Chlorine-36 evidence for the Mono Lake event in the Summit GRIP ice core

被引：97

作者：

Wagner, G

Beer, J

Laj, C

Kissel, C

Masarik, J

Muscheler, R

Synal, HA

机构：

[1] EAWAG, CH-8600 Dubendorf, Switzerland

[2] CEA, CNRS, Lab Sci Climat & Environm, Unite Mixte, F-91198 Gif Sur Yvette, France

[3] Comenius Univ, Fac Math & Phys, Dept Nucl Phys, SK-84215 Bratislava, Slovakia

[4] ETH Honggerberg, Paul Scherrer Inst, CH-8093 Zurich, Switzerland

来源：

EARTH AND PLANETARY SCIENCE LETTERS | 2000年 / 181卷 / 1-2期

关键词：

Cl-36; magnetic field; paleomagnetism; cosmogenic elements; radioactive elements;

D O I：

10.1016/S0012-821X(00)00196-5

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

A distinct peak has been discovered in the Cl-36 data from the GRIP ice core between the Dansgaard Oeschger (D-O) events 6 and 7 at approximately 32 kyr BP. This peak can be attributed to a minimum of the geomagnetic dipole field associated with the Mono Lake event, Since the Cl-36 peak reflects a higher production rate of all cosmogenic radionuclides, it has an impact on the C-14 dating of the last ice age. Furthermore, it provides an additional time marker similar to a peak found earlier corresponding to the Laschamp event at approximately 39 kyr BP. (C) 2000 Elsevier Science B,V, All rights reserved.

引用

页码：1 / 6

页数：6

共 20 条

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