Published December 31, 2013
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Fig. 1 in 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
Description
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.
Notes
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
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- Journal article: 10.4467/16890027AP.13.0015.1112 (DOI)
- Journal article: urn:lsid:plazi.org:pub:FFAD12797F6BFFE59710D25FFFD47D05 (LSID)
- Journal article: https://zenodo.org/record/13193225 (URL)