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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorEL BANI ALTUNA, Naima
dc.contributor.authorPIEŃKOWSKI, Anna J.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorEYNAUD, Frederique
IDREF: 144113570
dc.contributor.authorTHIESSEN, Rabecca
dc.date.accessioned2024-04-24T14:55:04Z
dc.date.available2024-04-24T14:55:04Z
dc.date.issued2018-06-01
dc.identifier.issn0377-8398en_US
dc.identifier.urioai:crossref.org:10.1016/j.marmicro.2018.05.004
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199329
dc.description.abstractEnNeogloboquadrina pachyderma represents a key planktonic foraminifera species in the boreal Atlantic and has been extensively used as a paleoceanographic tool in polar to subpolar environments. The species shows an intraspecific morphological variability, displaying at least 5 different morphotypes previously documented from northern and southern oceans. The present work focuses on the distribution of these morphotypes in modern surface sediment samples from the Canadian Arctic Archipelago (CAA). Our results, obtained for the first time for this area, show the prevalence of morphotypes 1, 2 and 3 (abundance on average 19%, 48% and 22%, respectively). Two types of assemblages were observed in the inner and outer parts of the Northwest Passages on the basis of the abundance and diversity of morphotypes. Their geographical and vertical positions regarding the water depth in the CAA argue for a strong influence of water mass stratification on morphotype distribution. The detailed morphometric study of test morphology together with SEM imagery provides a way to re-evaluate and complete previous classifications of N. pachyderma morphotypes. This morphological approach is supported by stable isotope analyses that document a link between δ18O and δ13C and morphotype mean sizes. This relationship is interpreted as indicative of water column position, with large morphotypes living in relatively shallower (but also fresher, colder and more productive) waters compared to small morphotypes. The former interpretation is further supported by the increased pore concentration in larger morphotypes, which is tentatively interpreted as a strategy to increase buoyancy and to adapt to lower salinity. Consequently, we propose that a coupled approach of using morphology and stable isotopes may constitute an improved tool for oceanographic reconstructions (particularly water column stratification) when used with N. pachyderma assemblages. Furthermore, the additional morphometric criteria defined in the current work are the basis of a useful and updated identification key for N. pachyderma morphotypes.
dc.language.isoENen_US
dc.sourcecrossref
dc.title.enThe morphotypes of Neogloboquadrina pachyderma : Isotopic signature and distribution patterns in the Canadian Arctic Archipelago and adjacent regions
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.marmicro.2018.05.004en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalMarine Micropaleontologyen_US
bordeaux.page13-24en_US
bordeaux.volume142en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04558164
hal.version1
hal.date.transferred2024-04-24T14:55:06Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Marine%20Micropaleontology&rft.date=2018-06-01&rft.volume=142&rft.spage=13-24&rft.epage=13-24&rft.eissn=0377-8398&rft.issn=0377-8398&rft.au=EL%20BANI%20ALTUNA,%20Naima&PIE%C5%83KOWSKI,%20Anna%20J.&EYNAUD,%20Frederique&THIESSEN,%20Rabecca&rft.genre=article


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