LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from 10Be 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: Zech, Roland, Kull, Christoph, Kubik, Peter W., Veit, Heinz
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus 2007
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/8656
https://doi.org/10.3929/ethz-b-000008656
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spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/8656 2023-05-15T17:33:32+02:00 LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from 10Be surface exposure dating Zech, Roland Kull, Christoph Kubik, Peter W. Veit, Heinz 2007 application/application/pdf https://hdl.handle.net/20.500.11850/8656 https://doi.org/10.3929/ethz-b-000008656 en eng Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-3-623-2007 http://hdl.handle.net/20.500.11850/8656 doi:10.3929/ethz-b-000008656 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/2.5/ Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic CC-BY-NC-SA Climate of the Past, 3 (4) info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2007 ftethz https://doi.org/20.500.11850/8656 https://doi.org/10.3929/ethz-b-000008656 https://doi.org/10.5194/cp-3-623-2007 2022-04-25T13:50:25Z 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 ~22–25 ka and was thus synchronous to the global temperature minimum. We were also able to date several Late Glacial moraines to ~11–13 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. ISSN:1814-9324 ISSN:1814-9332 Article in Journal/Newspaper North Atlantic ETH Zürich Research Collection
institution Open Polar
collection ETH Zürich Research Collection
op_collection_id ftethz
language English
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 ~22–25 ka and was thus synchronous to the global temperature minimum. We were also able to date several Late Glacial moraines to ~11–13 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. ISSN:1814-9324 ISSN:1814-9332
format Article in Journal/Newspaper
author Zech, Roland
Kull, Christoph
Kubik, Peter W.
Veit, Heinz
spellingShingle Zech, Roland
Kull, Christoph
Kubik, Peter W.
Veit, Heinz
LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from 10Be surface exposure dating
author_facet Zech, Roland
Kull, Christoph
Kubik, Peter W.
Veit, Heinz
author_sort Zech, Roland
title LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from 10Be surface exposure dating
title_short LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from 10Be surface exposure dating
title_full LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from 10Be surface exposure dating
title_fullStr LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from 10Be surface exposure dating
title_full_unstemmed LGM and Late Glacial glacier advances in the Cordillera Real and Cochabamba (Bolivia) deduced from 10Be surface exposure dating
title_sort lgm and late glacial glacier advances in the cordillera real and cochabamba (bolivia) deduced from 10be surface exposure dating
publisher Copernicus
publishDate 2007
url https://hdl.handle.net/20.500.11850/8656
https://doi.org/10.3929/ethz-b-000008656
genre North Atlantic
genre_facet North Atlantic
op_source Climate of the Past, 3 (4)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-3-623-2007
http://hdl.handle.net/20.500.11850/8656
doi:10.3929/ethz-b-000008656
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-sa/2.5/
Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic
op_rightsnorm CC-BY-NC-SA
op_doi https://doi.org/20.500.11850/8656
https://doi.org/10.3929/ethz-b-000008656
https://doi.org/10.5194/cp-3-623-2007
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