Syntrophic growth of alkaliphilic anaerobes controlled by ferric and ferrous minerals transformation coupled to acetogenesis.

Redox-active iron minerals can act as energy sources or electron-transferring mediators in microbial syntrophic associations, being important means of interspecies metabolic cooperation in sedimentary environments. Alkaline conditions alter the thermodynamic stability of iron minerals, influencing their availability for interspecies syntrophic interactions. We have modeled anaerobic alkaliphilic microbial associations in ethanol-oxidizing co-culture of an obligate syntroph Candidatus "Contubernalis alkalaceticum" and a facultative lithotroph Geoalkalibacter ferrihydriticus, which is capable of dissimilatory Fe(III) reduction and homoacetogenic oxidation of Fe(II) with CO2. The co-cultures were cultivated with thermodynamically metastable ferric-containing ferrihydrite, or ferrous-containing siderite, or without minerals. Mössbauer spectral analysis revealed the transformation of both minerals to the stable magnetite. In the presence of ferrihydrite, G. ferrihydriticus firstly reduced Fe(III) with ethanol and then switched to syntrophic homoacetogenesis, providing the growth of obligate syntroph on ethanol. The ability of G. ferrihydriticus to accept hydrogen from its syntrophic partner and produce extra acetate from carbonate during ethanol oxidation was confirmed by co-culture growth without minerals. In the presence of siderite, G. ferrihydriticus performed homoacetogenesis using two electron donors simultaneously- siderite and hydrogen. Pieces of evidence for direct and indirect hydrogen-mediated electron exchange between partner organisms were obtained. Relative abundancies of partner organisms and the rate of acetate production by their co-cultures were strongly determined by thermodynamic benefits, which G. ferrihydriticus got from redox transformations of iron minerals. Even the minor growth of G. ferrihydriticus sustained the growth of the syntroph. Accordingly, microbe-to-mineral interactions could represent underestimated drivers of syntrophic interactions in alkaline sedimentary environments.

Fervidobacterium riparium sp. nov., a thermophilic anaerobic cellulolytic bacterium isolated from a hot spring.

A novel obligately anaerobic, extremely thermophilic, organotrophic bacterium, strain 1445t(T), was isolated from a hot spring on Kunashir Island (Kuril Islands, Russia). Cells were motile rods (0.4-0.5 × 1.0-3.0 µm). The temperature range for growth at pH 7.8 was 46-80 °C, with optimum growth at 65 °C. The pH range for growth at 65 °C was pH 5.7-9.0, with optimum growth at pH 7.8. Growth was not observed at or below 40 °C, at or above 84 °C, at or below pH 5.4 or at or above pH 9.5. The isolate degraded a wide range of substrates including starch, cellulose and cellulose derivatives. Elemental sulfur stimulated growth, but sodium sulfate, sulfite and thiosulfate did not. DNA G+C content was 31 mol%. Phylogenetic analysis of 16S rRNA gene sequences showed that strain 1445t(T) belonged to the genus Fervidobacterium. 16S rRNA gene sequence similarities with strains of other species of the genus Fervidobacterium were 94.9-98.3 %; the type strain of Fervidobacterium gondwanense was the closest relative of strain 1445t(T). DNA-DNA hybridization of strain 1445t(T) and F. gondwanense AB39(T) revealed a relatedness value of 20 %. Based on phylogenetic data and physiological properties of the isolate, a novel species, designated Fervidobacterium riparium sp. nov., is proposed with strain 1445t(T) ( = DSM 21630(T) = VKM B-2549(T)) as the type strain.