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One of the ways to study the evolution of natural environment, in particular, the soil cover is a comprehensive study of soils buried under archaeological sites. Comparative analysis of the properties of paleosols buried in different historical epochs allows us to examine in detail the spatial and temporal dynamics of the natural environment and its components in time. The use of such comparative analysis is possible because the burial of soil under embankments of defensive ramparts, burial mounds and cultural lay...

Humid and arid climatic cycles during Sub-Atlantic time in the forest-steppe area of the East European Plain were studied based on soils buried under archaeological sites of different time. The shift of the boundary between steppe and forest patches is recorded in the shift of the studied soils: Luvic Greyzemic Fhaeozems of the forest patches and Luvic Chernozems under steppe environment. The complex research is based on archaeological investigation, assemblages of morphological (marco-, meso- and micromorphologic...