Phylogeny of Choanozoa,Apusozoa, and Other Protozoa and Early Eukaryote Megaevolution

Abstract The primary diversification of eukaryotes involved protozoa, especially zooflagellates—flagellate protozoa without plastids. Understanding the origins of the higher eukaryotic kingdoms (two purely heterotrophic, Animalia and Fungi, and two primarily photosynthetic, Plantae and Chromista) depends on clarifying evolutionary relationships among the phyla of the ancestral kingdom Protozoa. We therefore sequenced 18S rRNA genes from 10 strains from the protozoan phyla Choanozoa and Apusozoa. Eukaryote diversity is encompassed by three early-radiating, arguably monophyletic groups: Amoebozoa, opisthokonts, and bikonts. Our taxon-rich rRNA phylogeny for eukaryotes allowing for intersite rate variation strongly supports the opisthokont clade (animals, Choanozoa, Fungi). It agrees with the view that Choanozoa are sisters of or ancestral to animals and reveals a novel nonflagellate choanozoan lineage, Ministeriida, sister either to choanoflagellates, traditionally considered animal ancestors, or to animals. Maximum likelihood trees suggest that within animals Placozoa are derived from medusozoan Cnidaria (we therefore place Placozoa as a class within subphylum Medusozoa of the Cnidaria) and hexactinellid sponges evolved from demosponges. The bikont and amoebozoan radiations are both very ill resolved. Bikonts comprise the kingdoms Plantae and Chromista and three major protozoan groups: alveolates, excavates, and Rhizaria. Our analysis weakly suggests that Apusozoa, represented by Ancyromonas and the apusomonads (Apusomonas and the highly diverse and much more ancient genus Amastigomonas, from which it evolved), are not closely related to other Rhizaria and may be the most divergent bikont lineages. Although Ancyromonas and apusomonads appear deeply divergent in 18S rRNA trees, the trees neither refute nor support the monophyly of Apusozoa. The bikont phylum Cercozoa weakly but consistently appears as sister to Retaria (Foraminifera; Radiolaria), together forming a hitherto largely unrecognized major protozoan assemblage (core Rhizaria) in the eukaryote tree. Both 18S rRNA sequence trees and a rare deletion show that nonciliate haplosporidian and paramyxid parasites of shellfish (together comprising the Ascetosporea) are not two separate phyla, as often thought, but part of the Cercozoa, and may be related to the plant-parasitic plasmodiophorids and phagomyxids, which were originally the only parasites included in the Cercozoa. We discuss rRNA trees in relation to other evidence concerning the basal diversification and root of the eukaryotic tree and argue that bikonts and opisthokonts, at least, are holophyletic. Amoebozoa and bikonts may be sisters—jointly called anterokonts, as they ancestrally had an anterior cilium, not a posterior one like opisthokonts; this contrasting ciliary orientation may reflect a primary divergence in feeding mode of the first eukaryotes. Anterokonts also differ from opisthokonts in sterol biosynthesis (cycloartenol versus lanosterol pathway), major exoskeletal polymers (cellulose versus chitin), and mitochondrial cristae (ancestrally tubular not flat), possibly also primary divergences.     

Molecular phylogeny, scale evolution and taxonomy of centrohelid heliozoa

Heliozoa are ubiquitous, unicellular phagotrophs with slender radiating axopodia for trapping prey. We sequenced 18S rRNA genes from 35 cultured centrohelid heliozoa (18 studied by electron microscopy) and 28 environmental libraries (18 freshwater, 10 marine), yielding 97 new sequences, this exceeding described species. Phylogenetic analyses show two major groups and that ancestral centrohelids probably had inner plate-like tangential and distinct outer radial silica scales, the latter diverging early into contrasting scale types seen in extant Pterocystis/Choanocystis and Acanthocystis/Raphidiophryidae. Scales were lost at least thrice. Pterocystis is paraphyletic, as was the classical family Acanthocystidae; Heterophrys was polyphyletic. Using scale morphology and rRNA sequences, we establish new families Pterocystidae (Pterocystis, Raineriophrys, Chlamydaster), Marophryidae (type Marophrys (Heterophrys) marina gen. et comb. nov.) and Choanocystidae, new suborders Pterocystina (Pterocystidae, Choanocystidae, Heterophryidae) and Acanthocystina (Acanthocystidae, Raphidiophryidae, Marophryidae), and ten new Pterocystis, Acanthocystis and Choanocystis species. Most clades are exclusively freshwater or exclusively marine; evolutionary transitions between these habitats have been rare.     

Phylogeny of the Centrohelida Inferred from SSU rRNA, Tubulins, and Actin Genes

Amoeboid protists are major targets of recent molecular phylogeny in connection with reconstruction of global phylogeny of eukaryotes as well as the search for the root of eukaryotes. The Centrohelida are one of the major groups of Heliozoa, classified in the Actinopodida, whose evolutionary position is not well understood. To clarify the relationships between the Centrohelida and other eukaryotes, we sequenced SSU rRNA, α-tubulin, and β-tubulin genes from a centroheliozoan protist, Raphidiophrys contractilis. The SSU rRNA phylogeny showed that the Centrohelida are not closely related to other heliozoan groups, Actinophryida, Desmothoracida, or Taxopodida. Maximum likelihood analyses of the combined phylogeny using a concatenate model for an α- + β-tubulin + actin data set, and a separate model for SSU rRNA, α- and β-tubulin, and actin gene data sets revealed the best tree, in which the Centrohelida have a closer relationship to Rhodophyta than to other major eukaryotic groups. However, both weighted Shimodaira–Hasegawa and approximately unbiased tests for the concatenate protein phylogeny did not reject alternative trees in which Centrohelida were constrained to be sisters to the Amoebozoa. Moreover, alternative trees in which Centrohelida were placed at the node branching before and after Amoebozoa or Viridiplantae were not rejected by the WSH tests. These results narrowed the possibilities for the position of Centrohelida to a sister to the Rhodophyta, to the Amoebozoa, or to an independent branch between the branchings of Amoebozoa and Rhodophyta (or possibly Plantae) at the basal position within the bikonts clade in the eukaryotic tree. [Reviewing Editor: Dr. Martin Kreitman]     

Oxnerella micra sp. n. (Oxnerellidae fam. n.), a tiny naked centrohelid, and the diversity and evolution of heliozoa

We describe a new tiny naked centrohelid heliozoan, Oxnerella micra, and sequenced its 18S and 28S rRNA genes. Its extremely slender axopodia have prominent extrusomes and are normally stretched across the substratum like those of many tiny granofilosean Cercozoa. Phylogenetic analysis of 18S rDNA shows that Oxnerella does not branch within any of the six known centrohelid families but very deeply in the order Pterocystida, between Choanocystidae and Pterocystidae; therefore we place it in a new family, Oxnerellidae. Oxnerella arose from ancestors with siliceous scales by losing them; as independently did Heterophryidae and Marophryidae, which replaced them by organic spicules, and Chlamydaster that is not truly naked but retains a mucilage coat and nests extremely shallowly within Pterocystidae. 28S rDNA has a group I intron. Concatenated Bayesian 18S/28S rRNA phylogeny shows centrohelids weakly as sisters to the naked non-centrohelid heliozoan Microheliella maris (Microhelida: Heliozoa). The centrohelid Marophrys marina possesses an elongation factor α-like (EFL) protein related to that of Polyplacocystis; Microheliella also has EFL. We also analysed Hsp90 and 18S rDNA sequences from 'Pinaciophora sp.' ATCC50355; they must be from a centrohelid, probably misidentified as Pinaciophora, the rDNA sequence branching deeply within Pterocystida. We reclassify two Polyplacocystis, Luffisphaera, Phaeodaria and Rotosphaerida.     

Phylogenetic Analysis of Eukaryotes Using Heat-Shock Protein Hsp90

Most eukaryote molecular phylogenies have been based on small-subunit ribosomal RNA as its database includes the most species, but serious problems have been encountered that can make these trees misleading. More recent studies using concatenated protein sequences have increased the data per organism, reducing misleading signals from a single sequence, but taxon sampling is limited. To increase the database of protein-coding genes we sequenced the cytosolic form of heat-shock protein Hsp90 from a broad variety of previously unsampled eukaryote groups: protozoan flagellates (phyla Choanozoa, Apusozoa, Cercozoa) and all three groups of chromists (Cryptophyta, Heterokonta, Haptophyta). Gamma-corrected distance trees robustly show three groups: bacterial sequences are sister to all eukaryote sequences, which are cleanly subdivided into the cytosolic sequences and a clade comprising the chloroplast and endoplasmic reticulum (ER) Hsp90 sequences. The eukaryote cytosolic sequences comprise a robust opisthokont clade (animals/Choanozoa/fungi), a bikont clade, and an amoebozoan branch. However their topology is not robust. When the cytosolic sequences are rooted using only the ER/chloroplast clade as outgroup the amoebozoan Dictyostelium is sister to the opisthokonts forming a unikont clade in the distance tree. Congruence of this tree with that for concatenated mitochondrial proteins suggests that the root of the eukaryote tree is between unikonts and bikonts. Gamma-corrected maximum likelihood analyses of cytosolic sequences alone (519 unambiguously aligned amino acid positions) show bikonts as a clade, as do least-squares distance trees, but with other distance methods and parsimony the sole amoebozoan species branches weakly within bikonts. Choanozoa are clearly sisters to animals. Some major bikont groups (e.g. green plants, alveolates, Euglenozoa) are consistently recovered, but others (e.g. discicristates, chromalveolates) appear only in some trees; the backbone of the bikont subtree is not resolved, the position of groups represented only by single sequences being particularly unclear. Although single-gene trees will probably never resolve these uncertainties, the congruence of Hsp90 trees with other data is greater than for most other molecules and further taxon sampling of this molecule is recommended.     

Megaphylogeny,Cell Body Plans,Adaptive Zones: Causes and Timing of Eukaryote Basal Radiations1

ABSTRACT. I discuss eukaryote megaphylogeny and the timing of major innovations in the light of multigene trees and the rarity of marine/freshwater evolutionary transitions. The first eukaryotes were aerobic phagotrophs, probably substratum‐associated heterotrophic amoeboflagellates. The primary eukaryote bifurcation generated unikonts (ancestrally probably unicentriolar, with a conical microtubular [MT] cytoskeleton) and bikonts (ciliary transformation from anterior cilium to ancestrally gliding posterior cilium; cytoskeleton of ventral MT bands). Unikonts diverged into Amoebozoa with anterior cilia, lost when lobosan broad pseudopods evolved for locomotion, and Choanozoa with posterior cilium and filose pseudopods that became unbranched tentacles/microvilli in holozoa and eventually the choanoflagellate/choanocyte collar. Of choanozoan ancestry, animals evolved epithelia, fibroblasts, eggs, and sperm. Fungi and Ichthyosporea evolved walls. Bikonts, ancestrally with ventral grooves, include three adaptively divergent megagroups: Rhizaria (Retaria and Cercozoa, ancestrally reticulofilose soft‐surfaced gliding amoeboflagellates), and the originally planktonic Excavata, and the corticates (Plantae and chromalveolates) that suppressed pseudopodia. Excavata evolved cilia‐generated feeding currents for grooval ingestion; corticates evolved cortical alveoli and ciliary hairs. Symbiogenetic origin and transfers of chloroplasts stimulated an explosive radiation of corticates—hard to resolve on multigene trees—and opisthokonts, and ensuing Cambrian explosions of animals and protists. Plantae lost phagotrophy and multiply evolved walls and macroalgae. Apusozoa, with dorsal pellicle and ventral pseudopods, are probably the most divergent bikonts or related to opisthokonts. Eukaryotes probably originated 800–850 My ago. Amoebozoa, Apusozoa, Loukozoa, and Metamonada may be the only extant eukaryote phyla pre‐dating Neoproterozoic snowball earth. New subphyla are established for Choanozoa and Loukozoa; Amoebozoa are divided into three revised subphyla, with Variosea transferred into Conosa.     

Microheliella maris (Microhelida ord. n.), an ultrastructurally highly distinctive new axopodial protist species and genus, and the unity of phylum Heliozoa

A new heliozoan, Microheliella maris, has sufficiently distinctive ultrastructure to merit a new order, Microhelida. Its 18S and 28S rRNA genes were sequenced earlier under the informal name 'marine microheliozoan'; we here sequenced its Hsp90 gene. A three-gene tree suggests that it is distantly related to centrohelids and others in chromist subkingdom Hacrobia; but it is too divergent to be placed accurately by few genes. Unlike centrohelids, its central spherical centrosome has two concentric granular shells and a dense core devoid of a trilaminar central disc. Microtubules radiate from the centrosomal shells. Unlike centrohelids, axopodia have only three microtubules, fixed basally by dense plasma membrane anchors, and bear terminal and lateral haptosome-like extrusomes. As in the heliomonad Heliomorpha, the centrosome is embedded in a nuclear cavity, and centrosomal microtubules traverse the nucleus inside cytoplasmic channels. A novel filogranular network interconnects mitochondria, ER, and plasma membrane. The microbody is attached to the nucleus and mitochondrion, which has vermicular tubular cristae. We group Microhelida and Heliomonadida, purged of dissimilar flagellates, as a new tubulicristate class Endohelea within phylum Heliozoa. Previously misassigned GenBank 18S rDNA sequences reveal Microhelida as diverse and ancient. We discuss principles underlying the biogenesis and diversity of axopodial patterns.     

The Zooflagellates Stephanopogon and Percolomonas are a Clade (Class Percolatea: Phylum Percolozoa)

ABSTRACT. The enigmatic marine protozoan Stephanopogon was first classified with ciliate protozoa because its pellicle also has rows of cilia. As ciliates have nuclear dimorphism with separate germline and somatic nuclei, Stephanopogon with several identical nuclei was regarded as a model for a hypothetical homokaryotic ancestor of ciliates. When electron microscopy revealed radical differences from ciliates this idea was abandoned, but its evolutionary position remains controversial, affinities with three other phyla being suggested. We sequenced 18S rDNA from Stephanopogon aff. minuta and actin genes from it and Stephanopogon apogon to clarify their evolutionary position. Phylogenetic analyses of 18S rRNA nest S. aff. minuta and Stephanopogon minuta securely within the protozoan phylum Percolozoa with zooflagellates of the genus Percolomonas, their closest relatives, comprising the clade Percolatea. This supports a previous grouping of Stephanopogon (order Pseudociliatida) with Percolomonas (order Percolomonadida) as a purely zooflagellate class Percolatea within Percolozoa, in contrast to the fundamentally amoeboid Heterolobosea, which are probably ancestral to Percolatea. Stephanopogon actins evolve exceptionally fast: actin trees place them as a long branch within bikont eukaryotes without revealing their sisters. We establish Percolomonadidae fam. n. for Percolomonas, excluding Pharyngomonas kirbyi g., sp. n. and Pharyngomonas (=Tetramastix=Percolomonas) salina comb. n., which unlike Percolomonas have two anterior and two posterior cilia and a pocket‐like pharynx, like “Macropharyngomonas”, now grouped with Pharyngomonas as a new purely zooflagellate class Pharyngomonadea, within a new subphylum Pharyngomonada; this contrasts them with the revised ancestrally amoeboflagellate subphylum Tetramitia. We discuss evolution of the percolozoan cytoskeleton and different body forms.     

Collodictyon--an ancient lineage in the tree of eukaryotes

The current consensus for the eukaryote tree of life consists of several large assemblages (supergroups) that are hypothesized to describe the existing diversity. Phylogenomic analyses have shed light on the evolutionary relationships within and between supergroups as well as placed newly sequenced enigmatic species close to known lineages. Yet, a few eukaryote species remain of unknown origin and could represent key evolutionary forms for inferring ancient genomic and cellular characteristics of eukaryotes. Here, we investigate the evolutionary origin of the poorly studied protist Collodictyon (subphylum Diphyllatia) by sequencing a cDNA library as well as the 18S and 28S ribosomal DNA (rDNA) genes. Phylogenomic trees inferred from 124 genes placed Collodictyon close to the bifurcation of the "unikont" and "bikont" groups, either alone or as sister to the potentially contentious excavate Malawimonas. Phylogenies based on rDNA genes confirmed that Collodictyon is closely related to another genus, Diphylleia, and revealed a very low diversity in environmental DNA samples. The early and distinct origin of Collodictyon suggests that it constitutes a new lineage in the global eukaryote phylogeny. Collodictyon shares cellular characteristics with Excavata and Amoebozoa, such as ventral feeding groove supported by microtubular structures and the ability to form thin and broad pseudopods. These may therefore be ancient morphological features among eukaryotes. Overall, this shows that Collodictyon is a key lineage to understand early eukaryote evolution.     

Early evolution of eukaryote feeding modes,cell structural diversity,and classification of the protozoan phyla Loukozoa,Sulcozoa, and Choanozoa

I discuss how different feeding modes and related cellular structures map onto the eukaryote evolutionary tree. Centrally important for understanding eukaryotic cell diversity are Loukozoa: ancestrally biciliate phagotrophic protozoa possessing a posterior cilium and ventral feeding groove into which ciliary currents direct prey. I revise their classification by including all anaerobic Metamonada as a subphylum and adding Tsukubamonas. Loukozoa, often with ciliary vanes, are probably ancestral to all protozoan phyla except Euglenozoa and Percolozoa and indirectly to kingdoms Animalia, Fungi, Plantae, and Chromista. I make a new protozoan phylum Sulcozoa comprising subphyla Apusozoa (Apusomonadida, Breviatea) and Varisulca (Diphyllatea; Planomonadida, Discocelida, Mantamonadida; Rigifilida). Understanding sulcozoan evolution clarifies the origins from them of opisthokonts (animals, fungi, Choanozoa) and Amoebozoa, and their evolutionary novelties; Sulcozoa and their descendants (collectively called podiates) arguably arose from Loukozoa by evolving posterior ciliary gliding and pseudopodia in their ventral groove. I explain subsequent independent cytoskeletal modifications, accompanying further shifts in feeding mode, that generated Amoebozoa, Choanozoa, and fungi. I revise classifications of Choanozoa, Conosa (Amoebozoa), and basal fungal phylum Archemycota. I use Choanozoa, Sulcozoa, Loukozoa, and Archemycota to emphasize the need for simply classifying ancestral (paraphyletic) groups and illustrate advantages of this for understanding step-wise phylogenetic advances.     

Global eukaryote phylogeny: Combined small- and large-subunit ribosomal DNA trees support monophyly of Rhizaria, Retaria and Excavata

Resolution of the phylogenetic relationships among the major eukaryotic groups is one of the most important problems in evolutionary biology that is still only partially solved. This task was initially addressed using a single marker, the small-subunit ribosomal DNA (SSU rDNA), although in recent years it has been shown that it does not contain enough phylogenetic information to robustly resolve global eukaryotic phylogeny. This has prompted the use of multi-gene analyses, especially in the form of long concatenations of numerous conserved protein sequences. However, this approach is severely limited by the small number of taxa for which such a large number of protein sequences is available today. We have explored the alternative approach of using only two markers but a large taxonomic sampling, by analysing a combination of SSU and large-subunit (LSU) rDNA sequences. This strategy allows also the incorporation of sequences from non-cultivated protists, e.g., Radiozoa (=radiolaria minus Phaeodarea). We provide the first LSU rRNA sequences for Heliozoa, Apusozoa (both Apusomonadida and Ancyromonadida), Cercozoa and Radiozoa. Our Bayesian and maximum likelihood analyses for 91 eukaryotic combined SSU+LSU sequences yielded much stronger support than hitherto for the supergroup Rhizaria (Cercozoa plus Radiozoa plus Foraminifera) and several well-recognised groups and also for other problematic clades, such as the Retaria (Radiozoa plus Foraminifera) and, with more moderate support, the Excavata. Within opisthokonts, the combined tree strongly confirms that the filose amoebae Nuclearia are sisters to Fungi whereas other Choanozoa are sisters to animals. The position of some bikont taxa, notably Heliozoa and Apusozoa, remains unresolved. However, our combined trees suggest a more deeply diverging position for Ancyromonas, and perhaps also Apusomonas, than for other bikonts, suggesting that apusozoan zooflagellates may be central for understanding the early evolution of this huge eukaryotic group. Multiple protein sequences will be needed fully to resolve basal bikont phylogeny. Nonetheless, our results suggest that combined SSU+LSU rDNA phylogenies can help to resolve several ambiguous regions of the eukaryotic tree and identify key taxa for subsequent multi-gene analyses.     

Multigene phylogeny of choanozoa and the origin of animals

Animals are evolutionarily related to fungi and to the predominantly unicellular protozoan phylum Choanozoa, together known as opisthokonts. To establish the sequence of events when animals evolved from unicellular ancestors, and understand those key evolutionary transitions, we need to establish which choanozoans are most closely related to animals and also the evolutionary position of each choanozoan group within the opisthokont phylogenetic tree. Here we focus on Ministeria vibrans, a minute bacteria-eating cell with slender radiating tentacles. Single-gene trees suggested that it is either the closest unicellular relative of animals or else sister to choanoflagellates, traditionally considered likely animal ancestors. Sequencing thousands of Ministeria protein genes now reveals about 14 with domains of key significance for animal cell biology, including several previously unknown from deeply diverging Choanozoa, e.g. domains involved in hedgehog, Notch and tyrosine kinase signaling or cell adhesion (cadherin). Phylogenetic trees using 78 proteins show that Ministeria is not sister to animals or choanoflagellates (themselves sisters to animals), but to Capsaspora, another protozoan with thread-like (filose) tentacles. The Ministeria/Capsaspora clade (new class Filasterea) is sister to animals and choanoflagellates, these three groups forming a novel clade (filozoa) whose ancestor presumably evolved filose tentacles well before they aggregated as a periciliary collar in the choanoflagellate/sponge common ancestor. Our trees show ichthyosporean choanozoans as sisters to filozoa; a fusion between ubiquitin and ribosomal small subunit S30 protein genes unifies all holozoa (filozoa plus Ichthyosporea), being absent in earlier branching eukaryotes. Thus, several successive evolutionary innovations occurred among their unicellular closest relatives prior to the origin of the multicellular body-plan of animals.     

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.     

The novel marine gliding zooflagellate genus Mantamonas (Mantamonadida ord. n.: Apusozoa)

Mantamonasis a novel genus of marine gliding zooflagellates probably related to apusomonad and planomonad Apusozoa. Using phase and differential interference contrast microscopy we describe the type species Mantamonas plasticasp. n. from coastal sediment in Cumbria, England. Cells are ～5μm long, ～5μm wide, asymmetric, flattened, biciliate, and somewhat plastic. The posterior cilium, on which they glide smoothly over the substratum, is long and highly acronematic. The much thinner, shorter, and almost immobile anterior cilium points forward to the cell's left. These morphological and behavioural traits suggest thatMantamonasis a member of the protozoan phylum Apusozoa. Analyses of 18S and 28S rRNA gene sequences of Mantamonas plasticaand a second genetically very different marine species from coastal sediment in Tanzania show Mantamonasas a robustly monophyletic clade, that is very divergent from all other eukaryotes. 18S rRNA trees mostly placeMantamonaswithin unikonts (opisthokonts, Apusozoa, and Amoebozoa) but its precise position varies with phylogenetic algorithm and/or taxon and nucleotide position sampling; it may group equally weakly as sister to Planomonadida, Apusomonadida or Breviata. On 28S rRNA and joint 18/28S rRNA phylogenies (including 11 other newly obtained apusozoan/amoebozoan 28S rRNA sequences) it consistently strongly groups with Apusomonadida (Apusozoa).     

Heterotrophic flagellates, centrohelid heliozoa and filose amoebae from marine and freshwater sites in the Antarctic

Heterotrophic flagellates, centrohelid heliozoa and filose amoebae were recorded from cultures derived from water collected at marine and freshwater sites in the Antarctic. Marine samples were collected in the vicinity of Prydz Bay, southeast Antarctica and freshwater samples from Sombre Lake on Signy Island and Crooked and Druzhby Lakes in the Vestfold Hills. Thirty-five species were identified. One new species, Kiitoksia kaloista (Protista incertae sedis), is described. The other species have been previously reported from other geographic locations, providing no evidence for endemism in protozoan species found in Antarctica. Received: 23 September 1996 / Accepted: 28 December 1996     

Phylogeny and molecular signatures for the phylum Thermotogae and its subgroups

Thermotogae species are currently identified mainly on the basis of their unique toga and distinct branching in the rRNA and other phylogenetic trees. No biochemical or molecular markers are known that clearly distinguish the species from this phylum from all other bacteria. The taxonomic/evolutionary relationships within this phylum, which consists of a single family, are also unclear. We report detailed phylogenetic analyses on Thermotogae species based on concatenated sequences for many ribosomal as well as other conserved proteins that identify a number of distinct clades within this phylum. Additionally, comprehensive analyses of protein sequences from Thermotogae genomes have identified >60 Conserved Signature Indels (CSI) that are specific for the Thermotogae phylum or its different subgroups. Eighteen CSIs in important proteins such as PolI, RecA, TrpRS and ribosomal proteins L4, L7/L12, S8, S9, etc. are uniquely present in various Thermotogae species and provide molecular markers for the phylum. Many CSIs were specific for a number of Thermotogae subgroups. Twelve of these CSIs were specific for a clade consisting of various Thermotoga species except Tt. lettingae, which was separated from other Thermotoga species by a long branch in phylogenetic trees; Fourteen CSIs were specific for a clade consisting of the Fervidobacterium and Thermosipho genera and eight additional CSIs were specific for the genus Thermosipho. In addition, the existence of a clade consisting of the deep branching species Petrotoga mobilis, Kosmotoga olearia and Thermotogales bacterium mesG1 was supported by seven CSIs. The deep branching of this clade was also supported by a number of CSIs that were present in various Thermotogae species, but absent in this clade and all other bacteria. Most of these clades were strongly supported by phylogenetic analyses based on two datasets of protein sequences and they identify potential higher taxonomic grouping (viz. families) within this phylum. We also report 16 CSIs that are shared by either some or all Thermotogae species and some species from other taxa such as Archaea, Aquificae, Firmicutes, Proteobacteria, Deinococcus, Fusobacteria, Dictyoglomus, Chloroflexi and eukaryotes. The shared presence of some of these CSIs could be due to lateral gene transfers between these groups. However, no clear preference for any particular group was observed in this regard. The molecular probes based on different genes/proteins, which contain these Thermotogae-specific CSIs, provide novel and highly specific means for identification of both known as well as previously unknown Thermotogae species in different environments. Additionally, these CSIs also provide valuable tools for genetic and biochemical studies that could lead to discovery of novel properties that are unique to these bacteria.     

Evolutionary relationships of apusomonads inferred from taxon-rich analyses of 6 nuclear encoded genes

The phylogenetic relationships of the biflagellate protist group Apusomonadidae have been unclear despite the availability of some molecular data. We analyzed sequences from 6 nuclear encoded genes-small-subunit rRNA, large-subunit rRNA, alpha-tubulin, beta-tubulin, actin, and heat shock protein 90-to infer the phylogenetic position of Apusomonas proboscidea Aléxéieff 1924. To increase the taxon richness of the study, we also obtained new sequences from representatives of several other major eukaryotic groups: Chrysochromulina sp. National Institute for Environmental Studies 1333 (Haptophyta), Cyanophora paradoxa (Glaucophyta), Goniomonas truncata (Cryptophyceae), Leucocryptos marina (Kathablepharidae), Mesostigma viride (Streptophyta, Viridiplantae), Peridinium limbatum (Alveolata), Pterosperma cristatum (Prasinophytae, Viridiplantae), Synura sphagnicola (Stramenopiles), and Thaumatomonas sp. (Rhizaria). In most individual gene phylogenies, Apusomonas branched close to either of the 2 related taxa-Opisthokonta (including animals, fungi, and choanoflagellates) or Amoebozoa. Combined analyses of all 4 protein-coding genes or all 6 studied genes strongly supported the hypothesis that Apusomonadidae is closely related to Opisthokonta (or to all other eukaryotic groups except Opisthokonta, depending on the position of the eukaryotic root). Alternative hypotheses were rejected in approximately unbiased tests at the 5% level. However, the strong phylogenetic signal supporting a specific affiliation between Apusomonadidae and Opisthokonta largely originated from the alpha-tubulin data. If alpha-tubulin is not considered, topologies in which Apusomonadidae is sister to Opisthokonta or is sister to Amoebozoa were more or less equally supported. One current model for deep eukaryotic evolution holds that eukaryotes are divided into primary "unikont" and "bikont" clades and are descended from a "uniflagellate" common ancestor. Together with other information, our data suggest instead that unikonts (=Opisthokonta and Amoebozoa) are not strictly monophyletic and are descended from biflagellate ancestors.     

A canonical FtsZ protein in <Emphasis Type="Italic">Verrucomicrobium spinosum</Emphasis>, a member of the Bacterial phylum <Emphasis Type="Italic">Verrucomicrobia</Emphasis> that also includes tubulin-producing <Emphasis Type="Italic">Prosthecobacter</Emphasis> species

Background  

The origin and evolution of the homologous GTP-binding cytoskeletal proteins FtsZ typical of Bacteria and tubulin characteristic of eukaryotes is a major question in molecular evolutionary biology. Both FtsZ and tubulin are central to key cell biology processes – bacterial septation and cell division in the case of FtsZ and in the case of tubulins the function of microtubules necessary for mitosis and other key cytoskeleton-dependent processes in eukaryotes. The origin of tubulin in particular is of significance to models for eukaryote origins. Most members of domain Bacteria possess FtsZ, but bacteria in genus Prosthecobacter of the phylum Verrucomicrobia form a key exception, possessing tubulin homologs BtubA and BtubB. It is therefore of interest to know whether other members of phylum Verrucomicrobia possess FtsZ or tubulin as their FtsZ-tubulin gene family representative.     

Phylogeny and Megasystematics of Phagotrophic Heterokonts (Kingdom Chromista)

Heterokonts are evolutionarily important as the most nutritionally diverse eukaryote supergroup and the most species-rich branch of the eukaryotic kingdom Chromista. Ancestrally photosynthetic/phagotrophic algae (mixotrophs), they include several ecologically important purely heterotrophic lineages, all grossly understudied phylogenetically and of uncertain relationships. We sequenced 18S rRNA genes from 14 phagotrophic non-photosynthetic heterokonts and a probable Ochromonas, performed phylogenetic analysis of 210–430 Heterokonta, and revised higher classification of Heterokonta and its three phyla: the predominantly photosynthetic Ochrophyta; the non-photosynthetic Pseudofungi; and Bigyra (now comprising subphyla Opalozoa, Bicoecia, Sagenista). The deepest heterokont divergence is apparently between Bigyra, as revised here, and Ochrophyta/Pseudofungi. We found a third universal heterokont signature sequence, and deduce three independent losses of ciliary hairs, several of 1-2 cilia, 10 of photosynthesis, but perhaps only two plastid losses. In Ochrophyta, heterotrophic Oikomonas is sister to the photosynthetic Chrysamoeba, whilst the abundant freshwater predator Spumella is biphyletic; neither clade is specifically related to Paraphysomonas, indicating four losses of photosynthesis by chrysomonads. Sister to Chrysomonadea (Chrysophyceae) is Picophagea cl. nov. (Picophagus, Chlamydomyxa). The diatom-parasite Pirsonia belongs in Pseudofungi. Heliozoan-like actinophryids (e.g. Actinosphaerium) are Opalozoa, not related to pedinellids within Hypogyristea cl. nov. of Ochrophyta as once thought. The zooflagellate class Bicoecea (perhaps the ancestral phenotype of Bigyra) is unexpectedly diverse and a major focus of our study. We describe four new biciliate bicoecean genera and five new species: Nerada mexicana, Labromonas fenchelii (=Pseudobodo tremulans sensu Fenchel), Boroka karpovii (=P. tremulans sensu Karpov), Anoeca atlantica and Cafeteria mylnikovii; several cultures were previously misidentified as Pseudobodo tremulans. Nerada and the uniciliate Paramonas are related to Siluania and Adriamonas; this clade (Pseudodendromonadales emend.) is probably sister to Bicosoeca. Genetically diverse Caecitellus is probably related to Anoeca, Symbiomonas and Cafeteria (collectively Anoecales emend.). Boroka is sister to Pseudodendromonadales/Bicoecales/Anoecales. Placidiales are probably divergent bicoeceans (the GenBank Placidia sequence is a basidiomycete/heterokont chimaera). Two GenBank ‘opalinid’ sequences are fungal; Pseudopirsonia is cercozoan; two previous GenBank ‘Caecitellus’ sequences are Adriamonas. Electronic Supplementary Material Electronic Supplementary material is available for this article at and accessible for authorised users. [Reviewing Editior: Patnck J. Keeling]