Foi realizado um estudo da adsorção de L-alanina, L-tirosina, L-ácido glutâmico e L-lisina em areia do mar. Somente L-lisina adsorveu na areia do mar, provavelmente devido à sua cadeia lateral que é positivamente carregada. Portanto, estes resultados apontam dúvidas sobre a importância de areia para a pré-concentração de aminoácidos antes condensação de peptídeos na Terra primitiva.A study of adsorption of L-alanine, L-tyrosine, L-glutamic acid, and L-lysine on sea sand was carried out. Only L-lysine showed adsorption on sea sand, probably due to the presence of the positively charged R group. Our results raise some doubts as to whether sand was important for the pre-concentration of amino acids prior to peptide condensation on the Pre-Biotic Earth.
Keywords: adsorption, sand, amino acids, origin of life
IntroductionSince 1951, when Bernal 1 first suggested that mineral clays could have played an important role in the origin of life, because they took part in processes such as selection and concentration of key monomers from dilute solution and their subsequent condensation to biopolymers, much research on this subject has been undertaken.There are many studies on the adsorption of amino acids 2-6 as well as other biomolecules, 7,8 and biopolymers 9-13 on clays. Clays were used in many experiments because they have a large surface-area-to-volume ratio in comparison with quartz or sand whose surface-area-to-volume ratios are small. However, sand (35-50%) is more widespread than clays (25-35%). 14 The present paper describes the utilization of sea sand from Enseada Beach at Guarujá-SP, Brazil, to study the adsorption of the following amino acids: L-alanine, Ltyrosine, L-glutamic acid and L-lysine. Our results raise some doubts about whether sand was important as a concentrator of amino acids.
Material and methods
MaterialVisible spectrophotometry was carried out on a Shimadzu UV-Vis 1203 spectrophotometer. The mineralogical composition of sea sand was determined on a petrographic microscope (KM Plival, Carl Zeiss/Aus Jena Company) and magnifying glass (Carl Zeiss/Aus Jena Company). The sea sand was centrifuged using a Model 243 Microcentrifuge (FANEM Ltda.). All reagents were of analytical grade.Standard solutions of 20.0 mmol L -1 of the amino acids L-alanine (Nuclear P.A.), L-glutamic acid (Aktron P.A.), Ltyrosine (Merck P.A.) and L-lysine (Merck P.A.) were used in all adsorption experiments. For the dissolution of Ltyrosine and L-glutamic acid it was necessary to add sodium hydroxide.Sea sand with the following percentage (m/m) and particle size distribution: 0.02%, 0.50-0.42 mm; 15.1%, 0.42-0.149 mm; 0.4%, 0.15-0.125 mm, and 84.5%, 0.13-0.074 mm, respectively, was collected from Enseada Beach at Guarujá -SP, Brazil, and was prepared as described by Rohlfing and McAlhaney. 15
Composition of sea sandThe mineralogical analysis of sea sand indicates that it is 99% quartz. Quartz is essentially, pure silica. However, the sea sand is, surely, impure silica. Thus, some (or many) silanol groups would be present and t...