Risnes S
Department of Anatomy, Dental Faculty, University of Oslo, Norway.
J Biol Buccale. 1990 Sep;18(3):237-48.
The study provides a survey of shark tooth morphogenesis based on SEM and EDX analyses of whole tooth families in six shark species. The teeth, demonstrating different stages of development, were acid-etched and coated with palladium. Calcium content was determined semi-quantitatively by using the palladium coating as an internal standard. Due to the rapid development of the enameloid, all major events took place in the two or three youngest teeth of a tooth family. Enameloid appeared to develop as a transformation of the peripheral part of the dental papilla. Mineralization started immediately. Based on morphological criteria the middle zone of the enameloid was established at an early stage, excluding the possibility of an unambiguous centrifugal or centripetal direction of growth. Substantial mineral increase first occurred in the middle zone, spreading from the tooth tip toward the base. Dentin formed after the enameloid was completely established. Dentin formation started basally as a direct prolongation of the enameloid cap, then spreading toward the tooth tip, first along the edges. It is concluded that shark enameloid has a mesenchymal background, but a role played by the inner dental epithelium can not be excluded.
该研究基于对六种鲨鱼整个牙齿家族的扫描电子显微镜(SEM)和能量色散X射线光谱(EDX)分析,对鲨鱼牙齿形态发生进行了调查。将显示不同发育阶段的牙齿进行酸蚀并镀上钯。以钯涂层作为内标,半定量测定钙含量。由于釉质样组织发育迅速,所有主要事件都发生在一个牙齿家族中最年轻的两三颗牙齿上。釉质样组织似乎是由牙乳头的周边部分转变而来。矿化立即开始。根据形态学标准,釉质样组织的中间区域在早期就已确立,排除了明确的离心或向心生长方向的可能性。大量矿物质增加首先发生在中间区域,从牙尖向牙根扩散。牙本质在釉质样组织完全形成后形成。牙本质形成从基部开始,是釉质样帽的直接延续,然后向牙尖扩散,首先沿着边缘扩散。得出的结论是,鲨鱼釉质样组织具有间充质背景,但不能排除内釉上皮所起的作用。