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Non-redfieldian mesopelagic nutrient remineralization in the eastern North Atlantic subtropical gyre

Non-redfieldian mesopelagic nutrient remineralization in the eastern North Atlantic subtropical gyre
Non-redfieldian mesopelagic nutrient remineralization in the eastern North Atlantic subtropical gyre
The eastern boundary of the North Atlantic subtropical gyre (NASTG) receives organic materials produced in the nearby Canary upwelling system (CanUS), which has important implications for the metabolic balance of the region. Here we computed absolute geostrophic, Ekman and eddy diffusive transports and net budgets of oxygen, nitrate, and phosphate, with an inverse model applied to annual climatologies from the World Ocean Atlas 2013, in a large box covering the eastern boundary of the NASTG. The surface waters (<100 m) of the box exported  mol O2 m−2 yr−1 to the adjacent ocean and atmosphere, and imported  mol N m−2 yr−1 and  mmol P m−2 yr−1 of nitrate and phosphate, respectively, indicating that net autotrophy prevailed in the euphotic waters of the eastern NASTG. The central, intermediate and deep waters (100 m-bottom) imported  mol O2 m−2 yr−1, and exported  mol N m−2 yr−1 and  mmol P m−2 yr−1 of nitrate and phosphate, respectively, indicative of net remineralization. Mesopelagic remineralization rates exceeded epipelagic net community production, implying a net deficit of carbon and nutrients in the region. Remineralization occurred at high N:P molar ratios (28) in central waters, and thus, a excess nitrate (DINxs = NO3-16PO4) was produced at a rate of  mol N yr−1. This excess nitrate was exported to the gyre interior, influencing the biogeochemistry of the whole NASTG and leaving the eastern margin with a strong nitrogen deficit, relative to carbon and phosphorus. According to the available literature, the organic carbon export from the CanUS could be sufficient to account for the carbon deficit, but the source of nitrogen remains elusive.
Eastern North Atlantic subtropical gyre, Excess nitrate, Metabolic balance, Nutrient cycling, Redfield ratios, Remineralization
0079-6611
136-153
Fernández-Castro, Bieito
8017e93c-d5ee-4bba-b443-9c72ca512d61
Mouriño-Carballido, Beatriz
1bfd941d-9ec6-473f-94bd-bb6faac56fa5
Álvarez-Salgado, Xosé Antón
c1111fff-5252-4e37-a6c4-9921df939260
Fernández-Castro, Bieito
8017e93c-d5ee-4bba-b443-9c72ca512d61
Mouriño-Carballido, Beatriz
1bfd941d-9ec6-473f-94bd-bb6faac56fa5
Álvarez-Salgado, Xosé Antón
c1111fff-5252-4e37-a6c4-9921df939260

Fernández-Castro, Bieito, Mouriño-Carballido, Beatriz and Álvarez-Salgado, Xosé Antón (2019) Non-redfieldian mesopelagic nutrient remineralization in the eastern North Atlantic subtropical gyre. Progress in Oceanography, 171, 136-153. (doi:10.1016/j.pocean.2018.12.001).

Record type: Article

Abstract

The eastern boundary of the North Atlantic subtropical gyre (NASTG) receives organic materials produced in the nearby Canary upwelling system (CanUS), which has important implications for the metabolic balance of the region. Here we computed absolute geostrophic, Ekman and eddy diffusive transports and net budgets of oxygen, nitrate, and phosphate, with an inverse model applied to annual climatologies from the World Ocean Atlas 2013, in a large box covering the eastern boundary of the NASTG. The surface waters (<100 m) of the box exported  mol O2 m−2 yr−1 to the adjacent ocean and atmosphere, and imported  mol N m−2 yr−1 and  mmol P m−2 yr−1 of nitrate and phosphate, respectively, indicating that net autotrophy prevailed in the euphotic waters of the eastern NASTG. The central, intermediate and deep waters (100 m-bottom) imported  mol O2 m−2 yr−1, and exported  mol N m−2 yr−1 and  mmol P m−2 yr−1 of nitrate and phosphate, respectively, indicative of net remineralization. Mesopelagic remineralization rates exceeded epipelagic net community production, implying a net deficit of carbon and nutrients in the region. Remineralization occurred at high N:P molar ratios (28) in central waters, and thus, a excess nitrate (DINxs = NO3-16PO4) was produced at a rate of  mol N yr−1. This excess nitrate was exported to the gyre interior, influencing the biogeochemistry of the whole NASTG and leaving the eastern margin with a strong nitrogen deficit, relative to carbon and phosphorus. According to the available literature, the organic carbon export from the CanUS could be sufficient to account for the carbon deficit, but the source of nitrogen remains elusive.

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More information

Accepted/In Press date: 6 December 2018
e-pub ahead of print date: 10 December 2018
Published date: 1 February 2019
Keywords: Eastern North Atlantic subtropical gyre, Excess nitrate, Metabolic balance, Nutrient cycling, Redfield ratios, Remineralization

Identifiers

Local EPrints ID: 453586
URI: http://eprints.soton.ac.uk/id/eprint/453586
ISSN: 0079-6611
PURE UUID: c4a34d62-c487-4712-a9a2-8321ee9849e9
ORCID for Bieito Fernández-Castro: ORCID iD orcid.org/0000-0001-7797-854X

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Date deposited: 20 Jan 2022 17:32
Last modified: 17 Mar 2024 04:04

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Contributors

Author: Beatriz Mouriño-Carballido
Author: Xosé Antón Álvarez-Salgado

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