Loricate choanoflagellates (Acanthoecida) from warm water seas. V. Thomsenella Özdikmen (= Platypleura Thomsen)

Loricate choanoflagellate genera that incorporate flattened costal strips in the lorica (i.e. Calotheca, Stephanacantha, Thomsenella (= Platypleura) and Syndetophyllum) are prevalent in warm water habitats. The genus Thomsenella (=Platypleura) thus comprises four species and three of these have an Andaman Sea type locality. Our ongoing examination of loricate choanoflagellate material from all major warm water oceans has provided us with the opportunity of revisiting species of Thomsenella in order to test and fortunately verify, in a morpho-specific context, the robustness of the species matrix initially defined.     

Loricate choanoflagellates (Acanthoecida) from warm water seas. II. Bicosta,Apheloecion, Campyloacantha,Crucispina, Calliacantha and Saroeca

The main outcome of this and subsequent papers is to provide a baseline survey of heterotrophic protist diversity from warm water marine ecosystems, exemplified by loricate choanoflagellates (Acanthoecida). Genera in focus here (i.e. Bicosta, Apheloecion, Campyloacantha, Crucispina, Calliacantha and Saroeca) possess anterior spines or projections and a posterior pedicel, and have 0, 1 or 2 transverse costae. Longitudinal costae are, with the exception of Campyloacantha, external to transverse costal elements across all genera examined here. We describe here Apheloecion eqpacia sp. nov. and Calliacantha magna sp. nov., both of which are so far distributionally confined to warm water habitats. A ‘form A’ of Bicosta minor is introduced to facilitate the distinction between B. minor sensu stricto and a presumed warm water adapted variant with a posterior lorica chamber twist of the longitudinal costae.     

Stephanoeca arndti spec. nov. – First cultivation success including molecular and autecological data from a freshwater acanthoecid choanoflagellate from Samoa

Until recently acanthoecid choanoflagellates have been described only from marine and brackish waters. Here I describe a distinct, strictly freshwater acanthoecid species from Samoa based on its morphology, ecology and molecular biological data (partial Small Subunit rDNA). The lorica of the species is characterised by two extensions at the posterior chamber which are used for attachment to the substratum. The posterior chamber is constructed of irregularly arranged costae. The anterior chamber consists of four transverse costal rings and 14–18 longitudinal costae. Despite its sturdy appearance, the lorica was extremely sensitive to water turbulence and movements of the water. The species showed a salinity tolerance of 0.5 practical salinity units with reduced growth rates and a temperature tolerance range of 20–34 °C. According to the morphology, phylogenetic analysis, and autecology of the species it was classified as a member of the genus Stephanoeca.     

Kakoeca antarctica gen. et sp.n., a loricate choanoflagellate (Acanthoecidae, Choanoflagellida) from Antarctic sea ice with a unique protoplast suspensory membrane

A new genus and species of loricate choanoflagellate, Kakoeca aniarctica Buck & Marchant gen. et sp.n. grown in rough culture from an Antarctic sea ice innoculum is described. This organism has a distinctive lorica morphology consisting of more than 200 costal strips arranged in transverse and longitudinal costae that arc perpendicular to one another in the posterior portion of the lorica. The transverse costae show declination with respect to the lorica axis in the anterior part of the lorica. The cell is suspended in the lorica by a robust protoplast suspensory membrane. This membrane blocks water flow from the posterior of the lorica necessitating water entry through the side of the lorica, an area where the maximum sized apertures in the lorica are found. Terminology (lorica lining and protoplast suspensory) is suggested for the two types of lorica membranes which have been found associated with loricas.     

Loricate choanoflagellates (Acanthoecida) from warm water seas. VI. Pleurasiga Schiller and Parvicorbicula Deflandre

The loricate choanoflagellate genera Pleurasiga and Parvicorbicula are taxonomically ambiguous. Pleurasiga because of the uncertainty that relates to the true identity of the type species, and Parvicorbicula because too many newly described species over time have been dumped here in lack of better options. While all species currently allocated to the genus Pleurasiga (with the exception of the type species) are observed in our samples from the global warm water belt, the genus Parvicorbicula is represented by just a few and mostly infrequently recorded taxa. Two new species, viz. Pl. quadrangiella sp. nov. and Pl. minutissima sp. nov., are described here. While the former is closely related to Pl. echinocostata, the latter is reminiscent of Pl. minima. Core species of Pleurasiga and Parvicorbicula deviate from the vast majority of loricate choanoflagellates in having both the anterior and the mid-lorica transverse costae located exterior to the longitudinal costae. In Pl. quadrangiella there is no mid-lorica transverse costa but rather a small posterior transverse costa located inside the longitudinal costae. In Pl. minutissima the mid-lorica transverse costa has extensive costal strip overlaps which reveal patterns of costal strip junctions that deviate from the norm.     

Developmental studies on the loricate choanoflagellate Stephanoeca diplocostata Ellis. III. Growth and turnover of silica,preliminary observations

Growth, turnover of silica and lorica morphology of Stephanoeca diplocostata Ellis have been investigated in batch cultures at 20 °C. Mean cell doubling times for separate experiments ranged from 9.1–13.8 h. During exponential growth, uptake of reactive silicate progressed steadily and throughout this phase the average amount of biogenic silicon per cell was 2.1 pg. Once growth declined, net dissolution of silica from loricae became apparent and progressed steadily throughout the stationary and death phases. The minor difference in solubility between loricae of living cells and costal strips cleaned with acid indicates that even if an organic component is associated with the silica of costal strips it does not inhibit silica dissolution. The first effects of silica dissolution on cells as revealed by electron microscopy are limited to corrosion on the surfaces and the hollowing out of the centres of costal strips but ultimately a consistent pattern of lorica disintegration occurs.     

Developmental studies on the loricate choanoflagellateStephanoeca diplocostata Ellis VI. Effects of silica replenishment on silica impoverished cells

Summary Stephanoeca diplocostata has a facultative requirement for silica in that silica starvation does not inhibit growth as measured by increase in cell numbers. In spite of the absence of a lorica silica impoverished protoplasts still divide in the characteristic tectiform manner and a juvenile protoplast, when released from the parent cell, still extends its lorica assembling tentacles despite the absence of costal strips with which to produce a lorica. Replenishment of silica to silica starved cells in mid to late exponential phase cultures results in a decrease in the growth rate but at the same time silica is taken up and utilised for the deposition of costal strips. Mature costal strips are extruded and accumulated in bundles of 5–8 on the surface of the protoplast but are not passed to the top of the collar as would be expected in silica enriched loricate cells. Eventually silica replenished protoplasts use the bundles of costal strips to assemble loricae for themselves. In early exponential phase cultures naked protoplasts are capable of division whilst at the same time depositing costal strips in preparation for subsequent lorica assembly. An undamaged protoplast deprived of its lorica by ultrasonic treatment also ultimately replaces the lost lorica. The manner in which the tectiform mode of costal strip accumulation and lorica assembly is modified to allow a cell to produce its own lorica is discussed.Abbrevations SDV silica deposition vesicle     

A new choanoflagellate species from Taiwan: morphological and molecular biological studies of Diplotheca elongata nov. spec. and D. costata

A new species of acanthoecid choanoflagellate isolated from brackish waters of the Danshui estuary in North Taiwan has a mineralized lorica that consists of two chambers with a total length of 19-36microm. It shares with Diplotheca costata the features of a posterior lorica chamber formed from broad and flattened costal strips and an anterior chamber with spatula-shaped costal strips. The new species has therefore been placed in the same genus and named Diplotheca elongata. A phylogenetic analysis of partial SSU rDNA sequences from Diplotheca costata and D. elongata supports this taxonomic affiliation. This is a large and distinctive choanoflagellate which has not been reported in any previous study, suggesting that it may be an endemic species of restricted distribution.     

Choanoflagellates (Sarcomastigophora, Protozoa) from the Coastal Waters of Taiwan and Japan. I. Three New Species

Three new acanthoecidaean species collected from the coastal waters of Taiwan and Japan are described: Acanthocorbis camarensis n. sp. resembles Acanthocorbis unguiculata in lorica morphology, but differs in having regularly arranged longitudinal and transverse costae at the anterior lorica chamber, and in lacking a nail at the apical end of anterior spine; Diaphanoeca spiralifurca n. sp. is characterized by the spiral arrangement of the costal strips in the posterior half of the lorica chamber and is closely related to Diaphanoeca grandis; Stephanoeca supracostata n. sp. is closely related to Stephanoeca elegans, but differs in having an additional transverse costa at the anterior lorica chamber.     

Costal strip production and lorica assembly in the large tectiform choanoflagellate Diaphanoeca grandis Ellis

Diaphanoeca grandis posseses a voluminous flask-shaped lorica comprising an outer layer of 12 longitudinal costae and an inner layer of four transverse costae. The cell is suspended just above the centre of the lorica chamber by tentacles that are attached to the anterior transverse ring. The component costal strips are superficially similar although four different strip categories can be distinguished on the basis of length and morphology. Costal strips are produced ‘upside-down’ within the parent cell and accumulated in a close-packed horizontal ring at the top of the inner surface of the collar. The order in which costal strips are produced is consistent, starting with those for the transverse rings, basal to anterior, and then the longitudinal costae, again with the posterior first and the anterior later. Cell division is of the classical tectiform variety with the juvenile cell being inverted and pushed backwards out of the parent lorica. Lorica assembly entails firstly the rotation of the anterior vertical strips so they become horizontal and then their movement backwards under the posterior layer of longitudinal strips. From this time onwards, lorica assembly proceeds in a standard manner with the lorica-assembling tentacles providing a forward and left-handed rotational movement.     

Boreal Tintinnid Assemblage in the Northwest Pacific and Its Connection with the Japan Sea in Summer 2014

Tintinnids are planktonic ciliates that play an important role in marine ecosystem. According to their distribution in the world oceans, tintinnid genera were divided into several biogeographical types such as boreal, warm water, austral and neritic. Therefore, the oceanic tintinnid assemblage could be correspondingly divided into boreal assemblage, warm water assemblage and austral assemblage. The purpose of this study was to investigate the characteristics of boreal tintinnid assemblage in the Northwest Pacific and the Arctic, and to identify the connection between boreal tintinnid assemblage and neighboring assemblages. Surface water samples were collected along a transect from the East China Sea to the Chukchi Sea in summer 2014. According to the presence of boreal genera and warm water genera, three tintinnid assemblages (the East China Sea neritic assemblage, the Japan Sea warm water assemblage, and the boreal assemblage) were identified along the transect. The boreal assemblage extended from the Chukchi Sea to the waters north of the Sōya Strait. Densities peaks occurred at stations in the two branches of the Alaska Current and decreased both northward and southward. The densities were <10 ind./dm³ at most stations in Arctic region. The dominant genera (Acanthostomella, Codonellopsis, Parafavella, and Ptychocylis) accounted for 79.07±29.67% (n = 49) of the abundance in the boreal assemblage. The densities of the dominant genera covaried with strongly significant positive correlations. Tintinnids with lorica oral diameter of 22–26 μm and 38–42 μm were dominant and contributed 67.35% and 15.13%, respectively, to the total abundance in the boreal assemblage. The distribution and densities of tintinnids in the study area suggest that the Sōya Strait might be a geographical barrier for tintinnids expansion.     

LIFE HISTORY AND TAXONOMY OF RHIZOOCHROMONAS ENDOLORICATA GEN. ET SP. NOV., A NEW FRESHWATER CHRYSOPHYTE INHABITING DINOBRYON LORICAE1

The life cycle of a previously undescribed chrysophyte, assigned to the new genus Rhizoochromonas, is described. It includes a small motile stage with heterokont flagellation which invades a Dinobryon lorica. Reproduction by cell division of the nearly spherical rhizopodial vegetative stage frequently leads to expulsion of the host protoplast through overcrowding of the lorica. Endogenous cysts (stomatocysts) are also formed within the Dinobryon lorica. The new family, Brehmiellaceae, is established to accommodate pseudopodial/rhizopodial chrysophytes with heterokont flagellation in the motile stage. Rhizoochromonas endoloricata gen. et sp. nov. has been found at two widely separated softwater locations in Ontario, and at one it constituted a major component of the planktonic flora during the autumns of six successive years.     

Developmental and ultrastructural observations on two stalked marine choanoflagellates, Acanthoecopsis spiculifera Norris and Acanthoeca spectabilis Ellis.

Acanthoecopsis spiculifera and Acanthoeca spectabilis are stalked, loricate choanoflagellates found in littoral sea water pools. The two taxa are distinguished from each other by the arrangement of costae forming the lorica chamber. In addition, Acanthoecopsis spiculifera usually has a longer stalk and may be colonial, consisting of two or more attached individuals. Division in Acanthoeca results in the production of a juvenile, flagellated, protoplast without a lorica. After separation, the juvenile protoplast swims away, settles down and produces an accumulation of costal strips. When sufficient strips have been produced the lorica is rapidly assembled.     

Revision of the Family Lagenophryidae Bütschli, 1889 and Description of the Family Usconophryidae N. Fam. (Ciliophora,Peritricha)1

Ten species of lagenophryid peritrichs in three genera are redescribed or described for the first time. Based on this information, the family Lagenophryidae was found to consist of five genera: Lagenophrys, Paralagenophrys, Clistolagenophrys n. g., Setonophrys, and Operculigera. Lagenophryid genera differ in gross structure of the lorica aperture and the peristomial sphincter associated with it. Shape of the lorica and mode of attachment to the host are not generic characteristics in the Lagenophryidae. Differences in shape evolved within each of the three largest lagenophryid genera merely as adaptations for attachment to different parts of a host. Usconophrys, formerly in the Lagenophryidae, and Cyclodonta are assigned to the family Usconophryidae n. fam., which is characterized by possession of a lorica, lack of a closure apparatus operated by the peristomial sphincter, and possession of an operculariform peristome. Lagenophrys, Setonophrys, and Paralagenophrys appear to have evolved separately and convergently from ancestors within Operculigera. Lagenophryid lorica apertures consisting of opposing lips probably evolved as tight seals to prevent water loss when the host is temporarily out of water. The greater diversity and wider distribution of Lagenophrys compared with other lagenophryid genera may result from an advantage in recolonizing hosts conferred by second-type division.     

Life Cycle and Morphology of a Cambrian Stem-Lineage Loriciferan

Cycloneuralians form a rich and diverse element within Cambrian assemblages of exceptionally preserved fossils. Most resemble priapulid worms whereas other Cycloneuralia (Nematoda, Nematomorpha, Kinorhyncha, Loricifera), well known at the present day, have little or no fossil record. First reports of Sirilorica Peel, 2010 from the lower Cambrian Sirius Passet fauna of North Greenland described a tubular lorica covering the abdomen and part of a well developed introvert with a circlet of 6 grasping denticles near the lorica. The introvert is now known to terminate in a narrow mouth tube, while a conical anal field is also developed. Broad muscular bands between the plates in the lorica indicate that it was capable of movement by rhythmic expansion and contraction of the lorica. Sirilorica is regarded as a macrobenthic member of the stem-lineage of the miniaturised, interstitial, present day Loricifera. Like loriciferans, Sirilorica is now known to have grown by moulting. Evidence of the life cycle of Sirilorica is described, including a large post-larval stage and probably an initial larva similar to that of the middle Cambrian fossil Orstenoloricusshergoldii .     

New Species of Lagenophrys (Ciliophora,Peritrichia) from New Zealand and Australia1

Lagenophrys novazealandae n. sp. occurs on the gills of Paranephrops zealandicus, a parastacid crayfish from New Zealand. The new species has the hemispheroidal lorica most common among members of its genus and is distinguished by its possession of large tubercles on the thickened edge of the anterior lip of the lorica aperture, a deep cleft in the left side of the lip's edge, and a ovoid to reniform macronucleus located in the right-hand part of the body. It is probable that an as yet unnamed species of Lagenophrys known to occur on another species of Paranephrops in New Zealand is distinct from L. novazealandae but phylogenetically related to it. Lagenophrys petila n. sp. occurs on setae of Parastacoides tasmanicus, a parastacid from Tasmania. The new species has an ovoid lorica tapering to a slender pseudostalk at the posterior end, a type of lorica possessed by only two other members of its genus that also attach to their host's setae. It is distinguished from the other ovoid species by the proportions of the lorica, the extreme shortness of the lips of the lorica aperture, and an ovoid macronucleus located in the right, anterior part of the body. Clefts in the lips of L. novazealandae and other members of Lagenophrys may function as points of flexure to allow the lips to bend in ways that accommodate interspecific differences in the size of the epistomial disk and its operation during suspension feeding.