Horizontal Gene Transfer in Aminoacyl-tRNA Synthetases Including Leucine-Specific Subtypes

Aminoacyl-tRNA synthetases catalyze a fundamental reaction for the flow of genetic information from RNA to protein. Their presence in all organisms known today highlights their important role in the early evolution of life. We investigated the evolutionary history of aminoacyl-tRNA synthetases on the basis of sequence data from more than 200 Archaea, Bacteria, and Eukaryota. Phylogenetic profiles are in agreement with previous observations that many genes for aminoacyl-tRNA synthetases were transferred horizontally between species from all domains of life. We extended these findings by a detailed analysis of the history of leucyl-tRNA synthetases. Thereby, we identified a previously undetected case of horizontal gene transfer from Bacteria to Archaea based on phylogenetic profiles, trees, and networks. This means that, finally, the last subfamily of aminoacyl-tRNA synthetases has lost its exceptional position as the sole subfamily that is devoid of horizontal gene transfer. Furthermore, the leucyl-tRNA synthetase phylogenetic tree suggests a dichotomy of the archaeal/eukaryotic-cytosolic and bacterial/eukaryotic-mitochondrial proteins. We argue that the traditional division of life into Prokaryota (non-chimeric) and Eukaryota (chimeric) is favorable compared to Woese’s trichotomy into Archaea/Bacteria/Eukaryota. Electronic Supplementary Material Electronic Supplementary material is available for this article at and accessible for authorised users. [Reviewing Editor: Dr. Yves Van de Peer]     

Recent advances in genetic analyses of hyperthermophilic Archaea and Bacteria

Hyperthermophilic Archaea and Bacteria are an extraordinarily important class of organisms for which genetic tools remain to be developed. Unique technological obstacles to this goal are posed by the thermophilic and, in some cases, strictly anaerobic nature of these organisms. However, recent advances in the cultivation of hyperthermophiles, in the discovery of genetic elements for vector development, and in the construction of genetic markers point toward the achievement of this goal in the near future. Transformation protocols have already been reported for Sulfolobus and Pyrococcus, and plasmid-mediated conjugation was recently found in Sulfolobus. Plasmids are available for Sulfolobus, Pyrococcus, and the bacterial hyperthermophile Thermotoga, and these provide the bases for vector construction in these hosts. A Desulfurococcus mobile intron may provide a novel means to introduce genes into a variety of archaeal hosts. With full genome sequences of several hyperthermophiles available soon, genetic tools will allow full exploitation of this information to study these organisms in depth and to utilize their unique properties in biotechnological applications. Received: 27 January 1997 / Accepted: 24 April 1997     

The effects of heavy meteorite bombardment on the early evolution — The emergence of the three Domains of life

A characteristic of many molecular phylogenies is that the three domains of life (Bacteria, Archaea, Eucarya) are clearly separated from each other. The analyses of ancient duplicated genes suggest that the last common ancestor of all presently known life forms already had been a sophisticated cellular prokaryote. These findings are in conflict with theories that have been proposed to explain the absence of deep branching lineages. In this paper we propose an alternative scenario, namely, a large meteorite impact that wiped out almost all life forms present on the early Earth. Following this nearly complete frustation of life on Earth, two surviving extreme thermophilic species gave rise to the now existing major groups of living organisms, the Bacteria and Archaea. [The latter also contributed the major portion to the nucleo-cytoplasmic component of the Eucarya]. An exact calibration of the molecular record with regard to time is not yet possible. The emergence of Eucarya in fossil and molecular records suggests that the proposed late impact should have occurred before 2100 million years before present (BP). If the 3500 million year old microfossils [Schopf, J. W. 1993: Science 260: 640–646] are interpreted as representatives of present day existing groups of bacteria (i.e., as cyanobacteria), then the impact is dated to around 3700 million years BP.The analysis of molecular sequences suggests that the separation between the Eucarya and the two prokaryotic domains is less deep then the separation between Bacteria and Archaea. The fundamental cell biological differences between Archaea and Eucarya were obtained over a comparatively short evolutionary distance (as measured in number of substitution events in biological macromolecules).Our interpretation of the molecular record suggests that life emerged early in Earth's history even before the time of the heavy bombardment was over. Early life forms already had colonized extreme habitats which allowed at least two prokaryotic species to survive a late nearly ocean boiling impact. The distribution of ecotypes on the rooted universal tree of life should not be interpreted as evidence that life originated in extremely hot environments.     

Model organisms for genetics in the domain Archaea: methanogens, halophiles, Thermococcales and Sulfolobales

The tree of life is split into three main branches: eukaryotes, bacteria, and archaea. Our knowledge of eukaryotic and bacteria cell biology has been built on a foundation of studies in model organisms, using the complementary approaches of genetics and biochemistry. Archaea have led to some exciting discoveries in the field of biochemistry, but archaeal genetics has been slow to get off the ground, not least because these organisms inhabit some of the more inhospitable places on earth and are therefore believed to be difficult to culture. In fact, many species can be cultivated with relative ease and there has been tremendous progress in the development of genetic tools for both major archaeal phyla, the Euryarchaeota and the Crenarchaeota. There are several model organisms available for methanogens, halophiles, and thermophiles; in the latter group, there are genetic systems for Sulfolobales and Thermococcales. In this review, we present the advantages and disadvantages of working with each archaeal group, give an overview of their different genetic systems, and direct the neophyte archaeologist to the most appropriate model organism.     

Isolation of haloarchaea that grow at low salinities

Summary Archaea, the third domain of life, were long thought to be limited to environmental extremes. However, the discovery of archaeal 16S rRNA gene sequences in water, sediment and soil samples has called into question the notion of Archaea as obligate extremophiles. Until now, none of these novel Archaea has been brought into culture, a critical step for discovering their ecological roles. We have cultivated three novel halophilic Archaea (haloarchaea) genotypes from sediments in which the pore-water salinity was close to that of sea water. All previously reported haloarchaeal isolates are obligate extreme halophiles requiring at least 9% (w/v) NaCl for growth and are typically the dominant heterotrophic organisms in salt and soda lakes, salt deposits and salterns. Two of these three newly isolated genotypes have lower requirements for salt than previously cultured haloarchaea and are capable of slow growth at sea-water salinity (2.5% w/v NaCl). Our data reveal the existence of Archaea that can grow in non-extreme conditions and of a diverse community of haloarchaea existing in coastal salt marsh sediments. Our findings suggest that the ecological range of these physiologically versatile prokaryotes is much wider than previously supposed.     

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.     

Taxol from fungal endophytes and the issue of biodiversity

Fungi represent one of the most understudied and diverse group of organisms. Commonly, these organisms make associations with higher life forms and may proceed to biochemically mimic the host organism. An excellent example of this is the anticancer drug, taxol, which had been previously supposed to occur only in the plant genusTaxus (yew). However, taxol has been reported in a novel endophytic fungus—Taxomyces andreanae, but also has been demonstrated to occur in a number of unrelated fungal endophytes includingPestalotia, Pestalotiopsis, Fusarium, Alternaria, Pithomyces, Monochaetia and others. Thus, this report presents information on the presence of taxol among disparate fungal genera, and uses these observations as an additional argument to support efforts to study fungal endophytes and preserve their associated host plants.     

On How Many Fundamental Kinds of Cells are Present on Earth: Looking for Phylogenetic Traits that Would Allow the Identification of the Primary Lines of Descent

The phylogenetic analyses as far as the identification of the number of domains of life is concerned have not reached a clear conclusion. In the attempt to improve this circumstance, I introduce the concept that the amino acids codified in the genetic code might be of markers with outstanding phylogenetic power. In particular, I hypothesise the existence of a biosphere populated, for instance, by three groups of organisms having different genetic codes because codifying at least a different amino acid. Evidently, these amino acids would mark the proteins that are present in the three groups of organisms in an unambiguous way. Therefore, in essence, this mark would not be other than the one that we usually try to make in the phylogenetic analyses in which we transform the protein sequences in phylogenetic trees, for the purpose to identify, for example, the domains of life. Indeed, this mark would allow to classify proteins without performing phylogenetic analyses because proteins belonging to a group of organisms would be recognisable as marked in a natural way by at least a different amino acid among the diverse groups of organisms. This conceptualisation answers the question of how many fundamental kinds of cells have evolved from the Last Universal Common Ancestor (LUCA), as the genetic code has unique proprieties that make the codified amino acids excellent phylogenetic markers. The presence of the formyl-methionine only in proteins of bacteria would mark them and would identify these as domain of life. On the other hand, the presence of pyrrolysine in the genetic code of the euryarchaeota would identify them such as another fundamental kind of cell evolved from the LUCA. Overall, the phylogenetic distribution of formyl-methionine and pyrrolysine would identify at least two domains of life—Bacteria and Archaea—but their number might be actually four; that is to say, Bacteria, Euryarchaeota, archeobacteria that are not euryarchaeota and Eukarya. The usually accepted domains of life represented by Bacteria, Archaea and Eukarya are not compatible with the phylogenetic distribution of these two amino acids and therefore this last classification might be mistaken.     

Divergent methylation pattern in adult stage between two forms of Tetranychus urticae (Acari: Tetranychidae)

The two‐spotted spider mite, Tetranychus urticae Koch has two forms: green form and red form. Understanding the molecular basis of how these two forms established without divergent genetic background is an intriguing area. As a well‐known epigenetic process, DNA methylation has particularly important roles in gene regulation and developmental variation across diverse organisms that do not alter genetic background. Here, to investigate whether DNA methylation could be associated with different phenotypic consequences in the two forms of T. urticae, we surveyed the genome‐wide cytosine methylation status and expression level of DNA methyltransferase 3 (Tudnmt3) throughout their entire life cycle. Methylation‐sensitive amplification polymorphism (MSAP) analyses of 585 loci revealed variable methylation patterns in the different developmental stages. In particular, principal coordinates analysis (PCoA) indicates a significant epigenetic differentiation between female adults of the two forms. The gene expression of Tudnmt3 was detected in all examined developmental stages, which was significantly different in the adult stage of the two forms. Together, our results reveal the epigenetic distance between the two forms of T. urticae, suggesting that DNA methylation might be implicated in different developmental demands, and contribute to different phenotypes in the adult stage of these two forms.     

Cellular differentiation and individuality in the ‘minor’ multicellular taxa

Biology needs a concept of individuality in order to distinguish organisms from parts of organisms and from groups of organisms, to count individuals and compare traits across taxa, and to distinguish growth from reproduction. Most of the proposed criteria for individuality were designed for ‘unitary’ or ‘paradigm’ organisms: contiguous, functionally and physiologically integrated, obligately sexually reproducing multicellular organisms with a germ line sequestered early in development. However, the vast majority of the diversity of life on Earth does not conform to all of these criteria. We consider the issue of individuality in the ‘minor’ multicellular taxa, which collectively span a large portion of the eukaryotic tree of life, reviewing their general features and focusing on a model species for each group. When the criteria designed for unitary organisms are applied to other groups, they often give conflicting answers or no answer at all to the question of whether or not a given unit is an individual. Complex life cycles, intimate bacterial symbioses, aggregative development, and strange genetic features complicate the picture. The great age of some of the groups considered shows that ‘intermediate’ forms, those with some but not all of the traits traditionally associated with individuality, cannot reasonably be considered ephemeral or assumed transitional. We discuss a handful of recent attempts to reconcile the many proposed criteria for individuality and to provide criteria that can be applied across all the domains of life. Finally, we argue that individuality should be defined without reference to any particular taxon and that understanding the emergence of new kinds of individuals requires recognizing individuality as a matter of degree.     

Temperature modulation and the presence of C20 fatty acids in mono‐ and digalactosyldiacylglycerol of Euglena gracilis and Lepocinclis acus: A modern interpretation of euglenid galactolipids using positive‐ion electrospray ionization/mass spectrometry

Mono‐ and digalactosyldiacylglycerol (MGDG and DGDG, respectively) are important galactolipids that comprise photosynthetic membranes in almost all photosynthetic organisms. Intact forms of MGDG and DGDG of Euglena gracilis and Lepocinclis acus, two example euglenids with secondary plastids of green algal origin, were elucidated with fatty acid regiochemistry via positive‐ion electrospray ionization/mass spectrometry at two growth temperatures. At 20°C, E. gracilis and L. acus produced predominantly 18:3/16:4 (sn‐1/sn‐2) MGDG, whereas at 30°C this was supplanted by 18:2/16:2 MGDG. At both temperatures were also observed a variety of other MGDG and DGDG forms, including C₂₀ fatty acid‐containing forms not expected in a green algal‐derived plastid. In addition to providing structural details of MGDG and DGDG not available in past studies, these results suggest a previously unknown relationship between these two organisms and the red algae. This study also illustrates that temperature modulation of galactolipids occurs via modification of unsaturation of both the sn‐1 and sn‐2 fatty acids; this is fundamentally different from previously published studies from our laboratory on other algal classes.     

Protein transport in Archaea: Sec and twin arginine translocation pathways

The transport of proteins into and across hydrophobic membranes is an essential cellular process. The majority of proteins that are translocated in an unfolded conformation traverse the membrane by way of the universally conserved Sec pathway, whereas the twin arginine translocation pathway is responsible for the transport of folded proteins across the membrane. Structural, biochemical and genetic analyses of these processes in Archaea have revealed unique archaeal features, and have also provided a better understanding of these pathways in organisms of all domains. Further study of these pathways in Archaea might elucidate fundamental principles involved in each type of transport and could help determine their relative costs and benefits as well as evolutionary adaptations in protein secretion strategies.     

Transcriptional regulation in Archaea

During the past few decades, it has become clear that microorganisms can thrive under the most diverse conditions, including extremes of temperature, pressure, salinity and pH. Most of these extremophilic organisms belong to the third domain of life, that of the Archaea. The organisms of this domain are of particular interest because most informational systems that are associated with archaeal genomes and their expression are reminiscent of those seen in Eucarya, whereas, most of their metabolic aspects are similar to those of Bacteria. A better understanding of the regulatory mechanisms of gene expression in Archaea will, therefore, help to integrate the body of knowledge regarding the regulatory mechanisms that underlie gene expression in all three domains of life.     

Size comparisons among integral membrane transport protein homologues in bacteria, Archaea, and Eucarya

Integral membrane proteins from over 20 ubiquitous families of channels, secondary carriers, and primary active transporters were analyzed for average size differences between homologues from the three domains of life: Bacteria, Archaea, and Eucarya. The results showed that while eucaryotic homologues are consistently larger than their bacterial counterparts, archaeal homologues are significantly smaller. These size differences proved to be due primarily to variations in the sizes of hydrophilic domains localized to the N termini, the C termini, or specific loops between transmembrane alpha-helical spanners, depending on the family. Within the Eucarya domain, plant homologues proved to be substantially smaller than their animal and fungal counterparts. By contrast, extracytoplasmic receptors of ABC-type uptake systems in Archaea proved to be larger on average than those of their bacterial homologues, while cytoplasmic enzymes from different organisms exhibited little or no significant size differences. These observations presumably reflect evolutionary pressure and molecular mechanisms that must have been operative since these groups of organisms diverged from each other.     

Diversification of Ferredoxins across Living Organisms

Ferredoxins, iron-sulfur (Fe-S) cluster proteins, play a key role in oxidoreduction reactions. To date, evolutionary analysis of these proteins across the domains of life have been confined to observing the abundance of Fe-S cluster types (2Fe-2S, 3Fe-4S, 4Fe-4S, 7Fe-8S (3Fe-4s and 4Fe-4S) and 2[4Fe-4S]) and the diversity of ferredoxins within these cluster types was not studied. To address this research gap, here we propose a subtype classification and nomenclature for ferredoxins based on the characteristic spacing between the cysteine amino acids of the Fe-S binding motif as a subtype signature to assess the diversity of ferredoxins across the living organisms. To test this hypothesis, comparative analysis of ferredoxins between bacterial groups, Alphaproteobacteria and Firmicutes and ferredoxins collected from species of different domains of life that are reported in the literature has been carried out. Ferredoxins were found to be highly diverse within their types. Large numbers of alphaproteobacterial species ferredoxin subtypes were found in Firmicutes species and the same ferredoxin subtypes across the species of Bacteria, Archaea, and Eukarya, suggesting shared common ancestral origin of ferredoxins between Archaea and Bacteria and lateral gene transfer of ferredoxins from prokaryotes (Archaea/Bacteria) to eukaryotes. This study opened new vistas for further analysis of diversity of ferredoxins in living organisms.     

STUDIES OF CARBONIFEROUS FUNGI. II. THE STRUCTURE AND ORGANIZATION OF MYCOCARPON,SPOROCARPON, DUBIOCARPON,AND COLEOCARPON (ASCOMYCOTINA)

The problematic organism, Sporocarpon, was among the first fossil fungi to be described. The genus was actually a heterogeneous assemblage of fungal forms, and was eventually divided into several taxa including Sporocarpon, Dubiocarpon, and Mycocarpon. In the present paper these organisms, as well as a similar, previously undescribed genus, Coleocarpon; are described from Lower, Middle, and Upper Pennsylvanian strata in North America, and from Upper Carboniferous sediments in England. Although initially considered to be radiolarian-like protozoa, these structures show far more similarity to ascomycetous cleistothecia. All forms are ornamented, spherical bodies with a complex wall which encloses scattered asci and ascospores. Taxa are distinguished primarily by differences in the organization of the cleistothecial wall. Structurally similar organisms are found today among the Eurotiales.     

What Does the Microsporidian <Emphasis Type="Italic">E. cuniculi</Emphasis> Tell Us About the Origin of the Eukaryotic Cell?

The relationship among the three cellular domains Archaea, Bacteria, and Eukarya has become a central problem in unraveling the tree of life. This relationship can now be studied as the completely sequenced genomes of representatives of these cellular domains become available. We performed a bioinformatic investigation of the Encephalitozoon cuniculi proteome. E. cuniculi has the smallest sequenced eukaryotic genome, 2.9 megabases coding for 1997 proteins. The proteins of E. cuniculi were compared with a previously characterized set of eukaryotic signature proteins (ESPs). ESPs are found in a eukaryotic cell, whether from an animal, a plant, a fungus, or a protozoan, but are not found in the Archaea and the Bacteria. We demonstrated that 85% of the ESPs have significant sequence similarity to proteins in E. cuniculi. Hence, E. cuniculi, a minimal eukaryotic cell that has removed all inessential proteins, still preserves most of the ESPs that make it a member of the Eukarya. The locations and functions of these ESPs point to the earliest history of eukaryotes.Reviewing Editor: Dr. Manyuan Long     

Glycobiology of surface layer proteins

Over the last two decades, a significant change of perception has taken place regarding prokaryotic glycoproteins. For many years, protein glycosylation was assumed to be limited to eukaryotes; but now, a wealth of information on structure, function, biosynthesis and molecular biology of prokaryotic glycoproteins has accumulated, with surface layer (S-layer) glycoproteins being one of the best studied examples. With the designation of Archaea as a second prokaryotic domain of life, the occurrence of glycosylated S-layer proteins had been considered a taxonomic criterion for differentiation between Bacteria and Archaea. Extensive structural investigations, however, have demonstrated that S-layer glycoproteins are present in both domains. Among Gram-positive bacteria, S-layer glycoproteins have been identified only in bacilli. In Gram-negative organisms, their presence is still not fully investigated; presently, there is no indication for their existence in this class of bacteria. Extensive biochemical studies of the S-layer glycoprotein from Halobacterium halobium have, at least in part, unravelled the glycosylation pathway in Archaea; molecular biological analyses of these pathways have not been performed, so far. Significant observations concern the occurrence of unusual linkage regions both in archaeal and bacterial S-layer glycoproteins. Regarding S-layer glycoproteins of bacteria, first genetic data have shed some light into the molecular organization of the glycosylation machinery in this domain. In addition to basic S-layer glycoprotein research, the biotechnological application potential of these molecules has been explored. With the development of straightforward molecular biological methods, fascinating possibilities for the expression of prokaryotic glycoproteins will become available. S-layer glycoprotein research has opened up opportunities for the production of recombinant glycosylation enzymes and tailor-made S-layer glycoproteins in large quantities, which are commercially not yet available. These bacterial systems may provide economic technologies for the production of biotechnologically and medically important glycan structures in the future.