For instance, sulfate-reducing

bacteria have the ability to utilize H2 at lower concentrations than minimum required by methanogens, in the presence of sulfate. Consequently, sulfidogenesis generally prevails in estuarine, marine, and hypersaline sediments where sulfate diffuses from overlying water (McGenity, 2010b). However, increased salinity in many cases supplies higher concentrations of noncompetitive substrates, which derive from compatible solutes synthesized by the environmental microbiota. Such high-salinity-associated solutes include methylated amines and dimethylsulfide. At high salt concentration, neither the reduction of carbon dioxide by hydrogen nor the aceticlastic reaction was shown to occur. Acetate splitting methanogens appear to be very little salt find more tolerant. The upper salt concentration for growth of cultures of methanogenic Archaea greatly depends on the substrate used: 270 g L−1 for group 2 methanogens, 120 g L−1 for group 1 methanogens, and 40 g L−1 for group 3 methanogens (Oren, 1999). These salinities should not be considered as the upper limit of activity in situ, but to be indicative of the relative importance of these substrates at different salinities

(McGenity, 2010b). The absence of group 1 and group 3 methanogens at high salinity may be governed by the relative energy gain from different methanogenic reactions per mole of substrate (methylotrophic ≫ hydrogenotrophic ≥ aceticlastic), especially because halophiles

must expend a lot of energy to maintain an osmotically balanced and functional cytoplasm MRIP via the biosynthesis and/or uptake of organic click here compatible solutes, and/or uptake of potassium ions (Oren, 1999). This may further explain the predominance of methylotrophic methanogens like Methanohalophilus spp. in hypersaline environments. On the other hand, we must approach this interpretation with caution, because standard Gibbs free energy yields are only one determinant of the total metabolic energy yield, and we must take into consideration the rate of substrate flux/consumption. Trimethylamine is often found in saline systems, where it is formed from glycine betaine or other osmoprotectants used by the resident organisms to equilibrate the cytoplasmic osmolarity to that of the water. This substance is rapidly transformed by methanogens to methane, CO2, and ammonia, but it is not easily utilized by sulfidogenic bacteria. Trimethylamine-degrading methanogens from saline environments belong to the family Methanosarcinaceae, and all methanogens that have been isolated to date from high-salinity ecosystems use trimethylamine as catabolic substrate (with the exception of M. halotolerans, which uses H2 + CO2 or formate and has a relatively restricted salt tolerance, and does not grow above 120 g L−1 salt). Hypersaline environments harbor surprisingly diverse communities of Archaea, aerobic as well as anaerobic.