Publication Date:
2013-11-10
Description:
Article Upwelling of CO 2 from the Southern Ocean may have played a key role in deglacial warming, but marine sediment studies are hindered by inaccurate chronologies. Siani et al . present new surface reservoir 14 C ages derived from tephra and show that deglacial CO 2 escape was synchronous with Antarctic warming. Nature Communications doi: 10.1038/ncomms3758 Authors: Giuseppe Siani, Elisabeth Michel, Ricardo De Pol-Holz, Tim DeVries, Frank Lamy, Mélanie Carel, Gulay Isguder, Fabien Dewilde, Anna Lourantou
Electronic ISSN:
2041-1723
Topics:
Biology
,
Chemistry and Pharmacology
,
Natural Sciences in General
,
Physics
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