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By use of ESR and UV-vis spectral studies, this work identifies the protonation states of one-electron oxidized G:C (viz. G˙+:C, G(N1–H)˙:C(+H+), G(N1–H)˙:C, and G(N2-H)˙:C) in a DNA oligomer d[TGCGCGCA]2. Benchmark ESR and UV-vis spectra from one electron oxidized 1-Me-dGuo are employed to analyze the spectral data obtained in one-electron oxidized d[TGCGCGCA]2 at various pHs. At pH ≥7, the initial site of deprotonation of one-electron oxidized d[TGCGCGCA]2 to the surrounding solvent is found to be at N1 forming G(N1–H)˙:C at 155 K. However, upon annealing to 175 K, the site of deprotonation to the solvent shifts to an equilibrium mixture of G(N1–H)˙:C and G(N2–H)˙:C. For the first time, the presence of G(N2–H)˙:C in a ds DNA-oligomer is shown to be easily distinguished from the other prototropic forms, owing to its readily observable nitrogen hyperfine coupling (Azz(N2) = 16 G). In addition, for the oligomer in H2O, an additional 8 G N2–H proton HFCC is found. This ESR identification is supported by a UV-vis absorption at 630 nm which is characteristic for G(N2–H)˙ in model compounds and oligomers. We find that the extent of photo-conversion to the C1′ sugar radical (C1′˙) in the one-electron oxidized d[TGCGCGCA]2 allows for a clear distinction among the various G:C protonation states which can not be easily distinguished by ESR or UV-vis spectroscopies with this order for the extent of photo-conversion: G˙+:C &gt; G(N1–H)˙:C(+H+) ≫ G(N1–H)˙:C. We propose that it is the G˙+:C form that undergoes deprotonation at the sugar and this requires reprotonation of G within the lifetime of exited state

Prototropic equilibria in DNA containing one-electron oxidized GC: intra-duplex vs. duplex to solvent deprotonation