Sensitivities of extant animal taxa to ocean acidification
Anthropogenic CO 2 emitted to the atmosphere is absorbed by the oceans, causing a progressive increase in ocean inorganic carbon concentrations and resulting in decreased water pH and calcium carbonate saturation. This phenomenon, called ocean acidification, is in addition to the warming effects of...
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Published in: | Nature climate change Vol. 3; no. 11; pp. 995 - 1001 |
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Main Authors: | , |
Format: | Journal Article |
Language: | English |
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Nature Publishing Group UK
01-11-2013
Nature Publishing Group |
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Abstract | Anthropogenic CO
2
emitted to the atmosphere is absorbed by the oceans, causing a progressive increase in ocean inorganic carbon concentrations and resulting in decreased water pH and calcium carbonate saturation. This phenomenon, called ocean acidification, is in addition to the warming effects of CO
2
emissions. Ocean acidification has been reported to affect ocean biota, but the severity of this threat to ocean ecosystems (and humans depending on these ecosystems) is poorly understood. Here we evaluate the scale of this threat in the context of widely used representative concentration pathways (RCPs) by analysing the sensitivities of five animal taxa (corals, echinoderms, molluscs, crustaceans and fishes) to a wide range of CO
2
concentrations. Corals, echinoderms and molluscs are more sensitive to RCP8.5 (936 ppm in 2100) than are crustaceans. Larval fishes may be even more sensitive than the lower invertebrates, but taxon sensitivity on evolutionary timescales remains obscure. The variety of responses within and between taxa, together with observations in mesocosms and palaeo-analogues, suggest that ocean acidification is a driver for substantial change in ocean ecosystems this century, potentially leading to long-term shifts in species composition.
The severity of the ecological threat posed by ocean acidification remains poorly understood. Now analysis of the sensitivities of five animal groups to a wide range of CO
2
concentrations finds a variety of responses within and between taxa, indicating that acidification will drive substantial changes in ocean ecosystems this century. |
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AbstractList | Anthropogenic CO sub(2) emitted to the atmosphere is absorbed by the oceans, causing a progressive increase in ocean inorganic carbon concentrations and resulting in decreased water pH and calcium carbonate saturation. This phenomenon, called ocean acidification, is in addition to the warming effects of CO sub(2) emissions. Ocean acidification has been reported to affect ocean biota, but the severity of this threat to ocean ecosystems (and humans depending on these ecosystems) is poorly understood. Here we evaluate the scale of this threat in the context of widely used representative concentration pathways (RCPs) by analysing the sensitivities of five animal taxa (corals, echinoderms, molluscs, crustaceans and fishes) to a wide range of CO sub(2) concentrations. Corals, echinoderms and molluscs are more sensitive to RCP8.5 (936 ppm in 2100) than are crustaceans. Larval fishes may be even more sensitive than the lower invertebrates, but taxon sensitivity on evolutionary timescales remains obscure. The variety of responses within and between taxa, together with observations in mesocosms and palaeo-analogues, suggest that ocean acidification is a driver for substantial change in ocean ecosystems this century, potentially leading to long-term shifts in species composition. Anthropogenic CO 2 emitted to the atmosphere is absorbed by the oceans, causing a progressive increase in ocean inorganic carbon concentrations and resulting in decreased water pH and calcium carbonate saturation. This phenomenon, called ocean acidification, is in addition to the warming effects of CO 2 emissions. Ocean acidification has been reported to affect ocean biota, but the severity of this threat to ocean ecosystems (and humans depending on these ecosystems) is poorly understood. Here we evaluate the scale of this threat in the context of widely used representative concentration pathways (RCPs) by analysing the sensitivities of five animal taxa (corals, echinoderms, molluscs, crustaceans and fishes) to a wide range of CO 2 concentrations. Corals, echinoderms and molluscs are more sensitive to RCP8.5 (936 ppm in 2100) than are crustaceans. Larval fishes may be even more sensitive than the lower invertebrates, but taxon sensitivity on evolutionary timescales remains obscure. The variety of responses within and between taxa, together with observations in mesocosms and palaeo-analogues, suggest that ocean acidification is a driver for substantial change in ocean ecosystems this century, potentially leading to long-term shifts in species composition. The severity of the ecological threat posed by ocean acidification remains poorly understood. Now analysis of the sensitivities of five animal groups to a wide range of CO 2 concentrations finds a variety of responses within and between taxa, indicating that acidification will drive substantial changes in ocean ecosystems this century. Anthropogenic CO2 emitted to the atmosphere is absorbed by the oceans, causing a progressive increase in ocean inorganic carbon concentrations and resulting in decreased water pH and calcium carbonate saturation. This phenomenon, called ocean acidification, is in addition to the warming effects of CO2 emissions. Ocean acidification has been reported to affect ocean biota, but the severity of this threat to ocean ecosystems (and humans depending on these ecosystems) is poorly understood. Here we evaluate the scale of this threat in the context of widely used representative concentration pathways (RCPs) by analysing the sensitivities of five animal taxa (corals, echinoderms, molluscs, crustaceans and fishes) to a wide range of CO2 concentrations. Corals, echinoderms and molluscs are more sensitive to RCP8.5 (936 ppm in 2100) than are crustaceans. Larval fishes may be even more sensitive than the lower invertebrates, but taxon sensitivity on evolutionary timescales remains obscure. The variety of responses within and between taxa, together with observations in mesocosms and palaeo-analogues, suggest that ocean acidification is a driver for substantial change in ocean ecosystems this century, potentially leading to long-term shifts in species composition. |
Author | Wittmann, Astrid C. Pörtner, Hans-O. |
Author_xml | – sequence: 1 givenname: Astrid C. surname: Wittmann fullname: Wittmann, Astrid C. email: Astrid.Wittmann@awi.de organization: Integrative Ecophysiology, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung – sequence: 2 givenname: Hans-O. orcidid: 0000-0001-6535-6575 surname: Pörtner fullname: Pörtner, Hans-O. organization: Integrative Ecophysiology, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung |
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emitted to the atmosphere is absorbed by the oceans, causing a progressive increase in ocean inorganic carbon concentrations and resulting... Anthropogenic CO2 emitted to the atmosphere is absorbed by the oceans, causing a progressive increase in ocean inorganic carbon concentrations and resulting in... Anthropogenic CO sub(2) emitted to the atmosphere is absorbed by the oceans, causing a progressive increase in ocean inorganic carbon concentrations and... |
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SubjectTerms | 631/158/2455 Acidification Animal, plant and microbial ecology Anthropogenic factors Applied ecology Biological and medical sciences Biota Calcium carbonate Carbon dioxide emissions Climate Change Climate Change/Climate Change Impacts Conservation, protection and management of environment and wildlife Crustaceans Ecotoxicology, biological effects of pollution Environment Environmental degradation: ecosystems survey and restoration Environmental Law/Policy/Ecojustice Fundamental and applied biological sciences. Psychology Inorganic carbon Marine Marine and brackish environment Marine ecosystems Mollusca Mollusks Ocean acidification Oceans Shellfish Species composition Taxa |
Title | Sensitivities of extant animal taxa to ocean acidification |
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