Electron spectroscopic diffraction and imaging of the early and mature stages of calcium phosphate formation in the epiphyseal growth plate

Aspects of collagen mineralization in hard tissue formation

Collagen is the dominant fibrous protein not only in connective tissues but also in hard tissues, bone, dentin, cementum, and even the mineralizing cartilage of the epiphyseal growth plate. It comprises about 80-90% (by weight) of the organic substance in demineralized dentin and bone. When collagen fibers are arranged in parallel to form thicker bundles, as in lamellar bone and cementum, interior regions may be less mineralized; in dentin, however, the collagen fibers form a network and collagen fibers are densely filled with a mineral substance. In the biomineralization of collagen fibers in hard tissues, matrix vesicles play a fundamental role in the induction of crystal formation. The mineralization of matrix vesicles precedes the biomineralization of the collagen fibrils and the intervening ground substance. In addition, immobilized noncollagenous fibrous macromolecules, bound in a characteristic way to the fibrous collagen surface, initiate, more intensely than collagen, mineral nucleation in the hard tissue matrix.

Localizational alterations of calcium, phosphorus, and calcification-related organics such as proteoglycans and alkaline phosphatase during bone calcification

To further approach the mechanisms of bone calcification, embryonic rat calvariae were observed at electron microscopic level by the means of fine structures and various cytochemical localizations, including nonspecific proteoglycan (PG) stained by cuprolinic blue (CB), decorin, chondroitin sulfate, hyaluronan, and alkaline phosphatase (ALP), as well as the elemental mapping of calcium (Ca) and phosphorus (P) by energy-filtering transmission electron microscopy (EFTEM). In the calvariae, calcification advanced as the distance from osteoblasts increased. Closer to the osteoblasts, the osteoid was marked by an abundance of CB-positive PGs around collagen fibrils. After crystallization within matrix vesicles, calcified nodules formed and expanded, creating a coherent calcified matrix. The sizes of CB-positive PG-like structures diminished as calcification proceeded. Although small CB-positive structures were accumulated in early stage-calcified nodules, they were localized along the periphery of larger calcified nodules. Cytochemical tests for decorin, chondroitin sulfate, and hyaluronan determined their presence in the areas around collagen fibrils of the osteoid, as well as in and around calcified nodules, whereas ALP was found in the matrix vesicles, as well as in and around the calcified nodules. Ca tended to localize at the PG sites, while P often mapped to the collagen fibril structures, in the uncalcified matrix. In contrast, Ca/P colocalization was visible in and around the calcified nodules, where ALP and smaller CB-positive structures were observed. The difference in the localization patterns of Ca and P in uncalcified areas may limit the local [Ca2+][PO4(3-)] product, leading to the general inhibition of hydroxyapatite crystallization. The downsizing of CB-positive structures suggested enzymatic fragmentation of PGs. Such structural alterations would contribute to the preservation and transport of calcium. ALP possesses the ability to boost local phosphate anion concentration. Therefore, structurally altered PGs and ALP may cooperate in Ca/P colocalization, thus promoting bone calcification.

Characterization of deposits in human lung tissue by a combination of different methods of analytical electron microscopy

Energy-filtering transmission electron microscopy (EFTEM) was used for imaging of deposits in anthracotic areas of human lung tissue. Unstained ultrathin sections were investigated with a Philips CM20 operated at 200 kV acceleration voltage and equipped with a GATAN imaging filter and an X-ray detector for correlative analysis. The distribution of soot particles in the anthracotic areas could be visualized by recording C-K elemental maps, and inorganic particles between the soot by recording C-K jump ratio images. They could be identified as the mineral muscovite and as an iron oxide phase, which would have been overlooked and obviously their composition would not have been recognized using conventional TEM investigations with stained ultrathin sections. Oxide phases of the inorganic particulates were imaged by recording O-K elemental maps, and silicate and Fe phases with Si-L23 and Fe-L23 jump ratio images, respectively. The interpretation of the elemental maps was supported by recording EEL and EDX spectra from interesting specimen regions. Electron diffraction patterns were used to characterize the mineral crystals.

Morphological analysis of renal cell culture models of calcium phosphate stone formation

Cell culture models of calcium phosphate renal stone formation were established using the MDCK cell line. Renal microliths were detected within pseudocysts in three-dimensional soft agar cultures, and were also observed in the basal region of cells lining the cell sheet, and immediately beneath domes or blisters in monolayers and collagen gel cultures. Light and scanning electron microscopy indicated that these microliths had a similar lamellated and spherical appearance to those in humans. These microliths were first detected microscopically after 21 days of culture, and were found to be composed of calcium phosphate by X-ray and micro-infrared spectroscopic analyses. These culture models may provide a powerful new tool to study the pathogenesis of renal stone diseases and/or calcium phosphate stone formation in humans and animals.

Synthetic calcium phosphates: models for biological crystals?

Characterization of the mineral phases of calcified tissues or ectopic calcifications has demonstrated the complexity of biological calcium phosphate salts. Chemists and numerous biologists involved in calcified tissue research have generally described bone and teeth crystallites as hydroxyapatite rather than biological apatites. All biological calcium phosphates have a non-stoichiometric formula, and numerous and variable substitutions. Moreover, in vivo transformations/maturations occur. There is no particular representative synthetic calcium phosphate crystal either for the normal mineral phases of calcified tissues or for the pathological phases. However, they constitute efficient models for the understanding of biological mineralization, and are good approaches to in vitro studies of biomaterials.

Iron distribution in thalassemic bone by energy-loss spectroscopy and electron spectroscopic imaging

Iron overload occurs frequently in thalassemia as a consequence of regular blood transfusions, and iron has been found to accumulate in bone, but skeletal toxicity of iron is not clearly established. In this study, bone biopsies of thalassemic patients were investigated by light (n = 6) and electron microscopy (n = 8) in order to analyze iron distribution and possible iron-associated cellular lesions. Sections (5 microns thick) were used for histomorphometry and iron histochemistry. Ultrathin sections were examined with an energy filtering transmission electron microscope. Iron was identified by electron energy loss spectroscopy (EELS), and iron distribution was visualized by electron spectroscopic imaging (ESI) associated with computer-assisted treatment (two-window method). This study shows that EELS allows the detection of 4500-9000 iron atoms, and that computer-assisted image processing is essential to eliminate background and to obtain the net distribution of an element by ESI. This study shows also that stainable iron was present along trabecular surfaces, mineralizing surfaces, and on cement lines in the biopsies of all patients. Moreover, iron was detected by EELS in small granules (diffusely distributed or condensed in large clusters), in osteoid tissue, and in the cytoplasm of bone cells, but not in the mineralized matrix. The shape and size (9-13 nm) of these granules were similar to those reported for ferritin. As for iron toxicity, all patients had osteoid volume and thickness and osteoblast surface in the normal range. Stainable iron surfaces did not correlate with osteoblast surfaces, plasma ferritin concentrations, or the duration of transfusion therapy.(ABSTRACT TRUNCATED AT 250 WORDS)

Electron energy-loss spectroscopical and image analysis of experimentally induced rat microliths. II

Following a microlith-inducing diet of ethylene glycol plus ammonium chloride, intraluminal and intracellular crystals are observed in aldehyde-fixed rat proximal and distal tubule cells by light and electron microscopy. Qualitative, in-situ analysis with electron-probe X-ray microanalysis (EPMA) of these intraluminal and intracellular crystals shows the presence of calcium, a trace of magnesium, some chlorine and the virtual absence of phosphorus and sulphur. Electron energy-loss spectroscopical element (EELS) analysis and electron-spectroscopic imaging (ESI) confirm, at both sites, the presence of calcium. Selected area electron diffraction (a) confirmed the crystallinity of both the intracellular and intraluminal crystals; (b) produced identical diffractograms from intracellular crystals in proximal tubule cells and deliberately internalized exogenous COM-crystals in cultured LLC-PK1 cells and (c) produced mean dhkl-values, identical to the dhkl-values from calcium oxalate monohydrate (14-771) in the ASTM index, from 4 different intracellular crystals in proximal-tubule cells.

The application of electron spectroscopic imaging for quantification of the area fractions of calcium-containing precipitates in nervous tissue

Energy-filtering transmission electron microscopy has been applied to the quantification of area fractions of calcium-containing cytochemical reaction products in central nervous tissue and the retina of fish. The method of electron spectroscopic imaging using electrons with an energy loss of 250 eV produces images with a very high, structure-sensitive contrast. This is a suitable imaging condition for the reliable detection of reaction products and structural details in unstained ultrathin sections. The images were recorded with a sensitive TV camera and evaluated with the integrated digital image-analysis system of the Zeiss CEM 902 energy-filtering electron microscope. An empirical procedure was developed which objectively detects reaction products and calculates characteristic values, taking into account different staining intensities. This new and sensitive method enabled an assessment to be made of the influence of temperature and light adaptation on cytochemically detectable calcium in nervous tissue of fish. Higher amounts of calcium-containing reaction product were detected in synaptic clefts of the optic tectum in warm-adapted fish than in cold-adapted fish. In synaptic vesicles of photoreceptor cells in the fish retina, higher amounts of reaction product were found in dark-adapted fish than in light-adapted fish.

Analysis of the calcium distribution in predentine by EELS and of the early crystal formation in dentine by ESI and ESD

Predentine is a collagen-rich extracellular matrix between the odontoblasts and the dentine with a width of about 15-20 microns. Electron energy-loss spectroscopy of rat incisors shows a significantly higher calcium content in the predentine at the predentine-dentine border than in the middle region of the predentine. At the predentine-dentine border in the dentine, the calcium and the phosphate groups combine to form apatite crystallites. Electron spectroscopic diffraction with zero-loss filtering revealed that the earliest crystallites contain only Debye-Scherrer rings of apatite, which are fewer in number and more diffuse than the diffraction rings from the mature crystallites. We therefore conclude that the early crystallites still contain lattice defects, which are annealed out to some degree with crystal growth. Electron spectroscopic imaging with zero-loss filtering also showed that the earliest crystallites are chains of dots (or small islands); they build up strands composed of islands, which rapidly acquire a needle-like character and coalesce laterally to form ribbon-or plate-like crystallites. The parallel strands sometimes appear to reinforce the macroperiod of the collagen microfibrils (67 nm) by tiny holes without any crystal-substance lined up perpendicular to the parallel strands of the crystallites.