Site selection of small round holes in crinoid pluricolumnals, Trearne Quarry SSSI (Mississippian, Lower Carboniferous), north Ayrshire, UK

IF 0.5 4区 地球科学 Q4 GEOLOGY
S. Donovan, Gary Hoare
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引用次数: 2

Abstract

Small round holes, Oichnus Bromley, are a locally common feature of crinoid pluricolumnals in the Mississippian of the British Isles. Numerous examples have been found from mudrocks in the Brigantian (Mississippian) Blackhall Limestone, Lower Limestone Formation, at Trearne Quarry, near Beith, north Ayrshire, all assigned to Oichnus simplex Bromley. These trace fossils are typically associated with growth deformities of the pluricolumnals, which are commonly swollen and more rarely grew a lip around the pit. Oichnus simplex is commonly centred on a columnal latus and adjacent sutures between columnals are deflected towards it. More rarely, pits are centred on the sutures between columnals. The O. simplex borings are interpreted as domiciles developed in live crinoids by an indeterminate, unmineralized invertebrate. The pluricolumnals are similar and are presumed to be derived from a single species, perhaps the poteriocrinine cladid Ureocrinus bockshii (Geinitz), the only nominal crinoid recorded from this site.
英国艾尔郡北部Trearne采石场SSSI(密西西比,下石炭纪)海百合多柱体小圆孔的选址
小圆孔,Oichnus Bromley,是不列颠群岛密西西比地区多柱海百合的常见特征。在北艾尔郡贝思附近的Trearne采石场,在Brigantian(密西西比)Blackhall石灰岩下石灰岩组的泥岩中发现了许多例子,所有这些都被分配到Oichnus simplex Bromley。这些痕迹化石通常与多柱骨的生长畸形有关,多柱骨通常肿胀,更罕见的是在坑周围长出唇形。单纯腺瘤通常以柱状体为中心,柱状体之间的相邻缝合线向其偏转。更罕见的是,凹坑集中在柱状骨之间的缝合线上。O. simplex钻孔被解释为由一种不确定的、未矿化的无脊椎动物在活海百合中形成的住所。多柱类相似,推测来自单一种,可能是poteriocrinine cladid Ureocrinus bockshii (Geinitz),这是该地点唯一记录的名义类海麻科植物。
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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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