Kinetics and activation parameter analysis for the prebiotic oligocytidylate formation on Na(+)-montmorillonite at 0-100 degrees C

The kinetic analysis of the temperature dependence of the formation of oligocytidylate (oligo(C)) from the 5'-monophosphorimidazolide moiety of cytidine (ImpC) in the presence of Na (+)-montmorillonite (Na (+)-Mont) catalyst has been carried out at 0-100 degrees C. The rate constants for the formation of oligo(C), hydrolysis of ImpC with and without Na (+)-Mont and degradation of oligo(C) were determined. The apparent activation parameters were 30.8 +/- 3.9 kJ mol (-1) ( Ea), 28.3 +/- 4.0 kJ mol (-1) (Delta H++), and -231 +/- 13 J mol (-1) K (-1) (Delta S++) for the formation of the 2-mer; 45.6 +/- 2.9 kJ mol (-1) ( Ea), 43.0 +/- 3.0 kJ mol (-1) (Delta H++), -164 +/- 10 J mol (-1) K (-1) (Delta S++) for the 3-mer; and 45.2 +/- 0.6 kJ mol (-1) ( Ea), 42.7 +/- 0.7 kJ mol (-1) (Delta H++), -159 +/- 2 J mol (-1) K (-1) (Delta S++) for the 4-mer in the presence of Na (+)-Mont. An increasing trend for the rate constants for the formation of oligo(C) in the order 2-mer << 3-mer <4-mer was observed at high temperatures, which is consistent with that observed at low temperatures. These analyses implied for the first time that the associate formation between an activated nucleotide monomer and an elongating oligonucleotide prior to the phosphodiester bond formation during the elongation of an oligonucleotide on a clay surface would be based on the interaction between the two reactants at the phosphoester and/or ribose moieties rather than at the nucleotide bases. The hydrolysis rate of ImpC at 25-100 degrees C was 5.3-10.6 times greater in the presence of Na (+)-Mont than in its absence. Although the degradation of oligo(C) in the presence of Na (+)-Mont was slower than the formation of the 3-mer and longer oligo(C) on Na (+)-Mont, its yield decreased with temperature. This is mainly because the ratios of the rate constant of the 2-mer formation to those of ImpC hydrolysis and the 3-mer and 4-mer formation decrease with an increase in temperature, which is attributed to the enthalpy and entropy changes for the formation of the 2-mer. This trend resembles the case of the template-directed formation of oligo(G) on a poly(C) template but is different from the Pb (2+)-ion-catalyzed oligo(C) formation. According to the kinetics and activation parameter analyses regarding the clay reaction and other prebiotic polymerase models, the possible pathways for the oligonucleotide formation are discussed and compared.

Chemical evolution of RNA under hydrothermal conditions and the role of thermal copolymers of amino acids for the prebiotic degradation and formation of RNA

The roles of thermal copolymers of amino acids (TCAA) were studied for the prebiotic degradation of RNA. A weak catalytic ability of TCAA consisted of Glu, L-Ala, L-Val, L-Glu, L-Asp, and optionally L-His was detected for the cleavage of the ribose phosphodiester bond of a tetranucleotide (5'-dCrCdGdG) in aqueous solution at 80 degees C. The rate constants of the disappearance of 5'-dCrCdGdG were determined in aqueous solutions using different pH buffer and TCAA. The degradation rates were enhanced 1.3-3.0 times in the presence of TCAA at pH 7.5 and 8.0 at 80 degrees C, while the hydrolysis of oligoguanylate (oligo(G)) was accelerated about 1.6 times at pH 8.0. A weak inhibitory activity for the cleavage of oligo(G) was detected in the presence of 0.055 M TCAA-Std. On the other hand, our recent study on the influences of TCAA for the template-directed reaction of oligo(G) on a polycytidylic acid template showed that TCAA has an acceleration activity for the degradation of the activated nucleotide monomer and an acceleration activity for the formation of G5' ppG capped oligo(G). This series of studies suggest that efficient and selective catalytic or inhibitory activities for either the degradation or formation of RNA under hydrothermal conditions could have hardly emerged from the simple thermal condensation products of amino acids. A scenario is going to be deduced on the chemical evolution of enzymatic activities and RNA molecules concerning hydrothermal earth conditions.