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Anaerobic bacteria from hypersaline environments
B Ollivier1, P Caumette, J L Garcia
1Laboratoire de Microbiologie ORSTOM, Université de Provence, Marseille, France.
Microbiological Reviews
|March 1, 1994
Summary
Anaerobic bacteria like fermentative, sulfate-reducing, and phototrophic microbes oxidize organic carbon in hypersaline environments. Methanogenesis is limited at high salt concentrations, with sulfate reduction becoming dominant.
Area of Science:
- Microbiology
- Environmental Science
- Biochemistry
Background:
- Hypersaline environments host diverse strictly anaerobic halophilic bacteria crucial for organic carbon oxidation.
- These include fermentative, sulfate-reducing, homoacetogenic, phototrophic, and methanogenic bacteria.
Purpose of the Study:
- To review the diversity and roles of anaerobic halophilic bacteria in hypersaline environments.
- To detail the specific genera, species, and metabolic functions within these extreme ecosystems.
Main Methods:
- Literature review and analysis of existing studies on anaerobic halophiles.
- Identification based on 16S rRNA sequences and optimal growth conditions (salinity, substrates).
Main Results:
- Nine species across six fermentative genera (two homoacetogens) are described, with six in Haloanaerobiaceae.
- Two moderately halophilic sulfate reducers (Desulfohalobium retbaense, Desulfovibrio halophilus) are reported.
- Phototrophic bacteria (purple bacteria) thrive at 6-11% NaCl (Rhodospirillum, Chromatium, Thiocapsa) and 20-25% NaCl (Ectothiorodhospiraceae), utilizing compatible solutes for osmoregulation.
- Methanogenesis is limited above 15% NaCl, with sulfate reduction dominating organic carbon oxidation at higher salinities.
Conclusions:
- Anaerobic halophiles play significant roles in carbon cycling in hypersaline environments.
- Specific bacterial groups dominate at different salinity levels, with distinct metabolic strategies.
- Sulfate reduction becomes a key terminal process at very high salinities, while methanogenesis is restricted.