Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific

dc.contributor.authorRobinson, Rebecca S.
dc.contributor.authorMartinez, P.
dc.contributor.authorPena González, Leopoldo David
dc.contributor.authorCacho Lascorz, Isabel
dc.date.accessioned2016-05-05T09:12:43Z
dc.date.available2016-05-05T09:12:43Z
dc.date.issued2009-12-15
dc.date.updated2016-05-05T09:12:48Z
dc.description.abstractThe Eastern Equatorial Pacific (EEP) is a high nutrientâ "low chlorophyll region of the ocean. Downcore nitrogen isotope records from the EEP have been previously interpreted as a direct reflection of changes in nutrient consumption. However, the observed changes in sedimentary δ15N since the last glacial maximum have no coherent relationship with export productivity or an inferred variation in the iron-to-nitrate ratio of the surface waters. Rather, downcore N isotope records in the EEP strongly resemble changes in the extent of water column denitrification as recorded in nearby sedimentary δ15N records along the western margin of the Americas. This similarity is attributed to the overprinting of the N isotopic composition of nitrate in the EEP through the advection of nitrate westward from the margins in the subsurface. A local nitrogen isotope record of changes in the degree of nutrient consumption is extracted from the bulk sedimentary record by subtracting two different sedimentary δ15N records of denitrification changes from two new EEP δ15N records (TR163-22 and ODP Site 1240). The denitrification records used are from 1) the Central American margin (ODP Site 1242) and 2) the South American margin (GeoB7139-2). The degree of consumption in the surface waters declines rapidly from elevated values during the last glacial maximum to a pair of minima around 15 and 11â "13 ka, and finally it increases into the Holocene. The derived EEP nitrogen isotope record indicates that the regional peak in export productivity occurred when the supply of nutrients exceeded the apparently high demand. The influx of nutrients during the deglaciation is attributed to the resumption of intense overturning in the Southern Ocean and the release of sequestered CO2 and nutrient-rich, O2 poor waters from the deep ocean. This has important implications for understanding the glacial-interglacial scale variation in intermediate water suboxia and water column denitrification.
dc.format.extent12 p.
dc.format.mimetypeapplication/pdf
dc.identifier.idgrec580259
dc.identifier.issn0883-8305
dc.identifier.urihttps://hdl.handle.net/2445/98311
dc.language.isoeng
dc.publisherAmerican Geophysical Union
dc.relation.isformatofReproducció del document publicat a: http://dx.doi.org/10.1029/2008PA001702
dc.relation.ispartofPaleoceanography, 2009, vol. 24, num. 4, p. 1-12
dc.relation.urihttp://dx.doi.org/10.1029/2008PA001702
dc.rights(c) American Geophysical Union, 2009
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess
dc.sourceArticles publicats en revistes (Dinàmica de la Terra i l'Oceà)
dc.subject.classificationOceanografia química
dc.subject.classificationGeoquímica
dc.subject.classificationClimatologia
dc.subject.classificationOceanografia
dc.subject.classificationPacífic, Oceà
dc.subject.otherChemical oceanography
dc.subject.otherGeochemistry
dc.subject.otherClimatology
dc.subject.otherOceanography
dc.subject.otherPacific Ocean
dc.titleNitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion

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