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Assessment of sea surface temperature changes in the Gulf of Cadiz during the last 30 ka: Implications for glacial changes in the regional hydrography

dc.contributor.authorPenaud, A.
dc.contributor.authorEynaud, F.
dc.contributor.authorVoelker, Antje
dc.contributor.authorKageyama, M.
dc.contributor.authorMarret, F.
dc.contributor.authorTuron, J.L.
dc.contributor.authorBlamart, D.
dc.contributor.authorMulder, T.
dc.contributor.authorRossignol, L.
dc.date.accessioned2020-07-24T12:27:51Z
dc.date.available2020-07-24T12:27:51Z
dc.date.issued2011
dc.date.updated2020-07-23T15:22:25Z
dc.description.abstractNew dinocyst analyses were conducted on core MD99-2339 retrieved from the central Gulf of Cadiz. Dinocyst and foraminiferal assemblages from this core are combined with existing data off SW Portugal and NW Morocco to investigate past hydrological and primary productivity regimes in the subtropical NE Atlantic Ocean over the last 30 ka. Our results have revealed highest upwelling intensity during Heinrich Stadial 1 (HS 1) and the Younger Dryas and weaker upwelling cells during the Last Glacial Maximum (LGM) and HS 2, off the SW Iberian and NW Moroccan margins. Similar assemblages between the Gulf of Cadiz and the NW Moroccan margin, and distinct species off Portugal, were observed during the cold climatic extremes that punctuated the last 30 ka. This pattern has been linked to the occurrence of a hydrological structure between SW Iberia and Cadiz during the last glacial period, perhaps similar to the modern Azores Front. This front was probably responsible locally for heterotrophic dinocysts found in the Gulf of Cadiz during the last glacial period, even if this sector is not conductive to upwelling phenomena by Ekman transport. Regional reconstructions of paleo-sea-surface temperatures (SSTs) using dinocyst and foraminiferal transfer functions, as well as alkenones, are also discussed and depict coherent scenarios over the last 30 ka. Seasonal reconstructions Correspondence to: A. Penaud (aurelie.penaud@univ-brest.fr.) of LGM SSTs obtained with this multi-proxy panel are discussed jointly with model outputs in order to contribute to ongoing efforts in model-data comparisonpt_PT
dc.description.sponsorshipC2007-FCT/319/2006pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doi10.5194/bg-8-2295-2011pt_PT
dc.identifier.issn1726-4170
dc.identifier.slugcv-prod-423505
dc.identifier.urihttp://hdl.handle.net/10400.1/14513
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherEuropean Geosciences Unionpt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectDinocystspt_PT
dc.subjectGulf of Cadizpt_PT
dc.subjectPlanktonic foraminiferapt_PT
dc.subjectMicropaleontologypt_PT
dc.subjectPaleotemperaturept_PT
dc.subjectLast Glacial Maximumpt_PT
dc.subjectAbrupt climate changept_PT
dc.titleAssessment of sea surface temperature changes in the Gulf of Cadiz during the last 30 ka: Implications for glacial changes in the regional hydrographypt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage2316pt_PT
oaire.citation.issue8pt_PT
oaire.citation.startPage2295pt_PT
oaire.citation.titleBiogeosciencespt_PT
oaire.citation.volume8pt_PT
person.familyNameVoelker
person.givenNameAntje
person.identifier2315310
person.identifier.ciencia-idC11E-D8E6-CDFA
person.identifier.orcid0000-0001-6465-6023
person.identifier.ridC-5427-2012
person.identifier.scopus-author-id8784446000
rcaap.cv.cienciaidC11E-D8E6-CDFA | Antje Helga Luise Voelker
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationbca80a86-eb35-4bca-a4ba-85b53831d69e
relation.isAuthorOfPublication.latestForDiscoverybca80a86-eb35-4bca-a4ba-85b53831d69e

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