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dc.contributor.authorLópez-Sáez, José Antonio
dc.contributor.authorAbel-Schaad, Daniel
dc.contributor.authorPérez Díaz, Sebastián 
dc.contributor.authorBlanco-González, Antonio
dc.contributor.authorAlba Sánchez, Francisca
dc.contributor.authorDorado, Miriam
dc.contributor.authorRuiz-Zapata, Blanca
dc.contributor.authorGil-García, María José
dc.contributor.authorGómez-González, Clemencia
dc.contributor.authorFranco-Múgica, Fátima
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2025-01-24T11:15:39Z
dc.date.available2025-01-24T11:15:39Z
dc.date.issued2014-12-05
dc.identifier.issn1040-6182
dc.identifier.issn1873-4553
dc.identifier.otherCSD2007-00058es_ES
dc.identifier.otherP11-RNM-7033es_ES
dc.identifier.urihttps://hdl.handle.net/10902/35155
dc.description.abstractIn this paper we present a review of the available Holocene pollen records from the Spanish Central System (113 sites and 150 14C dates). Palynological data obtained from pollen analyses of peat-bogs, lakes and archaeological sites, as well as radiocarbon dating, were used to infer the human impact on vegetation and landscape during the last 9 millennia. The Neolithic contribution to the configuration of landscape is scarce, limited to the valleys, while Chalcolithic settlements and their related activities (agriculture and grazing) represent the first evidence of significant human impact on the high-mountains. The pollen record has allowed us to relate two cultural periods of changing, the Copper Age-Early Bronze Age and Late Bronze Age-Early Iron Age transitions, to abrupt climate disruptions, the so-called 4.2 and 2.8 ka cal BP events respectively. From the Iron Age to the Early Middle Ages, anthropic activities were still sporadic, mainly located in the lowlands, but from the Feudal Period onwards, when La Mesta transhumance system takes place, high-mountain landscapes changed dramatically. Late Modern Period brings a further intensification of human pressure, especially related to forestry, with widespread pinewood afforestation.es_ES
dc.description.sponsorshipWe are indebted to the CONSOLIDER-INGENIO 2010 Program (CSD2007-00058), EXCELENCIA 2011 Program (RNM-7033) and AGRIWESTMED (ERC-Advanced Grants, proposal n° 230561) for financial and technical support. We wish to thank to Fernando Pulido and Ana Valdeolmillos for valuable suggestions. SPD is currently supported by a post-doctoral research grant (Basque Government) at Toulouse-Le Mirail Universityes_ES
dc.format.extent25 p.es_ES
dc.language.isoenges_ES
dc.publisherElsevier Ltdes_ES
dc.rights© 2014. This manuscript version is made available under the CC-BY-NC-ND 4.0 licensees_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.sourceQuaternary International, 2014, 353, 98-122es_ES
dc.titleVegetation history, climate and human impact in the Spanish Central System over the last 9000 yearses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.1016/j.quaint.2013.06.034es_ES
dc.rights.accessRightsopenAccesses_ES
dc.identifier.DOI10.1016/j.quaint.2013.06.034
dc.type.versionacceptedVersiones_ES


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© 2014. This manuscript version is made available under the CC-BY-NC-ND 4.0 licenseExcepto si se señala otra cosa, la licencia del ítem se describe como © 2014. This manuscript version is made available under the CC-BY-NC-ND 4.0 license