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We demonstrate here that the Saccharomyces cerevisiae Mlh1-Pms1 heterodimer required for DNA mismatch repair and other cellular processes is a DNA binding protein. Binding was evaluated using a variety of single and double-stranded DNA molecules. Mlh1-Pms1 bound short substrates with low affinity and showed a slight preference for single-stranded DNA. In contrast, Mlh1-Pms1 exhibited a much higher affinity for long DNA molecules, suggesting that binding is cooperative. High affinity binding required a duplex DNA length greater than 241 base-pairs. The rate of association with DNA was rapid and dissociation of protein-DNA complexes following extensive dilution was very slow. However, in competition experiments, we observed a rapid active transfer of Mlh1-Pms1 from labeled to unlabeled DNA. Binding was non-sequence specific and highly sensitive to salt type and concentration, suggesting that Mlh1-Pms1 primarily interacts with the DNA backbone via ionic contacts. Cooperative binding was observed visually by atomic force microscopy as long, continuous tracts of Mlh1-Pms1 protein bound to duplex DNA. These images also showed that Mlh1-Pms1 simultaneously interacts with two different regions of duplex DNA. Taken together, the atomic force microscope images and DNA binding assays provide strong evidence that Mlh1-Pms1 binds duplex DNA with positive cooperativity and that there is more than one DNA binding site on the heterodimer. These DNA binding properties of Mlh1-Pms1 may be relevant to its participation in DNA mismatch repair, recombination and cellular responses to DNA damage.

Examining solute-induced changes in protein conformational equilibria is a long-standing method for probing the role of water in maintaining protein stability. Interpreting the molecular details governing the solute-induced effects, however, remains controversial. We present experimental and theoretical data for osmolyte-induced changes in the stabilities of the A and N states of yeast iso-1-ferricytochrome c. Using polyol osmolytes of increasing size, we observe that osmolytes alone induce A-state formation from acid-denatured cytochrome c and N state formation from the thermally denatured protein. The stabilities of the A and N states increase linearly with osmolyte concentration. Interestingly, osmolytes stabilize the A state to a greater degree than the N state. To interpret the data, we divide the free energy for the reaction into contributions from nonspecific steric repulsions (excluded volume effects) and from binding interactions. We use scaled particle theory (SPT) to estimate the free energy contributions from steric repulsions, and we estimate the contributions from water-protein and osmolyte-protein binding interactions by comparing the SPT calculations to experimental data. We conclude that excluded volume effects are the primary stabilizing force, with changes in water-protein and solute-protein binding interactions making favorable contributions to stability of the A state and unfavorable contributions to the stability of the N state. The validity of our interpretation is strengthened by analysis of data on osmolyte-induced protein stabilization from the literature, and by comparison with other analyses of solute-induced changes in conformational equilibria.