Soil formation types and conditions during the last third of holocene in the Central-Tuvinian hollow

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The soil formation types and conditions during the last third of Holocene in the Central-Tuvinian hollow are revealed in the article. Paleo-soils analogues of Tuvinian modern soils were determined by means of organic and mineral interaction products notably by means of the humic substances specificity in sediments.

Holocene, tuva, central-tuvinian hollow, paleosoil, pedogenesis

Короткий адрес: https://sciup.org/14082147

IDR: 14082147

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