Prionessus is a genus of extinct mammal from the Paleocene of what is now Central Asia. It was a member of the extinct order Multituberculata within the suborder Cimolodonta and superfamily Taeniolabidoidea. The genus was named by William Diller Matthew and Walter Granger in 1925, and is based on a single species P.lucifer.[1]
Prionessus Temporal range: Thanetian
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Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Mammalia |
Order: | †Multituberculata |
Family: | †Lambdopsalidae |
Genus: | †Prionessus |
Species: | †P. lucifer
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Binomial name | |
†Prionessus lucifer W.D. Matthew and W. Granger, 1925
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Kielan-Jarowoska and Hurum believe that members of the Taeniolabidoidea, such as Prionessus, are all quite similar. For example, they all share a short wide snout and a blocky head [2] so it is probably instructive to look at a close and more commonly occurring relative, Lambdopsalis bulla, a likely burrower.[3][4] Matthew and Granger noted in their discovery that P.lucifer had a robust lower incisor, supportive of this similarity.[5]
Fossil remains have been found in the Late Paleocene Nomogen and Khashat Formations of Gashato, Naran and Nomogen in Bayan Ulan of Mongolia and China. Prionessus fossils range from 59-55 million years ago, through the Thanetian age of the late Paleocene. They were estimated to have had a body mass of about 370 grams (13 oz).[6]
Notes
editReferences
edit- Dykes, Trevor. "Mesozoic Mammals;Eucosmodontidae, Microcosmodontidae and Taeniolabidoidea, an internet directory". Archived from the original on 16 July 2012.
- Kielan-Jaworowska, Zofia; Hurum, J.H. (2001). "Phylogeny and Systematics of Multituberculate Mammals". Palaeontology. 44 (3): 389–429. doi:10.1111/1475-4983.00185.
- Kielan-Jaworowska, Zofia; Qi, Tao (1990). "Fossorial adaptations of a Taeniolabidoid Multituberculate mammal from the Eocene of China". Vertebrata PalAsiatica. 28 (2): 83–94.
- Kielan-Jaworowska, Kielan; Sloan, Robert E. (1979). "Catopsalis (Multituberculata) from Asia and North America and the problem of taeniolabidid dispersal in the Late Cretaceous". Acta Palaeontologica Polonica. 24 (2): 187–197.
- Matthew, W.D.; Granger, W. (1925). "Fauna and Correlation of the Gashato Formation of Mongolia". American Museum Novitates (189). American Museum of Natural History, New York: 1–12.