Journal of Physical Chemistry B, Vol.107, No.1, 344-357, 2003
pK(a) values of guanine in water: Density functional theory calculations combined with Poisson-Boltzmann continuum-solvation model
It has long been postulated that rare tautomeric or ionized forms of DNA bases may play a role in mispair formation. To investigate the role this phenomenon plays in the mispairing of guanine and to develop a calculation methodology that can be extended to mutagenic DNA damage products, we used first principles quantum mechanics (density functional theory (B3LYP) with the Poisson-Boltzmann continuum-solvation model) to calculate the relative stabilities of tautomers of guanine in various environments and their pK(a) values in aqueous solution. This method allows us to calculate site specific pK(a) values - information that is experimentally inaccessible - as well as overall pK(a) values for each stage, wherein our numbers are in agreement with experimental values. We find that neutral guanine exists in aqueous phase as a mixture of two major keto tautomers, the N9H form (1) and a N7H form (3). These keto forms are also major species present in the gas phase, as well as the O6H enol tautomer (7a). These results show that tautomeric configurations can be drastically different depending on the environment. Here, we discuss the reasons for this environmental variability and suggest some possible implications. Finally, we estimate that the relative population of deprotonated guanine is 0.2-2% in the range of pH 7-8, a significant enough population to potentially play a role in mispair formation.