首页> 外文期刊>Comptes rendus. Palevol >A new tool for determining degrees of mineralization in fossil amphibian skeletons: The example of the Late Palaeozoic branchiosaurid Apateon from the Autun Basin, France [Un nouvel outil pour la détermination du degré de minéralisation du squelette chez les amphibiens fossiles: l'exemple du branchiosauride Apateon du Paléozo?que supérieur du Bassin d'Autun, France]
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A new tool for determining degrees of mineralization in fossil amphibian skeletons: The example of the Late Palaeozoic branchiosaurid Apateon from the Autun Basin, France [Un nouvel outil pour la détermination du degré de minéralisation du squelette chez les amphibiens fossiles: l'exemple du branchiosauride Apateon du Paléozo?que supérieur du Bassin d'Autun, France]

机译:一种确定两栖动物化石骨架矿化程度的新工具:以法国Autun盆地晚古生代分支龙兽化石Apateon为例[确定化石两栖动物骨架的矿化度的一种新工具:分支龙兽化石为例法国Autun盆地上古生界的Apateon]

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摘要

Studying ontogenetic features of fossil tetrapods is of major interest for investigating the adaptive strategies of early tetrapods to their palaeoenvironments. To determine the degree of calcification of skeletal elements, biologists have until now relied on X-ray radiographs of organisms or isolated bones, or on thin sections. An X-ray tomographic scan of Apateon, a Carboniferous - Permian branchiosaurid from the Autun Basin, France, reveals distinct density properties related to different mineralized tissues (calcified cartilage versus bone). The rendering of Apateon as a "test individual" provides a 3D map of the degrees of ossification of the axial and cranial elements. The combination of these anatomical observations with histological information from classical thin sections made in limb bones of several other specimens of the same locality allows the detailed determination of their ontogenetic stage. A comparison with the well-known specimens of the Saar-Nahe Basin, Germany, makes it possible to investigate the influence of different palaeoenvironments on ontogenetic features.
机译:研究化石四足动物的个体发育特征是研究早期四足动物对其古环境的适应策略的主要兴趣。为了确定骨骼元素的钙化程度,生物学家迄今为止一直依靠生物体或离体骨骼的X射线照相或薄切片。来自法国Autun盆地的石炭纪-二叠纪分支龙的Apateon的X射线断层扫描显示,与不同矿化组织(钙化软骨与骨骼)相关的独特密度特性。将Apateon渲染为“测试个体”可提供轴向和颅骨骨化程度的3D图。这些解剖学观察与来自在相同位置的其他多个标本的四肢骨骼中制成的经典薄片的组织学信息相结合,可以详细确定其发生的阶段。通过与德国萨尔-纳赫盆地的著名标本进行比较,可以研究不同的古环境对个体发育特征的影响。

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