Hypoosmolarity inhibits archaeal ammonia oxidation

Salinity strongly influences the physiology and distribution of nitrifying microorganisms, yet the effects of low salinity on them remain understudied. This study investigates the impact of hypoosmolarity on different groups of ammonia oxidizers in soil and lake environments, as well as in pure culture isolates. In soil microcosms amended with ammonium, at low salinity levels ([~]120 S/cm), comparable to values commonly found in pristine terrestrial and aquatic environments, the abundance of ammonia-oxidizing bacteria (AOB), dominated by Nitrosomonas oligotropha, significantly increased. In contrast, the growth of ammonia-oxidizing archaea (AOA), dominated by "Ca. Nitrosotenuis" of the Nitrosopumilaceae family, was stimulated by high salinity ([~]760 S/cm). In ammonium-fed lake microcosms, the abundance of AOB, dominated by N. oligotropha, significantly increased under both low ([~]170 S/cm) and high salinity ([~]850 S/cm) conditions. In the presence of allylthiourea, a bacterial nitrification inhibitor, AOA were sensitive to low salinity in both soil and lake microcosms. Consistently, pure culture studies revealed marked growth inhibition of AOA, especially members of Nitrosopumilaceae, under hypoosmolarity, unlike AOB and complete ammonia oxidizer (comammox) strains. Comparative genomic analyses with AOB and comammox, along with transcriptomic studies, suggested that the sensitivity of AOA to hypoosmolarity stress was possibly due to a lack of sophisticated osmoregulatory transport systems and their S-layer cell wall structure. Overall, this study highlights hypoosmolarity as a key factor shaping the ecological niches and distribution of ammonia oxidizers, as well as nitrification activities, in terrestrial and aquatic environments that are increasingly affected by intensified water cycles due to climate change.