Pyrite Interference in Prebiotic Chiral Selection of Amino Acids

L-amino acids are ubiquitous in biology, yet the origin of their homochirality is an enduring mystery. Prebiotic chiral selection process of amino acids could significantly influence subsequent molecular evolution and emergence of life. However, the distribution of chirality of amino acids remains convoluted, which poses obstacles to the in-depth study of prebiotic chiral selection of amino acids. Here, we propose that minerals in the prebiotic environment might hindered the absolute selection of L-amino acids, inducing a random distribution of L- and D-amino acids during the early stages of life's evolution. Pyrite, abundant in the prebiotic world, predominantly selected D-amino acids in the photocatalytic reductive amination of α-keto acids, resisting the enantioselectivity of chiral driving forces (CDFs) like chiral structures, magnetic fields, circularly polarized light, and chiral molecules. This resistance is due to the wavy atomic arrangement of pyrite surfaces, which causes larger reaction energy differences between enantiomers. Our findings provide evidence to assess the validity of prebiotic chiral selection scenarios for biomolecules, an important step in understanding the origin of life.