北艾尔郡Trearne Quarry SSSI(密西西比系,下石炭世)海鲷新记录

IF 0.5 4区 地球科学 Q4 GEOLOGY Scottish Journal of Geology Pub Date : 2021-03-08 DOI:10.1144/sjg2020-012
Gary Hoare, S. Donovan
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引用次数: 0

摘要

苏格兰西南部艾尔郡(Ayrshire)的密西西比演替区,虽然主要以碎片形式保存下来,但仍有丰富的海鲷化石。Trearne采石场在某些地平线上生产中等常见的海百合杯和海百合。在已有文献记载的两个名义分类群的基础上,我们又增加了七个,除了一个例外,都是支群。这些物种都来自下灰岩组(密西西比期Visean)的Blackhall石灰岩。在Trearne采石场发现的名称海蝇类包括:Rhabdocrinus scotocarbonarius (Wright)、Ureocrinus bockschii (Geinitz)、Ureocrinus globulus (de Koninck)、Tyrieocrinus laxus Wright、Fifeocrinus tielensis (Wright)、Hydreionocrinus formosus Wright、Parazeacrinites konincki (Bather)和Phanocrinus ardrossensis (Wright);和Diplobathrida, Camerata: Cribanocrinus baccatus (Wright)。物种的分布局限于一个或几个泥岩层。可识别的海百合在块状、富含珊瑚的珊瑚礁相中是罕见的。
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New records of crinoids from Trearne Quarry SSSI (Mississippian, Lower Carboniferous), north Ayrshire
The Mississippian succession of Ayrshire, SW Scotland, is rich in fossil crinoids, albeit mainly preserved as fragments. Trearne Quarry is exceptional in yielding moderately common crinoid cups and thecae from certain horizons. To the two nominal taxa that have been documented hitherto, we add a further seven, all cladids with one exception. These species all come from the Blackhall Limestone of the Lower Limestone Formation (Visean, Mississippian). Nominal crinoid species identified from Trearne Quarry include Cladida: Rhabdocrinus scotocarbonarius (Wright), Ureocrinus bockschii (Geinitz), Ureocrinus globulus (de Koninck), Tyrieocrinus laxus Wright, Fifeocrinus tielensis (Wright), Hydreionocrinus formosus Wright, Parazeacrinites konincki (Bather) and Phanocrinus ardrossensis (Wright); and Diplobathrida, Camerata: Cribanocrinus baccatus (Wright). Species have distributions limited to one or a few mudrock beds. Identifiable crinoids are uncommon in massive, coral-rich reefal facies.
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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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