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dc.creatorNaqvi,S.W.A
dc.date2006-10-01
dc.date.accessioned2019-04-24T21:24:02Z
dc.date.available2019-04-24T21:24:02Z
dc.identifierhttps://scielo.conicyt.cl/scielo.php?script=sci_arttext&pid=S0717-65382006000300011
dc.identifier.urihttp://revistaschilenas.uchile.cl/handle/2250/56916
dc.descriptionThe Indian Ocean contains one of the oceans' most pronounced oxygen minimum zones (OMZ), which, anomalously, is the most intense in the northwestern sector (Arabian Sea). It also contains the majority of the area of oceanic continental margins in contact with oxygen-depleted waters. Impacts of the oxygen deficiency on regional biogeochemistry, especially anaerobic nitrogen transformations, are described. A comparison of the perennial, mesopelagic OMZ in the open Northwestern Indian Ocean is made with a shallower oxygen deficient system that develops seasonally (during late summer and autumn) over the western Indian shelf. The latter appears to have intensified in recent years presumably due to anthropogenic nutrient loading from land.
dc.formattext/html
dc.languageen
dc.publisherFacultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción
dc.relation10.4067/S0717-65382006000300011
dc.rightsinfo:eu-repo/semantics/openAccess
dc.sourceGayana (Concepción) v.70 suppl.1 2006
dc.subjectIndian Ocean
dc.subjectnitrogen cycling
dc.subjectdenitrification
dc.subjectN2O
dc.subjecteutrophication
dc.titleOxygen deficiency in the north indian ocean


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