A new large embolomere from East Kirkton

IF 0.5 4区 地球科学 Q4 GEOLOGY Scottish Journal of Geology Pub Date : 2020-09-22 DOI:10.1144/sjg2020-008
J. Clack, T. Smithson
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引用次数: 2

Abstract

The well-known late Mississippian/early Carboniferous locality of East Kirkton in Scotland has the earliest described fauna of terrestrial tetrapods. Seven species are now known, represented by articulated skeletons of moderate-sized animals with snout-vent length of up to 200 mm, and each is unique to East Kirkton. Here we describe the skull bones of a much larger tetrapod that closely resembles those of embolomeres from the Pennsylvanian. Although the new material is too incomplete to be named as a new species, it enhances the taxonomic diversity of the East Kirkton tetrapod fauna, predates the embolomeres from other sites in Scotland and extends the range of the group earlier into the Mississippian.
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来自东柯克顿的一个新的大型栓子
苏格兰东柯克顿著名的密西西比晚期/石炭纪早期地区拥有最早描述的陆生四足动物群。目前已知有七个物种,以中等大小动物的关节骨骼为代表,吻孔长度可达200 毫米,每一个都是东柯克顿独有的。在这里,我们描述了一个更大的四足动物的头骨,它与宾夕法尼亚人的栓子非常相似。尽管新材料太不完整,无法作为一个新物种命名,但它增强了东柯克顿四足动物群的分类多样性,早于苏格兰其他地点的栓子虫,并将该类群的范围更早地扩展到密西西比系。
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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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