New taxa refresh the phylogeny and classification of pleurostomatid ciliates (Ciliophora,Litostomatea)

A high diversity of pleurostomatid ciliates has been discovered in the last decade, and their systematics needs to be improved in the light of new findings concerning their morphology and molecular phylogeny. In this work, a new genus, Protolitonotus gen. n., and two new species, Protolitonotus magnus sp. n. and Protolitonotus longus sp. n., were studied. Furthermore, 19 novel nucleotide sequences of SSU rDNA, LSU rDNA and ITS1‐5.8S‐ITS2 were collected to determine the phylogenetic relationships and systematic positions of the pleurostomatid ciliates in this study. Based on both molecular and morphological data, the results demonstrated that: (i) as disclosed by the sequence analysis of SSU rDNA, LSU rDNA and ITS1‐5.8S‐ITS2, Protolitonotus gen. n. is sister to all other pleurostomatids and thus represents an independent lineage and a separate family, Protolitonotidae fam. n., which is defined by the presence of a semi‐suture formed by the right somatic kineties near the dorsal margin of the body; (ii) the families Litonotidae and Kentrophyllidae are both monophyletic based on both SSU rDNA and LSU rDNA sequences, whereas Amphileptidae are non‐monophyletic in trees inferred from SSU rDNA sequences; and (iii) the genera Loxophyllum and Kentrophyllum are both monophyletic, whereas Litonotus is non‐monophyletic based on SSU rDNA analyses. ITS1‐5.8S‐ITS2 sequence data were used for the phylogenetic analyses of pleurostomatids for the first time; however, species relationships were less well resolved than in the SSU rDNA and LSU rDNA trees. In addition, a major revision to the classification of the order Pleurostomatida is suggested and a key to its families and genera is provided.     

GRACILARIOPSIS MCLACHLANII SP. NOV. AND GRACILARIOPSIS PERSICA SP. NOV. OF THE GRACILARIACEAE (GRACILARIALES,RHODOPHYCEAE) FROM THE INDIAN OCEAN1

Two new species of Gracilariopsis from the Indian Ocean are proposed—Gracilariopsis (Gp.) mclachlanii Buriyo, Bellorin et M. C. Oliveira sp. nov. from Tanzania and Gracilariopsis persica Bellorin, Sohrabipour et E. C. Oliveira sp. nov. from Iran—based on morphology and DNA sequence data (rbcL gene and SSU rDNA). Both species fit the typical features of Gracilariopsis: axes cylindrical throughout, freely and loosely ramified up to four orders, with an abrupt transition in cell size from medulla to cortex, cystocarps lacking tubular nutritive cells and superficial spermatangia. Nucleotide sequence comparisons of rbcL and SSU rDNA placed both species into the Gracilariopsis clade as distinct species from all the accepted species for this genus, forming a deeply divergent lineage together with some species from the Pacific. The new species are very difficult to distinguish on morphological grounds from other species of Gracilariopsis, stressing the importance of homologous molecular marker comparisons for the species recognition in this character‐poor genus.     

Short rDNA Barcodes for Species Identification in Foraminifera

ABSTRACT. Ribosomal DNA (rDNA) sequences have been shown to be very useful for identification of microbial eukaryotes. Usually, complete or long partial sequences of the rDNA genes are analysed. However, the development of new massive sequencing technologies producing a large amount of relatively short sequences raises the question about the minimum length of rDNA fragments necessary for species distinction in environmental sampling. To answer this question, we compared six variable regions of the small subunit (SSU) rDNA of foraminifera, known to have rapidly evolving ribosomal genes. For each region, we analysed (1) the sequence divergence between and within foraminiferal morphospecies, (2) the intraspecific polymorphism, and (3) the ability of each region to recognize the phylotypes inferred from analysis of a longer fragment. Our results show that although the variable regions differ considerably between taxonomic groups, most of them perform very well as species identifiers. Taking into account different analyses, the expansion segment of Helix 37 appears to be the best candidate for barcoding foraminifera. We propose that this relatively short region, averaging 50–60 nt in length, could be an ideal barcode for identification of foraminifera in environmental samples using massive sequencing approach.     

Morphological and Molecular Characterization of a New Species of Stephanopogon,Stephanopogon pattersoni n. sp.

Stephanopogon is a taxon of multiciliated protists that is now known to belong to Heterolobosea. Small subunit ribosomal DNA (SSU rDNA) phylogenies indicate that Stephanopogon is closely related to or descended from Percolomonas, a small tetraflagellate with a different feeding structure, thus these morphologically dissimilar taxa are of ongoing evolutionary interest. A new strain of Stephanopogon, KM041, was cultured, then characterized by light microscopy, electron microscopy, and SSU rDNA sequencing. KM041 is 18–35 μm (mean 26.8 μm) long, with six main ventral ciliary rows, one ventro‐lateral ciliary row, and three anterior barbs. It closely resembles Stephanopogon minuta Lei et al. 1999 in morphology, and is very closely related to an extinct culture “S. aff. minuta”, yet is markedly dissimilar in SSU rDNA sequence from a different isolate identified as S. minuta. This confirms that there are at least two distinct lineages of S. minuta‐like cells, and we describe KM041 as a new species, Stephanopogon pattersoni n. sp. The ultrastructure of KM041 resembles that of previously studied Stephanopogon species, though it has a novel paraxonemal structure in a few cilia. We note that a sub‐basal‐body pad and bulbous axosome are unlikely to be apomorphies for the Stephanopogon–Percolomonas clade.     

Phylogenetic placement of Cibicidoides wuellerstorfi (Schwager, 1866) from methane seeps and non‐seep habitats on the Pacific margin

Benthic foraminifera are among the most abundant groups found in deep‐sea habitats, including methane seep environments. Unlike many groups, no endemic foraminiferal species have been reported from methane seeps, and to our knowledge, genetic data are currently sparse for Pacific deep‐sea foraminifera. In an effort to understand the relationships between seep and non‐seep populations of the deep‐sea foraminifera Cibicidoides wuellerstorfi, a common paleo‐indicator species, specimens from methane seeps in the Pacific were analyzed and compared to one another for genetic similarities of small subunit rDNA (SSU rDNA) sequences. Pacific Ocean C. wuellerstorfi were also compared to those collected from other localities around the world (based on 18S gene available on Genbank, e.g., Schweizer et al., 2009). Results from this study revealed that C. wuellerstorfi living in seeps near Costa Rica and Hydrate Ridge are genetically similar to one another at the species level. Individuals collected from the same location that display opposite coiling directions (dextral and sinstral) had no species level genetic differences. Comparisons of specimens with genetic information available from Genbank (SSU rDNA) showed that Pacific individuals, collected for this study, are genetically similar to those previously analyzed from the North Atlantic and Antarctic. These observations provide strong evidence for the true cosmopolitan nature of C. wuellerstorfi and highlight the importance of understanding how these microscopic organisms are able to maintain sufficient genetic exchange to remain within the same species between seep and non‐seep habitats and over global distances.     

Arnoldiellina fluorescens gen. et sp. nov. – A new green autofluorescent foraminifer from the Gulf of Eilat (Israel)

A new monothalamous (single-chambered) soft-walled foraminiferal species, Arnoldiellina fluorescens gen. et sp. nov., was isolated from samples collected in the Gulf of Eilat, Israel. The species is characterized by a small elongate organic theca with a single aperture of allogromiids. It is characterized by the emission of green autofluorescence (GAF) that has so far not been reported from foraminifera. Phylogenetic analysis of a fragment of the 18S rDNA indicates that the species is related to a group of monothalamous foraminiferans classified as clade I. Although the morphology of the new species is very different compared to the other members of this clade, a specific helix in 18S rRNA secondary structure strongly supports this position.     

Molecular evidence for plastid robbery (Kleptoplastidy) in Dinophysis,a dinoflagellate causing diarrhetic shellfish poisoning

The dinoflagellate genus Dinophysis contains species known to cause diarrhetic shellfish poisoning. Although most photosynthetic dinoflagellates have plastids with peridinin, photosynthetic Dinophysis species have cryptophyte-like plastids containing phycobilin rather than peridinin. We sequenced nuclear- and plastid-encoded SSU rDNA from three photosynthetic species of Dinophysis for phylogenetic analyses. In the tree of nuclear SSU rDNA, Dinophysis was a monophyletic group nested with peridinin-containing dinoflagellates. However, in the tree of plastid SSU rDNA, the Dinophysis plastid lineage was within the radiation of cryptophytes and was closely related to Geminigera cryophila. These analyses indicate that an ancestor of Dinophysis, which may have originally possessed peridinin-type plastid and lost it subsequently, adopted a new plastid from a cryptophyte. Unlike dinoflagellates with fully integrated plastids, the Dinophysis plastid SSU rDNA sequences were identical among the three species examined, while there were species-specific base substitutions in their nuclear SSU rDNA sequences. Queries of the DNA database showed that the plastid SSU rDNA sequence of Dinophysis is almost identical to that of an environmental DNA clone of a <10 pm sized plankter, possibly a cryptophyte and a likely source of the Dinophysis plastid. The present findings suggest that these Dinophysis species engulfed and temporarily retained plastids from a cryptophyte.     

Assessing SSU rDNA Barcodes in Foraminifera: A Case Study using Bolivina quadrata

The Small Subunit Ribosomal RNA gene (SSU rDNA) is a widely used tool to reconstruct phylogenetic relationships among foraminiferal species. Recently, the highly variable regions of this gene have been proposed as DNA barcodes to identify foraminiferal species. However, the resolution of these barcodes has not been well established, yet. In this study, we evaluate four SSU rDNA hypervariable regions (37/f, 41/f, 43/e, and 45/e) as DNA barcodes to distinguish among species of the genus Bolivina, with particular emphasis on Bolivina quadrata for which ten new sequences ( KY468817 – KY468826 ) were obtained during this study. Our analyses show that a single SSU rDNA hypervariable sequence is insufficient to resolve all Bolivina species and that some regions (37/f and 41/f) are more useful than others (43/e and 45/e) to distinguish among closely related species. In addition, polymorphism analyses reveal a high degree of variability. In the context of barcoding studies, these results emphasize the need to assess the range of intraspecific variability of DNA barcodes prior to their application to identify foraminiferal species in environmental samples; our results also highlight the possibility that a longer SSU rDNA region might be required to distinguish among species belonging to the same taxonomic group (i.e. genus).     

Morphological and Molecular Identification of a New Ciliate,Zoothamnium palmphlatum nov. spec. (Ciliophora,Peritrichia) from North China

A new peritrichous ciliate, Zoothamnium palmphlatum nov. spec., was collected from an estuary in Yantai, China. It was investigated, using both live observation and silver staining. The new species can be identified by a palm‐shaped colony consisting of highly developed and alternately arranged secondary branches, a double‐layered peristomial lip, and an infundibular polykinety 3 composed of two parallel kinetosomal rows. Phylogenetic analyses of the small subunit (SSU) rRNA gene sequence show that Z. palmphlatum clusters with other members of the family Zoothamniidae. Furthermore, the comparison of primary and secondary SSU rDNA structures indicates that Z. palmphlatum is distinctly different from its morphologically similar species (93.2–97.0% in sequence similarity) in combination of H10 and H31 regions. Although Z. palmphlatum shares highest sequence similarity with Zoothamnium mucedo (98.9%), the new species has distinctly different structures in the H11, H12, H18, and H31 regions compared to Z. mucedo, which indicates that sequence similarity may not determine the similarity of the secondary structure.     

Molecular evidence for widespread occurrence of Foraminifera in soils

Environmental SSU rDNA‐based surveys are contributing to the dramatic revision of eukaryotic high‐level diversity and phylogeny as the number of sequence data increases. This ongoing revolution gives the opportunity to test for the presence of some eukaryotic taxa in environments where they have not been found using classical microscopic observations. Here, we test whether the foraminifera, a group of single‐celled eukaryotes, considered generally as typical for the marine ecosystems are present in soil. We performed foraminiferal‐specific nested PCR on 20 soil DNA samples collected in contrasted environments. Unexpectedly, we found that the majority of the samples contain foraminiferal SSU rDNA sequences. In total, we obtained 49 sequences from 17 localities. Phylogenetic analysis clusters them in four groups branching among the radiation of early foraminiferal lineages. Three of these groups also include sequences originated from previous freshwater surveys, suggesting that there were up to four independent colonization events of terrestrial and/or freshwater ecosystems by ancestral foraminifera. As shown by our data, foraminifera are a widespread and diverse component of soil microbial communities. Yet, identification of terrestrial foraminiferal species and understanding of their ecological role represent an exciting challenge for future research.     

Can Abundance of Protists Be Inferred from Sequence Data: A Case Study of Foraminifera

Protists are key players in microbial communities, yet our understanding of their role in ecosystem functioning is seriously impeded by difficulties in identification of protistan species and their quantification. Current microscopy-based methods used for determining the abundance of protists are tedious and often show a low taxonomic resolution. Recent development of next-generation sequencing technologies offered a very powerful tool for studying the richness of protistan communities. Still, the relationship between abundance of species and number of sequences remains subjected to various technical and biological biases. Here, we test the impact of some of these biological biases on sequence abundance of SSU rRNA gene in foraminifera. First, we quantified the rDNA copy number and rRNA expression level of three species of foraminifera by qPCR. Then, we prepared five mock communities with these species, two in equal proportions and three with one species ten times more abundant. The libraries of rDNA and cDNA of the mock communities were constructed, Sanger sequenced and the sequence abundance was calculated. The initial species proportions were compared to the raw sequence proportions as well as to the sequence abundance normalized by rDNA copy number and rRNA expression level per species. Our results showed that without normalization, all sequence data differed significantly from the initial proportions. After normalization, the congruence between the number of sequences and number of specimens was much better. We conclude that without normalization, species abundance determination based on sequence data was not possible because of the effect of biological biases. Nevertheless, by taking into account the variation of rDNA copy number and rRNA expression level we were able to infer species abundance, suggesting that our approach can be successful in controlled conditions.     

Species boundaries in gregarine apicomplexan parasites: a case study-comparison of morphometric and molecular variability in Lecudina cf. tuzetae (Eugregarinorida, Lecudinidae)

Trophozoites of gregarine apicomplexans are large feeding cells with diverse morphologies that have played a prominent role in gregarine systematics. The range of variability in trophozoite shapes and sizes can be very high even within a single species depending on developmental stages and host environmental conditions; this makes the delimitation of different species of gregarines based on morphological criteria alone very difficult. Accordingly, comparisons of morphological variability and molecular variability in gregarines are necessary to provide a pragmatic framework for establishing species boundaries within this diverse and poorly understood group of parasites. We investigated the morphological and molecular variability present in the gregarine Lecudina cf. tuzetae from the intestines of Nereis vexillosa (Polychaeta) collected in two different locations in Canada. Three distinct morphotypes of trophozoites were identified and the small subunit (SSU) rDNA was sequenced either from multicell isolates of the same morphotype or from single cells. The aim of this investigation was to determine whether the different morphotypes and localities reflected phylogenetic relatedness as inferred from the SSU rDNA sequence data. Phylogenetic analyses of the SSU rDNA demonstrated that the new sequences did not cluster according to morphotype or locality and instead were intermingled within a strongly supported clade. A comparison of 1,657 bp from 45 new sequences demonstrated divergences between 0% and 3.9%. These data suggest that it is necessary to acquire both morphological and molecular data in order to effectively delimit the "clouds" of variation associated with each gregarine species and to unambiguously reidentify these species in the future.     

A new genus of xenophyophores (Foraminifera) from Japan Trench: morphological description,molecular phylogeny and elemental analysis

The deep‐sea floor is inhabited by a number of unusual and enigmatic taxa, unknown in shallow waters. These include the xenophyophores, a group of giant protists that construct fragile agglutinated tests. Here, we describe Shinkaiya lindsayi gen. et sp. nov. , a new xenophyophore collected by the submersible Shinkai 6500 at a depth of 5435 m near the Japan Trench. The phylogenetic analysis performed on its complete small‐subunit ribosomal DNA (SSU rDNA) sequence confirms that Sh. lindsayi sp. nov. is a foraminiferan that is closely related to another xenophyophore, Syringammina corbicula Richardson, 2001, and to a monothalamous (single‐chambered) foraminiferan Rhizammina algaeformis Brady, 1879. In terms of morphology, the new genus resembles Syringammina, but its test wall is thicker, softer, and more weakly cemented. Moreover, the SSU rDNA sequences of the two genera are highly divergent. Mass spectra analyses reveal unusually high concentrations of some elements, such as lead, uranium, and mercury. The granellare system (the cytoplasm and the organic sheath that encloses it) is apparently devoid of barite crystals, which are usually abundant as intracellular inclusions in xenophyophores, but is rich in mercury (with 12 times the concentration of mercury found in the surrounding sediment). Fecal pellets retained within a tubular system (stercomare) concentrate heavy metals, including lead and uranium (respectively, two and six times more than that of the sediment). Based on a comparison of the compositions of the agglutinated test wall, the granellare, the stercomare, and the surrounding sediment, we discuss the impact of xenophyophores on their habitat. © 2009 The Linnean Society of London, Zoological Journal of the Linnean Society, 2009, 156 , 455–464.     

Molecular evidence for an independent origin of modern triserial planktonic foraminifera from benthic ancestors

Gallitellia vivans is the only Recent representative of the triserial planktonic foraminiferal family Guembelitriidae. The origin and evolution of this interesting albeit poorly known family are enigmatic. To elucidate the phylogenetic relationships between G. vivans and other planktonic foraminifera, we sequenced the small subunit ribosomal DNA (SSU rDNA) for comparison to our extensive database of planktonic and benthic species. Our analyses suggest that G. vivans represents a separate lineage of planktonic foraminifera, which branches close to the benthic rotaliids Stainforthia and Virgulinella. Both genera resemble Gallitellia in general morphological appearance, having elongate triserial tests at least in their early ontogenic stages. The divergence time of G. vivans is estimated at ca. 18 Ma (early Miocene), suggesting an origin independent from the Cretaceous and Paleogene triserial planktonic foraminifera. Our study thus indicates that modern triserial planktonic foraminifera are not related to the Cretaceous–Paleogene triserial species, and that the sporadic occurrences in the fossil record are not the result of poor preservation, but reflect multiple transitions from benthic to planktonic mode of life.     

Morphological and Molecular Identification of the New Species,Trichodina pseudoheterodentata sp. n. (Ciliophora,Mobilida, Trichodinidae) from the Channel Catfish,Ictalurus punctatus,in Chongqing China

It is difficult to differentiate similar trichodinids solely based on morphological examination, thus other identification methods, such as molecular identification, are necessary for identification. One mobilid ciliate named Trichodina pseudoheterodentata sp. n. was isolated from the gills of channel catfish, Ictalurus punctatus, in Chongqing, China. In the present study, its SSU rDNA was sequenced for the first time. Based on the results from both morphological identification and SSU rDNA sequencing, the new species was identified and compared with similar species. The morphological analysis revealed that T. pseudoheterodentata is a large Trichodina species (cell diameter 73.0–82.5 μm) and possesses robust denticles with broad blades and well‐developed blade connections. Characterization of its primary and secondary SSU rDNA structures indicated that T. pseudoheterodentata was distinctly different from congeneric species in H12, H15, E10_1, and V4 regions. Phylogenetic analysis revealed that the genetic distances among the new species and similar species reached interspecific levels, furthermore, the phylogenetic study also validated the identification of T. pseudoheterodentata and its placement in the genus Trichodina.     

INTRAGENOMIC NUCLEOTIDE POLYMORPHISM AMONG SMALL SUBUNIT (18S) RDNA PARALOGS IN THE DIATOM GENUS SKELETONEMA (BACILLARIOPHYTA)1

Morphological features of the siliceous cell wall traditionally have been used to diagnose and classify species of diatoms, though an increasing number of studies distinguish new species, in part, by phylogenetic analysis of rDNA sequences. Intragenomic sequence variation is common among the hundreds to thousands of rDNA cistrons present within a genome, and this variation has strong potential to obscure species boundaries based on rDNA sequences. We screened six Skeletonema culture strains for intragenomic nucleotide polymorphisms in the small subunit (SSU) rDNA gene and found that all strains had polymorphic sites, with proportions ranging from 0.57% to 1.81%. In all cases, transitions accounted for more than 70% of nucleotide differences at polymorphic sites. Polymorphic sites were split nearly evenly in the SSU rRNA molecule between the base‐paired regions of helices (52%) and the unpaired regions of loops and bulges (48%). Phylogenetic analysis showed that SSU rDNA genotypes were monophyletic for two of the six culture strains examined. Genotypes from the other four culture strains either showed little or no phylogenetic structure compared with genotypes of other conspecific culture strains or had phylogenetic structure that was incongruent with existing species boundaries. Moderate to strong support for monophyly was recovered for four of the seven species included in the analysis. Phylogenetic results combined with the low sequence divergence of SSU rDNA genotypes within species suggest that concerted evolution has not proceeded to completion in these species and/or that the rate at which variation is being generated exceeds the rate at which concerted evolution is expunging variation.