LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from <sup>10</sup>Be surface exposure dating

Surface exposure dating (SED) is an innovative tool already being widely applied for moraine dating and for Late Quaternary glacier and climate reconstruction. Here we present exposure ages of 28 boulders from the Cordillera Real and the Cordillera Cochabamba, Bolivia. Our results indicate that the...

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Main Authors: H. Veit, P. W. Kubik, Ch. Kull, R. Zech
Format: Article
Language:English
Published: Copernicus Publications 2007-10-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/3/623/2007/cp-3-623-2007.pdf
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spelling doaj-995c028a433544d38a22393e08283d952020-11-24T23:22:59ZengCopernicus PublicationsClimate of the Past1814-93241814-93322007-10-0134623635LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from <sup>10</sup>Be surface exposure datingH. VeitP. W. KubikCh. KullR. ZechSurface exposure dating (SED) is an innovative tool already being widely applied for moraine dating and for Late Quaternary glacier and climate reconstruction. Here we present exposure ages of 28 boulders from the Cordillera Real and the Cordillera Cochabamba, Bolivia. Our results indicate that the local Last Glacial Maximum (LGM) in the Eastern Cordilleras occurred at ~22&ndash;25 ka and was thus synchronous to the global temperature minimum. We were also able to date several Late Glacial moraines to ~11&ndash;13 ka, which likely document lower temperatures and increased precipitation ("Coipasa" humid phase). Additionally, we recognize the existence of older Late Glacial moraines re-calculated to ~15 ka from published cosmogenic nuclide data. Those may coincide with the cold Heinrich 1 event in the North Atlantic region and the pronounced "Tauca" humid phase. We conclude that (i) exposure ages in the tropical Andes may have been overestimated so far due to methodological uncertainties, and (ii) although precipitation plays an important role for glacier mass balances in the tropical Andes, it becomes the dominant forcing for glaciation only in the drier and thus more precipitation-sensitive regions farther west and south. http://www.clim-past.net/3/623/2007/cp-3-623-2007.pdf
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language English
format Article
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author H. Veit
P. W. Kubik
Ch. Kull
R. Zech
spellingShingle H. Veit
P. W. Kubik
Ch. Kull
R. Zech
LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from <sup>10</sup>Be surface exposure dating
Climate of the Past
author_facet H. Veit
P. W. Kubik
Ch. Kull
R. Zech
author_sort H. Veit
title LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from <sup>10</sup>Be surface exposure dating
title_short LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from <sup>10</sup>Be surface exposure dating
title_full LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from <sup>10</sup>Be surface exposure dating
title_fullStr LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from <sup>10</sup>Be surface exposure dating
title_full_unstemmed LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from <sup>10</sup>Be surface exposure dating
title_sort lgm and late glacial glacier advances in the cordillera real and cochabamba (bolivia) deduced from <sup>10</sup>be surface exposure dating
publisher Copernicus Publications
series Climate of the Past
issn 1814-9324
1814-9332
publishDate 2007-10-01
description Surface exposure dating (SED) is an innovative tool already being widely applied for moraine dating and for Late Quaternary glacier and climate reconstruction. Here we present exposure ages of 28 boulders from the Cordillera Real and the Cordillera Cochabamba, Bolivia. Our results indicate that the local Last Glacial Maximum (LGM) in the Eastern Cordilleras occurred at ~22&ndash;25 ka and was thus synchronous to the global temperature minimum. We were also able to date several Late Glacial moraines to ~11&ndash;13 ka, which likely document lower temperatures and increased precipitation ("Coipasa" humid phase). Additionally, we recognize the existence of older Late Glacial moraines re-calculated to ~15 ka from published cosmogenic nuclide data. Those may coincide with the cold Heinrich 1 event in the North Atlantic region and the pronounced "Tauca" humid phase. We conclude that (i) exposure ages in the tropical Andes may have been overestimated so far due to methodological uncertainties, and (ii) although precipitation plays an important role for glacier mass balances in the tropical Andes, it becomes the dominant forcing for glaciation only in the drier and thus more precipitation-sensitive regions farther west and south.
url http://www.clim-past.net/3/623/2007/cp-3-623-2007.pdf
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