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UPDATE ON CHALLENGES OF TERRESTRIAL AND EXTRA - TERRESTRIAL ORIGINS OF LIFE

机译:关于陆地和陆地起源的挑战更新

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The origin and dispersion of lie in the universe is a long debated scientific and philosophical issue. One of the greatest puzzles of all time is how did life arise? It has been universally presumed that life arose in a soup rich in carbon compounds, but from where did these organic molecules come? These organic molecules may come from endogenous or exogenous sources or from both is still a subject of debate. According to first channel, endogeneous theory for origins of life is supported by the work of scientists Miller, Orgel, Bernal, Ferris, Lahav, Chang, and Kamaladdin etc. basic organic molecules needed for the origins of an early life. Synthesized from inorganic compounds abundant in the early earth atmosphere 4.5 billion year ago. According to second channel, exogenous theory for origin of life supported by the work of scientists Oro, Chyba, Sagan, Horneck, Russell and Greenberg etc. It was suggested that molecular precursors needed for origins of life transferred from space to the primitive earth. According to third channel, which is midway between first and second, this hypothesis is supported by the work of scientists Kobayashi, Kasting, Fox, Pizzarellow and Tewari etc. which suggests that precursors for first life on primitive earth was input of both exogenous and endogenous sources. In the present work adsorptive interaction of 2, 4 - dinitroaniline (2, 4 - DNA) and 2, 4, 6 - trintroaniline (2, 4, 6 - TNA) with hectorite, kaolinite and nontronite clay minerals have been studied at neutral pH (7 0.01) and a temperature 30 1 C. The progress of the adsorption was followed spectrophotometrically by measuring the absorbance of amines solution at their corresponding max. The adsorption process followed Langmuir model in general. Kaolinitc and nontronite showed maximum and minimum uptake capacity, respectively with both adsorbates. The 2, 4, 6-TNA showed more adsorption than 2, 4 - DNA with all three adsorbents. Present studies suggest the importance of clay minerals in the stabilization of biomolecules from degradation on primitive earth. This study supports the hypothesis of terrestrial origins of life. Detail will be presented.
机译:位于宇宙中的起源和分散是一个很长的争论科学和哲学问题。所有时间的最大谜题之一就是生命如何出现?它普遍推测,生命在富含碳化合物的汤中出现,但是从这些有机分子到来的汤?这些有机分子可能来自内源性或外源性源或两者仍然是争论的主题。根据第一渠道,科学家米勒,Orgel,伯纳尔,弗里斯,骆驼,张和Kamaladdin等的基础上的生命的起源理论是支持的。早期生命的起源所需的基本有机分子。从早期地球大气中丰富的无机化合物合成4.5亿年前。根据第二频道,科学家oro,Chyba,Sagan,Horneck,罗素和格林伯格的工作支持的生命起源理论。建议从空间转移到原始地球的生命起源所需的分子前体。根据第三渠道,这是第一和第二段,这一假设得到了科学家Kobayashi,Kasting,Fox,Pizzarlow和Tewari的支持,这表明原始地球上的第一生命的前体被引入外源性和内源性来源。在中性pH下研究了在中性pH下进行了2,4-二硝基苯胺(2,4,4 - DNA)和2,4,6 - TNA的2,4,6 - TNA)2,4 - 二硝基苯胺(2,4-DNA)和2,4,6 - TNA)的吸附相互作用。已经在中性pH下进行了含量的,高岭石和非巨石粘土矿物质(70.01)和温度30 1 C.通过测量它们相应的最大值的胺溶液的吸光度来遵循分光光度仔细的吸附进度。吸附过程遵循Langmuir模型一般。高岭土和非巨石分别与吸附剂分别显示出最大和最小摄取能力。 2,4,6-TNA显示出比2,4 - DNA更多的吸附,具有所有三种吸附剂。目前的研究表明粘土矿物质在原始地球中退化的生物分子稳定的重要性。本研究支持陆地起源的假设。详细信息将显示。

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