“…The determination of terrigenous particle provenance, of both eolian or riverine input, in Mediterranean marine sediments has, in general, been based on geochemical and mineralogical data (e.g., Coudé-Gaussen et al, 1987;Foucault and Mélières, 2000;Wehausen and Brumsack, 2000;Caquineau et al, 2002;Weldeab et al, 2002aWeldeab et al, , 2002bWeldeab et al, , 2003Díaz-Hernández et al, 2011;Formentti et al, 2011) as well as on remote sensing methods, analysis of surface dust observations, back-trajectory analysis, and the use of mineral tracers (e.g., Goudie and Middleton, 2001;Laurent et al, 2008). Radiogenic isotopes (Sr, Nd, Pb) are likewise powerful tracers for identifying and characterizing source areas of terrigenous material, which may in turn give us additional information about the provenance and transport mechanisms (e.g., Grousset et al, , 1992Grousset et al, , 1998Revel et al, 1996;Tütken et al, 2002;Grousset and Biscaye, 2005;Jullien et al, 2007;Cole et al, 2009;Box et al, 2011;Meyer et al, 2011;Stumpf et al, 2011;Scheuvens et al, 2013).…”