Hypsirhophus
Hypsirhophus discurus Temporal range: Late Jurassic, 146 Ma | |
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Scientific classification | |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Reptilia |
Clade: | Dinosauria |
Order: | †Ornithischia |
Suborder: | †Stegosauria |
Family: | †Stegosauridae |
Genus: | Hypsirhophus |
Species: | H. discurus |
Binomial name | |
Hypsirhophus discurus Cope, 1878 | |
Hypsirhophus (often spelled Hypsirophus) is a dubious genus of stegosaurian dinosaurs. It contains a single species, Hypsirhophus discurus, which is known only from a fragmentary specimen. The fossil consists of partial vertebrae from the back, three from the tail, and a piece of rib.
The specimen was excavated from Edward Drinker Cope's Quarry 3 near the "Cope's Nipple" site in Garden Park, Colorado, near the very top of the late Jurassic Morrison Formation.[1] In 1878, Cope named the specimen Hypsirhophus discurus. Some later researchers have considered Hypsirhophus to be a synonym of Stegosaurus,[2] or as a nomen dubium,[3] though Ken Carpenter and Peter Galton have suggested that it is distinct based on differences in the vertebrae.[4]
References
- ↑ Carpenter, K. (1998). Vertebrate biostratigraphy of the Morrison Formation near Canon City, Colorado. Modern Geology, 23: 407-426.
- ↑ Gilmore CW (1914). "Osteology of the armored Dinosauria in the United States National Museum, with special reference to the genus Stegosaurus". Series: Smithsonian Institution. United States National Museum. Bulletin 89. Government Printing Office, Washington (89).
- ↑ Maidment, S. C. R.; Brassey, Charlotte; Barrett, Paul Michael (2015). "The Postcranial Skeleton of an Exceptionally Complete Individual of the Plated Dinosaur Stegosaurus stenops (Dinosauria: Thyreophora) from the Upper Jurassic Morrison Formation of Wyoming, U.S.A.". PLoS ONE. 10 (10): e0138352. doi:10.1371/journal.pone.0138352.
- ↑ Galton, P.M. (2010). "Species of plated dinosaur Stegosaurus (Morrison Formation, Late Jurassic) of western USA: new type species designation needed". Swiss Journal of Geosciences. 103 (2): 187–198. doi:10.1007/s00015-010-0022-4.
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