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

被引:0
|
作者
Yoshinori Iizuka
Ryu Uemura
Hideaki Motoyama
Toshitaka Suzuki
Takayuki Miyake
Motohiro Hirabayashi
Takeo Hondoh
机构
[1] Institute of Low Temperature Science,Department of Chemistry
[2] Hokkaido University,Department of Earth and Environmental Sciences
[3] Sapporo 060-0819,undefined
[4] Japan,undefined
[5] Biology and Marine Science,undefined
[6] Faculty of Science,undefined
[7] University of the Ryukyus,undefined
[8] Okinawa 903-0213,undefined
[9] Japan,undefined
[10] National Institute of Polar Research,undefined
[11] Tokyo 190-8518,undefined
[12] Japan,undefined
[13] Faculty of Science,undefined
[14] Yamagata University,undefined
[15] Yamagata 990-8560,undefined
[16] Japan,undefined
[17] Present address: School of Environmental Science,undefined
[18] The University of Shiga Prefecture,undefined
[19] Shiga 522-8533,undefined
[20] Japan.,undefined
来源
Nature | 2012年 / 490卷
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中图分类号
学科分类号
摘要
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.
引用
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页码:81 / 84
页数:3
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