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Query: UMLS:C0276640 (TEM)
 20,729 document(s) hit in 31,850,051 MEDLINE articles (0.00 seconds)

The present study, using classical microscopy, scanning electron microscopy, transmission electron microscopy, X-ray diffraction, infrared spectroscopy, has shown the dental hard tissues of the fangs of Viperidae (poisonous serpents with terrestrial or semi-aquatic habits) to be constituted of: a calcified outer layer, 0.4 microns thick, made of very small needle-like crystals, randomly distributed. The calcified outer layer contains organic invaginations inducing pores at the surface and many collagen fibres incompletely mineralized, which may suggest enameloid. a calcified inner layer, in the wall of the poison canal. The calcified inner layer, 0.6 microns thick, is constituted of very small crystals, which are parallel to each other and perpendicular to the calcified outer layer. It might be the inner layer of enameloid, an orthodentine, whose tubules present a special lateral branching system resembling a fish bone. The TEM data, which show the dentine to be constituted of very small ill-defined crystals and incompletely mineralized collagen fibres are corroborated by chemical analyses which reveal a poorly mineralized apatite with high carbonate content.
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PMID:[The structure, ultrastructure and physicochemical analysis of the hard dental tissues of the Viperidae]. 263 49

The dark line which is observed in enamel crystallites represents a planar defect involving a single 100 plane of the hydroxyapatite structure. It may occur in the majority of crystals throughout the enamel, although it is only observed in specific diffraction conditions. Its presence may be related both to the formation and growth of crystallites in the developing tooth and to the manner in which the crystallites dissolve during caries. TEM studies show clearly that the central defect is not a dislocation, stacking fault or lattice twin boundary. They further indicate that it cannot represent a structural twin boundary. The remaining possibilities are that it represents a substitution in the HAP lattice, most likely involving carbonate ion, or a separate compatible calcium phosphate phase.
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PMID:TEM study of the central dark line in enamel crystallites. 694 42

Physical, chemical, and mineralogical investigations of mineral concretions found in the human pineal gland were performed by means of optical microscopy and modern techniques of analytical electron microscopy and x-ray powder diffraction (OM,SEM + EDS,TEM + EDS,XRD). The mineral concretions were found to be nano-crystalline carbonate-hydroxyapatite with a mean Ca/P molar ratio equal to 1.65, very close to the theoretical value of 1.67. TEM and XRD showed that this is the only inorganic phase present in the concretions without the presence of amorphous phosphate as precursor. SEM and EDS, performed on cross-sectioned samples, showed a concentric layered distribution of the inorganic phase permeated by organic matter, within the concretions, with a slight increasing of the Ca/P molar ratio in their internal part.
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PMID:Physical, chemical, and mineralogical characterization of carbonate-hydroxyapatite concretions of the human pineal gland. 838 51

The New Zealand solitary ascidian Pyura pachydermatina (Phylum Chordata, Subphylum Urochordata) is a sessile filter feeder in rocky wave-swept coastal areas. The body is on a long stalk; both are covered by a tough fibrous tunic. Two types of spicules are formed in vascularized areas: "antler-shaped" branched spicules of amorphous calcium carbonate in blood sinuses in the body tissues and "dogbone-shaped" knobbed calcitic spicules in the tunic blood vessels. Both types form extracellularly, contain intraspicular organic components and are covered by an organic matrix coat within an epithelium of sclerocytes. SEM and TEM analysis of the spicules and their formation is included, along with calcein incorporation data used to estimate rate of growth. A comparison with spicules of other ascidians and in selected other organisms is included, with comments on the shared features of biomineralization that these disparate groups exhibit.
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PMID:Spicule formation in the New Zealand ascidian Pyura pachydermatina (Chordata, Ascidiacea). 908 35

The aim of this study was to evaluate the maternal toxicity and teratogenicity of lithium following intraperitoneal injection (i.p.) with lithium carbonate (Li2CO3) in pregnant CD-1 mice at the developmental stage of neurulation (E8; day of vaginal plug, E0). Light (LM) and electron (TEM) microscopic studies were also done to document the tissue and cellular changes occurring in embryonic tissues during the 48 h following treatment with 300 mg/kg body wt. Li2CO3. Controls were untreated or given equimolar amounts of NaCl or Na2CO3. A pharmacokinetic study showed that lithium was rapidly absorbed from the peritoneal cavity after the above-stated dose, achieved peak serum levels of 9.8 mmol/l within 1 h, had a half-life in the blood of 5 h and was completely cleared by 16 to 24 h after injection. Doses of Li2CO3 > 300 mg/kg body wt. were toxic to adult CD-1 mice. The latter dose had no detectable maternal toxicity but caused a 19% resorption rate and 2% incidence of open cranial neural tube defect in gestations terminated on E18. The malformation and resorption rates in gestations terminated on E11, E12 and E14 were not significantly different from those of E18. A strong litter effect was seen both for the resorption and malformation rates at all stages examined. At 3 h after treatment cell death became evident in the neuroepithelium. Cells continued to die for approximately 17 h and all necrotic debris had been cleared by 48 h. Also at 3 h after treatment small densely stained inclusions began to appear in mesodermal cells. TEM showed these to be non-membrane bound with an irregular shape and variable size; the lack of staining for acid phosphatase indicated a non-lysosomal structure; the ultrastructural features suggested a lipoid basis. At 24 h after treatment vascular ruptures and surface ectodermal ruptures were seen in the cranial mesoderm. These ruptures with extravascated blood were also seen at 48 h after treatment. A litter effect was also noted with respect to the tissue and cellular changes. These experiments suggest that the developing vascular system may be a target for lithium. In addition, the possibility is discussed that lithium induced cell death in the neuroepithelium may lead to neural tube defects.
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PMID:The effects of lithium on neurulation stage mouse embryos. 924 31

Pure goethite particles in the nanometer size range (from approximately 200 to approximately 80 nm) with an elongated shape (axial ratio from approximately 5 to approximately 8) useful as iron precursors for magnetic recording have been prepared by oxidation of the suspensions resulting from the addition of sodium carbonate to Fe(II) sulfate aqueous solutions under a restrictive set of experimental conditions (Fe(II) concentration, carbonate/Fe(II) mole ratio, temperature, and air flow rate). In all cases, the goethite particles were formed by a dissolution-recrystallization mechanism through an intermediate green-rust phase. The particle size was determined by the carbonate/Fe(II) ratio (which controls the formation pH), the FeSO(4) concentration, and the air flow rate. The smallest particles (length 80 nm) were obtained for a high carbonate/Fe(II) mole ratio (>/=3), a low Fe(II) concentration (0.075 mol dm(-3)), and an air flow rate of 2 dm(3) min(-1). The goethite particles were also characterized by the electron diffraction and high-resolution TEM finding that they were monocrystalline, having the crystalline c axis parallel to the longest particle dimension.
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PMID:Uniform nanosized goethite particles obtained by aerial oxidation in the FeSO4-Na2CO3 system. 1270 28

Chemically unaltered melanosomes from black hair were isolated using a mild enzymatic procedure reported by Novellino et al. involving sequential treatment of a homogenized hair sample with different protease enzymes. Time-dependent fluorescence studies show, under identical conditions, that the rate of bleaching upon NH3/H2O2 treatment of hair melanosomes is twice that of Sepia melanosomes. The structure and morphology of hair melanosomes are compared to Sepia eumelanin using ESEM and TEM imaging studies. Black hair melanosomes are aggregates of rice-shaped ellipsoidal particles (0.8-1.0 microm in length and 0.2-0.6 microm in width) surrounded by an amorphous material suspected to be made of non-proteinacious materials. Sepia eumelanin aggregates are larger (2-5 microm) particles with a "doughnut" shape comprised of 100-150-nm spherical particles. Time-dependent TEM imaging studies of ammonia-treated (pH 10) hair melanosomes showed an initial breakdown of melanosomal aggregates followed by rupture of the melanosomal membrane, releasing melanin nanoparticles and leaving a ghost membrane behind. After prolonged treatment with aqueous NH3, a total loss of characteristic melanosome morphology was observed leading to an amorphous material. By contrast, Sepia melanosomes under identical conditions of ammonia treatment did not show such changes, probably due to different surface properties and aggregation behavior. Sodium hydroxide or sodium carbonate at identical pH did not show similar changes to ammonia, suggesting that the changes are not merely due to alkaline pH, but, rather, are specific to ammonia. Co-treatment with ammonia and peroxide induced a faster disintegration of the melanosomes, resulting in a complete dissolution and discoloration of melanin in 30 minutes. The data suggest that ammonia helps to release melanin nanoparticles out of melanosomes, making them more susceptible to oxidative attack by H2O2.
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PMID:New insights into the physicochemical effects of ammonia/peroxide bleaching of hair and Sepia melanins. 1452 91

The organic matrix surrounding bullet-shaped, cubo-octahedral, D-shaped, irregular arrowhead-shaped, and truncated hexa-octahedral magnetosomes was analysed in a variety of uncultured magnetotactic bacteria. The matrix was examined using low- (80 kV) and intermediate- (400 kV) voltage TEM. It encapsulated magnetosomes in dehydrated cells, ultraviolet-B-irradiated dehydrated cells and stained resin-embedded fixed cells, so the apparent structure of the matrix does not appear to be an artefact of specimen preparation. High-resolution images revealed lattice fringes in the matrix surrounding magnetite and greigite magnetosomes that were aligned with lattice fringes in the encapsulated magnetosomes. In all except one case, the lattice fringes had widths equal to or twice the width of the corresponding lattice fringes in the magnetosomes. The lattice fringes in the matrix were aligned with the [311], [220], [331], [111] and [391] related lattice planes of magnetite and the [222] lattice plane of greigite. An unidentified material, possibly an iron hydroxide, was detected in two immature magnetosomes containing magnetite. The unidentified phase had a structure similar to that of the matrix as it contained [311], [220] and [111] lattice fringes, which indicates that the matrix acts as a template for the spatially controlled biomineralization of the unidentified phase, which itself transforms into magnetite. The unidentified phase was thus called pre-magnetite. The presence of the magnetosomal matrix explains all of the five properties of the biosignature of the magnetosomal chain proposed previously by Friedmann et al. and supports their claim that some of the magnetite particles in the carbonate globules in the Martian meteorite ALH84001 are biogenic. Two new morphologies of magnetite magnetosomes are also reported here (i.e. tooth-shaped and hexa-octahedral magnetosomes). Tooth-shaped magnetite magnetosomes elongated in the [110] direction are reported, and are distinct from arrowhead-shaped and bullet-shaped magnetosomes. Elongation of magnetite magnetosomes in the [110] direction has not been reported previously. A Martian hexa-octahedral magnetite particle was previously characterized by Thomas-Keptra et al. and compared with truncated hexa-octahedral magnetite magnetosomes. Hexa-octahedral magnetite magnetosomes with the same morphology and similar sizes and axial ratios as those reported by Thomas-Keptra et al. are characterized here. These observations support their claim that ALH84001 contains evidence for a past Martian biota.
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PMID:Magnetosomal matrix: ultrafine structure may template biomineralization of magnetosomes. 1473 1

The acidic amino acid, such as aspartic acid (l-Asp), and glutamic acid are the primary active molecules of the glycoprotein on the organic/inorganic interface of biomineralized tissue. In this study, aspartic acid was used as the organic template in inducing the nucleation and growth of calcium carbonate. With the analysis of X-ray diffraction we investigated the relationship between the l-Asp concentration and the precipitation phase crystal structure of calcium carbonate. SEM and TEM were employed in the analysis of the morphological characteristic of the precipitation and the aggregation of the nanoscale porous phase. In order to get the direct evidence of the interaction between Ca2+ and l-Asp, the technique of QCM was used in the investigation of the coordinate interaction of Ca2+/l-Asp. As the results have shown, l-Asp alone is adequate to switch the transformation between calcite and vaterite, and neither soluble organic additions nor metal ions are needed. Meanwhile, the morphology, size and aggregative way of the deposition are also mediated with change of l-Asp concentration. To interpret the cause of the hierarchic structure range from nanoscale to micron-scale and the formation of the porous spheres of vaterite, an assumption of limited-fusion was proposed from the view of the small biomolecules polarity that can control over the growth of the crystals and the aggregation of the micro crystals. The conclusion also provide a new material synthesize strategy.
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PMID:Control over the crystal phase, shape, size and aggregation of calcium carbonate via a L-aspartic acid inducing process. 1502 Jan 69

When Penicillium digitatum Saccardo cultures are exposed to aqueous solutions containing soluble uranium salts, considerable amounts of this element are accumulated in the fungal mycelium. The accumulated uranium is retained after thorough rinsing with distilled water but is removed by alkali carbonate solutions. Analysis of thick sections (0.5 microm) of the fungal hyphae with TEM, after incubation in UO(2)Cl(2) solutions of varying concentrations under both light and dark conditions, revealed conspicuous crystal-like deposits in UO(2)Cl(2)-exposed hyphae, but none in the control hyphae. Thick sections were necessary for crystal visualization. Using energy-dispersive X-ray analysis, uranium was detected as the only heavy element in these crystals. Uranium crystal biosorption was localized on the outside surface of the hyphal cell wall (following short exposures to relatively low uranium concentrations) or inside the cell wall (following long exposure to relatively high uranium concentrations). In some cases, crystal-like deposits of uranium salts were located on the outside surface as well as inside the cell.
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PMID:Ultrastructural localization of uranium biosorption in Penicillium digitatum by stem X-ray microanalysis. 1509 99


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