Elliot Formation Explained

Elliot Formation
Type:Geological formation
Age:Norian-Pliensbachian
~
Period:Sinemurian
Prilithology:Mudstone, sandstone
Otherlithology:Siltstone, conglomerate
Namedfor:Elliot, Eastern Cape
Region:Eastern Cape, Free State, Mafeteng, Maseru, Quthing, Qacha's Nek & Mohale's Hoek
Country:
Coordinates:-30.5°N 27.4°W
Paleocoordinates:-44.1°N -1.9°W
Unitof:Stormberg Group
Subunits:Upper Elliot, Lower Elliot
Underlies:Clarens Formation
Overlies:Molteno Formation
Thickness:up to 500m (1,600feet)

The Elliot Formation is a geological formation and forms part of the Stormberg Group, the uppermost geological group that comprises the greater Karoo Supergroup. Outcrops of the Elliot Formation have been found in the northern Eastern Cape, southern Free State, and in the eastern KwaZulu-Natal provinces of South Africa. Outcrops and exposures are also found in several localities in Lesotho such as Qacha's Neck, Hill Top, Quthing, and near the capital, Maseru. The Elliot Formation is further divided into the lower (LEF) and upper (UEF) Elliot formations to differentiate significant sedimentological differences between these layers. The LEF is dominantly Late Triassic (Norian-Hettangian) in age while the UEF is mainly Early Jurassic (Sinemurian-Pliensbachian) and is tentatively regarded to preserve a continental record of the Triassic-Jurassic boundary in southern Africa.[1] This geological formation is named after the town of Elliot in the Eastern Cape, and its stratotype locality is located on the Barkly Pass, 9 km north of the town.[2] [3] [4]

Geology

The Elliot Formation unconformably overlies the Molteno Formation and is conformably overlain by the Clarens Formation. Due to the reddish colour of the rocks, the Elliot Formation is colloquially referred to as the “Red Beds” in older geologic literature.

The Elliot Formation is dominated by mudstones and siltstones that can be finely laminated. However, the internal structures in the mudstones are often not visible due to locally poor laminations. Calcareous nodules are also found in the mudstone layers and become more frequent up section into the UEF. The mudstones range in colour from greyish purple red in the LEF and turn a more brick red colour with more mature palaeosols in the UEF. Localized intraformational pebble conglomerates that comprise intrabasinal clasts that comprise mud chips, quartzite pebbles, pedogenic nodules, and fossil bone fragments only occur in the UEF. The lower and upper Elliot formations both contain sandstones but they vary in their internal geometries. The sandstones of the LEF mainly comprise laterally accreting channel deposits that are multi-story and contain trough, low angle, and planar, cross-bedding. Ripple cross laminations with good horizontal lamination are also present. In the UEF, sandstone beds are single story and mainly reflect downstream accretion channel geometries and are more tabular in appearance. Common internal sedimentary structures of UEF sandstones are planar, low angle cross-bedding, horizontal and ripple-cross laminations.

The LEF was deposited in a fluvio-lacustrine environment where rivers were more perennial and formed meandering channel geometries, as evidenced by the presence of lateral accretion. However, this depositional environment changed at the onset of the UEF deposits where evidence of shallower river channels, longer periods of floodplain stasis (mature palaeosols) and flash flood events (pedogenic nodule conglomerates) shows that the climate became more arid.[5] [6] [7] [8]

Correlation

The Elliot Formation is currently considered to correlate chronostratigraphically with geological formations of the Bodibeng Sandstone of the Tuli Basin in Botswana, the Omingonde Formation of the Etjo Basin in Namibia, and the Chinle Formation of the Colorado Plateau in Utah, United States.[9] [10] [11] [12] [13] [14]

Paleontology

The Elliot Formation is well known for its diverse dinosaur fossils. The most common dinosaur species is of the sauropodomorph species Massospondylus carinatus.[15] [16] Other species include Blikanasaurus cromptoni, Aardonyx celestae, Euskelosaurus browni, Antetonitrus ingenipes, Pulanesaura eocollum, and the largest sauropodomorph yet found, Ledumahadi mafube.[17] [18] [19] [20] [21] [22] [23] [24] Fossilised Massospondylus eggs, some with the fossilized remains of embryos intact, have been recovered from UEF deposits in the Golden Gate Highlands National Park.[25] [26] Euskelosaurus fossils are more common in the LEF while Massospondylus are only found in the UEF. The basal ornithischian dinosaurs, Heterodontosaurus tucki, Lesothosaurus diagnosticus, Abrictosaurus consors, and Lycorhinus angustidens have also been recovered from the UEF.[27] [28] In addition this formation has yielded various crocodylomorph species,[29] namely Litargosuchus leptorhynchus, Sphenosuchus acutus and Orthosuchus stormbergi.[30] [31] [32] [33] A large theropod dinosaur, Dracovenator regenti, has been found in the UEF.[34] Synapsids from the formation include the dicynodont Pentasaurus goggai[35] the tritheledontid cynodont Elliotherium kersteni[36] [37] and the mammaliaform Megazostrodon rudnerae.[38] More recent vertebrate fossil finds near the town Qhemegha in the Eastern Cape have yielded possible fossil material of a poposauroid pseudosuchian. The mudstones of the LEF sometimes yield petrified wood, fossil plant matter, crustaceans, fishes, and turtles while the sandstones of the upper Elliot Formation more often contain various trace fossils. These include vertebrate trackways of basal ornithischian dinosaurs found in the Leribe, Mafeteng, and Mohales Hoek Districts of Lesotho. Possible trackways of the dicynodont Pentasaurus have been found on Morobong Hill in the Mohales Hoek District of Lesotho.[39] [40] [41] [42]

Dinosaurs

Ornithischians

Ornithischians of the Elliot Formation
GenusSpeciesLocationStratigraphyNotesImages
AbrictosaurusA. consors
  • Upper Elliot
A heterodontosaurid, formerly species of Lycorhinus
EocursorE. parvus
  • Upper Elliot
A basal ornithischian
FabrosaurusF. australis
  • Upper Elliot
A basal ornithischian, nomen dubium
HeterodontosaurusH. tucki
  • Upper Elliot
A heterodontosaurid
LesothosaurusL. diagnosticus
  • Upper Elliot
A basal neornithischian or thyreophoran, formerly species of Fabrosaurus
LycorhinusL. angustidens
  • Upper Elliot
A heterodontosaurid
PegomastaxP. africana
  • Upper Elliot
A heterodontosaurid

Sauropodomorphs

Sauropodomorphs of the Elliot Formation
GenusSpeciesLocationStratigraphyNotesImages
AardonyxA. celestae
  • Upper Elliot
A derived sauropodomorph
AntetonitrusA. ingenipes
  • Upper Elliot
A derived sauropodomorph or basal sauropod
ArcusaurusA. pereirabdalorum
  • Spion Kop Heelbo
  • Upper Elliot
A basal sauropodomorph, known from juveniles
BlikanasaurusB. cromptoni
  • Blikana Mountain
  • Lower Elliot
A derived sauropodomorph or basal sauropod
EucnemesaurusE. fortis
  • Lower Elliot
A possible riojasaurid
E. entaxonis
EuskelosaurusE. browni
  • Lower Elliot
A plateosaurid, potentially dubious
GryponyxG. africanus
  • Upper Elliot
A massospondylid, potentially dubious
IgnavusaurusI. rachelis
  • Upper Elliot
A massospondylid, known from a juvenile, potential synonym of Massospondylus
KholumolumoK. ellenbergerorum
  • Lower Elliot
A basal sauropodiform
LedumahadiL. mafubeA derived sauropodomorph or basal sauropod, largest in the formation
MassospondylusM. carinatus
  • Upper Elliot
A massospondylid, most common fossil found
M. kaalae
  • Upper Elliot
A massospondylid, differs from M. carinatus in cranial features
MelanorosaurusM. readi
  • Thaba 'Nyama
  • Lower Elliot
A derived sauropodomorph
MeroktenosM. thabanensis
  • Thabana Morena
  • Lower Elliot
A derived sauropodomorph, formerly a species of Melanorosaurus
PlateosauravusP. cullingworthi
  • Lower Elliot
A basal sauropodomorph, formerly specimens of Euskelosaurus
PulanesauraP. eocollum
  • Upper Elliot
A derived sauropodomorph or basal sauropod
SefapanosaurusS. zastronensis
  • Upper or Lower Elliot
A derived sauropodomorph

Theropods

Theropods of the Elliot Formation
GenusSpeciesLocationStratigraphyNotesImages
DracovenatorD. regenti
  • Upper Drumbo Farm
  • Upper Elliot
A dilophosaurid
MegapnosaurusM. rhodesiensis
  • Syntarsus site.
  • Upper Elliot
A coelophysid

Suchians

Crocodylomorphs

Crocodylomorphs of the Elliot Formation
GenusSpeciesLocationStratigraphyNotesImages
BasutodonB. ferox
  • Lower Elliot
A dubious suchian
LitargosuchusL. leptorhynchus
  • Eagles Crag Farm
  • Upper Elliot
A basal crocodylomorph
OrthosuchusO. stormbergi
  • Upper Elliot
A possible protosuchid
Rauisuchian
  • Lower Elliot
A indeterminate large "Rauisuchian"
SphenosuchusS. acutus
  • Upper Elliot
A large basal crocodylomorph

Synapsids

Synapsids of the Elliot Formation
GenusSpeciesLocationStratigraphyNotesImages
ElliotheriumE. kersteni
  • Lower Elliot
A tritheledontid cynodont
MegazostrodonM. rudnerae
  • Upper Elliot
A megazostrodontid cynodont
PentasaurusP. goggai
  • Lower Elliot
A stahleckeriid dicynodont
ScalenodontoidesS. macrodontes
  • Lower Elliot
A very large traversodontid cynodont

Notes and References

  1. Bordy . Emese M. . Abrahams . Miengah . Sharman . Glenn R. . Viglietti . Pia A. . Benson . Roger B.J. . McPhee . Blair W. . Barrett . Paul M. . Sciscio . Lara . Condon . Daniel . Mundil . Roland . Rademan . Zandri . April 2020 . A chronostratigraphic framework for the upper Stormberg Group: Implications for the Triassic-Jurassic boundary in southern Africa . Earth-Science Reviews . 203 . 103120 . 10.1016/j.earscirev.2020.103120 . 2020ESRv..20303120B . 213646670 . 0012-8252.
  2. 2004-03-01. Fluvial style variations in the Late Triassic–Early Jurassic Elliot formation, main Karoo Basin, South Africa. Journal of African Earth Sciences. en. 38. 4. 383–400. 10.1016/j.jafrearsci.2004.02.004. 1464-343X. Bordy. Emese M.. John Hancox. P.. Rubidge. Bruce S.. 2004JAfES..38..383B.
  3. 2004-09-01. A description of the sedimentology and palaeontology of the Late Triassic–Early Jurassic Elliot Formation in Lesotho. WIReDSpace Wits. en. 0078-8554.
  4. 2015-09-01. South African Journal of Geology. en. 118. 3. 311–316. 10.2113/gssajg.118.3.311. 1012-0750. Bordy. E.M.. Lithostratigraphy of the Elliot Formation (Karoo Supergroup), South Africa. Eriksson. P.. 2015SAJG..118..311B . 2263/55739. free.
  5. 2009-09-01. Tectonic evolution of the Cape and Karoo basins of South Africa. Marine and Petroleum Geology. en. 26. 8. 1379–1412. 10.1016/j.marpetgeo.2009.01.022. 0264-8172. Tankard. Anthony. Welsink. Herman. Aukes. Peter. Newton. Robert. Stettler. Edgar. 2009MarPG..26.1379T .
  6. 1980-01-01. Meander channel, point bar, crevasse splay and aeolian deposits from the Elliot Formation in Barkly Pass, North-eastern Cape. South African Journal of Geology. en. 83. 1. 1012-0750.
  7. 2015-09-01. South African Journal of Geology. en. 118. 3. 311–316. 10.2113/gssajg.118.3.311. 1012-0750. Bordy. E.M.. Lithostratigraphy of the Elliot Formation (Karoo Supergroup), South Africa. Eriksson. P.. 2015SAJG..118..311B . 2263/55739. free.
  8. 2017-11-01. Magnetostratigraphy across the Triassic-Jurassic boundary in the main Karoo Basin. Gondwana Research. en. 51. 177–192. 10.1016/j.gr.2017.07.009. 1342-937X. Sciscio. Lara. De Kock. Michiel. Bordy. Emese. Knoll. Fabien. 2017GondR..51..177S. 10261/338607. free.
  9. Attridge. J.. Crompton. A. W.. Jenkins. Farish A.. June 1985. The Southern African Liassic prosauropodMassospondylusdiscovered in North America. Journal of Vertebrate Paleontology. en. 5. 2. 128–132. 10.1080/02724634.1985.10011850. 1985JVPal...5..128A . 0272-4634.
  10. September 2015. South African Journal of Geology. en. 118. 3. 311–316. 10.2113/gssajg.118.3.311. 1012-0750. 2263/55739. Lithostratigraphy of the Elliot Formation (Karoo Supergroup), South Africa. Eriksson. P.. Bordy. E. M.. 2015SAJG..118..311B . free.
  11. 2002-06-01. Changing Fluvial Environments and Vertebrate Taphonomy in Response to Climatic Drying in a Mid-Triassic Rift Valley Fill: The Omingonde Formation (Karoo Supergroup) of Central Namibia. PALAIOS. en. 17. 3. 249–267. 10.1669/0883-1351(2002)017<0249:CFEAVT>2.0.CO;2. 0883-1351. Smith. R. M.H.. Swart. R.. 2002Palai..17..249S. 130316395 .
  12. Abdala. Fernando. Smith. Roger M. H.. 2009-09-12. A Middle Triassic cynodont fauna from Namibia and its implications for the biogeography of Gondwana. Journal of Vertebrate Paleontology. en. 29. 3. 837–851. 10.1671/039.029.0303. 2009JVPal..29..837A . 129096876. 0272-4634.
  13. Walker. A. D.. 1990-10-29. A revision of Sphenosuchus acutus Haughton, a crocodylomorph reptile from the Elliot Formation (late Triassic or early Jurassic) of South Africa. Phil. Trans. R. Soc. Lond. B. en. 330. 1256. 1–120. 10.1098/rstb.1990.0185. 0962-8436.
  14. 1982-12-01. Triassic environments, climates and reptile evolution. Palaeogeography, Palaeoclimatology, Palaeoecology. en. 40. 4. 361–379. 10.1016/0031-0182(82)90034-7. 0031-0182. Tucker. Maurice E.. Benton. Michael J.. 1982PPP....40..361T. free.
  15. Sues, H.D., Reisz, R.R., Hinic, S. and Raath, M.A., 2004. On the skull of Massospondylus carinatus Owen, 1854 (Dinosauria: Sauropodomorpha) from the Elliot and Clarens formations (Lower Jurassic) of South Africa. Annals of Carnegie Museum, 73(4), pp.239–257.
  16. Web site: Bone histology and growth trajectory of the prosauropod dinosaur Massospondylus carinatus Owen Request PDF. Chinsamy. Anusuya. ResearchGate. en. 2018-11-14.
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  18. Yates. Adam M.. 2003. A definite prosauropod dinosaur from the Lower Elliot Formation (Norian: Upper Triassic) of South Africa. Palaeontologia Africana. en. 0078-8554.
  19. Barrett. Paul M.. 2004-09-01. Sauropodomorph dinosaur diversity in the upper Elliot Formation (Massospondylus range zone: Lower Jurassic) of South Africa: research letter. South African Journal of Science. en. 100. 9–10. 0038-2353.
  20. McPhee. Blair. Bordy. Emese. Sciscio. Lara. Choiniere. Jonah. 2017. The sauropodomorph biostratigraphy of the Elliot Formation of southern Africa: Tracking the evolution of Sauropodomorpha across the Triassic–Jurassic boundary. Acta Palaeontologica Polonica. EN. 62. 3. 10.4202/app.00377.2017. 0567-7920. free.
  21. First record of a sauropod dinosaur from the upper Elliot Formation (Early Jurassic) of South Africa: research letter . Hancox . P. John . Rubidge . Bruce S. . Yates . Adam M. . South African Journal of Science . 100 . 9 . 1 September 2004 . 504–506.
  22. Blair W. . McPhee . Adam M. . Yates . Jonah N. . Choiniere . Fernando . Abdala . 2014-04-25 . The complete anatomy and phylogenetic relationships of Antetonitrus ingenipes (Sauropodiformes, Dinosauria): implications for the origins of Sauropoda . Zoological Journal of the Linnean Society . en . 171 . 1 . 10.1111/zoj12127 . 1096-3642. free .
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  28. October 2005. The 'fabrosaurid' ornithischian dinosaurs of the Upper Elliot Formation (Lower Jurassic) of South Africa and Lesotho. Zoological Journal of the Linnean Society. en. 145. 2. 175–218. 10.1111/j.1096-3642.2005.00182.x. 1096-3642. Butler. Richard J.. free.
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  30. Walker. A. D.. 1990-10-29. A revision of Sphenosuchus acutus Haughton, a crocodylomorph reptile from the Elliot Formation (late Triassic or early Jurassic) of South Africa. Phil. Trans. R. Soc. Lond. B. en. 330. 1256. 1–120. 10.1098/rstb.1990.0185. 0962-8436.
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  32. Nash, D.S., 1975. The morphology and relationships of a crocodilian, Orthosuchus stormbergi, from the Upper Triassic of Lesotho. South African Museum.
  33. Dollman. K. N.. Viglietti. P. A.. Choiniere. J. N.. 2017-10-12. A new specimen of Orthosuchus stormbergi (Nash 1968) and a review of the distribution of Southern African Lower Jurassic crocodylomorphs. Historical Biology. 31. 5. en. 653–664. 10.1080/08912963.2017.1387110. 134134524. 0891-2963.
  34. Web site: A new theropod dinosaur from the Early Jurassic of South Africa and its implication for the early evolution of theropods Request PDF. ResearchGate. en. 2018-11-16.
  35. F.. Kammerer, Christian. 2018. The first skeletal evidence of a dicynodont from the lower Elliot Formation of South Africa. Palaeontologia Africana. en. 2410-4418.
  36. March 2006. Elliotherium Kersteni, A New Tritheledontid from the Lower Elliot Formation (Upper Triassic) of South Africa. Journal of Paleontology. en. 80. 2. 333–342. 10.1666/0022-3360(2006)080[0333:EKANTF]2.0.CO;2. 0022-3360. 10.1.1.557.9156. Hancox. P. J.. Sidor. C. A.. 130003909.
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  39. Late Triassic ecosystems of the Molteno Lower Elliot biome of southern Africa. J.M. . Anderson . H.M. . Anderson . A.R.I. . Cruickshank . Palaeontology . 41 . 3 . 387–421 . 1998.
  40. 1997-06-01. Sedimentology and vertebrate taphonomy of the Tritylodon Acme Zone: a reworked palaeosol in the Lower Jurassic Elliot Formation, Karoo Supergroup, South Africa. Palaeogeography, Palaeoclimatology, Palaeoecology. en. 131. 1–2. 29–50. 10.1016/S0031-0182(96)00143-5. 0031-0182. Smith. R.. Kitching. J.. 1997PPP...131...29S.
  41. Knoll. Fabien. January 2005. The tetrapod fauna of the Upper Elliot and Clarens formations in the main Karoo Basin (South Africa and Lesotho). Bulletin de la Société Géologique de France. en. 176. 1. 81–91. 10.2113/176.1.81. 0037-9409.
  42. December 2015 . Sciscio . Lara . Position of the Triassic-Jurassic boundary in South Africa and Lesotho: a multidisciplinary approach aimed at improving the chronostratigraphy and biostratigraphy of the Elliot Formation, Stormberg Group. University of Cape Town . OpenUCT.