“…Diel O 2 fluctuations have been observed within aquatic systems, including freshwater wetlands, with near anoxic levels occurring at night and elevated O 2 concentrations occurring during daytime hours (Cornell & Klarer, 2008; Reeder, 2011; Maynard et al, 2012). In aquatic ecosystems other than wetlands (such as oceans and salt marshes), microbial community activity and structure can respond to short-term daily changes in environmental conditions (Ghiglione et al, 2007; Ottesen et al, 2014; Andrade et al, 2015; Morris et al, 2016; Kearns et al, 2017). As a consequence, geochemical processes can respond daily to diel environmental fluxes (Jørgensen et al, 1979; Laursen & Seitzinger, 2004; Harrison et al, 2005), as many geochemical transformations are driven by microbial communities that are sensitive to shifting environmental variables such as O 2 , pH, temperature, and light levels.…”