“…A few investigations concerning the degradation of RNA and its precursors have been conducted from the standpoint of the hydrothermal origin of life. ,,,,– According to the empirical data regarding the stability of RNA molecules, it is considered that the RNA molecules are too labile under redox-constrained hydrothermal conditions, , although some minerals appear to protect nucleotides and their precursors from degradations. , On the other hand, while the prebiotic formation of RNA was rarely investigated at high temperatures, we have recently accumulated kinetic data on the temperature dependence of prebiotic RNA polymerase model reactions, that is, the TD reaction, cyclization reaction of hexanucleotides, and Pb 2+ -ion-catalyzed oligonucleotide formation (PB reaction). – These investigations not only showed that the phosphodiester bond becomes labile at high temperatures but also suggested that its prebiotic formation could be faster than its degradation at high temperatures. – Naturally, this estimation does not give a direct proof of the accumulation of the RNA molecules could under the primitive hydrothermal conditions. Nevertheless, it would be theoretically true that the accumulation of the RNA molecules may be kinetically controlled in an open system by both the formation and decomposition rates of RNA, even at high temperatures. , In particular, it has been elucidated that mineral catalysts could have played important roles in the spontaneous formation of long oligonucleotides from monomeric nucleotides. ,, Thus, for the RNA world hypothesis and hydrothermal origin of life hypothesis to be compatible, it is important to accumulate kinetic data regarding the temperature dependence of the prebiotic simulation reactions of the RNA molecules to validate the rate of the prebiotic formation of RNA at high temperatures.…”