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ABSTRACT An inverse method,is used to evaluate the information,contained,in sediment,data for the Atlantic basin during the Last Glacial Maximum,(defined here as the time interval 18–21 kyr before present). The data being considered,are an updated,compilation,of the isotopic ratios ,CDIC in the glacial Atlantic must be reduced,to increase the power,of the test.

On the Abyssal Circulation in the Glacial Atlantic