Abstract
A record of biogenic opal production in the subtropical Atlantic Ocean fuels the theory that ocean circulation, rather than winds, drove the release of carbon dioxide from deep marine waters at the end of the last ice age. See Letter p.495 ELISABETH
Cite
CITATION STYLE
APA
Sikes, E. (2013). How the ocean exhales. Nature, 495(7442), 454–455. https://doi.org/10.1038/495454a
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