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Palaeoclimatic implications of the magnetic record from loess/palaeosol sequence Viatovo (NE Bulgaria).
Авторы: Jordanova D., Hus J., Geeraerts P.
2007 г.
Geoph.J.Int.
Loess-palaeosol deposits in the lower Danube area represent the southeastern edge of the loess cover in Europe. Detailed rock magnetic investigations of the loess/palaeosol sequence in Viatovo in NE Bulgaria reveal that magnetite and maghemite of very fine superparamagnetic grain size are responsible for the magnetic enhancement of palaeosol units. A detailed palaeoclimatic record is obtained through high-resolution measurements of magnetic susceptibility, frequency dependent magnetic susceptibility and CaCO3 content. Magnetic proxies indicate a more warm and humid climate during the development of the older palaeosol units (S4–S6).
Файл: 612.pdf
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