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Historical Biology
An International Journal of Paleobiology
Volume 33, 2021 - Issue 4
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Articles

New species of Ballusia Ginsburg and Morales, 1998 (Ursidae, Carnivora) from Miocene of Eastern Siberia, Russia

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Pages 486-497 | Received 19 Mar 2019, Accepted 26 Jun 2019, Published online: 18 Jul 2019
 

ABSTRACT

The new basal ursine bear, Ballusia zhegalloi n. sp., is described from the Early Miocene Tagay 1 locality (Baikal region, Russia) based on isolated M1. Previously described maxillary fragment with M1-2 from the closely synchronous fauna of Khirgis-Nur I in Mongolia, originally referred to Ballusia elemensis, is here included into the new species. The M1 of the new species shares similarities with M1 of previously known Early Miocene European species B. elmensis but is more derived in lower medial cusps, transversally closer spaced medial ridge and lingual cingulum, and by a slightly expressed antero-external angle. The new Asian species shares some derived features with Ballusia orientalis from Early Miocene of China, such as a more rounded M1 outline, and incipient buccal styles in M1. The other characters in the two forms of Asian Ballusia imply their parallel evolution. The Tagay find represents the first record of the genus Ballusia in Russia. It elucidates phyletic affinities of early ursine bears and refines the geographic and stratigraphic range of the genus Ballusia.

Acknowledgments

Jan Wagner (Prague) is thanked for providing photographs of casts of Ballusia hareni and Ursavus isorei . Alexander Lavrov provided an access to the specimen PIN 3380/56. Sergey Bagirov (PIN RAS) is thanked for the quality photographs in . Ekaterina Firsova is acknowledged for compiling . The two reviewers, Alberto Valenciano and Jan Wagner are sincerely thanked for the professional review. The field work was supported by the Russian Foundation for Basic Research, grant no. 14-04-00575. The study was conducted in accordance with the plan of scientific research of the Geological Institute of the Russian Academy of Sciences and the Institute of Earth Crust, Siberian branch of the Russian Academy of Sciences.

Disclosure statement

No potential conflict of interest was reported by the authors.

Additional information

Funding

This work was supported by the Russian Foundation for Basic Research (RFBR) [14-04-00575].

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