Abstract
Equilibrium as well as pre-steady-state measurements were performed to characterize the molecular basis of DNA binding and nucleotide incorporation by the thermostable archaeal DinB homologue (Dbh) DNA polymerase of Sulfolobus solfataricus. Equilibrium titrations show a DNA binding affinity of about 60 nM, which is ∼ 10-fold lower compared with other DNA polymerases. Investigations of the binding kinetics applying stopped-flow and pressure jump techniques confirm this weak binding affinity. Furthermore, these measurements suggest that the DNA binding occurs in a single step, diffusion-controlled manner. Single-turnover, single dNTP incorporation studies reveal maximal pre-steady-state burst rates of 0.64, 2.5, 3.7, and 5.6 s-1 for dTTP, dATP, dGTP, and dCTP (at 25 °C), which is 10-100-fold slower than the corresponding rates of classical DNA polymerases. Another unique feature of the Dbh is the very low nucleotide binding affinity (Kd ∼ 600 μM), which again is 10-20-fold lower compared with classical DNA polymerases as well as other Y-family polymerases. Surprisingly, the rate-limiting step of nucleotide incorporation (correct and incorrect) is the chemical step (phosphoryl transfer) and not a conformational change of the enzyme. Thus, unlike replicative polymerases, an "induced fit" mechanism to select and incorporate nucleotides during DNA polymerization could not be detected for Dbh.
| Original language | English |
|---|---|
| Journal | Journal of Biological Chemistry |
| Volume | 280 |
| Issue number | 49 |
| Pages (from-to) | 40552-40558 |
| Number of pages | 7 |
| ISSN | 0021-9258 |
| DOIs | |
| Publication status | Published - 09.12.2005 |
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