Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific
The 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...
| Autores: | , , , |
|---|---|
| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2009 |
| País: | España |
| Institución: | Universidad de Barcelona |
| Repositorio: | Dipòsit Digital de la UB |
| OAI Identifier: | oai:diposit.ub.edu:2445/98311 |
| Acceso en línea: | https://hdl.handle.net/2445/98311 |
| Access Level: | acceso abierto |
| Palabra clave: | Oceanografia química Geoquímica Climatologia Oceanografia Pacífic, Oceà Chemical oceanography Geochemistry Climatology Oceanography Pacific Ocean |
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Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial PacificRobinson, Rebecca S.Martinez, P.Pena González, Leopoldo DavidCacho Lascorz, IsabelOceanografia químicaGeoquímicaClimatologiaOceanografiaPacífic, OceàChemical oceanographyGeochemistryClimatologyOceanographyPacific OceanThe 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.American Geophysical Union2009info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://hdl.handle.net/2445/98311Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)reponame:Dipòsit Digital de la UBinstname:Universidad de BarcelonaInglésReproducció del document publicat a: http://dx.doi.org/10.1029/2008PA001702Paleoceanography, 2009, vol. 24, num. 4, p. 1-12http://dx.doi.org/10.1029/2008PA001702(c) American Geophysical Union, 2009info:eu-repo/semantics/openAccessoai:diposit.ub.edu:2445/983112026-05-27T06:46:51Z |
| dc.title.none.fl_str_mv |
Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific |
| title |
Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific |
| spellingShingle |
Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific Robinson, Rebecca S. Oceanografia química Geoquímica Climatologia Oceanografia Pacífic, Oceà Chemical oceanography Geochemistry Climatology Oceanography Pacific Ocean |
| title_short |
Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific |
| title_full |
Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific |
| title_fullStr |
Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific |
| title_full_unstemmed |
Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific |
| title_sort |
Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific |
| dc.creator.none.fl_str_mv |
Robinson, Rebecca S. Martinez, P. Pena González, Leopoldo David Cacho Lascorz, Isabel |
| author |
Robinson, Rebecca S. |
| author_facet |
Robinson, Rebecca S. Martinez, P. Pena González, Leopoldo David Cacho Lascorz, Isabel |
| author_role |
author |
| author2 |
Martinez, P. Pena González, Leopoldo David Cacho Lascorz, Isabel |
| author2_role |
author author author |
| dc.subject.none.fl_str_mv |
Oceanografia química Geoquímica Climatologia Oceanografia Pacífic, Oceà Chemical oceanography Geochemistry Climatology Oceanography Pacific Ocean |
| topic |
Oceanografia química Geoquímica Climatologia Oceanografia Pacífic, Oceà Chemical oceanography Geochemistry Climatology Oceanography Pacific Ocean |
| description |
The 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. |
| publishDate |
2009 |
| dc.date.none.fl_str_mv |
2009 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.none.fl_str_mv |
https://hdl.handle.net/2445/98311 |
| url |
https://hdl.handle.net/2445/98311 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
Reproducció del document publicat a: http://dx.doi.org/10.1029/2008PA001702 Paleoceanography, 2009, vol. 24, num. 4, p. 1-12 http://dx.doi.org/10.1029/2008PA001702 |
| dc.rights.none.fl_str_mv |
(c) American Geophysical Union, 2009 info:eu-repo/semantics/openAccess |
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(c) American Geophysical Union, 2009 |
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openAccess |
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application/pdf |
| dc.publisher.none.fl_str_mv |
American Geophysical Union |
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American Geophysical Union |
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Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) reponame:Dipòsit Digital de la UB instname:Universidad de Barcelona |
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Universidad de Barcelona |
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Dipòsit Digital de la UB |
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Dipòsit Digital de la UB |
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1869408415714902016 |
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15,300724 |