International audienceIt is a common practice to reconstruct glacier activity from lake sediment records. Such an approach is generally applied to proglacial lakes. However in some cases, terrigenous inputs from glaciated areas are dominating enough to make distant sedimentary basins sensitive to glacier fluctuations. This is the case in Lake Bourget, located on the course of the French higher Rhône, 250km downstream the Mont Blanc Massif. Two Holocene-long sediment cores were studied, in order to reconstruct past terrigenous fluxes. We coupled a high resolution geochemical approach to a source-to-sink monitoring (isotope geochemistry and clay mineralogy) of sediment provenance in order to prove the main influence of glacier fluctuations up...