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首页> 外文期刊>Journal of vertebrate paleontology >The braincase and inner ear of Placodus gigas (Sauropterygia, Placodontia)a new reconstruction based on micro-computed tomographic data
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The braincase and inner ear of Placodus gigas (Sauropterygia, Placodontia)a new reconstruction based on micro-computed tomographic data

机译:一种基于显微计算机断层扫描数据的新重建方法,用于Picodus gigas(Sauropterygia,Placodontia)的脑箱和内耳

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Placodus gigas is an unarmored placodont marine reptile (Diapsida, Sauropterygia) known from the Middle Triassic of Europe, most commonly found in the shallow marine carbonate facies of the German Muschelkalk (lower Anisian to middle Ladinian, approximately 243-235 Ma). Generally, the morphology of the skull is well understood, with the exception of the braincase, which is partially obscured by dermatocranial bone. Two skulls that display well-preserved and intact chondrocranial elements were scanned using industrial micro-computed tomography (CT), thus revealing parts of the braincase that were previously obscured and allowing a new three-dimensional reconstruction of the region to be constructed. This includes a complete osteological description, the first reconstruction of a sauropterygian vestibular apparatus, and a new virtual cranial endocast. The morphology of the braincase and sphenoid region has been revised, revealing the position of the hypophyseal pit. The enigmatic alisphenoid bridge has been reinterpreted as being a dorsally extended dorsum sellae. The vestibular apparatus is shown to have strongly dorsoventrally compressed vertical semicircular canals, a commonly observed morphology of other marine reptiles, and an alert head position of about 20, indicating a highly aquatic lifestyle. Because placodonts are the sister group to all other sauropterygians, these new data are of great comparative and phylogenetic significance, providing insight into some of the morphological and functional changes that occurred on the stem leading to the more derived sauropterygians.
机译:Placodus gigas是一种无甲的斑纹海生爬行动物(Diapsida,Sauropterygia),起源于欧洲中三叠纪,最常见于德国Muschelkalk的浅海相碳酸盐岩相(下阿尼阶至中拉迪尼阶,约243-235 Ma)。通常,除了脑箱外,颅骨的形态已广为人知,脑箱被皮颅骨部分遮盖了。使用工业微型计算机断层扫描(CT)扫描了两个保存完好且完整的软骨成分的颅骨,从而揭示了先前被遮盖的部分脑箱,并可以对该区域进行新的三维重建。这包括完整的骨科描述,首次对腕足前庭进行重建,以及进行新的虚拟颅内膜植入术。脑箱和蝶骨区域的形态已被修改,揭示了垂体凹坑的位置。神秘的类蝶形桥已被重新解释为背侧背侧蝶鞍。显示前庭装置具有强烈的背腹垂直垂直半规管,其他海洋爬行动物的常见形态以及大约20的机敏头部位置,表明其高度水生生活方式。由于斑牙are是所有其他变色龙的姊妹群,因此这些新数据具有重大的比较和系统发育意义,可洞悉茎上发生的某些形态和功能变化,从而导致更多的变色龙。

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