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Irdin Manha Formation : ウィキペディア英語版
Irdin Manha Formation
The Irdin Manha Formation is a palaeontological formation from the Eocene located in Inner Mongolia, China, a few kilometres south of the Mongolian border (, paleocoordinates ).〔. Retrieved July 2013.〕
U.S. paleontologists Henry Fairfield Osborn and Roy C. Andrews discovered two premolars on the site in 1923, and assigned the specimen to the new genus ''Eudinoceras'' because he believed it to be related to "''Dinoceras''" (now known as ''Uintatherium''). Within a decade, however, as more complete specimens were recovered, the animal was identified as a Mongolian relative to the North American pantodont ''Coryphodon''.
==See also==

*List of fossil sites

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Irdin Manha Formation」の詳細全文を読む



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