Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/60010
Campo DC Valoridioma
dc.contributor.authorAzzaro, Maurizioen_US
dc.contributor.authorPackard, Theodore T.en_US
dc.contributor.authorMonticelli, Luis Salvadoren_US
dc.contributor.authorMaimone, Giovannaen_US
dc.contributor.authorRappazzo, Alessandro Ciroen_US
dc.contributor.authorAzzaro, Filippoen_US
dc.contributor.authorGrilli, Federicaen_US
dc.contributor.authorCrisafi, Ermannoen_US
dc.contributor.authorLa Ferla, Rosabrunaen_US
dc.date.accessioned2019-12-30T11:35:05Z-
dc.date.available2019-12-30T11:35:05Z-
dc.date.issued2019en_US
dc.identifier.issn1314-6947en_US
dc.identifier.otherWoS-
dc.identifier.urihttp://hdl.handle.net/10553/60010-
dc.description.abstractThe Ross Sea is one of the most productive areas of the Southern Ocean and includes several functionally different marine ecosystems. With the aim of identifying signs and patterns of microbial response to current climate change, seawater microbial populations were sampled at different depths, from surface to the bottom, at two Ross Sea mooring areas southeast of Victoria Land in Antarctica. This oceanographic experiment, the XX Italian Antarctic Expedition, 2004-05, was carried out in the framework of the ABIOCLEAR project as part of LTER-Italy. Here, microbial biogeochemical rates of respiration, carbon dioxide production, total community heterotrophic energy production, prokaryotic heterotrophic activity, production (by H-3-Ieucine uptake) and prokaryotic biomass (by image analysis) were determined throughout the water column. As ancillary parameters, chlorophyll a, adenosine-triphosphate concentrations, temperature and salinity were measured and reported. Microbial metabolism was highly variable amongst stations and depths. In epi- and mesopelagic zones, respiratory rates varied between 52.4-437.0 and 6.3-271.5 nanol O-2 l(-1)h(-1); prokaryotic heterotrophic production varied between 0.46-29.5 and 0.3-6.11 nanog C l(-1) h(-1) and prokaryotic biomass varied between 0.8-24.5 and 1.1-9.0 mu g C l(-1), respectively. The average heterotrophic energy production ranged between 570 and 103 mJ l(-1)h(-1)in upper and deeper layers, respectively. In the epipelagic layer, the Prokaryotic Carbon Demand and Prokaryotic Growth Efficiency averaged 9 times higher and 2 times lower, respectively, than in the mesopelagic one. The distribution of plankton metabolism and organic matter degradation was mainly related to the different hydrological and trophic conditions. In comparison with previous research, the Ross Sea results, here, evidenced a relatively impoverished oligotrophic microbial community, throughout the water column.en_US
dc.languageengen_US
dc.relation.ispartofNature Conservationen_US
dc.sourceNature Conservation-Bulgaria [ISSN 1314-6947], n. 34, p. 441-475en_US
dc.subject251001 Oceanografía biológicaen_US
dc.subject.otherBacterial-Growth Efficiencyen_US
dc.subject.otherElectron-Transport Activityen_US
dc.subject.otherLeucine Incorporationen_US
dc.subject.otherBiomass Productionen_US
dc.subject.otherMediterranean Seaen_US
dc.subject.otherProtein-Synthesisen_US
dc.subject.otherOrganic-Matteren_US
dc.subject.otherWater-Columnen_US
dc.subject.otherCarbon Fluxen_US
dc.subject.otherDeep-Wateren_US
dc.subject.otherMicrobial respirationen_US
dc.subject.otherHeterotrophic productionen_US
dc.subject.otherHeterotrophic energy productionen_US
dc.subject.otherRoss Seaen_US
dc.subject.otherAntarcticaen_US
dc.subject.otherLTERen_US
dc.titleMicrobial metabolic rates in the Ross Sea: the ABIOCLEAR Projecten_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.3897/natureconservation.34.30631en_US
dc.identifier.scopus85065591416-
dc.identifier.isi000466756300019-
dc.contributor.authorscopusid6602752439-
dc.contributor.authorscopusid7004249480-
dc.contributor.authorscopusid8580879000-
dc.contributor.authorscopusid7801432695-
dc.contributor.authorscopusid57193571185-
dc.contributor.authorscopusid8516485200-
dc.contributor.authorscopusid9744835500-
dc.contributor.authorscopusid6701399786-
dc.contributor.authorscopusid6603903241-
dc.identifier.eissn1314-3301-
dc.description.lastpage475en_US
dc.identifier.issue34-
dc.description.firstpage441en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.contributor.daisngid242445-
dc.contributor.daisngid311411-
dc.contributor.daisngid1687522-
dc.contributor.daisngid1731347-
dc.contributor.daisngid8339441-
dc.contributor.daisngid1405492-
dc.contributor.daisngid2091705-
dc.contributor.daisngid28240357-
dc.contributor.daisngid1991283-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Azzaro, M-
dc.contributor.wosstandardWOS:Packard, TT-
dc.contributor.wosstandardWOS:Monticelli, LS-
dc.contributor.wosstandardWOS:Maimone, G-
dc.contributor.wosstandardWOS:Rappazzo, AC-
dc.contributor.wosstandardWOS:Azzaro, F-
dc.contributor.wosstandardWOS:Grilli, F-
dc.contributor.wosstandardWOS:Crisafi, E-
dc.contributor.wosstandardWOS:La Ferla, R-
dc.date.coverdateMayo 2019en_US
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-BASen_US
dc.description.sjr0,532
dc.description.jcr1,58
dc.description.sjrqQ2
dc.description.jcrqQ3
dc.description.scieSCIE
item.fulltextCon texto completo-
item.grantfulltextopen-
crisitem.author.deptGIR ECOAQUA: Ecofisiología de Organismos Marinos-
crisitem.author.deptIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.orcid0000-0002-5880-1199-
crisitem.author.parentorgIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.fullNamePackard, Theodore Train-
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