The methods from geochemistry of stable isotopes, and spore-pollen and paleopedological data on climate humidification variation have been used to reveal three time intervals: the beginning of the 4th millennium BC, and the 3rd-4th and 8th-14th centuries AD when the indices of local climate changes showed oppositely directed tendencies, which suggests a contribution of the anthropogenic factor (pasture digression) to the modification of vegetation of the landscapes under investigation. © 2009.

Reconstructing the anthropogenic aridization of landscapes in antiquity and in the Middle Ages from isotopic data / Ryskov, Yag.; Demkin, V. A.; Nikolayev, V. I.; Oleinik, S. A.; Iacumin, P.. - In: GEOGRAPHY AND NATURAL RESOURCES. - ISSN 1875-3728. - 30:2(2009), pp. 187-193. [10.1016/j.gnr.2009.06.017]

Reconstructing the anthropogenic aridization of landscapes in antiquity and in the Middle Ages from isotopic data

Iacumin P.
2009-01-01

Abstract

The methods from geochemistry of stable isotopes, and spore-pollen and paleopedological data on climate humidification variation have been used to reveal three time intervals: the beginning of the 4th millennium BC, and the 3rd-4th and 8th-14th centuries AD when the indices of local climate changes showed oppositely directed tendencies, which suggests a contribution of the anthropogenic factor (pasture digression) to the modification of vegetation of the landscapes under investigation. © 2009.
2009
Reconstructing the anthropogenic aridization of landscapes in antiquity and in the Middle Ages from isotopic data / Ryskov, Yag.; Demkin, V. A.; Nikolayev, V. I.; Oleinik, S. A.; Iacumin, P.. - In: GEOGRAPHY AND NATURAL RESOURCES. - ISSN 1875-3728. - 30:2(2009), pp. 187-193. [10.1016/j.gnr.2009.06.017]
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11381/2912851
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