Benthic organic matter transformation drives pH and carbonate chemistry in Arctic marine sediments
Carbonate chemistry of the Arctic Ocean seafloor and its vulnerability to ocean acidification remains poorly explored. This limits our ability to quantify how biogeochemical processes and bottom water conditions shape sedimentary carbonate chemistry, and to predict how climate change may affect such...
Published in: | Global Biogeochemical Cycles |
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Language: | English |
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Wiley
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Online Access: | http://nora.nerc.ac.uk/id/eprint/532784/ https://nora.nerc.ac.uk/id/eprint/532784/1/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Freitas%20-%20Benthic%20Organic%20Matter%20Transformation%20Drives%20pH%20and%20Carbonate%20Chemistry%20in.pdf https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021GB007187 |
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ftnerc:oai:nora.nerc.ac.uk:532784 2023-05-15T14:27:06+02:00 Benthic organic matter transformation drives pH and carbonate chemistry in Arctic marine sediments Freitas, F.S. Arndt, S. Hendry, K.R. Faust, J.C. Tessin, A.C. März, C. 2022-07-07 text http://nora.nerc.ac.uk/id/eprint/532784/ https://nora.nerc.ac.uk/id/eprint/532784/1/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Freitas%20-%20Benthic%20Organic%20Matter%20Transformation%20Drives%20pH%20and%20Carbonate%20Chemistry%20in.pdf https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021GB007187 en eng Wiley https://nora.nerc.ac.uk/id/eprint/532784/1/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Freitas%20-%20Benthic%20Organic%20Matter%20Transformation%20Drives%20pH%20and%20Carbonate%20Chemistry%20in.pdf Freitas, F.S.; Arndt, S.; Hendry, K.R. orcid:0000-0002-0790-5895 Faust, J.C.; Tessin, A.C.; März, C. 2022 Benthic organic matter transformation drives pH and carbonate chemistry in Arctic marine sediments. Global Biogeochemical Cycles, 36 (7), e2021GB007187. 26, pp. https://doi.org/10.1029/2021GB007187 <https://doi.org/10.1029/2021GB007187> cc_by_4 CC-BY Publication - Article PeerReviewed 2022 ftnerc https://doi.org/10.1029/2021GB007187 2023-02-04T19:53:22Z Carbonate chemistry of the Arctic Ocean seafloor and its vulnerability to ocean acidification remains poorly explored. This limits our ability to quantify how biogeochemical processes and bottom water conditions shape sedimentary carbonate chemistry, and to predict how climate change may affect such biogeochemical processes at the Arctic Ocean seafloor. Here, we employ an integrated data-model assessment that explicitly resolves benthic pH and carbonate chemistry along a S—N transect in the Barents Sea. We identify the main drivers of observed carbonate dynamics and estimate benthic fluxes of dissolved inorganic carbon and alkalinity to the Arctic Ocean. We explore how bottom water conditions and in-situ organic matter degradation shape these processes and show that organic matter transformation strongly impacts pH and carbonate saturation (Ω) variations. Aerobic organic matter degradation drives a negative pH shift (pH < 7.6) in the upper 2—5 cm, producing Ω < 1. This causes shallow carbonate dissolution, buffering porewater pH to around 8.0. Organic matter degradation via metal oxide (Mn/Fe) reduction pathways further increases pH and carbonate saturation state. At the northern stations, where Ω > 5 at around 10–25 cm, model simulations result in authigenic carbonate precipitation. Furthermore, benthic fluxes of dissolved inorganic carbon (12.5—59.5 µmol cm−2 yr−1) and alkalinity (11.3—63.2 µmol cm−2 yr−1) are 2—3-fold greater in the northern sites due to greater carbonate dissolution. Our assessment is of significant relevance to predict how changes in the Arctic Ocean may shift carbon burial and pH buffering into the next century. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Barents Sea Climate change Ocean acidification Natural Environment Research Council: NERC Open Research Archive Arctic Arctic Ocean Barents Sea Global Biogeochemical Cycles 36 7 |
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Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
language |
English |
description |
Carbonate chemistry of the Arctic Ocean seafloor and its vulnerability to ocean acidification remains poorly explored. This limits our ability to quantify how biogeochemical processes and bottom water conditions shape sedimentary carbonate chemistry, and to predict how climate change may affect such biogeochemical processes at the Arctic Ocean seafloor. Here, we employ an integrated data-model assessment that explicitly resolves benthic pH and carbonate chemistry along a S—N transect in the Barents Sea. We identify the main drivers of observed carbonate dynamics and estimate benthic fluxes of dissolved inorganic carbon and alkalinity to the Arctic Ocean. We explore how bottom water conditions and in-situ organic matter degradation shape these processes and show that organic matter transformation strongly impacts pH and carbonate saturation (Ω) variations. Aerobic organic matter degradation drives a negative pH shift (pH < 7.6) in the upper 2—5 cm, producing Ω < 1. This causes shallow carbonate dissolution, buffering porewater pH to around 8.0. Organic matter degradation via metal oxide (Mn/Fe) reduction pathways further increases pH and carbonate saturation state. At the northern stations, where Ω > 5 at around 10–25 cm, model simulations result in authigenic carbonate precipitation. Furthermore, benthic fluxes of dissolved inorganic carbon (12.5—59.5 µmol cm−2 yr−1) and alkalinity (11.3—63.2 µmol cm−2 yr−1) are 2—3-fold greater in the northern sites due to greater carbonate dissolution. Our assessment is of significant relevance to predict how changes in the Arctic Ocean may shift carbon burial and pH buffering into the next century. |
format |
Article in Journal/Newspaper |
author |
Freitas, F.S. Arndt, S. Hendry, K.R. Faust, J.C. Tessin, A.C. März, C. |
spellingShingle |
Freitas, F.S. Arndt, S. Hendry, K.R. Faust, J.C. Tessin, A.C. März, C. Benthic organic matter transformation drives pH and carbonate chemistry in Arctic marine sediments |
author_facet |
Freitas, F.S. Arndt, S. Hendry, K.R. Faust, J.C. Tessin, A.C. März, C. |
author_sort |
Freitas, F.S. |
title |
Benthic organic matter transformation drives pH and carbonate chemistry in Arctic marine sediments |
title_short |
Benthic organic matter transformation drives pH and carbonate chemistry in Arctic marine sediments |
title_full |
Benthic organic matter transformation drives pH and carbonate chemistry in Arctic marine sediments |
title_fullStr |
Benthic organic matter transformation drives pH and carbonate chemistry in Arctic marine sediments |
title_full_unstemmed |
Benthic organic matter transformation drives pH and carbonate chemistry in Arctic marine sediments |
title_sort |
benthic organic matter transformation drives ph and carbonate chemistry in arctic marine sediments |
publisher |
Wiley |
publishDate |
2022 |
url |
http://nora.nerc.ac.uk/id/eprint/532784/ https://nora.nerc.ac.uk/id/eprint/532784/1/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Freitas%20-%20Benthic%20Organic%20Matter%20Transformation%20Drives%20pH%20and%20Carbonate%20Chemistry%20in.pdf https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021GB007187 |
geographic |
Arctic Arctic Ocean Barents Sea |
geographic_facet |
Arctic Arctic Ocean Barents Sea |
genre |
Arctic Arctic Arctic Ocean Barents Sea Climate change Ocean acidification |
genre_facet |
Arctic Arctic Arctic Ocean Barents Sea Climate change Ocean acidification |
op_relation |
https://nora.nerc.ac.uk/id/eprint/532784/1/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Freitas%20-%20Benthic%20Organic%20Matter%20Transformation%20Drives%20pH%20and%20Carbonate%20Chemistry%20in.pdf Freitas, F.S.; Arndt, S.; Hendry, K.R. orcid:0000-0002-0790-5895 Faust, J.C.; Tessin, A.C.; März, C. 2022 Benthic organic matter transformation drives pH and carbonate chemistry in Arctic marine sediments. Global Biogeochemical Cycles, 36 (7), e2021GB007187. 26, pp. https://doi.org/10.1029/2021GB007187 <https://doi.org/10.1029/2021GB007187> |
op_rights |
cc_by_4 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1029/2021GB007187 |
container_title |
Global Biogeochemical Cycles |
container_volume |
36 |
container_issue |
7 |
_version_ |
1766300692284178432 |