| Literature DB >> 25580188 |
Alexey Savelyev, Alexander D MacKerell.
Abstract
The present report demonstrates that the conformational properties of DNA in solution are sensitive to the type of monovalent ion. Results are based on the ability of a polarizable force field using the classical Drude oscillator to reproduce experimental solution X-ray scattering data more accurately than two nonpolarizable DNA models, AMBER Parmbsc0 and CHARMM36. The polarizable model is then used to calculate scattering profiles of DNA in the presence of four different monovalent salts, LiCl, NaCl, KCl, and RbCl, showing the conformational properties of DNA to vary as a function of ion type, with that effect being sequence-dependent. The primary conformational mode associated with the variations is contraction of the DNA minor groove width with decreasing cation size. These results indicate that the Drude polarizable model provides a more realistic representation of ion-DNA interactions than additive models that may lead to a new level of understanding of the physical mechanisms driving salt-mediated biological processes involving nucleic acids.Entities:
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Year: 2015 PMID: 25580188 PMCID: PMC4285411 DOI: 10.1021/jz5024543
Source DB: PubMed Journal: J Phys Chem Lett ISSN: 1948-7185 Impact factor: 6.475
Figure 1Solution scattering profiles for the 1DCV and EcoRI systems from the experiments (upper row) and computed from MD simulations utilizing Drude polarizable (middle row) and additive CHARMM36 and AMBER Parmbsc0 (lower row) DNA models solvated in ∼100 mM NaCl ionic buffer. Positions of the experimental peaks are projected onto the computational results. Intensities for the additive AMBER and C36 systems are shifted with respect to each other to facilitate their comparison.
Peak Positions Inferred from Experimental and Computational Solution Scattering Profiles
| MD | ||||
|---|---|---|---|---|
| peak | EXP | C36 | AMBER | DRUDE |
| P1 | 0.456 | 0.442 | 0.507 | |
| P2 | 0.750 | 0.800 | 0.640 | 0.785 |
| P3 | 1.127 | 1.101 | 1.055 | 1.117 |
| P4 | 1.513 | 1.478 | 1.472 | 1.490 |
| P5 | 1.834 | 1.829 | 1.861 | 1.803 |
| rmsd (P2 – P5) | 0.033 | 0.084 | 0.018 | |
| rmsd_all | 0.030 | 0.027 | ||
| 1DCV, 10 base pairs | ||||
| P1 | 0.510 | 0.480 | 0.520 | |
| P2 | 0.755 | 0.800 | 0.700 | 0.820 |
| P3 | 1.180 | 1.100 | 1.050 | 1.110 |
| P4 | 1.525 | 1.455 | 1.435 | 1.495 |
| P5 | 1.790 | 1.825 | 1.830 | 1.800 |
| rmsd (P2 – P5) | 0.060 | 0.086 | 0.050 | |
| rmsd_all | 0.055 | 0.045 | ||
Peak positions were determined from zero crossing points in the first derivative; values are in Å–1.
Approximate positions of the plateau at P2.
Only internal eight base pairs were considered to be consistent with the experimentally studied sequence.
Approximate positions of the spike at P2.
Figure 2Solution scattering profiles computed from the Drude polarizable (A,C) and CHARMM36 additive (B,D) MD simulations of the 1DCV and EcoRI DNA sequences solvated in LiCl, NaCl, KCl, and RbCl containing aqueous buffers. For the Drude model demonstrating spectral variability with the ion type, the approximate positions of the first and two last peaks are schematically shown.
Figure 3Probability distributions for the minor groove width computed from the Drude polarizable and additive CHARMM36 MD simulations of the 1DCV, EcoRI, and 2L8Q DNA systems solvated in various monovalent ionic buffers. For comparison, estimates of the minor groove width inferred from selected NMR (PDB for 1DCV: 1G80; PDB for EcoRI: 1DUF) and crystallographic (PDB for 1DCV: 250D; PDB for EcoRI: 1BNA) structures are shown in panels A and C as dashed and dotted lines, respectively.