Synchronous deglacial thermocline and deep-water ventilation in the eastern equatorial Pacific
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DOI: 10.1038/ncomms14203
Abstract: The deep ocean is most likely the primary source of the radiocarbon-depleted CO2 released to the atmosphere during the last deglaciation. While there are well-documented millennial scale Δ14C changes during the most recent deglaciation, most… read more here.
Keywords: eastern equatorial; deglaciation; equatorial pacific; ventilation ... See more keywords