Chiniquodon
| Chiniquodon | |
|---|---|
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| Fossil of C. theotonicus in the Museum of Paleontology, Tuebingen | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Synapsida |
| Clade: | Therapsida |
| Clade: | Cynodontia |
| Family: | †Chiniquodontidae |
| Genus: | †Chiniquodon von Huene 1936 |
| Type species | |
| †Chiniquodon theotonicus | |
| Species | |
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| Synonyms | |
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Chiniquodon is an extinct genus of carnivorous cynodonts, which lived during the Late Triassic (Carnian) in South America (Argentina and Brazil) and Africa (Namibia and Madagascar). Chiniquodon was closely related to the genus Aleodon,[1] and close to the ancestry of mammals.
Other contemporaries included early dinosaurs. As both groups filled a similar ecological niche, fairly large therapsid hunters such as Chiniquodon may have been outcompeted by dinosaurs.
Classification
Chiniquodon theotonicus, the type species, is from the Santa Maria Formation, Brazil and Chañares Formation, Ischigualasto-Villa Unión Basin, northwestern Argentina. This species is known from a number of skulls. The holotype is in the paleontological collection at Tübingen University, Germany.
Chiniquodon kitchingi, from the Santa Maria Formation of Brazil, was described in 1982 by A. M. Sá-Teixeira based on a single skull missing the lower jaw. When first described, it was assigned to the genus Probelesodon, but was reassigned to Chiniquodon in a 1995 paper by Fernando Abdala, as the type species of Probelesodon (P. lewisi) was found to be a
Chiniquodon sanjuanensis
Chiniquodon kalanoro UA 10607).
Chiniquodon omaruruensis[6] is from the Omingonde Formation of Namibia. It is known from a single specimen (GSN F315), consisting of a complete skull and parts of the postcranial skeleton.
References
Further reading
- Von Huene. Die Fossilien Reptilien des südamerikanischen Gondwanalandes an der Zeitenwende (Denwa-Molteno-Unterkeuper = Ober-Karnisch). Ergebnisse der Sauriergrabungen in Südbrasilien 1928/29. (The fossil reptiles of South American Gondwana during the temporal transition) (Denwa-Molteno-Upper Triassic = Upper Carnian). Results of the excavations in South Brazil 1928/29, part II.) 1936. Pages 93–159.