Ferris J P, Joshi P C, Edelson E H, Lawless J G
J Mol Evol. 1978 Oct 6;11(4):293-311. doi: 10.1007/BF01733839.
Dilute (0.1 M) solutions of HCN condense to oligomers at pH 9.2. Hydrolysis of these oligomers yields 4,5-dihydroxypyrimidine, orotic acid, 5-hydroxyuracil, adenine, 4-aminoimidazole-5-carboxamide and amino acids. These results, together with the earlier data, demonstrate that the three main classes of nitrogen-containing biomolecules, purines, pyrimidines and amino acids may have originated from HCN on the primitive earth. The observation of orotic acid and 4-aminoimidazole-5-carboxyamide suggests that the contemporary biosynthetic pathways for nucleotides may have evolved from the compounds released on hydrolysis of HCN oligomers.
pH值为9.2时,稀(0.1M)氢氰酸溶液会缩合成低聚物。这些低聚物水解后会产生4,5-二羟基嘧啶、乳清酸、5-羟基尿嘧啶、腺嘌呤、4-氨基咪唑-5-甲酰胺和氨基酸。这些结果与早期数据一起表明,含氮生物分子的三大主要类别,即嘌呤、嘧啶和氨基酸,可能起源于原始地球上的氢氰酸。乳清酸和4-氨基咪唑-5-甲酰胺的发现表明,当代核苷酸生物合成途径可能是从氢氰酸低聚物水解释放的化合物演变而来的。