The directionality of the hole-transfer processes between DNA backbone and base was investigated by using phosphorodithioate [P(S
−)=S] components. ESR spectroscopy in homogeneous frozen aqueous solutions and pulse radiolysis in aqueous solution at ambient temperature confirmed initial formation of G
.+-P(S
−)=S. The ionization potential of G-P(S
−)=S was calculated to be slightly lower than that of guanine in 5′-dGMP. Subsequent thermally activated hole transfer from G
.+ to P(S
−)=S led to dithiyl radical (P-2S
.) formation on the μs timescale. In parallel, ESR spectroscopy, pulse radiolysis, and density functional theory (DFT) calculations confirmed P-2S
. formation in an abasic phosphorodithioate model compound. ESR investigations at low temperatures and higher G-P(S
−)=S concentrations showed a bimolecular conversion of P-2S
. to the σ
2-σ*
1-bonded dimer anion radical [-P-2S 2S-P-]
− [Δ
G (150 K, DFT)=−7.2 kcal mol
−1]. However, [-P-2S 2S-P-]
− formation was not observed by pulse radiolysis [Δ
G° (298 K, DFT)=−1.4 kcal mol
−1]. Neither P-2S
. nor [-P-2S 2S-P-]
− oxidized guanine base; only base-to-backbone hole transfer occurs in phosphorodithioate.
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