Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa y Monte Perdido durante el Holoceno

[EN] New and more detailed geomorphological, hydrological, vegetational and climatic reconstructions for the Holocene in the PNOMP have been obtained from the pluridisciplinary study of three records (La Larri, La Estiva and Marboré). La Larri paleolake was originated when the Pineta glacier blocked...

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Autores: Valero-Garcés, Blas L., Oliva-Urcia, Belén, Moreno Caballud, Ana, Rico, María Teresa, Mata Campo, Maria Pilar, Salazar Rincón, Ángel Enrique, Rieradevall, María, García-Ruiz, José María, Chueca Cía, Javier, González-Sampériz, Penélope, Pérez-Sanz, Ana, Salabarnada, Ariadna, Pardo, Alfonso, Sancho Marcén, Carlos, Barreiro-Lostres, Fernando, Bartolomé, Miguel, García-Prieto, E., Gil-Romera, Graciela, López Merino, Lourdes, Sevilla-Callejo, Miguel, Tarrats, P.
Tipo de recurso: otro
Fecha de publicación:2013
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/100566
Acceso en línea:http://hdl.handle.net/10261/100566
Access Level:acceso abierto
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spelling Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa y Monte Perdido durante el HolocenoValero-Garcés, Blas L.Oliva-Urcia, BelénMoreno Caballud, AnaRico, María TeresaMata Campo, Maria PilarSalazar Rincón, Ángel EnriqueRieradevall, MaríaGarcía-Ruiz, José MaríaChueca Cía, JavierGonzález-Sampériz, PenélopePérez-Sanz, AnaSalabarnada, AriadnaPardo, AlfonsoSancho Marcén, CarlosBarreiro-Lostres, FernandoBartolomé, MiguelGarcía-Prieto, E.Gil-Romera, GracielaLópez Merino, LourdesSevilla-Callejo, MiguelTarrats, P.[EN] New and more detailed geomorphological, hydrological, vegetational and climatic reconstructions for the Holocene in the PNOMP have been obtained from the pluridisciplinary study of three records (La Larri, La Estiva and Marboré). La Larri paleolake was originated when the Pineta glacier blocked the valley before 35 ka and existed till 11 ka when it was drained when the glacier receded. Marboré Lake record spans the last 11 kyrs. Facies, geochemistry and magnetic properties identify a large glacier influence between 11 and 9.2 ka. The 9.2- 4.1 ka was relatively more humid. The Mid Holocene transition ca 5 – 4.5 ka to more arid conditions was detected in both Marboré and La Estiva. During the last 3 millennia several arid phases occurred (end of the Roman Period, the High Middle Ages, the Medieval Climate Anomaly). The LIA is characterized by higher runoff and colder climate. However, pollen studies indicate a higher human pressure in the mountains during this period. Both, historic global atmospheric contamination and local influx of the mining activities in the Alto Cinca valley are detected in the Marboré record. The Marboré and Monte Perdido glaciers have been receding during the last centuries, with several moraines ascribed to the first phase of the LIA, and a large expansion during the early XXth century. The main factors controlling recent glacier retreat are the increase in maximum summer temperatures and the decrease in snow precipitation in winter.Proyecto financiado por el Organismo Autónomo Parques Nacionales Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa - Monte Perdido durante el Holoceno (ref: 83/2009). Agradecemos a todo el personal del PNOMP su apoyo para la realización de los trabajos de campo.Peer ReviewedOrganismo Autónomo Parques Nacionales (España)2014201420132014info:eu-repo/semantics/otherhttp://purl.org/coar/resource_type/c_3248info:eu-repo/semantics/bookParthttp://hdl.handle.net/10261/100566reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Españolhttp://www.magrama.gob.es/es/parques-nacionales-oapn/programa-investigacion/01_VALERO_tcm7-313570.pdfinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/1005662026-05-22T06:33:51Z
dc.title.none.fl_str_mv Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa y Monte Perdido durante el Holoceno
title Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa y Monte Perdido durante el Holoceno
spellingShingle Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa y Monte Perdido durante el Holoceno
Valero-Garcés, Blas L.
title_short Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa y Monte Perdido durante el Holoceno
title_full Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa y Monte Perdido durante el Holoceno
title_fullStr Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa y Monte Perdido durante el Holoceno
title_full_unstemmed Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa y Monte Perdido durante el Holoceno
title_sort Dinámica glacial, clima y vegetación en el Parque Nacional de Ordesa y Monte Perdido durante el Holoceno
dc.creator.none.fl_str_mv Valero-Garcés, Blas L.
Oliva-Urcia, Belén
Moreno Caballud, Ana
Rico, María Teresa
Mata Campo, Maria Pilar
Salazar Rincón, Ángel Enrique
Rieradevall, María
García-Ruiz, José María
Chueca Cía, Javier
González-Sampériz, Penélope
Pérez-Sanz, Ana
Salabarnada, Ariadna
Pardo, Alfonso
Sancho Marcén, Carlos
Barreiro-Lostres, Fernando
Bartolomé, Miguel
García-Prieto, E.
Gil-Romera, Graciela
López Merino, Lourdes
Sevilla-Callejo, Miguel
Tarrats, P.
author Valero-Garcés, Blas L.
author_facet Valero-Garcés, Blas L.
Oliva-Urcia, Belén
Moreno Caballud, Ana
Rico, María Teresa
Mata Campo, Maria Pilar
Salazar Rincón, Ángel Enrique
Rieradevall, María
García-Ruiz, José María
Chueca Cía, Javier
González-Sampériz, Penélope
Pérez-Sanz, Ana
Salabarnada, Ariadna
Pardo, Alfonso
Sancho Marcén, Carlos
Barreiro-Lostres, Fernando
Bartolomé, Miguel
García-Prieto, E.
Gil-Romera, Graciela
López Merino, Lourdes
Sevilla-Callejo, Miguel
Tarrats, P.
author_role author
author2 Oliva-Urcia, Belén
Moreno Caballud, Ana
Rico, María Teresa
Mata Campo, Maria Pilar
Salazar Rincón, Ángel Enrique
Rieradevall, María
García-Ruiz, José María
Chueca Cía, Javier
González-Sampériz, Penélope
Pérez-Sanz, Ana
Salabarnada, Ariadna
Pardo, Alfonso
Sancho Marcén, Carlos
Barreiro-Lostres, Fernando
Bartolomé, Miguel
García-Prieto, E.
Gil-Romera, Graciela
López Merino, Lourdes
Sevilla-Callejo, Miguel
Tarrats, P.
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
description [EN] New and more detailed geomorphological, hydrological, vegetational and climatic reconstructions for the Holocene in the PNOMP have been obtained from the pluridisciplinary study of three records (La Larri, La Estiva and Marboré). La Larri paleolake was originated when the Pineta glacier blocked the valley before 35 ka and existed till 11 ka when it was drained when the glacier receded. Marboré Lake record spans the last 11 kyrs. Facies, geochemistry and magnetic properties identify a large glacier influence between 11 and 9.2 ka. The 9.2- 4.1 ka was relatively more humid. The Mid Holocene transition ca 5 – 4.5 ka to more arid conditions was detected in both Marboré and La Estiva. During the last 3 millennia several arid phases occurred (end of the Roman Period, the High Middle Ages, the Medieval Climate Anomaly). The LIA is characterized by higher runoff and colder climate. However, pollen studies indicate a higher human pressure in the mountains during this period. Both, historic global atmospheric contamination and local influx of the mining activities in the Alto Cinca valley are detected in the Marboré record. The Marboré and Monte Perdido glaciers have been receding during the last centuries, with several moraines ascribed to the first phase of the LIA, and a large expansion during the early XXth century. The main factors controlling recent glacier retreat are the increase in maximum summer temperatures and the decrease in snow precipitation in winter.
publishDate 2013
dc.date.none.fl_str_mv 2013
2014
2014
2014
dc.type.none.fl_str_mv info:eu-repo/semantics/other
http://purl.org/coar/resource_type/c_3248
dc.type.openaire.fl_str_mv info:eu-repo/semantics/bookPart
format other
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/100566
url http://hdl.handle.net/10261/100566
dc.language.none.fl_str_mv Español
language_invalid_str_mv Español
dc.relation.none.fl_str_mv http://www.magrama.gob.es/es/parques-nacionales-oapn/programa-investigacion/01_VALERO_tcm7-313570.pdf
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Organismo Autónomo Parques Nacionales (España)
publisher.none.fl_str_mv Organismo Autónomo Parques Nacionales (España)
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
instname_str Consejo Superior de Investigaciones Científicas (CSIC)
reponame_str DIGITAL.CSIC. Repositorio Institucional del CSIC
collection DIGITAL.CSIC. Repositorio Institucional del CSIC
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15.812429

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