Environmental change indicated by a site-specific grain size ratio - the example of the Semlac loess-paleosol sequence (Romania)

Researchdata & Literature
Maintained by Janina Bösken
Created at 15.5.2015

Abstract

Loess sequences provide important and at least a partial continuous record of Quaternary palaeoenvironmental change. In addition, loess-palaeosol sequences provide valuable information concerning environmental change and climate evolution. It is customary to reconstruct such changes by means of grain sizes ratios. In this study, we calculated an site-specific grain size (GS) ratio (Schulte et al. in review) and compare this ratio with the common U-ratio (Vandenberghe et al.1985) and, in addition, with selected geochemical parameters. As an example we present the Middle to Late Pleistocene loess-paleosol section of Semlac in western Romania (MIS 10 – 1).

Bibliography

Schulte, P., Lehmkuhl, F., Kels, H., Klasen, N. (2014): Environmental change indicated by a site-specific grain size ratio - the example of the Semlac loess-paleosol sequence (Romania). Stefan del Mare University Press

authorSCHULTE, P. and LEHMKUHL, F. and KELS, H. and KLASEN, N.
keyP.SCHULTE2014
pages157-160
publisherStefan del Mare University Press
seriesLate Pleistocene and Holocene Climatic Variability in the Carpathian-Balkan Region
typeproceedings
urlhttp://georeview.ro/ojs/index.php/revista/article/view/242
year2014
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