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      Impacts of ocean acidification on marine organisms: quantifying sensitivities and interaction with warming

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          Abstract

          Ocean acidification represents a threat to marine species worldwide, and forecasting the ecological impacts of acidification is a high priority for science, management, and policy. As research on the topic expands at an exponential rate, a comprehensive understanding of the variability in organisms' responses and corresponding levels of certainty is necessary to forecast the ecological effects. Here, we perform the most comprehensive meta-analysis to date by synthesizing the results of 228 studies examining biological responses to ocean acidification. The results reveal decreased survival, calcification, growth, development and abundance in response to acidification when the broad range of marine organisms is pooled together. However, the magnitude of these responses varies among taxonomic groups, suggesting there is some predictable trait-based variation in sensitivity, despite the investigation of approximately 100 new species in recent research. The results also reveal an enhanced sensitivity of mollusk larvae, but suggest that an enhanced sensitivity of early life history stages is not universal across all taxonomic groups. In addition, the variability in species' responses is enhanced when they are exposed to acidification in multi-species assemblages, suggesting that it is important to consider indirect effects and exercise caution when forecasting abundance patterns from single-species laboratory experiments. Furthermore, the results suggest that other factors, such as nutritional status or source population, could cause substantial variation in organisms' responses. Last, the results highlight a trend towards enhanced sensitivity to acidification when taxa are concurrently exposed to elevated seawater temperature.

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          Meta-analysis reveals negative yet variable effects of ocean acidification on marine organisms.

          Ocean acidification is a pervasive stressor that could affect many marine organisms and cause profound ecological shifts. A variety of biological responses to ocean acidification have been measured across a range of taxa, but this information exists as case studies and has not been synthesized into meaningful comparisons amongst response variables and functional groups. We used meta-analytic techniques to explore the biological responses to ocean acidification, and found negative effects on survival, calcification, growth and reproduction. However, there was significant variation in the sensitivity of marine organisms. Calcifying organisms generally exhibited larger negative responses than non-calcifying organisms across numerous response variables, with the exception of crustaceans, which calcify but were not negatively affected. Calcification responses varied significantly amongst organisms using different mineral forms of calcium carbonate. Organisms using one of the more soluble forms of calcium carbonate (high-magnesium calcite) can be more resilient to ocean acidification than less soluble forms (calcite and aragonite). Additionally, there was variation in the sensitivities of different developmental stages, but this variation was dependent on the taxonomic group. Our analyses suggest that the biological effects of ocean acidification are generally large and negative, but the variation in sensitivity amongst organisms has important implications for ecosystem responses. © 2010 Blackwell Publishing Ltd/CNRS.
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            THE META-ANALYSIS OF RESPONSE RATIOS IN EXPERIMENTAL ECOLOGY

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              Ocean acidification causes bleaching and productivity loss in coral reef builders.

              Ocean acidification represents a key threat to coral reefs by reducing the calcification rate of framework builders. In addition, acidification is likely to affect the relationship between corals and their symbiotic dinoflagellates and the productivity of this association. However, little is known about how acidification impacts on the physiology of reef builders and how acidification interacts with warming. Here, we report on an 8-week study that compared bleaching, productivity, and calcification responses of crustose coralline algae (CCA) and branching (Acropora) and massive (Porites) coral species in response to acidification and warming. Using a 30-tank experimental system, we manipulated CO(2) levels to simulate doubling and three- to fourfold increases [Intergovernmental Panel on Climate Change (IPCC) projection categories IV and VI] relative to present-day levels under cool and warm scenarios. Results indicated that high CO(2) is a bleaching agent for corals and CCA under high irradiance, acting synergistically with warming to lower thermal bleaching thresholds. We propose that CO(2) induces bleaching via its impact on photoprotective mechanisms of the photosystems. Overall, acidification impacted more strongly on bleaching and productivity than on calcification. Interestingly, the intermediate, warm CO(2) scenario led to a 30% increase in productivity in Acropora, whereas high CO(2) lead to zero productivity in both corals. CCA were most sensitive to acidification, with high CO(2) leading to negative productivity and high rates of net dissolution. Our findings suggest that sensitive reef-building species such as CCA may be pushed beyond their thresholds for growth and survival within the next few decades whereas corals will show delayed and mixed responses.
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                Author and article information

                Journal
                Glob Chang Biol
                Glob Chang Biol
                gcb
                Global Change Biology
                Blackwell Publishing Ltd
                1354-1013
                1365-2486
                June 2013
                03 April 2013
                : 19
                : 6
                : 1884-1896
                Affiliations
                [* ]Bodega Bay Laboratory, University of California 2099 Westside Rd, Bodega Bay, CA, 94923, USA
                []University of British Columbia Vancouver, BC, Canada, V6T1Z4
                []Puget Sound Restoration Fund 590 Madison Ave N, Bainbridge Island, WA, 98110, USA
                [§ ]Global Change department, IMEDEA (CSIC-UIB), Instituto Mediterráneo de Estudios Avanzados C/Miquel Marqués 21, Esporles (Mallorca), 07190, Spain
                []Laboratorio de Ecologia y Cambio Climatico, Facultad de Ciencias Universidad Santo Tomas C/Ejercito, 146, Santiago de Chile
                []The UWA Oceans Institute and School of Plant Biology, University of Western Australia 35 Stirling Highway, Crawley, 6009, Australia
                [** ]Laboratoire d'Océanographie de Villefranche-sur-Mer, CNRS-INSU BP 28, Villefranche-sur-Mer Cedex, 06234, France
                [†† ]Université Pierre et Marie Curie-Paris 6 Observatoire Océanologique de Villefranche, Villefranche-sur-Mer Cedex, 06230, France
                Author notes
                Kristy J. Kroeker, tel. + (707) 875-1961, fax + (707) 875-2211, e-mail: kjkroeker@ 123456ucdavis.edu
                Article
                10.1111/gcb.12179
                3664023
                23505245
                df1ee856-28a6-45f4-a0bd-fc1663e261a0
                Copyright © 2013 Blackwell Publishing Ltd

                Re-use of this article is permitted in accordance with the Creative Commons Deed, Attribution 2.5, which does not permit commercial exploitation.

                History
                : 14 October 2012
                : 07 January 2013
                : 07 February 2013
                Categories
                Primary Research Articles

                calcification,carbonate chemistry,climate change,cumulative effects,ph

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