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骨粘连蛋白的糖基化模式在软骨内骨形成过程中发生改变。

The glycosylation profile of osteoadherin alters during endochondral bone formation.

机构信息

Oral Biology, Department of Dental Medicine, Karolinska Institutet, SE141-04 Huddinge, Sweden.

出版信息

Bone. 2013 Apr;53(2):459-67. doi: 10.1016/j.bone.2013.01.022. Epub 2013 Jan 19.

Abstract

Endochondral bone formation involves the dynamic interplay between the cells and their extracellular environment to facilitate the deposition of a calcified matrix. Numerous molecules are involved within this process, including collagens and non-collagenous proteins, and their post-translational modifications have been shown to effect their biomolecular interactions. Osteoadherin (OSAD), a keratin sulfate (KS)-substituted small leucine-rich proteoglycan has been isolated from mineralized tissues and is considered to be a mineralized tissue-specific protein. However, to date, information is limited concerning the dynamic expression and role of this proteoglycan during bone formation and the biomineralization process. The current study aimed to examine the dynamic expression of this protein throughout mouse metatarsal long bone development, from the cartilage anlagen (E15) to the fully formed bone (Adult). Using quantitative gene expression analysis we observed that OSAD was produced with the onset of mineralization and the formation of the ossification center. This finding was reflected in the localization studies, using both light and electron microscopy, and showed that initial OSAD localization was restricted to the endosteal surfaces of the diaphysis and forming metaphysis. Furthermore, we analyzed protein extracts, both mineral and non-mineral associated fractions, and showed that OSAD was substituted with varying patterns of glycosylation during bone development. Sequential enzymatic digestions of the non-mineral bound protein extracts demonstrated that OSAD lacked any KS chains throughout all development stages. Whereas, in the mineral bound fractions, with long bone maturation the substitution with KS became more apparent with development. Therefore, it can be concluded that different pools of OSAD are produced during endochondral bone formation and these may have specific roles in directing the mineralization process.

摘要

软骨内成骨涉及细胞与其细胞外环境之间的动态相互作用,以促进钙化基质的沉积。在此过程中涉及许多分子,包括胶原蛋白和非胶原蛋白,并且已经表明它们的翻译后修饰会影响其生物分子相互作用。骨粘连蛋白(OSAD)是一种角蛋白硫酸盐(KS)取代的小富含亮氨酸的蛋白聚糖,已从矿化组织中分离出来,被认为是一种矿化组织特异性蛋白。然而,迄今为止,有关该蛋白聚糖在骨形成和生物矿化过程中的动态表达和作用的信息有限。本研究旨在检查该蛋白聚糖在从小鼠跖骨长骨发育的软骨原基(E15)到完全形成的骨(成年)的整个过程中的动态表达。通过定量基因表达分析,我们观察到 OSAD 在矿化开始和骨化中心形成时产生。这一发现反映在使用光镜和电子显微镜进行的定位研究中,表明 OSAD 的最初定位仅限于骨干的内骨表面和正在形成的骨骺。此外,我们分析了蛋白提取物,包括矿化和非矿化相关的部分,并表明 OSAD 在骨发育过程中具有不同的糖基化模式。对非矿化结合蛋白提取物的连续酶消化表明,OSAD 在所有发育阶段均缺乏任何 KS 链。然而,在矿化结合部分,随着长骨成熟,KS 的取代在发育过程中变得更加明显。因此,可以得出结论,在软骨内成骨过程中产生了不同的 OSAD 池,这些池可能在指导矿化过程中具有特定的作用。

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