Chlorine-36 evidence for the mono lake event in the summit grip ice core, Earth Planet
Abstract A distinct peak has been discovered in the 36 Cl 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 36 Cl peak ref...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1044.3366 2023-05-15T16:38:45+02:00 Chlorine-36 evidence for the mono lake event in the summit grip ice core, Earth Planet G Wagner J Beer C Laj C Kissel J Masarik R Muscheler H.-A Synal The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1044.3366 http://www.dnp.fmph.uniba.sk/etext/33/text/EPSL181Wagner.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1044.3366 http://www.dnp.fmph.uniba.sk/etext/33/text/EPSL181Wagner.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.dnp.fmph.uniba.sk/etext/33/text/EPSL181Wagner.pdf text ftciteseerx 2020-04-05T00:15:42Z Abstract A distinct peak has been discovered in the 36 Cl 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 36 Cl peak reflects a higher production rate of all cosmogenic radionuclides, it has an impact on the 14 C 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. ß Text ice core Unknown |
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English |
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Abstract A distinct peak has been discovered in the 36 Cl 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 36 Cl peak reflects a higher production rate of all cosmogenic radionuclides, it has an impact on the 14 C 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. ß |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
G Wagner J Beer C Laj C Kissel J Masarik R Muscheler H.-A Synal |
spellingShingle |
G Wagner J Beer C Laj C Kissel J Masarik R Muscheler H.-A Synal Chlorine-36 evidence for the mono lake event in the summit grip ice core, Earth Planet |
author_facet |
G Wagner J Beer C Laj C Kissel J Masarik R Muscheler H.-A Synal |
author_sort |
G Wagner |
title |
Chlorine-36 evidence for the mono lake event in the summit grip ice core, Earth Planet |
title_short |
Chlorine-36 evidence for the mono lake event in the summit grip ice core, Earth Planet |
title_full |
Chlorine-36 evidence for the mono lake event in the summit grip ice core, Earth Planet |
title_fullStr |
Chlorine-36 evidence for the mono lake event in the summit grip ice core, Earth Planet |
title_full_unstemmed |
Chlorine-36 evidence for the mono lake event in the summit grip ice core, Earth Planet |
title_sort |
chlorine-36 evidence for the mono lake event in the summit grip ice core, earth planet |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1044.3366 http://www.dnp.fmph.uniba.sk/etext/33/text/EPSL181Wagner.pdf |
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ice core |
genre_facet |
ice core |
op_source |
http://www.dnp.fmph.uniba.sk/etext/33/text/EPSL181Wagner.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1044.3366 http://www.dnp.fmph.uniba.sk/etext/33/text/EPSL181Wagner.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766029094252707840 |