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dc.rights.licenseopenen_US
hal.structure.identifierBirbal Sahni Institute of Palaeosciences
dc.contributor.authorKUMAR SHUKLA, Sunil
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCROSTA, Xavier
dc.date.accessioned2024-10-07T08:44:09Z
dc.date.available2024-10-07T08:44:09Z
dc.date.issued2016-11-02
dc.identifier.issn0954-1020en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202273
dc.description.abstractEnIn the open Southern Ocean (SO), both modern and past size changes of the diatom Fragilariopsis kerguelensis appear to be strongly controlled by iron availability. Conversely, sea surface temperatures (SST) and sea ice seasonal dynamics take over in the seasonal sea-ice zone where iron is not limiting. No information exists on F. kerguelensis biometry from the subtropical SO, on the other extreme of the thermal and nutrient gradients. We present here new data on mean valve area of F. kerguelensis (FkergArea) from a sediment core covering the last ~ 42 cal kyrs from the southern Subtropical Front (SSTF) of the Indian sector of the SO, where iron and silica stocks are thought to have been consistently low over this period. Our results suggest that larger F. kerguelensis valves occurred during the Last Glacial period, and declined during the Holocene period. These findings indicate that more favourable SST, within the F. kerguelensis ecological range, during the Last Glacial period may have enabled F. kerguelensis to make better use of the low silica stocks prevailing in the subtropical zone leading to larger valves. Conversely, declining FkergArea during the deglacial and the Holocene periods may have been a result of higher SST which hampered the utilization of silica.
dc.language.isoENen_US
dc.subject.enbiometry
dc.subject.endiatoms
dc.subject.ennutrient cycling
dc.subject.ensea surface temperature
dc.title.enFragilariopsis kerguelensis size variability from the Indian subtropical Southern Ocean over the last 42 000 years
dc.typeArticle de revueen_US
dc.identifier.doi10.1017/S095410201600050Xen_US
dc.subject.halPlanète et Univers [physics]/Océan, Atmosphèreen_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Océanographieen_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Climatologieen_US
bordeaux.journalAntarctic Scienceen_US
bordeaux.page139-146en_US
bordeaux.volume29en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue2en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-02105540
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=Antarctic%20Science&rft.date=2016-11-02&rft.volume=29&rft.issue=2&rft.spage=139-146&rft.epage=139-146&rft.eissn=0954-1020&rft.issn=0954-1020&rft.au=KUMAR%20SHUKLA,%20Sunil&CROSTA,%20Xavier&rft.genre=article


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