Activity and Diversity of Fe(III)-Reducing Bacteria in a 3000-Year-Old Acid Mine Drainage Site Analogue

Abstract

The diversity and activity of dissimilatory Fe(III)-reducing bacteria was investigated in acidic, ochre-precipitating springs on Mam Tor, East Midlands, UK. The springs at this acid rock drainage site are located below a 3000 year old landslip, where biooxidation of exposed pyrite-containing minerals has resulted in the production of metal-laden acidic waters. A diverse microbial community was found downstream in the sediments dominated by Fe(III) minerals, and included close relatives to known acidophilic (Acidimicrobium and Acidiphilium) and neutraphilic (Geobacter and Pelobacter) Fe(III)-reducing bacteria. Analysis by XRD and TEM confirmed the presence of both amorphous and well-defined Fe(III) mineral phases in the sediments including lepidocrocite, goethite and schwertmannite. Microcosm-based experiments demonstrated that the bioavailable Fe(III) was reduced under anaerobic conditions, concomitant with sulphate release. XRD analysis suggested that schwertmannite (an iron sulphate hydroxide) was utilized preferentially by the Fe(III)-reducing bacteria, leading to the release of sulphate. Although the microcosms contained sufficient concentrations of naturally occurring electron donor to sustain significant levels of Fe(III) reduction, this process was stimulated by the addition of glycerol and complex electron donors. Thus, the acidic Fe(III)-containing sediments contain a diversity of DIRBs that can be stimulated by the addition of electron donor as a first step in the reversal of acid rock and acid mine drainage contamination.