Biological and Abiological Sulfur Reduction at High Temperatures

Reduction of elemental sulfur was studied in the presence and absencè of thermophilic sulfur-reducing bacteria, at temperatures ranging from 65 to 110°C, in anoxic artificial seawater media. Above 80°C, significant amounts of sulfide were produced abiologically at linear rates, presumably by the disproportionation of sulfur. These rates increased with increasing temperature and pH and were enhanced by yeast extract. In the same medium, the sulfur respiration of two recent thermophilic isolates, a eubacterium and an archaebacterium, resulted in sulfide production at exponential rates. Although not essential for growth, sulfur increased the cell yield in both strains up to fourfold. It is suggested that sulfur respiration is favored at high temperatures and that this process is not limited to archaebacteria, but is shared by other extreme thermophiles.     

A novel ATPase complex selectively accumulated upon heat shock is a major cellular component of thermophilic archaebacteria.

We have discovered a large cylindrical protein complex which is an abundant component of the cytoplasm of extremely thermophilic archaebacteria. Structural analysis by image processing of electron micrographs suggests that the complex is composed of two stacked rings of eight subunits each; the rings enclose a central channel. The complex purified from the hyperthermophile Pyrodictium occultum is composed of equal quantities of two polypeptides of Mr 56,000 and 59,000. It exhibits an extremely thermostable ATPase activity with a temperature optimum of 100 degrees C. The basal level of the ATPase complex in the cell is high, and it becomes highly enriched as a result of heat shock (shift from 102 degrees C to 108 degrees C) or balanced growth at temperatures near the physiological upper limit. Immunoblotting results indicate that a related protein is present in most thermophilic archaebacteria and in Escherichia coli. This protein complex may play an important role in the adaptation of thermophilic archaebacteria to life at high temperature.     

Enzymes of the reductive citric acid cycle in the autotrophic eubacterium Aquifex pyrophilus and in the archaebacterium Thermoproteus neutrophilus

The autotrophic carbon fixation pathway was studied in the thermophilic hydrogen oxidizing eubacterium Aquifex pyrophilus and in the thermophilic sulfur reducing archaebacterium Thermoproteus neutrophilus. Neither organism contained ribulose-1,5-bisphosphate carboxylase activity suggesting that the Calvin cycle is not operating. Rather, all enzymes of the reductive citric acid cycle were found in A. pyrophilus. In T. neutrophilus ATP citrate lyase activity was detected which has not been achieved so far; this finding corroborates earlier work suggesting the presence of the reductive citric acid cycle in this archaebacterium. The reductive citric acid cycle for autotrophic CO₂ fixation now has been documented in the eubacterial branches of the proteobacteria, in green sulfur bacteria, and in the thermophilic Knallgas bacteria as well as in the branch of the sulfur dependent archaebacteria.     

13C-NMR study of autotrophic CO2 fixation in Thermoproteus neutrophilus

The pathway of autotrophic CO2 fixation has been investigated in the extremely thermophilic sulfur-respiring anaerobic archaebacterium Thermoproteus neutrophilus. [1,4-13C2]Succinate was used as a tracer since this compound was incorporated in small amounts virtually into all cell compounds without affecting the organism's ability to synthesize all cell constituents from CO2. Three representative amino acids, glutamate, aspartate and alanine were isolated from cells after growth for several generations in the presence of [1,4-13C2]succinate and their labelling patterns were determined by 13C NMR spectroscopy. The data is consistent with CO2 fixation by a reductive citric acid cycle, as proposed earlier for the green sulfur bacterium Chlorobium limicola, the sulfate-reducing Desulfobacter hydrogenophilus and the microaerophilic Knallgasbacterium Hydrogenobacter thermophilus. The presence of a reductive citric acid cycle in archaebacteria indicates that this CO2 fixation mechanism which is an alternative to the Calvin cycle is present in many anaerobic or facultative anaerobic microorganisms.     

Comparison of plasmid DNA topology among mesophilic and thermophilic eubacteria and archaebacteria.

Several plasmid DNAs have been isolated from mesophilic and thermophilic archaebacteria. Their superhelical densities were estimated at their host strain's optimal growth temperature, and in some representative strains, the presence of reverse gyrase activity (positive DNA supercoiling) was investigated. We show here that these plasmids can be grouped in two clusters with respect to their topological state. The group I plasmids have a highly negatively supercoiled DNA and belong to the mesophilic archaebacteria and all types of eubacteria. The group II plasmids have DNA which is close to the relaxed state and belong exclusively to the thermophilic archaebacteria. All archaebacteria containing a relaxed plasmid, with the exception of the moderately thermophilic methanogen Methanobacterium thermoautotrophicum Marburg, also exhibit reverse gyrase activity. These findings show that extrachromosomal DNAs with very different topological states coexist in the archaebacterial domain.     

Thiosulfate, polythionates and elemental sulfur assimilation and reduction in the bacterial world

Among sulfur compounds, thiosulfate and polythionates are present at least transiently in many environments. These compounds have a similar chemical structure and their metabolism appears closely related. They are commonly used as energy sources for photoautotrophic or chemolithotrophic microorganisms, but their assimilation has been seldom studied and their importance in bacterial physiology is not well understood. Almost all bacterial strains are able to cleave these compounds since they possess thiosulfate sulfur transferase, thiosulfate reductase or S-sulfocysteine synthase activities. However, the role of these enzymes in the assimilation of thiosulfate or polythionates has not always been clearly established. Elemental sulfur is, on the contrary, very common in the environment. It is an energy source for sulfur-reducing eubacteria and archaebacteria and many sulfur-oxidizing archaebacteria. A phenomenon still not well understood is the 'excessive assimilatory sulfur metabolism' as observed in methanogens which perform a sulfur reduction which exceeds their anabolic needs without any apparent benefit. In heterotrophs, assimilation of elemental sulfur is seldom described and it is uncertain whether this process actually has a physiological significance. Thus, reduction of thiosulfate and elemental sulfur is a common but incompletely understood feature among bacteria. These activities could give bacteria a selective advantage, but further investigations are needed to clarify this possibility. Presence of thiosulfate, polythionates and sulfur reductase activities does not imply obligatorily that these activities play a role in thiosulfate, polythionates or sulfur assimilation as these compounds could be merely intermediates in bacterial metabolism. The possibility also exists that the assimilation of these sulfur compounds is just a side effect of an enzymatic activity with a completely different function. As long as these questions remain unanswered, our understanding of sulfur and thiosulfate metabolism will remain incomplete.     

Thiosulfate, polythionates and elemental sulfur assimilation and reduction in the bacterial world

Abstract Among sulfur compounds, thiosulfate and polythionates are present at least transiently in many environments. These compounds have a similar chemical structure and their metabolism appears closely related. They are commonly used as energy sources for photoautotrophic or chemolithotrophic microorganisms, but their assimilation has been seldom studied and their importance in bacterial physiology is not well understood. Almost all bacterial strains are able to cleave these compounds since they possess thiosulfate sulfur transferase, thiosulfate reductace or S -sulfocysteine synthase activities. However, the role of these enzymes in the assimilation of thiosulfate or polythionates has not always been clearly established.
Elemental sulfur is, on the contrary, very common in the environmental. It is an energy source for sulfur-reducing eubacteria and archaebacteria and many sulfur-oxidizing archaebacteria. A phenomenon still not well understood is the 'excessive assimilatory sulfur metabolism' as observed in methanogens which perform a sulfur reduction which exceeds their anabolic needs without any apparent benefit. In heterotrophs, assimilation of elemental sulfur is seldom described and it is uncertain whether this process actually has a physiological significance.
Thus, reduction of thiosulfate and elemental sulfur is a common by incompletely understood feature among bacteria. These activities could give bacteria a selective advantage, but futher investigations are needed to clarify this possibility. Presence of thiosulfate, polythionates and sulfur reductase activities does not imply obligatorily that these activities play a role in thiosulfate, polythionates or sulfur assimilation as these compounds could be merely intermediates in bacterial metabolism. The possibility also exists that the assimilation of these sulfur compounds is just a side effect of an enzymatic activity with a completely different function.     

Reverse gyrase in thermophilic eubacteria.

The presence of reverse gyrase, an unusual ATP-dependent type I topoisomerase first isolated from thermophilic archaebacteria, has been detected in four strains of Thermotogales, an order of extremely thermophilic eubacteria. This result suggests that reverse gyrase plays a key role in high-temperature-living organisms, independently of the evolutionary kingdom to which they belong.     

Early assembly proteins of the large ribosomal subunit of the thermophilic archaebacterium Sulfolobus. Identification and binding to heterologous rRNA species

Studies of ribosome structure in thermophilic archaebacteria may provide valuable information on (i) the mechanisms involved in the stabilization of nucleic acid-protein complexes at high temperatures and (ii) the degree of evolutionary conservation of the ribosomal components in the primary kingdoms of cell descent. In this work we investigate certain aspects of RNA/protein interaction within the large ribosomal subunits of the extremely thermophilic archaebacterium Sulfolobus solfataricus. The ribosomal proteins involved in the early reactions leading to in vitro particle assembly have been identified; it is shown that they can interact with the RNA in a temperature-independent fashion, forming a thermally stable "core" particle that can subsequently be converted into complete 50 S ribosomes. Among the protein components of the core particle, those capable of independently binding to 23 and 5 S RNA species have also been identified. Finally, we show that the early assembly proteins of Sulfolobus large ribosomal subunits are able to interact cooperatively with 23 S RNAs from other archaebacteria or from eubacteria, thereby suggesting that RNA/protein recognition sites are largely conserved within prokaryotic ribosomes. By contrast, no specific binding of the archaebacterial proteins to eukaryotic RNA could be demonstrated.     

1H and 13C NMR assignment of benzothiophenquinones from the sulfur-oxidizing archaebacterium Sulfolobus solfataricus

From Sulfolobus solfataricus, a sulfur-oxidizing thermophilic member of archaebacteria, three unusual benzothiophenquinones were isolated. Detailed NMR studies on these quinones, including multipulse mono-dimensional and two-dimensional techniques, were performed to obtain carbon and proton assignments, one-bond, geminal and vicinal coupling constants and T1 relaxation times. This report extends the known quinone composition of thermophilic archaebacteria and further supports the concept that these biomolecules can serve as a useful chemotaxonomic tool.     

DNA substrate specificity of reverse gyrase from extremely thermophilic archaebacteria

It has been shown earlier that eukaryotic type I DNA topoisomerases act on duplex DNA regions, while eubacterial type I topoisomerases require single-stranded regions. The present paper demonstrates that the type I topoisomerase from extremely thermophilic archaebacteria, reverse gyrase, winds DNA by binding to single-stranded DNA regions. Thus, type I topoisomerases, both relaxing one in eubacteria and reverse gyrase in extremely thermophilic archaebacteria share a substrate specificity to melted DNA regions. The important consequence of this specificity is that the cellular DNA superhelical stress actively controlled by bacterial topoisomerases is confined to a narrow range characterized by a low stability of the double helix. Hence we suppose that bacterial topoisomerase systems control duplex stability near its minimum, for which purpose they create an appropriate negative superhelicity at moderate temperatures or a positive one at extremely high temperatures, the feedback being ensured by the aforesaid specificity of type I bacterial topoisomerases.     

削偶合今祖法的提出

以低等真核生物的5.8S rRNA为材料进行研究。发现在用今祖法消除了进化速度之差的影响所得到的差异矩阵d＇中,各组理应彼此相等的数值会因核苷酸偶合的影响而成为不等值的。取各组中各自的的最大值作为受偶合的影响最小者,以之对今祖法所得到的分枝型式进行校正,即可得到更为正确的结果。在此基础上提出了对差异矩阵d＇进行最大值成聚以代替原法中的平均值成聚的削偶合今祖法。新法在结果的正确性、稳定性和一致性上都优于原法。     

A new extremely thermophilic,sulfur-reducing heterotrophic,marine bacterium

An extremely thermophilic (optimum growth at 88° C), anaerobic bacterium was isolated from a shallow submarine thermal spring. It appears to be an obligate heterotroph, capable of reducing sulfur to H₂S. Oxygen sensitivity is apparent only at and above those temperatures where growth occurs, while the cultures retain their viability for long periods under air at 4° C. Insensitivity to chloramphenicol, vancomycin and streptomycin, and lack of muramic acid in its cell wall, indicate a possible affilitation of the new isolate to the thermoacidophilic archaebacteria. However, its neutrophilic and hetertrophic nature, as well as its DNA base composition (39.1 mol % guanine plus cytosine) set it apart from the known genera of this group.Abbreviations ASW Artifical sea water medium - Bis-tris propane 1,3-bis[tris(hydroxymethyl)-methylamino]-propane - Mes 2(N-morpholino)ethanesulfonic acid - Pipes Piperazine-N,N-bis(2-ethanesulfonic acid)     

The metabolism of hydrogen by extremely thermophilic, sulfur-dependent bacteria

Abstract In just the last few years, a group of bacteria have been discovered that have the remarkable property of growing near and above 100°C. These extremely thermophilic organisms, defined here as having the ability to grow at 90°C with optimum growth at 80°C and above, have been isolated mainly from sulfur-rich, marine geothermal environments, both shallow and deep sea. They comprise over a dozen different genera, and except for one novel eubacterium, all may be classified as archaebacteria. The majority of the extremely thermophilic genera metabolize elemental sulfur (S°) and a survey of the various organisms reveals that most of them also depend upon the oxidation of hydrogen gas (H₂) as an energy source. In addition, two extremely thermophilic genera are known that actively produce H₂ as end-products of novel fermentative metabolisms. The enzyme hydrogenase, which is responsible for catalysing H₂ activation and H₂ production, appears to play several roles in electron and energy transfer during the growth of these organisms. Hydrogenase has so far been purified from only one extremely thermophilic species, from Pyrococcus furiosus ( T _opt = 100°C), and hydrogenase activity has been exmained in cell-free extracts of only a few others. However, a comparison of their properties with those of hydrogenases from mesophilic bacteria suggests that (a) the hydrogenase responsible for catalysing H₂ oxidation in extremely thermophilic organisms may be an extremely thermostable version of the mesophilic enzyme, and (b) a new type of 'evolution' hydrogenase, lacking the Ni-S or Fe-S catalytic sites of the mesophilic enzymes, is required for catalysing H₂ evolution at temperatures near and above 100°C.     

Bacterial sulfur reduction in hot vents

Abstract: Elemental sulfur can be reduced through different microbial processes, including catabolically significant sulfur respiration and reduction of sulfur in the course of fermentation. Both of these processes are found in thermophilic microorganisms inhabiting continental and submarine hot vents, where elemental sulfur is one of the most common sulfur species. Among extreme thermophiles, respresented mainly by Archaea, sulfur-respiring bacteria include hydrogen-utilizing lithoautotrophs and heterotrophs, oxidizing complex organic substrates. Some marine heterotrophic sulfur-reducing Archaea were found to ferment peptides and polysaccharides, using elemental sulfur as an electron sink and thus avoiding the formation of molecular hydrogen which is highly inhibiting. Moderately thermophilic communities contain eubacterial sulfur reducers capable of lithotrophic and heterotrophic growth. Total mineralization of organic matter is carried out by a complex microbial system consisting of fermentative heterotrophs, which use elemental sulfur as an electron sink, and sulfur-respiring bacteria of the genus Desulfurella , which oxidize other fermentation products, yielding only CO_f2 and H_f2S. The most remarkable thermophilic microbial community is the thermophilic cyanobacterial mat found in the Uzon caldera, Kamchatka, which contains elemental sulfur among the layers. Organic matter produced by the thermophilic Oscillatoria is completely and rapidly mineralized by means of sulfur reduction.     

Reverse gyrase, a hallmark of the hyperthermophilic archaebacteria.

Investigation of the presence of a reverse gyrase-like activity in archaebacteria revealed wide distribution of this activity in hyperthermophilic species, including methanogens and sulfur-dependent organisms. In contrast, no reverse gyrase activity was detected in mesophilic and moderately thermophilic organisms, which exhibited only an ATP-independent activity of DNA relaxation. These results suggest that the presence of reverse gyrase in archaebacteria is tightly linked to the high growth temperatures of these organisms. With respect to antigenic properties, the enzyme appeared similar among members of the genus Sulfolobus. In contrast, no close antigenic relatedness was found between the reverse gyrase of members of the order Sulfolobales and that of the other hyperthermophilic organisms.     

Transsulfuration in archaebacteria.

The transfer of sulfur from methionine to cysteine in the archaebacteria Sulfolobus acidocaldarius and Halobacterium marismortui was studied by feeding 34S-labeled methionine to cells and measuring the incorporation of 34S into protein-bound cellular cysteine and methionine by mass spectrometry. It was found that, as are eucaryotes, both of these archaebacteria were able to convert the sulfur of methionine to cysteine.     

Anaerobic life at extremely high temperatures

Continental and submarine solfataric fields turned out to contain various extremely thermophilic anaerobic organisms which all belong to the archaebacteria. They are living autotrophically on sulphur, hydrogen and CO₂ or by methanogenesis or heterotrophically on different organic substrates by sulphur respiration or, less frequently, by fermentation. The most extremely thermophilic isolates are growing between 80 and 110°C with an optimum around 105°C.     

Acdidophilic thermophilic archaebacteria: Potential application for metals recovery

Abstract The acidophilic thermophilic archaebacteria Sulfolobus and Acidianus have the potential for applid use in the recovery of metal values from ores through the process of baterial leaching. These microbes readily adapt to the conditions of low pH and high concentrations of metals required for bacterial leaching. In addition, these archaebacteria can exist at high temperatures which can occur during the oxidation of metal sulfides in bioleaching reactors. The acidophilic of copper and molybdenum from chalcopyrite and molybdenite minerals, respectively. The microbes can also enhance the recovery of gold by oxidation of pyrite which occludes gold preventing recovery by standard metallurgical procedures. The ability of this group of microbes to facilitate metals recovery is yet to be developed on a commercial scale.