The remarkable hydration of the antifreeze protein Maxi: a computational study.

Abstract

The long four-helix bundle antifreeze protein Maxi contains an unusual core for a globular protein. More than 400 ordered waters between the helices form a nano-pore of internal water about 150 Å long. Molecular dynamics simulations of hydrated Maxi were carried out using the CHARMM27 protein forcefield and the TIP3P water model. Solvation in the core and non-core first hydration shell was analyzed in terms of water-water H-bond distance-angle distributions. The core had an increased population of low-angle H-bonds between water pairs relative to bulk water. Enhancement of low angle H-bonds was particularly pronounced for water pairs at the interfaces between apolar and polar regions inside the protein core, characteristic of the anchored clathrate solvation structure seen previously in the ice-nuclei binding surfaces of type I, type III, and beta-helical antifreeze proteins. Anchored clathrate type solvation structure was not seen in the exterior solvation shell except around residues implicated in ice binding. Analysis of solvation dynamics using water residence times and diffusion constants showed that exterior solvation shell waters exchanged rapidly with bulk water, with no difference between ice-binding and non-binding residues. Core waters had about ten-fold slower diffusion than bulk water. Water residence times around core residues averaged about 8 ps, similar to those on the exterior surface, but they tended to exchange primarily with other core water, resulting in longer, >40 ps residence times within the core. Preferential exchange or diffusion of the water along the long axis of the water core of Maxi was not detected.