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Prodeinodon
Extinct genus of dinosaurs From Wikipedia, the free encyclopedia
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Prodeinodon (meaning "before Deinodon") is a wastebasket taxon and a dubious genus of theropod dinosaur from the Early Cretaceous (Barremian to Aptian stages) from the Xinlong Formation in the Napai Basin of China and from the Oosh Formation of Mongolia.[1] Two species have been formally identified (with a third informal species), all three known only from tooth fragments, showing no diagnostic features, making them difficult to classify, though they may belong to a carnosaur. At least some of the referred species may represent basal carcharodontosaurid theropods similar to Acrocanthosaurus.[2]
The type species, P. mongoliense, was described by Henry Fairfield Osborn in 1924.[3] A second species, P. kwangshiensis, was named in 1975.[4] "P. tibetensis" has not been formally described, and it may have belonged to its own, separate genus.[5]
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Species
- P. mongoliense (Osborn, 1924) is known from a single tooth, collected around 1923 and described by Henry Fairfield Osborn in a 1924 paper, where he also described several other theropods and sauropods discovered in Mongolia.[3] The holotype of P. mongoliense, which is the holotype for the entire genus, is AMNH 6265, a single tooth collected from the Oosh Formation. Some scientists have considered P. mongoliense to have been a carnosaur.[6]
- P. kwangshiensis (Hou et al., 1975) is known from four incomplete teeth and a tibia, found in the Xinlong Formation, China.[4] It can confidently be identified to Theropoda but it was probably not the same type of theropod as P. mongoliense.[6] It could represent a carcharodontosaurid closely related to Acrocanthosaurus.[7]
- "P. tibetensis" is an informal species of Prodeinodon that was briefly mentioned in 1986.[5] Known from a single vertebra found in the Hettangian Daye Group in China, this species was probably a theropod but it most likely did not belong to the same animal as P. mongoliense and it may have belonged to its own, entirely separate genus.[6] It is geographically present in Xizang Zizhiqu, China.[8]
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References
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