The development of chernozems on the Dniester-Prut interfluve in the Holocene

The development of forest-steppe and steppe chernozems on the Dniester-Prut interfluve in the Holocene was studied on the basis of data on the paleosols buried under archaeological monuments of different ages. The parameters of the mathematic models of the development of the soil humus horizons in d...

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Veröffentlicht in:Eurasian soil science 2013-05, Vol.46 (5), p.491-504
Hauptverfasser: Lisetskii, F. N., Goleusov, P. V., Chepelev, O. A.
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creator Lisetskii, F. N.
Goleusov, P. V.
Chepelev, O. A.
description The development of forest-steppe and steppe chernozems on the Dniester-Prut interfluve in the Holocene was studied on the basis of data on the paleosols buried under archaeological monuments of different ages. The parameters of the mathematic models of the development of the soil humus horizons in different subtypes of chernozems were calculated. They were used to determine the rate of this process and the age of the soils formed on the surface of Trajan’s lower rampart. The climate-controlled changes in the character of the soil’s development in the Late Holocene were differently pronounced in the different subtypes of chernozems. The suggested differentiation of the trends in the development of the humus horizon in the studied chernozems corresponds to the differences in the soil-forming potential of particular areas (as judged from the energy consumption for pedogenesis).
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subjects Analysis
Archaeology
Decomposing organic matter
Earth and Environmental Science
Earth Sciences
Energy consumption
Genesis and Geography of Soils
Geotechnical Engineering & Applied Earth Sciences
Grasslands
Holocene
Humus
Paleosols
Soil formation
Soil mechanics
Soil sciences
Steppes
title The development of chernozems on the Dniester-Prut interfluve in the Holocene
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