Abstract
The interaction strength of progressively longer oligomers of glycine, (Gly), di-Gly, tri-Gly, and penta-Gly, with a natural pyrite surface was directly measured using the force mode of an atomic force microscope (AFM). In recent years, selective activation of abiotically formed amino acids on mineral surfaces, especially that of pyrite, has been proposed as an important step in many origins of life scenarios. To investigate such notions, we used AFM-based force measurements to probe possible non-covalent interactions between pyrite and amino acids, starting from the simplest amino acid, Gly. Although Gly itself interacted with the pyrite surface only weakly, progressively larger unbinding forces and binding frequencies were obtained using oligomers from di-Gly to penta-Gly. In addition to an expected increase of the configurational entropy and size-dependent van der Waals force, the increasing number of polar peptide bonds, among others, may be responsible for this observation. The effect of chain length was also investigated by performing similar experiments using l-lysine vs. poly-l-lysine (PLL), and l-glutamic acid vs. poly-l-glutamic acid. The results suggest that longer oligomers/polymers of amino acids can be preferentially adsorbed on pyrite surfaces.
Highlights
All life on Earth derives from a small cohort of cellular ancestors that emerged some ~3.5 billion years ago [1,2,3]
The interaction of amino acids and mineral surface may have played an important role in chemical evolution leading to the origins of life [12,25]
The degree to which concentration or catalysis could occur depends on the strength of amino acid-mineral adsorption
Summary
All life on Earth derives from a small cohort of cellular ancestors that emerged some ~3.5 billion years ago [1,2,3]. For example, zeta-potential measurements [15], X-ray Photoelectron Spectroscopy (XPS) [16], and catalytic degradation of peptides [17], have been used to study the adsorption of amino acids to mineral surfaces. The adsorption of amino acids on the surface of pyrite has been studied experimentally and theoretically [12,23,24,25,26,27,28].
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