Evolutionary history of larval skeletal morphology in sea urchin Echinometridae (Echinoidea: Echinodermata) as deduced from mitochondrial DNA molecular phylogeny

The larval skeletons of sea urchins show considerable morphological diversity, even between closely related species, although the evolutionary history and functional significance of this diversity are poorly understood. To infer the evolutionary history of the skeletal morphology, we focused on echinometrid species for which the morphological variation in larval skeletons had been investigated qualitatively and quantitatively. We reconstructed the phylogenetic relationships among 14 echinometrid species based on mitochondrial ND1 and ND2 genes and mapped the morphological characters onto the resultant trees. The monophyly of each genus in the Echinometridae was well supported by our results, as was the close affinity between Colobocentrotus, Heterocentrotus, and Echinometra. The mapping of the morphological characters of the larval skeletons indicated that the length, direction, and density of spines on the postoral rods was well conserved in each group of Echinometridae and that the abundance of spines and the size and shape of the body skeleton changed relatively frequently and hence were less conserved. In Echinometrid species, morphological variation in relatively unconserved features tends to be associated with latitudinal distributions, rather than phylogenetic relationships, indicating that the morphological diversity of larval skeletons could have been caused by adaptation to the habitat environment. Some morphological differences, however, seem to be nonfunctional and generated by the constraints on larval skeletogenesis. Thus, echinometrid species can be a good model with which to study the evolutionary history from both ecological and developmental standpoints.     

Study of larval and adult skeletogenic cells in developing sea urchin larvae

The larval skeleton of sea urchin embryos is formed by primary mesenchyme cells (PMCs). Thereafter, the larvae start feeding and additional arms develop. An adult rudiment that contains spines, tube feet, tests, and other parts of the adult body is formed in the eight-armed larva. The cellular mechanism of the later skeletogenesis and the lineage of the adult skeletogenic cells are not known. In this study, the morphogenesis of larval and adult skeletons during larval development of the sea urchin Hemicentrotus pulcherrimus was investigated by immunostaining cells with PMC-specific monoclonal antibodies, which are useful markers of skeletogenic cells. All spicules and the associated cells in the later larvae were stained with the antibodies. We could observe the initiation of skeletal morphogenesis at each developmental stage and visualize the cellular basis of skeleton formation in whole-mount embryos that possessed an intact morphology. There were some similarities between PMCs and the later skeletogenic cells. Both had a rounded shape with some filopodia, and the antigen expression started just before overt spicule formation. In the later-stage embryos, cells with filopodia and faint antigen expression were observed migrating in the blastocoel or aggregating in the presumptive location of new skeletogenesis.     

Perspectives in coral reef hydrodynamics

Knowledge of skeletogenesis in scleractinian corals is central to reconstructing past ocean and climate histories, assessing and counteracting future climate and ocean acidification impacts upon coral reefs, and determining the taxonomy and evolutionary path of the Scleractinia. To better understand skeletogenesis and mineralogy in extant scleractinian corals, we have investigated the nature of the initial calcium carbonate skeleton deposited by newly settling coral recruits. Settling Acropora millepora larvae were sampled daily for 10 days from initial attachment, and the carbonate mineralogy of their newly deposited skeletons was investigated. Bulk analyses using Raman and infrared spectroscopic methods revealed that the skeletons were predominantly comprised of aragonite, with no evidence of calcite or an amorphous precursor phase, although presence of the latter cannot be discounted. Sensitive selected area electron diffraction analyses of sub-micron areas of skeletal regions further consolidated these data. These findings help to address the uncertainty surrounding reported differences in carbonate mineralogy between larval and adult extant coral skeletons by indicating that skeletons of new coral recruits share the same aragonitic mineralogy as those of their mature counterparts. In this respect, we can expect that skeletogenesis in both larval and mature growth stages of scleractinian corals will be similarly affected by ocean acidification and predicted environmental changes.     

Early Tithonian Saturnalidae (Radiolaria) from the Solnhofen area (Southern Franconian Alb, southern Germany)

In order to complete the study of the very rich early Tithonian (Hybonoticeras hybonotum Zone) radiolarian fauna from the Mühlheim Member of the Mörnsheim Formation outcropping in the Solnhofen area, the taxa of the family Saturnalidae are described. Although rather rare, the Saturnalidae of this member contain 14 species, ten of which are new. These species belong to four genera, one of which is new (Moebicircus n. gen.), and two subfamilies (Hexasaturnalinae and Saturnalinae). The taxonomy at generic level of these late Jurassic radiolarians is founded on the basis of the position of the blades along the ring and number and morphology of the spines. Type of spines (simple or forked) has either species level value or none, depending on species. Special attention was given to anomalies, which sometimes are rather frequent, since they can give Information of paleobiological and paleoecological Orders. Among them frequent cases of open ring and additional spines withDicerosaturnalis and Siamese twins skeletons withSpongosaturninus andDicerosaturnalis are to be noted. The authors hope that this new taxonomy will give a better image of the evolution and radiation of the Saturnalidae during the Tithonian.     

A general survey and some taxonomic implications of diterpenes in the Asteraceae

This paper provides a general survey of the occurrence of diterpenes in the Asteraceae. Data on 4351 botanical occurrences were obtained from the literature. These were grouped by skeleton for each genus. Then, the genera were grouped by subtribes, which, in turn, were gathered in tribes, followed by subfamilies. In spite of the low number of species containing diterpenes, it was possible to describe some structural features of these compounds, i.e. the skeletal types in various taxa and the positions in some skeletons that are always oxidized or never undergo oxidation in some genera. Thus, it was verified that: in the subfamily Cichorioideae, only a few of the studied species possess diterpenes, wherein kaurane is the most frequent diterpene skeleton. In the Asteroideae, the presence of diterpenes is much greater than that in the Cichorioideae and Carduoideae. At tribal taxonomic level, for example, the Astereae produce labdanes and clerodanes; Heliantheae and Eupatorieae produce kauranes and labdanes, respectively; and Calenduleae produce pimaranes. Some taxonomic implications are presented.  © 2005 The Linnean Society of London, Botanical Journal of the Linnean Society , 2005, 147 , 291–308.     

Unshelled abalone and corrupted urchins: development of marine calcifiers in a changing ocean

The most fragile skeletons produced by benthic marine calcifiers are those that larvae and juveniles make to support their bodies. Ocean warming, acidification, decreased carbonate saturation and their interactive effects are likely to impair skeletogenesis. Failure to produce skeleton in a changing ocean has negative implications for a diversity of marine species. We examined the interactive effects of warming and acidification on an abalone (Haliotis coccoradiata) and a sea urchin (Heliocidaris erythrogramma) reared from fertilization in temperature and pH/pCO(2) treatments in a climatically and regionally relevant setting. Exposure of ectodermal (abalone) and mesodermal (echinoid) calcifying systems to warming (+2°C to 4°C) and acidification (pH 7.6-7.8) resulted in unshelled larvae and abnormal juveniles. Haliotis development was most sensitive with no interaction between stressors. For Heliocidaris, the percentage of normal juveniles decreased in response to both stressors, although a +2°C warming diminished the negative effect of low pH. The number of spines produced decreased with increasing acidification/pCO(2), and the interactive effect between stressors indicated that a +2°C warming reduced the negative effects of low pH. At +4°C, the developmental thermal tolerance was breached. Our results show that projected near-future climate change will have deleterious effects on development with differences in vulnerability in the two species.     

Skeletal development in Hermesinum adriaticum Zacharias, a flagellate from the Salton Sea, California

Hermesinum adriaticum is a rarely reported unicellular biflagellated organism with a solid siliceous skeleton. Live specimens were not observed but many skeletons were found in sediments and, in small numbers, in cyanobacterial mats and the water column of the Salton Sea, a salt lake in California, U.S.A. Stages of the developing skeleton were studied with scanning electron microscopy, and the progression from small tetraxial daughter skeletons to complete asymmetrical adult skeletons is presented. Some variability in the adult skeletons is illustrated.     

The pre-cephalic development of the skeleton of Amphimelissa setosa (Actinopoda: Nassellarida)

The ontogeny of the skeleton of the nassellarian radiolarian Amphimelissa setosa begins with the formation of three radial bars of silica; these correspond to the medial bar and spines L₁ and L₂ in the adult. By a precise sequence of the addition of various siliceous arcs and spines, this basic structure develops into the eucephalus. A new growth mechanism, in which existing skeletal elements serve as templates for the formation of new skeletal members, is hypothesized to explain the observed developmental patterns. The early ontogeny of nassellarian skeletons can be used to determine which skeletal features develop earliest. Among the structural characteristics used by radiolarian systematists, these conservative features are most suitable for use in interpretation of the taxonomic relationships and phylogeny of the group.     

Structures of bacterial flagellar motors from two FliF-FliG gene fusion mutants

Flagella purified from Salmonella enterica serovar Typhimurium contain FliG, FliM, and FliN, cytoplasmic proteins that are important in torque generation and switching, and FliF, a transmembrane structural protein. The motor portion of the flagellum (the basal body complex) has a cytoplasmic C ring and a transmembrane M ring. Incubation of purified basal bodies at pH 4.5 removed FliM and FliN but not FliG or FliF. These basal bodies lacked C rings but had intact M rings, suggesting that FliM and FliN are part of the C ring but not a detectable part of the M ring. Incubation of basal bodies at pH 2.5 removed FliG, FliM, and FliN but not FliF. These basal bodies lacked the C ring, and the cytoplasmic face of the M ring was altered, suggesting that FliG makes up at least part of the cytoplasmic face of the M ring. Further insights into FliG were obtained from cells expressing a fusion protein of FliF and FliG. Flagella from these mutants still rotated but cells were not chemotactic. One mutant is a full-length fusion of FliF and FliG; the second mutant has a deletion lacking the last 56 residues of FliF and the first 94 residues of FliG. In the former, C rings appeared complete, but a portion of the M ring was shifted to higher radius. The C-ring-M-ring interaction appeared to be altered. In basal bodies with the fusion-deletion protein, the C ring was smaller in diameter, and one of its domains occupied space vacated by missing portions of FliF and FliG.     

Saponins, classification and occurrence in the plant kingdom

Saponins are a structurally diverse class of compounds occurring in many plant species, which are characterized by a skeleton derived of the 30-carbon precursor oxidosqualene to which glycosyl residues are attached. Traditionally, they are subdivided into triterpenoid and steroid glycosides, or into triterpenoid, spirostanol, and furostanol saponins. In this study, the structures of saponins are reviewed and classified based on their carbon skeletons, the formation of which follows the main pathways for the biosynthesis of triterpenes and steroids. In this way, 11 main classes of saponins were distinguished: dammaranes, tirucallanes, lupanes, hopanes, oleananes, taraxasteranes, ursanes, cycloartanes, lanostanes, cucurbitanes, and steroids. The dammaranes, lupanes, hopanes, oleananes, ursanes, and steroids are further divided into 16 subclasses, because their carbon skeletons are subjected to fragmentation, homologation, and degradation reactions. With this systematic classification, the relationship between the type of skeleton and the plant origin was investigated. Up to five main classes of skeletons could exist within one plant order, but the distribution of skeletons in the plant kingdom did not seem to be order- or subclass-specific. The oleanane skeleton was the most common skeleton and is present in most orders of the plant kingdom. For oleanane type saponins, the kind of substituents (e.g. -OH, =O, monosaccharide residues, etc.) and their position of attachment to the skeleton were reviewed. Carbohydrate chains of 18 monosaccharide residues can be attached to the oleanane skeleton, most commonly at the C3 and/or C17 atom. The kind and positions of the substituents did not seem to be plant order-specific.     

Cell division of Giardia intestinalis: assembly and disassembly of the adhesive disc, and the cytokinesis

Trophozoites of Giardia are equipped with a special organelle of attachment, essential for parasite survival and pathogenicity, the ventral disc. Although its basic structure is well established, its reorganization and assembly during cell replication is poorly understood. We addressed some of these problems with aid of conventional, confocal and electron microscopy. We found that dividing Giardia alternates attached and free swimming phases in accordance with functional competence of the parent or newly assembled discs. The division started in attached cells by detachment of the disc microtubules from basal bodies. Shortening and eventual loss of the giardin microribbons, and unfolding of the microtubular layer resulting in collapse of the disc chamber and parasite detachment underlined gradual disassembly of the parent disc skeleton. Two daughter discs assembled on the dorsal side of the attached cell, with their ventral sides exposed on the parent cell surface and their microtubular skeletons growing in counter-clockwise direction. A depression between the assembling discs marked the cleavage plane. The splitting continued during the free-swimming phase with ventral-ventral axial symmetry in a plane of the daughter discs. Finally, the daughter cells with fully developed discs but still connected tail to tail by a cytoplasmic bridge, attached to a substrate and terminated the division by a process resembling adhesion-dependent cytokinesis. The mode of assembly of the daughter discs and plane of the division is compatible with maintenance of the left-right asymmetry of the Giardia cytoskeleton in progeny, which cannot be satisfactorily explained by alternative models proposed so far.     

The skeletal structure of Desmophyllum cristagalli: the use of deep-water corals in sclerochronology

Skeletal banding has been found in the deep-water scleractinian coral Desmophyllum cristagalli , an important animal in studies of climate change. This banding pattern sheds light on skeletogenesis and suggests methods by which the record of climate change contained within the coral skeletons may be interpreted. A central wall built of trabeculae forms the interior of the septa and rings the theca. Lamellae form a sheath over the trabecular frame, showing continuity from thecal edge to septum. Skeletal bands are added by the tissue layer, which overlaps and seals the internal coral and upper portion of the outer theca. Truncated inner bands on the outer theca indicate a pattern of skeletal deposition and dissolution dependent on the presence or absence of the live tissue layer. A long-term record will be difficult to collect from D. cristagalli since lamellae are less than 10 μm thick and band position is unpredictable. Density banding in shallow-water coral skeletons has long been recognized as a valuable paleo-oceanographic tool, and deep-water corals are now being used to reconstruct deep-ocean environments. Pattern of skeletal growth must be carefully considered if deep-water corals are to be used as proxy climate recorders.     

FINE STRUCTURE OF CELL DIVISION IN PYRAMIMONAS PARKEAE NORRIS AND PEARSON (CHLOROPHYTA,PRASINOPHYCEAE)1

Cell division in Pyramimonas parkeae is described and compared with some other green algae. The first indication of mitosis is division of the chloroplast, accompanied by growth of a prominent microbody, followed by replication of the 4 basal bodies. Also closely timed with this is the replication of the Golgi and other components of the basal body complex. Two basal body complexes separate, each taking a position at either pole of the nucleus which has migrated to a characteristic position just beneath the plasmalemma of a broadened and flattened flagellar pit. Cytokinesis is accomplished by the fusion of ducts and vesicles with the simultaneous release of scales to the newly formed exterior. Cells swim throughout division.     

Chemical composition of spines and tests of sea urchins

The skeleton of spines and tests of the species of sea urchins Strongylocentrotus intermedius, Mesocentrotus nudus, Scaphechinus mirabilis, and Echinocardium cordatum from the Sea of Japan is composed of a spongy stereom, consisting of calcite with a high content of magnesium. It was found that the tests and spines of the skeletons of sea urchins are composed of calcium–organic composite materials inlaid with other metals: Mg, Fe, Zn, and Rb. In the four species of sea urchins studied, the strength and other mechanical properties of the tests and spines differ and depend on the chemical composition and structural organization of their components. It was shown that the content of volatile substances correlates with their fragility or elasticity. It is revealed that the chemical composition of the tests of two species of the spherical sea urchins S. intermedius and M. nudus indicates significant differences between these two species of sea urchins.     

中国栅藻属植物数量分类初探

作者采用双向指示种分析法,对在中国分布的栅藻属植物进行了数量分类的初步研究。结果表明,52种栅藻属植物可分成5类。对该属的一些系统分类问题也进行了讨论。       

Cell morphology and life history of Dictyocha octonaria (Dictyochophyceae,Ochrophyta) from Wellington Harbour,New Zealand

Even though many aspects of Dictyocha fibula and D. speculum have long been studied, very little is known about D. octonaria. For the first time a clonal culture derived from a single cell of D. octonaria from Wellington Harbour was studied in detail. In the skeleton‐bearing stage three morphotypes were observed – skeleton bearing, mucocyst‐bearing and amoeboid, while in the naked stage only the naked form was studied. In this study the mucocyst‐bearing form was described as a new morphotype. Vegetative reproduction of the skeleton‐bearing form in the exponential growth phase was by both direct binary fission and by first forming a doublet and then two separate daughter cells, while that of naked form was by simple binary fission. Occasionally double skeletons were observed as end products of both the vegetative and sexual reproductions. In sexual reproduction all three forms in the skeleton‐bearing stage exhibited the same polymorphic life history involving a multinucleate stage. The newly formed daughter cells of all three forms developed individual siliceous skeletons prior to being released from the parent cell. The naked form in the naked stage, however, exhibited a separate polymorphic life history that produced only skeleton‐free daughter cells. For the first time both vegetative and sexual reproduction of D. octonaria were documented.     

The timing and manner of disassembly of the apparatuses for chloroplast and mitochondrial division in the red alga Cyanidioschyzon merolae

The timing and manner of disassembly of the apparatuses for chloroplast division (the plastid-dividing ring; PD ring) and mitochondrial division (the mitochondrion-dividing ring; MD ring) were investigated in the red alga Cyanidioschyzon merolae De Luca, Taddei and Varano. To do this, we synchronized cells both at the final stage of and just after chloroplast and mitochondrial division, and observed the rings in three dimensions by transmission electron microscopy. The inner (beneath the stromal face of the inner envelope) and middle (in the inter-membrane space) PD rings disassembled completely, and disappeared just before completion of chloroplast division. In contrast, the outer PD and MD rings (on the cytoplasmic face of the outer envelope) remained in the cytosol between daughter organelles after chloroplast and mitochondrial division. The outer rings started to disassemble and disappear from their surface just after organelle division, initially clinging to the outer envelopes at both edges before detaching. The results suggest that the two rings inside the chloroplast disappear just before division, and that this does not interfere with completion of division, while the outer PD and MD rings function throughout and complete chloroplast and mitochondrial division. These results, together with previous studies of C. merolae, disclose the entire cycle of change of the PD and MD rings. Received: 19 May 2000 / Accepted: 3 August 2000     

Skeletal structures and habitats of Recent and fossil Acanthochaetetes (subclass Tetractinomorpha,Demospongiae, Porifera)

The investigation of the habitats, the spicular skeletons, and the structure and chemistry of the nonspicular high-Mg calcite skeletons of a fossil Acanthochaetetes from the Late Albian (Cretaceous) of Northern Spain and the extant Acanthochaetetes wellsi from Pacific reefs demonstrates an astonishing correspondence. The skeletons of both species are hemispherical or pyriform with the lower part containing an epitheca. They are built up of single calicles which are subdivided by tabulae. Spines protrude from the walls into the calicles. Scanning electron microscopy and thin sections reveal that the high-Mg calcite skeleton consists of two different microstructures: a irregular ssensu Wendt 1979 or microlamellar (sensu Cuif et al. 1979) and a completely irregular structure. AAS and EDAX analysis of the calcite skeletons produce roughly the same Mg and Sr contents. Tylostyle megascleres and aster-like microscleres are observed in the spicular skeletons of both species. The only difference between the two species is the greater variability of the microscleres in the extant species. Moreover, the fossil species incorporates the scleres in the non-spicular skeleton, while the extant species does not. Both species live/lived in the same niches of tropical reefs: the cryptic habitats of submarine caves in the reef core and the dimly lighted habitats of the deeper fore-reef.     

The oligomeric state of c rings from cyanobacterial F-ATP synthases varies from 13 to 15

We isolated the c rings of F-ATP synthases from eight cyanobacterial strains belonging to four different taxonomic classes (Chroococcales, Nostocales, Oscillatoriales, and Gloeobacteria). These c rings showed different mobilities on sodium dodecyl sulfate-polyacrylamide gel electrophoresis (SDS-PAGE), probably reflecting their molecular masses. This supposition was validated with the previously characterized c(11), c(14), and c(15) rings, which migrated on SDS-PAGE in proportion to their molecular masses. Hence, the masses of the cyanobacterial c rings can conveniently be deduced from their electrophoretic mobilities and, together with the masses of the c monomers, allow the calculation of the c ring stoichiometries. The method is a simple and fast way to determine stoichiometries of SDS-stable c rings and hence a convenient means to unambiguously determine the ion-to-ATP ratio, a parameter reflecting the bioenergetic efficacy of F-ATP synthases. AFM imaging was used to prove the accuracy of the method and confirmed that the c ring of Synechococcus elongatus SAG 89.79 is a tridecameric oligomer. Despite the high conservation of the c-subunit sequences from cyanobacterial strains from various environmental groups, the stoichiometries of their c rings varied between c(13) and c(15). This systematic study of the c-ring stoichiometries suggests that variability of c-ring sizes might represent an adaptation of the individual cyanobacterial species to their particular environmental and physiological conditions. Furthermore, the two new examples of c(15) rings underline once more that an F(1)/F(o) symmetry mismatch is not an obligatory feature of all F-ATP synthases.     

Thoracic structure and enrolment style in middle Cambrian Eccaparadoxides pradoanus presages caudalization of the derived trilobite trunk

Abstract: The ability to enrol effectively evolved several times among trilobites. Here, we show that, unlike most redlichiid trilobites that could not enrol, both morphotypes of Eccaparadoxides pradoanus from the middle Cambrian of Spain enrolled so as to enclose most of the ventral surface beneath the exoskeleton and possessed specialized articulating devices that facilitated this behaviour. The holaspid thorax of all E. pradoanus was divided into two principal regions. The boundary between these marked a transition from anterior segments with short pleural spines, fulcra and ridge‐and‐groove inner pleural regions to posterior segments with longer, acuminate pleural spines that lack fulcra and inner pleural regions. Devices that aid articulation, such as fulcra with short articulating pleural surfaces, the petaloid articulating facet and long articulating half rings, are concentrated in the anterior region. These features, and the large number of specimens preserved in various degrees of enrolment, suggest an enrolment procedure in which the rear part of the trunk, containing both the posterior thorax and the pygidium, rotated as a single unit without significant internal flexure. As these posterior trunk articulations were apparently not required to permit enrolment, concentrating flexure in the anterior may have presaged the caudalized condition seen in many derived trilobite groups that encapsulated, in which a larger proportion of the trunk segments were allocated to the mature pygidium, and therefore unable to articulate.