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Hydrostatic pressure together with the temperature is an important environmental variable that plays an essential role in biological adaptation of extremophilic organisms. In particular, the effects of hy-drostatic pressure on the rates of the protein folding/unfolding reaction are determined by the magni-tude and sign of the activation volume changes. Here we provide computational description of the ac-tivation volume changes for folding/unfolding reaction, and compare them with the experimental data for six different globular proteins. We find that the volume of the transition state ensemble is always in-between the folded and unfolded states. Based on this, we conclude that hydrostatic pressure will invariably slow down protein folding and accelerate protein unfolding. 

Abstract Hydrostatic pressure has a vital role in the biological adaptation of the piezophiles, organisms that live under high hydrostatic pressure. However, the mechanisms by which piezophiles are able to adapt their proteins to high hydrostatic pressure is not well understood. One proposed hypothesis is that the volume changes of unfolding (ΔV_Tot) for proteins from piezophiles is distinct from those of nonpiezophilic organisms. Since ΔV_Totdefines pressure dependence of stability, we performed a comprehensive computational analysis of this property for proteins from piezophilic and nonpiezophilic organisms. In addition, we experimentally measured the ΔV_Totof acylphosphatases and thioredoxins belonging to piezophilic and nonpiezophilic organisms. Based on this analysis we concluded that there is no difference in ΔV_Totfor proteins from piezophilic and nonpiezophilic organisms. Finally, we put forward the hypothesis that increased concentrations of osmolytes can provide a systemic increase in pressure stability of proteins from piezophilic organisms and provide experimental thermodynamic evidence in support of this hypothesis.