Dr John Grant Malcolmson and a reconciliation of the Middle Devonian Lethen Bar and Lethen House fish bearing nodule localities

IF 0.5 4区 地球科学 Q4 GEOLOGY Scottish Journal of Geology Pub Date : 2023-11-28 DOI:10.1144/sjg2023-011
R. G. Davidson, N. H. Trewin, J. Armstrong, S. R. Waters
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Abstract

The area known as Lethen Bar and Clune, SE of Nairn, Scotland, is a classic Middle Devonian locality which has yielded nodules or concretions, some of which contain fossil fishes with the highest quality of preservation. The locality was largely centred on farm limestone quarries situated around the perimeter of an isolated outlier of the main fishbed. It was first described in the 19 th century, although the upsurge in collecting fossil fishes only occurred some twelve years after the quarries were first mentioned in the scientific literature. Our knowledge of the provenance of the locality is based on very limited accounts, which have never been scientifically tested; these accounts also contain apparent anomalies that have never been adequately addressed. Based on these anomalies, the author of a paper published in 1983 proposed that the locality had been untraceable since the late 19 th century and that the outcrop was quarried out. In 2005, the present authors recorded the first scientifically detailed stratigraphical section of the fishbed, followed in 2021-2023 by detailed field surveys and by a re-appraisal of the literature. This work has resolved the 19 th century anomalies and enabled us to confirm the locations of old quarries, to give affirmation to two previously unrecognised sites, and to show that the outcrop is still present. Thematic collection: This article is part of the Geology of Scotland collection available at: https://www.lyellcollection.org/topic/collections/geology-of-scotland
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约翰-格兰特-马尔科姆森博士与中泥盆世勒森巴尔和勒森豪斯含鱼结核地点的核对工作
位于苏格兰奈恩东南部的莱森巴尔和克鲁恩地区是典型的中泥盆纪地点,这里出产结核或凝块,其中一些含有保存质量极高的鱼类化石。该地点主要以农场石灰岩采石场为中心,这些采石场位于主鱼床一个孤立的外围。尽管在采石场首次被科学文献提及约 12 年后,收集鱼类化石的热潮才兴起,但 19 世纪就首次对该地点进行了描述。我们对该地点来源的了解是基于非常有限的描述,这些描述从未经过科学检验;这些描述还包含明显的异常现象,但从未得到充分解决。基于这些异常现象,1983 年发表的一篇论文的作者提出,该地点自 19 世纪晚期以来就已无迹可寻,露头已被采光。2005 年,本文作者首次对鱼床进行了科学详细的地层剖面记录,随后在 2021-2023 年进行了详细的实地调查,并对文献进行了重新评估。这项工作解决了 19 世纪的异常现象,使我们能够确认旧采石场的位置,确认两个以前未确认的遗址,并表明露头仍然存在。 专题文集: 本文是《苏格兰地质》文集的一部分,可从以下网址获取: https://www.lyellcollection.org/topic/collections/geology-of-scotland
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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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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