Silicon isotopes indicate enhanced carbon export efficiency in the North Atlantic during deglaciation

TitleSilicon isotopes indicate enhanced carbon export efficiency in the North Atlantic during deglaciation
Publication TypeJournal Article
Year of Publication2014
AuthorsHendry, KR, Robinson, LF, McManus, JF, Hays, JD
JournalNature Communications
Volume5
Date PublishedNov-01-2015
KeywordsBiogeochemistry, Cryospheric science, Ocean sciences
Abstract

Today’s Sargasso Sea is nutrient starved, except for episodic upwelling events caused by wind-driven winter mixing and eddies. Enhanced diatom opal burial in Sargasso Sea sediments indicates that silicic acid, a limiting nutrient today, may have been more available in subsurface waters during Heinrich Stadials, millennial-scale climate perturbations of the last glacial and deglaciation. Here we use the geochemistry of opal-forming organisms from different water depths to demonstrate changes in silicic acid supply and utilization during the most recent Heinrich Stadial. We suggest that during the early phase (17.5–18 ka), wind-driven upwelling replenished silicic acid to the subsurface, resulting in low Si utilization. By 17 ka, stratification reduced the surface silicic acid supply leading to increased Si utilization efficiency. This abrupt shift in Si cycling would have contributed to high regional carbon export efficiency during the recent Heinrich Stadial, despite being a period of increasing atmospheric CO2.

URLhttp://www.nature.com/doifinder/10.1038/ncomms4107
DOI10.1038/ncomms4107