The late Pleistocene and Holocene glaciation in the Pyrenees: A critical review and new evidence from 10Be exposure ages, south-central Pyrenees.

A compilation and a critical assessment of the 14C data set available show that the chronology of glacial events in the Pyrenees is not well constrained. After reviewing the literature on glacial reconstruction, we suggest a simplified subdivision of the Pyrenean last glacial cycle record into Last...

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Autores: Pallàs i Serra, Raimon, Rodés Bolumburu, Ángel, Braucher, Régis, Carcaillet, J., Ortuño Candela, Maria, Bordonau i Ibern, Jaume, Bourlès, Didier, Vilaplana, Joan Manuel, Masana, Eulàlia, Santanach i Prat, Pere F., 1946-
Tipo de recurso: artículo
Estado:Versión aceptada para publicación
Fecha de publicación:2006
País:España
Institución:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Repositorio:Recercat. Dipósit de la Recerca de Catalunya
OAI Identifier:oai:recercat.cat:2445/163388
Acceso en línea:https://hdl.handle.net/2445/163388
Access Level:acceso abierto
Palabra clave:Paleoclimatologia
Plistocè
Holocè
Pirineus
Paleoclimatology
Pleistocene
Holocene
Pyrenees
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spelling The late Pleistocene and Holocene glaciation in the Pyrenees: A critical review and new evidence from 10Be exposure ages, south-central Pyrenees.Pallàs i Serra, RaimonRodés Bolumburu, ÁngelBraucher, RégisCarcaillet, J.Ortuño Candela, MariaBordonau i Ibern, JaumeBourlès, DidierVilaplana, Joan ManuelMasana, EulàliaSantanach i Prat, Pere F., 1946-PaleoclimatologiaPlistocèHolocèPirineusPaleoclimatologyPleistoceneHolocenePyreneesA compilation and a critical assessment of the 14C data set available show that the chronology of glacial events in the Pyrenees is not well constrained. After reviewing the literature on glacial reconstruction, we suggest a simplified subdivision of the Pyrenean last glacial cycle record into Last Pleniglacial, Deglaciation, and Neoglacial. To improve the numerical glacial chronology, we provide 10Be surface exposure ages for 5 glacial erosion surfaces, 9 moraines and 2 erratics in the Upper Noguera Ribagorc-ana Valley (south-central Pyrenees). Published corrected 14C data and new 10Be exposure ages indicate that the major phase of moraine building recorded in this valley during the Last Pleniglacial probably occurred after 25 ka BP. This age calls in question the generally accepted hypothesis of a very early deglaciation of the Pyrenees ca 70-40 ka BP, and strongly suggests that the Pyrenees could have been in pleniglacial conditions during the Last Glacial Maximum (LGM). However, we do not exclude the possibility that the maximum glacier extent during the last glacial cycle had taken place much earlier than the LGM, as indicated by some published U-Th, AMS 14C and OSL data. We suggest that pleniglacial conditions could have taken place during a longer (b30-20 ka) period than generally assumed, and that the Last Pleniglacial could include several glacier fluctuations recorded irregularly in different valleys, with a last major glacier readvance taking place around the LGM. In addition, the Deglaciation is represented by a series of moraines deposited between ca 13.770.9 and 10.170.6 ka. This moraine series indicates a highly variable climatic pattern that is partly correlated with Greenland Stadial 1 (the Younger Dryas), and suggests that the Deglaciation could have continued into the early Holocene.Elsevier Ltd2020202020062020info:eu-repo/semantics/articleinfo:eu-repo/semantics/acceptedVersion59 p.application/pdfapplication/pdfhttps://hdl.handle.net/2445/163388Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)reponame:Recercat. Dipósit de la Recerca de Catalunyainstname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)InglésVersió postprint del document publicat a: https://doi.org/10.1016/j.quascirev.2006.04.004Quaternary Science Reviews, 2006, vol. 25, num. 21-22, p. 2937-2963https://doi.org/10.1016/j.quascirev.2006.04.004(c) Elsevier Ltd, 2006info:eu-repo/semantics/openAccessoai:recercat.cat:2445/1633882026-05-29T05:05:01Z
dc.title.none.fl_str_mv The late Pleistocene and Holocene glaciation in the Pyrenees: A critical review and new evidence from 10Be exposure ages, south-central Pyrenees.
title The late Pleistocene and Holocene glaciation in the Pyrenees: A critical review and new evidence from 10Be exposure ages, south-central Pyrenees.
spellingShingle The late Pleistocene and Holocene glaciation in the Pyrenees: A critical review and new evidence from 10Be exposure ages, south-central Pyrenees.
Pallàs i Serra, Raimon
Paleoclimatologia
Plistocè
Holocè
Pirineus
Paleoclimatology
Pleistocene
Holocene
Pyrenees
title_short The late Pleistocene and Holocene glaciation in the Pyrenees: A critical review and new evidence from 10Be exposure ages, south-central Pyrenees.
title_full The late Pleistocene and Holocene glaciation in the Pyrenees: A critical review and new evidence from 10Be exposure ages, south-central Pyrenees.
title_fullStr The late Pleistocene and Holocene glaciation in the Pyrenees: A critical review and new evidence from 10Be exposure ages, south-central Pyrenees.
title_full_unstemmed The late Pleistocene and Holocene glaciation in the Pyrenees: A critical review and new evidence from 10Be exposure ages, south-central Pyrenees.
title_sort The late Pleistocene and Holocene glaciation in the Pyrenees: A critical review and new evidence from 10Be exposure ages, south-central Pyrenees.
dc.creator.none.fl_str_mv Pallàs i Serra, Raimon
Rodés Bolumburu, Ángel
Braucher, Régis
Carcaillet, J.
Ortuño Candela, Maria
Bordonau i Ibern, Jaume
Bourlès, Didier
Vilaplana, Joan Manuel
Masana, Eulàlia
Santanach i Prat, Pere F., 1946-
author Pallàs i Serra, Raimon
author_facet Pallàs i Serra, Raimon
Rodés Bolumburu, Ángel
Braucher, Régis
Carcaillet, J.
Ortuño Candela, Maria
Bordonau i Ibern, Jaume
Bourlès, Didier
Vilaplana, Joan Manuel
Masana, Eulàlia
Santanach i Prat, Pere F., 1946-
author_role author
author2 Rodés Bolumburu, Ángel
Braucher, Régis
Carcaillet, J.
Ortuño Candela, Maria
Bordonau i Ibern, Jaume
Bourlès, Didier
Vilaplana, Joan Manuel
Masana, Eulàlia
Santanach i Prat, Pere F., 1946-
author2_role author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Paleoclimatologia
Plistocè
Holocè
Pirineus
Paleoclimatology
Pleistocene
Holocene
Pyrenees
topic Paleoclimatologia
Plistocè
Holocè
Pirineus
Paleoclimatology
Pleistocene
Holocene
Pyrenees
description A compilation and a critical assessment of the 14C data set available show that the chronology of glacial events in the Pyrenees is not well constrained. After reviewing the literature on glacial reconstruction, we suggest a simplified subdivision of the Pyrenean last glacial cycle record into Last Pleniglacial, Deglaciation, and Neoglacial. To improve the numerical glacial chronology, we provide 10Be surface exposure ages for 5 glacial erosion surfaces, 9 moraines and 2 erratics in the Upper Noguera Ribagorc-ana Valley (south-central Pyrenees). Published corrected 14C data and new 10Be exposure ages indicate that the major phase of moraine building recorded in this valley during the Last Pleniglacial probably occurred after 25 ka BP. This age calls in question the generally accepted hypothesis of a very early deglaciation of the Pyrenees ca 70-40 ka BP, and strongly suggests that the Pyrenees could have been in pleniglacial conditions during the Last Glacial Maximum (LGM). However, we do not exclude the possibility that the maximum glacier extent during the last glacial cycle had taken place much earlier than the LGM, as indicated by some published U-Th, AMS 14C and OSL data. We suggest that pleniglacial conditions could have taken place during a longer (b30-20 ka) period than generally assumed, and that the Last Pleniglacial could include several glacier fluctuations recorded irregularly in different valleys, with a last major glacier readvance taking place around the LGM. In addition, the Deglaciation is represented by a series of moraines deposited between ca 13.770.9 and 10.170.6 ka. This moraine series indicates a highly variable climatic pattern that is partly correlated with Greenland Stadial 1 (the Younger Dryas), and suggests that the Deglaciation could have continued into the early Holocene.
publishDate 2006
dc.date.none.fl_str_mv 2006
2020
2020
2020
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/acceptedVersion
format article
status_str acceptedVersion
dc.identifier.none.fl_str_mv https://hdl.handle.net/2445/163388
url https://hdl.handle.net/2445/163388
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Versió postprint del document publicat a: https://doi.org/10.1016/j.quascirev.2006.04.004
Quaternary Science Reviews, 2006, vol. 25, num. 21-22, p. 2937-2963
https://doi.org/10.1016/j.quascirev.2006.04.004
dc.rights.none.fl_str_mv (c) Elsevier Ltd, 2006
info:eu-repo/semantics/openAccess
rights_invalid_str_mv (c) Elsevier Ltd, 2006
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 59 p.
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier Ltd
publisher.none.fl_str_mv Elsevier Ltd
dc.source.none.fl_str_mv Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)
reponame:Recercat. Dipósit de la Recerca de Catalunya
instname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
instname_str Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
reponame_str Recercat. Dipósit de la Recerca de Catalunya
collection Recercat. Dipósit de la Recerca de Catalunya
repository.name.fl_str_mv
repository.mail.fl_str_mv
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