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从水-黄铁矿界面上释放氨基酸和肽:生命起源于矿物表面的案例研究。

Unbinding events of amino acids and peptides from water-pyrite interfaces: A case study of life's origin on mineral surfaces.

机构信息

Chemical Evolution Lab Unit, Earth-Life Science Institute (ELSI), Tokyo Institute of Technology, 2-12-1-IE-1 Ookayama, Meguro-ku, Tokyo 152-8550, Japan; School of Materials and Chemical Technology, Tokyo Institute of Technology, 4259 Nagatsuta, Midori-ku, Yokohama 226-8502, Japan.

School of Materials and Chemical Technology, Tokyo Institute of Technology, 4259 Nagatsuta, Midori-ku, Yokohama 226-8502, Japan.

出版信息

Biophys Chem. 2020 May;260:106338. doi: 10.1016/j.bpc.2020.106338. Epub 2020 Feb 26.

Abstract

Selective binding of aqueous-phase amino acids to mineral surfaces is regarded as a plausible first step in oligopeptide formation on early Earth. To clarify the strength and underlying mechanism of amino acid binding to pyrite surfaces, we measured the unbinding (pull-off) force of ten amino acids and two oligo-peptides from water-pyrite interfaces using atomic force microscopy (AFM). The most probable unbinding force could be described by a linearly increasing function with the size of the amino acid and a characteristic offset. A good correlation was obtained between the most probable unbinding force and the residue volume, surface area and polarizability of samples suggesting at least a partial contribution of van der Waals (vdW) forces, especially the London dispersion force. These results are useful in analysis of adhesion phenomena of amino acids in the given environmental settings such as in this work.

摘要

水相向矿物表面的选择性结合被认为是早期地球上寡肽形成的合理第一步。为了阐明氨基酸与黄铁矿表面结合的强度和潜在机制,我们使用原子力显微镜(AFM)测量了来自水-黄铁矿界面的十种氨基酸和两种寡肽的解吸(拉开)力。最可能的解吸力可以用氨基酸的大小和特征偏移的线性递增函数来描述。最可能的解吸力与样品的残基体积、表面积和极化率之间存在很好的相关性,表明至少有范德华(vdW)力的部分贡献,特别是伦敦色散力。这些结果对于分析给定环境设置(如本工作中)下氨基酸的粘附现象很有用。

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