Clevosaurus


Clevosaurus is an extinct genus of rhynchocephalian reptile from the Late Triassic and the Early Jurassic periods. Species of Clevosaurus were widespread across Pangaea, and have been found on all continents except Australia and Antarctica. Five species of Clevosaurus have been found in ancient fissure fill deposits in south-west England and Wales, alongside other sphenodontians, early mammals and dinosaurs. In regards to its Pangaean distribution, C. hadroprodon is the oldest record of a sphenodontian from Gondwana, though its affinity to Clevosaurus has been questioned.

History of discovery

The first species of Clevosaurus to be described was C. hudsoni, which was described by William Elgin Swinton in 1939 from a fissure fill deposit in Cromhall Quarry in the county of Gloucestershire, England, with the name of the county lending its name to the genus.
Another notable specimen was discovered in 1953 in Cromhall Quarry alongside the holotype of Cryptovaranoides microlanius.

Description

Species of Clevosaurus varied in body size, with Clevosaurus sectumsemper having an estimated total length of, while C. hudsoni had a total length of around . The skull length could range from as little as in C. sectumsemper and up to in C. hudsoni. The reptilian encephalisation quotient of C. brasiliensis is much lower than that of the modern tuatara, whose REQ is 0.84–1.16. The teeth of European Clevosaurus tended to be mesio-distally elongated, blade-like, and occluded precisely with the opposite pair of teeth, leaving conspicuous diagonal wear facets and acting as a self-sharpening cutting surface. However, the teeth of C. brasiliensis have a very different morphology with no diagonal wear facets, the teeth of the dentary are all conical excluding the posterior-most tooth which can be up to three-times bigger than any of the other teeth, they also have a unique form of implantation, where the base of the teeth sit deeply within the jaw bones, which is not known of in any other rhynchocephalian.

Paleobiology

Species of Clevosaurus were likely insectivorous. Biomechanical modelling suggests that they had high enough tooth pressures and strong enough bite force to crush chitin, indicating that they had the ability to feed on thick-shelled beetles as well as possibly small vertebrates.

Taxonomy

At least 9 species of Clevosaurus are considered valid:
The three species known from the Sinemurian aged Lufeng Formation of China are now considered indeterminate within the genus. Indeterminate remains are also known from the Stormberg Group of South Africa, dating to the Hettangian. Indeterminate clevosaur remains, possibly representing Clevosaurus, are also known from the Norian aged Fleming Fjord Group of Jameson Land, east Greenland.
Below is a cladogram of the relationships within Clevosauridae based on the phylogenetic analysis of Hsiou et al. :
"Clevosaurus" latidens was recovered outside of Clevosauridae, as the sister taxon of Opisthodontia. It was subsequently assigned to a new genus, Fraserosphenodon, in 2018.
Clevosaurus is considered to be a member of the group Eusphenodontia by the groups definition, due to it possessing characters not shared with more primitive sphenodontians. By definition, it is excluded from Neosphenodontia.
Position of Clevosaurus within Rhynchocephalia, after DeMar et al. 2022.

Additional reading

  • Gill PG, Säilä LK, Corfe IJ, Challands TJ, Williams M, Clemens WA. The fauna and palaeoenvironment of St. Brides Island: Evidence from the lower Jurassic fissure fills of South Wales. In Barrett PM, Evans SE. Ninth international symposium on Mesozoic terrestrial ecosystems and biota. pp 48−51. London: Natural History Museum.
  • Jones MEH The Early Jurassic clevosaurs from China. Natl Mus Nat Hist Sci Bull, 37:548–562.
  • Jones MEH. Dentary tooth shape in Sphenodon and its fossil relatives. In Koppe T, Meyer G, Alt KW,. Interdisciplinary Dental Morphology, Frontiers of Oral Biology. Greifswald, Germany; Karger. 9–15.