ad th la record from Greenland Ice Core GISP2 show a close correlation of sea-surface water conditions and deep-sea contouritic sedimentation in the Gulf of Cadiz with Northern Hemisphere climate variability on millennial timescales. A high MOW velocity Dansgaard-Oeschger (D-O) stadials and intersta...

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Other Authors: The Pennsylvania State University CiteSeerX Archives
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.9091
http://www.epoc.u-bordeaux.fr/indiv/Zaragosi/Toucanne_et_al_2007a.pdf
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Summary:ad th la record from Greenland Ice Core GISP2 show a close correlation of sea-surface water conditions and deep-sea contouritic sedimentation in the Gulf of Cadiz with Northern Hemisphere climate variability on millennial timescales. A high MOW velocity Dansgaard-Oeschger (D-O) stadials and interstadials been recognized as far south as the Portuguese margin