Sensitivity of pelagic calcification to ocean acidification
Ocean acidification might reduce the ability of calcifying plankton to produce and maintain their shells of calcite, or of aragonite, the more soluble form of CaCO 3 . In addition to possibly large biological impacts, reduced CaCO 3 production corresponds to a negative feedback on atmospheric CO 2 ....
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ftdoajarticles:oai:doaj.org/article:c02675d2961f49e5bf86dda5ebb4d9a6 2023-05-15T17:50:19+02:00 Sensitivity of pelagic calcification to ocean acidification R. Gangstø F. Joos M. Gehlen 2011-02-01T00:00:00Z https://doi.org/10.5194/bg-8-433-2011 https://doaj.org/article/c02675d2961f49e5bf86dda5ebb4d9a6 EN eng Copernicus Publications http://www.biogeosciences.net/8/433/2011/bg-8-433-2011.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-8-433-2011 1726-4170 1726-4189 https://doaj.org/article/c02675d2961f49e5bf86dda5ebb4d9a6 Biogeosciences, Vol 8, Iss 2, Pp 433-458 (2011) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2011 ftdoajarticles https://doi.org/10.5194/bg-8-433-2011 2022-12-31T09:06:43Z Ocean acidification might reduce the ability of calcifying plankton to produce and maintain their shells of calcite, or of aragonite, the more soluble form of CaCO 3 . In addition to possibly large biological impacts, reduced CaCO 3 production corresponds to a negative feedback on atmospheric CO 2 . In order to explore the sensitivity of the ocean carbon cycle to increasing concentrations of atmospheric CO 2 , we use the new biogeochemical Bern3D/PISCES model. The model reproduces the large scale distributions of biogeochemical tracers. With a range of sensitivity studies, we explore the effect of (i) using different parameterizations of CaCO 3 production fitted to available laboratory and field experiments, of (ii) letting calcite and aragonite be produced by auto- and heterotrophic plankton groups, and of (iii) using carbon emissions from the range of the most recent IPCC Representative Concentration Pathways (RCP). Under a high-emission scenario, the CaCO 3 production of all the model versions decreases from ~1 Pg C yr −1 to between 0.36 and 0.82 Pg C yr −1 by the year 2100. The changes in CaCO 3 production and dissolution resulting from ocean acidification provide only a small feedback on atmospheric CO 2 of −1 to −11 ppm by the year 2100, despite the wide range of parameterizations, model versions and scenarios included in our study. A potential upper limit of the CO 2 -calcification/dissolution feedback of −30 ppm by the year 2100 is computed by setting calcification to zero after 2000 in a high 21st century emission scenario. The similarity of feedback estimates yielded by the model version with calcite produced by nanophytoplankton and the one with calcite, respectively aragonite produced by mesozooplankton suggests that expending biogeochemical models to calcifying zooplankton might not be needed to simulate biogeochemical impacts on the marine carbonate cycle. The changes in saturation state confirm previous studies indicating that future anthropogenic CO 2 emissions may lead to irreversible changes in ... Article in Journal/Newspaper Ocean acidification Directory of Open Access Journals: DOAJ Articles Biogeosciences 8 2 433 458 |
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Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
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Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 R. Gangstø F. Joos M. Gehlen Sensitivity of pelagic calcification to ocean acidification |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
Ocean acidification might reduce the ability of calcifying plankton to produce and maintain their shells of calcite, or of aragonite, the more soluble form of CaCO 3 . In addition to possibly large biological impacts, reduced CaCO 3 production corresponds to a negative feedback on atmospheric CO 2 . In order to explore the sensitivity of the ocean carbon cycle to increasing concentrations of atmospheric CO 2 , we use the new biogeochemical Bern3D/PISCES model. The model reproduces the large scale distributions of biogeochemical tracers. With a range of sensitivity studies, we explore the effect of (i) using different parameterizations of CaCO 3 production fitted to available laboratory and field experiments, of (ii) letting calcite and aragonite be produced by auto- and heterotrophic plankton groups, and of (iii) using carbon emissions from the range of the most recent IPCC Representative Concentration Pathways (RCP). Under a high-emission scenario, the CaCO 3 production of all the model versions decreases from ~1 Pg C yr −1 to between 0.36 and 0.82 Pg C yr −1 by the year 2100. The changes in CaCO 3 production and dissolution resulting from ocean acidification provide only a small feedback on atmospheric CO 2 of −1 to −11 ppm by the year 2100, despite the wide range of parameterizations, model versions and scenarios included in our study. A potential upper limit of the CO 2 -calcification/dissolution feedback of −30 ppm by the year 2100 is computed by setting calcification to zero after 2000 in a high 21st century emission scenario. The similarity of feedback estimates yielded by the model version with calcite produced by nanophytoplankton and the one with calcite, respectively aragonite produced by mesozooplankton suggests that expending biogeochemical models to calcifying zooplankton might not be needed to simulate biogeochemical impacts on the marine carbonate cycle. The changes in saturation state confirm previous studies indicating that future anthropogenic CO 2 emissions may lead to irreversible changes in ... |
format |
Article in Journal/Newspaper |
author |
R. Gangstø F. Joos M. Gehlen |
author_facet |
R. Gangstø F. Joos M. Gehlen |
author_sort |
R. Gangstø |
title |
Sensitivity of pelagic calcification to ocean acidification |
title_short |
Sensitivity of pelagic calcification to ocean acidification |
title_full |
Sensitivity of pelagic calcification to ocean acidification |
title_fullStr |
Sensitivity of pelagic calcification to ocean acidification |
title_full_unstemmed |
Sensitivity of pelagic calcification to ocean acidification |
title_sort |
sensitivity of pelagic calcification to ocean acidification |
publisher |
Copernicus Publications |
publishDate |
2011 |
url |
https://doi.org/10.5194/bg-8-433-2011 https://doaj.org/article/c02675d2961f49e5bf86dda5ebb4d9a6 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Biogeosciences, Vol 8, Iss 2, Pp 433-458 (2011) |
op_relation |
http://www.biogeosciences.net/8/433/2011/bg-8-433-2011.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-8-433-2011 1726-4170 1726-4189 https://doaj.org/article/c02675d2961f49e5bf86dda5ebb4d9a6 |
op_doi |
https://doi.org/10.5194/bg-8-433-2011 |
container_title |
Biogeosciences |
container_volume |
8 |
container_issue |
2 |
container_start_page |
433 |
op_container_end_page |
458 |
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1766157027950723072 |