Projected pH reductions by 2100 might put deep North Atlantic biodiversity at risk

This study aims to evaluate the potential for impacts of ocean acidification on North Atlantic deep-sea ecosystems in response to IPCC AR5 Representative Concentration Pathways (RCPs). Deep-sea biota is likely highly vulnerable to changes in seawater chemistry and sensitive to moderate excursions in...

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Published in:Biogeosciences
Main Authors: Gehlen, M., Séférian, R., Jones, D. O. B., Roy, T., Roth, R., Barry, J., Bopp, L., Doney, S. C., Dunne, J. P., Heinze, C., Joos, F., Orr, J. C., Resplandy, L., Segschneider, J., Tjiputra, J.
Format: Text
Language:English
Published: 2018
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Online Access:https://doi.org/10.5194/bg-11-6955-2014
https://www.biogeosciences.net/11/6955/2014/
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spelling ftcopernicus:oai:publications.copernicus.org:bg25356 2023-05-15T17:27:21+02:00 Projected pH reductions by 2100 might put deep North Atlantic biodiversity at risk Gehlen, M. Séférian, R. Jones, D. O. B. Roy, T. Roth, R. Barry, J. Bopp, L. Doney, S. C. Dunne, J. P. Heinze, C. Joos, F. Orr, J. C. Resplandy, L. Segschneider, J. Tjiputra, J. 2018-09-27 application/pdf https://doi.org/10.5194/bg-11-6955-2014 https://www.biogeosciences.net/11/6955/2014/ eng eng doi:10.5194/bg-11-6955-2014 https://www.biogeosciences.net/11/6955/2014/ eISSN: 1726-4189 Text 2018 ftcopernicus https://doi.org/10.5194/bg-11-6955-2014 2019-12-24T09:53:55Z This study aims to evaluate the potential for impacts of ocean acidification on North Atlantic deep-sea ecosystems in response to IPCC AR5 Representative Concentration Pathways (RCPs). Deep-sea biota is likely highly vulnerable to changes in seawater chemistry and sensitive to moderate excursions in pH. Here we show, from seven fully coupled Earth system models, that for three out of four RCPs over 17% of the seafloor area below 500 m depth in the North Atlantic sector will experience pH reductions exceeding −0.2 units by 2100. Increased stratification in response to climate change partially alleviates the impact of ocean acidification on deep benthic environments. We report on major pH reductions over the deep North Atlantic seafloor (depth >500 m) and at important deep-sea features, such as seamounts and canyons. By 2100, and under the high CO 2 scenario RCP8.5, pH reductions exceeding −0.2 (−0.3) units are projected in close to 23% (~15%) of North Atlantic deep-sea canyons and ~8% (3%) of seamounts – including seamounts proposed as sites of marine protected areas. The spatial pattern of impacts reflects the depth of the pH perturbation and does not scale linearly with atmospheric CO 2 concentration. Impacts may cause negative changes of the same magnitude or exceeding the current target of 10% of preservation of marine biomes set by the convention on biological diversity, implying that ocean acidification may offset benefits from conservation/management strategies relying on the regulation of resource exploitation. Text North Atlantic Ocean acidification Copernicus Publications: E-Journals Biogeosciences 11 23 6955 6967
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language English
description This study aims to evaluate the potential for impacts of ocean acidification on North Atlantic deep-sea ecosystems in response to IPCC AR5 Representative Concentration Pathways (RCPs). Deep-sea biota is likely highly vulnerable to changes in seawater chemistry and sensitive to moderate excursions in pH. Here we show, from seven fully coupled Earth system models, that for three out of four RCPs over 17% of the seafloor area below 500 m depth in the North Atlantic sector will experience pH reductions exceeding −0.2 units by 2100. Increased stratification in response to climate change partially alleviates the impact of ocean acidification on deep benthic environments. We report on major pH reductions over the deep North Atlantic seafloor (depth >500 m) and at important deep-sea features, such as seamounts and canyons. By 2100, and under the high CO 2 scenario RCP8.5, pH reductions exceeding −0.2 (−0.3) units are projected in close to 23% (~15%) of North Atlantic deep-sea canyons and ~8% (3%) of seamounts – including seamounts proposed as sites of marine protected areas. The spatial pattern of impacts reflects the depth of the pH perturbation and does not scale linearly with atmospheric CO 2 concentration. Impacts may cause negative changes of the same magnitude or exceeding the current target of 10% of preservation of marine biomes set by the convention on biological diversity, implying that ocean acidification may offset benefits from conservation/management strategies relying on the regulation of resource exploitation.
format Text
author Gehlen, M.
Séférian, R.
Jones, D. O. B.
Roy, T.
Roth, R.
Barry, J.
Bopp, L.
Doney, S. C.
Dunne, J. P.
Heinze, C.
Joos, F.
Orr, J. C.
Resplandy, L.
Segschneider, J.
Tjiputra, J.
spellingShingle Gehlen, M.
Séférian, R.
Jones, D. O. B.
Roy, T.
Roth, R.
Barry, J.
Bopp, L.
Doney, S. C.
Dunne, J. P.
Heinze, C.
Joos, F.
Orr, J. C.
Resplandy, L.
Segschneider, J.
Tjiputra, J.
Projected pH reductions by 2100 might put deep North Atlantic biodiversity at risk
author_facet Gehlen, M.
Séférian, R.
Jones, D. O. B.
Roy, T.
Roth, R.
Barry, J.
Bopp, L.
Doney, S. C.
Dunne, J. P.
Heinze, C.
Joos, F.
Orr, J. C.
Resplandy, L.
Segschneider, J.
Tjiputra, J.
author_sort Gehlen, M.
title Projected pH reductions by 2100 might put deep North Atlantic biodiversity at risk
title_short Projected pH reductions by 2100 might put deep North Atlantic biodiversity at risk
title_full Projected pH reductions by 2100 might put deep North Atlantic biodiversity at risk
title_fullStr Projected pH reductions by 2100 might put deep North Atlantic biodiversity at risk
title_full_unstemmed Projected pH reductions by 2100 might put deep North Atlantic biodiversity at risk
title_sort projected ph reductions by 2100 might put deep north atlantic biodiversity at risk
publishDate 2018
url https://doi.org/10.5194/bg-11-6955-2014
https://www.biogeosciences.net/11/6955/2014/
genre North Atlantic
Ocean acidification
genre_facet North Atlantic
Ocean acidification
op_source eISSN: 1726-4189
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https://www.biogeosciences.net/11/6955/2014/
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