Green-house gas fluxes and soil microbial functional genes abundance in saturated and drained peatlands in South-West Iceland.

The drainage of peatlands followed by land use conversion significantly impacts on the fluxes of green-house gases (GHGs, i.e. CO, CH, and NO) to and from the atmosphere, driven by changes in soil properties and microbial communities. In this study, we compared saturated peatlands with drained ones used for sheep grazing or cultivated, which are common in South-West Iceland. These areas exhibit different degrees of soil saturation and nitrogen (N) content, reflecting the anthropic pressure gradient. We aimed at covering knowledge gaps about lack of estimates on NO fluxes and drainage, by assessing the emissions of GHGs, and the impact of land conversion on these emissions. Moreover, we investigated soil microbial community functional diversity, and its connection with processes contributing to GHGs emission. GHGs emissions differed between saturated and drained peatlands, with increased soil respiration rates (CO emissions) and N mineralization (NO), consistent with the trend of anthropogenic pressure. Drainage drastically reduced methane (CH) emissions but increased CO emissions, resulting in a higher global warming potential (GWP). Cultivation, involving occasional tillage and fertilization, further increased NO emissions, mediated by higher N availability and conditions favorable to nitrification. Functional genes mirrored the overall trend, showing a shift from prevalent methanogenic archaea (mcrA) in saturated peatlands to nitrifiers (amoA) in drained-cultivated areas. Environmental variables and nutrient content were critical factors affecting community composition in both environments, which overall affected the GHGs emissions and the relative contribution of the three gases.