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Sulphate–climate coupling over the past 300,000 years in inland Antarctica

Author

Listed:
  • Yoshinori Iizuka

    (Institute of Low Temperature Science, Hokkaido University, Sapporo 060-0819, Japan)

  • Ryu Uemura

    (Biology and Marine Science, Faculty of Science, University of the Ryukyus, Okinawa 903-0213, Japan)

  • Hideaki Motoyama

    (National Institute of Polar Research, Tokyo 190-8518, Japan)

  • Toshitaka Suzuki

    (Faculty of Science, Yamagata University, Yamagata 990-8560, Japan)

  • Takayuki Miyake

    (National Institute of Polar Research, Tokyo 190-8518, Japan
    Present address: School of Environmental Science, The University of Shiga Prefecture, Shiga 522-8533, Japan.)

  • Motohiro Hirabayashi

    (National Institute of Polar Research, Tokyo 190-8518, Japan)

  • Takeo Hondoh

    (Institute of Low Temperature Science, Hokkaido University, Sapporo 060-0819, Japan)

Abstract

Profiles of sulphate fluxes over the past 300,000 years from an Antarctic ice core show that, whereas the flux of sulphate-adhered dust has remained almost constant, that of sulphate salts correlates inversely with temperature, suggesting a coupling between particulate sulphur and temperature.

Suggested Citation

  • Yoshinori Iizuka & Ryu Uemura & Hideaki Motoyama & Toshitaka Suzuki & Takayuki Miyake & Motohiro Hirabayashi & Takeo Hondoh, 2012. "Sulphate–climate coupling over the past 300,000 years in inland Antarctica," Nature, Nature, vol. 490(7418), pages 81-84, October.
    • Handle: RePEc:nat:nature:v:490:y:2012:i:7418:d:10.1038_nature11359
    DOI: 10.1038/nature11359
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