New malacostracan crustaceans from the Lower Coal Measures (Langsettian, Carboniferous) North Lanarkshire, Scotland

IF 0.5 4区 地球科学 Q4 GEOLOGY Scottish Journal of Geology Pub Date : 2024-07-23 DOI:10.1144/sjg2024-004
Neil D. L. Clark
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Abstract

Two malacostracan crustacean genera are described from the Langsettian (upper part of the Bashkirian, Lower Pennsylvanian) of the Scottish Coal Fields in the Midland Valley of Scotland. One is the youngest occurrence of Tealliocaris Peach, 1908 and was found at Polkemmet Colliery near Whitburn. It is recognised as a new species, Tealliocaris elliotti , based on the presence of eight spines on its scaphocerites and lateral convergent carinae of the telson. The other crustacean is a unique specimen from the Ardenrigg Colliery at Wester Bracco, North Lanarkshire in similar shales of Langsettian age. There are no distinguishing characters preserved that would identify it as a new species, but it can be placed in Palaeocaris Meek and Worthen, 1865 based on the well preserved features of the tail fan. This is the first record of this genus in Scotland, although specimens of Minicaris brandi Schram, 1979 from the Namurian (Serpukhovian, Upper Mississippian) shales of Bearsden are now here also considered to be a species of Palaeocaris .
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来自苏格兰北拉纳克里下煤层(兰塞特石炭统,石炭纪)的新槌壳类甲壳动物
本报告描述了苏格兰中部山谷苏格兰煤田朗塞梯(下宾夕法尼亚统巴什基尔上统)中的两个甲壳动物属。其中一种是最年轻的 Tealliocaris Peach(1908 年),发现于惠特本附近的 Polkemmet Colliery。它被认定为一个新物种,即 Tealliocaris elliotti,因为它的鳞甲上有八根刺,而且尾柄有侧向会聚的瓣纹。另一种甲壳类动物是北拉纳克郡 Wester Bracco 的 Ardenrigg Colliery 在类似的兰塞梯时代页岩中发现的独特标本。虽然没有保存下来的特征可以将其确定为一个新物种,但根据尾扇保存完好的特征,可以将其归入 Palaeocaris Meek 和 Worthen,1865 年。这是该属在苏格兰的首个记录,不过,1979 年从比尔斯登的纳穆里亚(Serpukhovian,上密西西比统)页岩中发现的 Minicaris brandi Schram 标本现在也被认为是 Palaeocaris 的一个物种。
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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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