Slyusarchuk I. The Late Holocene evolution of Zbruch region soils.

System research is carried out the dissertation for the first time for territory of Ukraine buried under Trayan mound of soils. It is revealed, that about 2500-3000 years ago there were changes of a climate from steppe aside more humidity wood (forest-steppe) to respective transformation of vegetation - from steppe (meadow -steppe) to wood (forest-steppe). Therefore for the period of building of earthen mound in a soil cover of Dnister region prevailed chernozem soils. Now here grey wood soils are extended, mainly podzolized soil. Properties buried under Trayan mound of soils essentially differ from modern background which developed naturally.