Archaeal habitats--from the extreme to the ordinary

The domain Archaea represents a third line of evolutionary descent, separate from Bacteria and Eucarya. Initial studies seemed to limit archaea to various extreme environments. These included habitats at the extreme limits that allow life on earth, in terms of temperature, pH, salinity, and anaerobiosis, which were the homes to hyper thermo philes, extreme (thermo)acidophiles, extreme halophiles, and methanogens. Typical environments from which pure cultures of archaeal species have been isolated include hot springs, hydrothermal vents, solfataras, salt lakes, soda lakes, sewage digesters, and the rumen. Within the past two decades, the use of molecular techniques, including PCR-based amplification of 16S rRNA genes, has allowed a culture-independent assessment of microbial diversity. Remarkably, such techniques have indicated a wide distribution of mostly uncultured archaea in normal habitats, such as ocean waters, lake waters, and soil. This review discusses organisms from the domain Archaea in the context of the environments where they have been isolated or detected. For organizational purposes, the domain has been separated into the traditional groups of methanogens, extreme halophiles, thermoacidophiles, and hyperthermophiles, as well as the uncultured archaea detected by molecular means. Where possible, we have correlated known energy-yielding reactions and carbon sources of the archaeal types with available data on potential carbon sources and electron donors and acceptors present in the environments. From the broad distribution, metabolic diversity, and sheer numbers of archaea in environments from the extreme to the ordinary, the roles that the Archaea play in the ecosystems have been grossly underestimated and are worthy of much greater scrutiny.     

Protein Ser/Thr/Tyr Phosphorylation in the Archaea

The third domain of life, the Archaea (formerly Archaebacteria), is populated by a physiologically diverse set of microorganisms, many of which reside at the ecological extremes of our global environment. Although ostensibly prokaryotic in morphology, the Archaea share much closer evolutionary ties with the Eukarya than with the superficially more similar Bacteria. Initial genomic, proteomic, and biochemical analyses have revealed the presence of “eukaryotic” protein kinases and phosphatases and an intriguing set of serine-, threonine-, and tyrosine-phosphorylated proteins in the Archaea that may offer new insights into this important regulatory mechanism.     

The bioenergetic basis for the decrease in metabolic diversity at increasing salt concentrations: implications for the functioning of salt lake ecosystems

Examination of the microbial diversity in hypersaline lakes of increasing salt concentrations shows that certain types of dissimilatory metabolism do not occur at the highest salinities. Examples are methanogenesis from hydrogen and carbon dioxide or from acetate, dissimilatory sulfate reduction with oxidation of acetate, and autotrophic nitrification. The observations can be explained on the basis of the energetic cost of haloadaptation used by the different metabolic groups and the free-energy change associated with the dissimilatory reactions. All halophilic microorganisms spend large amounts of energy to maintain steep gradients of Na⁺ and K⁺concentrations across their cytoplasmic membrane. Most Bacteria and also the methanogenic Archaea produce high intracellular concentrations of organic osmotic solutes at a high energetic cost. The halophilic aerobic Archaea (order Halobacteriales) and the halophilic fermentative Bacteria (order Halanaerobiales) use KCl as the main intracellular solute. This strategy, while requiring far-reaching adaptations of the intracellular machinery, is energetically more favorable than production of organic compatible solutes. By combining information on the amount of energy available to each physiological group and the strategy used to cope with salt stress, a coherent model emerges that provides explanations for the upper salinity limit at which the different microbial conversions occur in hypersaline lakes.     

Bacillus species in the intestine of termites and other soil invertebrates

Soil invertebrates harbour a complex microbial community in their intestinal system. The total number of microbes in the hindgut of soil invertebrates can reach a titre of 10(11) ml(-1). The gut microbes play an indispensable role in the digestion of food and are of ecological importance in the global carbon cycle. The gut microbiota can include a variety of micro-organisms from the three domains Bacteria, Archaea and Eucarya. The bacterial groups from the intestinal systems are mainly affiliated to the proteobacteria, the gram-positive groups Firmicutes and Actinobacteria, the Bacteroides/Flavobacterium branch and the spirochetes. The Archaea are represented by methanogens. The eukaryotic groups consist of protozoa, yeasts and fungi. Intestinal bacteria are involved in the degradation of cellulose, hemicellulose and aromatic compounds as well as nitrogen fixation. They also contribute to the redox status of the gut. Bacilli form a significant portion of the intestinal microbial community of soil invertebrates, especially among cellulose degraders. The diversity and function of bacilli in soil invertebrates will be discussed in this paper.     

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.     

古菌在红树林沉积物中的多样性及其碳代谢机制

红树林湿地生态系统具有维持生物多样性、净化环境及维持海岸带生态平衡等多种功能。古菌普遍存在于红树林沉积物中,在元素的生物地球化学循环中发挥着重要作用。古菌具有丰富的碳代谢多样性,能固定CO_2,参与甲烷循环,产乙酸,降解蛋白质、多聚碳水化合物等有机质,但目前对于红树林沉积物中古菌碳代谢的研究才刚刚起步。高通量测序技术的快速发展促进了大量新的古菌门类的发现,这些新的古菌门类具备多样的碳代谢潜力。本文简要概述古菌的主要类群与分布,综述国内外有关古菌碳代谢多样性的最新研究进展,并阐明这些古菌在红树林生态系统中的生态分布和功能特征,为进一步探究古菌代谢机制提供知识基础。     

On the evolution of the tRNA-dependent amidotransferases, GatCAB and GatDE

Glutaminyl-tRNA synthetase and asparaginyl-tRNA synthetase evolved from glutamyl-tRNA synthetase and aspartyl-tRNA synthetase, respectively, after the split in the last universal communal ancestor (LUCA). Glutaminyl-tRNA^Gln and asparaginyl-tRNA^Asn were likely formed in LUCA by amidation of the mischarged species, glutamyl-tRNA^Gln and aspartyl-tRNA^Asn, by tRNA-dependent amidotransferases, as is still the case in most bacteria and all known archaea. The amidotransferase GatCAB is found in both domains of life, while the heterodimeric amidotransferase GatDE is found only in Archaea. The GatB and GatE subunits belong to a unique protein family that includes Pet112 that is encoded in the nuclear genomes of numerous eukaryotes. GatE was thought to have evolved from GatB after the emergence of the modern lines of decent. Our phylogenetic analysis though places the split between GatE and GatB, prior to the phylogenetic divide between Bacteria and Archaea, and Pet112 to be of mitochondrial origin. In addition, GatD appears to have emerged prior to the bacterial-archaeal phylogenetic divide. Thus, while GatDE is an archaeal signature protein, it likely was present in LUCA together with GatCAB. Archaea retained both amidotransferases, while Bacteria emerged with only GatCAB. The presence of GatDE has favored a unique archaeal tRNA^Gln that may be preventing the acquisition of glutaminyl-tRNA synthetase in Archaea. Archaeal GatCAB, on the other hand, has not favored a distinct tRNA^Asn, suggesting that tRNA^Asn recognition is not a major barrier to the retention of asparaginyl-tRNA synthetase in many Archaea.     

Membrane binding of ribosomes occurs at SecYE-based sites in the Archaea Haloferax volcanii

Whereas ribosomes bind to membranes at eukaryal Sec61alphabetagamma and bacterial SecYEG sites, ribosomal membrane binding has yet to be studied in Archaea. Accordingly, functional ribosomes and inverted membrane vesicles were prepared from the halophilic archaea Haloferax volcanii. The ability of the ribosomes to bind to the membranes was determined using a flotation approach. Proteolytic pretreatment of the vesicles, as well as quantitative analyses, revealed the existence of a proteinaceous ribosome receptor, with the affinity of binding being comparable to that found in Eukarya and Bacteria. Inverted membrane vesicles prepared from cells expressing chimeras of SecE or SecY fused to a cytoplasmically oriented cellulose-binding domain displayed reduced ribosome binding due to steric hindrance. Pretreatment with cellulose drastically reduced ribosome binding to chimera-containing but not wild-type vesicles. Thus, as in Eukarya and Bacteria, ribosome binding in Archaea occurs at Sec-based sites. However, unlike the situation in the other domains of Life, ribosome binding in haloarchaea requires molar concentrations of salt. Structural information on ribosome-Sec complexes may provide insight into this high salt-dependent binding.     

RNase P: interface of the RNA and protein worlds

Ribonuclease P (RNase P) is an endonuclease involved in processing tRNA. It contains both RNA and protein subunits and occurs in all three domains of life: namely, Archaea, Bacteria and Eukarya. The RNase P RNA subunits from bacteria and some archaea are catalytically active in vitro, whereas those from eukaryotes and most archaea require protein subunits for activity. RNase P has been characterized biochemically and genetically in several systems, and detailed structural information is emerging for both RNA and protein subunits from phylogenetically diverse organisms. In vitro reconstitution of activity is providing insight into the role of proteins in the RNase P holoenzyme. Together, these findings are beginning to impart an understanding of the coevolution of the RNA and protein worlds.     

The unique DNA topology and DNA topoisomerases of hyperthermophilic archaea

Abstract: Hyperthermophilic archaea exhibit a unique pattern of DNA topoisomerase activities. They have a peculiar enzyme, reverse gyrase, which introduces positive superturns into DNA at the expense of ATP. This enzyme has been found in all hyperthermophiles tested so far (including Bacteria) but never in mesophiles. Reverse gyrases are formed by the association of a helicase-like domain and a 5'-type I DNA topoisomerase. These two domains might be located on the same polypeptide. However, in the methanogenic archaeon Methanopyrus kandleri , the topoisomerase domain is divided between two subunits. Besides reverse gyrase, Archaea contain other type I DNA topoisomerases; in particular, M. kandleri harbors the only known procaryotic 3'-type I DNA topoisomerase (Topo V). Hyperthermophilic archaea also exhibit specific type II DNA topoisomerases (Topo II), i.e. whereas mesophilic Bacteria have a Topo II that produces negative supercoiling (DNA gyrase), the Topo II from Sulfolobus and Pyrococcus lack gyrase activity and are the smallest enzymes of this type known so far. This peculiar pattern of DNA topoisomerases in hyperthermophilic archaea is paralleled by a unique DNA topology, i.e. whereas DNA isolated from Bacteria and Eucarya is negatively supercoiled, plasmidic DNA from hyperthermophilic archaea are from relaxed to positively supercoiled. The possible evolutionary implications of these findings are discussed in this review. We speculate that gyrase activity in mesophiles and reverse gyrase activity in hyperthermophiles might have originated in the course of procaryote evolution to balance the effect of temperature changes on DNA structure.     

Bioenergetics of the Archaea

In the late 1970s, on the basis of rRNA phylogeny, Archaea (archaebacteria) was identified as a distinct domain of life besides Bacteria (eubacteria) and Eucarya. Though forming a separate domain, archaea display an enormous diversity of lifestyles and metabolic capabilities. Many archaeal species are adapted to extreme environments with respect to salinity, temperatures around the boiling point of water, and/or extremely alkaline or acidic pH. This has posed the challenge of studying the molecular and mechanistic bases on which these organisms can cope with such adverse conditions. This review considers our cumulative knowledge on archaeal mechanisms of primary energy conservation, in relationship to those of bacteria and eucarya. Although the universal principle of chemiosmotic energy conservation also holds for Archaea, distinct features have been discovered with respect to novel ion-transducing, membrane-residing protein complexes and the use of novel cofactors in bioenergetics of methanogenesis. From aerobically respiring archaea, unusual electron-transporting supercomplexes could be isolated and functionally resolved, and a proposal on the organization of archaeal electron transport chains has been presented. The unique functions of archaeal rhodopsins as sensory systems and as proton or chloride pumps have been elucidated on the basis of recent structural information on the atomic scale. Whereas components of methanogenesis and of phototrophic energy transduction in halobacteria appear to be unique to archaea, respiratory complexes and the ATP synthase exhibit some chimeric features with respect to their evolutionary origin. Nevertheless, archaeal ATP synthases are to be considered distinct members of this family of secondary energy transducers. A major challenge to future investigations is the development of archaeal genetic transformation systems, in order to gain access to the regulation of bioenergetic systems and to overproducers of archaeal membrane proteins as a prerequisite for their crystallization.     

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.     

海洋古菌多样性研究进展

海洋古菌是海洋微生物中的一个大的类群,然而绝大多数的古菌不能分离培养.近年来分子生物学的方法广泛地应用于微生物多样性的研究中,研究发现,海洋古菌广泛地生活在各类海域环境中,而不仅仅是生活在极端的环境中.海洋古菌为海洋生态系统中主要的原核细胞成分,在海洋生态系统中的物质与能量循环中扮演着重要角色.主要阐述了生活在海洋不同环境中海洋古菌的多样性,有海洋浮游古菌的多样性、海底环境及海洋沉积物中古菌的多样性、附着或寄共生古菌多样性等的研究状况,以及研究海洋古菌多样性的分子生物学的主要方法.     

Purification,overproduction, and partial characterization of beta-RFAP synthase,a key enzyme in the methanopterin biosynthesis pathway

Methanopterin is a folate analog involved in the C1 metabolism of methanogenic archaea, sulfate-reducing archaea, and methylotrophic bacteria. Although a pathway for methanopterin biosynthesis has been described in methanogens, little is known about the enzymes and genes involved in the biosynthetic pathway. The enzyme beta-ribofuranosylaminobenzene 5'-phosphate synthase (beta-RFAP synthase) catalyzes the first unique step to be identified in the pathway of methanopterin biosynthesis, namely, the condensation of p-aminobenzoic acid with phosphoribosylpyrophosphate to form beta-RFAP, CO2, and inorganic pyrophosphate. The enzyme catalyzing this reaction has not been purified to homogeneity, and the gene encoding beta-RFAP synthase has not yet been identified. In the present work, we report on the purification to homogeneity of beta-RFAP synthase. The enzyme was purified from the methane-producing archaeon Methanosarcina thermophila, and the N-terminal sequence of the protein was used to identify corresponding genes from several archaea, including the methanogen Methanococcus jannaschii and the sulfate-reducing archaeon Archaeoglobus fulgidus. The putative beta-RFAP synthase gene from A. fulgidus was expressed in Escherichia coli, and the enzymatic activity of the recombinant gene product was verified. A BLAST search using the deduced amino acid sequence of the beta-RFAP synthase gene identified homologs in additional archaea and in a gene cluster required for C1 metabolism by the bacterium Methylobacterium extorquens. The identification of a gene encoding a potential beta-RFAP synthase in M. extorquens is the first report of a putative methanopterin biosynthetic gene found in the Bacteria and provides evidence that the pathways of methanopterin biosynthesis in Bacteria and Archaea are similar.     

Membrane binding of SRP pathway components in the halophilic archaea Haloferax volcanii.

Across evolution, the signal recognition particle pathway targets extra-cytoplasmic proteins to membranous translocation sites. Whereas the pathway has been extensively studied in Eukarya and Bacteria, little is known of this system in Archaea. In the following, membrane association of FtsY, the prokaryal signal recognition particle receptor, and SRP54, a central component of the signal recognition particle, was addressed in the halophilic archaea Haloferax volcanii. Purified H. volcanii FtsY, the FtsY C-terminal GTP-binding domain (NG domain) or SRP54, were combined separately or in different combinations with H. volcanii inverted membrane vesicles and examined by gradient floatation to differentiate between soluble and membrane-bound protein. Such studies revealed that both FtsY and the FtsY NG domain bound to H. volcanii vesicles in a manner unaffected by proteolytic pretreatment of the membranes, implying that in Archaea, FtsY association is mediated through the membrane lipids. Indeed, membrane association of FtsY was also detected in intact H. volcanii cells. The contribution of the NG domain to FtsY binding in halophilic archaea may be considerable, given the low number of basic charges found at the start of the N-terminal acidic domain of haloarchaeal FtsY proteins (the region of the protein thought to mediate FtsY-membrane association in Bacteria). Moreover, FtsY, but not the NG domain, was shown to mediate membrane association of H. volcanii SRP54, a protein that did not otherwise interact with the membrane.     

Diversity and Spatial Distribution of Prokaryotic Communities Along A Sediment Vertical Profile of A Deep-Sea Mud Volcano

We investigated the top 30-cm sediment prokaryotic community structure in 5-cm spatial resolution, at an active site of the Amsterdam mud volcano, East Mediterranean Sea, based on the 16S rRNA gene diversity. A total of 339 and 526 sequences were retrieved, corresponding to 25 and 213 unique (≥98% similarity) phylotypes of Archaea and Bacteria, respectively, in all depths. The Shannon–Wiener diversity index H was higher for Bacteria (1.92–4.03) than for Archaea (0.99–1.91) and varied differently between the two groups. Archaea were dominated by anaerobic methanotrophs ANME-1, -2 and -3 groups and were related to phylotypes involved in anaerobic oxidation of methane from similar habitats. The much more complex Bacteria community consisted of 20 phylogenetic groups at the phylum/candidate division level. Proteobacteria, in particular δ-Proteobacteria, was the dominant group. In most sediment layers, the dominant phylotypes of both the Archaea and Bacteria communities were found in neighbouring layers, suggesting some overlap in species richness. The similarity of certain prokaryotic communities was also depicted by using four different similarity indices. The direct comparison of the retrieved phylotypes with those from the Kazan mud volcano of the same field revealed that 40.0% of the Archaea and 16.9% of the Bacteria phylotypes are common between the two systems. The majority of these phylotypes are closely related to phylotypes originating from other mud volcanoes, implying a degree of endemicity in these systems.     

Doing it in reverse: 3'-to-5' polymerization by the Thg1 superfamily

The tRNA(His) guanylyltransferase (Thg1) family of enzymes comprises members from all three domains of life (Eucarya, Bacteria, Archaea). Although the initial activity associated with Thg1 enzymes was a single 3'-to-5' nucleotide addition reaction that specifies tRNA(His) identity in eukaryotes, the discovery of a generalized base pair-dependent 3'-to-5' polymerase reaction greatly expanded the scope of Thg1 family-catalyzed reactions to include tRNA repair and editing activities in bacteria, archaea, and organelles. While the identification of the 3'-to-5' polymerase activity associated with Thg1 enzymes is relatively recent, the roots of this discovery and its likely physiological relevance were described ≈ 30 yr ago. Here we review recent advances toward understanding diverse Thg1 family enzyme functions and mechanisms. We also discuss possible evolutionary origins of Thg1 family-catalyzed 3'-to-5' addition activities and their implications for the currently observed phylogenetic distribution of Thg1-related enzymes in biology.     

Phylogenomic analysis of lipid biosynthetic genes of Archaea shed light on the ‘lipid divide’

The lipid membrane is one of the most characteristic traits distinguishing the three domains of life. Membrane lipids of Bacteria and Eukarya are composed of fatty acids linked to glycerol‐3‐phosphate (G3P) via ester bonds, while those of Archaea possess isoprene‐based alkyl chains linked by ether linkages to glycerol‐1‐phosphate (G1P), resulting in the opposite stereochemistry of the glycerol phosphate backbone. This ‘lipid divide’ has raised questions on the evolution of microbial life since eukaryotes are thought to have evolved from the Archaea, requiring a radical change in membrane composition. Here, we searched for homologs of enzymes involved in membrane lipid and fatty acid synthesis in a wide variety of archaeal genomes and performed phylogenomic analyses. We found that two uncultured archaeal groups, i.e. marine euryarchaeota group II/III and ‘Lokiarchaeota’, recently discovered descendants of the archaeal ancestor leading to eukaryotes, lack the gene to synthesize G1P and, consequently, the capacity to synthesize archaeal membrane lipids. However, our analyses reveal their genetic capacity to synthesize G3P‐based ‘chimeric lipids’ with either two ether‐bound isoprenoidal chains or with an ester‐bound fatty acid instead of an ether‐bound isoprenoid. These archaea may reflect the ‘archaea‐to‐eukaryote’ membrane transition stage which have led to the current ‘lipid divide’.     

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.