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鲨鱼牙齿釉质层的成釉细胞分泌与钙化

Ameloblastic secretion and calcification of the enamel layer in shark teeth.

作者信息

Kemp N E

出版信息

J Morphol. 1985 May;184(2):215-30. doi: 10.1002/jmor.1051840211.

Abstract

Tooth primordia at early stages of mineralization in the sharks Negaprion brevirostris and Triaenodon obesus were examined electron microscopically for evidence of ameloblastic secretion and its relation to calcification of the enamel (enameloid) layer. Ameloblasts are polarized with most of the mitochondria and all of the Golgi dictyosomes localized in the infranuclear end of the cell toward the squamous outer cells of the enamel organ. Endoplasmic reticular membranes and ribosomes are also abundant in this region. Ameloblastic vesicles bud from the Golgi membranes and evidently move through perinuclear and supranuclear zones to accumulate at the apical end of the cell. The vesicles secrete their contents through the apical cell membrane in merocrine fashion and appear to contribute precursor material both for the basal lamina and the enameline matrix. The enamel layer consists of four zones: a juxta-laminar zone containing newly polymerized mineralizing fibrils (tubules); a pre-enamel zone of assembly of matrix constituents; palisadal zones of mineralizing fibrils (tubules); and interpalisadal zones containing granular amorphous matrix, fine unit fibrils, and giant cross-banded fibers with a periodicity of 17.9 nm. It seems probable that amorphous, non-mineralizing fibrillar and mineralizing fibrillar constituents of the matrix are all products of ameloblastic secretion. Odontoblastic processes are tightly embedded in the matrix of the palisadal zones and do not appear to be secretory at the stages investigated. The shark tooth enamel layer is considered homologous with that of other vertebrates with respect to origin of its mineralizing fibrils from the innerental epithelium. The term enameloid is appropriate to connote the histological distinction that the enamel layer contains odontoblastic processes but should not signify that shark tooth enamel is a modified type of dentine. How amelogenins and/or enamelins secreted by amelo- blasts in the shark and other vertebrates are related to nucleation and growth of enamel crystallites is still not known.

摘要

利用电子显微镜检查了短吻真鲨(Negaprion brevirostris)和灰三齿鲨(Triaenodon obesus)处于矿化早期阶段的牙原基,以寻找成釉细胞分泌的证据及其与釉质(类釉质)层钙化的关系。成釉细胞呈极性分布,大部分线粒体和所有高尔基体囊泡位于细胞的核下末端,朝向釉器的鳞状外细胞。内质网膜和核糖体在该区域也很丰富。成釉细胞囊泡从高尔基体膜上芽生,显然穿过核周和核上区域,在细胞顶端积累。这些囊泡以局部分泌方式通过顶端细胞膜分泌其内容物,似乎为基膜和釉质基质提供前体物质。釉质层由四个区域组成:一个近层区域,含有新聚合的矿化原纤维(小管);一个基质成分组装的前釉质区域;矿化原纤维(小管)的柱状区域;以及柱间区域,含有颗粒状无定形基质、细单位原纤维和周期为17.9nm的巨大交叉带纤维。基质的无定形、非矿化纤维状和矿化纤维状成分似乎都是成釉细胞分泌的产物。成牙本质细胞突起紧密嵌入柱状区域的基质中,在所研究的阶段似乎不具有分泌功能。就其矿化原纤维起源于内釉上皮而言,鲨鱼牙釉质层被认为与其他脊椎动物的牙釉质层同源。类釉质这个术语适用于表示组织学上的区别,即釉质层含有成牙本质细胞突起,但不应表示鲨鱼牙釉质是一种改良型的牙本质。鲨鱼和其他脊椎动物的成釉细胞分泌的釉原蛋白和/或釉蛋白如何与釉质微晶的成核和生长相关,目前仍不清楚。

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