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.     

Enzymes of aerobic respiration on iron

Abstract: Bacteria capable of aerobic respiration on ferrous ions are spread throughout eubacterial and archaebacterial phyla. Comparative spectroscopic analyses revealed that phylogenetically distinct organisms expressed copious quantities of spectrally distinct redox-active biomolecules during autotrophic growth on soluble iron. Thiobaeillus ferrooxidans, Leptospirillum ferrooxidans, Sulfobacillus thermosulfidooxidans , and Metallosphaera sedula possessed iron respiratory chains dominated by a blue copper protein, a novel red cytochrome, a novel yellow protein, and a novel yellow cytochrome, respectively. Further investigation of each type of respiratory chain will be necessary to deduce the advantages and disadvantages of each.     

Evolution of enzymes involved in the photorespiratory 2-phosphoglycolate cycle from cyanobacteria via algae toward plants

The photorespiratory pathway was shown to be essential for organisms performing oxygenic photosynthesis, cyanobacteria, algae, and plants, in the present day O(2)-containing atmosphere. The identification of a plant-like 2-phosphoglycolate cycle in cyanobacteria indicated that not only genes of oxygenic photosynthesis but also genes encoding photorespiratory enzymes were endosymbiotically conveyed from ancient cyanobacteria to eukaryotic oxygenic phototrophs. Here, we investigated the origin of the photorespiratory pathway in photosynthetic eukaryotes by phylogenetic analysis. We found that a mixture of photorespiratory enzymes of either cyanobacterial or α-proteobacterial origin is present in algae and higher plants. Three enzymes in eukaryotic phototrophs clustered closely with cyanobacterial homologs: glycolate oxidase, glycerate kinase, and hydroxypyruvate reductase. On the other hand, the mitochondrial enzymes of the photorespiratory cycle in algae and plants, glycine decarboxylase subunits and serine hydroxymethyltransferase, evolved from proteobacteria. Other than most genes for proteins of the photosynthetic machinery, nearly all enzymes involved in the 2-phosphogylcolate metabolism coexist in the genomes of cyanobacteria and heterotrophic bacteria.     

<Emphasis Type="Italic">Bd</Emphasis> oxidase homologue of photosynthetic purple sulfur bacterium <Emphasis Type="Italic">Allochromatium vinosum</Emphasis> is co-transcribed with a nitrogen fixation related gene

Purple sulfur bacteria, which are known to be the most ancient among anoxygenic phototrophs, play an important role in the global sulfur cycle. Allochromatium vinosum oxidizes reduced sulfur compounds such as hydrogen sulfide, elemental sulfur and thiosulfide. At low oxygen concentrations, A. vinosum can grow chemotrophically using oxygen as the terminal electron acceptor. Being also a nitrogen fixer, A. vinosum is faced with the paradox of co-existence of aerobic metabolism and nitrogen fixation. Due to growth difficulties, only a few studies have dealt with the aerobic metabolism of the organism and, until now, there has been no information about the genes involved in the respiratory metabolism of purple sulfur bacteria. In this article we show the first terminal oxidase gene for A. vinosum. The presence of a Bd type of quinol oxidase is necessary to protect nitrogenases against the inhibitory effects of oxygen. In this case, a nitrogen fixation related gene is part of the cyd operon and this gene is co-transcribed with cydAB genes. Bd oxidase of A. vinosum may be the earliest form of oxidase where the function of the enzyme is to scavenge the contaminant oxygen during nitrogen fixation. This may be an important clue about the early evolution of oxygenic photosynthesis, perhaps as a protective mechanism for nitrogen fixation.     

Heme-copper oxidases and their electron donors in cyanobacterial respiratory electron transport

Cyanobacteria are the paradigmatic organisms of oxygenic (plant-type) photosynthesis and aerobic respiration. Since there is still an amazing lack of knowledge on the role and mechanism of their respiratory electron transport, we have critically analyzed all fully or partially sequenced genomes for heme-copper oxidases and their (putative) electron donors cytochrome c(6), plastocyanin, and cytochrome c(M). Well-known structure-function relationships of the two branches of heme-copper oxidases, namely cytochrome c (aa(3)-type) oxidase (COX) and quinol (bo-type) oxidase (QOX), formed the base for a critical inspection of genes and ORFs found in cyanobacterial genomes. It is demonstrated that at least one operon encoding subunits I-III of COX is found in all cyanobacteria, whereas many non-N(2)-fixing species lack QOX. Sequence analysis suggests that both cyanobacterial terminal oxidases should be capable of both the four-electron reduction of dioxygen and proton pumping. All diazotrophic organisms have at least one operon that encodes QOX. In addition, the highly refined specialization in heterocyst forming Nostocales is reflected by the presence of two paralogs encoding COX. The majority of cyanobacterial genomes contain one gene or ORF for plastocyanin and cytochrome c(M), whereas 1-4 paralogs for cytochrome c(6) were found. These findings are discussed with respect to published data about the role of respiration in wild-type and mutated cyanobacterial strains in normal metabolism, stress adaptation, and nitrogen fixation. A model of the branched electron-transport pathways downstream of plastoquinol in cyanobacteria is presented.     

On the evolutionary descent of organisms and organelles: a global phylogeny based on a highly conserved structural core in small subunit ribosomal RNA

To probe the earliest evolutionary events attending the origin of the five known genome types (archaebacterial, eubacterial, nuclear, mitochondrial and plastid), we have analyzed sequences corresponding to a ubiquitous, highly conserved core of secondary structure in small subunit rRNA. Our results support (i) the existence of three primary lineages (archaebacterial, eubacterial, and nuclear), (ii) a specific eubacterial ancestry for plastids and mitochondria (plant, animal, fungal), and (iii) an endosymbiotic, evolutionary origin of the two types of organelle from within distinct groups of eubacteria (blue-green algae (cyanobacteria) in the case of plastids, nonphotosynthetic aerobic bacteria in the case of mitochondria). In addition, our analysis suggests (iv) a biphyletic origin of mitochondria, with animal and fungal mitochondria branching together but separately from plant mitochondria, and (v) a monophyletic origin of plastids. The method described here provides a powerful and generally applicable molecular taxonomic approach towards a global phylogeny encompassing all organisms and organelles.     

Respiratory Chains in the Last Common Ancestor of Living Organisms

Sequences in current databases show that a number of proteins involved in respiratory processes are homologous in archaeal and bacterial species. In particular, terminal oxidases belonging to oxygen, nitrate, sulfate, and sulfur respiratory pathways have been sequenced in members of both domains. They include cytochrome oxidase, nitrate reductase, adenylylsulfate reductase, sulfite reductase, and polysulfide reductase. These proteins can be assigned to the last common ancestor of living organisms assuming that the deepest split of the three domains of life occurred between Archaea and Bacteria and that they were not acquired through lateral gene transfer by one of these domains. These molecular data indicate that several of the most important respiratory pathways arose early in evolution and that the last common ancestor of living organisms was not a simple organism in its energetic metabolism. Rather, it may have been able to gain energy by means of at least four electron transport chains, and therefore it may have been prepared to face a wide range of environmental conditions.     

Origins, evolutionary history, and taxonomic distribution of alternative oxidase and plastoquinol terminal oxidase

Alternative oxidase (AOX) and plastoquinol terminal oxidase (PTOX) are related quinol oxidases associated with respiratory and photosynthetic electron transport chains, respectively. Contrary to previous belief, AOX is present in numerous animal phyla, as well as heterotrophic and marine phototrophic proteobacteria. PTOX appears limited to organisms capable of oxygenic photosynthesis, including cyanobacteria, algae and plants. We propose that both oxidases originated in prokaryotes from a common ancestral di-iron carboxylate protein that diversified to AOX within ancient proteobacteria and PTOX within ancient cyanobacteria. Each then entered the eukaryotic lineage separately; AOX by the endosymbiotic event that gave rise to mitochondria and later PTOX by the endosymbiotic event that gave rise to chloroplasts. Both oxidases then spread through the eukaryotic domain by vertical inheritance, as well as by secondary and potentially tertiary endosymbiotic events.     

Homologous Protein Domains in Superkingdoms Archaea,Bacteria, and Eukaryota and the Problem of the Origin of Eukaryotes

The distribution of protein domains was analyzed in superkingdoms Archaea, Bacteria, and Eukaryota. About a half of eukaryotic domains have prokaryotic origin. Many domains related to information processing in the nucleocytoplasm were inherited from archaea. Sets of domains associated with metabolism and regulatory and signaling systems were inherited from bacteria. Many signaling and regulatory domains common for bacteria and eukaryotes were responsible for the cellular interaction of bacteria with other components of the microbial community but were involved in coordination of the activity of eukaryotic organelles and cells in multicellular organisms. Many eukaryotic domains of bacterial origin could not originate from ancestral mitochondria and plastids but rather were adopted from other bacteria. An archaeon with the induced incorporation of alien genetic material could be the ancestor of the eukaryotic nucleocytoplasm.__________Translated from Izvestiya Akademii Nauk, Seriya Biologicheskaya, No. 4, 2005, pp. 389–400.Original Russian Text Copyright © 2005 by Markov, Kulikov.     

Terminal oxidases of Bacillus subtilis strain 168: one quinol oxidase, cytochrome aa(3) or cytochrome bd, is required for aerobic growth

The gram-positive endospore-forming bacterium Bacillus subtilis has, under aerobic conditions, a branched respiratory system comprising one quinol oxidase branch and one cytochrome oxidase branch. The system terminates in one of four alternative terminal oxidases. Cytochrome caa(3) is a cytochrome c oxidase, whereas cytochrome bd and cytochrome aa(3) are quinol oxidases. A fourth terminal oxidase, YthAB, is a putative quinol oxidase predicted from DNA sequence analysis. None of the terminal oxidases are, by themselves, essential for growth. However, one quinol oxidase (cytochrome aa(3) or cytochrome bd) is required for aerobic growth of B. subtilis strain 168. Data indicating that cytochrome aa(3) is the major oxidase used by exponentially growing cells in minimal and rich medium are presented. We show that one of the two heme-copper oxidases, cytochrome caa(3) or cytochrome aa(3), is required for efficient sporulation of B. subtilis strain 168 and that deletion of YthAB in a strain lacking cytochrome aa(3) makes the strain sporulation deficient.     

Evolution of mitochondrial-type cytochrome c domains and of the protein machinery for their assembly

Proteins containing mitochondrial-type cytochrome c domains, defined here as protein domains having the mitochondrial cytochrome c fold, are found in organisms from all domains of life, and constitute essential components in several different metabolic pathways. The number of cytochrome c domains present in a given organism as well as their functional roles can vary widely even for quite closely related organisms. In this work, we have analysed in detail the distribution of mitochondrial-type cytochrome c domains along the tree of life and attempted to define the evolutionary relationships among them. In parallel, we have similarly analysed also the occurrence and distribution of the different machineries for cytochrome c assembly. It is found that the first appearance of mitochondrial-type cytochrome c domains has likely happened in the bacterial world, together with the first apparatus for their assembly. Evolution of cytochrome c domains has been extensive, involving several gene duplication and gene transfer events. Of particular relevance are gene transfer events from Bacteria to Eukarya and Archaea. The transfer of genes encoding cytochrome c domains has generally co-occurred with transfer of the assembly machinery. This has occurred also in Eukarya, where however the latter machinery has been subsequently replaced by a new one. It is possible that of the three known enzymatic systems for cytochrome c assembly, system II (found, among others, in cyanobacteria and Gram-positive bacteria) is the most ancient. Archaea have inherited from Bacteria system I or, possibly, an evolutionary intermediate between system II and system I.     

On the origins of cells: a hypothesis for the evolutionary transitions from abiotic geochemistry to chemoautotrophic prokaryotes,and from prokaryotes to nucleated cells

All life is organized as cells. Physical compartmentation from the environment and self-organization of self-contained redox reactions are the most conserved attributes of living things, hence inorganic matter with such attributes would be life's most likely forebear. We propose that life evolved in structured iron monosulphide precipitates in a seepage site hydrothermal mound at a redox, pH and temperature gradient between sulphide-rich hydrothermal fluid and iron(II)-containing waters of the Hadean ocean floor. The naturally arising, three-dimensional compartmentation observed within fossilized seepage-site metal sulphide precipitates indicates that these inorganic compartments were the precursors of cell walls and membranes found in free-living prokaryotes. The known capability of FeS and NiS to catalyse the synthesis of the acetyl-methylsulphide from carbon monoxide and methylsulphide, constituents of hydrothermal fluid, indicates that pre-biotic syntheses occurred at the inner surfaces of these metal-sulphide-walled compartments, which furthermore restrained reacted products from diffusion into the ocean, providing sufficient concentrations of reactants to forge the transition from geochemistry to biochemistry. The chemistry of what is known as the RNA-world could have taken place within these naturally forming, catalyticwalled compartments to give rise to replicating systems. Sufficient concentrations of precursors to support replication would have been synthesized in situ geochemically and biogeochemically, with FeS (and NiS) centres playing the central catalytic role. The universal ancestor we infer was not a free-living cell, but rather was confined to the naturally chemiosmotic, FeS compartments within which the synthesis of its constituents occurred. The first free-living cells are suggested to have been eubacterial and archaebacterial chemoautotrophs that emerged more than 3.8 Gyr ago from their inorganic confines. We propose that the emergence of these prokaryotic lineages from inorganic confines occurred independently, facilitated by the independent origins of membrane-lipid biosynthesis: isoprenoid ether membranes in the archaebacterial and fatty acid ester membranes in the eubacterial lineage. The eukaryotes, all of which are ancestrally heterotrophs and possess eubacterial lipids, are suggested to have arisen ca. 2 Gyr ago through symbiosis involving an autotrophic archaebacterial host and a heterotrophic eubacterial symbiont, the common ancestor of mitochondria and hydrogenosomes. The attributes shared by all prokaryotes are viewed as inheritances from their confined universal ancestor. The attributes that distinguish eubacteria and archaebacteria, yet are uniform within the groups, are viewed as relics of their phase of differentiation after divergence from the non-free-living universal ancestor and before the origin of the free-living chemoautotrophic lifestyle. The attributes shared by eukaryotes with eubacteria and archaebacteria, respectively, are viewed as inheritances via symbiosis. The attributes unique to eukaryotes are viewed as inventions specific to their lineage. The origin of the eukaryotic endomembrane system and nuclear membrane are suggested to be the fortuitous result of the expression of genes for eubacterial membrane lipid synthesis by an archaebacterial genetic apparatus in a compartment that was not fully prepared to accommodate such compounds, resulting in vesicles of eubacterial lipids that accumulated in the cytosol around their site of synthesis. Under these premises, the most ancient divide in the living world is that between eubacteria and archaebacteria, yet the steepest evolutionary grade is that between prokaryotes and eukaryotes.     

Origin of eukaryotic cell nuclei by symbiosis of Archaea in Bacteria supported by the newly clarified origin of functional genes

In the previous report, we demonstrated the origin of eukaryotic cell nuclei as the symbiosis of Archaea in Bacteria by the newly developed "Homology-Hit Analysis". In that case, we counted yeast Open Reading Frames (ORFs) showing the highest similarity to a bacterial ORF as orthologous ORFs (Orthologous ORFs were produced by speciation from a common ancestor, and have the highest similarity to each other.) by comparing whole ORFs of yeast with those of individual bacteria. However, we could not count all yeast ORFs showing the highest similarity to a bacterial ORF in functional categories of yeast. Therefore, the origin of ORFs in the functional categories of yeast could not be inferred strictly. Here, we have improved the method for detecting orthologous ORFs. In this method, we count the numbers of ORF with the highest similarity between individual yeast functional categories and individual bacteria as orthologous ORFs. By this method, it was possible to detect the correct orthologous ORFs and to infer the origins of the functional categories in eukaryotic cells. As a result, two categories, assembly of protein complexes and DNA repair were newly judged to be of Archaeal origin, while five categories, lipid (fatty-acid and isoprenoid) metabolism, protein folding and stabilization, signal transduction, organization of the plasma membrane and organization of the cytoplasm, were newly judged to be of Bacterial origin. On the other hand, the origins of two categories (meiosis and cellular import, which were determined in the previous analysis) could not be judged. It is considered that functional categories related to the nucleus have origins common to Archaea, while those related to the cytoplasm have origins common to Bacteria. From these data including the origin of plasma membrane, it was further clarified that cell nucleus originated by the symbiosis of Archaea in Bacteria.     

Horizontal gene flow from Eubacteria to Archaebacteria and what it means for our understanding of eukaryogenesis

The origin of the eukaryotic cell is considered one of the major evolutionary transitions in the history of life. Current evidence strongly supports a scenario of eukaryotic origin in which two prokaryotes, an archaebacterial host and an α-proteobacterium (the free-living ancestor of the mitochondrion), entered a stable symbiotic relationship. The establishment of this relationship was associated with a process of chimerization, whereby a large number of genes from the α-proteobacterial symbiont were transferred to the host nucleus. A general framework allowing the conceptualization of eukaryogenesis from a genomic perspective has long been lacking. Recent studies suggest that the origins of several archaebacterial phyla were coincident with massive imports of eubacterial genes. Although this does not indicate that these phyla originated through the same process that led to the origin of Eukaryota, it suggests that Archaebacteria might have had a general propensity to integrate into their genomes large amounts of eubacterial DNA. We suggest that this propensity provides a framework in which eukaryogenesis can be understood and studied in the light of archaebacterial ecology. We applied a recently developed supertree method to a genomic dataset composed of 392 eubacterial and 51 archaebacterial genera to test whether large numbers of genes flowing from Eubacteria are indeed coincident with the origin of major archaebacterial clades. In addition, we identified two potential large-scale transfers of uncertain directionality at the base of the archaebacterial tree. Our results are consistent with previous findings and seem to indicate that eubacterial gene imports (particularly from δ-Proteobacteria, Clostridia and Actinobacteria) were an important factor in archaebacterial history. Archaebacteria seem to have long relied on Eubacteria as a source of genetic diversity, and while the precise mechanism that allowed these imports is unknown, we suggest that our results support the view that processes comparable to those through which eukaryotes emerged might have been common in archaebacterial history.     

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.     

Anaerobic microbial communities in Lake Pavin, a unique meromictic lake in France

The Bacteria and Archaea from the meromictic Lake Pavin were analyzed in samples collected along a vertical profile in the anoxic monimolimnion and were compared to those in samples from the oxic mixolimnion. Nine targeted 16S rRNA oligonucleotide probes were used to assess the distribution of Bacteria and Archaea and to investigate the in situ occurrence of sulfate-reducing bacteria and methane-producing Archaea involved in the terminal steps of the anaerobic degradation of organic material. The diversity of the complex microbial communities was assessed from the 16S rRNA polymorphisms present in terminal restriction fragment (TRF) depth patterns. The densities of the microbial community increased in the anoxic layer, and Archaea detected with probe ARCH915 represented the largest microbial group in the water column, with a mean Archaea/Eubacteria ratio of 1.5. Terminal restriction fragment length polymorphism (TRFLP) analysis revealed an elevated archaeal and bacterial phylotype richness in anoxic bottom-water samples. The structure of the Archaea community remained rather homogeneous, while TRFLP patterns for the eubacterial community revealed a heterogeneous distribution of eubacterial TRFs.     

Analysis of phenetic trees based on metabolic capabilites across the three domains of life

Here, we used data of complete genomes to study comparatively the metabolism of different species. We built phenetic trees based on the enzymatic functions present in different parts of metabolism. Seven broad metabolic classes, comprising a total of 69 metabolic pathways, were comparatively analyzed for 27 fully sequenced organisms of the domains Eukarya, Bacteria and Archaea. Phylogenetic profiles based on the presence/absence of enzymatic functions for each metabolic class were determined and distance matrices for all the organisms were then derived from the profiles. Unrooted phenetic trees based upon the matrices revealed the distribution of the organisms according to their metabolic capabilities, reflecting the ecological pressures and adaptations that those species underwent during their evolution. We found that organisms that are closely related in phylogenetic terms could be distantly related metabolically and that the opposite is also true. For example, obligate bacterial pathogens were usually grouped together in our metabolic trees, demonstrating that obligate pathogens share common metabolic features regardless of their diverse phylogenetic origins. The branching order of proteobacteria often did not match their classical phylogenetic classification and Gram-positive bacteria showed diverse metabolic affinities. Archaea were found to be metabolically as distant from free-living bacteria as from eukaryotes, and sometimes were placed close to the metabolically highly specialized group of obligate bacterial pathogens. Metabolic trees represent an integrative approach for the comparison of the evolution of the metabolism and its correlation with the evolution of the genome, helping to find new relationships in the tree of life.     

Accounting for evolutionary rate variation among sequence sites consistently changes universal phylogenies deduced from rRNA and protein-coding genes.

Phylogenetic analyses of gene and protein sequences have led to two major competing views of the universal phylogeny, the evolutionary tree relating the three kinds of living organisms, Bacteria, Archaea, and Eukarya. In the first scheme, called "the archaebacterial tree, " organisms of the same type are clustered together. In the second scenario, called "the eocyte tree," the archaeal phylum of Crenarchaeota is more closely related to eukaryotes than are other Archaea. A major property of the evolution of functional ribosomal and protein-encoding genes is that the rate of nucleotide and amino acid substitution varies across sequence sites. Here, using distance-based and maximum-likelihood methods, we show that universal phylogenies of ribosomal RNAs and RNA polymerases built by ignoring this variation are biased toward the archaebacterial tree because of attraction between long branches. In contrast, taking among-site rate variability into account gives support for the eocyte tree.     

Archaea sister group of Bacteria? Indications from tree reconstruction artifacts in ancient phylogenies.

The 54-kDa signal recognition particle and the receptor SR alpha, two proteins involved in the cotranslational translocation of proteins, are paralogs. They originate from a gene duplication that occurred prior to the last universal common ancestor, allowing one to root the universal tree of life. Phylogenetic analysis using standard methods supports the generally accepted cluster of Archaea and Eucarya. However, a new method increasing the signal-to-noise ratio strongly suggests that this result is due to a long-branch attraction artifact, with the Bacteria evolving fastest. In fact, the Archaea/Eucarya sisterhood is recovered only by the fast-evolving positions. In contrast, the most slowly evolving positions, which are the most likely to retain the ancient phylogenetic signal, support the monophyly of prokaryotes. Such a eukaryotic rooting provides a simple explanation for the high similarity of Archaea and Bacteria observed in complete-genome analysis, and should prompt a reconsideration of current views on the origin of eukaryotes.     

The multiple evolutionary histories of dioxygen reductases: Implications for the origin and evolution of aerobic respiration

Understanding the origin and evolution of cellular processes is fundamental to understand how biological activity has shaped the history of our planet. Among these, aerobic respiration is probably one of the most debated. We have applied a phylogenomics approach to investigate the origin and evolution of dioxygen reductases (O(2)Red), the key enzymes of aerobic respiratory chains. The distribution and phylogenetic analysis of the four types of O(2)Red (Cyt-bd and the A, B, and C families of heme-copper O(2)Red) from 673 complete bacterial and archaeal genomes show that these enzymes have very different evolutionary histories: Cyt-bd are of bacterial origin and were transferred to a few archaea; C-O(2)Red are of proteobacterial origin and were transferred to a few other bacteria; B-O(2)Red are of archaeal origin and were transferred to a few bacteria; and A-O(2)Red are the most ancient O(2)Red and were already present prior to the divergence of major present-day bacterial and archaeal phyla, thus before the emergence of Cyanobacteria and oxygenic photosynthesis. Implications for the origin and the evolution of aerobic respiration are discussed.