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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, María Francisca
dc.contributor.authorDorado Valiño, Miriam
dc.contributor.authorRuiz Zapata, María Blanca
dc.contributor.authorGil García, María José
dc.contributor.authorGómez González, Clemencia
dc.contributor.authorFranco Múgica, Fátima
dc.date.accessioned2025-04-24T11:20:55Z
dc.date.available2025-04-24T11:20:55Z
dc.date.issued2014
dc.identifier.citationJ.A. López-Sáez; D. Abel-Schaad; S. Pérez-Díaz; A. Blanco-González; F. Alba-Sánchez; M. Dorado-Valiño; B. Ruiz-Zapata; M. Gil-García; M. Gómez-González; F. Franco-Múgica (2014): "Vegetation history, climate and human impact in the Spanish Central System over the last 9,000 years." Quaternary International, 353, pp. 98 - 122. http://dx.doi.org/10.1016/j.quaint.2013.06.034es_ES
dc.identifier.issn1040-6182
dc.identifier.urihttp://hdl.handle.net/10366/164792
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 highmountains. The pollen record has allowed us to relate two cultural periods of changing, the Copper AgeeEarly Bronze Age and Late Bronze AgeeEarly 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.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectPalynologyes_ES
dc.subjectHuman impactes_ES
dc.subjectClimate changees_ES
dc.subjectLater prehistoryes_ES
dc.subjectCentral System (Spain)es_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.subject.unesco2416.03 Palinologíaes_ES
dc.subject.unesco5504.05 Prehistoriaes_ES
dc.subject.unesco5505.01 Arqueologíaes_ES
dc.identifier.doi10.1016/j.quaint.2013.06.034
dc.rights.accessRightsinfo:eu-repo/semantics/closedAccesses_ES
dc.journal.titleQuaternary Internationales_ES
dc.volume.number353es_ES
dc.page.initial98es_ES
dc.page.final122es_ES
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones_ES


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