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Upper Pleistocene-Holocene morphosedimentary evolution of the Valsalada alluvial system (Leciñena, Monegros): palaeoenvironmental approach

dc.contributor.authorSancho, Carlos
dc.contributor.authorMuñoz Jiménez, Arsenio
dc.contributor.authorPeña, José Luis
dc.contributor.authorGonzález, P.
dc.date.accessioned2014-07-09T11:13:03Z
dc.date.available2014-07-09T11:13:03Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10272/8481
dc.description.abstractA first approach to the palaeoenvironmental significance of the Valsalada (Central Ebro basin) alluvial record, Upper Pleistocene-Holocene in age, is presented starting from geomorhological, sedimentological and radiocarbon data. This morphosedimentary sequence is made up by three evolutionary phases: 1) lacustrine stage (37,050±50 BP) under cool and humid conditions, 2) alluvial stage (from 10,550±80 BP to 3,225±50 BP) related to cold and wet climate and 3) colluvial fans stage (1,640±50 BP) during arid climate with human action influence. The Valsalada alluvial system shows a singular morphosedimentary evolution strongly influenced by climatic changes bearing variations in water dischar ges and hydrological availability in surrounding saline wetlandsen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherMorphosedimentary alluvial recorden_US
dc.subject.otherUpper Pleistocene-Holoceneen_US
dc.subject.otherEnvironmental changeen_US
dc.subject.otherCentral Ebro basinen_US
dc.titleEvolución morfosedimentaria del sistema aluvial de Valsalada (Leciñena, Los Monegros) durante el Pleistoceno superior-Holoceno: aproximación paleoambientalen_US
dc.titleUpper Pleistocene-Holocene morphosedimentary evolution of the Valsalada alluvial system (Leciñena, Monegros): palaeoenvironmental approacheng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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