Does a low-pH microenvironment around phototrophic Fe(II) -oxidizing bacteria prevent cell encrustation by Fe(III) minerals?
Neutrophilic Fe(II) -oxidizing bacteria precipitate positively charged Fe(III) minerals that are expected to sorb to the negatively charged cell surface, leading to encrustation and thus limiting the cells' accessibility to substrates and nutrients. However, electron-microscopy analysis of phototrophic iron-oxidizing Thiodictyon sp. strain F4 cells showed no encrustation, but mineral precipitation at a distance from the cell surface. In situ fluorescence microscopy analysis of F4 cells using a pH-sensitive fluorescent dye revealed a low cell surface pH (6.0 ± 0.1) in contrast to the bulk pH (6.6 ± 0.1). Biogeochemical modeling showed that the pH difference reduces Fe(III) sorption and Fe(III) precipitation rates at the cell surface, therefore directing mineral formation away from the cells. The results from this study therefore suggest that the establishment of a low cell surface pH could provide a mechanism for photoferrotrophs to successfully prevent Fe(III) mineral precipitation on the cell surface.
Geomicrobiology, Center for Applied Geosciences, University of Tuebingen, Tuebingen, Germany.
Florian
F
Hegler
Caroline
C
Schmidt
Heinz
H
Schwarz
Andreas
A
Kappler
D002841:Chromatiaceae / Q000378:metabolism*; D004777:Environment; D005290:Ferric Compounds / Q000378:metabolism*; D005296:Ferrous Compounds / Q000378:metabolism*; D006863:Hydrogen-Ion Concentration; D007501:Iron / Q000378:metabolism; D018613:Microscopy, Confocal; D008956:Models, Chemical; D010084:Oxidation-Reduction; D052817:Phototrophic Processes; D059010:Single-Cell Analysis
D005290:Ferric Compounds; D005296:Ferrous Compounds; D007501:Iron