Centemodon

{{Short description|Extinct genus of reptiles}}

{{Automatic taxobox

| fossil_range = Late Triassic, {{fossilrange|221|218}}

| taxon = Centemodon

| authority = Lea, 1856

| type_species = {{extinct}}Centemodon sulcatus

| type_species_authority = Lea, 1856

| synonyms = *Paleorhinus sulcatus (Lea, 1856)

}}

Centemodon (meaning "point tooth") is an extinct genus of basal phytosaur from the Late Triassic Period. It lived in what is now Pennsylvania, United States. It is classified as a nomen dubium.[https://web.archive.org/web/20090208132300/http://dinosauria.com/dml/names/phyto.htm#C Centemodon] in the Dinosaur On-Line Omnipedia It was found in the Red Sandstone Formation near the Schuyklill River.[http://www.paleofile.com/Pseudosuchia/Centemodon.asp Centemodon] at Paleofile.org Centemodon may have been related to Suchoprion. It was a small phytosaur, weighing no more than {{convert|200|kg|lbs}} when fully grown.

Discovery and naming

Sometime before the Bone Wars, a palaeontologist known as Dr. Leo (surname unknown) discovered several fossil fragmentary teeth that later became the Centemodon holotype.{{cite web|url=http://m.prehistoric-world7.webnode.cz/news/centemodon/|title=Centemodon: Prehistoric World|website=m.prehistoric-world7.webnode.cz}} When Leo described the fragments, he was unsure of what they belonged to, and Leo did not name the fragments. They were eventually named in 1856 by Isaac Lea.Lea, I. 1856. Description of Centemodon sulcatus. Proceedings of the Academy of Natural Sciences, Philadelphia 10: pp. 77-78.

References