Closure of the Central American Isthmus and its effect on deep-water formation in the North Atlantic

Modern ocean thermohaline-driven circulation influences global climate by transporting heat to high latitudes 1,2 and by affecting the exchange of CO 2 between ocean and atmosphere 3 . North Atlantic Deep Water (NADW) plays a key role in this circulation, and Quaternary climate cycles have been link...

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Veröffentlicht in:Nature (London) 1997-03, Vol.386 (6623), p.382-385
Hauptverfasser: Burton, Kevin W., Ling, Hong-Fei, O'Nions, R. Keith
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Sprache:eng
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