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The role of acidic phosphoproteins in biomineralization

机译:酸性磷蛋白在生物矿化中的作用

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Biomineralization is the process by which living organisms deposit mineral in the extracellular matrix. In nature, almost 50% of biominerals are calcium-bearing minerals. In addition to calcium, we find biominerals formed from silica and magnetite. Calcium-containing biominerals could be either calcium phosphate as in apatite found in vertebrates or calcium carbonate as in calcite and aragonite found in many invertebrates. Since all biomineralization is matrix mediated, an understanding of the nature of the proteins involved is essential in elucidating its mechanism. This review will discuss some of the proteins involved in the process of biomineralization involving calcium. Two proteins, dentin matrix protein 1 and dentin phosphoprotein (Phosphophoryn) will serve as models for the vertebrate system, and two others-P16 and phosphodontin will serve as models for the invertebrate system.
机译:生物矿化是生物体在细胞外基质中沉积矿物质的过程。在自然界中,几乎50%的生物矿物都是含钙的矿物质。除钙外,我们还发现了由二氧化硅和磁铁矿组成的生物矿物。含钙生物矿物质既可以是在脊椎动物中发现的磷灰石中的磷酸钙,也可以是在许多无脊椎动物中发现的方解石和文石中的碳酸钙。由于所有生物矿化作用都是通过基质介导的,因此对所涉及蛋白质的性质的理解对于阐明其机理至关重要。这篇综述将讨论涉及钙的生物矿化过程中涉及的一些蛋白质。两种蛋白质,牙本质基质蛋白1和牙本质磷蛋白(Phosphophoryn),将作为脊椎动物系统的模型,另外两种蛋白质-P16和磷酸化牙本质蛋白,将作为无脊椎动物系统的模型。

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