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Evolution of dental tissue mineralization: an analysis of the jawed vertebrate SPARC and SPARC-L families

机译:牙组织矿化的演变:颚脊椎动物SPARC和SPARC-L家族的分析

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摘要

BackgroundThe molecular bases explaining the diversity of dental tissue mineralization across gnathostomes are still poorly understood. Odontodes, such as teeth and body denticles, are serial structures that develop through deployment of a gene regulatory network shared between all gnathostomes. Dentin, the inner odontode mineralized tissue, is produced by odontoblasts and appears well-conserved through evolution. In contrast, the odontode hypermineralized external layer (enamel or enameloid) produced by ameloblasts of epithelial origin, shows extensive structural variations. As EMP (Enamel Matrix Protein) genes are as yet only found in osteichthyans where they play a major role in the mineralization of teeth and others skeletal organs, our understanding of the molecular mechanisms leading to the mineralized odontode matrices in chondrichthyans remains virtually unknown.
机译:背景技术牙齿组织矿化在整个咬牙切开术中的多样性的分子基础仍然知之甚少。齿状牙齿,例如牙齿和身体的齿状体,是通过部署在所有咬虫之间共享的基因调控网络而形成的系列结构。牙本质内部的牙本质矿化组织牙本质是由成牙本质细胞产生的,并通过进化表现出良好的保守性。相比之下,上皮来源成釉细胞产生的齿状超矿化外层(牙釉质或同名金属)表现出广泛的结构变异。由于EMP(牙釉质基质蛋白)基因仅在骨软骨动物中发现,而它们在牙齿和其他骨骼器官的矿化中起着重要作用,因此我们对导致软骨软骨中矿化的齿状体基质的分子机制的了解仍然未知。

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