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The current paper offers a protocol for the analytic assessment of the intraspecific variability of dental morphology in shrews. Our approach blends a temporal aspect together with a comparative morphological analysis in terms of a unified morphogenetic concept based on the 'activator-inhibitor cascades model' and 'decreasing heritability model'. We used material from the upper Pleistocene and Holocene fossiliferous deposits of Koridornaya and Sukhaya caves in the Russian Far East and analysed the first upper molars of specimens that were similar in size to the teeth of Crocidura lasiura but differed in some proportions and qualitative features. We analysed the temporal variation of the molar shape against samples of the extant species C. lasiura, Crocidura sibirica and Crocidura shantungensis along with fossil specimens using geometric morphometry based on three-dimensional landmarks and semi-landmark datasets. Our results revealed correspondence of the fossil teeth to intraspecies variation of C. lasiura with a slight increase in the morphospace size. We also found two deviant teeth, which, however, also fell in the range of C. lasiura and were determined as Crocidura cf. C. lasiura. A detailed description of the dental features became possible with the use of the computed microtomography approach. [ABSTRACT FROM AUTHOR]

Extinct cave bears inhabited a large part of Eurasia in a wide diversity of habitats during the Pleistocene. This study investigates via tooth wear analysis the feeding habits of 66 individuals belonging to three genetically different species located in the Urals and eastern Europe: Ursus rossicus from Kizel cave, U. kanivetz from Secrets cave, and U. ingressus from Shiriaevo 1 cave. For the microwear analysis, the three species were compared with a reference collection of extant ursids. The dietary space of U. kanivetz does not match any of the extant species' spaces. U. rossicus and U. ingressus tended towards some of the extant species' measurements without any overlapping. For all three sites, the same microwear pattern was identified for all age groups (juvenile, prime, and old adult), meaning no differences related to ontogeny were found. The extinct species presented a larger number of coarse scratches compared to extant species, pointing to a preference for abrasive food items like dry grass or shrubs typical of the mammoth steppe biome during the cold season. These results indicate a niche partitioning between U. rossicus and U. kanivetz that co-existed in the same area, and in this way they avoiding competition. [ABSTRACT FROM AUTHOR]

The current paper first time describes a small Beremendia from the late Pleistocene deposits in the Koridornaya Cave locality (Russian Far East), which associated with the extinct Beremendia minor. The paper is the first attempt to use a comparative analytical method to evaluate a possible case of redeposition of fossil remains of this shrew. In this case, the 'comparative' part of the method corresponds to the 'faunistic approach' of Jelle Reumer, and the 'analytical' part of the method corresponds to his extended 'morphological approach. ' The analytic method uses morphospace size estimation (MSE) based on principal component analysis and estimation of the variance to evaluate redeposition of Beremendia minor from the late Pleistocene deposits in the Koridornaya Cave. This result allows us to suggest the significant environmental contribution to the East Asian beremendiin extinction, such as climatic fluctuation, landscape changes and shrew community changes between the late Pliocene and early Pleistocene. We discuss the last remains of East Asian Beremendia (Peisorex) described from the Chinese early Pleistocene localities (Chiachiashan, Haimao, Renzidong) and the last remains of Lunanosorex described from the Chinese late Pliocene localities (Qipanshan Hill and Houxushan Hill). MSE was performed for soricine tribes with the 'elongated' condylar process. [ABSTRACT FROM AUTHOR]

Although the present-day distributional boundary between the European badger (Meles meles) and the Asian badger (Meles leucurus) is around the Volga River, studies of ancient bone remains have indicated changes in the distribution of M. meles and M. leucurus in the Urals–Volga region during the Holocene. To examine past changes in distribution using genetic data, changes in genetic diversity, and the relationships of Holocene to modern populations, we sequenced ~150 bp of the mitochondrial DNA control region from the 44 ancient badger remains excavated from European Russian, Ural and Western Siberian sites, and we detected 12 haplotypes. Our study revealed Holocene changes in the distributional boundary between these badger species. Meles meles inhabited the Ural Mountains east of the Volga River in the Early Holocene, whereas M. leucurus expanded its distribution westwards, starting ~2500 years ago. Thereafter, M. leucurus rapidly replaced M. meles in the region between the Urals and the Volga, resulting in the present-day boundary in the Volga–Kama region. Among the 12 haplotypes detected, three for M. leucurus and four for M. meles were identical to partial sequences of haplotypes detected in modern populations, indicating considerable genetic continuity between Holocene and modern populations. [ABSTRACT FROM AUTHOR]

Crown shape variation of the first lower molar in the arctic (Vulpes lagopus) and red foxes (Vulpes vulpes) was analyzed using five groups of morphotypes. Carnassial morphologies were compared between the species and between spatially and temporally distant populations: one Late Pleistocene (n = 45) and seven modern populations of the arctic fox (n = 259), and one Late Pleistocene (n = 35) and eight modern populations of the red fox (n = 606). The dentition of Holocene red foxes had larger morphotype variability than that of arctic foxes. The lower carnassials of the red fox kept have some primitive characters (additional cusps and stylids, complex shape of transverse cristid), whereas the first lower molars of the arctic fox have undergone crown shape simplification, with the occlusal part of the tooth undergoing a more pronounced adaptation to a more carnivorous diet. From the Late Pleistocene of Belgium to the present days, the arctic fox's crown shape has been simplified and some primitive characters have disappeared. In the red fox chronological changes in the morphology of the lower carnassials were not clearly identified. The phyletic tree based on morphotype carnassial characteristics indicated the distinctiveness of both foxes: in the arctic fox line, the ancient population from Belgium and recent Greenland made separate branches, whereas in the red foxes the ancient population from Belgium was most similar to modern red foxes from Belgium and Italy. [ABSTRACT FROM AUTHOR]

The multilayer ion-plasma coating TiN/CrN, 6 layers of CrN and 5 lauers of TiN, for hardening of piston rings is proposed. It is established that as a result of hardening, the wear rate of rings decreases 15.7 times. A new method for estimating the residual thickness of the coating, which gives recommendations for improving the quality of coatings, is proposed. [ABSTRACT FROM AUTHOR]

During the last several years, new multi- and single-layered archaeological sites, in which the most ancient Neolithic pottery in the Eastern Europe had been found, were excavated in the region of Lower Volga. Animal bones and organic materials were sampled from these sites for radiocarbon (14C) dating and diet investigations. The evidence from these studies suggests that the first domestic animals in the Lower Volga region appeared in the Cis-Caspian culture of the Early Eneolithic. Lipid analysis of food crusts from pottery allowed the cooked food to be characterized. The detailed chronology from Neolithic (6500–5400 cal BC) to Eneolithic (5300–4700 cal BC) cultures, as well as the diet of these ancient people, were reconstructed. [ABSTRACT FROM AUTHOR]

New paleodietary data were obtained after the discovery and excavation in 2015–2017 of the Cherepakha 13 site in the southern part of Primorye (Maritime) Province in far eastern Russia. The site is located near the coast of Ussuri Bay (Sea of Japan) and belongs to the Yankovsky cultural complex of the Early Iron Age 14C-dated to ca. 3000 BP (ca. 1200 cal BC). The stable isotope composition of the bone collagen for 11 humans and 30 animals was determined. For humans, the following values (with±1 sigma) were yielded: δ13C=–10.2±0.8‰; and δ15N=+12.4±0.3‰. The majority of terrestrial animals show the usual isotopic signals: δ13C=–19.4 ÷ –23.3‰; and δ15N=+4.6÷+6.6‰ (for wolves, up to +10.1‰); dogs, however, have an isotopic composition similar to humans: δ13C= –11.7±1.2‰; and δ15N=+12.4±0.4‰. Marine mammals have common values for pinnipeds: δ13C=–13.7 ÷ –14.6‰; and δ15N=+17.4 ÷ +18.0‰. The main food resources for the population of Cherepakha 13 site were (1) marine mollusks, fish, and mammals; and (2) terrestrial mammals; and possibly C4 plants (domesticated millets). [ABSTRACT FROM AUTHOR]

The aim of this study was to investigate the unique find from medieval Novgorod the Great-an almost complete skull of a young Eurasian beaver ( Castor fiber L.). Comparisons of the craniometry of this skull with the skulls of the autochthonous and reintroduced populations of beavers from the same and adjacent regions suggest that a type of large beaver once inhabited the Volkhov basin. Further studies are necessary to accept or reject this hypothesis. Copyright © 2016 John Wiley & Sons, Ltd. [ABSTRACT FROM AUTHOR]

The Asian badger (Meles leucurus amurensis) is widely distributed throughout the northeast of China, and plays an important role in regulating the prey population stability of forest eco-system as mesopredators. We first determined and annotated the whole mtDNA genome of the Asian badgerMeles leucurus amurensisto better understand the evolutionary relationship of this subspecies. The complete mitogenome is 16 497 bp in length, includes 13 protein-coding genes, 22 tRNA genes, 2 rRNA genes and 1 control region. We built the phylogenetic tree of Asian badger and other 10 most closelyMustelidaespecies. [ABSTRACT FROM PUBLISHER]