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Trace fossils in Quaternary glacial varved clays near Uppsala, Sweden

机译:瑞典乌普萨拉附近第四纪冰川裂隙粘土中的痕迹化石

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摘要

Trace fossils Broomichnium cf. fliri, Glaciichnium cf. liebegastensis, Planolites isp., ?Undichna isp. and ?Warvichnium ulbrichi have been recognised in early Holocene glacial varved clays near Vittinge, west of Uppsala, Sweden. They are referred to different arthropods and fishes that periodically colonised the lake floor and were important components of the ecosystem. The trace fossils are typical of the Glaciichnium ichnocoenosis within the Mermia ichnofacies, which suggests less stressful conditions in Vittinge than in many other Quaternary varved clays in Europe typified by the Cochlichnus ichnocoenosis.
机译:微量化石Broomichnium cf.弗利里(Gliciichnium),参见liebegastensis,Planolites isp。,Undichna isp。在瑞典乌普萨拉以西的维廷格附近的早期全新世冰川裂隙粘土中,人们已经认识到了α和Warvichnium ulbrichi。它们被称为不同的节肢动物和鱼类,它们定期定居在湖底,是生态系统的重要组成部分。痕迹化石是Mermia ichnofacies中典型的Glaciichnium ichnocoenosis的特征,与欧洲其他以Cochlichnus ichnocoenosis为代表的其他第四纪带瓣粘土相比,Vittinge的应力条件要少。

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