Calcifying species sensitivity distributions for ocean acidification

Increasing CO2 atmospheric levels lead to increasing ocean acidification, thereby enhancing calcium carbonate dissolution of calcifying species. We gathered peer-reviewed experimental data on the effects of acidified seawater on calcifying species growth, reproduction, and survival. The data were us...

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Main Authors: Azevedo, L., De Schryver, A.M., Hendriks, A.J., Huijbregts, M.A.J.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Chemical Society (ACS) 2015
Subjects:
Online Access:http://pure.iiasa.ac.at/id/eprint/11515/
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spelling ftiiasalaxendare:oai:pure.iiasa.ac.at:11515 2023-05-15T17:49:54+02:00 Calcifying species sensitivity distributions for ocean acidification Azevedo, L. De Schryver, A.M. Hendriks, A.J. Huijbregts, M.A.J. 2015-02 http://pure.iiasa.ac.at/id/eprint/11515/ unknown American Chemical Society (ACS) Azevedo, L. <http://pure.iiasa.ac.at/view/iiasa/21.html>, De Schryver, A.M., Hendriks, A.J., & Huijbregts, M.A.J. (2015). Calcifying species sensitivity distributions for ocean acidification. Environmental Science & Technology 49 (3) 1495-1500. 10.1021/es505485m <https://doi.org/10.1021/es505485m>. info:eu-repo/semantics/closedAccess Article PeerReviewed info:eu-repo/semantics/article 2015 ftiiasalaxendare 2022-04-15T12:35:24Z Increasing CO2 atmospheric levels lead to increasing ocean acidification, thereby enhancing calcium carbonate dissolution of calcifying species. We gathered peer-reviewed experimental data on the effects of acidified seawater on calcifying species growth, reproduction, and survival. The data were used to derive species-specific median effective concentrations, i.e., pH50, and pH10, via logistic regression. Subsequently, we developed species sensitivity distributions (SSDs) to assess the potentially affected fraction (PAF) of species exposed to pH declines. Effects on species growth were observed at higher pH than those on species reproduction (mean pH10 was 7.73 vs 7.63 and mean pH50 was 7.28 vs 7.11 for the two life processes, respectively) and the variability in the sensitivity of species increased with increasing number of species available for the PAF (pH10 standard deviation was 0.20, 0.21, and 0.33 for survival, reproduction, and growth, respectively). The SSDs were then applied to two climate change scenarios to estimate the increase in PAF (.PAF) by future ocean acidification. In a high CO2 emission scenario, .PAF was 3 to 10% (for pH50) and 21 to 32% (for pH10). In a low emission scenario, .PAF was 1 to 4% (for pH50) and 7 to 12% (for pH10). Our SSDs developed for the effect of decreasing ocean pH on calcifying marine species assemblages can also be used for comparison with other environmental stressors. Article in Journal/Newspaper Ocean acidification IIASA DARE (Data Repository of the International Institute of Applied Systems Analysis)
institution Open Polar
collection IIASA DARE (Data Repository of the International Institute of Applied Systems Analysis)
op_collection_id ftiiasalaxendare
language unknown
description Increasing CO2 atmospheric levels lead to increasing ocean acidification, thereby enhancing calcium carbonate dissolution of calcifying species. We gathered peer-reviewed experimental data on the effects of acidified seawater on calcifying species growth, reproduction, and survival. The data were used to derive species-specific median effective concentrations, i.e., pH50, and pH10, via logistic regression. Subsequently, we developed species sensitivity distributions (SSDs) to assess the potentially affected fraction (PAF) of species exposed to pH declines. Effects on species growth were observed at higher pH than those on species reproduction (mean pH10 was 7.73 vs 7.63 and mean pH50 was 7.28 vs 7.11 for the two life processes, respectively) and the variability in the sensitivity of species increased with increasing number of species available for the PAF (pH10 standard deviation was 0.20, 0.21, and 0.33 for survival, reproduction, and growth, respectively). The SSDs were then applied to two climate change scenarios to estimate the increase in PAF (.PAF) by future ocean acidification. In a high CO2 emission scenario, .PAF was 3 to 10% (for pH50) and 21 to 32% (for pH10). In a low emission scenario, .PAF was 1 to 4% (for pH50) and 7 to 12% (for pH10). Our SSDs developed for the effect of decreasing ocean pH on calcifying marine species assemblages can also be used for comparison with other environmental stressors.
format Article in Journal/Newspaper
author Azevedo, L.
De Schryver, A.M.
Hendriks, A.J.
Huijbregts, M.A.J.
spellingShingle Azevedo, L.
De Schryver, A.M.
Hendriks, A.J.
Huijbregts, M.A.J.
Calcifying species sensitivity distributions for ocean acidification
author_facet Azevedo, L.
De Schryver, A.M.
Hendriks, A.J.
Huijbregts, M.A.J.
author_sort Azevedo, L.
title Calcifying species sensitivity distributions for ocean acidification
title_short Calcifying species sensitivity distributions for ocean acidification
title_full Calcifying species sensitivity distributions for ocean acidification
title_fullStr Calcifying species sensitivity distributions for ocean acidification
title_full_unstemmed Calcifying species sensitivity distributions for ocean acidification
title_sort calcifying species sensitivity distributions for ocean acidification
publisher American Chemical Society (ACS)
publishDate 2015
url http://pure.iiasa.ac.at/id/eprint/11515/
genre Ocean acidification
genre_facet Ocean acidification
op_relation Azevedo, L. <http://pure.iiasa.ac.at/view/iiasa/21.html>, De Schryver, A.M., Hendriks, A.J., & Huijbregts, M.A.J. (2015). Calcifying species sensitivity distributions for ocean acidification. Environmental Science & Technology 49 (3) 1495-1500. 10.1021/es505485m <https://doi.org/10.1021/es505485m>.
op_rights info:eu-repo/semantics/closedAccess
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