What are archaebacteria: life's third domain or monoderm prokaryotes related to Gram-positive bacteria? A new proposal for the classification of prokaryotic organisms

The evolutionary relationship within prokaryotes is examined based on signature sequences (defined as conserved inserts or deletions shared by specific taxa) and phylogenies derived from different proteins. Archaebacteria are indicated as being monophyletic by a number of proteins related to the information transfer processes. In contrast, for several other highly conserved proteins, common signature sequences are present in archaebacteria and Gram-positive bacteria, whereas Gram-negative bacteria are indicated as being distinct. For these proteins, archaebacteria do not form a phylogenetically distinct clade but show polyphyletic branching within Gram-positive bacteria. A closer relationship of archaebacteria to Gram-positive bacteria in comparison with Gram-negative bacteria is generally seen for the majority of the available gene/protein sequences. To account for these results and the fact that both archaebacteria and Gram-positive bacteria are prokaryotes surrounded by a single cell membrane, I propose that the primary division within prokaryotes is between monoderm prokaryotes (surrounded by a single membrane) and diderm prokaryotes (i.e. all true Gram-negative bacteria containing both an inner cytoplasmic membrane and an outer membrane). This proposal is consistent with both cell morphology and signature sequences in different proteins. The monophyletic nature of archaebacteria for some genes, and their polyphyletic branching within Gram-positive bacteria as suggested by others, is critically examined, and several explanations, including derivation of archaebacteria from Gram-positive bacteria in response to antibiotic selection pressure, are proposed. Signature sequences in proteins also indicate that the low-G + C Gram-positive bacteria are phylogenetically distinct from the high-G + C Gram-positive group and that the diderm prokaryotes (i.e. Gram-negative bacteria) appear to have evolved from the latter group. Protein phylogenies and signature sequences also show that all eukaryotic cells have received significant gene contributions from both an archaebacterium and a Gram-negative eubacterium. Thus, the hypothesis that archaebacteria and eukaryotes shared a common ancestor exclusive of eubacteria is not supported. These observations provide evidence for an alternate view of the evolutionary relationship among living organisms that is different from the currently popular three-domain proposal.     

Evolution of HSP70 gene and its implications regarding relationships between archaebacteria,eubacteria, and eukaryotes

The 70-kDa heat-shock protein (HSP70) constitutes the most conserved protein present in all organisms that is known to date. Based on global alignment of HSP70 sequences from organisms representing all three domains, numerous sequence signatures that are specific for prokaryotic and eukaryotic homologs have been identified. HSP70s from the two archaebacterial species examined (viz., Halobacterium marismortui and Methanosarcina mazei) have been found to contain all eubacterial but no eukaryotic signature sequences. Based on several novel features of the HSP70 family of proteins (viz., presence of tandem repeats of a 9-amino-acid [a.a.] polypeptide sequence and structural similarity between the first and second quadrants of HSP70, homology of the N-terminal half of HSP70 to the bacterial MreB protein, presence of a conserved insert of 23–27 a.a. in all HSP70s except those from archaebacteria and gram-positive eubacteria) a model for the evolution of HSP70 gene from an early stage is proposed. The HSP70 homologs from archaebacteria and gram-positive bacteria lacking the insert in the N-terminal quadrants are indicated to be the ancestral form of the protein. Detailed phylogenetic analyses of HSP70 sequence data (viz., by bootstrap analyses, maximum parsimony, and maximum likelihood methods) provide evidence that archaebacteria are not monophyletic and show a close evolutionary linkage with the gram-positive eubacteria. These results do not support the traditional archaebacterial tree, where a close relationship between archaebacterial and eukaryotic homologs is observed. To explain the phylogenies based on HSP70 and other gene sequences, a model for the origin of eukaryotic cells involving fusion between archaebacteria and gram-negative eubacteria is proposed. Correspondence to: R. S. Gupta     

Sequencing of heat shock protein 70 (DnaK) homologs from Deinococcus proteolyticus and Thermomicrobium roseum and their integration in a protein-based phylogeny of prokaryotes.

The 70-kDa heat shock protein (hsp70) sequences define one of the most conserved proteins known to date. The hsp70 genes from Deinococcus proteolyticus and Thermomicrobium roseum, which were chosen as representatives of two of the most deeply branching divisions in the 16S rRNA trees, were cloned and sequenced. hsp70 from both these species as well as Thermus aquaticus contained a large insert in the N-terminal quadrant, which has been observed before as a unique characteristic of gram-negative eubacteria and eukaryotes and is not found in any gram-positive bacteria or archaebacteria. Phylogenetic analysis of hsp70 sequences shows that all of the gram-negative eubacterial species examined to date (which includes members from the genera Deinococcus and Thermus, green nonsulfur bacteria, cyanobacteria, chlamydiae, spirochetes, and alpha-, beta-, and gamma-subdivisions of proteobacteria) form a monophyletic group (excluding eukaryotic homologs which are derived from this group via endosybitic means) strongly supported by the bootstrap scores. A closer affinity of the Deinococcus and Thermus species to the cyanobacteria than to the other available gram-negative sequences is also observed in the present work. In the hsp7O trees, D. proteolyticus and T. aquaticus were found to be the most deeply branching species within the gram-negative eubacteria. The hsp70 homologs from gram-positive bacteria branched separately from gram-negative bacteria and exhibited a closer relationship to and shared sequence signatures with the archaebacteria. A polyphyletic branching of archaebacteria within gram-positive bacteria is strongly favored by different phylogenetic methods. These observations differ from the rRNA-based phylogenies where both gram-negative and gram-positive species are indicated to be polyphyletic. While it remains unclear whether parts of the genome may have variant evolutionary histories, these results call into question the general validity of the currently favored three-domain dogma.     

Protein-based phylogenies support a chimeric origin for the eukaryotic genome

The phylogenetic position of the archaebacteria and the place of eukaryotes in the history of life remain a question of debate. Recent studies based on some protein-sequence data have obtained unusual phylogenies for these organisms. We therefore collected the protein sequences that were available with representatives from each of the major forms of life: the gram-negative bacteria, gram-positive bacteria, archaebacteria, and eukaryotes. Monophyletic, unrooted phylogenies based on these sequence data show that seven of 24 proteins yield a significant gram-positive-archaebacteria clade/gram-negative- eukaryotic clade. The phylogenies for these seven proteins cannot be explained by the traditional three-way split of the eukaryotes, archaebacteria, and eubacteria. Nine of the 24 proteins yield the traditional gram-positive-gram-negative clade/archaebacteria-eukaryotic clade. The remaining eight proteins give phylogenies that cannot be statistically distinguished. These results support the hypothesis of a chimeric origin for the eukaryotic cell nucleus formed from the fusion of an archaebacteria and a gram-negative bacteria.      

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.     

Phylogenetic analysis of 70 kD heat shock protein sequences suggests a chimeric origin for the eukaryotic cell nucleus

Background: The evolutionary relationships between archaebacteria, eubacteria and eukaryotic cells are of central importance in biology. The current view is that each of these three groups of organisms constitutes a monophyletic domain, and that eukaryotic cells have evolved from an archaebacterial ancestor. Recent studies on a number of highly conserved protein sequences do not, however, support this view and raise important questions concerning the evolutionary relationships between all extant organisms, particularly regarding the origin of eukaryotic cells.Results We have used sequences of 70 kD heat shock protein (hsp70) — the most conserved protein found to date in all species — to examine the evolutionary relationship between various species. We have obtained two new archaebacterial hsp70 sequences from the species, Thermoplasma acidophilum and Halobacterium cutirubrum. A global comparison of hsp70 sequences, including our two new sequences, shows that all known archaebacterial homologs share a number of sequence signatures with the Gram-positive group of bacteria that are not found in any other prokaryotic or eukaryotic species. In contrast, the eukaryotic homologs are shown to share a number of unique sequence features with the Gram-negative bacteria that are not present in any archaebacteria. Detailed phylogenetic analyses of hsp70 sequences strongly support a specific evolutionary relationship between archaebacteria and Gram-positive bacteria on the one hand, and Gram-negative bacteria and eukaryotes on the other. The phylogenetic analyses also indicate a polyphyletic branching of archaebacteria within the Gram-positive species. The possibility that the observed relationships are due to horizontal gene transfers can be excluded on the basis of sequence characteristics of different groups of homologs.Conclusion Our results do not support the view that archaebacteria constitute a monophyletic domain, but instead suggest a close evolutionary linkage between archaebacteria and Gram-positive bacteria. Furthermore, in contrast to the presently accepted view, eukaryotic hsp70s show a close and specific relationship to those from Gram-negative species. To explain the phylogenies based on different gene sequences, a chimeric model for the origin of the eukaryotic cell nucleus involving fusion between an archaebacterium and a Gram-negative eubacterium is proposed. Several predictions from the chimeric model are discussed.     

Cloning of the HSP70 gene from Halobacterium marismortui: relatedness of archaebacterial HSP70 to its eubacterial homologs and a model for the evolution of the HSP70 gene.

Heat shock induces the synthesis of a set of proteins in Halobacterium marismortui whose molecular sizes correspond to the known major heat shock proteins. By using the polymerase chain reaction and degenerate oligonucleotide primers for conserved regions of the 70-kDa heat shock protein (HSP70) family, we have successfully cloned and sequenced a gene fragment containing the entire coding sequence for HSP70 from H. marismortui. HSP70 from H. marismortui shows between 44 and 47% amino acid identity with various eukaryotic HSP70s and between 51 and 58% identity with its eubacterial and archaebacterial homologs. On the basis of a comparison of all available HSP70 sequences, we have identified a number of unique sequence signatures in this protein family that provide a clear distinction between eukaryotic organisms and prokaryotic organisms (archaebacteria and eubacteria). The archaebacterial (viz., H. marismortui and Methanosarcina mazei) HSP70s have been found to contain all of the signature sequences characteristic of eubacteria (particularly the gram-positive bacteria), which suggests a close evolutionary relationship between these groups. In addition, detailed analyses of HSP70 sequences that we have carried out have revealed a number of additional novel features of the HSP70 protein family. These include (i) the presence of an insertion of about 25 to 27 amino acids in the N-terminal quadrants of all known eukaryotic and prokaryotic HSP70s except those from archaebacteria and the gram-positive group of bacteria, (ii) significant sequence similarity in HSP70 regions comprising its first and second quadrants from organisms lacking the above insertion, (iii) highly significant similarity between a protein, MreB, of Escherichia coli and the N-terminal half of HSP70s, (iv) significant sequence similarity between the N-terminal quadrant of HSP70 (from gram-positive bacteria and archaebacteria) and the m-type thioredoxin of plant chloroplasts. To account for these and other observations, a model for the evolution of HSP70 proteins involving gene duplication is proposed. The model proposes that HSP70 from archaebacteria (H. marismortui and M. mazei) and the gram-positive group of bacteria constitutes the ancestral form of the protein and that all other HSP70s (viz., other eubacteria as well as eukaryotes) containing the insert have evolved from this ancient protein.     

Molecular Evolutionary Analysis of the Thiamine-Diphosphate-Dependent Enzyme,Transketolase

Members of the transketolase group of thiamine-diphosphate-dependent enzymes from 17 different organisms including mammals, yeast, bacteria, and plants have been used for phylogenetic reconstruction. Alignment of the amino acid and DNA sequences for 21 transketolase enzymes and one putative transketolase reveals a number of highly conserved regions and invariant residues that are of predicted importance for enzyme activity, based on the crystal structure of yeast transketolase. One particular sequence of 36 residues has some similarities to the nucleotide-binding motif and we designate it as the transketolase motif. We report further evidence that the recP protein from Streptococcus pneumoniae might be a transketolase and we list a number of invariant residues which might be involved in substrate binding. Phylogenies derived from the nucleotide and the amino acid sequences by various methods show a conventional clustering for mammalian, plant, and gram-negative bacterial transketolases. The branching order of the gram-positive bacteria could not be inferred reliably. The formaldehyde transketolase (sometimes known as dihydroxyacetone synthase) of the yeast Hansenula polymorpha appears to be orthologous to the mammalian enzymes but paralogous to the other yeast transketolases. The occurrence of more than one transketolase gene in some organisms is consistent with several gene duplications. The high degree of similarity in functionally important residues and the fact that the same kinetic mechanism is applicable to all characterized transketolase enzymes is consistent with the proposition that they are all derived from one common ancestral gene. Transketolase appears to be an ancient enzyme that has evolved slowly and might serve as a model for a molecular clock, at least within the mammalian clade. Received: 13 September 1995 / Accepted: 14 November 1996     

Evolution of proton pumping ATPases: Rooting the tree of life

Proton pumping ATPases are found in all groups of present day organisms. The F-ATPases of eubacteria, mitochondria and chloroplasts also function as ATP synthases, i.e., they catalyze the final step that transforms the energy available from reduction/oxidation reactions (e.g., in photosynthesis) into ATP, the usual energy currency of modern cells. The primary structure of these ATPases/ATP synthases was found to be much more conserved between different groups of bacteria than other parts of the photosynthetic machinery, e.g., reaction center proteins and redox carrier complexes.These F-ATPases and the vacuolar type ATPase, which is found on many of the endomembranes of eukaryotic cells, were shown to be homologous to each other; i.e., these two groups of ATPases evolved from the same enzyme present in the common ancestor. (The term eubacteria is used here to denote the phylogenetic group containing all bacteria except the archaebacteria.) Sequences obtained for the plasmamembrane ATPase of various archaebacteria revealed that this ATPase is much more similar to the eukaryotic than to the eubacterial counterpart. The eukaryotic cell of higher organisms evolved from a symbiosis between eubacteria (that evolved into mitochondria and chloroplasts) and a host organism. Using the vacuolar type ATPase as a molecular marker for the cytoplasmic component of the eukaryotic cell reveals that this host organism was a close relative of the archaebacteria.A unique feature of the evolution of the ATPases is the presence of a non-catalytic subunit that is paralogous to the catalytic subunit, i.e., the two types of subunits evolved from a common ancestral gene. Since the gene duplication that gave rise to these two types of subunits had already occurred in the last common ancestor of all living organisms, this non-catalytic subunit can be used to root the tree of life by means of an outgroup; that is, the location of the last common ancestor of the major domains of living organisms (archaebacteria, eubacteria and eukaryotes) can be located in the tree of life without assuming constant or equal rates of change in the different branches.A correlation between structure and function of ATPases has been established for present day organisms. Implications resulting from this correlation for biochemical pathways, especially photosynthesis, that were operative in the last common ancestor and preceding life forms are discussed.     

Molecular signatures for the main phyla of photosynthetic bacteria and their subgroups

The bacterial groups corresponding to different photosynthetic prokaryotes are presently identified mainly on the basis of their branching in phylogenetic trees. The availability of genome sequences is enabling identification of many molecular signatures that are specific for different groups of photosynthetic bacteria. Our recent work has identified large numbers of signatures consisting of conserved inserts or deletions (indels) in widely distributed proteins, as well as whole proteins that are specific for various sequenced species/strains from Cyanobacteria, Chlorobi, and Proteobacteria phyla. Based upon these signatures, it is now possible to identify/distinguish bacteria from these phyla of photosynthetic bacteria as well as their major subclades in clear molecular terms. The use of these signatures in conjunction with phylogenomic analyses, summarized here, is leading to a holistic picture concerning the branching order and evolutionary relationships among the above groups of photosynthetic bacteria. Although detailed studies in this regard have not yet been carried on Chloroflexi and Heliobacteriaceae, we have identified some conserved indels that are specific for these groups. Some of the conserved indels for the photosynthetic bacteria are present in photosynthesis-related proteins. These include a 4 aa insert in the pyruvate flavodoxin/ferridoxin oxidoreductase that is specific for the genus Chloroflexus, a 2 aa insert in magnesium chelatase that is uniquely shared by all Cyanobacteria except the deepest branching Clade A (Gloebacterales), a 6 aa insert in an A-type flavoprotein that is specific for various marine unicellular Cyanobacteria, a 2 aa insert in heme oxygenase that is specific for various Prochlorococcus strains/isolates, and 1 aa deletion in the protein protochlorophyllide oxidoreductase that is commonly shared by various Prochlorococcus strains except the deepest branching isolates MIT 9303 and MIT 9313. The identified CSIs are located in the structures of these proteins in surface loops indicating that they may be important in mediating protein–protein interactions. The cellular functions of these conserved indels, or most of the signature proteins are presently unknown, but they provide valuable means for discovering novel properties that are unique to different groups of photosynthetic bacteria.     

The presence of a dnaK (HSP70) multigene family in members of the orders Planctomycetales and Verrucomicrobiales.

Sequences of the dnaK gene, coding for the 70-kDa heat shock protein (HSP70), were determined for six members of the order Planctomycetales, including representatives of three genera, and for the only cultivated member of the order Verrucomicrobiales, Verrucomicrobium spinosum. A fragment of the dnaK gene was amplified from these strains by PCR with oligonucleotide primers targeting regions of the dnaK gene that are conserved at the amino acid level, and the resulting PCR products were cloned into a plasmid vector. Sequence analysis of the cloned dnaK fragments revealed the presence of two different types of dnaK sequence in one of the planctomycete strains, Planctomyces maris, and in V. spinosum. Only one type of dnaK sequence was found for each of the remaining strains. Phylogenetic analysis of the partial sequence data suggested that the majority of planctomycete strains, including one of the Planctomyces maris sequences, form a coherent phylogenetic group branching adjacent to other main lines of descent within the domain Bacteria, as has been shown previously by 16S rRNA sequence analysis. One of the two V. spinosum dnaK sequences also appears to constitute a separate lineage within the gram-negative bacteria. Each of the remaining sequences from P. maris and V. spinosum, together with the single sequence obtained from Planctomyces limnophilus, appeared to be unrelated to the other planctomycete sequences and to occupy a position distant from that of other gram-negative bacteria. The phylogenetic diversity of dnaK sequences exhibited by P. maris and V. spinosum was comparable to that found in Synechococcus sp. strain PCC7942 and Escherichia coli, the only other prokaryotes for which a dnaK multigene family has been demonstrated.     

New Findings on Evolution of Metal Homeostasis Genes: Evidence from Comparative Genome Analysis of Bacteria and Archaea

In order to examine the natural history of metal homeostasis genes in prokaryotes, open reading frames with homology to characterized P_IB-type ATPases from the genomes of 188 bacteria and 22 archaea were investigated. Major findings were as follows. First, a high diversity in N-terminal metal binding motifs was observed. These motifs were distributed throughout bacterial and archaeal lineages, suggesting multiple loss and acquisition events. Second, the CopA locus separated into two distinct phylogenetic clusters, CopA1, which contained ATPases with documented Cu(I) influx activity, and CopA2, which contained both efflux and influx transporters and spanned the entire diversity of the bacterial domain, suggesting that CopA2 is the ancestral locus. Finally, phylogentic incongruences between 16S rRNA and P_IB-type ATPase gene trees identified at least 14 instances of lateral gene transfer (LGT) that had occurred among diverse microbes. Results from bootstrapped supported nodes indicated that (i) a majority of the transfers occurred among proteobacteria, most likely due to the phylogenetic relatedness of these organisms, and (ii) gram-positive bacteria with low moles percent G+C were often involved in instances of LGT. These results, together with our earlier work on the occurrence of LGT in subsurface bacteria (J. M. Coombs and T. Barkay, Appl. Environ. Microbiol. 70:1698-1707, 2004), indicate that LGT has had a minor role in the evolution of P_IB-type ATPases, unlike other genes that specify survival in metal-stressed environments. This study demonstrates how examination of a specific locus across microbial genomes can contribute to the understanding of phenotypes that are critical to the interactions of microbes with their environment.     

Identification of microorganisms by PCR amplification and sequencing of a universal amplified ribosomal region present in both prokaryotes and eukaryotes

The small ribosomal subunit contains 16S rRNA in prokaryotes and 18S rRNA in eukaryotes. Even though it has been known that some small ribosomal sequences are conserved in 16S rRNA and 18S rRNA molecules, they have been used separately for taxonomic and phylogenetic studies. Here, we report the existence of two highly conserved ribosomal sequences in all organisms that allow the amplification of a zone containing approximately 495 bp in prokaryotes and 508 bp in eukaryotes which we have named the "Universal Amplified Ribosomal Region" (UARR). Amplification and sequencing of this zone is possible using the same two universal primers (U1F and U1R) designed on the basis of two highly conserved ribosomal sequences. The UARR encompasses the V6, V7 and V8 domains from SSU rRNA in both prokaryotes and eukaryotes. The internal sequence of this zone in prokaryotes and eukaryotes is variable and the differences become less marked on descent from phyla to species. Nevertheless, UARR sequence allows species from the same genus to be differentiated. Thus, by UARR sequence analysis the construction of universal phylogenetic trees is possible, including species of prokaryotic and eukaryotic microorganisms together. Single isolates of prokaryotic and eukaryotic microorganisms from different sources can be identified by amplification and sequencing of UARR using the same pair of primers and the same PCR and sequencing conditions.     

Origin of diderm (Gram-negative) bacteria: antibiotic selection pressure rather than endosymbiosis likely led to the evolution of bacterial cells with two membranes

The prokaryotic organisms can be divided into two main groups depending upon whether their cell envelopes contain one membrane (monoderms) or two membranes (diderms). It is important to understand how these and other variations that are observed in the cell envelopes of prokaryotic organisms have originated. In 2009, James Lake proposed that cells with two membranes (primarily Gram-negative bacteria) originated from an ancient endosymbiotic event involving an Actinobacteria and a Clostridia (Lake 2009). However, this Perspective argues that this proposal is based on a number of incorrect assumptions and the data presented in support of this model are also of questionable nature. Thus, there is no reliable evidence to support the endosymbiotic origin of double membrane bacteria. In contrast, many observations suggest that antibiotic selection pressure was an important selective force in prokaryotic evolution and that it likely played a central role in the evolution of diderm (Gram-negative) bacteria. Some bacterial phyla, such as Deinococcus-Thermus, which lack lipopolysaccharide (LPS) and yet contain some characteristics of the diderm bacteria, are postulated as evolutionary intermediates (simple diderms) in the transition between the monoderm bacterial taxa and the bacterial groups that have the archetypal LPS-containing outer cell membrane found in Gram-negative bacteria. It is possible to distinguish the two stages in the evolution of diderm-LPS cells (viz. monoderm bacteria → simple diderms lacking LPS → LPS containing archetypal diderm bacteria) by means of conserved inserts in the Hsp70 and Hsp60 proteins. The insert in the Hsp60 protein also distinguishes the traditional Gram-negative diderm bacterial phyla from atypical taxa of diderm bacteria (viz. Negativicutes, Fusobacteria, Synergistetes and Elusimicrobia). The Gram-negative bacterial phyla with an LPS-diderm cell envelope, as defined by the presence of the Hsp60 insert, are indicated to form a monophyletic clade and no loss of the outer membrane from any species from this group seems to have occurred. This argues against the origin of monoderm prokaryotes from diderm bacteria by loss of outer membrane.     

Microflorae of aquatic moss pillars in a freshwater lake, East Antarctica, based on fatty acid and 16S rRNA gene analyses

Aquatic mosses in the genera Bryum and Leptobryum form unique tower-like ??moss pillars?? underwater in some Antarctic lakes, in association with algae and cyanobacteria. These are communities with a two-layer structure comprising an oxidative exterior and reductive interior. Although habitats and photosynthetic properties of moss pillars have been reported, microfloral composition of the two-layer structure has not been described. Here we report fatty acid analysis of one moss pillar and molecular phylogenetic analysis, based on the 16S rRNA gene, of this and one other moss pillar. Cluster analysis of the phospholipid fatty acid composition showed three groups corresponding to the exterior, upper interior, and lower interior of the pillar. This suggested that species composition differed by section, with the exterior dominated by photosynthetic organisms such as mosses, algae, and cyanobacteria, the upper interior primarily containing gram-positive bacteria and anaerobic sulfate-reducing bacteria, and the lower interior dominated by gram-negative bacteria. Molecular phylogenetic analysis revealed that Proteobacteria dominate the moss pillar as a whole; cyanobacteria were found on the exterior and the gram-positive obligate anaerobe Clostridium in the interior, while gram-positive sulfate-reducing bacteria were present in the lowest part of the interior. Nitrogen-fixing bacteria and denitrifying bacteria were found in all sections. Thus, fatty acid analysis and genetic analysis showed similar patterns. These findings suggest that microorganisms of different phylogenetic groups inhabit different sections of a single moss pillar and form a microbial community that performs biogeochemical cycling to establish and maintain a structure in an oxidation?Creduction gradient between exterior and interior.     

Physiological responses of bacteria to cytochalasin A: effects on growth, transport, and enzyme induction.

Cytochalasin A at 5 to 25 microgram/ml (1.0 x 10(-5) to 5.2 x 10(-5) M) inhibited the growth of three gram-positive bacteria, Arthrobacter sialophilus, Staphyloccus aureus, and Bacillus amyloliquifaciens, but had little or no effect on the growth of three gram-negative bacteria, Excherichia coli, Pseudomonas maltophilia, and Aeromonas proteolytica. A. sialophilus and S. aureus recovered spontaneously from cytochalasin A-mediated growth inhibition after a considerable lag period, which was dependent on the drug dose. It was demonstrated that this long-term recovery did not involve selection of resistant variants. Cytochalasin A had no detrimental effect on cell viability in A. sialophilus or S. aureus, but caused lysis of B. amyloliquifaciens. The drug prevented enzyme inductions and inhibited transport of valine, uridine, and glucose in the gram-positive organisms. It had little or no effect on these processes in the gram-negative organisms. In studies with A. sialophilus, the drug inhbitied respiration of exogenous substrates, but did not depress endogenous respiration. These results constitute the first unequivocal evidence for the bacteriostatic properties of this class of compounds and indicate that cytochalasin A halts various physiological processes in gram-positive bacteria primarily by inhibiting solute transport.     

A major clade of prokaryotes with ancient adaptations to life on land

Evolutionary trees of prokaryotes usually define the known classes and phyla but less often agree on the relationships among those groups. This has been attributed to the effects of horizontal gene transfer, biases in sequence change, and large evolutionary distances. Furthermore, higher level clades of prokaryote phyla rarely are supported by information from ecology and cell biology. Nonetheless, common patterns are beginning to emerge as larger numbers of species are analyzed with sophisticated methods. Here, we show how combined evidence from phylogenetic, cytological, and environmental data support the existence of an evolutionary group that appears to have had a common ancestor on land early in Earth's history and includes two-thirds of known prokaryote species. Members of this terrestrial clade (Terrabacteria), which includes Cyanobacteria, the gram-positive phyla (Actinobacteria and Firmicutes), and two phyla with cell walls that differ structurally from typical gram-positive and gram-negative phyla (Chloroflexi and Deinococcus-Thermus), possess important adaptations such as resistance to environmental hazards (e.g., desiccation, ultraviolet radiation, and high salinity) and oxygenic photosynthesis. Moreover, the unique properties of the cell wall in gram-positive taxa, which likely evolved in response to terrestrial conditions, have contributed toward pathogenicity in many species. These results now leave open the possibility that terrestrial adaptations may have played a larger role in prokaryote evolution than currently understood.     

原核生物eno基因在系统进化中应用及水平转移分析

多基因系统发育研究方法是系统发育分析中的一个重要手段,基因树冲突已成为分子系统发育研究中日益突出的问题。烯醇化酶基因(eno)及其编码的蛋白广泛存在于五界系统中,烯醇化酶为糖酵解途径中重要酶类。文章选取原核生物已注释的eno基因序列进行了系统发育分析。对其中的138个模式菌株的eno基因序列进行系统发育分析和同源性搜索,发现19个模式菌株的eno基因是通过水平转移而来;并通过核苷酸组成、密码子偏好性和基因排列等基因特征分析,进一步验证了水平转移基因的外源性。结果表明:原核生物eno序列具有较高保守性,其大小适中,是研究原核生物系统发育的良好材料。文章在对基因水平转移的供体和受体菌株生活习性、进化历史以及烯醇化酶的结构和功能的研究过程中提供重要参考价值。     

Phylogenetic Analysis Reveals Multiple Lateral Transfers of Adenosine-5′-Phosphosulfate Reductase Genes among Sulfate-Reducing Microorganisms

Lateral gene transfer affects the evolutionary path of key genes involved in ancient metabolic traits, such as sulfate respiration, even more than previously expected. In this study, the phylogeny of the adenosine-5'-phosphosulfate (APS) reductase was analyzed. APS reductase is a key enzyme in sulfate respiration present in all sulfate-respiring prokaryotes. A newly developed PCR assay was used to amplify and sequence a fragment ( approximately 900 bp) of the APS reductase gene, apsA, from a taxonomically wide range of sulfate-reducing prokaryotes (n = 60). Comparative phylogenetic analysis of all obtained and available ApsA sequences indicated a high degree of sequence conservation in the region analyzed. However, a comparison of ApsA- and 16S rRNA-based phylogenetic trees revealed topological incongruences affecting seven members of the Syntrophobacteraceae and three members of the Nitrospinaceae, which were clearly monophyletic with gram-positive sulfate-reducing bacteria (SRB). In addition, Thermodesulfovibrio islandicus and Thermodesulfobacterium thermophilum, Thermodesulfobacterium commune, and Thermodesulfobacterium hveragerdense clearly branched off between the radiation of the delta-proteobacterial gram-negative SRB and the gram-positive SRB and not close to the root of the tree as expected from 16S rRNA phylogeny. The most parsimonious explanation for these discrepancies in tree topologies is lateral transfer of apsA genes across bacterial divisions. Similar patterns of insertions and deletions in ApsA sequences of donor and recipient lineages provide additional evidence for lateral gene transfer. From a subset of reference strains (n = 25), a fragment of the dissimilatory sulfite reductase genes (dsrAB), which have recently been proposed to have undergone multiple lateral gene transfers (M. Klein et al., J. Bacteriol. 183:6028-6035, 2001), was also amplified and sequenced. Phylogenetic comparison of DsrAB- and ApsA-based trees suggests a frequent involvement of gram-positive and thermophilic SRB in lateral gene transfer events among SRB.