“…In such systems, dense cyanoHABs can often be found throughout the water column. However, in the past several decades, cyanoHABs and associated impacts have been increasingly reported in low‐ and moderate‐nutrient lakes and reservoirs (Callieri et al, 2014; Carey et al, 2014; Reinl et al, 2021), including deep, thermally stratified systems in the United States (Sterner et al, 2020) and in New York State (NYS; Matthews et al, 2021; Smith et al, 2020; Vaughan et al, 2021). Several factors that may be important for cyanoHAB formation in low nutrient waters include: increases in water temperature (Carey et al, 2012; Paerl & Otten, 2013), alteration of thermal stratification patterns (Planas & Paquet, 2016; Stetler et al, 2021), the presence of dreissenid mussels (Raikow et al, 2004; Sarnelle et al, 2012), physiological adaptative advantages of cyanobacteria, such as buoyancy regulation to utilize light and available nutrients (Ibelings et al, 1991; Reynolds, 2006), uptake and storage of phosphorus (Carr & Whitton, 1982; Coleman, 1992; Whitton et al, 1991), and sequestration of reduced iron (Fe 2+ ; Pick, 2016; Reinl et al, 2021).…”