Role of loop residues and cations on the formation and stability of dimeric DNA G-quadruplexes.

Formation of guanine-quadruplexes by four DNA oligonucleotides with common sequence dG4-loop-dG4 has been studied by a combination of NMR and UV spectroscopy. The loops consisted of 1',2'-dideoxyribose, propanediol, hexaethylene glycol, and thymine residues. The comparison of data on modified and parent oligonucleotides gave insight into the role of loop residues on formation and stability of dimeric G-quadruplexes. All modified oligonucleotides fold into dimeric fold-back G-quadruplexes in the presence of sodium ions. Multiple structures form in the presence of potassium and ammonium ions, which is in contrast to the parent oligonucleotide with dT4 loop. 15N-filtered 1H NMR spectra demonstrate that all studied G-quadruplexes exhibit three 15NH4(+) ion binding sites. Topology of intermolecular G-quadruplexes was evaluated by NMR measurements and diffusion experiments. The spherical, prolate-ellipsoid and symmetric cylinder models were used to interpret experimental translational diffusion constants in terms of diameters and lengths of unfolded oligonucleotides and their respective G-quadruplexes. UV melting and annealing curves show that oligonucleotides with non-nucleosidic loop residues fold faster, exhibit no hysteresis, and are less stable than dimeric d(G4T4G4)2 which can be attributed to the absence of H-bonds, stacking between loop residues and the outer G-quartets as well as cation-pi interactions. Oligonucleotide consisting of hexaethylene glycol linkage with only two phosphate groups in the loop exhibits higher melting temperature and more negative deltaH(o) and deltaG(o) values than oligonucleotides with four 1',2'-dideoxyribose or propanediol residues.