Asynchroneity of maximum glacier advances in the central Spanish Pyrenees
31 páginas, 7 figuras, 1 tabla The deglaciation history of the Escarra and Lana Mayor glaciers (Upper Gállego valley, Central Spanish Pyrenees) was reconstructed on the basis of detailed geomorphological studies of glacier deposits, sedimentological and palynological analyses of glacial lakes sedime...
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Online Access: | http://hdl.handle.net/10261/47613 https://doi.org/10.1002/jqs.715 |
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ftcsic:oai:digital.csic.es:10261/47613 2024-02-11T10:04:54+01:00 Asynchroneity of maximum glacier advances in the central Spanish Pyrenees García-Ruiz, José María Valero-Garcés, Blas L. Martí Bono, Carlos Enrique González-Sampériz, Penélope 2002-11-28 http://hdl.handle.net/10261/47613 https://doi.org/10.1002/jqs.715 en eng Wiley-Blackwell http://dx.doi.org/10.1002/jqs.715 Journal of quaternary science 18 (1): 61-72 (2003) 0267-8179 http://hdl.handle.net/10261/47613 doi:10.1002/jqs.715 1099-1417 open Last Glacial Maximum Glaciers Upper Gállego Valley Central Pyrenees artículo http://purl.org/coar/resource_type/c_6501 2002 ftcsic https://doi.org/10.1002/jqs.715 2024-01-16T09:36:56Z 31 páginas, 7 figuras, 1 tabla The deglaciation history of the Escarra and Lana Mayor glaciers (Upper Gállego valley, Central Spanish Pyrenees) was reconstructed on the basis of detailed geomorphological studies of glacier deposits, sedimentological and palynological analyses of glacial lakes sediments and an AMS chronology based on minimum ages from glacial lake deposits. The maximum extent of the Pyrenean glaciers during the last glaciation was before 30,000 years B.P. and predated the maximum advances of the Scandinavian Ice Sheet and some Alpine glaciers. A later advance occurred during the coldest period (around 20,000 years B.P.) synchronous with the maximum global ice extent, but in the Pyrenees it was less extensive than the previous one. Later, there were minor advances followed by a stage of debris-covered glaciers and a phase of moraine formation near cirque backwalls. The deglaciation chronology of the Upper Gállego valley provides more examples of the general asynchroneity between mountain and continental glaciers. The asynchroneity of maximum advances may be explained by different regional responses to climatic forcing and by the southern latitudes of the Pyrenees. This work was part of the Project "Isotope sedimentology of 40 ka time-series from Iberian sites as a test for abrupt arid/humid switching within the Mediterranean climate zone" (EAR 941-8657), funded by the National Science Foundation, USA, and the Project "Arid periods in the Mediterranean area since the Last Glacial Maximum" (REN2000-1136/CLI), funded by the Spanish “Comisión Interministerial de Ciencia y Tecnología”. The authors thank Dr. Colin Ballantyne, Dr. Valérie Andrieu-Ponel and Dr. María Fernanda Sánchez-Goñi for their criticisms and suggestions that improved the manuscript. Peer reviewed Article in Journal/Newspaper Ice Sheet Digital.CSIC (Spanish National Research Council) Glacial Lake ENVELOPE(-129.463,-129.463,58.259,58.259) Journal of Quaternary Science 18 1 61 72 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
topic |
Last Glacial Maximum Glaciers Upper Gállego Valley Central Pyrenees |
spellingShingle |
Last Glacial Maximum Glaciers Upper Gállego Valley Central Pyrenees García-Ruiz, José María Valero-Garcés, Blas L. Martí Bono, Carlos Enrique González-Sampériz, Penélope Asynchroneity of maximum glacier advances in the central Spanish Pyrenees |
topic_facet |
Last Glacial Maximum Glaciers Upper Gállego Valley Central Pyrenees |
description |
31 páginas, 7 figuras, 1 tabla The deglaciation history of the Escarra and Lana Mayor glaciers (Upper Gállego valley, Central Spanish Pyrenees) was reconstructed on the basis of detailed geomorphological studies of glacier deposits, sedimentological and palynological analyses of glacial lakes sediments and an AMS chronology based on minimum ages from glacial lake deposits. The maximum extent of the Pyrenean glaciers during the last glaciation was before 30,000 years B.P. and predated the maximum advances of the Scandinavian Ice Sheet and some Alpine glaciers. A later advance occurred during the coldest period (around 20,000 years B.P.) synchronous with the maximum global ice extent, but in the Pyrenees it was less extensive than the previous one. Later, there were minor advances followed by a stage of debris-covered glaciers and a phase of moraine formation near cirque backwalls. The deglaciation chronology of the Upper Gállego valley provides more examples of the general asynchroneity between mountain and continental glaciers. The asynchroneity of maximum advances may be explained by different regional responses to climatic forcing and by the southern latitudes of the Pyrenees. This work was part of the Project "Isotope sedimentology of 40 ka time-series from Iberian sites as a test for abrupt arid/humid switching within the Mediterranean climate zone" (EAR 941-8657), funded by the National Science Foundation, USA, and the Project "Arid periods in the Mediterranean area since the Last Glacial Maximum" (REN2000-1136/CLI), funded by the Spanish “Comisión Interministerial de Ciencia y Tecnología”. The authors thank Dr. Colin Ballantyne, Dr. Valérie Andrieu-Ponel and Dr. María Fernanda Sánchez-Goñi for their criticisms and suggestions that improved the manuscript. Peer reviewed |
format |
Article in Journal/Newspaper |
author |
García-Ruiz, José María Valero-Garcés, Blas L. Martí Bono, Carlos Enrique González-Sampériz, Penélope |
author_facet |
García-Ruiz, José María Valero-Garcés, Blas L. Martí Bono, Carlos Enrique González-Sampériz, Penélope |
author_sort |
García-Ruiz, José María |
title |
Asynchroneity of maximum glacier advances in the central Spanish Pyrenees |
title_short |
Asynchroneity of maximum glacier advances in the central Spanish Pyrenees |
title_full |
Asynchroneity of maximum glacier advances in the central Spanish Pyrenees |
title_fullStr |
Asynchroneity of maximum glacier advances in the central Spanish Pyrenees |
title_full_unstemmed |
Asynchroneity of maximum glacier advances in the central Spanish Pyrenees |
title_sort |
asynchroneity of maximum glacier advances in the central spanish pyrenees |
publisher |
Wiley-Blackwell |
publishDate |
2002 |
url |
http://hdl.handle.net/10261/47613 https://doi.org/10.1002/jqs.715 |
long_lat |
ENVELOPE(-129.463,-129.463,58.259,58.259) |
geographic |
Glacial Lake |
geographic_facet |
Glacial Lake |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
http://dx.doi.org/10.1002/jqs.715 Journal of quaternary science 18 (1): 61-72 (2003) 0267-8179 http://hdl.handle.net/10261/47613 doi:10.1002/jqs.715 1099-1417 |
op_rights |
open |
op_doi |
https://doi.org/10.1002/jqs.715 |
container_title |
Journal of Quaternary Science |
container_volume |
18 |
container_issue |
1 |
container_start_page |
61 |
op_container_end_page |
72 |
_version_ |
1790601662783553536 |