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骨矿物质成分的性质及钙化机制。

The nature of the mineral component of bone and the mechanism of calcification.

作者信息

Glimcher M J

出版信息

Instr Course Lect. 1987;36:49-69.

PMID:3325562
Abstract

From the physical chemical standpoint, the formation of a solid phase of Ca-P in bone represents a phase transformation, a process exemplified by the formation of ice from water. Considering the structural complexity and abundance of highly organized macromolecules in the cells and extracellular tissue spaces of mineralized tissues generally and in bone particularly, it is inconceivable that this phase transformation occurs by homogeneous nucleation, i.e., without the active participation of an organic component acting as a nucleator. This is almost surely true in biologic mineralization in general. Electron micrographs and low-angle neutron and X-ray diffraction studies clearly show that calcification of collagen fibrils occurs in an extremely intimate and highly organized fashion: initiation of crystal formation within the collagen fibrils in the hole zone region, with the long axes (c-axis) of the crystals aligned roughly parallel to the long axis of the fibril within which they are located. Crystals are initially formed in hole zone regions within individual fibrils separated by unmineralized regions. Calcification is initiated in spatially distinct nucleation sites. This indicates that such regions within a single, undirectional fibril represents independent sites for heterogeneous nucleation. Clearly, sites where mineralization is initiated in adjacent collagen fibrils are even further separated, emphasizing even more clearly that the process of progressive calcification of the collagen fibrils and therefore of the tissue is characterized principally by the presence of increasing numbers of independent nucleation sites within additional hole zone regions of the collagen fibrils. The increase in the mass of Ca-P apatite accrues principally by multiplication of more crystals, mostly by secondary nucleation from the crystals initially deposited in the hole zone region. Very little additional growth of the crystals occurs with time, the additional increase in mineral mass being principally the result of increase in the number of crystals (multiplication), not size of the crystals (crystal growth). The crystals within the collagen fibers grow in number and possibly in size to extend into the overlap zone of the collagen fibrils ("pores") so that all of the available space within the fibrils, which has possibly expanded in volume from its uncalcified level, is eventually occupied by the mineral crystals. It must be recognized that the calcification of separate tissue components and compartments (collagen, mitochondria, matrix vesicles) must be an independent physical chemical event.(ABSTRACT TRUNCATED AT 400 WORDS)

摘要

从物理化学角度来看,骨骼中钙磷固相的形成代表了一种相变,这一过程就如同水结冰一样。考虑到矿化组织(尤其是骨骼)的细胞和细胞外组织空间中高度有序的大分子结构复杂且数量众多,很难想象这种相变是通过均匀成核发生的,即没有作为成核剂的有机成分的积极参与。一般来说,生物矿化几乎肯定是这样。电子显微镜图像以及低角度中子和X射线衍射研究清楚地表明,胶原纤维的钙化以极其紧密和高度有序的方式发生:在孔区区域的胶原纤维内开始形成晶体,晶体的长轴(c轴)大致平行于其所在纤维的长轴排列。晶体最初在由未矿化区域分隔的单个纤维的孔区区域形成。钙化在空间上不同的成核位点开始。这表明在单个单向纤维内的此类区域代表了异相成核的独立位点。显然,相邻胶原纤维中矿化开始的位点距离更远,这更清楚地强调了胶原纤维进而组织的渐进钙化过程主要特征是在胶原纤维额外的孔区区域内存在越来越多的独立成核位点。钙磷磷灰石质量的增加主要是通过更多晶体的增殖,大多是由最初沉积在孔区区域的晶体进行二次成核。随着时间推移,晶体很少有额外生长,矿物质质量的额外增加主要是晶体数量增加(增殖)的结果,而非晶体尺寸(晶体生长)。胶原纤维内的晶体数量增加,可能尺寸也增大,延伸到胶原纤维的重叠区(“孔隙”),这样纤维内所有可用空间(其体积可能已从未钙化水平扩展)最终都被矿物晶体占据。必须认识到,不同组织成分和隔室(胶原、线粒体、基质小泡)的钙化必定是一个独立的物理化学事件。(摘要截选至400字)

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