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dc.rights.licenseopenen_US
hal.structure.identifierGéosciences Montpellier
dc.contributor.authorDEZILEAU, Laurent
hal.structure.identifierUniversidad de Murcia
dc.contributor.authorPEREZ-RUZAFA, Angel
hal.structure.identifierArchéologie des Sociétés Méditerranéennes [ASM]
dc.contributor.authorBLANCHEMANCHE, Philippe
hal.structure.identifierArchéologie des Sociétés Méditerranéennes [ASM]
dc.contributor.authorDEGEAI, Jean-Philippe
hal.structure.identifierUniversité MohammedV-Agdal, Rabat
dc.contributor.authorRAJI, Otmane
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARTINEZ, Philippe
IDREF: 154067628
hal.structure.identifierUniversidad de Murcia
dc.contributor.authorMARCOS, Concepcion
hal.structure.identifierLaboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]
hal.structure.identifierGéochrononologie Traceurs Archéométrie [GEOTRAC]
hal.structure.identifierGlaces et Continents, Climats et Isotopes Stables [GLACCIOS]
dc.contributor.authorVON GRAFENSTEIN, Ulrich
dc.date.accessioned2024-10-11T09:19:41Z
dc.date.available2024-10-11T09:19:41Z
dc.date.issued2016
dc.identifier.issn1814-9324en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202424
dc.description.abstractEnStorms and tsunamis, which may seriously endanger human society, are amongst the most devastating marine catastrophes that can occur in coastal areas. Many such events are known and have been reported for the Mediterranean, a region where high-frequency occurrences of these extreme events coincides with some of the most densely populated coastal areas in the world. In a sediment core from the Mar Menor (SE Spain), we discovered eight coarse-grained layers which document marine incursions during periods of intense storm activity or tsunami events. Based on radiocarbon dating, these extreme events occurred around 5250, 4000, 3600, 3010, 2300, 1350, 650, and 80 years cal BP. No comparable events have been observed during the 20th and 21st centuries. The results indicate little likelihood of a tsunami origin for these coarse-grained layers, although historical tsunami events are recorded in this region. These periods of surge events seem to coincide with the coldest periods in Europe during the late Holocene, suggesting a control by a climatic mechanism for periods of increased storm activity. Spectral analyses performed on the sand percentage revealed four major periodicities of 1228 ± 327, 732 ± 80, 562 ± 58, and 319 ± 16 years. Amongst the well-known proxies that have revealed a millennial-scale climate variability during the Holocene, the ice-rafted debris (IRD) indices in the North Atlantic developed by Bond et al. (1997, 2001) present a cyclicity of 1470 ± 500 years, which matches the 1228 ± 327-year periodicity evidenced in the Mar Menor, considering the respective uncertainties in the periodicities. Thus, an in-phase storm activity in the western Mediterranean is found with the coldest periods in Europe and with the North Atlantic thermohaline circulation. However, further investigations, such as additional coring and high-resolution coastal imagery, are needed to better constrain the main cause of these multiple events.
dc.language.isoENen_US
dc.rightsAttribution 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.title.enExtreme storms during the last 6500 years from lagoonal sedimentary archives in the Mar Menor (SE Spain)
dc.typeArticle de revueen_US
dc.identifier.doi10.5194/cp-12-1389-2016en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Climatologieen_US
dc.subject.halSciences de l'environnement/Milieux et Changements globauxen_US
bordeaux.journalClimate of the Pasten_US
bordeaux.page1389-1400en_US
bordeaux.volume12en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue6en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-01357199
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=Climate%20of%20the%20Past&rft.date=2016&rft.volume=12&rft.issue=6&rft.spage=1389-1400&rft.epage=1389-1400&rft.eissn=1814-9324&rft.issn=1814-9324&rft.au=DEZILEAU,%20Laurent&PEREZ-RUZAFA,%20Angel&BLANCHEMANCHE,%20Philippe&DEGEAI,%20Jean-Philippe&RAJI,%20Otmane&rft.genre=article


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