Analysis of Migration Processes due to Environmental Conditions between 40,000 and 14,000 a BP in the Balkan region through Luminescence Dating

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This PhD topic lies within the B1 project, which deals with the paleoenvironmental conditions during modern human migration through southeastern Europe. A multi-proxy approach combining sedimentology, geochemistry, rock magnetism and luminescence dating is applied on loess-paleosol sequences on geoarchives in Hungary, Serbia and Romania.

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First results from Achenheim, France concerning the paleoenvironmental conditions between 40,000 and 14,000 a BP

zens_krauß_bannerDuring the Aurignacian (35,000 – 30,000 BP) Homo sapiens arrived for the first time in the Rhineland and recolonized the region after the Last Glacial Maximum (LGM) in the Magdalenian (20,000 – 14,000 BP). The D1 Project is part of the “Collaborative Research Centre 806 (CRC 806) – Our Way To Europe – Culture-Environment Interaction and Human Mobility in the Late Quaternary“ and focuses on reconstructing environmental conditions during the last glacial cycle (40,000 – 14,000 BP) in connection with archaeological research on migration processes of Homo sapiens in Western and Central Europe.

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