Novel cultured protists identify deep-branching environmental DNA clades of cercozoa: New Genera Tremula, Micrometopion, Minimassisteria, Nudifila, Peregrinia

We describe three new orders of filosan Cercozoa, five new deep-branching genera, eight new species of Thaumatomonas, Reckertia, Spongomonas, Rhogostoma, Agitata, Neoheteromita and Paracercomonas, sequence their 18S rDNA, and construct 18S rDNA trees for 148 Cercozoa. Our phylogeny indicates that Filosa were ancestrally gliding flagellates; non-flagellate filose amoebae evolved from them five times independently. The new genera are more closely related to environmental DNA sequences than cultured organisms. Tremula longifila, a zooflagellate glider on both flagella (unlike other Cercozoa), is the most divergent filosan (Tremulida ord. n.). Micrometopion nutans is a eukaryote-eating gliding zooflagellate like Metopion and Metromonas. Minimassisteria diva is a widespread trimorphic marine amoeboflagellate granofilosan. Peregrinia clavideferens, a non-testate, scale-bearing, filose amoeba, branches deeply in Thaumatomonadida, which are probably sisters to Spongomonadida. Nudifila producta is a filose amoeboflagellate related to Clautriavia and Marimonadida (ord. n., e.g. Pseudopirsonia, Auranticordis). We substantially revise Imbricatea, now including Spongomonadida, and Thecofilosea to include Phaeodaria. Thecofilosea and Imbricatea and Thecofilosea are sisters, both arguably ancestrally rigid gliding flagellates with ventral pseudopod-emitting grooves. Scale-free Ovulinata parva is sister to Paulinella, so imbricate silica scales can be lost. Internal hollow silica skeletons evolved twice in Thecofilosea (Ebriida, Phaeodaria) or were multiply lost. Protaspa replaces preoccupied 'Protaspis'.     

Phylogeny of novel naked Filose and Reticulose Cercozoa: Granofilosea cl. n. and Proteomyxidea revised

Naked filose and reticulose protozoa were long lumped as proteomyxids or left outside higher groups. We cultivated eight naked filose or reticulose strains, did light microscopy, 18S rDNA sequencing and phylogeny (showing all are Cercozoa), and sequenced 80 environmental 18S-types. Filose species belong in subphylum Filosa and reticulose ones in subphylum Endomyxa, making proteomyxids polyphyletic. We therefore transfer the classically mainly reticulose Proteomyxidea to Endomyxa, removing evident filosans as new class Granofilosea (including Desmothoracida, Acinetactis and new heliomonad family Heliomorphidae (new genus Heliomorpha (=Dimorpha)). Five new species of Limnofila gen. n. (L. mylnikovi; L. anglica; L. longa; L. oxoniensis; L. borokensis, previously misidentified as Biomyxa (=Gymnophrys) cometa) form a large freshwater clade (new order Limnofilida). Mesofila limnetica gen., sp. n. and Nanofila marina gen., sp. n. group separately in Granofilosea (Cryptofilida ord. n.). In Endomyxa, a new genus of reticulose proteomyxids (Filoreta marina, F. japonica, F. turcica spp. n., F. (=Corallomyxa) tenera comb. n.) forms a clade (Reticulosida) related to Gromiidea/Ascetosporea. Platyreta germanica gen., sp. n. and Arachnula impatiens are related vampyrellids (Aconchulinida) within a large clade beside Phytomyxea. Biomyxidae and Rhizoplasmidae fam. n. remain incertae sedis within Proteomyxidea. Gymnophrydium and Borkovia are revised. The reticulose Corallomyxa are unlike Filoreta and possibly Amoebozoa, not Cercozoa.     

Phylogenetic position of Gromia oviformis Dujardin inferred from nuclear-encoded small subunit ribosomal DNA

Gromia oviformis Dujardin is a common marine protist characterised by a large, globular test and filose pseudopodia. First considered a foraminifer, Gromia was later placed within the Filosea and recently included among amoebae of uncertain affinities. In order to clarify the phylogenetic position of this genus, we sequenced the complete small-subunit ribosomal DNA gene of G. oviformis collected at five different geographic localities. The high divergence of obtained sequences suggests that G. oviformis is a species complex composed of several genetically distinct sibling species. Sequence analyses show Gromia to be a member of the Cercozoa, a heterogeneous assemblage which includes filose amoebae, the amoeboflagellate cercomonads, the chlorarachniophytes and the plasmodiophorid plant pathogens. Contrary to traditional classification, Gromia is not closely related to other testate filose amoebae (the Euglyphida), but seems to branch early among the Cercozoa. Our analyses also show a close relationship between the Cercozoa and the Acantharea. Because the Cercozoa are related to the Foraminifera based on other molecular data, we propose that most protists possessing filopodia, reticulopodia and axopodia have a common origin.     

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.     

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.     

Shedding light on vampires: the phylogeny of vampyrellid amoebae revisited

With the advent of molecular phylogenetic techniques the polyphyly of naked filose amoebae has been proven. They are interspersed in several supergroups of eukaryotes and most of them already found their place within the tree of life. Although the 'vampire amoebae' have attracted interest since the middle of the 19th century, the phylogenetic position and even the monophyly of this traditional group are still uncertain. In this study clonal co-cultures of eight algivorous vampyrellid amoebae and the respective food algae were established. Culture material was characterized morphologically and a molecular phylogeny was inferred using SSU rDNA sequence comparisons. We found that the limnetic, algivorous vampyrellid amoebae investigated in this study belong to a major clade within the Endomyxa Cavalier-Smith, 2002 (Cercozoa), grouping together with a few soil-dwelling taxa. They split into two robust clades, one containing species of the genus Vampyrella Cienkowski, 1865, the other containing the genus Leptophrys Hertwig & Lesser, 1874, together with terrestrial members. Supported by morphological data these clades are designated as the two families Vampyrellidae Zopf, 1885, and Leptophryidae fam. nov. Furthermore the order Vampyrellida West, 1901 was revised and now corresponds to the major vampyrellid clade within the Endomyxa, comprising the Vampyrellidae and Leptophryidae as well as several environmental sequences. In the light of the presented phylogenetic analyses morphological and ecological aspects, the feeding strategy and nutritional specialization within the vampyrellid amoebae are discussed.     

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.     

Molecular phylogeny of Amoebozoa and the evolutionary significance of the unikont Phalansterium

The taxonomic position of the uniciliate, unicentriolar zooflagellate Phalansterium is problematic; its distinctive ultrastructure with a pericentriolar microtubular cone placed it in its own order and suggested phenotypic closeness to the eukaryote cenancestor. We sequenced the 18S rRNA of a unicellular Phalansterium. Phylogenetic analysis shows that it belongs to Amoebozoa, decisively rejecting a postulated relationship with the cercozoan Spongomonas; Phalansterium groups with Varipodida ord. nov. (Gephyramoeba/Filamoeba) or occasionally Centramoebida emend. (Acanthamoebidae/Balamuthiidae fam. nov.), centrosomes of the latter suggesting flagellate ancestors. We also studied Phalansterium solitarium cyst ultrastructure; unlike previously studied P. solitarium, this strain has pentagonally symmetric walls like P. consociatum. We also sequenced 18S rRNA genes of further isolates of Hyperamoeba, an aerobic unicentriolar amoeboflagellate with conical microtubular skeleton; both group strongly with myxogastrid Mycetozoa. However, the four Hyperamoeba strains do not group together, suggesting that Hyperamoeba are polyphyletic derivatives of myxogastrids that lost fruiting bodies independently. We revise amoebozoan higher-level classification into seven classes, establishing Stelamoebea cl. nov. for Protosteliida emend. plus Dictyosteliida (biciliate former ‘protostelids’ comprise Parastelida ord. nov. within Myxogastrea), and new subphylum Protamoebae to embrace Variosea cl. nov. (Centramoebida, Phalansteriida, Varipodida), Lobosea emend., Breviatea cl. nov. for ‘Mastigamoeba invertens’ and relatives, and Discosea cl. nov. comprising Glycostylida ord. nov. (vannellids, vexilliferids, paramoebids, Multicilia), Dermamoebida ord. nov. (Thecamoebidae) and Himatismenida. We argue that the ancestral amoebozoan was probably unikont and that the cenancestral eukaryote may have been also.     

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.     

Distribution of protozoa in subsurface sediments of a pristine groundwater study site in oklahoma

Sediment core samples were obtained at a groundwater study site in Oklahoma in January and June 1985. Most-probable-number estimates showed that protozoan numbers declined steeply with depth in subsoil. Flagellates and amoebae dominated the protozoan population, which declined to a most probable number of 28 . g (dry weight) in a clay loam layer at the bottom of the unsaturated zone. Samples from a texturally variable interface zone between 3 and 4 m down also were variable in their content of protozoa. Four contiguous clay loam samples in a single core from this zone contained variable numbers of amoebae ranging from 0.2 to 44 . g (dry weight). However, a sandy clay loam layer at the bottom of the core contained a mixture of flagellates and amoebae with a combined population density of 67 . g (dry weight). A slow-growing filose amoeba was isolated from interface zone samples and was tentatively classified in a new family in the order Aconchulinida. Protozoa were not detected in the saturated zone except in a very permeable gravelly, loamy sand layer at a depth of approximately 7.5 m. Low numbers (4 to 6 . g [dry weight]) of surface-type flagellates and amoebae, as well as the filose amoeba seen in the interface zone, were observed in this layer. Acid-treated and untreated samples contained equivalent numbers of protozoa, showing that the majority of protozoa in the layer at 7.5 m and the interface zone samples were encysted. Increased numbers of bacteria also were found in the layer at 7.5 m, indicating that it was biologically more active than other saturated-zone layers. Cyanobacteria grew in illuminated samples from this layer, suggesting that it may be connected hydrologically to a nearby river.     

Molecular Evolutionary Analyses of Nuclear-Encoded Small Subunit Ribosomal RNA Identify an Independent Rhizopod Lineage Containing the Euglyphina and the Chlorarachniophyta

The Rhizopoda comprise a diverse assemblage of protists which depend on lobose or filose pseudopodia for locomotion. The biochemical and morphological diversity of rhizopods has led to an uncertain taxonomy. Ribosomal RNA sequence comparisons offer a measure of evolutionary relatedness that is independent of morphology and has been used to demonstrate a polyphyletic origin of the Lobosea. We sequenced complete small subunit ribosomal RNA coding regions from the filose amoebae, Euglypha rotunda and Paulinella chromatophora (Euglyphina) to position these taxa in the eukaryote phylogeny. The neighbor-joining analyses show that E. rotunda and P. chromatophora share a monophyletic origin and are not closely related to any lobose amoebae in our analyses. Instead, the Euglyphina form a robust sister group to the Chlorarachniophyta. These results provide further evidence for the polyphyly of the Rhizopoda and support the creation of a new amoeboid lineage which includes the Euglyphina and the chlorarachniophyte algae; taxa with tubular mitochondrial cristae and filose or reticulate pseudopodia.     

Archamoebae: the ancestral eukaryotes?

The archezoan phylum Archamoebae Cavalier-Smith, 1983 is here modified by adding a new order Phreatamoebida (presently containing only Phreatamoeba) and removing the family Entamoebidae. Entamoebidae are instead tentatively placed as a class Entamoebea together with the classes Heterolobosea, Percolomonadea and Pseudociliatea in the new protozoan phylum Percolozoa Cavalier-Smith, 1991. Thus emended the phylum Archamoebae is more homogeneous; it is more distinguished from the other two phyla of the primitively amitochondrial kingdom and superkingdom Archezoa (i.e. Metamonada and Microsporidia) by having kinetids with only a single flagellum and basal body and a flagellar root consisting of a cone of evenly spaced microtubules. This unikont character of the archamoebae suggests that they may be ancestral to the tetrakont Metamonada, from which the non-flagellate Microsporidia possibly evolved. Higher eukaryotes (superkingdom Metakaryota) probably evolved from a tetrakont metamonad by the symbiotic origin of mitochondria and peroxisomes. If so, the Archamoebae are the most primitive extant phylum of eukaryotes; if molecular phylogenetic studies confirm this idea, Archamoebae will deserve intensive study, which could reveal much about the origin of the eukaryote condition and also establish what is truly universal among eukaryotes. Archamoebae, like other Archezoa, lack mitochondria and peroxisomes and have no obvious Golgi dictyosomes. Their evolutionary significance is discussed and a detailed classification is presented in which the two earlier classes are merged into a single one: Pelobiontea Page, 1976 stat. nov., containing two orders Mastigamoebida Frenzel, 1892 (Syn. Rhizo-Flagellata Kent, 1880 non Rhizomastigida auct.) (including Mastigamoeba, Mastigina, Mastigella, Pelomyxa and probably a few other genera, which have one or more flagella or cilia (motile or immotile, 9 + 2 or otherwise) in the amoeboid trophic phase), and Phreatamoebida ord. nov. (including only Phreatamoeba in the new family Phreatamoebidae, which has alternating phases of non-flagellate amoebae and uniflagellate cells). Mastigamoebida are divided into three families: Mastigamoebidae Goldschmidt, 1907; Mastigellidae fam. nov.; Pelomyxidae Schulze, 1877. Archamoebae may be uni- or multi-nucleate and either gut parasites or (more usually) free-living in soil, freshwater, or marine habitats. Some can form cysts that would probably fossilize; the earliest (1450 My old) smooth-walled fossil cells large enough to be probable eukaryotes might therefore be archamoebal cysts.     

Reinvestigations of Three “Well-known” Marine Scuticociliates: Uronemella filificum (Kahl, 1931) nov. gen., nov. comb., Pseud cohnilembus hargisi Evans & Thompson, 1964 and Cyclidium citrullus Cohn 1865, with Description of the New Genus Uronemella (Protozoa, Ciliophora, Scuticociliatida)

The living morphology, infraciliature and silverline system of 3 “well-known” marine scuticociliates, Uronemella filificum (Kahl, 1931) nov. gen., nov. comb. (formerly Uronema filificum Kahl, 1931), Pseudocohnilembus hargisi Evans & Thompson, 1964 and Cyclidium citrullus Cohn 1865 are reinvestigated and redescribed.

Based on the data obtained, we suggest an establishment of a new genus Uronemella. The diagnosis for the new taxon: thigmotactic Uronematidae with generally pear-shaped body and subequatorially positioned cytostome; apical plate dominant; oral apparatus Uronema-like, one-rowed membranelle 1 about as long as membranelle 2; paroral membrane extending anteriorly to about mid-level of membrane 2; one caudal cilium; in vivo exhibiting typical rotatory movement with help of a caudal-cilium-associated sticky thread; generally in marine habitats. According to this definition, three nominal species as new combinations are transferred into this genus: Uronemella binucleata (Song, 1993) nov. comb. (= Homalogastra binucleata Song, 1993), Uronemella filificum (Kahl, 1931) nov. comb. (= Uronema filificum Kahl, 1931) and Uronemella cymruensis (Pérez-Uz & Hope, 1997) nov. comb. (=Urocyclon cymruensis Pérez-Uz & Hope, 1997). For comparison with Uronemella, some other closely-related taxa are also briefly outlined in the present paper.     

Spatial distribution of gymnamoebae (Rhizopoda, Lobosea) in brackish-water sediments at the scale of centimeters and millimeters

In order to study micro-spatial distribution of amoebae, an intact slice of sandy sediment from the brackish-water Nivå Bay (Baltic Sea, The Sound), 40 × 24 mm in size and 2 mm in thickness was gently sectioned into cubes, 2 × 2 × 2 mm in size. Each cube was inoculated into enrichment media to reveal the biodiversity of amoebae. Seventeen species of amoebae were recovered. The 2-D map of amoebae species distribution in the slice, consisting of 240 2 × 2 mm cells was drawn and analyzed. Results show heterogeneous distribution of amoebae at the scale of centimeters and millimeters and confirm the idea of the presence of microhabitats, selectively occupied by amoebae species. Three types of distribution patterns were found: random, aggregated and equally spaced. Microelectrode studies indicated that amoebae distribution was not related to the dissolved oxygen content in the sediment. The studied slice of sediment contained several pronounced “hotspots” of amoebae biodiversity, where up to four species co-occur in the same area. Seven species of amoebae numbered 1–4 specimens in the studied slice (i.e. there was 0.5–2 cell ml^–1). Analysis of the amoebae distribution map shows the high probability of undersampling rare amoebae species during faunistic studies.     

Morphology and phylogeny of Sainouron acronematica sp. n. and the ultrastructural unity of Cercozoa

Sainouron are soil zooflagellates of obscure taxonomy. We studied the ultrastructure of S. acronematica sp. n. and sequenced its extremely divergent 18S rDNA and that of Cholamonas cyrtodiopsidis (here grouped as new family Sainouridae) to clarify their phylogeny. Ultrastructurally similar, they weakly group together, deeply within Monadofilosa. Sainouron has three cytoplasmic microtubules; all organelles specifically link to them or the nucleus. Mature centrioles have fibrous rhizoplasts. The posterior centriole bearing the motile cilium (with cortical filaments) has a transitional hub-lattice; a dense spiral fibre links its thicker rhizoplast and triplets; its ciliary root has two microtubules: mt1, underlying the plasma membrane, initiates at the spiral fibre; mt2, laterally attached to mt1 and nucleus, initiates in the amorphous centrosomal region. The anterior younger cilium, an immotile stub with submembrane skeleton as in Cholamonas, lacks axoneme, microtubular root, rhizoplasts and spiral fibre, but becomes the posterior one every cell cycle. The nuclear envelope donates coated vesicles directly to the Golgi, which makes kinetocyst-type extrusomes, concentrated at the cell anterior for extrusion into phagosomes. Ciliary transition region proximal hub-lattices (postulated to contain centrin) and distal nonagonal fibres are cercozoan synapomorphies, found with slight structural variation in all flagellate Cercozoa, but not in outgroups.     

Transfer of the Thecate Amoeba Lecythium mutabilis to a Novel Genus Omnivora (Fiscullidae,Thecofilosea, Cercozoa)

Thecofilosea is a class in Cercozoa (Rhizaria) comprising mainly freshwater‐inhabiting algivores. Recently, numerous isolates of thecofilosean amoebae have been cultured and were characterized by an integrated morphological and molecular approach. As attempts to establish a culture of Lecythium mutabilis repeatedly failed, it was not yet investigated by molecular means. We isolated single cells of L. mutabilis directly from their habitat and successfully sequenced the V4 region of their SSU rDNA. Phylogenetic analyses showed that L. mutabilis is not directly related to the genus Lecythium and instead branches within the Fiscullidae (Tectofilosida, Thecofilosea). Accordingly, we transfer the species L. mutabilis to a novel genus Omnivora gen. nov.     

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     

Effects of Mannose on Pathogenesis of Acanthamoeba castellanii

Acanthamoeba spp. are single-celled protozoan organisms that are widely distributed in the environment. In this study, to understand functional roles of a mannose-binding protein (MBP), Acanthamoeba castellanii was treated with methyl-alpha-D-mannopyranoside (mannose), and adhesion and cytotoxicity of the amoeba were analyzed. In addition, to understand the association of MBP for amoeba phagocytosis, phagocytosis assay was analyzed using non-pathogenic bacterium, Escherichia coli K12. Amoebae treated with mannose for 20 cycles exhibited larger vacuoles occupying the most area of the amoebic cytoplasm in comparison with the control group amoebae and glucose-treated amoebae. Mannose-selected amoebae exhibited lower levels of binding to Chinese hamster ovary (CHO) cells. Exogenous mannose inhibited >50% inhibition of amoebae (control group) binding to CHO cells. Moreover, exogenous mannose inhibited amoebae (i.e., man-treated) binding to CHO cells by <15%. Mannose-selected amoebae exhibited significantly decreased cytotoxicity to CHO cells compared with the control group amoebae, 25.1% vs 92.1%. In phagocytic assay, mannose-selected amoebae exhibited significant decreases in bacterial uptake in comparison with the control group, 0.019% vs 0.03% (P<0.05). Taken together, it is suggested that mannose-selected A. castellanii trophozoites should be severely damaged and do not well interact with a target cell via a lectin of MBP.