Published online 2 August 2004
Nucleic Acids Research, Vol. 32 No. 13 © Oxford University Press 2004; all rights reserved
Origin of the intrinsic rigidity of DNA
Department of Biochemistry and Molecular Genetics, University of Colorado School of Medicine, 4200 East Ninth Avenue, Denver, CO 80262, USA and 1 Department of Biochemistry and Molecular Medicine, School of Medicine, University of California, One Shields Avenue, Davis, CA 95616, USA
* To whom correspondence should be addressed. Tel: +1 530 754 7266; Fax: +1 530 754 7269; Email: pjhagerman{at}ucdavis.edu
Received May 21, 2004; Revised and Accepted July 15, 2004
The intrinsic rigidities of DNA and RNA helices are generally thought to arise from some combination of vertical base-stacking interactions and intra-helix phosphatephosphate 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 (meA). Upon addition of meA, 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 dTndAn homopolymer derives from base pair stacking effects, with phosphatephosphate interactions contributing relatively little to net helix rigidity at moderate salt concentrations.
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