Opercular regeneration in Pomatoceros lamarckii Quatrefages (Polychaeta: Serpulidae). Differentiation of the operculum and deposition of the calcareous opercular plate

Following opercular amputation, stages in opercular regeneration in Pomatoceros lamarckii have been described by light, transmission and scanning electron microscopy. Two to three days after amputation, the rudimentary opercular filament is invested with a delicate cuticle composed of an outer filamentous layer and an inner thicker component composed of orthogonally-arranged layers of small fibril bundles. The opercular plate is uncalcified and composed of two major components, an outer, thin, electron-dense layer and an inner, thicker component which structurally resembles that of the opercular filament cuticle. Between five and eight days, opercular plate calcification is initiated as needle-like crystallites. The structural organization of the organic components of the opercular plate show changes which are related to the onset of calcification. From 13–17 days, the opercular plate becomes heavily calcified and is composed of highly-ordered, prism-like crystals. X-ray diffraction shows these crystals to be aragonite. The structure of the cuticle remains unchanged except that the orthogonally-arranged fibril bundles aggregate into thicker fibres. Amino acid analysis of the regenerated cuticle and organic components of the opercular plate show that they differ from one another and from the normal cuticle and opercular plate. During opercular regeneration, the differentiation of the cuticle and opercular plate-secreting cells are described and the mechanisms of cuticle and calcareous opercular plate secretion are discussed.     

Formation and excretion of calcareous bodies by the metacestode (Tetrathyridium) of Mesocestoides vogae

The function of calcareous bodies, commonly found in the parenchyma of cestodes and trematodes, is relatively poorly understood. The present histochemical ultrastructural study of the proliferative tetrathyridia of Mesocestoides vogae revealed that calcareous corpuscles begin to form as organic (lipid-protein) masses that coalesce in parenchymal (calcareogenic) cells. Concentric accretion of organic and inorganic crystalline material then leads to the formation of typical refractile calcareous bodies. The precise composition of such bodies, determined by x-ray diffraction, revealed that their major inorganic constituent is indeed calcium, with significant amounts of phosphorus, silicon, and zinc as well. Emission of calcareous bodies through the tegument was observed by scanning electron microscopy, explaining their accumulation in the intracapsular spaces around worms embedded in liver tissue of the host. Following their emission, the crystalline substance of corpuscles dissolves, leaving only nonrefractile, membrane-bound cytoplasmic debris. These observations do not preclude the possibility that calcareous bodies may play some role as buffers or reservoirs of inorganic ions. However, it is difficult to accept such a function for unencapsulated worms in the coelom or intestinal lumen; we suggest that excretion is a more likely role in such sites.     

P PROTEIN IN THE PHLOEM OF CUCURBITA : II. The P Protein of Mature Sieve Elements

During maturation of sieve elements in Cucurbita maxima Duchesne, the P-protein bodies (slime bodies) usually disperse in the tonoplast-free cell. In some sieve elements the P-protein bodies fail to disperse. The occurrence of dispersal or nondispersal of P-protein bodies can be related to the position of the sieve elements in the stem or petiole. In the sieve elements within the vascular bundle the bodies normally disperse; in the extrafascicular sieve elements the bodies often fail to disperse. Extrafascicular sieve elements showing partial dispersal also occur. The appearance of the sieve plate in fixed material is related to the degree of dispersal or nondispersal of the P-protein bodies. In sieve elements in which complete dispersal occurs the sieve plate usually has a substantial deposit of callose, and the sieve-plate pores are filled with P protein. In sieve elements containing nondispersing P-protein bodies the sieve plate bears little or no callose, and its pores usually are essentially "open." The dispersed P-protein components may aggregate into loosely organized "strands," which sometimes extend vertically through the cell and continue through the sieve-plate pores; but they may be oriented otherwise in the cell, even transversely.     

Evaluation of membrane-bound black bodies in trophozoites and cysts of Naegleria spp

Various Naegleria strains were examined to determine the possible origin and significance of membrane-bound black bodies that were found in all exponentially growing cell populations. The bodies, 40–80 nm in diameter, were distributed randomly in the cytoplasm of Naegleria with ultrastructural features typical of trophozoites. No evidence was obtained that the contents of the black bodies were synthesized in the rough endoplasmic reticulum (ER) and packaged by membranous components, which could be a primitive “Golgi complex” in these amoebae. Examination of cells in various stages of encystment indicated that at least some of the cyst wall material was synthesized and packaged by the rough ER. After condensation into amorphous granules in the cisternae, the cyst wall material appeared in vesicles of the rough ER; these were frequently seen in close proximity to the cell membrane in the vicinity of developing cyst wall. Amorphous granules (～100 nm in diameter), which had variable densities and did not appear to be membrane bound, were seen in the cytoplasm of encysting cells. The substance of these granules also seemed to be incorporated into the cyst wall. The membrane-bound black bodies appeared to be destroyed in lysosomal elements during encystment. The membrane-bound black bodies were concluded to be characteristic of trophozoites and unrelated to encytment of Naegleria.     

Styletogenesis in nemertean worms: The ultrastructure of organelles involved in intracellular calcification

The ultrastructure of cellular organelles involved in stylet formation is examined in six species of nemertean worms by transmission electron microscopy (TEM). Stylets are nail-shaped structures containing calcium phosphate that are assembled intracellularly in large uninucleate cells, called styletocytes. Each stylet develops within a membrane-bound vacuole in the styletocyte cytoplasm. Well developed arrays of Golgi bodies are typically found in the vicinity of developing stylet vacuoles, and fully formed vacuoles are filled with PAS+ material that appears to be derived from the smooth endoplasmic reticulum. At the onset of styletogenesis, a conical sliver of organic material differentiates on the inner surface of the vacuolar membrane. This material displays a species-specific banding pattern in decalcified sections, and apparently acts as a template during calcification of the stylet shaft. After the organic core of the shaft is formed, mitochondria aggregate around the stylet vacuole and presumably help accumulate the calcium used in mineralization of the stylet. A knob-shaped proximal piece is subsequently assembled on the base of the shaft. The proximal piece contains a nonbanded matrix and has electron-dense material at its surface that may help in correctly orienting this region toward the basis during replacement of the central stylet.     

A scanning electron microscopic study of the inorganic and organic matrices comprising the mature shell of Amblema, a fresh-water mollusc

The scanning electron microscope has been used to describe the morphology of the mature shell in a fresh-water bivalve. The structure of the organic and inorganic components within the nacre, the myostracum, and the prismatic layer is described. A transitional or intermediate zone, interposed between the prismatic layer and the nacre, was identified. In demineralized samples, the organic component of the nacre was found to consist of parallel matricial sheets interconnected by irregular transverse bridges. The structure of the mineral component of the nacre was found to vary with the method of specimen preparation. With polished-etched samples, brick-like units were seen. When shells were simply broken and fixed in osmium, the layers of nacreous material consisted of fusing rhomboidal crystals of aragonite which demonstrated subconchoidal fractures. On the inner surface of the shell, the rhomboidal crystals showed an apparent spiral growth pattern. The myostracum was characterized by regions of modified nacreous structure consisting of enlarged aragonite crystals with a pyramidal morphology. The peripheral aspect of the muscle scars was characterized by rhomboidal crystals, the latter fusing to form the typical nacreous laminae. The uniqueness of the anterior adductor scar is exemplified by the presence of pores, each pore walled by pyramidal units, for the insertion of adductor fibres. In most regions of the shell, the prismatic layer consisted of one prism unit thickness with a height of approximately 225–250 μm. However, in two specialized regions of the shell, this layer was seen to consist of multiple layers of stacked prisms. The organic matrices of the prismatic layer are arranged in a honeycomb-like arrangement and packed with mineralized spherical subunits.     

Microstructure,mechanical, and biomimetic properties of fish scales from Pagrus major

The fish scale of Pagrus major has an orthogonal plywood structure of stratified lamellae, 1-2 microm in thickness, consisting of closely packed 70- to 80-nm-diameter collagen fibers. X-ray diffraction, energy-dispersive X-ray analysis, and infrared spectroscopy indicate that the mineral phase in the scale is calcium-deficient hydroxyapatite containing a small amount of sodium and magnesium ions, as well as carbonate anions in phosphate sites of the apatite lattice. The tensile strength of the scale is high (approximately 90 MPa) because of the hierarchically ordered structure of mineralized collagen fibers. Mechanical failure occurs by sliding of the lamellae and associated pulling out and fracture of the collagen fibers. In contrast, demineralized scales have significantly lower tensile strength (36 MPa), indicating that interactions between the apatite crystals and collagen fibers are of fundamental importance in determining the mechanical properties. Thermal treatment of fish scales to remove the organic components produces remarkable inorganic replicas of the native orthogonal plywood structure of the fibrillary plate. The biomimetic replica produced by heating to 873 K consists of stratified porous lamellae of c-axis-aligned apatite crystals that are long, narrow plates, 0.5-0.6 microm in length and 0.1-0.2 microm in width. The textured inorganic material remains intact when heated to 1473 K, although the size of the constituent crystals increases as a result of thermal sintering.     

Microstructure and formation of the calcareous operculum in Pyrgopolonctenactis and Spirobranchusgiganteus (Annelida, Serpulidae)

The calcareous operculum of Pyrgopolon ctenactis is composed of spherulitic prismatic structures. The opercular cup consists of regular spherulitic prismatic crystals; the talon has two layers, an inner with an irregular spherulitic prismatic structure (150 μm thick) and an outer with a regular spherulitic prismatic structure (110 μm thick). The outer regular structure has thick (1 μm) organic interprismatic sheets unique in biomineralization of this group, but similar to that of Bivalvia. We infer that control over biomineralization is stronger during the formation of the outer regular layer, with its thick organic interprismatic sheets, than during the formation of the inner irregular spherulitic prismatic structure, without such sheets. In Spirobranchus giganteus, opercular formation differs from that of P. ctenactis. S. giganteus has numerous pores in its opercular plate, and calcification starts with the formation of an outer irregularly oriented prismatic structure followed by an oriented prismatic structure without interprismatic sheets.     

An ultrastructural study of the mantle of the barnacle, Elminius modestus Darwin in relation to shell formation

The fine structure of the mantle and shell of the barnacle, Elminius modestus Darwin has been examined by electron microscopy. The epithelial cells along the outer face of the mantle differ in size, shape, and organelle complexity according to the different components of the shell they secrete. The shell consists of a non-calcareous basis and calcareous mural and opercular plates which are connected by a flexible opercular hinge. Both the basis and opercular hinge are composed of two main units: an outer cuticulin layer and a lamellate component of well ordered arched fibrils. During the deposition of the latter structures morphological changes in the cells occur which may be correlated with the moulting cycle. Preliminary results show that the calcareous plates are covered by an outer epicuticle, which is bordered by a cuticulin layer; the inner calcareous component, consists of an orderly arrangement of organic matrix envelopes within which crystals may be initiated.

The cells lining the inner surface of the mantle are uniform in appearance with a thin cuticle at their free surface which lines the body cavity. The latter structure of the cuticle and manner of its deposition are similar to those of the basis and opercular hinge. Separating the outer and inner mantle epithelial cells is connective tissue which comprises several differing cell types. The possibilities are discussed of the rôle these cells may play in shell deposition. The modes by which underlying cells secrete the different shell components and the cuticle lining the inner face of the mantle, are also discussed.     

Morphologic characteristics of the large bodies in cultures of the L-forms of bacteria according to scanning electron microscope studies]

Large bodies appear at the time of protoplast and spheroplast formation and are revealed at all the L-transformation stages and at the initial stage of reversion. They can be represented both by a single giant cell and by a conglomerate of different cells connected with one another. They are not only spheroid, but can be of the most varied shape, and structurally they are connected with other L-colony elements: filamentous structures, spheroid cells, elementary bodies and the so-called acellular material. At the early L-transformation stage the large bodies probably appear as a result of coalescence of lysed cells and represent polygenome formations. Elementary bodies and spheroid cells form within the large bodies and on their surface at the late stage of L-transformation. In case of reversion bacterial cells form from them.     

Carbonate organo-mineral micro- and ultrastructures in sub-fossil stromatolites: Marion lake, South Australia

Sub-fossil stromatolites (5000-3000 years old) occur on the marginal flat surrounding Marion Lake (South Australia). A micrite/microsparite crystal fabric characterises these fine-grained, well-laminated stromatolites, which lack trapped grains. The internal lamination is characterised by a sub-millimetric alternation of porous and dense laminae. The microfabric of the laminae is ubiquitously composed of a fine (10-20 μm) peloidal texture, with many thinner aphanitic layers. Aggregates of very fine, low-Mg calcite and aragonite constitute both peloidal and aphanitic micrite, which is coated, respectively, by spherulitic and fringing acicular microspar. Micrite, with a high organic matter content, is formed of coalescing nanospheres grading into small polyhedrons, probably composed mainly of aragonite, with less calcite enriched in Mg, Sr, Na and S. Bacteria-like microfossils and relics of extracellular polymeric substance (EPS) occur abundantly within this micritic framework. The former consist of empty moulds and mineralised bodies of coccoid forms, whereas EPS relics consist of sheet-like or filamentous structures that appear both mineralised and more often still preserved as a C-enriched dehydrated substance that represents the main organic matter component of the deposit. Acicular crystals, which show a prismatic elongate shape, are composed of Mg-depleted aragonite that lacks fossils or organic relicts. Degrading EPS and micro-organisms appear gradually to be replaced and entombed by the nanospherical precipitates, implying the existence of processes of organo-mineralisation within an original syn-sedimentary microbial community. Succeeding micron-scale crystals merge to form isolated or connected micritic aggregates (the peloids), followed by the gradual formation of the acicular crystals as purely inorganic precipitates.     

Chemical analysis of stalk components of Dictyostelium discoideum

Structural components of the stalks of mature fruiting bodies of Dictyostelium discoideum have been isolated and characterized after solubilizing non-structural components with urea and sodium dodecyl sulfate. The urea/sodium dodecyl sulfate-insoluble stalks are composed of about 52% cellulose, 15% proteins and 3% of a non-cellulosic heteropolymer in a covalently bound matrix. Non-covalently bound fatty acid containing material was also found. The composition and structural interrelationships of these components are essentially identical to that of the urea/sodium dodecyl sulfate-insoluble surface sheath which is produced earlier in development before culmination. These results suggest that the same components are involved in making structural elements which differ substantially in their functional role in the developmental sequence as well as in their spatial and temporal localization and morphological appearance.     

Membrane-bound Plastid Inclusions and Chloroplast Thylakoid Formation in Sunflower (Helianthus annuus L.)

The ultrastructure, distribution and frequency of membrane-boundplastid inclusions present in the epidermal cells of leavesof intact sunflower plants (Helianthus annuus L.) and in theepidermal and mesophyll cells of sunflower leaf discs culturedin darkness have been studied. These inclusions appear to bedilated thylakoids containing a granular material which, undernormal conditions, is probably involved in chloroplast membraneformation. It is suggested that this material accumulates, andinclusions form, in the chloroplasts of sunflower leaves intwo specific situations. Firstly, in the completely differentiatedcells of the epidermis where the chloroplasts, although at arelatively immature stage, have nevertheless reached a terminalstage of development. Secondly, in the mesophyll cells of youngleaves when chloroplast development has been arrested at animmature stage by a 5-day dark period. In the latter situationthe material can be remobilized if plastid development is restimulated.The plastids of sunflower leaf discs cultured in darkness containboth membrane-bound inclusions and prolamellar bodies, indicatingthat they are separate and distinct structures possibly containingdifferent membrane components. Helianthus annuus L., sunflower, chloroplast, ultrastructure, plastid inclusions, thylakoid formation     

The effect of adenosine triphosphate,magnesium chloride and phospholipids on crystal formation in the demineralized shell-repair membrane of the snail,Helix pomatia L.

Summary The effect of adenosine triphosphate (ATP), magnesium chloride (MgCl₂) and phospholipids on the calcium-binding activity and crystal formation within the decalcified shell-repair membrane of the snail, Helix pomatia, was studied in vitro. The application of ATP produced a characteristic dual effect on calcification: (1) It strongly inhibited the formation of inorganic calcium carbonate (CaCO₃) crystals. (2) It stimulated the development of organic crystalline bodies and induced deposition of amorphous calcium carbonate. The demineralized shell-repair membranes became white and rigid after incubation for 7 days in the medium containing 1.0mM ATP. The inhibitory effect of Mg²⁺ on CaCO₃ crystal formation was diminished by reduction of the concentration of MgCl₂ in the incubation solution. Thus, after incubation for only 24h, 1.0mM MgCl₂ promoted the formation of birefringent CaCO₃ crystals within the repair membranes. The principal effect of phospholipids on the demineralized shell-repair membrane was stimulatory, but after application of phospholipids to the medium, the formation of crystals proceeded slowly. The very large, composite crystals that were formed within the repair membranes showed strong birefringence. In all cases the development of the crystals and the organic crystalline bodies occurred in close vicinity to the amoebocytes. The role of ATP, MgCl₂ and phospholipids in the recalcification of shell-repair membrane is discussed.The author wishes to thank Mrs. E. Hellmén for valuable technical assistance     

Comparative Ultrastructure and Organization of the Prismatic Region of Two Bivalves and its Possible Relation to the Chemical Mechanism of Boring

The prismatic region of two bivalve molluscs exemplifies, inits structure and organization, one of the types of differentiatedcalcareous substrates through which boring organisms must penetrate. The oriented inorganic crystals, separated from one anotherby intercrystalline "spaces", are structurally organized intowell defined prisms. The prisms of each bivalve vary in shapeand size and are delineated from one another by electron-lucent,non-calcified regions. The demineralized organic matrix is also structurally organizedinto prisms, delineated from one another by prism sheaths, andan intraprismatic matrix structurally organized into closelypacked sheet-like compartments and subcompartments in whichthe inorganic crystals are deposited. The non-mineralized intercrystalline "spaces" between the individualinorganic crystals of the same or adjacent rows in a mineralizedsection are occupied by the walls of the intraprismalic sheet-likecompartments. Similarly, the non-calcified electronlucent regionsdelineating one mineralized prism from the next are occupiedby the thick prism sheaths. These portions of the organic matrixwhich fail to mineralize completely undoubtedly provide readypathways for the passage of solutes and solvents through thesetissues of highly ordered, densely packed, inorganic crystals.Moreover, the framework of the organic matrix, which fails tomineralize in these heavily calcified, molluscan substrates,may provide the primary, not the secondary source of chemicalattack during boring, for once the sheaths and compartmentssurrounding the crystals are broken down or solubilized, thecrystals are themselves loosened and freed for mechanical removalby shell-penetrating organisms.     

P-protein and inclusion bodies in root protophloem of Salix viminalis

The formation of P-protein in the protophloem of 9- to 14-day-old adventitious roots of Salix viminalis was studied. In immature sieve elements a finely granular material was present. This was considered to be nascent P-protein. Small aggregations of tubular P-protein were observed 17 cells from the first "cleared" sieve element. In older cells the bodies were up to 7 μm long. Nondispersed and disaggregating P-protein bodies were present in mature sieve elements. P-protein bodies were also observed in parenchyma cells adjoining mature sieve elements. In addition, inclusion bodies of unknown origin are described. They had a granular content and were most often found in mature sieve elements.     

On the structure of the Z pseudo-organ in Xiphinema diversicaudatum

The structure of the Z pseudo-organ in Xiphinema diversicaudatum consists of a muscular mass of about 80 cells arranged in rings of four cells each. These cells have peripheral nuclei and are connected with a glandular monolayered epithelium, which lines the lumen of the Z pseudo-organ. Globular bodies originate from the membranes of the epithelial tissue. They consist of a series of closed vesicles containing secretions, and of tubules through which the secretions flow into the lumen. The globular bodies have a helicoidal distribution within the lumen of the Z pseudo-organ which presumably slows the passage of the egg. Enzymatic digestion, in vivo, indicates that the secretion consists of acid and basic proteins involved in egg shell formation.     

Shell formation and calcium transport in the barnacle Chthamalus fragilis

The mantle epithelium of the barnacle Chthamalus fragilis (Darwin) exhibits several ultrastructural features which may serve to regulate the calcification process. At the basis-mural plate and intermural plate junctions where rapid shell growth occurs, cells are characterized by long apical cytoplasmic projections and large intercellular spaces. These features may increase the functional surface area of the epithelium and enable more rapid deposition of calcium. The cells underlying the general shell surfaces contain numerous electron-dense inclusion bodies and show frequent cellular disintegration near the growing shell interface. Release of the granular contents of these inclusion bodies has been observed in both disintegrating and non-disintegrating cells. X-ray microanalysis revealed significantly higher calcium levels in the inclusion bodies than in the surrounding cytoplasm. This suggests a calcium transport role for these inclusion bodies. Cellular debris produced as a result of the disintegration of the mantle cells near the shell may play some role in the formation of the organic matrix of the shell. The presence of large numbers of mitochondria and well-developed apical microvilli in the cells of the inner mantle epithelium suggest that these cells serve to transport calcium into the mantle from the ambient sea water.     

Electron microscopic and cytochemical studies of the mouse subcommissural organ

Summary In mice most of the ependymal cells of the subcommissural organ (SCO cells) are densely packed with dilated cisternae of the endoplasmic reticulum (ER) containing either finely granular or flocculent materials. The well developed supra-nuclear Golgi apparatus consists of stacks of flattened saccules and small vesicles; the two or three outer Golgi saccules are moderately dilated and exhibit numerous fenestrations; occasional profiles suggesting the budding of coated vesicles and formation of membrane-bound dense bodies from the ends of the innermost Golgi saccules are seen. A few coated vesicles and membrane-bound dense bodies of various sizes and shapes are also found in the Golgi region.The contents of the dilated ER cisternae are stained with periodic acid-silver methenamine techniques. In the Golgi complex the two or three inner saccules are stained as deeply as the dense bodies, and the outer saccules are only slightly stained. The stained contents of ER cisternae are more electron opaque than those of the outer but less opaque than those of the inner Golgi saccules and the dense bodies.Acid phosphatase activities are localized in the dense bodies, some of the coated vesicles in the Golgi region, and in the one or two inner Golgi saccules.On the basis of these results the following conclusions have been reached: (1) In mouse SCO cells the finely granular and the flocculent materials in the lumen of ER cisternae contain a complex carbohydrate(s) which is secreted into the ventricle to form Reissner's fiber; (2) the secretory substance is assumed to be synthesized by the ER and stored in its cisternae, and the Golgi apparatus might play only a minor role, if any, in the elaboration of the secretory material; (3) most of the dense bodies in the mouse SCO cells are lysosomal in nature instead of being so-called dark secretory granules.Sponsored by the National Science Council, Republic of China.     

莫桑鼻给非鲫滤泡闭锁中液晶形成的冰冻蚀刻研究

本文运用电镜的冰冻蚀刻术研究了莫桑鼻给非鲫滤泡闭锁中液晶形成的过程.结果表明,卵巢内的颗粒细胞吞噬大量的卵黄物质,消化后形成同心圆片层体,这是一种类脂加水以及镶嵌少量的蛋白质的溶致液晶态;细胞内的酶类参与液晶的形成;同时讨论了生物体内相变及液晶态存在的意义.