Biogenic hydroxysulfate green rust, a potential electron acceptor for SRB activity

Abstract

Microbiological reduction of a biogenic sulfated green rust ( GR 2 ( SO 4 2 - ) ) , was examined using a sulfate reducing bacterium ( Desulfovibrio alaskensis). Experiments investigated whether GR2 ( SO 4 2 - ) could serve as a sulfate source for D. alaskensis anaerobic respiration by analyzing mineral transformation. Batch experiments were conducted using lactate as the electron donor and biogenic GR 2 ( SO 4 2 - ) as the electron acceptor, at circumneutral pH in unbuffered medium. GR2 ( SO 4 2 - ) transformation was monitored with time by X-ray diffraction (XRD), Transmission Mössbauer Spectroscopy (TMS), Diffuse Reflectance Infrared Fourier Transform Spectroscopy (DRIFTS), Transmission Electron Microscopy (TEM) and X-ray Photoelectron Spectroscopy (XPS). The reduction of sulfate anions and the formation of iron sulfur mineral were clearly identified by XPS analyses. TMS showed the formation of additional mineral as green rust (GR) and vivianite. XRD analyses discriminated the type of the newly formed GR as GR1. The formed GR1 was GR 1 ( CO 3 2 - ) as indicated by DRIFTS analysis. Thus, the results presented in this study indicate that D. alaskensis cells were able to use GR 2 ( SO 4 2 - ) as an electron acceptor. GR 1 ( CO 3 2 - ) , vivianite and an iron sulfur compound were formed as a result of GR 2 ( SO 4 2 - ) reduction by D. alaskensis. Hence, in environments where geochemical conditions promote biogenic GR 2 ( SO 4 2 - ) formation, this mineral could stimulate the anaerobic respiration of sulfate reducing bacteria.