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Ecca Group

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1486: 1864: 1809: 886:, siltstones, and sandstones that exhibit ball-and-pillow structures are also found in the uppermost sections. The presence of the shales in the lower Tierberg indicate a low energy marine environment that transitioned to pro-delta to distal delta depositional environments with the appearance of the upward coarsening sequences and other associated geological features. Various invertebrate fossils have been recovered, namely fish scales, sponge spiracles, and trace fossils of Planolites and Nereites. 320: 501: 6364: 811: 249: 6350: 6376: 293: 282: 260: 271: 6388: 603:, the geological formations of the Ecca Group can only be found in one of the three previously aforementioned facies successions. This is because each of these facies successions represents differing preserved environments that can be observed in their diagnostic geological features. The facies successions, along with their geological formations, are described below: 3249: 1590:
respectively. The rock sediments are predominantly arranged in upward-coarsening cycles, although some fining-upward cycles are found in this formation's easternmost deposits. The alternating rock types observed in the Vryheid Formation indicate seasonal variations of storms and fairer weather in a
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Example of a peat swamp environment, similar to the depositional environment preserved in the Vryheid Formation rocks. Plant material would have sunk below surface to the bottom of the swamp, being preserved in the anoxic environment. Over time plant material would be compacted and buried by
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Almond, J.E., 2010. PALAEONTOLOGICAL IMPACT ASSESSMENT: DESKTOP & FIELD SCOPING STUDY Waste Water Treatment Works, Water Pipeline and Low Income Housing Development, Klaarstroom, Prince Albert Municipality, Western Cape Province. John E. Almond (Natura Viva cc, Cape Town). April
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Jorge J.P. Figueiredo, David M.Hodgson, Stephen S.Flint, and John P.Kavanagh (2013-03-01). "Architecture of a channel complex formed and filled during long-term degradation and entrenchment on the upper submarine slope, Unit F, Fort Brown Fm., SW Karoo Basin, South Africa".
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Jirah, Sifelani; McPhee, Blair W.; Viglietti, Pia A.; Bamford, Marion K.; Choiniere, Jonah N.; Hancox, P. John; Barbolini, Natasha; Day, Michael O.; Rubidge, Bruce S. (2016), "Advances in Nonmarine Karoo Biostratigraphy: Significance for Understanding Basin Development",
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Wickens, H.D.V., 1992. Submarine fans of the Permian Ecca Group in the SW Karoo Basin: Their origin and reflection on the tectonic evolution of the basin and its source areas. Inversion Tectonics of the Cape Fold Belt, Karoo and Cretaceous Basins of Southern Africa,
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Almond, J.E., 2013. PALAEONTOLOGICAL SPECIALIST STUDY: FIELD ASSESSMENT. Expansion of an existing Borrow Pit in the Prince Albert townlands, Prince Albert District, Western Cape. John E. Almond (Natura Viva cc, Cape Town). March
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Cole, D.I. and McLachlan, I.R., 1991. Oil potential of the Permian Whitehill Shale Formation in the Main Karoo Basin, South Africa. Proceedings, Gondwana Seven: SĂŁo Paulo, Instituto de Geociencias, Universidade de SĂŁo Paulo,
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Almond, J.E., 2005. PALAEONTOLOGICAL IMPACT ASSESSMENT: Exceptional fossil starfish bed, Prince Albert District, Western Cape. John E. Almond (Natura Viva cc, Cape Town) and Derek Ohland (Iziko Museums, Cape Town). January
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Van Vuuren, C.J. and Cole, D.I., 1979. The stratigraphy and depositional environments of the Ecca Group in the northern part of the Karoo Basin. Geological Society of South Africa Special Publication, 6,
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Anderson, J.M. and Cruickshank, A.R.J., 1973. The biostratigraphy of the Permian and Triassic, Part 2. A preliminary review of the distribution of Permian and Triassic strata in time and space.
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rock in this formation weather out white on the surface, often referred to in literature as the “white band”. It is the main diagnostic feature of this formation in this facies succession. The
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Tietjen, Kristen; Criswell, Katharine E.; Finarelli, John A.; Gess, Robert W.; Coates, Michael I. (2017-01-01). "A symmoriiform chondrichthyan braincase and the origin of chimaeroid fishes".
3400:"Trace fossils as sedimentological and palaeoenvironmental indices in the Ecca Group (Lower Permian) of the Transvaal. Transactions of the Geological Society of South Africa, 83, pp.333-344" 2583:
Johnson, M.R., Van Vuuren, C.J., Visser, J.N.J., Cole, D.I., Wickens, H.D.V., Christie, A.D.M., Roberts, D.L. and Brandl, G., 2006. Sedimentary rocks of the Karoo Supergroup.
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B.R. Turner, G. Stanistreet, M.K.G. Whateley (1981-11-01). "Trace fossils and palaeoenvironments in the Ecca group of the Nongoma Graben, northern Zululand, South Africa".
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O. Catuneanu, P.J Hancox, B. Cairncross, and B.S Rubidge (2002-11-01). "Foredeep submarine fans and forebulge deltas: orogenic off-loading in the underfilled Karoo Basin".
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often overlies unconformably on much older basement rocks unlike the other facies of the Ecca Group. It comprises three geological formations (from oldest to youngest):
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O. Catuneanu, H. Wopfner, P.G. Eriksson, B. Cairncross, and B.S.Rubidge, R.M.H. Smith, and P.J. Hancox (2005-10-01). "The Karoo basins of south-central Africa".
3989: 942:. Minor upward thickening cycles are observed here which grow more prominent in the upper sections. The rock type changes in the upper sections to alternating 1027:
burrow traces are found. Together with the underlying Tierberg, Skoorsteenberg, and Kookfontein Formation, the Waterford Formation forms an upward-coarsening
3675: 1980:
R.M.H. Smith, P.G.Eriksson, W.J.Botha (1993-01-01). "A review of the stratigraphy and sedimentary environments of the Karoo-aged basins of Southern Africa".
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A mountain in the Tanqua Karoo, South Africa, with multiple layers of turbidites formed in the south-western portion of the Karoo Sea about 300 million years
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B. Cairncross (1989-06-01). "Paleodepositional environments and tectonosedimentary controls of the postglacial Permian coals, Karoo Basin, South Africa".
4678: 3685: 1108:: In the southern facies the Whitehill Formation loses its diagnostic white band marker horizon. The rock type changes here to light brown, fine-grained 2527:
M.R Johnson, C.J Van Vuuren, W.F Hegenberger, R. Key, and U. Show (1996-07-01). "Stratigraphy of the Karoo Supergroup in southern Africa: an overview".
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A simplified geological map of the outcrops of Karoo Supergroup rocks in Southern Africa. The Ecca Group is represented by the orange key on the map.
2704:"Depositional Environments and Sequence Stratigraphy of an Exhumed Permian Mudstone-Dominated Submarine Slope Succession, Karoo Basin, South Africa" 3831: 3423: 3318: 3144: 2785: 2570: 2320: 2263: 2023: 2832:"Petrographical and geophysical investigation of the Ecca Group between Fort Beaufort and Grahamstown, in the Eastern Cape Province, South Africa" 2167:"Reciprocal flexural behaviour and contrasting stratigraphies: a new basin development model for the Karoo retroarc foreland system, South Africa" 3974: 2801:"A composite submarine fan-delta-fluvial model for the Ecca and Lower Beaufort Groups of Permian Age in the Eastern Cape Province, South Africa" 6157: 4935: 3914: 580:. These individual formations have been grouped into three geographical areas, which are the southern, western/northwestern, and northeastern 4973: 3939: 3929: 3856: 3463:
Vogt, A., 2004. National monuments in Namibia: An inventory of proclaimed national monuments in the Republic of Namibia. Gamsberg Macmillan.
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Biostratigraphic correlation of fossils in the greater Gondwana across present-day South America, southern Africa, Antarctica and Australia
2411:"Grain size statistics and depositional pattern of the Ecca Group sandstones, Karoo Supergroup in the Eastern Cape Province, South Africa" 6441: 4940: 468:. The mountain-building and erosion caused by the growing Gondwanide mountain range was the initial subsidence mechanism acting on the 2276: 3068:
Modesto, S. P. (2010-09-15). "The postcranial skeleton of the aquatic parareptile Mesosaurus tenuidens from the Gondwanan Permian".
2372:"Interplay of static loads and subduction dynamics in foreland basins: Reciprocal stratigraphies and the "missing" peripheral bulge" 6436: 3333:
https://www.sahra.org.za/sahris/sites/default/files/heritagereports/PIA_Mbila%20Phase%20I_Prevec%20March%202014_revised%20Final.pdf
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occur throughout this formation. All these are indicative of a deep-water depositional environment. Carbonised plant fragments and
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beds. The fine-grained nature of the sediments indicate that the depositional environment was a low energy suspension setting in a
3105:"Shale Gas Characteristics of Permian Black Shales in South Africa: Results from Recent Drilling in the Ecca Group (Eastern Cape)" 3029:"The cranial skeleton of the Early Permian aquatic reptile Mesosaurus tenuidens: implications for relationships and palaeobiology" 6421: 6446: 4257: 3866: 3158:
Richard G. Vos and David K. Hobday (1977-01-01). "Storm beach deposits in the late Palaeozoic Ecca Group of South Africa".
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Baiyegunhi, Christopher; Nxantsiya, Zusakhe; Pharoe, Kinshasa; Baiyegunhi, Temitope L.; Mepaiyeda, Seyi (1 January 2019).
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Petrology, geochronology and provenance of the Laingsburg and Tanqua Karoo submarine fan systems, Ecca Group, South Africa
992:. Alternating slump and slide and coarsening upward cycles are observed in the lower sections while in the upper sections 6456: 4779: 1361:
intercalations are found in its upper sections, displaying horizontal, wavy, ripple, and ripple-drift cross lamination.
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R.M.H. Smith (1990-01-01). "A review of stratigraphy and sedimentary environments of the Karoo Basin of South Africa".
2498:"Deposition of the Early to Late Permian Whitehill Formation during a sea-level highstand in a juvenile foreland basin" 2112:
Richard G.Vos, David K.Hobday (1977-01-01). "Storm beach deposits in the late Palaeozoic Ecca Group of South Africa".
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rock deposits. The rock sediments are fine-grained overall, indicating that the rock sediments were deposited in both
6451: 6426: 4714: 4087: 3259: 2686: 2058: 398:. The Ecca sea was vast but shallow, reaching only around 500 m at its deepest in its west/northwestern and southern 2950:"Mesosaurus tenuidens and Stereosternum tumidum from the Permian Gondwana of both Southern Africa and South America" 690:
are a character diagnostic of its western outcrops. These rock sediments were deposited in a deep marine and distal
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Fossil tree from the Permian Ecca Group of the Karoo Sequence at the petrified forest, east of Doro !Nawas, Namibia
599:, Collingham, and the uppermost Waterford Formations which are found in both the southern and western/northwestern 346:
in some sections, but in some localities overlying unconformably over much older basement rocks. It underlies the
5544: 134:, Collingham Formation, Tierberg Formation, Skoorsteenberg Formation, Kookfontein Formation, Waterford Formation. 2395: 6214: 6152: 5549: 1860:
were brought into the area and are considered to have been sourced from the nearby deposits of the Huab Basin.
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systems in the lower deposits which grade steadily north-eastwards to shallow marine deposits including shelf (
142:, Collingham Formation, Vischkuil Formation, Laingsburg Formation, Fort Brown Formation, Waterford Formation. 1046:
succession is the largest of the three facies succession. Its lowermost formations are deep marine comprising
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and channel-fill deposits are observed. These features indicate that the depositional environment constituted
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deposits also occur intermittently. It is regarded as a distal, southern equivalent of the Vryheid Formation.
2748: 2166: 1409:, which are generally light in colour and are frequently interbedded with dark-grey to light yellowish grey 5810: 5554: 6115: 4978: 648:: In the west/northwestern facies the Prince Albert Formation is characterized by either greyish or olive 5805: 5539: 517: 4833: 4823: 4797: 3680: 1853: 1775:. Deposits of this formation interfinger laterally with the underlying Vryheid Formation and overlying 993: 1425:
layers. Outcrops of this formation are extremely diagnostic as a result of the alternating “bands” of
892:: Only found in the southernmost area of the western facies. A lens-shaped formation composed of five 641:
systems known from the marine Ecca. Associated formations are listed below (from oldest to youngest):
6234: 4759: 4057: 1929: 1190: 509: 2970: 2356: 2098: 1193:. The depositional environment is considered to have been deep marine within a basin-plain or outer 5855: 4724: 4375: 4311: 1365:
are sometimes found due to the Cape Orogenic event taking place during the time of deposition. The
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is found in this facies succession and include the following formations (from oldest to youngest):
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Marion K. Bamford (2004-01-01). "Diversity of the Woody Vegetation of Gondwanan Southern Africa".
6204: 5684: 4792: 4507: 4461: 4385: 4273: 2526: 1924: 6219: 6147: 6110: 4802: 4683: 4446: 4077: 4047: 3778: 3439:"Karoo supergroup palaeontology of Namibia and brief description of a Thecodont from Omingonde" 2702:
Kavanagh, John P.; Flint, Stephen S.; Hodgson, David M.; Figueiredo, Jorge J. P. (2010-01-01).
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Second of the main subdivisions of the Karoo Supergroup of geological strata in southern Africa
2078:"Fluvial Deposits of the Ecca and Beaufort Groups in the Eastern Karoo Basin, Southern Africa" 4729: 4092: 4072: 3612: 3312: 3138: 2957: 2779: 2564: 2497: 2343: 2314: 2257: 2085: 2017: 1287: 861: 3103:
Claire Geel, Hans-Martin Schulz, Peter Booth, Maarten de Wit, Brian Horsfield (2013-01-01).
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are found in the northernmost section of the western/northwestern facies, and upward-fining
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Taxonomy, palaeoecology and palaeobiogeography of some palaeozoic fish of Southern Gondwana
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Permian-Triassic Pangean Basins and Foldbelts Along the Panthalassan Margin of Gondwanaland
2645: 2619:"A new vertebrate biozone at the base of the Beaufort Group, Karoo sequence (South Africa)" 2536: 2422: 2383: 2286: 2229: 2178: 2121: 1989: 1817: 851: 577: 391: 464:
Plate. This resulted in the rise of the Gondwanide mountain range in what is known as the
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of the Ecca Group, the depositional environment, with some exceptions, was predominantly
139: 131: 3486: 3288: 3171: 2997: 2902: 2847: 2719: 2540: 2426: 2387: 2290: 2233: 2219: 2182: 2125: 1993: 1951:"Water depth in the Main Karoo Basin, South Africa, during Ecca (Permian) sedimentation" 6229: 6194: 5478: 4918: 4913: 4752: 4747: 4658: 4556: 4527: 4456: 4405: 4316: 4231: 4201: 4152: 4147: 3964: 3753: 3690: 3632: 3085: 2930: 2440: 2202: 1418: 465: 31: 4037: 3512: 3494: 2548: 2335: 2241: 1133:: The southern facies deposits of this formation yield diagnostic pale yellowish-grey 931:: The lower section of this formation is composed of horizontally laminated dark-grey 6319: 6224: 5900: 5493: 4923: 4588: 4583: 4561: 4517: 4512: 4480: 4468: 4390: 4321: 4172: 4132: 4122: 4107: 4062: 4042: 3979: 3949: 3934: 3881: 3826: 3821: 3806: 3498: 3446: 3417: 3399: 3363: 3300: 3296: 3255: 3202: 3183: 3179: 3126: 3089: 3050: 3045: 3028: 3009: 3005: 2922: 2914: 2861: 2812: 2767: 2731: 2682: 2657: 2626: 2552: 2509: 2478: 2474: 2444: 2302: 2298: 2245: 2194: 2190: 2137: 2133: 2054: 2005: 2001: 1962: 1530:
and exposures. The majority of the data collected from this formation have been from
1465: 1374: 1058: 1001: 909: 629:, pro-delta and beach environment deposits. The deposits of the western/northwestern 626: 431: 415: 359: 2949: 2763: 2598: 2206: 1522:
layers. This formation is only found in the easternmost section of the northeastern
5448: 5328: 5313: 5137: 5040: 4578: 4566: 4497: 4331: 4127: 4102: 4097: 3768: 3748: 3695: 3670: 3604: 3585: 3575: 3490: 3292: 3175: 3116: 3077: 3040: 3001: 2934: 2906: 2851: 2759: 2723: 2544: 2470: 2430: 2391: 2294: 2237: 2186: 2129: 2046: 1997: 1863: 1626: 561: 489: 477: 469: 335: 4027: 3438: 3355: 2618: 1557:
have been found, and the depositional environment is thought to be shallow marine.
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comprise the bulk of the lower deposits of the Fort Brown Formation. Minor impure
621:. The rocks contain a complete transition, grading laterally into one other, from 6324: 6079: 6011: 5976: 5940: 5744: 5719: 5644: 5498: 5483: 5398: 5212: 5152: 5132: 5050: 4688: 4668: 4663: 4551: 4490: 4441: 4370: 4196: 4032: 3899: 3871: 3758: 3652: 3637: 3627: 3622: 3549: 3397: 3121: 3104: 3081: 2050: 1579: 1434: 1298: 1201:
layers indicates that volcanic activity took place during the time of deposition.
199: 1872: 6354: 6244: 6074: 5996: 5950: 5925: 5870: 5789: 5714: 5699: 5679: 5669: 5619: 5574: 5513: 5428: 5358: 5318: 5112: 4999: 4828: 4818: 4653: 4648: 4502: 4485: 4451: 4211: 4162: 4137: 4117: 4019: 3994: 3816: 3763: 3738: 3733: 3728: 1857: 1829: 1776: 1772: 1715: 1657: 1653: 1622: 1460:
is shallow marine in its lowermost and uppermost sections, and then changes to
1306: 1186: 1117: 1093: 1008: 964:: The western/northwestern deposits of this formation are composed of a mix of 901: 787: 767: 755: 715: 706: 565: 449: 347: 154: 117: 1490:
sediment. Over millions of years the plant material mineralized, becoming coal
319: 6410: 6178: 6105: 6043: 5915: 5910: 5885: 5835: 5754: 5739: 5729: 5654: 5629: 5624: 5614: 5609: 5579: 5463: 5438: 5408: 5353: 5303: 5272: 5267: 5262: 5247: 5242: 5237: 5217: 5207: 5172: 5142: 5117: 5091: 5030: 4891: 4886: 4326: 4157: 4112: 4052: 4009: 4004: 3796: 3642: 3570: 3558: 3502: 3450: 3367: 3304: 3187: 3130: 3054: 3013: 2918: 2865: 2816: 2771: 2735: 2661: 2630: 2556: 2513: 2482: 2306: 2249: 2198: 2141: 2009: 1966: 1912: 1904: 1900: 1721: 1634: 1543: 1373:
are extremely fine-grained, finely laminated and are considered to represent
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Waschbusch, Paula; Beaumont, Christopher; Catuneanu, Octavian (1997-12-01).
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are known from the Vryheid Formation, including their fertile organs and
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This is thought to represent a marginal marine setting either within the
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of the Skoorsteenberg Formation where sediments were deposited in a pro-
6100: 6064: 5935: 5920: 5905: 5895: 5845: 5764: 5749: 5734: 5674: 5634: 5594: 5584: 5388: 5363: 5338: 5227: 5222: 5187: 5167: 5147: 4994: 4881: 4420: 4206: 4191: 3904: 3662: 1889: 1727: 1700: 1692: 1629:
water accumulated. The Vryheid Formation reaches a maximum of 1030m in
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layers. It grades laterally into the upper Ripon Formation in the east.
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layers with yellowish grey weathering are only known from the southern
1062: 875: 872: 792: 634: 488:, and backbulge flexural provinces. This resulted in deposition of the 457: 403: 363: 94: 59: 6349: 6048: 6027: 5986: 5704: 5689: 5508: 5458: 5443: 5413: 5368: 5348: 5308: 5202: 5157: 5122: 5107: 5086: 5070: 5009: 5004: 4693: 4226: 4221: 4182: 1979: 1792: 1769: 1765: 1709: 1688: 1679: 1671: 1587: 1519: 1511: 1430: 1426: 1422: 1410: 1406: 1402: 1358: 1355: 1347: 1328: 1324: 1320: 1316: 1291: 1279: 1268: 1264: 1260: 1253: 1249: 1239: 1231: 1216: 1208: 1183: 1167: 1163: 1155: 1152: 1113: 1109: 1097: 1023: 1012: 985: 981: 977: 973: 969: 947: 943: 939: 893: 847: 827: 771: 719: 683: 679: 671: 667: 533: 485: 473: 213: 191: 187: 99: 43: 3331:
Prevec, R., 2014. PHASE 1 PALAEONTOLOGICAL IMPACT ASSESSMENT. Link:
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are considered to have been deposited in a suspension setting under
146:: Pietermaritzburg Formation, Vryheid Formation, Volksrust Formation 5890: 5865: 5830: 5282: 5232: 5065: 5035: 4737: 3919: 2829: 1845: 1841: 1837: 1796: 1740: 1568: 1531: 1515: 1414: 1398: 1346:, which are usually olive grey in color, are extremely common. The 1017: 904:. The depositional environment is thought to have been an unstable 883: 831: 797: 703: 589: 545: 481: 461: 446: 406:
are situated respectively. The marine environment ranged from deep
375: 298: 287: 265: 183: 89: 84: 69: 64: 54: 3157: 1080:. These rock sediments were deposited in a deep marine and distal 6329: 5639: 1884: 1849: 1833: 1825: 1674: 1630: 1535: 1527: 1366: 1351: 1343: 1332: 882:
are found in the upper sections. Upwards-coarsening sequences of
731: 675: 553: 453: 379: 351: 276: 104: 79: 1903:
has also proven the lower Ecca formations to correlate with the
1397::This formation is exposed along a series of east-west trending 1057:
systems that grade upwards into channelized submarine slopes to
5930: 3894: 3720: 3600: 1880: 1876: 1784: 1732: 1643: 1596: 1572: 1564: 1547: 1523: 1499: 1479: 1457: 1377: 1336: 1302: 1089: 1077: 1047: 1043: 951: 783: 759: 751: 739: 699: 687: 660: 630: 622: 614: 600: 581: 557: 419: 399: 339: 217: 2701: 2045:, Regional Geology Reviews, Springer, Cham, pp. 141–149, 1610:
formed from compacted plant matter deposited at the bottom of
2646:"Sedimentology of the Collingham Formation, Karoo Supergroup" 2596: 2409:
Baiyegunhi, Christopher; Liu, Kuiwu; Gwavava, Oswald (2017).
2111: 1788: 1758: 1649: 1618: 1614: 1599: 1575: 1507: 1475: 1442: 1370: 1339: 1235: 1212: 1175: 1159: 1148: 1138: 1134: 1073: 1000:
front deposits in the lower sections which transitioned to a
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beds are found in the lower sections of this formation while
864: 775: 763: 747: 743: 735: 663: 656: 423: 395: 195: 179: 2888: 950:
beds. This formation is a continuation of the environmental
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10.1130/0091-7613(1997)025<1087:IOSLAS>2.3.CO;2
2369: 2336:"A basin analysis of the northern facies of the Ecca group" 2165:
Rubidge, B. S.; Hancox, P. J.; Catuneanu, O. (1998-12-01).
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there is a locally well-known national monument called the
1780: 1754: 1744: 1661: 1646: 1611: 1607: 1503: 1472: 1461: 1362: 1198: 1171: 1124: 868: 843: 835: 653: 649: 427: 203: 2603:(Thesis thesis). Stellenbosch: University of Stellenbosch. 2043:
Origin and Evolution of the Cape Mountains and Karoo Basin
1563:: This formation has been subdivided into three different 1546:
where deposits of this formation are only found. Sporadic
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marine deposits through to channelized submarine slope to
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List of fossiliferous stratigraphic units in South Africa
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List of fossiliferous stratigraphic units in South Africa
4142: 1248:: Consists mainly of tabular, poorly-sorted fine-grained 1137:, often referred to in literature as the “Maijiesfontein 618: 439: 1234:. Coalified plant fragments are frequently found in the 512:
in its westernmost deposits, and continues east through
3542: 3207:(Thesis thesis). Stellenbosch: Stellenbosch University. 2986:
Journal of African Earth Sciences (and the Middle East)
1982:
Journal of African Earth Sciences (and the Middle East)
1824:, correlate in age with the Huab Basin of northwestern 3398:
Stanistreet, I.G., Le Blanc Smith, G. and Cadle, A.B.
2164: 1747:
seams themselves are classified as compaction fossils.
548:. In the extreme northeast deposits are found east of 456:) that had previously begun to take course due to the 452:. This foreland system was caused by crustal uplift ( 2408: 4679:
Tectonic evolution of the Barberton greenstone belt
1949:Visser, J. C.; Loock, J. N. J. & (1978-05-01). 988:are horizontally laminated and often exhibit wave- 442:settings are also well known from the Ecca Group. 370:, the Ecca Group ranges between Early to earliest 3472: 3356:"THE BIOSTRATIGRAPHY OF THE PERMIAN AND TRIASSIC" 3277:Palaeogeography, Palaeoclimatology, Palaeoecology 1820:of the Ecca Group, particularly the rocks of the 1567:arrangements. They are dominated by fine-grained 1211:units that are interbedded with planar-laminated 588:there are deposits of as of yet undifferentiated 6408: 2675:Veevers, J. J.; Powell, Chris McA (1994-01-01). 2612: 2610: 2035: 2033: 818:(syn.Mesosaurus brasiliensis), Permian (270 myo) 6137: 1526:succession and is not well studied due to poor 1478:settings in its central deposits. The northern 532:. In the central north deposits are found near 6158:Geological Commission of the Cape of Good Hope 4936:Department of Mineral Resources (South Africa) 3247: 2071: 2069: 1871:Abroad, Ecca-aged deposits are known from the 1061:marine and beach environments. The Laingsburg 860:: Predominantly composed of blackish, planar, 508:The rocks of the Ecca Group first appear near 334:is the second of the main subdivisions of the 4974:Archean life in the Barberton Greenstone Belt 4258: 3528: 2674: 2607: 2460: 2030: 1384:setting. Fragmentary plant hash material and 1151:in its westernmost outcrops which grade into 3422:: CS1 maint: multiple names: authors list ( 3317:: CS1 maint: multiple names: authors list ( 3248:Collinson, J. D.; Lewin, John (2009-04-15). 3143:: CS1 maint: multiple names: authors list ( 2983: 2784:: CS1 maint: multiple names: authors list ( 2597:Mve Nguema and Oliver Patrice (2005-12-01). 2569:: CS1 maint: multiple names: authors list ( 2319:: CS1 maint: multiple names: authors list ( 2262:: CS1 maint: multiple names: authors list ( 2022:: CS1 maint: multiple names: authors list ( 1534:cores. In addition exposed outcrops quickly 576:The Ecca Group comprises sixteen recognized 4272: 3201:Evans, F. J. (Fiona Jocelyn) (2005-12-01). 2456: 2454: 2066: 1948: 1282:layers along with larger, brown-weathering 6387: 5798: 5522: 4941:Department of Mineral Resources and Energy 4265: 4251: 3535: 3521: 806:, have been recovered from this formation. 342:. It mainly follows conformably after the 318: 4633: 4285: 3120: 3044: 3033:Zoological Journal of the Linnean Society 2855: 2434: 595:With the exception of the Prince Albert, 3436: 3353: 2798: 2451: 1862: 1807: 1484: 1100:have been recovered from this formation. 809: 722:have been recovered from this formation. 686:sequences that often contain ice rafted 592:sequences attributed to the Ecca Group. 499: 460:of the Palaeo-pacific plate beneath the 3067: 3026: 2643: 2616: 1799:has been recovered from this formation. 1602:were formed below the water surface in 850:took place during the time of sediment 445:The Ecca Group was deposited in a vast 6409: 2947: 2495: 2158: 2075: 1294:and slump structures, are found here. 896:-rich units that are interbedded with 571: 6308: 6281: 6280: 6136: 4957: 4870: 4632: 4284: 4246: 3516: 3200: 2463:International Journal of Coal Geology 1637:, within the Nongoma Graben. Diverse 1498:: Generally composed of dark colored 1015:layers, and in the other rock layers 4871: 3867:West and Central African Rift System 3027:Modesto, Sean Patrick (2006-03-01). 834:alternated with softer, yellow-grey 495: 6432:Geologic formations of South Africa 3543:Major African geological formations 2948:D.c, Araujo; B.w, Oelofsen (1987). 1899:have also been recovered. Finally, 13: 6163:Geological Society of South Africa 3251:Modern and Ancient Fluvial Systems 3070:Journal of Vertebrate Paleontology 2333: 1162:layers alternate with subordinate 774:remains are frequently found. The 738:dominant in the west/northwestern 14: 6468: 6442:Geologic formations of Madagascar 4715:List of volcanoes in South Africa 2681:. Geological Society of America. 2529:Journal of African Earth Sciences 2279:Journal of African Earth Sciences 2222:Journal of African Earth Sciences 1011:logs are frequently found in the 426:deposits in younger successions. 338:of geological strata in southern 6386: 6375: 6374: 6362: 6348: 6260:Eduard Meine van Zinderen-Bakker 4958: 3046:10.1111/j.1096-3642.2006.00205.x 2805:South African Journal of Geology 2650:South African Journal of Geology 2644:Viljoen, J. H. A. (1994-01-01). 2502:South African Journal of Geology 2299:10.1016/j.jafrearsci.2005.07.007 2191:10.1046/j.1365-2117.1998.00078.x 1955:South African Journal of Geology 608:Western/Northwestern Ecca facies 402:where the Tanqua and Laingsburg 291: 280: 269: 258: 247: 47: 6437:Geologic formations of Botswana 5545:Pristerognathus Assemblage Zone 3466: 3457: 3430: 3391: 3374: 3347: 3337: 3325: 3268: 3241: 3231: 3221: 3211: 3194: 3151: 3096: 3061: 3020: 2977: 2941: 2882: 2872: 2823: 2792: 2764:10.1016/j.marpetgeo.2012.02.006 2742: 2708:Journal of Sedimentary Research 2695: 2668: 2637: 2590: 2577: 2520: 2496:Visser, J. N. J. (1992-01-01). 2489: 2402: 2363: 2327: 1230:are often found in the massive 6422:Carboniferous System of Africa 6153:Evolutionary Studies Institute 5550:Tapinocephalus Assemblage Zone 2799:Kingsley, C. S. (1981-01-01). 2270: 2213: 2148: 2105: 1973: 1942: 1879:and the Petolas Basin of both 1828:, and lower formations of the 1803: 826:: Is composed of thin beds of 528:, and up until the coast near 1: 5535:Daptocephalus Assemblage Zone 5530:Cistecephalus Assemblage Zone 4931:Minerals Council South Africa 4788:1620 Robben Island earthquake 3495:10.1016/S1342-937X(05)70314-2 2549:10.1016/S0899-5362(96)00048-6 2334:Cj, Van Vuuren (2016-09-22). 2242:10.1016/S0899-5362(02)00154-9 1935: 1667:Asterotheca hammanskraalensis 1417:. Well-preserved symmetrical 1380:that were deposited in a pro- 1147:: Dominated by dark coloured 976:, and fine to medium-grained 842:environment. The presence of 418:) marine and marginal marine 385: 366:analyses, and other means of 6447:Paleontology in South Africa 6138:Research and administration‎ 5811:Lystrosaurus Assemblage Zone 5555:Tropidostoma Assemblage Zone 3297:10.1016/0031-0182(81)90053-5 3180:10.1016/0037-0738(77)90032-X 3122:10.1016/j.egypro.2013.08.030 3082:10.1080/02724634.2010.501443 3006:10.1016/0899-5362(90)90050-O 2752:Marine and Petroleum Geology 2475:10.1016/0166-5162(89)90058-X 2134:10.1016/0037-0738(77)90032-X 2051:10.1007/978-3-319-40859-0_14 2002:10.1016/0899-5362(93)90164-L 1207:: Composed of four, massive 584:successions. In the east of 7: 5806:Cynognathus Assemblage Zone 5540:Eodicynodon Assemblage Zone 2585:The geology of South Africa 1918: 1582:seams, and coarse-grained, 1578:with alternating layers of 1550:plant material and various 919:of worm feeding trails and 138:: Prince Albert Formation, 130:: Prince Albert Formation, 128:Western/Northwestern facies 10: 6473: 6457:Paleontology in Madagascar 4834:Vredefort impact structure 4824:Morokweng impact structure 4798:2006 Mozambique earthquake 3681:Central African Shear Zone 2617:Rubidge, Bruce S. (1990). 1703:. Abundant, low diversity 994:ball-and-pillow structures 935:that are interbedded with 6342: 6315: 6309: 6304: 6287: 6276: 6235:Daniel Rossouw Kannemeyer 6187: 6171: 6143: 6132: 6116:Waterloo Farm lagerstätte 6088: 6057: 6036: 6020: 5969: 5823: 5567: 5291: 5100: 5079: 5018: 4987: 4979:Waterloo Farm lagerstätte 4964: 4953: 4877: 4866: 4842: 4811: 4778: 4760:Barberton Greenstone Belt 4707: 4639: 4628: 4604: 4431: 4345: 4304: 4291: 4280: 4181: 4058:Central Pangean Mountains 4018: 3880: 3787: 3719: 3711:Western Meseta Shear Zone 3661: 3599: 3548: 3437:Pickford, Martin (1995). 3254:. John Wiley & Sons. 2076:Hobday, David K. (1977). 1930:Geography of South Africa 1844:. Near the small town of 1496:Pietermarizberg Formation 1256:alternate with dark-grey 902:bouma turbidite sequences 790:fossils, most notably of 711:Dwykaselachus oosthuizeni 317: 309: 304: 242: 228: 223: 209: 175: 170: 160: 150: 123: 113: 26: 21: 6452:Paleontology in Botswana 6427:Permian System of Africa 5856:Coelophysis rhodesiensis 4725:Pilanesberg Game Reserve 4376:Table Mountain Sandstone 4312:Bushveld Igneous Complex 3354:Anderson, J. M. (1973). 1451:Northeastern Ecca facies 1170:, and minor yellow-grey 890:Skoorsteenberg Formation 564:and all the way down to 354:and exposures. Based on 6369:South Africa portal 6205:Charles Kimberlin Brain 4793:1969 Tulbagh earthquake 4508:Abrahamskraal Formation 4462:Sundays River Formation 4386:Abrahamskraal Formation 4274:Geology of South Africa 3443:Palaeontologia Africana 3360:Palaeontologia Africana 2623:Palaeontologia Africana 1925:Geology of South Africa 1743:, and fish scales. The 1421:are often found in the 1070:Prince Albert Formation 766:. Fossil plant matter, 646:Prince Albert Formation 633:fall within the Tanqua 390:During the time of the 6220:Anusuya Chinsamy-Turan 6148:Council for Geoscience 6111:West Coast Fossil Park 4803:2014 Orkney earthquake 4684:Terra Australis Orogen 4634:‎Tectonics and orogeny 4447:Buffelskloof Formation 4078:Eastern Rift mountains 4000:Tanzania Coastal Basin 3779:Terra Australis Orogen 2965:Cite journal requires 2351:Cite journal requires 2093:Cite journal requires 1868: 1813: 1491: 1116:deposits that contain 900:layers. These contain 819: 782:, although shallower, 505: 4730:Prince Edward Islands 4286:Geological formations 4093:Great Karas Mountains 4073:Eastern Arc Mountains 3613:Arabian-Nubian Shield 2857:10.1515/geo-2019-0025 2436:10.1515/geo-2017-0042 1866: 1818:geological formations 1811: 1757:-rich, grey to black 1488: 1178:layers often contain 1072:: Black to dark grey 929:Kookfontein Formation 813: 803:Stereosternum tumidum 694:setting, and various 617:succession is purely 578:geological formations 503: 6292:Geology of Cape Town 6250:John Talbot Robinson 6200:Lieuwe Dirk Boonstra 4906:Coal in South Africa 4897:Banket (mining term) 4594:Normandien Formation 4337:Transvaal Supergroup 3990:Somali Coastal Basin 3701:Mwembeshi Shear Zone 3404:www.researchgate.net 2728:10.2110/jsr.2010.002 1621:formed on abandoned 1313:Fort Brown Formation 1286:structures. Various 1205:Laingsburg Formation 1131:Collingham Formation 1037:Southern Ecca facies 846:beds indicates that 824:Collingham Formation 816:Mesosaurus tenuidens 793:Mesosaurus tenuidens 536:, running along the 6255:George William Stow 6096:Cradle of Humankind 4850:Bellsbank meteorite 4743:Finsch diamond mine 4699:Witwatersrand Basin 4674:Makhonjwa Mountains 4545:Whitehill Formation 4523:Middleton Formation 4411:Whitehill Formation 4401:Ganigobis Formation 4361:Ganigobis Formation 4168:Teffedest Mountains 4083:Ethiopian Highlands 3774:Pan-African orogens 3744:East African Orogen 3676:Broodkop Shear Zone 3648:West African Craton 3591:Victoria Microplate 3487:2004GondR...7..153B 3289:1981PPP....36..113T 3172:1977SedG...19..217V 3160:Sedimentary Geology 2998:1990JAfES..10..117S 2911:10.1038/nature20806 2903:2017Natur.541..208C 2848:2019OGeo...11...25B 2720:2010JSedR..80...97F 2541:1996JAfES..23....3J 2427:2017OGeo....9...42B 2388:1997Geo....25.1087C 2291:2005JAfES..43..211C 2234:2002JAfES..35..489C 2183:1998BasR...10..417C 2126:1977SedG...19..217V 2114:Sedimentary Geology 1994:1993JAfES..16..143S 1909:Marcellus Formation 1822:Whitehill Formation 1753:: Mainly comprises 1751:Volksrust Formation 1606:conditions and the 1395:Waterford Formation 1290:structures, namely 1271:layers. Spherical, 1145:Vischkuil Formation 1105:Whitehill Formation 962:Waterford Formation 925:fossils are common. 727:Whitehill Formation 572:Stratigraphic units 144:Northeastern facies 140:Whitehill Formation 132:Whitehill Formation 28:Stratigraphic range 6355:Geology portal 6230:Alfred W. Crompton 6195:Andrew Geddes Bain 5479:Pristerognathoides 4919:Titanium in Africa 4914:Platinum in Africa 4910:Iron ore in Africa 4753:Koffiefontein mine 4748:Jagersfontein Mine 4659:Gondwanide orogeny 4557:Bushveld Sandstone 4528:Teekloof Formation 4457:Kirkwood Formation 4406:Teekloof Formation 4317:Fig Tree Formation 4232:List of inselbergs 4202:Jugurtha Tableland 4153:Sankwala Mountains 4148:Rwenzori Mountains 3965:Ouled Abdoun Basin 3960:Orange River Basin 3882:Sedimentary basins 3691:Foumban Shear Zone 3633:Saharan Metacraton 1869: 1814: 1791:settings. A large 1492: 1263:composed of thin, 1197:. The presence of 908:-front slope of a 858:Tierberg Formation 820: 707:cartilaginous fish 637:, one of the vast 568:in the southeast. 506: 466:Gondwanide orogeny 360:lithostratigraphic 32:Late Carboniferous 6404: 6403: 6338: 6337: 6320:Pothole (geology) 6300: 6299: 6282:Regional articles 6272: 6271: 6268: 6267: 6225:H. Basil S. Cooke 6128: 6127: 6124: 6123: 5901:Heterodontosaurus 5819: 5818: 5563: 5562: 5494:Promoschorhynchus 4949: 4948: 4924:Uranium in Africa 4872:‎Mineral deposits 4862: 4861: 4858: 4857: 4624: 4623: 4620: 4619: 4589:Molteno Formation 4584:Katberg Formation 4562:Clarens Formation 4518:Katberg Formation 4513:Balfour Formation 4481:Drakensberg Group 4469:Kalahari Deposits 4391:Balfour Formation 4322:Komatii Formation 4240: 4239: 4173:Tibesti Mountains 4133:Mitumba Mountains 4123:Mandara Mountains 4108:Imatong Mountains 4063:Chaillu Mountains 4043:Bambouk Mountains 3980:Rio del Rey Basin 3950:Niger Delta Basin 3935:Iullemmeden Basin 3827:Gulf of Suez Rift 3822:East African Rift 3807:Bahr el Arab rift 3754:Gondwanide Orogen 3686:Chuan Shear Zones 3475:Gondwana Research 2897:(7636): 208–211. 2382:(12): 1087–1090. 1901:geological dating 1887:where fossils of 1761:containing thin, 1561:Vryheid Formation 1518:with subordinate 1456:The northeastern 1278:are found in the 1158:in the east. The 1084:setting. Various 946:and fine-grained 848:volcanic activity 786:conditions. Rare 496:Geographic extent 422:, and finally to 368:geological dating 328: 327: 6464: 6390: 6389: 6378: 6377: 6367: 6366: 6365: 6353: 6352: 6306: 6305: 6278: 6277: 6169: 6168: 6134: 6133: 5796: 5795: 5520: 5519: 5449:Macroscelesaurus 5329:Cistecephaloides 5314:Blattoidealestes 5138:Cistecephaloides 5041:Deltacephalaspis 4985: 4984: 4955: 4954: 4868: 4867: 4705: 4704: 4630: 4629: 4579:Elliot Formation 4567:Elliot Formation 4498:Karoo Supergroup 4332:Onverwacht Group 4302: 4301: 4282: 4281: 4267: 4260: 4253: 4244: 4243: 4128:Marrah Mountains 4103:Hoggar Mountains 4098:Guinea Highlands 4088:Great Escarpment 3852:Sangha Aulacogen 3769:Mauritanide Belt 3696:Kandi Fault Zone 3671:Aswa Dislocation 3586:Seychelles Plate 3576:Madagascar Plate 3537: 3530: 3523: 3514: 3513: 3507: 3506: 3470: 3464: 3461: 3455: 3454: 3434: 3428: 3427: 3421: 3413: 3411: 3410: 3395: 3389: 3378: 3372: 3371: 3351: 3345: 3341: 3335: 3329: 3323: 3322: 3316: 3308: 3283:(1–2): 113–123. 3272: 3266: 3265: 3245: 3239: 3235: 3229: 3225: 3219: 3215: 3209: 3208: 3198: 3192: 3191: 3155: 3149: 3148: 3142: 3134: 3124: 3100: 3094: 3093: 3076:(5): 1378–1395. 3065: 3059: 3058: 3048: 3024: 3018: 3017: 2992:(1–2): 117–137. 2981: 2975: 2974: 2968: 2963: 2961: 2953: 2945: 2939: 2938: 2886: 2880: 2876: 2870: 2869: 2859: 2836:Open Geosciences 2827: 2821: 2820: 2796: 2790: 2789: 2783: 2775: 2746: 2740: 2739: 2699: 2693: 2692: 2672: 2666: 2665: 2641: 2635: 2634: 2614: 2605: 2604: 2594: 2588: 2581: 2575: 2574: 2568: 2560: 2524: 2518: 2517: 2508:(5–6): 181–193. 2493: 2487: 2486: 2469:(1–4): 365–380. 2458: 2449: 2448: 2438: 2415:Open Geosciences 2406: 2400: 2399: 2367: 2361: 2360: 2354: 2349: 2347: 2339: 2331: 2325: 2324: 2318: 2310: 2285:(1–3): 211–253. 2274: 2268: 2267: 2261: 2253: 2217: 2211: 2210: 2162: 2156: 2152: 2146: 2145: 2109: 2103: 2102: 2096: 2091: 2089: 2081: 2073: 2064: 2063: 2037: 2028: 2027: 2021: 2013: 1988:(1–2): 143–169. 1977: 1971: 1970: 1946: 1854:Petrified Forest 1405:. It is rich in 1299:fossil trackways 1226:and clay pebble 990:rippled surfaces 878:and clay pellet 562:Pietermaritzburg 476:partitioned the 336:Karoo Supergroup 322: 297: 295: 294: 286: 284: 283: 275: 273: 272: 264: 262: 261: 253: 251: 250: 109: 46: 19: 18: 6472: 6471: 6467: 6466: 6465: 6463: 6462: 6461: 6407: 6406: 6405: 6400: 6363: 6361: 6347: 6334: 6325:Steep structure 6311: 6296: 6283: 6264: 6188:Paleontologists 6183: 6167: 6139: 6120: 6084: 6080:Vulpes skinneri 6053: 6032: 6016: 6012:Ptychoceratodus 5977:Acanthohoplites 5965: 5941:Ptychoceratodus 5815: 5794: 5745:Ptychoceratodus 5720:Platycraniellus 5645:Ictidosuchoides 5559: 5518: 5499:Scalopocephalus 5484:Pristerognathus 5399:Homodontosaurus 5287: 5213:Ictidosuchoides 5153:Dicynodontoides 5133:Charassognathus 5096: 5075: 5051:Gondwanascorpio 5014: 4983: 4960: 4945: 4873: 4854: 4838: 4807: 4774: 4703: 4689:Transvaal Basin 4669:Kalahari Craton 4664:Kaapvaal Craton 4635: 4616: 4600: 4552:Stormberg Group 4491:Uitenhage Group 4442:Uitenhage Group 4427: 4371:Bokkeveld Group 4341: 4300: 4287: 4276: 4271: 4241: 4236: 4197:Mount Gorongosa 4177: 4038:Aurès Mountains 4033:Atlas Mountains 4020:Mountain ranges 4014: 3900:Blue Nile Basin 3876: 3872:White Nile rift 3783: 3749:Eburnean Orogen 3715: 3706:Todi Shear Zone 3657: 3653:Zimbabwe Craton 3638:Tanzania Craton 3628:Kalahari Craton 3623:Kaapvaal Craton 3595: 3544: 3541: 3511: 3510: 3471: 3467: 3462: 3458: 3435: 3431: 3415: 3414: 3408: 3406: 3396: 3392: 3382:Palaeontol. Aft 3379: 3375: 3352: 3348: 3342: 3338: 3330: 3326: 3310: 3309: 3273: 3269: 3262: 3246: 3242: 3236: 3232: 3226: 3222: 3216: 3212: 3199: 3195: 3156: 3152: 3136: 3135: 3109:Energy Procedia 3101: 3097: 3066: 3062: 3025: 3021: 2982: 2978: 2966: 2964: 2955: 2954: 2946: 2942: 2887: 2883: 2877: 2873: 2828: 2824: 2797: 2793: 2777: 2776: 2747: 2743: 2700: 2696: 2689: 2673: 2669: 2642: 2638: 2615: 2608: 2595: 2591: 2582: 2578: 2562: 2561: 2525: 2521: 2494: 2490: 2459: 2452: 2407: 2403: 2368: 2364: 2352: 2350: 2341: 2340: 2332: 2328: 2312: 2311: 2275: 2271: 2255: 2254: 2218: 2214: 2163: 2159: 2153: 2149: 2110: 2106: 2094: 2092: 2083: 2082: 2074: 2067: 2061: 2038: 2031: 2015: 2014: 1978: 1974: 1947: 1943: 1938: 1921: 1806: 1654:fruitifications 1623:alluvial plains 1580:bituminous coal 1538:out due to the 1435:intertidal zone 1391:are found here. 1319:of alternating 1309:are also found. 1246:Ripon Formation 1195:basin-floor fan 1191:liesegang rings 1009:Fossilized tree 574: 498: 388: 323: 292: 290: 281: 279: 270: 268: 259: 257: 248: 246: 136:Southern facies 108: 107: 102: 97: 92: 87: 82: 77: 72: 67: 62: 57: 52: 41: 40: 38: 17: 12: 11: 5: 6470: 6460: 6459: 6454: 6449: 6444: 6439: 6434: 6429: 6424: 6419: 6402: 6401: 6399: 6398: 6391: 6384: 6372: 6358: 6343: 6340: 6339: 6336: 6335: 6333: 6332: 6327: 6322: 6316: 6313: 6312: 6302: 6301: 6298: 6297: 6295: 6294: 6288: 6285: 6284: 6274: 6273: 6270: 6269: 6266: 6265: 6263: 6262: 6257: 6252: 6247: 6245:James Kitching 6242: 6237: 6232: 6227: 6222: 6217: 6212: 6207: 6202: 6197: 6191: 6189: 6185: 6184: 6182: 6181: 6175: 6173: 6166: 6165: 6160: 6155: 6150: 6144: 6141: 6140: 6130: 6129: 6126: 6125: 6122: 6121: 6119: 6118: 6113: 6108: 6103: 6098: 6092: 6090: 6086: 6085: 6083: 6082: 6077: 6075:Panthera shawi 6072: 6067: 6061: 6059: 6055: 6054: 6052: 6051: 6046: 6040: 6038: 6034: 6033: 6031: 6030: 6024: 6022: 6018: 6017: 6015: 6014: 6009: 6004: 5999: 5997:Macroscaphites 5994: 5989: 5984: 5979: 5973: 5971: 5967: 5966: 5964: 5963: 5958: 5953: 5951:Sefapanosaurus 5948: 5943: 5938: 5933: 5928: 5926:Massospondylus 5923: 5918: 5913: 5908: 5903: 5898: 5893: 5888: 5883: 5878: 5873: 5871:Erythrotherium 5868: 5863: 5858: 5853: 5848: 5843: 5838: 5833: 5827: 5825: 5821: 5820: 5817: 5816: 5814: 5813: 5808: 5802: 5800: 5793: 5792: 5790:Zorillodontops 5787: 5782: 5777: 5772: 5767: 5762: 5757: 5752: 5747: 5742: 5737: 5732: 5727: 5722: 5717: 5715:Plateosauravus 5712: 5707: 5702: 5700:Olivierosuchus 5697: 5692: 5687: 5682: 5680:Microgomphodon 5677: 5672: 5670:Melanorosaurus 5667: 5662: 5657: 5652: 5647: 5642: 5637: 5632: 5627: 5622: 5620:Erythrotherium 5617: 5612: 5607: 5602: 5597: 5592: 5587: 5582: 5577: 5575:Batrachosuchus 5571: 5569: 5565: 5564: 5561: 5560: 5558: 5557: 5552: 5547: 5542: 5537: 5532: 5526: 5524: 5517: 5516: 5514:Uranocentrodon 5511: 5506: 5501: 5496: 5491: 5486: 5481: 5476: 5471: 5466: 5461: 5456: 5451: 5446: 5441: 5436: 5431: 5429:Lanthanostegus 5426: 5421: 5416: 5411: 5406: 5401: 5396: 5391: 5386: 5381: 5376: 5371: 5366: 5361: 5359:Cynariognathus 5356: 5351: 5346: 5341: 5336: 5331: 5326: 5321: 5319:Brachyprosopus 5316: 5311: 5306: 5301: 5295: 5293: 5292:Beaufort Group 5289: 5288: 5286: 5285: 5280: 5275: 5270: 5265: 5260: 5255: 5250: 5245: 5240: 5235: 5230: 5225: 5220: 5215: 5210: 5205: 5200: 5195: 5190: 5185: 5180: 5175: 5170: 5165: 5160: 5155: 5150: 5145: 5140: 5135: 5130: 5125: 5120: 5115: 5113:Alopecognathus 5110: 5104: 5102: 5098: 5097: 5095: 5094: 5089: 5083: 5081: 5077: 5076: 5074: 5073: 5068: 5063: 5058: 5053: 5048: 5043: 5038: 5033: 5028: 5022: 5020: 5016: 5015: 5013: 5012: 5007: 5002: 5000:Onychopterella 4997: 4991: 4989: 4982: 4981: 4976: 4971: 4965: 4962: 4961: 4951: 4950: 4947: 4946: 4944: 4943: 4938: 4933: 4927: 4926: 4921: 4916: 4911: 4908: 4902: 4901: 4900: 4899: 4889: 4884: 4878: 4875: 4874: 4864: 4863: 4860: 4859: 4856: 4855: 4853: 4852: 4846: 4844: 4840: 4839: 4837: 4836: 4831: 4829:Tswaing crater 4826: 4821: 4819:Kalkkop crater 4815: 4813: 4812:Impact craters 4809: 4808: 4806: 4805: 4800: 4795: 4790: 4784: 4782: 4776: 4775: 4773: 4772: 4767: 4762: 4757: 4756: 4755: 4750: 4745: 4740: 4732: 4727: 4722: 4717: 4711: 4709: 4702: 4701: 4696: 4691: 4686: 4681: 4676: 4671: 4666: 4661: 4656: 4654:Ellisras Basin 4651: 4649:Cape Fold Belt 4646: 4640: 4637: 4636: 4626: 4625: 4622: 4621: 4618: 4617: 4615: 4614: 4608: 4606: 4602: 4601: 4599: 4598: 4597: 4596: 4591: 4586: 4581: 4573: 4572: 4571: 4570: 4569: 4564: 4559: 4549: 4548: 4547: 4537: 4532: 4531: 4530: 4525: 4520: 4515: 4510: 4503:Beaufort Group 4495: 4494: 4493: 4488: 4486:Enon Formation 4483: 4474: 4473: 4472: 4471: 4466: 4465: 4464: 4459: 4454: 4452:Enon Formation 4449: 4435: 4433: 4429: 4428: 4426: 4425: 4424: 4423: 4415: 4414: 4413: 4408: 4403: 4398: 4393: 4388: 4380: 4379: 4378: 4373: 4365: 4364: 4363: 4358: 4352:Carboniferous 4349: 4347: 4343: 4342: 4340: 4339: 4334: 4329: 4324: 4319: 4314: 4308: 4306: 4305:Palaeoarchaean 4299: 4298: 4292: 4289: 4288: 4278: 4277: 4270: 4269: 4262: 4255: 4247: 4238: 4237: 4235: 4234: 4229: 4224: 4219: 4217:Mont NiĂ©nokouĂ© 4214: 4212:Mulanje Massif 4209: 4204: 4199: 4194: 4188: 4186: 4179: 4178: 4176: 4175: 4170: 4165: 4163:Serra da Chela 4160: 4155: 4150: 4145: 4140: 4138:Nuba Mountains 4135: 4130: 4125: 4120: 4118:Loma Mountains 4115: 4110: 4105: 4100: 4095: 4090: 4085: 4080: 4075: 4070: 4065: 4060: 4055: 4050: 4048:Blue Mountains 4045: 4040: 4035: 4030: 4024: 4022: 4016: 4015: 4013: 4012: 4007: 4002: 3997: 3995:Taoudeni Basin 3992: 3987: 3982: 3977: 3972: 3967: 3962: 3957: 3952: 3947: 3942: 3937: 3932: 3927: 3922: 3917: 3912: 3907: 3902: 3897: 3892: 3886: 3884: 3878: 3877: 3875: 3874: 3869: 3864: 3859: 3854: 3849: 3844: 3839: 3834: 3832:Lamu Embayment 3829: 3824: 3819: 3817:Blue Nile rift 3814: 3809: 3804: 3799: 3793: 3791: 3785: 3784: 3782: 3781: 3776: 3771: 3766: 3761: 3759:Kibaran Orogen 3756: 3751: 3746: 3741: 3736: 3734:Cape Fold Belt 3731: 3725: 3723: 3717: 3716: 3714: 3713: 3708: 3703: 3698: 3693: 3688: 3683: 3678: 3673: 3667: 3665: 3659: 3658: 3656: 3655: 3650: 3645: 3640: 3635: 3630: 3625: 3620: 3615: 3609: 3607: 3597: 3596: 3594: 3593: 3588: 3583: 3578: 3573: 3567: 3563:Minor plates: 3561: 3557:Major plates: 3554: 3552: 3546: 3545: 3540: 3539: 3532: 3525: 3517: 3509: 3508: 3481:(1): 153–164. 3465: 3456: 3429: 3390: 3373: 3346: 3336: 3324: 3267: 3260: 3240: 3230: 3220: 3210: 3193: 3150: 3095: 3060: 3039:(3): 345–368. 3019: 2976: 2967:|journal= 2940: 2881: 2871: 2842:(1): 313–326. 2822: 2791: 2741: 2694: 2687: 2667: 2656:(2): 167–183. 2636: 2606: 2589: 2576: 2519: 2488: 2450: 2421:(1): 554–576. 2401: 2362: 2353:|journal= 2326: 2269: 2228:(4): 489–502. 2212: 2177:(4): 417–439. 2171:Basin Research 2157: 2147: 2104: 2095:|journal= 2065: 2059: 2029: 1972: 1961:(2): 185–191. 1940: 1939: 1937: 1934: 1933: 1932: 1927: 1920: 1917: 1858:Petrified logs 1830:Kalahari Basin 1805: 1802: 1801: 1800: 1777:Beaufort Group 1748: 1737:conchostracans 1716:Diplocraterion 1699:, and diverse 1558: 1447: 1446: 1413:and sometimes 1392: 1310: 1243: 1202: 1174:deposits. The 1142: 1128: 1101: 1053:sediments and 1033: 1032: 959: 926: 887: 855: 808: 807: 796:, and another 788:marine reptile 723: 573: 570: 566:Port St. Johns 497: 494: 450:foreland basin 387: 384: 372:Middle Permian 348:Beaufort Group 326: 325: 315: 314: 311: 307: 306: 302: 301: 244: 240: 239: 230: 226: 225: 221: 220: 211: 207: 206: 177: 173: 172: 168: 167: 162: 158: 157: 155:Beaufort Group 152: 148: 147: 125: 121: 120: 118:Geologic group 115: 111: 110: 103: 98: 93: 88: 83: 78: 73: 68: 63: 58: 53: 48: 24: 23: 15: 9: 6: 4: 3: 2: 6469: 6458: 6455: 6453: 6450: 6448: 6445: 6443: 6440: 6438: 6435: 6433: 6430: 6428: 6425: 6423: 6420: 6418: 6415: 6414: 6412: 6397: 6396: 6392: 6385: 6383: 6382: 6373: 6371: 6370: 6359: 6357: 6356: 6351: 6345: 6344: 6341: 6331: 6328: 6326: 6323: 6321: 6318: 6317: 6314: 6307: 6303: 6293: 6290: 6289: 6286: 6279: 6275: 6261: 6258: 6256: 6253: 6251: 6248: 6246: 6243: 6241: 6238: 6236: 6233: 6231: 6228: 6226: 6223: 6221: 6218: 6216: 6213: 6211: 6208: 6206: 6203: 6201: 6198: 6196: 6193: 6192: 6190: 6186: 6180: 6179:Hans Merensky 6177: 6176: 6174: 6170: 6164: 6161: 6159: 6156: 6154: 6151: 6149: 6146: 6145: 6142: 6135: 6131: 6117: 6114: 6112: 6109: 6107: 6106:Scylacorhinus 6104: 6102: 6099: 6097: 6094: 6093: 6091: 6087: 6081: 6078: 6076: 6073: 6071: 6068: 6066: 6063: 6062: 6060: 6056: 6050: 6047: 6045: 6044:Africanacetus 6042: 6041: 6039: 6035: 6029: 6026: 6025: 6023: 6019: 6013: 6010: 6008: 6005: 6003: 6000: 5998: 5995: 5993: 5990: 5988: 5985: 5983: 5980: 5978: 5975: 5974: 5972: 5968: 5962: 5959: 5957: 5954: 5952: 5949: 5947: 5944: 5942: 5939: 5937: 5934: 5932: 5929: 5927: 5924: 5922: 5919: 5917: 5916:Litargosuchus 5914: 5912: 5911:Lesothosaurus 5909: 5907: 5904: 5902: 5899: 5897: 5894: 5892: 5889: 5887: 5886:Gigantoscelus 5884: 5882: 5879: 5877: 5874: 5872: 5869: 5867: 5864: 5862: 5859: 5857: 5854: 5852: 5849: 5847: 5844: 5842: 5839: 5837: 5836:Abrictosaurus 5834: 5832: 5829: 5828: 5826: 5822: 5812: 5809: 5807: 5804: 5803: 5801: 5797: 5791: 5788: 5786: 5783: 5781: 5778: 5776: 5773: 5771: 5768: 5766: 5763: 5761: 5758: 5756: 5755:Scaloposaurus 5753: 5751: 5748: 5746: 5743: 5741: 5740:Proterosuchus 5738: 5736: 5733: 5731: 5730:Progalesaurus 5728: 5726: 5723: 5721: 5718: 5716: 5713: 5711: 5708: 5706: 5703: 5701: 5698: 5696: 5693: 5691: 5688: 5686: 5683: 5681: 5678: 5676: 5673: 5671: 5668: 5666: 5663: 5661: 5658: 5656: 5655:Lepidodendron 5653: 5651: 5648: 5646: 5643: 5641: 5638: 5636: 5633: 5631: 5630:Euskelosaurus 5628: 5626: 5625:Eucnemesaurus 5623: 5621: 5618: 5616: 5615:Erythrosuchus 5613: 5611: 5610:Ericiolacerta 5608: 5606: 5603: 5601: 5598: 5596: 5593: 5591: 5588: 5586: 5583: 5581: 5580:Blikanasaurus 5578: 5576: 5573: 5572: 5570: 5566: 5556: 5553: 5551: 5548: 5546: 5543: 5541: 5538: 5536: 5533: 5531: 5528: 5527: 5525: 5521: 5515: 5512: 5510: 5507: 5505: 5502: 5500: 5497: 5495: 5492: 5490: 5487: 5485: 5482: 5480: 5477: 5475: 5472: 5470: 5467: 5465: 5464:Pelictosuchus 5462: 5460: 5457: 5455: 5452: 5450: 5447: 5445: 5442: 5440: 5439:Lepidodendron 5437: 5435: 5432: 5430: 5427: 5425: 5422: 5420: 5417: 5415: 5412: 5410: 5409:Ictidochampsa 5407: 5405: 5402: 5400: 5397: 5395: 5392: 5390: 5387: 5385: 5382: 5380: 5377: 5375: 5372: 5370: 5367: 5365: 5362: 5360: 5357: 5355: 5354:Cryptocynodon 5352: 5350: 5347: 5345: 5342: 5340: 5337: 5335: 5332: 5330: 5327: 5325: 5322: 5320: 5317: 5315: 5312: 5310: 5307: 5305: 5304:Anomocephalus 5302: 5300: 5297: 5296: 5294: 5290: 5284: 5281: 5279: 5276: 5274: 5273:Thliptosaurus 5271: 5269: 5268:Theriognathus 5266: 5264: 5263:Stereosternum 5261: 5259: 5256: 5254: 5251: 5249: 5248:Scylacosaurus 5246: 5244: 5243:Procynosuchus 5241: 5239: 5238:Odontocyclops 5236: 5234: 5231: 5229: 5226: 5224: 5221: 5219: 5218:Lepidodendron 5216: 5214: 5211: 5209: 5208:Ictidognathus 5206: 5204: 5201: 5199: 5196: 5194: 5191: 5189: 5186: 5184: 5181: 5179: 5176: 5174: 5173:Dwykaselachus 5171: 5169: 5166: 5164: 5161: 5159: 5156: 5154: 5151: 5149: 5146: 5144: 5143:Crapartinella 5141: 5139: 5136: 5134: 5131: 5129: 5126: 5124: 5121: 5119: 5118:Anomocephalus 5116: 5114: 5111: 5109: 5106: 5105: 5103: 5099: 5093: 5092:Lepidodendron 5090: 5088: 5085: 5084: 5082: 5080:Carboniferous 5078: 5072: 5069: 5067: 5064: 5062: 5059: 5057: 5054: 5052: 5049: 5047: 5044: 5042: 5039: 5037: 5034: 5032: 5031:Antarctilamna 5029: 5027: 5024: 5023: 5021: 5017: 5011: 5008: 5006: 5003: 5001: 4998: 4996: 4993: 4992: 4990: 4986: 4980: 4977: 4975: 4972: 4970: 4967: 4966: 4963: 4959:Paleontology‎ 4956: 4952: 4942: 4939: 4937: 4934: 4932: 4929: 4928: 4925: 4922: 4920: 4917: 4915: 4912: 4909: 4907: 4904: 4903: 4898: 4895: 4894: 4893: 4892:Witwatersrand 4890: 4888: 4887:Merensky Reef 4885: 4883: 4880: 4879: 4876: 4869: 4865: 4851: 4848: 4847: 4845: 4841: 4835: 4832: 4830: 4827: 4825: 4822: 4820: 4817: 4816: 4814: 4810: 4804: 4801: 4799: 4796: 4794: 4791: 4789: 4786: 4785: 4783: 4781: 4777: 4771: 4768: 4766: 4763: 4761: 4758: 4754: 4751: 4749: 4746: 4744: 4741: 4739: 4736: 4735: 4733: 4731: 4728: 4726: 4723: 4721: 4718: 4716: 4713: 4712: 4710: 4706: 4700: 4697: 4695: 4692: 4690: 4687: 4685: 4682: 4680: 4677: 4675: 4672: 4670: 4667: 4665: 4662: 4660: 4657: 4655: 4652: 4650: 4647: 4645: 4642: 4641: 4638: 4631: 4627: 4613: 4610: 4609: 4607: 4603: 4595: 4592: 4590: 4587: 4585: 4582: 4580: 4577: 4576: 4574: 4568: 4565: 4563: 4560: 4558: 4555: 4554: 4553: 4550: 4546: 4543: 4542: 4541: 4538: 4536: 4533: 4529: 4526: 4524: 4521: 4519: 4516: 4514: 4511: 4509: 4506: 4505: 4504: 4501: 4500: 4499: 4496: 4492: 4489: 4487: 4484: 4482: 4479: 4478: 4476: 4475: 4470: 4467: 4463: 4460: 4458: 4455: 4453: 4450: 4448: 4445: 4444: 4443: 4440: 4439: 4437: 4436: 4434: 4430: 4422: 4419: 4418: 4416: 4412: 4409: 4407: 4404: 4402: 4399: 4397: 4394: 4392: 4389: 4387: 4384: 4383: 4381: 4377: 4374: 4372: 4369: 4368: 4366: 4362: 4359: 4357: 4354: 4353: 4351: 4350: 4348: 4344: 4338: 4335: 4333: 4330: 4328: 4327:Moodies Group 4325: 4323: 4320: 4318: 4315: 4313: 4310: 4309: 4307: 4303: 4297: 4294: 4293: 4290: 4283: 4279: 4275: 4268: 4263: 4261: 4256: 4254: 4249: 4248: 4245: 4233: 4230: 4228: 4225: 4223: 4220: 4218: 4215: 4213: 4210: 4208: 4205: 4203: 4200: 4198: 4195: 4193: 4190: 4189: 4187: 4184: 4180: 4174: 4171: 4169: 4166: 4164: 4161: 4159: 4158:Serra da Leba 4156: 4154: 4151: 4149: 4146: 4144: 4143:Rif Mountains 4141: 4139: 4136: 4134: 4131: 4129: 4126: 4124: 4121: 4119: 4116: 4114: 4113:Jebel Uweinat 4111: 4109: 4106: 4104: 4101: 4099: 4096: 4094: 4091: 4089: 4086: 4084: 4081: 4079: 4076: 4074: 4071: 4069: 4066: 4064: 4061: 4059: 4056: 4054: 4053:Cameroon line 4051: 4049: 4046: 4044: 4041: 4039: 4036: 4034: 4031: 4029: 4028:AĂŻr Mountains 4026: 4025: 4023: 4021: 4017: 4011: 4010:Turkana Basin 4008: 4006: 4005:Tindouf Basin 4003: 4001: 3998: 3996: 3993: 3991: 3988: 3986: 3983: 3981: 3978: 3976: 3975:Reggane Basin 3973: 3971: 3968: 3966: 3963: 3961: 3958: 3956: 3953: 3951: 3948: 3946: 3943: 3941: 3938: 3936: 3933: 3931: 3928: 3926: 3923: 3921: 3918: 3916: 3913: 3911: 3908: 3906: 3903: 3901: 3898: 3896: 3893: 3891: 3888: 3887: 3885: 3883: 3879: 3873: 3870: 3868: 3865: 3863: 3860: 3858: 3855: 3853: 3850: 3848: 3845: 3843: 3840: 3838: 3835: 3833: 3830: 3828: 3825: 3823: 3820: 3818: 3815: 3813: 3810: 3808: 3805: 3803: 3800: 3798: 3797:Afar Triangle 3795: 3794: 3792: 3790: 3786: 3780: 3777: 3775: 3772: 3770: 3767: 3765: 3764:Kuunga Orogen 3762: 3760: 3757: 3755: 3752: 3750: 3747: 3745: 3742: 3740: 3739:Damara Orogen 3737: 3735: 3732: 3730: 3729:Alpine Orogen 3727: 3726: 3724: 3722: 3718: 3712: 3709: 3707: 3704: 3702: 3699: 3697: 3694: 3692: 3689: 3687: 3684: 3682: 3679: 3677: 3674: 3672: 3669: 3668: 3666: 3664: 3660: 3654: 3651: 3649: 3646: 3644: 3643:Tuareg Shield 3641: 3639: 3636: 3634: 3631: 3629: 3626: 3624: 3621: 3619: 3616: 3614: 3611: 3610: 3608: 3606: 3602: 3598: 3592: 3589: 3587: 3584: 3582: 3579: 3577: 3574: 3572: 3571:Lwandle Plate 3569:Microplates: 3568: 3566: 3562: 3560: 3559:African Plate 3556: 3555: 3553: 3551: 3547: 3538: 3533: 3531: 3526: 3524: 3519: 3518: 3515: 3504: 3500: 3496: 3492: 3488: 3484: 3480: 3476: 3469: 3460: 3452: 3448: 3444: 3440: 3433: 3425: 3419: 3405: 3401: 3394: 3387: 3383: 3377: 3369: 3365: 3361: 3357: 3350: 3340: 3334: 3328: 3320: 3314: 3306: 3302: 3298: 3294: 3290: 3286: 3282: 3278: 3271: 3263: 3261:9781444303780 3257: 3253: 3252: 3244: 3234: 3224: 3214: 3206: 3205: 3197: 3189: 3185: 3181: 3177: 3173: 3169: 3165: 3161: 3154: 3146: 3140: 3132: 3128: 3123: 3118: 3114: 3110: 3106: 3099: 3091: 3087: 3083: 3079: 3075: 3071: 3064: 3056: 3052: 3047: 3042: 3038: 3034: 3030: 3023: 3015: 3011: 3007: 3003: 2999: 2995: 2991: 2987: 2980: 2972: 2959: 2951: 2944: 2936: 2932: 2928: 2924: 2920: 2916: 2912: 2908: 2904: 2900: 2896: 2892: 2885: 2875: 2867: 2863: 2858: 2853: 2849: 2845: 2841: 2837: 2833: 2826: 2818: 2814: 2810: 2806: 2802: 2795: 2787: 2781: 2773: 2769: 2765: 2761: 2757: 2753: 2745: 2737: 2733: 2729: 2725: 2721: 2717: 2714:(1): 97–118. 2713: 2709: 2705: 2698: 2690: 2688:9780813711843 2684: 2680: 2679: 2671: 2663: 2659: 2655: 2651: 2647: 2640: 2632: 2628: 2624: 2620: 2613: 2611: 2602: 2601: 2593: 2587:, pp.461-499. 2586: 2580: 2572: 2566: 2558: 2554: 2550: 2546: 2542: 2538: 2534: 2530: 2523: 2515: 2511: 2507: 2503: 2499: 2492: 2484: 2480: 2476: 2472: 2468: 2464: 2457: 2455: 2446: 2442: 2437: 2432: 2428: 2424: 2420: 2416: 2412: 2405: 2397: 2393: 2389: 2385: 2381: 2377: 2373: 2366: 2358: 2345: 2337: 2330: 2322: 2316: 2308: 2304: 2300: 2296: 2292: 2288: 2284: 2280: 2273: 2265: 2259: 2251: 2247: 2243: 2239: 2235: 2231: 2227: 2223: 2216: 2208: 2204: 2200: 2196: 2192: 2188: 2184: 2180: 2176: 2172: 2168: 2161: 2151: 2143: 2139: 2135: 2131: 2127: 2123: 2119: 2115: 2108: 2100: 2087: 2079: 2072: 2070: 2062: 2060:9783319408583 2056: 2052: 2048: 2044: 2036: 2034: 2025: 2019: 2011: 2007: 2003: 1999: 1995: 1991: 1987: 1983: 1976: 1968: 1964: 1960: 1956: 1952: 1945: 1941: 1931: 1928: 1926: 1923: 1922: 1916: 1914: 1913:United States 1910: 1906: 1905:Barnett Shale 1902: 1898: 1897: 1892: 1891: 1886: 1882: 1878: 1874: 1865: 1861: 1859: 1855: 1851: 1847: 1843: 1839: 1835: 1831: 1827: 1823: 1819: 1810: 1798: 1794: 1790: 1786: 1782: 1778: 1774: 1771: 1767: 1764: 1760: 1756: 1752: 1749: 1746: 1742: 1739:, non-marine 1738: 1734: 1730: 1729: 1724: 1723: 1722:Helminthopsis 1718: 1717: 1712: 1711: 1706: 1705:trace fossils 1702: 1698: 1694: 1690: 1686: 1682: 1681: 1676: 1673: 1669: 1668: 1663: 1659: 1655: 1651: 1648: 1645: 1642: 1641: 1636: 1635:KwaZulu-Natal 1632: 1628: 1624: 1620: 1616: 1613: 1609: 1605: 1601: 1598: 1595:setting. The 1594: 1589: 1585: 1581: 1577: 1574: 1570: 1566: 1562: 1559: 1556: 1555:trace fossils 1553: 1549: 1545: 1544:KwaZulu-Natal 1541: 1537: 1533: 1529: 1525: 1521: 1517: 1513: 1509: 1505: 1501: 1497: 1494: 1493: 1487: 1483: 1481: 1477: 1474: 1471: 1467: 1463: 1459: 1454: 1453: 1452: 1444: 1440: 1436: 1432: 1428: 1424: 1420: 1416: 1412: 1408: 1404: 1400: 1396: 1393: 1390: 1389:trace fossils 1387: 1383: 1379: 1376: 1372: 1368: 1364: 1360: 1357: 1353: 1349: 1345: 1341: 1338: 1334: 1330: 1326: 1322: 1318: 1314: 1311: 1308: 1304: 1300: 1297: 1293: 1289: 1285: 1281: 1277: 1274: 1270: 1266: 1262: 1259: 1255: 1251: 1247: 1244: 1241: 1237: 1233: 1229: 1225: 1222: 1218: 1214: 1210: 1206: 1203: 1200: 1196: 1192: 1188: 1185: 1181: 1177: 1173: 1169: 1165: 1161: 1157: 1154: 1150: 1146: 1143: 1140: 1136: 1132: 1129: 1126: 1122: 1119: 1115: 1111: 1107: 1106: 1102: 1099: 1095: 1094:palaeoniscoid 1091: 1087: 1083: 1082:submarine fan 1079: 1075: 1071: 1068: 1067: 1066: 1064: 1060: 1056: 1055:submarine fan 1052: 1049: 1045: 1040: 1039: 1038: 1030: 1026: 1025: 1020: 1019: 1014: 1010: 1006: 1003: 999: 995: 991: 987: 983: 979: 975: 971: 967: 963: 960: 957: 953: 949: 945: 941: 938: 934: 930: 927: 924: 923: 918: 917:Trace fossils 914: 911: 907: 903: 899: 895: 891: 888: 885: 881: 880:conglomerates 877: 874: 870: 866: 863: 859: 856: 853: 849: 845: 841: 840:submarine fan 837: 833: 829: 825: 822: 821: 817: 812: 805: 804: 799: 795: 794: 789: 785: 781: 777: 773: 769: 768:palaeoniscoid 765: 761: 757: 753: 749: 745: 741: 737: 733: 729: 728: 724: 721: 717: 716:palaeoniscoid 713: 712: 708: 705: 701: 697: 693: 692:submarine fan 689: 685: 681: 677: 673: 669: 665: 662: 658: 655: 651: 647: 644: 643: 642: 640: 639:submarine fan 636: 632: 628: 624: 620: 616: 611: 610: 609: 604: 602: 598: 593: 591: 587: 583: 579: 569: 567: 563: 559: 555: 551: 547: 543: 539: 535: 531: 527: 523: 519: 518:Prince Albert 515: 511: 502: 493: 491: 487: 483: 479: 475: 471: 467: 463: 459: 455: 451: 448: 443: 441: 437: 433: 429: 425: 421: 417: 413: 412:submarine fan 409: 405: 401: 397: 393: 383: 381: 377: 373: 369: 365: 364:palynological 362:correlation, 361: 357: 356:stratigraphic 353: 350:in all known 349: 345: 341: 337: 333: 321: 316: 312: 308: 303: 300: 289: 278: 267: 256: 245: 241: 238: 234: 231: 227: 222: 219: 215: 212: 208: 205: 201: 197: 193: 189: 185: 181: 178: 174: 169: 166: 163: 159: 156: 153: 149: 145: 141: 137: 133: 129: 126: 122: 119: 116: 112: 106: 101: 96: 91: 86: 81: 76: 71: 66: 61: 56: 51: 45: 42:303–290  37: 36:Early Permian 33: 29: 25: 20: 6393: 6379: 6360: 6346: 6240:Andre Keyser 6215:Alfred Brown 6210:Robert Broom 6002:Nqwebasaurus 5992:Kangnasaurus 5956:Sphenosuchus 5881:Geranosaurus 5861:Dracovenator 5841:Antetonitrus 5785:Ufudocyclops 5770:Tetracynodon 5760:Scymnosaurus 5665:Lystrosaurus 5650:Kannemeyeria 5605:Elliotherium 5504:Silpholestes 5454:Moschorhinus 5434:Leontosaurus 5404:Icticephalus 5394:Euchambersia 5344:Colobodectes 5334:Choerosaurus 5299:Aelurosaurus 5278:Trochosaurus 5258:Simorhinella 5253:Scymnosaurus 5198:Glossopteris 5183:Eunotosaurus 5061:Serenichthys 5046:Diplacanthus 5026:Africanaspis 4770:Karoo-Ferrar 4539: 4185:(aka koppie) 3970:Owambo Basin 3955:Ogaden Basin 3945:Murzuq Basin 3915:Douala Basin 3890:Angola Basin 3862:Urema Valley 3847:Red Sea Rift 3842:Muglad Basin 3812:Benue Trough 3618:Congo Craton 3581:Rovuma Plate 3565:Somali Plate 3478: 3474: 3468: 3459: 3442: 3432: 3407:. Retrieved 3403: 3393: 3385: 3381: 3376: 3359: 3349: 3339: 3327: 3313:cite journal 3280: 3276: 3270: 3250: 3243: 3233: 3223: 3213: 3203: 3196: 3163: 3159: 3153: 3139:cite journal 3112: 3108: 3098: 3073: 3069: 3063: 3036: 3032: 3022: 2989: 2985: 2979: 2958:cite journal 2943: 2894: 2890: 2884: 2874: 2839: 2835: 2825: 2811:(1): 27–40. 2808: 2804: 2794: 2780:cite journal 2755: 2751: 2744: 2711: 2707: 2697: 2677: 2670: 2653: 2649: 2639: 2622: 2599: 2592: 2584: 2579: 2565:cite journal 2532: 2528: 2522: 2505: 2501: 2491: 2466: 2462: 2418: 2414: 2404: 2379: 2375: 2365: 2344:cite journal 2329: 2315:cite journal 2282: 2278: 2272: 2258:cite journal 2225: 2221: 2215: 2174: 2170: 2160: 2150: 2117: 2113: 2107: 2086:cite journal 2042: 2018:cite journal 1985: 1981: 1975: 1958: 1954: 1944: 1896:Glossopteris 1894: 1888: 1873:Paraná Basin 1870: 1815: 1787:and shallow 1750: 1726: 1720: 1714: 1708: 1707:, namely of 1701:palynomorphs 1678: 1665: 1640:Glossopteris 1638: 1597:carbonaceous 1573:carbonaceous 1560: 1552:invertebrate 1540:sub-tropical 1500:carbonaceous 1495: 1455: 1450: 1449: 1448: 1437:or within a 1419:wave ripples 1394: 1386:invertebrate 1375:shelf marine 1337:carbonaceous 1312: 1296:Invertebrate 1245: 1204: 1144: 1130: 1103: 1096:fishes, and 1086:invertebrate 1069: 1041: 1036: 1035: 1034: 1022: 1016: 961: 928: 922:Glossopteris 920: 889: 862:argillaceous 857: 830:, dark grey 823: 815: 801: 791: 754:and contain 752:carbonaceous 725: 718:fishes, and 709: 696:invertebrate 661:carbonaceous 645: 612: 607: 606: 605: 594: 586:South Africa 575: 550:Johannesburg 538:Orange River 507: 444: 389: 331: 329: 305:Type section 255:South Africa 237:Eastern Cape 143: 135: 127: 6070:Homo naledi 6058:Pleistocene 6007:Paranthodon 5982:Algoasaurus 5961:Tritheledon 5946:Pulanesaura 5876:Fabrosaurus 5851:Coelophysis 5799:Assemblages 5780:Trirachodon 5775:Thrinaxodon 5725:Procolophon 5710:Pentasaurus 5695:Noteosuchus 5685:Micropholis 5660:Lydekkerina 5600:Dinanomodon 5590:Cynognathus 5523:Assemblages 5489:Procolophon 5474:Pristerodon 5469:Polycynodon 5424:Ictidostoma 5419:Ictidodraco 5384:Eohyosaurus 5379:Eodicynodon 5374:Dinanomodon 5324:Broomistega 5193:Glanosuchus 5178:Endothiodon 5163:Dinanomodon 5128:Bulbasaurus 5056:Priscomyzon 4780:Earthquakes 4765:Drakensberg 4720:Pilanesberg 4644:Algoa Basin 4612:Algoa Group 4535:Dwyka Group 4438:Cretaceous 4417:Ordovician 4396:Dwyka Group 4356:Dwyka Group 4068:Drakensberg 3985:Sirte Basin 3940:Kufra Basin 3930:Gabon Basin 3925:Karoo Basin 3910:Congo Basin 3857:Atbara rift 3837:Melut Basin 3802:Anza trough 3663:Shear zones 3388:, pp.59-83. 3344:pp.379-390. 3166:: 217–232. 3115:: 256–265. 2879:pp.117-125. 2758:: 104–116. 2535:(1): 3–15. 2155:pp.103-111. 2120:: 217–232. 1804:Correlation 1763:bioturbated 1735:, possible 1697:fossil wood 1685:cordaitales 1584:bioturbated 1565:lithofacies 1542:climate of 1307:fossil logs 1288:deformation 1276:concretions 1224:concretions 1189:, and also 1121:concretions 1048:basin floor 1005:delta-plain 876:concretions 623:basin-floor 542:Petrusville 530:Port Alfred 526:Grahamstown 522:Jansenville 490:Karoo Basin 478:Karoo Basin 472:. Flexural 470:Karoo Basin 416:continental 404:Depocenters 344:Dwyka Group 165:Dwyka Group 6417:Ecca Group 6411:Categories 6172:Geologists 6101:Planolites 6065:Boskop Man 5970:Cretaceous 5936:Pegomastax 5921:Lycorhinus 5906:Ledumahadi 5896:Gyposaurus 5846:Arcusaurus 5765:Shansiodon 5750:Regisaurus 5735:Prolacerta 5675:Mesosuchus 5635:Galesaurus 5595:Diademodon 5585:Bolotridon 5389:Emyduranus 5364:Cynosaurus 5339:Clelandina 5228:Mesosaurus 5223:Lycosuchus 5188:Galechirus 5168:Dinogorgon 5148:Cynosaurus 4995:Notiodella 4988:Ordovician 4882:Kimberlite 4843:Meteorites 4734:Diatremes 4540:Ecca Group 4421:Soom Shale 4207:Mount Mabu 4192:Anti-Atlas 4183:Inselbergs 3905:Chad Basin 3409:2018-12-13 2080:: 413–429. 1936:References 1890:Mesosaurus 1816:The lower 1781:lacustrine 1728:planolites 1693:ginkgoales 1588:sandstones 1407:sandstones 1403:anticlines 1348:rhythmites 1317:Rhythmites 1292:load casts 1284:calcareous 1273:calcareous 1254:sandstones 1250:sandstones 1232:sandstones 1221:Calcareous 1217:siltstones 1184:phosphatic 1180:calcareous 1168:siltstones 1164:sandstones 1156:sandstones 1098:coprolites 1063:Depocenter 1031:megacycle. 986:siltstones 982:sandstones 978:sandstones 940:rhythmites 873:calcareous 852:deposition 798:mesosaurid 770:fish, and 720:coprolites 704:chimaeroid 668:rhythmites 635:Depocenter 514:Laingsburg 510:Sutherland 458:subduction 454:orogenesis 392:deposition 386:Background 382:) in age. 358:position, 332:Ecca Group 22:Ecca Group 6049:Nummulite 6028:Nummulite 6021:Paleogene 5987:Baculites 5705:Orosaurus 5690:Myosaurus 5509:Tamboeria 5459:Paliguana 5444:Lycideops 5414:Ictidodon 5369:Diictodon 5349:Compsodon 5309:Basilodon 5203:Hofmeyria 5158:Diictodon 5123:Basilodon 5108:Abdalodon 5087:Dadoxylon 5071:Umzantsia 5010:Soomaspis 5005:Promissum 4708:Volcanism 4694:Witteberg 4575:Triassic 4477:Jurassic 4367:Devonian 4346:Paleozoic 4227:Zuma Rock 4222:Wase Rock 3503:1342-937X 3451:0078-8554 3368:0078-8554 3305:0031-0182 3188:0037-0738 3131:1876-6102 3090:131561248 3055:0024-4082 3014:0899-5362 2919:1476-4687 2866:2391-5447 2817:1996-8590 2772:0264-8172 2736:1527-1404 2662:1996-8590 2631:0078-8554 2557:1464-343X 2514:1996-8590 2483:0166-5162 2445:135113186 2307:1464-343X 2250:1464-343X 2199:1365-2117 2142:0037-0738 2010:0899-5362 1967:1996-8590 1832:found in 1793:pelecypod 1770:sandstone 1766:siltstone 1710:Skolithos 1680:Annularia 1672:horsetail 1586:immature 1520:sandstone 1512:siltstone 1464:-bearing 1431:siltstone 1427:sandstone 1423:sandstone 1411:siltstone 1399:synclines 1356:sandstone 1333:claystone 1329:siltstone 1325:siltstone 1321:sandstone 1280:sandstone 1269:siltstone 1265:sandstone 1261:rhythmite 1240:siltstone 1209:sandstone 1153:greywacke 1118:carbonate 1114:siltstone 1110:sandstone 1024:Skolithos 1013:sandstone 974:rhythmite 970:siltstone 948:sandstone 944:siltstone 894:sandstone 884:mudstones 828:siliceous 814:A fossil 784:sea floor 772:arthropod 684:siltstone 680:sandstone 650:micaceous 597:Whitehill 534:Britstown 486:forebulge 480:into the 474:tectonics 462:Gondwanan 430:-bearing 310:Named for 214:Quartzite 192:siltstone 188:claystone 171:Lithology 151:Underlies 124:Sub-units 6395:Glossary 6381:Category 5891:Gryponyx 5866:Eocursor 5831:Aardonyx 5824:Jurassic 5568:Triassic 5283:Youngina 5233:Moschops 5066:Tutusius 5036:Bainella 5019:Devonian 4738:Big Hole 4605:Cenozoic 4432:Mesozoic 4382:Permian 3920:El Djouf 3418:cite web 2927:28052054 2207:56420970 1919:See also 1846:Khorixas 1842:Zimbabwe 1838:Botswana 1785:lagoonal 1741:bivalves 1689:conifers 1677:such as 1664:such as 1658:lycopods 1627:stagnant 1617:. These 1569:mudstone 1532:borehole 1528:outcrops 1516:mudstone 1445:setting. 1415:mudstone 1367:mudrocks 1344:mudrocks 1335:layers, 1018:Cruziana 958:setting. 915:system. 832:mudstone 676:arenites 590:mudstone 546:Hopetown 540:between 482:foredeep 447:retroarc 376:Asselian 352:outcrops 299:Zimbabwe 288:Botswana 266:Eswatini 224:Location 200:dolomite 184:mudstone 161:Overlies 6330:Swazian 6037:Neogene 5640:Howesia 5101:Permian 3721:Orogens 3605:shields 3601:Cratons 3483:Bibcode 3285:Bibcode 3168:Bibcode 2994:Bibcode 2935:4455946 2899:Bibcode 2844:Bibcode 2716:Bibcode 2537:Bibcode 2423:Bibcode 2384:Bibcode 2376:Geology 2287:Bibcode 2230:Bibcode 2179:Bibcode 2122:Bibcode 1990:Bibcode 1911:of the 1885:Uruguay 1850:Namibia 1834:Namibia 1826:Namibia 1797:bivalve 1795:marine 1789:coastal 1733:insects 1731:, rare 1695:, rare 1675:species 1660:, rare 1631:Nongoma 1510:rocks, 1470:deltaic 1466:fluvial 1352:mudrock 1303:burrows 1258:clastic 1090:fossils 1088:marine 1051:pelagic 1029:deltaic 1002:fluvial 937:clastic 910:fluvial 732:Mudrock 700:fossils 698:marine 554:Vryheid 440:peatbog 436:deltaic 432:fluvial 408:pelagic 380:Roadian 277:Namibia 243:Country 233:Western 176:Primary 30:: Late 5931:Ngwevu 3895:Aoukar 3550:Plates 3501:  3449:  3366:  3303:  3258:  3186:  3129:  3088:  3053:  3012:  2933:  2925:  2917:  2891:Nature 2864:  2815:  2770:  2734:  2685:  2660:  2629:  2555:  2512:  2481:  2443:  2305:  2248:  2205:  2197:  2140:  2057:  2008:  1965:  1881:Brazil 1877:Brazil 1840:, and 1773:lenses 1650:floras 1644:fossil 1625:where 1619:swamps 1615:swamps 1604:anoxic 1600:shales 1548:fossil 1524:facies 1514:, and 1506:-rich 1480:facies 1458:facies 1378:facies 1371:shales 1342:, and 1340:shales 1252:. The 1228:clasts 1187:lenses 1078:facies 1044:facies 980:. The 952:facies 933:shales 865:shales 780:anoxic 776:shales 760:pyrite 756:lenses 748:shales 742:. The 740:facies 702:, the 688:debris 672:Wackes 666:, and 631:facies 619:marine 615:facies 601:facies 582:facies 558:Durban 438:, and 420:facies 400:facies 396:marine 340:Africa 296:  285:  274:  263:  252:  235:& 229:Region 218:pyrite 6310:Other 6089:Other 3789:Rifts 3238:2013. 3228:2010. 3218:2005. 3086:S2CID 2931:S2CID 2441:S2CID 2203:S2CID 1759:shale 1662:ferns 1593:delta 1576:shale 1536:erode 1508:shale 1476:swamp 1443:beach 1439:delta 1382:delta 1363:Tuffs 1359:wacke 1236:shale 1213:shale 1176:shale 1160:shale 1149:shale 1141:Bed”. 1139:Chert 1135:chert 1074:chert 1059:shelf 1042:This 998:delta 966:shale 956:delta 913:delta 906:delta 898:shale 764:chert 744:shale 736:shale 664:shale 657:shale 654:silty 627:shelf 613:This 552:past 424:beach 210:Other 196:chert 180:Shale 3603:and 3499:ISSN 3447:ISSN 3424:link 3364:ISSN 3319:link 3301:ISSN 3256:ISBN 3184:ISSN 3145:link 3127:ISSN 3051:ISSN 3010:ISSN 2971:help 2923:PMID 2915:ISSN 2862:ISSN 2813:ISSN 2786:link 2768:ISSN 2732:ISSN 2683:ISBN 2658:ISSN 2627:ISSN 2571:link 2553:ISSN 2510:ISSN 2479:ISSN 2357:help 2321:link 2303:ISSN 2264:link 2246:ISSN 2195:ISSN 2138:ISSN 2099:help 2055:ISBN 2024:link 2006:ISSN 1963:ISSN 1907:and 1893:and 1883:and 1755:silt 1745:coal 1725:and 1647:coal 1612:peat 1608:coal 1591:pro- 1504:silt 1502:and 1473:peat 1462:coal 1429:and 1401:and 1369:and 1350:and 1301:and 1238:and 1215:and 1199:tuff 1182:and 1172:tuff 1125:Tuff 1112:and 1021:and 984:and 869:Tuff 844:tuff 836:tuff 762:and 750:are 734:and 682:and 674:and 544:and 428:Coal 330:The 313:Ecca 204:coal 114:Type 50:Preęž’ 3491:doi 3293:doi 3176:doi 3117:doi 3078:doi 3041:doi 3037:146 3002:doi 2907:doi 2895:541 2852:doi 2760:doi 2724:doi 2545:doi 2471:doi 2431:doi 2392:doi 2295:doi 2238:doi 2187:doi 2130:doi 2047:doi 1998:doi 1875:of 1848:in 1783:to 1768:or 1441:or 1327:or 758:of 652:or 6413:: 3497:. 3489:. 3477:. 3445:. 3441:. 3420:}} 3416:{{ 3402:. 3386:16 3384:, 3362:. 3358:. 3315:}} 3311:{{ 3299:. 3291:. 3281:36 3279:. 3182:. 3174:. 3164:19 3162:. 3141:}} 3137:{{ 3125:. 3113:40 3111:. 3107:. 3084:. 3074:30 3072:. 3049:. 3035:. 3031:. 3008:. 3000:. 2990:10 2988:. 2962:: 2960:}} 2956:{{ 2929:. 2921:. 2913:. 2905:. 2893:. 2860:. 2850:. 2840:11 2838:. 2834:. 2809:84 2807:. 2803:. 2782:}} 2778:{{ 2766:. 2756:41 2754:. 2730:. 2722:. 2712:80 2710:. 2706:. 2654:97 2652:. 2648:. 2625:. 2621:. 2609:^ 2567:}} 2563:{{ 2551:. 2543:. 2533:23 2531:. 2506:95 2504:. 2500:. 2477:. 2467:12 2465:. 2453:^ 2439:. 2429:. 2417:. 2413:. 2390:. 2380:25 2378:. 2374:. 2348:: 2346:}} 2342:{{ 2317:}} 2313:{{ 2301:. 2293:. 2283:43 2281:. 2260:}} 2256:{{ 2244:. 2236:. 2226:35 2224:. 2201:. 2193:. 2185:. 2175:10 2173:. 2169:. 2136:. 2128:. 2118:19 2116:. 2090:: 2088:}} 2084:{{ 2068:^ 2053:, 2032:^ 2020:}} 2016:{{ 2004:. 1996:. 1986:16 1984:. 1959:81 1957:. 1953:. 1915:. 1856:. 1836:, 1719:, 1713:, 1691:, 1687:, 1683:, 1670:, 1656:, 1633:, 1571:, 1315:: 1219:. 1166:, 1123:. 1092:, 1007:. 972:, 968:, 867:. 800:, 730:: 714:, 670:. 659:, 560:, 556:, 524:, 520:, 516:, 492:. 484:, 410:, 378:- 216:, 202:, 198:, 194:, 190:, 186:, 182:, 100:Pg 44:Ma 4266:e 4259:t 4252:v 3536:e 3529:t 3522:v 3505:. 3493:: 3485:: 3479:7 3453:. 3426:) 3412:. 3370:. 3321:) 3307:. 3295:: 3287:: 3264:. 3190:. 3178:: 3170:: 3147:) 3133:. 3119:: 3092:. 3080:: 3057:. 3043:: 3016:. 3004:: 2996:: 2973:) 2969:( 2952:. 2937:. 2909:: 2901:: 2868:. 2854:: 2846:: 2819:. 2788:) 2774:. 2762:: 2738:. 2726:: 2718:: 2691:. 2664:. 2633:. 2573:) 2559:. 2547:: 2539:: 2516:. 2485:. 2473:: 2447:. 2433:: 2425:: 2419:9 2398:. 2394:: 2386:: 2359:) 2355:( 2338:. 2323:) 2309:. 2297:: 2289:: 2266:) 2252:. 2240:: 2232:: 2209:. 2189:: 2181:: 2144:. 2132:: 2124:: 2101:) 2097:( 2049:: 2026:) 2012:. 2000:: 1992:: 1969:. 1468:- 1331:/ 1323:/ 1267:/ 854:. 434:- 374:( 105:N 95:K 90:J 85:T 80:P 75:C 70:D 65:S 60:O 55:ęž’ 39:~ 34:-

Index

Stratigraphic range
Late Carboniferous
Early Permian
Ma
Preęž’
ęž’
O
S
D
C
P
T
J
K
Pg
N
Geologic group
Whitehill Formation
Whitehill Formation
Beaufort Group
Dwyka Group
Shale
mudstone
claystone
siltstone
chert
dolomite
coal
Quartzite
pyrite

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