Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 22 (2007): PA1215, doi:10.1029/2005PA001205. In a piston core from the centra...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/3442 2023-05-15T15:43:16+02:00 Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes Brunelle, Brigitte G. Sigman, Daniel M. Cook, Mea S. Keigwin, Lloyd D. Haug, Gerald H. Plessen, Birgit Schettler, Georg Jaccard, Samuel L. 2007-03-02 application/postscript application/pdf text/plain https://hdl.handle.net/1912/3442 en_US eng American Geophysical Union https://doi.org/10.1029/2005PA001205 Paleoceanography 22 (2007): PA1215 https://hdl.handle.net/1912/3442 doi:10.1029/2005PA001205 Paleoceanography 22 (2007): PA1215 doi:10.1029/2005PA001205 Nitrogen isotopes Subarctic North Pacific Polar stratification hypothesis Article 2007 ftwhoas https://doi.org/10.1029/2005PA001205 2022-05-28T22:57:58Z Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 22 (2007): PA1215, doi:10.1029/2005PA001205. In a piston core from the central Bering Sea, diatom microfossil-bound N isotopes and the concentrations of opal, biogenic barium, calcium carbonate, and organic N are measured over the last glacial/interglacial cycle. Compared to the interglacial sections of the core, the sediments of the last ice age are characterized by 3‰ higher diatom-bound δ 15N, 70 wt % lower opal content and 1200 ppm lower biogenic barium. Taken together and with constraints on sediment accumulation rate, these results suggest a reduced supply of nitrate to the surface due to stronger stratification of the upper water column of the Bering Sea during glacial times, with more complete nitrate consumption resulting from continued iron supply through atmospheric deposition. This finding extends the body of evidence for a pervasive link between cold climates and polar ocean stratification. In addition, we hypothesize that more complete nutrient consumption in the glacial age subarctic Pacific contributed to the previously observed ice age reduction in suboxia and denitrification in the eastern tropical North Pacific by lowering the nutrient content of the intermediate-depth water formed in the subpolar North Pacific. In the deglacial interval of the Bering Sea record, two apparent peaks in export productivity are associated with maxima in diatom-bound and bulk sediment δ 15N. The high δ 15N in these intervals may have resulted from greater surface nutrient consumption during this period. However, the synchroneity of the deglacial peaks in the Bering Sea with similar bulk sediment δ 15N changes in the eastern Pacific margin and the presence of sediment lamination within the Bering Sea during the deposition of the productivity peaks raise the possibility that both regional and ... Article in Journal/Newspaper Bering Sea Subarctic Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Bering Sea Pacific Paleoceanography 22 1 n/a n/a |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Nitrogen isotopes Subarctic North Pacific Polar stratification hypothesis |
spellingShingle |
Nitrogen isotopes Subarctic North Pacific Polar stratification hypothesis Brunelle, Brigitte G. Sigman, Daniel M. Cook, Mea S. Keigwin, Lloyd D. Haug, Gerald H. Plessen, Birgit Schettler, Georg Jaccard, Samuel L. Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes |
topic_facet |
Nitrogen isotopes Subarctic North Pacific Polar stratification hypothesis |
description |
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 22 (2007): PA1215, doi:10.1029/2005PA001205. In a piston core from the central Bering Sea, diatom microfossil-bound N isotopes and the concentrations of opal, biogenic barium, calcium carbonate, and organic N are measured over the last glacial/interglacial cycle. Compared to the interglacial sections of the core, the sediments of the last ice age are characterized by 3‰ higher diatom-bound δ 15N, 70 wt % lower opal content and 1200 ppm lower biogenic barium. Taken together and with constraints on sediment accumulation rate, these results suggest a reduced supply of nitrate to the surface due to stronger stratification of the upper water column of the Bering Sea during glacial times, with more complete nitrate consumption resulting from continued iron supply through atmospheric deposition. This finding extends the body of evidence for a pervasive link between cold climates and polar ocean stratification. In addition, we hypothesize that more complete nutrient consumption in the glacial age subarctic Pacific contributed to the previously observed ice age reduction in suboxia and denitrification in the eastern tropical North Pacific by lowering the nutrient content of the intermediate-depth water formed in the subpolar North Pacific. In the deglacial interval of the Bering Sea record, two apparent peaks in export productivity are associated with maxima in diatom-bound and bulk sediment δ 15N. The high δ 15N in these intervals may have resulted from greater surface nutrient consumption during this period. However, the synchroneity of the deglacial peaks in the Bering Sea with similar bulk sediment δ 15N changes in the eastern Pacific margin and the presence of sediment lamination within the Bering Sea during the deposition of the productivity peaks raise the possibility that both regional and ... |
format |
Article in Journal/Newspaper |
author |
Brunelle, Brigitte G. Sigman, Daniel M. Cook, Mea S. Keigwin, Lloyd D. Haug, Gerald H. Plessen, Birgit Schettler, Georg Jaccard, Samuel L. |
author_facet |
Brunelle, Brigitte G. Sigman, Daniel M. Cook, Mea S. Keigwin, Lloyd D. Haug, Gerald H. Plessen, Birgit Schettler, Georg Jaccard, Samuel L. |
author_sort |
Brunelle, Brigitte G. |
title |
Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes |
title_short |
Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes |
title_full |
Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes |
title_fullStr |
Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes |
title_full_unstemmed |
Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes |
title_sort |
evidence from diatom-bound nitrogen isotopes for subarctic pacific stratification during the last ice age and a link to north pacific denitrification changes |
publisher |
American Geophysical Union |
publishDate |
2007 |
url |
https://hdl.handle.net/1912/3442 |
geographic |
Bering Sea Pacific |
geographic_facet |
Bering Sea Pacific |
genre |
Bering Sea Subarctic |
genre_facet |
Bering Sea Subarctic |
op_source |
Paleoceanography 22 (2007): PA1215 doi:10.1029/2005PA001205 |
op_relation |
https://doi.org/10.1029/2005PA001205 Paleoceanography 22 (2007): PA1215 https://hdl.handle.net/1912/3442 doi:10.1029/2005PA001205 |
op_doi |
https://doi.org/10.1029/2005PA001205 |
container_title |
Paleoceanography |
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22 |
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1 |
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1766377334831579136 |