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Development of larval and transformed teeth in Ambystoma mexicanum (Urodela, Amphibia): an ultrastructural study

机译:墨西哥Ambystoma(Urodela,两栖动物)幼虫和转化牙齿的发育:超微结构研究

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Odontogenesis of early larval non-pedicellate teeth, late larval teeth with a more or less distinct dividing zone and fully transformed pedicellate teeth in Ambystoma mexicanum (Urodela) was studied to obtain insights into the development of differently structured teeth in lower vertebrates. Using transmission electron microscopy we investigated five developmental stages: (1) papilla; (2) bell stage (secretion of the matrix begins); (3) primordium (mineralization and activity of ameloblasts starts); (4) replacement tooth (young, old); and (5) established, functional tooth. Development of the differently structured teeth is largely identical in the first three stages. Mineralization takes place in apico-basal direction up to the (prospective) pedicel (early and some late larvae) or up to the zone that divides the late larval and transformed tooth in pedicel and dentine shaft (pedicellate condition). Mineralization starts directly at the collagen and by means of matrix vesicles. First odontoblasts develop small processes that extend to the basal lamina of the inner epithelial layer of the enamel organ. The processes are small and lack organelles in early larval teeth, but become larger, arborescent, and contain some organelles in late larval and transformed teeth. The processes are surrounded by unmineralized matrix (predentine). Odontoblasts at the basis of the teeth, at the pedicel, and in the zone of division do not develop significant cytoplasmic processes that extend into the matrix. Cells of the inner enamel epithelium differentiate to ameloblasts that secrete the enamel. In the early larval tooth they show an extensive basal labyrinth that becomes regressive when the enamel layer is completed. In late larval and transformed teeth, however, a large cavity arises between the basal ruffled border of ameloblasts and their basal lamina. This cavity appears to mediate amelogenesis. A small apical zone in early, but not in late larval teeth directly below the thin enamel layer consists of enameloid and is free of dentine channels. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 40]
机译:研究了早熟幼虫非齿状牙齿,具有或多或少明显的分隔区的晚幼虫齿以及完全转化的成齿状齿的齿形,以了解下脊椎动物中不同结构的牙齿的发育情况。使用透射电子显微镜,我们研究了五个发育阶段:(1)乳头; (2)钟声阶段(矩阵的分泌开始); (3)原基(成矿和成釉细胞的活性开始); (4)更换牙齿(年轻,旧); (5)功能完备的牙齿。在前三个阶段中,结构不同的牙齿的发育在很大程度上是相同的。矿化作用发生在基部向上,直至(预期的)花梗(早期和某些后期的幼虫),或直至在花梗和牙本质的轴上将后期的幼虫和转化的牙齿分开的区域(有齿状)。矿化作用直接从胶原蛋白开始,并通过基质囊泡开始。最初的成牙本质细胞发展出小的过程,延伸到釉质器官内上皮层的基底层。该过程很小,在幼虫早期的牙齿中缺乏细胞器,但是变大了,呈树状,并且在幼虫后期和转化的牙齿中含有一些细胞器。这些过程被未矿化的基质(牙本质)包围。成牙细胞在牙齿的基础上,在花梗上和在分裂区域内不会发育出延伸到基质中的明显细胞质过程。内釉质上皮细胞分化为分泌釉质的成釉细胞。在早期的幼虫牙齿中,它们显示出广泛的基底迷路,当釉质层完成时,它们会逐渐退缩。然而,在后期幼虫和牙齿转化后,成釉细胞的基底皱纹边界和基底层之间会形成一个大洞。该腔似乎可以介导牙釉质形成。在薄釉质层正下方的幼虫牙齿的早期但不晚期的小根尖区由牙釉质组成,没有牙本质通道。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:40]

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