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

机译:陆地和陆地外部生命挑战的最新进展。

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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:谎言在宇宙中的起源和散布是一个长期争论的科学和哲学问题。有史以来最大的困惑之一就是生命是如何产生的?普遍认为,生命源于富含碳化合物的汤,但是这些有机分子从何而来呢?这些有机分子可能来自内源性或外源性,还是来自两者仍是争论的话题。根据第一个渠道,生命起源的内生性理论得到了米勒,奥尔格,伯纳尔,弗里斯,拉哈夫,张和卡玛拉丹等科学家的工作的支持。早期生命起源所需的基本有机分子。由45亿年前的地球早期大气中丰富的无机化合物合成而成。根据第二个渠道,生命起源的外生理论得到了Oro,Chyba,Sagan,Horneck,Russell和Greenberg等科学家的支持。有人提出,生命起源所需的分子前体是从太空转移到原始地球的。根据介于第一和第二之间的第三通道,该假设得到了小林,卡斯特丁,福克斯,披萨勒洛和特瓦里等科学家的研究的支持。这表明原始地球上第一生命的先驱物是外源性和内源性的输入。资料来源。在目前的工作中,已经研究了在中性pH下2,4-二硝基苯胺(2,4-DNA)和2,4,4,6-三硝基苯胺(2,4,6-TNA)与锂蒙脱石,高岭石和绿脱石粘土矿物的吸附相互作用。 (7 0.01)和温度30 1C。分光光度法通过在相应的最大值下测量胺溶液的吸光度来跟踪吸附的进程。吸附过程一般遵循Langmuir模型。高岭土和绿脱石分别显示出两种被吸附物的最大和最小吸收能力。与所有三种吸附剂相比,2、4、6-TNA显示出比2、4-DNA更强的吸附。目前的研究表明粘土矿物在稳定原始地球上降解生物分子方面的重要性。这项研究支持了地球生命起源的假说。详细介绍。

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