| Centemodon Temporal range: Late Triassic, | |
|---|---|
| Scientific classification | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Reptilia |
| Clade: | Archosauromorpha |
| Clade: | Archosauriformes |
| Order: | † Phytosauria |
| Genus: | † Centemodon Lea, 1856 |
| Type species | |
| †Centemodon sulcatus | |
| Synonyms | |
| |
Centemodon (meaning "point tooth") is an extinct genus of basal [2] phytosaur from the Late Triassic Period. It lived in what is now Pennsylvania, United States. [2] It is classified as a nomen dubium . [3] It was found in the Red Sandstone Formation near the Schuyklill River. [4] Centemodon may have been related to Suchoprion . It was a small phytosaur, weighing no more than 200 kilograms (440 lb) when fully grown. [2]
Sometime before the Bone Wars, a palaeontologist known as Dr. Leo (surname unknown) discovered several fossil fragmentary teeth that later became the Centemodon holotype. [2] 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. [1]