关于这个题目——石炭纪的时间尺度

Special Publications Pub Date : 2022-04-13 DOI:10.1144/sp512
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引用次数: 0

摘要

石炭纪是冈瓦南超大陆与拉俄斯超大陆碰撞形成泛大陆的时期,是晚古生代冰期的主要间歇期。这些构造和气候事件引起了剧烈的海平面波动和气候变化,并产生了一个在地形和气候上都很多样化的石炭纪世界,在这种多样性上,也许只有晚新生代世界才能与之匹敌。此外,石炭纪是一个积累了大量具有重大经济和社会意义的煤矿的时代。因此,石炭纪地质和生物事件的时间顺序对于解释地球历史上一些独特和关键的事件至关重要。这种时间顺序是基于石炭纪的时间尺度,它已经发展和完善了近两个世纪。这本书回顾了石炭系年代地层尺度的发展历史,包括石炭系放射性同位素年龄、磁地层学、同位素对比、旋回地层学和与时间尺度相关的海洋和非海洋生物地层学和生物年代学的综合分析。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
About this title - The Carboniferous Timescale
The Carboniferous was the time of the assembly of Pangaea by the collision of the Gondwanan and Larussian supercontinents, and the principal interval of the late Paleozoic ice ages. These tectonic and climatic events caused dramatic sea-level fluctuations and climate changes and produced a Carboniferous world that was diverse topographically and climatologically, perhaps only rivalled in that diversity by the late Cenozoic world. Furthermore, the Carboniferous was a time of the accumulation of vast coal deposits of great economic and societal significance. The temporal ordering of geological and biotic events during Carboniferous time thus is critical to the interpretation of some unique and pivotal events in Earth history. This temporal ordering is based on the Carboniferous timescale, which has been developed and refined for nearly two centuries. This book reviews the history of the development of the Carboniferous chronostratigraphic scale and includes comprehensive analyses of Carboniferous radioisotopic ages, magnetostratigraphy, isotope-based correlations, cyclostratigraphy and timescale-relevant marine and non-marine biostratigraphy and biochronology.
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