Please use this identifier to cite or link to this item: http://elar.urfu.ru/handle/10995/117915
Title: Morphology and evolutionary position of the Early Pliocene vole Propliomys jalpugensis from Eastern Europe
Other Titles: Морфология и эволюционная позиция раннеплиоценовой полёвки Propliomys jalpugensis из Восточной Европы
Authors: Yakimova, A. A.
Tesakov, A. S.
Pogodina, N. V.
Issue Date: 2022
Publisher: KMK Scientific Press
Citation: Yakimova A. A. Morphology and evolutionary position of the Early Pliocene vole Propliomys jalpugensis from Eastern Europe [Морфология и эволюционная позиция раннеплиоценовой полёвки Propliomys jalpugensis из Восточной Европы] / A. A. Yakimova, A. S. Tesakov, N. V. Pogodina // Russian Journal of Theriology. — 2022. — Vol. 21. — Iss. 1. — P. 13-23.
Abstract: Propliomys jalpugensis, a fossil rhizodont vole (late Early Pliocene, late Ruscinian, MN15), is revised based on materials from the type locality Kotlovina (southwestern Ukraine). This form is interpreted as a phyletic stage, marked by dental complication of first lower molar and hypsodonty, intermediate between the preceding late Early Pliocene Propliomys kowalskii and P. destinatus, and successive Late Pliocene Propliomys ucrainicus. Molar enamel of P. jalpugensis shows a pattern with the radial enamel in leading edges, occasionally with the incipient lamellar enamel, and the inner radial and outer primitive tangental enamel in trailing and closing edges © RUSSIAN JOURNAL OF THERIOLOGY, 2022
Keywords: ARVICOLINAE
EASTERN EUROPE
ENAMEL MICROSTRUCTURE
PLEISTOCENE
PLIOCENE
STRATIGRAPHY
URI: http://elar.urfu.ru/handle/10995/117915
Access: info:eu-repo/semantics/openAccess
SCOPUS ID: 85131719065
WOS ID: 000876552800002
PURE ID: 30455509
ISSN: 16823559
DOI: 10.15298/rusjtheriol.21.1.02
Sponsorship: Government Council on Grants, Russian Federation
We thank the technical staff of the Geological Institute RAS, Paleontological Institute RAS, and the Ural Center for Shared Use “Modern nanotechnology” SNSM UrFU for the assistance with SEM microscopy and preparing of helped to refine the manuscript. The work was supported by Act 211 Government of the Russian Federation, contract No. 02.A03.21.0006. This work conforms to the scientific plan of the Geological Institute of the Russian Academy of Sciences
ACKNOWLEDGEMENTS. We thank the technical staff of the Geological Institute RAS, Paleontological Institute RAS, and the Ural Center for Shared Use “Modern nanotechnology” SNSM UrFU for the assistance with SEM microscopy and preparing of samples. We thank the two reviewers for comments that helped to refine the manuscript. The work was supported by Act 211 Government of the Russian Federation, contract No. 02.A03.21.0006. This work conforms to the scientific plan of the Geological Institute of the Russian Academy of Sciences.
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