First report of fish trace fossils (Undichna) from the Middle Devonian Achanarras Limestone, Caithness Flagstone Group

IF 0.5 4区 地球科学 Q4 GEOLOGY
Benjamin H. Tindal, Anthony P. Shillito, N. Davies
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引用次数: 1

Abstract

Two newly discovered specimens of the fish locomotion trace Undichna (U. britannica and Undichna isp.) are described from the Middle Devonian Achanarras Limestone Member (Caithness Flagstone Group, NE Scotland). Fish trace fossils have not previously been reported from the Achanarras Limestone Member, despite decades of study of the unit as a key locality for fish body fossils. The traces comprise discontinuous sinusoidal grooves; one showing multiple parallel incisions, created by the fins of an acanthodian fish swimming close to the substrate. The apparent absence of trace fossils attributable to infaunal or epifaunal benthic organisms suggests that the sediment at the bottom of the lake was relatively inhospitable. The low ichnodiversity of the Achanarras Limestone Member is likely due to low oxygen levels in the depositional environment. Thematic collection: This article is part of the SJG Early Career Research available at: https://www.lyellcollection.org/cc/SJG-early-career-research
中泥盆世Caithness石板群Achanarras石灰岩鱼迹化石(Undichna)首次报道
描述了苏格兰东北部Caithness Flagstone群中泥盆世Achanarras石灰岩段的两个新发现的鱼类运动痕迹Undichna (U. britannica和Undichna isp.)。尽管数十年来一直将阿查那拉斯石灰岩单元作为鱼体化石的关键地点进行研究,但此前从未报道过鱼类化石的痕迹。所述轨迹包括不连续的正弦凹槽;其中一个显示了多个平行的切口,这是由棘棘鱼的鳍靠近基底游动造成的。明显缺乏归因于动物或底栖生物的痕迹化石表明,湖底的沉积物相对不适宜生存。Achanarras灰岩段的低生物多样性可能是由于沉积环境中的低氧水平造成的。主题集:这篇文章是SJG早期职业研究的一部分,可在:https://www.lyellcollection.org/cc/SJG-early-career-research
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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