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A quantitative analysis of planktonic foraminifera, coupled with petrophysical and paleomagnetic measurements and 14 C-AMS calibrations, was carried out on a deep core recovered in the Sardinia Channel (Western Mediterranean Sea), during the CIESM Sub2 survey, providing an integrated stratigraphic time-framework over the last 80kyr. Significant changes in the quantitative distribution of planktonic...
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