Palaeoclimatic record in the loess–palaeosol sequence of the Strelitsa type section (Don glaciation area, Russia) deduced from rock magnetic and palynological data
Identifieur interne : 000E86 ( Main/Exploration ); précédent : 000E85; suivant : 000E87Palaeoclimatic record in the loess–palaeosol sequence of the Strelitsa type section (Don glaciation area, Russia) deduced from rock magnetic and palynological data
Auteurs : Elena I. Virina [Russie] ; Friedrich Heller [Suisse] ; Stanislav S. Faustov [Russie] ; Nathalia S. Bolikhovskaya [Russie] ; Robert V. Krasnenkov [Russie] ; Tatyana Gendler [Russie] ; Ernie A. Hailwood [Royaume-Uni] ; Jozeph Hus [Belgique]Source :
- Journal of Quaternary Science [ 0267-8179 ] ; 2000-07.
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Abstract
Until now, palaeoclimatic reconstructions for the major stages in the development of the Quaternary loess–palaeosol sequence on the Russian Plain have been based on pedological, palynological and faunal (vertebrates and molluscs) analyses. In order to demonstrate the palaeoclimatic influence on the magnetic properties of this sequence, the magnetic susceptibility signature of the Strelitsa type section in the Upper Don basin is compared with a detailed landscape – climate reconstruction of loess and soil from palynological data. Large amplitude fluctuations of palaeoclimate and palaeoenvironment are reflected clearly in the lithology and in the rock magnetic properties, which usually are enhanced in wet and warm interglacial periods, but stay at low levels during cold glacial epochs. Palynological climate zonation, however, is sometimes in conflict with the pedologic–magnetic record. Strong climate fluctuations, as indicated by changing pollen assemblages, are not always paralleled by corresponding changes in lithology and/or rock magnetic properties. Alternatively, light coloured illuvial horizons with low magnetic signal sometimes appear to have formed during early stages of interglacials, and the top parts of some palaeosols apparently formed during glacial stages. Copyright © 2000 John Wiley & Sons, Ltd.
Url:
DOI: 10.1002/1099-1417(200007)15:5<487::AID-JQS512>3.0.CO;2-F
Affiliations:
- Belgique, Royaume-Uni, Russie, Suisse
- Angleterre, District fédéral central
- Moscou
- Université d'État de Moscou
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In order to demonstrate the palaeoclimatic influence on the magnetic properties of this sequence, the magnetic susceptibility signature of the Strelitsa type section in the Upper Don basin is compared with a detailed landscape – climate reconstruction of loess and soil from palynological data. Large amplitude fluctuations of palaeoclimate and palaeoenvironment are reflected clearly in the lithology and in the rock magnetic properties, which usually are enhanced in wet and warm interglacial periods, but stay at low levels during cold glacial epochs. Palynological climate zonation, however, is sometimes in conflict with the pedologic–magnetic record. Strong climate fluctuations, as indicated by changing pollen assemblages, are not always paralleled by corresponding changes in lithology and/or rock magnetic properties. 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