The first finding of Mimomys in the Russian Far East

A new species of the Mimomys is described from the Far East Russia (the Medvezhyi Klyk cave, Sikhote-Alin). Layer 7 of the Medvezhyi Klyk cave (1.08–1.18 m) was dated to be 13 790–14 200 BP. Mimomys chandolensis sp. nov. was found in a deeper layer (2.63–2.68 m) and therefore assuming there was no r...

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Main Authors: Mikhail P. Tiunov, Fedor N. Golenishchev, Leonid L. Voyta
Format: Article
Language:English
Published: Institute of Paleobiology PAS 2016-02-01
Series:Acta Palaeontologica Polonica
Subjects:
Online Access:http://www.app.pan.pl/archive/published/app61/app000822014.pdf
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spelling doaj-5194f9d208404f719986fdaa341140752020-11-25T01:08:47ZengInstitute of Paleobiology PASActa Palaeontologica Polonica0567-79201732-24212016-02-0161120521010.4202/app.00082.2014The first finding of Mimomys in the Russian Far EastMikhail P. Tiunov0Fedor N. Golenishchev1Leonid L. Voyta2Institute of Biology and Soil FEB RAS, Prospekt 100-letia 159, 690022 Vladivostok, Russian FederationZoological Institute of RAS, Universitetskaya emb., 1, 199034 St.-Petersburg, Russian FederationZoological Institute of RAS, Universitetskaya emb., 1, 199034 St.-Petersburg, Russian Federation; Institute of Natural Resources, Ecology and Cryology SD RAS, Butina st., 26, 672090 Chita, Russian Federation.A new species of the Mimomys is described from the Far East Russia (the Medvezhyi Klyk cave, Sikhote-Alin). Layer 7 of the Medvezhyi Klyk cave (1.08–1.18 m) was dated to be 13 790–14 200 BP. Mimomys chandolensis sp. nov. was found in a deeper layer (2.63–2.68 m) and therefore assuming there was no redeposition of the remains and that the accumulation proceeded gradually, the molar specimen we found is 30–50 kyr old. Due to the extent of the preservation we observed in the molar and the structure of the cave, the specimen does not seem likely to have been redeposited. Our hypothesis is that due to the warm and wet climate of the region, the vole, which became extinct more than 600 kyr ago, had been extant there by the Late Pleistocene period. The new species is hypsodont, with a few cement, a lack of enamel isle or prismatic fold; tangential and lamellar layers of enamel ultrastructure are poorly expressed.http://www.app.pan.pl/archive/published/app61/app000822014.pdfMimomysRussiaPleistocene
collection DOAJ
language English
format Article
sources DOAJ
author Mikhail P. Tiunov
Fedor N. Golenishchev
Leonid L. Voyta
spellingShingle Mikhail P. Tiunov
Fedor N. Golenishchev
Leonid L. Voyta
The first finding of Mimomys in the Russian Far East
Acta Palaeontologica Polonica
Mimomys
Russia
Pleistocene
author_facet Mikhail P. Tiunov
Fedor N. Golenishchev
Leonid L. Voyta
author_sort Mikhail P. Tiunov
title The first finding of Mimomys in the Russian Far East
title_short The first finding of Mimomys in the Russian Far East
title_full The first finding of Mimomys in the Russian Far East
title_fullStr The first finding of Mimomys in the Russian Far East
title_full_unstemmed The first finding of Mimomys in the Russian Far East
title_sort first finding of mimomys in the russian far east
publisher Institute of Paleobiology PAS
series Acta Palaeontologica Polonica
issn 0567-7920
1732-2421
publishDate 2016-02-01
description A new species of the Mimomys is described from the Far East Russia (the Medvezhyi Klyk cave, Sikhote-Alin). Layer 7 of the Medvezhyi Klyk cave (1.08–1.18 m) was dated to be 13 790–14 200 BP. Mimomys chandolensis sp. nov. was found in a deeper layer (2.63–2.68 m) and therefore assuming there was no redeposition of the remains and that the accumulation proceeded gradually, the molar specimen we found is 30–50 kyr old. Due to the extent of the preservation we observed in the molar and the structure of the cave, the specimen does not seem likely to have been redeposited. Our hypothesis is that due to the warm and wet climate of the region, the vole, which became extinct more than 600 kyr ago, had been extant there by the Late Pleistocene period. The new species is hypsodont, with a few cement, a lack of enamel isle or prismatic fold; tangential and lamellar layers of enamel ultrastructure are poorly expressed.
topic Mimomys
Russia
Pleistocene
url http://www.app.pan.pl/archive/published/app61/app000822014.pdf
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