A total of 1250 lower first molars (m1) of voles (Arvicolini) were studied from Late Pleistocene deposits (the radiocarbon dates from rodent bones: 17 100 ± 50 IGAN-9117; 13 255 ± 60 IGAN-9116) of the Imanay Cave (southern Urals, 53°02' N, 56°26' E). Of these, 24 m1 of voles of the subgenus Stenocranius were found to have broadly connected triangles T4 and T5 (Pitymys-Rhombus) at the base of the anteroconid. This structure is characteristic of lower m1 of Lasiopodomys (Stenocranius) gregaloides (Hinton, 1923) from faunas of the second half of the Early Pleistocene and the first half of the Middle Pleistocene. Molars with such morphology have not been found so far in the Late Pleistocene and Holocene locations of Europe and the Urals.
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http://dx.doi.org/10.1134/S0012496622040019 | DOI Listing |
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