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dc.contributor.authorMoreira-Coello, Víctoren_US
dc.contributor.authorMouriño-Carballido, Beatrizen_US
dc.contributor.authorMarañón, Emilioen_US
dc.contributor.authorFernández Carrera, Anaen_US
dc.contributor.authorBode, Antonioen_US
dc.contributor.authorSintes, Evaen_US
dc.contributor.authorZehr, Jonathan P.en_US
dc.contributor.authorTurk-Kubo, Kendraen_US
dc.contributor.authorVarela, Marta M.en_US
dc.date.accessioned2026-01-08T13:51:18Z-
dc.date.available2026-01-08T13:51:18Z-
dc.date.issued2019en_US
dc.identifier.issn2045-2322en_US
dc.identifier.urihttps://accedacris.ulpgc.es/jspui/handle/10553/154475-
dc.description.abstractKnowledge of the ecology of N2-fixing (diazotrophic) plankton is mainly limited to oligotrophic (sub)tropical oceans. However, diazotrophs are widely distributed and active throughout the global ocean. Likewise, relatively little is known about the temporal dynamics of diazotrophs in productive areas. Between February 2014 and December 2015, we carried out 9 one-day samplings in the temperate northwestern Iberian upwelling system to investigate the temporal and vertical variability of the diazotrophic community and its relationship with hydrodynamic forcing. In downwelling conditions, characterized by deeper mixed layers and a homogeneous water column, non-cyanobacterial diazotrophs belonging mainly to nifH clusters 1G (Gammaproteobacteria) and 3 (putative anaerobes) dominated the diazotrophic community. In upwelling and relaxation conditions, affected by enhanced vertical stratification and hydrographic variability, the community was more heterogeneous vertically but less diverse, with prevalence of UCYN-A (unicellular cyanobacteria, subcluster 1B) and non-cyanobacterial diazotrophs from clusters 1G and 3. Oligotyping analysis of UCYN-A phylotype showed that UCYN-A2 sublineage was the most abundant (74%), followed by UCYN-A1 (23%) and UCYN-A4 (2%). UCYN-A1 oligotypes exhibited relatively low frequencies during the three hydrographic conditions, whereas UCYN-A2 showed higher abundances during upwelling and relaxation. Our findings show the presence of a diverse and temporally variable diazotrophic community driven by hydrodynamic forcing in an upwelling system.en_US
dc.languageengen_US
dc.relation.ispartofScientific Reportsen_US
dc.sourceScientific Reports [ISSN 2045-2322], v. 9en_US
dc.subject251001 Oceanografía biológicaen_US
dc.titleTemporal variability of diazotroph community composition in the upwelling region off NW Iberiaen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.identifier.doi10.1038/s41598-019-39586-4en_US
dc.identifier.issue1-
dc.relation.volume9en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.description.numberofpages13en_US
dc.utils.revisionen_US
dc.date.coverdateMarzo 2019en_US
dc.identifier.ulpgcNoen_US
dc.contributor.buulpgcBU-BASen_US
dc.description.sjr1,341
dc.description.jcr3,998
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.fulltextCon texto completo-
item.grantfulltextopen-
crisitem.author.deptGIR IOCAG: Oceanografía Biológica y Algología Aplicada-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.orcid0000-0001-8347-0996-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameFernández Carrera, Ana-
Colección:Artículos
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