Abstract
The territorial specific character of the main stages of Holocene pedogenesis is demonstrated. The study uncovers the characteristic features of bioclimatic evolution of chernozemic and texture-differentiated soils of the Mid-Holocene into organo-accumulative (soddy) soils typical of contemporary landscapes. For the Mid-Late Holocene five stages of soil formation have been identified, which are interrupted by an intensification of denudation-accumulative processes as a consequence of global coolings.
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