2019
DOI: 10.1016/j.cej.2018.11.168
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Bioadsorption and microbe-mediated reduction of Sb(V) by a marine bacterium in the presence of sulfite/thiosulfate and the mechanism study

Abstract: Microbe-Sb interactions remain poorly understood and the molecular mechanism of microbe-mediated Sb(V) reduction remains unclear. In the present study, we investigated the process and mechanism of Sb(V) bioreduction by Shewanella sp. CNZ-1, which was isolated from the sediment of the Bohai Strait, in the absence or presence of sulfate/sulfite/thiosulfate. Results demonstrate that Sb(V) could be reduced to Sb(III) (including Sb 2 O 3 and Sb(III)(aq) etc.) by CNZ-1 cells. Kinetic studies are carried out using th… Show more

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Cited by 36 publications
(9 citation statements)
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“…The concentrations of Sb species and the dissolved sulfide were analyzed as described in our previous study [22]. The products of photo-catalytic reaction were analyzed using mass spectrum fitted with Sapphire C18 column (4.6 mm × 200 mm).…”
Section: Methodsmentioning
confidence: 99%
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“…The concentrations of Sb species and the dissolved sulfide were analyzed as described in our previous study [22]. The products of photo-catalytic reaction were analyzed using mass spectrum fitted with Sapphire C18 column (4.6 mm × 200 mm).…”
Section: Methodsmentioning
confidence: 99%
“…Compared to the detailed data on microbial reduction of S species, however, the knowledge of microbial Sb(V) reduction is much limited [27]. To the best of our knowledge, there are only three reported pure culture bacteria that capable of reducing Sb(V) to Sb(III) [20][21][22]. Recently, more and more studies have focused on the reduction of high valence metal ions with marine microorganisms, due to their strong adaptability to bad environment as they get exposure to such unfavorable conditions naturally [28].…”
Section: The Directional Selection Of Bacterial Resources For Sb 2 S mentioning
confidence: 99%
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“…Sb(V)-reducing bacteria and archaea have been identified in, or isolated from, soils and sediments from a wide range of aquatic and terrestrial environments (Abin and Hollibaugh 2014;Kulp et al, 2014;Nguyen and Lee 2014;Lai et al 2016Lai et al , 2018Nguyen et al, 2018;Wang et al, 2018;Zhang and Hu 2019), suggesting that direct (enzymatic) microbial reduction of Sb(V) may be a significant component of Sb biogeochemical cycling, particularly in environments with low S. Our results suggest that in natural and engineered environments with sufficient S to support active S redox cycling, Sb(V) reduction may be driven primarily by a coupled biotic-abiotic process wherein biogenic sulfide species are the primary reductants, which is consistent with similar observations from field and laboratory studies (Wang et al, 2013;Couture et al, 2015;Zhang et al, 2016;Liang et al, 2018). Moreover, our results also suggest that the presence of Fe(III) oxides in sulfidogenic environments can impact the distribution of Sb(III) species (e.g., sorbed Sb(III) versus Sb 2 S 3 precipitation), which has implications for the fate and transport of Sb.…”
Section: Implications For Sb Biogeochemistrymentioning
confidence: 99%
“…In the majority of these species, oxidation of Sb(III) to Sb(V) is linked to an enzymatic process for detoxification; however, at least two species have been shown to link Sb(III) oxidation to chemoautotrophic growth (Lialikova 1974;Terry et al, 2015). Several bacteria capable of using Sb(V) as a terminal electron acceptor for anaerobic respiration have been identified in both pure culture or as members of enriched microbial consortia (Nguyen and Lee 2014;Lai et al, 2016;Abin and Hollibaugh 2017;Nguyen et al 2018Nguyen et al , 2019Zhu et al, 2018;Zhang and Hu 2019;Yang et al, 2020), as well as an archaeon that can use Sb(V) as an electron acceptor for anaerobic methane oxidation (Lai et al, 2018). In addition to direct microbial redox transformations of Sb(III) and Sb(V), microbial processes can indirectly impact Sb speciation/mobility by altering the geochemical conditions of their environment, particularly microbes involved in the biogeochemical cycling of Fe and S. For example, reductive dissolution of Fe(III) oxides by dissimilatory Fe(III)-reducing bacteria (DIRB) could lead to release of sorbed Sb(V) and potential reduction to Sb(III) by Fe(II)-bearing secondary minerals such as magnetite or incorporation of Sb(V) into more crystalline secondary Fe(III) oxides (Burton et al, 2019).…”
Section: Introductionmentioning
confidence: 99%