EARLY MIOCENE RODENTS FROM THE AKTAU MOUNTAINS (SOUTH-EASTERN KAZAKHSTAN)

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dc.contributor.author Kordikova E.G.
dc.contributor.author de Bruijn H.
dc.date.accessioned 2021-03-02T07:43:50Z
dc.date.available 2021-03-02T07:43:50Z
dc.date.issued 2001
dc.identifier https://elibrary.ru/item.asp?id=27763170
dc.identifier.citation Senckenbergiana Lethaea, 2001, 81, 2, 391-405
dc.identifier.issn 0037-2110
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/26035
dc.description.abstract The rodent assemblage from the Middle Members of the Chul’adyr Formation contains seven species that belong to six (sub)families. The dominant Cricetidae are represented by a new genus and species:Aktaumys dzhungaricus and by a new species ofKarydomys: K. dzerzhinskii. Each of the other rodent species: ?Sinosminthus gen. et sp. indet.,Sayimys aff.obliquidens, Asiacastor aff.baschanovi and Tachyoryctoidinae gen. A, sp. 1, is represented by a few cheek teeth only (altogether 8% of the specimens). The composition of the assemblage resembles Oligo-Miocene material from Anatolia, but the closest relatives of most of the species are found in Central Asia. The stage of evolution ofKarydomys dzerzhinskii, Sayimys aff.obliquidens and the tachyoryctoidine suggests an Early Miocene (MN4 rather than MN3) age for the assemblage.
dc.subject Miocene
dc.subject rodent assemblage
dc.subject Aktau Mountains
dc.subject South – Eastern Kazakhstan
dc.title EARLY MIOCENE RODENTS FROM THE AKTAU MOUNTAINS (SOUTH-EASTERN KAZAKHSTAN)
dc.type Статья
dc.subject.age Cenozoic::Neogene::Miocene en
dc.subject.age Кайнозой::Неоген::Миоцен ru


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