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Simple Summary: Global warming at the border of Late Pleistocene-Holocene, around ten thousand years ago caused a dramatic rearrangement of habitats in the Northern Hemisphere. Populations of cold-adapted megafauna species, which were spread over large areas of Eurasia, did not survive it. At the same time, small representatives of this mammoth fauna complex survived, including lemmings and arctic fox, but greatly reduced their distribution northward. However, it is uncertain whether species survived by habitat tracking the elusive tundra, or if they came from other places where they survived warming, and local populations died out without leaving descendants. To answer this, we studied ancient DNA from new fossil remains of arctic foxes from caves in the northern and polar Urals. The data received do not show any connectivity between ancient and modern individuals, supporting the hypothesis of local extinction of arctic fox in the region rather than the tracking habitat hypothesis. These findings are important in light of global climate warming expectations. It is predicted that the most severe effects are expected to occur in high-latitude biomes and the results obtained must be kept in mind when planning conservation policy measures. Despite the high level of interest, the population history of arctic foxes during the Late Pleistocene and Holocene remains poorly understood. Here we aimed to fill gaps in the demographic and colonization history of the arctic fox by analyzing new ancient DNA data from fossil specimens aged from 50 to 1 thousand years from the Northern and Polar Urals, historic DNA from museum specimens from the Novaya Zemlya Archipelago and the Taymyr Peninsula and supplementing these data by previously published sequences of recent and extinct arctic foxes from other regions. This dataset was used for reconstruction of a time-calibrated phylogeny and a temporal haplotype network covering four time intervals: Late Pleistocene (ranging from 30 to 13 thousand years bp), Holocene (ranging from 4 to 1 thousand years bp), historical (approximately 150 years), and modern. Our results revealed that Late Pleistocene specimens showed no genetic similarity to either modern or historical specimens, thus supporting the earlier hypothesis on local extinction rather than habitat tracking. [ABSTRACT FROM AUTHOR]

Investigations of the unconsolidated Upper Pleistocene – Holocene cave deposits of the Northern Urals resulted in detailed biostratigraphical and palaeoenvironmental data. The article summarizes data from important stratigraphical levels exposed in 19 cave localities, most part of which represent several layers dated to different periods. These data cover the period from the beginning of the Upper Pleistocene (MIS 5-4) to the end of the Upper Holocene. At the beginning of Marine Isotope Stage 3 (MIS 3), open woodlands were distributed, which at the end of MIS 3 were replaced by Forest–steppe landscapes. At the beginning of MIS 2 (LGM), Periglacial steppe landscape was distributed. At the end of MIS 2 and at the beginning of the Holocene (MIS 1), semi-open landscapes were common. At the beginning of the Middle Holocene, they were replaced by taiga landscapes. Fish were present in the fauna of the Northern Urals in the Upper Pleistocene and Holocene. Amphibians in the Upper Pleistocene as part of the fauna of the region appear only at its beginning (MIS 5-4) and end (Bølling – Allerød period). Since the beginning of the Holocene (MIS 1), they have been constantly present in the fauna of the Northern Urals. Reptiles appear in the fauna of the region only in the Middle Holocene. During the Upper Pleistocene, the avifauna and fauna of small mammals were dominated by species of open landscapes, and the fauna of large mammals was dominated by species of open and semi-open landscapes. At the beginning of the Holocene, the avifauna and theriofauna increased the number of species associated with tree and shrub vegetation and near-aquatic species. Since the beginning of the Middle Holocene, the avifauna and theriofauna have been dominated by species of taiga landscapes. Palynological data and data on the fauna of small and large mammals allow us to separate the deposits of the Upper Pleistocene and Holocene. These data also allow us to separate the deposits of the beginning (MIS 5-4), middle (MIS 3), end (MIS 2)) of the Upper Pleistocene, Lower, Middle and Upper Holocene (MIS 1). [ABSTRACT FROM AUTHOR]

The present phylogeographic pattern of red deer in Eurasia is not only a result of the contraction of their distribution range into glacial refugia and postglacial expansion, but probably also an effect of replacement of some red deer s.l. mtDNA lineages by others during the last 50 000 years. To better recognize this process, we analysed 501 sequences of mtDNA cytochrome b , including 194 ancient and 75 contemporary samples newly obtained for this study. The inclusion of 161 radiocarbon-dated samples enabled us to study the phylogeny in a temporal context and conduct divergence-time estimation and molecular dating. Depending on methodology, our estimate of divergence between Cervus elaphus and Cervus canadensis varied considerably (370 000 or 1.37 million years BP, respectively). The divergence times of genetic lineages and haplogroups corresponded to large environmental changes associated with stadials and interstadials of the Late Pleistocene. Due to the climatic oscillations, the distribution of C. elaphus and C. canadensis fluctuated in north–south and east–west directions. Some haplotypes dated to pre-Last Glacial Maximum periods were not detected afterwards, representing possibly extinct populations. We indicated with a high probability the presence of red deer sensu lato in south-eastern Europe and western Asia during the Last Glacial Maximum. [ABSTRACT FROM AUTHOR]

Aim: The Expansion‐Contraction model has been used to explain the responses of species to climatic changes. During periods of unfavourable climatic conditions, species retreat to refugia from where they may later expand. This paper focuses on the palaeoecology of red deer over the past 54 ka across Europe and the Urals, to reveal patterns of change in their range and explore the role of environmental conditions in determining their distribution. Location: Europe and western Asia to 63°E. Taxon: Red deer (Cervus elaphus). Methods: We collected 984 records of radiocarbon‐dated red deer subfossils from the Late Pleistocene and the Holocene, including 93 original dates. For each deer sample we compiled climatic and biome type data for the corresponding time intervals. Results: During the last 54 ka changes in red deer range in Europe and the Urals were asynchronous and differed between western and eastern Europe and western Asia due to different environmental conditions in those regions. The range of suitable areas for deer during the Last Glacial Maximum (LGM) was larger than previously thought and covered vast regions not only in southern but also in western and eastern Europe. Throughout the period investigated the majority of specimens inhabited forests in the temperate climatic zone. The contribution of forests in deer localities significantly decreased during the last 4 ka, due to deforestation of Europe caused by humans. Mean January temperature was the main limiting factor for species distribution. Over 90% of the samples were found in areas where mean January temperature was above −10°C. Main conclusions: Red deer response to climatic oscillations are in agreement with the Expansion‐Contraction model but in contradiction to the statement of only the southernmost LGM refugia of the species. During the last 54 ka red deer occurred mostly in forests of the temperate climatic zone. [ABSTRACT FROM AUTHOR]

The composition of large mammal fauna from the Imanay Cave in the Southern Urals (53°02' N, 56°26' E) is described in the present study. The paper aims to provide an preliminary description of the large mammal remains from the Imanay Cave in order to establish their taxonomic status, geological age and to detect the factors that led to accumulation of the bone remains in the cave. An analysis of species composition of vertebrate fauna, archaeological finds and radiocarbon dates has shown that accumulation of fossils in the Imanay Cave spanned the whole period of the Late Pleistocene and Holocene. Remains of the small cave bear (Ursus " savini ") and cave lion (Panthera ex gr. fossilis-spelaea) are prevalent in the Pleistocene groups: 9414 (93%) and 536 (5%) bone specimens, respectively. The cave is the only site in the world where mass bone assemblages of two large terrestrial Carnivora species - small cave bear and cave lion – were found simultaneously. The composition of the skeletal samples for both species was described and the age and sex distributions were determined. Though Mousterian stone tools were found in the cave, no trace of the hunt of the bears and lions by humans was detected. The period during which the accumulation of the fossils took place can be broadly determined as the first half of the Late Pleistocene (MIS5–3). [ABSTRACT FROM AUTHOR]

Seven species of red-toothed shrews (Sorex araneus, Sorex isodon, Sorex tundrensis, Sorex caecutiens, Sorex minutus, Sorex minutissimus, Neomys fodiens), white-toothed shrews (Crocidura sp.), moles (Talpa sp.) and hedgehogs (Erinaceus sp.) were found in Late Pleistocene and Holocene deposits of the southern part of the western slope of the Ural Mountains. In the Late Pleistocene and Early Holocene deposits, the red-toothed shrews were dominated by S. tundrensis. This species disappeared from the area by the Late Holocene, when S. araneus became the predominant species. Smaller mandibular sizes have been registered for S. araneus in the Middle and Late Holocene, as compared to the sizes of older samples. The morphometric criteria have been established for a species differential diagnosis of the Late Pleistocene – Early Holocene mandibular samples of S. araneus and S. tundrensis , found in local deposits of the southern Pre-Urals area studied. • Bones of insectivorous mammals (10 taxons) were found in the deposits of caves and grottoes in the southern Pre-Urals. • Sorex tundrensis was dominant species in the Late Pleistocene and Early Holocene deposits. • Fossil Sorex araneus and Sorex tundrensis are well differentiated by three morphometric parameters. • Temporal variability was traced within the samples of mandibles of Sorex araneus. [ABSTRACT FROM AUTHOR]

Body size is correlated with many critical behavioral and developmental patterns in carnivores, including domestic dogs. The body masses and bite forces of archaeological dog remains from Siberia and the Russian Far East were estimated to make inferences regarding their behaviors and capacitis. The dogs date from ∼10,000–100 cal. BP and derive from archaeological sites spanning from steppe environments in the south to tundra regions of the northern Arctic. The dogs exhibit a four-fold difference in body mass, ranging from 7.6 to 32.5 kg, but have a mean body mass of only 16.4 kg. Bite forces are around only half those of modern wolves, indicating that the dogs had greatly reduced abilities to grasp and masticate prey and food items. The dogs exhibit a slight decrease in body size through time, perhaps due to human selection or greater survival rates for smaller individuals in human-dominated food environments. Dog body size variance within individual archaeological sites was as high as in a sample of modern wolves from throughout the study area, suggesting little strict human control over body size. No correlation was found between body size and site latitude, suggesting that Bergmann's rule does not hold for these canids. Human shelters may provide a buffer against low temperatures that might favour larger body sizes at high latitudes. About 90% of the analyzed dogs have estimated body masses less than 21.5 kg, suggesting most were best adapted for procuring prey smaller than themselves—the dogs were not capable of taking down larger prey without the assistance of humans. Estimated dog body masses cannot eliminate the possibility that many of the animals were used for pulling sleds, and nearly all were capable of packing modest loads on their backs. Livestock guarding dogs are not well-evidenced by the body mass data, but herding dogs are a possibility in all of the pastoral or agricultural settings analyzed. Image 1 • Body masses and bite forces were estimated for 199 archaeological dog remains from Siberia and the Russian Far East. • The dogs' body masses range from 7.6 to 32.5 kg, with a mean of 16.4 kg. • The dogs' bite forces are around half those of modern wolves. • The dogs exhibit a slight decrease in body size through time. • Many of the dogs were of sufficient size to pull sleds, and all could have carried packs. [ABSTRACT FROM AUTHOR]