Elliot Formation

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Elliot Formation
Stratigraphic range: Norian-Pliensbachian
~220–190  Ma
Elliot Formation Caves in 'Matalane Valley, Leribe, Lesotho - panoramio.jpg
Elliot Formation caves in the Matalane Valley, Leribe, Lesotho
Type Geological formation
Unit of Stormberg Group
Sub-unitsUpper Elliot, Lower Elliot
Underlies Clarens Formation
Overlies Molteno Formation
Thicknessup to 500 m (1,600 ft)
Lithology
Primary Mudstone, sandstone
Other Siltstone, conglomerate
Location
Coordinates 30°30′S27°24′E / 30.5°S 27.4°E / -30.5; 27.4
Approximate paleocoordinates 44°06′S1°54′W / 44.1°S 1.9°W / -44.1; -1.9
Region Eastern Cape, Free State, Mafeteng, Maseru, Quthing, Qacha's Nek & Mohale's Hoek
Country Lesotho
South Africa
Type section
Named for Elliot, Eastern Cape
South Africa relief location map.svg
Blue pog.svg
Elliot Formation (South Africa)

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 mainly Late Triassic (Norian-Rhaetian) in age while the UEF is mainly Early Jurassic (Hettangian-earliest 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]

Contents

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] [4] [7]

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. [8] [4] [9] [10] [11] [12]

Age

U-Pb radiometric dating using zircon grains has refined the duration of the Elliot Formation. Zircons of the Lower Elliot Formation are entirely Late Triassic, ranging from around 220 to 205 million years old (Norian to Rhaetian stages). Zircons of the Upper Elliot are mostly Early Jurassic, ranging from around 202 to 192 million years old (latest Rhaetian to Sinemurian stages). The oldest zircons of the overlying Clarens Formation are about 187 million years old (mid-Pliensbachian stage). [1]

The entire Elliot Formation also preserves a record of magnetostratigraphy, with at least nine reverse-normal polarity chron pairs (EF1r to EF9n). The lower-upper Elliot boundary is in the middle of chron EF6n. The Elliot Formation's magnetostratigraphy can be partially correlated with similar records in the Newark Basin (northeast United States), Chinle and Moenave formations (southwest United States), and Los Colorados Formation (Argentina). [7] [1]

Paleontology

The Elliot Formation is well known for its diverse fossils of dinosaur and other vertebrates. The formation is divided into two biozones, the Scalenodontoides Assemblage Zone and Massospondylus Assemblage Zone. The Scalenodontoides Assemblage Zone corresponds to the Lower Elliot Formation. Formerly known as the 'Euskelosaurus' Range Zone, its index taxa include the cynodont Scalenodontoides and the sauropodomorphs Blikanasaurus and Melanorosaurus . [13] The Massospondylus Assemblage Zone extends from the Upper Elliot Formation into the Clarens Formation. Its index taxa include the sauropodomorph Massospondylus , the ornithischian Lesothosaurus , and the crocodylomorph Protosuchus . [14]

Sauropodomorphs are particularly diverse in the Elliot Formation. [15] [16] [17] [18] The most common dinosaur is a sauropodomorph species, Massospondylus carinatus . [19] [20] Fossilised Massospondylus eggs, some with the fossilized remains of embryos intact, have been recovered from UEF deposits in the Golden Gate Highlands National Park. [21] [22]

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. [23] [24] [25] [26]

Dinosaurs

Color key
Taxon Reclassified taxonTaxon falsely reported as presentDubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Ornithischians

Ornithischians of the Elliot Formation
Genus / TaxonSpeciesLocationStratigraphyNotesImages
Abrictosaurus A. consorsUpper ElliotA heterodontosaurid, formerly species of Lycorhinus
Abrictosaurus dinosaur.png
Eocursor E. parvusUpper ElliotA basal ornithischian Eocursor BW.jpg
Fabrosaurus F. australisUpper ElliotA basal ornithischian, nomen dubium
Heterodontosaurus H. tuckiUpper ElliotA heterodontosaurid Heterodontosaurus restoration.jpg
Lesothosaurus L. diagnosticusUpper ElliotA basal neornithischian or thyreophoran, formerly considered a species of Fabrosaurus. [27] Larger Lesothosaurus specimens are sometimes given the name Stormbergia . [28] Lesothosaurus diagnosticus.png
Lycorhinus L. angustidensUpper ElliotA heterodontosaurid
Moyenisauropus Upper ElliotLarge ornithischian footprints similar to Anomoepus . [29]
Pegomastax P. africanaUpper ElliotA heterodontosaurid Pegomastax africana reconstruction.jpg
Thyreophora Thyreophora indetUpper ElliotKnown from scutes [30]
Trisauropodiscus T. aviformaLower–Upper ElliotVery small bird-like dinosaur footprints, potentially produced by theropods or heterodontosaurid ornithischians. [31]

Sauropodomorphs

Prosauropods of the Elliot Formation
GenusSpeciesLocationStratigraphyNotesImages
Aardonyx A. celestaeUpper ElliotA derived sauropodomorph Aardonyx NT.jpg
Antetonitrus A. ingenipesUpper ElliotA lessemsaurid, either a derived sauropodomorph or basal sauropod. [32] Antetonitrus reconstruction.jpg
Arcusaurus A. pereirabdalorumSpion Kop HeelboUpper ElliotA basal sauropodomorph, known from juveniles
Arcusaurus LM.png
Blikanasaurus B. cromptoniBlikana MountainLower ElliotA derived sauropodomorph or basal sauropod. [33]
Blikanasaurus pes.png
Eucnemesaurus E. fortisLower ElliotA possible riojasaurid
E. entaxonis
Euskelosaurus E. browniLower ElliotA plateosaurid, potentially dubious
Gryponyx G. africanusUpper ElliotA massospondylid, potentially dubious
Ignavusaurus I. rachelisUpper ElliotA massospondylid, known from a juvenile. A potential synonym of Massospondylus
Kholumolumo K. ellenbergerorumLower ElliotA basal massopodan.
Ledumahadi [34] L. mafubeUpper ElliotA lessemsaurid, either a derived sauropodomorph or basal sauropod. The largest dinosaur in the formation. [34] [35] Ledumahadi NT.jpg
Massospondylus M. carinatusUpper ElliotA massospondylid, the most common dinosaur in the formation. [19] [20] Massospondylus reconstruction.png
M. kaalaeUpper ElliotA massospondylid which differs from M. carinatus in cranial features
Melanorosaurus M. readiThaba 'NyamaLower ElliotA derived sauropodomorph Melanorosaurus life restoration 2018.jpg
Meroktenos M. thabanensisThabana MorenaLower ElliotA derived sauropodomorph, formerly a species of Melanorosaurus
Right femur of Meroktenos.png
Plateosauravus P. cullingworthiLower ElliotA basal sauropodomorph, formerly specimens of Euskelosaurus
Pseudotetrasauropus P. bipedoidaLower ElliotLarge bipedal sauropodomorph footprints. [36] [37]
P. jaquesiLower ElliotLarge quadrupedal sauropodomorph footprints, sometimes considered a species of Lavinipes . [37]
Pulanesaura P. eocollumUpper ElliotA derived sauropodomorph or basal sauropod
Pulanesaura eocollum.jpg
Sefapanosaurus S. zastronensisLower Elliot?A derived sauropodomorph
Tetrasauropus T. unguiferusLower ElliotLarge quadrupedal sauropodomorph footprints. [36] [37]

Theropods

Large theropod-like teeth have been found in the Lower Elliot Formation. [38] Various exposures of the formation (primarily in Lesotho) preserve informative interactions between theropod trackmakers and soft sediment. [39] [40] [41] [42]

Theropods of the Elliot Formation
GenusSpeciesLocationStratigraphyNotesImages
Dracovenator [43] D. regentiUpper Drumbo FarmUpper ElliotA large neotheropod, potentially close to Dilophosaurus .
Dracovenator regenti.jpg
Eubrontes Lower–Upper ElliotLarge theropod footprints.
Grallator Lower–Upper ElliotSmall theropod footprints.
Kayentapus K. ambrokholohaliUpper ElliotVery large theropod footprints. The largest prints, measuring 57 cm (22 in) in length, may belong to a theropod up to 9 m (30 ft) long. [40] [44]
Megapnosaurus M. rhodesiensisSyntarsus siteUpper ElliotA coelophysid, also known as Syntarsus.
Coelophysis rhodesiensis.JPG

Pseudosuchians

Pseudosuchians of the Elliot Formation
Genus / TaxonSpeciesLocationStratigraphyNotesImages
Basutodon B. feroxLower ElliotA dubious archosaur based on a "rauisuchian"-like tooth. [45]
Batrachopus Upper ElliotSmall crocodylomorph footprints. [46] [25]
Brachychirotherium B. cf. thuringiacumLower ElliotLarge "chirothere" footprints. [46] [36] [1]
Litargosuchus [47] L. leptorhynchusEagles Crag FarmUpper ElliotA basal crocodylomorph
Litargosuchus leptorhynchus.jpg
Orthosuchus O. stormbergiUpper ElliotA possible protosuchid crocodylomorph. [48] [49] [50]
Paratetrasauropus P. seakensisLower ElliotLarge crocodilian-like footprints, probably from crocodylomorphs. [36]
Poposauroidea indet.Lower ElliotAn indeterminate poposauroid. [45]
Protosuchus P. haughtoniUpper ElliotA protosuchid crocodylomorph.
Protosuchus BW.jpg
Rauisuchia indet.Lower ElliotA indeterminate large "rauisuchian" (non-crocodylomorph loricatan). Many "rauisuchian" fossils have been found in the formation, [45] including very large limb bones from near Qhemegha, Eastern Cape. [51] A large toothed maxilla, formerly considered part of " Aliwalia rex ", may be rauisuchian in origin. [1]
Sauropodopus S. antiquusLower ElliotLarge Brachychirotherium -like footprints with a narrow gait. [46] [36]
Sphenosuchus S. acutusUpper ElliotA basal crocodylomorph. [52]
Sphenosuchus skeletal.png

Other reptiles

Other reptiles of the Elliot Formation
GenusSpeciesLocationStratigraphyNotesImages
Australochelys A. africanusUpper ElliotAn australochelyid testudinate (early turtle). [53]
Clevosaurus C. sp.Upper ElliotAn clevosaurid rhynchocephalian. [54]

Synapsids

A possible late-surviving diademodontid cynodont may be present in the Upper Elliot Formation. [55] [1]

Synapsids of the Elliot Formation
GenusSpeciesLocationStratigraphyNotesImages
Ameghinichnus A. sp.Upper Elliot Tritylodontid cynodont footprints. [46]
Diarthrognathus D. broomiUpper ElliotA tritheledontid cynodont
Elliotherium [56] E. kersteniUpper Elliot [1] A tritheledontid cynodont
Erythrotherium E. parringtoniUpper ElliotA mammaliaform cynodont
Megazostrodon M. rudneraeUpper ElliotA megazostrodontid mammaliaform cynodont. [57]
Megazostrodon sp. Natural History Museum - London.jpg
Pachygenelus P. monusUpper ElliotA tritheledontid cynodont
Pachygenelus.jpg
Pentasauropus P. incredibilisLower Elliot Dicynodont footprints
Pentasaurus [58] P. goggaiLower ElliotA stahleckeriid dicynodont, undoubtedly the trackmaker of Pentasauropus. [58]
Pentasaurus holotype.png
Scalenodontoides S. macrodontesLower ElliotA very large traversodontid cynodont
Tritheledon T. riconoiUpper ElliotA tritheledontid cynodont
Tritylodon T. longaevusUpper ElliotA tritylodontid cynodont
Tritylodon longaevusDB24.jpg

Other vertebrates

Amphibians and fish of the Elliot Formation
Genus / TaxonSpeciesLocationStratigraphyNotesImages
Brachyopoidea Quthing, Lesotho [59] Upper Elliot [1] An enormous brachyopoid amphibian based on a skull fragment. Potentially the largest amphibian which has ever lived. [59]
Ceratodus C. sp.Lower–Upper ElliotA ceratodontid lungfish.
Chigutisauridae Lower–Upper ElliotIndeterminate chigutisaurid amphibians.
Daedalichthys D. formosaUpper ElliotA redfieldiiform ray-finned fish, previously identified as Helichthys .
Endemichthys E. likhoeliUpper ElliotA redfieldiiform ray-finned fish.
Episcopopus E. ventrosusUpper ElliotVery large amphibian footprints. [60]
Semionotus S. capensisUpper ElliotA semionotid ray-finned fish.

References

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