Clovesuurdameredeor

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Clovesuurdameredeor
Temporal range: Bathonian, 168.3–166.1  Ma
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Clovesuurdameredeor.png
Holotype skull
Scientific classification Red Pencil Icon.png
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Suborder: Thalattosuchia
Family: Machimosauridae
Genus: Clovesuurdameredeor
Johnson et al., 2020
Species:
C. stephani
Binomial name
Clovesuurdameredeor stephani
(Hulke, 1867)
Synonyms

Clovesuurdameredeor (meaning "sea creature of Closworth"; from the Medieval Latin Clovesuurda and the Old English meredeor) is an extinct genus of machimosaurid teleosauroid from the Bathonian Cornbrash Formation of England. [1]

Illustration of the holotype Proceedings BHL21302445.jpg
Illustration of the holotype

The type species, C. stephani, was originally named "Steneosaurus" stephani by Hulke in 1867. [2] Vignaud (1995) considered S. stephani to be a minor synonym of Yvridiosuchus boutilieri (then still in the genus Steneosaurus ), [3] but Johnson (2019) and Johnson et al. (2020) discovered that S. stephani was a basal machimosaur that was separate from Yvridiosuchus, erecting the genus Clovesuurdameredeor for this. [4] [1]

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Cornbrash Formation

The Cornbrash Formation is a Middle Jurassic geological formation in England. It ranges in age from Bathonian to Callovian, the uppermost part of the Middle Jurassic. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus. The name Cornbrash is an old English agricultural name applied in Wiltshire to a variety of loose rubble or brash which, in that part of the country, forms a good soil for growing corn. The name was adopted by William Smith for a thin band of shelly limestone which, in the south of England, breaks up in the manner indicated. Although only a thin group of rocks, it is remarkably persistent; it may be traced from Weymouth to the Yorkshire coast, but in north Lincolnshire it is very thin, and probably dies out in the neighborhood of the Humber. It appears again, however, as a thin bed in Gristhorpe Bay, Cayton Bay, Wheatcroft, Newton Dale and Langdale. In the inland exposures in Yorkshire it is difficult to follow on account of its thinness, and the fact that it passes up into dark shales in many places the so-called clays of the Cornbrash, with Avicula echinata. The Cornbrash is of little value for building or road-making, although it is used locally; in the south of England it is not oolitic, but in Yorkshire it is a rubbly, marly, frequently ironshot oolitic limestone. In Bedfordshire it has been termed the Bedford limestone.

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<i>Neosteneosaurus</i> Genus of reptiles (fossil)

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<i>Charitomenosuchus</i> Extinct genus of reptiles

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<i>Proexochokefalos</i> Extinct genus of reptiles

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<i>Seldsienean</i> Extinct genus of machimosaurid thalattosuchian

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References

  1. 1 2 Johnson, Michela M.; Young, Mark T.; Brusatte, Stephen L. (2020). "The phylogenetics of Teleosauroidea (Crocodylomorpha, Thalattosuchia) and implications for their ecology and evolution". PeerJ. 8: e9808. doi: 10.7717/peerj.9808 . PMC   7548081 . PMID   33083104.
  2. Hulke, JW, "Gharial skull from the Cornbrash of Closworth." Proceedings of the Dorset Natural History and Antiquarian Field Club, 1877, p. 29
  3. Vignaud, P., “The Thalattosuchia, Mesozoic marine crocodiles: phylogenetic systematics, paleoecology, biochronology and palaeogeographical implications." Unpublished PhD thesis, University of Poitiers, 1995, p.410
  4. Johnson, Michela Maria Angeline (2019). "The taxonomy, systematics and ecomorphological diversity of Teleosauroidea (Crocodylomorpha, Thalattosuchia), and the evaluation of the genus 'Steneosaurus'". Archives of the University of Edinburgh .