Wind morpholithogenesis and climate rhythms of south-western Transbaikalye in the final of Neopleistocene and Holocene

Studies of the subaerial formations in the southwestern Transbaikalia ascertained the fact of wide occurrence of aeolian processes on fluvial and lacustrine-fluvial terraces different in age. Radiocarbon dates obtained on fossil soils suggest repeated climatic changes during the Holocene. The fact of self-induced overgrowing of naked sand surface as a result of reduced anthropogenic load at the turn of century suggests stable enough climatic conditions in the region through the last 200-250 years.