Bacterial diversity of the Inner Mongolian Baer Soda Lake as revealed by 16S rRNA gene sequence analyses

Bacterial diversity associated with Baer Soda Lake in Inner Mongolia of China was investigated using a culture-independent method. Bacterial 16S rRNA gene libraries were generated using bacterial oligonucleotide primers, and 16S rRNA gene sequences of 58 clones were analyzed phylogenetically. The library was dominated by 16S rDNAs of Gram-negative bacteria (24% -Proteobacteria, 31% -Proteobacteria, 33% -Proteobacteria, and 2% -Proteobacteria), with a lower percentage of clones corresponding to Gram-positive bacteria. Forty cloned sequences were similar to that of known bacterial isolates (>97% sequence similarity), represented by the species of the genera Brevundimonas, Comamonas, Alcaligenes, Stenotrophomonas, and Klebsiella. Eighteen cloned sequences showed less affiliation with known taxa (<97% sequence similarity) and may represent novel taxa.Communicated by K. Horikoshi     

Microbial Diversity in Sediments Collected from the Deepest Cold-Seep Area, the Japan Trench

The Japan Trench land slope at a depth of 6,400 m is the deepest cold-seep environment with Calyptogena communities. Sediment samples from inside and beside the Calyptogena communities were collected, and the microbial diversity in the sediment samples was studied by molecular phylogenetic techniques. From DNA extracted directly from the sediment samples, 16S rDNAs were amplified by the polymerase chain reaction method. The sequences of the amplified 16S rDNAs selected by restriction fragment length polymorphism analysis were determined and compared with sequences in DNA databases. The results showed that 33 different bacterial 16S rDNA sequences from the two samples analyzed fell into similar phylogenetic categories, the α-, γ-, δ-, and ɛ-subdivisions of Proteobacteria, Cytophaga, and gram-positive bacteria; some of the 16S rDNA sequences were common to both samples. δ- and ɛ-Proteobacteria-related sequences were abundant in both sediments. These sequences are mostly related to sulfate-reducing or sulfur-reducing bacteria and epibionts, respectively. Eight different archaeal 16S rDNA sequences were cloned from the sediments. The majority of the archaeal 16S rDNA sequences clustered in Crenarchaeota and showed high similarities to marine group I archaeal rDNA. A Methanococcoides burtonii–related sequence obtained from the sediment clustered in the Euryarchaeota indicating that M. burtonii–related strains in the area of Calyptogena communities may contribute to production of methane in this environment. From these results, we propose a possible model of sulfur circulation within the microbial community and that of Calyptogena clams in the cold-seep environment. Received June 15, 1998; accepted November 10, 1998.     

Vertical distribution and diversity of bacteria and archaea in sulfide and methane-rich cold seep sediments located at the base of the Florida Escarpment

The bacterial and archaeal communities of the sediments at the base of the Florida Escarpment (Gulf of Mexico, USA) were investigated using molecular phylogenetic analysis. The total microbial community DNA of each of three vertical zones (top, middle and bottom) of a sediment core was extracted and the 16S rRNA genes were amplified by PCR, cloned and sequenced. Shannon–Weaver Diversity measures of bacteria were high in all three zones. For the archaea, diversity was generally low, but increased with depth. The archaeal clonal libraries were dominated by representatives of four groups of organisms involved in the anaerobic oxidation of methane (ANME groups). Phylogenetic analysis of bacteria suggests the dominance of -proteobacteria in the top zone, the -, - and -proteobacteria in the middle zone and the -proteobacteria in the bottom zone of the core. Members of the Cytophaga–Flexibacter–Bacteroidetes group, the Chloroflexi/green non-sulfur bacteria, the Gram+ (Firmicutes), the Planctomyces, candidate division WS3 and Fusobacterium were also detected. Our data suggest that the community structure and diversity of microorganisms can shift greatly within small vertical distances, possibly in response to changes in the physical and chemical conditions.     

Microbial Communities Associated with Electrodes Harvesting Electricity from a Variety of Aquatic Sediments

The microbial communities associated with electrodes from underwater fuel cells harvesting electricity from five different aquatic sediments were investigated. Three fuel cells were constructed with marine, salt-marsh, or freshwater sediments incubated in the laboratory. Fuel cells were also deployed in the field in salt marsh sediments in New Jersey and estuarine sediments in Oregon, USA. All of the sediments produced comparable amounts of power. Analysis of 16S rRNA gene sequences after 3–7 months of incubation demonstrated that all of the energy-harvesting anodes were highly enriched in microorganisms in the -Proteobacteria when compared with control electrodes not connected to a cathode. Geobacteraceae accounted for the majority of -Proteobacterial sequences or all of the energy-harvesting anodes, except the one deployed at the Oregon estuarine site. Quantitative PCR analysis of 16S rRNA genes and culturing studies indicated that Geobacteraceae were 100-fold more abundant on the marine-deployed anodes versus controls. Sequences most similar to microorganisms in the family Desulfobulbaceae predominated on the anode deployed in the estuarine sediments, and a significant proportion of the sequences recovered from the freshwater anodes were closely related to the Fe(III)-reducing isolate, Geothrix fermentans. There was also a specific enrichment of microorganisms on energy harvesting cathodes, but the enriched populations varied with the sediment/water source. Thus, future studies designed to help optimize the harvesting of electricity from aquatic sediments or waste organic matter should focus on the electrode interactions of these microorganisms which are most competitive in colonizing anodes and cathodes.This revised version was published online in November 2004 with corrections to Volume 48.     

Molecular Characterization and In Situ Localization of Endosymbiotic 16S Ribosomal RNA and RuBisCO Genes in the Pogonophoran Tissue

Gutless pogonophorans are generally thought to live in symbiosis with methane-oxidizing bacteria (methanotrophs). We identified a 16S ribosomal RNA gene (rDNA) and a ribulose-1,5-bisphosphate carboxlase/oxygenase (RuBisCO, E.C.4.1.1.39) gene that encode the form I large subunit (cbbL) from symbiont-bearing tissue of the pogonophoran Oligobrachia mashikoi. Phylogenetic analysis of the 16S rDNA sequence suggested that the pogonophoran endosymbiont belonged to the -subdivision of Proteobacteria. The endosymbiont was most closely related to an uncultured bacterium from a hydrocarbon seep, forming a unique clade adjacent to the known methanotrophic 16S rDNA cluster. The RuBisCO gene from the pogonophoran tissue was closely related to those of the chemoautotrophic genera Thiobacillus and Hydrogenovibrio. Presence of the RuBisCO gene suggested a methanotrophic symbiosis because some methanotrophic bacteria are known to be capable of autotrophy via the Calvin cycle. In contrast, particulate and soluble methane monooxygenase genes (pmoA and mmoX) and the methanol dehydrogenase gene (mxaF), which are indicators for methanotrophs or methylotrophs, were not detected by repeated trial of polymerase chain reaction. For 16S rRNA and RuBisCO genes, endosymbiotic localizations were confirmed by in situ hybridization. These results support the possibilities that the pogonophoran host has a novel endosymbiont which belongs to the -subdivision of Proteobacteria, and that the endosymbiont has the gene of the autotrophic enzyme RuBisCO.     

Evolutionary relationships of bacterial and archaeal glutamine synthetase genes

Glutamine synthetase (GS), an essential enzyme in ammonia assimilation and glutamine biosynthesis, has three distinctive types: GSI, GSII and GSIII. Genes for GSI have been found only in bacteria (eubacteria) and archaea (archaebacteria), while GSII genes only occur in eukaryotes and a few soil-dwelling bacteria. GSIII genes have been found in only a few bacterial species. Recently, it has been suggested that several lateral gene transfers of archaeal GSI genes to bacteria may have occurred. In order to study the evolution of GS, we cloned and sequenced GSI genes from two divergent archaeal species: the extreme thermophile Pyrococcus furiosus and the extreme halophile Haloferax volcanii. Our phylogenetic analysis, which included most available GS sequences, revealed two significant prokaryotic GSI subdivisions: GSI-a and GSI-. GSIa-genes are found in the thermophilic bacterium, Thermotoga maritima, the low G+C Gram-positive bacteria, and the Euryarchaeota (includes methanogens, halophiles, and some thermophiles). GSI--type genes occur in all other bacteria. GSI-- and GSI--type genes also differ with respect to a specific 25-amino-acid insertion and adenylylation control of GS enzyme activity, both absent in the former but present in the latter. Cyanobacterial genes lack adenylylation regulation of GS and may have secondarily lost it. The GSI gene of Sulfolobus solfataricus, a member of the Crenarchaeota (extreme thermophiles), is exceptional and could not be definitely placed in either subdivision. The S. solfataricus GSI gene has a shorter GSI--type insertion, but like GSI-a-type genes, lacks conserved sequences about the adenylylation site. We suspect that the similarity of GSI- genes from Euryarchaeota and several bacterial species does not reflect a common phylogeny but rather lateral transmission between archaea and bacteria.Correspondence to: J.R. Brown 1073     

Genes encoding light-harvesting and reaction center proteins from Chromatium vinosum

Sequencing of a 3.4 kb DNA fragment isolated from the photosynthetic purple sulfur bacterium Chromatium vinosum and of PCR products has resulted in identification of the Chr. vinosum pufL, pufM, and pufC genes, reading from the 5 to the 3 direction, and coding, respectively, for the L, M and cytochrome c subunits of the reaction center of this bacterium. Other PCR products have been used to obtain complete sequences for the pufB and pufA genes, located immediately upstream from pufL and encoding the apoproteins of two Chr. vinosum light- harvesting proteins. The 3-portion of the bchZ gene, a gene that codes for a protein involved in the biosynthesis of bacteriochlorophyll, has been located immediately upstream from pufB. A second pufB gene, pufB2, has been located downstream from pufC, as has the 5-portion of a second pufA gene, pufA2. The location of a second set of pufB and pufA genes, encoding light- harvesting proteins, downstream from pufC has not previously been reported for any photosynthetic bacterium. Translation of the gene sequences encoding these Chr. vinosum light-harvesting proteins reveals both similarities to and differences from the amino acid sequences, obtained from direct sequencing of the apoproteins, previously reported for Chr. vinosum light-harvesting proteins. Translation of these gene sequences, and of those for pufL, pufM and pufC, revealed significant homology, at the amino acid level, to the corresponding peptides of photosynthetic purple non-sulfur bacteria.     

Cloning and characterization of genes coding for ribosomal RNA inCampylobacter jejuni

The DNA fragments coding for ribosomal RNA inCampylobacter jejuni have been cloned from a genomic library ofC. jejuni constructed inEscherichia coli. Clones carrying DNA Sequences for rRNA were identified by hybridization of 5-end-labeled rRNA fromC. jejuni to colony blots of transformants from this gene library. Cloned DNA sequences homologous to each of 5S, 16S, and 23S rRNA were idenfified by hybridization of labeled plasmid DNA to Northern blots of rRNA. The gene coding for 23S rRNA was found to be located on a 5.5kb HindIII fragment, while the 5S and 16S rRNA genes were on HindIII fragments of 1.65 and 1.7 kb, respecitively. The DNA fragment containing the 16S rRNA gene was characterized by restriction endonuclease mapping, and the location of the 16S rRNA gene on this fragment was determined by hybridization of 5-end-labeled rRNA to restriction fragments and also by DNA sequence determination. It appears that the major portion of the coding region for 16S rRNA is located on the 1.7-kb HindIII fragment, while a small portion is carried on an adjacent HindIII fragment of 7.5 kb. Cloned rRNA genes fromC. jejuni were used to study the organization of the rDNA inC. jejuni and other members of the genùsCampylobacter.     

Isolation and identification of bacteria from spent nuclear fuel pools

The aim of the present research was to isolate and identify bacteria from spent nuclear fuel pools of a Spanish nuclear power plant. Water samples were collected and inoculated onto different culture media to isolate the highest number of species. 16S rDNA fragments from colonies growing on solid media were amplified and analysed by denaturing gradient gel electrophoresis. Sequencing revealed the presence of 21 different bacteria belonging to several phylogenetic groups (, , and -Proteobacteria, Actinomycetales, Flavobacterium, and the Bacillus/Staphylococcus group). The isolation of these microorganisms in this particular environment (oligotrophic and radioactive) is highly interesting because of the possibility of their being used for the bioremediation of radionuclide-contaminated waters.     

A mathematical model for the growth of bacterial microcolonies on marine sediment

Counts of bacterial microcolonies attached to deep-sea sediment particles showed 4-, 8-, 16-, and 32-celled microcolonies to be very rare. This was investigated with a mathematical model in which microcolonies grew from single cells at a constant growth rate (), detached from particles at constant rate (), and reattached as single cells. Terms for attachment of foreign bacteria (a) and death of single cells (d) were also included. The best method of fitting the model to the microcolony counts was a weighted least-squares approach by which(0.83 hour^–1) was estimated to be about 20 times greater than(0.038 hour^–1). This showed that the bacteria were very mobile between sediment particles and this mobility was explained in terms of attachment by reversible sorption. The implications of the results for the frequency of dividing cell method for estimating growth rates of sediment bacteria are discussed. The ratio of and was found to be very robust both in terms of the errors associated with the microcolony counts and the range of microcolony sizes used to obtain the solution.     

Isolation of extremophiles with the detection and retrieval of<Emphasis Type="Italic"> Shewanella</Emphasis> strains in deep-sea sediments from the west Pacific

Tests to detect the presence of piezophilic Shewanella strains in the deep-sea sediments of the west, mid- and east Pacific at different depths were done by amplification of previously identified pressure-regulated operons (ORF1,2 and ORF3). The operon fragments were detected in all the deep-sea sediment samples, indicating the broad presence of piezophilic deep-sea Shewanella species or related species in the deep-sea sediments across the Pacific. Extremophiles were isolated from the deep-sea sediment of the west Pacific under atmospheric pressure. Two psychrophilic/psychrotrophic strains, WP2 and WP3, were assigned to the Shewanella genus as determined by their 16S rDNA sequences. WP2 and WP3 were both capable of amplifying pressure-regulated operons; the sequences of the pressure-regulated operons of WP2 and WP3 share high identity between each other, but have more differences from those of S. benthica and S. violacea. The major fatty acids of WP2 and WP3 are 3OH-i-13:0, 14:0, i-15:0, 16:0, 16:1, 18:1, and 20:5. Combined phenotypic analysis, 16S rDNA sequences, and DNA–DNA hybridization results suggest that WP2 and WP3 are two new deep-sea Shewanella species.Communicated by K. Horikoshi     

Bioactive peptides encrypted in milk proteins: proteolytic activation and thropho-functional properties

The bioactivities of peptides encrypted in major milk proteins are latent until released and activated by enzymatic proteolysis, e.g. during gastrointestinal digestion or food processing. The proteolytic system of lactic acid bacteria can contribute to the liberation of bioactive peptides. In vitro, the purified cell wall proteinase of Lactococcus lactis was shown to liberate oligopeptides from - and -caseins which contain amino acid sequences present in casomorphins, casokinines, and immunopeptides. The further degradation of these peptides by endopeptidases and exopeptidases of lactic acid bacteria could lead to the liberation of bioactive peptides in fermented milk products. However, the sequences of practically all known biologically active peptides can also be cleaved by peptidases from lactic acid bacteria. Activated peptides are potential modulators of various regulatory processes in the body: Opioid peptides are opioid receptor ligands which can modulate ab sorption processes in the intestinal tract, angiotensin-I-converting enzyme (ACE)-inhibitory peptides are hemodynamic regulators and exert an antihypertensive effect, immunomodulating casein peptides stimulate the activities of cells of the immune system, antimicrobial peptides kill sensitive microorganisms, antithrombotic peptides inhibit aggregation of platelets and caseinophosphopeptides may function as carriers for different minerals, especially calcium. Bioactive peptides can interact with target sites at the luminal side of the intestinal tract. Furthermore, they can be absorbed and then reach peripheral organs. Food-derived bioactive peptides are claimed to be health enhancing components which can be used for functional food and pharmaceutical preparations.     

Molecular analyses of the sediment of the 11000-m deep Mariana Trench

We have obtained sediment samples from the world's deepest sea-bottom, the Mariana Trench challenger point at a depth of 10 898 m, using the new unmanned submersible Kaiko. DNA was extracted from the sediment, and DNA fragments encoding several prokaryotic ribosomal RNA small-subunit sequences and pressure-regulated gene clusters, typically identifed in deep-sea adapted bacteria, were amplifed by the polymerase chain reaction. From the sequencing results, at least two kinds of bacterial 16S rRNAs closely related to those of the genus Pseudomonas and deep-sea adapted marine bacteria, and archaeal 16S rRNAs related to that of a planktonic marine archaeon were identifed. The sequences of the amplifed pressure-regulated clusters were more similar to those of deep-sea barophilic bacteria than those of barotolerant bacteria. These results suggest that deep-sea adapted barophilic bacteria, planktonic marine archaea, and some of the world's most widespread bacteria (the genus Pseudomonas) coexist on the world's deepest sea-bottom. Received: October 10, 1996 / Accepted: March 3, 1997     

Phenanthrene mineralization along a natural salinity gradient in an Urban Estuary,Boston Harbor,Massachusetts

The effect of varying salinity on phenanthrene and glutamate mineralization was examined in sediments along a natural salinity gradient in an urban tidal river. Mineralization was measured by trapping¹⁴CO₂ from sediment slurries dosed with trace levels of [¹⁴C]phenanthrene or [¹⁴C]glutamate. Sediments from three sites representing three salinity regimes (0, 15, and 30%.) were mixed with filtered column water from each site. Ambient phenanthrene concentrations were also determined to calculate phenanthrene mineralization rates. Rates of phenanthrene mineralization related significantly to increasing salinity along the transect as determined by linear regression analysis. Rates ranged from 1 ng/hour/g dry sediment at the freshwater site to > 16 ng/hour/g dry sediment at the 30 salinity site. Glutamate mineralization also increased from the freshwater to the marine site; however, the relationship to salinity was not statistically significant.To examine the effect of salinity on mineralizing activities, individual sediments were mixed with filtered water of the other two sites. Slurries were also made with artificial seawater composed of 0, 15, or 30 g NaCl/ liter to substitute for overlying water. Rates of phenanthrene mineralization in the 0 ambient salinity sediments were not affected by higher salinity waters. Activities in the 15 and 30 ambient salinity sediments, however, were significantly inhibited by incubation with 0 salinity water. The inhibition, in large part, appears to be due to the decreased NaCl concentration of the water phase. Glutamate mineralization was affected in a similar manner, but not as dramatically as phenanthrene mineralization. The results suggest that phenanthrene degraders in low salinity estuarine sediments subject to salt water intrusion are tolerant to a wide range of salinities but phenanthrene degradation in brackish waters is mainly a function of obligate marine microorganisms.     

Specific 16S rDNA Sequences Associated with Naphthalene Degradation under Sulfate-Reducing Conditions in Harbor Sediments

Previous studies have demonstrated that naphthalene and other polycyclic aromatic hydrocarbons (PAHs) can be anaerobically oxidized with the reduction of sulfate in PAH-contaminated marine harbor sediments, including those in San Diego Bay. In order to learn more about the microorganisms that might be involved in anaerobic naphthalene degradation, the microorganisms associated with naphthalene degradation in San Diego Bay sediments were evaluated. A dilution-to-extinction enrichment culture strategy, designed to recover the most numerous culturable naphthalene-degrading sulfate reducers, resulted in the enrichment of microorganisms with 16S rDNA sequences in the d-Proteobacteria, which were closely related to a previously described pure culture of a naphthalene-degrading sulfate reducer, NaphS2, isolated from sediments in Germany. A more traditional enrichment culture approach, expected to enrich for the fastest-growing naphthalene-degrading sulfate reducers, yielded 16S rDNA sequences closely related to those found in the dilution-to-extinction enrichments and NaphS2. Analysis of 16S rDNA sequences in sediments from two sites in San Diego Bay that had been adapted for rapid naphthalene degradation by continual amendment with low levels of naphthalene suggested that the microbial community composition in the amended sediments differed from that present in the unamended sediments from the same sites. Most significantly, 6-8% of the sequences recovered from 100 clones of each of the naphthalene-amended sediments were closely related to the 16S rDNA sequences in the enrichment cultures as well as the sequence of the pure culture, NaphS2. No sequences in this NaphS2 phylotype were recovered from the sediments that were not continually exposed to naphthalene. A PCR primer, which was designed based on these phylotype sequences, was used to amplify additional 16S rDNA sequences belonging to the NaphS2 phylotype from PAH-degrading sediments from Island End River (Boston), MA, and Liepaja Harbor, Latvia. Closely related sequences were also recovered from highly contaminated sediment from Tampa Bay, FL. These results suggest that microorganisms closely related to NaphS2 might be involved in naphthalene degradation in harbor sediments. This finding contrasts with the frequent observation that the environmentally relevant microorganisms cannot be readily recovered in pure culture and suggests that further study of the physiology of NaphS2 may provide insights into factors controlling the rate and extent of naphthalene degradation in marine harbor sediments.     

Benthic bacterial biomass supported by streamwater dissolved organic matter

Bacterial biomass in surface sediments of a headwater stream was measured as a function of dissolved organic carbon (DOC) flux and temperature. Bacterial biomass was estimated using epifluorescence microscopic counts (EMC) and ATP determinations during exposure to streamwater containing 1,788g DOC/liter and after transfer to groundwater containing 693g DOC/liter. Numbers of bacteria and ATP concentrations averaged 1.36×10⁹ cells and 1,064 ng per gram dry sediment, respectively, under initial DOC exposure. After transfer to low DOC water, biomass estimates dropped by 53 and 55% from EMC and ATP, respectively. The decline to a new steady state occurred within 4 days from ATP assays and within 11 days from EMC measures. A 4°C difference during these exposures had little effect on generation times. The experiment indicated that 27.59 mg/hour of natural DOC supported a steady state bacterial biomass of approximately 10g C/g dry weight of sediment (from EMC determinations). Steady state bacterial biomass estimates on sediments that were previously muffled to remove organic matter were approximately 20-fold lower. The ratio of GTPATP indicated differences in physiological condition or community composition between natural and muffled sediments.     

Structural features of the plastid ribosomal RNA operons of two red algae: Antithamnion sp. and Cyanidium caldarium

The nucleotide sequences of the plastid 16S rDNA of the multicellular red alga Antithamnion sp. and the 16S rDNA/23S rDNA intergenic spacers of the plastid DNAs of the unicellular red alga Cyanidium caldarium and of Antithamnion sp. were determined. Sequence comparisons support the idea of a polyphyletic origin of the red algal and the higher-plant chloroplasts. Both spacer regions include the unsplit tRNA^Ile (GAU) and tRNA^Ala (UGC) genes and so the plastids of both algae form a homogeneous group with those of chromophytic algae and Cyanophora paradoxa characterized by small-sized rDNA spacers in contrast to green algae and higher plants. Nevertheless, remarkable sequence differences within the rRNA and the tRNA genes give the plastids of Cyanidium caldarium a rather isolated position.     

Restriction site and length polymorphism of the rDNA unit in the cultivated basidiomycetePleurotus cornucopiae

In the ribosomal DNA unit ofPleurotus cornucopiae, the rDNA coding regions are in the order 5, 5S-18S-5.8S-25S, 3, with the 5 location of the 5S gene differing from its 3 location found in other basidiomycetes. The most discriminating probe used to study the rDNA polymorphism consisted of a fragment that included the 5S, 18S and part of the 5.8S and 25S genes flanking three intergenic sequences. A high degree of rDNA polymorphism was observed in the sevenP. cornucopiae dikaryons studied. For the first time within a basidiomycete species, the restrictions maps distinguished two types of rDNA units (I and II). In each rDNA type, length variations in the external intergenic sequence IGS 1 located between the 25S and 5S genes allowed characterization of two different rDNA units in type I and four rDNA units in type II. This suggested that theP. cornucopiae rDNA units were derived from two kinds of ancestors (type I and II) by insertion or deletion events (100–700 bp) in the IGS 1. In four dikaryotic strains, two rDNA units of the same type (I or II) differing only by the IGS 1 length, were found in a similar number of copies, and presented a meiotic segregation in homokaryotic progeny. In one progeny, some homokaryotic strains possessed two different rDNA units: one with a high copy number and another with a lower one, showing that two different rDNA units could coexist in a single nucleus.     

Phylogenetic analysis of photosynthetic genes of Rhodocyclus gelatinosus: Possibility of horizontal gene transfer in purple bacteria

Nucleotide sequences of the genes coding for the M and cytochrome subunits of the photosynthetic reaction center of Rhodocyclus gelatinosus, a purple bacterium in the subdivision, were determined. The deduced amino acid sequences of these proteins were compared with those of other photosynthetic bacteria. Based on the homology of these two photosynthetic proteins, Rc. gelatinosus was placed in the subdivision of purple bacteria, which disagrees with the phylogenetic trees based on 16S rRNA and soluble cytochrome c ₂. Horizontal transfer of the genes which code for the photosynthetic apparatus in purple bacteria can be postulated if the phylogenetic trees based on 16S rRNA and soluble cytochrome c ₂ reflect the real history of purple bacteria.Abbreviations LH I light harvesting complex I - RC reaction center     

Organization of ribosomal RNA genes in Mycoplasma capricolum

Summary DNA segments carrying rRNA genes of Mycoplasma capricolum have been cloned and characterized by restriction endonuclease mapping, DNA-RNA hybridization and nucleotide sequencing. The M. capricolum genome has two sets of rRNA gene clusters, where the arrangement is in the order of (5)16S-23S-5S(3). The spacer region between 16S and 23S rDNA is extremely rich in AT and does not carry any tRNA genes. Present address: Division of Hematology and Immunology of Internal Medicine, Kanazawa Medical University, Uchinada-Cho, Kahoku-Gun Ishikawa Pref. 920-02, Japan