Linde A
Department of Oral Biochemistry, Faculty of Odontology, Gothenburg University, Sweden.
Anat Rec. 1989 Jun;224(2):154-66. doi: 10.1002/ar.1092240206.
Dentin may be regarded as a mineralized connective tissue. In its composition as well as its mode of formation, dentin exhibits several similarities with bone, but also definite differences. The dentin organic phase, the matrix, determines its morphology and is believed to be instrumental in the formation of the mineral phase. A fibrous web of collagen type I dominates the organic matrix. Also, minor amounts of other collagen types may be present. The noncollagenous proteins (NCPs), which constitute about 10% of the matrix, fall into several categories: phosphoproteins, Gla-proteins of the osteocalcin type as well as matrix Gla-protein, proteoglycans, different acidic glycoproteins, and serum proteins. Some of these NCPs have unique chemical compositions that give them specific properties. Dentinogenesis occurs by two simultaneous processes: the formation of a collagenous web in predentin, which is followed by the formation of the inorganic phase at the mineralization front. The composition of the predentin organic matrix differs from that of dentin, as some NCP components are secreted extracellularly just in advance of the mineralization front. In addition, some constituents of predentin seem to be metabolized. The NCPs may be important to several processes during dentinogenesis. Much evidence indicates that noncollagenous components in the matrix are instrumental in mineral formation. New data show that polyanionic NCPs, such as phosphoprotein and proteoglycans, when immobilized on a solid support, induce apatite formation under physiological conditions. These data indicate that polyanionic NCPs may function as mineral nucleators in vivo. They may also act as size and rate regulators for crystallization and promote calcium ion diffusion in the tissue. In addition, NCPs may regulate collagen fibrillogenesis.
牙本质可被视为一种矿化的结缔组织。在其组成以及形成方式上,牙本质与骨表现出一些相似之处,但也存在明显差异。牙本质有机相即基质,决定了其形态,并且被认为在矿化相的形成中起重要作用。I型胶原纤维网在有机基质中占主导地位。此外,可能还存在少量其他类型的胶原。非胶原蛋白(NCPs)约占基质的10%,可分为几类:磷蛋白、骨钙素类型的Gla蛋白以及基质Gla蛋白、蛋白聚糖、不同的酸性糖蛋白和血清蛋白。其中一些NCPs具有独特的化学组成,赋予它们特定的性质。牙本质形成通过两个同时进行的过程发生:前期牙本质中胶原网的形成,随后在矿化前沿形成无机相。前期牙本质有机基质的组成与牙本质不同,因为一些NCP成分在矿化前沿之前就被分泌到细胞外。此外,前期牙本质的一些成分似乎会被代谢。NCPs在牙本质形成过程中的几个过程中可能很重要。许多证据表明,基质中的非胶原成分在矿物质形成中起重要作用。新数据表明,多阴离子NCPs,如磷蛋白和蛋白聚糖,当固定在固体支持物上时,在生理条件下可诱导磷灰石形成。这些数据表明,多阴离子NCPs可能在体内作为矿物成核剂发挥作用。它们还可能作为结晶的大小和速率调节剂,并促进钙离子在组织中的扩散。此外,NCPs可能调节胶原纤维形成。