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Microfossils, biomolecules and biominerals in carbonaceous meteorites: implications to the origin of life

机译:碳质陨石中的微生物,生物分子和生物体:对生命起源的影响

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Environmental and Field Emission Scanning Electron Microscopy (ESEM and FESEM) investigations haveshown that a wide variety of carbonaceous meteorites contain the remains of large filaments embedded withinfreshly fractured interior surfaces of the meteorite rock matrix. The filaments occur singly or in denseassemblages and mats and are often encased within carbon-rich, electron transparent sheaths. ElectronDispersive X-ray Spectroscopy (EDS) spot analysis and 2D X-Ray maps indicate the filaments rarely havedetectable nitrogen levels and exhibit elemental compositions consistent with that interpretation that of themeteorite rock matrix. Many of the meteorite filaments are exceptionally well-preserved and show evidenceof cells, cell-wall constrictions and specialized cells and processes for reproduction, nitrogen fixation,attachment and motility. Morphological and morphometric analyses permit many of the filaments to beassociated with morphotypes of known genera and species of known filamentous trichomic prokaryotes(cyanobacteria and sulfur bacteria). The presence in carbonaceous meteorites of diagenetic breakdownproducts of chlorophyll (pristane and phytane) along with indigenous and extraterrestrial chiral protein aminoacids, nucleobases and other life-critical biomolecules provides strong support to the hypothesis that thesefilaments represent the remains of cyanobacteria and other microorganisms that grew on the meteorite parentbody. The absence of other life-critical biomolecules in the meteorites and the lack of detectable levels ofnitrogen indicate the filaments died long ago and can not possibly represent modern microbial contaminantsthat entered the stones after they arrived on Earth. This paper presents new evidence for microfossils,biomolecules and biominerals in carbonaceous meteorites and considers the implications to some of the majorhypotheses for the Origin of Life.© (2012) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
机译:环境和场发射扫描电子显微镜(ESEM和FESEM)调查haveshown,多种碳质陨石包含嵌入的陨石岩石基质的withinfreshly断裂内表面大长丝的遗迹。长丝发生单独或denseassemblages和垫和通常富碳,电子透明护套内包住。 ElectronDispersive X射线光谱(EDS)分析点和2D X射线图表明长丝很少havedetectable氮水平并且表现出themeteorite岩石基体的与解释相一致的元素组成。许多陨石长丝是格外保存完好,并显示用于再现,固氮,附着和蠕动evidenceof细胞,细胞壁和收缩特化细胞和进程。形态学和形态分析允许许多长丝的与已知的属已知丝状trichomic原核生物(蓝藻和硫细菌)的物种的形态beassociated。与土著和外星人手性蛋白氨基酸,核酸碱基和其他生命攸关的生物分子沿叶绿素的成岩breakdownproducts(姥鲛烷和植烷)的碳质陨石存在提供了thesefilaments代表蓝藻和其他微生物的生长出的遗体的假设强有力的支持陨石parentbody。由于没有在陨石其他生命攸关的生物分子和缺乏检测水平的ofnitrogen表明细丝很早就去世,也不可能代表了现代微生物contaminantsthat进入石头他们来到地球之后。本文介绍了在碳质陨石微体化石,生物分子和生物矿物新的证据,并考虑到一些majorhypotheses生命起源的意义。©(2012)光光学仪器工程师著作权协会(SPIE)。抽象的下载被允许仅供个人使用。

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