Partitioning pathways of CO2 production in peatlands with stable carbon isotopes

Although methanogenic pathways generally produce equimolar amounts of carbon dioxide and methane, CO₂ concentrations are often reported to be higher than CH₄ concentrations in both field and laboratory incubation studies of peat decomposition. In field settings, higher pore water concentrations of CO₂ may result from the loss of methane by: (1) ebullition due to the low solubility of methane in pore water and (2) vascular-plant transport. Higher CO₂ concentrations may also be caused by: (1) production of additional CO₂ by high-molecular weight (HMW) organic matter (OM) fermentation and/or (2) respiration from non-methanogenic pathways. In this study of a peatland where advection and transverse dispersion were the dominant pore water solute transport mechanisms, an isotope-mass balance approach was used to determine the proportions of CO₂ formed from non-fractionating OM respiration and HMW fermentation relative to CO₂ production from methanogenesis. This approach also allowed us to estimate the loss of CH₄ from the belowground system. The pathways of CO₂ production varied with depth and surface vegetation type. In a Carex-dominated fen, methane production initially produced 40 % of the total CO₂ and then increased to 90–100 % with increasing depth. In a Sphagnum-dominated bog, methanogenesis resulted in 60 % of total CO₂ production which increased to 100 % at depth. Both bogs and fens showed 85–100 % of methane loss from pore waters. Our results indicate that the isotopic composition of dissolved CO₂ is a powerful indicator to allow partitioning of the processes affecting peat remineralization and methane production.