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      Elevated ozone reduces photosynthetic carbon gain by accelerating leaf senescence of inbred and hybrid maize in a genotype-specific manner

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          Global warming and 21st century drying

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            Indirect radiative forcing of climate change through ozone effects on the land-carbon sink.

            The evolution of the Earth's climate over the twenty-first century depends on the rate at which anthropogenic carbon dioxide emissions are removed from the atmosphere by the ocean and land carbon cycles. Coupled climate-carbon cycle models suggest that global warming will act to limit the land-carbon sink, but these first generation models neglected the impacts of changing atmospheric chemistry. Emissions associated with fossil fuel and biomass burning have acted to approximately double the global mean tropospheric ozone concentration, and further increases are expected over the twenty-first century. Tropospheric ozone is known to damage plants, reducing plant primary productivity and crop yields, yet increasing atmospheric carbon dioxide concentrations are thought to stimulate plant primary productivity. Increased carbon dioxide and ozone levels can both lead to stomatal closure, which reduces the uptake of either gas, and in turn limits the damaging effect of ozone and the carbon dioxide fertilization of photosynthesis. Here we estimate the impact of projected changes in ozone levels on the land-carbon sink, using a global land carbon cycle model modified to include the effect of ozone deposition on photosynthesis and to account for interactions between ozone and carbon dioxide through stomatal closure. For a range of sensitivity parameters based on manipulative field experiments, we find a significant suppression of the global land-carbon sink as increases in ozone concentrations affect plant productivity. In consequence, more carbon dioxide accumulates in the atmosphere. We suggest that the resulting indirect radiative forcing by ozone effects on plants could contribute more to global warming than the direct radiative forcing due to tropospheric ozone increases.
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              Five ways to stay green.

              The relationship between carbon income and expenditure over the life of a leaf is described and related to the productivity benefits of altering the timing of senescence initiation. In genetic variants with delayed leaf senescence ('stay-greens') deconstruction of the photosynthetic apparatus during leaf senescence is partially or completely prevented. Although the staygreen phenotype is superficially similar in all species and genotypes, the genetic and physiological routes to the trait are diverse. In one type of stay-green, chlorophyll catabolism is disabled. Legumes and monocots with pigment breakdown lesions are discussed. Sorghum is presented as an example of another kind of stay-green in which perennial tendencies have been bred into a monocarpic annual crop species. Transgenic approaches are briefly discussed (enhanced endogenous cytokinins, reduced ethylene production or perception). An alternative route towards making a stay-green phenotype is through quantitative trait mapping and marker-assisted selection. Loci for greenness in pearl millet have been identified, some of which are associated with drought responses or flowering time. Finally the question of the limits on stay-green as a productivity-enhancing character is addressed.
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                Author and article information

                Journal
                Plant, Cell & Environment
                Plant Cell Environ
                Wiley
                01407791
                December 2017
                December 2017
                October 17 2017
                : 40
                : 12
                : 3088-3100
                Affiliations
                [1 ]Carl R. Woese Institute for Genomic Biology; University of Illinois at Urbana Champaign; Urbana IL 61801 USA
                [2 ]Department of Plant Biology; University of Illinois at Urbana Champaign; Urbana IL 61801 USA
                [3 ]Department of Crop Sciences; University of Illinois at Urbana Champaign; Urbana IL 61801 USA
                [4 ]Department of Molecular Genetics and Microbiology; University of Florida; Gainesville FL 32610 USA
                [5 ]Genetics Institute; University of Florida; Gainesville FL 32610 USA
                [6 ]Global Change and Photosynthesis Research Unit; USDA ARS; Urbana IL 61801 USA
                Article
                10.1111/pce.13075
                29044553
                b0581d64-ed8f-4b6a-abff-22e4b49e14ee
                © 2017

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

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