Cryogenic-lateral hypothesis of the formation of the parent rock of soddy-podzolic soils using the example of the Ryshkovo paleosol (mis 5e) in the Taneyev quarry, Kursk Region

Abstract

The Ryshkovo paleosol of the Mikulino Interglacial (MIS 5e), Late Moscow loess (MIS 6), and buried small erosional landforms were studied in the Taneyev Quarry of Kursk oblast, in the center of the East European Plain. Macro- and micromorphological and palynological analyses of the soil samples were carried out, and the OSL age and physicochemical properties were determined