4.1 Article

Variability of the lower incisors in the cave bears (Carnivora, Ursidae) from the Caucasus and Urals

Journal

COMPTES RENDUS PALEVOL
Volume 20, Issue 25, Pages 539-553

Publisher

MUSEUM NATL HISTOIRE NATURELLE
DOI: 10.5852/cr-palevol-2021v20a25

Keywords

Carnivora; Ursidae; Pleistocene; Caucasus; Ural; cave bears; morphotypes; size; variations; lower incisor

Categories

Funding

  1. Theriology laboratory of the Zoological Institute RAS [AAAA-A17-117022810195-3]
  2. Palaeoecology laboratory of the Institute of Plant and Animal Ecology RAS [AAAAA19-119031890086-0]
  3. Russian Federation [MK-1130.2019.4]

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The study examined the morphometric and morphotypic variability of cave bear lower incisors from different geographic regions, stratigraphic periods, and mitochondrial haplogroups. Results showed clear distinctions between Urals Ursus kanivetz and Caucasian U. kudarensis in morphology, with the former displaying more derived features. U. kanivetz had the largest average size of lower incisors, distinct from U. kudarensis, which also showed clear separation from other cave bear groups. The study suggests that cave bear incisors demonstrate a hypocarnivorous adaptation trend in the Spelearctos group during the Late Pleistocene.
Morphometric and morphotypic variability of the cave bear lower incisors from two different geographic regions (Caucasus and Urals), different stratigraphic periods (Middle and Late Pleistocene), and bearing different mitochondrial haplogroups (kudarensis (Baryshnikov, 1985) and ingressus Rabeder, Hofreiter & Withalm, 2004) was studied. Urals Ursus kanivetz Vereshchagin, 1973 is clearly distinguished from Caucasian U. kudarensis by morphology of the upper and lower incisors. The Urals cave bear exhibits more derived features compared to the Caucasian cave bears. Ursus kanivetz exhibits the largest average size of the lower incisors. The lower incisors of U. kanivetz are clearly distinct from those in U. kudarensis. Also, U. kudarensis specimens display a clear separation from all other groups of cave bears. Morphology of the incisors of the cave bears is clearly different from that of Early Pleistocene U. etruscus G. Cuvier, 1823, as well as from that of recent U. arctos L., 1758 (Rabeder, 1999) and U. maritimus Phipps, 1774. Our results suggest that the incisors of the cave bears are similar to each other and demonstrate a hypocarnivorous adaptation as a major evolution trend in the lineage of Spelearctos group. These adaptation features were perhaps developed in parallel in different lineages of the cave bears (U. spelaeus Rosenmuller, 1794 and U. kanivetz on the one hand and U. kudarensis on the other hand) in the Late Pleistocene.

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