Varied contribution of the Southern Ocean to deglacial atmospheric CO2 rise

Type Article
Date 2019-12
Language English
Author(s) Moy Andrew D.1, Palmer Martin R.2, Howard William R.3, Bijma Jelle4, Cooper Matthew J.5, Calvo Eva6, Pelejero Carles7, Gagan Michael K.8, Chalk Thomas B.9
Affiliation(s) 1 : Australian Antarctic Division, Kingston, Tasmania, Australia
2 : Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart, Tasmania, Australia
3 : Ocean and Earth Science, University of Southampton, Southampton, UK
4 : Climate Change Institute, The Australian National University, Canberra, Australian Capital Territory, Australia
5 : Marine Biogeosciences, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
6 : ICM-CSIC, Institut de Ciències del Mar, Barcelona, Spain
7 : ICREA, Institució Catalana de Recerca i Estudis Avançats, Barcelona, Spain
8 : School of Earth and Environmental Sciences, The University of Queensland, Brisbane, Queensland, Australia
9 : Research School of Earth Sciences, The Australian National University, Canberra, Australian Capital Territory, Australia
Source Nature Geoscience (1752-0894) (Springer Science and Business Media LLC), 2019-12 , Vol. 12 , N. 12 , P. 1006-1011
DOI 10.1038/s41561-019-0473-9
WOS© Times Cited 11

Glacial–interglacial changes in atmospheric CO2 are generally attributed to changes in seawater carbon chemistry in response to large-scale shifts in the ocean’s biogeochemistry and general circulation. The Southern Ocean currently takes up more CO2 than any other and it is likely to have played a crucial role in regulating past atmospheric CO2. However, the physical, biological and chemical variables that control ocean–atmosphere CO2 exchange during glacial–interglacial cycles are not completely understood. Here we use boron isotopes and carbon isotopes in planktonic foraminifera and an alkenone-based proxy of temperature to reconstruct seawater pH and CO2 partial pressure in sub-Antarctic surface waters south of Tasmania over the past 25,000 years, and investigate the mechanisms that regulate seawater CO2. The new record shows that surface waters in this region were a sink for atmospheric CO2 during the Last Glacial Maximum. Our reconstruction suggests changes in the strength of the biological pump and the release of deep-ocean CO2 to surface waters contributed to the last deglacial rise in atmospheric CO2. These findings demonstrate that variations in upwelling intensity and the distribution of Southern Ocean water masses in this sector played a key role in regulating atmospheric CO2 during the last glacial–interglacial cycle.

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Moy Andrew D., Palmer Martin R., Howard William R., Bijma Jelle, Cooper Matthew J., Calvo Eva, Pelejero Carles, Gagan Michael K., Chalk Thomas B. (2019). Varied contribution of the Southern Ocean to deglacial atmospheric CO2 rise. Nature Geoscience, 12(12), 1006-1011. Publisher's official version : , Open Access version :