首页> 外文期刊>Astrobiology >Blogenicity of Morphologically Diverse Carbonaceous Microstructures from the ca. 3400 Ma Strelley Pool Formation, in the Pilbara Craton, Western Australia
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Blogenicity of Morphologically Diverse Carbonaceous Microstructures from the ca. 3400 Ma Strelley Pool Formation, in the Pilbara Craton, Western Australia

机译:从ca.形态多样的碳质微结构的生泡性。西澳大利亚州Pilbara Craton的3400 Ma Strelley泳池形成

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摘要

Morphologically diverse structures that may constitute organic microfossils are reported from three remote and widely separated localities assigned to the ca. 3400 Ma Strelley Pool Formation in the Pilbara Craton, Western Australia. These localities include the Panorama, Warralong, and Goldsworthy greenstone belts. From the Panorama greenstone belt, large (>40 μm) lenticular to spindle-like structures, spheroidal structures, and mat-forming thread-like structures are found. Similar assemblages of carbonaceous structures have been identified from the Warralong and Goldsworthy greenstone belts, though these assemblages lack the thread-like structures but contain film-like structures.All structures are syngenetic with their host sedimentary black chert, which is associated with stromatolites and evaporites. The host chert is considered to have been deposited in a shallow water environment. Rigorous assessment of biogenicity (considering composition, size range, abundance, taphonomic features, and spatial distributions) suggests that cluster-forming small (<15μm) spheroids, lenticular to spindle-like structures, and film-like structures with small spheroids are probable microfossils. Thread-like structures are more likely fossilized fibrils of biofilm, rather than microfossils. The biogenicity of solitary large (>15 μm) spheroids and simple film-like structures is less certain. Although further investigations are required to confirm the biogenicity of carbonaceous structures from the Strelley Pool Formation, this study presents evidence for the existence of morphologically complex and large microfossils at 3400 Ma in the Pilbara Craton, which can be correlated to the contemporaneous, possible microfossils reported from South Africa. Although there is still much to be learned, they should provide us with new insights into the early evolution of life and shallow water ecosystems.
机译:据报道,从三个偏远和广泛分离的地区,据报道可能构成有机微化石的形态多样的结构。西澳大利亚州Pilbara Craton的3400 Ma Strelley泳池形成。这些地区包括Panorama,Warralong和Goldsworthy绿岩带。在Panorama绿岩带中,发现大的(> 40μm)透镜状至纺锤状结构,球状结构和形成垫的线状结构。从Warralong和Goldsworthy绿岩带中发现了相似的碳质结构组合,尽管这些组合缺少线状结构但包含膜状结构。所有结构均与它们的宿主沉积黑石同生,后者与叠层石和蒸发岩有关。认为该母石已沉积在浅水环境中。严格的生物成因评估(考虑组成,大小范围,丰度,自发特征和空间分布)表明,形成簇状的小球体(<15μm),球状到纺锤状的结构以及具有小球状的膜状结构都是可能的微化石。 。线状结构更可能是生物膜的化石原纤维,而不是微化石。单独的大(> 15μm)球状体和简单的膜状结构的生物成因性尚不确定。尽管需要进一步的研究来确认Strelley Pool组碳质结构的生物成因,但这项研究提供了Pilbara Craton 3400 Ma处形态复杂而大型的微化石存在的证据,这可能与据报道同时存在的可能的微化石有关来自南非。尽管还有很多东西要学,但它们应该为我们提供有关生命和浅水生态系统早期演变的新见解。

著录项

  • 来源
    《Astrobiology》 |2010年第9期|p.899-920|共22页
  • 作者单位

    Department of Environmental Engineering and Architecture Graduate School of Environmental Studies Nagoya University Nagoya 464-8601 Japan;

    Department of Geology, University of Liege, Liege, Belgium;

    School of Informatics and Sciences, Nagoya University, Nagoya, Japan;

    Department of Earth and Environmental Sciences, Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan;

    Geological Survey of Western Australia, Department of Mines and Petroleum, East Perth, Australia,Australian Centre for Astrobiology, University of New South Wales, Sydney, Australia;

    Australian Centre for Astrobiology, University of New South Wales, Sydney, Australia,Astromaterials Research and Exploration Science, NASA Johnson Space Center, Houston, Texas, USA;

    Australian Centre for Astrobiology, University of New South Wales, Sydney, Australia;

  • 收录信息 美国《科学引文索引》(SCI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    archean; biogenicity; microfossils; pilbara;

    机译:太古代生物成因微化石皮巴拉;
  • 入库时间 2022-08-17 13:09:34

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