Modern studies of the resources of fossil mammoth tusks in the Arctic zone of Yakutia (northeast Siberia, Russia)

Mammoth tusk is an important material for the economy of the Republic of Sakha (Yakutia), in which bone carving is historically widespread. In addition, in recent decades, Yakutia is the largest exporter of mammoth tusks abroad. The Arctic part of Yakutia is the only region of Russia and the World where a long and steady mining of fossil mammoth bones and tusks has taken place. In this regard, the question of assessing the resources of the mammoth tusks in the Arctic zone of Yakutia is actual. To calculate the annual collection amounts of the mammoth tusks in the Arctic zone of Yakutia, we used various sources. In order to determine the prognostic resources of the mammoth tusks in the Arctic zone of Yakutia, we calculated the area of Yedoma sediments, containg the mammoth tusks. According to recent estimates, based on new data on the melting of Yedoma sediments in the north of Yakutia and the level of collection of mammoth tusks in last years, Yedoma sediments in the Arctic zone of Yakutia can contain from 143, 539.03 to 170,220.7 tons of mammoth tusks. These calculations are very rough, but in general they are very close to the results of our previous calculations (maximum about 140 thousand tons) and calculations of other researchers (N. Vereshchagin - 150 thousand tons, A. Smirnov - 184 thousand tons). Thus, Yedoma sediments of Northern Yakutia can contain from 140 thousand tons to almost 200 thousand tons of mammoth tusks. Large amount of this valuable raw material can play a significant economic role for the Republic of Sakha (Yakutia)in future

Northernmost record of the Merck's rhinoceros Stephanorhinus kirchbergensis (Jäger) and taxonomic status of Coelodonta jacuticus Russanov (Mammalia, Rhinocerotidae)

A lower jaw of Stephanorhinus kirchbergensis from the Mus Khaya locality on the Yana River in Yakutia is described. This jaw was previously designated as a paratype of Coelodonta jacuticus, but morphological and morphometric analysis has shown that it actually belongs to a typical S. kirchbergensis. Morphometric parameters of the holotype (skull) of C. jacuticus fall within the range of intraspecific variation of C. antiquitatis. The same results of a morphometric study were obtained for the subspecies Coelodonta antiquitatis pristinus and C. a. humilis. This suggests that C. jacuticus, Coelodonta antiquitatis pristinus, and C. a. humilis are invalid taxa which should be regarded as junior synonyms of C. antiquitatis. The find of S. kirchbergensis in northern Yakutia is the northernmost occurrence of this species

Genetic variation at hair length candidate genes in elephants and the extinct woolly mammoth

<p>Abstract</p> <p>Background</p> <p>Like humans, the living elephants are unusual among mammals in being sparsely covered with hair. Relative to extant elephants, the extinct woolly mammoth, <it>Mammuthus primigenius</it>, had a dense hair cover and extremely long hair, which likely were adaptations to its subarctic habitat. The fibroblast growth factor 5 (<it>FGF5</it>) gene affects hair length in a diverse set of mammalian species. Mutations in <it>FGF5 </it>lead to recessive long hair phenotypes in mice, dogs, and cats; and the gene has been implicated in hair length variation in rabbits. Thus, <it>FGF5 </it>represents a leading candidate gene for the phenotypic differences in hair length notable between extant elephants and the woolly mammoth. We therefore sequenced the three exons (except for the 3' UTR) and a portion of the promoter of <it>FGF5 </it>from the living elephantid species (Asian, African savanna and African forest elephants) and, using protocols for ancient DNA, from a woolly mammoth.</p> <p>Results</p> <p>Between the extant elephants and the mammoth, two single base substitutions were observed in <it>FGF5</it>, neither of which alters the amino acid sequence. Modeling of the protein structure suggests that the elephantid proteins fold similarly to the human FGF5 protein. Bioinformatics analyses and DNA sequencing of another locus that has been implicated in hair cover in humans, type I hair keratin pseudogene (<it>KRTHAP1</it>), also yielded negative results. Interestingly, <it>KRTHAP1 </it>is a pseudogene in elephantids as in humans (although fully functional in non-human primates).</p> <p>Conclusion</p> <p>The data suggest that the coding sequence of the <it>FGF5 </it>gene is not the critical determinant of hair length differences among elephantids. The results are discussed in the context of hairlessness among mammals and in terms of the potential impact of large body size, subarctic conditions, and an aquatic ancestor on hair cover in the Proboscidea.</p

New records of Holocene polar bear and walrus (Carnivora) in the Russian Arctic

This article discusses recent finds of Holocene polar bear and walrus from the northern regions of Russia. The ulna of a polar bear was found on Vaygach Island and radiocarbon dated to 1,971 +/- 25 BP (OxA-23631). This calibrates to 430-540 AD, taking into account the marine reservoir effect. The size of the bone is similar to that of a recent Ursus maritimus. The locality of the fossil bone is within the modern species range, which developed about two millennia ago. In 2014 a walrus tusk was found on the coast of New Siberia Island and is radiocarbon dated to 5,065 +/- 35 BP (GrA-62452). This calibrates to 3,510-3,370 BC, taking into account the marine reservoir effect. Its size and morphology are identical to that of an adult male of the subspecies Odobenus rosmarus laptevi. This subspecies populates the eastern parts of the Kara Sea, the entire Laptev Sea and the western parts of the East Siberian Sea. This new discovery could mean that populations of O. rosmarus laptevi inhabited the waters near the New Siberian Islands during the Middle Holocene, and that the present-day coastline of the Siberian Arctic Islands was already formed at that time

Evolutionary history and palaeoecology of brown bear in North-East Siberia re-examined using ancient DNA and stable isotopes from skeletal remains

Over 60% of the modern distribution range of brown bears falls within Russia, yet palaeoecological data from the region remain scarce. Complete modern Russian brown bear mitogenomes are abundant in the published literature, yet examples of their ancient counterparts are absent. Similarly, there is only limited stable isotopic data of prehistoric brown bears from the region. We used ancient DNA and stable carbon (δ13C) and nitrogen (δ15N) isotopes retrieved from five Pleistocene Yakutian brown bears (one Middle Pleistocene and four Late Pleistocene), to elucidate the evolutionary history and palaeoecology of the species in the region. We were able to reconstruct the complete mitogenome of one of the Late Pleistocene specimens, but we were unable to assign it to any of the previously published brown bear mitogenome clades. A subsequent analysis of published mtDNA control region sequences, which included sequences of extinct clades from other geographic regions, assigned the ancient Yakutian bear to the extinct clade 3c; a clade previously identified from Late Quaternary specimens from Eastern Beringia and Northern Spain. Our analyses of stable isotopes showed relatively high δ15N values in the Pleistocene Yakutian brown bears, suggesting a more carnivorous diet than contemporary brown bears from Eastern Beringia

Past climate and continentality inferred from ice wedges at Batagay megaslump in the Northern Hemisphere’s most continental region, Yana Highlands, interior Yakutia

Ice wedges in the Yana Highlands of interior Yakutia – the most continental region of the Northern Hemisphere –were investigated to elucidate changes in winter climate and continentality that have taken place since the Middle Pleistocene. The Batagay megaslump exposes ice wedges and composite wedges that were sampled from three cryostratigraphic units: the lower ice complex of likely pre-Marine Isotope Stage (MIS) 6 age, the upper ice complex (Yedoma) and the upper sand unit (both MIS 3 to 2). A terrace of the nearby Adycha River provides a Late Holocene (MIS 1) ice wedge that serves as a modern reference for interpretation. The stable-isotope composition of ice wedges in the MIS 3 upper ice complex at Batagay is more depleted (mean δ18O about−35‰) than those from 17otherice-wedge study sites across coastal and central Yakutia. This observation points to lower winter temperatures and therefore higher continentality in the Yana Highlands during MIS 3. Likewise, more depleted isotope values are found in Holocene wedge ice (mean δ18O about−29‰) compared to other sites in Yakutia. Ice-wedge isotopic signatures of the lower ice complex (mean δ18O about −33‰) and of the MIS 3–2 upper sand unit (mean δ18O from about−33‰ to−30‰) are less distinctive regionally. The latter unit preserves traces of fast formation in rapidly accumulating sand sheets and of postdepositional isotopic fractionation