Priconodon

Extinct genus of dinosaurs From Wikipedia, the free encyclopedia

Priconodon (meaning "saw cone tooth"[1]) is an extinct genus of ankylosaurian dinosaur (perhaps nodosaurid), mainly known from its large teeth. Its remains have been found in the Early Cretaceous (Aptian-Albian age) Arundel Formation of Muirkirk, Prince George's County, Maryland, USA, and possibly the Potomac Group, also located in Maryland. As an ankylosaur, Priconodon would have been a large armored quadrupedal herbivore, though no size estimation has been done due to the scarcity of described remains.

Phylum:Chordata
Class:Reptilia
Clade:Ornithischia
Quick facts Scientific classification, Binomial name ...
Priconodon
Temporal range: Early Cretaceous, 113 Ma
Priconodon tooth in multiple views
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Dinosauria
Clade: Ornithischia
Clade: Thyreophora
Clade: Ankylosauria
Family: Nodosauridae
Genus: Priconodon
Species:
P. crassus
Binomial name
Priconodon crassus
Marsh, 1888
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History of discovery

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]

Additional specimens

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] In 2018, three new ankylosaur teeth described from the Potomac Formation were assigned to Priconodon crassus based on their similarity to the holotype.[8] In 2023, large ankylosaur fossils (including a vertebra and a osteroderms) were announced to be found at Dinosaur Park by John-Paul Hodnett,[9][10] which may potentially represent additional specimens of Priconodon.[11]

See also

References

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