Sediments at the edge of Antarctica are a largely unexploited source of information about climate change. They have now provided a valuable local record of sea surface temperatures for the past 12,000 years. See Letter p.250
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References
Shevenell, A. E., Ingalls, A. E., Domack, E. W. & Kelly, C. Nature 470, 250–254 (2011).
Vaughan, D. G. et al. Clim. Change 60, 243–274 (2003).
Bentley, M. J. et al. Holocene 19, 51–69 (2009).
Renssen, H., Goosse, H., Fichefet, T., Masson-Delmotte, V. & Koç, N. Holocene 15, 951–964 (2005).
Domack, E. et al. Holocene 11, 1–9 (2001).
Schouten, S., Hopmans, E. C., Schefuss, E. & Damsté, J. S. S. Earth Planet. Sci. Lett. 204, 265–274 (2002).
Kim, J.-H. et al. Geochim. Cosmochim. Acta 74, 4639–4654 (2010).
Murray, A. E. et al. Appl. Environ. Microbiol. 64, 2585–2595 (1998).
Expedition 318 Scientists. IODP Prelim. Rep. 318, doi:10.2204/iodp.pr.318.2010 (2010).
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Bendle, J. Core data from the Antarctic margin. Nature 470, 181–182 (2011). https://doi.org/10.1038/470181a
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DOI: https://doi.org/10.1038/470181a