Metal ion-binding properties of (N3)-deprotonated uridine, thymidine, and related pyrimidine nucleosides in aqueous solution.

The acidity constants for (N3)H of the uridine-type ligands (U) 5-fluorouridine, 5-chloro-2'-deoxyuridine, uridine, and thymidine (2'-deoxy-5-methyluridine) and the stability constants of the M(U-H)(+) complexes for M(2+) = Mg(2+), Ca(2+), Sr(2+), Ba(2+), Mn(2+), Co(2+), Ni(2+), Cu(2+), Zn(2+), Cd(2+), and Pb(2+) were measured (potentiometric pH titrations; aqueous solution; 25 degrees C; I = 0.1 M, NaNO(3)). Plots of logK(M(U-H))(M) vs. pK(U)(H) result in straight lines that are compared with previous plots for simple pyridine-type and o-amino(methyl)pyridine-type ligands as well as with the stabilities of the corresponding M(cytidine)(2+) complexes. The results indicate monodentate coordination to (N3)(-) in M(U-H)(+) for Co(2+) and Ni(2+). For the M(U-H)(+) species of Cd(2+), Zn(2+), or Cu(2+), increased stabilities imply that semichelates form, i.e., M(2+) is (N3)(-)-bound and coordinated water molecules form hydrogen bonds to (C2)O and (C4)O; these "double" semichelates are in equilibrium with "single" semichelates involving either (C2)O or (C4)O and possibly also with four-membered chelates for which M(2+) is innersphere-coordinated to (N3)(-) and a carbonyl oxygen. For the alkaline earth ions, semichelates dominate with the M(2+) outersphere bound to (N3)(-) and innersphere to one of the carbonyl oxygens. Mn(U-H)(+) is with its properties between those of Cd(2+) (which probably also hold for Pb(2+)) and the alkaline earth ions. In nucleic acids, M(2+)-C(O) interactions are expected, if support is provided by other primary binding sites. (N3)H may possibly be acidified via carbonyl-coordinated M(2+) to become a proton donor in the physiological pH range, at which direct (N3)(-) binding of M(2+) also seems possible.