Pucapristis
Pucapristis is a prehistoric genus of sclerorhynchid ray whose fossils first appear in the fossil record in rocks dating from the Maastrichtian stage. The genus was described in 1963 by Schaeffer.[1] Fossils of Pucapristis have not been found in any subsequent strata. Incidentally, the Maastrichtian is the final portion of the Cretaceous Period and its endpoint marks the advent of the Cretaceous–Paleogene extinction event. This major geological transition is famous for being the mass extinction that wiped out the dinosaurs.
| Pucapristis Temporal range: Maastrichtian | |
|---|---|
 | |
| Teeth | |
Scientific classification  | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Chondrichthyes |
| Superorder: | Batoidea |
| Order: | Rajiformes |
| Family: | †Sclerorhynchidae |
| Genus: | †Pucapristis Schaeffer, 1963 |
| Species: | †P. branisi |
| Binomial name | |
| †Pucapristis branisi Schaeffer, 1963 | |
Biogeography
To date, Pucapristis fossils have been found only in the Maastrichtian deposits of central South America. The El Molino Formation of Bolivia produces Pucapristis tooth fossils in abundance. These Bolivian specimens have been recovered near the cities of Potosi and Sucre The Yacoraite Formation of Salta Province in northwestern Argentina is another locality from which Pucapristis remains can be excavated.
See also
References
- Pucapristis at Fossilworks.org
Further reading
- M. Gayet, L. G. Marshall, T. Sempere, F. J. Meunier, H. Capetta and J. Rage. 2001. Middle Maastrichtian vertebrates (fishes, amphibians, dinosaurs and other reptiles, mammals) from Pajcha Pata (Bolivia). Biostratigraphic, palaeoecologic and palaeobiogeographic implications. Palaeogeography, Palaeoclimatology, Palaeoecology 169(1–2):39–68