Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4725571 | Quaternary Geochronology | 2008 | 13 Pages |
Abstract
The archaeological site of Payre (France) yielded Middle Palaeolithic layers with Neanderthal remains, which are partly bracketed by two stalagmitic flowstones. To obtain a precise chronological framework for the human occupation and the faunal remains of this site, several dating methods were used: uranium-series (U-series by alpha spectrometry and TIMS) and electron spin resonance (ESR) on stalagmitic flowstones, combined ESR/U-series on teeth and bones, and thermoluminescence (TL) on burnt flints. Most of the ages obtained for levels H to C range from â¼300 to â¼140Â ka. The age-spread obtained for the anthropic (burnt flints) and faunal remains (bones and teeth) suggests that the dated levels represent several human occupation periods, near the transition from MIS8 to MIS7 (levels G-F) and from MIS6 to MIS5 (levels D-E).
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
H. Valladas, N. Mercier, L.K. Ayliffe, C. Falguères, J.-J. Bahain, J.-M. Dolo, L. Froget, J.-L. Joron, H. Masaoudi, J.-L. Reyss, M.-H. Moncel,