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Contribution of seasonal sub-Antarctic surface water variability to millennial-scale changes in atmospheric CO<inf>2</inf> over the last deglaciation and Marine Isotope Stage 3

J Gottschalk, LC Skinner, C Waelbroeck

OAI: oai:www.repository.cam.ac.uk:1810/246795

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Abstract

South Atlantic planktonic foraminifera stable oxygen and carbon isotopes atmospheric CO2 last glacial period