Oxidative stress response in Clostridium perfringens

Redox fluctuation structures microbial communities in a wet tropical soil

Frequent high-amplitude redox fluctuation may be a strong selective force on the phylogenetic and physiological composition of soil bacterial communities and may promote metabolic plasticity or redox tolerance mechanisms. To determine effects of fluctuating oxygen regimens, we incubated tropical soils under four treatments: aerobic, anaerobic, 12-h oxic/anoxic fluctuation, and 4-day oxic/anoxic fluctuation. Changes in soil bacterial community structure and diversity were monitored with terminal restriction fragment length polymorphism (T-RFLP) fingerprints. These profiles were correlated with gross N cycling rates, and a Web-based phylogenetic assignment tool was used to infer putative community composition from multiple fragment patterns. T-RFLP ordinations indicated that bacterial communities from 4-day oxic/anoxic incubations were most similar to field communities, whereas those incubated under consistently aerobic or anaerobic regimens developed distinctly different molecular profiles. Terminal fragments found in field soils persisted either in 4-day fluctuation/aerobic conditions or in anaerobic/12-h treatments but rarely in both. Only 3 of 179 total fragments were ubiquitous in all soils. Soil bacterial communities inferred from in silico phylogenetic assignment appeared to be dominated by Actinobacteria (especially Micrococcus and Streptomycetes), "Bacilli," "Clostridia," and Burkholderia and lost significant diversity under consistently or frequently anoxic incubations. Community patterns correlated well with redox-sensitive processes such as nitrification, dissimilatory nitrate reduction to ammonium (DNRA), and denitrification but did not predict patterns of more general functions such as N mineralization and consumption. The results suggest that this soil's indigenous bacteria are highly adapted to fluctuating redox regimens and generally possess physiological tolerance mechanisms which allow them to withstand unfavorable redox periods.

Discovery and characterization of a Coenzyme A disulfide reductase from Pyrococcus horikoshii. Implications for this disulfide metabolism of anaerobic hyperthermophiles

We have cloned NADH oxidase homologues from Pyrococcus horikoshii and P. furiosus, and purified the recombinant form of the P. horikoshii enzyme to homogeneity from Escherichia coli. Both enzymes (previously referred to as NOX2) have been shown to act as a coenzyme A disulfide reductases (CoADR: CoA-S-S-CoA + NAD(P)H + H+-->2CoA-SH + NAD(P)+). The P. horikoshii enzyme shows a kcat app of 7.2 s(-1) with NADPH at 75 degrees C. While the enzyme shows a preference for NADPH, it is able to use both NADPH and NADH efficiently, with both giving roughly equal kcats, while the Km for NADPH is roughly eightfold lower than that for NADH. The enzyme is specific for the CoA disulfide, and does not show significant reductase activity with other disulfides, including dephospho-CoA. Anaerobic reductive titration of the enzyme with NAD(P)H proceeds in two stages, with an apparent initial reduction of a nonflavin redox center with the first reduction resulting in what appears to be an EH2 form of the enzyme. Addition of a second of NADPH results in the formation of an apparent FAD-NAD(P)H complex. The behavior of this enzyme is quite different from the mesophilic staphylococcal version of the enzyme. This is only the second enzyme with this activity discovered, and the first from a strict anaerobe, an Archaea, or hyperthermophilic source. P. furiosus cells were assayed for small molecular mass thiols and found to contain 0.64 micromol CoA.g dry weight(-1) (corresponding to 210 microM CoA in the cell) consistent with CoA acting as a pool of disulfide reducing equivalents.