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Glacial erosion dynamics in a small mountainous watershed (Southern French Alps): A source-to-sink approach
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文摘
We used εNdεNd to track the sediment routing in the Var system over the last 50 kyr. Glaciers are the main driver of the glacial/interglacial cycle of sediment flux. The estimated sediment fluxes are 2.5 times higher during the LGM than today. A major change in turbidite activity and sources is observed between 19 and 16 ka. The glacial sediment transfer to the sea depends on the catchment's characteristics.

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