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dc.rights.licenseopenen_US
hal.structure.identifierBiogéochimie-Traceurs-Paléoclimat [BTP]
dc.contributor.authorSICRE, Marie-Alexandrine
hal.structure.identifierGEOGLOB FSS
hal.structure.identifierLaboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques [LOCEAN]
dc.contributor.authorJALALI, Bassem
hal.structure.identifierConsejo Superior de Investigaciones Cientificas [España] = Spanish National Research Council [Spain] [CSIC]
dc.contributor.authorMARTRAT, Belen
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
hal.structure.identifierCentre de Formation et de Recherche sur les Environnements Méditérranéens [CEFREM]
dc.contributor.authorBASSETTI, Maria-Angela
hal.structure.identifierGEOGLOB FSS
dc.contributor.authorKALLEL, Nejib
dc.date.accessioned2024-10-11T07:17:11Z
dc.date.available2024-10-11T07:17:11Z
dc.date.issued2016
dc.identifier.issn0012-821Xen_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202417
dc.description.abstractEnThis study investigates the multidecadal-scale variability of sea surface temperatures (SSTs) in the convection region of the Gulf of Lion (NW Mediterranean Sea) over the full past 2000 yr (Common Era) using alkenone biomarkers. Our data show colder SSTs by 1.7 °C over most of the first millennium (200–800 AD) and by 1.3 °C during the Little Ice Age (LIA; 1400–1850 AD) than the 20th century mean (17.9 °C). Although on average warmer, those of the Medieval Climate Anomaly (MCA) (1000–1200 AD) were lower by 1 °C. We found a mean SST warming of 2 °C/100 yr over the last century in close agreement with the 0.22 and 0.26 °C/decade values calculated for the western Mediterranean Sea from in situ and satellite data, respectively. Our results also reveal strongly fluctuating SSTs characterized by cold extremes followed by abrupt warming during the LIA. We suggest that the coldest decades of the LIA were likely caused by prevailing negative EA states and associated anticyclone blocking over the North Atlantic resulting in cold continental northeasterly winds to blow over Western Europe and the Mediterranean region.
dc.language.isoENen_US
dc.subject.enCommon Era
dc.subject.ensea surface temperature
dc.subject.enalkenones
dc.subject.enMediterranean Sea
dc.subject.enEast 28
dc.title.enSea surface temperature variability in the North Western Mediterranean Sea (Gulf of Lion) during the Common Era
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.epsl.2016.09.032en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalEarth and Planetary Science Lettersen_US
bordeaux.page124-133en_US
bordeaux.volume456en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamGEOLSEDen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-01386646
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Earth%20and%20Planetary%20Science%20Letters&rft.date=2016&rft.volume=456&rft.spage=124-133&rft.epage=124-133&rft.eissn=0012-821X&rft.issn=0012-821X&rft.au=SICRE,%20Marie-Alexandrine&JALALI,%20Bassem&MARTRAT,%20Belen&SCHMIDT,%20Sabine&BASSETTI,%20Maria-Angela&rft.genre=article


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