We report a new series of radiocarbon (14C) dates on the MIS 3 megafauna for a previously poorly studied region of southeastern West Siberia. Some species, like woolly mammoth and woolly rhinoceros, and Pleistocene bison and horse, existed throughout the MIS 3 (ca. 29–59 ka cal BP); cave hyaena is dated to ca. 46,400 cal BP. The very late 14C dates on Khozarian steppe elephant (Mammuthus trogontherii chosaricus), ca. 45,100–45,400 cal BP, may indicate the survival of this species in Siberia up to MIS 3. More work is needed to confirm or reject this suggestion. Previously, Khozarian steppe elephant was known in Siberia only at the beginning of the Late Pleistocene (MIS 5e).

Recent revision of the Pleistocene glaciation boundaries in northern Eurasia has encouraged the search for nonglacial geological records of the environmental history of northern West Siberia. We studied an alluvial paleosol-sedimentary sequence of the high terrace of the Vakh River (middle Ob basin) to extract the indicators of environmental change since Marine Oxygen Isotope Stage (MIS) 6. Two levels of the buried paleosols are attributed to MIS 5 and MIS 3, as evidenced by U/Th and radiocarbon dates. Palynological and pedogenetic characteristics of the lower pedocomplex recorded the climate fluctuations during MIS 5, from the Picea-Larix taiga environment during MIS 5e to the establishment of the tundra-steppe environment due to the cooling of MIS 5d or MIS 5b and partial recovery of boreal forests with Picea and Pinus in MIS 5c or MIS 5a. The upper paleosol level shows signs of cryogenic hydromorphic pedogenesis corresponding to the tundra landscape, with permafrost during MIS 3. Boulders incorporated in a laminated alluvial deposit between the paleosols are dropstones brought from the Enisei valley by ice rafting during the cold MIS 4. An abundance of eolian morphostructures on quartz grains from the sediments that overly the upper paleosol suggests a cold, dry, and windy environment during the MIS 2 cryochron.

Objective. The aim of this work was to study the prevalence and genetic diversity of Babesia in Ixodes persulcatus ticks and small mammals from Ural and Siberia in Russia. Methods. In total, 481 small mammals and 922 questing adult I. persulcatus from North Ural (Sverdlovsk region) and West Siberia (Novosibirsk region) were examined for the presence of Babesia by nested PCR based on the 18S rRNA gene. Results. Babesia microti of the ‘Munich’-type was found in 36·2% of blood samples of the small mammals from the Sverdlovsk region and B. microti of the ‘US’-type in 5·3% of the animals from the Novosibirsk region. Babesia DNA was not detected in 133 analysed I. persulcatus from the Sverdlovsk region; however, it was found in 24 of 789 ticks from the Novosibirsk region. Three distinct Babesia species were detected in I. persulcatus. B. microti ‘US’-type was identified in 10 ticks, Babesia closely related to B. divergens/B. capreoli in 2 ticks, and Babesia closely related to B. venatorum (EU1) in 12 ticks. Conclusion. To our knowledge, this is the first detection of Babesia sensu stricto in I. persulcatus ticks and of B. microti in I. persulcatus in the Asian part of Russia.