
Pleniglacial varves (?), postglacial alluvium and peat in the Cleurie valley (Vosges, 88)
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Pleniglacial varves (?), postglacial alluvium and peat in the Cleurie valley (Vosges, 88)
Research topics in “Fluvial chronometers” globally aim to reconstruct the Quaternary evolution of selected fluvial systems and to better understand the complex interactions between tectonics and climate (and man-induced impact on shorter timescales) that drive their evolution through time. At the crossroads of fluvial geomorphology and Quaternary geochronology, we focus on:
Thanks to long-lasting collaborations with dedicated laboratories (e.g. CEREGE/ASTER) and scientific experts, the most usual dating methods are threefold: in situ cosmogenic nuclides, luminescence (OSL/IRSL) and electron spin resonance (ESR). Fluvial chronometers primarily involve physical geographers within the LIVE (UMR 7362).
Dr. Gilles RIXHON, geomorphologist, geochronologist Université de Strasbourg |