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doi: 10.24412/2687-1092-2022-9-339-343 1 Saint-Petersburg State University, St. Petersburg, Russia 2 Herzen State Pedagogical University of Russia, St. Petersburg, Russia 3 Institute of Geography, Russian Academy of Sciences, Moscow, Russia
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Abstract. The problem of the duration and temporal boundaries of the Mikulino Interglacial does not currently has a final solution. Therefore, it is necessary to conduct detailed comprehensive studies of a large number of sections of the Mikulino sediments using the methods of their paleobotanical study and 230Th/U dating. In September 2022, field work was carried out on the Verkhniye Nemykary section on the Dnieper River bank in the Smolensk region. Samples of organic-rich deposits (every 2-4 cm) from 2 peat layers were taken for palynological and carpological analyzes and 230Th/U dating. The results of further study of the collected samples will make it possible to clarify the chronology of the Last Interglacial deposits formation on the Russian Plain. Keywords: Northwest Russian Plain, Mikulino interglacial, geochronology, uranium-thorium dating, spore-pollen analysis, paleocarpology
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Cite this article:
Koroleva T.A., Maksimov F.E., Kuznetsov V.Yu., Baranov D.V., Petrov A.Yu., Grigoriev V.A. 2022. Geochronology of the Mikulino interglacial according to the study of the northwestern Russian Plain sections // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. Issue 9. P. 339-343. doi: 10.24412/2687-1092-2022-9-339-343
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