The Prairie Pothole Region (PPR) of North America encompasses nearly 750,000 km 2 of the Upper Great Plains that straddle the United States and Canada. This region is composed of a heavily glaciated landscape densely populated by depressional wetlands connected hydrologically by groundwater with little surface water connectivity. Thus, wetland surface area varies greatly with annual precipitation patterns (Liu & Schwartz, 2011). These wetlands also exhibit a salinity gradient ranging from <800 to >60,000 µS/cm that mirrors groundwater flow from higher elevation freshwater "recharge" (output only) wetlands to increasingly saline and sulfidic lower elevation "flow though" (input and output) and ultimately "discharge" (input only) water bodies (Mushet et al., 2015;Winter & Rosenberry, 1998). In contrast pothole surface waters are either saturated or super-saturated with respect to calcite and occupy a narrow pH range (8-9+) relative to lower alkalinity surface waters (Mushet et al., 2015).Prairie pothole wetlands provide significant ecosystem services ranging from important waterfowl habitats to pesticide attenuation and carbon sequestration (Euliss et al., 2006;Zeng et al., 2011Zeng et al., , 2012. However, landscape alterations caused by increased agricultural activity in the PPR (e.g., loss of wetlands, tilling of soils) may negatively impact these important ecosystem functions. For example, 90% of wetlands in the Des Moines Lobe of the Iowa PPR have been lost to anthropogenic activity, with a disproportionate loss of small upland wetlands and a resulting increased mean distance between wetlands (Van Meter & Basu, 2015). Others have observed accelerating rates of wetland loss in North and South Dakota with a higher proportion of central wetlands (i.e., those in the same region as the Cottonwood Lakes Study Area) being lost to row