About: Asiaceratops   Sponge Permalink

An Entity of Type : owl:Thing, within Data Space : 134.155.108.49:8890 associated with source dataset(s)

The type species, Asiaceratops salsopaludalis, was formally described by Lev Nesov, L.F. Kaznyshkina and Gennadiy Olegovich Cherepanov in 1989. The generic name combines a reference to Asia with ~ceratops, "horned face". The specific name means "of the salt marsh" in Latin. In the same publication Microceratops sulcidens Bohlin 1953 was renamed into a second species of Asiaceratops: Asiaceratops sulcidens.[1] Asiaceratops has often been considered a nomen dubium, in view of the limited holotype material.

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  • Asiaceratops
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  • The type species, Asiaceratops salsopaludalis, was formally described by Lev Nesov, L.F. Kaznyshkina and Gennadiy Olegovich Cherepanov in 1989. The generic name combines a reference to Asia with ~ceratops, "horned face". The specific name means "of the salt marsh" in Latin. In the same publication Microceratops sulcidens Bohlin 1953 was renamed into a second species of Asiaceratops: Asiaceratops sulcidens.[1] Asiaceratops has often been considered a nomen dubium, in view of the limited holotype material.
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  • The type species, Asiaceratops salsopaludalis, was formally described by Lev Nesov, L.F. Kaznyshkina and Gennadiy Olegovich Cherepanov in 1989. The generic name combines a reference to Asia with ~ceratops, "horned face". The specific name means "of the salt marsh" in Latin. In the same publication Microceratops sulcidens Bohlin 1953 was renamed into a second species of Asiaceratops: Asiaceratops sulcidens.[1] The holotype of Asiaceratops salsopaludalis, CCMGE 9/12457, was found in Uzbekistan in a layer of the Khodzhakul Formation dating from the early Cenomanian, about ninety-nine million years old. It consists of a part of a left maxilla. Some other fragments were in 1989 referred to the species, among them teeth and a phalanx. In 1995 Nesov referred more material, from three Uzbek sites, mostly skull elements and a partial humerus, of individuals of different ages.[2] Asiaceratops has often been considered a nomen dubium, in view of the limited holotype material.
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