Geomagnetic modulation of the 36Cl flux in the GRIP ice core, Greenland

被引:94
作者
Baumgartner, S
Beer, J [1 ]
Masarik, J
Wagner, G
Meynadier, L
Synal, HA
机构
[1] Swiss Fed Inst Sci & Technol, CH-8600 Dubendorf, Switzerland
[2] Inst Phys Globe, CNRS, Lab Geochim & Cosmochim 1758, F-75252 Paris 5, France
[3] ETH Honggerberg, Paul Scherrer Inst, CH-8093 Zurich, Switzerland
关键词
D O I
10.1126/science.279.5355.1330
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
Geomagnetic field strength is expected to affect the production rate of cosmogenic isotopes such as beryllium-10, carbon-14, or chlorine-36. Chlorine-36 data from the Greenland Ice Gore Project (GRIP) ice core agree well with a production rate calculation based on a paleomagnetic reconstruction for the past 100,000 years over both lane-and short-term variations, A chlorine-36 peak at 38,000 years ago previously found in the beryllium-10 record from the Vostok ice core can be explained by a period of law geomagnetic field intensity.
引用
收藏
页码:1330 / 1332
页数:3
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