1. valley runoff discussed in this study. The respective influence of the upstream (q) vs. downstream (r) FM drainage system for sediments carried out up to the Bay of Biscay is roughly summarized through a through a blue color gradient: the darker the color, the stronger the influence. Figure 8: Synthesis of main results discussed in this study;Fersi;Data from cores MD13-3438 (d) and MD95-2002 (e, f), presented and described in Figure 2 (cf. e, f, g in Fig. 2), are plotted along main palynological data : dinocyst (g) and pollen (h), as well as data from literature: a) Greenland ? 18 O NGRIP record (GICCO05; Svensson et al., 2008), b) insolation data,1991
2. The W�rmian Late-glacial in Iowland Switzerland;B Ammann;Journal of Quaternary Science,1994
3. Towards understanding potential atmospheric contributions to abrupt climate changes: characterizing changes to the North Atlantic eddy-driven jet over the last deglaciation;H J Andres;Clim. Past
4. Heinrich events" (& sediments): a history of terminology and recommendations for future usage;J T Andrews;Quat. Sci. Rev,2018
5. Terrigenous fluxes at the Celtic margin during the last glacial cycle;G Auffret;Mar. Geol,2002