Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/60009
DC FieldValueLanguage
dc.contributor.authorHerrera, Inmaen_US
dc.contributor.authorYebra, Lidiaen_US
dc.contributor.authorAntezana, Tarsicioen_US
dc.contributor.authorGiraldo, Alanen_US
dc.contributor.authorFärber-Lorda, Jaimeen_US
dc.contributor.authorHernandez-Leon, Santiagoen_US
dc.date.accessioned2019-12-30T11:26:40Z-
dc.date.available2019-12-30T11:26:40Z-
dc.date.issued2019en_US
dc.identifier.issn0142-7873en_US
dc.identifier.otherWoS-
dc.identifier.urihttp://hdl.handle.net/10553/60009-
dc.description.abstractKnowledge of metabolic rates of euphausiid diel vertical migrants in the ocean is of paramount importance to understand the role of these organisms in the downward transport of carbon due to their feeding in the epipelagic zone and subsequent respiration, egestion, excretion and mortality in the mesopelagic zone. Enzymatic activities are used as proxies for the estimation of metabolism in deep waters because of the logistical problems related to measure these rates at depth. However, metabolic activities of euphausiids in the so-called oxygen minimum zones (OMZs) are still not well understood. The OMZs are expanding as the effect of the global warming. Knowledge about the metabolic response of organisms transiting these zones will help to understand the fate of zooplanktonic communities and vertical active flux. The electron transport system (ETS) and aminoacyl-tRNA synthetases (AARS) activities were used as proxies for potential respiration and growth in planktonic organisms. Here, we measured these enzymatic activities in Euphausia distinguenda in the well-oxygenated epipelagic layer and in the OMZ of the northern boundary of the Eastern Tropical Pacific off Mexico. E. distinguenda was found in the mixed layer at night (similar to 3.5 mL O-2 L-1) and near the core of the OMZ (0.2 mL O-2 L-1) during daytime between 200 and 350 m depth. We found higher ETS and AARS specific activities in the warm mixed layer at night and significantly lower in the colder OMZ during daytime because of temperature differences. However, when the effect of temperature was subtracted in both enzyme activities, higher values in the mesopelagic layer were observed. This result is tentatively explained by the increase in substrates as the effect of feeding at night in the upper layers and their oxygen consumption at depth during day in order to compensate for the colder temperature and low dissolved oxygen concentration. This physiological mechanism allows E. distinguenda diel vertical migrants to partly face the physical constraints of vertical migration imposed to avoid predators.en_US
dc.languageengen_US
dc.relationBiomasa y Flujo Activo en la Zona Batipelágicaen_US
dc.relation.ispartofJournal of Plankton Researchen_US
dc.sourceJournal of Plankton Research [ISSN 0142-7873], v. 41 (2), p. 165-176, (Marzo-Abril 2019)en_US
dc.subject251001 Oceanografía biológicaen_US
dc.subject.otherElectron-Transport Systemen_US
dc.subject.otherMeganyctiphanes Norvegicaen_US
dc.subject.otherNematoscelis-Megalopsen_US
dc.subject.otherZooplankton Biomassen_US
dc.subject.otherFeeding-Behavioren_US
dc.subject.otherNorthern Krillen_US
dc.subject.otherTemperatureen_US
dc.subject.otherRespirationen_US
dc.subject.otherGrowthen_US
dc.subject.otherSuppressionen_US
dc.subject.otherAARSen_US
dc.subject.otherEastern tropical Pacificen_US
dc.subject.otherETSen_US
dc.subject.otherEuphausia distinguendaen_US
dc.subject.otherOxygen minimum zoneen_US
dc.titleVertical variability of Euphausia distinguenda metabolic rates during diel migration into the oxygen minimum zone of the Eastern Tropical Pacific off Mexicoen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1093/plankt/fbz004en_US
dc.identifier.scopus85064261098-
dc.identifier.isi000465115600008-
dc.contributor.orcid#NODATA#-
dc.contributor.orcid#NODATA#-
dc.contributor.orcid#NODATA#-
dc.contributor.orcid#NODATA#-
dc.contributor.orcid#NODATA#-
dc.contributor.orcid#NODATA#-
dc.contributor.authorscopusid55096034700-
dc.contributor.authorscopusid55880102100-
dc.contributor.authorscopusid6602730276-
dc.contributor.authorscopusid7005608949-
dc.contributor.authorscopusid6602278222-
dc.contributor.authorscopusid6701465678-
dc.identifier.eissn1464-3774-
dc.description.lastpage176en_US
dc.identifier.issue2-
dc.description.firstpage165en_US
dc.relation.volume41en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.contributor.daisngid9255411-
dc.contributor.daisngid1456786-
dc.contributor.daisngid1906894-
dc.contributor.daisngid983404-
dc.contributor.daisngid3345130-
dc.contributor.daisngid3635323-
dc.identifier.external54561544-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Herrera, I-
dc.contributor.wosstandardWOS:Yebra, L-
dc.contributor.wosstandardWOS:Antezana, T-
dc.contributor.wosstandardWOS:Giraldo, A-
dc.contributor.wosstandardWOS:Farber-Lorda, J-
dc.contributor.wosstandardWOS:Hernandez-Leon, S-
dc.date.coverdateMarzo-Abril 2019en_US
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-BASen_US
dc.description.sjr0,943-
dc.description.jcr2,149-
dc.description.sjrqQ1-
dc.description.jcrqQ2-
dc.description.scieSCIE-
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.deptGIR ECOAQUA: Biodiversidad y Conservación-
crisitem.author.deptIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.deptGIR IOCAG: Oceanografía Biológica y Cambio Global-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Biología-
crisitem.author.orcid0000-0002-5043-2181-
crisitem.author.orcid0000-0002-3085-4969-
crisitem.author.parentorgIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameHerrera Rivero, Inmaculada-
crisitem.author.fullNameHernández León, Santiago Manuel-
crisitem.project.principalinvestigatorHernández León, Santiago Manuel-
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