Quintana C, Sandoz D
Calcif Tissue Res. 1978 May 26;25(2):145-59. doi: 10.1007/BF02010763.
The egg-shell of Japanese quail was studied by several techniques. Semithin sections (1 micron thick) of non-decalcified shell were observed by normal and polarized light microscopy. Thin sections of non-decalcified shell, examined by transmission electron microscopy, permitted us to observe the forms and dimensions of crystals of calcite within different layers of the shell: mammilary layer, layer of cones, palissade layer and surface crystal layer. There appears to be two distinct zones in the layer of cones as well as in the superficial crystal layer. Electron microdiffraction revealed the orientation of calcite crystals in the columns. Some crystal defects (twins?) were described and the possibility of their artefactual formation during ultramicrotomy is discussed. Localization of Ca, Mg, P and S were made by X-ray microanalysis of semithin sections. This technique shows that shell membranes, and chiefly the true cuticle, are also mineralized but, in these layers, minerals are not crystallized. Otherwise the distribution of Mg is not uniform throughout the shell thickness; it is less concentrated in the external zone of the layer of cones. These results together with observation of developing shells by scanning electron microscopy allowed us to propose a scheme for shell organization of the quail egg. This organization was related with decalcification which occurs during hatching.
采用多种技术对日本鹌鹑蛋的蛋壳进行了研究。通过普通光学显微镜和偏光显微镜观察了未脱钙蛋壳的半薄切片(1微米厚)。通过透射电子显微镜检查未脱钙蛋壳的薄切片,使我们能够观察到蛋壳不同层(乳头层、锥体层、栅栏层和表面晶体层)中方解石晶体的形态和尺寸。在锥体层以及表面晶体层中似乎存在两个不同的区域。电子微衍射揭示了柱状方解石晶体的取向。描述了一些晶体缺陷(孪晶?),并讨论了它们在超薄切片过程中人为形成的可能性。通过对半薄切片进行X射线微分析确定了钙、镁、磷和硫的定位。这项技术表明,壳膜,主要是真正的角质层,也发生了矿化,但在这些层中,矿物质没有结晶。此外,镁在整个蛋壳厚度中的分布并不均匀;它在锥体层的外部区域浓度较低。这些结果以及通过扫描电子显微镜对发育中蛋壳的观察,使我们能够提出鹌鹑蛋蛋壳结构的方案。这种结构与孵化过程中发生的脱钙有关。