Antimony
(Sb) mobilization is widely explored with dissimilatory
metal-reducing bacteria (DMRB) via microbial iron(III)-reduction.
Here, our study found a previously unknown pathway whereby DMRB release
adsorbed antimonite (SbIII-O) from goethite via elemental
sulfur (S0) respiratory reduction under mild alkaline conditions.
We incubated SbIII-O-loaded goethite with Shewanella oneidensis MR-1 in the presence of S0 at pH 8.5. The incubation results showed that MR-1 reduced
S0 instead of goethite, and biogenic sulfide induced the
formation of thioantimonite (SbIII-S). SbIII-S was then oxidized by S0 to mobile thioantimonate (SbV-S), resulting in over fourfold greater Sb release to water
compared with the abiotic control. SbIV-S was identified
as the intermediate during the oxidation process by Fourier transform
ion cyclotron resonance mass spectrometry and electron spin resonance
analysis. The existence of SbIV-S reveals that the oxidation
of SbIII-S to SbV-S follows a two-step consecutive
one-electron transfer from Sb to S atoms. SbV-S then links
with SbIII-S by sharing S atoms and inhibits SbIII-S polymerization and SbIII
2S3 precipitation
like a “capping agent”. This study clarifies the thiolation
and oxidation pathway of SbIII-O to SbV-S by
S0 respiration and expands the role of DMRB in the fate
of Sb.