Abstract-These studies concern the catalytic activity of clays on amino acids, particularly tyrosine. Polyhydric phenols were included to help understand the tyrosine reactions.Below pH 3, tyrosine is adsorbed on clay minerals by cation exchange. Above pH 3, oxidative degradation of tyrosine occurs, the L-isomer altering more rapidly. The rate of alteration depends upon the particular clay mineral, surface modifications such as polyphosphate treatment, heating, and the presence of copper, aluminium, and mercury. A free radical mechanism is proposed for the alteration.INTRODUCTION THE EFFECT of clay minerals on amino acids is of importance not only because these organic compounds are used to date sediments, but also because of the possible role of fine-grained silicates in the prebiotic synthesis of polypeptides. Both areas of study depend upon the catalytic activity of clay minerals. Age dating, as indicated by the loss of optical activity or racemization, (Bada et al., 1970;Kvenvolden and Peterson, 1970) is considered to be a first order reaction, but independent of any specific influence of the fine-grained sediments. The development of polypeptides from amino acids by 'template catalysis' on clay mineral surfaces has been studied by Degens, Mathejar andJackson (1970) andJackson (1971). Their findings were of exceptional interest; the L-isomer, which predominates in nature, showed an increased adsorption and polymerization rate over that of the Disomer.These investigations prompted the study of the catalytic activity of clays on some optically active amino acids and polyhydric phenols. The following compounds were selected: D-and L-tyrosine, Dand L-phenylalanine, pyrogallol, pyrocatechol, resorcinol and hydroquinone. These particular amino acids were chosen because they absorb light in the u.v. a property which makes possible the quantitative determination of concentration and structural changes.