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Stable isotopes of carbon (δ13C) in terrestrial geological materials (paleosol humus and carbonates) as well as fossil bones (collagen and tooth enamel) are established as highly specific records on paleoenvironmental characteristics. It was assumed that comparing the results of different types of materials on regional or local scales provides more accurate and reliable reconstructions and even opens...
Paleosols, surface soils, mammal bone remains of Late Pleistocene and Holocene deposits of the rock shelter Svetly were studied. The joint analysis of paleontological and paleosol data was carried out. The paleoenvironment underwent considerable transformation, which resulted in changes in type of soil formation and in the structure of the mammal community. Cryoarid conditions with mammoth complex...
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