Some 34 million years ago, there was a rapid growth of ice on Antarctica. A modelling study indicates that the ultimate cause of this glaciation was a decrease in the concentration of atmospheric carbon dioxide. See Letter p.574
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References
Goldner, A., Herold, N. & Huber, M. Nature 511, 574–577 (2014).
Francis, J. E. et al. in Antarctic Climate Evolution (eds Florindo, F. & Siegert, M.) 309–368 (Elsevier, 2008).
Lear, C. H., Bailey, T. R., Pearson, P. N., Coxall, H. K. & Rosenthal, Y. Geology 36, 251–254 (2008).
Liu, Z. et al. Science 323, 1187–1190 (2009).
Cramer, B. S., Toggweiler, J. R., Wright, J. D., Katz, M. E. & Miller, K. G. Paleoceanography 24, PA4216 (2009).
Sijp, W. P., England, M. H. & Huber, M. Paleoceanography 26, PA4207 (2011).
Cornford, S. L. et al. J. Comput. Phys. 232, 529–549 (2013).
Knorr, G. & Lohmann, G. Nature Geosci. 7, 376–381 (2014).
Pearson, P. N., Foster, G. L. & Wade, B. S. Nature 461, 1110–1113 (2009).
Pagani, M. et al. Science 334, 1261–1264 (2011).
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Lunt, D. Causes and effects of Antarctic ice. Nature 511, 536–537 (2014). https://doi.org/10.1038/511536a
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DOI: https://doi.org/10.1038/511536a