Rapid climatic changes and resilient vegetation during the Lateglacial and Holocene in a continental region of south-western Europe

Palynological, sedimentological and geochemical analyses performed on the Villarquemado paleolake sequence (987 m a.s.l, 40°30′N; 1°18′W) reveal the vegetation dynamics and climate variability in continental Iberia over the last 13,500 cal yr BP. The Lateglacial and early Holocene periods are charac...

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Autores: Aranbarri, J., González-Sampériz, Penélope, Valero-Garcés, Blas L., Moreno Caballud, Ana, Sevilla-Callejo, Miguel, García-Prieto, E., Di Rita, Federico, Mata Campo, Maria Pilar, Morellón, Mario, Magri, Donatella, Rodríguez-Lázaro, Julio, Carrión, José S., Gil-Romera, Graciela
Tipo de recurso: artículo
Fecha de publicación:2014
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/90385
Acceso en línea:http://hdl.handle.net/10261/90385
Access Level:acceso abierto
Palabra clave:Holocene
Multiproxy reconstruction
Vegetation resilience
Pinewoods
Aridity
Continental Iberia
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spelling Rapid climatic changes and resilient vegetation during the Lateglacial and Holocene in a continental region of south-western EuropeAranbarri, J.González-Sampériz, PenélopeValero-Garcés, Blas L.Moreno Caballud, AnaSevilla-Callejo, MiguelGarcía-Prieto, E.Di Rita, FedericoMata Campo, Maria PilarMorellón, MarioMagri, DonatellaRodríguez-Lázaro, JulioCarrión, José S.Gil-Romera, GracielaHoloceneMultiproxy reconstructionVegetation resiliencePinewoodsAridityContinental IberiaPalynological, sedimentological and geochemical analyses performed on the Villarquemado paleolake sequence (987 m a.s.l, 40°30′N; 1°18′W) reveal the vegetation dynamics and climate variability in continental Iberia over the last 13,500 cal yr BP. The Lateglacial and early Holocene periods are characterized by arid conditions with a stable landscape dominated by pinewoods and steppe until ca. 7780 cal yr BP, despite sedimentological evidence for large paleohydrological fluctuations in the paleolake. The most humid phase occurred between ca. 7780 and 5000 cal yr BP and was characterized by the maximum spread of mesophytes (e.g., Betula, Corylus, Quercus faginea type), the expansion of a mixed Mediterranean oak woodland with evergreen Quercus as dominant forest communities and more frequent higher lake level periods. The return of a dense pinewood synchronous with the depletion of mesophytes characterizes the mid-late Holocene transition (ca. 5000 cal yr BP) most likely as a consequence of an increasing aridity that coincides with the reappearance of a shallow, carbonate wetland environment. The paleohydrological and vegetation evolution shows similarities with other continental Mediterranean areas of Iberia and demonstrates a marked resilience of terrestrial vegetation and gradual responses to millennial-scale climate fluctuations. Human impact is negligible until the Ibero-Roman period (ca. 2500 cal yr BP) when a major deforestation occurred in the nearby pine forest. The last 1500 years are characterized by increasing landscape management, mainly associated with grazing practices shaping the current landscape.The funding for the present study derives from DINAMO (CGL-BOS 2009–07992), DINAMO2 (CGL-BOS 2012–33063), IBERIAN PALEOFLORA (CGL-BOS 2012–31717) and GRACCIE-CONSOLIDER (CSD2007-00067) projects, provided by the Spanish Inter-Ministry Commission of Science and Technology (CICYT). Josu Aranbarri acknowledges the predoctoral funding provided by the Basque Country Government (ref: FI-2010-5). Ana Moreno, Graciela Gil-Romera and Mario Morellón hold post-doctoral contracts funded by “Ramon y Cajal (ref: RYC-2008-02431)”, “Juan de la Cierva (ref: JCI2009-04345)” and “JAE DOC CSIC (ref: JAEDOC-2011-026)” programms, respectively. Eduardo García-Prieto is supported by a predoctoral FPI grant (BES-2010-038593). We are very greateful to Aida Adsuar, Beatriz Bueno and Raquel López-Cantero for their assistance in core sampling and laboratory procedures. Josu Aranbarri thanks collegues from the Dipartimento di Biologia Ambientale, especially Alessandra Celant, for continuous encouragement. We would also like to thank Thomas M. Cronin, Anthony C. Stevenson and an anonymous reviewer for their valuable suggestions.Peer reviewedElsevierConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]201420142014info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501http://hdl.handle.net/10261/90385reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Ingléshttp://dx.doi.org/10.1016/j.gloplacha.2014.01.003Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/903852026-05-22T06:33:51Z
dc.title.none.fl_str_mv Rapid climatic changes and resilient vegetation during the Lateglacial and Holocene in a continental region of south-western Europe
title Rapid climatic changes and resilient vegetation during the Lateglacial and Holocene in a continental region of south-western Europe
spellingShingle Rapid climatic changes and resilient vegetation during the Lateglacial and Holocene in a continental region of south-western Europe
Aranbarri, J.
Holocene
Multiproxy reconstruction
Vegetation resilience
Pinewoods
Aridity
Continental Iberia
title_short Rapid climatic changes and resilient vegetation during the Lateglacial and Holocene in a continental region of south-western Europe
title_full Rapid climatic changes and resilient vegetation during the Lateglacial and Holocene in a continental region of south-western Europe
title_fullStr Rapid climatic changes and resilient vegetation during the Lateglacial and Holocene in a continental region of south-western Europe
title_full_unstemmed Rapid climatic changes and resilient vegetation during the Lateglacial and Holocene in a continental region of south-western Europe
title_sort Rapid climatic changes and resilient vegetation during the Lateglacial and Holocene in a continental region of south-western Europe
dc.creator.none.fl_str_mv Aranbarri, J.
González-Sampériz, Penélope
Valero-Garcés, Blas L.
Moreno Caballud, Ana
Sevilla-Callejo, Miguel
García-Prieto, E.
Di Rita, Federico
Mata Campo, Maria Pilar
Morellón, Mario
Magri, Donatella
Rodríguez-Lázaro, Julio
Carrión, José S.
Gil-Romera, Graciela
author Aranbarri, J.
author_facet Aranbarri, J.
González-Sampériz, Penélope
Valero-Garcés, Blas L.
Moreno Caballud, Ana
Sevilla-Callejo, Miguel
García-Prieto, E.
Di Rita, Federico
Mata Campo, Maria Pilar
Morellón, Mario
Magri, Donatella
Rodríguez-Lázaro, Julio
Carrión, José S.
Gil-Romera, Graciela
author_role author
author2 González-Sampériz, Penélope
Valero-Garcés, Blas L.
Moreno Caballud, Ana
Sevilla-Callejo, Miguel
García-Prieto, E.
Di Rita, Federico
Mata Campo, Maria Pilar
Morellón, Mario
Magri, Donatella
Rodríguez-Lázaro, Julio
Carrión, José S.
Gil-Romera, Graciela
author2_role author
author
author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
dc.subject.none.fl_str_mv Holocene
Multiproxy reconstruction
Vegetation resilience
Pinewoods
Aridity
Continental Iberia
topic Holocene
Multiproxy reconstruction
Vegetation resilience
Pinewoods
Aridity
Continental Iberia
description Palynological, sedimentological and geochemical analyses performed on the Villarquemado paleolake sequence (987 m a.s.l, 40°30′N; 1°18′W) reveal the vegetation dynamics and climate variability in continental Iberia over the last 13,500 cal yr BP. The Lateglacial and early Holocene periods are characterized by arid conditions with a stable landscape dominated by pinewoods and steppe until ca. 7780 cal yr BP, despite sedimentological evidence for large paleohydrological fluctuations in the paleolake. The most humid phase occurred between ca. 7780 and 5000 cal yr BP and was characterized by the maximum spread of mesophytes (e.g., Betula, Corylus, Quercus faginea type), the expansion of a mixed Mediterranean oak woodland with evergreen Quercus as dominant forest communities and more frequent higher lake level periods. The return of a dense pinewood synchronous with the depletion of mesophytes characterizes the mid-late Holocene transition (ca. 5000 cal yr BP) most likely as a consequence of an increasing aridity that coincides with the reappearance of a shallow, carbonate wetland environment. The paleohydrological and vegetation evolution shows similarities with other continental Mediterranean areas of Iberia and demonstrates a marked resilience of terrestrial vegetation and gradual responses to millennial-scale climate fluctuations. Human impact is negligible until the Ibero-Roman period (ca. 2500 cal yr BP) when a major deforestation occurred in the nearby pine forest. The last 1500 years are characterized by increasing landscape management, mainly associated with grazing practices shaping the current landscape.
publishDate 2014
dc.date.none.fl_str_mv 2014
2014
2014
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/90385
url http://hdl.handle.net/10261/90385
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv http://dx.doi.org/10.1016/j.gloplacha.2014.01.003

dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
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
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repository.mail.fl_str_mv
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