Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/58372
Campo DC Valoridioma
dc.contributor.authorOrtega-Retuerta, Evaen_US
dc.contributor.authorMazuecos, Ignacio P.en_US
dc.contributor.authorReche, Isabelen_US
dc.contributor.authorGasol, Josep M.en_US
dc.contributor.authorAlvarez-Salgado, Xose A.en_US
dc.contributor.authorAlvarez, Martaen_US
dc.contributor.authorMontero del Pino, María Fernandaen_US
dc.contributor.authorAristegui, Javieren_US
dc.date.accessioned2019-12-12T14:52:37Z-
dc.date.available2019-12-12T14:52:37Z-
dc.date.issued2019en_US
dc.identifier.issn0079-6611en_US
dc.identifier.otherWoS-
dc.identifier.urihttp://hdl.handle.net/10553/58372-
dc.description.abstractTransparent exopolymer particles (TEP) play a key role in ocean carbon export and structuring microbial habitats, but information on their distribution across different ocean basins and depths is scarce, particularly in the dark ocean. We measured TEP vertical distribution from the surface to bathypelagic waters in an east-to-west transect across the Mediterranean Sea (MedSea) and the adjacent North East Atlantic Ocean (NEA), and explored their physical and biological drivers. TEP ranged from 0.6 to 81.7 mu g XG eq L-1, with the highest values in epipelagic waters above the deep chlorophyll maximum, and in areas near the Gibraltar and Sicily Straits. TEP were significantly related to particulate organic carbon (POC) in all basins and depth layers (epipelagic vs. deep), but the contribution of TEP to POC was higher in the NEA (85%, 79% and 67% in epi-, meso- and bathypelagic waters, respectively) than in the MedSea (from 53% to 62% in epipelagic waters, and from 45% to 48% in mesoand bathypelagic waters), coinciding with higher carbon to nitrogen particulate organic matter ratios in the NEA. The TEP connectivity between epipelagic waters and mesopelagic waters was less straightforward than between mesopelagic waters and bathypelagic waters, with a 23% and 55% of the variance in the relationship between layers explained respectively. Prokaryotes were found to be a likely net source of TEP as inferred by the significant direct relationship observed between prokaryotic heterotrophic abundance and TEP. This assumption was confirmed using experimental incubations, where prokaryotes produced TEP in concentrations ranging from 0.7 (Western Mediterranean, bathypelagic) to 232 (Western Mediterranean, mesopelagic) mu g XG eq. L-1 day(-1).en_US
dc.languageengen_US
dc.relationZonas de Mezcla y Frentes en El Océano Oscuro Como ¿Hot-Spots? de Biodiversidad y Flujos Biogeoquímicos A Través Del Mar Mediterráneo y Atlántico Nordeste - I.en_US
dc.relationFlujos de Carbono en Un Sistema de Afloramiento Costero (Cabo Blanco, Nw de Africa). Papel Del Carbono Disuelto y en Suspension en El Contexto de la Bomba Biologica.en_US
dc.relation.ispartofProgress in Oceanographyen_US
dc.sourceProgress In Oceanography [ISSN 0079-6611], v. 173, p. 180-191en_US
dc.subject251001 Oceanografía biológicaen_US
dc.subject.otherDissolved Organic-Matteren_US
dc.subject.otherPhosphorus Limitationen_US
dc.subject.otherSeasonal Dynamicsen_US
dc.subject.otherFlow-Cytometryen_US
dc.subject.otherDiatom Bloomen_US
dc.subject.otherWater Massesen_US
dc.subject.otherPhytoplanktonen_US
dc.subject.otherBacterialen_US
dc.subject.otherAggregationen_US
dc.subject.otherAbundanceen_US
dc.titleTransparent exopolymer particle (TEP) distribution and in situ prokaryotic generation across the deep Mediterranean Sea and nearby North East Atlantic Oceanen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.pocean.2019.03.002
dc.identifier.scopus85062691501
dc.identifier.isi000471739000013-
dc.contributor.authorscopusid14063577900
dc.contributor.authorscopusid36542617400
dc.contributor.authorscopusid6603791726
dc.contributor.authorscopusid7003299234
dc.contributor.authorscopusid7004656202
dc.contributor.authorscopusid35072563600
dc.contributor.authorscopusid7102553402
dc.contributor.authorscopusid7006816204
dc.description.lastpage191-
dc.description.firstpage180-
dc.relation.volume173-
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.contributor.daisngid1462677
dc.contributor.daisngid5965710
dc.contributor.daisngid676677
dc.contributor.daisngid97985
dc.contributor.daisngid237391
dc.contributor.daisngid981000
dc.contributor.daisngid1878283
dc.contributor.daisngid227201
dc.contributor.wosstandardWOS:Ortega-Retuerta, E
dc.contributor.wosstandardWOS:Mazuecos, IP
dc.contributor.wosstandardWOS:Reche, I
dc.contributor.wosstandardWOS:Gasol, JM
dc.contributor.wosstandardWOS:Alvarez-Salgado, XA
dc.contributor.wosstandardWOS:Alvarez, M
dc.contributor.wosstandardWOS:Montero, MF
dc.contributor.wosstandardWOS:Aristegui, J
dc.date.coverdateAbril 2019
dc.identifier.ulpgces
dc.description.sjr1,803
dc.description.jcr4,06
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.project.principalinvestigatorArístegui Ruiz, Javier-
crisitem.project.principalinvestigatorArístegui Ruiz, Javier-
crisitem.author.deptGIR IOCAG: Oceanografía Biológica y Algología Aplicada-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Biología-
crisitem.author.deptGIR IOCAG: Oceanografía Biológica y Algología Aplicada-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Biología-
crisitem.author.orcid0000-0001-8124-8136-
crisitem.author.orcid0000-0002-7526-7741-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameMontero Del Pino, María Fernanda-
crisitem.author.fullNameArístegui Ruiz, Javier-
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