具有真细菌和真核生物融合特征的古生菌转录系统

古生菌是一类区别于真细菌和真核生物的第三域生命形式 ,转录是生物体遗传信息传递系统中的一个中心环节。近年来研究结果表明 ,古生菌的转录系统具有真细菌和真核生物的融合特征 :古生菌的基本转录装置包括RNA聚合酶、基本转录因子、启动子元件等与真核生物相似 ;而古生菌的转录调控机制却更加类似于真细菌 ,在古生菌中发现并鉴定了许多类似于真细菌的转录调控蛋白。另外古生菌还具有某些独特的转录调控方式     

Zelloberflächenstrukturen der Bacteria und Archaea

Cell wall types of Bacteria and Archaea The acaryote microorganisms are divided into the two domains Bacteria and Archaea. The third domain represent the Eukarya. There is no universal cell wall polymer found in all Bacteria and Archaea. Due to their morphology several cell wall types can be identified, but the chemical diversity of the individual polymers is considerably greater. Certain cell wall polymers are limited to one of the two domains of Bacteria or Archaea like the murein of the Bacteria or the pseudomurein of some methanogens. Peptidoglycans (murein, pseudomurein) do not occur in eukaryotes. On the other hand individual cell wall polymers possess similarities to polymers of other domains. The structural principle of the methanochondroitin is also implemented in the eukaryotic connective tissue. The cell wall polymers consist frequently of glycoconjugates in which the amino acid content (glycoproteins) or the glycan moiety (proteoglycan‐like polymers) predominate. Both components (carbohydrates, amino acids) can also occur in similar amounts (peptidoglycan). There exist also cell wall polymers, which consist only of glycans (slimes, methanochondroitin) or amino acids (proteins, poly‐γ‐D‐glutamyl polymers). Cell wall‐free species (Mycoplasma) also occur. The chemical composition of the cell surface polymers was one of the first phenotypic characteristics that supported the 16 sRNA concept of Carl Woese to assign acaryote organisms into the two domains Bacteria and Archaea. A common feature of all Archaea is the lack of muramic acid and an outer membrane. The later occurs in the gramnegative Bacteria. During the evolution of Bacteria and Archaea a great variety of chemically different cell wall polymers has been developed which allow the growth and interaction of Bacteria and Archaea in different habitats. In this paper, some important surface polymers of Bacteria and Archaea are presented according to their chemical composition.     

The proportional lack of archaeal pathogens: Do viruses/phages hold the key?

Although Archaea inhabit the human body and possess some characteristics of pathogens, there is a notable lack of pathogenic archaeal species identified to date. We hypothesize that the scarcity of disease-causing Archaea is due, in part, to mutually-exclusive phage and virus populations infecting Bacteria and Archaea, coupled with an association of bacterial virulence factors with phages or mobile elements. The ability of bacterial phages to infect Bacteria and then use them as a vehicle to infect eukaryotes may be difficult for archaeal viruses to evolve independently. Differences in extracellular structures between Bacteria and Archaea would make adsorption of bacterial phage particles onto Archaea (i.e. horizontal transfer of virulence) exceedingly hard. If phage and virus populations are indeed exclusive to their respective host Domains, this has important implications for both the evolution of pathogens and approaches to infectious disease control.     

Origin of eukaryotic cell nuclei by symbiosis of Archaea in Bacteria is revealed by homology-hit analysis

The origin of eukaryotic cell nuclei by symbiosis of Archaea in Bacteria was proposed on the basis of the phylogenetic topologies of genes. However, it was not possible to conclude whether or not the genes involved were authentic representative genes. Furthermore, using the BLAST and FASTA programs, the similarity of open reading frame (ORF) groups between three domains (Eukarya, Archaea and Bacteria) was estimated at one threshold. Therefore, their similarities at other thresholds could not be clarified. Here we use our newly developed 'homology-hit analysis' method, which uses multiple thresholds, to determine the origin of the nucleus. We removed mitochondria-related ORFs from yeast ORFs, and determined the number of yeast orthologous ORFs in each functional category to the ORFs in six Archaea and nine Bacteria at several thresholds (E-values) using the BLAST. Our results indicate that yeast ORFs related to the nucleus may share their origins with archaeal ORFs, whereas ORFs that are related to the cytoplasm may share their origins with bacterial ORFs. Our results thus strongly support the idea of nucleus symbiosis.     

Eukaryotes first: how could that be?

In the half century since the formulation of the prokaryote : eukaryote dichotomy, many authors have proposed that the former evolved from something resembling the latter, in defiance of common (and possibly common sense) views. In such ‘eukaryotes first’ (EF) scenarios, the last universal common ancestor is imagined to have possessed significantly many of the complex characteristics of contemporary eukaryotes, as relics of an earlier ‘progenotic’ period or RNA world. Bacteria and Archaea thus must have lost these complex features secondarily, through ‘streamlining’. If the canonical three-domain tree in which Archaea and Eukarya are sisters is accepted, EF entails that Bacteria and Archaea are convergently prokaryotic. We ask what this means and how it might be tested.     

Genetic technologies for Archaea

Members of the third domain of life, the Archaea, possess structural, physiological, biochemical and genetic features distinct from Bacteria and Eukarya and, therefore, have drawn considerable scientific interest. Physiological, biochemical and molecular analyses have revealed many novel biological processes in these important prokaryotes. However, assessment of the function of genes in vivo through genetic analysis has lagged behind because suitable systems for the creation of mutants in most Archaea were established only in the past decade. Among the Archaea, sufficiently sophisticated genetic systems now exist for some thermophilic sulfur-metabolizing Archaea, halophilic Archaea and methanogenic Archaea. Recently, there have been developments in genetic analysis of thermophilic and methanogenic Archaea and in the use of genetics to study the physiology, metabolism and regulatory mechanisms that direct gene expression in response to changes of environmental conditions in these important microorganisms.     

Archaea and the prokaryote-to-eukaryote transition.

Since the late 1970s, determining the phylogenetic relationships among the contemporary domains of life, the Archaea (archaebacteria), Bacteria (eubacteria), and Eucarya (eukaryotes), has been central to the study of early cellular evolution. The two salient issues surrounding the universal tree of life are whether all three domains are monophyletic (i.e., all equivalent in taxanomic rank) and where the root of the universal tree lies. Evaluation of the status of the Archaea has become key to answering these questions. This review considers our cumulative knowledge about the Archaea in relationship to the Bacteria and Eucarya. Particular attention is paid to the recent use of molecular phylogenetic approaches to reconstructing the tree of life. In this regard, the phylogenetic analyses of more than 60 proteins are reviewed and presented in the context of their participation in major biochemical pathways. Although many gene trees are incongruent, the majority do suggest a sisterhood between Archaea and Eucarya. Altering this general pattern of gene evolution are two kinds of potential interdomain gene transferrals. One horizontal gene exchange might have involved the gram-positive Bacteria and the Archaea, while the other might have occurred between proteobacteria and eukaryotes and might have been mediated by endosymbiosis.     

Disordered nucleiome: Abundance of intrinsic disorder in the DNA‐ and RNA‐binding proteins in 1121 species from Eukaryota,Bacteria and Archaea

Intrinsically disordered proteins (IDPs) are abundant in various proteomes, where they play numerous important roles and complement biological activities of ordered proteins. Among functions assigned to IDPs are interactions with nucleic acids. However, often, such assignments are made based on the guilty‐by‐association principle. The validity of the extension of these correlations to all nucleic acid binding proteins has never been analyzed on a large scale across all domains of life. To fill this gap, we perform a comprehensive computational analysis of the abundance of intrinsic disorder and intrinsically disordered domains in nucleiomes (～548 000 nucleic acid binding proteins) of 1121 species from Archaea, Bacteria and Eukaryota. Nucleiome is a whole complement of proteins involved in interactions with nucleic acids. We show that relative to other proteins in the corresponding proteomes, the DNA‐binding proteins have significantly increased disorder content and are significantly enriched in disordered domains in Eukaryotes but not in Archaea and Bacteria. The RNA‐binding proteins are significantly enriched in the disordered domains in Bacteria, Archaea and Eukaryota, while the overall abundance of disorder in these proteins is significantly increased in Bacteria, Archaea, animals and fungi. The high abundance of disorder in nucleiomes supports the notion that the nucleic acid binding proteins often require intrinsic disorder for their functions and regulation.     

Bacteria rather than Archaea dominate microbial ammonia oxidation in an agricultural soil

Agricultural ecosystems annually receive approximately 25% of the global nitrogen input, much of which is oxidized at least once by ammonia-oxidizing prokaryotes to complete the nitrogen cycle. Recent discoveries have expanded the known ammonia-oxidizing prokaryotes from the domain Bacteria to Archaea . However, in the complex soil environment it remains unclear whether ammonia oxidation is exclusively or predominantly linked to Archaea as implied by their exceptionally high abundance. Here we show that Bacteria rather than Archaea functionally dominate ammonia oxidation in an agricultural soil, despite the fact that archaeal versus bacterial amoA genes are numerically more dominant. In soil microcosms, in which ammonia oxidation was stimulated by ammonium and inhibited by acetylene, activity change was paralleled by abundance change of bacterial but not of archaeal amoA gene copy numbers. Molecular fingerprinting of amoA genes also coupled ammonia oxidation activity with bacterial but not archaeal amoA gene patterns. DNA-stable isotope probing demonstrated CO₂ assimilation by Bacteria rather than Archaea . Our results indicate that Archaea were not important for ammonia oxidation in the agricultural soil tested.     

Adaptations to energy stress dictate the ecology and evolution of the Archaea

The three domains of life on Earth include the two prokaryotic groups, Archaea and Bacteria. The Archaea are distinguished from Bacteriabased on phylogenetic and biochemical differences, but currently there is no unifying ecological principle to differentiate these groups. The ecology of the Archaea is reviewed here in terms of cellular bioenergetics. Adaptation to chronic energy stress is hypothesized to be the crucial factor that distinguishes the Archaea from Bacteria. The biochemical mechanisms that enable archaea to cope with chronic energy stress include low-permeability membranes and specific catabolic pathways. Based on the ecological unity and biochemical adaptations among archaea, I propose the hypothesis that chronic energy stress is the primary selective pressure governing the evolution of the Archaea.     

Combining catalyzed reporter deposition-fluorescence in situ hybridization and microautoradiography to detect substrate utilization by bacteria and Archaea in the deep ocean

The recently developed CARD-FISH protocol was refined for the detection of marine Archaea by replacing the lysozyme permeabilization treatment with proteinase K. This modification resulted in about twofold-higher detection rates for Archaea in deep waters. Using this method in combination with microautoradiography, we found that Archaea are more abundant than Bacteria (42% versus 32% of 4',6'-diamidino-2-phenylindole counts) in the deep waters of the North Atlantic and that a larger fraction of Archaea than of Bacteria takes up l-aspartic acid (19% versus 10%).     

艾丁嗜盐小盒菌B2菌株16S rRNA核苷酸序列

艾丁嗜盐小盒菌B2菌株(Haloarcula aidinensis, strain B2)16Sr RNA的核苷酸序列已以双脱氧核苷酸链终止法确定。该菌16Sr RNA显示出了典型的古生物类(Archaea)特性。虽然艾丁嗜盐小盒菌B2菌株在序列方面更接近细菌类(Bacteria)的16SrRNA,但它的序列也显示出与真核生物类(Eucarya)的某些特殊的相似性。在序列和结构方面,该菌与细菌类或真核生物类之间的相似程度要高于细菌类与真核生物类之间的相似程度。另外,该菌16SrRNA的序列与其它嗜盐菌序列相比较支持了以前的结论,即艾丁嗜盐小盒菌B2菌株应属于嗜盐小盒菌属(Haloarcula)的一新种。     

Adaptation of proteins from hyperthermophiles to high pressure and high temperature

Further clarification of the adaptations permitting the persistence of life at temperatures above 100 degrees C depends in part on the analysis of adaptive mechanisms at the protein level. The hyperthermophiles include both Bacteria and Archaea, although the majority of isolates growing at or above 100 degrees C are Archaea. Newly described adaptive features of hyperthermophiles include proteins whose structural integrity persists at temperatures up to 200 degrees C, and under elevated hydrostatic pressure, which in some cases adds significant increments of stability.     

Gene Descent, Duplication, and Horizontal Transfer in the Evolution of Glutamyl- and Glutaminyl-tRNA Synthetases

In translation, separate aminoacyl-tRNA synthetases attach the 20 different amino acids to their cognate tRNAs, with the exception of glutamine. Eukaryotes and some bacteria employ a specific glutaminyl-tRNA synthetase (GlnRS) which other Bacteria, the Archaea (archaebacteria), and organelles apparently lack. Instead, tRNA^Gln is initially acylated with glutamate by glutamyl-tRNA synthetase (GluRS), then the glutamate moiety is transamidated to glutamine. Lamour et al. [(1994) Proc Natl Acad Sci USA 91:8670–8674] suggested that an early duplication of the GluRS gene in eukaryotes gave rise to the gene for GlnRS—a copy of which was subsequently transferred to proteobacteria. However, questions remain about the occurrence of GlnRS genes among the Eucarya (eukaryotes) outside of the ``crown' taxa (animals, fungi, and plants), the distribution of GlnRS genes in the Bacteria, and their evolutionary relationships to genes from the Archaea. Here, we show that GlnRS occurs in the most deeply branching eukaryotes and that putative GluRS genes from the Archaea are more closely related to GlnRS and GluRS genes of the Eucarya than to those of Bacteria. There is still no evidence for the existence of GlnRS in the Archaea. We propose that the last common ancestor to contemporary cells, or cenancestor, used transamidation to synthesize Gln-tRNA^Gln and that both the Bacteria and the Archaea retained this pathway, while eukaryotes developed a specific GlnRS gene through the duplication of an existing GluRS gene. In the Bacteria, GlnRS genes have been identified in a total of 10 species from three highly diverse taxonomic groups: Thermus/Deinococcus, Proteobacteria γ/β subdivision, and Bacteroides/Cytophaga/Flexibacter. Although all bacterial GlnRS form a monophyletic group, the broad phyletic distribution of this tRNA synthetase suggests that multiple gene transfers from eukaryotes to bacteria occurred shortly after the Archaea–eukaryote divergence.     

Protein length in eukaryotic and prokaryotic proteomes

We analyzed length differences of eukaryotic, bacterial and archaeal proteins in relation to function, conservation and environmental factors. Comparing Eukaryotes and Prokaryotes, we found that the greater length of eukaryotic proteins is pervasive over all functional categories and involves the vast majority of protein families. The magnitude of these differences suggests that the evolution of eukaryotic proteins was influenced by processes of fusion of single-function proteins into extended multi-functional and multi-domain proteins. Comparing Bacteria and Archaea, we determined that the small but significant length difference observed between their proteins results from a combination of three factors: (i) bacterial proteomes include a greater proportion than archaeal proteomes of longer proteins involved in metabolism or cellular processes, (ii) within most functional classes, protein families unique to Bacteria are generally longer than protein families unique to Archaea and (iii) within the same protein family, homologs from Bacteria tend to be longer than the corresponding homologs from Archaea. These differences are interpreted with respect to evolutionary trends and prevailing environmental conditions within the two prokaryotic groups.     

The bacterial species dilemma and the genomic-phylogenetic species concept

The number of species of Bacteria and Archaea (ca 5000) is surprisingly small considering their early evolution, genetic diversity and residence in all ecosystems. The bacterial species definition accounts in part for the small number of named species. The primary procedures required to identify new species of Bacteria and Archaea are DNA-DNA hybridization and phenotypic characterization. Recently, 16S rRNA gene sequencing and phylogenetic analysis have been applied to bacterial taxonomy. Although 16S phylogeny is arguably excellent for classification of Bacteria and Archaea from the Domain level down to the family or genus, it lacks resolution below that level. Newer approaches, including multilocus sequence analysis, and genome sequence and microarray analyses, promise to provide necessary information to better understand bacterial speciation. Indeed, recent data using these approaches, while meagre, support the view that speciation processes may occur at the subspecies level within ecological niches (ecovars) and owing to biogeography (geovars). A major dilemma for bacterial taxonomists is how to incorporate this new information into the present hierarchical system for classification of Bacteria and Archaea without causing undesirable confusion and contention. This author proposes the genomic-phylogenetic species concept (GPSC) for the taxonomy of prokaryotes. The aim is twofold. First, the GPSC would provide a conceptual and testable framework for bacterial taxonomy. Second, the GPSC would replace the burdensome requirement for DNA hybridization presently needed to describe new species. Furthermore, the GPSC is consistent with the present treatment at higher taxonomic levels.     

Interrelationships between <Emphasis Type="Italic">Dunaliella</Emphasis> and halophilic prokaryotes in saltern crystallizer ponds

Thanks to their often very high population densities and their simple community structure, saltern crystallizer ponds form ideal sites to study the behavior of halophilic microorganisms in their natural environment at saturating salt concentrations. The microbial community is dominated by square red halophilic Archaea, recently isolated and described as Haloquadratum walsbyi, extremely halophilic red rod-shaped Bacteria of the genus Salinibacter, and the unicellular green alga Dunaliella as the primary producer. We review here, the information available on the microbial community structure of the saltern crystallizer brines and the interrelationships between the main components of their biota. As Dunaliella produces massive amounts of glycerol to provide osmotic stabilization, glycerol is often postulated to be the most important source of organic carbon for the heterotrophic prokaryotes in hypersaline ecosystems. We assess here, the current evidence for the possible importance of glycerol and other carbon sources in the nutrition of the Archaea and the Bacteria, the relative contribution of halophilic Bacteria and Archaea to the heterotrophic activity in the brines, and other factors that determine the nature of the microbial communities that thrive in the salt-saturated brines of saltern crystallizer ponds. Three-letter abbreviations for names of genera of Halobacteriaceae conform the recommendations of the ICSP Subcommittee on the Taxonomy of Halobacteriaceae.