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Inferring past current contributions to the deep Atlantic using Nd isotope records

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Today the Nd isotope signature of deep currents in the Atlantic relates to their direction of flow. I will use Nd isotope records, reconstructed from sediment cores from the NW, NE and S Atlantic, to infer past variations in current direction. I will then discuss the possibility of calculating past watermass mixing using a combination of Nd and carbon isotope records.

This talk is part of the BPI Seminar Series series.

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