Atmospheric methane and nitrous oxide of the late Pleistocene from Antarctic ice cores

被引:309
作者
Spahni, R
Chappellaz, J
Stocker, TF
Loulergue, L
Hausammann, G
Kawamura, K
Flückiger, J
Schwander, J
Raynaud, D
Masson-Delmotte, V
Jouzel, J
机构
[1] Univ Bern, Inst Phys, CH-3012 Bern, Switzerland
[2] UJF, CNRS, Lab Glaciol & Geophys Environm, F-38402 St Martin Dheres, France
[3] Ctr Etud Saclay, Inst Pierre Simon Laplace, Lab Sci Climat & Environm, CEA CNRS 1572, F-91191 Gif Sur Yvette, France
关键词
D O I
10.1126/science.1120132
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The European Project for Ice Coring in Antarctica Dome C ice core enables us to extend existing records of atmospheric methane (CH4) and nitrous oxide (N2O) back to 650,000 years before the present. A combined record of CH4 measured along the Dome C and the Vostok ice cores demonstrates, within the resolution of our measurements, that preindustrial concentrations over Antarctica have not exceeded 773 +/- 15 ppbv (parts per billion by volume) during the past 650,000 years. Before 420,000 years ago, when interglacials were cooler, maximum CH4 concentrations were only about 600 ppbv, similar to lower Holocene values. In contrast, the N2O record shows maximum concentrations of 278 +/- 7 ppbv, slightly higher than early Holocene values.
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页码:1317 / 1321
页数:5
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