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Microfossils from the Paleoproterozoic Hutuo Group, Shanxi, North China: Early evidence for eukaryotic metabolism

机译:来自华北山西山西古水古代古托集团的Microfossils:真核新陈代谢的早期证据

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摘要

The Paleoproterozoic Hutuo Group is well-developed and distributed in the Wutai Mountains in the Xinzhou area of Shanxi Province, North China. Its middle part - the Dongye Subgroup is more suitable for obtaining microfossils in deposited sediments characterized with sandstone or slate in the lower part, and upward into interbedded sandstone, carbonate with stromatolites and phyllite. Based on recent zircon dating, the Hutuo Group was deposited around 2150-1950 Ma. In this study, eight morphological genera of microfossils, including the spheroid and filamentous cyanobacteria Eoentophysalis, Sphaerophycus, Siphonophycus, Pseudodendron, and the acritarchs Dictyosphaera, Dongyesphaera gen. nov., Leiosphaeridia, Satka were identified from the Wenshan, Hebiancun and Tianpengnao Formations of the Dongye Subgroup. The identified microfossils reveal that eukaryotic protists exercised metabolic activities rarely observed to have occurred in what are thought to have been suitable environments.
机译:古普罗佐奇河道集团在华北山西省鑫州地区的五泰山区开发和分发。 其中间部分 - 东亚亚群更适合于在沉积的沉积物中获得微生物,其特征在于砂岩或下部的砂岩,并向上进入夹层夹层,碳酸盐与血栓抗植物和植物。 基于最近的锆浦约会,Hutuo Group沉积在2150-1950 mA左右。 在这项研究中,八种形态学属的微生物,包括球茎和丝状菌eoo球茎,Sphaerophycus,虹吸膜炎,假蒽醌和Acritachs Dictyosphaera,Dongyesphaera Gen。 11月,莱西沙伊西亚,Satka是从文山,Hebiancun和Diangengnao组的核心亚组的形成。 所识别的微溶胶表明,真核保护物行使代谢活动很少被观察到所认为是合适的环境。

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