','2023-01-04 23:05:22'),('Souk el Had',4401,'Tizra','Carboniferous','Mississippian','Visean','Asbian',336.00,340.00,12,'middle Visean - Serpukhovian',329,340,'Middle Mississippian (Early Visean, 338.8Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'2','Below fair weather wave base','1','Corals','1','Corals','2','Corals only',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,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3345,NULL,'Coral biostromes',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,33.17,-5.31,NULL,NULL,NULL,NULL,-42.6683996916,-17.135922042,-22.7180915211,-31.7109980916,-21.043,-3.7547,'Krause','Kiessling','2023-01-04 17:36:53','2023-03-14 15:39:39'),('Kef en N’sour section',4402,'Tizra','Carboniferous','Mississippian','Visean','Brigantian',331.00,336.00,12,'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','4','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','1','Corals',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,'0','',0,'No or unknown reservoir potential',3345,NULL,'Coral biostromes.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,32.75,-5.8,NULL,NULL,NULL,NULL,-38.4825571158,-14.8127151497,-23.8280420259,-26.8584125526,-18.0102,-3.03137,'Krause','Krause','2023-01-04 18:00:13','2023-01-04 23:06:42'),('Tizra Section',4403,'Tizra','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',NULL,'2','10 - 100 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'3','Microbes',NULL,NULL,NULL,NULL,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,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3345,NULL,'Microbial reefs',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,33.32,-5.27,NULL,NULL,NULL,NULL,-40.2556631138,-15.1723377617,-23.3005253366,-28.4720955452,-17.8585,-2.28865,'Krause','Krause','2023-01-04 22:28:38','2023-01-04 23:07:37'),('Akerchi section',4404,'Akerchi','Carboniferous','Mississippian','Serpukhovian','upper Serpukhovian',323.20,330.90,12,'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','4','1','Less than 10 m wide',NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,'1','Above fair weather wave base','3','Microbes',NULL,NULL,NULL,NULL,NULL,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',3345,NULL,'Coral biostromes',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,33.32,-5.23,NULL,NULL,NULL,NULL,-31.9576235278,-9.74201975424,-23.9678188342,-21.7636223437,-17.8799,-2.26162,'Krause','Krause','2023-01-04 22:59:38','2023-03-10 13:16:52'),('Sunmayu, Stage 4,     Shandong, China',4405,'Zhushadong','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','6','1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','5','4','Microbial precipitation',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3347,NULL,'These reefs are inferred to have formed in a high-energy shoal setting\r\nThe calcimicrobes Kordephyton and Epiphyton and tubiform microbes are dominant at the Sunmayu section. The calcimicrobe Amgaina is locally abundant',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.624,117.997,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-10 13:16:48','2023-03-10 17:18:04'),('Jinhe, Stage 4, Shandong, China',4406,'Zhushadong','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','8','1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,'30','4405',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,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3347,NULL,'The calcimicrobes Epiphyton and Kordephyton and tubiform microbes are the main components. Tubiform microbes occur sporadically or as tangled\r\naggregations.\r\nCalcimicrobes occupy a maximum of 30%–78% of thin sections.\r\nThis reefs slightly deeper than 4405',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,35.078,118.173,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-10 13:24:26','2023-03-10 15:49:58'),('Yanbanzhai coral reef, Guizhou',4407,'Xiaodushan','Carboniferous','Pennsylvanian','Kasimovian','Kasimovian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','5.5','2','10 - 100 m wide',NULL,'2','10 - 100 m','50',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below 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','2','1','Constructor guild',NULL,NULL,'1','Present','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',3349,NULL,'Fomichevella framestone.\r\nlate Kasimovian base on fusulinids\r\nThe coral (Fomichevella) framestone is considered to have developed in a platform-margin slope environment.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,10,10,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-10 15:49:54','2023-03-10 17:18:04'),('Maustrenk, Lower Austria',4408,'Leitha Limestone','Neogene','Miocene','Middle Miocene','lower Sarmatian',12.50,13.80,31,'Burdigalian - Serravallian',14,10,'Middle/Late Miocene (Serravallian&Tortonian, 10.5 Ma)',NULL,3,'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','1',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','7','Bryozoans','8','Serpulids, worms, vermetids','18','Bryozoans - microbes - (algae) - (crinoids)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','4',NULL,NULL,'1','Present','1','Present','2','Medium zonation','1','Low zonation','1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3350,NULL,'Sarmatian Bryozoan–serpulid–algal–thrombolite bioherms of up to 50 cm size.\r\nThe buildups are globular, lense-like or columnar in shape and reach more than 50 cm in height and width. Along the outcrop of approx. 20 m 8–9 individual buildups can be observed',NULL,NULL,NULL,NULL,'Austria','Europe',NULL,NULL,48.554,16.7,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-10 17:18:00','2023-03-14 15:39:39'),('Ricklow Quarry, Monyash, Derbyshire',4409,'Monsal Dale','Carboniferous','Mississippian','Visean','Brigantian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','28','3','101-1000 m wide','100','3','More than 100 m','250','20',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','11','Siliceous sponges','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,'1','Present','2','Medium zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3352,NULL,'The Ricklow mud mound complex originated during a period of creation of accommodation in an intraplatform middle-ramp dysphotic environment with dispersed food resources. The mud mound complex growth was interrupted by a subaerial exposure due to a relative sea-level fall.',NULL,NULL,NULL,NULL,'United Kingdom','Europe',NULL,NULL,53.192,-1.755,NULL,'229499',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-14 15:39:36','2023-03-15 13:39:41'),('Dunmore boreholes',4410,'Kilbryan Limestone','Carboniferous','Mississippian','Tournaisian','upper Tournaisian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',NULL,3,'1','Seismic data available ',3,'Mud mound or bank','3','101-500 m thick','120','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'60',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','3','Below storm 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',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3353,NULL,'Waulsortian limestones occupy a little more than half the thickness of the sequence in which they lie in the two Dunmore cores. There is no sure way of determining whether individual banks extend from one core to the other, but if they do then they number about 10; if not then the number could rise to about 15. Banks of both flat-lying and clinoform depositional structure are present. Their individual thickness ranges from <1m to about 10m; units up to c.20m occur but as they are of flat-lying structure they may include more than one bank. The banks probably resembled in type and dimensions those seen in natural and quarry exposures in the Loughrea area about 60km away.',NULL,NULL,NULL,NULL,'Ireland','Europe',NULL,NULL,53.62,-8.77,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-15 13:39:37','2023-03-17 15:38:45'),('Vel-ky Lipnik',4411,'unknown','Paleogene','Paleocene','Selandian-Thanetian','early Thanetian',56.00,59.20,27,'Thanetian - Ypresian',53,55,'Paleocene/Eocene Boundary (PETM, 56 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','11','2','10 - 100 m wide','40','3','More than 100 m','200','20','747',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','11','1','Constructor guild','2','Intensive','1','Present','1','Low zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3354,NULL,'The age of this reef complex is contracted\r\ninto the interval 57-58 Ma, i. e. lower part of the\r\nThanetian.\r\nCorals are the main constructors of reef framework. Their surfaces are bearing also encrustings of coralline algae and sessile foraminifers, but their volume portion on the construction of rigid reef buildups is small.\r\n\r\nPeculiarity of this locality consists from the fact that deposits of reef complex are probable in situ on the place of their origin (under the deposits of Early Eocene) and they were not transported into younger deposits as is a\r\nrule in other Paleocene reef deposits of Slovakia.',NULL,NULL,NULL,NULL,'Slovakia','Europe',NULL,NULL,49.3766,20.4967,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-17 15:38:42','2023-03-17 17:45:37'),('Usabide complex, Pyrenees',4412,'unknown','Paleogene','Paleocene','Danian','Selandian',59.20,61.60,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','6','2','10 - 100 m wide','50','3','More than 100 m','110',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',NULL,NULL,NULL,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',559,NULL,'Growth phase 4. Indicate as early Thanetian, but should be Selandian.\r\nBioconstructions within the Usabide and Legunbe\r\ncomplexes (growth phases 4 and 5) appear as lowrelief, tabular-shaped bodies of variable dimensions.\r\nThe former (Usd-1 and Usd-2 in Fig. 2B) are of\r\nrelatively small size, being between 5 and 7 m thick and 70 and 110 m laterally\r\n',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,42.87,-2.04,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-03-17 17:45:34','2023-03-17 17:51:58'),('Shouxinghu',4413,'Lazhuglung','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 ',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','',0,'No or unknown reservoir potential',3355,NULL,'coral-stromatoporoid patch reefs',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,34.9499,81.4656,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2023-04-03 17:28:33',NULL),('Test1',4414,'Test1','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 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,'1','Present',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3356,NULL,'Test test test\r\nNochmal 4,59',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,44.55,55.44,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Krause','Krause','2023-04-03 20:31:41',NULL),('Seer Southern Reef',4418,'Burgasutay','Cambrian','Series 2','Stage 4','Botomian-Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','200','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','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',3357,NULL,'Stage 4\r\n\r\nInteresting example of a large archaeocyathan reef lacking typical kalyptrate structures.\r\n\r\nAnother specific feature of the Seer Reef is its principal composition of solitary archaeocyaths and synsedimentory fibrous calcite cement, enveloping their cups, with subdued calcimicrobal\r\npatches. Mud fillings are restricted to the reef top and some areas of lava breccia development. Such composition indicates higher-energy conditions.',NULL,NULL,NULL,NULL,'Mongolia','Asia',NULL,NULL,48.38,92.85,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2023-07-10 11:50:41',NULL),('Queensland Plateau, Site 811A',4419,'unknown','Neogene','Miocene','Middle Miocene','mid-Miocene',11.60,13.80,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,1,'1','Seismic data available ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown',NULL,NULL,NULL,NULL,NULL,NULL,'1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','2',NULL,NULL,NULL,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',3358,NULL,'The Middle Miocene rimmed carbonate platform was dominated by a tropical photozoan skeletal assemblage, including green algae, corals, and large benthic foraminifera. Bryozoans occur as a minor component.\r\nDrowning due to excess heat.',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-16.5162,148.1572,NULL,NULL,NULL,NULL,-22.4964479579,145.612237474,-24.3835461809,146.723123768,-25.2574,145.616,'Kiessling','Kiessling','2023-07-28 13:32:40',NULL),('Serdrar reef, Amellago',4420,'unknown','Jurassic','Lower Jurassic','Sinemurian','Sinemurian',190.80,199.30,19,'late Hettangian - early Aalenian',188,190,'Early Jurassic (Sinemurian/Pliensbachian, 190.8 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','2','Shelf or Platform margin','1e','Open-marine shelf','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','7','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',3359,NULL,'A pinnacle coral reef (220 m high), located in an open marine environment on a paleo-rim of a tilted block, drowned during the lattermost Sinemurian (Oxynotumto Raricostatum Chronozones) and progressively capped by lower offshore deposits',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,32.0075,-4.9453,NULL,NULL,NULL,NULL,15.7690873969,3.01960094662,25.9836351535,5.59015314374,26.1733,-3.04318,'Krause','Krause','2023-08-29 15:19:27',NULL),('Castle olistoliths, Jebel Taabest',4421,'unknown','Jurassic','Lower Jurassic','Sinemurian','Sinemurian/Pliensbachian',182.70,199.30,19,'late Hettangian - early Aalenian',188,190,'Early Jurassic (Sinemurian/Pliensbachian, 190.8 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',NULL,NULL,'1','Corals','15','Non-rudist bivalves',NULL,NULL,NULL,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',3359,NULL,'Coral bioherms',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.9414,-4.9585,NULL,NULL,NULL,NULL,17.7469863041,3.30399404096,27.2127383876,6.1436944933,26.1179,-3.08525,'Krause','Krause','2023-08-29 16:22:03',NULL),('Dades Valley 1',4422,'Choucht','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 ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'1','Corals','15','Non-rudist bivalves',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3359,NULL,'Coral reefs with rare lithiotid bivalves.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.5612,-5.90378,NULL,NULL,NULL,NULL,19.8502410986,3.4533117641,27.121028701,5.1082696411,26.216,-3.23716,'Krause','Krause','2023-08-31 16:02:36',NULL),('Koudiat Ech Chehem',4423,'unknown','Jurassic','Lower Jurassic','Pliensbachian','Domerian',182.70,190.80,19,'late Hettangian - early Aalenian',188,185,'Early Jurassic (Pliensbachian, 186.8 Ma)',NULL,3,'0','Outcropping reef ',2,'Reef mound','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,'1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)','4',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',3359,NULL,'Reef mounds. Giant complex bioherm composed of interlayered boundstones (pillarstones and mixstones) and crinoidal grainstones and packstones. Optimal reef window at the boundary between shoreface and offshore. It is a ca. 100 meter high buildup.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,31.8243,-6.0905,NULL,NULL,NULL,NULL,20.1567157049,3.47795822649,27.4238833551,5.167183942,26.5225,-3.26219,'Krause','Krause','2023-08-31 17:45:36',NULL),('Coral biostrome',4424,'Djenien Formation','Carboniferous','Mississippian','Serpukhovian','upper Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','10','4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','3b','Deeper slope or outer ramp','2','Below fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3360,NULL,'The biostrome contains a 10 m-thick coral biostrome in its middle unit formed by Siphonodendron, Diphyphyllum and Lithostrotion.Few brachiopods and solitary corals are found as dwellers within the biostrome. The coral biostrome records a quieter setting at the interface of middle and outer ramp settings, as seen in the co-existence of in situ coral growth, input of reworked material, deposition of carbonate mud, and sparitic textures.',NULL,NULL,NULL,NULL,'Algeria','Africa',NULL,NULL,30.99,-2.02,NULL,NULL,NULL,NULL,-36.2382119585,-6.3684716528,-27.5376027662,-21.4735000506,-20.4023,1.78604,'Siphonodendron','Siphonodendron','2023-09-22 15:37:59',NULL),('Hippuritid reef, l-Espa, Pyrenees',4426,'unknown','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 ',NULL,NULL,'1','Less than 10 m thick','2.5','1','Less than 10 m wide','6','2','10 - 100 m','20','1',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','5','Rudists','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','5','1','Constructor guild',NULL,NULL,NULL,NULL,'3','Pronounced 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',3362,NULL,'This late Campanian reef is exposed along some 20 × 6 m outcrop. Builders are mainly Hippurites radiosus, although other rudists, such as Hippuritella lapeirousei, Hippuritella sp. and Mitrocaprina sp. are also present together with corals. The orientation of 325 specimens of mainly H. radiosus was plotted in stereographic and cartesian projections. Orientations and microfacies permit to differentiate 5 vertically stacked intervals (settings) along the outcrop.\r\n\r\nVertical succession of environments depicts a complete rudist reef progradation',NULL,NULL,NULL,NULL,'Spain','Europe',NULL,NULL,42.2207,1.687,NULL,NULL,NULL,NULL,34.7483293082,4.38828235612,36.75291409,2.87183283878,31.7906,2.79329,'Kiessling','Kiessling','2023-10-18 16:07:42',NULL),('Yadana Gas Field',4428,'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,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','95','3','101-1000 m wide','500','4','More than 1000 m','3000','4',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'1','Present',2,'Actual reservoir',3366,NULL,'Upper Burman Limestone Formation, early Miocene in age, that is made up of one single carbonate platform, the top of which corresponds to the gas reservoir of the Yadana Field.\r\nModerate dolomitization has affected the top and flanks of the platform during the depositional hiatus.\r\nData from seismics and four wells.\r\nThe high (28%) average porosity of the reservoir is dominantly related to strong development of microporosity, moldic and vuggy porosity.\r\nSkeletal grains are dominated by non-geniculate coralline algae and large benthic foraminifers (Fig. 3A, B, C). Corals may be common in a few intervals (Fig. 3D). Non-geniculate coralline red algae are dominated by encrusting to branching forms, commonly forming nodules (rhodoliths) (Fig. 3A). The dominant genera are Lithothamnion, Mesophyllum and Sporolithon. Larger benthic foraminiferal association is characterized by Lepidocyclinids, Spiroclypeus, Cycloclypeus commonly displaying flat-shaped morphologies (Fig. 3C). Scleractinian assemblage includes robust branching or massive forms. Subordinate components include echninoderms, bryozoans, green algae and rare planktic foraminifera.',NULL,NULL,NULL,NULL,'Burma','Asia',NULL,NULL,15.123,94.783,NULL,NULL,NULL,NULL,11.2139590721,92.5759025937,6.39499632872,92.1671254561,8.66559,98.6033,'Kiessling','Kiessling','2024-06-25 14:04:02',NULL),('Gelati, Tertiary Piedmont Basin',4429,'Molare','Paleogene','Oligocene','Chattian','middle Chattian',25.00,27.50,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','10','1','Less than 10 m wide','10','2','10 - 100 m','200',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','1','Corals','2','Algae',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','20','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',3367,NULL,'Brown mesophotic coral reefs in prodelta setting.\r\nlate middle Chattian according to Sr-isotope stratigraphy.\r\nCoral-bearing beds are in general alternated with clay-rich horizons and along the measured sections they display a variable overall thickness, from about 4.5 m (Cascine section) up to 10.5 m (Valletta section). Four different coral facies have been identified: branching Stylophora floatstone (BSF), Acropora-Stylophora floatstone/rudstone (ASFR), Goniopora/Caulastraea pillarstone (GCP), mixed-coral domestone (MCD); their descriptions and interpretation are reported below and summarized in Table 1.',NULL,NULL,NULL,NULL,'Italy','Europe',NULL,NULL,44.546,8.446,NULL,NULL,NULL,NULL,41.2512314658,5.20514770885,41.4713601204,9.41450989903,43.0286,7.50688,'Kiessling','Kiessling','2024-06-25 15:48:36',NULL),('Nors Stenbrott 1, Gotland',4430,'Tufta','Silurian','Wenlock','Sheinwoodian','Sheinwoodian',430.50,433.40,7,'Wenlock - early Pridoli',425,425,'Middle Silurian (Wenlock, 430.4 Ma)',NULL,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1','1','Less than 10 m wide','2','1','Less than 20 m','2',NULL,NULL,1,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8','3','Binder guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3368,NULL,'Lower Sheinwoodian bryostromatolite reef in midst of positive isotope excursion.\r\nBryozoan-stromatolite reef. Some tabulate corals and stromatoproids present.\r\nCoordinates and more details provided by Claussen et al. (2022, Sedimentology):\r\nBryzoans 28-43%, porostromate (0-14%) and spongiostromate microbes (14-46%).\r\nMacroboring and microboring present. Bivalve borings',NULL,NULL,NULL,NULL,'Sweden','Europe',NULL,NULL,57.919167,18.921972,NULL,'226712',NULL,NULL,-8.16390399834,-49.5536668696,-8.16390399834,-49.5536668696,-13.9422,-2.4286,'Kiessling','Kiessling','2024-07-18 14:12:34',NULL),('Hallsarve, Gotland',4431,'Eke','Silurian','Ludlow','Ludfordian','Ludfordian',423.00,425.60,7,'Wenlock - early Pridoli',425,420,'Late Silurian (Pridoli - Ludlow, 425.2 Ma)',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1','1','Less than 10 m wide','2','1','Less than 20 m','10',NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species','8','3','Binder guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3369,NULL,'Bryostromatolite - bryozoans and spongiostromate microbes dominant. Some tabulate corals.\r\nSurrounded by coarse-grained, poorly sorted reef debris.\r\nHigh amount of phosphatic components indicated high nutrient input.',NULL,NULL,NULL,NULL,'Sweden','Europe',NULL,NULL,57.288,18.640111,NULL,NULL,NULL,NULL,2.0492591942,-44.075974426,2.0492591942,-44.075974426,-13.7966,-1.91382,'Kiessling','Kiessling','2024-07-18 15:32:28',NULL),('Maʼahm patch reef',4432,'Ma\'ahm','Paleogene','Oligocene','Chattian','Chattian',23.00,28.10,30,'Chattian - Aquitanian',22,25,'Late Oligocene (Chattian, 25.6 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','24','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','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','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',3371,NULL,'Perhaps already starting in Rupelian, but main coral-reef development in the Chattian (dated by Racey 1995). \r\nMa\'ahm beds 112 m thick. Patch reefs at top. ',NULL,NULL,NULL,NULL,'Oman','Asia',NULL,NULL,23.58,58.21,NULL,NULL,NULL,NULL,17.1697785902,52.3066962507,21.7876707593,56.6630694403,18.3319,53.5237,'Kiessling','Kiessling','2024-08-20 13:32:19',NULL),(' Minami-dai, Akiyoshi Limestone Group',4433,'unknown','Carboniferous','Pennsylvanian','Bashkirian','Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,320,'Early Pennsylvanian (Bashkirian, 319.2 Ma)',NULL,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick','400','3','101-1000 m wide','350','3','More than 100 m','400',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope',NULL,NULL,'3','Below storm wave base','4','Stromatoporoids','11','Siliceous sponges','22','Stromatoporoids/sponges - corals - (algae)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species','3','1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low zonation','3','Pronounced zonation','1','Less than 30% micrite',NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',3372,NULL,'Stromatoporoids (laminated skeletons made up of cystose or flat laminae and pillar-like vertical structures) are abundantreef-builders together with Chaetetes.',NULL,NULL,NULL,NULL,'Japan','Asia',NULL,NULL,34.28,131.26,NULL,NULL,NULL,NULL,14.8169360741,129.065604086,3.70402835081,66.6900747942,4.60251,87.6966,'Krause','Krause','2024-08-28 17:15:35',NULL),('D4, Raghama',4435,'Raghama','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,NULL,NULL,NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','24','2','10 - 100 m wide','15','4','More than 1000 m','1100','30','4434',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',3373,NULL,'Southern end of reefal sections (4 sections in total)\r\nThe fore reef facies in the study area disconformably overlay the clastic sediments of the Raghama Formation and are represented by 6 m thick sandy coralline boundstone and microbial laminites, with rhodolith of red algae, and domal and heads of scleractinian corals of Favites,\r\nTarbellastraea, Porites, Thegioastraea spp., as well as echinoids, algae, bivalves, and miliolids.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,27.659167,35.501389,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-09-02 16:17:50',NULL),('D1, Raghama',4434,'Raghama','Neogene','Miocene','Middle Miocene','Middle Miocene',11.60,16.00,31,'Burdigalian - Serravallian',14,15,'Middle Miocene (Langhian, 14.9 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20','2','10 - 100 m wide','15','4','More than 1000 m','1100','30',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','',1,'No or unknown reservoir potential',3373,NULL,'Northern end of reefal sections (4 sections in total)\r\nThe fore reef facies in the study area disconformably overlay the clastic sediments of the Raghama Formation and are represented by 6 m thick sandy coralline boundstone and microbial laminites, with rhodolith of red algae, and domal and heads of scleractinian corals of Favites,\r\nTarbellastraea, Porites, Thegioastraea spp., as well as echinoids, algae, bivalves, and miliolids.',NULL,NULL,NULL,NULL,'Saudi Arabia','Asia',NULL,NULL,27.370556,35.664444,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-09-02 13:58:55',NULL),('St. Paul, Gulf of Suez',4436,'Gharamul','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 ',1,'True reef','1','Less than 10 m thick','5','1','Less than 10 m wide','10','1','Less than 20 m','10','5',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',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 6 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3374,NULL,'The Gharamul Formation\r\nconsists of a 29-m-thick succession of limestone with an occasional sandstone bed.\r\nThe limestone comprises low-diversity\r\nbiotas of bivalves, gastropods, corals, red algae, algal stromatolites, echinoids and benthic foraminifera. Corals occur both as in situ patch reefs and as reworked debris (Figure 5d,e).\r\nStromatolites are 2-to 5-mm-thick\r\nlaminations of gently undulating type (Figure 5f). Red algae occur as encrustations on patch reefs or as algal debris in the lime mud matrix (Lithothamnium sp., Mesophyllum sp. and\r\nLithophyllum sp.).',NULL,NULL,NULL,NULL,'Egypt','Africa',NULL,NULL,28.873,32.61,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-09-02 16:57:15',NULL),('Sugaitebulak, Tarim',4437,'Xiaoerbulak','Cambrian','Series 2','Stage 3','Atdabanian',514.00,521.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','70',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'1','Low 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',3375,NULL,'Archaeocyath-Epiphyton reef-rimmed platform.\r\nPlatform marginal buildup facies are mainly composed of massive Archaeocyath-Epiphyton boundstone (AERPF4) and massive dendrolite (AERPF5).\r\nMassive up-convex geometry (up to 70 m thick). Mesofabric characterized by erecting light-coloured aggregates/speckles intergrown with in-situ cup-shaped, branching and massive archaeocyaths or overturned fragments particularly in seaward portion. Bush-like calcified Epiphyton colonies dominate the bioconstructors with subordinate Renalcis elements and build up the skeletal/rigid framework. Inter-constructor cavities lined with submarine cements common. Constituting the core portions of phase S2 buildup complexes.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,40.908361,79.482525,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-09-04 14:17:16',NULL),('Wirrealpa microbialites',4438,'Wirrealpa','Cambrian','Series 3','Stage 5','Toyonian',509.00,514.00,1,'Nemakit/Daldynian - Toyonian',520,520,'Early/Middle Cambrian boundary (520 Ma)',NULL,1,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','7','2','10 - 100 m wide','10','1','Less than 20 m','40','20','3764',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',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3376,NULL,'Upper Stage 4 (Redlichia cf. versabunda Zone).\r\nThe buildup is composed of a series of parallel erected, cylindrical columns that are 1.5–4 m high and 20–50 cm in diameters.\r\nAbundant ooids and calcareous metazoan skeletons, associated with micritic sediments, fill the inter-framework spaces of the microbialite, forming a packstone fabric. The calcareous metazoan skeletons, including chancelloriid sclerites, trilobite fragments, and rare mollusk shells, are scattered in the matrix.\r\n\r\nthrombolite-stromatolite complex was formed within an ecosystem lacking archaeocyaths but dominated by microbes (reef builders) and chancelloriids (reef dwellers).',NULL,NULL,NULL,NULL,'Australia','Oceania',NULL,NULL,-35.09556,138.8944,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-10-08 11:00:48',NULL),('Likva, Brac',4439,'Sumartin','Cretaceous','Upper Cretaceous','Maastrichtian','upper Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','25','2','10 - 100 m wide','12','2','10 - 100 m','40','1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','6','Calcisponges','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3377,NULL,'Four sections: Likva 1-4\r\nThe Likva-2 section comprises a 51.5 m-thick continuous succession of shallow marine carbonates. Reef levels composed of scleractinian corals, layered domical and bulbous growth forms (calcified sponges?) and unidentified fossil remains in growth positions (LF3b).\r\n10 reef levels in 6 lithostratigraphic units, 8 levels in unit B.',NULL,NULL,NULL,NULL,'Croatia','Europe',NULL,NULL,43.389,16.46,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-12-08 12:11:57',NULL),('Majerovica, Hvar',4440,'Sumartin','Cretaceous','Upper Cretaceous','Maastrichtian','upper Maastrichtian',66.00,72.10,26,'middle Campanian - Danian/Selandian',75,70,'Late Cretaceous (Maastrichtian, 69 Ma)',NULL,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','9','1','Less than 10 m wide',NULL,'2','10 - 100 m','90',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,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',3377,NULL,'Several reef horizons in the late Maastrichtian. Each horizon 0.5-3 m thick. Cumulative thickness about 9 m.\r\nLayered sponges, corals and stromatolites',NULL,NULL,NULL,NULL,'Croatia','Europe',NULL,NULL,43.1727,16.427,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2024-12-08 15:31:25',NULL),('Likva, Brac',4441,'Sumartin','Paleogene','Paleocene','Danian','lower Danian',61.60,66.00,27,'Thanetian - Ypresian',53,60,'Paleocene (Danian&Thanetian, 61 Ma)',64,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','3','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','6','Calcisponges','50','Corals - stromatoporoids (chaetetids) - algae (stromatolites) - rudists - (spicular sponges)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present','1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potentia',3377,NULL,'Four sections: Likva 1-4\nThis is the Danian part of Likva 2',NULL,NULL,NULL,NULL,'Croatia',' 	Europe',NULL,NULL,43.389,16.46,NULL,NULL,NULL,NULL,33.2740259509,15.3169702621,36.3029700953,16.3526153545,33.1822,14.938,'Kiessling','Kiessling','2024-12-11 18:05:08',NULL),('Binping Tubiphytes reef, Guizhou',4442,'unknown','Carboniferous','Pennsylvanian','Gzhelian','Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',NULL,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','5','2','10 - 100 m wide','10','2','10 - 100 m','20',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','9','Tubiphytes','1','Corals','21','Tubiphytes - cyanophyceans - corals - (algae) - sponges',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','1','Less than 30% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3378,NULL,'The reef, 5 m high and about 20 m in lateral extension, is lens-like. The main reef-building organisms are Tubiphytes, Archaeolithoporella (and other encrusting calcimicrobes), and bryozoans.\r\nLarger foram zuggest Gzhelian age.\r\nAbundant marine cement sugges high-energy environment. High-energy above FWWB.\r\nTriple hybrid carbonate: Skeleton-microbial-cement reef.',NULL,NULL,NULL,NULL,'China','Asia',NULL,NULL,25.52,106.22,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2025-01-20 15:03:57',NULL),('Corni Quarry, coral-rudist biostrome',4443,'unknown','Cretaceous','Upper Cretaceous','Santonian','Santonian',83.60,86.30,25,'late Cenomanian - early Campanian',91,85,'Late Cretaceous (Santonian&Coniacian, 86.7 Ma)',NULL,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5','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','5','Rudists','91','Rudists - corals - algae/microbes - (brachiopods)','1',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','6 to 24 reef building species',NULL,'1','Constructor guild','2','Intensive','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',3379,NULL,'Based on sedimentological features and faunal associations, the following facies associations have been identified: 1) Marls and limestone with terrigenous clasts; 2) Build-ups with tubular/massive corals and rudists; 3) pillarstone-type bioaccumulations with branching/platy corals; 4) bioclastic rudstone/grainstone; 5) bioclastic floatstone/packstone. All these facies associations indicate a coastal environment developed along a shelf margin influenced by both the terrigenous supply, and the relative sea level\r\nvariations.',NULL,NULL,NULL,NULL,'Romania','Europe',NULL,NULL,46.6544,23.3966,NULL,'240129',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2025-04-22 09:35:02',NULL),('Tizra mounds',4444,'Tizra','Carboniferous','Cisuralian','Visean','Brigantian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',NULL,1,'0','Outcropping reef ',3,'Mud mound or bank','3',NULL,'110','2',NULL,NULL,'3',NULL,'200',NULL,NULL,0,'Tropical or unknown','3',NULL,'3a',NULL,'1',NULL,'3','','3',NULL,'64',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1',NULL,NULL,'4',NULL,NULL,NULL,'1',NULL,'1',NULL,'1',NULL,'3','More than 60% micrite','3','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',3381,NULL,'Microbial mounds with close relationship with ooids, frequent ooids embedded in the microbial facies, an ecological parameter used by previous authors to identified shallower stages in the microbial growths.\r\nLess than 40% of samples yield ooids generated in situ, whereas there is a predominance of transported ooids.',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,33.554167,-5.429722,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'Kiessling','Kiessling','2025-07-22 09:08:38',NULL);
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