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dc.contributor.authorFarrell, Hazeles_ES
dc.contributor.authorVelo-Suárez, Lourdeses_ES
dc.contributor.authorReguera Ramírez, Beatrizes_ES
dc.contributor.authorRaine, Robines_ES
dc.coverage.spatialAtlantic Oceanes_ES
dc.coverage.spatialEastern Atlantices_ES
dc.coverage.spatialNortheast Atlantices_ES
dc.coverage.spatialIrish Seaes_ES
dc.date.accessioned2023-06-21T09:06:47Z-
dc.date.available2023-06-21T09:06:47Z-
dc.date.issued2014-
dc.identifier.citationDeep Sea Research - Part II - Topical Studies in Oceanography 101 : 249-254 (2014)es_ES
dc.identifier.issn0967-0645-
dc.identifier.urihttp://hdl.handle.net/10261/324160-
dc.description.abstractThe proportions of viable cells ofDinophysisspp. that were paired (dividing) and recently divided during a cell cycle were measured on populations ofD. acutaandD. acuminataobserved off the south coast of Ireland in July 2007 and July 2009. Both species exhibited phased cell division in 2009 with maximum frequency of division (fmax) 2 h after sunrise. Different patterns of division (timing offmax) were shown by D. acutain 2007, when the population aggregated in a thin layer was transported by a coastal jet flow. High resolution (decimetre-scale) profiles within the thin layer showed large differences in the vertical distribution of biological properties (feeding status, mortality). Values of the specific growth ratemwere compared to estimates derived in similar fashion from observations onDinophysispopulations elsewhere. Different patterns exhibited by the same species in different regions may be attributed to adaptations to latitudinal differences (length of photoperiod). The question of whether phased cell division always occurs inDinophysispopulations, and the incorporation of the potential specific division rate into models of Dinophysisgrowth are discussed. Comprehensivefield data sets demonstrate the impact of the results on the coherence of Dinophysispopulations during their transport along the Irish coast in jet-likeflows towards sites of intensive shellfish culturees_ES
dc.description.sponsorshipThe authors would like to thank M. Lunven and M. Sourisseau for use and operation of the Fine Scale Sampler. This work was supported by projects HABIT (EC 6FP, GOCE-CT-2005–003932), ASIMUTH (EC 7FP, SPACE, Grant Agreement # 261860), and shiptime funding from the Marine Institute (Refs. RV/ST/07/02 and RV/ST/09/18) through the Sea Change programme. LV-S was supported by a Marie Curie Fellowship (IOF; MOHAB agreement: PIOF-GA-252260). This is a contribution to the SCOR-IOC GEOHAB Programme, Core Research Project HABs in Stratified Systems.es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.relationinfo:eu-repo/grantAgreement/EC/FP7/261860es_ES
dc.relation.ispartof10000-02-28es_ES
dc.rightsclosedAccesses_ES
dc.subjectMedio Marinoes_ES
dc.subjectDinophysises_ES
dc.subjectCentro Oceanográfico de Vigoes_ES
dc.subjectDinophysis acuminatees_ES
dc.subjectDinophysis acutaes_ES
dc.subjectSpecific growth ratees_ES
dc.subjectThin layerses_ES
dc.titlePhased cell division, specific division rates and other biological observations of Dinophysis populations off the south coast of Irelandes_ES
dc.typeartículoes_ES
dc.identifier.doi10.1016/j.dsr2.2013.05.031-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://doi.org/10.1016/j.dsr2.2013.05.031es_ES
dc.identifier.e-issn1879-0100-
dc.relation.csices_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
dc.page.initial249es_ES
dc.page.final254es_ES
dc.volume.number101es_ES
dc.identifier.sipi5946es_ES
item.openairetypeartículo-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextnone-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextNo Fulltext-
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