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Origin of the intrinsic rigidity of DNA.

The intrinsic rigidities of DNA and RNA helices are generally thought to arise from some combination of vertical base-stacking interactions and intra-helix phosphate-phosphate charge repulsion; however, the relative contributions of these two types of interaction to helix rigidity have not been quantified. To address this issue, we have measured the rotational decay times of a 'gapped-duplex' DNA molecule possessing a central, single-stranded region, dT24, before and after addition of the free purine base, N6-methyladenine ((me)A). Upon addition of (me)A, the bases pair with the T residues, forming a continuous stack within the gap region. Formation of the gapped duplex is accompanied by a nearly 2-fold increase in decay time, to values that are indistinguishable from the full duplex control for monovalent salt concentrations up to 90 mM. These results indicate that at least 90% of the rigidity of the dT(n)-dA(n) homopolymer derives from base pair stacking effects, with phosphate-phosphate interactions contributing relatively little to net helix rigidity at moderate salt concentrations.