Microbial and surface chemistry controls on reduction of synthetic Fe(III)oxide minerals by the dissimilatory iron-reducing bacterium Shewanella alga

Citation
Mm. Urrutia et al., Microbial and surface chemistry controls on reduction of synthetic Fe(III)oxide minerals by the dissimilatory iron-reducing bacterium Shewanella alga, GEOMICROB J, 15(4), 1998, pp. 269-291
Citations number
47
Categorie Soggetti
Environment/Ecology
Journal title
GEOMICROBIOLOGY JOURNAL
ISSN journal
01490451 → ACNP
Volume
15
Issue
4
Year of publication
1998
Pages
269 - 291
Database
ISI
SICI code
0149-0451(199810/12)15:4<269:MASCCO>2.0.ZU;2-O
Abstract
The role of Fe(ll) biosorption and the effect of medium components on the r are and long-term extent of Fe(lll) oxide reduction (FeRed) by a dissimilat ory Fe(lll)-reducing bacterium (Shewanella alga strain BrY) were examined i n batch culture experiments. introduction of fresh S. alga cells into month -old cultures in which Fe(III) reduction had ceased resulted in further red uction of synthetic amorphous Fe(lll) oxide, hematite, and two forms of goe thite (Gt). Fresh S. alga cells were also able to reduce a substantial amou nt of synthetic Ct that had been partly or completely saturated with sorbed Fe(ll). Cells that had been precoated with Fe(ll) showed a reduced rate an d capacity for FeRed These results indicated that biosorption of Fe(II) had a major impact on FeRed S. alga cells were shown to have an Fe(ll) sorptio n capacity of similar to 0.1 mmol g(-1), compared with similar to 0.25 mmol g(-1) determined for the synthetic Ct. Sorption experiments with component mixtures indicated that direct interaction between cells and oxide resulte d in increased Fe(II)-binding capacity of the mixed system, possibly throug h production of exopolymeric materials by the cells. Medium constituents th at affected Fe(ll) speciation were shown to have a significant indirect inf luence on the extent of oxide reduction. Malate, which formed soluble compl exes with Fe(ll), promoted the extent of oxide reduction. In contrast, high (mM) PO43- concentrations favored surface/bulk precipitation processes whi ch reduced the extent of oxide reduction. Collectively, our results indicat e that Fe(ll) sorption by oxide and cell surfaces, together with Fe(ll) com plexation by or precipitation with medium components, all influence the rat e and extent of FeRed. Furthermore, saturation of sorption cites with Fe(ll ) does not appear to limit the ability of S. alga to reduce Fe(lll) oxides, especially if conditions favor growth.