Paleontologic Technique for Defining Ancient Ocean Currents

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Science  14 May 1965:
Vol. 148, Issue 3672, pp. 943-946
DOI: 10.1126/science.148.3672.943-a


Subtraction from the new data, of a quadratic surface fitted to the taxonomic diversity data of recent planktonic foraminifera yields a residual surface closely related to ocean current systems. This technique could be applied to fossil materials to develop knowledge of ocean circulation patterns during glacial and interglacial climatic episodes.

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