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Climate of the Past
<p><strong>Abstract.</strong> A multiproxy study – coupling mineralogical, grain size and geochemical approaches – was used to tentatively retrace eolian and fluvial contributions to sedimentation in the Sicilian–Tunisian Strait since the last glacial. The eolian supply is dominant over the whole interval, excepted during the sapropel S1 when riverine contribution apparently became significant. Saharan contribution increased during the Bølling–Allerød, evidencing the persistence of aridity overdoi:10.5194/cp-9-1065-2013 fatcat:u2mdlwonprdmlnxr7kpnvrrsdi