Contrasting biogeochemistry of nitrogen in the Atlantic and Pacific Oxygen Minimum Zones
We present new data for the stable isotope ratio of inorganic nitrogen species from the contrasting oxygen minimum zones (OMZs) of the Eastern Tropical North Atlantic, south of Cape Verde, and the Eastern Tropical South Pacific off Peru. Differences in minimum oxygen concentration and corresponding...
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ftdoajarticles:oai:doaj.org/article:c20e940af6e04d4eb7578c4b52dde5ad 2023-05-15T17:34:59+02:00 Contrasting biogeochemistry of nitrogen in the Atlantic and Pacific Oxygen Minimum Zones E. Ryabenko A. Kock H. W. Bange M. A. Altabet D. W. R. Wallace 2012-01-01T00:00:00Z https://doi.org/10.5194/bg-9-203-2012 https://doaj.org/article/c20e940af6e04d4eb7578c4b52dde5ad EN eng Copernicus Publications http://www.biogeosciences.net/9/203/2012/bg-9-203-2012.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 doi:10.5194/bg-9-203-2012 https://doaj.org/article/c20e940af6e04d4eb7578c4b52dde5ad Biogeosciences, Vol 9, Iss 1, Pp 203-215 (2012) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2012 ftdoajarticles https://doi.org/10.5194/bg-9-203-2012 2022-12-31T14:34:42Z We present new data for the stable isotope ratio of inorganic nitrogen species from the contrasting oxygen minimum zones (OMZs) of the Eastern Tropical North Atlantic, south of Cape Verde, and the Eastern Tropical South Pacific off Peru. Differences in minimum oxygen concentration and corresponding N-cycle processes for the two OMZs are reflected in strongly contrasting δ 15 N distributions. Pacific surface waters are marked by strongly positive values for δ 15 N-NO 3 – ) reflecting fractionation associated with subsurface N-loss and partial NO 3 – utilization. This contrasts with negative values in NO 3 – depleted surface waters of the Atlantic which are lower than can be explained by N supply via N 2 fixation. We suggest the negative values reflect inputs of nitrate, possibly transient, associated with deposition of Saharan dust. Strong signals of N-loss processes in the subsurface Pacific OMZ are evident in the isotope and N 2 O data, both of which are compatible with a contribution of canonical denitrification to overall N-loss. However the apparent N isotope fractionation factor observed is relatively low (ε d =11.4 ‰) suggesting an effect of influence from denitrification in sediments. Identical positive correlation of N 2 O vs. AOU for waters with oxygen concentrations ([O 2 ] < 5 μmol l −1 ) in both regions reflect a nitrification source. Sharp decrease in N 2 O concentrations is observed in the Pacific OMZ due to denitrification under oxygen concentrations O 2 < 5 μmol l −1 . Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Pacific Biogeosciences 9 1 203 215 |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
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Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 E. Ryabenko A. Kock H. W. Bange M. A. Altabet D. W. R. Wallace Contrasting biogeochemistry of nitrogen in the Atlantic and Pacific Oxygen Minimum Zones |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
We present new data for the stable isotope ratio of inorganic nitrogen species from the contrasting oxygen minimum zones (OMZs) of the Eastern Tropical North Atlantic, south of Cape Verde, and the Eastern Tropical South Pacific off Peru. Differences in minimum oxygen concentration and corresponding N-cycle processes for the two OMZs are reflected in strongly contrasting δ 15 N distributions. Pacific surface waters are marked by strongly positive values for δ 15 N-NO 3 – ) reflecting fractionation associated with subsurface N-loss and partial NO 3 – utilization. This contrasts with negative values in NO 3 – depleted surface waters of the Atlantic which are lower than can be explained by N supply via N 2 fixation. We suggest the negative values reflect inputs of nitrate, possibly transient, associated with deposition of Saharan dust. Strong signals of N-loss processes in the subsurface Pacific OMZ are evident in the isotope and N 2 O data, both of which are compatible with a contribution of canonical denitrification to overall N-loss. However the apparent N isotope fractionation factor observed is relatively low (ε d =11.4 ‰) suggesting an effect of influence from denitrification in sediments. Identical positive correlation of N 2 O vs. AOU for waters with oxygen concentrations ([O 2 ] < 5 μmol l −1 ) in both regions reflect a nitrification source. Sharp decrease in N 2 O concentrations is observed in the Pacific OMZ due to denitrification under oxygen concentrations O 2 < 5 μmol l −1 . |
format |
Article in Journal/Newspaper |
author |
E. Ryabenko A. Kock H. W. Bange M. A. Altabet D. W. R. Wallace |
author_facet |
E. Ryabenko A. Kock H. W. Bange M. A. Altabet D. W. R. Wallace |
author_sort |
E. Ryabenko |
title |
Contrasting biogeochemistry of nitrogen in the Atlantic and Pacific Oxygen Minimum Zones |
title_short |
Contrasting biogeochemistry of nitrogen in the Atlantic and Pacific Oxygen Minimum Zones |
title_full |
Contrasting biogeochemistry of nitrogen in the Atlantic and Pacific Oxygen Minimum Zones |
title_fullStr |
Contrasting biogeochemistry of nitrogen in the Atlantic and Pacific Oxygen Minimum Zones |
title_full_unstemmed |
Contrasting biogeochemistry of nitrogen in the Atlantic and Pacific Oxygen Minimum Zones |
title_sort |
contrasting biogeochemistry of nitrogen in the atlantic and pacific oxygen minimum zones |
publisher |
Copernicus Publications |
publishDate |
2012 |
url |
https://doi.org/10.5194/bg-9-203-2012 https://doaj.org/article/c20e940af6e04d4eb7578c4b52dde5ad |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Biogeosciences, Vol 9, Iss 1, Pp 203-215 (2012) |
op_relation |
http://www.biogeosciences.net/9/203/2012/bg-9-203-2012.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 doi:10.5194/bg-9-203-2012 https://doaj.org/article/c20e940af6e04d4eb7578c4b52dde5ad |
op_doi |
https://doi.org/10.5194/bg-9-203-2012 |
container_title |
Biogeosciences |
container_volume |
9 |
container_issue |
1 |
container_start_page |
203 |
op_container_end_page |
215 |
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1766134003325206528 |