Structural dynamics of bacterial ribosomes: V. Magnesium-dependent dissociation of tight couples into subunits: Measurements of dissociation constants and exchange rates |
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Authors: | Markus Noll Hans Noll |
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Institution: | Department of Biochemistry and Molecular Biology Northwestern University, Evanston, Ill. 60201, U.S.A. |
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Abstract: | The magnesium ion-dependent equilibrium of vacant ribosome couples with their subunits has been studied quantitatively with a novel equilibrium displacement labeling method which is more sensitive and precise than light-scattering. At a concentration of 10?7m, tight couples (ribosomes most active in protein synthesis) dissociate between 1 and 3 mm-Mg2+ at 37 °C with a 50% point at 1.9 mm. The corresponding association constants Ka′ are 5.1 × 105m?1 (1 mm-Mg2+), 3.5 × 107m?1 (2 mm), and 1.2 × 109m?1 (3 mm), about five orders of magnitude higher than the Ka′ value of loose couples studied by Spirin et al. (1971) and Zitomer & Flaks (1972).In this range of Mg2+ concentrations () the rate constants depend exponentially and in opposite ways on the Mg2+ concentration: k1 = 2.2 × 10?3s?1, k?1 = 7.7 × 104m?1s?1 (2mm-Mg2+); k1 = 1.5 × 10?4s?1, k?1 = 1.7 × 107m?1s?1 (5 mm-Mg2+). Under physiological conditions (Mg2+ ~- 4 mm, ribosome concn ~- 10?7m), the equilibrium strongly favors association and the rate of exchange is slow (). In the range of dissociation (2 mm-Mg2+), association of subunits proceeds without measurable entropy change and hence ΔGO = ΔHO. The negative enthalpy change of ΔHO = ? 10 kcal suggests that association of subunits involves a shape change.Below a critical Mg2+ concentration (~- 2 mm), the 50 S subunits are converted irreversibly into the b-form responsible for the transition to loose couples. The results are compatible with two classes of binding sites, one class binding Mg2+ non-co-operatively and contributing to the free energy of association by reduction of electrostatic repulsion, and another class probably consisting of hydrogen bonds between components at opposite interfaces whose critical spatial alignment rapidly denatures in the absence of stabilizing magnesium ions. |
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