A possible role of fluctuating clay-water systems in the production of ordered prebiotic oligomers.
A model is proposed for the intermediate stages of prebiotic evolution, based on the characteristics of the adsorption and condensation of amino acids and nucleotides on the surface area of clay minerals in a fluctuating environment. Template replication and translation of adsorbed oligonucleotides and catalytic effects by peptide products on further condensation are proposed, due to specific properties of hypohydrous clay surfaces as well as the biomolecules themselves. Experimental evidence supports some of the proposed interactions, and all of them can be tested experimentally.
D000327:Adsorption; D000538:Aluminum Silicates; D000596:Amino Acids; D005075:Biological Evolution; D002384:Catalysis; D055598:Chemical Phenomena; D002627:Chemistry, Physical; D000077215:Clay; D009711:Nucleotides; D009841:Oligonucleotides / Q000138:chemical synthesis*; D009842:Oligopeptides / Q000138:chemical synthesis*; D013698:Templates, Genetic
D000538:Aluminum Silicates; D000596:Amino Acids; D009711:Nucleotides; D009841:Oligonucleotides; D009842:Oligopeptides; D000077215:Clay