Data Publications

Dome Fuji 360KYr Stable Isotope Data and Temperature Reconstruction

  • Japanese Antarctic Research Expedition
  • 2012
  • Dome Fuji 360KYr Stable Isotope Data and Temperature Reconstruction
  • A20180613-007
  • oxygen isotopes
  • Dome Fuji
  • Ice Core
  • hydrogen isotopes
  • reconstruction
  • Uemura, R., V. Masson-Delmotte, J. Jouzel, A. Landais, H. Motoyama, and B. Stenni. 2012. Ranges of moisture-source temperature estimated from Antarctic ice cores stable isotope records over glacial-interglacial cycles. Climate of the Past, Vol. 8, No. 3, pp. 1109-1125. doi:10.5194/cp-8-1109-2012 / Watanabe, O., J. Jouzel, S. Johnsen, F. Parrenin, H. Shoji, and N. Yoshida. 2003. Homogeneous climate variability across East Antarctica over the past three glacial cycles. Nature, Vol. 422, pp. 509-512. / Uemura, R., N. Yoshida, N. Kurita, M. Nakawo, and O. Watanabe. 2004. An observation-based method for reconstructing ocean surface changes using a 340,000-year deuterium excess record from the Dome Fuji ice core, Antarctica. Geophys. Res. Lett., 31, doi:10.1029/2004GL019954. / Kawamura, K., F. Parrenin, L. Lisiecki, R. Uemura, F. Vimeux, J.P. Severinghaus, M. A. Hutterli, T. Nakazawa, S. Aoki, J. Jouzel, M. E. Raymo, K. Matsumoto, H. Nakata, H. Motoyama, S. Fujita, K. Goto-Azuma, Y. Fujii, and O. Watanabe. 2007. Northern Hemisphere forcing of climatic cycles in Antarctica over the past 360,000 years. Nature, Vol. 448, pp. 912-916. doi:10.1038/nature06015.
  • Stable isotope data (d18O and dD) and temperature reconstruction from Dome Fuji ice cores, Antarctica for the past 360,000 years. Data from core DF1 are deltaD (Uemura et al., 2004) and delta18O (Watanabe et al., 2003). The data-set is corrected and updated in Uemura et al. (2012). Data from core DF2 includes deltaD and delta18O (Uemura et al., 2012). Temperature estimates are based on combined isotope data from both cores (Uemura et al., 2012). The age scale adopted here is the Dome Fuji Ice Core O2/N2 timescale (DFO-2006) (Kawamura et al., 2007).
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