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dc.contributor.authorPérez Díaz, Sebastián 
dc.contributor.authorRuiz Alonso, Mónica
dc.contributor.authorLópez Sáez, José Antonio
dc.contributor.authorAlday Ruiz, Alfonso
dc.contributor.authorCava Almuzara, Ana
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2024-04-05T10:04:14Z
dc.date.available2024-04-05T10:04:14Z
dc.date.issued2024-05
dc.identifier.issn0939-6314
dc.identifier.issn1617-6278
dc.identifier.otherPID2020-116598GB-I00es_ES
dc.identifier.otherPGC2018-093925-B-C33es_ES
dc.identifier.urihttps://hdl.handle.net/10902/32496
dc.description.abstractA strategic aim of research into climate change in the distant past is to respond to the contemporary challenges of global warming at the present. Determining the processes of adaptation by ecosystems to these challenges, evaluating the effects of environmental change on human communities and finding which regions are more or less sensitive to climate change are among the key topics of environmental research today. Throughout the past millennia, some of the most abrupt envi ronmental upheavals were the successive phases of the Late Pleistocene to Early Holocene transition, ranging from cold and dry to mild and damp climates. These phases differed in intensity and effects across all regions of the planet. In this paper, the long-term changes to both vegetation cover and human settlements within the upper Ebro river basin (northern Iberia, western Mediterranean) are shown by new palaeoenvironmental sequences from two archaeological sites dated between ca. 14,000 and 8,000 cal BP, which serve as proxy evidence for past vegetation cover. Summed radiocarbon probability distributions of other nearby archaeological sites were also used to study the dynamics of land occupation throughout the period. The main findings point to vegetation changes changing from the dominance of open landscapes with pines and deciduous woods during the late Pleistocene to the dominance of deciduous forest cover with few areas with open landscapes and far fewer pinewoods during the early Holocene.es_ES
dc.description.sponsorshipThis work has been developed under the “Gaps and Dates. Cultural dynamics in the Prehistoric Ebro Basin” project (PID2020-116598GB-I00-MCIN/AEI, Ministerio de Ciencia e Innovaciòn y la Agencia Estatal de Innovación); “Le Tardiglaciaire dans l’Arc atlantique: Interactions techniques, socio-économiques et graphiques entre communautés Humaines et Animales durant la transition Pléistocène-Holocène (14500–11000 cal bp), the TAIHA project (Agence National pour la Recherche 21-CE27-0007-01) and “Geología geocronología y paleobiología de los yacimientos de la sierra de Atapuerca VII” project ((2018-093925-B-C33- MCIU/AEI).es_ES
dc.format.extent19 p.es_ES
dc.language.isoenges_ES
dc.publisherSpringer Naturees_ES
dc.rights© The Author(s) 2023es_ES
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.sourceVegetation History and Archaeobotany, 2024, 33(3), 323-341es_ES
dc.subject.otherPalaeoenvironmentes_ES
dc.subject.otherArchaeological sitees_ES
dc.subject.otherRock shelteres_ES
dc.subject.otherLate Pleistocenees_ES
dc.subject.otherEarly Holocenees_ES
dc.subject.otherNorthern Iberian Peninsulaes_ES
dc.titleEnvironmental dynamics of the western european mediterranean landscape during the Pleistocene to Holocene transitiones_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.1007/s00334-023-00942-0es_ES
dc.rights.accessRightsopenAccesses_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PID2020-116598GB-I00/ES/GAPS AND DATES. DINAMICAS CULTURALES EN LA PREHISTORIA DE LA CUENCA DEL EBRO/
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PGC2018-093925-B-C33/ES/GEOLOGIA, GEOCRONOLOGIA Y PALEOBIOLOGIA DE LOS YACIMIENTOS DE LA SIERRA DE ATAPUERCA VII/
dc.identifier.DOI10.1007/s00334-023-00942-0
dc.type.versionpublishedVersiones_ES


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