Kodaka T, Mori R, Debari K, Yamada M
Department of Oral Anatomy, School of Dentistry, Showa University, Tokyo, Japan.
J Electron Microsc (Tokyo). 1994 Oct;43(5):307-17.
The calcareous concretions of human pineal bodies were investigated with scanning electron microscopy and electron probe microanalysis. The initial concretions measuring 5-7 microns in diameter may have started at the calcified pinealocytes. They grew appositionally forming concentric laminations, and then the simple calcospherulites over 20 microns occasionally aggregated with each other. Some of them became numerous spherulite-aggregated concretions. Others individually grew with scallop-shaped concentric laminations at intervals of 0.05-1 microns and became lobated calcospherulites up to 0.5 mm. The concretions over 0.5 mm were formed by their attachments. The major elements were Ca and P, while traces of S, Mg, and Na were detected. In the calcification and crystallization values, the center of the concretions over 50 microns was significantly higher than the periphery, while there were no differences among the centers and also among the peripheries. The Ca and P amounts in the center were 30.8% and 14.2% by weight and the Ca/P molar ratio was 1.68; thereby the sand-grain-shaped crystals may be nearly hydroxyapatite, as reported previously.
利用扫描电子显微镜和电子探针微分析技术对人类松果体的钙质结石进行了研究。直径为5 - 7微米的初始结石可能始于钙化的松果体细胞。它们以同位生长的方式形成同心层,然后偶尔会相互聚集形成直径超过20微米的简单钙球晶。其中一些形成了大量球晶聚集的结石。其他的则以0.05 - 1微米的间隔单独生长出扇贝形同心层,形成了直径达0.5毫米的叶状钙球晶。超过0.5毫米的结石是通过它们的附着形成的。主要元素是钙和磷,同时检测到微量的硫、镁和钠。在钙化和结晶值方面,直径超过50微米的结石中心明显高于周边,而中心之间以及周边之间没有差异。中心的钙和磷含量按重量计分别为30.8%和14.2%,钙/磷摩尔比为1.68;因此,如先前报道的那样,沙粒状晶体可能接近羟基磷灰石。