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Chronostratigraphic units in the Jurassic and their boundaries: Definition, recognition and correlation, causal mechanisms

机译:侏罗纪年代地层单位及其边界:定义,认识和相关,因果机制

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摘要

The historical development of the chronostratigraphic classification of the Jurassic into series, stages and zones is summarised. Traditionally, the series and stages are defined hierarchically in terms of the standard (ammonite) zones they contained but since Hedberg (1976) they have been defined by a basal boundary stratotype (GSSP) . To date four Jurassic Stages have ratified GSSPs; progress with the others is outlined. The primary marker for the definition of the Stage boundaries is biochronology based on evolution of ammonites, with secondary markers based on biostratigraphy of other fossil groups, chemostratigraphy and magnetostratigraphy. Causal mechanisms for the environmental changes that caused ammonite evolution are reviewed and possible methods of correlation with non-marine successions are briefly discussed.
机译:总结了侏罗纪年代地层分类在系列,阶段和地区上的历史发展。传统上,系列和阶段是根据它们所包含的标准(炸药)区域进行分层定义的,但是自Hedberg(1976年)以来,它们已经由基础边界平层型(GSSP)定义了。迄今为止,已经有四个侏罗纪阶段批准了GSSP。概述了与他人的进步。阶段边界定义的主要标记是基于铵矿演化的生物年代学,辅助标记是基于其他化石群的生物地层学,化学地层学和磁地层学。综述了引起铵盐演化的环境变化的成因机制,并简要讨论了与非海洋演替相关的可能方法。

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