dc.creatorTorres, Américo Iadran
dc.creatorFaleschini, Mauricio
dc.creatorEsteves, Jose Luis
dc.date.accessioned2018-03-07T20:55:47Z
dc.date.accessioned2018-11-06T13:16:36Z
dc.date.available2018-03-07T20:55:47Z
dc.date.available2018-11-06T13:16:36Z
dc.date.created2018-03-07T20:55:47Z
dc.date.issued2016-05
dc.identifierTorres, Américo Iadran; Faleschini, Mauricio; Esteves, Jose Luis; Benthic fluxes and nitrate reduction activity in a marine park (Northern San Jorge Gulf) from Patagonia Argentina; Springer Verlag; Environmental Earth Sciences; 75; 9; 5-2016; 1-9
dc.identifier1866-6280
dc.identifierhttp://hdl.handle.net/11336/38210
dc.identifier1866-6299
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1873717
dc.description.abstractThe Northern San Jorge Gulf (NSJG) was declared Coastal Marine Park in 2008 with the goal of preserving its biodiversity. In situ benthic fluxes experiments were performed using an opaque chamber in Sara Creek (SC) and Malaspina Creek (MC). Moreover, ex situ nitrate reduction activity was assessed using a continuous flow-through system. Benthic fluxes in MC, showed a consumption of oxygen (794 ± 196 mg m−2 h−1) and nitrate (103 ± 68 µmol m−2 h−1) by sediment and release of ammonium (175 ± 60 µmol m−2 h−1), phosphate (66 ± 10 µmol m−2 h−1) and silicate (116 ± 66 µmol m−2 h−1) towards the water column. In SC, the same pattern was observed and the fluxes values were 375 ± 132, 128 ± 1, 76 ± 12, 39 ± 24 and 133 ± 81, respectively. Only, ammonium and oxygen fluxes showed significant differences between sites, due to the highest organic matter content and the particular hydrodynamic conditions in MC. These are the first benthic flux measurements made within the protected area. Nitrate uptake rate, based on Michaelis–Menten kinetic, was Km: 155.3 µM and Vmax: 0.053 µM g−1 h−1 in SC and Km: 131.2 µM and Vmax: 0.039 µM g−1 h−1 in MC. Considering the nitrate dynamic we concluded that the sediments both SC and MC act as a sink of nitrate. This ion could be principally used as a terminal electron acceptor during the oxidation process of organic compounds in sediments of NSJG.
dc.languageeng
dc.publisherSpringer Verlag
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1007/s12665-016-5628-z
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007%2Fs12665-016-5628-z
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectARGENTINEAN PATAGONIA
dc.subjectBENTHIC FLUX CHAMBER
dc.subjectCONTINUOUS FLOW-THROUGH SYSTEM
dc.subjectMARINE PARK
dc.subjectNITRATE-REDUCTION
dc.subjectSEDIMENT–WATER INTERFACE
dc.titleBenthic fluxes and nitrate reduction activity in a marine park (Northern San Jorge Gulf) from Patagonia Argentina
dc.typeArtículos de revistas
dc.typeArtículos de revistas
dc.typeArtículos de revistas


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