Maitland M E, Arsenault A L
Sports Medicine Centre, University of Calgary, Alberta, Canada.
Calcif Tissue Int. 1991 May;48(5):341-52. doi: 10.1007/BF02556154.
We have determined the localization of apatite within type I collagen fibrils of calcifying turkey leg tendons by both bright field and selected-area dark field (SADF) electron microscopy and have compared this to computer-modeled, chick type I collagen amino acid sequence data. Apatite crystals occur in both the gap and overlap zones at early stages of mineralization in an asymmetric pattern that corresponds to the polarity, N- to C- orientation, of the collagen molecule. Based on comparisons with computer-generated models of known amino acid sequence of collagen, it was determined for early stages of mineral deposition that apatite is restricted by areas of high hydrophobicity. The gap zone is less hydrophobic than the overlap zone on average but each of these zones had areas of high hydrophobicity that correlated with sites of low localization of mineral. Possible interactions between hydrophobic regions and the process of mineral deposition are discussed.
我们通过明场和选区暗场(SADF)电子显微镜确定了钙化火鸡腿肌腱I型胶原纤维中磷灰石的定位,并将其与计算机模拟的鸡I型胶原氨基酸序列数据进行了比较。在矿化早期,磷灰石晶体以不对称模式出现在间隙区和重叠区,这与胶原分子的极性(从N端到C端方向)相对应。基于与计算机生成的已知胶原氨基酸序列模型的比较,确定在矿物沉积的早期阶段,磷灰石受到高疏水区的限制。间隙区平均疏水性低于重叠区,但这些区域中的每一个都有与矿物低定位位点相关的高疏水区。讨论了疏水区与矿物沉积过程之间可能的相互作用。