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Nitrite oxidation in the Namibian oxygen minimum zone

Nitrite oxidation in the Namibian oxygen minimum zone
Nitrite oxidation in the Namibian oxygen minimum zone
Nitrite oxidation is the second step of nitrification. It is the primary source of oceanic nitrate, the predominant form of bioavailable nitrogen in the ocean. Despite its obvious importance, nitrite oxidation has rarely been investigated in marine settings. We determined nitrite oxidation rates directly in (15)N-incubation experiments and compared the rates with those of nitrate reduction to nitrite, ammonia oxidation, anammox, denitrification, as well as dissimilatory nitrate/nitrite reduction to ammonium in the Namibian oxygen minimum zone (OMZ). Nitrite oxidation (?372 nM NO(2)(-) d(-1)) was detected throughout the OMZ even when in situ oxygen concentrations were low to non-detectable. Nitrite oxidation rates often exceeded ammonia oxidation rates, whereas nitrate reduction served as an alternative and significant source of nitrite. Nitrite oxidation and anammox co-occurred in these oxygen-deficient waters, suggesting that nitrite-oxidizing bacteria (NOB) likely compete with anammox bacteria for nitrite when substrate availability became low. Among all of the known NOB genera targeted via catalyzed reporter deposition fluorescence in situ hybridization, only Nitrospina and Nitrococcus were detectable in the Namibian OMZ samples investigated. These NOB were abundant throughout the OMZ and contributed up to ~9% of total microbial community. Our combined results reveal that a considerable fraction of the recently recycled nitrogen or reduced NO(3)(-) was re-oxidized back to NO(3)(-) via nitrite oxidation, instead of being lost from the system through the anammox or denitrification pathways.
1751-7362
1200-1209
Füssel, Jessika
6abc0a9f-01d7-4ec4-ab88-d12c58442087
Lam, Phyllis
996aef80-a15d-4827-aed8-1b97b378f6ad
Lavik, Gaute
29014780-d97c-41c0-8b59-a230bdfcdb37
Jensen, Marlene M.
23ff1ce5-4644-4816-be78-4762c15266e0
Holtappels, Moritz
cbfb5d6a-39bf-4116-a37f-a466869a4b13
Günter, Marcel
d6dbe6e7-8d4e-469a-a77b-cb567a71d44d
Kuypers, Marcel M.M.
b6288cfb-42bc-469c-93fe-8fbb40d97bec
Füssel, Jessika
6abc0a9f-01d7-4ec4-ab88-d12c58442087
Lam, Phyllis
996aef80-a15d-4827-aed8-1b97b378f6ad
Lavik, Gaute
29014780-d97c-41c0-8b59-a230bdfcdb37
Jensen, Marlene M.
23ff1ce5-4644-4816-be78-4762c15266e0
Holtappels, Moritz
cbfb5d6a-39bf-4116-a37f-a466869a4b13
Günter, Marcel
d6dbe6e7-8d4e-469a-a77b-cb567a71d44d
Kuypers, Marcel M.M.
b6288cfb-42bc-469c-93fe-8fbb40d97bec

Füssel, Jessika, Lam, Phyllis, Lavik, Gaute, Jensen, Marlene M., Holtappels, Moritz, Günter, Marcel and Kuypers, Marcel M.M. (2012) Nitrite oxidation in the Namibian oxygen minimum zone. The ISME Journal, 6 (6), 1200-1209. (doi:10.1038/ismej.2011.178). (PMID:22170426)

Record type: Article

Abstract

Nitrite oxidation is the second step of nitrification. It is the primary source of oceanic nitrate, the predominant form of bioavailable nitrogen in the ocean. Despite its obvious importance, nitrite oxidation has rarely been investigated in marine settings. We determined nitrite oxidation rates directly in (15)N-incubation experiments and compared the rates with those of nitrate reduction to nitrite, ammonia oxidation, anammox, denitrification, as well as dissimilatory nitrate/nitrite reduction to ammonium in the Namibian oxygen minimum zone (OMZ). Nitrite oxidation (?372 nM NO(2)(-) d(-1)) was detected throughout the OMZ even when in situ oxygen concentrations were low to non-detectable. Nitrite oxidation rates often exceeded ammonia oxidation rates, whereas nitrate reduction served as an alternative and significant source of nitrite. Nitrite oxidation and anammox co-occurred in these oxygen-deficient waters, suggesting that nitrite-oxidizing bacteria (NOB) likely compete with anammox bacteria for nitrite when substrate availability became low. Among all of the known NOB genera targeted via catalyzed reporter deposition fluorescence in situ hybridization, only Nitrospina and Nitrococcus were detectable in the Namibian OMZ samples investigated. These NOB were abundant throughout the OMZ and contributed up to ~9% of total microbial community. Our combined results reveal that a considerable fraction of the recently recycled nitrogen or reduced NO(3)(-) was re-oxidized back to NO(3)(-) via nitrite oxidation, instead of being lost from the system through the anammox or denitrification pathways.

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Published date: June 2012
Organisations: Ocean Biochemistry & Ecosystems

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Local EPrints ID: 349909
URI: http://eprints.soton.ac.uk/id/eprint/349909
ISSN: 1751-7362
PURE UUID: ce831537-2004-4741-9cf5-afbd56c93c30
ORCID for Phyllis Lam: ORCID iD orcid.org/0000-0003-2067-171X

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Date deposited: 13 Mar 2013 13:22
Last modified: 15 Mar 2024 03:47

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Contributors

Author: Jessika Füssel
Author: Phyllis Lam ORCID iD
Author: Gaute Lavik
Author: Marlene M. Jensen
Author: Moritz Holtappels
Author: Marcel Günter
Author: Marcel M.M. Kuypers

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