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Titlebook: Reconstructing Ocean History; A Window into the Fu Fatima Abrantes,Alan C. Mix Book 1999 Springer Science+Business Media New York 1999 Atla

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978-1-4613-6883-0Springer Science+Business Media New York 1999
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The Overturning Circulation of the Glacial Atlanticantic Deep Water export (13Sv). We find evidence for substantially reduced flow relative to today (17Sv), especially at intermediate depths. The simplest explanation for the reduced flow is a severe reduction in the strength of the meridional overturning circulation during the Last Glacial Maximum.
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Deconvolving Glacial Ocean Carbonate Chemistry from the Planktonic Foraminifera Carbon Isotope Recorractice of analyzing multiple shells from each interval in a core should average out these vital effects. Hence, lower glacial δ.C values are thought to reflect changes in mean ocean δ.C (Shackleton, 1977).
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