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J Topol  D M Ruden  C S Parker 《Cell》1985,42(2):527-537
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Pyrococcus woesei (Pw) is a hyperthermophilic archaeal organism that exists under conditions of high salt and elevated temperature. In a previous study [O'Brien, R., DeDecker, B., Fleming, K., Sigler, P. B., and Ladbury, J. E., (1998) J. Mol. Biol. 279, 117-125], we showed that, despite the similarity of primary and secondary structure, the TATA box binding protein (TBP) from Pw binds thermodynamically in a fundamentally different way to its mesophilic counterparts. The affinity of the interaction increases as the salt concentration is increased. The formation of the protein-DNA complex involves the release of water and the uptake of ions, which were hypothesized to be cations. Here we test this hypothesis by selecting potential cation binding sites at negatively charged, acidic residues in the complex interface. These were substituted using site-directed mutagenesis of specific residues. Changes in the thermodynamic parameters on formation of the mutant protein-DNA complex were determined using isothermal titration calorimetry and compared to the wild type interaction. Removal of a glutamate residue from the binding site resulted in the uptake of one less cation on formation of the complex. This glutamate (E12) is directly involved in the binding of cations in the complex interface. Substitution of another acidic residue proximal to the DNA binding site (D101) had no effect on cation uptake, suggesting that the location of the amino acid on the protein surface is important in dictating the potential to coordinate cations. Removal of the cation binding site provided a more favorable entropy of binding; however, this effect is significantly reduced at higher salt concentrations. The removal of the cation binding site led to an increase in affinity with respect to the wild-type TBP at low salt concentrations.  相似文献   

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Structural and biochemical studies of Cys(2)His(2) zinc finger proteins initially led several groups to propose a "recognition code" involving a simple set of rules relating key amino acid residues in the zinc finger protein to bases in its DNA site. One recent study from our group, involving geometric analysis of protein-DNA interactions, has discussed limitations of this idea and has shown how the spatial relationship between the polypeptide backbone and the DNA helps to determine what contacts are possible at any given position in a protein-DNA complex. Here we report a study of a zinc finger variant that highlights yet another source of complexity inherent in protein-DNA recognition. In particular, we find that mutations can cause key side-chains to rearrange at the protein-DNA interface without fundamental changes in the spatial relationship between the polypeptide backbone and the DNA. This is clear from a simple analysis of the binding site preferences and co-crystal structures for the Asp20-->Ala point mutant of Zif268. This point mutation in finger one changes the specificity of the protein from GCG TGG GCG to GCG TGG GC(G/T), and we have solved crystal structures of the D20A mutant bound to both types of sites. The structure of the D20A mutant bound to the GCG site reveals that contacts from key residues in the recognition helix are coupled in complex ways. The structure of the complex with the GCT site also shows an important new water molecule at the protein-DNA interface. These side-chain/side-chain interactions, and resultant changes in hydration at the interface, affect binding specificity in ways that cannot be predicted either from a simple recognition code or from analysis of spatial relationships at the protein-DNA interface. Accurate computer modeling of protein-DNA interfaces remains a challenging problem and will require systematic strategies for modeling side-chain rearrangements and change in hydration.  相似文献   

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