“…Moreover, 37 putative keystone taxa have higher average relative abundance (ranging from 0.01 to 0.38%) in the reducing high-As groundwater samples, namely, Pseudomonas (number of putative keystone taxa, 8), Sphingomonas (5), Rheinheimera (4), Vogesella (3), Acidovorax (2), Sphingopyxis (1), Novosphingobium (1), Erythrobacter (1), Sphingobium (1), Bacteriovorax (1), and unclassified genera from Planctomycetes (3), Sphingomonadales (1), Alphaproteobacteria (1), Sphingomonadales (1), Rhodobacteraceae (1), Nitrospirae (1), Micrococcaceae (1), and Caulobacterales (1) (Figure c). Members of the genera Pseudomonas, Sphingomonas , Enhydrobacter , and the family Rhodobacteraceae have been found to participate in ammonium oxidation, Fe(III) reduction, and/or As-related metabolism (As tolerance, As methylation, As(V) reduction, and As(III) oxidation). − Genera from the Planctomycetes are widely reported to be capable of anaerobic ammonium oxidation . Therefore, these putative keystone taxa may critically contribute to and/or respond to the groundwater As enrichment.…”