Sawada T, Inoue S
Department of Ultrastructural Science, Tokyo Dental College, Chiba City, Japan.
Calcif Tissue Int. 2000 Apr;66(4):277-81. doi: 10.1007/s002230010056.
A basement membrane-like structure associated with the maturation stage ameloblasts of the monkey (Macaca fuscata) tooth germ was examined with high resolution electron microscopy. The tissue was prepared either with or without demineralization. This structure was composed of a lamina lucida-like (lamina lucida) and lamina densa-like (lamina densa) structure. The latter was made up of a fine "cord" network, the major constituent of the basement membrane. It was closely associated with the third layer of a 200 nm wide looser cord network. In specimens without demineralization the third layer and a part of the lamina densa were calcified, and it formed the edge of the enamel. This particular area had a higher electron density, and the size, shape, and arrangement of mineral crystals were different from those of the rest of the enamel. Also, mineralization appeared to be proceeding along the cords. These observations indicate that this dense layer is a highly specialized basement membrane which mediates the firm association of maturation stage ameloblasts with the enamel by means of the mineralization of a part of this basement membrane itself which becomes integrated as a part of the enamel. Also, this highly specialized manner of association is favorable with the reported control of the loss of organic substances in the maturing enamel by maturation stage ameloblasts.
利用高分辨率电子显微镜对与猕猴(食蟹猴)牙胚成熟阶段成釉细胞相关的类似基底膜结构进行了检查。组织制备时进行或未进行脱矿处理。该结构由类透明板层(透明板层)和类致密板层(致密板层)结构组成。后者由精细的“索状”网络构成,是基底膜的主要成分。它与宽200nm的较松散索状网络的第三层紧密相关。在未脱矿的标本中,第三层和部分致密板层钙化,并形成釉质边缘。这个特定区域具有较高的电子密度,矿物晶体的大小、形状和排列与釉质其余部分不同。此外,矿化似乎沿着索状结构进行。这些观察结果表明,这个致密层是一种高度特化的基底膜,它通过该基底膜自身一部分的矿化介导成熟阶段成釉细胞与釉质的牢固结合,而这部分基底膜成为釉质的一部分。此外,这种高度特化的结合方式有利于成熟阶段成釉细胞对成熟釉质中有机物质损失的报道性控制。