Evolution of occlusal shape of the first and second upper molars of Middle–Late Pleistocene collared lemmings ( Dicrostonyx, Arvicolinae, Rodentia) in northeast European Russia

• Published in: Boreas
• Main Authors: Ponomarev, Dmitry, Puzachenko, Andrey
• Other Authors: RFBR
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2015
• Subjects: Pechora
• Online Access: http://dx.doi.org/10.1111/bor.12131; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12131; https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12131

An approach combining traditional morphotypical methods, multivariate analysis and informational‐statistical methods was used to study evolutionary changes in the occlusal shape of the first and second upper molars of Recent and Middle–Late Pleistocene Dicrostonyx (32 samples) from localities in northeast European Russia (northeastern Russian Plain, the Timan Ridge and the northern part of the Urals). The evolutionary history is described in terms of morphological evolutionary levels of teeth suggested by Smirnov et al . (1997, Materialy Po Istorii I Sovremennomu Sostojaniju Fauny Severa Zapadnoj Sibiri: Sbornik Nauchnyh Trudov, Chelyabinsk, slightly modified). Based on 14 C‐dated samples, levels of molar evolution did not always successively replace each other in time, but rather there were often synchronous populations at any given level. This finding supports the notion of a mosaic pattern of morphotypical diversity and relatively independent, parallel evolution of lemming teeth amongst different populations. Six relatively distinct stages in the evolutionary history of Dicrostonyx from the Pechora (Dnieper) to Recent time have been described, but estimations of their relative ages are often debatable. The rates of change in the M1 and M2 morphotypes and morphological diversity in collared lemmings varied over the entire time interval. The fastest replacement of morphotypes and the highest level of morphological diversity in the study area occurred approximately during the Lateglacial (16–10 cal. ka BP ). In the present study, we suggest a new version of evolutionary history of collared lemmings in northeast European Russia, taking into consideration the morphological variability of molars, radiocarbon dates and geological data. Our results provide a more detailed pattern of species evolution in the studied region and specific ages of some localities.