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Articles

Haramiyidan mammals from the Middle Jurassic of Western Siberia, Russia. Part 1: Shenshouidae and Maiopatagium

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Article: e1669159 | Received 05 Feb 2019, Accepted 02 Aug 2019, Published online: 05 Nov 2019
 

ABSTRACT

Three new euharamiyidan taxa are described based on isolated teeth from the Middle Jurassic (Bathonian) Itat Formation of the Berezovsk coal mine in Krasnoyarsk Territory, Western Siberia, Russia. The newly erected Sharypovoia, gen. nov., is referred to the Shenshouidae based on a premolariform p4, in which the main cusp and basined heel are surrounded by two rows of cusps. Attributed upper molars have the main labial cusps A1 and A2 connected by a ridge that lacks small additional cusps. In the smaller species S. arimasporum, sp. nov., there are one to two additional cusps mesial to cusp A2, whereas the larger S. magna, sp. nov., lacks these additional cusps. Maiopatagium sibiricum, sp. nov. (Euharamiyida incertae sedis), is similar to M. furculiferum from the Late Jurassic Yanliao Biota of northeastern China in having coalesced crest-like lingual cusps and an open occlusal furrow medially on the upper cheek teeth. Sineleutherus uyguricus from the Upper Jurassic (Oxfordian) Qigu Formation in Xinjiang, China, is restricted to the holotype only, a lower molar, and referred to the Arboroharamiyidae. The previously published sample of ‘Sineleutherusissedonicus from the Itat Formation represents a mixture of shenshouid and arboroharamiyid euharamiyidan taxa, and the holotype of that species, a lower molar, should be referred to a new genus of Arboroharamiyidae. The Asiatic euharamiyidan taxa are referable either to Shenshouidae or Arboroharamiyidae, but not to Eleutherodontidae.

ACKNOWLEDGMENTS

We thank two anonymous reviewers for reading the paper and useful suggestions. For assistance in the field and/or picking the concentrate, we thank I. Danilov, T. Engler, D. Grigoriev, O. Shcheglova (Grigorieva), R. Hielscher, K. Jäger, J. Könen, I. Kuzmin, A. Lang, B. Peters, E. Postolnik, D. Rohkamp, M. Scheske, A. Schwermann, L. Schwermann, E. Syromyatnikova, and A. Valeev. We thank A. Mirolyubov (Saint Petersburg) for taking SEM micrographs of LMCCE 010/1 and LMCCE 010/3 () and G. Oleschinski (Bonn) for the SEM micrographs of other specimens. Financial support was provided by the Deutsche Forschungsgemeinschaft (DFG) (grant MA 1643/14-1, 3), the Russian Foundation for Basic Research (project 11-04-91331-NNIO), the state task of the Ministry of Education and Science of the Russian Federation (project 5.4217.2017/4.6), and the Russian Science Foundation (project 19-14-00020). A. A. was also supported by the Zoological Institute, Russian Academy of Sciences (project АААА-А17-117022810195-3), and a Humboldt Research Award by the Alexander von Humboldt Foundation. The work was performed according to the Russian Government Program of Competitive Growth of Kazan Federal University.

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