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Palynology of a terrestrial coal-bearing series across the Triassic/Jurassic boundary (Mecsek Mts, Hungary)

机译:跨越三叠纪/侏罗纪边界的陆上含煤系列的孢粉学(匈牙利,梅切克山)

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摘要

Abstract Palynology and palynofacies patterns of terrestrial Triassic/Jurassic boundary series of the South Hungarian Mecsek Mountains were studied in search of paleoenvironmental and vegetation changes and climatic signatures related to one of the major mass extinction events in Earth's history. Two selected and studied boreholes comprise continuous boundary sections and yield a diverse Late Rhaetian to Hettangian palynomorph assemblage. The most striking feature within the boundary interval is the series of cyclic short-term paleoenvironmental changes from fluvial/deltaic to swamp settings, as inferred from changes in palynomorph associations. However, increasing humidity is documented by a striking increase in trilete spores. These signatures display the response of terrestrial vegetation to regional and global environmental changes, although we found no clear evidence for a mass extinction as documented in the microflora.
机译:摘要为了研究与地球历史上主要的物种大灭绝事件有关的古环境和植被变化以及气候特征,研究了匈牙利南部麦切克山地陆三叠纪/侏罗纪边界系列的古生物学和古相格局。经过选择和研究的两个钻孔包括连续的边界部分,产生了不同的晚Rhaetian至Hettangian palynomorph组合。边界区间内最显着的特征是从河流/三角洲到沼泽环境的一系列周期性短期古环境变化,这是由古怪形态相关性推断得出的。但是,Trilete孢子的显着增加证明了湿度的增加。这些签名显示了陆地植被对区域和全球环境变化的响应,尽管我们没有发现微生物群落中记载的大规模灭绝的明确证据。

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