Nitrogen is an essential, often limiting, element for biological growth that can act as a pollutant if present at high concentrations. Excessive nitrogen in highly biologically available forms, especially nitrate (NO 3 − ), is common in urban ecosystems. Urban ecosystems tend to have higher NO 3 − burdens due to higher inputs from fertilizer application (Baker et al., 2001;Law et al., 2004), deposition from fossil fuel combustion (Bettez & Groffman, 2013;Hale et al., 2014), and treatment of sewage (Lauver & Baker, 2000). In addition, urban stormwater infrastructure quickly transports runoff to storm drains that can discharge into water bodies (Baker et al., 2001;Kaye et al., 2006). Whether this high NO 3 − burden causes eutrophication partially depends on the capacity of the aquatic ecosystem to attenuate NO 3 − inputs. Wetland ecosystems can be hotpots for NO 3 − attenuation due to the availability of water, organic matter, and variable oxygen zones (Ehrenfeld, 2000;Mitsch & Gosselink, 2015). These environmental conditions are conducive to NO 3 − attenuation through pathways such as denitrification and dissimilatory NO 3 − reduction to ammonium (NH 4 + ) (DNRA). Indeed, urban wetland ecosystems are thought to