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Benthic nitrogen loss in the Arabian Sea off Pakistan

Benthic nitrogen loss in the Arabian Sea off Pakistan
Benthic nitrogen loss in the Arabian Sea off Pakistan
A pronounced deficit of nitrogen (N) in the oxygen minimum zone (OMZ) of the Arabian Sea suggests the occurrence of heavy N-loss that is commonly attributed to pelagic processes. However, the OMZ water is in direct contact with sediments on three sides of the basin. Contribution from benthic N-loss to the total N-loss in the Arabian Sea remains largely unassessed. In October 2007, we sampled the water column and surface sediments along a transect cross-cutting the Arabian Sea OMZ at the Pakistan continental margin, covering a range of station depths from 360 to 1430?m. Benthic denitrification and anammox rates were determined by using (15)N-stable isotope pairing experiments. Intact core incubations showed declining rates of total benthic N-loss with water depth from 0.55 to 0.18?mmol?N?m(-2)?day(-1). While denitrification rates measured in slurry incubations decreased from 2.73 to 1.46?mmol?N?m(-2)?day(-1) with water depth, anammox rates increased from 0.21 to 0.89?mmol?N?m(-2)?day(-1). Hence, the contribution from anammox to total benthic N-loss increased from 7% at 360?m to 40% at 1430?m. This trend is further supported by the quantification of cd(1)-containing nitrite reductase (nirS), the biomarker functional gene encoding for cytochrome cd(1)-Nir of microorganisms involved in both N-loss processes. Anammox-like nirS genes within the sediments increased in proportion to total nirS gene copies with water depth. Moreover, phylogenetic analyses of NirS revealed different communities of both denitrifying and anammox bacteria between shallow and deep stations. Together, rate measurement and nirS analyses showed that anammox, determined for the first time in the Arabian Sea sediments, is an important benthic N-loss process at the continental margin off Pakistan, especially in the sediments at deeper water depths. Extrapolation from the measured benthic N-loss to all shelf sediments within the basin suggests that benthic N-loss may be responsible for about half of the overall N-loss in the Arabian Sea.
arabian sea, benthic n-loss, anammox, denitrification, qPCR, nirS
1664-302X
1-17
Sokoll, Sarah
17277bd1-d1b0-4cf2-af50-71706de43bd3
Holtappels, Moritz
cbfb5d6a-39bf-4116-a37f-a466869a4b13
Lam, Phyllis
996aef80-a15d-4827-aed8-1b97b378f6ad
Collins, Gavin
5c4706d8-adfb-4d23-8768-e43ae27c83d9
Schlüter, Michael
0f783422-422e-4fc9-9992-22b4dc96718e
Lavik, Gaute
29014780-d97c-41c0-8b59-a230bdfcdb37
Kuypers, Marcel M.M.
b6288cfb-42bc-469c-93fe-8fbb40d97bec
Sokoll, Sarah
17277bd1-d1b0-4cf2-af50-71706de43bd3
Holtappels, Moritz
cbfb5d6a-39bf-4116-a37f-a466869a4b13
Lam, Phyllis
996aef80-a15d-4827-aed8-1b97b378f6ad
Collins, Gavin
5c4706d8-adfb-4d23-8768-e43ae27c83d9
Schlüter, Michael
0f783422-422e-4fc9-9992-22b4dc96718e
Lavik, Gaute
29014780-d97c-41c0-8b59-a230bdfcdb37
Kuypers, Marcel M.M.
b6288cfb-42bc-469c-93fe-8fbb40d97bec

Sokoll, Sarah, Holtappels, Moritz, Lam, Phyllis, Collins, Gavin, Schlüter, Michael, Lavik, Gaute and Kuypers, Marcel M.M. (2012) Benthic nitrogen loss in the Arabian Sea off Pakistan. Frontiers in Microbiology, 3 (395), 1-17. (doi:10.3389/fmicb.2012.00395). (PMID:23226143)

Record type: Article

Abstract

A pronounced deficit of nitrogen (N) in the oxygen minimum zone (OMZ) of the Arabian Sea suggests the occurrence of heavy N-loss that is commonly attributed to pelagic processes. However, the OMZ water is in direct contact with sediments on three sides of the basin. Contribution from benthic N-loss to the total N-loss in the Arabian Sea remains largely unassessed. In October 2007, we sampled the water column and surface sediments along a transect cross-cutting the Arabian Sea OMZ at the Pakistan continental margin, covering a range of station depths from 360 to 1430?m. Benthic denitrification and anammox rates were determined by using (15)N-stable isotope pairing experiments. Intact core incubations showed declining rates of total benthic N-loss with water depth from 0.55 to 0.18?mmol?N?m(-2)?day(-1). While denitrification rates measured in slurry incubations decreased from 2.73 to 1.46?mmol?N?m(-2)?day(-1) with water depth, anammox rates increased from 0.21 to 0.89?mmol?N?m(-2)?day(-1). Hence, the contribution from anammox to total benthic N-loss increased from 7% at 360?m to 40% at 1430?m. This trend is further supported by the quantification of cd(1)-containing nitrite reductase (nirS), the biomarker functional gene encoding for cytochrome cd(1)-Nir of microorganisms involved in both N-loss processes. Anammox-like nirS genes within the sediments increased in proportion to total nirS gene copies with water depth. Moreover, phylogenetic analyses of NirS revealed different communities of both denitrifying and anammox bacteria between shallow and deep stations. Together, rate measurement and nirS analyses showed that anammox, determined for the first time in the Arabian Sea sediments, is an important benthic N-loss process at the continental margin off Pakistan, especially in the sediments at deeper water depths. Extrapolation from the measured benthic N-loss to all shelf sediments within the basin suggests that benthic N-loss may be responsible for about half of the overall N-loss in the Arabian Sea.

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More information

e-pub ahead of print date: 28 November 2012
Published date: 2012
Keywords: arabian sea, benthic n-loss, anammox, denitrification, qPCR, nirS
Organisations: Ocean Biochemistry & Ecosystems

Identifiers

Local EPrints ID: 348377
URI: http://eprints.soton.ac.uk/id/eprint/348377
ISSN: 1664-302X
PURE UUID: 6a14570e-3351-4885-962d-6abd5e413e5c
ORCID for Phyllis Lam: ORCID iD orcid.org/0000-0003-2067-171X

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Date deposited: 13 Mar 2013 13:18
Last modified: 15 Mar 2024 03:47

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Contributors

Author: Sarah Sokoll
Author: Moritz Holtappels
Author: Phyllis Lam ORCID iD
Author: Gavin Collins
Author: Michael Schlüter
Author: Gaute Lavik
Author: Marcel M.M. Kuypers

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