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

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

Aug 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000e%26psl.181....1w&link_type=abstract

Earth and Planetary Science Letters, Volume 181, Issue 1-2, p. 1-6.

Physics

43

Scientific paper

A distinct peak has been discovered in the 36Cl 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 36Cl peak reflects a higher production rate of all cosmogenic radionuclides, it has an impact on the 14C 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.

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