Abundant and diverse arsenic‐metabolizing microorganisms in peatlands treating arsenic‐contaminated mining wastewaters

• Published in: Environmental Microbiology
• Main Authors: Kujala, Katharina, Besold, Johannes, Mikkonen, Anu, Tiirola, Marja, Planer‐Friedrich, Britta
• Other Authors: Biotieteiden ja Ympäristön Tutkimuksen Toimikunta, Deutsche Forschungsgemeinschaft, FP7 Ideas: European Research Council
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2020
• Subjects: Northern Finland
• Online Access: http://dx.doi.org/10.1111/1462-2920.14922; https://onlinelibrary.wiley.com/doi/pdf/10.1111/1462-2920.14922; https://onlinelibrary.wiley.com/doi/full-xml/10.1111/1462-2920.14922

Summary Mining operations produce large quantities of wastewater. At a mine site in Northern Finland, two natural peatlands are used for the treatment of mining‐influenced waters with high concentrations of sulphate and potentially toxic arsenic (As). In the present study, As removal and the involved microbial processes in those treatment peatlands (TPs) were assessed. Arsenic‐metabolizing microorganisms were abundant in peat soil from both TPs (up to 10 8 cells g dw −1 ), with arsenate respirers being about 100 times more abundant than arsenite oxidizers. In uninhibited microcosm incubations, supplemented arsenite was oxidized under oxic conditions and supplemented arsenate was reduced under anoxic conditions, while little to no oxidation/reduction was observed in NaN 3 ‐inhibited microcosms, indicating high As‐turnover potential of peat microbes. Formation of thioarsenates was observed in anoxic microcosms. Sequencing of the functional genemarkers aioA (arsenite oxidizers), arrA (arsenate respirers) and arsC (detoxifying arsenate reducers) demonstrated high diversity of the As‐metabolizing microbial community. The microbial community composition differed between the two TPs, which may have affected As removal efficiencies. In the present situation, arsenate reduction is likely the dominant net process and contributes substantially to As removal. Changes in TP usage (e.g. mine closure) with lowered water tables and heightened oxygen availability in peat might lead to re‐oxidation and re‐mobilization of bound arsenite.