Margarita Alexandrovna Lazareva

Margarita Al. Lazareva
V.V. Dokuchaev Central Museum of Soil Science
E-mail: margoflams@mail.ru
ORCID ID: https://orcid.org/0000-0002-5791-110X
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Paleosol record of the transition thermochron MIS5 – MIS4 in the Belaya gora section (the Vakh river, West Siberia)Moscow University Bulletin. Series 17. Soil science. 2025. N 4.
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Paleopedological studies were conducted on the territory of the Kostenkovsko-Borshchevsky district. The K12 ancient human site is a reference section for regional studies of paleopedology, paleoecology, geological and cultural sequences. K12 contains a complete series of cultural layers related to the first part of MIS-3 in the range of 53–42 thousand years BP. This study is a continuation of previously conducted work on the K1 site, located on the opposite side of the “Pokrovsky Log” balka. In excavation K12, 16 lithological layers were identified, differing in structure, composition and properties. The material composition of the sediments is represented by chalk eluvium, which forms the sides of the balka, and loess-like loams of the watershed. Deposits with different proportions of chalk and loam were formed in the aqueous and aerial phases of sedimentation. In the excavation, about 5 m deep, three buried soils were found. The age of the lower one is about 50 thousand years BP. Cultural layers are confined to paleosols. Paleosols are an indicator of breaks in sedimentation. Four soil-sedimentary complexes were identified in the excavation. A description of the processes and the chronological sequence of their formation is given. The conducted research opens up new aspects in the study of buried soils of gully sedimentary complexes.Keywords: paleosols; cultural layers; soil-sedimentary complexes; chronology; Kostenki-Borshchevsky district; climate
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