Current Research on the Gravettian of the Swabian Jura

Abstract

Abstract: The Gravettian of the Swabian Jura developed roughly 30,000 years ago, and no clear stratigraphic break separates the lowest Gravettian from the uppermost Aurignacian deposits which also date to roughly 30,000 years ago. A chronological reversal in the radiocarbon sequence at Hohle Fels could reflect taphonomic processes at the site or peaks in radiocarbon production. Unlike the Aurignacian that is well documented in both the Lone and Ach Valleys, the Gravettian is found primarily in the Ach Valley, where particularly rich assemblages are known from sites including Brillenhöhle, Hohle Fels and Geißenklösterle. After 27,000 BP evidence for Gravettian occupations in the region decreases and only scant traces of occupation are visible during the Last Glacial Maximum. As research and excavations proceed, a coherent picture of the Gravettian of the Swabian Jura is beginning to emerge. Future work needs to address patterns of variability and cultural change during the Gravettian.

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