Arsenault A L
Department of Anatomy, University of British Columbia, Vancouver, Canada.
Bone Miner. 1989 May;6(2):165-77. doi: 10.1016/0169-6009(89)90048-2.
Crystal-collagen relationships in calcified turkey leg tendons and cortical bone and dentin of the rat were studied by bright field and selected-area dark field electron microscopy. The latter imaging technique enables the specific and direct visualization of apatite crystal sizes and their crystallographic orientations within collagen fibrils. Cortical bone possessed the longest mean c-axial length (170 +/- 50 A), then the tendon (142 +/- 43 A) and the smallest was dentin (110 +/- 30 A). Crystallographic orientations of apatite were found to alternate between a,b- and c-axial planes along the axial period of longitudinally sectioned collagen. This distribution of apatite may reflect a crystal alignment with collagen molecules as they spiral in superhelical fashion along the long axis of the collagen fibril. Apatite crystals were localized within both the gap and overlap zones of collagen fibrils even at very early stages of mineralization. The relative amounts of mineral within single collagen periods were determined as a function of electron absorbency. In the tendon at the onset of mineralization 80% of the mineral was located in the gap zone and 20% in the overlap zone; with further mineralization these relative amounts changed to 55% in the gap zone and 45% in the overlap zone. This 55/45% ratio observed in the heavily mineralized tendon was also observed in both cortical bone and dentin. The implications of these findings are discussed in view of collagen molecular ordering and the spread of apatite along collagen fibrils.
通过明场和选区暗场电子显微镜研究了钙化火鸡腿部肌腱以及大鼠皮质骨和牙本质中的晶体 - 胶原蛋白关系。后一种成像技术能够特异性地直接观察磷灰石晶体的大小及其在胶原纤维内的晶体取向。皮质骨的平均c轴长度最长(170±50 Å),其次是肌腱(142±43 Å),最小的是牙本质(110±30 Å)。发现磷灰石的晶体取向在纵向切片胶原的轴向周期内,在a、b和c轴平面之间交替。磷灰石的这种分布可能反映了晶体与胶原分子的排列,因为它们沿着胶原纤维的长轴以超螺旋方式螺旋排列。即使在矿化的非常早期阶段,磷灰石晶体也定位在胶原纤维的间隙和重叠区域内。根据电子吸收能力确定单个胶原周期内矿物质的相对含量。在矿化开始时,肌腱中80%的矿物质位于间隙区域,20%位于重叠区域;随着矿化的进一步进行,这些相对含量变为间隙区域55%,重叠区域45%。在矿化严重的肌腱中观察到的这种55/45%的比例,在皮质骨和牙本质中也观察到了。鉴于胶原分子的排列以及磷灰石沿胶原纤维的扩散,讨论了这些发现的意义。