Archaeal and bacterial community composition of sediment and plankton from a suboxic freshwater pond

We studied the composition of archaeal and bacterial communities present in the sediment and plankton of a shallow suboxic-to-anoxic freshwater pond with high organic matter input, as an example of a kind of inland freshwater system widely distributed in forests of temperate regions. Molecular surveys based on small subunit rRNA genes showed a remarkably high diversity of lineages within the Bacteria, with a total of 18 phyla or candidate divisions being detected, in addition to a few highly divergent phylotypes of unknown affiliation. We identified members of the five subdivisions of the Proteobacteria, as well as Acidobacteria, Verrucomicrobia, Planctomycetes, Bacteroidetes, Chlorobi, Actinobacteria, Firmicutes, Chloroflexi, Gemmatimonadetes, Spirochaetes, Fibrobacteres and the candidate divisions OD1, OP11, TM6, WS1, WS6 and Termite Group 1 ("Endobacteria"). Candidate division OD1 and beta-Proteobacteria were dominant in the environmental libraries of plankton and sediment, respectively. Archaea were also very diverse, but only members of the Euryarchaeota, including Methanosarcinales, Methanomicrobiales and some divergent lineages, were identified. The application of various species richness estimators confirmed the highly diverse nature of both plankton and sediment samples. The pond is a microbial-based complex ecosystem mainly fueled by the degradation of allochthonous organic matter that maintains tightly coupled carbon and sulfur cycles.

Eukaryotic diversity associated with carbonates and fluid?seawater interface in Lost City hydrothermal field

Lost City is a unique off-axis hydrothermal vent field characterized by highly alkaline and relatively low-temperature fluids that harbours huge carbonate chimneys. We have carried out a molecular survey based on 18S rDNA sequences of the eukaryotic communities associated with fluid-seawater interfaces and with carbonates from venting areas and the chimney wall. Our study reveals a variety of lineages belonging to eight major taxa: Metazoa, Fungi, Heterokonta (Stramenopiles), Alveolata, Radiolaria, Cercozoa, Heterolobosea and Euglenozoa. We detected one fungal lineage that appears to be widespread in hydrothermal systems both submarine and continental. Alveolates were the most abundant and diverse group in Lost City samples, although their distribution was very different in carbonate, where ciliates dominated, and in fluid-seawater libraries, where dinoflagellates, Group I and Group II (Syndiniales) marine alveolates were profuse. Similarly, Euglenozoa also displayed a differential distribution, kinetoplastids being present on carbonates and a novel group of diplonemids so far exclusively observed in the deep sea being dominant in fluid-seawater libraries. Protist lineages identified in this ecosystem likely correspond to grazers, decomposers and parasites, playing key roles in the food web of the Lost City ecosystem.

Uncultured Archaea in a hydrothermal microbial assemblage: phylogenetic diversity and characterization of a genome fragment from a euryarchaeote

The polychaete Alvinella pompejana lives in organic tubes on the walls of active hydrothermal chimneys along the East Pacific Rise. To examine the diversity of the archaeal community associated with the polychaete tubes, we constructed libraries by direct PCR amplification and cloning of 16S rRNA genes. Almost half of the sequences of the 16S rRNA gene libraries clustered with uncultured archaeal groups. In an effort to access genomic information from uncultured archaeal members we further constructed a fosmid library from the same DNA source. One of the clones, Alv-FOS5, was sequenced completely. Its sequence analysis revealed an incomplete rRNA operon and 32 predicted ORFs. Seventeen of these ORFs have been assigned putative functions, including transcription and translation, cellular processes and signalling, transport systems and metabolic pathways. Phylogenetic analyses of the 16S rRNA gene suggested that Alv-FOS5 formed a new lineage related to members of Deep-Sea Hydrothermal Vent Euryarchaeota group II. Phylogenetic analyses of predicted proteins revealed the existence of likely cases of horizontal gene transfer, both between Crenarchaeota and Euryarchaeota and between Archaea and Bacteria. This study is the first step in using genomics to reveal the physiology of an as yet uncultured group of archaea from deep-sea hydrothermal vents.

Mature data on neoadjuvant capecitabine chemoradiation (X-RT) for patients (pts) with locally advanced breast cancer (LABC) failing anthracycline-based neoadjuvant therapy

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Background: In Brazil, LABC remains a serious health problem, representing approx. 30% of all newly diagnosed breast cancers. Anthracycline-based neoadjuvant therapy is a standard treatment, but around 30% of pts do not respond. There is no standard approach in these refractory pts. In our institution, these pts receive RT, but almost half (46%) of pts are not rendered operable by RT alone. Because X is the reference treatment for anthracycline- and/or taxane-pretreated MBC and X and RT are supra-additive in in vivo models, there is a clear rationale for evaluating X-RT in this setting. Methods: Pts eligible for this prospective, open-label, single-center, non-randomized study had inoperable LABC refractory to FAC, ECOG PS ≥1 and adequate organ functions. Pts received RT 20c Gy/d ×5w (total dose 50Gy) plus X 850mg/m2 bid orally d1–14, q3w for 2 cycles. Pts underwent surgery, if possible, after completion of neoadjuvant therapy. Pts with hormone receptor-positive tumors received tamoxifen after surgery. Results: Baseline characteristics of the 30 pts enrolled between Jan 2003 and May 2004: median age 47 years (range, 26–70); median ECOG PS 1; median tumor size (after anthracyclines) 80 cm2 (range, 36–357cm2); tumor grade II/III/unknown 20/37/43%; inflammatory carcinoma 21%. Two pts were excluded from this analysis as they received the incorrect X dosing regimen. 23/28 evaluable pts (82%) were operable after X-RT; 4 (14%) pts did not undergo surgery because of disease progression. Median tumor size after X-RT was 49 cm2 (range, 6–196 cm2). The median relative reduction in tumor size was 33%. After surgery, median residual tumor size was 12 cm2 (range, 0−72) and the median number of positive nodes was 2 (range, 0−27). Pathological complete response was observed in 3 (11%) pts. The most common treatment-related adverse events (all grade 1/2) were mucositis, diarrhea, nausea and emesis. There were no grade 3/4 events. Conclusions: Our data indicate that neoadjuvant X-RT is feasible, well tolerated and appears more effective than RT alone in pts with LABC refractory to FAC, rendering a high proportion (82%) of pts eligible for surgery.

No significant financial relationships to disclose.

Metagenomic analysis of mesopelagic Antarctic plankton reveals a novel deltaproteobacterial group

Phylogenetic screening of 3200 clones from a metagenomic library of Antarctic mesopelagic picoplankton allowed the identification of two bacterial 16S-rDNA-containing clones belonging to the Deltaproteobacteria, DeepAnt-1F12 and DeepAnt-32C6. These clones were very divergent, forming a monophyletic cluster with the environmental sequence GR-WP33-58 that branched at the base of the myxobacteria. Except for the possession of complete rrn operons without associated tRNA genes, DeepAnt-1F12 and DeepAnt-32C6 were very different in gene content and organization. Gene density was much higher in DeepAnt-32C6, whereas nearly one-third of DeepAnt-1F12 corresponded to intergenic regions. Many of the predicted genes encoded by these metagenomic clones were informational (i.e. involved in replication, transcription, translation and related processes). Despite this, a few putative cases of horizontal gene transfer were detected, including a transposase. DeepAnt-1F12 contained one putative gene encoding a long cysteine-rich protein, probably membrane-bound and Ca2+-binding, with only eukaryotic homologues. DeepAnt-32C6 carried some predicted genes involved in metabolic pathways that suggested this organism may be anaerobic and able to ferment and to degrade complex compounds extracellularly.

Thermophilic lifestyle for an uncultured archaeon from hydrothermal vents: evidence from environmental genomics

We present a comparative analysis of two genome fragments isolated from a diverse and widely distributed group of uncultured euryarchaea from deep-sea hydrothermal vents. The optimal activity and thermostability of a DNA polymerase predicted in one fragment were close to that of the thermophilic archaeon Thermoplasma acidophilum, providing evidence for a thermophilic way of life of this group of uncultured archaea.

The extent of protist diversity: insights from molecular ecology of freshwater eukaryotes

Classical studies on protist diversity of freshwater environments worldwide have led to the idea that most species of microbial eukaryotes are known. One exemplary case would be constituted by the ciliates, which have been claimed to encompass a few thousands of ubiquitous species, most of them already described. Recently, molecular methods have revealed an unsuspected protist diversity, especially in oceanic as well as some extreme environments, suggesting the occurrence of a hidden diversity of eukaryotic lineages. In order to test if this holds also for freshwater environments, we have carried out a molecular survey of small subunit ribosomal RNA genes in water and sediment samples of two ponds, one oxic and another suboxic, from the same geographic area. Our results show that protist diversity is very high. The majority of phylotypes affiliated within a few well established eukaryotic kingdoms or phyla, including alveolates, cryptophytes, heterokonts, Cercozoa, Centroheliozoa and haptophytes, although a few sequences did not display a clear taxonomic affiliation. The diversity of sequences within groups was very large, particularly that of ciliates, and a number of them were very divergent from known species, which could define new intra-phylum groups. This suggests that, contrary to current ideas, the diversity of freshwater protists is far from being completely described.

Selective forces for the origin of the eukaryotic nucleus

The origin of the eukaryotic cell nucleus and the selective forces that drove its evolution remain unknown and are a matter of controversy. Autogenous models state that both the nucleus and endoplasmic reticulum (ER) derived from the invagination of the plasma membrane, but most of them do not advance clear selective forces for this process. Alternative models proposing an endosymbiotic origin of the nucleus fail to provide a pathway fully compatible with our knowledge of cell biology. We propose here an evolutionary scenario that reconciles both an ancestral endosymbiotic origin of the eukaryotic nucleus (endosymbiosis of a methanogenic archaeon within a fermentative myxobacterium) with an autogenous generation of the contemporary nuclear membrane and ER from the bacterial membrane. We specifically state two selective forces that operated sequentially during its evolution: (1) metabolic compartmentation to avoid deleterious co-existence of anabolic (autotrophic synthesis by the methanogen) and catabolic (fermentation by the myxobacterium) pathways in the cell, and (2) avoidance of aberrant protein synthesis due to intron spreading in the ancient archaeal genome following mitochondrial acquisition and loss of methanogenesis.

Polyubiquitin insertions and the phylogeny of Cercozoa and Rhizaria

A single or double amino acid insertion at the monomer-monomer junction of the universal eukaryotic protein polyubiquitin is unique to Cercozoa and Foraminifera, closely related 'core' phyla in the protozoan infrakingdom Rhizaria. We screened 11 other candidate rhizarians for this insertion: Radiozoa (polycystine and acantharean radiolaria), a 'microheliozoan', and Apusozoa; all lack it, supporting suggestions that Foraminifera are more closely related to Cercozoa than either is to other eukaryotes. The insertion's size was ascertained for 12 additional Cercozoa to help resolve their basal branching order. The earliest branching Cercozoa generally have a single amino acid insertion, like all Foraminifera, but a large derived clade consisting of all Monadofilosa except Metopion, Helk-esimastix, and Cercobodo agilis has two amino acids, suggesting one doubling event and no reversions to a single amino acid. Metromonas and Sainouron, cercozoans of uncertain position, have a double insertion, suggesting that they belong in Monadofilosa. An alternative interpretation, suggested by the higher positions for Metopion and Cercobodo on Bayesian trees compared with most distance trees, cannot be ruled out, i.e. that the second insertion took place earlier, in the ancestral filosan, and was followed by three independent reversions to a single amino acid in Chlorarachnea, Metopion and Cercobodo.

Aurigamonas solis n. gen., n. sp., a soil-dwelling predator with unusual helioflagellate organisation and belonging to a novel clade within the Cercozoa

A flagellate predator, Aurigamonas solis n. gen., n. sp., with numerous radiating axopodia-like appendages, has been isolated in culture from soils. Despite its heliozoan-like appearance, Aurigamonas is not a sit-and-wait predator but a mobile hunter and its stiff appendages are not microtubule-supported axopodia but elongate haptopodia, each supported by a cylindrical core of microfilaments and bearing at its capitate tip a single extrusome-like body (haptosome). Prey flagellates are trapped on the sticky tips of the haptopodia and a large funnel-shaped pseudopodium then emerges to engulf the prey or suck out part of it for internal digestion. Pseudopodial contact is accompanied by killing, possibly as a result of the injection of spicules by the predator. Cytoplasmic haptosomes appear to induce formation of a haptopodium on making contact with the plasma membrane. Propulsion of the organism along the substratum is effected by beating of a long trailing flagellum, the short and inconspicuous second flagellum lacks motility. Small subunit rDNA sequencing shows that Aurigamonas arose within the Cercozoa. Its closest relatives are Cercobodo agilis and several flagellates currently known only as environmental sequences. This conclusion is supported further by the presence of only a single amino acid insertion in the polyubiquitin sequence of Aurigamonas solis.

Global dispersal and ancient cryptic species in the smallest marine eukaryotes

Small eukaryotic species (<1 mm) are thought to behave as prokaryotes in that, lacking geographical barriers to their dispersal due to their tiny size, they are ubiquitous. Accordingly, the absence of geographical insulation would imply the existence of a relatively small number of microeukaryotic species. To test these ideas, we sequenced and compared several nuclear, mitochondrial, and chloroplast genes from the isolates of a marine picoeukaryotic alga (approximately 2 microm), Micromonas pusilla, collected worldwide. Independent and combined phylogenetic analyses demonstrate that this traditional single morphospecies actually comprises several independent lineages, some of which are shown to be ubiquitous in oceans. However, while some lineages group closely related strains, others form distant clusters, revealing the existence of cryptic species. Moreover, molecular dating using a relaxed clock suggests that their first diversification may have started as early as during the Late Cretaceous (approximately 65 MYA), implying that "M. pusilla" is the oldest group of cryptic species known to date. Our results illustrate that global dispersal of a picoeukaryote is possible in oceans, but this does not imply a reduced species number. On the contrary, we show that the morphospecies concept is untenable because it overlooks a large genetic and species diversity and may lead to incorrect biological assumptions.

Phylogenetic Analysis of Eukaryotic Thiolases Suggests Multiple Proteobacterial Origins

Eukaryotic thiolases are essential enzymes located in three different compartments (peroxisome, mitochondrion, and cytosol) that can display catabolic or anabolic functions. They are responsible for the thiolytic cleavage of oxidized acyl-CoA (thiolase I; EC 2.3.1.16) and the synthesis or degradation of acetoacetyl-CoA (thiolase II; EC 2.3.1.9). Phylogenetic analysis of eukaryotic thiolase sequences showed that they form six distinct clusters, one of them highly divergent, which are in good correlation with their class and subcellular location. When analyzed together with a representative sample of prokaryotic thiolases, all eukaryotic thiolase groups emerged close to proteobacterial sequences. Metazoan cytosolic thiolase II was related to alpha-proteobacterial sequences, suggesting a mitochondrial origin. Unexpectedly, cytosolic thiolases from green plants and fungi as well as at least one member of all eukaryotic peroxisomal and mitochondrial thiolases had delta-proteobacteria as closest relatives. Our analysis suggests that these eukaryotic peroxisomal and mitochondrial thiolases may have been acquired from delta-proteobacteria prior to the ancestor of all known eukaryotes.

Bacterial diversity and carbonate precipitation in the giant microbialites from the highly alkaline Lake Van, Turkey

Lake Van harbors the largest known microbialites on Earth. The surface of these huge carbonate pinnacles is covered by coccoid cyanobacteria whereas their central axis is occupied by a channel through which neutral, relatively Ca-enriched, groundwater flows into highly alkaline (pH approximately 9.7) Ca-poor lake water. Previous microscopy observations showed the presence of aragonite globules composed by rounded nanostructures of uncertain origin that resemble similar bodies found in some meteorites. Here, we have carried out fine-scale mineralogical and microbial diversity analyses from surface and internal microbialite samples. Electron transmission microscopy revealed that the nanostructures correspond to rounded aragonite nanoprecipitates. A progressive mineralization of cells by the deposition of nanoprecipitates on their surface was observed from external towards internal microbialite areas. Molecular diversity studies based on 16S rDNA amplification revealed the presence of bacterial lineages affiliated to the Alpha-, Beta- and Gammaproteobacteria, the Cyanobacteria, the Cytophaga-Flexibacter-Bacteroides (CFB) group, the Actinobacteria and the Firmicutes. Cyanobacteria and CFB members were only detected in surface layers. The most abundant and diverse lineages were the Firmicutes (low GC Gram positives). To the exclusion of cyanobacteria, the closest cultivated members to the Lake Van phylotypes were most frequently alkaliphilic and/or heterotrophic bacteria able to degrade complex organics. These heterotrophic bacteria may play a crucial role in the formation of Lake Van microbialites by locally promoting carbonate precipitation.

An updated view of kinetoplastid phylogeny using environmental sequences and a closer outgroup: proposal for a new classification of the class Kinetoplastea

Given their ecological and medical importance, the classification of the kinetoplastid protists (class Kinetoplastea) has attracted much scientific attention for a long time. Morphology-based taxonomic schemes distinguished two major kinetoplastid groups: the strictly parasitic, uniflagellate trypanosomatids and the biflagellate bodonids. Molecular phylogenetic analyses based on 18S rRNA sequence comparison suggested that the trypanosomatids emerged from within the bodonids. However, these analyses revealed a huge evolutionary distance between the kinetoplastids and their closest relatives (euglenids and diplonemids) that makes very difficult the correct inference of the phylogenetic relationships between the different kinetoplastid groups. Using direct PCR amplification of 18S rRNA genes from hydrothermal vent samples, several new kinetoplastid-like sequences have been reported recently. Three of them emerge robustly at the base of the kinetoplastids, breaking the long branch leading to the euglenids and diplonemids. One of these sequences belongs to a close relative of Ichthyobodo necator (a fish parasite) and of the 'Perkinsiella amoebae'-like endosymbiont of Neoparamoeba spp. amoebae. The authors have studied the reliability of their basal position and used all these slow-evolving basal-emerging sequences as a close outgroup to analyse the phylogeny of the apical kinetoplastids. They thus find a much more stable and resolved kinetoplastid phylogeny, which supports the monophyly of groups that very often emerged as polyphyletic in the trees rooted using the traditional, distant outgroup sequences. A new classification of the class Kinetoplastea is proposed based on the results of the phylogenetic analysis presented. This class is now subdivided into two new subclasses, Prokinetoplastina (accommodating the basal species I. necator and 'Perkinsiella amoebae') and Metakinetoplastina (containing the Trypanosomatida together with three additional new orders: Eubodonida, Parabodonida and Neobodonida). The classification of the species formerly included in the genus Bodo is also revised, with the amendment of this genus and the genus Parabodo and the creation of a new genus, Neobodo.

Diversity of functional genes of methanogens, methanotrophs and sulfate reducers in deep-sea hydrothermal environments

To contribute to the identification of methanogens, methanotrophs and sulfate-reducing bacteria (SRB) in microbial communities from the 13 degrees N (East Pacific Rise) and Rainbow (Mid-Atlantic Ridge) hydrothermal vent fields, we investigated the diversity of mcrA, pmoA and dsrAB genes sequences. Clone libraries were obtained using DNA isolated from fragments of diffuse vents, sediment and in situ samplers. The clones were categorized by restriction fragment length polymorphism, and representatives of each group were sequenced. Sequences were related to that of hyperthermophilic (order Methanopyrales and family Methanocaldococcaceae), thermophilic and mesophilic (family Methanococcaceae) methanogens, thermophilic (proposed genus 'Methylothermus') and mesophilic type I methanotrophs, and hyperthermophilic (order Archaeoglobales), thermophilic (order Thermodesulfobacteriales) and mesophilic (family Desulfobulbaceae) SRB. Several of the obtained sequences were distantly related to the genes of cultivated organisms, providing evidence of the existence of novel lineages in the three functional groups. This study provides for the first time an insight into the diversity of several functional genes of deep-sea hydrothermal system microorganisms.

Evolutionary relationships of Fusobacterium nucleatum based on phylogenetic analysis and comparative genomics

Background

The phylogenetic position and evolutionary relationships of Fusobacteria remain uncertain. Especially intriguing is their relatedness to low G+C Gram positive bacteria (Firmicutes) by ribosomal molecular phylogenies, but their possession of a typical gram negative outer membrane. Taking advantage of the recent completion of the Fusobacterium nucleatum genome sequence we have examined the evolutionary relationships of Fusobacterium genes by phylogenetic analysis and comparative genomics tools.

Results

The data indicate that Fusobacterium has a core genome of a very different nature to other bacterial lineages, and branches out at the base of Firmicutes. However, depending on the method used, 35–56% of Fusobacterium genes appear to have a xenologous origin from bacteroidetes, proteobacteria, spirochaetes and the Firmicutes themselves. A high number of hypothetical ORFs with unusual codon usage and short lengths were found and hypothesized to be remnants of transferred genes that were discarded. Some proteins and operons are also hypothesized to be of mixed ancestry. A large portion of the Gram-negative cell wall-related genes seems to have been transferred from proteobacteria.

Conclusions

Many instances of similarity to other inhabitants of the dental plaque that have been sequenced were found. This suggests that the close physical contact found in this environment might facilitate horizontal gene transfer, supporting the idea of niche-specific gene pools. We hypothesize that at a point in time, probably associated to the rise of mammals, a strong selective pressure might have existed for a cell with a Clostridia-like metabolic apparatus but with the adhesive and immune camouflage features of Proteobacteria.

Analysis of a genome fragment of a deep-sea uncultivated Group II euryarchaeote containing 16S rDNA, a spectinomycin-like operon and several energy metabolism genes

We have sequenced and analysed a 39.5 kbp genome fragment of a marine Group II euryarchaeote identified in a metagenomic library of 500 m deep plankton at the Antarctic Polar Front. The clone contains a 16S rRNA gene that is separated from the 23S rRNA gene in the genome. This appears to be a trait shared by Thermoplasmatales and Group II euryarchaeota. This genome fragment exhibits a compact organization, including a few overlapping genes in the canonical spectinomycin-like (spc) operon for ribosomal proteins that is immediately upstream the 16S rDNA. Most open reading frames (ORFs) encoded proteins involved in housekeeping processes and, as expected, exhibited a phylogenetic distribution congruent with that of the 16S rRNA. A considerable number of proteins with predicted transmembrane helices was identified. Among those, two proteins encoded by genes likely forming an operon appear to be part of a membrane terminal electron transport chain. One of these proteins has an unusual domain arrangement including ferredoxin, flavodoxin and one succinate dehydrogenase/fumarate reductase subunit. These proteins probably constitute a new succinate dehydrogenase-like oxidoreductase involved in what could be a novel pathway for energy metabolism in Group II euryarchaeota.

Macrofilamentous microbial communities in the metal-rich and acidic River Tinto, Spain

A novel type of macroscopic microbial community consisting of large dendritic filaments (up to 1.5 m) in a pH 2.0 dam of the River Tinto (South-western Spain) is described. The combined use of 16S rRNA-gene surveys and fluorescent in situ hybridisation (FISH) suggested that gamma-proteobacteria and a relative large diversity of alpha-proteobacteria dominated these structures. beta-Proteobacteria, Actinobacteria and Firmicutes were also detected. Whereas acidophilic bacteria of the genera Acidithiobacillus, Leptospirillum and Acidiphilium, and archaea belonging to the Thermoplasmatales dominate mine acid drainage waters and streamers (riverbed filamentous biofilms), none of the lineages identified in this study affiliate to typical acid mine drainage acidophilic bacteria. Bacteria of the Tinto macrofilaments might be heterotrophic, and could be feeding on the organic matter entrapped in the filamentous structure.

Horizontal gene transfer and archaeal origin of deoxyhypusine synthase homologous genes in bacteria

The initiation factor 5A (IF-5A) of archaea and eukaryotes undergoes an unusual post-translational modification consisting of the transformation of a specific conserved lysine residue into the amino acid hypusine. This occurs in a two-step reaction catalysed by the enzymes deoxyhypusine synthase (DHS) and deoxyhypusine hydroxylase. Bacteria do not have IF-5A but only a very distant homologue, the elongation factor P (EF-P). Consequently, all bacteria appeared to also lack genes with significant homology to DHS genes. However, we have carried out BLAST searches and found DHS-like genes in a number of bacterial species. The phylogenetic analysis of these sequences strongly suggests that they have been acquired from archaea by horizontal gene transfer (HGT). Our analysis also suggests, although with weaker support, that a single HGT event from archaea, followed by several HGT between bacterial species, accounts for the patchy distribution of DHS-like genes in bacteria. The activity of these genes in bacteria is enigmatic, since we have not found any evidence of interaction between this protein and the bacterial EF-P. Nevertheless, we cannot discard that it exists, since it appears that the interaction between the DHS and its natural substrate, the IF-5A, is rather weak. This is exemplified by the fact that, in archaea, the complex evolutionary history of the DHS is not paralleled by that of the IF-5A, indicating that these proteins do not follow a perfect co-evolution.

Bacterial diversity in hydrothermal sediment and epsilonproteobacterial dominance in experimental microcolonizers at the Mid-Atlantic Ridge

We report here a molecular survey based on 16S rRNA genes of the bacterial diversity found in two deep-sea vent niches at the Mid-Atlantic Ridge: hydrothermal sediment (Rainbow site), and microcolonizers made of three different substrates (organic-rich, iron-rich and pumice) that were exposed for 15 days to a vent emission. Bacterial diversity in sediment samples was scattered through many bacterial divisions. The most abundant and diverse environmental sequences (phylotypes) in our libraries corresponded to the Gammaproteobacteria, followed by the Acidobacteria. We detected members of all the subdivisions within the Proteobacteria. Myxobacterial lineages were the most represented within the delta subdivision. Phylotypes ascribing to the Cytophaga-Flavobacterium-Bacteroides, Planctomycetales, high and low G + C Gram-positives, Nitrospirae, and the candidate division TM7 were also identified. Compared to this broad taxonomic coverage, microcolonizers were almost exclusively colonized by epsilonproteobacteria, although these exhibited considerable morphological and phylogenetic in-group diversity. No specificity for any of the substrates tested was seen. This observation further supports the idea of the ecological dominance of epsilonproteobacteria in the fluid-seawater interface environment. Because oxidation of reduced S species and/or sulphur-reduction is thought to be essential for their energetic metabolism in these areas, we mapped different oxidation states of S in individual bacterial filaments from the iron-rich microcolonizer. For this, we used high-resolution, non-destructive synchrotron micro-X-ray Absorption Near-Edge Spectroscopy (micro-XANES), which revealed the co-existence of different S oxidation states, from sulphide to sulphate, at the level of individual cells. This suggests that these cells were metabolizing sulphur in situ.

Rampant horizontal gene transfer and phospho-donor change in the evolution of the phosphofructokinase

Previous work on the evolution of the phosphofructokinase (PFK) has shown that this key regulatory enzyme of glycolysis has undergone an intricate evolutionary history. Here, we have used a comprehensive data set to address the taxonomic distribution of the different types of PFK (ATP-dependent and PPi-dependent ones) and to estimate the frequency of horizontal gene transfer (HGT) events. Numerous HGT events appear to have occurred. In addition, we focused on the analysis of sites 104 and 124 (usually Gly(104)+Gly(124) or Asp(104)+Lys(124)), known to be involved in catalysis (J. Biol. Chem. 275 (2000) 35677). It revealed the existence of numerous sequences from distantly related species carrying atypical combinations of amino acids. Several adaptive changes of phospho-donors, probably requiring a single mutation at position 104, have likely occurred independently in many lineages. The analysis of this gene suggests the existence of a high rate of both HGT and substitution in its active sites. These rampant HGT events and flexibility in phospho-donor use illustrate the importance of tinkering in molecular evolution.

Phytoplankton diversity and cyanobacterial dominance in a hypereutrophic shallow lake with biologically produced alkaline pH

In this work, we have characterized the diversity of phytoplanktonic species in a highly alkaline and hypereutrophic shallow lake, Santa Olalla (southwestern Spain), the evolution of their relative abundances, and that of several physicochemical parameters over 2 years. In the absence of an external input of alkaline water, Santa Olalla's stable high pH (average pH 9.52, with several maxima >10.5) is explained by an extremely high photosynthetic primary productivity. A variety of phytoplankton species was observed even during pH maxima. These included several species of green algae, diatoms, and euglenoids and several cyanobacteria from the orders Nostocales and Chroococcales. Quantitatively, cyanobacteria dominated. A blooming event due to Aphanothece clathrata was observed at one pH maximum, during which the diversity as measured by the Shannon-Weaver index was extremely low. Santa Olalla's cyanobacteria are alkaliphilic and/or extremely alkalitolerant and appear to be responsible for the generation and maintenance of stable high-pH conditions in their environment.

Comparative analysis of a genome fragment of an uncultivated mesopelagic crenarchaeote reveals multiple horizontal gene transfers

Marine planktonic crenarchaeota have escaped all cultivation attempts to date, all crenarchaeota growing in pure culture so far being hyperthermophiles. Here, we present a comparative genomic analysis of a 16S- plus 23S-rDNA-containing fragment of a crenarchaeote retrieved from an environmental genomic library constructed from picoplankton collected at 500 m depth in the Antarctic Polar Front. The clone DeepAnt-EC39 contained an insert of 33.3 kbp, which was completely sequenced. DeepAnt-EC39 appears to represent a lineage specific to deep-sea waters but widespread geographically, as revealed by the analysis of the 16S-23S-rDNA intergenic spacer region. A comparison with previously sequenced marine crenarchaeotal genomic clones also containing an rrn operon (74A4, 4B7 and Cenarchaeum symbiosum strains A and B) revealed a highly variable structure involving gene rearrangements and insertions/deletions. The surroundings of the rrn operon and the contiguous glutamate-1-semialdehyde aminotransferase gene appear hot spots for recombination. Phylogenetic analyses of all individual predicted proteins revealed the existence of several likely cases of horizontal gene transfer both, between the two archaeal kingdoms and between the two prokaryotic domains. The most frequent horizontal transfers appear to involve genes from mesophilic methanogenic euryarchaeota related to Methanosarcinales. We hypothesise that the acquisition of genes from mesophilic bacteria and euryarchaeota has played a major role in the adaptation of Group I crenarchaeota to life at lower temperatures.

Autochthonous eukaryotic diversity in hydrothermal sediment and experimental microcolonizers at the Mid-Atlantic Ridge

The diversity and mode of life of microbial eukaryotes in hydrothermal systems is very poorly known. We carried out a molecular survey based on 18S ribosomal RNA genes of eukaryotes present in different hydrothermal niches at the Mid-Atlantic Ridge. These included metal-rich and rare-earth-element-rich hydrothermal sediments of the Rainbow site, fluid-seawater mixing regions, and colonization devices (microcolonizers) containing organic, iron-rich, and porous mineral substrates that were exposed for 15 days to a fluid source. We identified considerable phylogenetic diversity, both at kingdom level and within kinetoplastids and alveolates. None of our sequences affiliates to photosynthesizing lineages, suggesting that we are targeting only autochthonous deep-sea communities. Although sediment harbored most phylogenetic diversity, microcolonizers predominantly contained bodonids and ciliates, indicating that these protists pioneer the colonization process. Given the large variety of divergent lineages detected within the alveolates in deep-sea plankton, hydrothermal sediments, and vents, alveolates seem to dominate the deep ocean in terms of diversity. Compared with data from the Pacific Guaymas basin, some protist lineages seem ubiquitous in hydrothermal areas, whereas others, notably kinetoplastid lineages, very abundant and diverse in our samples, so far have been detected only in Atlantic systems. Unexpectedly, although alvinellid polychaetes are considered endemic of Pacific vents, we detected alvinellid-related sequences at the fluid-seawater interface and in microcolonizers. This finding can boost further studies on deep-sea vent animal biology and biogeography.

Wide bacterial diversity associated with tubes of the vent worm Riftia pachyptila

We carried out a 16S rDNA-based molecular survey of the prokaryotic diversity associated with the chitin tubes of the giant vent tubeworm Riftia pachyptila (collected at the East Pacific Rise, 9 degrees N and 13 degrees N). Scanning electron microscopy showed dense microbial populations, particularly on the external surface of the middle and upper tube regions, which included very diverse prokaryotic morphotypes. We used archaeal- and bacterial-specific primers for polymerase chain reaction (PCR) amplification, but only bacterial amplicons were obtained. We analysed a total of 87 clones. Most belonged to the epsilon-Proteobacteria, but also to the delta-, alpha- and gamma-Proteobacteria. A broad diversity of phylotypes belonging to other bacterial divisions was detected, including Verrucomicrobia, the Cytophaga-Flavobacterium-Bacteroides group and the candidate division OP8. We also retrieved a sequence, R76-B150, of uncertain phylogenetic affiliation, which could represent a novel candidate division. The sequence of the R. pachyptilagamma-proteobacterial endosymbiont was not detected. The bacterial diversity found suggests that complex metabolic interactions, particularly based on sulphur chemistry, may be occurring in different microniches of the R. pachyptila tubes.

Evolution of Eukaryotic Translation Elongation and Termination Factors: Variations of Evolutionary Rate and Genetic Code Deviations

Translation is carried out by the ribosome and several associated protein factors through three consecutive steps: initiation, elongation, and termination. Termination remains the least understood of them, partly because of the nonuniversality of the factors involved. To get some insights on the evolution of eukaryotic translation termination, we have compared the phylogeny of the release factors eRF1 and eRF3 to that of the elongation factors EF-1alpha and EF-2, with special focus on ciliates. Our results show that these four translation proteins have experienced different modes of evolution. This is especially evident for the EF-1alpha, EF-2, and eRF1 ciliate sequences. Ciliates appear as monophyletic in the EF-2 phylogenetic tree but not in the EF-1alpha and eRF1 phylogenetic trees. This seems to be mainly because of phylogeny reconstruction artifacts (the long-branch attraction) produced by the acceleration of evolutionary rate of ciliate EF-1alpha and eRF1 sequences. Interaction with the highly divergent actin found in ciliates, or on the contrary, loss of interaction, could explain the acceleration of the evolutionary rate of the EF-1alpha sequences. In the case of ciliate eRF1 sequences, their unusually high evolutionary rate may be related to the deviations in the genetic code usage found in diverse ciliates. These deviations involve a relaxation (or even abolition) of the recognition of one or two stop codons by eRF1. To achieve this, structural changes in eRF1 are needed, and this may affect its evolutionary rate. Eukaryotic translation seems to have followed a mosaic evolution, with its different elements governed by different selective pressures. However, a correlation analysis shows that, beneath the disagreement shown by the different translation proteins, their concerted evolution can still be made apparent when they are compared with other proteins that are not involved in translation.

Eubacterial phylogeny based on translational apparatus proteins

Lateral gene transfers are frequent among prokaryotes, although their detection remains difficult. If all genes are equally affected, this questions the very existence of an organismal phylogeny. The complexity hypothesis postulates the existence of a core of genes (those involved in numerous interactions) that are unaffected by transfers. To test the hypothesis, we studied all the proteins involved in translation from 45 eubacterial taxa, and developed a new phylogenetic method to detect transfers. Few of the genes studied show evidence for transfer. The phylogeny based on the genes devoid of transfer is very consistent with the ribosomal RNA tree, suggesting that an eubacterial phylogeny does exist.

The molecular ecology of microbial eukaryotes unveils a hidden world

In spite of the great success of small-subunit ribosomal RNA (SSU rRNA)-based studies for the analysis of environmental prokaryotic diversity, this molecular approach has seldom been applied to microbial eukaryotes. Recent molecular surveys of the smallest eukaryotic planktonic fractions at different oceanic surface regions and in deep-sea Antarctic samples revealed an astonishing protist diversity. Many of the phylotypes found in the photic region affiliate with photosynthetic groups that are known to contain picoeukaryotic representatives in the range 1-2 microm. Surprisingly, a vast diversity of presumably heterotrophic or mixotrophic lineages is also found. Among these, several novel lineages of heterokonts, and a large diversity of alveolates clustering in two major groups (Groups I and II), are present at all depths in the water column. Many of these new phylotypes appear biogeographically ubiquitous. These initial studies suggest that a wide diversity of small eukaryotes remains to be discovered not only in the ocean but also in other environments. For both ecology and evolutionary studies, it is predicted that environmental molecular identification of eukaryotes will have a profound impact in the immediate future.

New insights into the phylogenetic position of diplonemids: G+C content bias, differences of evolutionary rate and a new environmental sequence

The phylum Euglenozoa consists of three distinct groups: the euglenoids, diplonemids and kinetoplastids. The phylogenetic position of the diplonemids within this phylum remains unsettled, since both morphological and molecular data produce weak and contradictory results. It is shown here that taxonomic sampling, G+C content bias, mutational saturation and differences of evolutionary rate among lineages are major factors affecting the topology of the small-subunit rRNA euglenozoan tree. When these problems are minimized by using a larger diplonemid sampling (including a sequence of environmental origin) and correcting for G+C bias (by using both paralinear distances or an unbiased dataset), a diplonemids+euglenoids sisterhood is retrieved. Bootstrap support for this relationship is still moderate, but it is retrieved by all analysis methods, overcoming previously reported disagreements. In addition, the inclusion of a large number of euglenoid sequences in the analysis improves some phylogenetic relationships within this group. Some problematic taxa, such as the species Khawkinea quartana, are now placed with high bootstrap support and monophyly is found for two interesting groups (the photosynthetic genera Eutreptia+Eutreptiella and the loricate genera Strombomonas+Trachelomonas), although with weak statistical support.

Sure facts and open questions about the origin and evolution of photosynthetic plastids

Some eukaryotic groups carry out photosynthesis thanks to plastids, which are endosymbiotic organelles derived from cyanobacteria. Increasing evidence suggests that the plastids from green plants, red algae, and glaucophytes arose directly from a single common primary symbiotic event between a cyanobacterium and a phagotrophic eukaryotic host. They are therefore known as primary plastids. All other lineages of photosynthetic eukaryotes seem to have acquired their plastids by secondary or tertiary endosymbioses, which are established between eukaryotic algae, already containing plastids, and other eukaryotic hosts. Both primary and secondary symbioses have been followed by extensive plastid genome reduction through gene loss and gene transfer to the host nucleus. All this makes the reconstruction of the evolutionary history of plastids a very complex task, indissoluble from the resolution of the general phylogeny of eukaryotes.

Candida spp. biotypes in the oral cavity of school children from different socioeconomic categories in Piracicaba-SP, Brazil

Two hundred and thirty-nine (239) Brazilian children, distributed into five distinct socioeconomic categories (A to E) were studied. Saliva samples were analyzed as to flow rate, pH, buffer capacity and microbial parameters. The results revealed the presence of Candida spp. in 47.3% of the samples. The most commonly isolated species was C. albicans, in all socioeconomic categories, followed by C. tropicalis, C. krusei and C. parapsilosis. There was no statistical correlation between secretion rate, buffer capacity and Candida spp. CFU/ml. The prevalence of Candida spp. did not differ substantially among the groups; however the microorganisms were more detected in categories B and C. Among all species, C. albicans was the most prevalent. Only 5% of the sample presented more than one species--C. albicans associated with C. tropicalis, C. parapsilosis or C. krusei. It was possible to detect a significant correlation between caries indices and the socioeconomic categories. All categories presented increased caries indices; however the studied population was considered of low caries risk. There was no positive correlation between the presence of Candida and caries risk in the analyzed population.

Diversity of free-living prokaryotes from a deep-sea site at the Antarctic Polar Front

To contribute to the understanding of deep-sea planktonic communities, we explored the prokaryotic diversity of a 3000 m deep site at the Antarctic Polar Front using molecular methods. Bacterial 16S rDNA-amplified sequences corresponded to the as yet uncultivated groups SAR11, within the alpha-Proteobacteria, and SAR324, within the delta-Proteobacteria, as well as to the gamma-Proteobacteria, Cytophagales, Planctomyces, Gram-positives, and the group of environmental sequences SAR406. Among them, gamma-proteobacterial sequences were the most abundant and diverse. Within Archaea, and using six different primer sets for 16S rDNA amplification, only euryarchaeotal sequences were retrieved. Most of them clustered with the Thermoplasma-related marine groups II and III, but some corresponded to a recently described group of marine sequences emerging at the base of haloarchaea. Our data suggest that gamma-Proteobacteria and Euryarchaeota may be dominant elements in terms of genetic diversity of the two prokaryotic domains in this deep-sea pelagic area.

Unexpected diversity of small eukaryotes in deep-sea Antarctic plankton

Phylogenetic information from ribosomal RNA genes directly amplified from the environment changed our view of the biosphere, revealing an extraordinary diversity of previously undetected prokaryotic lineages. Using ribosomal RNA genes from marine picoplankton, several new groups of bacteria and archaea have been identified, some of which are abundant. Little is known, however, about the diversity of the smallest planktonic eukaryotes, and available information in general concerns the phytoplankton of the euphotic region. Here we recover eukaryotes in the size fraction 0.2-5 microm from the aphotic zone (250-3,000 m deep) in the Antarctic polar front. The most diverse and relatively abundant were two new groups of alveolate sequences, related to dinoflagellates that are found at all studied depths. These may be important components of the microbial community in the deep ocean. Their phylogenetic position suggests a radiation early in the evolution of alveolates.

A novel haloarchaeal-related lineage is widely distributed in deep oceanic regions

During our study of the 16S rRNA gene sequence-based archaeal diversity of a deep-sea site located at a 3,000 m depth at the Antarctic Polar Front, we detected several phylotypes ascribed to already known Group II and III Euryarchaeota, and a cluster of distinct sequences that branched off at the base of haloarchaea. The position of this lineage (marine Group IV) was very robust using distance (neighbour-joining) and maximum-likelihood methods. Subsequently, we designed specific primers for the detection of this archaeal group in other marine environments using polymerase chain reaction amplification and sequence comparison. Group IV archaea were found in the Antarctic area (across a gradient from the Southern ocean to the South Atlantic), and also in North Atlantic and Mediterranean waters. In all oceanic locations, Group IV archaea were never detected in surface waters, but were vertically distributed in the deepest part of the water column.