Spatial Variation in Anaerobic Microbial Communities in Wetland Margin Soils

Climate change is predicted to increase the severity and frequency of precipitation and drought events, which may result in substantial temporal variation in the size of wetlands. Wetlands are the world's largest natural emitter of methane, a greenhouse gas that is 20 times more effective at trapping heat than carbon dioxide. Changes in the dynamics of wetland size may lead to changes in the extent and timing of inundation of soils in ephemeral margins, which is likely to influence microbes that rely on anoxic conditions. The impact on process rates may depend on the structure of the community of microbes present in the soil, however, the link between microbial structure and patterns in process rates in soils is not well understood. Our goal was to use molecular techniques to compare microorganism communities in two wetlands that differ in the extent and duration of inundation of marginal soils to assess how these communities may change with changes in climate, and the potential consequences for methane production. This will allow us to examine how community composition changes with soil conditions such as moisture content, frequency of drought and abundance of available carbon. The main focus of this project was to determine the presence or absence of acetoclastic (AC) and hydrogenotrophic (HT) methanogens. AC methanogens use acetate as their main substrate, while HT methanogens use Hydrogen and Carbon dioxide. The relative proportion of these pathways depends on soil conditions, such as competition with other anaerobic microbes and the amount of labile carbon, and spatial patterns in the presence of each can give insight into the soil conditions of a wetland site. We sampled soil from three different wetland ponds of varying permanence in the St Olaf Natural Lands in Northfield, Minnesota, and extracted DNA from these soil samples with a MoBio PowerSoil DNA Isolation Kit. With PCR and seven different primer sets, we tested the extracted DNA for the presence of four different methanogen taxa as well as denitrifying, iron reducing and sulfate reducing bacteria. We used the percentage of soil replicates that tested positive for a primer as an indicator of the population size of each microorganism at each site. The results of the presence/absence test suggested a relationship between soil moisture and abundance of methanogens. The sites with over 25% moisture content showed a higher percent presence than the soil sites with under 25% moisture content for all taxa except for sulfate reducing bacteria. The impact of soil moisture is likely due to negative effects of oxygen on methanogens. However, the presence of methanogens in drier soils shows that methanogens can still exist in a dormant state in aerobic environments. Methanogens may be ubiquitous but vary in population size and activity depending on soil conditions. With changes in wetland soil moisture in response to changes in precipitation patterns, the populations of methanogens may change, affecting the amount of methane production and ultimately the amount of heat trapped by the atmosphere.