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Synthesis of Organic Matter in Aqueous Environments Simulating Small Bodies in the Solar System and the Effects of Minerals on Amino Acid Formation

机译:在太阳系中模拟小型体的水环境中有机质的合成及矿物质对氨基酸形成的影响

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摘要

The extraterrestrial delivery of organics to primitive Earth has been supported by many laboratory and space experiments. Minerals played an important role in the evolution of meteoritic organic matter. In this study, we simulated aqueous alteration in small bodies by using a solution mixture of H2CO and NH3 in the presence of water at 150 °C under different heating durations, which produced amino acids after acid hydrolysis. Moreover, minerals were added to the previous mixture to examine their catalyzing/inhibiting impact on amino acid formation. Without minerals, glycine was the dominant amino acid obtained at 1 d of the heating experiment, while alanine and β-alanine increased significantly and became dominant after 3 to 7 d. Minerals enhanced the yield of amino acids at short heating duration (1 d); however, they induced their decomposition at longer heating duration (7 d). Additionally, montmorillonite enhanced amino acid production at 1 d, while olivine and serpentine enhanced production at 3 d. Molecular weight distribution in the whole of the products obtained by gel chromatography showed that minerals enhanced both decomposition and combination of molecules. Our results indicate that minerals affected the formation of amino acids in aqueous environments in small Solar System bodies and that the amino acids could have different response behaviors according to different minerals.
机译:许多实验室和太空实验支持了对原始地球的有机物的外星分娩。矿物质在陨石有机物的演变中发挥了重要作用。在这项研究中,我们通过在不同加热持续时间下在150℃下使用H 2 CO和NH 3的溶液混合物来模拟小体的水性改变,在不同的加热持续时间下产生酸性水解后的氨基酸。此外,将矿物添加到先前的混合物中以检查它们对氨基酸形成的催化/抑制抗冲击。没有矿物质,甘氨酸是在加热实验的1 d处获得的主要氨基酸,而丙氨酸和β-丙氨酸显着增加,并且在3至7天后变得显着。矿物质在短加热持续时间(1d)增强氨基酸的产率;然而,它们在更长的加热持续时间(7d)诱导它们的分解。此外,Montmorillonite在1 d处增强氨基酸产生,而橄榄石和蛇形增强的生产在3天。通过凝胶色谱法获得的整个产物中的分子量分布表明,矿物质增强了分解和分子的组合。我们的结果表明,矿物质影响小太阳系体中的水环境中氨基酸的形成,并且氨基酸可根据不同的矿物质具有不同的响应行为。

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