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dc.contributor.authorJiménez-Arias, Juan L.es_ES
dc.contributor.authorMata, M. Pilares_ES
dc.contributor.authorCorzo Rodríguez, Alfonsoes_ES
dc.contributor.authorPoulton, Simon W.es_ES
dc.contributor.authorMärz, Christianes_ES
dc.contributor.authorSánchez-Bellón, Ángeles_ES
dc.contributor.authorMartínez-López, Javieres_ES
dc.contributor.authorCasas Ruiz, Melquíadeses_ES
dc.contributor.authorGarcía-Robledo, Emilioes_ES
dc.contributor.authorBohórquez, Julioes_ES
dc.contributor.authorPapaspyrou, Sokratises_ES
dc.date.accessioned2019-01-04T12:43:23Z-
dc.date.available2019-01-04T12:43:23Z-
dc.date.issued2016-09-01-
dc.identifier.citationHolocene 26(9): 1355-1370 (2016)es_ES
dc.identifier.issn0959-6836-
dc.identifier.urihttp://hdl.handle.net/10261/173766-
dc.description.abstractIn this study, we reconstruct the recent environmental evolution of the inner Cadiz Bay using sedimentary records reaching back as far as AD 1700. We report lithological descriptions of the sediments and extensive mineralogical and geochemical analyses. An extraction technique that identifies different Fe phases provides an assessment of diagenetic alteration, which allows an estimation of the original organic matter inputs to the inner Cadiz Bay. Downcore variations in Corg/N ratios, δ13Corg and δ15N are related to changes in organic matter sources and the trophic state of the water column. The downcore records of selected trace metals (e.g. Pb, Zn and Cu) are interpreted to reflect changes in heavy metal pollution in the bay, while records of other elements (e.g. Mn and P) are likely overprinted by diagenetic alteration. Major environmental shifts took place during the 20th century, when the population around Cadiz Bay increased exponentially. Increases in sediment accumulation rates, organic matter inputs and heavy metal contents, in parallel with increases in δ13Corg and δ15N over this period, are interpreted as direct effects of the increasing anthropogenic influence in the area. The results of this study suggest that multiproxy approaches and detailed consideration of diagenetic overprinting are required to reconstruct past environmental conditions from coastal sediments.es_ES
dc.language.isoenges_ES
dc.publisherSage Publicationses_ES
dc.rightsclosedAccesses_ES
dc.subject210Pb datinges_ES
dc.subjectCadiz Bayes_ES
dc.subjectCoastal sedimentses_ES
dc.subjectEarly Holocenees_ES
dc.subjectIron speciationes_ES
dc.subjectMultiproxyes_ES
dc.subjectOrganic matter sourceses_ES
dc.subjectPollutiones_ES
dc.subjectSedimentation rateses_ES
dc.subjectSpaines_ES
dc.subjectStable isotopeses_ES
dc.subjectx-ray fluorescence core scanneres_ES
dc.titleA multiproxy study distinguishes environmental change from diagenetic alteration in the recent sedimentary record of the inner Cadiz Bay (SW Spain)es_ES
dc.typeartículoes_ES
dc.identifier.doi10.1177/0959683616640046-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://doi.org/10.1177/0959683616640046es_ES
dc.identifier.e-issn1477-0911-
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
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