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      The future of the northeast Atlantic benthic flora in a high CO2world

          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Abstract

          Seaweed and seagrass communities in the northeast Atlantic have been profoundly impacted by humans, and the rate of change is accelerating rapidly due to runaway CO2 emissions and mounting pressures on coastlines associated with human population growth and increased consumption of finite resources. Here, we predict how rapid warming and acidification are likely to affect benthic flora and coastal ecosystems of the northeast Atlantic in this century, based on global evidence from the literature as interpreted by the collective knowledge of the authorship. We predict that warming will kill off kelp forests in the south and that ocean acidification will remove maerl habitat in the north. Seagrasses will proliferate, and associated epiphytes switch from calcified algae to diatoms and filamentous species. Invasive species will thrive in niches liberated by loss of native species and spread via exponential development of artificial marine structures. Combined impacts of seawater warming, ocean acidification, and increased storminess may replace structurally diverse seaweed canopies, with associated calcified and noncalcified flora, with simple habitats dominated by noncalcified, turf-forming seaweeds.

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          Most cited references185

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          Is Open Access

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

          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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            Evidence for upwelling of corrosive "acidified" water onto the continental shelf.

            The absorption of atmospheric carbon dioxide (CO2) into the ocean lowers the pH of the waters. This so-called ocean acidification could have important consequences for marine ecosystems. To better understand the extent of this ocean acidification in coastal waters, we conducted hydrographic surveys along the continental shelf of western North America from central Canada to northern Mexico. We observed seawater that is undersaturated with respect to aragonite upwelling onto large portions of the continental shelf, reaching depths of approximately 40 to 120 meters along most transect lines and all the way to the surface on one transect off northern California. Although seasonal upwelling of the undersaturated waters onto the shelf is a natural phenomenon in this region, the ocean uptake of anthropogenic CO2 has increased the areal extent of the affected area.
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              Volcanic carbon dioxide vents show ecosystem effects of ocean acidification.

              The atmospheric partial pressure of carbon dioxide (p(CO(2))) will almost certainly be double that of pre-industrial levels by 2100 and will be considerably higher than at any time during the past few million years. The oceans are a principal sink for anthropogenic CO(2) where it is estimated to have caused a 30% increase in the concentration of H(+) in ocean surface waters since the early 1900s and may lead to a drop in seawater pH of up to 0.5 units by 2100 (refs 2, 3). Our understanding of how increased ocean acidity may affect marine ecosystems is at present very limited as almost all studies have been in vitro, short-term, rapid perturbation experiments on isolated elements of the ecosystem. Here we show the effects of acidification on benthic ecosystems at shallow coastal sites where volcanic CO(2) vents lower the pH of the water column. Along gradients of normal pH (8.1-8.2) to lowered pH (mean 7.8-7.9, minimum 7.4-7.5), typical rocky shore communities with abundant calcareous organisms shifted to communities lacking scleractinian corals with significant reductions in sea urchin and coralline algal abundance. To our knowledge, this is the first ecosystem-scale validation of predictions that these important groups of organisms are susceptible to elevated amounts of p(CO(2)). Sea-grass production was highest in an area at mean pH 7.6 (1,827 (mu)atm p(CO(2))) where coralline algal biomass was significantly reduced and gastropod shells were dissolving due to periods of carbonate sub-saturation. The species populating the vent sites comprise a suite of organisms that are resilient to naturally high concentrations of p(CO(2)) and indicate that ocean acidification may benefit highly invasive non-native algal species. Our results provide the first in situ insights into how shallow water marine communities might change when susceptible organisms are removed owing to ocean acidification.
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                Author and article information

                Journal
                Ecology and Evolution
                Ecol Evol
                Wiley
                20457758
                July 2014
                July 2014
                June 18 2014
                : 4
                : 13
                : 2787-2798
                Affiliations
                [1 ]Department of Life Sciences; The Natural History Museum; Cromwell Road London SW7 5BD UK
                [2 ]School of Earth and Ocean Sciences; Cardiff University; Main Building Park Place Cardiff CF10 3YE UK
                [3 ]Marine Biological Association of the UK; Citadel Hill Plymouth PL1 2PB UK
                [4 ]Ocean and Earth Science; National Oceanography Centre; University of Southampton; Waterfront Campus European Way Southampton SO14 3ZH UK
                [5 ]School of Geographical and Earth Sciences; University of Glasgow; Glasgow G12 8QQ UK
                [6 ]Marine Plant Ecology Research Group (ALGAE); Centre of Marine Sciences (CCMAR); University of Algarve; Campus of Gambelas Faro 8005-139 Portugal
                [7 ]School of Biological Sciences; University of Essex; Colchester CO4 3SQ UK
                [8 ]Institute of Zoology; Zoological Society of London; Regent's Park London NW1 4RY UK
                [9 ]Department of Zoology; The University of British Columbia; #4200-6270 University Blvd. Vancouver British Columbia V6T 1Z4 Canada
                [10 ]DiSTAV - University of Genoa; C.so Europa 26 Genoa 16132 Italy
                [11 ]Department of Earth and Environmental Sciences; University of St Andrews; St Andrews Fife KY16 9AL UK
                [12 ]Scottish Oceans Institute; University of St Andrews; St Andrews Fife KY16 8LB UK
                [13 ]Scottish Marine Institute; Oban Argyll PA37 1QA UK
                [14 ]Institute of Evolutionary Biology; University of Edinburgh; The King's Building West Mains Road Edinburgh EH9 3JT UK
                [15 ]Institute of Biology, Environmental and Rural Sciences; Aberystwyth University; Aberystwyth UK
                [16 ]Marine Biology and Ecology Research Centre; School of Marine Sciences and Engineering; Plymouth University; PL4 8AA UK
                [17 ]CNRS; UMR; 7144, Station Biologique de Roscoff Place Georges Teissier Roscoff Cedex 29688 France
                [18 ]UPMC Univ. Paris 6; UMR 7144; Station Biologique de Roscoff Place Georges Teissier Roscoff Cedex 29688 France
                [19 ]Plymouth Marine Laboratory; Prospect Place The Hoe Plymouth PL1 3DH UK
                [20 ]School of Earth Sciences; University of Bristol; Wills Memorial Building Queen's Road Bristol BS8 1RJ UK
                [21 ]Division of Plant Science; University of Dundee at the James Hutton Institute; Invergowrie Dundee DD2 5DA UK
                [22 ]Plant Functional Biology and Climate Change Cluster; University of Technology Sydney; Ultimo NSW 2007 Australia
                [23 ]Leibniz-Zentrum für Marine Tropenökologie; Fahrenheitstraße 6 Bremen D-28359 Germany
                Article
                10.1002/ece3.1105
                60ec3ccd-aa31-4ca3-9b61-7afc5eacf4c1
                © 2014

                http://doi.wiley.com/10.1002/tdm_license_1.1

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