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鲨鱼内骨骼镶嵌结构中钙化软骨的超微结构。

Ultrastructure of calcified cartilage in the endoskeletal tesserae of sharks.

作者信息

Kemp N E, Westrin S K

出版信息

J Morphol. 1979 Apr;160(1):75-109. doi: 10.1002/jmor.1051600106.

Abstract

The tesserate pattern of endoskeletal calcification has been investigated in jaws, gill arches, vertebral arches and fins of the sharks Carcharhinus menisorrah, Triaenodon obesus and Negaprion brevirostris by techniques of light and electron microscopy. Individual tesserae develop peripherally at the boundary between cartilage and perichondrium. An inner zone, the body, is composed of calcified cartilage containing viable chondroxytes separated by basophilic contour lines which have been called Liesegang waves or rings. The outer zone of tesserae, the cap, is composed of calcified tissue which appears to be produced by perichondrial fibroblasts more directly, i.e., without first differentiating as chondroblasts. Furthermore, the cap zone is penetrated by acidophilic Sharpey fibers of collagen. It is suggested that scleroblasts of the cap zone could be classified as osteoblasts. If so, the cap could be considered a thin veneer of bone atop the calcified cartilage of the body of a tessera. By scanning electron microscopy it was observed that outer and inner surfaces of tesserae differ in appearance. Calcospherites and hydroxyapatite crystals similar to those commonly seen on the surface of bone are present on the outer surface of the tessera adjacent to the perichondrium. On the inner surface adjoining hyaline cartilage, however, calcospherites of variable size are the predominant surface feature. Transmission electron microscopy shows calcification in close association with coarse collagen fibrils on the outer side of a tessera, but such fibrils are absent from the cartilaginous matrix along the under side of tesserae. Calcified cartilage as a tissue type in the endoskeleton of sharks is a primitive vertebrate characteristic. Calcification in the tesserate pattern occurring in modern Chondrichthyes may be derived from an ancestral pattern of a continuous bed of calcified cartilage underlying a layer of perichondral bone, as theorized by Orvig ('51); or the tesserate pattern in these fish may itself be primitive.

摘要

利用光学显微镜和电子显微镜技术,对黑印真鲨、灰三齿鲨和短吻真鲨的颌骨、鳃弓、椎弓和鳍中的内骨骼钙化的镶嵌模式进行了研究。单个镶嵌体在软骨和软骨膜之间的边界处外周发育。内部区域,即主体,由钙化软骨组成,其中含有由嗜碱性轮廓线分隔的活软骨细胞,这些轮廓线被称为李泽冈波或环。镶嵌体的外部区域,即帽,由钙化组织组成,似乎是由软骨膜成纤维细胞更直接产生的,即无需先分化为成软骨细胞。此外,帽区被嗜酸性的胶原沙比纤维穿透。有人认为帽区的成骨细胞可归类为成骨细胞。如果是这样,帽可被视为镶嵌体主体钙化软骨顶部的一层薄骨片。通过扫描电子显微镜观察到,镶嵌体的外表面和内表面外观不同。与通常在骨表面看到的类似的钙球和羟基磷灰石晶体存在于与软骨膜相邻的镶嵌体外表面。然而,在与透明软骨相邻的内表面,大小不一的钙球是主要的表面特征。透射电子显微镜显示,钙化与镶嵌体外侧面上的粗胶原纤维密切相关,但沿着镶嵌体下侧的软骨基质中没有这种纤维。钙化软骨作为鲨鱼内骨骼中的一种组织类型是原始脊椎动物的特征。现代软骨鱼类中出现的镶嵌模式钙化可能源自奥维格(1951年)提出的理论,即源自一层软骨膜骨下方连续钙化软骨床的祖先模式;或者这些鱼类中的镶嵌模式本身可能是原始的。

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