The origin of pressure resistance in deep-sea lactate dehydrogenase

17 October 2024, Version 2
This content is a preprint and has not undergone peer review at the time of posting.

Abstract

High hydrostatic pressure has a dramatic effect on biochemical systems, as exposure to high pressure can result in structural perturbations ranging from dissociation of protein complexes to complete denaturation. The deep ocean presents an interesting paradox since it is teeming with life despite the high-pressure environment. This is due to evolutionary adaptations in deep-sea organisms, such as amino acid substitutions in their proteins, which aid in resisting the denaturing effects of pressure. However, the physicochemical mechanism by which these substitutions can induce pressure resistance remains unknown. Here, we use molecular dynamics simulations to study pressure-adapted lactate dehydrogenase from the deep-sea abyssal grenadier (C. armatus), in comparison with that of the shallow-water Atlantic cod (G. morhua). We examined structural, thermodynamic and volumetric contributions to pressure resistance, and report that the amino acid substitutions result in a decrease in volume of the deep-sea protein accompanied by a decrease in thermodynamic stability of the native protein. Our simulations at high pressure also suggest that differences in compressibility may be important for understanding pressure resistance in deep-sea proteins.

Keywords

high pressure
molecular dynamics
partial molar volume
reaction volume
alchemical free energy
thermodynamic stability

Supplementary materials

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Supplementary figures and tables
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Supporting figures and tables including: Convergence tests for ΔG of mutation and ADM calculations; Contact maps for GMLDH and CA-LDH, along with a differential contact map; Sample structure from the unfolded ensemble; dI/dS plots for LDH dimers in comparison with experimental data; Full numerical results for: Solvent-accessible surface area, number of amino acid and water contacts, ΔG of mutation, radius of gyration, Partial molar volumes at ambient and elevated pressure, calculated with the ADM, ΔV of dissociation at ambient and elevated pressure at 300K and 277K.
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