Watershed export of excessive reactive nitrogen (N) is a major environmental concern globally, as eutrophication of coastal waters causes hypoxia, habitat degradation, and loss of biodiversity (Howarth, 2008;Schaefer et al., 2009). Functioning riparian zones that are hydrologically connected to streams and rivers help mitigate downstream N transport through N removal by numerous biogeochemical pathways (Vidon et al., 2010;Zhao et al., 2021). Complete denitrification is a particularly important removal pathway by which facultative anaerobic bacteria reduce nitrate and nitrite to N 2 gas, permanently removing N from reactive pools (Groffman et al., 1992;Hill, 2019;Lutz et al., 2020). Denitrification occurs in areas with available organic carbon (C), high concentrations of nitrate, and wet, low oxygen sediments (Zhao et al., 2021). These conditions are often present in riparian