Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/113422
Campo DC Valoridioma
dc.contributor.authorValiente, S.en_US
dc.contributor.authorFernández-Castro, B.en_US
dc.contributor.authorCampanero, R.en_US
dc.contributor.authorMarrero Díaz, María De Los Ángelesen_US
dc.contributor.authorRodríguez Santana, Ángelen_US
dc.contributor.authorGelado Caballero, María Doloresen_US
dc.contributor.authorNieto-Cid, M.en_US
dc.contributor.authorDelgado-Huertas, A.en_US
dc.contributor.authorArístegui Ruiz, Javieren_US
dc.contributor.authorÁlvarez-Salgado, X. A.en_US
dc.date.accessioned2022-01-20T09:28:08Z-
dc.date.available2022-01-20T09:28:08Z-
dc.date.issued2022en_US
dc.identifier.issn0079-6611en_US
dc.identifier.otherScopus-
dc.identifier.urihttp://hdl.handle.net/10553/113422-
dc.description.abstractThe Cape Verde Frontal Zone (CVFZ) is a highly dynamic region located in the southern boundary of the Canary Current Eastern Boundary Upwelling Ecosystem. Due to the interaction of the Cape Verde Front with the Mauritanian coastal upwelling, the area features large vertical and horizontal export fluxes of organic matter. While the flux, composition and biogeochemical role of sinking organic matter have been thoroughly studied, much less attention has been paid to the dissolved (DOM) and suspended particulate (POM) organic matter fractions. Full-depth profiles of DOM and POM were recorded during an oceanographic cruise in the CVFZ, with four consecutive transects defining a box embracing the giant filament of Cape Blanc and the Cape Verde front. The distributions of DOM and POM and their C:N stoichiometric ratios in the epipelagic layer were strongly influenced by the position of the transects relative to the giant filament and the front. Geographical heterogeneity in POM and DOM distributions and elemental composition was also observed within each of the different water masses of contrasting origin present in the area (North and South Atlantic Central Water, Subpolar Mode Water, Mediterranean Water, Antarctic Intermediate Water, Labrador Sea Water and North East Atlantic Deep Water). These facts suggest that water masses properties are re-shaped by biogeochemical processes occurring within the CVFZ. Nevertheless, our analysis indicates that DOM and POM mineralisation represents only 8.1% of the inorganic carbon and 17.8% of the inorganic nitrogen produced by the local mineralisation of organic matter. Intense lateral export of POM and DOM out of the boundaries of the CVFZ is the likely reason behind these low contributions, which confirm the prominent role of sinking fluxes of organic matter for mineralisation processes in this region. The DOM distribution in the CVFZ interior is apparently affected by the dissolution of fast sinking particles.en_US
dc.languageengen_US
dc.relationFlujos de Carbono en Un Sistema de Afloramiento Costero (Cabo Blanco, Nw de África); Modulación A Submesoscala de la Producción, Exportación y Consumo de Carbonoen_US
dc.relationBiogeochemical impact of mesoscale and sub-mesoscale processes along the life history of cyclonic and anticyclonic eddies PID2019-109084RB-C2en_US
dc.relationBES-2016-079216en_US
dc.relationBES-2016-076462en_US
dc.relationMarie Skłodowska-Curie grant agreement No. 834330 (SO-CUP)en_US
dc.relationFERMIO (MINECO, CTM2014–57334–JIN)en_US
dc.relationSUMMER (AMD-817806-5)en_US
dc.relation.ispartofProgress in Oceanographyen_US
dc.sourceProgress in Oceanography [ISSN 0079-6611], v. 201, (Febrero 2022)en_US
dc.subject2510 Oceanografíaen_US
dc.subject251001 Oceanografía biológicaen_US
dc.subject251002 Oceanografía químicaen_US
dc.subject.otherCape Verde Frontal Zoneen_US
dc.subject.otherCarbon Cyclingen_US
dc.subject.otherDissolved Organic Matteren_US
dc.subject.otherNitrogen Cyclingen_US
dc.subject.otherParticulate Organic Matteren_US
dc.subject.otherWater Massesen_US
dc.titleDissolved and suspended organic matter dynamics in the Cape Verde Frontal Zone (NW Africa)en_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.pocean.2021.102727en_US
dc.identifier.scopus85121295884-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.authorscopusid57374577800-
dc.contributor.authorscopusid55328276500-
dc.contributor.authorscopusid57374577900-
dc.contributor.authorscopusid6507074043-
dc.contributor.authorscopusid6506514177-
dc.contributor.authorscopusid57374686700-
dc.contributor.authorscopusid8934243800-
dc.contributor.authorscopusid14015420100-
dc.contributor.authorscopusid7006816204-
dc.contributor.authorscopusid7004656202-
dc.relation.volume201en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.description.notasThis work was supported by Spanish National Science Plan research grants FLUXES (CTM2015-69392-C3) and e-IMPACT (PID2019-109084RB-C2). S.V.R and R.C.N were supported by PhD fellowships from the Spanish Ministry of Science and Innovation (BES-2016-079216 and BES-2016-076462); B.F.C was supported by a Juan de La Cierva Formación fellowship (FJCI-641-2015-25712) and by the European Union’s Horizon 2020 research and innovation program under the Marie Skłodowska-Curie grant agreement No. 834330 (SO-CUP). M.N.–C. was partially supported by the project FERMIO (MINECO, CTM2014–57334–JIN), co–financed with FEDER funds. J.A. was partly supported by the project SUMMER (AMD-817806-5) from the European Union’s Horizon 2020 research and innovation programen_US
dc.utils.revisionen_US
dc.date.coverdateFebrero 2022en_US
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-BASen_US
dc.description.sjr1,198
dc.description.jcr4,1
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
dc.description.miaricds11,0
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.deptGIR ECOAQUA: Oceanografía Física y Geofísica Aplicada-
crisitem.author.deptIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR ECOAQUA: Oceanografía Física y Geofísica Aplicada-
crisitem.author.deptIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR Tecnologías, Gestión y Biogeoquímica Ambiental-
crisitem.author.deptDepartamento de Química-
crisitem.author.deptGIR IOCAG: Oceanografía Biológica y Algología Aplicada-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Biología-
crisitem.author.orcid0000-0001-7697-0036-
crisitem.author.orcid0000-0003-1960-6777-
crisitem.author.orcid0000-0003-4001-9673-
crisitem.author.orcid0000-0002-7526-7741-
crisitem.author.parentorgIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.parentorgIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.parentorgDepartamento de Química-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameMarrero Díaz, María De Los Ángeles-
crisitem.author.fullNameRodríguez Santana, Ángel-
crisitem.author.fullNameGelado Caballero, María Dolores-
crisitem.author.fullNameArístegui Ruiz, Javier-
crisitem.project.principalinvestigatorRodríguez Santana, Ángel-
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