Hydrogenosomal ferredoxin of the anaerobic protozoon, Tritrichomonas foetus

A low molecular weight iron-sulfur protein has been purified from Tritrichomonas foetus by deoxycholate extraction of whole cells, ion exchange chromatography, and gel filtration. The purified protein was essentially homogeneous as judged by isoelectric focusing, polyacrylamide gel electrophoresis, and gel filtration. A pI of 4.3 was observed. The molecular weight of the protein was estimated to be 12,000. Chemical and spectral analysis showed the protein to have a [2Fe-2S] cluster. The absorbance spectrum of the oxidized protein showed maxima at 280, 340, 458 and shoulders at 410 and 550 nm. The maximum observed A458/A280 ratio was 0.82 and the absorbance of the oxidized protein at 458 nm was 8,000 M-1 X cm-1. The low temperature EPR spectrum of the protein reduced with dithionite revealed axial symmetry with features at g values of g = 1.94 and g = 2.02. The oxidized protein gave no EPR signal in the g = 1.8 to 2.2 range. Cell fractionation studies indicated the localization of this protein in the hydrogenosome. The protein was able to function as an electron transport component in the reduction of metronidazole (a 5-nitroimidazole derivative) by pyruvate:ferredoxin oxidoreductase and hydrogenase from T. foetus and also from Trichomonas vaginalis and Clostridium pasteurianum as well as in the reduction of cytochrome c by plant NADPH:ferredoxin oxidoreductase. This protein has the characteristics of a ferredoxin and is likely to be a physiological electron carrier in hydrogenosomal pyruvate oxidation.     

Empirical testing of cryoconite granulation: Role of cyanobacteria in the formation of key biogenic structure darkening glaciers in polar regions

Cryoconite, the dark sediment on the surface of glaciers, often aggregates into oval or irregular granules serving as biogeochemical factories. They reduce a glacier's albedo, act as biodiversity hotspots by supporting aerobic and anaerobic microbial communities, constitute one of the organic matter (OM) sources on glaciers, and are a feeder for micrometazoans. Although cryoconite granules have multiple roles on glaciers, their formation is poorly understood. Cyanobacteria are ubiquitous and abundant engineers of cryoconite hole ecosystems. This study tested whether cyanobacteria may be responsible for cryoconite granulation as a sole biotic element. Incubation of Greenlandic, Svalbard, and Scandinavian cyanobacteria in different nutrient availabilities and substrata for growth (distilled water alone and water with quartz powder, furnaced cryoconite without OM, or powdered rocks from glacial catchment) revealed that cyanobacteria bind mineral particles into granules. The structures formed in the experiment resembled those commonly observed in natural cryoconite holes: they contained numerous cyanobacterial filaments protruding from aggregated mineral particles. Moreover, all examined strains were confirmed to produce extracellular polymeric substances (EPS), which suggests that cryoconite granulation is most likely due to EPS secretion by gliding cyanobacteria. In the presence of water as the only substrate for growth, cyanobacteria formed mostly carpet-like mats. Our data empirically prove that EPS-producing oscillatorialean cyanobacteria isolated from the diverse community of cryoconite microorganisms can form granules from mineral substrate and that the presence of the mineral substrate increases the probability of the formation of these important and complex biogeochemical microstructures on glaciers.