Abstract
The mineral composition of paleosols intercalated in series of young loess was determined. The following conclusions were drawn: 1) The mineralogical composition of the total soil showed correlation with the ecological conditions having prevailed during sedimentation. 2) The processes of soil formation can be described well by the mineral composition of the fraction of particle size less than 0.002 mm. It displays strong similarities in the fine-dispersed fractions of soils representing identical genetic types from different loess profiles. Since paleosols of identical type are assumed to have formed under similar climatic conditions, the latter can be characterized by the mineral composition of the fine-dispersed fraction.
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