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• W4226303977 endingPage "231" @default.
• W4226303977 startingPage "197" @default.
• W4226303977 abstract "This chapter discusses the influence of climate change on coastal wetland productivity, organic carbon burial, CO2 and CH4 production, and their emissions. We reviewed studies that were performed in atmosphere-controlled greenhouses or open-top chambers to quantify the role of climate change on mangrove and saltmarsh productivity, as well as in situ studies that used the eddy-covariance method or incubation chambers at the various interfaces to quantify CO2 and CH4 flux variability with temperature, precipitation, or tides. Coastal wetland productivity responses to the increases of temperature and of atmospheric CO2 concentrations will not be a simple increase but will most probably vary with the biogeographic settings and the position of the stand in the intertidal zone, both influencing pore-water salinity and nutrient inputs. The productivity of mangroves may respond more significantly to elevated CO2 than that of saltmarshes. Changes in rainfall pattern will not only have an influence on ecosystem gross productivity but also on ecosystem respiration, modifying subsequently the net carbon budget of coastal wetlands. The effect of tidal flooding will be species-specific and will depend on the prevalent climate and the position of the stand along the intertidal zone (optimum for growth or not). Eventually, enhanced cyclonic intensity may reduce the productivity of these ecosystems. Increased tidal flushing and pore-water seepage resulting from sea-level rise will limit carbon burial, while productivity and sedimentation rates will increase. However, the effect of sea-level rise in modifying soil moisture and the rate of electron acceptors renewal will be site-specific depending on climate, soil permeability, and position along the tidal zone. Sea-level rise results in more water-saturated soils, which will limit greenhouse gas (GHG) production and emission. However, rise in temperature will enhance organic carbon mineralization. Eventually, GHG diffusion also depends on the responses of the microphytobenthos, bioturbation, and aerial root density to climate change." @default.
• W4226303977 created "2022-05-05" @default.
• W4226303977 creator A5021088987 @default.
• W4226303977 creator A5048608638 @default.
• W4226303977 creator A5079106013 @default.
• W4226303977 creator A5085789188 @default.
• W4226303977 date "2022-01-01" @default.
• W4226303977 modified "2023-09-25" @default.
• W4226303977 title "Impact of climate change and related disturbances on CO2 and CH4 cycling in coastal wetlands" @default.
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