Calcium localized in odontogenic cells of rat mandibular teeth by the glyoxal bis (2-hydroxyanil) method

A silicon cell cycle in a bacterial model of calcium phosphate mineralogenesis

The prokaryote Corynebacterium matruchotii produces calcium phosphate (bone salt) and may serve as a convenient model for examining individual factors relevant to vertebrate calcification. A factor of current clinical uncertainty is silicon. To investigate its possible role in biomineralisation advanced optical (digital deconvolution and 3D fluorescent image rendering) and electron microscopy (EDX microanalysis and elemental mapping) were applied to calcifying microbial colonies grown in graded Si concentrations (0-60mM). Cell viability was confirmed throughout by TO-PRO-3-iodide and SYTO-9 nucleic acid staining. It was observed that calcium accumulated in dense intracellular microspherical objects (types i-iii) as nanoparticles (5 nm, type i), nanospheres (30-50 nm, type ii) and filamentous clusters (0.1-0.5 μm, type iii), with a regular transitory Si content evident. With bacterial colony development (7-28 days) the P content increased from 5 to 60%, while Si was displaced from 60 to 5%, distinguishing the phenomenon from random contamination, and with a significant relationship (p<0.001) found between calcified object number and Si supplementation (optimum 0.01mM). The Si-containing, intracellular calcified objects (also positive for Mg and negative with Lysensor blue DND-167 for acidocalcisomes) were extruded naturally in bubble-like chains to complete the cycle by coating the cell surface with discrete mineral particles. These could be harvested by lysis, French press and density fractionation when Si was confirmed in a proportion. It was concluded that the unexplained orthopaedic activity of Si may derive from its special property to facilitate calcium phosphorylation in biological systems, thereby recapitulating an ancient and conserved bacterial cycle of calcification via silicification.

Cryopreservation and image enhancement of juvenile and adult dentine mineral

The inorganic component of bone and related hard tissues is generally described as sheets of uniform needle- and plate-like crystals. However, cryofixation has become the method of choice for ultrastructural studies of bone mineral when ladder-like arrangements of filaments contained within deformable microspheres about 1 microm in diameter are apparently the prime structural feature and are consistent with the optical image. The same methodology has now been applied to mature human dentine in caries-free juvenile and adult teeth. These were fixed, sliced, stained for mineral and examined optically or were snap frozen, fragmented under liquid nitrogen, freeze-substituted with methanol or acetone and embedded without thawing in Lowicryl K4M for electron microscopy. Others were processed by traditional transmission electron microscopy methods. To obtain maximum resolution, the electron micrographs were photographically printed as negatives and image-enhanced by digitisation using a Polaroid Sprint Scan 45 and laser printer. In both optical and cryopreparations of juvenile and adult dentine, mineral microspheres up to 1 microm in diameter, were present in the dentinal tubules and peritubular dentine. Within these objects, the mineral was primarily in the form of sinuous electron dense filaments, 5 nm thick, which had a characteristic periodicity. In these preparations needle-like and plate-like structures were rare. In contrast, after traditional transmission electron microscopy preparation although similar filamentous structures remained, the mineral more generally had the familiar form of needles measuring approximately 50 nm in the long axis. The cryopreserved calcified filaments were apparently particularly densely distributed in the intertubular dentine where their parallel ladder-like arrays often formed highly orientated struts and stays. It was concluded that early dentine mineral has the form of filamentous microspheres and as in bone (and other calcifying tissues and cells) has no specific association with collagen. It was also concluded that these structures compact and deform with maturity into a sub-structural framework which may relate to powerful biomechanical forces transmitted through the tissue. Needle- or plate-like mineral is probably rare in vivo in dentine, only becoming commonplace after extensive chemical processing.

Pathway and speed of calcium movement from blood to mineralizing enamel

We studied by autoradiography the distribution of 45Ca in the enamel organ of frozen rats 4.3, 6.1, 7.8, 10.6 and 13.7 sec after an i.v. injection. The intercellular junctions of the proximal side of the smooth-ended ameloblast (SA) and the distal side of the ruffle-ended ameloblast (RA) were closed to calcium. The junctions of the distal side of SA, the proximal side of RA, and both sides of the secretory stage ameloblasts were not. The time required for calcium to pass through the ameloblast layer was less than 1.8 sec in the secretory stage and SA region. The time in the RA region was 3.5-6.3 sec. In the transitional region from RA to SA, a band of strong radioactivity appeared from the papillary layer of RA region towards the enamel of the SA region. The radioactivity in the secretory stage enamel increased almost linearly with time. The diffusion speed of calcium in the enamel was more than 50 microns for 1.8 sec in the maturation stage and less than 15 microns for 9.4 sec in the secretory stage. These results indicate that in the secretory and SA regions calcium moves to the enamel surface through the intercellular spaces of ameloblasts and in the RA region via RA cells.

Histochemical, ultrastructural, and electron microprobe analytical studies on the localization of calcium in rat incisor ameloblasts at early stage amelogenesis

The enamel organs of rat incisors were separated from the enamel surface and processed for rapid freezing and freeze-substitution. A histochemical stain for calcium (GBHA) of thick Epon sections revealed intense calcium reactions in the secretory ameloblasts, exclusively in the tubulovesicular structures extending throughout their distal cytoplasm. Electron microscopy revealed a thin layer of amorphous material with clusters of electron-dense granules along the distal surface of secretory ameloblasts. In young secretory ameloblasts without typical Tomes' processes, a considerable number of mitochondria were located in the distal cytoplasm and contained numerous electron-dense granules. Similar dense granules as well as fine ribbon-like electron-dense figures, all containing significant amounts of calcium, were observed in some of the tubulovesicular structures at the distal end of these cells. A putative exocytotic figure of such dense granules was also observed. The electron-dense granules were rare in more differentiated ameloblasts with elongated Tomes' processes, which occasionally displayed ribbon-like figures in some of the tubulovesicular structures in the process region. No significant calcium peak was detected in the extracellular amorphous material, secretory granules, or along the lateral plasma membranes. These observations may imply high calcium concentrations in mitochondria and tubulovesicular structures in the distal cytoplasm of secretory ameloblasts relative to that of the cytosol and support the possible contribution of these organelles in secretory ameloblasts to cellular calcium regulation at least in the early stage of amelogenesis.

Banding patterns in rat incisor enamel stained by histochemical complexing methods for calcium

A characteristic banding pattern can be visualized at the surface of the rat incisor in the maturation zone of amelogenesis by staining with glyoxal bis(2-hydroxyanil) (GBHA). Other banding patterns can be obtained with certain histological and fluorochrome stains and by radioautography following 45Ca injection. In this study, several histochemical reagents known to complex with different states of calcium were used to stain the surface of enamel. Rat incisors were quickly dissected and immediately immersed in solutions containing the following calcium-binding reagents: arsenazo III, calmagite, murexide, N,N-naphthaloylhydroxylamine, and calcein. Routinely, one contralateral lower incisor from each pair was counterstained with GBHA in order to relate each of the staining patterns to the banded distribution of maturation ameloblasts that is reflected by the characteristic GBHA staining pattern in the enamel. Each of the reagents used in this study demonstrated a staining pattern consisting of a series of broad bands running transversely and obliquely across the enamel. In all cases, the dyes stained predominantly that enamel associated with ruffle-ended ameloblasts, i.e. enamel left unstained by GBHA. Some of the reagents also stained enamel in the secretion zone. The appearance and distribution of the staining patterns reflect the banded distribution of maturation ameloblasts and appear to be controlled on a time scale related to the rapid modulation of these cells.

Interleukin-1 beta is a potent inhibitor of bone formation in vitro

The effect of interleukin-1 beta, the major component of osteoclast-activating factor (OAF), on bone formation by fetal rat osteoblast-rich cells was investigated. An in vitro culture system developed by Ecarot-Charrier et al. (1983) and Bellows et al. (1986) was utilized in which osteoblasts form mineralized nodules which closely resemble woven bone. Continuous exposure of cultures to homogenous IL-1 beta resulted in potent inhibition of mineralized nodule formation, which was half maximal at 0.1 U/ml (7.5 X 10(-13) M). Bone formation may thus be considerably more sensitive to IL-1 beta than is bone resorption (half maximal at 3.8 X 10(-11) M). Inhibition of bone formation occurred when cultures were exposed to IL-1 beta at both early and late time periods and was unaffected by the presence of indomethacin or by the osteoclast inhibitors calcitonin and gamma-interferon. Instead, IL-1 beta exerted multiple inhibitory effects on osteoblast functions, including inhibition of collagen and noncollagen protein synthesis, alkaline phosphatase expression, and cell replication. On a dose response basis, the inhibition of protein synthesis correlated most closely with inhibition of bone formation. IL-1 beta is clearly inhibitory rather than stimulatory for bone formation as assessed in this system and is therefore unlikely to function as a coupling factor linking the processes of bone resorption and bone formation.

Modification of the enamel maturation pattern by vinblastine as revealed by glyoxal bis(2-hydroxyanil) staining and 45calcium radioautography

Patterns characteristic of enamel maturation can be visualized at the surface of the rat incisor by staining with glyoxal bis(2-hydroxyanil) (GBHA) and radioautography following 45calcium injection. In this study, the effects of vinblastine on enamel maturation were monitored by these two methods. At 4 h after injection of vinblastine, the darkly-stained GBHA bands had widened incisally into the interband regions when compared to normal, control teeth. Radioautography at 5 min after calcium injection in vinblastine-treated animals (4 h) showed a modified maturation pattern of weaker labeling and less distinct banding. At 8 h after vinblastine injection, most of the enamel stained uniformly with GBHA, and bands and interband regions could not be resolved. Radioautography at 5 min after calcium injection showed that the 8 h vinblastine treatment removed the banding pattern, leaving only a weakly-labeled area. Vinblastine is known to destroy and prevent the formation and turnover of microtubules, and hence the formation of ruffled borders of ruffle-ended ameloblasts (Akita et al. 1983). The concomitant decrease in calcium incorporation implies that events taking place in relation to the ruffled border may affect calcium exchange or accretion within the enamel.

Effects of various agents on staining of the maturation pattern at the surface of rat incisor enamel

In the maturation zone, two types of ameloblasts are arranged as bands across the rat incisor; these corresponded with a staining pattern at the surface which reflected the alternating pattern of ruffle-ended and smooth-ended ameloblasts. PAS stain showed bands and stripes similar to those following glyoxal bis(2-hydroxyanil) (GBHA) staining; these stains visualize the organic (PAS) and inorganic (GBHA) components of the maturation pattern. To further elucidate the nature of these bands, dissected rat incisors were treated with various agents prior to staining with GBHA or PAS. Guanidine for 2 h at room temperature showed no maturation pattern when stained with GBHA, as did teeth treated with EDTA and a bisophosphonate (HEBP). Hydrochloric acid and nitric acid removed the layer of outer enamel and incisors did not stain with GBHA, suggesting that the staining is a surface-related phenomenon. As staining was abolished by either the removal of mineral (EDTA) or protein (guanidine), the concurrent localization of non-crystal-bound calcium by GBHA staining, and of glycoprotein by PAS staining, indicates that calcium is associated with glycoprotein at the surface of the enamel.

The pyroantimonate reaction and transcellular transport of calcium in rat molar enamel organs

The distribution of calcium in the cells of the enamel organ of developing rat molar tooth germs was studied by the pyroantimonate method. It was found that there was a specific localization to the inner leaflet of the plasma membrane of both secretory and maturation phase ameloblasts. This information can be used to support the model for transcellular transport of calcium involving membrane fluidity, with phosphatidylserine as a carrier (Reith 1983). It can also support an alternative model involving movement of calcium ions over a surface of acidic phospholipids on the inner leaflet of the plasma membrane, without involving the necessity for membrane fluidity.

Microprobe analysis of calcifying matrices and formative cells in developing mouse molars

The distribution of Calcium and Phosphorus and of Na, K, S and Cl was studied in the mineralizing matrices and strata of ameloblasts and odontoblasts in developing mouse molars (5-14 days). Sections cut in a cryostat were prepared by freeze-drying and examined in an SEM by the method of energy dispersive x-ray analysis. In enamel a gradient of mineralization was observed with respect to age and topography. Progesssive loss of sulfur was also demonstrated. Less striking mineralization gradients were found in dentin. Predentin accumulated Ca at a concentration about 2% that of dentin and the Ca/P ratio was lower than that for apatite. Significant concentrations of calcium were localized in ameloblast and odontoblast strata. The concentration increased five-fold in ameloblasts as the cells matured and enamel mineralization entered the final phases, levels in odontoblasts remained stable. With age in both cellular strata, potassium counts decreased. In maturing ameloblasts the concentrations of sodium and chloride rose.

The association of amorphous mineral deposits with the plasma membrane of pre- and young odontoblasts and their relationship to the origin of dentinal matrix vesicles in rat incisor teeth

Young and preodontoblasts and matrix vesicles which occur in the presecretory region of incisor teeth of growing rats were examined in stained and unstained ultrathin sections in order to characterize sites involved in the initial mineralization of dentin. Common to pre- and young odontoblasts in the presecretory region were hemispherical membrane-associated amorphous densities, measuring 5-35 nm in diameter after fixation in glutaraldehyde-osmium tetroxide or glutaraldehyde only. Amorphous densities were associated also with the limiting membranes of some vesicles in the extracellular matrix. Other vesicles in the extracellular matrix contained needle-like crystalline deposits typical of dentinal matrix vesicles. Fully differentiated odontoblasts in more incisal regions of the tooth lacked plasma membrane-associated amorphous densities. Neither amorphous nor crystalline densities were associated with any other cellular or subcellular structures in cells of the presecretory region. Flotation of ultrathin sections on solutions of EDTA or EGTA removed the amorphous densities from the plasma membranes, suggesting that the amorphous densities are calcium-containing mineral deposits. Amorphous deposits were associated with the membrane of vesicular structures protruding from the surfaces of pre- and young odontoblasts, suggesting that vesicles found in the extracellular matrix arise by budding from the plasma membranes of pre- and young odontoblasts. The occurrence of amorphous mineral deposits in association with the limiting membrane of some vesicles in the extracellular matrix, and the occurrence of needle-like mineral crystals within other matrix vesicles, suggest that an amorphous-to-crystalline phase transformation of mineral takes place within the matrix vesicle. The results of this study suggest that calcium-binding sites associated with plasma membranes of pre- and young odontoblasts act as nucleating centers for primary mineral deposition in tooth dentin.

Calcium transport and the secretory ameloblast

The distribution of calcium in the enamel organ of the rat incisor was investigated using potassium pyroantimonate for ultrastructural localization of calcium. Substantial amounts of precipitate occurred in the intercellular compartment of the enamel organ and modest deposits were observed in specific organelles of the secretory ameloblast. Mitochondria, nuclei granular endoplasmic reticulum, Golgi vesicles and secretory granules consistently contained small deposits of pyroantimonate. Complexing of calcium by the pyroantimonate was confirmed by EGTA decalcification and scanning electron microscope energy dispersive X-ray analysis. The observed distribution is discussed in light of potential for an intercellular pathway of calcium transport as well as controlled movement of the ion along the synthetic and secretory route followed by organic components of enamel.

Tooth enamel: current state of the art

Important progress has been made relative to the growth, structure and function of enamel. Better understanding of the epithelial mesenchymal interactions during odontogenesis has been gained through tissue culture, and the predominant role of the dental papilla has been established. Differences between rodent and human amelogenesis have been demonstrated. With radioautography and cytochemistry, a significant amount of new information has been obtained on the metabolism of the ameloblasts, concerning the synthesis of proteins, glycoproteins and proteoglycans, as well as calcium transport. Numerous biochemical investigations have been devoted to developing and mature enamel matrix. The organic components of human adult enamel are mainly constituted of lipids and proteins, but further investigations are still needed to elucidate their precise nature. The so-called key-hole configuration of adult enamel can be questioned when amelogenesis is considered since the tissue does not develop in a prismatic head-tail fashion. The most important results have probably been obtained in the field of individual enamel apatite crystals shape and ultrastructure as well as in the description of the precise patterns of their carious dissolution which bears great similarities to the dissolution of synthetic apatites in acids.

Fluoride-induced mineralization within vacuoles in maturative ameloblasts of the rat

Dense crystalline deposits appeared within vacuoles in rat maturative ameloblasts as a result of repeated injections of sodium fluoride. The crystals assumed varied arrangements but were always observed within intracellular vacuoles. The crystals resemble those of normal enamel and resist microincineration. They are readily dissolved by decalcification and leave behind an organic framework which matches the outline of the crystals. An experimental model is presented which may be useful in further studies of calcium transport, enamel matrix absorption or digestion of cellular debris.

Histochemical and electron probe analysis of secretory ameloblasts of developing rat molar teeth

Calcium was not found in secretory ameloblasts and stratum intermedium cells when treated with OsO4-pyroantimonate or when surfaces prepared by fracturing fresh, rapidly frozen, developing molar tooth germs were subject to electron probe X-ray analysis. Pyroantimonate reaction product, considered to be calcium, was found in mitochondria of enamel organ cells which were first placed in a bath containing calcium and potassium. The plasma membrane was disrupted in cells ehich showed mitochondrial localization of reaction product. The results provide no data which indicates that enamel organ cells have a direct, active role in the movement of calcium into the enamel. Rather, it is suggested that the secretory enamel organ might serve as a selective barrier in regulating the initial mineralization of enamel.

In vitro study of cellular influence on 45Ca uptake in developing rat enamel

The in vitro method for culture of molar teeth from eight-day-old rats, as reported in this study, appeared to sustain reasonably normal activity in the cells of the enamel organ and pulp through culture periods of four to eight hours. Inhibition of metabolic activity in the explants by addition of 5 mM iodoacetate or 2,4-dinitrophenol to the culture medium, or by heating at 70 C for 10 minutes, did not appear to affect the intensity or pattern of 45Ca uptake in the more advanced, rapidly mineralizing areas of the enamel. Neither did stripping of the enamel organ from the surface of the enamel have a demonstrable effect in those areas. However, metabolic inhibition with 2,4-dinitrophenol, heat killing or stripping of the enamel organ resulted in increased 45Ca uptake in newly formed enamel adjacent to the secreting ameloblasts. It is hypothesized that calcium flux into newly formed enamel matrix is controlled, in part, by movement of the calcium, which diffuses between the ameloblasts toward the enamel surface, away from the enamel through the ameloblasts.

Qualitative electron probe analysis of secretory ameloblasts and odontoblasts in the rat incisor

Rapidly frozen growing rat incisors were freeze fractured and freeze dried in preparation for energy dispersive X-ray emission microanalysis in a scanning electron microscope. Ca levels were found to be elevated in the distal cell body of odontoblasts, whereas Ca was uniformly low over all parts of the cell body of secretory ameloblasts. The results suggest fundamental differences in the mechanisms by which these two cell types process Ca, and that Ca possibly diffuses through the secretory ameloblast layer on its way to the enamel.

[Transfer of 45Ca during amelogenesis studied by autoradiography and electron microscopy]

45Ca transfer through the stratum intermedium and the secreting ameloblasts towards enamel has been studied by quantitative electron microscopical autoradiography in tooth-germs of newborn cats following intravenous injection of the isotope. Two transfer pathways were demonstrated. The relatively more important direct path passed through the stratum intermedium and ameloblast intercellular spaces and reached the enamel directly. The second pathway consisted in an intracellular transfer through the ameloblasts. 45Ca penetrated the cell through its basal pole. The mitochondria were the most highly labeled organelles at the different experimental time intervals studied. A maximum of radioactivity was respectively noticed at 30 min and 1 h in the endoplasmic reticulum and the Golgi apparatus. A total absence of silver grains was noted over the secretory ameloblastic bodies. At 6 h, the highest labeling was observed over enamel and especailly over the inner enamel along the enameldentin junction.