矿化组织中细胞及其基质的界面研究进展。

Scanning electron microscopy Pub Date : 1986-01-01
S J Jones, A Boyde, N N Ali
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引用次数: 0

摘要

在体内形成的矿化组织中,细胞和基质之间的界面主要是通过观察基质表面来研究的,因为基质表面很容易制备,而不是观察细胞表面,因为细胞表面存在问题。脊椎动物的钙化组织范围从非细胞到高度细胞,但对于所有的组织,形成细胞放置并组织一个细胞特异性基质,尽管这可能最初沉积在不同的组织类型上。硬组织的形成是许多细胞的集体活动;吸收是一个细胞的事,虽然它可能受到附近其他细胞的控制。体外形成的细胞-基质界面也主要在基质方面进行了研究。硬组织界面的体外研究的主要困难在于,在复杂的生理调节控制下,细胞不具有与体内相同的活性甚至细胞功能。成骨细胞破骨问题就属于这一类。这有可能为形成性和再吸收性硬组织细胞提供新的基质,以测试细胞与它们所处的“基质”之间的相互作用。细胞-基质界面的变化也可以通过计算机模拟破骨细胞在基质上的运动来模拟,这种模拟基于其他细胞类型在体外所表现出的已知模式。与复杂吸收坑的形状比较,发现了惊人的匹配。这表明破骨细胞运动的轨迹和骨吸收机制导致的轨迹上的凹坑可能是单独控制的现象。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The interface of cells and their matrices in mineralized tissues: a review.

The interface between cells and matrices in mineralized tissues formed in vivo has been studied mainly by looking at the matrix surface, which is easily prepared, and not at the cell surface, which presents problems. Vertebrate calcified tissues range from being acellular to highly cellular, but for all the tissues the formative cells lay down and organise a cell-specific matrix, although this may be deposited initially on a different tissue-type. The formation of hard tissues is a group activity of many cells; resorption is the province of one cell, though it may be controlled by others in the vicinity. Cell-matrix interfaces that develop in vitro have also mainly been studied at the matrix side. The main difficulty with in vitro studies of hard tissue interfaces is that the cells do not have the same activity or even cellular functions as they had in vivo under the complex control of physiological regulation. The question of osteoblastic osteoclasis falls into this category. It is possible to provide new substrata for both formative and resorptive hard tissue cells to test for the interaction between the cells and the 'matrix' on to which they are seeded. The changing cell-matrix interface may also be modelled using computer simulation of osteoclastic movement across a substrate based on known patterns exhibited by other cell types in vitro. Comparison with the shapes of complex resorption pits shows a surprising match. This suggests that the track of the osteoclast due to cell motility and the bone resorptive mechanism resulting in pits along that track are likely to be separately controlled phenomena.

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