Quite remarkably, this result is reminiscent of the famous criterion for melting of solids proposed by F.A. Lindemann in 1910, which states that crystals liquefy when their atomic root mean square fluctuations exceed a certain threshold value. The common scaling we found for protein mean square displacements at melting not only sheds unique light on the relationship between protein flexibility and stability, but also opens the possibility to predict protein unfolding in special environments (e.g., the cell interior) by following thermal local fluctuations.
The striking analogy between the melting of inorganic crystals and native biomolecules suggests that these seemingly very different systems may share similar behavior in correspondence of phase transitions. On these grounds, we may speculate that simplified theories of solids can also be effectively applied to interpret the behavior of complex biological systems.