Green Non-sulphur Bacteria Research Articles

Prokaryotic community composition and biogeochemical processes in deep subseafloor sediments from the Peru Margin

The community compositions of Bacteria and Archaea were investigated in deep, sub-seafloor sediments from the highly productive Peru Margin (ODP Leg 201, sites 1228 and 1229, c. 25 km apart) down to nearly 200 m below the seafloor using taxonomic (16S rRNA) and functional (mcrA and dsrA) gene markers. Bacterial and archaeal groups identified from clone libraries of 16S rRNA gene sequences at site 1229 agreed well with sequences amplified from bands excised from denaturing gradient gel electrophoresis (DGGE) depth profiles, with the exception of the Miscellaneous Crenarchaeotic Group (MCG). This suggested that the prokaryotic community at site 1228, obtained from DGGE profiling alone, was reliable. Sites were dominated by Bacteria in the Gammaproteobacteria, Chloroflexi (green non-sulphur bacteria) and Archaea in the MCG and South African Gold Mine Euryarchaeotic Group, although community composition changed with depth. The candidate division JS1 was present throughout both sites but was not dominant. The populations identified in the Peru Margin sediments consisted mainly of prokaryotes found in other deep subsurface sediments, and were more similar to communities from the Sea of Okhotsk (pelagic clays) than to those from the low organic carbon Nankai Trough sediments. Despite broad similarities in the prokaryotic community at the two sites, there were some differences, as well as differences in activity and geochemistry. Methanogens (mcrA) within the Methanosarcinales and Methanobacteriales were only found at site 1229 (4 depths analysed), whereas sulphate-reducing prokaryotes (dsrA) were only found at site 1228 (one depth), and these terminal-oxidizing prokaryotes may represent an active community component present at low abundance. This study clearly demonstrates that the deep subsurface sediments of the Peru Margin have a large diverse and metabolically active prokaryotic population.

Real-time PCR for quantification of aerobic anoxygenic phototrophic bacteria based on pufM gene in marine environment

The abundance of aerobic anoxygenic phototrophic bacteria (AAPB), a new functional group that plays important roles in marine carbon cycling, is determined frequently by infrared epifluorescence microscopic analysis (IREM) or high-performance liquid chromatography (HPLC) based on detecting BChl a (bacteriochlorophyll a) fluorescence signal at 880 nm. Unfortunately, the fluorescence signal is often influenced by environmental variables and physiological state of cell. Here we developed a real-time quantitative PCR (qPCR) assay based on pufM gene to specifically quantify AAPB in marine environments. High specificity and sensitivity for estimation of AAPB abundance were revealed by analysis of amplification products, melting curves and target sequences. The phylogenetic tree indicated that this primer set is suitable for a wide genetic diversity of AAPB, including α-3, α-4 Proteobacteria and clones of unclear taxonomic position. In contrast, no amplicon was obtained from green non-sulphur bacteria and oxygenic phototrophic bacteria such as Cyanobacterial genomic DNA. The melting behavior could indicate predominant phenotypes in AAPB community in addition to validating the products of qPCR. The AAPB was estimated to range from 1.3 × 10 4 cell/ml to 3.4 × 10 5 cell/ml in our 10 tested water samples by this qPCR assay. Further investigations on the abundance distribution of AAPB in marine environments using the qPCR assay may provide new insight into their ecological functions.

Carotenoid biosynthetic pathway: molecular phylogenies and evolutionary behavior of crt genes in eubacteria

Phylogenetic analysis of carotenoid biosynthetic pathway genes and their evolutionary rate variations were studied among eubacterial taxa. The gene sequences for the enzymes involved in this pathway were obtained for major phylogenetic groups of eubacteria (green sulfur bacteria, green nonsulphur bacteria, Gram-positive bacteria, proteobacteria, flavobacteria, cyanobacteria) and archeabacteria. These gene datasets were distributed under five major steps of carotenoid biosynthesis in eubacteria; isoprenoid precursor biosynthesis, phytoene synthesis, dehydrogenation of phytoene, lycopene cyclization, formation of acyclic xanthophylls, formation of cyclic xanthophylls and carotenoid biosynthesis regulation. The NJ algorithm was used on protein coding DNA sequences to deduce the evolutionary relationship for the respective crt genes among different eubacterial lineages. The rate of nonsynonymous nucleotide substitutions per nonsynonymous site ( d N) and synonymous nucleotide substitutions per synonymous site ( d S) were calculated for different clades of the respective phylogenetic tree for specific crt genes. The phylogenetic analysis suggests that evolutionary pattern of crt genes in eubacteria is characterized by lateral gene transfer and gene duplication events. The d N values indicate that carotenoid biosynthetic genes are more conserved in proteobacteria than in any other eubacterial phyla. Furthermore, of the genes involved in carotenoid biosynthesis pathway, structural genes evolve slowly than the regulatory genes in eubacteria.

Use of low nutrient enrichments to access novel amylase genes in silent diversity of thermophiles

By combining low nutrient enrichments and molecular methods, a high diversity of new amylase genes was detected in a neutral sulphide-rich hot spring in Iceland. Enrichments based on hot spring water and low concentrations of starch were used to select slow-growing, starch-degrading microorganisms. Six enrichments had in total 17 bacterial types detected by 16S rRNA analysis, mostly related to the Thermus-Deinococcus group, green non-sulphur bacteria, gram positives, and uncultivated new candidate divisions. No Archaea were found. The apparent 16S rRNA species composition of the enrichments was very different from that of the microbial mat in the same hot spring. DNA samples obtained from 4 enrichments and from hot spring biomass were screened by PCR for amylase genes in glycoside-hydrolase family 13. Degenerate primers, based on conserved amino acid sequences from multiple␣alignments of family 13, enabled the detection of 18 amylase sequence types in the enrichments, including α-amylases, α-glucosidases, 1,4-α-glucan branching enzymes, cyclomaltodextrin hydrolases, maltogenic amylases and neopullulanases, and unspecified family 13 glycoside-hydrolases. Only one unique neopullulanase sequence, also found in most of the enrichments, was detected in the hot spring biomass DNA. The results suggest that the enrichment method combined with sequence-based screening is an efficient way to access the silent, i.e. not detectable, gene diversity in natural environments.

Analysis and comparison of the microbial community structures of two enrichment cultures capable of reductively dechlorinating TCE and cis-DCE.

In order to study the effect of different chloroethenes (electron acceptors) on the bacterial composition of dechlorinating communities, two reductive dechlorinating enrichment cultures were developed that were able to reduce trichloroethene (TCE) and cis-1,2-dichloroethene (cis-DCE) to ethene using hydrogen as electron donor, respectively. The inoculum for the cultures was material from a methanogenic fluidized bed reactor (FBR), which was originally seeded with digester sludge and showed a stable capacity for tetrachloroethene (PCE) reduction to ethene for over six years. Molecular methods were used to determine and compare the microbial communities of these two enrichment cultures. A clone library of bacterial 16S rRNA genes was generated for each enrichment. The clones were screened into different groups by restriction fragment length polymorphism (RFLP) analysis using two different four base pair recognition restriction enzymes. A total of 12 sequence types were identified by phylogenetic analysis of nearly complete 16S rDNA sequences ( approximately 1450 bp). The sequences were affiliated with six recognized phyla of the domain Bacteria: Firmicutes (low G+C Gram-positives), Chloroflexi (green non-sulphur bacteria), Actinobacteria (high G+C Gram-positives), Bacteroidetes (Cytophaga-Flexibacter-Bacteroides), Nitrospira and Spirochaetes. The results led to the identification of an organism closely related to Dehalococcoides ethenogenes to be the presumptive dechlorinator in both enrichments. Different electron acceptors affected the bacterial diversity and the community profiles of the two enrichments. Most of the sequences identified in our dechlorinating enrichments shared high similarities with sequences previously obtained from other enriched dechlorinating cultures and chlorinated-compound-contaminated sediments or aquifers, suggesting these bacteria may have direct or indirect roles in reductive dechlorination.

Opal-A and associated microbes from Wairakei, New Zealand: the first 300 days

AbstractAll samples of silica sinter, <2 y old taken from the discharge drain of the Wairakei geothermal power station and the Rainbow Terrace of Orakei Korako, consist of non-crystalline opal-A. This silica phase deposits directly upon the concrete drain wall and filamentous templets, extending from this wall, afforded by the microbial community present in the drain, whose nature was determined by a culture- independent strategy that entailed construction, fingerprinting and sequencing of a 16S clone library. The bacterial community is dominated by five major groups of organisms, present in approximately equal proportions, and which account for ∼50% of the community. None of the 16S sequences from these dominant groups yielded a perfect match with 16S sequences for named organisms in the international databases. However one dominant group clusters withHydrogenophilus thermoluteus,a thermophilic filamentous bacterium, and two cluster with putatively thermophilic members of theCyanobacteriaand green non-sulphur bacteria respectively. Initial opal-A deposits rapidly as agglomerations of silica nanospheres that, in turn, form chains of coalesced, oblate, microspheres <0.4 x 0.2 mm about the barbicel-like filaments, to produce a mat of fine woven strands. The majority of individual filaments are <8 μm long and 0.8 mm wide but may be up to 55 mm long by 1 mm wide. Where laminar flow dominates, most strands develop parallel to the drain current but some strands crisscross while others protrude above the mat surface. Where flow is turbulent, strands lack preferred orientation and some adopt a helical form. In general, following deposition, the values of the scattering broadband at half (FWHM) and three quarters (FWTM) of the maximum intensity decrease with increasing sample age. The behaviour of the band at one quarter maximum intensity (FWQM) is less consistent, but, in general, the youngest sinters possess the highest FWQM, FWHM and FWTM values that prove independent of fabric type. Opal-A silica matures following its removal from the parent fluid, especially where the sinter surface is filmed by water. A continual movement of silica is shown by a second generation of microspheres formed on the silica mat surface, by an increase in size of the initial microspheres, and by an increase in maximum intensity of the X-ray scattering broadbands. Similar silica aging behaviour occurs among young sinters developed upon microbial mats at Orakei Korako. The deposition and aging processes accord with the known behaviour of juvenile opaline silica in both natural and artificial systems whose pH, temperature and dissolved salt content are similar to Wairakei and Rainbow terrace: gelling of silica is favoured by the high pH (∼8.3) and temperature (∼60°C) of the Wairakei discharge fluid but the high dissolved salt content of the water (Na+= 930 μg/g, Ca2+= 12 μg/g, Cl = 1500 μg/g) and abundant microbial community facilitate rapid and copious flocculation of solid silica within the drain, in contrast to the slower accumulation on the natural sinter terrace at lower temperature (30—45°C) from less saline dilute bicarbonate-chloride waters (Na+= 180 μg/g, Ca2+= 0.2 μg/g, Cl = 400 μg/g, pH = 8.1).

Phylogenetic 16S rRNA analysis reveals the presence of complex and partly unknown bacterial communities in Tito Bustillo cave, Spain, and on its Palaeolithic paintings.

Tito Bustillo cave (Ribadesella, Spain) contains valuable Palaeolithic paintings, which date back 15 000-20 000 years. Since 1969, the cave has been open to the public. Rock wall surfaces, spelaeothems and soils are covered by apparent biofilms of phototrophic microorganisms, which develop under artificial lighting. In addition, rock surfaces present conspicuous bacterial growth in the form of round colonies of different colours and about 1-2 mm in diameter. Even the famous Paintings Panel shows some evident microbial growth. In the present study, bacterial communities on the paintings and on the rock surfaces near the paintings were analysed by culture-independent techniques, including polymerase chain reaction (PCR) amplification of bacterial 16S rRNA genes (16S rDNA), phylogenetic sequence analyses and genetic community fingerprinting by denaturing gradient gel electrophoresis (DGGE). DGGE fingerprints showed complex bacterial community patterns. Forty-one clones matching DGGE bands of the community fingerprints were sequenced, representing about 39% of DNA fragments in the DGGE patterns. Phylogenetic sequence analyses revealed a high number of phylogenetically novel 16S rDNA sequence types and a high diversity of putatively chemotrophic and heterotrophic bacteria. Sequences were phylogenetically most closely related to the Proteobacteria (20 clones), green non-sulphur bacteria (three clones), Planctomycetales order (one clone), Cytophaga-Flexibacter- Bacteroides division (one clone) and the Actinobacteria (four clones). Furthermore, we report the presence of members of the Acidobacterium division (12 clones) in a karstic hypogean environment. Members of this phylum have not so far been detected in these particular environments.

Identification of a microorganism that links its growth to the reductive dechlorination of 2,3,5,6-chlorobiphenyl.

Anaerobic bacteria reductively dechlorinate polychlorinated biphenyls (PCBs) in aquatic sediments, but these microorganisms remain uncultured and, until now, unidentified. Through denaturing gradient gel electrophoresis (DGGE) of 16S rDNA from a highly enriched ortho-PCB dechlorinating culture, the growth of a single microorganism was shown to be dependent upon the presence and dechlorination of 2,3,5,6-tetrachlorobiphenyl. This is the first identification of a microorganism that catalyses the reductive dechlorination of a PCB. The organism, bacterium o-17, has high sequence similarity with the green non-sulphur bacteria and with a group that includes Dehalococcoides ethenogenes. Bacterium o-17 required acetate for dechlorination and growth. H2:CO2 (80:20 at 101 kPa) did not support dechlorination or growth of the dechlorinator. Archaeal 16S rDNA was not detected in actively dechlorinating bromoethanesulphonate-treated non-methanogenic cultures, which indicated that methanogenic Archaea were not required for dechlorination. The consistent association with dechlorinating activity combined with high similarity to other known dechlorinating microorganisms indicates that bacterium o-17 catalyses the reductive ortho-dechlorination of 2,3,5,6-tetrachlorobiphenyl.

The use of signature sequences in different proteins to determine the relative branching order of bacterial divisions: evidence that Fibrobacter diverged at a similar time to Chlamydia and the Cytophaga-Flavobacterium-Bacteroides division.

The phylogenetic placement of the rumen bacterium Fibrobacter succinogenes was determined using a signature sequence approach that allows determination of the relative branching order of the major divisions among Bacteria [Gupta, R. S. (2000) FEMS Microbiol Rev 24, 367-402]. For this purpose, segments of the Hsp60 (groEL), Hsp70 (dnaK), CTP synthase and alanyl-tRNA synthetase genes, which are known to contain signature sequences that are useful for phylogenetic deterministic purposes, were cloned. Using degenerate oligonucleotide primers for highly conserved regions in these proteins, 1.4 kb, 0.75 kb, 401 bp and 171 bp fragments of the Hsp70, Hsp60, CTP synthase and alanyl-tRNA synthetase genes respectively were amplified by PCR, and these fragments were cloned and sequenced. These primers, because of their high degree of conservation, could also be used for cloning these genes from other bacterial species. The Hsp70 homologues from different Gram-negative bacteria contain a 21-23 aa insert that is not found in any Gram-positive bacteria. The presence of this insert in the F. succinogenes Hsp70 supports its placement within the Gram-negative group of bacteria. A conserved insert in F. succinogenes Hsp60 that is commonly present in all bacterial species, except various Gram-positive bacteria, Deinococcus-Thermus groups and green non-sulphur bacteria, provides evidence that F. succinogenes does not belong to these taxa. A particularly useful signature consisting of a 4 aa insert is found in Ala-tRNA synthetase. This insert is present in all proteobacterial homologues as well as in homologues from species belonging to the Chlamydia and Cytophaga-Flavobacterium- Bacteroides (CFB) groups, but it is not found in homologues from any other groups of bacteria. The presence of this insert in F. succinogenes Ala-tRNA synthetase provides evidence that this species is related to these groups. However, two other signatures in CTP synthase and Hsp70 proteins, that are distinctive of the proteobacterial species, are not present in the F. succinogenes homologues. These results provide evidence that F. succinogenes does not belong to the proteobacterial division and thus should be placed in a similar position as the Chlamydia and CFB groups of species.

Autotrophy of green non-sulphur bacteria in hot spring microbial mats: biological explanations for isotopically heavy organic carbon in the geological record.

Inferences about the evidence of life recorded in organic compounds within the Earth's ancient rocks have depended on 13C contents low enough to be characteristic of biological debris produced by the well-known CO2 fixation pathway, the Calvin cycle. 'Atypically' high values have been attributed to isotopic alteration of sedimentary organic carbon by thermal metamorphism. We examined the possibility that organic carbon characterized by a relatively high 13C content could have arisen biologically from recently discovered autotrophic pathways. We focused on the green non-sulphur bacterium Chloroflexus aurantiacus that uses the 3-hydroxypropionate pathway for inorganic carbon fixation and is geologically significant as it forms modern mat communities analogous to stromatolites. Organic matter in mats constructed by Chloroflexus spp. alone had relatively high 13C contents (-14.9%) and lipids diagnostic of Chloroflexus that were also isotopically heavy (-8.9% to -18.5%). Organic matter in mats constructed by Chloroflexus in conjunction with cyanobacteria had a more typical Calvin cycle signature (-23.5%). However, lipids diagnostic of Chloroflexus were isotopically enriched (-15.1% to -24.1%) relative to lipids typical of cyanobacteria (-33.9% to -36.3%). This suggests that, in mats formed by both cyanobacteria and Chloroflexus, autotrophy must have a greater effect on Chloroflexus carbon metabolism than the photoheterotrophic consumption of cyanobacterial photosynthate. Chloroflexus cell components were also selectively preserved. Hence, Chloroflexus autotrophy and selective preservation of its products constitute one purely biological mechanism by which isotopically heavy organic carbon could have been introduced into important Precambrian geological features.

Evolutionary relationships among photosynthetic prokaryotes (Heliobacterium chlorum, Chloroflexus aurantiacus, cyanobacteria, Chlorobium tepidum and proteobacteria): implications regarding the origin of photosynthesis.

The presence of shared conserved insertions or deletions in proteins (referred to as signature sequences) provides a powerful means to deduce the evolutionary relationships among prokaryotic organisms. This approach was used in the present work to deduce the branching orders of various eubacterial taxa consisting of photosynthetic organisms. For this purpose, portions of the Hsp60 and Hsp70 genes, covering known signature sequence regions, were PCR-amplified and sequenced from Heliobacterium chlorum, Chloroflexus aurantiacus and Chlorobium tepidum. This information was integrated with sequence data for several other proteins from numerous species to deduce the branching orders of different photosynthetic taxa. Based on signature sequences that are present in different proteins, it is possible to infer that the various eubacterial phyla evolved from a common ancestor in the following order: low G+C Gram-positive (H. chlorum) --> high G+C Gram-positive --> Deinococcus-Thermus --> green non-sulphur bacteria (Cf. aurantiacus ) --> cyanobacteria --> spirochaetes --> Chlamydia-Cytophaga-Aquifex-flavobacteria-green sulphur bacteria (Cb. tepidum) --> proteobacteria (alpha, delta and epsilon) and --> proteobacteria (beta and gamma). The members of the Heliobacteriaceae family that contain a Fe-S type of reaction centre (RC-1) and represent the sole photosynthetic phylum from the Gram-positive or monoderm group of prokaryotes are indicated to be the most ancestral of the photosynthetic lineages. Among the Gram-negative bacteria or diderm prokaryotes, green non-sulphur bacteria such as Cf. aurantiacus, which contains a pheophytin-quinone type of reaction centre (RC-2), are indicated to have evolved very early. Thus, the organisms containing either RC-1 or RC-2 existed before the evolution of cyanobacteria, which contain both these reaction centres to carry out oxygenic photosynthesis. The eubacterial divisions consisting of green sulphur bacteria and proteobacteria are indicated to have diverged after cyanobacteria. Some implications of these results concerning the origin of photosynthesis and the earliest prokaryotic fossils are discussed.

Biological Versus Abiological Mechanisms Explaining Isotopically Heavy Isua Organic Matter

The anomalously heavy organic carbon from Isua rocks of 3.8 billion years ago has been explained as an artifact of metamorphism (Schidlowski, 1988). The 613C value of -13.0+4.9%o does not fit within the a13C values 'characteristic' for biological debris (Hayes, 1996). The relatively small 13C content of organic matter considered 'typical' for biological CO2 fixation is based on the assumption that the Calvin cycle is the major CO2 fixation pathway and that other carbon fixation pathways with different carbon isotope fractionation effects have played a minor role in the Earth's history. However, assuming that the Isua organic matter is of a Calvin cycle origin the effect of metamorphism on the ~3C content of the organic matter must have been large, an increase of more than 10%o. Recently the effect of metamorphism on the ~3C content of organic matter is being discussed and an increase in 13C of 2-3~ due to metamorphism has been suggested (Watanabe et al., 1997; DesMarais, 1997). This implies that the 13C value of the original Isua organic matter of- 15 to - 16%0. Based on analyses of organic matter produced by green non-sulphur bacteria preserved in modern laminated microbial mat systems resembling stromatolites, a biological alternative for the heavy organic matter in the Isua formation is suggested. The organic matter produced by these bacteria, representing an early divergence from the tree of life, is substantially enriched in 13C relative to organic matter assimilated via the Calvin cycle. Chloroflexus aurantiacus, such a green non-sulphur bacterium, uses the 3-hydroxypropionate pathway for carbon fixation (Holo and Sirevag, 1986). This pathway

5S rRNA sequences of representatives of the genera Chlorobium, Prosthecochloris, Thermomicrobium, Cytophaga, Flavobacterium, Flexibacter and Saprospira and a discussion of the evolution of eubacteria in general

5S rRNA sequences were determined for the green sulphur bacteria Chlorobium limicola, Chlorobium phaeobacteroides and Prosthecochloris aestuarii, for Thermomicrobium roseum, which is a relative of the green non-sulphur bacteria, and for Cytophaga aquatilis, Cytophaga heparina, Cytophaga johnsonae, Flavobacterium breve, Flexibacter sp. and Saprospira grandis, organisms allotted to the phylum 'Bacteroides-Cytophaga-Flavobacterium' and relatives as determined by 16S rRNA analyses. By using a clustering algorithm a dendrogram was constructed from these sequences and from all other known eubacterial 5S RNA sequences. The dendrogram showed differences, as well as similarities, with respect to results obtained by 16S RNA analyses. The 5S RNA sequences of green sulphur bacteria were closely related to one another, and to a cluster containing 5S RNA sequences from Bacteroides and its relatives, including Cytophaga aquatilis. 5S RNA sequences of all other representatives of the 'Bacteroides-Cytophaga-Flavobacterium' phylum as distinguished by 16S RNA analysis failed to group with Bacteroides and related clusters. On the basis of 5S RNA sequences, Thermomicrobium roseum clustered with Chloroflexus aurantiacus, as was expected from 16S RNA analysis.