A5044438521- Evolution and Paleontology Studies
- Pleistocene-Era Hominins and Archaeology
- Geology and Paleoclimatology Research
- Ecology and biodiversity studies
- Wildlife Ecology and Conservation
- Archaeology and ancient environmental studies
- Geological Studies and Exploration
- Environmental and Biological Research in Conflict Zones
- Animal Ecology and Behavior Studies
- Geotechnical and Geomechanical Engineering
- Bat Biology and Ecology Studies
- Marine and environmental studies
- Methane Hydrates and Related Phenomena
- Yersinia bacterium, plague, ectoparasites research
- Animal Diversity and Health Studies
- Lichen and fungal ecology
- Identification and Quantification in Food
- Morphological variations and asymmetry
- Isotope Analysis in Ecology
- Genetic diversity and population structure
- Geochemistry and Geologic Mapping
- Soil and Environmental Studies
- Aquatic Invertebrate Ecology and Behavior
- Geological Modeling and Analysis
National Research Tomsk State University
2014-2024
V.S. Sobolev Institute of Geology and Mineralogy
2020
Queen's University Belfast
2016-2020
S. Toraighyrov Pavlodar State University
2016
Pavlodar State Pedagogical University
2016
Abstract The present phylogeographic pattern of red deer in Eurasia is not only a result the contraction their distribution range into glacial refugia and postglacial expansion, but probably also an effect replacement some s.l. mtDNA lineages by others during last 50 000 years. To better recognize this process, we analysed 501 sequences cytochrome b, including 194 ancient 75 contemporary samples newly obtained for study. inclusion 161 radiocarbon-dated enabled us to study phylogeny temporal...
The history and palaeoecology of the steppe bison (
skeletons or even their articulated fragments are rare.Occasionally, the remains represent postcranial (Shpansky, unpublished data).In West Siberian Plain, only three relatively complete bison have been discovered to date.These include records in sites of Vladimirskaya mine (Tom River, Kemerovo Region), Grigorievka Village (Irtysh Pavlodar and Krasniy Yar (Ob Tomsk Region; Fig. 1).The burial was described by P.M. Ryzhkov (1927).The skeleton located diagonally layered alluvial sands at a...
Climatic oscillations are considered primary factors influencing the distribution of various life forms on Earth. Large species adapted to cold climates particularly vulnerable extinction due climate changes. In our study, we investigated whether temperature increase since Late Pleistocene and contraction environmental niche during Holocene were main contributing decreasing range moose (Alces alces) in Europe. We also examined there significant differences conditions between areas inhabited...
Muskox Ovibos moschatus is a Pleistocene relic, which has survived only in North America and Greenland. During the Pleistocene, it was widely distributed Eurasia America. To evaluate its morphological variability through time space, we conducted an extensive morphometric study of 217 Praeovibos skull remains. The analyses showed that skulls grew progressively wider from sp. to O. moschatus, while recent facial regions turned narrower shorter. We also noticed significant geographic...
A new locality of fossil mammals near Kozhamzhar in Pavlodar Priirtysh Region has been described. The article provides the description quaternary sediments section found outcrop Kozhamzhar. In Karginian Age (MIS 3) alluvial deposits described we remains Elasmotherium sibiricum, Mammuthus ex gr. trogontherii-chosaricus, primigenius, Bison sp. AMS Radiocarbon dating skull gave a young age-26038±356 BP (UBA-30522). sibiricum exceeds size from Eastern Europe. lower jaw elephant, considering and...
ВОПРОСЫ ПАЛЕОЗООГЕОГРАФИИ НОСОРОГА МЕРКА (STEPHANORHINUS KIRCHBERGENSIS JÄGER 1839) (RHINOCEROTIDAE, MAMMALIA) А.В. ШпанскийНациональный исследовательский Томский государственный университет
Ursus arctos is a large carnivore and common species for Western Siberia. The earliest traces of it date back to the Middle Pleistocene. During Holocene, its population grew range significantly extended northwards. modern West Siberian habitat lies between 55° 67°N, dynamics are being affected by human activity climate change. beginning twenty-first century has been marked growth brown bear occurrence in unusual habitats. Earlier studies genetic structure prove existence Pleistocene refugium...
Abstract New data were obtained for the Chulym River basin in southeastern part of West Siberian Plain, one understudied parts Siberia terms age and composition carbon nitrogen stable isotopes Late Pleistocene megafauna. The 14 C dates from Sergeevo outcrop, most complete section Quaternary deposits region, are mostly greater than ~30 550 bp. Other localities yielded values range >44 500 to ~19 300 finite date ~42 270 bp Khozarian steppe elephant ( Mammuthus trogontherii chosaricus )...
А.В. Шпанский, С
А.В. Шпанский, Д.Г
Cases of variations in the morphology isolated upper teeth M3 Mammuthus primigenius (Blumenbach, 1799) from south-east West Siberia and Yakutiya are described. The anomaly M. tooth is expressed changing crown shape position dental plates M3. Development was probably associated with a delay loosing previous generation (M2) disorder formation at stage its mineralization. Two Novosibirsk Province characterized by wearing surface root shape. One them shows two surfaces parallel to initial...
New data on the timing of maximum distribution and diet Ovibos moschatus in south Siberia Late Pleistocene are presented.The southern border range musk ox West Siberian Plain during Karginian time (Denekamp Interstadial, DEN) was located Tomsk Ob' River region.During cooling Sartanian (LGM), boundary limited by Minusinsk Depression foothill plain Altai Mountains.Musk oxen region had a normal similar to that reindeer, slightly different from modern ox.The both oxen, it close horses woolly...
ABSTRACT We report a new series of radiocarbon ( 14 C) dates on the MIS 3 megafauna for previously poorly studied region southeastern West Siberia. Some species, like woolly mammoth and rhinoceros, Pleistocene bison horse, existed throughout (ca. 29–59 ka cal BP); cave hyaena is dated to ca. 46,400 BP. The very late C Khozarian steppe elephant Mammuthus trogontherii chosaricus ), 45,100–45,400 BP, may indicate survival this species in Siberia up 3. More work needed confirm or reject...