Abstract:In this paper we focused on the micromorphology of the Late and Middle Pleistocene paleosols exposed in twelve loess-paleosol sequences sections in the central part of the East European Plain. Each studied paleosol complex known as Mesin (MIS 5), Kamenka (MIS 6 (8) -7 ( 9)), and Inzhavino (MIS 8 (10) -9 (11)) pedocomplexes (PCs) consists typically of two members, the earlier -main -phase of the soil development taking place during an interglacial, and the later one -at the subsequent interstadial time. Intergl… Show more
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