Carbonate counter pump stimulated by natural iron fertilization in the Polar Frontal Zone

The production of organic carbon in the ocean’s surface and its subsequent downward export transfers carbon dioxide to the deep ocean. This CO2 drawdown is countered by the biological precipitation of carbonate, followed by sinking of particulate inorganic carbon, which is a source of carbon dioxide...

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Published in:Nature Geoscience
Main Authors: Salter, Ian, Schiebel, Ralf, Ziveri, Patrizia, Movellan, Aurore, Lampitt, Richard, Wolff, George A.
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/508917/
https://nora.nerc.ac.uk/id/eprint/508917/1/Salter%20et%20al%202014%20draft%208.pdf
https://doi.org/10.1038/ngeo2285
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spelling ftnerc:oai:nora.nerc.ac.uk:508917 2023-05-15T13:48:08+02:00 Carbonate counter pump stimulated by natural iron fertilization in the Polar Frontal Zone Salter, Ian Schiebel, Ralf Ziveri, Patrizia Movellan, Aurore Lampitt, Richard Wolff, George A. 2014-11-10 text http://nora.nerc.ac.uk/id/eprint/508917/ https://nora.nerc.ac.uk/id/eprint/508917/1/Salter%20et%20al%202014%20draft%208.pdf https://doi.org/10.1038/ngeo2285 en eng https://nora.nerc.ac.uk/id/eprint/508917/1/Salter%20et%20al%202014%20draft%208.pdf Salter, Ian; Schiebel, Ralf; Ziveri, Patrizia; Movellan, Aurore; Lampitt, Richard; Wolff, George A. 2014 Carbonate counter pump stimulated by natural iron fertilization in the Polar Frontal Zone. Nature Geoscience, 7. 885-889. https://doi.org/10.1038/ngeo2285 <https://doi.org/10.1038/ngeo2285> Publication - Article PeerReviewed 2014 ftnerc https://doi.org/10.1038/ngeo2285 2023-02-04T19:40:35Z The production of organic carbon in the ocean’s surface and its subsequent downward export transfers carbon dioxide to the deep ocean. This CO2 drawdown is countered by the biological precipitation of carbonate, followed by sinking of particulate inorganic carbon, which is a source of carbon dioxide to the surface ocean, and hence the atmosphere over 100–1,000 year timescales1. The net transfer of CO2 to the deep ocean is therefore dependent on the relative amount of organic and inorganic carbon in sinking particles2. In the Southern Ocean, iron fertilization has been shown to increase the export of organic carbon3, 4, 5, but it is unclear to what degree this effect is compensated by the export of inorganic carbon. Here we assess the composition of sinking particles collected from sediment traps located in the Polar Frontal Zone of the Southern Ocean. We find that in high-nutrient, low-chlorophyll regions that are characterized by naturally high iron concentrations, fluxes of both organic and inorganic carbon are higher than in regions with no iron fertilization. However, the excess flux of inorganic carbon is greater than that of organic carbon. We estimate that the production and flux of carbonate in naturally iron-fertilized waters reduces the overall amount of CO2 transferred to the deep ocean by 6–32%, compared to 1–4% at the non-fertilized site. We suggest that an increased export of organic carbon, stimulated by iron availability in the glacial sub-Antarctic oceans, may have been accompanied by a strengthened carbonate counter pump. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Natural Environment Research Council: NERC Open Research Archive Antarctic Southern Ocean Nature Geoscience 7 12 885 889
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
description The production of organic carbon in the ocean’s surface and its subsequent downward export transfers carbon dioxide to the deep ocean. This CO2 drawdown is countered by the biological precipitation of carbonate, followed by sinking of particulate inorganic carbon, which is a source of carbon dioxide to the surface ocean, and hence the atmosphere over 100–1,000 year timescales1. The net transfer of CO2 to the deep ocean is therefore dependent on the relative amount of organic and inorganic carbon in sinking particles2. In the Southern Ocean, iron fertilization has been shown to increase the export of organic carbon3, 4, 5, but it is unclear to what degree this effect is compensated by the export of inorganic carbon. Here we assess the composition of sinking particles collected from sediment traps located in the Polar Frontal Zone of the Southern Ocean. We find that in high-nutrient, low-chlorophyll regions that are characterized by naturally high iron concentrations, fluxes of both organic and inorganic carbon are higher than in regions with no iron fertilization. However, the excess flux of inorganic carbon is greater than that of organic carbon. We estimate that the production and flux of carbonate in naturally iron-fertilized waters reduces the overall amount of CO2 transferred to the deep ocean by 6–32%, compared to 1–4% at the non-fertilized site. We suggest that an increased export of organic carbon, stimulated by iron availability in the glacial sub-Antarctic oceans, may have been accompanied by a strengthened carbonate counter pump.
format Article in Journal/Newspaper
author Salter, Ian
Schiebel, Ralf
Ziveri, Patrizia
Movellan, Aurore
Lampitt, Richard
Wolff, George A.
spellingShingle Salter, Ian
Schiebel, Ralf
Ziveri, Patrizia
Movellan, Aurore
Lampitt, Richard
Wolff, George A.
Carbonate counter pump stimulated by natural iron fertilization in the Polar Frontal Zone
author_facet Salter, Ian
Schiebel, Ralf
Ziveri, Patrizia
Movellan, Aurore
Lampitt, Richard
Wolff, George A.
author_sort Salter, Ian
title Carbonate counter pump stimulated by natural iron fertilization in the Polar Frontal Zone
title_short Carbonate counter pump stimulated by natural iron fertilization in the Polar Frontal Zone
title_full Carbonate counter pump stimulated by natural iron fertilization in the Polar Frontal Zone
title_fullStr Carbonate counter pump stimulated by natural iron fertilization in the Polar Frontal Zone
title_full_unstemmed Carbonate counter pump stimulated by natural iron fertilization in the Polar Frontal Zone
title_sort carbonate counter pump stimulated by natural iron fertilization in the polar frontal zone
publishDate 2014
url http://nora.nerc.ac.uk/id/eprint/508917/
https://nora.nerc.ac.uk/id/eprint/508917/1/Salter%20et%20al%202014%20draft%208.pdf
https://doi.org/10.1038/ngeo2285
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_relation https://nora.nerc.ac.uk/id/eprint/508917/1/Salter%20et%20al%202014%20draft%208.pdf
Salter, Ian; Schiebel, Ralf; Ziveri, Patrizia; Movellan, Aurore; Lampitt, Richard; Wolff, George A. 2014 Carbonate counter pump stimulated by natural iron fertilization in the Polar Frontal Zone. Nature Geoscience, 7. 885-889. https://doi.org/10.1038/ngeo2285 <https://doi.org/10.1038/ngeo2285>
op_doi https://doi.org/10.1038/ngeo2285
container_title Nature Geoscience
container_volume 7
container_issue 12
container_start_page 885
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