Abstract
High-temperature origin-of-life theories require that the components of the first genetic material are stable. We therefore have measured the half- lives for the decomposition of the nucleobases. They have been found to be short on the geologic time scale. At 100°C, the growth temperatures of the hyperthermophiles, the half-lives are too short to allow for the adequate accumulation of these compounds (t( 1/4 ) for A and G ≃ 1 yr; U = 12 yr; C = 19 days). Therefore, unless the origin of life took place extremely rapidly (< 100 yr), we conclude that a high-temperature origin of life may be possible, but it cannot involve adenine, uracil, guanine, or cytosine. The rates of hydrolysis at 100°C also suggest that an ocean-boiling asteroid impact would reset the prebiotic clock, requiring prebiotic synthetic processes to begin again. At 0°C, A, U, G, and T appear to be sufficiently stable (t(1/2) ≤ 106 yr) to be involved in a low-temperature origin of life. However, the lack of stability of cytosine at 0°C °(t(1/2) = 17,000 yr) raises the possibility that the GC base pair may not have been used in the first genetic material unless life arose quickly (<106 yr) after a sterilization event. A two-letter code or an alternative base pair may have been used instead.
Original language | English (US) |
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Pages (from-to) | 7933-7938 |
Number of pages | 6 |
Journal | Proceedings of the National Academy of Sciences of the United States of America |
Volume | 95 |
Issue number | 14 |
DOIs | |
State | Published - Jul 7 1998 |
Externally published | Yes |
Keywords
- Chemical evolution
- Nucleobase hydrolysis
- RNA world
ASJC Scopus subject areas
- General