Proton-binding capacity of Staphylococcus aureus wall teichoic acid and its role in controlling autolysin activity.

Wall teichoic acid (WTA) or related polyanionic cell wall glycopolymers are produced by most gram-positive bacterial species and have been implicated in various cellular functions. WTA and the proton gradient across bacterial membranes are known to control the activity of autolysins but the molecular details of these interactions are poorly understood. We demonstrate that WTA contributes substantially to the proton-binding capacity of Staphylococcus aureus cell walls and controls autolysis largely via the major autolysin AtlA whose activity is known to decline at acidic pH values.

Influence of seasonal and geochemical changes on the geomicrobiology of an iron carbonate mineral water spring.

Fuschna Spring in the Swiss Alps (Engadin region) is a bicarbonate iron(II)-rich, pH-neutral mineral water spring that is dominated visually by dark green microbial mats at the side of the flow channel and orange iron(III) (oxyhydr)oxides in the flow channel. Gradients of O(2), dissolved iron(II), and bicarbonate establish in the water. Our goals were to identify the dominating biogeochemical processes and to determine to which extent changing geochemical conditions along the flow path and seasonal changes influence mineral identity, crystallinity, and microbial diversity.

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.

Extracellular iron biomineralization by photoautotrophic iron-oxidizing bacteria.

Iron oxidation at neutral pH by the phototrophic anaerobic iron-oxidizing bacterium Rhodobacter sp. strain SW2 leads to the formation of iron-rich minerals. These minerals consist mainly of nano-goethite (alpha-FeOOH), which precipitates exclusively outside cells, mostly on polymer fibers emerging from the cells.

Physiology of phototrophic iron(II)-oxidizing bacteria: implications for modern and ancient environments.

Phototrophic iron(II) [Fe(II)]-oxidizing bacteria are present in modern environments and evidence suggests that this metabolism was present already on early earth. We determined Fe(II) oxidation rates depending on pH, temperature, light intensity, and Fe(II) concentration for three phylogenetically different phototrophic Fe(II)-oxidizing strains (purple nonsulfur bacterium Rhodobacter ferrooxidans sp. strain SW2, purple sulfur bacterium Thiodictyon sp.