These environments are known to exist based on the rocks found in the time period life arose.
From: The Origin of Oxygen in Earth's Atmosphere
The role of metal ions in chemical evolution: Polymerization of alanine and glycine in a cation-exchanged clay environment
The effect of the exchangeable cation on the condensation of glycine and alanine was investigated using a series of homoionic bentonites. A cycling procedure of drying, warming and wetting was employed. Peptide bond formation was observed, and the effectiveness of metal ions to catalyze the condensation was Cu2+ > Ni2+ ≈ Zn2+ > Na+. Glycine showed 6% of the monomer incorporated into oligomers with the largest detected being the pentamer. Alanine showed less peptide bond formation (a maximum of 2%) and only the dimer was observed.
From: The Origin of Oxygen in Earth's Atmosphere
The role of metal ions in chemical evolution: Polymerization of alanine and glycine in a cation-exchanged clay environment
The effect of the exchangeable cation on the condensation of glycine and alanine was investigated using a series of homoionic bentonites. A cycling procedure of drying, warming and wetting was employed. Peptide bond formation was observed, and the effectiveness of metal ions to catalyze the condensation was Cu2+ > Ni2+ ≈ Zn2+ > Na+. Glycine showed 6% of the monomer incorporated into oligomers with the largest detected being the pentamer. Alanine showed less peptide bond formation (a maximum of 2%) and only the dimer was observed.