The cold origin of life: A. Implications based on the hydrolytic stabilities of hydrogen cyanide and formamide

被引:146
作者
Miyakawa, S
Cleaves, HJ
Miller, SL
机构
[1] Yokohama Natl Univ, Dept Chem & Biotechnol, Fac Engn, Yokohama, Kanagawa 2408501, Japan
[2] Univ Calif San Diego, Dept Chem & Biochem, La Jolla, CA 92093 USA
来源
ORIGINS OF LIFE AND EVOLUTION OF THE BIOSPHERE | 2002年 / 32卷 / 03期
基金
日本学术振兴会; 美国国家航空航天局;
关键词
ammonium cyanide; chemical evolution; cold origin of life; formamide; frozen earth; hydrogen cyanide polymerization; hydrolysis rate;
D O I
10.1023/A:1016514305984
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
It has been suggested that hydrogen cyanide (HCN) would not have been present in sufficient concentration to polymerize in the primitive ocean to produce nucleic acid bases and amino acids. We have measured the hydrolysis rates of HCN and formamide over the range of 30-150 degreesC and pH 0-14, and estimated the steady state concentrations in the primitive ocean. At 100 degreesC and pH 8, the steady state concentration of HCN and formamide were calculated to be 7 x 10(-13) M and 1 x 10(-15) M, respectively. Thus, it seems unlikely that HCN could have polymerized in a warm primitive ocean. It is suggested that eutectic freezing might have been required to have concentrated HCN sufficiantly for it to polymerize. If the HCN polymerization was important for the origin of life, some regions of the primitive earth might have been frozen.
引用
收藏
页码:195 / 208
页数:14
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