-- Table structure for table `reeflit_reef`
--

CREATE TABLE `reeflit_reef` (
  `REF` double NOT NULL,
  `R_NUMBER` double NOT NULL,
  PRIMARY KEY (`REF`,`R_NUMBER`),
  KEY `R_NUMBER` (`R_NUMBER`)
) ENGINE=MyISAM DEFAULT CHARSET=utf8 COLLATE=utf8_general_ci;

--
-- Dumping data for table `reeflit_reef`
--

INSERT INTO `reeflit_reef` VALUES 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--
-- Table structure for table `reefs`
--

CREATE TABLE `reefs` (
  `NAME` varchar(255) DEFAULT NULL,
  `R_NUMBER` int(11) NOT NULL AUTO_INCREMENT,
  `FORMATION` varchar(255) NOT NULL,
  `SYSTEM` varchar(255) DEFAULT NULL,
  `SERIES` varchar(255) DEFAULT NULL,
  `STAGE` varchar(255) DEFAULT NULL,
  `INTERVALL` varchar(255) DEFAULT NULL,
  `MIN_MA` decimal(8,2) DEFAULT NULL,
  `MAX_MA` decimal(8,2) DEFAULT NULL,
  `TIME_SLICE` double DEFAULT NULL,
  `TIME_SLICE_TEXT` varchar(255) DEFAULT NULL,
  `TIME_GPLATES` int(11) DEFAULT NULL,
  `SCOTESE_TIME` int(11) DEFAULT NULL,
  `SCOTESE_INTERVALLS` varchar(255) DEFAULT NULL,
  `TIME` double DEFAULT NULL,
  `RELIABILIT` int(11) DEFAULT NULL,
  `SUBSURFACE` varchar(60) DEFAULT NULL,
  `SUBSURFACE_TEXT` varchar(50) DEFAULT NULL,
  `TYPE` double DEFAULT NULL,
  `TYPE_TEXT` varchar(50) DEFAULT NULL,
  `THICKNESS` varchar(10) DEFAULT NULL,
  `THICKNESS_TEXT` varchar(50) DEFAULT NULL,
  `M_THICK` varchar(10) DEFAULT NULL,
  `WIDTH` varchar(10) DEFAULT NULL,
  `WIDTH_TEXT` varchar(50) DEFAULT NULL,
  `M_WIDTH` varchar(10) DEFAULT NULL,
  `EXTENSION` varchar(10) DEFAULT NULL,
  `EXTENSION_TEXT` varchar(50) DEFAULT NULL,
  `M_EXT` varchar(255) DEFAULT NULL,
  `EXT_BELT` varchar(10) DEFAULT NULL,
  `BELONGING` varchar(10) DEFAULT NULL,
  `TROPICAL` double DEFAULT NULL,
  `TROPICAL_TEXT` varchar(50) DEFAULT NULL,
  `ENVIRONMEN` varchar(255) DEFAULT NULL,
  `ENVIRONMENT_TEXT` varchar(60) DEFAULT NULL,
  `SUBENVIRON` varchar(255) DEFAULT NULL,
  `SUBENVIRONMENT_TEXT` varchar(60) DEFAULT NULL,
  `BATHYMETRY` varchar(3) DEFAULT NULL,
  `BATHYMETRY_TEXT` varchar(60) DEFAULT NULL,
  `BIOTA_MAIN` varchar(3) DEFAULT NULL,
  `BIOTA_MAIN_T` varchar(255) DEFAULT NULL,
  `BIOTA_SEC` varchar(10) DEFAULT NULL,
  `BIOTA_SEC_TEXT` varchar(50) DEFAULT NULL,
  `BIOTA_DETA` varchar(3) DEFAULT NULL,
  `BIOTA_DETA_TEXT` varchar(250) DEFAULT NULL,
  `ALG_TYPE` varchar(3) DEFAULT NULL,
  `ALG_TYPE_TEXT` varchar(50) DEFAULT NULL,
  `P_LMC` varchar(3) DEFAULT NULL,
  `P_ARAG` varchar(3) DEFAULT NULL,
  `P_HMC` varchar(3) DEFAULT NULL,
  `UPWELL` int(1) DEFAULT NULL,
  `UPWELL_TEXT` varchar(10) DEFAULT NULL,
  `CONTROL` int(1) DEFAULT NULL,
  `CONTROL_TEXT` varchar(10) DEFAULT NULL,
  `DIVERSITY` varchar(3) DEFAULT NULL,
  `DIVERSITY_TEXT` varchar(50) DEFAULT NULL,
  `M_SPEC` varchar(10) DEFAULT NULL,
  `GUILD` varchar(3) DEFAULT NULL,
  `GUILD_TEXT` varchar(50) DEFAULT NULL,
  `MACRO_BOR` varchar(3) DEFAULT NULL,
  `MACRO_BOR_TEXT` varchar(50) DEFAULT NULL,
  `MICRO_BOR` varchar(3) DEFAULT NULL,
  `MICRO_BOR_TEXT` varchar(50) DEFAULT NULL,
  `VERT_ZONAT` varchar(10) DEFAULT NULL,
  `VERT_ZONAT_TEXT` varchar(50) DEFAULT NULL,
  `HOR_ZONAT` varchar(10) DEFAULT NULL,
  `HOR_ZONAT_TEXT` varchar(50) DEFAULT NULL,
  `MICRITE` varchar(3) DEFAULT NULL,
  `MICRITE_TEXT` varchar(50) DEFAULT NULL,
  `SPARITE` varchar(3) DEFAULT NULL,
  `SPARITE_TEXT` varchar(50) DEFAULT NULL,
  `DEBRIS` varchar(5) DEFAULT NULL,
  `DEBRIS_TEXT` varchar(50) DEFAULT NULL,
  `DOLOMITE` varchar(3) DEFAULT NULL,
  `DOLOMITE_TEXT` varchar(50) DEFAULT NULL,
  `RESERVOIR` double DEFAULT NULL,
  `RESERVOIR_TEXT` varchar(50) DEFAULT NULL,
  `REF1` double DEFAULT NULL,
  `REF2` double DEFAULT NULL,
  `REMARKS` text DEFAULT NULL,
  `LAT_DEG` double DEFAULT NULL,
  `LON_DEG` double DEFAULT NULL,
  `M_LAT` double DEFAULT NULL,
  `M_LONG` double DEFAULT NULL,
  `COUNTRY` varchar(255) DEFAULT NULL,
  `CONTINENT` varchar(20) DEFAULT NULL,
  `GPLATESID` int(3) DEFAULT NULL,
  `OTHERS` varchar(255) DEFAULT NULL,
  `LATIT` double DEFAULT NULL,
  `LONGIT` double DEFAULT NULL,
  `PBDB` varchar(10) DEFAULT NULL,
  `COLLECTION` varchar(255) DEFAULT NULL,
  `PAL_LAT_old` double DEFAULT NULL,
  `PAL_LONG_old` double DEFAULT NULL,
  `PAL_LAT` double DEFAULT NULL,
  `PAL_LONG` double DEFAULT NULL,
  `PAL_LAT_M` double DEFAULT NULL,
  `PAL_LONG_M` double DEFAULT NULL,
  `PAL_LAT_SCOTESE` float DEFAULT NULL,
  `PAL_LONG_SCOTESE` float DEFAULT NULL,
  `USER` varchar(225) DEFAULT NULL,
  `USER_UPDATE` varchar(255) DEFAULT NULL,
  `DATE` datetime DEFAULT current_timestamp(),
  `DATE_UPDATE` datetime DEFAULT NULL,
  UNIQUE KEY `R_NUMBER` (`R_NUMBER`)
) ENGINE=MyISAM AUTO_INCREMENT=4445 DEFAULT CHARSET=utf8 COLLATE=utf8_general_ci;

--
-- Dumping data for table `reefs`
--

INSERT INTO `reefs` VALUES ('Tilkideligi Tepe',1,'','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',214,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','6','Calcisponges','4','Stromatoporoids','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','7','2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',91,1377,'Thallophytes microborings.',37,30,776871,2498401,'Turkey','Asia',522,'1376, 2377',37.0333,30.3833,'WAHR','38048',8.33867399166,35.6567703772,8.14569659055,35.6993151197,5.21276444499,27.4270265634,8.87947,21.7674,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hydra',2,'Pantokrator Limestone','Triassic','Upper Triassic','Carnian','upper Carnian',228.00,230.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',219,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'9',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','80','20',0,'no',0,'no','3','25 or more reef building species','41','1','Constructor guild','1','Present','1','Present','3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',33,218,'Predominantly late Carnian (Tuvalian, but covers late Carnian to early Norian and continues into late Norain and Rhaetian. From Flügel pers. comm.The Late Carnian to Early Norian part of the reef sequence consists of (a) biodetrital limestones with Tubiphytes and internal breccias, overlain by (b) a high-diverse coral-sponge reef limestones, followed by (c) sponge-coral reef limestones, (d) a breccia horizont, and (e) a coral reef limestone with dendroid corals (Retiophyllia) and abundant solenoporacean red algae. Diversity is high in the intervals b and c but decreases in interval e. Common fossils are sphinctozoids, inozoids and chaetetids (Senowbari-Daryan and Schäfer, 1983), corals (Turnsek and Senowbari-Daryan, 1994), algae (Schäfer and Senowbari-Daryan, 1982, Angiolini and others, 1992), microproblematica and foraminifera. Sphinctozoid sponges and scleractinian corals correspond to taxa known from Carnian reefs of the Alps. In contrast to the Alpine Carnian localities, corals seem to be more abundant in Hydra.',37,23,1202584,2133165,'Greece','Europe',338,'',37.3833,23.6333,'WAHR','38018',5.30728209358,30.7124281411,5.30728209358,30.7124281411,1.80492093455,20.9315359348,7.32517,20.2917,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shiraho, W-Pacific',3,'','Quarternary','Holocene','Holocene','Holocene',0.00,0.00,34,'Holocene',0,1,'Pleistocene - Calabrian - Gelasian',0,3,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'25',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','70','30',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',10,0,'',24,124,3299438,13043589,'Pacific','Pacific',NULL,'',24.3333,124.25,'','',24.3333,124.25,24.3333,124.25,24.3333,124.25,24.3795,124.163,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-09 21:13:14'),('Aksu-Terziler area',4,'','Triassic','Upper Triassic','Carnian','Tuvalian',227.00,237.00,17,'Induan - early Carnian',235,225,'Late Triassic (Carnian/Norian 227 Ma)',219,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100','1',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','6','Calcisponges','4','Stromatoporoids','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','24','2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',91,1377,'Cipit boulders \'composed\' of four different facieszones: in the same frequency bafflestones (in some parts framestone) and wackestones, while pelsparite grainstones and oncoidal grainstones rarely occur. Tuvalian 1-2. Bafflestones with sphinctozoans, inozoans, chaetetids, cerioid corals solenoporacean, porostromata and chaetetid crusts.',37,31,822681,2593461,'Turkey','Asia',522,'',37.8,31.0333,'WAHR','60649',4.92689474869,38.0981157209,4.92689474869,38.0981157209,0.728913373589,27.1457367653,-0.309389,26.3043,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Adnet, Salzburg',5,'','Triassic','Upper Triassic','Rhaetian','upper Rhaetian',201.30,204.00,18,'late Carnian - middle Hettangian',218,200,'Late Triassic (Rhaetian/Hettangian, 201.3 Ma)',201,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'1',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',1,'yes','3','25 or more reef building species','45','2','Baffler guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',11,49,'The Upper Rhaetian coral limestone of Adnet, southeast of Salzburg, Austria has been repeatedly referred to as one of the most spectacular examples of an ancient \'autochthonous\' coral reef structure. The \'Tropfbruch\' quarry is probably the best outcrop for interpreting the distributional patterns of biotic successions and communities of a late Triassic patch reef. Our study is based on the interpretation of a) outcrop photographs, b) reef maps resulting from quadrat transects, and c) the analysis of quantitative data describing the distribution and frequency of reef organisms and sediment. A new methodological approach (combination of reef mapping and photo-transects) is used to obtain quantitative field data which can be compared in greater detail with data from modern coral reefs investigated by corresponding quantitative surveys.  Three unconformities and three well-defined \'reef growth stages\' reflecting the vertical and lateral development of the reef structure were differentiated using transects:  Stage 1, representing the reef growth optimum, is characterized by laterally differentiated coral reef knobs with corals in growth position. Criteria supporting this interpretation are the extraordinary size of the corals, their preservation in situ and the great thickness of this interval. The massive coral Pamiroseris grew under higher energy conditions at the rim of the reef knob, whereas branching Retiophyllia colonies preferred less agitated water in the center. Vertical changes are reflected by an increase in frequency of the dasycladacean alga Diplopora adnetensis and by the decreasing size of Retiophyllia. These sedimentological and biological criteria together with the unconformity above indicate a fall in the sea level as a major control mechanism.  Stage 2, separated from stage 3 by an unconformity caused by partial subaerial exposure and karstification, is characterized by vertically stacked coral successions with diverse reef debris. Facies heterogeneity is reflected by differences in the diversity, taphonomy and packing density of reef-building organisms as well as by differences in sediment input from the platform. Water depths and accommodation space were lower, therefore minor sea level fluctuations had a stronger effect on the biotic composition. The high percentage of coral debris and corals reworked by storms and the increase in the input of platform sediment led to a reduction of reef growth.  Stage 3, again separated at the base by an unconformity associated with karstification, is characterized by bioclastic sediments with isolated reefbuilders forming a level-bottom community. The distribution of different coral morphotypes suggests that sea level fluctuations were not the only controlling factor. Variations in the substrate were caused by differences in the input of platform sediment.  The vertical changes in reef community structures correspond to a sequence of \'allogenic replacements\', because the change from one community to another is the result of extrinsic environmental factors (short-term subaerial exposure of parts of the reef structure and renewed flooding). Our new data provide no support for the model of ecological reef successions to the Adnet reef. The three-step development seen in Adnet documents the response of low-diverse coral associations to variations caused by small-scale sea level changes, storm activity and sedimentation.  The distribution of communities as well as the vertical development of the Adnet reef structure offer no general model of Alpine Upper Rhaetian reefs, because of the particular setting of the patch reef (platform reef surrounded by calcareous sands). Only the \'capping beds\' of the Upper Rhaetian Reef Limestone of the Steinplatte exhibit criteria similar to Adnet (high coverage of spatially separated Retiophyllia A and Retiophyllia B communities, strong inpact of freshwater dissolution pointing to subaerial exposure and small-scale karstification).  Potential modern analogues of features seen in the coral communities of Adnet are the internal structure of the Retiophyllia thickets, the key role of branching corals within the communities, the scattered distribution and low and even diversity of corals subsequent to breaks in settlement, segration patterns of corals indicating \'contact avoidance\', toppling of large coral colonies by intensive boring, and decreasing coral coverage from deeper and sheltered settings to more shallower water depths.',47,13,3812080,1522387,'Austria','Europe',301,'2240',47.7,13.1667,'WAHR','22963',26.9812146499,30.2546131111,28.1471802538,30.0885296173,29.8636407331,24.0155922233,32.6069,16.4294,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rötelwand',6,'','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'15',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','54','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',11,49,'Additionally encrusting algae (solenoporaceans) and forams important. Hexcorals and spongiomorphs about equally important. Radiolarians in underlying mudstones suggest slope deposition to me. Plenty of siliclastic input.',47,13,3812733,1523514,'Austria','Europe',301,'98',47.7,13.1833,'WAHR','36815',26.973000219,30.2631097621,26.973000219,30.2631097621,29.0064896519,22.9845268547,32.4826,15.5517,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rio Blanco',7,'','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','','Unknown','2','Below fair weather wave base','8','Serpulids, worms, vermetids','8','Serpulids, worms, vermetids','76','Worms only',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species','2','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',13,0,'',37,-3,2101135,429879,'Spain','Europe',304,'',37.325,-3.4333,'WAHR','67734',22.1495511267,11.6340063313,22.1495511267,11.6340063313,21.7241741366,12.0665468454,24.7231,0.828875,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Anxian, Sichuan',8,'Hanwang','Triassic','Upper Triassic','Carnian','upper Carnian',228.00,230.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',219,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','60',NULL,NULL,NULL,'3','More than 100 m',NULL,'25',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','11','Siliceous sponges','8','Serpulids, worms, vermetids','43','Siliceous sponges - serpulids - (bivalves) - (calcisponges) - (microbes)',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',14,71,'Diverse siliceous sponges. Some encrusting serpulids. 100 x 60m. No microbial crusts. 10-40 % fossils (locally 70 %).',31,104,3766718,10338664,'China','Asia',602,'662',31.6167,104.4333,'WAHR','25405',14.0299706971,111.469731315,14.0299706971,111.469731315,44.4731528493,112.921002826,29.1875,90.9345,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grimming',9,'','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','2',NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','30','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',6,15,'No detailed descriptions available\r\n',47,14,3841114,1602656,'Austria','Europe',301,'',47.5833,14.25,'','170644',19.9046280551,32.2611759172,22.810545692,31.3694883744,25.8777680422,20.8596955894,28.8474,16.8181,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lime Peak, Yukon',10,'Aksala','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',209,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','150','3','101-1000 m wide','1000','4','More than 1000 m','3000',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','22','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',16,57,'Stikinia terrane. Hankock member. Abstract of ref. 1404: An Upper Triassic reef complex, formed in the convergent margin of the Stikine Terrane, is well exposed at Lime Peak, in the southern Yokon. It consists of superimposed patch reefs and bedded inter-reef limestone and is  surrounded by volcaniclastic rocks. The reefs are up to 150 m thick and are composed of variable proportions of sponge-coral framework and skeletal sediment. They are the first Tethyan-type sponge reefs recognized in North America. The inter-reef limestones include thick-bedded accumulations of locally derived organisms, and thin-bedded deposits of reef-derived debris. The Lime Peak fossils are a mixture of those with Tethyan affinities, North American endemics, and new forms, possibly reflecting the origin of Stikinia between the Tethys and cratonic North America.',61,-134,4121052,-7080389,'Canada','North America',121,'108, 1404',61.0611,-134.8736,'WAHR','38033',34.6577639386,-47.2120023631,34.7787739156,-47.0645624726,45.9544864903,-47.3063778189,27.3014,-73.4842,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sarmeika reef, Argolis',11,'Pantokrator','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',208,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','7','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',17,247,'Ref 17 suggested a Carnian age Ref 247 Norian/Rhaetian Norian according to Flügel (2002). Calcisponges, sclerosponges, corals and solenoporaceans as main reef builders. Spongiostromata crusts important for stabilisation.',37,23,1260993,2102102,'Greece','Europe',338,'',37.6333,23.0833,'WAHR','24310',8.39577628723,29.2660400123,8.22315658532,29.3117714626,6.75526942422,22.5386626051,13.4597,17.9499,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Feichtenstein',12,'','Triassic','Upper Triassic','Rhaetian','upper Rhaetian',201.30,204.00,18,'late Carnian - middle Hettangian',218,200,'Late Triassic (Rhaetian/Hettangian, 201.3 Ma)',201,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'3',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','52','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',18,49,'',47,13,3817988,1530815,'Austria','Europe',301,'',47.7069,13.2972,'WAHR','36801',26.9213494155,30.3271132069,28.0878635994,30.1623744798,29.8301273656,24.1095201142,32.5632,16.5202,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gruber',13,'','Triassic','Upper Triassic','Rhaetian','upper Rhaetian',201.30,204.00,18,'late Carnian - middle Hettangian',218,200,'Late Triassic (Rhaetian/Hettangian, 201.3 Ma)',201,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','62','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',18,49,'',47,13,3815818,1532515,'Austria','Europe',301,'',47.6861,13.3039,'WAHR','36807',26.9039221226,30.3134119241,28.0703338058,30.1486944498,29.8095305887,24.1033401003,32.5434,16.5107,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wombat Plateau,  offshore Australia, Indian Ocean',14,'','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'25',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',20,69,'',-16,115,-4257245,7690201,'Indian Ocean','Indian Ocean',NULL,'',-16.8333,115.8333,'WAHR','36912',-23.8559009887,83.0865562234,-23.8559009887,83.0865562234,-42.7401319206,75.7108220549,-23.2476,70.8606,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mahlknecht',15,'','Triassic','Middle Triassic','Ladinian','upper Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',231,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',21,0,'Stratigraphy: Upper Longobardian',46,11,1398469,2326479,'Italy','Europe',344,'',46.5,11.3667,'WAHR','67723',16.8503148294,34.8754569196,16.8503148294,34.8754569196,10.8437350139,23.0385131365,7.90845,22.1236,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wilde Kirche+Tegernsee',16,'','Triassic','Upper Triassic','Rhaetian','upper Rhaetian',201.30,204.00,18,'late Carnian - middle Hettangian',218,200,'Late Triassic (Rhaetian/Hettangian, 201.3 Ma)',201,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'15',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',22,1763,'',47,11,3724511,1439267,'Austria','Europe',301,'',47.4333,11.7167,'WAHR','67807',27.5245998298,29.2915334001,28.6831065841,29.1097477586,24.6513087407,29.2671041065,32.9408,15.2906,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aflenz, Hochschwab',17,'','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'200',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','17','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',23,2370,'Abundance of micrite and cement uncertain. Age not well defined',47,15,3880278,1660012,'Austria','Europe',301,'',47.6167,15.1333,'WAHR','36450',19.4659095206,32.6904832918,22.3878502108,31.8254432384,25.6755553534,21.482937612,28.5504,17.4079,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Celje',18,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','80',NULL,NULL,NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin',NULL,NULL,'6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',24,0,'',46,15,1163535,2566730,'Slovenia','Europe',328,'',46.25,15.2667,'WAHR','36534',14.3818088572,36.0165897318,14.3818088572,36.0165897318,8.55589187104,25.091444435,6.1949,24.2289,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pokljuka',19,'','Triassic','Upper Triassic','Norian','middle/upper Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',206,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','20','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',24,0,'Halobian pockets within reef facies includes Pokljuka, Jelovica/Ratitovec and Bohinjska Bistrica reefs',46,14,2746166,1909337,'Slovenia','Europe',328,'',46.4,14.0333,'WAHR','36564',19.2696314044,31.1898020339,19.0905843757,31.2723207163,15.6171547344,23.1006475841,24.4212,16.6255,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hudajuzna and Cerkno area',20,'','Triassic','Upper Triassic','Carnian','early Carnian',233.00,235.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',226,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','26','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',24,27,'Bathymetry problematic. Quiet-water reef mounds Ladinian to Cordovolian Hudajuzna is Carnian according to Flügel (2002) and PBDB.',46,13,1234154,2463782,'Slovenia','Europe',328,'4',46.1833,13.7667,'WAHR','36558',15.7627553079,34.2616151043,15.7627553079,34.2616151043,9.78065466475,21.7591933852,11.7787,21.1428,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hohe Wand',21,'Dachstein','Triassic','Upper Triassic','Norian','Sevatian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'200','9',0,'Tropical or unknown','3','Ramp or Slope',NULL,NULL,'2','Below fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',28,40,'Dullo reference should be removed',47,16,3948518,1721953,'Austria','Europe',301,'',47.8167,16.25,'','170674',19.0189531939,33.364279942,21.9655021946,32.5303391542,25.5714007541,22.3374349476,28.3132,18.2499,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-20 13:22:33'),('Alichur, Pamir',22,'','Triassic','Middle Triassic','Ladinian','late Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',230,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','8',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',29,131,'Was Ladinian/Carnian.\nLadinian in PBDB',37,73,1232270,7987828,'Tajikistan','Asia',301,'',37.5833,73.3333,'WAHR','36694',40.5550698578,85.2689584988,40.5550698578,85.2689584988,4.57219319187,75.5633539667,6.02228,54.6735,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Schaimak, Pamir',23,'Shaimak','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',214,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','250','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'120',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','2','Below fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','22','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',30,31,'No reefal debris according to authors.\nHowever, bioclastic limestones were included in reef facies.\nShaimak 40-200 m thick, 500 m in places',37,74,3455347,8199692,'Tajikistan','Asia',301,'131, 2314',37.5,74.5,'WAHR','34646',47.4990239882,80.703239199,47.2942800417,80.7114717595,15.9725414617,80.2816824034,30.0306,54.4982,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Schachtessai, Pamir',24,'Bortepa','Triassic','Upper Triassic','Norian','Sevatian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','29',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',30,31,'Upper Sevatian\nIncludes data from Dzhilgakochusu reef',37,74,3432005,8220865,'Tajikistan','Asia',301,'',37.3333,74.6667,'WAHR','34647',47.3635183854,80.9459465197,50.146112412,81.7512942793,18.1019256513,85.2279602158,33.296,57.2672,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mala Fatra',25,'','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species','5','2','Baffler guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',32,2613,'',49,18,4208163,1801241,'Slovakia','Europe',336,'',49.1667,18.8333,'WAHR','42541',38.8888183828,25.1484150237,38.8888183828,25.1484150237,28.7500193915,27.5711427422,29.7007,22.0867,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Panormide, Sicily',26,'','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','6','Calcisponges','4','Stromatoporoids','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','40','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',34,149,'',38,13,1856037,1379721,'Italy','Europe',344,'',38.1333,13.3833,'WAHR','36454',NULL,NULL,NULL,NULL,14.4443608949,18.0155399037,21.1865,10.6646,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monti Cadini, Dolomites',27,'Cassian','Triassic','Upper Triassic','Carnian','lower Carnian',233.00,235.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',225,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',35,68,'Some of the best examples of cryptalgal\r\npatch reefs intercalated in well\r\nbedded arenitic limestones of the uppermost\r\nCassian Formation can be studied along\r\nthe southern slope of the Cadini Mountains\r\nabout 400 m WNW of Forcella Maraia. ',46,12,1359945,2388636,'Italy','Europe',344,'',46.5833,12.25,'','170920',16.8639460607,34.0480776552,16.8639460607,34.0480776552,10.7551602754,21.1979672105,11.7788,20.8909,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gosaukamm',28,'Dachstein','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'200','9',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','41','1','Constructor guild','1','Present','1','Present','3','Pronounced zonation','3','Pronounced zonation','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',36,2370,'Collection only contains solitary corals',47,13,3803725,1564751,'Austria','Europe',301,'',47.4833,13.6,'WAHR','38148',20.1826410316,31.8843741135,23.0744294175,30.9735325654,25.9598711745,20.3676515581,29.0054,16.3366,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-20 11:37:31'),('Spiti, Himalaya',29,'Nimaloksa','Triassic','Upper Triassic','Norian','middle Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',209,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','35',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','6','Calcisponges','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','12','2','Baffler guild','1','Present',NULL,NULL,'2','Medium zonation',NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',37,1306,'Middle Norian\nsolitary corals dominant.\nCorals>sphinctozoans>chaetetids\n\nPart of abstract from 1306.\nThe Nimaloksa Fm. documents progradation of a carbonate ramp in the latest Camian (Lower Member), followed in the Early Norian by subtidal mixed carbonate/terrigenous sedimentation (Middle Member) and by platform carbonate deposits (Upper Member). Next, the major disconformity at the base of  the Alaror Group testifies to an extensional tectonic event, followed by rapid increase in quartzo-feldspathic detritus in the late Early Norian. Siliciclastic supply is reduced only during flooding stages, marked by oolitic ironstone or phosphatic condensed horizons (\'Juvavites beds\', \'Monotis shale\'). Cleaner waters foster local development of knoll reefs around the Early/Middle Norian boundary (\'Coral limestone\'). Accumulation rates gradually begin to decrease before the close of the Triassic, when the \'Quartzite series\' records a sharp regressive event, followed by renewed transgression at the base of the Kioto Group. ',32,78,-3947515,5066863,'India','Asia',501,'',32.1,78.1667,'WAHR','36386',-27.4835489191,58.0808186702,-27.7275579543,58.053617142,-34.6115267375,51.4577932841,-24.8587,48.0545,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hangrang, Kinnaur, Himalaya',30,'Nimaloksa','Triassic','Upper Triassic','Norian','middle Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',209,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','6','Calcisponges','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',37,1306,'See also reef 29.',31,78,-4046310,4948587,'India','Asia',501,'',31.8,78.5333,'WAHR','36388',-27.9097133798,57.9998154332,-28.1536002799,57.9716144702,-35.0390179913,51.3806389947,-25.2862,47.9847,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Granada',31,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',234,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','8','Serpulids, worms, vermetids','3','Microbes','11','Serpulids - algae - microbes',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',39,0,'',37,-3,657974,995545,'Spain','Europe',304,'',37.1667,-3.5833,'','',37.1667,-3.5833,NULL,NULL,7.24944551097,9.49578126743,2.59829,9.99759,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gesäuse',32,'Dachstein','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','34','2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',41,0,'The central reef facies (widespread in the Kalbling reef and Schildmauer reef) is defined by an autochthonous reef-framework (composed of corals,\r\ncalcisponges, algae, and many epizoans), which interfingers with quantitatively prevailing reef debris. The reef-framework consists of various biocoenoses (high growing corals, low growing corals, calcisponges, hydrozoa and bryozoa,\r\nsolenoporacean algae).',47,14,3849734,1617265,'Austria','Europe',301,'',47.5833,14.4667,'WAHR','36516',19.7914468936,32.3595110981,22.7010603852,31.4745027429,25.8202640328,21.0090171662,28.7674,16.9577,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-20 11:40:55'),('Jebel Wasa south',33,'Jebel Wasa','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',209,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'6',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','4','Stromatoporoids','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','17','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',818,187,'Reef debris dominates with 72% floatstones and 28% rudstones. Some large reefal blocks.\nPoint counting results: 60% pharetronid sponges, 13% chaetetids, 13% dijectoporids/spongiomorphids,  8% corals, 4% solenoporaceans, 2% crinoids.\n',24,55,-1487549,5025864,'Oman','Asia',503,'42',24.7,55.8667,'WAHR','24304',-8.94505862839,52.7876049554,-9.18014824774,52.7880194756,-17.5094084543,43.7128298156,-6.82581,42.3446,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lovere',34,'Camorelli','Triassic','Middle Triassic','Anisian','middle Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',243,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',43,0,'Pelsonian to early Illyrian\nBindstones formed by Spongiostromata adn tubiphytes crusts. subordinate binding organisms are worms, prostromates and encrusting foraminifera. \nWidespread micritization.',45,10,1394911,2200168,'Italy','Europe',344,'',45.8167,10.0667,'WAHR','67717',16.0587753856,34.4963650325,16.0587753856,34.4963650325,10.4438098041,24.1996253362,6.62279,22.6089,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jebel Kawr',35,'Misfah','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',212,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','50',NULL,NULL,NULL,'3','More than 100 m',NULL,'40',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','18','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',818,187,'Solenopraceans probably more important than sponges.\nWas Norian/Rhaetian.\nNorian according to Flügel (2002)',23,57,-1714955,5102584,'Oman','Asia',503,'44',23.1722,57.0583,'WAHR','24306',-10.6362363735,53.6121457338,-10.8728501837,53.6099239289,-19.2632124152,44.4153688771,-8.63871,43.1808,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Olang',36,'Recoaro - Upper Serla','Triassic','Middle Triassic','Anisian','upper Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,'1','Less than 10 m wide',NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','6','Calcisponges','7','Bryozoans','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'30','70','0',0,'no',0,'no','2','6 to 24 reef building species','18','2','Baffler guild','1','Present','1','Present','2','Medium zonation',NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',45,0,'Late Pelsonian\nPaleobiology data combined for two formations and several reefs\n\nReefs rarely in situ\n\nDifferent types:\n- mixed faunas\n- Olangocoelia (main reef builder)\n- bryozoans\n- corals',46,11,1393793,2380413,'Italy','Europe',344,'',46.75,11.9667,'WAHR','23570',15.2917489076,35.9676603172,15.2917489076,35.9676603172,9.95752207662,25.9473455462,6.59908,24.1161,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Karwendel, Innsbruck',37,'Wetterstein','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','40',NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'5','85','10',0,'no',0,'no','2','6 to 24 reef building species','19','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',46,2373,'Up to 40 m thick patch reefs seaward of Wetterstein platform.\nFramework composed of branching corals, sphinctozoans bound by microbial micrite, Tubiphytes, sessile forams, bryozoans and Ladinella.',47,11,2298263,2001274,'Austria','Europe',301,'1331',47.3,11.4,'WAHR','38140',17.2052046652,35.6256824226,17.2052046652,35.6256824226,11.0600580138,23.7139268982,8.54778,22.6101,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hafelekar',38,'','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'15',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',46,1331,'',47,11,2298600,2001117,'Austria','Europe',301,'',47.3028,11.4,'WAHR','45428',17.684084012,34.5014183158,17.684084012,34.5014183158,11.6154606322,21.4473661616,13.1634,20.6356,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Idrija',39,'','Triassic','Upper Triassic','Carnian','Cordevolian',227.00,237.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',227,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','3','Microbes','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',48,321,'Corals > spongiostromata crusts = sponges > algae > hydrozoa as reef builders.\nCordevolian',46,13,1224365,2472680,'Slovenia','Europe',328,'',46.1667,13.9167,'','',15.8429195986,33.8790536316,15.8429195986,33.8790536316,9.97473809106,20.9392047963,13.5543,20.4318,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Fischerwiese, Steinplatte',40,'Zlambach Beds','Triassic','Upper Triassic','Rhaetian','upper Rhaetian',201.30,204.00,18,'late Carnian - middle Hettangian',218,200,'Late Triassic (Rhaetian/Hettangian, 201.3 Ma)',201,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','51','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',50,51,'Capping facies of Steinplatte:\nFisher\'s coral garden',47,12,3776977,1487601,'Austria','Europe',301,'2372',47.6,12.5667,'WAHR','38141',27.2114611991,29.8649120348,28.3744486813,29.6924284555,24.3388652727,29.827136996,32.7523,15.9659,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Richthofen',41,'Cassian Dolomite','Triassic','Upper Triassic','Carnian','lower Carnian',233.00,235.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',226,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'12',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','2','Intense',0,'No or unknown reservoir potential',52,68,'MOJSISOVICS (1879: 248) was the first to describe the so-called Richthofen Reef which,\ndue to its typical wedging out into marly\nCassian basinal deposits, has become the\nclassical example of the \'dolomitic reefs\'\nof South Tyrol. Overall dolomitization\nhas largely obliterated its sedimentary\nstructures and faunal content so that it\ncannot be decided whether transported reef\norganisms in Cassian basinal sediments\nare derived from this and larger buildups\nof Cassian Dolomite,',46,11,1369629,2367266,'Italy','Europe',344,'',46.5333,11.9667,'','',17.0055115427,33.8987497999,17.0055115427,33.8987497999,11.2338019803,20.9030014,11.8502,20.6987,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monte Caramolo',42,'Calcari','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'11',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','90','10',0,'no',0,'no','2','6 to 24 reef building species','14','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',53,0,'8 species of pharetronid sponges, spongiomorphids, microbial crusts, Tubiphytes and some microproblematica..\n',39,16,373480,2253234,'Italy','Europe',344,'',39.8,16.1167,'WAHR','25260',10.7897411486,29.8404331632,10.7897411486,29.8404331632,6.30705701099,20.2033294448,5.03422,19.2646,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Malajon, Palawan',43,'Coron','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',201,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','40','2','10 - 100 m wide',NULL,'3','More than 100 m',NULL,'15',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',1,'yes','2','6 to 24 reef building species','9','2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',54,253,'Microfacies poorly preserved.\nMost probably Rhaetian (Kiessling and Flügel 2000).',12,119,1395497,13081211,'Philippines','Asia',563,'335',12.15,119.8167,'WAHR','24144',34.5394988038,141.857922015,34.5394988038,141.857922015,27.5331441198,139.111118739,33.2683,116.607,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hochkönig',44,'Dachstein','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'200','9',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','27','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',55,2370,'A platform margin reef complex of exceptional thickness. The central reef area consists of relatively widely spaced small patch reefs that did\r\nnot develop wave-resistant reef framework structures. The bulk of the sediment in the central reef area is coarse bioclastic material, provided by the dense growth of reef organisms and the wave-induced disintegration of patch reefs.',47,13,3778861,1530516,'Austria','Europe',301,'',47.45,13.0667,'WAHR','25261',20.4432140997,31.6163375451,23.3248192971,30.689013014,20.7146083578,26.2999962387,29.1772,15.9719,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-20 13:22:33'),('Kotel, Luda-Kamcia',45,'Kotel','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',209,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'10','90','0',0,'no',0,'no','2','6 to 24 reef building species','17','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',1494,0,'Reef limestone in olistolites.\nCoral (11 species), bryozoans and sponges. 17 species in total',42,26,1382680,2795677,'Bulgaria','Europe',319,'',42.9,26.5,'','',10.4295514159,34.8537119949,10.2389954241,34.9032002559,29.5821876033,36.0276523687,14.5097,24.2988,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pilot Mountains I, Nevada',46,'Luning','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',216,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','4a','Shallow basin','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',57,63,'Dated by Kriistan-Tollmann and Tollmann as lower Norian.\nGarfield Hills locality.\nPreviously thought to be of deep water origin, but microatolls indicate coral growth to sea level (Stanley, 2005).',38,-118,1590369,-5850439,'United States','North America',101,'140, 423',38.4083,-118.0167,'WAHR','45520',15.2869787975,-43.3903160991,15.3955347522,-43.3181078623,21.1283899894,-50.5246367287,12.8399,-55.2316,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lake Shasta, California',47,'Hosselkus Limestone','Triassic','Upper Triassic','Carnian','upper Carnian',228.00,230.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',214,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','13','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',57,63,'Stratigraphy first from Flügel (2002) as lower Norian. The corrections is from Andrea Fucelli, 2021 (upper Carnian). \r\nCoordinates estimated from the map from 1th (original) paper.\r\nBivalve borings.',40,-122,1990516,-6125440,'United States','North America',101,'2363',40.6,-122.05,'WAHR','33354',18.3597912607,-46.2174192076,18.4776840371,-46.1357858056,24.6023763438,-52.876607809,15.5912,-58.3598,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-12-26 22:09:49'),('Summit Peak, N-Wallowa Mountains, Oregon',48,'Martin Bridge','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',214,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','180','2','10 - 100 m wide','75','2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','3','Microbes','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1',NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','23','3','Binder guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1150,63,'Early Norian. Dachstein-type reef according to G. Stanley (coral-calcareous sponge reef mound)\r\nRCM Edit May 2015: Updated with semi-quantitative data from Martindale et al 2012. This changes the patch reefs from coral-sponge reef mounds to microbial-coral or microbial-red algal true reefs. Several of the patch reefs show subtle vertical and horizontal zonation of the diminutive framework builders although due to the small size of the framework builders, this is difficult to see in outcrop. Summit Point reefs are multiple stacked patch reefs, roughly 5-60m thick with skeletal and oncoidal wackestones to floatstones (oncoids, ooids, and intraclasts or skeletal debris) between reef buildups.',45,-117,2515801,-5521820,'United States','North America',101,'76, 140, 57, 435',45.5,-117.5167,'WAHR','38063',19.961991555,-42.5630247514,20.0677295819,-42.4729557542,27.3822359732,-46.8314088831,19.7899,-53.7103,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('South Vancouver, British Columbia',49,'Sutton Limestone','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','6','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',57,63,'Wrangellia terrane\nCollection is from Coral zone, Cowichan Lake, Vancouver Island ',48,-124,423526,-6449407,'Canada','North America',121,'106, 2363',48.8569,-124.2319,'WAHR','45379',31.6777031243,-70.4401165034,31.8455060092,-70.3314391557,35.0424860075,-91.653346093,-6.2783,-66.0372,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gravina Island, Alaska',50,'Nehenta','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',213,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','20','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',57,63,'',55,-131,632820,-7396108,'United States','North America',101,'2363',55.3333,-131.75,'WAHR','33424',39.5382158289,-71.8640349441,39.7090232331,-71.732927792,41.2311631744,-97.9977830404,21.9169,-69.6056,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('North Vancouver',51,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',57,63,'',50,-127,401973,-6755011,'Canada','North America',121,'',50.5,-127.6333,'','172167',34.1076064632,-71.9641360511,34.2786415941,-71.8510397517,36.5310833436,-94.4984764784,-4.80998,-68.3689,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Iliamna, Alaska',52,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','4','Basin','','Unknown','2','Below fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','10','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',57,63,'Depth estimated to be some 200 m according to 423.',59,-155,1829734,-8951891,'United States','North America',101,'423, 2363',59.5,-155.5,'WAHR','33407',52.6622314918,-81.0042621719,52.6622314918,-81.0042621719,58.0869677103,-52.4106831213,5.47097,-80.9865,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Uffenheim',53,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',235,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'30','70','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',58,0,'Placunopsis bioherm.',49,10,2523853,1798839,'Germany','Europe',331,'',49.5489,10.2261,'WAHR','67651',29.2851218113,28.1463657803,29.2851218113,28.1463657803,22.8289617968,22.135246208,16.3277,17.6754,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Marktbreit',54,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',235,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'30','70','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',58,0,'Placunopsis bioherm',49,10,2535372,1786781,'Germany','Europe',331,'',49.6703,10.1433,'WAHR','67650',29.3881128172,28.0503263536,29.3881128172,28.0503263536,22.9010716399,22.0143126519,16.413,17.5694,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Enslingen',55,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',235,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'30','70','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',58,0,'Placunopsis bioherm',49,9,2453349,1791874,'Germany','Europe',331,'',49.1167,9.75,'WAHR','67649',28.7868801124,27.9329724136,28.7868801124,27.9329724136,22.2974780759,22.1091914467,15.8032,17.5826,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('La Riba',56,'','Triassic','Middle Triassic','Ladinian','upper Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',231,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,'3','101-1000 m wide',NULL,'4','More than 1000 m','2000','20',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',59,251,'Langobardian\nMud mounds with reefal caps\nIndividual mounds up to 2 km in length.',41,1,1052651,1515760,'Spain','Europe',304,'',41.2833,1.1667,'WAHR','73813',19.1120249316,22.9264148744,19.1120249316,22.9264148744,9.79596771028,14.4479771923,5.48093,14.7169,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zhenfeng (Chen-feng), Guizhou',57,'Yangliujing','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',234,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'150',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','15','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',60,61,'Probably only small coral patch reefs\n(problems with Chinese text)\n\nSimilarity with German Wellenkalk is emphasized\n\nBelt striking NE-SW',25,105,1689915,10199691,'China','Asia',602,'662',25.25,105.75,'WAHR','78652',-7.22817840183,109.279153855,-7.22817840183,109.279153855,25.4056860646,116.710293448,17.0487,94.7012,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shizong+Ch-iu-pei, Yunnan',58,'Lanmu','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',234,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'150','57',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',60,61,'Continuation of barrier reef tract',24,104,1502302,10092141,'China','Asia',602,'',24.5,104.2,'WAHR','78654',-7.95888451743,107.850312289,-7.95888451743,107.850312289,25.1128841731,114.978099175,15.7102,93.7997,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mianzhu, Sichuan',59,'','Triassic','Upper Triassic','Carnian','Carnian',228.00,235.00,17,'Induan - early Carnian',235,230,'Late Triassic (Carnian, 232 Ma)',224,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'25',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',61,166,'',31,104,2470935,9770692,'China','Asia',602,'662',31.3167,104.2167,'','',9.76029803283,110.353189153,9.76029803283,110.353189153,42.1967191816,113.120529455,27.0529,90.4128,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yangmeibao, Huaxi, Guizhou',60,'Qinyan','Triassic','Middle Triassic','Anisian','Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',241,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','2','Algae','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','1','Red algae','10','90','0',0,'no',0,'no','2','6 to 24 reef building species','8','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',61,166,'Dominated by red algae and cyanophyceans.\nOthers are sponges, bryozoans and brachiopods.\n\nNo detailed description of facies.\n\nReef belt striking NE-SW.\n\nAccording to ref. 420, rich Anisian coral fauna in fore reef area.',26,106,1872564,10241138,'China','Asia',602,'420, 662, 60',26.4667,106.7333,'WAHR','78655',-9.34247070233,109.05049725,-9.34247070233,109.05049725,20.0552802254,119.729341763,13.6812,96.11,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Manang, Annapurna',61,'Tarap','Triassic','Upper Triassic','Norian','middle Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','30',NULL,NULL,NULL,'3','More than 100 m',NULL,'15',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','2','Below fair weather wave base','1','Corals','4','Stromatoporoids','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',62,1339,'Coral patch reefs during time of reduced terrigenous input.\nAdditionally hydrozoans, ostracodes, echinoids, filaments.\nRef. 1339:\nAfter initial opening of Neotethys in the Permian, thermal subsidence and deepening continued in the Triassic. In the Scythian, three pelagic nodular carbonate intervals of Early Griesbachian to Early Dienerian, Early to mid-Smithian and latest Smithian to earliest Aegean age are interbedded with shelfal shales (Tamba Kurkur Formation). Ammonoid- and conodont-rich condensed carbonates were deposited on the outer shelf, with maximum depths around 150 div 200 m reached during transgressive stages. The Anisian to lowermost Norian shelfal succession mostly consists of marly limestones and marls (Mukut Formation). Thick calcareous siltstones rapidly accumulated in the Carnian, testifying to a new stage of tectonic extension affecting the Tethys Himalayan passive margin. The thick Tarap Formation of largely mid-Norian age points to strong continuing subsidence. Interbedded siltstones and subarkosic sandstones (\'lower member\') are locally overlain by coral-bearing patch reefs (\'middle member\'). Chamosite-bearing hybrid arenites deposited at transgressive stages characterize the \'upper member\'. The Triassic succession is capped by subarkoses and quartzarenites, interbedded with dolomitic to bioclastic hybrid sandstones and silty limestones (\'Quartzite Series\') , in turn overlain by the Kioto Lime stone. ',28,83,-4724138,4903387,'Nepal','Asia',NULL,'',28.7,83.9667,'WAHR','67621',-33.5278979839,58.2861430169,-33.7722038935,58.2472757291,-40.6508969777,51.8400260353,-30.8982,48.3935,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mission Creek, Lewiston, Idaho',62,'Martin Bridge','Triassic','Upper Triassic','Norian','early Sevatian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','14','2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',435,438,'14 coral species described by ref. 438.',46,-116,2623685,-5436568,'United States','North America',101,'',46.3667,-116.7333,'WAHR','38377',20.7098393936,-41.8174556309,19.7923379924,-43.0173621036,32.5728879973,-45.5407966148,21.3666,-54.6119,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('New Pass, Nevada',63,'Augusta','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','6','2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',63,1474,'Only North American locality with abundant calcareous algae.\nOldest Triassic reef in North America.\nThree coral species, one hydrozoan (real) species.',39,-117,1049397,-5081629,'United States','North America',101,'',39.6,-117.4833,'WAHR','42552',23.0997278623,-39.0560217134,23.0997278623,-39.0560217134,17.4782577273,-45.5367795444,6.47445,-44.7044,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tudiya, Wenxingchang, Laolongdong, Beipei buildup group, Sichuan',64,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','70',NULL,NULL,NULL,'3','More than 100 m','100','50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','6','Calcisponges','7','Bryozoans','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'30','60','10',0,'no',0,'no','3','25 or more reef building species','26','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',221,65,'Reef dwellers: Echinoderms, brachiopods, gastropods, benthic foraminifera, and calcareous algae. Rock type and reef-related depositional characteristic: Reef core:  less sponge framestone and more bafflestone and sponge-Tubiphytes-cyanobacteria bindstone. Reef type: Skeletal mound at the carbonate intraplatform. Coordinates stated in text: 106.50 E, 29.87 N, 40 m (part thick-ness). Comments for Laolongdong from Tian & Wang, 2021: Reef builders: Frame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, hydrozoans, and bryozoans. Binding organisms: Archaeolithoporella, Tubiphytes, sclerosponge, and cyanobacteria. Reef dwellers: Echinoderms, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and less rugose corals. Rock type and reef-related depositional characteristic: Reef core: sponge and hydrozoan bafflestone. Reef flat: bioclastic Colaniella- bryozoan-crinoid packstone to grainstone and bryozoan-echinoderm wackestone with reef breccia. Reef crest: foraminiferal-algal wackestone to packstone Reef base: bryozoan-crinoid packstone. Reef type: Skeletal mound at the carbonate intraplatform. Coordinates stated in text: 106.51E, 29.89N 36.33 m thick.',29,106,-344299,8817091,'China','Asia',602,'206, 207, 235',29.9167,106.4333,'WAHR','36221',-11.3578109393,105.146782629,-11.3578109393,105.146782629,10.7586468186,124.002574057,7.98772,95.6738,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-19 21:54:43'),('Mad`ene el Mrakib, Mader Basin',4427,'unknown','Devonian','Middle Devonian','Givetian','lower Givetian',382.70,387.70,10,'Givetian - early Famennian',375,385,'Middle Devonian (Givetian, 385.2 Ma)',NULL,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','3','3','101-1000 m wide','1000','4','More than 1000 m','1200',NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','9','Stromatoporoids - rugose/tabulate corals - microbes - (bryozoans) - (algae) - (echinoderms)',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',3364,NULL,'A very extensively exposed biostromal unit hosting a very diverse reefal assemblage.\r\n\r\nOne of the best preserved reefal palaeoecosystems of this area is found in the Givetian of Mad`ene el Mrakib (Anti-Atlas, Morocco), exposing a vast, at least ~1.2 km2 area of reef strata.\r\n\r\nA surprising feature of this assemblage is the rather subordinate role of stromatoporoids, generally regarded as a main component of the shallow-water Devonian reefs.\r\nPachyporids and alveolitids dominating, branching forms dominating\r\n\r\nThe ecological succession is characterised by an upsection increase in the abundance and diversity of the reefbuilding biota, accompanied by a shift in the dominant morphotypes of tabulate corals from platy (pioneering and diversification stages) to branching and massive forms (climax stage).',NULL,NULL,NULL,NULL,'Morocco','Africa',NULL,NULL,30.735278,4.712778,NULL,NULL,NULL,NULL,-41.540071998,1.5970401264,-50.492401371,-2.13809653838,-48.2524,27.3371,'Kiessling','Kiessling','2024-02-13 11:58:30',NULL),('Opole',65,'','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'150',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'11','Siliceous sponges','1','Corals','4','Siliceous sponges - echinoderms - scleractinian corals - worms',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'3','Pronounced 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',66,1358,'Siliceous sponges at base. Corals important at the top\nSuccession:\nTop: Corals - rigid framework\nMiddle: Silic. sponges with encrinits\nBase: Siliceous sponges only losely distributed.\n\nOpen shelf environment\nAdditional fauna: brachiopods, pelecypods, gastropods, polychaetes, corals.',50,18,2970580,2229314,'Poland','Europe',301,'195',50.5667,18.0833,'WAHR','34729',30.6947483656,34.4538768725,30.6947483656,34.4538768725,26.1211766682,28.5089631039,18.6575,23.8532,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Acotambo',66,'Chambara','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'5','95','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',67,86,'Only brachiopods in collection',-8,-76,-3008044,-4788393,'Peru','South America',201,'87,  96',-8.75,-76.75,'WAHR','36994',-20.7424251824,-35.0943827504,-20.6432593118,-35.1669970646,-14.8336912278,-47.6242634355,-20.6048,-44.7596,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lagazuoi',67,'Cassian','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',68,0,'',46,12,1366028,2371581,'Italy','Europe',344,'',46.5333,12.0333,'','',16.9223096349,34.0342509161,16.9223096349,34.0342509161,11.1429721533,21.1655266413,12.2857,20.5388,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aghdarband',68,'','Triassic','Lower Triassic','Olenekian','Spathian',247.20,251.20,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',246,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'3',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','12','Foraminifera','13','Algae - encrusting forams','2','Green algae','20','80','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',70,0,'Poorly described\nProbably only lagoonal\nOldest known Acicularia (dasyclad)\nCoordinates corrected',35,60,1280157,5102913,'Iran','Asia',505,'',35.9833,60.85,'WAHR','73814',28.5220209554,77.5201783609,28.5220209554,77.5201783609,36.3214397469,68.591617981,-0.846413,55.6974,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Latemar, Dolomites',69,'Schlern','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',238,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','700',NULL,NULL,NULL,'4','More than 1000 m',NULL,'15',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','20','80',0,'no',1,'yes','3','25 or more reef building species','24','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation','1','Less than 30% micrite','3','More than 25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',143,72,'Was Upper Anisian-lower Ladinian.\nNow most likely upper Anisian (Zühlke et al. 2000).\nTotal buildup 700 m thick.\nEncrusting sponges and baffling red algae also present.\nSome coral colonies\n',46,11,1373706,2333328,'Italy','Europe',344,'1704, 1789',46.3833,11.5833,'WAHR','49932',15.3634363632,35.5053352777,15.3634363632,35.5053352777,10.2327155952,25.3947386738,6.47341,23.6795,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Epinal',70,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',235,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'30','70','0',0,'no',0,'no','1','Less than 6 reef building species','1','3','Binder guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',73,0,'Placunopsis bioherm.',48,6,2213708,1621467,'France','Europe',331,'',48.1667,6.4333,'WAHR','73865',27.3260390642,25.79175803,27.3260390642,25.79175803,20.3324987203,20.6518261658,14.0212,15.9369,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mottgers',71,'','Triassic','Middle Triassic','Anisian','Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',241,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'1','Less than 20 m','2',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','15','Non-rudist bivalves','8','Serpulids, worms, vermetids','16','Serpulids - bivalves - (microbes)',NULL,NULL,'35','65','0',0,'no',0,'no','1','Less than 6 reef building species','2','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',74,0,'Placunopsis bioherm.\nAdditional frame builders are polychaets.\nOther fossils: crinoids',50,9,2594141,1722529,'Germany','Europe',331,'',50.3,9.6833,'WAHR','34703',29.0293133841,28.5849693513,29.0293133841,28.5849693513,22.8575690654,23.8433302621,16.0727,19.0709,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Begunjscica',72,'','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','20','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',75,0,'',46,14,2749848,1911266,'Slovenia','Europe',328,'',46.4333,14.0333,'WAHR','36572',25.6846019866,29.6730011367,25.6846019866,29.6730011367,22.0376813006,28.6801569687,31.1035,15.3227,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('W-Ceram',73,'Asinepe Limestone','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'15',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',77,0,'',-3,128,-4032179,10622824,'Indonesia','Asia',614,'',-3.25,128.6667,'WAHR','34892',-30.1240009079,112.345576853,-30.3358969063,112.449578925,-34.5254987436,104.741510507,-27.7444,100.984,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Central Ceram',74,'Asinepe Limestone','Triassic','Upper Triassic','Norian','Sevatian-Rhaetian',201.30,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',203,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','22','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',77,0,'20 species of corals and sponges described. Two added for encrusters',-3,129,-4113484,10672549,'Indonesia','Asia',614,'',-3.1667,129.6667,'WAHR','34893',-30.7867479241,113.217235602,-26.984638834,110.814064418,-39.2659600336,103.649317487,-26.781,98.5747,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Marawand, Delijan',75,'Nayband','Triassic','Upper Triassic','Norian','Sevatian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','80',NULL,NULL,NULL,'4','More than 1000 m',NULL,'25',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','7','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',9,1461,'Largest reef in Nayband Fm.\n80 m thick, 800 m lateral extension.\nWas Norian/Rhaetian.\nNow considered to be upper Norian\n\n\nAbstract of ref. 1461:\nSome small-scaled Norian-Rhaetian reefs and reef mounds are imbedded within the shales, siltstones and siliciclastic-carbonate deposits of the Nayband Formation in central Iran. These deposits belong to the central Iranian plate as part of the Cimmerian Continent. Most of the biogenic rocks have a biostromal geometry, biohermal\nconstructions are rare. Inozoid, sphinctozoid, and chaetetid sponges are, beside of corals and other reef builders, the most important reef organisms within these bioconstructions. In some reefs a variety of hexactinellid sponges also occur. The following inozoid sponges are described in this paper: Radiofibra norica n. sp., Permocorynella maxima n. sp., ? Sestrostomella robusta, Marawandia iranica, n. gen., n. sp. and Enaulofungia? triassica n. sp. The first four taxa are among the most abundant sponges within the Nayband Formation where it is exposed in several localities in central Iran. Enaulofungit? triassica, however, is not an abundant sponge there. These inozoid sponges have never been\nreported from the Triassic deposits of this region. Radiofibra, until now known only from the Upper Perrnian of Djebel Tebaga (Tunisia), is reported here for the first time from Triassic rocks. The stratigraphic as well as the\npaleogeographic distribution of all the genera are discussed. ',33,51,2927096,5311923,'Iran','Asia',505,'30',33.5667,51.4833,'WAHR','37960',21.6761199574,60.1638457353,26.359250245,60.6361376049,24.6026984295,64.025003497,33.1704,41.0511,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lakaftari, Esfahan',76,'Nayband','Triassic','Upper Triassic','Norian','middle Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',209,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','12',NULL,NULL,NULL,'2','10 - 100 m',NULL,'3',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',1,'yes','2','6 to 24 reef building species','9','2','Baffler guild','1','Present','1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',81,1461,'Bidestan Member Nayband Fm.\nCorals strongly bored.\nThamnasteria and solitary corals (Cuifia, Montlivaltia). Highly diverse sponge fauna.\nSponge dominated at the base, coral-dominated in central and upper part.\n12 m thick.\nSee reef 75 for further remarks',32,52,2896635,5399095,'Iran','Asia',505,'30',32.95,52,'WAHR','37983',21.2229788938,60.8099817182,20.8582693546,60.8203692463,21.1903892619,59.9546193891,30.381,39.8856,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tabas area including Parvadeh section',77,'Nayband','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'15',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','31','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',249,9,'See reef 75 for further remarks.',33,57,3616694,5743197,'Iran','Asia',505,'Baba, pers.',33.25,57.1667,'WAHR','36869',25.2113144857,67.1466173595,30.9553648753,67.2617271885,25.2499164929,69.2191800959,-12.232,44.7392,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Quebrada Granate',78,'','Triassic','Upper Triassic','Norian','Norian/Rhaetian',201.30,228.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',203,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'200',NULL,1,'Temperate','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','13','2','Baffler guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',78,127,'Slight bioerosion visible on figures.\nCoral diversity includes data from Portezuelo de la Sal, Chile',-24,-69,-5020880,-3424717,'Chile','South America',291,'',-24.75,-69.1667,'WAHR','34636',-36.3397441802,-23.8716338193,-36.2887475875,-24.0403689436,-29.1227526998,-40.2625803814,-34.7591,-33.0416,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gurumugl',79,'Kuta Limestone','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'13',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',79,88,'Typical alpine forams.\nCorals and solenoporaceans dominant.\nAdditional fauna: brachiopods, crinoids and ammonites.\nCollection is Rhaetian, but Sevatian is also present.',-6,144,-5016912,10860553,'Papua New Guinea','Oceania',615,'',-6.0167,144.8667,'WAHR','67687',-39.5240537727,119.047376832,-39.5240537727,119.047376832,-50.4288327128,119.193937244,-34.606,103.271,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hoher Göll, Bavaria',80,'Dachstein','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,'4','More than 1000 m wide',NULL,'4','More than 1000 m',NULL,'200','9',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'10','90','0',0,'no',0,'no','3','25 or more reef building species','61','1','Constructor guild','1','Present','1','Present','3','Pronounced zonation','3','Pronounced zonation','1','Less than 30% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2451,1376,'Many different facies types. Primary framework corals and calcisponges. Encrusted by forams, bryozoans and algae. \'Hydrozoans\' and Solenporaceans of minor importance. Organic framework to debris = 1:9 Most debris from cemented reef framework. Within reef 48 % organic origin. Carbonate cement 52 % Total: 62 % organic production. 20 genera (30 species) of sphinctozoans 10 genera (20 species) of inozoans 8 chaetetid sponge taxa 3 disjectoporids Gastrochaenid and lithophagid macroborings',47,13,2926642,1923551,'Germany','Europe',331,'1510, 2541',47.6333,13.1667,'WAHR','58093',20.5046365229,31.8142674147,23.3935685585,30.8881738801,26.2143456267,20.1361095023,29.2922,16.1528,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-20 11:47:05'),('Karaburun',81,'Laleköy','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'15',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','6','Calcisponges','2','Algae','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','9','2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',82,337,'',38,26,2104950,4067220,'Turkey','Asia',522,'',38.3333,26.5,'WAHR','73852',6.44924993435,35.3375558059,6.44924993435,35.3375558059,19.6834268963,36.4050749668,19.5366,31.2744,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chios',82,'','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'15','81',0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',82,0,'',38,26,2108751,4032661,'Greece','Europe',338,'',38.3833,26.1167,'','',26.043134707,42.2330901701,26.043134707,42.2330901701,19.5684063146,36.1055233908,19.8144,30.8314,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Waliabad',83,'Nayband','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'2',NULL,0,'Tropical or unknown','3','Ramp or Slope','','Unknown','2','Below fair weather wave base','6','Calcisponges','2','Algae','70','Spongiomorphids - siliceous sponges - pharetronids- corals','2','Green algae','5','95','0',0,'no',1,'yes','2','6 to 24 reef building species','12','1','Constructor guild','1','Present',NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',80,1461,'Abundant Oxycolpella.\nCodiacean limestones at base (Bouenia).\nStylothalamnia\nNeoguadalupia.\nSolitary corals predominate.',31,52,2752084,5622597,'Iran','Asia',505,'30',31.0333,52.8667,'WAHR','37044',29.74383737,64.5265280493,29.74383737,64.5265280493,24.0576615276,69.7545508076,33.7468,46.665,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monte Genuardo, Sicily',84,'','Triassic','Upper Triassic','Norian','Norian/Rhaetian',201.30,228.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',203,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'12',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','4','Stromatoporoids','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','21','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',83,0,'',37,13,1816634,1337757,'Italy','Europe',344,'',37.6806,13.1806,'WAHR','38061',NULL,NULL,NULL,NULL,12.152828537,16.4033949497,19.2217,10.6126,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Béchar',85,'','Carboniferous','Mississippian','Visean','upper Visean',330.90,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',332,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'6',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','11','Siliceous sponges','7','Bryozoans','14','Sponges - bryozoans - (microbes)',NULL,NULL,'70','0','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',84,0,'Upper Visean.\nUnusual Walsortian mound with large sponges.\n100-150 m water depth\nVertical zonation with sponge-dominated assemblages at base and sponge-bryozoan-crinoid facies above.\nAssociated: Rugose coral-microbial thickets.',31,-2,-2809331,172285,'Algeria','Africa',706,'',31.5667,-2.2667,'','',-47.2602894804,-13.5660776928,-44.1216640454,-11.2861029579,-26.3367867964,-27.8914949271,-22.7572,0.794545,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('El Capitan, Texas and McKittric, New Mexico',86,'Yates','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',262,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',1,'yes','3','25 or more reef building species','38','2','Baffler guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation','3','Pronounced zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',193,1368,'Submarine cement expecially important in reef edge and fore reef facies.\n\n34 sponge species according to ref. 1683.\nCollection data from Fagerstrom and Weidlich (1999)\n\nAbstract ref. 1368:\nThe Permian Capitan reef was a predominantly heterotrophic ecosystem strongly differentiated into open surface and cryptic communities. Unlike modern phototrophic coralgal reefs, most of the preservable epibenthos was housed within the cryptos and zonation developed only in the shallow parts of the reef. Contrary to established opinion, most sphinctozoan sponges did not grow upright to form a baffling framework but rather were pendent cryptobionts, as were nodular bryozoans and rare solitary rugose corals and crinoids. Indeed, many members of the cryptos were obligate    cryptobionts. Much of the Middle Capitan reef framework was constructed by a scaffolding of large frondose    bryozoans, with the subsidiary platy sphinctozoan Guadalupia zitteliana. Bathymetrically shallow areas of both the Middle and Upper Capitan reef, however, were characterized by platy sponges. In parts of the Upper Capitan, some platy sponges (Gigantospongia discoforma) reached up to 2 m in diameter and formed the ceilings of huge cavities which supported an extensive cryptos. In the absence of destructive forces (both biotic and physical) prevalent on modern reefs, the relatively fragile Capitan reef remained intact after the death of the constructing organisms. Rigidity was imparted to this community by a postmortem encrustation of Tubiphytes and Archaeolithoporella, together with\nmicrobial micrite. The resultant cavernous framework was partially infilled with sediment and preserved by\nsynsedimentary intergrowth of aragonitic botryoids and Archaeolithoporella. Extensive cement precipitation was\nfavoured by a number of factors including deep anoxia, which generated upwelling waters with elevated alkalinity.\nAlthough the accumulation rate of the Capitan may have been comparable to that of modern coralgal reefs, both the trophic structure and relative contributions of inorganic and organic carbonate were profoundly different. ',31,-104,484890,-3705133,'United States','North America',101,'85, 256,129,1683, 896',31.8728,-104.8583,'WAHR','24203',10.9093474899,-30.3165970674,10.9093474899,-30.3165970674,5.35392397197,-37.2500799735,4.06877,-33.4747,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shalypayco',87,'Chambara','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','10','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',86,87,'',-10,-75,-3282356,-4646073,'Peru','South America',201,'177',-10.85,-75.9833,'WAHR','36950',-22.7761040574,-34.1046155101,-22.6810567119,-34.1877621147,-17.005948594,-47.0919224625,-22.6027,-43.6897,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Huanincocha',88,'Chambara','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','8','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',87,86,'',-10,-75,-3284170,-4638149,'Peru','South America',201,'',-10.8667,-75.9167,'WAHR','36993',-22.7874318109,-34.032435853,-22.6926873145,-34.1156891746,-17.0299629536,-47.025943403,-22.6115,-43.6172,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pössneck',89,'Werrakarbonat','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',1,'Potential reservoir',89,128,'Stromatolites, bryozoans, algae',50,11,2157322,2586637,'Germany','Europe',331,'2424',50.6667,11.55,'WAHR','51381',26.8972449814,30.794988017,26.9006445531,30.7954943845,23.3280656582,27.0045295409,16.0326,23.1346,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Trogkofel',90,'Trogkofel','Permian','Cisuralian','Sakmarian','Sakmarian-Artinskian',283.50,298.90,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',284,3,'0','Outcropping reef ',3,'Mud mound or bank','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','9','Tubiphytes','3','Microbes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',90,2476,'Archaeolithoporella and Tubiphytes',46,13,119731,3139642,'Austria','Europe',301,'',46.5778,13.1972,'WAHR','61258',-9.85537984928,29.5410028605,-9.85537984928,29.5410028605,-4.81236611677,11.8155064899,-7.26554,24.8446,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kusunluk Hill, Bucakdere, Isparta',91,'','Triassic','Upper Triassic','Carnian','Carnian',228.00,235.00,17,'Induan - early Carnian',235,230,'Late Triassic (Carnian, 232 Ma)',221,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2602,91,'biostromes with corals and sponges\nSlice changed from 17.',37,31,817041,2571129,'Turkey','Asia',522,'',37.5333,31.15,'WAHR','73853',4.76889349461,38.0268933837,4.76889349461,38.0268933837,0.526083523026,26.8892610359,-0.133277,26.0223,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dereköy',92,'','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',214,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100','1',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','6','Calcisponges','4','Stromatoporoids','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',2377,1376,'Thallophytes microborings',36,30,748238,2477193,'Turkey','Asia',522,'91',36.75,30.3333,'WAHR','38047',8.07547856924,35.543421456,7.88284328449,35.5852134168,4.99351604127,27.2424795222,9.74247,21.1829,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Triglav',93,'','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','15','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',91,92,'Includes Rdeci rob reef',46,13,2754012,1899174,'Slovenia','Europe',328,'24',46.4,13.8833,'WAHR','36566',19.3496214345,31.1203024802,22.2134731884,30.2309321951,19.5686393554,25.9627506129,27.9936,15.8441,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Negaia Hill, Cimp Moti, Vascau',94,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','12','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',91,0,'',46,22,1998441,2706873,'Romania','Europe',348,'',46.4667,22.5,'WAHR','60388',14.9679725634,35.3129673345,14.7759998431,35.3765906699,19.6252663029,21.2738291281,19.0381,23.7351,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aldan River, Siberia',95,'','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',524,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','10','Archaeocyaths','3','Microbes','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',93,1045,'',58,129,-1848967,-196095,'Russia','Asia',624,'1093',58.5,129.5,'WAHR','80866',6.26748423912,-75.4848709174,6.26748423912,-75.4848709174,6.26748423912,-75.4848709174,-10.7096,-16.2827,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Riepl',96,'','Triassic','Middle Triassic','Anisian','upper Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','9','Tubiphytes','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',94,0,'',46,14,1224624,2536151,'Austria','Europe',301,'',46.4833,14.6,'WAHR','67646',13.5646550194,36.5868218102,13.5646550194,36.5868218102,8.5781930486,27.163178746,5.29473,25.4041,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sonora',97,'Antimonio','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',95,2347,'Oyster-like corals near the top of biostromes',30,-112,715027,-5541052,'Mexico','North America',105,'',30.7333,-112.55,'WAHR','34983',11.7282519579,-43.3224219656,11.8366011593,-43.262833107,13.7418221142,-49.7028491912,6.65565,-51.477,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pualaca, NE-Timor',98,'','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','11','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',97,328,'',-8,125,-4184662,9337854,'Timor','Oceania',NULL,'',-8.8167,125.95,'WAHR','21166',-30.6915148024,99.2128763723,-27.6300846791,98.1042725673,-42.3801224819,95.0655805961,13.1372,127.809,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('SW-Timor',99,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',97,328,'',-9,123,-4140754,8986116,'Indonesia','Asia',614,'',-9.8,123.9833,'','',-30.3242919577,96.7237923177,-30.5683133936,96.7917423327,-40.2479711854,94.5696494727,8.18962,121.962,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alsóhegy Plateau',100,'Wetterstein Limestone','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'4',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',99,91,'Check position!',46,17,2499895,2414900,'Hungary','Europe',336,'',46.8667,17.3,'WAHR','38050',14.0442873931,36.3243896057,14.0442873931,36.3243896057,14.477623631,18.7430955988,8.07787,25.817,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gela, Sicily',101,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,1,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','3','Microbes','3','Microbes',NULL,NULL,'2',NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',100,0,'',37,14,1685632,1384304,'Italy','Europe',344,'',37.0833,14.25,'','172798',NULL,NULL,NULL,NULL,9.00494714432,15.6637443531,16.5027,11.3769,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rhätikon',102,'','Triassic','Upper Triassic','Rhaetian','upper Rhaetian',201.30,204.00,18,'late Carnian - middle Hettangian',218,200,'Late Triassic (Rhaetian/Hettangian, 201.3 Ma)',201,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'14',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',101,0,'',47,9,3605012,1321683,'Switzerland','Europe',331,'',47.0667,9.7167,'','172799',28.2961797143,27.9611746283,29.4438323718,27.7567099274,25.4223577372,27.9691889342,33.5955,14.7852,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mratinje, Bosnia',103,'','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',102,0,'Some forams but no corals figured.\nWell description.',43,18,638944,2633635,'Bosnia and Herzegovina','Europe',328,'',43.25,18.7,'','',11.17620952,33.849578991,11.17620952,33.849578991,5.25850961939,22.9945226388,6.96076,22.7373,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mine Verhny, Sichote Alin',104,'','Triassic','Upper Triassic','Norian','Norian-Rhaetian',201.30,228.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',203,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','6','Calcisponges','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,'3','Pronounced zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',103,1359,'Only corals mentioned.\n8 species in reef frame, table reef.\nAstraeomorpha, Retiophyllia, Heterastrea, Protoheterastrea, Volzeia, Margarosmilia are the genera of Mine Verhny.\n15 % \'hydroids\'\n25 % sponges\n10 % corals\n20 % algae\n30 % mollusca and others\n\nOther reefs in area are Sakharnaya Mountain, Verkhnij Rudnik, Bolnichnaya Mountain, Kamennya Vorota, Partizansky Massif.\n\nUpper Carnian to Rhaetian corals:\nVolzeia badiotica - upper Carnian\nMargarosmilia charlyana - lower Norian\nGablonzeria kiparisovae - middle Norian\nMeandrostylis tener - upper Norian\nRetiophyllia buonamici - Rhaetian',44,135,4953076,14353038,'Russia','Asia',624,'1360, 1432',44.5167,135.5167,'WAHR','42751',55.6058367395,157.460863685,54.9969427414,156.939796833,70.1241822415,170.485497653,49.5947,137.983,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bleiberg',105,'','Triassic','Middle Triassic','Anisian','upper Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','9','Tubiphytes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',104,0,'Short abstract only.\nExtension of reef facies probably overestimated.\nLocality not clear.',46,13,1286708,2484943,'Austria','Europe',301,'',46.6167,13.7,'','',14.1734501863,36.4076514035,14.1734501863,36.4076514035,9.07841912427,26.7703708669,5.77045,24.9843,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lattari Mountains',106,'','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','11','Serpulids - algae - microbes',NULL,NULL,'70','30','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',105,136,'',40,14,2075278,1605105,'Italy','Europe',344,'215, 2173',40.6167,14.4667,'','172809',21.3770166342,25.3943988132,21.3770166342,25.3943988132,18.9337248588,22.5035037239,25.9701,12.1869,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Telkwa Range, British Columbia',107,'Nilkitkwa','Jurassic','Lower Jurassic','Sinemurian','upper Sinemurian',190.80,199.30,19,'late Hettangian - early Aalenian',188,195,'Early Jurassic (Hettangian&Sinemurian, 196 Ma)',191,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','48',NULL,NULL,NULL,'2','10 - 100 m','45',NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','6','2','Baffler guild','1','Present','1','Present','2','Medium zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',107,164,'Stikinia terrane.\nNilkitkwa Fm.\n44 m thick reef\n5 coral species in total.\nBioerosion intense (Lithophaga).\n\nAbstract ref. 426:\nAn Early Jurassic (Sinemurian) reef in Telkwa Range, British Columbia, Canada, yields coral species previously known from Morocco, Great Britain, Italy, Peru, and Chile. The principal constructional coral, Phacelostylophyllum rugosum (Laube), known from the Upper Triassic Dolomite Alps in northern Italy, is a holdover species. This coral survived the mass extinctions of the end-Triassic without leaving any other Jurassic records outside Canada. Other corals from the Telkwa reef include Stylophyllopsis victoriae (Duncan) and Actinastraea minima Beauvais known from Jurassic rocks of the Tethys. Closely related corals, Phacelostylophyllum chocolatensis (Wells) and Actinastraea plana (Duncan), are from southern Peru. The paleogeographic occurrence of the Canadian reef in the volcanic terrane of Stikinia supports the contention that volcanic islands in distant outposts of the ancient Pacific served as refugia. In the aftermath of the end-Triassic reef decimation affecting the Tethys, corals and reef-building activities continued on ancient islands of the ancestral Pacific. The Hispanic Corridor, connecting the western Tethys with the western Pacific, may have played an important role during Sinemurian time. ',54,-127,4213345,-6976434,'United States','North America',101,'426',54.3833,-127.1333,'WAHR','21251',40.4399168717,-61.1589357741,40.4399168717,-61.1589357741,51.068062605,-50.2912534689,26.7477,-69.4371,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Demascota well, Nova Scotia',108,'Abenaki','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','9','Tubiphytes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',109,456,'According to ref. 456 Stromatolite-Tubiphytes bioherms in deeper neritic enrivonment.\n',43,-60,3678610,-1482119,'Canada','North America',121,'466, 827',43.6908,-60.8317,'WAHR','67976',22.11389992,-3.286199134,22.11389992,-3.286199134,27.7900332898,-4.97501186715,33.6923,-10.0132,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Demascota well, Nova Scotia',109,'Abenaki','Jurassic','Upper Jurassic','Tithonian','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',147,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','11','Siliceous sponges','46','Corals - siliceous sponges - (algae) - (bryozoans) - (crinoids)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',109,456,'In the Berriasian development of lithistid sponge bioherms.',43,-60,3487141,-1883556,'Canada','North America',121,'466, 827',43.6908,-60.8317,'WAHR','67978',23.5210392851,-6.97553057082,23.5210392851,-6.97553057082,29.4858710092,-8.30059627708,35.2009,-12.7245,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cohasset well, Nova Scotia',110,'','Jurassic','Upper Jurassic','Tithonian','Tithonian',145.00,152.10,22,'late Tithonian - early Valanginian',141,150,'Late Jurassic (Tithonian, 148.6 Ma)',147,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100','109',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',109,0,'',43,-60,3521491,-1854260,'Canada','North America',121,'',43.9436,-60.4997,'','',23.7239112917,-6.66655478479,23.7239112917,-6.66655478479,29.6881517333,-7.97457740718,35.4335,-12.4068,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Suplee-Izee, Oregon',111,'Robertson','Jurassic','Lower Jurassic','Pliensbachian','Pliensbachian',182.70,190.80,19,'late Hettangian - early Aalenian',188,185,'Early Jurassic (Pliensbachian, 186.8 Ma)',187,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'10','90','0',0,'no',0,'no','1','Less than 6 reef building species','1','2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',110,1252,'Lithiotis bioherm, almost monospecific.\nAbstract of ref. 1252:\nThe epifaunal, rudist-like bivalve Lithiotis formed extensive bioherms during the Pliensbachian and Toarcian ages of the Early Jurassic. The best developed bioherms in North America occur in the Pliensbachian Robertson Formation of east-central Oregon, a unit deposited in a shallow sea transgressing across the Suplee shelf. A typical bioherm consists of three biofacies that coexisted laterally and replaced each other vertically. The reef flank assemblage is the most diverse consisting of Nerinea gastropods, terebratulid brachiopods and Lithiotis debris in a calcarenite or calcilutite matrix. The death assemblage consists of tightly packed, current-aligned Lithiotis valves with gastropods and brachiopods much reduced in numbers. The core of the reef is built almost exclusively of in situ Lithiotis forming a bafflestone with a calcilutite matrix. Lithiotis inhabited a stressful environment inimical to most invertebrates since diversity is very low and there is no evidence of bioerosion. During the Pliensbachian, Lithiotis formed an endemic centre encompassing western North America and the Tethyan Ocean, linked through central America and the central Atlantic by the Hispanic Corridor. By the close of the Pliensbachian it had disappeared from North America but in the Toarcian made its first appearance in South America. By the end of the Toarcian, Lithiotis was extinct. ',44,-119,3390579,-5984661,'United States','North America',101,'',44.05,-119.6833,'WAHR','21259',32.5718761076,-47.8457277248,32.5718761076,-47.8457277248,41.689893506,-50.3791546595,29.3093,-56.0165,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bullmoose Mt., British Columbia',112,'','Cretaceous','Lower Cretaceous','Albian','Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',108,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick','1',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','74','Non-rudist bivalves only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','2','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',111,0,'Almost monospecific Ostrea bioherm (20 m length, 1.4 m thickness) in siliciclastic intertidal environment.',55,-121,6590930,-5576846,'Canada','North America',121,'',55.2167,-121.5167,'WAHR','45360',56.7741248931,-65.6301357392,56.7741248931,-65.6301357392,58.5643559107,-72.9295946012,57.3787,-71.3855,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Acadia, Nova Scotia',113,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian/Kimmeridgian',157.30,157.30,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100','108',0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',112,827,'Thrombolite bioherms without sponges\nFew in situ corals',42,-61,3565168,-1576617,'Canada','North America',121,'',42.8622,-61.9167,'','',21.6944921525,-5.26400346877,21.6944921525,-5.26400346877,27.5176669021,-6.89594482421,33.3703,-11.86,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Demascota well, Nova Scotia',114,'Abenaki','Cretaceous','Lower Cretaceous','Valanginian','Valanginian',132.90,139.80,23,'late Valanginian - early Aptian',126,135,'Early Cretaceous (Valanginian, 136.4 Ma)',138,1,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','11','Siliceous sponges','9','Tubiphytes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,'10','30','60',0,'no',0,'no','2','6 to 24 reef building species','13','3','Binder guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',113,0,'Higher algae almost absent.\nEsentially sponge-tubiphytes bioherm\nLithistids (Gilletia-type) together with abundant Tubiphytes, and subordinate sclerosponges and nodular stromatoporoids (Ellipsactinia, Sphaeractinia) developed on a deep shelf margin, accompanied by lenticulinid and trocholinid foraminifers. The sponge mound organisms have Tethyan affinities.',43,-60,3487141,-1883556,'Canada','North America',121,'',43.6908,-60.8317,'WAHR','45348',25.6064017653,-6.95087314474,25.6064017653,-6.95087314474,31.072981702,-10.2129236685,35.1464,-13.6096,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Prince Patrick Island I',115,'Christopher','Cretaceous','Lower Cretaceous','Albian','Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',105,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','8','2','10 - 100 m wide',NULL,'2','10 - 100 m','60','9',NULL,2,'Cold - water','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','8','Serpulids, worms, vermetids','15','Non-rudist bivalves','16','Serpulids - bivalves - (microbes)',NULL,NULL,'95','5','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',114,718,'Methan seep related lithoherm',75,-120,8377144,-2259607,'Canada','North America',121,'',75.1333,-120.0528,'','',73.1837552589,-37.1947710923,73.1837552589,-37.1947710923,72.7132385589,-38.139199282,74.4055,-31.6262,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Prince Patrick Island II',116,'Christopher','Cretaceous','Lower Cretaceous','Albian','Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',105,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','3',NULL,NULL,NULL,'1','Less than 20 m','3','9',NULL,2,'Cold - water','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','8','Serpulids, worms, vermetids','15','Non-rudist bivalves','16','Serpulids - bivalves - (microbes)',NULL,NULL,'95','5','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',114,0,'See reef 115',76,-120,8426055,-2079517,'Canada','North America',121,'',76.2061,-120.125,'','',73.5441958573,-34.1177594775,73.5441958573,-34.1177594775,75.663935002,-39.6200755112,74.5297,-29.1557,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ellef Ringnes Island',117,'Christopher','Cretaceous','Lower Cretaceous','Albian','Albian',100.50,113.00,24,'late Aptian - middle Cenomanian',107,105,'Early Cretaceous (middle Albian, 107 Ma)',105,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','6',NULL,NULL,NULL,'1','Less than 20 m','15',NULL,NULL,2,'Cold - water','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','8','Serpulids, worms, vermetids','15','Non-rudist bivalves','16','Serpulids - bivalves - (microbes)',NULL,NULL,'95','5','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',114,718,'Christopher',78,-100,8156608,-1596683,'Canada','North America',121,'',78.1667,-100.2167,'','',71.4977809743,-19.6019617696,71.4977809743,-19.6019617696,73.5413737058,-23.3158582341,71.2321,-16.5183,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Holm Land, Greenland',118,'','Carboniferous','Pennsylvanian','Moscovian','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',309,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',115,0,'',80,-17,3403564,1146362,'Denmark','Europe',330,'',80.1667,-17.5,'','172810',20.7043465921,7.25528169992,20.7043465921,7.25528169992,19.9726083617,-13.1791042402,22.5323,9.23335,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Topuk + Tavuk Cesme, Isparta',119,'','Triassic','Upper Triassic','Norian','Lacian',220.00,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',215,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'100','1',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1377,2604,'Tectonically cut',37,31,793301,2602571,'Turkey','Asia',522,'Link, pers.',37.6667,31.2667,'WAHR','73860',8.2233176147,36.627345108,6.67515065915,37.1394909048,3.05354721385,27.23800099,6.69149,23.0702,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rahatalana Yayla',120,'','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'100','1',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',1377,0,'Upper Norian\nGlide block',37,31,794164,2604814,'Turkey','Asia',522,'Link, pers.',37.6833,31.2833,'','',8.78381663014,36.5243941895,11.8444605251,36.1117601496,8.78476920704,30.5072411553,10.0798,22.3535,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Swimming Woman, Big Snowy Mts., Montana',121,'Lodgepole','Carboniferous','Mississippian','Tournaisian','Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',358,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'150',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','4','4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',116,273,'Bryzoans are dominant macrofossils.\nOther fossil than bryozoans relatively rare.\nCement and micrite are main constituents.\n',46,-109,-542377,-4715064,'United States','North America',101,'370',46.7667,-109.35,'','',-14.6825569324,-53.7596137367,-14.6825569324,-53.7596137367,4.38543343837,-99.2703865876,-7.30442,-43.2951,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bridger Range, Montana',122,'Lodgepole','Carboniferous','Mississippian','Tournaisian','Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',358,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'150','121',0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',116,370,'',45,-110,-520858,-4875920,'United States','North America',101,'',45.8167,-110.9333,'','',-13.9142046336,-55.0272680136,-13.9142046336,-55.0272680136,4.49812370797,-100.719234023,-7.15992,-44.7483,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cedar Creek, Williston Basin, Montana',123,'Lodgepole','Carboniferous','Mississippian','Tournaisian','Kinderhookian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',358,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',116,2008,'Abstract ref. 2008:\nBuildups in the Lodgepole Formation were deposited throughout the Kinderhookian to Osagean Williston Basin. The Williston Basin was tectonically active at this\ntime as the depositional axis of the basin was shifting from a northerly connection to the ocean through the Elk Point Basin in Alberta to a westerly connection through\nthe Central Montana Trough. This structural setting provided a range of depositional sites for buildups to develop on shelves, ramps, intrabasinal blocks and around\nintrashelf basins. \n     A textural, compositional and geometric range of buildups record a spectrum of depositional processes from hydrodynamically deposited grainstone shoals to\norganically mediated reefs and mud-dominated mounds. Geometries range from lens-shaped shoals and banks to mounds. Lensoidal buildups are associated with\ncoarser grainstone and packstone textures as well as other shallow water indicators such as ooids and, or, photoautotrophic corals. Mound-shaped geometries\ngenerally are dominated by muddier textures and are associated with deeper-water indicators such as filter feeding organisms with delicate skeletons. \n     A textural spectrum of buildups ranges from mud-dominated with few bryozoans and crinoids, to crinoid, bryozoan grainstones with, and without, coral\nframestones or ooids. Mud dominated buildups are best exemplified by mud mound outcrops in two locations in the Bridger Range in Montana. The coarsest\nbuildups are exemplified by coral, crinoid, bryozoan reefs at two outcrops in the Little Belt Mountains in Montana, and by crinoid, ooid grainstones in the subsurface\nof  Manitoba (Canada), and along the Cedar Creek Anticline in North Dakota and Montana. Mound complexes comprised of a broad mixture of textures from\ngrainstones and organically mediated wackestones and mudstones are known from three outcrops in the Big Snowy Mountains in Montana, and drill cores from\nSaskatchewan (Canada), and Montana and North Dakota. \n     Buildup textures, compositions and depositional styles vary according to paleodepositional location in the Lodgepole sea as a response to hydrodynamic\nvariations, trophic requirements and water qualities. The occurrence of organically mediated buildups is widely distributed: 1) on, or around, intrabasinal blocks and\nbasins, 2) on the basin floor, 3) at the base of, or across the slope/ramp, or 4) near the top of the slope/ramp. Grainstone shoals and sheet sands were deposited on\nthe Lodgepole shelf near the break in shelf slope or high on the ramp. The spectrum of buildups reflects the wide range in environmental variables and the diversity of\nsettings for buildups to develop in the Lodgepole sea. ',46,-104,-927813,-4474587,'United States','North America',101,'',46.2,-104.3667,'','',-18.1041420482,-53.11389716,-18.1041420482,-53.11389716,1.62531046362,-97.1524242219,-10.0975,-41.1996,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wilsons Brook, New Brunswick',124,'','Carboniferous','Mississippian','Visean','Visean',330.90,346.70,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,2,'Cold - water','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','15','Algae - microbes - (encrusting forams) - (rare songes)',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',117,0,'Additional serpulid worm tubes\nHydrothermal vent setting?',45,-64,-1551955,-1178575,'Canada','North America',121,'',45.8506,-64.7139,'','',-34.6655104105,-27.9043612504,-34.6655104105,-27.9043612504,-12.1813365422,-54.8760478626,-14.5831,-14.0399,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Havelock, New Brunswick',125,'','Carboniferous','Mississippian','Visean','Visean',330.90,346.70,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','1','Red algae',NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',117,1517,'',45,-65,-1521997,-1221662,'Canada','North America',121,'',45.9972,-65.3083,'','',-34.338589603,-28.259326716,-34.338589603,-28.259326716,-11.9339569788,-55.2465102378,-14.3616,-14.431,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Devondal, Greenland',126,'unknown',' 	Permian','Guadalupian',NULL,'Guadalupian',259.80,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',265,1,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'1',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',118,232,'Reef formed elongated ridge',71,-22,3907694,1573147,'Denmark','Europe',330,'',71.5833,-22.8333,'','',31.0882799763,20.9530568225,31.0882799763,20.9530568225,29.2636704061,9.93373489149,27.6191,17.5262,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aguathuna, Newfoundland',127,'','Carboniferous','Mississippian','Visean','Visean',330.90,346.70,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'6',NULL,0,'Tropical or unknown','4','Basin','4b','Deep basin (> 200 m)','2','Below fair weather wave base','7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'90','10','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium 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',119,1819,'Bryozoan-microbial bioherms.\nAdditional serpulid worms (vent associated tube worms).\nRef. 721 with completely different interpretation but convincing arguments.\nBathymetry: at least 100 m instead of 10 m.',48,-58,-1248530,-690614,'Canada','North America',121,'721',48.65,-58.7333,'WAHR','76873',-33.8027619348,-22.033623843,-33.8027619348,-22.033623843,-10.281372486,-50.238953862,-12.3628,-9.51444,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Blue Mountains, Ellesmere Island, Nunavut',128,'Hare Fjord','Carboniferous','Pennsylvanian','Moscovian','early Moscovian',310.00,315.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',310,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','300',NULL,NULL,NULL,'4','More than 1000 m',NULL,'20',NULL,1,'Temperate','4','Basin','4a','Shallow basin','2','Below fair weather wave base','7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','10','10',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',120,2494,'Waulsortian type reef mounds dominated by fenestellid bryozoans.\nMicrobes responsible for early marine cementation\nAdditional fossils: crinoids, forams, algae, sponges',80,-85,3914395,163514,'Canada','North America',121,'',80.75,-85.5,'WAHR','62695',24.5130194665,-1.81885278435,22.9953387746,-2.64804656708,23.8480976177,-22.5878197985,26.2935,-0.456896,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Arthaber Creek, Axel Heiberg Island, Nunavut',129,'Nansen','Carboniferous','Pennsylvanian','Moscovian','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',309,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','180',NULL,NULL,NULL,'3','More than 100 m','800','1',NULL,1,'Temperate','4','Basin','4a','Shallow basin','2','Below fair weather wave base','7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'70','0','30',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',120,0,'Large Waulsortian type reef mound',80,-95,4053737,18930,'Canada','North America',121,'',80.55,-95.4667,'','',25.5815642979,-3.17680250017,25.5815642979,-3.17680250017,27.289085941,-24.8317189476,27.8614,-1.29896,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hare Fjord, Ellesmere',130,'Otto Fjord','Carboniferous','Pennsylvanian','Bashkirian','Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,320,'Early Pennsylvanian (Bashkirian, 319.2 Ma)',316,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','2','Algae','2','Algae','13','Algae - encrusting forams','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',121,316,'Tubular beresellid and donezellid algae form framework\nCyclic processes controlling buildup-growth\n\n',81,-81,3902257,264033,'Canada','North America',121,'',81.25,-81,'','',16.1659748263,-5.25162347367,16.1659748263,-5.25162347367,16.7741064249,-20.2597033653,24.2028,-1.63676,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Westerstein, Harz',131,'','Permian','Lopingian','Changhsingian','Zechstein 2',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',257,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',122,270,'One of the best developed Zechstein reefs.\nBryozoans especially at seperated cliffs (fore reef).',51,11,2269631,2515251,'Germany','Europe',331,'',51.6333,11.0833,'WAHR','75575',27.7814076119,30.2454758825,27.7848026129,30.2459560812,23.9834417803,26.1655946429,16.8526,22.5198,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Römerstein, Harz',132,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','20','0',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',122,270,'',51,11,2271736,2526842,'Germany','Europe',331,'2424',51.6167,11.25,'WAHR','51382',27.7867504848,30.3637913448,27.7901464964,30.3642751799,24.0254169983,26.2707259232,16.8703,22.6278,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Schale',133,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',123,0,'Detailed petrographic analysis by Füchtbauer (1980).\nExtension unknown.\nComplex dolomitisation and dedolomitisation',52,7,2285621,2283775,'Germany','Europe',331,'',52.3333,7.9667,'WAHR','75574',28.0914052628,27.9598081238,28.0947779069,27.9602128389,23.5635672169,23.9808603681,16.9301,20.3863,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Abenra',134,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'300',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',124,0,'Bryozoans only inferred by facies similarities',55,9,2669159,2268463,'Denmark','Europe',330,'',55.05,9.4333,'','',30.9243640592,28.337500732,30.9277407686,28.3378777692,26.3293282231,23.2132726317,19.7821,20.3968,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('E-Durham, England',135,'Ford','Permian','Lopingian','Changhsingian','Zechstein 2',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',257,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','4','3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',125,126,'Bryozoans, brachiopods and mollusks described.\nReef data compiled from several localities:\nHylton castle\nClaxheugh Railway Cutting\nRock Cottage\nMaiden Paps South and North\nRyhope Railway Cutting\nTunstall Hills East\nReef core facies: 24084\nReef base: 24085\nReef slope and talus: 24086',54,-1,2439445,1604252,'United Kingdom','Europe',331,'283',54.7833,-1.35,'WAHR','24084',29.6948518697,21.300076401,29.6981289407,21.3002375358,23.0549709453,17.4201657179,17.9505,14.1394,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Liebenstein',136,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20','89',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','3','Microbes','2','Algae','15','Algae - microbes - (encrusting forams) - (rare songes)','1','Red algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',128,0,'',50,10,2151645,2534744,'Germany','Europe',331,'',50.7667,10.8333,'','',26.9011280423,30.2739628088,26.904523288,30.274453461,23.1684295916,26.5295784811,15.9814,22.6541,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Karakorum, Kashmir',137,'','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',213,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',130,0,'Only fossils described.\nReef belt at least from Aksai tschin to northern part of \nKarakoram pass.',35,77,2887474,6077835,'Pakistan','Asia',501,'',35.55,77.85,'','',22.7639572946,74.0387681398,22.3128542058,73.8663957986,13.8022096446,82.8866024769,48.0725,72.5504,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Northern Caucasus',138,'Bolshoj Tkah\'c','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,1,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','220',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','2','Algae','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1','Red algae','5','95','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present',NULL,NULL,'2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',131,1413,'Upper part of Tkach and Bzheba rivers.\nPharetronids and solenoporaceans as main reef builders.\nScleractinia and stromatoporoids, bryozoans, cyanobacteria, encrusting forams are less abundant.',44,40,4677300,3544938,'Russia','Asia',624,'1430',44.0833,40.5,'WAHR','36722',36.5780638504,46.4040388997,36.3861244569,46.5042601925,36.6879294352,44.8030176792,38.5997,35.8352,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ussuri, Sichote Alin',139,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'15',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','12','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',131,1359,'No description of reef facies',44,133,5020880,14131926,'Russia','Asia',624,'',44.5,133.6667,'WAHR','36693',51.5737400868,151.892903589,50.9560903333,151.461922495,48.9851940438,156.788356641,49.2991,132.864,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Partizansk, Primorsky',140,'','Permian','Cisuralian','Kungurian','Kazanian',268.80,272.30,15,'Sakmarian - Kungurian',277,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',268,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','','Unknown',NULL,NULL,'2','Algae','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',131,0,'',43,133,4003820,16865909,'Russia','Asia',624,'',43.05,133.0833,'','',27.1685425243,139.455906426,27.1685425243,139.455906426,42.9680805235,130.731937549,28.4172,113.029,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nakhodka, Primorsky',141,'Lyudyanza','Permian','Lopingian','Wuchiapingian','Wuchiapingian',254.10,259.80,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',253,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','6','Calcisponges','7','Bryozoans','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',131,264,'Bryozans mentioned by ref. 131 and 2529 but not by 264.\r\nEvidence for both Wuchiapingian and Changhsingian age',42,132,3975360,16846309,'Russia','Asia',624,'2529',42.8667,132.6333,'WAHR','63899',20.7357660845,141.361671487,20.7356873572,141.356079131,32.7922334788,127.35408288,30.4509,111.81,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Karavan, Kirgiziya',142,'','Carboniferous','Pennsylvanian','Kasimovian','Kasimovian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown','3','Ramp or Slope','','Unknown','2','Below fair weather wave base','2','Algae','6','Calcisponges',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',131,0,'',40,72,3338941,6693439,'Kyrgyzstan','Asia',NULL,'',40.3167,72.1833,'','',16.2833168274,78.2333385769,16.2833168274,78.2333385769,32.8439214251,34.7199232465,26.7752,62.9819,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bakhchisaray, Krym',143,'unknown',' 	Permian','Guadalupian',NULL,'Guadalupian',259.80,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',265,1,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'6','Calcisponges','6','Calcisponges',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',131,0,'Olistostrome',44,33,2253366,4393589,'Ukraine','Europe',301,'',44.7333,33.8833,'','',16.3154663936,44.8054546022,16.3154663936,44.8054546022,24.7892160294,39.2122805086,14.1094,41.7377,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Areni, Armeniya',144,'','Permian','Cisuralian','Kungurian','Kazanian',268.80,272.30,15,'Sakmarian - Kungurian',277,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',268,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'6','Calcisponges','6','Calcisponges',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',131,0,'Very poor description',39,45,228053,4377740,'Armenia','Europe',526,'',39.7167,45.2,'','',-8.03773222439,51.4660638723,-8.03773222439,51.4660638723,1.68623217813,40.8799799371,-10.454,42.464,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Coron Island',145,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,1,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'15',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',54,253,'Reefal facies only in reworked blocks',11,120,1372779,13131880,'Philippines','Asia',563,'',11.9333,120.2167,'','',21.3755821995,133.019443811,20.6146280588,132.82491481,30.0095977722,130.359795416,25.6998,107.873,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Szentantalfa',146,'Tagyon','Triassic','Middle Triassic','Anisian','late Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',132,0,'',46,17,2525722,2443949,'Hungary','Europe',336,'',46.9,17.7833,'WAHR','67640',11.8671316759,38.0578851461,11.8671316759,38.0578851461,13.4659939565,23.7269750698,1.60329,29.4615,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('E-Sulawesi',147,'','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',133,1057,'Only \'reefal\' facies with corals, forams and green algae is mentioned.\nRetiophyllia, Blastochaetetes and solenoporaceans as main framebuilders.\n\nAbstract of ref. 1057:\nAn Upper Triassic (Upper Norian-Rhaetian) carbonate complex, composed of open marine to reefal deposits, has been investigated for the first time in Eastern Sulawesi. The age is based on the occurrence of benthic foraminifera, and also of the Upper Sevatian to Rhaetian conodont Misikella posthernsteini Kozur and Mock. Palynological assemblages contain Upper Triassic-Lower Jurassic palynomorphs. The scleractinian coral Retiophyllia seranica and the chaetetid sponge Blastochaetetes intabulata, together with Solenoporacean algae, are the main framebuilders of the reefal facies. The entire carbonate series, composed of conodont bearing limestones, reefal deposits, and intertidal/supratidal cryptalgal laminites, shows a general regressive trend from a marginal to an inner platform environment. The relationship between microfaunal distribution and sequence analysis is discussed. The Upper Triassic foraminifers and palynomorphs of Eastern Sulawesi show affinities to microfaunas of the Australian-Indonesian southern Tethyan domain, and the general organisation of the platform should be investigated through further studies from Banda Sea dredgings.',-1,121,-3237937,10472012,'Indonesia','Asia',614,'681',-1.9833,121.3333,'WAHR','67677',-18.6168872117,105.851587701,-18.6168872117,105.851587701,-37.0610137716,104.839100819,21.4298,125.493,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lhasa, Tibet',148,'','Triassic','Upper Triassic','Carnian','Carnian/Norian',208.50,235.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',216,2,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',134,0,'Paleontological description of corals.',29,91,-3589960,6636818,'China','Asia',602,'',29.9667,91.55,'','',-25.1829540547,72.3284006671,-27.2438187087,72.3793559233,0.563542453209,92.671358727,18.6346,68.4156,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Menina',149,'','Triassic','Upper Triassic','Carnian','lower Carnian',233.00,235.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',226,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'3',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',135,0,'Cordevolian\nSimilar to Julian Alps',46,14,1190430,2535689,'Slovenia','Europe',328,'',46.2667,14.7833,'WAHR','67628',15.2127454909,34.7246208586,15.2127454909,34.7246208586,9.40575396434,22.3685878824,11.4559,21.7863,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Yesilova',150,'','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'100','1',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','90','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',137,0,'Possibly extending into Rhaetian.\n\nSponges, corals and tubiphytes were mentioned',37,29,875474,2482420,'Turkey','Asia',522,'',37.55,29.7333,'WAHR','67685',8.97296667265,35.2891897035,11.9926940065,34.8586993474,9.39489559468,29.4198442062,14.0052,20.7666,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rowley Terrace, N',151,'','Triassic','Upper Triassic','Norian','Norian/Rhaetian',201.30,228.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',203,2,'1','Seismic data available ',NULL,NULL,'2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','1','Corals','20','Corals - forams',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',138,0,'Only dredge samples and seismic data',-16,118,-4532582,7861569,'Australia','Oceania',801,'',-16.3333,118.3333,'WAHR','38069',-30.106085697,86.6147309028,-30.3613620397,86.6564831278,-42.7398021779,82.1743048225,-27.9348,75.2606,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Gartnerkofel',152,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'2',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','9','Tubiphytes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',139,0,'All reefal carbonates reworked',46,13,1303466,2456458,'Austria','Europe',301,'',46.5778,13.2986,'WAHR','81063',15.7214173483,35.6102773831,15.7214173483,35.6102773831,9.66851301398,24.2377009775,7.21582,23.2703,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mina, Pilot Mountains, Nevada',153,'Luning','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',215,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','80','2','10 - 100 m wide','100','3','More than 100 m','150','5',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','12','1','Constructor guild','1','Present',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',140,2386,'Gastrochaenid and lithophagid macroborings in a spongiomorphid.\r\nScleractinian corals are the dominant bioconstructor in all five buildups at Mina\r\nUpdated with detailed information from ref. 2850.\r\nThe small patch reefs (~ 20-40 m high and ~ 50-150 m wide, obvious metre-scale elevation above the surrounding sediments) are from the Luning Allochthon and grew on an inner to middle ramp or in a deep lagoon. \r\nFive coral buildups contained within the lower member of the Upper Triassic Luning Formation located due east of Mina, Nevada, in Cinnabar Canyon (~ N 38°22.677´, W 117°58.248´) and Dunlop Canyon (~ N 38°24.038´, W 118°00.799´). ',38,-118,1591131,-5851728,'United States','North America',101,'2541, 2850',38.4111,-118.0667,'WAHR','33439',15.2999998328,-43.4287349305,15.4086846563,-43.356499461,21.1473249079,-50.5615334833,12.8487,-55.2709,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S-Wallowa Mountains, Oregon',154,'','Triassic','Upper Triassic','Norian','lower Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,220,'Late Triassic (early Norian, 222.4 Ma)',214,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',1150,435,'Was Carnian/Norian\nNow dated as early Norian (Flügel, 2002).',44,-117,2437615,-5533033,'United States','North America',101,'140',44.9333,-117.3333,'WAHR','33384',19.381051288,-42.5432326032,19.486726075,-42.4553698258,26.8158191601,-46.9779196392,19.21,-53.6675,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('W-Cyprus',155,'','Triassic','Upper Triassic','Carnian','Carnian/Norian',208.50,235.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',216,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)',NULL,NULL,'1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',141,0,'Systematic paper on heterastridians\nRadiolarians suggest early Norian for matrix',34,33,460475,2526879,'Cyprus','Europe',701,'',34.75,33.25,'WAHR','73866',NULL,NULL,NULL,NULL,-0.973666131696,28.1013887835,5.78868,21.8419,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wendelstein, Bavaria',156,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','21','2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',142,0,'',47,12,2371594,2019611,'Germany','Europe',331,'',47.7,12.0167,'WAHR','67652',27.8198076747,30.0072513846,27.8198076747,30.0072513846,21.9410369098,24.3064401128,8.63457,23.1876,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dajiang I, Great Bank of Guizhou',157,'','Triassic','Lower Triassic','Induan','Griesbachian',251.80,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',250,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','15',NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','2','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',144,225,'Identical to Cambrian Renalcis-Epiphyton bioherms.\n\nOccuring in pre platform carbonates (immediately above P-TR) and in the early platform stage.\n\nAbstract of ref. 1814:\nEarly Triassic framestones were discovered in the interior of an isolated, marine carbonate platform in the Nanpanjiang basin. The framestones occur in two horizons: (1) the lowermost Triassic (Griesbachian), as biostromes as much as 15 m thick, and (2) the upper part of the Lower Triassic (Smithian or Spathian) as isolated domal or inverted conical mounds as much as 1.5 m thick. The mounds and biostromes consist of a rigid calcimicrobial framework enclosing a network of internal cavities, 1 to 3 cm across, filled with peloidal-skeletal sediment. The framework is made of irregular-to-tufted masses of chambered-to-clotted micrite structures referable to Renalcis, a calcified coccoid cyanobacteria. The framework is reinforced by microbial induced micritic crusts as well as marine cement. Metazoan fossils within the framework include gastropods, bivalves, ostracodes, spirorbids, and brachiopods. The Early Triassic is widely considered to have been a global gap in reef and reef mound development. The global reef gap concept has formed the foundation of models of reef evolution and of the reorganization of reef ecosystems after the end-Permian extinction. These models should be revised to account for the existence of Early Triassic calcimicrobial mounds and biostromes discussed herein.',25,106,1752516,10294538,'China','Asia',602,'1814',25.55,106.8667,'WAHR','85070',-14.5196914142,107.12551547,-14.7553712322,106.930848233,8.79804365354,122.844153389,5.80665,98.3741,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bianyang I, Great Bank of Guizhou',158,'','Triassic','Middle Triassic','Anisian','middle Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',242,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','291',NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','9','Tubiphytes','3','Microbes','21','Tubiphytes - cyanophyceans - corals - (algae) - sponges',NULL,NULL,'0','5','95',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',144,225,'Good description\nCorals and sponges are rare, but increase in abundance up section.\nAtoll structure 291 m thick according to ref. 662.\n',25,106,1764104,10270246,'China','Asia',602,'662, 2549',25.6667,106.6667,'','',-10.1445252001,109.033290366,-10.1445252001,109.033290366,19.3026178357,119.434487979,12.9734,96.4981,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bianyang II',159,'','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'50','158',0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','9','Tubiphytes','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','40','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',144,225,'Coral-tubiphytes-sponge boundstones.\nReefs completely eroded, only clasts are to be found.',25,106,1769701,10285517,'China','Asia',602,'',25.6833,106.8333,'','',-0.354519770942,111.381463529,-0.354519770942,111.381463529,32.0446642279,115.485180719,20.5829,94.7249,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jinshajiang',160,'','Triassic','Upper Triassic','Carnian','Carnian/Norian',208.50,235.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',216,1,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'20',NULL,0,'Tropical or unknown','0',NULL,'','Unknown','2','Below fair weather wave base','1','Corals','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',145,0,'Position unclear\nNo description of reef facies',29,92,-3717461,6645366,'China','Asia',602,'',29,92,'','',-38.6391684449,64.2848919338,-40.6529836097,64.0325392406,-46.1752285644,60.1134076962,17.7375,68.9758,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Buru',161,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'0','Outcropping reef ',2,'Reef mound',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,NULL,'',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',146,0,'',-3,126,-3859527,10505624,'Indonesia','Asia',614,'',-3.5,126.5,'','',-28.7188411076,110.435964181,-28.9355708137,110.531230623,-33.3396533439,102.540466812,-26.2915,99.1639,'Kiessling','Kiessling','2021-05-28 15:21:12','2023-03-17 17:45:34'),('Seelandalpe',162,'Cassian','Triassic','Upper Triassic','Carnian','lower Carnian',233.00,235.00,17,'Induan - early Carnian',235,235,'Late Triassic (early Carnian, 233.6)',226,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','22','Stromatoporoids/sponges - corals - (algae)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','110','1','Constructor guild','1','Present','1','Present','3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',147,231,'Julian age.\nVery detailed description of reef fauna.\nAbout 70 sponge species and 40 coral species',46,12,1376488,2388207,'Italy','Europe',344,'',46.6833,12.15,'WAHR','34691',16.9742213606,34.1009057278,16.9742213606,34.1009057278,10.8758872689,21.2100166653,11.9001,20.8923,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kosmatiza, Karawanken',163,'Contrin','Triassic','Middle Triassic','Anisian','upper Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'4',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','9','Tubiphytes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'3','47','50',0,'no',0,'no','2','6 to 24 reef building species','21','3','Binder guild',NULL,NULL,'1','Present','2','Medium zonation','3','Pronounced zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',148,1825,'7 Sphinctozoan species\n2 Inozoan\nPorostromata, Spongiostromata, Solenoporaceans.\n7 Microproblematica.\nTubiphytes very abundant.\nSerpulids\nReef composition: \n14 % Spongiostromata\n4 % Porostromata\n14 % Tubiphytes\n2 % Solenopraceans\n11 % sponges (8 % sphinctoz)\n3 % sessile forams\n1 % bryozoans\n1 % serpulids\n< 1 % corals',46,14,1241650,2507917,'Austria','Europe',301,'',46.45,14.2,'','',13.7914819896,36.4222662095,13.7914819896,36.4222662095,8.72920267986,26.9276651084,5.4313,25.1614,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lugano',164,'','Triassic','Middle Triassic','Anisian','Anisian/Ladinian',237.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',237,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','9','Tubiphytes','21','Tubiphytes - cyanophyceans - corals - (algae) - sponges',NULL,NULL,'0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',150,0,'Vertical and lateral distribution not certain.\nOlangocoelia is dominant\nMany Tubiphytes and corals',45,8,1475846,2138065,'Switzerland','Europe',331,'',45.9764,8.9444,'','',17.4990729916,33.9760726605,17.4990729916,33.9760726605,11.2431750849,22.54897305,7.24587,22.1079,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lienz',165,'','Triassic','Middle Triassic','Anisian','Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',241,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','2','Below fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',151,0,'',46,12,2280669,2111541,'Austria','Europe',301,'',46.75,12.5833,'','',14.9148219726,36.1653228411,14.9148219726,36.1653228411,9.6789484709,26.269696532,6.34006,24.452,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kuma River, Kyushu',166,'Konose Group','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','2','Algae','3','Microbes','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','13','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',152,363,'Only reef blocks in basinal volcanoclastic facies.\n\nAlgae (solenporaceans) and microbes (crusts) more important than corals and sponges.\nSolenoporaceans > spongiostromata > calcisponges > scleractinia.',32,130,4323972,13266958,'Japan','Asia',625,'161',32.35,130.6,'WAHR','34883',40.0314822153,142.538581718,39.2969592407,142.170360164,40.9912431953,148.946316413,43.5213,125.069,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nara',167,'','Triassic','Upper Triassic','Carnian','Carnian',228.00,235.00,17,'Induan - early Carnian',235,230,'Late Triassic (Carnian, 232 Ma)',223,1,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)',NULL,NULL,'1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',153,0,'Reefal boulders only. \nNo description of facies.',34,136,3972094,12317145,'Japan','Asia',625,'',34.3333,136,'WAHR','38133',19.0535624737,139.496660685,19.0535624737,139.496660685,38.1511104014,145.593081572,42.4052,121.006,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Háj, Zádial Plateau',168,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',2,'Reef mound','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'5','95','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',154,183,'Corals, bryozoans also present',48,20,2867665,2522623,'Slovakia','Europe',336,'',48.6306,20.8833,'','',12.4309247346,40.164330325,12.4309247346,40.164330325,14.8906437194,23.9686008133,3.55542,30.8426,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zádial Plateau',169,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'200',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',154,183,'',48,20,4223835,1953496,'Slovakia','Europe',336,'',48.6333,20.65,'','',17.3654144538,36.0526575934,17.1712100799,36.1233528107,21.3561941017,22.4700430351,21.5329,23.9148,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Silica Plateau',170,'Wetterstein Limestone','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','22','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',154,167,'Includes data from several collections and collections in Plesivec Plateau',48,20,2846499,2508803,'Slovakia','Europe',336,'183',48.5667,20.5833,'WAHR','34882',13.1966311099,39.0562064704,13.1966311099,39.0562064704,15.4407009649,21.4501837086,8.22866,28.6283,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Veterlin, Malé Karpaty',171,'Wetterstein Limestone','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','9','Tubiphytes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','80','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',165,154,'Calcareous sponges, small colonial corals, dendroidal tubiphytes, solenoporaceans and Disjectoporata are frame builders.',48,17,2697390,2312767,'Slovakia','Europe',336,'',48.5333,17.3667,'WAHR','36639',14.3387170245,38.7924621682,14.3387170245,38.7924621682,15.5109750568,21.6431497593,4.76256,28.8465,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Liptovska Osada',172,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',211,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',154,0,'With facies map',48,19,4200655,1844148,'Slovakia','Europe',336,'',48.9417,19.2667,'','',18.2471221234,35.6481719393,18.0541232227,35.7222115648,21.9335111126,21.6419601997,22.3077,23.2999,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pljevlja, Montenegro',173,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',233,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',155,324,'No detailed descritpion of reef facies available',43,19,278074,2893630,'Yugoslavia','Europe',307,'',43.35,19.35,'','',10.3869368712,35.0796947663,10.3869368712,35.0796947663,4.49521662041,25.6491882588,2.21191,25.197,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bükk Mountains',174,'Wetterstein Limestone','Triassic','Middle Triassic','Ladinian','upper Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',229,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'15',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','70','30',0,'no',0,'no','3','25 or more reef building species','39','2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',157,158,'Reef classification doubtful.\nSponges and tubiphytes seem to prevail, but coral framestones are mentioned.\nwas Ladinian/Carnian - now assigned to late Ladinian following Velledits (2006).',47,20,2774639,2544387,'Hungary','Europe',336,'',47.9708,20.5,'WAHR','42258',12.2772637189,39.4575024496,12.2772637189,39.4575024496,14.3335901114,23.5180937005,3.13596,30.2721,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Moliterno, S-Apennin',175,'Mt. Facito','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','100',NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','2','Algae','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',159,1478,'Lenticular massive buildups 80-100 m thick.\nBoundstone predominantly of encrusting organisms (cyanobacteria, foraminifers), green algae and calcisponges.\nRare corals.\nClassified as spar-cemented organically bound skeletal debris reef.',40,15,437744,2260345,'Italy','Europe',344,'',40.2333,15.8667,'','',10.8781683095,30.9830728573,10.8781683095,30.9830728573,5.03456732837,20.5764490522,0.882946,21.3633,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Cerchiara, Brienza, S-Apennin',176,'Mt. Facito','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20','175',0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',1478,159,'See reef 175 for remarks.',40,15,478803,2259298,'Italy','Europe',344,'',40.4833,15.65,'WAHR','20659',11.1506777182,31.1099311997,11.1506777182,31.1099311997,5.33213722405,20.5413899419,1.18249,21.357,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Irpina',177,'','Triassic','Upper Triassic','Carnian','Carnian',228.00,235.00,17,'Induan - early Carnian',235,230,'Late Triassic (Carnian, 232 Ma)',223,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'8',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','4','Stromatoporoids','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',160,0,'Chaetetids are especially abundant',41,15,574022,2250948,'Italy','Europe',344,'',41.0333,15.0833,'WAHR','67620',12.3620707776,29.8730885909,12.3620707776,29.8730885909,6.93080485224,16.8551446637,9.27303,18.0525,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sambosan, Shikoku',178,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','4','Stromatoporoids','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',161,0,'',33,133,4399689,13549630,'Japan','Asia',625,'',33.55,133.5333,'','',40.8280664877,145.980557788,40.0833548898,145.579157975,41.393768033,152.545909038,44.0911,128.78,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('N-Calabria, microbe-serpulid reefs',179,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',209,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','3','Microbes','8','Serpulids, worms, vermetids','11','Serpulids - algae - microbes',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',162,2173,'Only small reefal clasts are reported\n\nSerpulid shells surrounded by microbial crusts. Locally corals, calcisponges, solenoporanceans and problematica are present (collection data).\n\nAbstract of ref. 2173:\nMicrobial-serpulid communities are the main reef-builders of most Norian-Rhaetian carbonate platforms of Italy. They represent minor, yet significant communities in the shallow western Tethys, in contrast with the highly diversified sponge- and coral-dominated Dachstein reefs widespread from Eastern Alps to Australia. The microbial-serpulid build-ups are systematically associated with narrow intraplatform troughs and developed on the outer margin-upper slope area under marine conditions unsuitable for the development of coralgal reefs. The development of these settings can be related to transtensional tectonics affecting an elongate belt which was roughly parallel to the Piedmont-Ligurian Ocean spreading axis during the Jurassic. Dysoxic and mesosaline waters are the main cause of the success of the Norian microbial-serpulid build-ups. Whereas, from the late Norian to the Rhaetian, eutrophication and climate change control their distribution. These environments acted during Norian-Rhaetian times as refuges, where opportunitistic organisms could survive and build frameworks during a period otherwise dominated by coralgal reefs.',39,15,1917203,1668921,'Italy','Europe',344,'2599',39.9167,15.8667,'WAHR','38046',14.0304925974,26.9652947726,13.8657057323,27.0324041417,12.2030780063,20.4606148257,18.245,14.0673,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zangla, Ladakh',180,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'5',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,'0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',163,0,'Embedded in predominantly siliciclastic sequence.\n\nCorals and bryozoans also in Carnian limestones.',33,77,-3725245,5200024,'India','Asia',501,'',33.6667,77.0167,'','',-25.8040611068,58.9228735928,-26.0493065615,58.9005749574,-32.9168904522,52.3213383309,23.9264,56.0425,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Peace River, Alberta',181,'Pekisko','Carboniferous','Mississippian','Tournaisian','middle Tournasian',346.70,358.90,11,'late Famennian - early Visean',351,350,'Early Mississippian (Tournaisian, 349 Ma)',352,3,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick','100','2','10 - 100 m wide','200','3','More than 100 m','400','40',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',168,0,'Middle Tournasian (TN2)\nWaulsortian bioherm\nBryzoans are dominant macrofossils.\nCrinoids in apron sediments',56,-117,814946,-4261420,'Canada','North America',121,'',56.25,-117.3,'','',-7.38714307932,-45.8059441025,-7.38714307932,-45.8059441025,14.3781582538,-95.4435392967,4.56922,-38.8486,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('N-Yukon',182,'','Permian','Cisuralian','Sakmarian','Sakmarian/Artinskian',283.50,298.90,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',284,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','4','1','Less than 10 m wide',NULL,'2','10 - 100 m','21',NULL,NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','2','Algae','2','Algae','25','Palaeoaplysina - phylloid algae','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',169,259,'Palaeoaplysina-mound.\nFloatstone with Epimastopora and phylloid algae.\nIntense micritization of mollusc shells\n\n3.7 m thick and more than 21 m long.\nPossibly marginal marine (enclosed in siliciclastics)\nPaleobathymetry uncertain.\n\nPreviously dated as Asselian by Davies (1971), ref. 259',68,-136,6004315,-2077132,'Canada','North America',121,'',68.2583,-136.4625,'WAHR','45346',38.2931495467,-20.5349337495,38.2931495467,-20.5349337495,35.8049358005,-37.7473646003,44.3532,-22.1804,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Arco Hills, Idaho',183,'Snaky Canyon','Carboniferous','Pennsylvanian','Gzhelian','Virgilian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',300,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','25',NULL,NULL,NULL,'4','More than 1000 m',NULL,'54',NULL,2,'Cold - water','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','2','Algae','2','Algae','25','Palaeoaplysina - phylloid algae','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',170,0,'Palaeoaplysina (Hydrozoa?) mounds.\nPalaeoa. together with other algae, bryozoans, corals as sediment bafflers and pelmatozoans, ostracodes and forams in the matrix',43,-113,2109360,-3938236,'United States','North America',101,'',43.65,-113.2667,'WAHR','45345',13.7304966462,-36.4554537189,13.7304966462,-36.4554537189,9.28315469809,-57.5990560928,11.3157,-37.9682,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Brookfield, Nova Scotia',184,'Windsor Group','Carboniferous','Mississippian','Visean','upper Visean',330.90,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',332,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','100','20',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','2','Below fair weather wave base','7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',171,0,'Kennetcook and Herbert River Limestone Members, upper part of the Windsor Group.\nBioerosion evident(?) on fig. 4 of ref. 171',45,-63,-1654777,-1081265,'Canada','North America',121,'',45.25,-63.3333,'','',-35.6461179227,-27.1976892568,-33.014788097,-24.3665356395,-13.3116433928,-48.8115058872,-14.336,-12.1312,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shubenacadie, Nova Scotia',185,'Gays River','Carboniferous','Mississippian','Visean','early to middle Visean',330.90,346.70,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',339,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','3','Microbes','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1','Red algae','20','60','20',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',172,0,'',45,-63,-1675883,-1090368,'Canada','North America',121,'',45.0833,-63.4167,'','',-35.7678989327,-27.3554754333,-35.7678989327,-27.3554754333,-13.1460393485,-54.1617547911,-15.4962,-13.2496,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Windsor, Nova Scotia',186,'Miller Creek','Carboniferous','Mississippian','Visean','middle-upper Visean',336.00,345.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','7','Bryozoans','13','Echinoderms','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'60','0','40',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',173,0,'Middle to late Visean\nAbundant brachiopods and crinoids',45,-64,-1675353,-1149248,'Canada','North America',121,'',45,-64.15,'','',-35.6021986626,-27.9685374319,-36.8825685758,-29.4946565574,-12.8614001518,-57.2085025978,-15.9999,-14.3209,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-25 17:30:22'),('Raanes Peninsula I, Ellesmere Island, Nunavut',187,'Nansen','Carboniferous',NULL,NULL,'Moscovian/Sakmarian',290.10,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',299,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'8',NULL,1,'Temperate','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','2','Algae','9','Tubiphytes','25','Palaeoaplysina - phylloid algae','2','Green algae','0','70','30',0,'no',0,'no','2','6 to 24 reef building species','7','3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',174,307,'Palaeoaplysina-phylloid algae as main reef builders.\nAdditionally Tubiphytes-bryozoans, crinoids',78,-85,4449353,206514,'Canada','North America',121,'',78.3667,-85.9,'','',29.2823191306,0.251723038039,29.2823191306,0.251723038039,26.8315842753,-24.2659712734,27.4896,-0.418599,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Raanes Peninsula II, Ellesmere Island, Nunavut',188,'Nansen','Carboniferous',NULL,NULL,'Moscovian/Sakmarian',290.10,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',299,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'7',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','2','Algae','2','Algae','25','Palaeoaplysina - phylloid algae','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',174,307,'Several patch reefs, elongated or dome shaped.',78,-85,4423119,192280,'Canada','North America',121,'',78.1333,-85.6667,'','',29.0779338438,0.111637150917,29.0779338438,0.111637150917,25.8579503359,-24.1422237133,27.2905,-0.565988,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bunde Fjord, Axel Heib. Is.',189,'','Carboniferous',NULL,NULL,'Moscovian/Sakmarian',290.10,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',299,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','2','Algae','2','Algae','25','Palaeoaplysina - phylloid algae','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',174,307,'',80,-94,4778184,256245,'Canada','North America',121,'',80.4667,-94.4667,'','',31.8611446692,0.779916567487,31.8611446692,0.779916567487,30.3983797156,-24.7185157598,30.0466,0.225547,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Raanes Peninsula III, Ellesmere Island, Nunavut',190,'','Permian','Cisuralian','Sakmarian','upper Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',286,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','7','Bryozoans','9','Tubiphytes','23','Bryozoans - Tubiphytes - phylloid algae - (microbes) - (encrusting forams)','2','Green algae','60','0','40',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',175,0,'Ramose bryozoans, Tubiphytes and sponge spicules as main constituents',78,-85,5104747,402146,'Canada','North America',121,'',78.3667,-85.9167,'WAHR','76088',31.400210156,1.78194755123,31.400210156,1.78194755123,29.6468295479,-18.3208425147,30.4192,-0.135369,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Blind Fjord, Raanes Penins., Ellesmere Isl., Nunav',191,'Great Bear Cape','Permian','Cisuralian','Artinskian','Early to upper Artinskian',283.50,290.10,15,'Sakmarian - Kungurian',277,285,'Early Permian (Artinskian, 286.8 Ma)',280,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','130','3','101-1000 m wide',NULL,'4','More than 1000 m',NULL,'6',NULL,2,'Cold - water','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','11','Siliceous sponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',176,0,'Bryozoan cementstones and bryozoan-sponge wacke- to packstones are present.',78,-85,5099528,404864,'Canada','North America',121,'',78.35,-85.7,'WAHR','76095',31.6861607926,1.93542967871,31.6861607926,1.93542967871,30.2959544041,-13.0934897565,32.7066,1.45118,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Raanes Peninsula V, Ellesmere Isl., Nunavut',192,'Great Bear Cape','Permian','Cisuralian','Artinskian','Artinskian',283.50,290.10,15,'Sakmarian - Kungurian',277,285,'Early Permian (Artinskian, 286.8 Ma)',280,2,'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,2,'Cold - water','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','11','Siliceous sponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',176,0,'',78,-85,5109926,411544,'Canada','North America',121,'',78.45,-85.7667,'','',31.7684742115,2.00402803281,31.7684742115,2.00402803281,31.1354152111,-13.320069607,32.7879,1.52222,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sotong B1, offshore',193,'Sotong Limestone','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'20','70','10',0,'no',0,'no','2','6 to 24 reef building species','10','3','Binder guild',NULL,NULL,'1','Present','3','Pronounced zonation',NULL,NULL,'2','30-60% micrite',NULL,NULL,'3','High production of reefal debris','1','Present',0,'No or unknown reservoir potential',178,1460,'Organic mound or biostrome rather than a wave-resistant bioherm or reef.\nBinding predominates over framebuilding:\nEncrusting forams, bryozoans and corals as binders.\nAge based on Alpinophragmium perforatum Flügel\nNon-segmented sponges more common than Sphinctozoa.\nTubiphytes, Bacinella, Cayeuxia, Panormidella, corals, Trepostomata as other important reef builders.',4,104,791097,10733256,'Malaysia','Asia',614,'',4.8769,104.7997,'WAHR','36890',11.9191743819,115.240772577,11.4897211163,114.99206269,7.72227581514,115.513965804,11.0348,97.9021,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Okumino',194,'','Permian','Cisuralian','Sakmarian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',289,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','9','Tubiphytes','3','Microbes','24','Tubiphytes - algae - cyanophyceans - (bryozoans) - (sponges)',NULL,NULL,'20','0','80',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',179,788,'Tubiphytes-Archaeolithoporella-Girvanella as main constituents. \nBryozoans common, corals rare.',35,136,1784737,11533463,'Japan','Asia',625,'',35.7,136.7667,'WAHR','75746',13.2907587374,138.877637168,13.2907587374,138.877637168,18.4253653715,84.1431645294,13.9586,107.675,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wengdao, Guizhou',195,'','Carboniferous','Pennsylvanian','Gzhelian','Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',301,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','10',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','2','Algae','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',180,2847,'Uppermost Carboniferous.\nThickness up to 10 m.\nPhylloid algae - cement mound.\nAlmost no micritic matrix',25,106,-1786407,10738716,'China','Asia',602,'',25.5,106.0333,'WAHR','76758',-11.6845691409,134.58175675,-11.6845691409,134.58175675,9.62759528121,103.487468891,-12.1752,98.0459,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ziyundong, Ziyun Co., Guizhou',196,'Houziguan Limestone','Permian','Guadalupian','Wordian','Maokouan',265.10,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',265,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'3',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','4','Stromatoporoids','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'10','80','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',181,297,'Good description of reef facies.\nCalcareous sponges, hydrozoans and Archaeolithoporella(!) most important. Additionally Tubiphytes and bryozoans.',25,106,-884985,8912942,'China','Asia',602,'298, 2457',25.8278,106.0361,'WAHR','47456',-18.5786589557,109.630974138,-16.7863466642,116.970690428,1.75812361187,131.501773955,-5.69934,97.7003,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ziyun County, Guizhou',197,'Shitouzhai','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','7','Bryozoans','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'30','70','0',0,'no',0,'no','2','6 to 24 reef building species','19','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',181,297,'Reefs at Monan, Tanluzai, Tunshang, Shitouzai, and Qincaichaong\nVery good description of reef facies and geometry.\nSponges dominate.\nBryozoans, solenoporaceans, stromatolites and corals are also important.\n',25,106,-880647,8918204,'China','Asia',602,'662',25.8417,106.0944,'WAHR','47457',-15.4319991099,105.465838004,-15.4319991099,105.465838004,6.69960737605,123.528475917,4.53774,97.8766,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Maltby, England',198,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'40',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',182,0,'Many small patch reefs figured along N-S trending belt.\nHere only the southern and northern limits are analyzed.',53,-1,2262653,1649215,'United Kingdom','Europe',331,'',53.4333,-1.1833,'','',28.3638563984,21.5813941039,28.3671384126,21.5815947705,21.8859101602,18.158394865,16.6459,14.5173,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aberford, England',199,'Cadeby','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'80','198',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','3','Microbes','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','5','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',182,0,'Microbial-bryozoan patch reefs\nBelt of patch reefs that runs N-S for some 90km east of Leeds',53,-1,2315878,1628925,'United Kingdom','Europe',331,'',53.85,-1.5,'WAHR','63887',28.7575783506,21.317134277,28.7608557238,21.3173177452,22.1781638864,17.7793208151,16.9601,14.9566,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Djebel Tebaga',200,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',266,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','105',NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','6','Calcisponges','3','Microbes','27','Pharetronid sponges - algae',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species','100','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',184,229,'Sponges very diverse.\nMany patch reefs. Total thickness of reefal facies exceeds 100 m.\nToomey (1991) suggested outer shelf deposition:\nThe only outcrops of marine Upper Permian strata in North Africa form an inlier in the Djebel Tebaga area of southern Tunisia. Those outcrops occupy 18km2 (6.9 M2), and comprise the western tip of the Late Permian tethyan seaway. Late Permian marine sediments exposed in southern Tunisia are up to 850m (2789 ft) thick, and grade upward into nonmarine red beds of Permo-Triassic age. Those are unconformably overlapped by flat-lying Jurassic and Cretaceous sediments. Paleogeographically, the Tunisian Permian outcrops represent a biohermal complex situated between a subsurface shale basin to the north, and to the south varied shelf sediments on the margin of the Sahara Shield. Comparison of the Tunisian bioherms to the Permian reef complex of the southwestern United States indicates similarities in biotic composition. Cement fabrics are of major significance at both locations, and are very similar. Both biohermal/reef sequences appear to have been deposited in a shelf-margin paleoenvironment, although the sediments in Tunisia are thin-bedded cyclical or repetitive lithologies associated with overall upward shoaling sequences.',33,10,-633765,2067141,'Tunisia','Africa',715,'185, 186, 1327',33.4333,10.3,'WAHR','41658',-4.21892733384,20.1052816835,-4.21892733384,20.1052816835,-3.925181548,13.1829468564,-7.00595,18.5345,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Birkat al Mawz',201,'Misfah','Triassic','Upper Triassic','Carnian','upper Carnian',228.00,230.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',219,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'4',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','8','1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',818,187,'Olistolithes in basinal chert facies.\nFaint traces of bioerosion.',22,57,-1785198,5142376,'Oman','Asia',503,'',22.8139,57.8194,'WAHR','24309',-15.4804386084,54.1927541464,-15.4804386084,54.1927541464,-22.7764754692,45.1022741351,-16.1554,47.3916,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jebel Wasa north, Oman Mountains',202,'Jebel Wasa','Triassic','Upper Triassic','Carnian','middle Carnian',230.00,232.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',224,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'6',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','2','Algae','27','Pharetronid sponges - algae','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species','10','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',818,42,'Almost only sponges and few algae',24,55,-1505449,5166728,'Oman','Asia',503,'187',24.7083,55.8667,'WAHR','24305',-13.8853229606,52.8386401015,-13.8853229606,52.8386401015,-21.0816751966,43.9568349416,-15.6558,46.852,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Il Karraba',203,'unknown','Neogene','Miocene',NULL,'Miocene',5.30,23.00,31,'Burdigalian - Serravallian',14,20,'Early Miocene (Aquitanian&Burdigalian, 19.5 Ma)',13,1,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','2','Algae','2','Algae','29','Coralline algae only (some corals)','1','Red algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',188,0,'',35,14,4677364,1285964,'Malta','Europe',719,'',35.8833,14.4167,'','',32.5249038195,10.5265107462,32.5249038195,10.5265107462,34.0151768784,14.2965069591,35.3142,13.7486,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Marcali',204,'','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',189,0,'No exposures, only drillhole data.',46,17,2477756,2444747,'Hungary','Europe',336,'',46.6,17.5,'','',13.7817047588,36.1752033584,13.7817047588,36.1752033584,14.1814854309,18.7917422469,7.78108,25.7738,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Grigna',205,'','Triassic','Middle Triassic','Ladinian','Ladinian',237.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',232,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','9','Tubiphytes','12','Cyanophyceans - Tubiphytes',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',190,0,'',45,9,1443468,2163490,'Italy','Europe',344,'',45.9167,9.4,'','',17.7879026974,33.6749690666,17.7879026974,33.6749690666,11.2245307511,21.5806574376,8.235,20.6649,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Phatthalung',206,'Chaiburi','Triassic','Upper Triassic','Carnian','middle-late Carnian',228.00,230.00,18,'late Carnian - middle Hettangian',218,225,'Late Triassic (Carnian/Norian 227 Ma)',222,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick','17',NULL,NULL,NULL,'2','10 - 100 m',NULL,'8',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','6','Calcisponges','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','16','2','Baffler guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',191,323,'Sibumus Terrane\nPreviously considered early Carnian.\nMiddle-Late Carnian according to Flügel (2002).\n\nAbstract ref. 323:\nCarbonate rocks in the Phatthalung area and others in Peninsular Thailand have been known as the Permian Rat Buri Limestone. The study area is characterized by several isolated limestone mountains and is located in Phatthalung province. Micropaleontological study of these carbonate rocks indicates that they should be assigned a late Early to Late Triassic age. The Chaiburi Formation is newly proposed and divided into three members: The Phukhaothong Dolomite, Chiak Limestone and Phanomwang Limestone in ascending order. The Phukhaothong Dolomite consists of thickly bedded to massive dolomite and yields Neospathodus kummeli Sweet, N. waageni Sweet, N. cfr. waageni Sweet and other conodonts that indicate Dienerian to Smithian (Early Triassic). The Chiak Limestone Member consists of bedded and laminated limestone with intercalated thin chert layers and nodules. This limestone commonly yields Early Triassic to Middle Triassic conodonts such as Neospathodus timorensis (Nogami) and Neospathodus kockeli (Tatge), both reliable indicators of latest Spathian to early Anisian, and rare occurrences of Neogondolella bulgarica (Budurov and Stefanov), an indicator of the middle Anisian. The Phanomwang Limestone Member is mostly massive limestone with intercalated reef limestone (coral buildups) and yields abundant fossils that indicate Carnian (Late Triassic). Microfacies analysis and stratigraphic sequences of carbonate rocks in this area show the gradual change of depositional environment from low to high energy conditions.',7,100,526629,10336868,'Thailand','Asia',604,'',7.1167,100.1667,'WAHR','34566',-1.73232540431,107.578006184,-1.73232540431,107.578006184,3.96751341632,105.287057638,2.46945,93.3833,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lake Tobe, Sumatra',207,'','Triassic','Middle Triassic','Ladinian','Ladinian/Carnian',227.00,242.00,17,'Induan - early Carnian',235,240,'Middle Triassic (Ladinian, 239.5 Ma)',228,2,'0','Outcropping reef ',NULL,NULL,'1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown','1','Above fair weather wave base','1','Corals','1','Corals',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',192,335,'Have not seen the paper',2,99,-1024746,11047187,'Indonesia','Asia',614,'',2.5,99,'','',-10.7971968096,109.080866926,-10.7971968096,109.080866926,-2.16019552646,108.91244231,-4.7167,98.3061,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Val Adrara and others, Lombardia',208,'Calcare di Zu','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','8','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',2375,194,'',45,9,2890118,1594068,'Italy','Europe',344,'',45.7167,9.9667,'WAHR','38128',27.2721964206,26.9478375727,27.2721964206,26.9478375727,23.5249961033,25.4084810779,32.032,12.0852,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Pogorzyce, Silesia',209,'Karchowice Beds','Triassic','Middle Triassic','Anisian','upper Anisian',242.00,247.20,17,'Induan - early Carnian',235,245,'Middle Triassic (Anisian, 244.6 Ma)',239,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick','1','1','Less than 10 m wide',NULL,'1','Less than 20 m','14','150','65',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','15','Non-rudist bivalves','6','Corals - bivalves - (stromatoporoids)',NULL,NULL,'10','90','0',0,'no',0,'no','2','6 to 24 reef building species','20','2','Baffler guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',195,0,'Late Pelsonian to early Illyrian.\n19 species of corals in 11 genera.',50,19,2970273,2340183,'Poland','Europe',301,'',50.0833,19.5,'WAHR','34732',30.501858743,35.6240312701,30.501858743,35.6240312701,26.2838546035,29.6374646846,18.6643,24.9356,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Iwaizaki',210,'Iwaizaki Limestone','Permian','Guadalupian','Wordian','Wordian-Capitanian',259.80,268.80,16,'Roadian - Changhsingian',261,265,'Middle Permian (Wordian/Capitanian Boundary 265.1 Ma)',265,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','45',NULL,NULL,NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1','Red algae','50','40','10',0,'no',0,'no','2','6 to 24 reef building species','10','1','Constructor guild',NULL,NULL,'1','Present','2','Medium zonation','2','Medium zonation','1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',196,203,'Abstract of ref. 196:\nThe early Late Permian (Kubergandian to Midian) Iwaizaki Limestone of the South Kitakami Terrane, situated in Northeast Japan, represents a coral reef complex which was formed on a faulted-bank in an active continental margin. The reef-building organisms include cerioid and dendroid rugose corals, a fasciculate tabulate coral and solenoporacean algae as constructors, calcisponges, bryozoans and crinoids as bafflers, and Tubiphytes, Archaeolithoporella and cyanobacteria as binders. The biotic composition is more diverse than the other coeval reefs. Characterized by the existence of an obvious framework, this reef is similar to the Recent coral reefs and unique among Late Permian reefs, most of which are mainly formed by calcisponges and calcareous algae.\n\nThe distribution of Late Permian reefs is closely related to the palaeoclimate. Coral reefs were developed mainly around the South China and Indochina continental masses between the Tethys Sea and the Panthalassa Ocean, in the tropics. While, calcisponge reefs and Tubiphytes-algal crust reefs were common in tropical to subtropical regions, and stromatolite-bryozoan reefs developed in arid areas. The gradational distribution of Late Permian organic reefs including localized development of coral reefs were probably caused by decreasing of the glaciers and changing of the ocean current systems.',38,141,2148589,11700644,'Japan','Asia',625,'2211',38.8833,141.6,'WAHR','24126',4.77470804451,136.509516621,4.77470804451,136.509516621,80.5502696868,-164.844416405,22.2463,120.462,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Chhidru',211,'','Permian','Guadalupian',NULL,'Murgabian/Dzhulfian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',262,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'3',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species','2','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',197,0,'No description of geometry and associative fauna.\nOnly Waagenophyllum-type corals are mentioned.',32,71,-5698599,5039438,'Pakistan','Asia',501,'',32.5333,71.8333,'','',-45.8192476811,52.3060672936,-45.8192476811,52.3060672936,-38.4651424694,55.8997165223,-46.3868,54.5476,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Korfu',212,'','Triassic','Upper Triassic','Rhaetian','Rhaetian',201.30,208.50,18,'late Carnian - middle Hettangian',218,205,'49 Late Triassic (Rhaetian, 204.9 Ma)',202,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','1','Scleractinian corals - red algae - (hydrozoans) - (foraminifera) - (microbes) - (sponges)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',198,199,'Dated as Liassic, but see Renz (1955)',39,19,1682233,1959023,'Greece','Europe',338,'',39.75,19.8333,'','',17.941894743,27.9423878534,17.941894743,27.9423878534,16.2215432152,25.8691207792,23.2015,15.6459,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Urakovs, Urals',213,'','Permian','Cisuralian','Asselian','Asselian/Sakmarian',290.10,298.90,NULL,NULL,NULL,295,'Early Permian (Asselian, 297 Ma)',294,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'170',NULL,2,'Cold - water','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','2','Algae','3','Microbes','28','Palaeoaplysina - microbes - bryozoans - Tubiphytes - (corals)','2','Green algae','20','80','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',200,326,'Palaeoaplysina with stromatolites, brachiopods and bryozoans.',56,58,3863286,4508075,'Russia','Asia',624,'',56.8333,58.8,'','',26.8281525981,42.7470449868,26.8281525981,42.7470449868,34.3100210171,18.937282104,26.2543,40.2193,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Shachtau, Sterlitamak, Bashkiria',214,'','Permian','Cisuralian','Asselian','Asselian-Sakmarian',290.10,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',294,2,'0','Outcropping reef ',1,'True reef','4','More than 500 m thick','600',NULL,NULL,NULL,'4','More than 1000 m',NULL,'240',NULL,1,'Temperate','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','7','Bryozoans','28','Palaeoaplysina - microbes - bryozoans - Tubiphytes - (corals)','2','Green algae','30','30','40',0,'no',0,'no','3','25 or more reef building species','150','3','Binder guild','1','Present','1','Present','2','Medium zonation',NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',200,485,'In contrast to 213, no terrigenous influx.\nCorals rare in reefs, but abundant on platform.\n\nFour reef mountains (shikhans) in area. From N-S:\nYuaktau\nKushtau\nShakhtau\nTratau\nSurface outcrop thickness 250-300 m. Well data > 500 m.\nMain reef builders: Tubiphytes, Palaeoaplysina, bryozoans, rare corals and other algae.\n35 species of algae\n2 species of stromatolites\n3 species of sponges\n80 species of bryozoans\n30 species of corals.\n\nReefs (also in subsurface with steep eastern slopes (45-50°) and gentle western slopes (5-12°).\n\nAbstract of ref. 1565:\nIn the geological record, paleontological taxa of uncertain affinity are receiving increasing attention in order to provide paleoecological data for paleoenvironment reconstructions. The present study deals with the taxon Tubiphytes and analyses some of its synecologic interactions, its role played in influencing community structure and its suspected affinity. Tubiphytes is an important skeletal framework element that occurs in several Lower Permian reef mounds of southern Urals (Russia). Tubiphytes acted as an incrusting, a binding organism and a support for others organisms both in Tratau and Nizhni-Irginsk reef mounds. Tubiphytes is constituted of a dark meshwork, microlaminated, and developed around an internal cavity. Thus, this taxon is restricted to the surrounding envelop. Three morphotypes have been recognized within these buildups, according to the shape and characteristics of their surrounding envelops. Therefore, the internal cavity of Tubiphytes can be represented by a sparitic hole or a preserved organic structure. Two assemblages of Tubiphytes with others organisms can be proved in the Uralian reef mounds: the combination of Tubiphytes with bryozoan zooecial and foraminifer structures. ',53,56,3426197,4742567,'Russia','Asia',624,'768, 1413, 1565',53.6167,56.0833,'WAHR','75594',23.5222138068,44.2353310056,23.5222138068,44.2353310056,31.71023299,21.8549799196,23.0103,41.8586,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sarginsk, Urals',215,'','Permian','Cisuralian','Artinskian','middle Artinskian',283.50,290.10,15,'Sakmarian - Kungurian',277,285,'Early Permian (Artinskian, 286.8 Ma)',280,3,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'300',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','2','Below fair weather wave base','7','Bryozoans','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',200,0,'Great thickness by vertical stacking of carbonate banks with low elevation.',58,56,4409834,4568768,'Russia','Asia',624,'',58.5,56.4833,'','',27.389195619,40.8363470761,27.389195619,40.8363470761,35.5841539347,23.8213086207,28.3609,40.8759,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sylvinsk, Urals',216,'','Permian','Cisuralian','Artinskian','Artinskian',283.50,290.10,15,'Sakmarian - Kungurian',277,285,'Early Permian (Artinskian, 286.8 Ma)',280,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'110',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','9','Tubiphytes','3','Microbes','23','Bryozoans - Tubiphytes - phylloid algae - (microbes) - (encrusting forams)','2','Green algae','0','0','100',0,'no',0,'no','2','6 to 24 reef building species','6','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',200,0,'Stromatolites become abundant upward.\nBrachipods also important.',57,57,4327654,4738998,'Russia','Asia',624,'',57.1667,57.3667,'','',26.8490996726,42.3043045593,26.8490996726,42.3043045593,35.5517509661,25.5589369704,27.8229,42.3579,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ufa River, Urals',217,'','Permian','Cisuralian','Kungurian','Kungurian',272.30,283.50,15,'Sakmarian - Kungurian',277,280,'Early Permian (early Kungurian, 280 Ma)',273,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','8',NULL,NULL,NULL,'1','Less than 20 m','12','120',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species','3','3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',200,326,'Two types:\n1. Stromatolitic 3-5 m vertically, 12 m laterally\n2. mounds (1-1.5 x 2-3 m) with problematic fossil: Sylvaella tubularis.',55,56,4131636,4898515,'Russia','Asia',624,'',55.4167,56.7333,'','',26.6292384494,44.8507383454,26.6292384494,44.8507383454,37.0567515193,34.7724541839,28.437,47.0751,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zhilyanka, Aktyubinsk',218,'','Permian','Cisuralian','Kungurian','Kungurian',272.30,283.50,15,'Sakmarian - Kungurian',277,280,'Early Permian (early Kungurian, 280 Ma)',273,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'3',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',201,0,'Cited in Chuvashov (1983).',50,57,3655686,5437578,'Kazakhstan','Asia',301,'',50.2667,57.2167,'','',23.2000414017,49.100667781,23.2000414017,49.100667781,35.1085357039,40.6839800291,24.8647,51.2399,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sitorman, Dobrogea',219,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian/Kimmeridgian',157.30,157.30,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',155,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'5','90','5',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',202,1015,'Corals, hydrozoans, crinoids and some bivalves described.',44,28,4782277,2243607,'Romania','Europe',348,'',44.3667,28.5333,'','',29.0033212026,40.7601759078,29.0033212026,40.7601759078,33.9228585152,43.172591686,37.0873,35.0334,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Tokyo',220,'','Permian','Guadalupian','Capitanian','Midian',259.80,265.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',262,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'90','10','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',203,0,'Coocurring Mizzia, Yabeina and Mollusks.\nBlack muddy limestone',35,139,1833657,11476035,'Japan','Asia',625,'',35.6667,139.75,'','',1.22512545159,132.935712048,1.22512545159,132.935712048,18.7140204447,117.595067514,21.2116,117.766,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Buffalo, Kansas',221,'','Carboniferous','Pennsylvanian','Kasimovian','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'120',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','3','Microbes','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',204,193,'Phylloid algal calcilutite\nMicrobial activity only inferred from cements.\nOther fossils are common echinoderms, pelecypods, gastropods, ì\nbryozoans and forams, and rare brachiopods and corals.\n',37,-95,-401150,-3128933,'United States','North America',101,'494',37.7167,-95.7167,'','',-2.86933854269,-28.2018676344,-2.86933854269,-28.2018676344,-4.31885763796,-51.3149522598,-3.3735,-28.4064,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jianshuigou - Chunmuping Reefs, Chuenmuping, Sichuan',222,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','2','Below fair weather wave base','6','Calcisponges','4','Stromatoporoids','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'20','70','10',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',205,298,'Sponges-tabulozoans-bryozoans-Tubiphytes-algae\r\nDiverse association with important microbial elements.\r\nDiversity and cement less than in Jiantianba, but micrite more important.\r\n\r\nAbstract of ref. 205:\r\nThe uppermost Permian Chuenmuping reef formed on the western side of a carbonate platform situated in the eastern Sichuan Basin, southern China. Contrasts exist between this western patch reef and the better known Jiantianba barrier reef complex on the eastern platform margin in western Hubei Province, 250 km to the east. Microbial micritic carbonates form significant components of the Chuenmuping reef limestones. Three types of fabric can be identified: irregular, clotted and scalloped-laminated. An additional, cuneiform fabric has been found only in fore-reef facies at Jiantianba. Irregular fabric is comparable with the surface of presently forming travertines at Rapolano Terme, central Italy, which are produced by calcification of cyanobacteria. Clotted fabric shows indistinct peloids which tend to lack rims, and are amalgated into irregular masses, some of which exhibit bush-like arrangements where traces of filaments can be seen. Traces of filaments are observed in both dark and light layers in the scalloped-laminated fabric, again suggesting a microbial origin. Cuneiform fabric consists of peloids and filaments, and closely resembles deposits in Quaternary travertines which may have been caused by bacterial action. Chuenmuping reef shows a shallowing sequence in normal marine conditions. The micritic fabrics interpreted here as microbial occur more commonly in the upper part of the reef. This indicates that microbial micrities, with a cementing role, formed coevally with reef growth within the upper part of the photic zone.\r\n\r\nComments für Chunmuping from Tian & Wang, 2021:\r\n\r\nReef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, hydrozoans, and bryozoans.\r\nBinding organisms: Tubiphytes, bryozoan, and cyanobacteria.\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: less sponge framestone and more bafflestone and sponge-Tubiphytes-cyanobacteria bindstone.\r\nReef crest (reef flat): dolomitic bioclastic packstone with crinoid fragments, algae, and reef breccia\r\nReef base: crinoidal packstone.\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform.\r\n\r\nCoordinates stated in text.\r\n\r\nComments für Jianshuigou from Tian & Wang, 2021:\r\n\r\nReef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges,sclerosponge, bryozoans, and hydrozoans\r\nBinding organisms: Archaeolithoporella, Tubiphytes, Palaeoaplysina (problematic “hydrozoan”), cyanobacteria, bryozoan, and hydrozoan.\r\n\r\nReef dwellers: Echinoderms, ammonites, bivalves,\r\nbrachiopods, gastropods, benthic foraminifera, and calcareous algae.\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: less sponge framestone and more sponge bafflestone and sponge-Tubiphytes-Archaeolithoporella-cyanobacteria bindstone.\r\nReef flat: dolomitic bioclastic packstone to grainstone with crinoid fragments, foraminifera, algae, and reef breccia.\r\nReef crest: micritic dolostone with gastropods and evaporite.\r\nReef base: dolomitic crinoidal packstone\r\n\r\nReef type: Skeletal mound at the carbonate intraplatform.\r\n\r\nCoordinates stated in text.',30,106,-277484,8856513,'China','Asia',602,'',30.2,106.8,'WAHR','47459',-11.0296515325,105.422778379,-11.0296515325,105.422778379,11.029106794,124.336995314,8.40483,95.7584,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-19 20:16:44'),('Jiantianba, Hubei',223,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','98',NULL,NULL,NULL,'4','More than 1000 m',NULL,'200',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','4','Stromatoporoids','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'20','60','20',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','3','High production of reefal debris','1','Present',1,'Potential reservoir',205,206,'Barrier reef with calcareous sponges, hydrozoans, Archaeolithoporella, Tubiphytes and bryozoans as main reef builders.\r\nMicrobial elements are important\r\n\r\nComment from Tian & Wang, 2021:\r\nReef builders: Frame-building and baffling\r\norganisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, stromatoporoid sponge, bryozoans, and hydrozoans.\r\nBinding organisms: Archaeolithoporella, Palaeoaplysina, Tubiphytes, and cyanobacteria.\r\n\r\nreef dwellers: \r\nEchinoderms, ammonites, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic:\r\nFore-reef slope: spiculitic-calcispherical cherty wackestone with reef breccias Reef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella\r\nReef flat (reef crest): packstone with reef breccia\r\nReef base: echinodermal packstone to grainstone\r\nBack-reef lagoon: bioclastic packstone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type:\r\nMetazoan reef at the shallow carbonate platform margin\r\n\r\n\r\n\r\n\r\n',30,109,-157920,9031949,'China','Asia',602,'216, 228, 274',30.4833,109.05,'WAHR','74928',-10.4268806771,107.323479177,-10.4268806771,107.323479177,11.2498444044,126.324323329,9.81039,97.1453,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-17 17:45:06'),('Xiangbo, Longlin County, Guangxi',224,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','86',NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'30','60','10',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',206,207,'Lopingian reef facies more than 130 m thick. starting in Wujiapingian to the top of Changhsingian. \r\nCyclic reef building.\r\nSponge framestone, coral bafflestone and Archaeolithoporella bindstone with reef breccias capping each cycle.\r\nSubstrate with phylloid algal grainstone\r\nReef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, stromatoporoid sponge, bryozoans, and hydrozoans (disjectoporids) Binding organisms: Archaeolithoporella, Tubiphytes, Palaeoaplysina, Fistulipora, and cyanobacteria.\r\n\r\nReef dwellers:\r\nEchinoderms,ammonites, ostracodes, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic:\r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella Inter-reef: bioclastic wackestone-packstone Reef flat (reef crest): packstone with reef breccia\r\n\r\nReef type:\r\nMetazoan reef at the shallow carbonate platform margin\r\n\r\n',24,105,-895440,8881618,'China','Asia',602,'298',24.9167,105.3333,'WAHR','47449',-16.4463719826,104.896669126,-16.4463719826,104.896669126,5.80609636777,122.796029145,3.38518,97.869,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-17 11:55:24'),('Xiangbo II, Longlin County, Guangxi',225,'Maokou','Permian','Guadalupian','Wordian','Maokouan',265.10,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',265,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','4','Stromatoporoids','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'10','80','10',0,'no',0,'no','2','6 to 24 reef building species','14','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',206,207,'Calcareous sponges, tabulozoans, Archaeolithoporella,\nHydrozoans, bryozoans, tubiphytes as reef builders.\nCyclic development of reef.',24,105,-902610,8850554,'China','Asia',602,'248, 298',24.9,105.4167,'WAHR','47454',-19.6494922395,109.455868096,-17.8663589649,117.062198187,0.675721321761,131.5514099,-6.7819,97.654,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dongnameng, Guangnan, Yunnan',226,'Maokou','Permian','Guadalupian','Wordian','Maokouan',265.10,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',265,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','90',NULL,NULL,NULL,'4','More than 1000 m',NULL,'20',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','7','Bryozoans','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'20','70','10',0,'no',0,'no','2','6 to 24 reef building species','12','1','Constructor guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',208,206,'Reef facies 90 m thick.\n\nAbstract of ref. 208:\nPermian reefs are widely distributed in the so-called Nanpan Jiang (Nanpan River) region in the neighboring parts of eastern Yunnan, southwestern Guizhou and northwestern Guangxi. Two types of reef occurrences are recognized by their stratigraphic and geographical distributions, 1) a barrier reef belt along a carbonate platform margin and 2) reefs that rim isolated carbonate platforms that occur irregularly within basin facies deposits. The Guangnan reefs of lower Permian age occur within the barrier reef belt and are typical of reefs within the Nanpan Jiang area. These reefs are well-exposed at Dongnameng, a small village about 5 km southeast of Guangnan City and crop out on the west flank on the Guangnan anticline which has been truncated by a major fault. Basin facies deposits occur east of the fault and equivalent carbonate platform deposits occur west of the fault. A succession of reefs  occurs in the late early Permian Maokou Formation and early late Permian Wujiaping Formation. The top of the upper Permian sequence is cut out by faults on the Guangnan anticline and elsewhere is directly overlain by middle Triassic rocks. The preserved upper Permian part may be equivalent to the Wujiaping Formation. The major time of reef development, however, was during early Permian. The reefs have foundations of light gray, thick-bedded, intraclastic-bioclastic grainstones that contain abundant fossils of shallow-water benthic organisms. These limestones represent subtidal bank deposits at the platform margin and functioned as foundations for most of the Permian reefs in the Nanpan Jiang area. Reef limestones consist of light gray, massive, framestones with distinctive textures and abundant fossils. Frame-building organisms are sphinctozoans, inozoans, tabulozoans, bryozoans and hydrozoans. Frame-building organisms total 40-50% of the volume of the reef  masses. Binding organisms are dominantly blue green algae, with subordinate fistuloporid bryozoans and Tubiphytes. Accessory organisms include echinoderms, fusulinids, gastropods, brachiopods, calcareous algae and foraminifers as skeletal debris. The frame-building organisms are generally encrusted by lamellar blue-green algae, which commonly are incorporated fine-grained skeletal fragments. Well developed fibrous calcite cement fills between frame-building organisms to form a typical framestone texture. Gray, thick-bedded, bioclastic packstones and wackestones overlie the  reefs. This stratigraphic relationship suggests that reefs were drowned and that reef development ceased because of the increasing depth. Twelve species of 8 genera of sphinctozoans are described in the present paper. These include: Waagenella salinaria irregularis Zhang, Waagenella sp., Rhabdactinia cf. columnaria Yabe and Sugiyama, Rhabdactinia sp., Intrasporeocoelia hubeienisis Fan and Zhang, Intrasporeocoelia sp., Uvanella guangnanensis sp., nov., Girtycoelia sp., Colospongia cf. dubia Laube, Colospongia sp., Verticillites sp., Lichuanospongia typica Zhang, and of these Uvanella guangnanensis is a new species. Two sizes of sphinctozoans can be differentiated in the collections. The smaller genera include Waagenella, Colospongia, Girtycoelia, and Uvanella. They also make up smaller volumes of the reefs, as compared to the larger forms such as Intrasporeocoelia and Rhabdactinia. The large sphinctozoans are abundant and baffled lime muds during growth of the reefs. All of the sphinctozoans mentioned above also occur in upper Permian reefs of the Lichuan district of west Hubei Province but the diversity in the Nanpan Jiang reefs is much less that in reefs  in the Lichuan district. The sphinctozoan faunas Guangnan may be compared with those of lower Permian reefs in the Bled distric of Yugoslavia. ',24,105,-1158344,8868694,'China','Asia',602,'298',24.0167,105.0833,'WAHR','47455',-20.5820738185,109.510260475,-18.7613228084,117.343580582,-0.228258065926,131.786229338,-7.70305,97.8095,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kemnitz Field, New Mexico',227,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,3,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'30',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','12','Foraminifera','30','Tubiphytes - forams',NULL,NULL,'0','0','100',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',209,193,'',32,-103,155492,-3722283,'United States','North America',101,'',32.8167,-103.55,'','',-0.33218506632,-34.3258453344,-0.33218506632,-34.3258453344,-3.84362631246,-55.0535164399,-2.84016,-35.8499,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Aneth Field, San Juan Canyon, Utah',228,'Hermosa','Carboniferous','Pennsylvanian','Moscovian','Desmoinesian',307.00,315.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',307,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','20',NULL,NULL,NULL,'3','More than 100 m',NULL,'8',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','2','Algae','12','Foraminifera','13','Algae - encrusting forams','2','Green algae','10','90','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',210,193,'20 m thick platy algal mounds.\nAlgal plates intermixed with peloidal sands\nPhylloid algae (mostly Ivanovia), tubular forams, bryozoans, Chaetetes, brachiopods.\nParadox Basin.\n\n10 % avg. porosity.',37,-109,733270,-4517948,'United States','North America',101,'1396',37.1667,-109.8333,'','',-0.303096363162,-40.7588190256,-0.303096363162,-40.7588190256,1.7800143554,-61.5602039968,2.81267,-43.4709,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ba-id',229,'','Permian','Guadalupian','Wordian','Murghabian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','1','Corals','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'30','60','10',0,'no',0,'no','3','25 or more reef building species','47','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',211,212,'Calcisponges, rugose corals and chaetetids mentioned as main reef builders.\nHowever Archaeolithoporella and Tubiphytes also seem to be important.',23,58,-4210270,5453449,'Oman','Asia',503,'1026, 1702, 2271',23.1333,58.3333,'WAHR','24325',-33.9651965687,53.073146628,-33.9651965687,53.073146628,-21.5776440235,51.0873664212,-35.0964,53.5713,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wadi Aday, Saih Hatat',230,'','Permian','Guadalupian','Wordian','Murghabian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','10','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',211,1702,'Described as coral-level bottom communities. Interpreted as biostromes herein.',23,58,-4167820,5503031,'Oman','Asia',503,'2271',23.5,58.6333,'WAHR','24326',-33.6744996127,53.5001776679,-33.6744996127,53.5001776679,-21.4468989773,51.559914398,-34.7816,53.9782,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rif',231,'','Carboniferous','Mississippian','Serpukhovian','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',324,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,'1','Less than 10 m wide',NULL,'1','Less than 20 m',NULL,'25',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','2','Algae','69','Non-coralline algae only','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species','1','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',213,0,'Very small monospecific buildups of algae (cm-dm).',35,-5,-2161972,-64979,'Morocco','Africa',714,'',35.2667,-5.1333,'WAHR','76727',NULL,NULL,NULL,NULL,-21.8565650262,-24.2400285424,-15.5585,-0.451504,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bolshetirsky, Siberia',232,'','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',525,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','100',NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','10','Archaeocyaths','7','Archaeocyaths - microbes',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',214,0,'Thickness 80-110 m.\nArchaeocyathids, Microphytolites, Epiphyton, Renalcis and Marcovella as main reef builders.',59,108,-2602264,851772,'Russia','Asia',624,'',59.3333,108.4167,'WAHR','80846',0.642730507789,-66.1614567052,0.642730507789,-66.1614567052,0.642730507789,-66.1614567052,-12.8638,-5.39648,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Srednebotuobinsky, Siberia',233,'','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',525,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','45',NULL,NULL,NULL,'3','More than 100 m',NULL,'45',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',214,1405,'Gas field\nLess diverse than 232.\n40-45 m thickness. \nMicrophytolites, Epiphyton, Renalcis as main reef builders.\nNepa-Botuoba anteclise.',61,112,-2712908,505834,'Russia','Asia',624,'',61.6667,112.6667,'WAHR','80847',-0.108127891654,-69.2033827769,-0.108127891654,-69.2033827769,-0.108127891654,-69.2033827769,-14.6444,-8.05076,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dulisminsky, Siberia',234,'','Cambrian','Terreneuvian','Stage 2','Tommotian',521.00,529.00,1,'Nemakit/Daldynian - Toyonian',520,530,'Early Cambrian (middle Terreneuvian, 530 Ma)',525,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'40',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',214,0,'Marcovella dominant. Other reef builders are Microphytolites and  Renalcis',58,109,-2430655,911425,'Russia','Asia',624,'',58,109,'WAHR','80848',1.9011070649,-65.6263885143,1.9011070649,-65.6263885143,1.9011070649,-65.6263885143,-11.4973,-5.34925,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Monte Lieggio, Salerno',235,'','Triassic','Upper Triassic','Norian','Norian',208.50,228.00,18,'late Carnian - middle Hettangian',218,215,'Late Triassic (mid Norian, 217.8 Ma)',210,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1b','Intraplatform basin','1','Above fair weather wave base','8','Serpulids, worms, vermetids','3','Microbes','11','Serpulids - algae - microbes',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',215,1479,'Very small \'mounds\' with serpulids, algae, bivalves and brachiopods and spongiostromate microbes. \nBoundstone facies types:\nMicrobialite-serpulid bindstone\nMicrobialite-serpulid bafflestone\nMicrobialite-serpulid-sphinctozoan boundstone\n',40,14,2065182,1644188,'Italy','Europe',344,'2173',40.7417,14.9,'WAHR','73879',15.1291592562,27.0985087137,14.9639025181,27.1695902272,12.1435786575,18.2283185267,19.335,13.8681,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Valdeteja',236,'Valdeteja','Carboniferous','Mississippian','Serpukhovian','Serpukhovian/Bashkirian',315.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',318,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','2','Green algae','20','60','20',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation',NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',217,0,'Mounds of open platform.\nDominated by Donezella (alga?) and Petschoria (red algae).',42,-5,-1594411,790218,'Spain','Europe',304,'',42.9167,-5.3917,'WAHR','76870',-22.0134067367,2.96289647292,-22.0134067367,2.96289647292,-17.3292926893,-15.7738371036,-10.8086,7.65982,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Valdeteja II',237,'Valdeteja','Carboniferous','Mississippian','Serpukhovian','Serpukhovian/Bashkirian',315.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',318,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','3','Microbes','1','Corals','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',217,0,'Zoned with cyanophycean-bindstone at the base and masses of almost monospecific corals at the top.',42,-5,-625791,1249802,'Spain','Europe',304,'',42.9167,-5.3667,'WAHR','76871',-22.0230630218,2.97967535653,-22.0230630218,2.97967535653,-17.3380341315,-15.7569847419,-10.818,7.67584,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rudnig Sattle',238,'','Carboniferous','Pennsylvanian','Gzhelian','Stephanian',303.70,307.00,14,'Gzhelian - Asselian',290,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',303,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'17',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','2','Below fair weather wave base','2','Algae','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',219,713,'Almost only phylloid algae: Eugonophyllum, Epimastopora, Archaeolithophyllum\nAlso Anthracoporalla\nRare forams, bryozoans and sponges\nCyanophyceans seem to be important.\nImportance of cement not mentioned, nor figured',46,13,-1551260,2597005,'Austria','Europe',301,'',46.55,13.2167,'WAHR','49710',-13.374327712,28.0275469142,-13.374327712,28.0275469142,-9.81137164646,2.85261362432,-12.5544,23.3963,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Herrlingen',239,'','Jurassic','Upper Jurassic','Kimmeridgian','Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',153,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1c','Epeiric sea','2','Below fair weather wave base','11','Siliceous sponges','3','Microbes','33','Siliceous sponges - microbes - (Tubiphytes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','2','6 to 24 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',220,0,'Siliceous sponges, cyanophyceans, bryozoans, serpulids and tubiphytes',48,9,4819748,1163841,'Germany','Europe',331,'',48.4056,9.8972,'WAHR','68425',28.5622350045,24.9571288773,28.5622350045,24.9571288773,33.8448545214,26.4492991025,39.8784,18.0247,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Torinosu, Sakawa, Shikoku',240,'Torinosu','Jurassic','Upper Jurassic','Tithonian','Tithonian/Berriasian',139.80,152.10,22,'late Tithonian - early Valanginian',141,145,'Jurassic/Cretaceous Boundary (145 Ma)',145,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',222,410,'Shimanto Terrane?\nAdditionally encrusting algae (solenoporaceans) and forams important.\nHexacorals and spongiomorphs about equally important.\nPlenty of siliclastic input',33,133,7174444,10830607,'Japan','Asia',625,'469',33.5,133.2667,'WAHR','68310',57.4690103619,148.218284917,57.4690103619,148.218284917,51.7809251239,151.499319089,40.2331,135.517,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Immouzer',241,'','Jurassic','Upper Jurassic','Oxfordian','Oxfordian',157.30,163.50,21,'late Bathonian - early Tithonian',151,160,'Late Jurassic (Oxfordian, 160.4 Ma)',157,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','1','Corals','4','Stromatoporoids','65','Corals - spongiomorphids - oysters - serpulids',NULL,NULL,'10','90','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',223,333,'Corals and spongiomorphids as main constituents.\nOyster shells and serpulids also important.',30,-9,2852727,-962428,'Morocco','Africa',714,'',30.6667,-9.5,'','',16.1230371698,-0.275320282338,16.1230371698,-0.275320282338,22.1098050544,-1.59102555669,28.3536,-7.60555,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Diezma',242,'','Carboniferous','Mississippian','Serpukhovian','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',323,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','2','Algae','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',224,0,'Lat 37.3167	Long -3.3167',37,-3,-2358024,615970,'Spain','Europe',304,'',37.9,-4.01,'WAHR','76854',-31.8148858537,-1.24714204663,-31.8148858537,-1.24714204663,-19.9238478743,-22.0959153446,-16.2416,5.65496,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Marbella',243,'','Carboniferous','Mississippian','Serpukhovian','Serpukhovian',323.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',323,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','3','Microbes','32','Cyanophyceans - corals - (forams) - (bryozoans) - (hydrozoans)','1','Red algae','70','0','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',224,0,'Lat 36.5167 Long -4.8833',36,-4,-2365274,447773,'Spain','Europe',304,'',37.01,-5.01,'WAHR','76855',-32.0979927423,-2.61256128622,-32.0979927423,-2.61256128622,-20.3581780015,-23.2789338091,-16.601,4.46948,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bianyang, Ziyun County, Guizhou',244,'Mobo','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',225,298,'Algae not mentioned in description of boundstone facies (ref. 225) but thich Archaeolithoporella crusts described by ref. 298 in surrounding facies.',25,106,-883589,8971458,'China','Asia',602,'662',25.65,106.5833,'WAHR','47458',-15.5549562934,105.947622448,-15.5549562934,105.947622448,6.49005986833,123.963513398,4.64561,98.3461,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hanlong, Guizhou',245,'','Permian','Lopingian','Wuchiapingian','Wuchiapingian',254.10,259.80,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',255,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','','Unknown','1','Above fair weather wave base','1','Corals','9','Tubiphytes','34','Corals - Tubiphytes',NULL,NULL,'60','0','40',0,'no',0,'no',NULL,NULL,NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',225,0,'Framework of rugose corals and Tubiphytes.\nEnvironment doubtful',25,106,-865976,8999613,'China','Asia',602,'',25.6833,106.8833,'','',-17.5043019969,105.988099787,-17.4979362755,105.978859944,-0.558910182868,129.929467642,1.8256,99.0444,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Madonie, Sicily',246,'','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,3,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','6','Calcisponges','6','Calcisponges','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Less than 30% micrite','2','10-25% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',34,149,'Description taken from reef 26.',37,13,1783188,1405704,'Italy','Europe',344,'',37.8014,13.9833,'WAHR','38016',NULL,NULL,NULL,NULL,13.9002527437,18.2161891709,20.658,10.9147,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Rötelstein',247,'Plassenkalk','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',152,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','30','60',0,'no',0,'no','2','6 to 24 reef building species','12','2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',227,0,'Ellipsactinia (hydrozoa) reefs.\nSome coral-chaetetid-boundstones are also present.',47,13,4118085,1826665,'Austria','Europe',301,'',47.5833,13.9167,'WAHR','36222',23.9006526866,29.105879604,23.9006526866,29.105879604,26.1003233878,25.699883684,33.5373,23.0136,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Krahstein',248,'Plassenkalk','Jurassic','Upper Jurassic','Kimmeridgian','upper Kimmeridgian',152.10,157.30,21,'late Bathonian - early Tithonian',151,155,'Late Jurassic (Kimmeridgian, 154.7 Ma)',152,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','4','Stromatoporoids','1','Corals','10','Scleractinian corals - (chaetetids, stromatoporoids-hydrozoans-spongiomorphids) - algae - microbes',NULL,NULL,'10','60','30',0,'no',0,'no','2','6 to 24 reef building species','19','2','Baffler guild',NULL,NULL,'1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','3','High production of reefal debris','0','',0,'No or unknown reservoir potential',227,0,'coral-chaetetid patch reefs',47,13,4115014,1831432,'Austria','Europe',301,'',47.5833,13.9833,'WAHR','36223',23.9207945849,29.1498035454,23.9207945849,29.1498035454,26.0792482867,25.7440571615,33.5072,23.0536,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Djebel Tebaga II',249,'','Permian',NULL,NULL,'Kazanian/Tartarian',268.80,272.30,15,'Sakmarian - Kungurian',277,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','20',NULL,NULL,NULL,'2','10 - 100 m','60','100',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','9','Tubiphytes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','30','70',0,'no',0,'no','3','25 or more reef building species',NULL,'3','Binder guild','1','Present','1','Present','2','Medium zonation','2','Medium zonation','2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',229,278,'East-west trending reef belt\nMainly composed of Archaeolithoporella and Tubiphytes.\nAbstract of ref. 1327:\nTubiphytes and Archaeolithoporella are two important building calcareous algae in Permian reefs, especially in the Upper Murghabian of Jebel Tebaga (Tunisia). Systematics of the two algae (probably blue-green) is reviewed.\nTubiphytes and Archaeolithoporella were previously poorly known in the Upper Permian beds from Jebel Tebaga. These algae, always associated, take a prominent part in the building of the reefs. The analysis of the reefs, 20 m thick and 60 m wide, shows the following biological sequence: a) Prereefal first stage: settling of clay-marly sediments including several calcareous organisms, mainly Calcisponges and Bivalves. b) Second stage: Whole organisms or\nremains are encrusted by a first generation of the stromatolitic algae Archaeolithoporella, which will be colonized in a second time by the blue-green algae Tubiphytes. The former, rapidly attached, show a growth which follow the exact shape of the anfractuosites of Archaeolithoporella laminae. Open spaces and cavities created by the growth of alga assemblages are progressively filled by an internal micritic sediment with pellets. This open space filling by a fine material suggests a growth of Tubiphytes in restricted conditions, where the luminosity is lessen, indicating a sciaphilous alga. c) Third stage: Attachment and proliferation of a second generation of dense Archaeolithoporella.\n    They encrust Tubiphytes and other substrates, growing laterally and vertically. The crusts of Archaeolithoporella are parallel to the substrate at the beginning of the growth, but a few millimeters higher appears a mammillated crust, which gives, at the end of the growth, some nodules with concentric laminations, often trapped in interstitial micritic fills.\n These nodules are called here tebagites. This biologic sequence occurs repeatly from the bottom to the top of the reef. Furthermore, examination of relations between the growth of Archaeolithoporella and the early diagenetic features (cements) allows to establish, in addition to the biologic sequence, a diagenetic sequence summarized as following: -\n    growth of dense micritic laminae. - Growth of clear and dark laminae (i.e. typical stage). - Growth of vesicular laminae filled by fibrous or botryoidal cement. - Stop of algae growth, followed by a filling of the interalgal porosity with a botryoidal cement or an internal peloidal sediment. In conclusion, Tubiphytes and Archaeolithoporella constitute the main building organisms of the studied reefs. Identical assemblages are known from the Lower Permian of Carnic Alps,\nfrom Upper Permian of Yugoslavia and Capitan Reef in U.S.A. as well, under the name of Calcisponges/Algal/Cements\n    Reefs (-CAC, new abbreviation). ',33,10,-632930,2062202,'Tunisia','Africa',715,'1327, 1376',33.4167,10.25,'','',-7.35835444208,18.9171955158,-7.35835444208,18.9171955158,-5.98258901575,11.7281148863,-7.5808,18.5902,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Palazzo Adriano, Sicily',250,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','9','Tubiphytes','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',230,257,'Wordian megablocks from eroded platform.\nTubiphytes-Archaeolithoporella reefs with plenty of cement.',37,13,-368022,2367011,'Italy','Europe',344,'',37.7,13.3833,'WAHR','75474',NULL,NULL,NULL,NULL,-1.63408379097,17.4171638894,-4.96599,21.6947,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Roccapalumba, Sicily',251,'Lercara','Permian','Cisuralian','Artinskian','Artinskian',283.50,290.10,15,'Sakmarian - Kungurian',277,285,'Early Permian (Artinskian, 286.8 Ma)',280,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','2','Algae','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present',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',230,268,'Allochthonous blocks',37,13,-719451,2432113,'Italy','Europe',344,'',37.8,13.6333,'WAHR','75509',NULL,NULL,NULL,NULL,-10.2534692746,9.32815119052,-11.7437,19.3902,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wegener Halvo, Greenland',252,'Wegener Halvo','Permian','Guadalupian','Wordian','Wordian-Capitanian',259.80,268.80,16,'Roadian - Changhsingian',261,265,'Middle Permian (Wordian/Capitanian Boundary 265.1 Ma)',265,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick','150',NULL,NULL,NULL,'3','More than 100 m',NULL,'22',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','7','Bryozoans','2','Algae','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','2','Green algae','60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',232,0,'Fenestrate bryozoans as main framework builders.\nAdditionally trepostome bryozoans, ?phylloid algae, encrusting algae and tubular forams.\nSubordinate brachiopods, ostracods and crinoids.\n\nAbstract of ref. 232:\nThe Upper Permian of Jameson Land includes two carbonate sequences, the Karstryggen and Wegener Halvo formations. The Karstryggen Formation contains hypersaline carbonates and localized evaporites that were heavily weathered and dissected prior to deposition of the overlying strata. The overlying Wegener Halvo Formation represents an abrupt and extensive marine inundation over the underlying karstified Karstryggen surface. Bryozoan-brachiopod-algal-cement buildups of the Wegener Halvo Formation are localized on karstic highs, and show up to 150 m of depositional relief. In-situ mound-core deposits are flanked by allodapic limestones, which pass laterally into intermound calcareous shales.\nThe diagenetic histories of the core and flank facies are very different. Core facies porosity was intially obliterated by marine cements, but repeated meteoric exposure altered unstable core facies constituents. This alteration produced extensive secondary porosity through grain and cement leaching with local collapse brecciation. Flank strata, however, underwent little sea-floor diagenesis, and low permeability and mineralogically stable grain composition protected these strata from meteoric alteration.\nEarly cementation and stabilization of core strata led to minimal burial-diagenetic porosity loss. Uncemented flank beds, however, underwent profound mechanical and chemical compaction during this stage. Thus, at the time of hydrocarbon generation, distal flank beds had less than 2% porosity, coarse upper flank beds had 5-10% remnant primary porosity, and core facies deposits had 8-12% secondary pore space.\nHydrocarbons generated from surrounding marine shales charged many of the bioherms with oil. Subsequent fracturing and hydrothermal fluid flow, however, flushed hydrocarbons and filled pores with ferroan calcite, barite, fluorite, galena, and baroque dolomite. This heating and flushing is thought to have been especially intense in the Wegener Halvo region. Thus, more basinal areas may still have reservoirs containing significant oil in equivalent Upper Permian limestones.\nIf, as is likely, the sea level changes affecting the Greenland Permian were eustatic, then this study may provide significant clues to porosity development throughout the largely unexplored northern Zechstein basin and the Arctic basin of the Barent Sea. This study also provides some important connections to the probably time-equivalent Guadalupian carbonate reservoir rocks of west Texas-New Mexico and Wyoming.',71,-23,3922684,1562034,'Denmark','Europe',330,'',71.7167,-23,'','',32.7487411635,21.4913469318,32.7487411635,21.4913469318,30.3855093477,10.7708866701,27.8705,17.2359,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('N-Amdrup Land, Greenland',253,'','Carboniferous','Pennsylvanian','Moscovian','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',309,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'60','0','40',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation',NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',233,234,'Crinoids as major constituents in lower part.\nBryozoans and cements important in upper parts.',80,-17,3469447,1133269,'Denmark','Europe',330,'',80.6667,-17,'','',21.201993413,7.15217203231,21.201993413,7.15217203231,20.4716807952,-13.2735310291,23.0316,9.13849,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('S-Amdrup Land, Greenland',254,'Kap Jungersen','Carboniferous','Pennsylvanian','Moscovian','lower Moscovian',310.00,315.20,13,'Bashkirian - Kasimovian',302,315,'Early/Middle Carboniferous (Baskirian/Moscovian boundary, 314.6 Ma)',310,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','7','Bryozoans','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'60','0','40',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',2439,234,'Early to late Moscovian. No detailed description.',80,-16,3491306,1128674,'Denmark','Europe',330,'',80.8333,-16.8333,'','',21.3672761526,7.1156967541,19.830267502,6.18171012183,18.9702002419,-13.011450724,22.768,8.59276,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Skyros',255,'','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,3,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',235,0,'Biostromal rather than bioherm morphology\nUpper parts of the reef mounds with solitary corals.\nDiversity increases upwards in reef development.',38,24,-1016966,3179852,'Greece','Europe',338,'',38.8667,24.5,'WAHR','74927',0.0951013094997,33.9344699654,0.0951013094997,33.9344699654,-2.38287949724,30.4636730655,-6.98681,28.5269,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nishino-dai',256,'','Carboniferous','Pennsylvanian','Moscovian','upper Atokan',310.00,312.00,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',311,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','35','Chaetetids - corals - cyanoyphyceans - algae - (bryozoans)',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',236,0,'Colonial rugose corals predominate.\nUpper Atokan, Fusulinella biconica zone',34,131,1538339,12079235,'Japan','Asia',625,'',34.1833,131.15,'','',14.0605408544,133.538926535,14.0508638814,133.599768967,11.2599438572,65.9827467094,10.3772,93.933,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Akiyoshi-dai',257,'','Carboniferous','Mississippian','Visean','middle-upper Visean',336.00,345.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','40',NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','1','Corals','2','Algae','19','Algae, microbes - bryozoans - corals - (sponges/stromatoporoids)','1','Red algae','90','10','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present','2','Medium zonation','3','Pronounced zonation','1','Less than 30% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',237,1363,'Nagatophyllum satoi zone\nAbout 40 m thick.\nRugose colonial corals extremely dominant. Additionally encrusting algae (solenoporaceans) and bryozoans.\nBryozoans forming individual reefs in Akago area.\n\nRef. 1897:\nStrong horizontal zonation:\nLower reef front (frame-bindstone)\nUpper reef front (framestone)\nreef crest (frame- bindstone)\nouter reef flat (frame- bafflestone)\ninner reef flat (bindstone)\nback reef slope (frame- bindstone)\n\nExamples of coral genera in reef core:\nPetalaxis\nOzakiphyllum\nPseudopavona\nIvanovia\nSiphonodendron\nEchigophyllum\nHiroshimaphyllum\nAmygdalophylloides\nGeyerophyllid gen. nov.\nTaisyakuphyllum\nDibunophyllum',34,131,76300,14610249,'Japan','Asia',625,'1897',34.2333,131.2167,'','',0.546648548155,123.60135322,-1.20524743777,121.480770373,8.35114889684,58.5329118512,-5.69054,78.0679,'Kiessling','Kiessling','2021-05-28 15:21:12','2022-08-25 17:30:32'),('Minamidai, Akiyoshi-dai',258,'','Carboniferous','Mississippian','Serpukhovian','Serpukhovian-Bashkirian',315.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',318,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'10',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','3','Microbes','4','Stromatoporoids','35','Chaetetids - corals - cyanoyphyceans - algae - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present',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',238,239,'Millerella yowarensis zone to Pseudostaffella antiqua zone\nUpper Serpukhovian to middle Bashkirian.\nMicrobes/algae always dominating over chaetetids. Maximum chaetetid cover is 27%. Microbes 50-72%, corals max. 8%.\nStratigraphic range of chaetetids from Nagatophyllym satoi Zone (upper Visean) to the Beedina akizoshiensis Zone (upper Moscovian).',34,131,77658,14604452,'Japan','Asia',625,'295, 362, 2166',34.2,131.1667,'WAHR','76321',14.7163449564,127.012310018,14.7163449564,127.012310018,4.64387098066,67.4422367629,4.67475,87.5865,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ryugoho, Akiyoshi-dai',259,'','Carboniferous','Mississippian','Serpukhovian','Serpukhovian-Bashkirian',315.20,330.90,12,'middle Visean - Serpukhovian',329,325,'Late Mississippian (Serpukhovian, 327 Ma)',318,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','3','Microbes','1','Corals','35','Chaetetids - corals - cyanoyphyceans - algae - (bryozoans)',NULL,NULL,'40','40','20',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',240,362,'Reef development from Millerella yowarensis zone (Serpukhovian-early Bashkirian) to Profusulinella beppensis zone (latest Bashkirian).\nStromatolites and tabulate corals as main reef builders.',34,131,1539769,12084787,'Japan','Asia',625,'',34.2167,131.2,'','',14.7297085567,127.042608495,14.7297085567,127.042608495,4.63576919544,67.473510561,4.6873,87.6162,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Olinalá, Guerrero',260,'Olinala','Permian','Guadalupian','Wordian','Wordian-Capitanian',259.80,268.80,16,'Roadian - Changhsingian',261,265,'Middle Permian (Wordian/Capitanian Boundary 265.1 Ma)',265,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','9','Tubiphytes','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,'10','40','50',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',241,1844,'Richthofenid brachiopods are also important.',17,-98,-933984,-4648520,'Mexico','North America',105,'',17.8,-98.7333,'WAHR','75577',-0.470813004538,-38.8519350925,-0.470813004538,-38.8519350925,-10.0283248812,-47.3046683365,-5.27032,-41.6682,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Klamath Mountains, California',261,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','2','Algae','2','Algae','25','Palaeoaplysina - phylloid algae','2','Green algae','10','80','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',242,0,'Crinoids, brachiopods and bryozoans are also common.',40,-122,2053609,-4623573,'United States','North America',101,'',40.8667,-122.2833,'WAHR','75627',15.4370666803,-40.6612033172,15.4370666803,-40.6612033172,12.558760324,-61.7686058744,11.5476,-44.173,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('El Portachuelo',262,'Palmarito',' 	Permian',NULL,NULL,'Leonardian/Guadalupian',268.00,280.00,15,'Sakmarian - Kungurian',277,275,'Early Permian (late Kungurian, 275 Ma)',270,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','11','Siliceous sponges','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,'20','80','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',243,244,'Lithistids, hexactinellids and sphinctozoans. \nOther fauna bryozoans, brachiopods and some corals.',8,-71,-533619,-3707077,'Venezuela','South America',201,'',8.0333,-71.35,'WAHR','41510',-7.00806500154,-35.6008050674,-7.00806500154,-35.6008050674,-10.0559719584,-41.2043279006,-4.86116,-34.2043,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baske Ostarije',263,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,3,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',245,0,'Murghabian (Wordian). Neoschwagerina-zone',44,15,180512,2999128,'Croatia','Europe',308,'',44.5,15.2333,'WAHR','62289',-2.1497443903,32.323827768,-2.1497443903,32.323827768,2.62114334755,24.1528971168,-1.34879,27.6285,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baske Ostarije II',264,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','6','Calcisponges','36','Bryozoans - sponges - microbes',NULL,NULL,'60','40','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,'3','Pronounced zonation',NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',245,0,'Murghabian (Wordian). Neoschwagerina-zone.\nSuccession of bryozoan dominated part to calcisponge-dominated part.',44,15,182748,2999883,'Croatia','Europe',308,'',44.5167,15.225,'WAHR','75510',-2.13684873286,32.3359865057,-2.13684873286,32.3359865057,2.63826840487,24.1574470728,-1.33296,27.6365,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Baske Ostarije III',265,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','7','Bryozoans','37','Sponges - microbes - Tubiphytes - (worms)',NULL,NULL,'40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',245,269,'No dimensions given but smaller than 264.\nBryozoans also important (ref. 269).',44,15,182446,2998773,'Croatia','Europe',308,'',44.5083,15.2167,'WAHR','62290',-2.13542107952,32.3258033334,-2.13542107952,32.3258033334,2.63467900719,24.1478084048,-1.33449,27.6264,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Azizia',266,'','Triassic','Upper Triassic','Carnian','Carnian',228.00,235.00,17,'Induan - early Carnian',235,230,'Late Triassic (Carnian, 232 Ma)',223,2,'0','Outcropping reef ',1,'True reef',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','2','Algae',NULL,NULL,'1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','High production of reefal debris','0','',0,'No or unknown reservoir potential',246,0,'',32,13,-290911,1856395,'Libya','Africa',715,'',32.5,13.0167,'','',8.39771830824,22.4009416689,8.39771830824,22.4009416689,-0.00523847556036,11.1916475071,3.57066,13.192,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hidaka, Hokkaido',267,'','Triassic','Upper Triassic','Carnian','Carnian',228.00,235.00,17,'Induan - early Carnian',235,230,'Late Triassic (Carnian, 232 Ma)',223,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','0',NULL,'','Unknown',NULL,NULL,'6','Calcisponges','6','Calcisponges',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',30,0,'',42,142,4099161,16737058,'Japan','Asia',625,'Baba pers.',42.8833,142.4667,'','',11.3854507631,163.433792879,11.3854507631,163.433792879,79.0155976218,-149.56549797,44.2217,129.421,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Naybandan',268,'Nayband','Triassic','Upper Triassic','Norian','upper Norian',208.50,214.00,18,'late Carnian - middle Hettangian',218,210,'Late Triassic (Norian, 213.2 Ma)',205,2,'0','Outcropping reef ',4,'Biostrome','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'100',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','6','Calcisponges','1','Corals','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild','1','Present',NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',249,56,'No description of reef facies in [56]',32,57,3574810,5841091,'Iran','Asia',505,'9, 1461',32.5,57.5667,'','36869',24.6408436783,67.798920127,30.4109322907,67.9775303581,24.5870003138,69.7547313763,-12.2022,43.8989,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Straza, Bled',269,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,3,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'4',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','6','Calcisponges','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','21','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',250,258,'Neoschwagerina beds.\nPlenty of debris, but not from the reefs',46,14,441555,3074767,'Slovenia','Europe',328,'',46.3708,14.1139,'WAHR','36241',-0.604872558379,33.6395560475,-0.604872558379,33.6395560475,4.14736527615,24.6191357378,0.506598,28.4497,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bohinjska Bela',270,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'4',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','6','Calcisponges','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',250,258,'Neoschwagerina beds.\nAutochthonous reef facies more widespread than in 269.',46,14,442296,3070769,'Slovenia','Europe',328,'',46.35,14.0708,'','',-0.587483967505,33.6076953783,-0.587483967505,33.6076953783,4.14978642689,24.5828260519,0.514205,28.4142,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Derbyshire, Great Britain',271,'','Carboniferous','Mississippian','Visean','Brigantian',331.00,336.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',329,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'31',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','7','Bryozoans','14','Brachiopods','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',252,366,'Bryozoans, molluscs and brachiopods as main constituents.\nMicrobial activity indicated by peloidal structure.',53,-1,-505301,525274,'United Kingdom','Europe',331,'611',53.0833,-1.5,'WAHR','76172',-30.8343090878,-8.02643176763,-25.6029324015,-4.9565297007,-4.45374211265,-26.771240013,-5.2969,3.09585,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Derbyshire II, Great Britain',272,'','Carboniferous','Mississippian','Visean','Asbian-Brigantian',330.90,340.00,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',332,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'31','271',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','7','Bryozoans','14','Brachiopods','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',252,487,'Bryozoans, molluscs and brachiopods as main constituents.\nMicrobial activity indicated by peloidal structure.\nCollections of Alroy refer mostly to trilobites.',53,-1,-492703,507804,'United Kingdom','Europe',331,'366, 611',53.2,-1.7333,'WAHR','5965',-30.7182681541,-8.18994880161,-27.4228451128,-6.21753839252,-4.38478120146,-29.9757345243,-5.7804,2.35906,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('El Nido, Philippines',273,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'8',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','1','Above fair weather wave base','15','Non-rudist bivalves','15','Non-rudist bivalves','68','Brachiopods - massive bivalves',NULL,NULL,'10','90','0',0,'no',0,'no','1','Less than 6 reef building species','3','2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',253,1988,'Neoschwagerina craticulifera zone.\nBiostromes of alatoconchid bivalves and richthofenid brachiopod.\nSome rugose corals are also present',11,119,-868946,10665314,'Philippines','Asia',563,'',11.15,119.3333,'','',-13.9109068657,130.851838044,-13.9109068657,130.851838044,11.15,119.3333,-10.5365,102.468,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lake Cumberland, Kentucky',274,'Fort Payne','Carboniferous','Mississippian','Visean','upper Osagean',342.00,346.70,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',343,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','15',NULL,NULL,NULL,'4','More than 1000 m','1500','15',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'40','0','60',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',254,368,'Crinoids are dominant macrofossils.\nMaximum thickness 15 m, lateral extension 1500 m at Owens Branch.\nSurrounded by siliciclastic sediments (abandoned delta slope).\nBioherm lithology described as bryozoan-coral-crinoidal wackestone.',36,-85,-3071992,-3569787,'United States','North America',101,'1714, 2410',36.95,-85.0167,'WAHR','76446',-35.1573255396,-54.6572305019,-35.1573255396,-54.6572305019,-14.1252480804,-90.4113447311,-25.8457,-34.1423,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Celina, Tennessee',275,'Fort Payne','Carboniferous','Mississippian','Visean','upper Osagean',342.00,346.70,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',343,3,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick','15',NULL,NULL,NULL,'3','More than 100 m','1500','20',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','13','Echinoderms','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'40','0','60',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',254,368,'Maximum thickness 15 m, lateral extension 1500 m at Owens Branch.\nSurrounded by siliciclastic sediments (abandoned delta slope).',36,-85,-3096308,-3628586,'United States','North America',101,'',36.5333,-85.5,'','',-35.0638126204,-55.3431923374,-35.0638126204,-55.3431923374,-14.3120305846,-90.9656731404,-26.0391,-34.7373,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Sheep Draw  and Dark Canyon, Capitan, New Mexico',276,'Tansill','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',262,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'500','86',0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','70','30',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',255,281,'Tansill stage\nCalcisponge-Archaeolithoporella-Tubiphytes boundstone, overlain by Parachaetetes boundstone and algal grainstone.',32,-104,508070,-3684483,'United States','North America',101,'',32.3833,-104.3111,'WAHR','47475',11.1591353022,-29.661876952,11.1591353022,-29.661876952,5.60667970801,-36.60567987,4.57686,-32.6325,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Qincaiyuan, Ziyun, Guizhou',277,'Jiyaopo','Permian','Lopingian','Wuchiapingian','Wuchiapingian',254.10,259.80,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',257,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick','5',NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species','6','1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',2617,181,'5 coral biostromes, up to 3.5 m thick. ',25,106,-881372,8917582,'China','Asia',602,'',25.75,106.0833,'WAHR','75027',-17.6050087901,105.236287622,-17.5982762489,105.227021008,-0.641547958707,129.210321528,1.44924,98.4258,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-17 11:55:24'),('Lop Buri',278,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'50',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','2','Algae','3','Corals - calcareous sponges (hydrozoans) - solenoporaceans - (Tubiphytes) - (bryozoans)','1','Red algae','70','30','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',260,0,'Neoschwagerina zone\nLoc. 15 and 17 of ref. 260.\nRugose corals dominating',14,100,-2629804,8438842,'Thailand','Asia',604,'',14.7167,100.9167,'','',-30.4275674535,115.917437864,-30.4275674535,115.917437864,-6.16229926313,102.224201718,-17.6168,98.21,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Phetchabun',279,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'5',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',260,0,'Reef formed by massive Waagenophyllidae.\nNeoschwagerina zone\nLocalities 27, 28, 29 of ref. 260',16,101,-2433415,8418371,'Thailand','Asia',604,'',16.25,101.2667,'','',-29.1176568336,114.920398889,-29.1176568336,114.920398889,-4.71998025143,101.601308685,-16.2718,97.3636,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Phet Buri',280,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,2,'0','Outcropping reef ',1,'True reef','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',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',260,0,'Neoschwagerina zone\nLoc. 8 of ref. 260.\nMassive colonies of Waagenophyllidae',13,99,-2891200,8389096,'Thailand','Asia',604,'',13.0167,99.9167,'','',-32.4498768223,97.6721729595,-32.4498768223,97.6721729595,-26.5364533726,99.8663204729,-29.8552,99.371,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lom Sak',281,'','Permian','Guadalupian','Wordian','Wordian',265.10,268.80,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',267,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'3',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',260,0,'Loc. 32, 33 of ref. 260.\nlenses of Waagenophyllidae and small solitary corals.',16,101,-2368549,8415344,'Thailand','Asia',604,'',16.7333,101.4167,'','',-28.6768016175,114.640816514,-28.6768016175,114.640816514,-4.24357994236,101.435549087,-15.8217,97.127,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Lemhi Range, Idaho',282,'','Carboniferous','Pennsylvanian','Gzhelian','Virgilian/Asselian',295.00,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',299,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','16',NULL,NULL,NULL,'3','More than 100 m',NULL,'20',NULL,2,'Cold - water','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','2','Algae','25','Palaeoaplysina - phylloid algae','2','Green algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',261,0,'Especially refering to Birch Pass buildup.\nTubular form. \nPaleoaplysina, Eugonophyllum, Archaeolithophyllum and tubular forams are important.\nMaximum thickness 16 m.\n\nAbstract of ref. 261:\nThe plate-shaped calcareous hydrozoan ? Palaeoaplysina Krotov is the main fossil in Late Pennsylvanian and Early Permian carbonate buildups in the Lemhi Range and Arco Hills of east-central Idaho (USA) Palaeoaplysina has an internal subparallel canal system imbedded in cellular tissue, and mamelon-like surface protuberances. Other fossils in the buildups include the calcareous phylloid alga Eugonophyllum, other unidentified phylloid algae, crustose bryozoans, and less common gastropods, crinoids, and brachiopods. Buildup sediment accumulated primarily by the baffling and entrapment of loose carbonate pellets, lime mud, and skeletal fragments in protected pockets and hollows\nbetween Palaeoaplysina and algal plates. There is a continuum between tabular and lenticular buildup geometries.\n    Broad tabular buildups are typically 2-10 m thick and as much as 15 km wide. The basal surfaces of the tabular\nbuildups conform to previous sea-floor topography, whereas upper surfaces are relatively flat and planar, suggesting that the buildups were limited in upward growth because they formed in the uppermost subtidal zone. The abundance of porcelaneous tubular foraminifers (resembling apterrinellids and Hedraites), which encrusted some unpreserved organisms, suggests that some buildups were carpeted by unfossilized vegetation such as noncalcareous algae. Strongly\nlenticular buildups are typically 2-16 m thick and a few tens to hundreds of meters wide. Most were large enough to modify depositional conditions nearby, resulting in fore-mound and back-mound beds. All of the lenticular buildups, and some of the tabular ones, stood topographically above the adjacent sea floor while they formed. Some buildups are stacked one above another. Others are in offlapping sequences which also include lenticular beds of crinoidal-bryozoan lime wackestone and grainstone. ',43,-112,2099579,-3896203,'United States','North America',101,'',43.8167,-112.7833,'','',14.6122118684,-35.7086140008,14.6122118684,-35.7086140008,9.29538826575,-56.4648439256,11.2771,-37.5885,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bihendula',283,'','Jurassic','Middle Jurassic','Callovian','Callovian',163.50,166.10,21,'late Bathonian - early Tithonian',151,165,'Middle Jurassic (Callovian, 164.8 Ma)',163,1,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf',NULL,NULL,'1','Corals','1','Corals','2','Corals only',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',262,1307,'Abstract ref. 262:\nTopographically, the southern half of Somalia is comparatively flat, with elevations of < 350 m above sea level. The northern half of the country rises northward to an elevation of 2000 m, where it drops off sharply to the Gulf of Aden. All of Somalia was a peneplain at the end of Paleozoic time. Jurassic limestone then was deposited uniformly over the entire country, but post-Jurassic erosion removed a considerable thickness of these rocks, locally exposing basement. A Cretaceous sea then covered all of Somalia. Transgressions and regressions took place during Cretaceous time, and locally the Cretaceous is disconformable with the overlying Eocene. Marine Eocene sedimentary rocks cover the northern half of Somalia, but are absent in southern Somalia except for a narrow strip along the coast where marine Eocene is present in the subsurface together with marine Oligocene, Miocene and Pliocene, the latter present locally in outcrops. Southern Somalia was subjected to epeirogenic uplift at the end of Cretaceous time and has remained above sea level ever since, except in the coastal areas. The rift faulting of middle and late Tertiary time uplifted the northern half of the country with the result that post-Eocene marine sedimentary rocks are known only along a narrow strip of the coast. There is no evidence of major compressive folding in Somalia, but northeast-southwest-trending anticlines of gentle dip have been mapped in Tertiary rocks in the north and identified in the subsurface in central and southern Somalia. The structures apparently were caused either by rejuvenation of Jurassic fault blocks causing arching of younger sediments, or by leaching of thick underlying evaporites. The most promising region for oil and gas prospecting in Somalia is the Mesozoic shelf and reef area around the Somali embayment and around the Nogal uplift. Secondary prospective oil and gas regions in Somalia are the coastal and offshore marine Tertiary sedimentary rocks. Stratigraphic traps in clastic sedimentary rocks caused by facies changes or overlaps against the uplift regions of Somalia, and monoclinal porosity pinchouts in carbonate sedimentary rocks are other possibilities. Commercial oil and gas deposits are probably present in Somalia. Quinqueloculina inconstans, Epistomina mosquensi, Cristellaria contralis, Lenticulina polonica, E. stellicostata, C. nodosa, E. ornata, Pseudocyclammina sequana, Orbitolina concava O. lenticularis, O. discoidea, Globigerina infracretacea, G. washitaensis, Robulus, Globotruncana, Gumbelina, Globorotalia velascoensis, G. crasia, Anomalina granosa, Cibicides, Sakesaria, Alveolina, Lockhartia tipperi, Nummulites somaliensis and Daviesina danieli are mentioned. ',10,45,-1930206,3513132,'Somalia','Africa',709,'',10.1667,45.1667,'','',-25.1677792246,35.3888539288,-25.1677792246,35.3888539288,-21.9043768954,31.4728384798,-11.9541,29.8472,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Scorpion, Tularosa, New Mexico',284,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','2','Algae','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',275,330,'Stromatactis very important. Cements make up 50-80 % of rock volume. Micrite with forams, brachipods, crinoids, bryozoans, mollusks, and algae.\nBotroyidal cements very prominent (ref. 339).\nReview paper (ref. 263), no description of particular reef.',33,-105,344079,-3891261,'United States','North America',101,'263',33.1,-105.9833,'','',1.0871403555,-35.8206093433,1.0871403555,-35.8206093433,-2.39645219462,-56.523481404,-1.40447,-37.3299,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Phrae',285,'','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'1',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','6','Calcisponges','11','Siliceous sponges','45','Siliceous sponges - calcisponges - microbes - (algae)',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species','20','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',265,296,'Calcisponges, sclerosponges and hexactinellids in decreasing order of abundance.\nReef or reefal limestone mentioned but no buildup structure is evident.',18,100,-2833694,9570844,'Thailand','Asia',604,'',18.1167,100.1167,'WAHR','34656',-19.2076071945,90.6972488383,-19.2076071945,90.6972488383,-13.493776054,101.640119053,-17.3481,89.0953,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Amanda, Adriatic Sea',286,'','Permian','Cisuralian','Sakmarian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',289,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','9','Tubiphytes','2','Algae','24','Tubiphytes - algae - cyanophyceans - (bryozoans) - (sponges)','1','Red algae','0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',2,'Actual reservoir',267,0,'Well data only.\nTubiphytes and Archaeolithoporella boundstones',45,12,28520,3032718,'Italy','Europe',344,'',45.4167,12.9833,'','',-10.4556305042,28.3957634805,-10.4556305042,28.3957634805,-5.62983577279,9.8445670318,-8.49047,23.6376,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Brunnachhöhe',287,'','Carboniferous','Mississippian','Visean','Visean',330.90,346.70,12,'middle Visean - Serpukhovian',329,330,'Late Mississippian (Visean/Serpukhovian boundary, 330.9 Ma)',336,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1e','Open-marine shelf','1','Above fair weather wave base','1','Corals','1','Corals','2','Corals only',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',271,0,'Limestone blocks in Olistostrome.',46,13,-2161931,2249289,'Austria','Europe',301,'',46.8333,13.8,'','',-44.7930343587,19.2745124893,-44.7930343587,19.2745124893,46.8333,13.8,-17.4653,19.3742,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Zeitz',288,'','Permian','Lopingian','Changhsingian','Zechstein 1',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'30',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'80','20','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','1','Present',1,'Potential reservoir',128,0,'Known only from wells',51,12,2221961,2608929,'Germany','Europe',331,'',51.05,12.1333,'','',27.3500025081,31.1077742143,27.3534045418,31.1082855938,23.8499011217,27.1146039511,16.5155,23.3659,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hess Ranch and Leonard Mt., Glass Mountains, Texas',289,'Lenox Hills','Permian','Cisuralian','Sakmarian','Sakmarian',290.10,295.00,15,'Sakmarian - Kungurian',277,290,'Early Permian (Sakmarian, 292.6 Ma)',287,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','25',NULL,NULL,NULL,'2','10 - 100 m','60','15',NULL,0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','7','Bryozoans','6','Calcisponges','14','Sponges - bryozoans - (microbes)',NULL,NULL,'80','20','0',0,'no',1,'yes','2','6 to 24 reef building species','18','2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',272,2500,'Bryozoans very dominant.\nSome calcisponges and brachiopods within the delicate framework thickets.\nMaximum dimension of mounds: 25 m thick, 60 m wide.\n17 bryozoan species indicated.\nAge indicated as Wolfcampian/Leonardian, but recent data suggest Sakmarian',30,-103,412407,-3606136,'United States','North America',101,'',30.35,-103.2833,'WAHR','43533',-2.12401864085,-35.319376024,-2.12401864085,-35.319376024,-5.18817613474,-52.6002434721,-3.89458,-36.3626,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jiannan well, Hubei',290,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,2,'1','Seismic data available ',1,'True reef','3','101-500 m thick','156',NULL,NULL,NULL,'4','More than 1000 m','5000',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','4','Stromatoporoids','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',2,'Actual reservoir',274,290,'Several reefs mapped by logging. Reef facies extends without interruption for at least 5 km.\r\n\r\nComments from Tian & Wang, 2021:\r\n\r\nReef builders:\r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, stromatoporoid sponge, bryozoans, and hydrozoans\r\nBinding organisms: Archaeolithoporella, Tubiphytes (Shamovella), and cyanobacteria.\r\n\r\nReef dwellers:\r\nEchinoderms, ammonites, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals\r\n\r\nRock type and reef-related depositional characteristic:\r\nFore-reef slope: spiculitic-calcispherical cherty wackestone with reef breccias.\r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella.\r\nReef flat (reef crest): packstone with reef breccia.\r\nReef base: echinodermal packstone to grainstone.\r\nBack-reef lagoon: bioclastic packstone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type:\r\nMetazoan reef at the shallow carbonate platform margin\r\n\r\n\r\n\r\n\r\n\r\n',30,108,-187302,8987710,'China','Asia',602,'662',30.4333,108.5333,'',NULL,-10.5546788941,106.886590811,-10.5546788941,106.886590811,11.2119239504,125.869019582,9.4979,96.8194,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-17 17:45:06'),('Huangnitang, Hubei',291,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,2,'0','Outcropping reef ',2,'Reef mound','3','101-500 m thick','135',NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','6','Calcisponges','4','Stromatoporoids','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','3','High production of reefal debris','1','Present',1,'Potential reservoir',274,290,'Calcisponges, Rhabdactinia and tabulozoans as main reef builders.\r\nOccuring at margin of intraplatform basin.\r\nAbundant sponge spicules in surrounging facies indicate deeper water than at 223.\r\n\r\nComments from Tian & Wang, 2021: \r\nReef builders: \r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, stromatoporoid sponge, bryozoans, and hydrozoans.\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria.\r\n\r\nReef dwellers:\r\nEchinoderms, ammonites, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic:\r\nFore-reef slope:\r\nspiculitic-calcispherical--\r\ncherty wackestone with reef\r\nbreccias\r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, and sponge framestone with the encrusting Archaeolithoporella\r\nReef flat (reef crest): packstone with reef breccia\r\nReef base: echinodermal packstone to grainstone\r\nBack-reef lagoon: bioclastic packstone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type:\r\nMetazoan reef at the shallow carbonate platform margin.\r\n\r\n\r\n\r\n\r\n\r\n',30,108,-218164,9038798,'China','Asia',602,'',30.05,108.9333,'WAHR','74930',-10.8712203858,107.301416299,-10.8712203858,107.301416299,10.8192992813,126.210236921,9.40642,97.3342,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-17 15:49:34'),('Taiyun, Sichuan',292,'Changxing','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','4','Stromatoporoids','8','Coralline sponges (chaetetids) - microbes - corals',NULL,NULL,'0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',1,'Potential reservoir',274,0,'comment from Tian & Wang (2021)\r\n\r\nReef builders: \r\nFrame-building and baffling organisms:\r\nhypercalcified sphinctozoan and inozoan sponges and hydrozoans Binding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria. \r\n\r\nReef dwellers:\r\nEchinoderms, ostracodes, ammonites,\r\ntrilobites, bryozoan, brachiopods,\r\ngastropods, benthic foraminifera, calcareous algae, and rugose corals\r\n\r\nRock type and reef-related\r\ndepositional characteristic\r\n\r\nReef core: less sponge framestone with the encruster Archaeolithoporella, more sponge bafflestone and Tubiphytes-cyanobacteria bindstone\r\nReef flat: dolomitic bioclastic packstone with brachiopod fragments, foraminifera, algae, and reef breccia.\r\nReef crest: dolomitic bioclastic wackestone to packstone with algae and evaporite\r\nReef base: bioclastic packstone\r\n\r\nSkeletal mound at the carbonate intraplatform',29,107,-283793,8954881,'China','Asia',602,'',29.8833,107.9333,'',NULL,-11.1849567,106.461368027,-11.1849567,106.461368027,10.677906507,125.323883862,8.74567,96.7423,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-17 11:55:23'),('Yucca Mound, Dry Canyon, New Mexico',293,'Holder','Carboniferous','Pennsylvanian','Gzhelian','Virgilian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',302,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'5',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','12','Foraminifera','13','Algae - encrusting forams','2','Green algae','0','100','0',0,'no',1,'yes','1','Less than 6 reef building species','3','2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','1','Low zonation','2','30-60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',275,315,'Cement makes up 30-50 % of rock volume.\nAccording to ref. 315 differentiated into lower and upper mound.\nPhylloid algae and Epimastopora.\n\nAbstract of ref. 315:\nThe Late Pennsylvanian Yucca Mound complex is a carbonate buildup on the western side of the Sacramento shelf facing the Oro Grande basin, in south-central New Mexico (USA). This complex is an accumulation of algal and foraminiferal boundstones and phylloid-algal packstones and wackestones which were subjected to several periods of subaerial exposure. The growth history of this organic complex is related closely to late Paleozoic cyclic sedimentation in a tectonically active area, and is thought to be the result of progressive offlapping growth stages down the western\nflank of the active La Luz anticline. The oldest beds exposed in the complex (plumose masses of algal and foraminiferal boundstone) formed within wave base on the crest of an earlier organic buildup. The crest of the older buildup was subaerially expised while a thick accumulation of carbonate mud replete with the phylloid algae, Ivanovia, started forming against its western (seaward) flank. As sea level rose and submerged the earlier mound, the phylloid-algal accumulation kept pace with sea-level rise and onlapped the older mound, despite a few brief interruptions. When the phylloid algae built up into wave base, and attained its climax stage of evolution, a typical shallow-water facies developed. This distinctive rock type on the preserved, rounded mound top contains abundant forams, both encrusting and mobile chambered forms, together with fish remains and corodonts. A bedded detrital flank facies, composed of\nbroken phylloid-algal material, and concentrated remains of forams, fish, and conodonts that inhabited the upper\nmound, is present on the shelfward (lee) side of the complex. Abundant, algally coated skeletal grains characterize the flank facies, which is easily recognizable elsewhere within the area, mainly in mound-flanking beds. When sea level dropped, Yucca Mound growth ceased, and smaller boundstone accumulations were formed down the offshore flank of the main mound complex. The varied growth history of this particular organic buildup demonstrates just how much   opportunity existed for subaerial and littoral diagenetic processes to act on and to modify the varied rock facies common in late Paleozoic phylloid-algal buildups. ',32,-105,-272972,-4190475,'United States','North America',101,'1362',32.9597,-105.915,'WAHR','49709',0.0108104178942,-36.4286180749,0.0108104178942,-36.4286180749,-3.04243471922,-59.5140259015,-1.92996,-37.6526,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nordkapp Basin I',294,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'200',NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','2','Algae','2','Algae','25','Palaeoaplysina - phylloid algae','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',276,0,'Well data',71,26,4124861,2132659,'Norway','Europe',301,'',71.4667,26.0167,'','',28.4345207454,20.0609581719,28.4345207454,20.0609581719,27.6798984132,-5.46407339294,26.475,17.6832,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nordkapp Basin II',295,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'1','Seismic data available ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'200','294',1,'Temperate','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','2','Algae','2','Algae','25','Palaeoaplysina - phylloid algae','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',276,0,'Well data.',71,29,4224171,2210525,'Norway','Europe',301,'',71.7333,29.3167,'','',29.2059997644,20.915547675,29.2059997644,20.915547675,28.6808187186,-5.01896859389,27.2711,18.4932,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nordkapp Basin III',296,'','Permian','Cisuralian','Artinskian','Artinskian',283.50,290.10,15,'Sakmarian - Kungurian',277,285,'Early Permian (Artinskian, 286.8 Ma)',280,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'110',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','7','Bryozoans','23','Bryozoans - Tubiphytes - phylloid algae - (microbes) - (encrusting forams)','2','Green algae','40','0','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',276,0,'Mostly seismic data. Interpretations based on comparison with nearby areas.',71,26,4787308,2380445,'Norway','Europe',301,'',71.6667,26.5,'','',29.3679224269,20.6164121668,29.3679224269,20.6164121668,30.6397407814,3.26289983566,30.2474,20.4619,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nordkapp Basin IV',297,'','Permian','Cisuralian','Artinskian','Artinskian',283.50,290.10,15,'Sakmarian - Kungurian',277,285,'Early Permian (Artinskian, 286.8 Ma)',280,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'110','296',1,'Temperate','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','9','Tubiphytes','23','Bryozoans - Tubiphytes - phylloid algae - (microbes) - (encrusting forams)','2','Green algae','0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',276,0,'Mostly seismic data. Interpretations based on comparison with nearby areas.',72,30,4928351,2432097,'Norway','Europe',301,'',72.3333,30,'','',30.5039458082,21.2721216536,30.5039458082,21.2721216536,31.9075959275,3.35317433656,31.3882,21.1123,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nordkapp Basin V',298,'','Permian','Cisuralian','Artinskian','Artinskian',283.50,290.10,15,'Sakmarian - Kungurian',277,285,'Early Permian (Artinskian, 286.8 Ma)',280,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'110','296',0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','9','Tubiphytes','23','Bryozoans - Tubiphytes - phylloid algae - (microbes) - (encrusting forams)','2','Green algae','0','0','100',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',276,0,'',71,32,4889319,2549904,'Norway','Europe',301,'',71.5833,32,'','',30.2280459362,22.3530843627,30.2280459362,22.3530843627,32.0215001549,4.49173668559,31.12,22.2059,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nordkapp Basin VI',299,'','Permian','Cisuralian','Kungurian','Kungurian/Kazanian',268.80,283.50,15,'Sakmarian - Kungurian',277,280,'Early Permian (early Kungurian, 280 Ma)',270,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'125',NULL,1,'Temperate','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',276,0,'Palaeontological data very vague, since mostly seismic data were considered.',71,27,5035930,2088767,'Norway','Europe',301,'',71.5,27.5,'','',32.055966623,23.1703616506,32.055966623,23.1703616506,34.441983475,10.2372744222,33.9481,24.7301,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Nordkapp Basin VII',300,'','Permian','Cisuralian','Kungurian','Kungurian/Kazanian',268.80,283.50,15,'Sakmarian - Kungurian',277,280,'Early Permian (early Kungurian, 280 Ma)',270,2,'1','Seismic data available ',2,'Reef mound','3','101-500 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'125','299',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','7','Bryozoans','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',276,0,'Palaeontological data very vague, since mostly seismic data were considered.',71,30,5091417,2160859,'Norway','Europe',301,'',71.5,30,'','',32.459878111,23.9776284659,32.459878111,23.9776284659,35.092410157,10.7899507725,34.3394,25.5638,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Kolosseum, Ekmanfjorden, Spitzbergen',301,'Nordenskjöldbreen','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'55',NULL,1,'Temperate','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','1','Corals','38','Palaeoaplysina - corals - tubular forams - bryozoans','2','Green algae','40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',277,1604,'Palaeoaplysina mounds with rugose corals, tabulate corals, chaetetid sponges and bryozoans.',78,14,4792008,1377924,'Norway','Europe',301,'',78.7333,14.75,'WAHR','75721',33.6281604296,13.2802435095,33.6281604296,13.2802435095,30.2540571145,-13.6769155133,31.4842,10.8582,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Boltonbreen, Spitzbergen',302,'Wordiekammen','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','35',NULL,NULL,NULL,'3','More than 100 m',NULL,'55','301',1,'Temperate','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','1','Corals','38','Palaeoaplysina - corals - tubular forams - bryozoans','2','Green algae','40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild','1','Present','1','Present',NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',277,279,'Palaeoaplysina mounds.\nForams, mollusks, corals, echinoderms, bryozoans and brachiopods as additional faunal element.\nThickness refers to cummulative thickness interrupted by bedded limestones and dolomites.',78,17,4788955,1441347,'Norway','Europe',301,'1604, 2210',78.5,17.1333,'WAHR','75722',33.6039012457,13.9100279321,33.6039012457,13.9100279321,30.4415506247,-13.1086431594,31.4756,11.4737,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bjornoya, Barents Sea',303,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,1,'Temperate','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','7','Bryozoans','38','Palaeoaplysina - corals - tubular forams - bryozoans','2','Green algae','40','60','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','1','Less than 10% sparite',NULL,NULL,'0','',0,'No or unknown reservoir potential',277,661,'Citation of unpublished thesis by Agdestein (1980).',74,19,4332301,1744836,'Russia','Asia',624,'',74.3333,19.1667,'WAHR','75719',30.0304753692,16.4932844446,30.0304753692,16.4932844446,28.028870046,-9.17750793634,27.9709,14.1258,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Heeseberg',304,'','Triassic','Lower Triassic','Induan','Scythian',247.20,251.90,17,'Induan - early Carnian',235,250,'Permo-Triassic Boundary (252 Ma)',249,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','3','Microbes','3','Microbes','64','Microbes/stromatolites  - (cements) - (worm tubes)',NULL,NULL,NULL,NULL,NULL,0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',280,0,'Stromatolitic domes only.',52,10,2854584,1695627,'Germany','Europe',331,'',52.0972,10.8833,'','',7.76669674761,20.9566960426,30.0373060766,29.8484850971,24.5408636271,25.7433748756,17.6594,20.7028,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Alytus',305,'','Permian','Lopingian','Changhsingian','Zechstein',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','306',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',1,'Potential reservoir',282,0,'Main reference is fig. 5B of ref. 282.',54,24,3000130,3162809,'Lithuania','Europe',301,'',54.4,24.05,'','',32.4883164283,38.1029199598,32.4917469307,38.1036444834,30.8478232307,31.3515261578,22.4217,29.0038,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Jonava, Pashulyai',306,'','Permian','Lopingian','Changhsingian','Zechstein',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick','70',NULL,NULL,NULL,'4','More than 1000 m',NULL,'500',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',2,'Actual reservoir',282,1413,'70 m thickness.\n470-520 km long reef belt.\nGood porosity.\n\nLower Kazanian - Nauyaakmyanian suite = Werrakalk.',55,24,3092265,3141412,'Lithuania','Europe',301,'',55.0667,24.4167,'','',33.1877282868,38.0890264596,33.1911587833,38.0897500226,31.4904047427,31.0284796127,23.1115,28.8783,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Silale',307,'','Permian','Lopingian','Changhsingian','Zechstein',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',258,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','306',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','3','Microbes','7','Bryozoans','18','Bryozoans - microbes - (algae) - (crinoids)',NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',282,0,'Main reference is fig. 5B of ref. 282.',55,22,3071806,2986771,'Lithuania','Europe',301,'',55.5167,22.1333,'','',33.2081171469,36.445086889,33.2115455166,36.4457460198,30.9864161229,29.5312698669,22.9301,27.3965,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hida Massif',308,'Ichinotani','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,NULL,NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','6','Calcisponges','2','Algae','14','Sponges - bryozoans - (microbes)','2','Green algae','10','80','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',284,0,'No reefal structure reported.\nFauna consists of calcareous algae, fusulinids, pharetronid sponges, bryozoans, and crinoids.\nSubordinate are brachiopods and mollusks.\n',36,137,1598957,12105573,'Japan','Asia',625,'',36.1667,137.3333,'WAHR','75644',13.8439908458,141.742041183,13.8439908458,141.742041183,16.9009987121,79.4760123378,14.6815,106.248,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wellman, Horseshoe Atoll, Texas',309,'','Carboniferous','Pennsylvanian','Kasimovian','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,3,'1','Seismic data available ',2,'Reef mound','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200','310',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','2','Green algae','40','60','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,'2','Medium production of reefal debris','0','',2,'Actual reservoir',193,1263,'Ref. 285 not seen.',33,-102,-507645,-3921522,'United States','North America',101,'285',33.05,-102.4167,'','',-3.76473908484,-35.3386717552,-3.76473908484,-35.3386717552,-4.79807008092,-58.5025342193,-3.99325,-35.5448,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Mungerville, Horseshoe Atoll, Texas',310,'','Carboniferous','Pennsylvanian','Kasimovian','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'200',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','7','Bryozoans','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'40','50','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',286,1263,'Framework composed of calcareous sponges, fenestrate and encrusting bryozoans, encrusting red algae, Tubiphytes, cyanophyceans and encrusting forams.\nSubsurface only.',32,-102,-561646,-3913971,'United States','North America',101,'287',32.7667,-102.0833,'','',-4.15777403634,-35.2742713187,-4.15777403634,-35.2742713187,-5.19423196955,-58.4616376406,-4.42194,-35.5215,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Martha van Eman, Texas',311,'','Permian','Cisuralian','Asselian','Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',296,2,'1','Seismic data available ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,NULL,NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','2','Algae','9','Tubiphytes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','2','Green algae','0','30','70',0,'no',0,'no','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',2,'Actual reservoir',287,0,'Archaeolithoporella, Tubiphytes, stromatolites, calcisponges and phylloid algae.\nSix distinct facies zones were distinguished.',34,-101,134738,-3452103,'United States','North America',101,'',34,-101,'','',-0.5522363105,-31.9004137117,-0.5522363105,-31.9004137117,-4.10418221083,-52.6263364577,-3.08327,-33.4235,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Ringmauer, Carnic Alps',312,'Auernig','Carboniferous','Pennsylvanian','Gzhelian','upper Gzhelian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',300,3,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick','22',NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','2','Algae','9','Tubiphytes','39','Algae - bivalves - (bryozoans) - (siliceous sponges)','2','Green algae','0','80','20',0,'no',0,'no','1','Less than 6 reef building species','4','2','Baffler guild',NULL,NULL,'1','Present','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',288,1419,'Anthracoporella is dominant. Other reef builders are Tubiphytes and microbes (micritic crusts).\nAbundant are also mollusk and brachiopod shells and possibly porostromate cyanophyceans.\nMaximum thickness 22 m.\n',46,13,-662262,2889855,'Austria','Europe',301,'713',46.5917,13.1667,'WAHR','24319',-11.4836227357,28.967697082,-11.4836227357,28.967697082,-7.83412606267,4.19589992266,-11.028,23.6975,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Val di Puartis',313,'','Carboniferous','Pennsylvanian','Kasimovian','lower Kasimovian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',305,3,'0','Outcropping reef ',2,'Reef mound','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'1','Less than 20 m',NULL,'1',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1d','Marginal marine - coastal -  siliciclastic shelf','1','Above fair weather wave base','1','Corals','4','Stromatoporoids','2','Corals only',NULL,NULL,'60','40','0',0,'no',0,'no','1','Less than 6 reef building species','2','2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',289,0,'Early Kasimovian.\nSmall mounds situated in transgressive cycles.\nAuloporid corals and some chaetetids',46,13,-1542124,2594139,'Italy','Europe',344,'',46.575,13.1167,'WAHR','49712',-13.3025497031,28.0130002145,-13.3025497031,28.0130002145,-9.74925640742,2.81338965856,-12.4869,23.3673,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Huangjindong, Hubei',314,'Changxing','Permian','Lopingian','Changhsingian','late Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,250,'Permo-Triassic Boundary (252 Ma)',251,3,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick','80',NULL,NULL,NULL,'4','More than 1000 m',NULL,'100',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','3','High production of reefal debris','0','',1,'Potential reservoir',290,298,'Description taken from Jiantianba reef.\r\n\r\nComment from Xuesong Tian, Yue Wang, 2021:\r\nReef builders: \r\nFrame-building and baffling organisms: hypercalcified sphinctozoan and inozoan sponges, sclerosponges, stromatoporoid sponge, bryozoans, and hydrozoans.\r\nBinding organisms: Archaeolithoporella, Tubiphytes, and cyanobacteria\r\n\r\nReef dwellers:\r\nEchinoderms, ammonites, bivalves, brachiopods, gastropods, benthic foraminifera, calcareous algae, and single rugose corals.\r\n\r\nRock type and reef-related depositional characteristic:\r\nFore-reef slope: spiculitic-calcispherical cherty wackestone with reef breccias\r\nReef core: sponge framestone and bafflestone, Archaeolithoporella and cyanobacteria bindstone, sponge framestone with the encrusting Archaeolithoporella.\r\nReef flat (reef crest): packstone with reef breccia Reef base: echinodermal packstone to grainstone.\r\nBack-reef lagoon: bioclastic packstone with calcareous algae, gastropods, and foraminifers.\r\n\r\nReef type: \r\nMetazoan reef at the shallow carbonate platform margin\r\n\r\nCoordinates stated in text.',29,109,-219892,9054939,'China','Asia',602,'',29.9833,109.0833,'','220873',-10.9135713994,107.443710401,-10.9135713994,107.443710401,10.7492741696,126.340660271,9.43342,97.4797,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-06-22 11:05:17'),('Hydra',315,'','Permian','Cisuralian','Asselian','upper Asselian',295.00,298.90,14,'Gzhelian - Asselian',290,295,'Early Permian (Asselian, 297 Ma)',295,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'5',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','9','Tubiphytes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','40','60',0,'no',0,'no','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','1','Low production of reefal debris','1','Present',0,'No or unknown reservoir potential',291,0,'No detailed description available.\nCompostion suggest time slice 14, although a late Asselian age was proposed.',37,23,-1514861,2986210,'Greece','Europe',338,'',37.3,23.45,'','',-21.9453082391,25.4654536915,-21.9453082391,25.4654536915,-15.8552480518,8.22222687086,-21.4397,23.3413,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Hackberry Draw and Chinaberry Draw, Capitan, Texas',316,'Capitan','Permian','Guadalupian','Capitanian','Capitanian',259.80,265.10,16,'Roadian - Changhsingian',261,260,'late Middle Permian (Capitanian, 262.5 Ma)',262,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'500','86',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','2','Below fair weather wave base','3','Microbes','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','90','10',0,'no',1,'yes','3','25 or more reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'2','Medium zonation','2','Medium zonation','2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',1533,293,'Abstract ref. 1533:\nThe Permian Capitan reef of the Guadalupe Mountains was\n  bound, lithified, and preserved by microbially precipitated micrite. A microbial origin or association is based on the distribution, texture, fossil content, and order of microstratigraphic succession. In samples from the\n  middle Capitan Formation, micrite layers (about 1 cm thick) encrusted the top, sides, and undersides of in situ organisms and also piled above organisms in thick (0.5 to > 3 cm) accumulations, with high angles of repose (up to 90°). Primary encrustations commonly consist of thin, homogeneous, subparallel layers of Archaeolithoporella---interpreted to be\n  a red alga that probably lived in dimly lit cavities. Secondary encrustations (0.5--30 mm thick) contain 10--50 µm diameter peloids and fossil cyanophytes, and are usually bound by thin layers of micrite. Secondary encrustations of gravity-defying peloidal micrites are interpreted as having precipitated within mucilaginous microbial aggregations, probably in dark\n  cavities. The secondary microbial micrites were followed by\n  cavity-filling, aragonitic botryoids. Thin (< 1 mm) layers of clotted micrite were deposited on the first botryoids, probably by microbial biofilms. \n\n  In contrast to samples from the middle Capitan Formation, samples from the upper Capitan Formation taken near the transition from reef to outer shelf are composed of smaller (1--2 mm) framework organisms and are bound by layers of thinner (< 1 mm) primary encrustations. In the upper Capitan Formation samples, dense, clotted micrite forms secondary encrustations (£ 1 mm thick), commonly underneath primary framework.\n  Secondary encrustations are succeeded by more abundant tertiary encrustations (1--4 mm thick) of sparse, clotted micrite with vague dendritic structures. The secondary and tertiary encrustations are interpreted as microbial. The samples from the upper Capitan Formation were deposited in the shallowest part of the reef (< 1 to 10 m deep), and most of the samples from the middle Capitan were deposited in deep water  (10--140 m). The difference in the encrustations and in the overall scale of  the two fabrics is probably related to differences in environmental energy   during deposition.',32,-104,486740,-3748525,'United States','North America',101,'292',32.1667,-104.4333,'WAHR','47714',11.011256408,-29.8544737944,11.011256408,-29.8544737944,5.45785477956,-36.7948202879,4.43781,-32.8287,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Brooks Ranch, Texas',317,'Gaptank','Carboniferous','Pennsylvanian','Gzhelian','Virgilian',298.90,303.70,14,'Gzhelian - Asselian',290,300,'Late Pennsylvanian (Gzhelian, 301.3 Ma)',300,2,'0','Outcropping reef ',4,'Biostrome','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'2',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform',NULL,NULL,'4','Stromatoporoids','4','Stromatoporoids',NULL,NULL,NULL,NULL,'0','100','0',0,'no',0,'no',NULL,NULL,NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite',NULL,NULL,NULL,NULL,'0','',1,'Potential reservoir',318,0,'wrong time sclice - check coordinates',30,-103,-752470,-4142102,'United States','North America',101,'',30.4,-103.0833,'','',-3.47516977428,-35.9760386062,-3.47516977428,-35.9760386062,-6.54275165797,-59.1897045278,-5.42712,-37.2962,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Dugot Mountain, Texas',318,'Cathedral Mountain','Permian','Cisuralian','Kungurian','Kungurian',272.30,283.50,15,'Sakmarian - Kungurian',277,280,'Early Permian (early Kungurian, 280 Ma)',272,2,'0','Outcropping reef ',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'30','319',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)',NULL,NULL,'7','Bryozoans','7','Bryozoans',NULL,NULL,NULL,NULL,'100','0','0',0,'no',0,'no',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',294,2500,'Wedin Member. Equivalent to Fifth Leonard Limestone Member of P.B. King, Leonardian (Cathedralian).',30,-103,409418,-3633489,'United States','North America',101,'',30.2083,-103.5167,'WAHR','43459',-0.517592955827,-34.5827574624,-0.517592955827,-34.5827574624,-2.4968106108,-40.9165730012,1.65323,-33.3551,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Leonard Mountain, Glass Mts., Texas',319,'Skinner Ranch','Permian','Cisuralian','Kungurian','Leonardian (Hessian)',270.60,280.00,15,'Sakmarian - Kungurian',277,275,'Early Permian (late Kungurian, 275 Ma)',274,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'50',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','9','Tubiphytes','9','Tubiphytes',NULL,NULL,NULL,NULL,'0','0','100',0,'no',1,'yes','2','6 to 24 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,'1','Low zonation','2','Medium zonation',NULL,NULL,NULL,NULL,NULL,NULL,'0','',0,'No or unknown reservoir potential',294,1401,'Hessian age. Personal observation identify Tubiphytes as dominant reef builder',30,-103,407101,-3602326,'United States','North America',101,'2500',30.3339,-103.2258,'WAHR','43534',-0.551543919341,-34.3039227709,-0.551543919341,-34.3039227709,-2.52253668707,-40.6366031009,1.62632,-33.0754,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Boone County I, Missouri',320,'Burlington Limestone','Carboniferous','Mississippian','Visean','Osagean (Tn3)',342.00,346.70,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',346,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m','100','30',NULL,0,'Tropical or unknown','3','Ramp or Slope','3a','Upper slope or inner ramp','2','Below fair weather wave base','3','Microbes','13','Echinoderms','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'30','0','70',0,'no',0,'no','1','Less than 6 reef building species',NULL,'4','Microbial precipitation',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',299,369,'Waulsortian mound.\nCrinoids are dominant macrofossils.',39,-92,-2409300,-4123597,'United States','North America',101,'',39,-92.8333,'','',-28.8210750733,-56.3209758917,-28.8210750733,-56.3209758917,-9.22850875212,-94.7640081562,-20.9696,-38.8137,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Boone County II, Missouri',321,'Burlington Limestone','Carboniferous','Mississippian','Visean','Osagean (Tn3)',342.00,346.70,11,'late Famennian - early Visean',351,340,'Middle Mississippian (Early Visean, 338.8Ma)',346,2,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'30','320',0,'Tropical or unknown','3','Ramp or Slope','3b','Deeper slope or outer ramp','2','Below fair weather wave base','13','Echinoderms','7','Bryozoans','17','Bryozoans - crinoids - sponge spicules - (brachiopods) - (microbes) - (Tubiphytes)',NULL,NULL,'40','0','60',0,'no',0,'no','1','Less than 6 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','2','10-25% sparite','2','Medium production of reefal debris','1','Present',0,'No or unknown reservoir potential',299,2431,'Waulsortian mound.\nTrapping of turbidites by stalked crinoids and bryozonas.\nMaximum water depth 100 m.',38,-92,-2427801,-4132320,'United States','North America',101,'',38.8333,-92.8333,'','',-28.8994580081,-56.4889623512,-28.8994580081,-56.4889623512,-9.36764649661,-94.8570432903,-21.1084,-38.9126,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Marble Falls, Texas',322,'','Carboniferous','Pennsylvanian','Bashkirian','Bashkirian',315.20,323.20,13,'Bashkirian - Kasimovian',302,320,'Early Pennsylvanian (Bashkirian, 319.2 Ma)',316,2,'0','Outcropping reef ',2,'Reef mound','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'150',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','2','Below fair weather wave base','2','Algae','7','Bryozoans','31','Algae - bryozoans - (crinoids) - (forams) - (sponges) - (vermetids)','1','Red algae','30','60','10',0,'no',1,'yes','2','6 to 24 reef building species',NULL,'2','Baffler guild',NULL,NULL,NULL,NULL,'1','Low zonation','1','Low zonation','3','More than 60% micrite','1','Less than 10% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',300,1056,'Tubular red algae dominant (Cuneiphycus, Foliophycus, Donezella). Others are bryozoans, phylloid algae, Girvanella and others.\nThree distinct buildups seperated by skeletal grainstone and spiculitic facies.',30,-98,-1063847,-3743488,'United States','North America',101,'1517',30.5667,-98.2667,'','',-17.1511937371,-44.1237197176,-17.1511937371,-44.1237197176,-14.5450346621,-60.0941739429,-11.7006,-38.5625,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Bend, Texas',323,'','Carboniferous','Pennsylvanian','Moscovian','Moscovian',307.00,315.20,13,'Bashkirian - Kasimovian',302,310,'Middle Pennsylvanian (Moscovian, 311.1 Ma)',309,2,'0','Outcropping reef ',3,'Mud mound or bank','1','Less than 10 m thick',NULL,NULL,NULL,NULL,'2','10 - 100 m',NULL,'10',NULL,0,'Tropical or unknown','1','Intrashelf/ Intraplatform','1a','Shallow intra-platform','1','Above fair weather wave base','2','Algae','3','Microbes','15','Algae - microbes - (encrusting forams) - (rare songes)','2','Green algae','0','100','0',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','1','Less than 10% sparite','1','Low production of reefal debris','0','',0,'No or unknown reservoir potential',300,0,'Phylloid algae dominant.',31,-98,-989697,-3736196,'United States','North America',101,'',31.0667,-98.5333,'','',-10.97808425,-37.4995411631,-10.97808425,-37.4995411631,-9.06656311299,-58.9440463187,-9.01661,-35.7862,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Elk City, Kansas',324,'','Carboniferous','Pennsylvanian','Kasimovian','Missourian',303.70,307.00,13,'Bashkirian - Kasimovian',302,305,'Late Pennsylvanian (Kasimovian, 305.4 Ma)',304,3,'0','Outcropping reef ',3,'Mud mound or bank','2','10 to 100 m thick','13',NULL,NULL,NULL,'4','More than 1000 m',NULL,'120','221',0,'Tropical or unknown','2','Shelf or Platform margin','2a','Margin of shallow basins (platform margin)','1','Above fair weather wave base','2','Algae','7','Bryozoans','26','Phylloid and other platy algae - cements - (microbes)','2','Green algae','40','50','10',0,'no',0,'no','1','Less than 6 reef building species',NULL,'3','Binder guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'3','More than 60% micrite','3','More than 25% sparite','1','Low production of reefal debris','0','',1,'Potential reservoir',204,193,'Bryozoans are also common.\nUp to 13 m thick.\nCaptain Creek mound complex.',37,-95,-443722,-3167472,'United States','North America',101,'494, 1257',37.2667,-95.8833,'','',-3.18562956748,-28.5486658773,-3.18562956748,-28.5486658773,-4.61495512624,-51.6797908908,-3.67803,-28.7637,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Wangmo, Guizhou',325,'','Permian','Lopingian','Changhsingian','Changhsingian',251.90,254.10,16,'Roadian - Changhsingian',261,255,'Late Permian (Lopingian, 256 Ma)',252,2,'0','Outcropping reef ',1,'True reef','2','10 to 100 m thick',NULL,NULL,NULL,NULL,'3','More than 100 m',NULL,'15','197',0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','2','Algae','4','Stromatoporoids','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)','1','Red algae','0','100','0',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','3','More than 25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',298,662,'A platy hydrozoan was mentioned most important. Thick Archaeolithoporella crusts and radaxial fibrous calcite cements.',25,106,-962451,8937413,'China','Asia',602,'',25.2,106.1,'','',-16.0658414273,105.569989898,-16.0658414273,105.569989898,6.05826722033,123.506264929,4.02425,98.2625,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Guanchang, Lingyun, Guangxi',326,'Maokou','Permian','Guadalupian','Wordian','middle-upper Maokouan',265.10,268.80,16,'Roadian - Changhsingian',261,265,'Middle Permian (Wordian/Capitanian Boundary 265.1 Ma)',265,3,'0','Outcropping reef ',1,'True reef','4','More than 500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'65',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2c','Atoll (circular structure)','1','Above fair weather wave base','6','Calcisponges','3','Microbes','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','80','20',0,'no',0,'no','3','25 or more reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',1,'Potential reservoir',298,662,'Middle to upper Moakouan.\nIsolated carbonate platform (atoll-like).',24,106,-1045432,8997397,'China','Asia',602,'2362',24.4167,106.4833,'WAHR','36262',-19.7236829318,110.603544096,-18.45637152,116.109306464,-0.612872853521,133.344123373,-5.66449,98.9197,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),('Guangnan II, Yunnan',327,'Maokou','Permian','Guadalupian','Wordian','Maokouan',265.10,272.30,16,'Roadian - Changhsingian',261,270,'Middle Permian (Roadian&Wordian, 268.7 Ma)',265,2,'0','Outcropping reef ',1,'True reef','3','101-500 m thick',NULL,NULL,NULL,NULL,'4','More than 1000 m',NULL,'200',NULL,0,'Tropical or unknown','2','Shelf or Platform margin','2b','Margin of deep basins (shelf margin)','1','Above fair weather wave base','6','Calcisponges','6','Calcisponges','5','Red algae - calcareous sponges - Tubiphytes - microbes - (bryozoans) - (corals)',NULL,NULL,'0','90','10',0,'no',0,'no','2','6 to 24 reef building species',NULL,'1','Constructor guild',NULL,NULL,NULL,NULL,NULL,NULL,NULL,NULL,'2','30-60% micrite','2','10-25% sparite','2','Medium production of reefal debris','0','',0,'No or unknown reservoir potential',298,206,'',24,105,-1154109,8862418,'China','Asia',602,'',24.0667,105.0333,'','',-20.5528363464,109.44502682,-18.7471739391,117.273649324,-0.211701788338,131.720571032,-7.68078,97.745,'Kiessling','Kiessling','2021-05-28 15:21:12','2021-05-29 18:44:48'),