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Palynology of Archean microfossils (c. 3.0 Ga) from the Mount Grant area, Pilbara Craton, Western Australia: Further evidence of biogenicity

机译:来自西澳大利亚州Pilbara Craton的Mount Grant地区的太古代微化石(约3.0 Ga)的孢粉学:生物成因的进一步证据

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Palynological techniques have only rarely been applied to Archean rocks, mainly because of concerns about contamination. However, where microstructures are abundant and well documented, palynology can add considerably to interpretations based on thin-section examination. A modified palynological preparation method, which avoids vigorous physical or chemical methods that might cause the fragmentation of fragile specimens, was applied to black chert from the c. 3.0 Ga Farrel Quartzite of the Mount Grant area, Pilbara Craton, Western Australia, known to contain abundant microstructures of putative biogenic origin. Four main morphological types have been reported from chert thin sections: threads, films, hollow spheres and spindles. These microstructures exhibit morphological and chemical signatures consistent with a biological origin as well as showing features indicative of taphonomic degradation. Nevertheless, the possibility remains that they are artefacts. Similar structures have been attributed to physical processes, such as the accretion of fine particulate matter that has subsequently been redistributed as a result of crystal growth. By extracting structures palynologically, we have increased the probability of a biogenic origin. Firstly, examination of the morphology free of the encompassing matrix demonstrates that they are indeed three-dimensional structures with complex morphology; secondly, the extraction of entire specimens militates against them being particulate matter aggregations, which would simply disintegrate during preparation and thirdly, the chemicals used remove silicates and most other minerals, confirming the organic composition of the structures. To date, we have extracted films, hollow spheres and a few poorly preserved spindles, but preparation continues. The fact that the specimens retain their morphological integrity during palynological extraction argues strongly in favour of a biogenic origin for the microstructures.
机译:孢粉学技术很少应用于太古代岩石,主要是因为担心污染。但是,在微观结构丰富且有据可查的地方,孢粉学可以大大增加基于薄层检查的解释。改良的孢粉学制备方法避免了可能导致易碎样品碎裂的剧烈物理或化学方法,并被用于从c中得到的黑black石。西澳大利亚州Pilbara Craton芒特格兰特地区的3.0 Ga Farrel石英岩,据称含有丰富的假定生物成因微结构。石薄层中已报告了四种主要的形态类型:线,薄膜,空心球和纺锤体。这些微结构表现出与生物学起源一致的形态学和化学特征,并且显示出指示出自相降解的特征。但是,仍然存在它们是人工制品的可能性。类似的结构也归因于物理过程,例如细小颗粒物质的积聚,其随后由于晶体生长而重新分布。通过昆虫学提取结构,我们增加了生物起源的可能性。首先,没有包容性基质的形态检查表明它们确实是具有复杂形态的三维结构。其次,整个标本的提取阻止了它们成为颗粒状物质的聚集,在制备过程中会简单地分解,其次,所用化学物质去除了硅酸盐和大多数其他矿物,从而确定了结构的有机组成。迄今为止,我们已经提取了薄膜,空心球和一些保存不良的纺锤,但是准备工作仍在继续。标本在孢粉提取过程中保持其形态完整性的事实强烈证明了微结构的生物起源。

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