Jungpleistozäner Löß und fossile Böden in Niederösterreich

Friedrich Brandtner
Up to now in Lower Austria 82 Upper Pleistocene loess sections with fossil soils were examined. It has been found out that the individual loess deposits (layers) are already primarily differentiated in their lithologic character by prevailing dust contents due to regional and local conditons and by similar climatic differences in their general habitus.The loess deposits in the area east of the Mannhartsberg (in the Weinviertel, March-feld, Wiener Becken), mostly lying on a calcareous tertiary...