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Biogeochemical controls on CO2 and CH4 fluxes in peatlands: From intracellular symbionts to plant-environment interactions. Lamers, Leon1, 2, Smolders, Alfons2, Tomassen, Hilde2, Roelofs, Jan1, 2, 1 Environmental Biology, Institute for Wetland and Water Research, Radboud University Nijmegen, Nijmegen, the Netherlands2 Research Centre B-Ware, Nijmegen, the Netherlands ABSTRACT- The direction and rates of fluxes of CO2 and CH4 between peatlands (bogs, fens, marshes) and the atmosphere are determined by the rates of microbial and chemical production, CO2 fixation by biomass production, CH4 consumption, and gas ebullition or diffusion. The flux regulation even includes small-scale phenomena like the recently discovered intracellular methanotrophic symbionts providing C for photosynthesis in Sphagnum, and reducing CH4 losses to the atmosphere. A wide range of physicochemical variables including temperature, humidity, pO2 , peat structure, alkalinity, pH, SO42-, NH4+, NO3-, HPO42- strongly interfere with CO2 and CH4 biogeochemistry. This holds for both pristine peatlands and for those disturbed by desiccation, global warming, and pollution (S, N, P). Fluxes of CO2 and CH4 are also indirectly influenced by changes in vegetation composition as a result of the biogeochemical changes mentioned above. These changes may significantly change decomposition rates (peat quality), C sequestration (biomass production), and physical pathways for both gases (funnel effect). The present paper will bring together these biogeochemical and biological controls on the fluxes of CO2 and CH4 into a conceptual model, and attempt to indicate the implications found at this peat soil scale for our understanding at higher scales (up to remote sensing by satellites). Key words: carbon fluxes, carbon dioxide, methane, peatlands |
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