Herpes simplex virus 1 fluidizes the nucleus, enabling condensate formation.

Molecular processes are profoundly influenced by the biophysical properties of the cell interior. However, the mechanisms that control these physical properties and the processes they impact remain poorly understood, especially in the nucleus. We hypothesized that some viruses might change the biophysical properties of the nucleus to favor virus survival and replication and found that herpes simplex virus 1 (HSV-1) increases the mesoscale fluidity of the nucleus. The HSV-1 protein ICP4 (infected cell protein 4) caused fluidization and enabled the growth of synthetic nuclear condensates. Conversely, conditions that decreased nuclear fluidity inhibited the growth of viral replication compartment condensates and reduced infectious virus production. Together, our data suggest that ICP4 increases nuclear fluidity to promote the formation of condensates that drive the progression of the HSV-1 life cycle. We speculate that a key function of ICP4 is to overcome the crowding and elastic confinement within cell nuclei that are a fundamental barrier to virus replication.