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dc.rights.licenseopenen_US
dc.contributor.authorDE VERNAL, Anne
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorEYNAUD, Frederique
IDREF: 144113570
dc.contributor.authorHENRY, Maryse
dc.contributor.authorLIMOGES, Audrey
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorLONDEIX, Laurent
dc.contributor.authorMATTHIESSEN, Jens
dc.contributor.authorMARRET, Fabienne
dc.contributor.authorPOSPELOVA, Vera
dc.contributor.authorRADI, Taoufik
dc.contributor.authorROCHON, André
dc.contributor.authorVAN NIEUWENHOVE, Nicolas
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZARAGOSI, Sebastien
IDREF: 189039159
dc.date.accessioned2024-04-24T12:56:17Z
dc.date.available2024-04-24T12:56:17Z
dc.date.issued2018-12-14
dc.identifier.issn0191-6122en_US
dc.identifier.urioai:crossref.org:10.1080/01916122.2018.1465730
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199318
dc.description.abstractEnIn marine sediments of late Cenozoic age, Spiniferites is a very common genus of dinoflagellate cysts (dinocysts). Despite some taxonomical ambiguities due to large range of morphological variations within given species and convergent morphologies between different species, the establishment of an operational taxonomy permitted to develop a standardized modern database of dinocysts for the mid-high latitudes of the Northern Hemisphere. In the database that includes 1490 surface sediment samples, Spiniferites mirabilis-hyperacanthus, Spiniferites ramosus and Spiniferites elongatus were counted in addition to Spiniferites belerius, Spiniferites bentorii, Spiniferites bulloideus, Spiniferites delicatus, Spiniferites lazus and Spiniferites membranaceus. Among these taxa, Spiniferites mirabilis-hyperacanthus, Spiniferites ramosus, and Spiniferites elongatus are easy to identify and are particularly common. Spiniferites bentorii and Spiniferites delicatus also are morphologically distinct and occur in relatively high percentages in many samples. Spiniferites lazus and Spiniferites membranaceus also bear distinctive features, but occur only in a few samples. The identification of other taxa (Spiniferites belerius, Spiniferites bulloideus, notably) may be equivocal and their reported distribution has to be used with caution. The spatial distribution of Spiniferites species, with emphasis on the five most common taxa, is documented here with reference to hydrography (salinity and temperature in winter and summer, sea ice cover), primary productivity and geographical setting (bathymetry, distance to the coastline). The results demonstrate distinct ecological affinities for Spiniferites elongatus, which has an Arctic-subarctic distribution and appears abundant in low productivity environments characterized by winter sea ice and large temperature contrast between winter and summer. Spiniferites mirabilis-hyperacanthus, which occurs in warm temperate water sites, is more abundant in high salinity environments. It shares its environmental domain with Spiniferites bentorii, which appears to have a narrower distribution towards the warm and high salinity end of the Spiniferites mirabilis-hyperacanthus distribution. In contrast, Spiniferites delicatus, which occurs in warm-temperate to tropical environments, shows preference for relatively low salinity and low seasonal contrasts of temperature. Spiniferites ramosus exhibits a particularly wide distribution that overlaps both cold and warm Spiniferites taxa. Its cosmopolitan occurrence and its long-ranging biostratigraphical distribution suggest a high plasticity of the species and/or co-occurrence of several cryptic species. Hence, whereas Spiniferites elongatus and Spiniferites mirabilis-hyperacanthus are useful palaeoecological indicators despite their large morphological variability, Spiniferites ramosus is a taxon with an unconstrained ecological significance.
dc.language.isoENen_US
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.sourcecrossref
dc.subject.enDinocysts
dc.subject.enQuaternary
dc.subject.enPalaeoceanography
dc.subject.enTemperature
dc.subject.enSalinity
dc.subject.enSea-ice
dc.subject.enProductivity
dc.title.enDistribution and (palaeo)ecological affinities of the mainSpiniferitestaxa in the mid-high latitudes of the Northern Hemisphere
dc.typeArticle de revueen_US
dc.identifier.doi10.1080/01916122.2018.1465730en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalPalynologyen_US
bordeaux.page182-202en_US
bordeaux.volume42en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issuesup1en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04557857
hal.version1
hal.date.transferred2024-04-24T12:56:21Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccCC BY-NC-NDen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Palynology&rft.date=2018-12-14&rft.volume=42&rft.issue=sup1&rft.spage=182-202&rft.epage=182-202&rft.eissn=0191-6122&rft.issn=0191-6122&rft.au=DE%20VERNAL,%20Anne&EYNAUD,%20Frederique&HENRY,%20Maryse&LIMOGES,%20Audrey&LONDEIX,%20Laurent&rft.genre=article


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