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Abstract: The anthropocentric term “extremophile” was introduced more than 30 years ago to describe any organism capable of living and growing under extreme conditions—i.e., particularly hostile to human and to the majority of the known microorganisms as far as temperature, pH, and salinity parameters are concerned. With the further development of studies on microbial ecology and taxonomy, more “extreme” environments were found and more extremophiles were described. Today, many different extremophiles have been isolated from habitats characterized by hydrostatic pressure, aridity, radiations, elevated temperatures, extreme pH values, high salt concentrations, and high solvent/metal concentrations, and it is well documented that these microorganisms are capable of thriving under extreme conditions better than any other organism living on Earth. Extremophiles have also been investigated as far as the search for life in other planets is concerned and even to evaluate the hypothesis that life on Earth came originally from space. Extremophiles are interesting for basic and applied sciences. Particularly fascinating are their structural and physiological features allowing them to stand extremely selective environmental conditions. These properties are often due to specific biomolecules (DNA, lipids, enzymes, osmolites, etc.) that have been studied for years as novel sources for biotechnological applications. In some cases (DNA polymerase, thermostable enzymes), the search was successful and the final application was achieved, but certainly further exploitations are next to come.

Under anaerobic conditions, microbial reductive dechlorination of polychlorinated biphenyls (PCBs) occurs in soils and aquatic sediments. In contrast to dechlorination of supplemented single congeners for which frequently orthodechlorination has been observed, reductive dechlorination mainly attacks metaand/or parachlorines of PCB mixtures in contaminated sediments, although in a few instances orthodechlorination of PCBs has been observed. Different microorganisms appear to be responsible for different dechlorination activities and the occurrence of various dehalogenation routes. No axenic cultures of an anaerobic microorganism have been obtained so far. Most probable number determinations indicate that the addition of PCB congeners, as potential electron acceptors, stimulates the growth of PCB‐dechlorinating microorganisms. A few PCB‐dechlorinating enrichment cultures have been obtained and partially characterized. Temperature, pH, availability of naturally occurring or of supplemented carbon sources, and the presence or absence of H2or other electron donors and competing electron acceptors influence the dechlorination rate, extent and route of PCB dechlorination. We conclude from the sum of the experimental data that these factors influence apparently the composition of the active microbial community and thus the routes, the rates and the extent of the dehalogenation. The observed effects are due to the specificity of the dehalogenating bacteria which become active as well as changing interactions between the dehalogenating and non‐dehalogenating bacteria. Important interactions include the induced changes in the formation and utilization of H2by non‐dechlorinating and dechlorinating bacteria, competition for substrates and other electron donors and acceptors, and changes in the formation of acidic fermentation products by heterotrophic and autotrophic acidogenic bacteria leading to changes in the pH of the sediments.

Under anaerobic conditions, microbial reductive dechlorination of polychlorinated biphenyls (PCBs) occurs in soils and aquatic sediments. In contrast to dechlorination of supplemented single congeners for which frequently orthodechlorination has been observed, reductive dechlorination mainly attacks metaand/or parachlorines of PCB mixtures in contaminated sediments, although in a few instances orthodechlorination of PCBs has been observed. Different microorganisms appear to be responsible for different dechlorination activities and the occurrence of various dehalogenation routes. No axenic cultures of an anaerobic microorganism have been obtained so far. Most probable number determinations indicate that the addition of PCB congeners, as potential electron acceptors, stimulates the growth of PCB-dechlorinating microorganisms. A few PCB-dechlorinating enrichment cultures have been obtained and partially characterized. Temperature, pH, availability of naturally occurring or of supplemented carbon sources, and the presence or absence of H2or other electron donors and competing electron acceptors influence the dechlorination rate, extent and route of PCB dechlorination. We conclude from the sum of the experimental data that these factors influence apparently the composition of the active microbial community and thus the routes, the rates and the extent of the dehalogenation. The observed effects are due to the specificity of the dehalogenating bacteria which become active as well as changing interactions between the dehalogenating and non-dehalogenating bacteria. Important interactions include the induced changes in the formation and utilization of H2by non-dechlorinating and dechlorinating bacteria, competition for substrates and other electron donors and acceptors, and changes in the formation of acidic fermentation products by heterotrophic and autotrophic acidogenic bacteria leading to changes in the pH of the sediments.

Abstract: Fresh and dichlorophenol (DCP)-adapted sediments from two ponds near Athens, Georgia exhibited distinctly different dechlorinating activities. These differences centered on the relative rates of reductive dehlorination in both fresh and adapted sediments and on the substrate specificity of the adapted sediments. Fresh Cherokee Trailer Park Pond sediment dechlorinated 2,3-, 2,4-, and 2,6-DCP to monochlorophenols at a faster rate and after a shorter lag period than fresh Bolton's Pond sediment. Lag periods were not observed in either Cherokee or Bolton's sediments that had been adapted to dechlorinate either 2,3-, 2,4-or 2,6-DCP. Adapted Cherokee sediments exhibited faster dechlorinating rates and a broader substrate specificity than the adapted Bolton's sediments. The broad substrate specificity of each of the adapted Cherokee sediments contrasted sharply with the narrow specificity of the 2,6-DCP-adapted Bolton's sediment. The preference for reductive dechlorination wasortho>meta orpara in sediments from both ponds.

Abstract: Organisms present in methanogenic freshwater lake sediments from the vicinity of Athens, Georgia, were adapted to mineralize 2,4-dichlorophenol. Repeated addition of 0.5 to 2.7 mmol/liter of phenol, and later of 0.5–6.2 mmol/liter p-hydroxybenzoate (p-OHB), to such enrichments led to the conversion of p-OHB to phenol at a rate of up to 100 mmol p-OHB per liter per day. Subsequently, a spore-forming, obligately anaerobic bacterium, strain JW/Z-1, was isolated which transformed p-OHB to phenol and 3,4-dihydroxybenzoate (3,4-OHB) to catechol (1,2-dihydroxybenzene) stoichiometrically without further metabolism of the phenols. The strain did not transform benzoate, 4-chlorophenol, 2,4-dichlorophenol, 4-chlorobenzoate, o- and m-hydroxybenzoate, 2,4- and 3,5-dihydroxybenzoate, 2,3,4- and 3,4,5-trihydroxybenzoate, or 4-aminobenzoate. Yeast extract was required for growth of strain JW/Z-1 and only high concentrations of casein hydrolysate or tryptone could substitute it, to some extent. Except for sodium acetate, and some amino acids together with a 20-fold increased concentration of vitamins, no single carbohydrate or defined organic compound has been found to support growth of this strain in the presence (or in the absence) of 0.2 to 0.5% (w/v) yeast extract. The fermentation products during growth on yeast extract indicated that the metabolism of amino acid degradation was the major source for growth. The decarboxylating activity was inducible by p-OHB for the decarboxylation of p-OHB, and at a lower rate for 3,4-OHB, and by 3,4-OHB only for 3,4-OHB, suggesting that two different enzyme systems exist. The addition of the aromatic amino acids phenol or benzoate did not induce the decarboxylation activity in cultures growing with yeast extract. Growth was observed at temperatures ranging from 12–41C (Topt, 33–34C) and at pH-values ranging from 6.0–10.0 (pHopt, 7.2–8.2). The shortest doubling time observed for strain JW/Z-1 was 3.2 hours.

Abstract: Although some anaerobic and aerobic mesophiles have long been known to grow at alkaline pH (above 9.5), little was known until recently about thermophilic alkaliphiles, termed now alkalithermophiles. This minireview describes presently known and recently validly described anaerobic alkalithermophilic bacteria (pHopt55C > 8.5; Topt > 55°C) and alkalitolerant thermophiles (pHopt55C < 8.5 but pHmax55C above 9.0). Some of these are widely distributed, but others have been isolated (thus far) only from one specific location. This novel group of anaerobic bacteria is comprised of physiologically different genera and species which, so far, all belong to the Gram-type positive Bacillus-Clostridium phylogenetic subbranch. An interesting feature of these anaerobic alkalithermophiles is that most of the isolates have short doubling times. The fastest growing among them are strains of Thermobrachium celere, with doubling times as short as 10 min while growing above pH 9.0 and above 55°C.

Abstract: Six sustainable enrichment cultures of thermophilic H2-oxidizing microorganisms utilizing Fe(III) as an electron acceptor were obtained from geothermally heated environments located on two continents (America, Eurasia) and on islands in the Northern (Iceland) and Southern (Fiji) hemispheres, demonstrating the wide distribution of these microorganisms. The main products of amorphic Fe(III) oxide reduction were magnetite and siderite. The observed temperature range for Fe(III) reduction in growing cultures was from 55°C to 87°C, extending the known limits for growth of Fe(III)-reducing microorganisms producing extracellular magnetite to nearly 90°C.

A mutant strain of ‘Thermoanaerobacter ethanolicus’ (ATCC 31 550) designated JW200 Fe 4 contains primary and secondary alcohol dehydrogenases (ADHs). The primary ADH from JW000 Fe 4 was formed early in the growth cycle compared to the primary ADH form the wild-type strain (JW200 wt). The secondary ADH displayed 2.5-fold greater activity during the growth cycle of JW200 Fe 4 compared to the secondary ADH form JW200 wt. Both primary and secondary ADHs from JW200 Fe 4 were purified to homogeneity ADHs from JW200 Fe 4 were purified to homogeneity as determined by sodium dodecyl sulphate-gel electrophoresis. Relative molecular weight estimations indicated that both ADHs were tetrameric. Each ADH from JW200 Fe 4 contained approximately four Zn atoms per subunit and displayed Arrhenius plots similar to the ADHs from JW200 wt. The substrate specificity for the ADHs from JW200 Fe 4 was similar to that of the ADHs from JW200 wt. The secondary ADH oxidized 2-propanol at 51 times the rate of ethanol. Both ADHs from JW200 Fe 4 apparently reduce acetaldehyde to ethanol while only the secondary ADH from JW200 wt was suggested to contribute significantly to ethanol production.

Abstract: The reductive dechlorination of 2,4- and 3,4-dichlorophenol (DCP) was studied in slurries of marine sediments and subsurface soils with dissolved organic carbon concentrations less than 1 ppm. Dechlorination was markedly greater in marine sediment slurries than in subsoil slurries, although similar products were observed in each case. From 25% to 98% of the 2,4- and 3,4-DCP (6.5 μm/l) added to most marine slurries was converted to 4- and 3-chlorophenol (CP) respectively, within 30 weeks. In contrast 2,4-DCP was dechlorinated to 4-CP (>90%) in only 1 of 24 replicate subsoil slurries after 32 weeks of incubation. Dechlorination was observed within 2 weeks when yeast extract was added to subsoil slurries; yeast extract additions also stimulated dechlorination in marine sediments but to a lesser extent. The intermediate monochlorophenol products did not persist in marine slurries but did persist in the subsoil slurries. It was concluded that the total organic carbon at a site is not always a good predictor of the site's ability to support dechlorination activity.

The industrial application of thermophilic (eu)bacteria is hampered by the lack of genetic systems for these bacteria. We report here the first unequivocal transformation of a Gram‐positive, thermophilic, anaerobic microorganism, Thermoanaerobacterium, with the kanamycin resistance‐mediating plasmid pIKM1. The construct pIKM1 is based on the Escherichia coli–Clostridium acetobutylicumshuttle vector pIMP1 and contains the thermostable kanamycin cassette from S. faecalisplasmid pKD102. Using electrotransformation, plasmid pIKM1 mediated kanamycin resistance in Thermoanaerobacteriumsp. strain JW/SL‐YS485 up to 400 μg ml−1at 48°C and 200 μg ml−1at 60°C.

13C-1 phenol was converted to 13C-4 benzoic acid by an anaerobic phenol converting enrichment, which did not form p-hydroxybenzoate as a free intermediate but converted p-hydroxybenzoate first phenol and then, probably by another organism, to benzoate. No isotopic effect was observed using D5- and D6-phenol, suggesting that the breakage of the C-H bond on the C-4 position was not a rate limiting step in the conversion.

The industrial application of thermophilic (eu)bacteria is hampered by the lack of genetic systems for these bacteria. We report here the first unequivocal transformation of a Gram-positive, thermophilic, anaerobic microorganism, Thermoanaerobacterium, with the kanamycin resistance-mediating plasmid pIKM1. The construct pIKM1 is based on the Escherichia coli–Clostridium acetobutylicum shuttle vector pIMP1 and contains the thermostable kanamycin cassette from S. faecalis plasmid pKD102. Using electrotransformation, plasmid pIKM1 mediated kanamycin resistance in Thermoanaerobacterium sp. strain JW/SL-YS485 up to 400 μg ml−1 at 48°C and 200 μg ml−1 at 60°C.