The hydrolytic deamination of cytosine and 5-methylcytosine residues in DNA appears to contribute significantly to the appearance of spontaneous mutations in microorganisms and in human disease. In the present work, we examined the mechanism of cytosine deamination and the response of the uncatalyzed reaction to changing temperature. The positively charged 1,3-dimethylcytosinium ion was hydrolyzed at a rate similar to the rate of acid-catalyzed hydrolysis of 1-methylcytosine, for which it furnishes a satisfactory kinetic model and a probable mechanism. In agreement with earlier reports, uncatalyzed deamination was found to proceed at very similar rates for cytosine, 1-methylcytosine, cytidine, and cytidine 5′-phosphate, and also for cytosine residues in single-stranded DNA generated from a phagemid, in which we sequenced an insert representing the gene of the HIV-1 protease. Arrhenius plots for the uncatalyzed deamination of cytosine were linear over the temperature range from 90°C to 200°C and indicated a heat of activation (ΔH ‡ ) of 23.4 ± 0.5 kcal/mol at pH 7. Recent evidence indicates that the surface of the earth has been cool enough to support life for more than 4 billion years and that life has been present for almost as long. If the temperature at Earth's surface is assumed to have followed Newton's law of cooling, declining exponentially from 100°C to 25°C during that period, then half of the cytosine-deaminating events per unit biomass would have taken place during the first 0.2 billion years, and <99.4% would have occurred during the first 2 billion years. spontaneous mutation | heat mutagenesis | cytosine deamination | HIV-1 protease I n the absence of enzymes, most biological reactions take place so slowly that they can be followed conveniently only at elevated temperatures (1). Among those reactions are several that may result in spontaneous mutation, notably the hydrolytic deamination of cytosine and 5-methylcytosine, which generate uracil and thymine, respectively. These deamination reactions have been shown to account for many of the single-site mutations that lead to inherited diseases in humans (2) and for the marked bias of spontaneous mutation toward increased AT content in microorganisms (3, 4). Rates of mutation have long been known to increase with increasing temperature, a phenomenon that Drake has termed "heat mutagenesis" (5).There is widespread (6-8), if not universal (9), agreement that life originated when the earth was warmer-perhaps much warmer-than it is today. A recent isotopic analysis of carbon inclusions in zircons from the Jack Hills in Western Australia indicates that life may have emerged as early as 4.1 billion years ago (10), shortly after water first appeared at the surface in liquid form (11). Several present-day organisms thrive at temperatures near the boiling point of water. Thus, Ignisphera aggregans (12) and Pyrococcus horikoshii (13) exhibit optimal growth temperature of 92°and 98°C, respectively, whereas another organism isolated from a hydrothermal vent has be...