Owens P D
J Anat. 1976 Nov;122(Pt 2):389-401.
In an attempt to clarify the nature of the human cemento-dentinal junction, ground sections of incompletely formed and fully formed extracted teeth were prepared and their histology compared with their microradiographic appearances. The results showed that incompletely formed teeth possess distinctive surface layers outside the granular layer of Tomes. The evidence indicates that these layers are of dentinal origin; their presence during development supports previous explanations by the author of the hyaline layer of Hopewell-Smith and of so-called intermediate cementum. The results also indicate that the granular layer of Tomes does not represent the outer limit of root dentine. The relationship of these surface layers to the definitive cementum which is present in fully formed teeth was studied in both young and older patients. From the results it was concluded that cementum formation begins in the more apical region of the teeth at a time when root formation is well advanced, and that it spreads towards the crown rather than in the generally accepted reverse direction.
为了阐明人类牙骨质-牙本质界的性质,制备了未完全形成和完全形成的离体牙的磨片,并将其组织学与显微放射照片进行了比较。结果表明,未完全形成的牙齿在托姆斯颗粒层之外具有独特的表层。证据表明这些层起源于牙本质;它们在发育过程中的存在支持了作者之前对霍普韦尔-史密斯透明层和所谓中间牙骨质的解释。结果还表明,托姆斯颗粒层并不代表牙根牙本质的外部界限。在年轻和老年患者中都研究了这些表层与完全形成的牙齿中存在的最终牙骨质的关系。从结果得出的结论是,牙骨质形成始于牙根形成进展良好时牙齿的更根尖区域,并且它向冠部扩散,而不是朝着普遍认为的相反方向。