Links between various climate records for the North Atlantic Ocean and the Mediterranean Sea have helped to identify a potential mechanism that enhanced sea-level rise during the last interglacial time interval. See Letter p.197
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References
Marino, G. et al. Nature 522, 197–201 (2015).
Grant, K. M. et al. Nature Commun. 5, 5076; http://dx.doi.org/10.1038/ncomms6076 (2014).
Fairbanks, R. G. Nature 342, 637–642 (1989).
Denton, G. H. et al. Science 328, 1652–1656 (2010).
Masson-Delmotte, V. et al. Quat. Sci. Rev. 29, 113–128 (2010).
Broecker, W. S. Paleoceanography 13, 119–121 (1998).
Pisias, N. G. & Moore, T. C. Jr Earth Planet. Sci. Lett. 52, 450–458 (1981).
Ruddiman, W. F. Earth's Climate: Past and Future 3rd edn, Ch. 12 (Freeman, 2013).
Lambeck, K., Rouby, H., Purcell, A., Sun, Y. & Sambridge, M. Proc. Natl Acad. Sci. USA 111, 15296–15303 (2014).
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Billups, K. Timing is everything during deglaciations. Nature 522, 163–164 (2015). https://doi.org/10.1038/522163a
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DOI: https://doi.org/10.1038/522163a