Survivability and pathways of amino acids in oceanic hydrothermal systems: A mechanistic study of phenylalanine

IF 4.5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Alexandria Aspin, Rhys Ellis, Megan Stull, Ziming Yang
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引用次数: 0

Abstract

The survivability and pathways of amino acids in oceanic hydrothermal systems can be affected by fluid chemistry and composition including the presence of inorganic materials, however, their specific effects and underlying mechanisms remain largely unexplored. Using phenylalanine as a model compound, we find that decarboxylation is the primary degradation pathway for amino acids followed by deamination, via either substitution or elimination. Amino acid reactivity is influenced by solution pH, with degradation being strongly inhibited under highly acidic or alkaline conditions. The presence of dissolved metal salts not only changes the distribution of decarboxylation and deamination products but also plays a protective role, inhibiting the decomposition of amino acids. Overall, this study suggests that both relatively extreme pH and surrounding metal salts could enhance the survivability of amino acids, which may provide new insights into understanding the preservation and distribution of amino acids in oceanic hydrothermal systems on and outside Earth.
氨基酸在海洋热液系统中的生存能力和途径:苯丙氨酸的机理研究
氨基酸在海洋热液系统中的生存能力和途径可能受到流体化学和组成(包括无机物质的存在)的影响,然而,它们的具体作用和潜在机制在很大程度上仍未被探索。使用苯丙氨酸作为模型化合物,我们发现脱羧是氨基酸的主要降解途径,然后是脱胺,通过取代或消除。氨基酸的反应性受溶液pH的影响,在高酸性或碱性条件下,氨基酸的降解受到强烈抑制。溶解的金属盐的存在不仅改变了脱羧和脱胺产物的分布,而且起到了保护作用,抑制了氨基酸的分解。总的来说,本研究表明,相对极端的pH值和周围的金属盐都可以增强氨基酸的生存能力,这可能为理解地球内外海洋热液系统中氨基酸的保存和分布提供新的见解。
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来源期刊
Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta 地学-地球化学与地球物理
CiteScore
9.60
自引率
14.00%
发文量
437
审稿时长
6 months
期刊介绍: Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes: 1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids 2). Igneous and metamorphic petrology 3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth 4). Organic geochemistry 5). Isotope geochemistry 6). Meteoritics and meteorite impacts 7). Lunar science; and 8). Planetary geochemistry.
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