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Gram-Negative Mesophilic Sulfate-Reducing Bacteria
TLDR
The utilization of polysaccharides or polypeptides, such as has been observed with the extremely thermophilic sulfate-reducing archaebacterium Archaeoglobus (Stetter, 1988; Stetter et al., 1987), has not been reported for mesophobic sulfate reducers.
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A marine microbial consortium apparently mediating anaerobic oxidation of methane
A large fraction of globally produced methane is converted to CO2 by anaerobic oxidation in marine sediments. Strong geochemical evidence for net methane consumption in anoxic sediments is based on…
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Studies on dissimilatory sulfate-reducing bacteria that decompose fatty acids
TLDR
Gliding motility, ultrastructure and nutrition of two newly isolated filamentous sulfate-reducing bacteria, strains 5ac10 and 4be13, were investigated; the capacity of complete oxidation was shown by stoichiometric measurements with acetate plus sulfate.
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Predictive Identification of Exonic Splicing Enhancers in Human Genes
Anaerobic, nitrate-dependent microbial oxidation of ferrous iron
TLDR
The newly observed bacterial process may significantly contribute to ferric iron formation in the suboxic zone of aquatic sediments.
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Dissimilatory Sulfate- and Sulfur-Reducing Prokaryotes
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Microbial Reefs in the Black Sea Fueled by Anaerobic Oxidation of Methane
TLDR
Obviously, anaerobic microbial consortia can generate both carbonate precipitation and substantial biomass accumulation, which has implications for the understanding of carbon cycling during earlier periods of Earth's history.
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Microbiology and ecology of sulfate-and sulfur-reducing bacteria
Studies on dissimilatory sulfate-reducing bacteria that decompose fatty acids
Three strains (2ac9, 3ac10 and 4ac11) of oval to rodshaped, Gram negative, nonsporing sulfate-reducing bacteria were isolated from brackish water and marine mud samples with acetate as sole electron…
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Anaerobic oxidation of ferrous iron by purple bacteria, a new type of phototrophic metabolism
TLDR
Anoxic iron-rich sediment samples that had been stored in the light showed development of brown, rusty patches and the existence of ferrous iron-oxidizing anoxygenic phototrophic bacteria may offer an explanation for the deposition of early banded-iron formations in an assumed anoxic biosphere in Archean times.
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