Paleosols and climate of the steppe zone in early iron age: Identifying short term warming of climate on slightly-sensors soils

Studies on paleosols under an archaeological landmark of a rare type (a complex of kurgans with “whiskers”) dating from the Early Iron Age (the fourth century AD) have been performed in the steppe zone of the Transural Plateau. The size and shape of third-order soil polygons under stony ridges (“whi...

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Main Author: Liudmila N. Plekhanova
Format: Article
Language:English
Published: Federation of Eurasian Soil Science Societies 2014-08-01
Series:Eurasian Journal of Soil Science
Subjects:
Online Access:http://dergipark.ulakbim.gov.tr/ejss/article/view/5000078325/5000072548
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author Liudmila N. Plekhanova
author_facet Liudmila N. Plekhanova
author_sort Liudmila N. Plekhanova
collection DOAJ
description Studies on paleosols under an archaeological landmark of a rare type (a complex of kurgans with “whiskers”) dating from the Early Iron Age (the fourth century AD) have been performed in the steppe zone of the Transural Plateau. The size and shape of third-order soil polygons under stony ridges (“whiskers”) between the kurgans have been described in detail. The results have shown that the paleosol under the kurgans erected at the turn of the Late Sarmatian and Hun times (1600 years ago) is characterized by a higher humus content and deeper location of the carbonate horizon, compared to the recent soil. This indicates that an increase in atmospheric humidity took place in the fourth century AD.
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spelling doaj.art-4ae0ddaabb7d411f869f8ef88ef1caad2023-09-03T08:55:51ZengFederation of Eurasian Soil Science SocietiesEurasian Journal of Soil Science2147-42492014-08-0133220229Paleosols and climate of the steppe zone in early iron age: Identifying short term warming of climate on slightly-sensors soilsLiudmila N. Plekhanova0Institute of Physico-Chemical and Biological Problems of Soil Science, Pushchino, RussiaStudies on paleosols under an archaeological landmark of a rare type (a complex of kurgans with “whiskers”) dating from the Early Iron Age (the fourth century AD) have been performed in the steppe zone of the Transural Plateau. The size and shape of third-order soil polygons under stony ridges (“whiskers”) between the kurgans have been described in detail. The results have shown that the paleosol under the kurgans erected at the turn of the Late Sarmatian and Hun times (1600 years ago) is characterized by a higher humus content and deeper location of the carbonate horizon, compared to the recent soil. This indicates that an increase in atmospheric humidity took place in the fourth century AD.http://dergipark.ulakbim.gov.tr/ejss/article/view/5000078325/5000072548paleosolspaleoclimatesteppe zoneEarly Iron Age
spellingShingle Liudmila N. Plekhanova
Paleosols and climate of the steppe zone in early iron age: Identifying short term warming of climate on slightly-sensors soils
Eurasian Journal of Soil Science
paleosols
paleoclimate
steppe zone
Early Iron Age
title Paleosols and climate of the steppe zone in early iron age: Identifying short term warming of climate on slightly-sensors soils
title_full Paleosols and climate of the steppe zone in early iron age: Identifying short term warming of climate on slightly-sensors soils
title_fullStr Paleosols and climate of the steppe zone in early iron age: Identifying short term warming of climate on slightly-sensors soils
title_full_unstemmed Paleosols and climate of the steppe zone in early iron age: Identifying short term warming of climate on slightly-sensors soils
title_short Paleosols and climate of the steppe zone in early iron age: Identifying short term warming of climate on slightly-sensors soils
title_sort paleosols and climate of the steppe zone in early iron age identifying short term warming of climate on slightly sensors soils
topic paleosols
paleoclimate
steppe zone
Early Iron Age
url http://dergipark.ulakbim.gov.tr/ejss/article/view/5000078325/5000072548
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