Palaeoclimatic implications of the magnetic record from loess/palaeosol sequence Viatovo (NE Bulgaria)

Details Palaeoclimatic implications of the magnetic record from loess/palaeosol sequence Viatovo (NE Bulgaria) Palaeoclimatic implications of the magnetic record from loess/palaeosol sequence Viatovo (NE Bulgaria)

Dec 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007geoji.171.1036j&link_type=abstract

Geophysical Journal International, Volume 171, Issue 2, pp. 1036-1047.

Astronomy and Astrophysics

Astronomy

3

Bulgaria, Loess, Magnetite, Maghemite, Palaeosol, Rock Magnetism

Scientific paper

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).

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