Temperature estimates derived from isotopes in polar ice cores reveal much about Earth's past climate. According to the latest analysis, interglacial periods were rather warmer than previously thought.
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References
Overpeck, J. T. et al. Science 311, 1747–1750 (2006).
Sime, L. C., Wolff, E. W., Oliver, K. I. C. & Tindall, J. C. Nature 462, 342–345 (2009).
Epstein, S., Sharp, R. P. & Goddard, I. J. Geol. 71, 698–720 (1963).
Dansgaard, W. et al. Science 218, 1273–1277 (1982).
Dansgaard, W. Tellus 16, 436–468 (1964).
Jouzel, J. et al. J. Geophys. Res. 102, 26471–26487 (1997).
Masson-Delmotte, V. et al. J. Clim. 21, 3359–3387 (2008).
Worden, J. et al. Nature 445, 528–532 (2007).
Noone, D. J. Geophys. Res. 113, D04102 (2008).
Lee, J.-E., Fung, I., DePaolo, D. J. & Otto-Bliesner, B. J. Geophys. Res. 113, D19109 (2008).
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Noone, D. Kink in the thermometer. Nature 462, 295–296 (2009). https://doi.org/10.1038/462295a
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DOI: https://doi.org/10.1038/462295a