Vancleavea

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Not to be confused with the flowering plant genus Vanclevea.
Vancleavea
Temporal range: 228–203.6Ma
Late Triassic
Vancleavea.jpg
Restoration
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Archosauriformes
Genus: Vancleavea
Long & Murry, 1995
Type species
Vancleavea campi
Long & Murry, 1995

Vancleavea is a genus of extinct, armoured, non-archosaurian archosauriform with relatively small limbs from the Late Triassic of western North America, and is the oldest known form to date. The type and only species is V. campi, named by Robert Long & Phillip A Murry, 1995.[1] A nearly complete and articulated skeleton was discovered at the Coelophysis Quarry in north-central New Mexico (Ghost Ranch), and was prepared at the Ruth Hall Museum of Paleontology in Abiquiú, New Mexico before being formally described in the Zoological Journal of the Linnean Society in 2009.[2][3] Vancleavea was first discovered in 1962 from the Petrified Forest Member of the Petrified Forest National Park and initially described by Long and Murry in 1995.[1] The genus is named after Phillip Van Cleave, who discovered the first known remains of the genus.[4] Vancleavea is a fairly common occurrence in most levels of the Chinle Formation, however, due to the poorly preserved remains, it is difficult to compare specimens across stratigraphic levels.[5][6]

Description[edit]

Vancleavea was around 1.2 m (3.9 ft) in length. Imbricating osteoderms cover the entire body, the limbs are relatively short, and the skull is highly ossified.[3] The supratemporal fenestra is absent, which may represent a secondary closure rather than a plesiomorphic trait.[7] The nares open dorsally (i.e. nostrils face upward) and the jaw contains enlarged caniniform fangs. Each osteoderm possesses a pronounced central keel and an anterior projection. The illium of Vancleavea resembles those of unrelated drepanosaurs.[4] The unique morphology of Vancleavea differs greatly from any other known basal archosauriform.[3]

Phylogenetics[edit]

Phylogenetic position of Vancleavea
1 

Mesosuchus


2

Proterosuchus




Erythrosuchus




Euparkeria




Chanaresuchus


3

Leptosuchus




Postosuchus



Desmatosuchus





Vancleavea



Doswellia



Turfanosuchus








Megalancosaurus



Prolacerta



1 Archosauromorpha, 2 Archosauriformes, 3 Archosauria

Parker & Barton 2008

Before the genus was described 1995, an additional specimen consisting of fragmentary skull material found by Charles Camp in 1923 was suggested to belong to a proterochampsid.[8] However, this material was later referred to a new taxon, Acallosuchus rectori, after having been shown to be distinct from the postcranial material found in 1962. In the initial description of Vancleavea, the genus was referred to Neodiapsida incertae sedis along with A. rectori.[1]

A 2008 phylogenetic study tentatively suggested that Vancleavea was a basal archosauriform more derived than Erythrosuchus, Proterosuchus, and possibly even Euparkeria.[4] In a new 2009 study, Vancleavea was found to be more closely related to Archosauria than both Erythrosuchus and Proterosuchus, and was also found to be outside of the crown group, with Euparkeria remaining the closest sister taxon of Archosauria.[3]

Controversy still remains as to whether or not the specimens referred to this genus are representative of a "single species-level taxon or a clade of closely related taxa that lived through much of the Late Triassic of North America, given the poor fossil record of the taxon."[3] Differences in the osteoderms as well as the shape of the internal tuberosity of the humerus in different specimens may suggest that they belong to different taxa, but because of the fragmentary preservation of these fossils, unambiguous autapomorphies cannot be distinguished that would indicate that there are different taxa.[4]

Paleobiology[edit]

Vancleavea has features that suggest a semi-aquatic lifestyle. These include the long body, short limbs, and deep tail. Vancleavea is unique among archosauriforms and tetrapods in general in that the fin-like tail is deepened by elongated osteoderms rather than tall neural spines.[7]

References[edit]

  1. ^ a b c Long, R. A. & Murry, P. A. (1995). "Late Triassic (Carnian and Norian) tetrapods from the southwestern United States". New Mexico Museum of Natural History and Science Bulletin 4: 1–254. 
  2. ^ Celeskey, Matt (August 12, 2007). "Stories from the Snyder Quarry 3: Part Three: The Art of Ghost Ranch, an O’Keefe-less Overview". The Hairy Museum of Natural History. Retrieved 2009-12-06. 
  3. ^ a b c d e Nesbitt, S. J.; Stocker, M. R.; Small, B. J.; & A. Downs (November 26, 2009). "The osteology and relationships of Vancleavea campi (Reptilia: Archosauriformes)". Zoological Journal of the Linnean Society 157 (4): 814–864. doi:10.1111/j.1096-3642.2009.00530.x. 
  4. ^ a b c d Parker, W. G.; Barton, B. (2008). "New information on the Upper Triassic archosauriform Vancleavea campi based on new material from the Chinle Formation of Arizona". Palaeontologia Electronica 11 (3): 20p. 
  5. ^ Parker, W. G. & Barton, B. J.. "New Information on the Upper Triassic Archosauriform Vancleavea campi Based on New Material From the Chinle Formation of Arizona". Palaeontologia Electronica (Society of Vertebrate Paleontology). 
  6. ^ Parker, Bill (November 27, 2009). "The osteology and relationships of Vancleavea campi (Reptilia: Archosauriformes)". Chinleana: Discussion of Late Triassic paleontology and other assorted topics. Retrieved 2009-11-29. 
  7. ^ a b Naish, Darren (November 28, 2009). "Yet more extreme Triassic weirdness: Vancleavea". Tetrapod Zoology. Retrieved 2009-12-02. 
  8. ^ Murry, P. A.; Long, R. A. (1989). "Geology and paleontology of the Chinle Formation, Petrified Forest National Park and vicinity, Arizona and a discussion of vertebrate fossils of the southwestern Upper Triassic". In Lucas, S.G. and Hunt, A.P. (eds.). Dawn of the Dinosaurs in the American Southwest. Albuquerque: New Mexico Museum of Natural History. pp. 29–64. 

External links[edit]