Contribution of seasonal sub-Antarctic surface water variability to millennial-scale changes in atmospheric CO2 over the last deglaciation and Marine Isotope Stage 3

Gottschalk, Julia and Skinner, Luke C. and Waelbroeck, Claire (2015) Contribution of seasonal sub-Antarctic surface water variability to millennial-scale changes in atmospheric CO2 over the last deglaciation and Marine Isotope Stage 3. Earth and Planetary Science Letters, 411. pp. 87-99. ISSN 0012821X DOI https://doi.org/10.1016/j.epsl.2014.11.051

Preview	Text Skinner.pdf - Published Version Available under License Creative Commons Attribution. Download (901kB) | Preview
Preview	Image 1-s2.0-S0012821X14007511-gr001.jpg - Published Version Available under License Creative Commons Attribution No Derivatives. Download (125kB) | Preview
Preview	Text Gottschalk et al. - 2015 - Contribution of seasonal sub-Antarctic surface wat.pdf - Published Version Available under License Creative Commons Attribution. Download (5MB) | Preview

Abstract

The Southern Ocean is thought to have played a key role in past atmospheric carbon dioxide (CO2,atm) changes. Three main factors are understood to control the Southern Ocean's influence on CO2,atm, via their impact on surface ocean pCO2 and therefore regional ocean–atmosphere CO2 fluxes: 1) the efficiency of air–sea gas exchange, which may be attenuated by seasonal- or annual sea-ice coverage or the development of a shallow pycnocline; 2) the supply of CO2-rich water masses from the sub-surface and the deep ocean, which is associated with turbulent mixing and surface buoyancy- and/or wind forcing; and 3) biological carbon fixation, which depends on nutrient availability and is therefore influenced by dust deposition and/or upwelling. In order to investigate the possible contributions of these processes to millennial-scale CO2,atm variations during the last glacial and deglacial periods, we make use of planktonic foraminifer census counts and stable oxygen- and carbon isotope measurements in the planktonic foraminifera Globigerina bulloides and Neogloboquadrina pachyderma (sinistral) from marine sediment core MD07-3076Q in the sub-Antarctic Atlantic. These data are interpreted on the basis of a comparison of core-top and modern seawater isotope data, which permits an assessment of the seasonal biases and geochemical controls on the stable isotopic compositions of G. bulloides and N. pachyderma (s.). Based on a comparison of our down-core results with similar data from the Southeast Atlantic (Cape Basin) we infer past basin-wide changes in the surface hydrography of the sub-Antarctic Atlantic. We find that millennial-scale rises in CO2,atm over the last 70 ka are consistently linked with evidence for increased spring upwelling, and enhanced summer air–sea exchange in the sub-Antarctic Atlantic. Parallel evidence for increased summer export production would suggest that seasonal changes in upwelling and air–sea exchange exerted a dominant influence on surface pCO2 in the sub-Antarctic Atlantic. These results underline the role of Southern Ocean dynamics, in particular their seasonal variations, in driving millennial-scale variations in CO2,atm.

Item Type:	Article
Uncontrolled Keywords:	2014AREP; IA68;
Subjects:	01 - Climate Change and Earth-Ocean Atmosphere Systems
Divisions:	01 - Climate Change and Earth-Ocean Atmosphere Systems 07 - Gold Open Access
Journal or Publication Title:	Earth and Planetary Science Letters
Volume:	411
Page Range:	pp. 87-99
Identification Number:	https://doi.org/10.1016/j.epsl.2014.11.051
Depositing User:	Sarah Humbert
Date Deposited:	06 Feb 2015 19:07
Last Modified:	16 Feb 2015 17:57
URI:	http://eprints.esc.cam.ac.uk/id/eprint/3227

Actions (login required)

View Item