Kinetic and thermodynamic origins of osmolyte-influenced nucleic acid folding.

The influential role of monovalent and divalent metal cations in facilitating conformational transitions in both RNA and DNA has been a target of intense biophysical research efforts. However, organic neutrally charged cosolutes can also significantly alter nucleic acid conformational transitions. For example, highly soluble small molecules such as trimethylamine N-oxide (TMAO) and urea are occasionally utilized by organisms to regulate cellular osmotic pressure. Ensemble studies have revealed that these so-called osmolytes can substantially influence the thermodynamics of nucleic acid conformational transitions. In the present work, we exploit single-molecule FRET (smFRET) techniques to measure, for first time, the kinetic origins of these osmolyte-induced changes to the folding free energy. In particular, we focus on smFRET RNA and DNA constructs designed as model systems for secondary and tertiary structure formation. These findings reveal that TMAO preferentially stabilizes both secondary and tertiary interactions by increasing kfold and decreasing kunfold, whereas urea destabilizes both conformational transitions, resulting in the exact opposite shift in kinetic rate constants (i.e., decreasing kfold and increasing kunfold). Complementary temperature-dependent smFRET experiments highlight a thermodynamic distinction between the two different mechanisms responsible for TMAO-facilitated conformational transitions, while only a single mechanism is seen for the destabilizing osmolyte urea. Finally, these results are interpreted in the context of preferential interactions between osmolytes, and the solvent accessible surface area (SASA) associated with the (i) nucleobase, (ii) sugar, and (iii) phosphate groups of nucleic acids in order to map out structural changes that occur during the conformational transitions.