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      Thermal sensitivity of CO 2 and CH 4 emissions varies with streambed sediment properties

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          Abstract

          Globally, rivers and streams are important sources of carbon dioxide and methane, with small rivers contributing disproportionately relative to their size. Previous research on greenhouse gas (GHG) emissions from surface water lacks mechanistic understanding of contributions from streambed sediments. We hypothesise that streambeds, as known biogeochemical hotspots, significantly contribute to the production of GHGs. With global climate change, there is a pressing need to understand how increasing streambed temperatures will affect current and future GHG production. Current global estimates assume linear relationships between temperature and GHG emissions from surface water. Here we show non-linearity and threshold responses of streambed GHG production to warming. We reveal that temperature sensitivity varies with substrate (of variable grain size), organic matter (OM) content and geological origin. Our results confirm that streambeds, with their non-linear response to projected warming, are integral to estimating freshwater ecosystem contributions to current and future global GHG emissions.

          Abstract

          Rivers and streams are important sources of carbon dioxide and methane; however, the drivers of these streambed gas fluxes are poorly understood. Here, the authors show that temperature sensitivity of streambed greenhouse gas emissions varies with substrate, organic matter content and geological origin.

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          Biogeochemical Hot Spots and Hot Moments at the Interface of Terrestrial and Aquatic Ecosystems

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            Outgassing from Amazonian rivers and wetlands as a large tropical source of atmospheric CO2.

            Terrestrial ecosystems in the humid tropics play a potentially important but presently ambiguous role in the global carbon cycle. Whereas global estimates of atmospheric CO2 exchange indicate that the tropics are near equilibrium or are a source with respect to carbon, ground-based estimates indicate that the amount of carbon that is being absorbed by mature rainforests is similar to or greater than that being released by tropical deforestation (about 1.6 Gt C yr-1). Estimates of the magnitude of carbon sequestration are uncertain, however, depending on whether they are derived from measurements of gas fluxes above forests or of biomass accumulation in vegetation and soils. It is also possible that methodological errors may overestimate rates of carbon uptake or that other loss processes have yet to be identified. Here we demonstrate that outgassing (evasion) of CO2 from rivers and wetlands of the central Amazon basin constitutes an important carbon loss process, equal to 1.2 +/- 0.3 Mg C ha-1 yr-1. This carbon probably originates from organic matter transported from upland and flooded forests, which is then respired and outgassed downstream. Extrapolated across the entire basin, this flux-at 0.5 Gt C yr-1-is an order of magnitude greater than fluvial export of organic carbon to the ocean. From these findings, we suggest that the overall carbon budget of rainforests, summed across terrestrial and aquatic environments, appears closer to being in balance than would be inferred from studies of uplands alone.
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              Plumbing the Global Carbon Cycle: Integrating Inland Waters into the Terrestrial Carbon Budget

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                Author and article information

                Contributors
                sxc469@bham.ac.uk
                Journal
                Nat Commun
                Nat Commun
                Nature Communications
                Nature Publishing Group UK (London )
                2041-1723
                18 July 2018
                18 July 2018
                2018
                : 9
                : 2803
                Affiliations
                [1 ]ISNI 0000 0004 1936 7486, GRID grid.6572.6, School of Geography, Earth and Environmental Sciences, University of Birmingham, ; Edgbaston, Birmingham B15 2TT UK
                [2 ]ISNI 0000 0001 1956 5915, GRID grid.474329.f, British Geological Survey, Maclean Building, ; Wallingford, Oxfordshire OX10 8BB UK
                Author information
                http://orcid.org/0000-0003-1260-3151
                http://orcid.org/0000-0002-6015-1332
                http://orcid.org/0000-0003-1714-1240
                Article
                4756
                10.1038/s41467-018-04756-x
                6052154
                30022025
                867c31af-9eaf-4729-8de3-14bf96fc9d51
                © The Author(s) 2018

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 6 July 2017
                : 21 May 2018
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