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1 History  





2 Material  





3 Paleobiology  





4 See also  





5 References  














Priconodon






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Priconodon
Temporal range: Early Cretaceous, 113 Ma

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Priconodon tooth in multiple views
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Ornithischia
Clade: Thyreophora
Clade: Ankylosauria
Family: Nodosauridae
Genus: Priconodon
Species:
P. crassus
Binomial name
Priconodon crassus

Marsh, 1888

Priconodon (meaning "saw cone tooth"[1]) is an extinct genusofdinosaur (perhaps nodosaurid), known from its large teeth. Its remains have been found in the Aptian-Albian age Lower Cretaceous Arundel FormationofMuirkirk, Prince George's County, Maryland, USA and the Potomac Group, also located in Maryland.

History

[edit]

O. C. Marsh named the genus for USNM 2135, a large worn tooth from what was then called the Potomac Formation. As ankylosaurians were by and large unknown at the time, he compared it to Diracodon (=Stegosaurus) teeth.[2] It was not identified as an ankylosaurian until Walter Coombs assigned it to Nodosauridae in 1978.[3]

In 1998 Kenneth Carpenter and James Kirkland, in a review of North American Lower Cretaceous ankylosaurs, considered it tentatively valid as an unusually large nodosaurid, larger than all those described before.[4] Carpenter (2001) retained it as a valid nodosaurid, but did not employ it in his phylogenetic analysis.[5] Vickaryous et al. (2004), in a review of armored dinosaurs, considered it to be dubious without comment.[6] West and Tibert, however, followed this with a preliminary account of a morphometric study that found it to be a unique genus.[7]

Material

[edit]
Tooth

Carpenter and Kirkland (1998) listed 12 additional teeth from the same area as the holotype tooth, and tentatively added a robust tibia (USNM 9154) to the genus. They found the lack of armor found in the Arundel to be peculiar, but noted that fossils are rare in that formation anyway.[4]

Paleobiology

[edit]

As a nodosaurid, Priconodon would have been a slow, armored, quadrupedal herbivore.[6] It would have been a large nodosaurid, but since only teeth are definitely known for the genus, size estimation has not been done.

See also

[edit]

References

[edit]
  1. ^ "Untitled Document".
  • ^ Marsh, O.C. (1888). Notice of a new genus of Sauropoda and other new dinosaurs from the Potomac Formation. American Journal of Science 135:89-94.
  • ^ Coombs, Jr., W.P. (1978). The families of the ornithischian dinosaur order Ankylosauria. Palaeontology 21(1):143-170.
  • ^ a b Carpenter, K., and Kirkland, J.I. (1998). Review of Lower and middle Cretaceous ankylosaurs from North America. In: Lucas, S.G., Kirkland, J.I., and Estep, J.W. (eds.). Lower and Middle Cretaceous Terrestrial Ecosystems. New Mexico Museum of Natural History and Science Bulletin 14:249-270.
  • ^ Carpenter, K. (2001). Phylogenetic analysis of the Ankylosauria. In: Carpenter, K. (ed.). The Armored Dinosaurs. Indiana University Press:Bloomington 455-483. ISBN 0-253-33964-2
  • ^ a b Vickaryous, M.K., Maryańska, T., and Weishampel, D.B., (2004). Ankylosauria. In: Weishampel, D.B., Dodson, P., and Osmólska, H. (eds.). The Dinosauria (second edition). University of California Press:Berkeley 363-392. ISBN 0-520-24209-2
  • ^ "West, A. and Tibert, N. (2004). Quantitative analysis for the type material of Priconodon crassus: a distinct taxon from the Arundel Formation in southern Maryland. Geological Society of America Abstracts with Programs, 36(5):423". Archived from the original on 2007-01-06. Retrieved 2007-01-05.

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Priconodon&oldid=1196857303"

    Categories: 
    Ankylosaurs
    Early Cretaceous dinosaurs of North America
    Taxa named by Othniel Charles Marsh
    Fossil taxa described in 1888
    Paleontology in Maryland
    Ornithischian genera
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    Short description is different from Wikidata
    Articles with 'species' microformats
     



    This page was last edited on 18 January 2024, at 18:27 (UTC).

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