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首页> 外文期刊>Journal of micropalaeontology: the journal of the British Micropalaeontological Society >Conodont micropalaeontology of mid-Ordovician aged limestone clasts from Lower Old Red Sandstone conglomerates, Lanark and Strathmore basins, Midland Valley, Scotland
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Conodont micropalaeontology of mid-Ordovician aged limestone clasts from Lower Old Red Sandstone conglomerates, Lanark and Strathmore basins, Midland Valley, Scotland

机译:来自苏格兰米德兰河谷拉纳克和斯特拉斯莫尔盆地下老红砂岩砾岩的奥陶纪中古年龄石灰岩碎屑的牙形石微古生物学

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摘要

Mid-Ordovician limestone clasts in the Lower Old Red Sandstone conglomerates of the Lanark and Strathmore basins of the Midland Valley, Scotland, were derived from a cryptic carbonate platform, now hidden beneath the Southern Uplands Allochthon. These have yielded 17 multi-element species of conodonts, which are systematically described herein and include the eponymous biozonal species Pygodus serra and Pygodus anserinus. The fauna represents an outer shelf-ocean margin biofacies, found only in Upper Ordovician conglomerates in the Southern Uplands and the Malopolska Terrane, Poland. [References: 67]
机译:苏格兰米德兰河谷Lanark和Strathmore盆地的下老红砂岩砾岩中的奥陶纪中部石灰石碎屑来自一个隐秘的碳酸盐岩台地,该地层现在隐藏在南部高地Allochthon之下。这些已经产生了17种牙形石的多元素物种,在本文中对其进行了系统地描述,并且包括同名的生物地带物种Pygodus serra和Pygodus anserinus。该动物群代表了一个外部陆架海洋边缘生物相,仅在南部高地和波兰的Malopolska Terrane的上奥陶纪砾岩中发现。 [参考:67]

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