Analyses of the tidemark on human femoral heads. I. Histochemical, ultrastructural and microanalytic characterization of the normal structure of the intercartilaginous junction.

Acta morphologica Hungarica Pub Date : 1989-01-01
R Oettmeier, K Abendroth, S Oettmeier
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Abstract

The tidemark as a boundary between non-calcified and calcified articular cartilage has a complicated structure and fulfils various physiological functions. 25 human femoral heads from healthy joints were examined. In non-decalcified preparations three structural components of the tidemark were demarcated: (1) the PAS-positive, proteoglycan-containing tidemark line adjacent to the basal cartilage, (2) the sublinear light-coloured zone and (3) the demarcation line to the calcified cartilage. Using scanning electron microscopy, the tidemark was characterized as an electron-dense impression between hyaline and calcified cartilage. The presence of specific architecture and orientation of collagenous fibres could not be shown. Concentrations of calcium, phosphorus and sulphur could not be detected in the tidemark by means of an X-ray microanalyzer. A morphological model of the tidemark region was established, which represents the intercartilaginous junction as a double layer of substantially and functionally different surfaces.

人类股骨头潮纹的分析。1 .软骨间连接处正常结构的组织化学、超微结构和显微分析表征。
潮迹是关节软骨非钙化与钙化的分界线,其结构复杂,具有多种生理功能。对25个健康关节的人股骨头进行了检查。在非脱钙制剂中,对潮标的三个结构成分进行了划分:(1)毗邻基软骨的pas阳性、含蛋白多糖的潮标线,(2)亚线性浅色区,(3)与钙化软骨的分界线。通过扫描电子显微镜,潮汐标记的特征是透明软骨和钙化软骨之间的电子密集的印象。胶原纤维的特定结构和取向无法显示。用x射线微量分析仪无法检测到潮标中钙、磷和硫的浓度。建立了潮标区形态学模型,该模型将软骨间连接处表示为实质上和功能上不同的双层表面。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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