The Mineral Phase of Calcified Cartilage: Its Molecular Structure and Interface with the Organic Matrix

被引:61
|
作者
Duer, Melinda J. [1 ]
Friscic, Tomislav [1 ]
Murray, Rachel C. [2 ]
Reid, David G. [1 ]
Wise, Erica R. [1 ]
机构
[1] Univ Cambridge, Dept Chem, Cambridge CB2 1EW, England
[2] Anim Hlth Trust, Newmarket, Suffolk, England
基金
英国生物技术与生命科学研究理事会; 英国工程与自然科学研究理事会;
关键词
SOLID-STATE; ARTICULAR-CARTILAGE; SUBCHONDRAL BONE; CROSS-POLARIZATION; COLLAGEN DYNAMICS; HYDROXYL IONS; THICKNESS; CRYSTALS; HYDROXYAPATITE; SPECTROSCOPY;
D O I
10.1016/j.bpj.2008.12.3954
中图分类号
Q6 [生物物理学];
学科分类号
071011 ;
摘要
We have studied the atomic level structure of mineralized articular cartilage with heteronuclear solid-state NMR, our aims being to identify the inorganic species present at the surfaces of the mineral crystals which may interact with the surrounding organic matrix and to determine which components of the organic matrix are most closely involved with the mineral crystals. One-dimensional H-1 and P-31 and two-dimensional C-13{P-31} heteronuclear correlation NMR experiments show that the mineral component is very similar to that in bone with regard to its surface structure. 13C(31 P) rotational echo double resonance experiments identify the organic molecules at the mineral surface as glycosaminoglycans, which concurs with our recent finding in bone. There is also evidence of gamma-carboxyglutamic acid residues interacting with the mineral. However, other matrix components appear more distant from the mineral compared with bone. This may be due to a larger hydration layer on the mineral crystal surfaces in calcified cartilage.
引用
收藏
页码:3372 / 3378
页数:7
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