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无定形矿物质沉积与大鼠切牙中前期及年轻成牙本质细胞的质膜的关联及其与牙本质基质小泡起源的关系。

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.

作者信息

AlMuddaris M F, Dougherty W J

出版信息

Am J Anat. 1979 Jun;155(2):223-44. doi: 10.1002/aja.1001550206.

Abstract

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.

摘要

为了确定参与牙本质初始矿化的部位,对生长中大鼠切牙分泌前期区域的年轻成牙本质细胞和前成牙本质细胞以及基质小泡进行了染色和未染色超薄切片检查。在分泌前期区域,前成牙本质细胞和年轻成牙本质细胞共有的特征是存在与膜相关的半球形无定形致密物,在经戊二醛-四氧化锇或仅用戊二醛固定后,其直径为5-35纳米。无定形致密物也与细胞外基质中一些小泡的界膜相关。细胞外基质中的其他小泡含有牙本质基质小泡特有的针状晶体沉积物。在牙齿更切端区域完全分化的成牙本质细胞缺乏与质膜相关的无定形致密物。在分泌前期区域的细胞中,无定形和晶体致密物均与任何其他细胞或亚细胞结构无关。将超薄切片漂浮在EDTA或EGTA溶液上可去除质膜上的无定形致密物,这表明无定形致密物是含钙的矿物质沉积物。无定形沉积物与从前成牙本质细胞和年轻成牙本质细胞表面突出的囊泡结构的膜相关,这表明细胞外基质中发现的小泡是由前成牙本质细胞和年轻成牙本质细胞的质膜出芽形成的。细胞外基质中一些小泡的界膜存在无定形矿物质沉积物,以及其他基质小泡内存在针状矿物质晶体,这表明矿物质在基质小泡内发生了从无定形到晶体的相变。本研究结果表明,与前成牙本质细胞和年轻成牙本质细胞质膜相关的钙结合位点作为牙本质中初级矿物质沉积的成核中心。

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