| Summary: | Homochiral proteins orchestrate biological functions throughout all domains of life, but the origin of the uniform <span style="font-variant: small-caps;">l</span>-stereochemistry of amino acids remains unknown. Here, we describe enantioselective adsorption experiments of racemic alanine and leucine onto homochiral <i>d</i>- and <i>l</i>-quartz as a possible mechanism for the abiotic emergence of biological homochirality. Substantial racemate resolution with enantiomeric excesses of up to 55% are demonstrated to potentially occur in interstitial pores, along grain boundaries or small fractures in local quartz-bearing environments. Our previous hypothesis on the enhanced enantioselectivity due to uranium-induced fission tracks could not be validated. Such capillary tubes in the near-surface structure of quartz have been proposed to increase the overall chromatographic separation of enantiomers, but no systematic positive correlation of accumulated radiation damage and enantioselective adsorption was observed in this study. In general, the natural <i>l</i>-quartz showed stronger enantioselective adsorption affinities than synthetic <i>d</i>-quartz without any significant trend in amino acid selectivity. Moreover, the <span style="font-variant: small-caps;">l</span>-enantiomer of both investigated amino acids alanine and leucine was preferably adsorbed regardless of the handedness of the enantiomorphic quartz sand. This lack of mirror symmetry breaking is probably due to the different crystal habitus of the synthetic z-bar of <i>d</i>-quartz and the natural mountain crystals of <i>l</i>-quartz used in our experiments.
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