Published as part of Garcia, Jennifer, Mojtahid, Meryem, Howa, Hélène, Michel, Elisabeth, Schiebel, Ralf, Charbonnier, Céline, Anschutz, Pierre & Jorissen, Franciscus J., 2013, Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay, pp. 161-180 in Acta Protozoologica 52 (3) on page 163, DOI: 10.4467/16890027AP.13.0015.1112, http://zenodo.org/record/13193225

Fig. 1. Study area bathymetry (Liu and Dittert 2010), surface circulation patterns (Koutsikopoulos et al. 1996), and location of the study Site WH (44°33′N, 2°45′W; 2,000 m water depth). The position of Site KS10b (Mojtahid et al. 2013) is marked by a white square. IPC – Iberian Poleward Current, ENACW – Eastern North Atlantic Central Waters.