RESEARCH PAPERS : A magnetic investigation of a Late Quaternary loess/palaeosol record in Siberia

Astronomy and Astrophysics – Astronomy

Scientific paper

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Loess, Magnetic Susceptibility, Palaeosol, Quaternary, Siberia

Scientific paper

A Late Quaternary loess/palaeosol sequence at Kurtak in the Yenisey River valley, southern Siberia, has been studied magnetically. The 34 m section (340 samples) exhibits variations in magnetic susceptibility which can be correlated with oxygen isotope stages 1-7. A detailed sampling of stage 5 (a further 209 samples) permits the identification of substages 5a-e. The susceptibility variations themselves are in the opposite sense to that found in the classic sections of the Chinese Loess Plateau, but are in agreement with the `wind-intensity' model which has been put forward to explain similar findings in loess sequences in Alaska. Published results for the susceptibility of magnetite imply volume fractions of ~0.2 per cent in glacial stages 2 and 4, dropping to ~0.05 per cent in stages 1, 3 and 5. These fluctuations match the aeolian flux variations observed in core V21-146 from the north Pacific. Even though the warmer intervals are characterized by lower susceptibilities, the observed frequency dependence of susceptibility indicates that new magnetic material is produced as a result of pedogenesis during interglacial and interstadial times.

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