Articles | Volume 14, issue 8
Clim. Past, 14, 1229–1252, 2018
https://doi.org/10.5194/cp-14-1229-2018

Special issue: Paleoclimate data synthesis and analysis of associated uncertainty...

Clim. Past, 14, 1229–1252, 2018
https://doi.org/10.5194/cp-14-1229-2018

Research article 16 Aug 2018

Research article | 16 Aug 2018

Deglacial carbon cycle changes observed in a compilation of 127 benthic δ13C time series (20–6 ka)

Carlye D. Peterson and Lorraine E. Lisiecki

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Cited articles

Allen, K. A., Sikes, E. L., Hönisch, B., Elmore, A. C., Guilderson, T. P., Rosenthal, Y., and Anderson, R. F.: Southwest Pacific deep water carbonate chemistry linked to high southern latitude climate and atmospheric CO2 during the last glacial termination, Quaternary Sci. Rev., 122, 180–191, 2015. a, b
Archer, D., Winguth, A., Lea, D., and Mahowald, N.: What caused the glacial/interglacial atmospheric pCO2 cycles?, Rev. Geophys., 38, 159–190, 2000. a
Archer, D. E., Martin, P. A., Milovich, J., Brovkin, V., Plattner, G.-K., and Ashendel, C.: Model sensitivity in the effect of Antarctic sea ice and stratification on atmospheric pCO2, Paleoceanography, 18, 1012, https://doi.org/10.1029/2002PA000760, 2003. a
Arz, H. W., Pätzold, J., and Wefer, G.: Stable oxygen and carbon isotope ratios of benthic foraminifera from sediment core GeoB3104-1, PANGAEA, https://doi.org/10.1594/PANGAEA.54790, 1999. a
Aydin, M., Campbell, J., Fudge, T., Cuffey, K., Nicewonger, M., Verhulst, K., and Saltzman, E.: Changes in atmospheric carbonyl sulfide over the last 54,000 years inferred from measurements in Antarctic ice cores, J. Geophys. Res.-Atmos., 121, 1943–1954, https://doi.org/10.1002/2015JD024235, 2016. a
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Short summary
Our study presents an analysis of a four-dimensional compilation of globally distributed carbon isotope time series that span 20 to 6 thousand years ago. We explore carbon cycle connections between the deep ocean, atmosphere, and land-based carbon storage on thousand-year time scales to provide useful constraints for global carbon cycle reconstructions. Additionally, these carbon isotope time series are suitable for comparison with deglacial simulations from isotope-enabled Earth system models.