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首页> 外文期刊>Precambrian Research >Carbonaceous biosignatures of diverse chemotrophic microbial communities from chert nodules of the Ediacaran Doushantuo Formation
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Carbonaceous biosignatures of diverse chemotrophic microbial communities from chert nodules of the Ediacaran Doushantuo Formation

机译:来自埃德拉甘山山尘器形成的Chert Nodules多种嗜培素微生物群落的碳质生物炎

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The Ediacaran Doushantuo Formation (DST) is renowned for exceptionally preserved Precambrian fossils including metazoans. Some of these fossils, particularly microfossils such as multicellular algae and acanthomorphic acritarchs, are preserved in DST chert nodules. To better understand the geomicrobiological processes that contributed to the authigenic formation of DST chert nodules and facilitated exceptional fossil preservation, we analyzed organic matter in these chert nodules and the surrounding matrix (calcareous mudstone) using multiple in-situ techniques: confocal laser Raman spectroscopy, micro-Fourier transform infrared spectroscopy (FTIR), and secondary ion mass spectroscopy (SIMS). We found strong ultrastructural, chemical, and isotopic heterogeneities in the organic matter as indicated by the Raman spectral parameter 1-1350/1600 ranging from 0.49 to 0.88, the infrared spectral index R-3/2 from 0.12 to 0.90, and an estimated delta 13C(org-SIMS) range of 44%, (V-PDB). These micron-scale heterogeneities imply that the organic matter preserved in the DST chert nodules is derived from different carbonaceous sources in a diverse microbial ecosystem, including eukaryotic and/or prokaryotic photoautotrophs, as well as chemotrophs involved in the fermentation and probably anaerobic oxidation of organic remains. Thus, the microbial ecosystems in Ediacaran ocean waters and sediments were more complex than previously thought, and these microbial processes controlled dynamic micro-environments in DST sediments where chert nodules were formed and fossils were mineralized. The results also show that variations in the relative abundances, activities, and interactions of co-existing microorganisms in DST sediments may have modulated delta 13C(org), shifts, causing local decoupling between delta 13C(org) and delta 13C(carb) as measured in bulk samples. (C) 2017 Elsevier B.V. All rights reserved.
机译:埃迪克兰·迪山沱组(DST)被着名,用于异常保存的预先预保证化石化石,包括美唑烷。这些化石中的一些,特别是微细胞藻类和刺激素素质的微生物,在DST Chert结节中保存。为了更好地了解有助于DST Chert结节的Authigenic形成和促进特殊化石保存的地质性工艺,我们使用多种原位技术分析了这些Chert结节和周围基质(钙质泥岩)中的有机物:共聚焦激光拉曼光谱,微傅里叶变换红外光谱(FTIR)和二次离子质谱(SIMS)。我们在有机质中发现了强大的超微结构,化学和同位素异质性,如拉曼光谱参数1-1350 / 1600从0.49到0.88,红外光谱指数R-3/2从0.12〜0.90,以及估计的三角洲13C(ORG-SIMS)范围为44%(V-PDB)。这些微级异质性意味着DST Chert结节中保存的有机物质衍生自不同的微生物生态系统中的不同碳质源,包括真核和/或原核光滑萎缩,以及参与发酵和有机厌氧氧化的嗜疗法遗迹。因此,埃德拉甘海水和沉积物中的微生物生态系统比以前认为更复杂,这些微生物过程控制了DST沉积物中的动态微环境,其中形成了Chert结节并矿化了化石。结果还表明,DST沉积物中共存微生物的相对丰富,活性和相互作用的变化可以具有调节的δ13C(ORG),换档,导致DELTA 13C(ORG)和DELTA 13C(CARB)之间的局部去耦。在散装样品中测量。 (c)2017 Elsevier B.v.保留所有权利。

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