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首页> 外文期刊>Palaeobiodiversity and Palaeoenvironments >Palynology of the Kazanian stratotype section (Permian, Russia): palaeoenvironmental and palaeoclimatic implications
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Palynology of the Kazanian stratotype section (Permian, Russia): palaeoenvironmental and palaeoclimatic implications

机译:喀山平流层剖面的孢粉学(俄罗斯二叠纪):古环境和古气候意义

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摘要

Palynomorph assemblages reflect changes in land plant communities and are thus significant proxies to interpret palaeoenvironmental and palaeoclimatic changes. The Middle Permian of the East European Platform is crucial to the understanding of marine and non-marine palaeoclimate archives and interregional correlations of marine and non-marine successions, utilising palaeoclimate signatures documented in the palynological record. New palynological data from the Kazanian stratotype section are presented and interpreted with respect to palaeoenvironment and palaeoclimate. This dataset will serve as a basis for ongoing studies on the type area of the Kazanian and the mid-Permian biodiversity patterns, preceding the end-Guadalupian crisis and the changes of the end-Permian biotic diversification followed by the most severe extinction event in Earth's history at the Permian-Triassic boundary.
机译:苔藓类植物组合反映了陆地植物群落的变化,因此是解释古环境和古气候变化的重要代表。利用古生物学记录中记载的古气候特征,东欧平台的中二叠纪对于理解海洋和非海洋古气候档案以及区域间海洋和非海洋演替的相互关系至关重要。提出并解释了来自喀山地层标本部分的新的古生物学数据,包括古环境和古气候。该数据集将为正在进行的喀山时期和二叠纪中部生物多样性类型区域研究提供基础,在瓜达卢普末危机之前,二叠纪末生物多样性的变化随后是地球上最严重的灭绝事件的变化。二叠纪-三叠纪边界的历史。

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