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Quinone methides and related intermediates have been implicated in a range of beneficial and detrimental processes in biology and effectively alkylate a variety of cellular components despite the ubiquitous presence of water. As a prerequisite to understanding the origins of their specificity, the major products generated by DNA and its components with an unsubstituted ortho quinone methide under aqueous conditions were recently characterized [Pande, P., Shearer, J., Yang, J., Greenberg, W. A., and Rokita, S. E. (1999) J. Am. Chem. Soc. 121, 6773-6779]. Investigations currently focus on the complete range of derivatives formed by deoxyguanosine (dG) and guanine residues in duplex DNA through product isolation and structure determination using reversed-phase chromatography and a range of one and two-dimensional NMR techniques. Previous construction of a synthetic standard for dG alkylation is now shown to have yielded the N1-linked adduct rather than the N(2)-linked adduct. This later adduct has also now been characterized and confirmed to be the major product of reaction between the quinone methide and both duplex DNA and dG under neutral conditions. An N7 adduct of guanine has additionally been identified under these conditions and appears to result from spontaneous deglycosylation of the corresponding N7 adduct of dG. A combination of steric and electronic properties of duplex DNA likely contribute to the enhanced selectivity of the quinone methide for its guanine N(2) position (7.8:3.2:1.0 for adducts of N(2):N7:N1) relative to that of dG (4.7:3.5:1.0 for adducts of N(2):N7:N1).

This paper presents results from a series of pulsed field gradient (PFG) NMR studies on lipophilic guanosine nucleosides that undergo cation-templated assembly in organic solvents. The use of PFG-NMR to measure diffusion coefficients for the different aggregates allowed us to observe the influences of cation, solvent and anion on the self-assembly process. Three case studies are presented. In the first study, diffusion NMR confirmed formation of a hexadecameric G-quadruplex [G 1](16)4 K(+)4 pic(-) in CD(3)CN. Furthermore, hexadecamer formation from 5'-TBDMS-2',3'-isopropylidene G 1 and K(+) picrate was shown to be a cooperative process in CD(3)CN. In the second study, diffusion NMR studies on 5'-(3,5-bis(methoxy)benzoyl)-2',3'-isopropylidene G 4 showed that hierarchical self-association of G(8)-octamers is controlled by the K(+) cation. Evidence for formation of both discrete G(8)-octamers and G(16)-hexadecamers in CD(2)Cl(2) was obtained. The position of this octamer-hexadecamer equilibrium was shown to depend on the K(+) concentration. In the third case, diffusion NMR was used to determine the size of a guanosine self-assembly where NMR signal integration was ambiguous. Thus, both diffusion NMR and ESI-MS show that 5'-O-acetyl-2',3'-O-isopropylidene G 7 and Na(+) picrate form a doubly charged octamer [G 7](8)2 Na(+)2 pic(-) 9 in CD(2)Cl(2). The anion's role in stabilizing this particular complex is discussed. In all three cases the information gained from the diffusion NMR technique enabled us to better understand the self-assembly processes, especially regarding the roles of cation, anion and solvent.

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Proton magnetic resonance experiments on the disodium salt of folic acid in aqueous solutions (pD 7.1) indicate that the folate ion exists in an unfolded, extended conformation in solution. However, based on a temperature and concentration dependence of the proton chemical shifts, folate ions are involved in intermolecular association consisting of a vertical stacking interaction. A stacking model is proposed for the association with the hydrophilic ends of the molecule alternating in orientation with respect to the hydrophobic portion of the neighboring molecules.Les experiences de r.m.n. sur le sel dissodique de I'acide folique en solutions aqueuses (pD 7.1) indiquent que I'ion folate existe dans une conformation non plissie et itirie. Cependant, les risultats fondis sur I'influence de la tempirature et de la concentration sur les diplacements chimiques du proton montrent que les ions folates sont impliquts dans une association intermoliculaire rigie par une interaction due i un empilement vertical. Un modele pour cet entassement est proposi oh les bouts hydrophiliques de la molicule alternent en orientation avec la portion hydrophobique des molicules voisines.