三叠纪鹿角直龙尾部皮肤甲的三维层析研究

IF 0.5 4区 地球科学 Q4 GEOLOGY Scottish Journal of Geology Pub Date : 2020-02-14 DOI:10.1144/sjg2019-026
E. Keeble, M. Benton
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引用次数: 4

摘要

Stagonolepis robertsoni以太龙是第一种从马里郡三叠纪晚期洛斯茅斯砂岩组命名的爬行动物。据报道,其特有的矩形甲板与骨骼遗骸分离并结合在一起。在这里,我们首次对尾部周围的甲板与尾椎骨和人字形进行了三维重建,以提供身体轮廓的直接证据。尾椎柱由八个骨骨皮、成对的正中旁背侧和腹侧板以及左右两侧的一对侧骨皮包围。尾巴的形状是半圆形的,宽于高。骨痂像瓦片一样重叠,每个骨痂的后缘与后面的骨痂重叠。这些扫描的成功表明,计算机断层扫描可以在未来揭示所有埃尔金爬行动物的优秀细节。补充材料:两个化石标本的三维模型可在以下网站获得:https://doi.org/10.6084/m9.figshare.c.4824183
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Three-dimensional tomographic study of dermal armour from the tail of the Triassic aetosaur Stagonolepis robertsoni
The aetosaur Stagonolepis robertsoni was the first reptile to be named from the Late Triassic Lossiemouth Sandstone Formation of Morayshire. Its characteristic rectangular armour plates have been reported in isolation and in association with skeletal remains. Here we present for the first time a three-dimensional reconstruction of the armour plates around the tail in association with caudal vertebrae and a chevron, to give direct evidence of the body outline. The caudal vertebral column was surrounded by eight bony osteoderms, paired paramedian dorsal and ventral plates, and a pair of lateral osteoderms on right and left. The tail shape was subcircular, broader than high. The osteoderms overlap like roofing tiles, the posterior margin of each overlapping the osteoderm following behind. The success of these scans suggests that computed tomography scanning could reveal excellent detail of all the Elgin reptiles in the future. Supplementary material: Three-dimensional models of the two fossil specimens are available at: https://doi.org/10.6084/m9.figshare.c.4824183
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来源期刊
Scottish Journal of Geology
Scottish Journal of Geology 地学-地质学
CiteScore
1.70
自引率
0.00%
发文量
10
审稿时长
>12 weeks
期刊介绍: Although published only since 1965, the Scottish Journal of Geology has a long pedigree. It is the joint publication of the Geological Society of Glasgow and the Edinburgh Geological Society, which prior to 1965 published separate Transactions: from 1860 in the case of Glasgow and 1863 for Edinburgh. Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology. The diverse geology of Scotland continues to provide an important natural laboratory for the study of earth sciences; many seminal studies in geology have been carried out on Scottish rocks, and over the years the results of much of this work had been published in the Journal and its predecessors. The Journal fully deserves its high reputation worldwide and intends to maintain its status in the front rank of publications in the Earth sciences.
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