Deglacial Subantarctic CO outgassing driven by a weakened solubility pump.

Nat Commun

Research School of Earth Sciences, The Australian National University, Canberra, ACT, Australia.

Published: September 2022

The Subantarctic Southern Ocean has long been thought to be an important contributor to increases in atmospheric carbon dioxide partial pressure (pCO) during glacial-interglacial transitions. Extensive studies suggest that a weakened biological pump, a process associated with nutrient utilization efficiency, drove up surface-water pCO in this region during deglaciations. By contrast, regional influences of the solubility pump, a process mainly linked to temperature variations, have been largely overlooked. Here, we evaluate relative roles of the biological and solubility pumps in determining surface-water pCO variabilities in the Subantarctic Southern Ocean during the last deglaciation, based on paired reconstructions of surface-water pCO, temperature, and nutrient utilization efficiency. We show that compared to the biological pump, the solubility pump imposed a strong impact on deglacial Subantarctic surface-water pCO variabilities. Our findings therefore reveal a previously underappreciated role of the solubility pump in modulating deglacial Subantarctic CO release and possibly past atmospheric pCO fluctuations.

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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9440897PMC
http://dx.doi.org/10.1038/s41467-022-32895-9DOI Listing

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