Phylogenomics reshuffles the eukaryotic supergroups

Background

Resolving the phylogenetic relationships between eukaryotes is an ongoing challenge of evolutionary biology. In recent years, the accumulation of molecular data led to a new evolutionary understanding, in which all eukaryotic diversity has been classified into five or six supergroups. Yet, the composition of these large assemblages and their relationships remain controversial.

Methodology/Principle Findings

Here, we report the sequencing of expressed sequence tags (ESTs) for two species belonging to the supergroup Rhizaria and present the analysis of a unique dataset combining 29908 amino acid positions and an extensive taxa sampling made of 49 mainly unicellular species representative of all supergroups. Our results show a very robust relationship between Rhizaria and two main clades of the supergroup chromalveolates: stramenopiles and alveolates. We confirm the existence of consistent affinities between assemblages that were thought to belong to different supergroups of eukaryotes, thus not sharing a close evolutionary history.

Conclusions

This well supported phylogeny has important consequences for our understanding of the evolutionary history of eukaryotes. In particular, it questions a single red algal origin of the chlorophyll-c containing plastids among the chromalveolates. We propose the abbreviated name ‘SAR’ (Stramenopiles+Alveolates+Rhizaria) to accommodate this new super assemblage of eukaryotes, which comprises the largest diversity of unicellular eukaryotes.

Bipolar gene flow in deep-sea benthic foraminifera

Despite its often featureless appearance, the deep-ocean floor includes some of the most diverse habitats on Earth. However, the accurate assessment of global deep-sea diversity is impeded by a paucity of data on the geographical ranges of bottom-dwelling species, particularly at the genetic level. Here, we present molecular evidence for exceptionally wide distribution of benthic foraminifera, which constitute the major part of deep-sea meiofauna. Our analyses of nuclear ribosomal RNA genes revealed high genetic similarity between Arctic and Antarctic populations of three common deep-sea foraminiferal species (Epistominella exigua, Cibicides wuellerstorfi and Oridorsalis umbonatus), separated by distances of up to 17, 000 km. Our results contrast with the substantial level of cryptic diversity usually revealed by molecular studies, of shallow-water benthic and planktonic marine organisms. The very broad ranges of the deep-sea foraminifera that we examined support the hypothesis of global distribution of small eukaryotes and suggest that deep-sea biodiversity may be more modest at global scales than present estimates suggest.

Higher-level phylogeny of Foraminifera inferred from the RNA polymerase II (RPB1) gene

Macroevolutionary relations among main lineages of Foraminifera have traditionally been inferred from the small subunit ribosomal genes (SSU rDNA). However, important discrepancies in the rates of SSU rDNA evolution between major lineages led to difficulties in accurate interpretation of SSU-based phylogenetic reconstructions. Recently, actin and beta-tubulin sequences have been used as alternative markers of foraminiferal phylogeny and their analyses globally confirm results obtained with SSU rDNA. In order to test new protein markers, we sequenced a fragment of the largest subunit of the RNA polymerase II (RPB1), a nuclear encoded single copy gene, for 8 foraminiferal species representing major orders of Foraminifera. Analyses of our data robustly confirm previous SSU rDNA and actin phylogenies and show (i) the paraphyly and ancestral position of monothalamid Foraminifera; (ii) the independent origin of miliolids; (iii) the monophyly of rotaliids, including buliminids and globigerinids; and (iv) the polyphyly of planktonic families Globigerinidae and Candeinidae. Additionally, the RPB1 phylogeny suggests Allogromiidae as the most ancestral foraminiferal lineage. In the light of our study, RPB1 appears as a valuable phylogenetic marker, particularly useful for groups of protists showing extreme variations of evolutionary rates in ribosomal genes.

First insights into the biodiversity and biogeography of the Southern Ocean deep sea

Shallow marine benthic communities around Antarctica show high levels of endemism, gigantism, slow growth, longevity and late maturity, as well as adaptive radiations that have generated considerable biodiversity in some taxa. The deeper parts of the Southern Ocean exhibit some unique environmental features, including a very deep continental shelf and a weakly stratified water column, and are the source for much of the deep water in the world ocean. These features suggest that deep-sea faunas around the Antarctic may be related both to adjacent shelf communities and to those in other oceans. Unlike shallow-water Antarctic benthic communities, however, little is known about life in this vast deep-sea region. Here, we report new data from recent sampling expeditions in the deep Weddell Sea and adjacent areas (748-6,348 m water depth) that reveal high levels of new biodiversity; for example, 674 isopods species, of which 585 were new to science. Bathymetric and biogeographic trends varied between taxa. In groups such as the isopods and polychaetes, slope assemblages included species that have invaded from the shelf. In other taxa, the shelf and slope assemblages were more distinct. Abyssal faunas tended to have stronger links to other oceans, particularly the Atlantic, but mainly in taxa with good dispersal capabilities, such as the Foraminifera. The isopods, ostracods and nematodes, which are poor dispersers, include many species currently known only from the Southern Ocean. Our findings challenge suggestions that deep-sea diversity is depressed in the Southern Ocean and provide a basis for exploring the evolutionary significance of the varied biogeographic patterns observed in this remote environment.

Mitochondrial Genome of Savalia savaglia (Cnidaria, Hexacorallia) and Early Metazoan Phylogeny

Mitochondrial genomes have recently become widely used in animal phylogeny, mainly to infer the relationships between vertebrates and other bilaterians. However, only 11 of 723 complete mitochondrial genomes available in the public databases are of early metazoans, including cnidarians (Anthozoa, mainly Scleractinia) and sponges. Although some cnidarians (Medusozoa) are known to possess atypical linear mitochondrial DNA, the anthozoan mitochondrial genome is circular and its organization is similar to that of other metazoans. Because the phylogenetic relationships among Anthozoa as well as their relation to other early metazoans still need to be clarified, we tested whether sequencing the complete mitochondrial genome of Savalia savaglia, an anthozoan belonging to the order Zoantharia (=Zoanthidea), could be useful to infer such relationships. Compared to other anthozoans, S. savaglia's genome is unusually long (20,766 bp) due to the presence of several noncoding intergenic regions (3691 bp). The genome contains all 13 protein coding genes commonly found in metazoans, but like other Anthozoa it lacks most of the tRNAs. Phylogenetic analyses of S. savaglia mitochondrial sequences show Zoantharia branching closely to other Hexacorallia, either as a sister group to Actiniaria or as a sister group to Actiniaria and Scleractinia. The close relationships suggested between Zoantharia and Actiniaria are reinforced by strong similarities in their gene order and the presence of similar introns in the COI and ND5 genes. Our study suggests that mitochondrial genomes can be a source of potentially valuable information on the phylogeny of Hexacorallia and may provide new insights into the evolution of early metazoans.

Psychological distress in Brazilian caregivers of relatives with dementia

The authors evaluated stress, anxiety, depression, and feelings of hopelessness in caregivers of relatives with dementia. One hundred and twenty-nine caregivers and 145 non-caregivers who lived in metropolitan Porto Alegre, Brazil completed Lipp's Inventory of Stress Symptoms for Adults, (ISSL), and Beck's Anxiety (BAI), Depression (BDI), and Hopelessness (BHS) scales. Caregivers showed higher levels of anxiety, depression, hopelessness, resistance/pre-exhaustion stress than controls. This study indicates that constant caregiving may significantly increase the risk of physical and mental health problems for caregivers in Brazil.

A molecular time-scale for eukaryote evolution recalibrated with the continuous microfossil record

Recent attempts to establish a molecular time-scale of eukaryote evolution failed to provide a congruent view on the timing of the origin and early diversification of eukaryotes. The major discrepancies in molecular time estimates are related to questions concerning the calibration of the tree. To limit these uncertainties, we used here as a source of calibration points the rich and continuous microfossil record of dinoflagellates, diatoms and coccolithophorids. We calibrated a small-subunit ribosomal RNA tree of eukaryotes with four maximum and 22 minimum time constraints. Using these multiple calibration points in a Bayesian relaxed molecular clock framework, we inferred that the early radiation of eukaryotes occurred near the Mesoproterozoic-Neoproterozoic boundary, about 1100 million years ago. Our results indicate that most Proterozoic fossils of possible eukaryotic origin cannot be confidently assigned to extant lineages and should therefore not be used as calibration points in molecular dating.

Phylogenetic position of Multicilia marina and the evolution of Amoebozoa

Recent molecular phylogenetic studies have led to the erection of the phylum Amoebozoa, uniting naked and testate lobose amoebae, the mycetozoan slime moulds and amitochondriate amoeboid protists (Archamoebae). Molecular data together with ultrastructural evidence have suggested a close relationship between Mycetozoa and Archamoebae, classified together in the Conosea, which was named after the cone of microtubules that, when present, is characteristic of their kinetids. However, the relationships of conoseans to other amoebozoans remain unclear. Here, we obtained the complete small-subunit (SSU) rRNA gene sequence (2746 bp) of the enigmatic, multiflagellated protist Multicilia marina, which has formerly been classified either in a distinct phylum, Multiflagellata, or among lobose amoebae. Our study clearly shows that Multicilia marina belongs to the Amoebozoa. Phylogenetic analyses including 60 amoebozoan SSU rRNA gene sequences revealed that Multicilia marina branches at the base of the Conosea, together with another flagellated amoebozoan, Phalansterium solitarium, as well as with Gephyramoeba sp., Filamoeba nolandi and two unidentified amoebae. This is the first report showing strong support for a clade containing all flagellated amoebozoans and we discuss the position of the root of the phylum Amoebozoa in the light of this result.

Analysis of expressed sequence tags from a naked foraminiferan Reticulomyxa filosa

Foraminifers are a major component of modern marine ecosystems and one of the most important oceanic producers of calcium carbonate. They are a key phylogenetic group among amoeboid protists, but our knowledge of their genome is still mostly limited to a few conserved genes. Here, we report the first study of expressed genes by means of expressed sequence tag (EST) from the freshwater naked foraminiferan Reticulomyxa filosa. Cluster analysis of 1630 valid ESTs enabled the identification of 178 groups of related sequences and 871 singlets. Approximately 50% of the putative unique 1059 ESTs could be annotated using Blast searches against the protein database SwissProt + TrEMBL. The EST database described here is the first step towards gene discovery in Foraminifera and should provide the basis for new insights into the genomic and transcriptomic characteristics of these interesting but poorly understood protists.Key words: Rhizaria, Foraminifera, cDNA library, annotation.

Monophyly of Rhizaria and multigene phylogeny of unicellular bikonts

Reconstructing a global phylogeny of eukaryotes is an ongoing challenge of molecular phylogenetics. The availability of genomic data from a broad range of eukaryotic phyla helped in resolving the eukaryotic tree into a topology with a rather small number of large assemblages, but the relationships between these "supergroups" are yet to be confirmed. Rhizaria is the most recently recognized "supergroup," but, in spite of this important position within the tree of life, their representatives are still missing in global phylogenies of eukaryotes. Here, we report the first large-scale analysis of eukaryote phylogeny including data for 2 rhizarian species, the foraminiferan Reticulomyxa filosa and the chlorarachniophyte Bigelowiella natans. Our results confirm the monophyly of Rhizaria (Foraminifera + Cercozoa), with very high bootstrap supports in all analyses. The overall topology of our trees is in agreement with the current view of eukaryote phylogeny with basal division into "unikonts" (Opisthokonts and Ameobozoa) and "bikonts" (Plantae, alveolates, stramenopiles, and excavates). As expected, Rhizaria branch among bikonts; however, their phylogenetic position is uncertain. Depending on the data set and the type of analysis, Rhizaria branch as sister group to either stramenopiles or excavates. Overall, the relationships between the major groups of unicellular bikonts are poorly resolved, despite the use of 85 proteins and the largest taxonomic sampling for this part of the tree available to date. This may be due to an acceleration of evolutionary rates in some bikont phyla or be related to their rapid diversification in the early evolution of eukaryotes.

Tempo and Mode of Spliceosomal Intron Evolution in Actin of Foraminifera

Spliceosomal introns are present in almost all eukaryotic genes, yet little is known about their origin and turnover in the majority of eukaryotic phyla. There is no agreement whether most introns are ancestral and have been lost in some lineage or have been gained recently. We addressed this question by analyzing the spatial and temporal distribution of introns in actins of foraminifera, a group of testate protists whose exceptionally rich fossil record permits the calibration of molecular phylogenies to date intron origins. We identified 24 introns dispersed along the sequence of two foraminiferan actin paralogues and actin deviating proteins, an unconventional type of fast-evolving actin found in some foraminifera. Comparison of intron positions indicates that 20 of 24 introns are specific to foraminifera. Four introns shared between foraminifera and other eukaryotes were interpreted as parallel gains because they have been found only in single species belonging to phylogenetically distinctive lineages. Moreover, additional recent intron gain due to the transfer between the actin paralogues was observed in two cultured species. Based on a relaxed molecular clock timescale, we conclude that intron gains in actin took place throughout the evolution of foraminifera, with the oldest introns inserted between 550 and 500 million years ago and the youngest ones acquired less than 100 million years ago.

Molecular phylogeny, evolutionary rates, and divergence timing of the symbiotic dinoflagellate genus Symbiodinium

Symbiotic dinoflagellates belonging to the genus Symbiodinium are found in association with a wide variety of shallow-water invertebrates and protists dwelling in tropical and subtropical coral-reef ecosystems. Molecular phylogeny of Symbiodinium, initially inferred using nuclear ribosomal genes, was recently confirmed by studies of chloroplastic and mitochondrial genes, but with limited taxon sampling and low resolution. Here, we present the first complete view of Symbiodinium phylogeny based on concatenated partial sequences of chloroplast 23S-rDNA (cp23S) and nuclear 28S-rDNA (nr28S) genes, including all known Symbiodinium lineages. Our data produced a well resolved phylogenetic tree and provide a strong statistical support for the eight distinctive clades (A-H) that form the major taxa of Symbiodinium. The relative-rate tests did not show particularly high differences between lineages and both analysed markers. However, maximum likelihood ratio tests rejected a global molecular clock. Therefore, we applied a relaxed molecular clock method to infer the divergence times of all extant lineages of Symbiodinium, calibrating its phylogenetic tree with the fossil record of soritid foraminifera. Our analysis suggests that Symbiodinium originated in early Eocene, and that the majority of extant lineages diversified since mid-Miocene, about 15 million years ago.

Constrictive bronchiolitis obliterans in patient with Castelman’s disease

A 37-year-old woman with hialin- vascular type Castelman’s disease (CD) localised in the retroperitoneal region, incompletely resected, developed progressive dyspnoea. The chest radiograph taken 3 months before the operation was normal. The chest CT scan revealed diffused bronchiectases, hyperinflation and air trapping. Pulmonary function tests disclosed severe obstructive impairment with hyperinflation. The bronchoscopic examination of the bronchial tree was normal. Cultures of sputum, bronchial washing and blood were negative. No pemphigus antibodies were found. Mycoplasmal, chlamydial and viral infections were excluded. Histological examination of specimens obtained by open lung biopsy revealed bronchiolar inflammation, submucosal bronchial fibrosis with obliteration of bronchiolar lumen. Constrictive bronchiolitis obliterans (CBO) was diagnosed. Despite slight clinical and spirometric improvements that were achieved due to corticosteroid therapy, one year later she died as a result of respiratory failure. It is widely known that patients with CD develop CBO during the course of paraneoplastic pemphigus. However we present the case of CBO and CD but without any symptoms of this condition.

Phylogenetic analysis and real time PCR detection of a presumbably undescribed Peronospora species on sweet basil and sage

Downy mildew of sweet basil (Ocimum basilicum) has become a serious disease issue for the producers of sweet basil in Switzerland since it was first recorded in 2001. Reported in Africa in Uganda as early as 1933, major outbreaks of this disease in Europe were first noted in Italy in 1999 and in the USA from 1993. Previous reports have named the pathogen as Peronospora lamii. Its preferential hosts belong to the Lamiaceae family including basils (Ocimum spp.), mints (Menta spp.), sages (Salvia spp.) and other aromatics. This study investigated the taxonomic status of the downy mildew pathogen, using both morphological characters and molecular analysis of the ITS region of the rDNA. The inherent variability of conidial dimensions made species differentiation difficult. Sequence homology and phylogenetic analysis of nine collections of the Peronospora on sweet basil showed unique ITS sequences distinct from those of P. lamii and any other sequenced Peronospora species. This paper describes and illustrates the morphology of this presumably undescribed species of Peronospora. Its taxonomic position and relationships with other related species in the same genus are presented and discussed. In addition to this work, PCR primers for real time PCR analysis have been developed for the specific detection of this downy mildew pathogen from infected tissues or seeds. It is shown that these primers can also be used in classic PCR.

Molecular Evidence for Host–Symbiont Specificity in Soritid Foraminifera

Symbiosis between the dinoflagellate genus Symbiodinium and various invertebrates and protists is an ubiquitous phenomenon in shallow tropical and subtropical waters. Molecular studies undertaken on cnidarian symbionts revealed the presence of several distinctive lineages or subgeneric clades of Symbiodinium whose taxonomic level provides limited information about the specificity between invertebrate hosts and their symbionts. This contrasts with the finding of several Symbiodinium clades being present almost exclusively in foraminifera and belonging to the subfamily Soritinae. To test whether such specificity also exists at a lower taxonomic level within Soritinae, we obtained the SSU rDNA sequences from 159 soritid individuals collected in nine localities worldwide and representing all known morphospecies of this subfamily. For each individual, the symbionts were determined either by sequencing or by RFLP analysis. We distinguished 22 phylotypes of Soritinae in relation with a number of symbiont "groups" corresponding to 3 clades and 5 subclades of Symbiodinium. Among the 22 soritid phylotypes, 14 show strict symbiont specificity and only one was found to be a host for more than two "groups" of Symbiodinium. It is suggested that the strong host-symbiont specificity observed in Soritinae is a combined effect of a selective recognition mechanism, vertical transmission of symbionts, and biogeographical isolation.

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.

The Testate Lobose Amoebae (Order Arcellinida Kent, 1880) Finally Find their Home within Amoebozoa

Testate lobose amoebae (order Arcellinida Kent, 1880) are common in all aquatic and terrestrial habitats, yet they are one of the last higher taxa of unicellular eukaryotes that has not found its place in the tree of life. The morphological approach did not allow to ascertain the evolutionary origin of the group or to prove its monophyly. To solve these challenging problems, we analyzed partial small-subunit ribosomal RNA (SSU rRNA) genes of seven testate lobose amoebae from two out of the three suborders and seven out of the 13 families belonging to the Arcellinida. Our data support the monophyly of the order and clearly establish its position among Amoebozoa, as a sister-group to the clade comprising families Amoebidae and Hartmannellidae. Complete SSU rRNA gene sequences from two species and a partial actin sequence from one species confirm this position. Our phylogenetic analyses including representatives of all sequenced lineages of lobose amoebae suggest that a rigid test appeared only once during the evolution of the Amoebozoa, and allow reinterpretation of some morphological characters used in the systematics of Arcellinida.

Higher-Order Phylogeny of Plasmodial Slime Molds (Myxogastria) Based on Elongation Factor 1-A and Small Subunit rRNA Gene Sequences

The Myxogastria are common soil microorganisms with a life cycle comprised of a plasmodial trophic stage and large fruiting bodies generally visible with the unaided eye. Until now, their classification has been based exclusively on a combination of morphological, ultrastructural, and developmental characters. Our study is the first attempt to examine phylogenetic relationships among these taxa using molecular data. Partial small-subunit ribosomal RNA and/or elongation factor 1-alpha gene sequences were obtained from eleven, mostly field-collected species representing the five orders of Myxogastria. Nineteen sequences were obtained and subjected to phylogenetic analysis together with 10 sequences available from GenBank. Separate and combined analyses of the two data sets support the division of Myxogastria into three distinct groups. The most basal clade consists of the Echinosteliales, an order considered to have affinities with Protostelia. The three species examined possess unpigmented or slightly pigmented spores. The second group consists of Liceales and Trichiales, taxa characterized by the presence of clear, but pigmented, spores. The third group consists of the two remaining orders, Physarales and Stemonitales, both possessing dark spores. This suggests that spore pigmentation is an evolutionarily conservative character in myxogastrians, and that the simple morphology of echinostelids is not a derived feature.

Molecular Phylogenetic Analysis Places Percolomonas cosmopolites within Heterolobosea: Evolutionary Implications

Percolomonas cosmopolitus is a common free-living flagellate of uncertain phylogenetic position that was placed within the Heterolobosea on the basis of ultrastructure studies. To test the relationship between Percolomonas and Heterolobosea, we analysed the primary structure of the actin and small-subunit ribosomal RNA (SSU rRNA) genes of P. cosmopolitus as well as the predicted secondary structure of the SSU rRNA. Percolomonas shares common secondary structure patterns of the SSU rRNA with heterolobosean taxa, which, together with the results of actin gene analysis, confirms that it is closely related to Heterolobosea. Phylogenetic reconstructions based on the sequences of the SSU rRNA gene suggest Percolomonas belongs to the family Vahlkampfiidae. The first Bayesian analysis of a large taxon sampling of heterolobosean SSU rRNA genes clarifies the phylogenetic relationships within this group.

Revised small subunit rRNA analysis provides further evidence that Foraminifera are related to Cercozoa

There is accumulating evidence that the general shape of the ribosomal DNA-based phylogeny of Eukaryotes is strongly biased by the long-branch attraction phenomenon, leading to an artifactual basal clustering of groups that are probably highly derived. Among these groups, Foraminifera are of particular interest, because their deep phylogenetic position in ribosomal trees contrasts with their Cambrian appearance in the fossil record. A recent actin-based phylogeny of Eukaryotes has proposed that Foraminifera might be closely related to Cercozoa and, thus, branch among the so-called crown of Eukaryotes. Here, we reanalyze the small-subunit ribosomal RNA gene (SSU rDNA) phylogeny by removing all long-branching lineages that could artifactually attract foraminiferan sequences to the base of the tree. Our analyses reveal that Foraminifera branch together with the marine testate filosean Gromia oviformis as a sister group to Cercozoa, in agreement with actin phylogeny. Our study confirms the utility of SSU rDNA as a phylogenetic marker of megaevolutionary history, provided that the artifacts due to the heterogeneity of substitution rates in ribosomal genes are circumvented.