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      Effects of CO 2 enrichment on photosynthesis, growth, and nitrogen metabolism of the seagrass Zostera noltii

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          Abstract

          Seagrass ecosystems are expected to benefit from the global increase in CO 2 in the ocean because the photosynthetic rate of these plants may be C i-limited at the current CO 2 level. As well, it is expected that lower external pH will facilitate the nitrate uptake of seagrasses if nitrate is cotransported with H + across the membrane as in terrestrial plants. Here, we investigate the effects of CO 2 enrichment on both carbon and nitrogen metabolism of the seagrass Zostera noltii in a mesocosm experiment where plants were exposed for 5 months to two experimental CO 2 concentrations (360 and 700 ppm). Both the maximum photosynthetic rate (P m) and photosynthetic efficiency ( α) were higher (1.3- and 4.1-fold, respectively) in plants exposed to CO 2-enriched conditions. On the other hand, no significant effects of CO 2 enrichment on leaf growth rates were observed, probably due to nitrogen limitation as revealed by the low nitrogen content of leaves. The leaf ammonium uptake rate and glutamine synthetase activity were not significantly affected by increased CO 2 concentrations. On the other hand, the leaf nitrate uptake rate of plants exposed to CO 2-enriched conditions was fourfold lower than the uptake of plants exposed to current CO 2 level, suggesting that in the seagrass Z. noltii nitrate is not cotransported with H + as in terrestrial plants. In contrast, the activity of nitrate reductase was threefold higher in plant leaves grown at high-CO 2 concentrations. Our results suggest that the global effects of CO 2 on seagrass production may be spatially heterogeneous and depend on the specific nitrogen availability of each system. Under a CO 2 increase scenario, the natural levels of nutrients will probably become limiting for Z. noltii. This potential limitation becomes more relevant because the expected positive effect of CO 2 increase on nitrate uptake rate was not confirmed.

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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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            Mineral nutrition of higher plant

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              Ecosystem effects of ocean acidification in times of ocean warming: a physiologist’s view

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                Author and article information

                Journal
                Ecol Evol
                Ecol Evol
                ece3
                Ecology and Evolution
                Blackwell Publishing Ltd
                2045-7758
                2045-7758
                October 2012
                19 September 2012
                : 2
                : 10
                : 2625-2635
                Affiliations
                [1 ]Marine Plant Ecology Research Group, CCMAR – Centre of Marine Sciences, Universidade do Algarve Faro, Portugal
                [2 ]Botany Department, Stockholm University Stockholm, Sweden
                Author notes
                Ana Alexandre, Marine Plant Ecology Research Group, CCMAR – Centre of Marine Sciences, Universidade do Algarve, Gambelas, 8005-139 Faro, Portugal. Tel: +351 289 800900; Fax: +351 289 800069; E-mail: aalexandre@ 123456ualg.pt

                Funding Information Funded by Fundação para a Ciência e a Tecnologia (SFRH/BD/21487/2005), cofunded by POCI 2010 and FSE.

                Article
                10.1002/ece3.333
                3492787
                23145346
                f514d920-3fb8-42a4-872e-7ebc2cc7ee64
                © 2012 Published by 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
                : 22 May 2012
                : 19 June 2012
                : 22 June 2012
                Categories
                Original Research

                Evolutionary Biology
                growth,nitrate reductase,nitrogen uptake,photosynthesis,glutamine synthetase,co 2 enrichment,seagrasses

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