Changes in continental precipitation patterns may drastically reshape landscapes and living-environments of humans in terms of geomorphological settings and sedimentological regimes. Dust based quaternary sediment archives like widespread loess-palaeosol-sequences (LPS) record climatic changes and provide key geomorphological and sedimentological information. These records are also essential for comprehending precipitation changes across continents and associated terrestrial system responses. Currently, precipitation quantities strongly vary along a W-E gradients across Europe, but this pattern is likely to have changed dramatically in the past – especially when the Nordic ice-sheets started to grow upon their massive extend during their glacial maxima. Here we present first precipitation estimates considering a suite of established chemical (δ13C of the total organic carbon) and magnetic measures for the Nantois section (northern Brittany, France) covering the Saalian (penultimate glaciation) with its cold and harsh conditions and the Eemian (last interglacial), when the climate was globally warmer than today. We discuss our sedimentological results considering the special geomorphological setting of the Nantois section and its role regarding the reaction to dry-moister cycles. Based on this, we demonstrate the advantage of combining sedimentological and geomorphological perspectives when aiming at a more holistic landscape understanding.