“…While some bacteria can perform complete oxidation of ammonia (Daims et al, 2015; van Kessel et al, 2015), this process is typically completed in two steps by chemolithoautotrophic microorganisms: ammonia‐oxidizing archaea (AOA) or bacteria (AOB) first oxidize NH 3 to nitrite (NO 2 − ), followed by the oxidation of NO 2 − to NO 3 − by nitrite‐oxidizing bacteria (NOB; e.g., Dworkin & Gutnick, 2012; Könneke et al, 2005). Nitrifiers present in freshwater habitats can include the AOA Nitrososphaerota (commonly known as Thaumarchaeota), AOB of the genera Nitrosomonas and Nitrosospira within the Nitrosomonadaceae, and NOB of the phylum Nitrospirota, genus Nitrobacter , and genus Nitrotoga (e.g., Alfreider et al, 2018; Boddicker & Mosier, 2018; Cabello‐Yeves et al, 2018, 2020; Hayden & Beman, 2014; Herber et al, 2019; Klotz et al, 2022; Lantz et al, 2021; Podowski et al, 2022; Ngugi et al, 2023). These lineages can represent large (>30%) proportions of lake and ocean prokaryotic communities (e.g., Francis et al, 2005; Karner et al, 2001; Ngugi et al, 2023), highlighting the importance of these organisms to both N and carbon cycles.…”