Regional specificity of the climatic evolution of soils in the southern part of Eastern Europe in the second half of the Holocene

Abstract

The analysis of characteristic features of chernozems and chestnut soils of different ages that have been formed in the south of the East European Plain in the past 5000 years attests to the spatial and temporal heterogeneity of the rate and direction of pedogenetic processes, i.e., to the metachronous development of the soil cover