Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
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isotopic signatures. According to the role of MOW in the modern Atlantic thermohaline circulation, the reduction of the MOW after the closure of the Guadalhorce Corridor | isotopic signatures. According to the role of MOW in the modern Atlantic thermohaline circulation, the reduction of the MOW after the closure of the Guadalhorce Corridor | ||
might have resulted in a decreased NADW formation rate between 6.0 and 5.5 Ma weakening the AMOC and promoting northern hemisphere cooling. | might have resulted in a decreased NADW formation rate between 6.0 and 5.5 Ma weakening the AMOC and promoting northern hemisphere cooling. | ||
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<font size="2">([http://www.agu.org/pubs/crossref/2012/2012PA002309.shtml ABSTRACT]) | <font size="2">([http://www.agu.org/pubs/crossref/2012/2012PA002309.shtml ABSTRACT]) | ||
