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Characterization of biomineralization mechanism mediated by dentin matrix protein 1 in vitro.

机译:牙本质基质蛋白1介导的生物矿化机制的表征。

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摘要

Biomineralization of bone and dentin is highly regulated by extracellular matrix secreted from the cells. Osteoblasts and odontoblasts synthesize a polymeric collagenous matrix which forms a template for apatite initiation and elongation. Coordinated and controlled reaction between type I collagen and bone/dentin specific noncollagenous proteins are necessary for well defined biogenic crystal formation. However, the mechanisms of protein mediated mineral initiation are far from understood. The present thesis shows that dentin matrix protein 1 (DMP1), an acidic protein, can nucleate hydroxyapatite in vitro in a multi-step process that begins by DMP1 binding calcium ions and initiating mineral deposition. Characterization of the functional domains in DMP1 demonstrated that inter-molecular assembly of acidic clusters into a beta-sheet template was essential for the observed mineral nucleation. Further studies showed that nascent calcium phosphate nuclei formed in solution were assembled into ordered protein-mineral complex with the aid of oligomerized DMP1. The interactions between DMP1 and type I collagen were examined comprehensively. It was demonstrated that specific binding of DMP1 on the collagen fibril might be a key step in collagen matrix organization and mineralization.; The current study demonstrates that formation of calcified tissues is a highly regulated process, involving a combination of both positive and negative events, i.e., prohibit spontaneous mineral precipitation and initiate temporally and spatially regulated mineral deposition. This initiation is highly dependent upon the formation of a preorganized template and molecular recognition functions. Such information is valuable and could be exploited for the synthesis of bone and dentin-like composites.
机译:骨骼和牙本质的生物矿化受到细胞分泌的细胞外基质的高度调节。成骨细胞和成牙本质细胞合成聚合物胶原基质,该基质形成磷灰石引发和伸长的模板。 I型胶原蛋白与骨/牙本质特异性非胶原蛋白之间的协调和受控反应对于明确定义的生物晶体形成是必需的。但是,蛋白质介导的矿物质引发的机制尚不清楚。本论文表明,牙本质基质蛋白1(DMP1)是一种酸性蛋白,可以在体外以多步过程成核羟磷灰石的过程,该过程以DMP1结合钙离子和引发矿物质沉积为开始。 DMP1中功能域的表征表明,酸性簇的分子间组装成β-sheet模板对于观察到的矿物成核至关重要。进一步的研究表明,在低聚的DMP1的帮助下,溶液中形成的新生磷酸钙核被组装成有序的蛋白质-矿物质复合物。全面检查了DMP1和I型胶原之间的相互作用。已经证明DMP1在胶原原纤维上的特异性结合可能是胶原基质组织和矿化的关键步骤。当前的研究表明钙化组织的形成是高度受控的过程,涉及正事件和负事件的组合,即,禁止自发性矿物质沉淀并开始在时间和空间上调节矿物质沉积。这种起始高度依赖于预组织模板的形成和分子识别功能。这样的信息是有价值的,可用于合成骨和类牙本质的复合材料。

著录项

  • 作者

    He, Gen.;

  • 作者单位

    University of Illinois at Chicago, Health Sciences Center.;

  • 授予单位 University of Illinois at Chicago, Health Sciences Center.;
  • 学科 Biology Molecular.
  • 学位 Ph.D.
  • 年度 2004
  • 页码 112 p.
  • 总页数 112
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 分子遗传学;
  • 关键词

  • 入库时间 2022-08-17 11:44:05

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