“…This N removal process, which oxidizes ammonium (NH 4 + ) via reducing nitrite (NO 2 ‐ ) to form N 2 under anaerobic environments [ Mulder et al ., ], is known to be mediated by chemolithoautotrophic bacteria belonging to the phylum Planctomycetes [ Strous et al ., ; Kartal et al ., ; Jetten et al ., ]. To date, five anammox bacterial genera have been recognized, which include Candidatus Kuenenia , Candidatus Brocadia , Candidatus Scalindua , Candidatus Anammoxoglobus , and Candidatus Jettenia [ Strous et al ., ; Schmid et al ., ; Kartal et al ., ; Quan et al ., ], and all these genera have been reported to exist in estuarine and coastal habitats [ Dale et al ., ; Fu et al ., ]. Although the process of anammox is an important pathway for removing N from estuarine and coastal environments [ Dale et al ., ; Hou et al ., ; Naeher et al ., ], little is known about how community dynamics and activity of anammox bacteria shift along the estuarine salinity gradient.…”