Loess and palaeosols on the High Terrace at Sierentz (France), and implications for the chronology of terrace formation in the Upper Rhine Graben |
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Authors: | Philippe Rentzel Frank Preusser Christine Pümpin Jean-Jacques Wolf |
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Institution: | 1. Institute for Prehistory and Archaeological Science, University of Basel, Spalenring 145, 4055, Basel, Switzerland 2. Institut für Geologie, Universit?t Bern, Baltzerstrasse 1 + 3, 3012, Bern, Switzerland 3. P?le d’Archéologie Interdépartemental Rhénan, 67600, Sélestat, France
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Abstract: | Pedological investigations in combination with luminescence dating have been used to reconstruct the genesis and chronology
of a sediment succession at Sierentz, France. The sequence comprises loess and palaeosols on top of gravel attributed to the
High Terrace of River Rhine. According to the dating results, three phases of soil development occurred during different warm
phases of Marine Isotope Stage (MIS) 7 (245–190 ka). Soil development on top of the gravel occurred either during early MIS
7 or during an earlier warm phase, possibly MIS 9. The results imply a minimum age of 250 ka for the formation of the High
Terrace in this part of the Upper Rhine Graben, contrary to previous assumptions that correlated gravel sheet deposition with
MIS 6 (ca. 150 ka). These results and recent findings at other sites suggest that the chronological setting of terrace formation
north of the Alps is much more complex than previously assumed. |
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