用有孔虫、钙质藻类和红珊瑚测定上vissaman石灰石(爱尔兰西北部)的生物地层年代

Q4 Earth and Planetary Sciences
P. Cózar, I. Somerville, M. Aretz, H. Herbig
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引用次数: 18

摘要

摘要:对爱尔兰西北部Glencar石灰岩、Dartry石灰岩、Bricklieve石灰岩和Meenymore地层多个剖面的有孔虫、钙质藻类和褶皱珊瑚进行了分析。动物群和微生物区系的结果表明,这些地层构成了Glencar石灰岩组和下Bricklieve石灰岩组的早期至晚期Asbian(Cf6β-Cf6γ有孔虫亚区),以及Dartry石灰岩组和上Brickliev石灰岩组的晚期Asbian的上部(Cf5γ亚区)。研究区域内的下一个Meenymore组被划分为Brigantian(Cf6δ亚带)。讨论了先前为Cuilcagh山脉东部的等效地层建立的Goniatite生物带方案,这些方案与本文提出的年代测定不一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Biostratigraphical Dating of Upper Viséan Limestones (NW Ireland) using Foraminiferans, Calcareous Algae and Rugose Corals
Abstract:Foraminiferans, calcareous algae and rugose corals from many sections in the Glencar Limestone, Dartry Limestone, Bricklieve Limestone and Meenymore formations in north-western Ireland have been analysed. Results from the fauna and microflora suggest that these formations constitute the early to late Asbian for the Glencar Limestone Formation and lower Bricklieve Limestone Formation (Cf6β-Cf6γ foraminiferal subzones), and the upper part of the late Asbian for the Dartry Limestone Formation and upper Bricklieve Limestone Formation (Cf6γ Subzone). The succeeding Meenymore Formation in the studied area is assigned to the Brigantian (Cf6δ Subzone). Goniatite biozonal schemes established previously for equivalent strata to the east in the Cuilcagh Mountains that are not in harmony with the dating proposed here are discussed.
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来源期刊
Irish Journal of Earth Sciences
Irish Journal of Earth Sciences Earth and Planetary Sciences-Earth and Planetary Sciences (all)
CiteScore
0.90
自引率
0.00%
发文量
2
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