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Palynology of the Kazanian stratotype section (Permian, Russia) : palaeoenvironmental and palaeoclimatic implications

机译:喀山阶层剖面(俄罗斯二叠纪)的孢粉学: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 thussignificant proxies to interpret palaeoenvironmental and palaeoclimatic changes. The Middle Permianof the East European Platform is crucial to the understanding of marine and non-marine palaeoclimatearchives and interregional correlations of marine and non-marine successions, utilizing palaeoclimatesignatures documented in the palynological record. New palynological data from the Kazanianstratotype 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 thePermian-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。东欧平台的中二叠纪对古生物学记录中记载的古气候特征而言,对于理解海洋和非海洋古气候档案和区域性海洋和非海洋演替的相互关系至关重要。提出并解释了喀山地层模式部分的新的古生物学数据,涉及古环境和古气候。该数据集将为继续研究喀山类型区域和二叠纪中部生物多样性模式,瓜达卢普末末危机和二叠纪末期生物多样性的变化,然后是二叠纪-三叠纪边界地球历史上最严重的灭绝事件。

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