Mechanisms of mineralization in the enameloid of elasmobranchs and teleosts

Ultrastructural and cytochemical studies on the mineralization of enameloid were performed using Heterodontus japonicus, an elasmobranch, and Tilapia buttikoferi, a teleost as materials. The mineralization of the enameloid in the Heterodontus was divided into the following two steps: (1) initial crystallization in the tubular vesicles that originated from the odontoblasts, and (2) crystal growth that was accompanied by the degeneration and removal of the organic matrix around the crystals. In the Tilapia, the mineralization of the cap enameloid followed three steps: (1) initial crystallization at the matrix vesicles, (2) aggregation of fine slender crystals along collagen fibrils, and (3) crystal growth with the degeneration and removal of the organic matrix. The pattern of early mineralization and the composition of organic matrix in enameloid were considerably different between the two species examined, while in both species the odontoblasts were mainly involved in the formation of the organic matrix of enameloid and in the initial mineralization. In the next step, remarkable crystal growth associated with the degeneration and removal of the organic matrix occurred in both the elasmobranch and the teleost species. The absorptive functions of the dental epithelial cells in the later stages of enameloid formation is probably similar in the two types of enameloid, and is essential for the production of well-mineralized enameloid.     

Ultrastructure of odontogenic cells during enameloid matrix synthesis in tooth buds from an elasmobranch,Raja erinacae

The ultrastructure of the inner epithelial cells (IDE) and odontoblasts in elasmobranch (Raja erinacae) tooth buds was investigated by transmission electron microscopy to determine what contribution each cell type makes to the forming enameloid matrix. Row II, early stage, IDE cells contained few organelles associated with protein synthesis, whereas preodontoblasts appeared competent to initiate extracellular matrix production. Row III IDE cells are also devoid of organelles related to secretory protein synthesis, although these IDE cells accumulated large pools of intracellular glycogen. The glycogen appeared to be packaged into vesicles and exocytosed into the lateral extracellular space toward the forming enameloid matrix. Row III odontoblasts had a morphology consistent with an active protein secretory cell. No procollagen granules were present within the odontoblasts, however, nor were many collagen fibers observed in the enameloid matrix. Instead, non-collagenous “giant” fibers having 17.5-nm periodic cross striations were associated with the imaginations of odontoblast cell processes. Giant fibers, which spanned a clear zone adjacent to the odontoblasts, terminated within the enameloid matrix. Smaller 25-nm-wide “unit” fibers emanated from the giant fiber tips to form the bulk of the enameloid matrix. The clear zone, which separated the odontoblasts from the enameloid matrix at early stages, diminished in size at later stages until the odontoblast processes were completely embedded in the enameloid matrix. Nascent enameloid crystallites were observed only after a layer of unmineralized predentin was deposited beneath fully formed enameloid matrix. The results suggest that the major constituent of the enameloid matrix in skates is a non-collagenous protein derived from the odontoblasts. The inner dental epithelial cells appear to contribute large quantities of carbohydrates to the forming enameloid matrix.     

Fine structure of dental epithelial cells and the enameloid during the enameloid formation stages in an elasmobranch, Heterodontus japonicus

The structural features of the dental epithelial cells and the enameloid in tooth germs of the Japanese Port Jackson shark, Heterodontus japonicus, in the stages of enameloid formation, were investigated by light and transmission electron microscopy. At the enameloid matrix-formation stage, tall columnar inner dental epithelial cells contained large numbers of glycogen particles. At the enameloid mineralization stage, when many sharply outlined crystals appeared throughout the enameloid, the inner dental epithelial cells exhibited well-developed Golgi apparatuses and many mitochondria in the proximal cytoplasm, and abundant vesicles and vacuoles in the distal cytoplasm. Marked interdigitations of the lateral membrane were visible in the inner dental epithelial cells. The outer dental epithelial cells contained many mitochondria, lysosomal bodies, vesicles and microtubules, and the capillaries usually approached the outer dental epithelial cells. At the enameloid maturation stage, large numbers of crystals occupied the enameloid, and most of the organic matrix had disappeared from the enameloid area after demineralization. The organelles in the inner and outer dental epithelial cells decreased in number, but there were still widely distributed Golgi apparatuses, abundant intermediate filaments and granules containing an electron-dense substance in the inner dental epithelial cells. It is probable that the dental epithelial cells are involved in the removal of organic matrix from the enameloid and in the process of mineralization at the later stages of enameloid formation, i.e., the mineralization and the maturation stages.     

Fine structure of dental epithelial cells and the enameloid during the enameloid formation stages in an elasmobranch, Heterodontus japonicus

The structural features of the dental epithelial cells and the enameloid in tooth germs of the Japanese Port Jackson shark, Heterodontus japonicus, in the stages of enameloid formation, were investigated by light and transmission electron microscopy. At the enameloid matrix-formation stage, tall columnar inner dental epithelial cells contained large numbers of glycogen particles. At the enameloid mineralization stage, when many sharply outlined crystals appeared throughout the enameloid, the inner dental epithelial cells exhibited well-developed Golgi apparatuses and many mitochondria in the proximal cytoplasm, and abundant vesicles and vacuoles in the distal cytoplasm. Marked interdigitations of the lateral membrane were visible in the inner dental epithelial cells. The outer dental epithelial cells contained many mitochondria, lysosomal bodies, vesicles and microtubules, and the capillaries usually approached the outer dental epithelial cells. At the enameloid maturation stage, large numbers of crystals occupied the enameloid, and most of the organic matrix had disappeared from the enameloid area after demineralization. The organelles in the inner and outer dental epithelial cells decreased in number, but there were still widely distributed Golgi apparatuses, abundant intermediate filaments and granules containing an electron-dense substance in the inner dental epithelial cells. It is probable that the dental epithelial cells are involved in the removal of organic matrix from the enameloid and in the process of mineralization at the later stages of enameloid formation, i.e., the mineralization and the maturation stages.     

The structure and development of the collar enameloid in two teleost fishes, Halichoeres poecilopterus and Pagrus major

Summary Histologically the outer layer of the collar enameloid obviously differs from the inner layer, and it has a degree of mineralization nearly as high as the cap enameloid which has the highest. In the stage of matrix formation, the organic matrix of the collar enameloid contains a number of collagen fibers, and odontoblasts display features suggesting that these cells actively synthesized and secreted collagen. A number of cell processes, matrix vesicles and some cell debris which were probably derived from the odontoblasts were observed in the organic matrix of the collar enameloid. We consider that the majority of the organic matrix in collar enameloid originates from the odontoblasts. In the stage of maturation, collagen fibers were not observed in the outer layer of the collar enameloid in demineralized specimens. In the IDE cells during this stage, the complex infoldings of cell membranes developed in the distal portion, and several lysosomal granules and irregular-shaped granules containing many tubular structures, were observed in the distal cytoplasm. In the ODE cells, abundant labyrinthine canals appeared in the cytoplasm, and capillary vessels were found close to the outer surface of the ODE cells. We assume that the higher mineralized outer layer of the collar enameloid is made possible by the absorptive and transport functions of the epithelial cells during the stage of maturation. It is considered that the collar enameloid in this study was initially produced by the odontoblasts and then reconstructed by the epithelial cells, so that the collar enameloid differs from true enamel.     

The effects of colchicine on the ultrastructure of odontogenic cells in the common skate,Raja erinacae

Ultrastructural alterations in duced by colchicine were investigated to determine the secretory activities of odontogenic cells during formation of tooth enameloid matrix in skates. Treated skate inner dental epithelial (IDE) cells did not display dilated cisternae of the granular endoplasmic reticulum (GER) nor accumulate Golgi-associated secretory granules at any dose level or time interval examined. This response was markedly different from that observed in teleost IDE cells synthesizing the enameloid collagen matrix. Treated skate IDE cells did show increased accumulations of glycogencontaining vesicles and intercellular glycogen associated with amorphous material, compared to controls. Additionally, the aberrant occurrence of large intracellular glycogen pools and amorphous material suggested that carbohydrate processing was a major function of skate IDE cells. Treated odontoblasts associated with enameloid matrix formation sometimes showed dilated GER cisternae, but procollagen secretory granules were not obsered. Instead, electron dense material was present within the Golgi cisternae, tubular granules, and large granules. Some elecron-dense material appeared to be shunted to a resorptive pathway via multivesicular bodies in treated odontoblasts. The continuity of tubular granules with the enameloid matrix suggested that they contained precursors of the enameloid matrix, and possibly the periodic, 17.5-nm crossstriated, “giant” fibers. Treated odontoblasts associated with predentin collagen matrix deposition showed dilated GER cisternae and accumulations of procollagen secretory granules, features consistent with the function of active collagen synthesis and secretion. The findings indicate that (1) skate IDE cells do not synthesize enameloid collagen as found in bony fish tooth development; (2) skate IDE cells do process glycogen for secretion into the enameloid matrix; (3) collagen, although present, is not a major constituent of skate enameloid matrix; (4) enameloid “giant” fibers are unique to elasmobranchs; and (5) odontoblasts synthesize and secrete proteins other than collagen into the enameloid matrix.     

Immunolocalization of enamel matrix protein-like proteins in the tooth enameloid of spotted gar,Lepisosteus oculatus,an actinopterygian bony fish

Enameloid is a well-mineralized tissue covering the tooth surface in fish and it corresponds to the outer-most layer of dentin. It was reported that both dental epithelial cells and odontoblasts are involved in the formation of enameloid. Nevertheless, the localization and timing of secretion of ectodermal enamel matrix proteins in enameloid are unclear. In the present study, the enameloid matrix during the stages of enameloid formation in spotted gar, Lepisosteus oculatus, an actinopterygian, was examined mainly by transmission electron microscopy-based immunohistochemistry using an anti-mammalian amelogenin antibody and antiserum. Positive immunoreactivity with the antibody and antiserum was found in enameloid from the surface to the dentin-enameloid junction just before the formation of crystallites. This immunoreactivity disappeared rapidly before the full appearance of crystallites in the enameloid during the stage of mineralization. Immunolabelling was usually found along the collagen fibrils but was not seen on the electron-dense fibrous structures, which were probably derived from matrix vesicles in the previous stage. In inner dental epithelial cells, the granules in the distal cytoplasm often showed positive immunoreactivity, suggesting that the enamel matrix protein-like proteins originated from inner dental epithelial cells. Enamel matrix protein-like proteins in the enameloid matrix might be common to the enamel matrix protein-like proteins previously reported in the collar enamel of teeth and ganoine of ganoid scales, because they exhibited marked immunoreactivity with the same anti-mammalian amelogenin antibodies. It is likely that enamel matrix protein-like proteins are involved in the formation of crystallites along collagen fibrils in enameloid.     

Fine structural and cytochemical observations on the dental epithelial cells during cap enameloid formation stages in Polypterus senegalus, a bony fish (Actinopterygii)

Tooth germs during cap enameloid formation stages in Polypterus senegalus were investigated by transmission electron microscopy and enzyme histo- and cytochemistry. Enameloid formation was divided into three stages: matrix formation, mineralization, and maturation. The enamel organ consisted of the inner dental epithelial cells, stellate reticulum, and outer dental epithelial cells during cap enameloid formation stages, but no stratum intermedium was found. During the matrix formation stage, the tall inner dental epithelial cells contained well-developed Golgi apparatus, abundant cisternae of rough endoplasmic reticulum and mitochondria. Spindle-shaped vesicles containing a filamentous structure were seen in the distal cytoplasm. During mineralization and maturation stages, many ACPase positive lysosomes were present in the cytoplasm, whereas the organelles were decreased in number. The infoldings of the distal plasma membrane of the inner dental epithelial cells were visible in the mineralization stage but were not marked in the maturation stage. The activity of nonspecific ALPase, Ca-ATPase, and K-NPPase was detected at the plasma membrane of the inner dental epithelial cells during the stages of mineralization and maturation. The results of fine structure and enzyme cytochemistry suggested that the dental epithelial cells were mainly involved in the degeneration and removal of enameloid matrix and in material transportation during the enameloid mineralization and maturation stages, rather than in the enameloid matrix formation. The results also showed that the structure of the dental epithelial cells in Polypterus was different from that in teleosts and gars, but that the function of the dental epithelial cells was similar to that in teleosts possessing well-mineralized cap enameloid.     

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.     

Fine structure of the cap enameloid and of the dental epithelial cells during enameloid mineralisation and early maturation stages in the tilapia, a teleost

Morphological features of the cap enameloid and dental epithelial cells were investigated by light and transmission electron microscopy during the various stages of enameloid mineralisation and early maturation in the tilapia. The pattern of mineralisation along collagen fibrils in the enameloid differed from that in the dentine. Many matrix vesicles were found in the predentine and in the enameloid, suggesting that they may be involved in the initial mineralisation in both regions. Most of the organic matrix disappeared from the cap enameloid during mineralisation and maturation. The disappearance of the organic matrix could be divided into 2 stages. Initially a fine network-like matrix, which probably consisted of glycosaminoglycans and extended between collagen fibrils, began to disappear. At the same time, fine crystallites and electron-dense, fine granular material covered the collagen fibrils as mineralisation of the enameloid began. In the second stage, the maturation of the enameloid, the collagen fibrils degenerated completely and disappeared from the cap enameloid, being replaced by large numbers of large crystals. At the mineralisation stage, the numbers of lysosomal bodies tended to increase in the inner dental epithelial (IDE) cells, which contained a well developed Golgi apparatus and rough endoplasmic reticulum (rER). At the early stage of maturation, a ruffled border was noted at the distal ends of the IDE cells, which contained many mitochondria and lysosomal bodies, but less rER. These features suggest that the cells actively absorb the organic matrix, which includes collagen fibrils, in the cap enameloid. The outer dental epithelial (ODE) cells were translucent cells that contained well developed labyrinthine canalicular spaces from the onset of the mineralisation stage to the middle stage of maturation. The IDE and ODE cells were clearly involved in the mineralisation of the cap enameloid at the mineralisation and maturation stages.     

Mechanism of mineral formation in bone

The mechanism of mineral formation in bone is seen best where active new bone formation is occurring, e.g., in newly forming subperiosteal bone of the embryo, in the growing bone of young animals, and in healing rickets where the calcification process in osteoid is reactivated. A large body of ultrastructural evidence, using conventional and anhydrous methods for tissue preparation, has shown convincingly that extracellular matrix vesicles are present at or near the mineralization front in all of the above, and that these vesicles are the initial site of apatite mineral deposition. Thus bone resembles growth plate cartilage, predentin, and turkey tendon in having calcification initiated by matrix vesicles. Once the calcification cascade is begun, matrix vesicles are no longer needed to support mineralization and are consumed by the advancing mineralization front in which performed crystals serve as nuclei for the formation of new crystals. The rate of crystal proliferation is promoted by the availability of Ca2+, PO4(3-), and the presence of collagen, and retarded by naturally occurring inhibitors of mineralization such as proteoglycans and several noncollagenous calcium-binding proteins of bone including bone-Gla protein (osteocalcin), phosphoproteins, osteonectin, and alpha-2HS-glycoproteins. New electron microscopic immunocytochemical findings in our laboratory suggest that the origin of alkaline phosphatase-positive bone matrix vesicles is polarized to the mineral-facing side of osteoblasts and may be concentrated near the intercellular junctions of human embryonic osteoblasts.     

Evidence of Two Types of Odontoblasts during Dentinogenesis in Elasmobranchs

The fine structure of the odontoblasts in the sting rays, Dasyatis akajei Dasyatidae, and Urolophus aurantiacus Urolophidae, was examined using light and transmission electron microscopy. In the dentinogenesis stage, the odontoblasts have been classified into two types, that is, dark cells and light cells, based on differences in their fine structure. Many dark odontoblasts found along the predentine displayed well-developed organelles with secretory activity around the nuclei. They contained large amounts of expanded rER, widely distributed Golgi apparatus and secretory granules. In contrast, light odontoblasts showed a relatively clear cytoplasm and extended long processes which passed through the predentine and penetrated into the dentine. They contained large numbers of microtubules in the processes and many mitochondria around the nuclei. It is suggested that the light odontoblasts play an important part in material transport to the dentine and/or act as a sensory organ of the tooth. The dark odontoblasts seem to produce the organic matrix of the dentine and to prepare for mineralization in the dentine.     

Studies on dentinogenesis in the rat

Summary The fine structure of differentiating odontoblasts and predentin in the rat was investigated. The cells gradually acquired a prominent endoplasmic reticulum and Golgi complex, indicative of a synthesizing capacity. Specific cytoplasmic bodies abounded within the Golgi area and the apical cell body regions of maturing odontoblasts. The possibility that such structures may be an expression of a transport and discharge mechanism for cellular products, e.g. collagen precursors is discussed.In initial stages of dentin formation, dentinal glubles were observed in the predentin. Furthermore, needle-like crystallites appeared within these globules before apatite crystals were observed in the predentin matrix. It is proposed that these globules are intimately related to initial predentin mineralization. In calcification at later stages of dentinogenesis no such globular elements are involved.     

Initial intramembraneous osteogenesis in vitro

Calvariae of fetal mice 12 to 13 days in utero were placed in Rose chambers and cultured in BGJb medium supplemented with 20% fetal calf serum and antibiotics. After periods of 7 and 12 days, the explants were harvested and processed for light and electron microscopy. The mesenchymal cells, after a brief lag time, differentiated into osteoblasts which produced woven bone. Light and electron microscopic observations showed that in vitro, as well as in vivo, growth and development share all of the same characteristics of initial intramembraneous osteogenesis: (1) migration and differentiation of mesenchymal cells into osteoblasts, (2) the subsequent appearance of matrix vesicles in the extra-cellular space, (3) crystallization of hydroxyapatite within and about these vesicles, (4) growth of hydroxyapatite crystals into spheroidal nodules of bone, and (5) the subsequent fusion of these nodules into seams of woven bone. Thus cellular involvement in initial osteogenesis has been observed in a system where differentiation into osteoblasts and initial calcification takes place in vitro, suggesting that the events responsible for these phenomena have occurred within the cells prior to their morphological differentiation.     

Biomineralization and matrix vesicles in biology and pathology

In normal healthy individuals, mineral formation is restricted to specialized tissues which form the skeleton and the dentition. Within these tissues, mineral formation is tightly controlled both in growth and development and in normal adult life. The mechanism of calcification in skeletal and dental tissues has been under investigation for a considerable period. One feature common to almost all of these normal mineralization mechanisms is the elaboration of matrix vesicles, small (20–200 nm) membrane particles, which bud off from the plasma membrane of mineralizing cells and are released into the pre-mineralized organic matrix. The first crystals which form on this organic matrix are seen in and around matrix vesicles. Pathologic ectopic mineralization is seen in a number of human genetic and acquired diseases, including calcification of joint cartilage resulting in osteoarthritis and mineralization of the cardiovasculature resulting in exacerbation of atherosclerosis and blockage of blood vessels. Surprisingly, increasing evidence supports the contention that the mechanisms of soft tissue calcification are similar to those seen in normal skeletal development. In particular, matrix vesicle-like membranes are observed in a number of ectopic calcifications. The purpose of this review is to describe how matrix vesicles function in normal mineral formation and review the evidence for their participation in pathologic calcification.     

Biomineralization in modern avian calcified eggshells: similarity versus diversity

ABSTRACT

Avian eggshells are composed of several layers made of organic compounds and a mineral phase (calcite), and the general structure is basically the same in all species. A comparison of the structure, crystallography, and chemical composition shows that despite an overall similarity, each species has its own structure, crystallinity, and composition. Eggshells are a perfect example of the crystallographic versus biological concept of the formation and growth mechanisms of calcareous biominerals: the spherulitic—columnar structure is described as “a typical case of competitive crystal growth”, but it is also said that the eggshell matrix components regulate eggshell mineralization. Electron back scattered diffraction (EBSD) analyses show that the crystallinity differs between different species. Nevertheless, the three layers are composed of rounded granules, and neither facets nor angles are visible. In-situ analyses show the heterogeneous distribution of chemical elements throughout the thickness of single eggshell. The presence of organic matrices other than the outer and inner membranes in eggshells is confirmed by thermograms and infrared spectrometry, and the differences in quality and quantity depend on the species. Thus, as in other biocrystals, crystal growth competition is not enough to explain these differences, and there is a strong biological control of the eggshell secretion.     

Dentin Matrix Proteins and Dentinogenesis

The precise mechanisms involved in dentinogenesis are not understood; however, the information to date suggests that a number of highly controlled extracellular events are involved. Mature odontoblasts secrete collagen at the cell border into predentin. They synthesize and secrete other non-collagenous proteins (NCPs) at the mineralization front, possibly through odontoblastic processes. A collagen-NCP complex is formed at the predentin-dentin border and apatite crystal initiation and growth takes place. One of the research needs is to uncover the nature of this dentin collagen-NCP complex and to understand how it controls mineralization. At least three dentin specific NCPs are known: phosphophoryn(s), dentin sialoprotein (DSP) and AG1 (Dmp1). Other macromolecules are commonly made by osteoblasts and odontoblasts and participate in bone and dentin formation.

Some progress in understanding dentin mineralization has been gained by focusing upon the role of phosphophoryns. These highly phosphorylated proteins are secreted at the mineralization front, where a small portion binds in the gap region of type I collagen fibrils. This portion of phosphoproteins probably initiates formation of plate-like apatite crystals. Additional phosphophoryns in higher concentrations bind to the growing apatite crystals and slow their growth, possibly influencing their size and shape.

Other areas which need careful investigations are those involving the mechanisms involved in odontoblast differentiation, how the synthesis of the dentin specific NCPs is controlled and the precise roles of these macromolecules in dentinogenesis. Future experimentation will focus on the gene structures for these NCPs and the mechanisms of tissue specific gene regulation. Tests for function can then be pursued in “gene knockout” experiments. There is no doubt that current “new” scientific approaches being utilized to answer many scientific questions in other fields will greatly impact our ability to answer the questions surrounding the process of dentinogenesis.     

Nucleation and growth of aragonite crystals at the growth front of nacres in pearl oyster,Pinctada fucata

The growth front of nacreous layer, which lies just above the outer prismatic layer, is one of the crucial areas to comprehend the formation of nacreous aragonite. The crystallographic properties of aragonite crystals at the growth front in pearl oyster, Pinctada fucata, were investigated using scanning electron microscopy with electron back-scattered diffraction, and transmission electron microscopy with focused ion beam sample preparation technique. Nano-sized aragonite crystals nucleate with random crystallographic orientation inside the dimples on the surface of the organic matrix that covers the outer prismatic columns. The dimples are filled with horn-like aragonite crystals, which enlarge from the bottom to the upper surface to form hemispheric domes. The domes grow concentrically and coalesce together to become the initial nacreous layer. The c-axes of aragonite at the top surface of the domes are preferentially oriented perpendicular to the surface. The horn-like aragonite and its crystallographic orientation are probably attained by geometrical selection with the fastest growth rate of aragonite along the c-axis, until organic sheets are continuously formed and interrupt the crystal growth of aragonite. The further crystal growth along the shell thickness is attained via mineral bridges through discontinuity or holes in the organic sheets. These results indicate that the crystal growth of aragonite at the growth front results from not only biotic process but also inorganic ones such as geometrical selection and mineral bridges.     

Dentin Mineralization and the Role of Odontoblasts in Calcium Transport

Dentin is formed by two simultaneous processes, in which the odontoblasts are instrumental—the formation of the collagenous matrix, and mineral crystal formation in this matrix. This pattern of formation is similar to that of bone, another mineralized connective tissue. Dentin and bone also have chemical compositions which are similar but with distinct differences. It is of fundamental importance to understand how the ions constituting the inorganic phase are transported from the circulation to the site of mineral formation and how this transport is regulated. For dentinogenesis, calcium is essentially the only ion for which data are available. Recent evidence suggests that a major portion of the Ca²⁺ ions are transported by a transcellular route, thus being under cellular control. The cells maintain a delicate Ca²⁺ ion balance by the concerted action of transmembraneous transport mechanisms, including Ca-ATPase, Na⁺/Ca²⁺ exchangers and calcium channels, and of intracellular Ca²⁺-binding proteins. The net effect of this is a maintenance of a sub-micromolar intracellular Ca²⁺ activity, and an extracellular accumulation of Ca²⁺ ions in predentin, at the mineralization front. Predentin can be regarded as a zone of formation and maturation of the scaffolding collagen web of the dentin organic matrix. In addition to collagen, it contains little but proteoglycan. Simultaneous with mineral formation, additional non-collagenous macromolecules are added to the extracellular matrix of dentin, these presumably being transported within the odontoblast process. Among these are highly phosphorylated dentin phosphoprotein (phospho-phoryn) and another pool of proteoglycan. The functionality of this may be explained by the fact that polyanionic macromolecules are capable of inducing the formation of hydroxyapatite at ionic conditions resembling those in vivo. They can also inhibit mineral growth and regulate crystal size.