MORPHOGENESIS OF THE LABIATE PROCESS IN THE ARAPHID PENNATE DIATOM DIATOM A VULGARE1

Each valve of the araphid pennate diatom Diatoma has a labiate process (LP) at one end; in a frustule, the LPs are at diagonally opposite ends. After mitosis is over, an elongated dense body detaches from the spindle pole and migrates to one end of the daughter cell, always diagonally opposite the LP of the parental valve. This dense body trails a cone-shaped array of microtubules (MTs). Meanwhile, the new valve has begun to form within the Silica Deposition Vesicle (SDV). Having reached the end of the cell, this dense body moves back slightly and then settles onto the SDV, developing a layered substructure as it does so. Immediately beneath it, the LP of the new daughter valve differentiates. This dense object is clearly the homologue of the fibrous Labiate Process Apparatus (LPA) involved in the differentiation of the LP in several centric diatoms. In a few cases, these LPAs also hair been shown to originate from some component of the spindle pole. Thus, the homologue of the LPA of centric diatoms has now been found in an araphid pennate diatom; in each case, the LPA apparently comes from the pole of the spindle and presumably uses a cytoskeleton of MTs to locate the LP in its correct position. These observations support the possibility that the raphe evolved from the LP.     

VALVE MORPHOGENESIS IN THE PENNATE DIATOM ACHNANTHES COARCTATA

Mitosis and valve morphogenesis in the pennate diatom Achnanthes coarctata (Bréb. in W. Sm.) Grun. are described. After cytokinesis, both daughter nuclei and their microtubule centers (MCs) are found near one side of the cell. Each new tubular silica deposition vesicle (SDV) arises centrally, forming a single rib running the length of the cell. Each MC then migrates around its nucleus and positions itself directly adjacent to the new SDV. The enlarging silicalemmas with their associated MCs, nuclei, microtubules (MTs) and microfilaments (MFs) appear in mirror image in the daughter cells. Both SDVs soon generate a second longitudinal rib alongside the first; the gap between the ribs ultimately becomes the future raphe fissure. The MC, MTs and nucleus are associated with each fissure. However, the subsequent behavior of the valve secreting machinery now becomes quite different in the daughter cells. In the cell that will form a raphid valve, the silicalemma, flanked by MFs, expands laterally in both directions over the cleavage furrow. Within the expanding SDV, silica secretion continues, eventually generating the structure of the mature valve, and during this phase the raphe fissure becomes delineated as in other raphid diatoms. In the other daughter cell, however, the MC and its MTs withdraw from the silicalemma, and the SDV moves laterally across the cleavage furrow until the double rib is at the corner of the cell. As silica is secreted into this expanding SDV, the raphe fissure completely fills in. This valve, therefore, lacks a raphe when mature and has a symmetry quite different from that of the valve formed in the other daughter cell. These events are compared with the course of morphogenesis described for other raphid diatoms.     

SILICON DEPOSITION IN DIATOMS: CONTROL BY THE pH INSIDE THE SILICON DEPOSITION VESICLE

To test the hypothesis that silicification occurs under acid conditions in the silicon deposition vesicle (SDV), the acidity of the SDV of the pennate diatoms Navicula pelliculosa (Brébisson et Kützing) Hilse, N. salinarum (Grunow) Hustedt, and Nitzschia sigma (Kützing) Smith was determined during development of new frustule valves. Cells were incubated with the weak base 3-(2,4-dinitroanilino)-3′-amino-N-methylpropylamine (DAMP) followed by immunocytochemical localization in whole cells and on ultrathin sections. After resupplying silicate to cells synchronized by silicon depletion, the uptake of this nutrient from the medium was the same with or without DAMP; new valves developed without morphological aberrations that could conceivably have been caused by the probe. DAMP was found in cellular compartments known to be acidic, such as vacuoles active as lysosomes, the lumen of thylakoids, and microbodies. In the nucleus and mitochondria, which are circumneutral and basic compartments, the probe did not appear. Besides its presence in acidic compartments, DAMP was specifically accumulated within the SDV during formation of new valves; during the process of valve maturation, the SDV seemed to become increasingly acidic. In control experiments using the ionophores chloroquine, valinomycin, and nigericin, the compartmental location of DAMP was clearly disturbed, resulting in a random intracellular distribution. Accumulation of the fluorescent probe rhodamine 123, which can be translocated over membranes by a reducing potential, confirmed that the SDV can translocate weak bases. The results with DAMP suggest that the pH of the SDV is important in the silicification of diatoms: It facilitates a fast nucleation and aggregation of silica particles, thus increasing the rate of formation of the mature frustules. In addition, the acidic environment might protect the newly formed valves against dissolution before completion and coverage by the organic casing prior to their secretion.     

The effect of drugs on diatom valve morphogenesis

Summary The effects of various drugs on cell wall (valve) morphogenesis was investigated in three species of diatoms (Pinnularia spp., Surirella robusta, andHantzschia amphioxys) using light microscopy (LM) and scanning electron microscopy (SEM). Treatment ofSurirella with the microtubule (MT) disrupting agent colchicine during early valve formation results in a characteristic malformation of the valve, whereby part of the normally circumferential raphe canal forms as an abnormal protruding lip on the valve surface, located up to 20 m from the edge of the valve. The position of this malformed lip coincides with the location of a microtubule center (MC) at the time of colchicine addition, suggesting that the MC may play a direct role in positioning the tip of the raphe canal during valve formation. The migration of this MC to the tip of the cell during early valve morphogenesis is reversibly inhibited by the metabolic inhibitor 2-4-dinitrophenol (DNP). The effect of colchicine onPinnularia valve formation is less severe, causing occasional malformation of the raphe, but little if any lateral displacement. InHantzschia, colchicine has no effect on the positioning of the raphe, but prolonged exposure causes fusion of the raphe canal with the valve face. Cochicine treatment also results in the absence of the normal curvature at the central interruption in the raphe, as well as abnormal pore formation in this central area. Addition of cytochalasin D during early valve formation inHantzschia causes the raphe canal to form in the center of the valve face, suggesting that the normal translocation of the raphe canal to the valve edge is actindependent. Comparison of valves from control and cytochalasintreatmentHantzschia suggest that the pore spacing within the valve is determined by the position relative to the raphe, and does not depend on whether to pores form on the side (mantle) or the face of the mature valve.Abbreviations DM diatom medium - DNP dinitrophenol - MT microtubule - MC microtubule center - PSS primary silicification site - SDV silica deposition vesicle     

Diversity of mineral cell coverings and their formation processes: a review focused on the siliceous cell coverings

Mineral cell coverings are found in various protists. Some macroalgae accumulate calcium carbonate in the intercellular space, and some unicellular organisms use calcium carbonate or silica for the construction of loricas, scales, and frustules. Diatoms are representatives of those utilizing silica for the material of the cell covering called a frustule. The development of the frustule is initiated in a silica-deposition vesicle (SDV), which occurs just beneath the plasma membrane and, subsequently, the silicified cell covering expands its area, following the expansion of the SDV from valve face to valve mantle. Sequential valve development with whole valves is reviewed in several diatoms placed in different phylogenetic positions. Every diatom commences its valve formation from its pattern center and then develops by means of individual procedures. The results indicate that the valve development reflects the phylogeny of diatoms. In addition, recent progress in silica biomineralization is briefly reviewed, and the phylogeny of ability concerning siliceous cell covering formation is inferred. Electronic Publication     

Characterizing the silica deposition vesicle of diatoms

Summary The present study on a centric diatom,Ditylum brightwellii, includes two parts: detection of sugars in the silica deposition vesicle (SDV) with lectins and labeling the developing siliceous cell wall in the SDV with rhodamine 123. Cells with developing valves are treated with SDS to remove all the cytoplasmic contents, then either stained with fluorescein labeled lectins or thin-sectioned and stained with colloidal gold labeled lectins. The results show that mannose is part of the organic matrix in the SDV. Rhodamine 123, a non-toxic fluorescent laser dye, enters the cell immediately and is trapped in the SDV probably by the high reducing potential of the SDV. Silica is co-deposited with rhodamine 123 in the SDV, and the resulting valves and girdle bands become fluorescent. Implications of this study for the mechanism of silicification are discussed.Abbreviation SDV Silica deposition vesicle     

MICROMORPHOGENESIS DURING DIATOM WALL FORMATION PRODUCES SILICEOUS NANOSTRUCTURES WITH DIFFERENT PROPERTIES1

Micromorphogenesis within the silica deposition vesicle (SDV) of the diatom Pinnularia viridis (Nitzsh) Ehrenb. resulted in distinct silica nanostructures and layers within forming valves and girdle bands. These siliceous components were similarly disclosed following alkaline etching of mature valves/girdle bands, where their different susceptibilities to dissolution over time resulted from apparent differences in silica density and/or chemistry. The bulk of silica appeared to be deposited at the interface of the forming valve or girdle band with the silicalemma and occurred by the outward expansion of microfibrils of silica that aligned perpendicularly to the silicalemma. Microfibrils originated from both sides of the “silica lamella,” the first nanostructure formed within the SDV, and several silica species of distinct nanostructure and density resulted, including distinctive inner and outermost silica “coverings” of mature valves/girdle bands and the central and terminal nodules. Not all silica deposition and micromorphogenesis occurred in contact with the expanding silicalemma, but was somehow directed within the SDV cavity, and resulted in the distinct silica layers that lined the raphe fissures and poroids. Following alkaline etching, the inner surfaces of valves/girdle bands, as well as the silica layers lining the raphes, poroids, and slits, were determined to be significantly more resistant to alkaline etching than the exterior surfaces, while the outer silica coating and the nodules were quickly dissolved. The processes of micromorphogenesis must have exerted precise control over the chemical nature of the silica formed at different positions within the SDV and affected the overall structure and function of the diatom wall.     

VALVE MORPHOGENESIS IN THE CENTRIC DIATOM PROBOSCIA ALATA SUNDSTROM1

Valve morphogenesis in Proboscia alata Sundstrom was followed in living cells and during treatment with antiactin and antimicrotubule drugs. Once cleaved, sibling cells rounded up and retracted. Soon, a granular organizing center (OC) appeared adjacent to the stub of the initiated valve. Silicification started within a silicon deposition vesicle (SDV) adjacent to the OC. The elongating valve was initially tubular and sealed at one end, creating the proboscis of the conical valve. The edge of the SDV and thinnest region of the forming valve was lined by a sleeve of bundled microtubules (MTs) that terminated short of the older more rigid part of the valve. The growing proboscis of living cells treated with the anti‐MT drug oryzalin became grossly distorted. EM revealed dense material lining the growing edge of the SDV; immunofluorescence microscopy showed a ring of actin here. Applied to living cells, the antiactin drug cytochalasin D caused the very young proboscis to collapse; in older valves, the base of the proboscis expanded. Thus, valve morphogenesis appeared controlled by the MT cytoskeleton, keeping the proboscis straight while actin molded its conical outline. At the tip of the proboscis was a slit resembling a labiate process. Its morphogenesis involved striated fibers and two MTs, reminiscent of the fibers and MTs associated with raphe morphogenesis. In contrast to spine‐like processes that elongate by tip growth, the tip of the proboscis was formed first, and the consequent “antitip growth” suggests the tip was originally the center of the valve face.     

Valve morphogenesis in Diploneis smithii (Bacillariophyta)

Diploneis species have perhaps the most complex valve structure among pennate diatoms. The development of this structure was studied in Diploneis smithii and begins with the formation of a primary band, which then develops secondary arms at both poles and the center, as in the classic Chiappino–Volcani model of raphid diatom ontogeny. Spine‐like projections grow out from the primary band and secondary arms to establish the transapical ribs (virgae) of the mature valve and themselves develop spines, which are spaced first oppositely and then alternately and fuse with each other to delimit the stria pores. Subsequently, new pattern and structures develop both externally (formation of bifurcating projections that fuse to delimit the outer, sieve‐like layer of the valve) and internally (growth and fusion of flanges from the first‐formed ribs to create the longitudinal canals and deposition of a hymenate strip over the internal face of each stria). Comparisons are made with morphogenesis in other diatoms. Diploneis smithii ontogeny suggests how very slight developmental changes might have created the very variable external morphology of Diploneis species. It also indicates that the longitudinal canals of Diploneis and Fallacia have different origins, since the porous external wall is not formed as a unilaterally attached flap in Diploneis and the canal is internal to the first‐formed rib–stria system in Diploneis, but external to it in Fallacia.     

Extensive and intimate association of the cytoskeleton with forming silica in diatoms: control over patterning on the meso- and micro-scale

BACKGROUND: The diatom cell wall, called the frustule, is predominantly made out of silica, in many cases with highly ordered nano- and micro-scale features. Frustules are built intracellularly inside a special compartment, the silica deposition vesicle, or SDV. Molecules such as proteins (silaffins and silacidins) and long chain polyamines have been isolated from the silica and shown to be involved in the control of the silica polymerization. However, we are still unable to explain or reproduce in vitro the complexity of structures formed by diatoms. METHODS/PRINCIPAL FINDING: In this study, using fluorescence microscopy, scanning electron microscopy, and atomic force microscopy, we were able to compare and correlate microtubules and microfilaments with silica structure formed in diversely structured diatom species. The high degree of correlation between silica structure and actin indicates that actin is a major element in the control of the silica morphogenesis at the meso and microscale. Microtubules appear to be involved in the spatial positioning on the mesoscale and strengthening of the SDV. CONCLUSIONS/SIGNIFICANCE: These results reveal the importance of top down control over positioning of and within the SDV during diatom wall formation and open a new perspective for the study of the mechanism of frustule patterning as well as for the understanding of the control of membrane dynamics by the cytoskeleton.     

VALVE MORPHOGENESIS IN SURIRELLA (BACILLARIOPHYCEAE)1

Valve morphogenesis in two Surirellae (S. ovalis Brebisson and S. robusta Ehrenberg) is described. Mitosis takes place at the broad end of the cell. After cleavage, a new Microtubule Center (MC) arises near each spindle pole and moves to the adjacent plasmalemma. Soon, a specific group of microtubules (MTs) extends from very near the MC around the periphery of the cell. Concurrently, the new tubular Silica Deposition Vesicle (SDV) grows around the periphery of the cell close to these MTs. A double rib of silica is rapidly formed inside the SDV; the space between the ribs becomes the raphe. Mitochondria line up along the MTs, and the SDV may be molded around these to create the canal raphe. Soon, the SDV expands in two directions to create the face and the mantle of the new valve. Meanwhile, each daughter nucleus, accompanied by the MC, moves to its interphase position at the center of the cell; this movement is colchicine-sensitive. As in several other pennate diatoms, an interruption in the raphe of the mature valve coincides with the initial position of the MC. The canal raphe thickens rapidly around the mitochondria; a rudimentary raphe fiber may be associated with the creation of a tiny curvature at the inner raphe fissure. As the SDV expands in the large S. robusta, the daughter cell protoplasts slowly shrink by plasmolysis, thereby creating the complex curved surface of the new valve surmounted by the arching canal raphes which are now quite rigid. In S. ovalis, the daughter cell protoplasts remain appressed and therefore the new valve surface is basically flat. The symmetry of Surirella is quite different from that of other pennate diatoms. However, the cytoplasmic events accompanying valve morphogenesis are similar in all important respects to those described in other raphid pennate diatoms, and clearly supports a naviculoid origin for this genus.     

DIATOMS (BACILLARIOPHYTA) OF ISOLATED ISLANDS: NEW TAXA IN THE GENUS NAVICULA SENSU STRICTO FROM THE GALáPAGOS ISLANDS1

The diatoms (Bacillariophyta) from a coastal lagoon from the Diablas wetlands (Isla Isabela, the Galápagos Islands) were studied in material from surface samples and a sediment core spanning the past 2,700 years in order to examine evidence of diatom evolution under geographic isolation. The total number of taxa found was ～100. Ultrastructural variation in valve morphology between members of Galápagos taxa was used to describe 10 species from the genus Navicula sensu stricto, which are new to science. Four taxa: N. isabelensis, N. isabelensoides, N. isabelensiformis, and N. isabelensiminor, shared several key characteristics that may be indicative of a common evolutionary heritage; these species therefore provide possible evidence for the in situ evolution of diatoms in the Galápagos coastal lagoons. Shared morphological characteristics include: (i) stria patterning in the central area, (ii) an elevated and thickened external raphe‐sternum, (iii) external central raphe endings that are slightly deflected toward the valve primary side, and (iv) an arched valve surface. To explain these findings, two models were proposed. The first suggested limited lateral diatomaceous transport of Navicula species between the Galápagos and continental South America. Alternatively, these new species may be ecological specialists arising from the unique environmental conditions of the Galápagos coastal lagoons, which restrict the colonization of common diatom taxa and enable the establishment of novel, rare species. The Diablas wetlands are an important site for diatom research, where local‐scale environmental changes have combined with global‐scale biogeographic processes resulting in unique diatom assemblages.     

Cell division and morphogenesis of the labiate process in the centric diatomDitylum brightwellii

Summary Cells of the centric diatomDitylum brightwellii were filmed undergoing cell division and valve secretion, and were fixed for transmission electron microscopy. Attention was directed particularly at the origin of the Labiate Process Apparatus (LPA).As reported previously (li andVolcani 1985 a), the nucleus, centrally situated during interphase, moves laterally to undergo mitosis against the girdle bands. We describe the spindle which splits up into numerous fibres of overlapped polar microtubules (MTs) by metaphase. The chromosomes are diffuse and the spindle elongates rapidly during anaphase. A complex of organelles is found at the poles and ill-defined, dense material extends to the nearby plasmalemma from prophase on. The two Silica Deposition Vesicles (SDVs) are initiated during anaphase close to the poles and by midcleavage, the dense LPA arises on each SDV close to dense polar material. After cleavage, the daughter protoplasts round up and the SDV, already containing a nascent valve, expands over the cleavage furrow. The labiate process, a long straight hollow tube of silica, is rapidly (ca. 25 minutes) secreted from directly under the LPA; a fibrous plug (polysaccharide?) always appears in the SDV immediately adjacent to the LPA during the initiation of this secretion. The ill-defined Microtubule-Organizing Center (MC) from the spindle pole remains close to the LPA and in it can be seen the tiny presumptive primordial spindle on the nuclear envelope.The raphe and the labiate process (LP), both highly differentiated apertures in the valve, probably function in a specialized form of the mucilage secretion involved in generation of movement in raphid diatoms, and in a simple form of movement in some centrics. Morphogenesis of the LP is associated with the LPA while differentiation of the raphe is almost associated with the MC; both MC and LPA have an intimate ontological relationship with the spindle pole and the postmitotic cytoskeletal system of MTs. This association also is seen in the formation of the LP in an araphid pennate,Diatoma (work in progress). Therefore, from functional, morphogenetic and ontogenetic observations, we support the proposal that the raphe of pennate diatoms arose from the LP of centric diatoms.     

APPLICATION OF THE PDMPO TECHNIQUE IN STUDYING SILICA DEPOSITION IN NATURAL POPULATIONS OF FRAGILARIA CROTONENSIS (BACILLARIOPHYCEAE) AT DIFFERENT DEPTHS IN A EUTROPHIC RESERVOIR1

At weekly intervals from July to October 2006, we measured silica deposition in the summer diatom assemblage at various depths in the eutrophic ?ímov Reservoir (Czech Republic) using PDMPO, the 2‐(4‐pyridyl)‐5{[4‐(2‐dimethylaminoethyl‐aminocarbamoyl)‐methoxy]phenyl}oxazole labeling technique. Fluorescence microscopy coupled with image analysis allows quantifying silicon (Si) deposition over time and a simple distinction between cells that are actively depositing Si and those that are not. Diatom assemblage was exclusively dominated by Fragilaria crotonensis Kitton, which formed pronounced subsurface maxima (2–6.5 m). Concentrations of the main nutrients (Si and phosphorus, P) were low over the whole season; however, at depth, the nutrient availability was higher than at the surface. Fragilaria silica deposition rates were eight times higher at the surface than at depth. Half the population was involved in silica deposition at the surface, while only 20% active cells were doing so at depth. At the surface, silica deposition was limited by P deficiency; the effect of dissolved Si (DSi) was not statistically significant. Silica deposition at depth was significantly constrained by low light availability despite the 1% average light attenuation at depth, which is supposed sufficient for photosynthesis. This study represents the first attempt to employ the PDMPO technique coupled with quantitative image analysis of PDMPO fluorescence in freshwater ecology. On the basis of our results, PDMPO probe appears to be an appropriate proxy for the study of resource limitation in natural diatom populations.     

Xenococconeis opunohusiensis gen. et sp. nov. and Xenococconeis neocaledonica comb. nov. (Bacillariophyta) from the tropical South Pacific

During a survey of the coral reef diatoms of Moorea Island (Society Archipelago, South Pacific) a small‐sized member of the order Achnanthales was studied using a light microscope (LM) and a scanning electron microscope (SEM). This marine taxon has: a raphe valve (RV) with a non‐crenulate edge; a high cingulum; a sternum valve (SV) often irregularly striated and areolae with concave hymenate pore occlusion; a thick and plain SV valvocopula (SVVC), ring‐shaped, composed of large fused fimbriae, with a central elliptic foramen bordered by the peg‐like edge of the fimbriae. On abvalvar side, the SVVC bears radiate concave and robust transapical ribs, interlinking with short elevated transverse ribs of the RV valvocopula (RVVC). Large marginal fenestrae of the RVVC give access to pseudoloculi. One oblong, unique and striated papilla is located on each RVVC rib. Given this unique set of features, we describe Xenococconeis opunohusiensis gen. et sp. nov. as a new taxon belonging to the Achnanthales. The characteristics of the new taxon are compared with Campyloneis Grunow and Cocconeis Ehrenberg. From New Caledonia, Cocconeis neocaledonica Maillard ex Lange‐Bertalot et Steindorf, a freshwater diatom, was described with two internal septa with marginal pseudoloculi. Based on subsequent SEM illustrations and remarks, we propose the transfer of C. neocaledonica to the new genus, and compare it to the type species, Xenococconeis opunohusiensis.     

Kulikovskiyia gen. nov. (Bacillariophyceae) from the lateritic rock pools of the Western Ghats,India and from Hainan Province,China

A new triundulate naviculoid diatom genus is described from the Western Ghats of Peninsular India and Hainan Province, China. The new taxon, Kulikovskiyia gen. nov. has robust conical spines along its margin and at the apices and the external valve face has longitudinally‐oriented siliceous slat system extending the length of the valve. The external distal raphe ends bifurcate and terminates on the valve face. There appear to be superficial similarities between this Asian genus and species and Playaensis, a genus comprised of two species found only in the western USA. The systematic position of Kulikovskiyia is discussed, and other than noting its similarities to other biraphid naviculoid diatoms due to symmetry features and the position of the raphe, we are uncertain about its systematic placement at finer levels of classification.     

Site‐specific inhibition of integrin αvβ3‐vitronectin association by a ser‐asp‐val sequence through an Arg‐Gly‐Asp‐binding site of the integrin

A functional proteomic technology using protein chip and molecular simulation was used to demonstrate a novel biomolecular interaction between P11, a peptide containing the Ser‐Asp‐Val (SDV) sequence and integrin αvβ3. P11 (HSDVHK) is a novel antagonistic peptide of integrin αvβ3 screened from hexapeptide library through protein chip system. An in silico docking study and competitive protein chip assay revealed that the SDV sequence of P11 is able to create a stable inhibitory complex onto the vitronectin‐binding site of integrin αvβ3. The Arg‐Gly‐Asp (RGD)‐binding site recognition by P11 was site specific because the P11 was inactive for the complex formation of a denatured form of integrin–vitronectin. P11 showed a strong antagonism against αvβ3‐GRGDSP interaction with an IC₅₀ value of 25.72±3.34 nM, whereas the value of GRGDSP peptide was 1968.73±444.32 nM. The binding‐free energies calculated from the docking simulations for each P11 and RGD peptide were ?3.99 and ?3.10 kcal/mol, respectively. The free energy difference between P11 and RGD corresponds to approximately a 4.5‐fold lower K_i value for the P11 than the RGD peptide. The binding orientation of the docked P11 was similar to the crystal structure of the RGD in αvβ3. The analyzed docked poses suggest that a divalent metal–ion coordination was a common driving force for the formation of both SDV/αvβ3 and RGD/αvβ3 complexes. This is the first report on the specific recognition of the RGD‐binding site of αvβ3 by a non‐RGD containing peptide using a computer‐assisted proteomic approach.     

一种硅藻中国新记录属种——科氏杜氏藻

科氏杜氏藻是一种泥生或附沙生硅藻。该文对最近刚确立的一个硅藻属——杜氏藻属进行了介绍,利用光学和扫描电子显微镜对2019年4月20日采自东洞庭湖国家级自然保护区的科氏杜氏藻标本进行了观察研究。结果表明该标本具有以下主要形态特征:(1)壳面椭圆披针形。(2)中央区为蝴蝶结形,没有延伸至壳缘。(3)线纹在壳面大部分区域呈辐射状排列,在两端近平行排列,中部线纹密度20~22条/10μm。(4)孔纹圆形或近圆形,在内壳面被圆顶状的孔膜覆盖。(5)在壳面两端存在假隔片。该文调查采集的科氏杜氏藻种群的形态特征与模式种群相吻合,该属在中国是首次报道,为中国新记录属。     

PHYLOGENETIC POSITION OF TOXARIUM,A PENNATE‐LIKE LINEAGE WITHIN CENTRIC DIATOMS (BACILLARIOPHYCEAE)1

The diatom genus Toxarium Bailey has been treated as a pennate because of its elongate shape and benthic lifestyle (it grows attached to solid substrata in the marine sublittoral). Yet its valve face lacks all structures that would ally it with the pennates, such as apical labiate processes, a midrib (sternum) subtending secondary ribs and rows of pores extending perpendicularly out from the midrib, or a raphe system. Instead, pores are scattered irregularly over the valve face and only form two distinct rows along the perimeter of the valve face. In our nuclear small subunit rDNA phylogenies, Toxarium groups with bi‐ and multipolar centrics, as sister to Lampriscus A. Schmidt. Thus, the genus acquired a pennate‐like shape and lifestyle independently from that of the true pennates. The two species known, T. hennedyanum Grunow and T. undulatum Bailey, differ only in a single feature: the valve perimeter of the former shows only a central expansion, whereas that of the latter possesses in addition a regular undulation. Yet both forms were observed in our monoclonal cultures, indicating that the two taxa represent extremes in a plasticity range. Toxarium resembles another elongate and supposedly araphid diatom, Ardissonea De Notaris, in being motile. Cells can move at speeds of up to 4 μm·s ^{? 1} 1 Received 7 June 2002. Accepted 4 October 2002. through secretion of mucilage from the cell poles or they remain stationary for longer periods, when they form short polysaccharide stalks. Division during longer periods of quiescence leads to the formation of small colonies of linked or radiating cells.     

Description of Conticribra tricircularis,a new genus and species of Thalassiosirales,with a discussion on its relationship to other continuous cribra species of Thalassiosira Cleve (Bacillariophyta) and its freshwater origin

A new diatom genus Conticribra is erected to accommodate C. tricircularis, described from a freshwater Pliocene deposit in Trout Creek, Oregon (USA). The genus accommodates species possessing: (i) loculate areolae with (semi-) continuous cribra; (ii) non-plicated valve face; (iii) rimoportula located on the valve mantle, replacing a fultoportula. Conticribra tricircularis has no valve face fultoportulae and can easily be distinguished by its marginal fultoportulae with four satellite pores arranged in three rings. Three species are transferred to the new genus from Thalassiosira sensu lato. Using evidence from the fossil record and recent molecular data, a hypothesis concerning the freshwater origin of Conticribra is discussed.