Separating water content from network dynamics in cell nuclei with Brillouin microscopy
Lucie Vovard, Alexis Viel, Estelle Bastien, Lou-Anne Goutier, Gaetan Jardine, Jeremie Margueritat, Sylvain Monnier, Thomas Dehoux
TL;DR
This study uses Brillouin microscopy to separate water content from solid-network dynamics in living cell nuclei under osmotic compression. By combining Brillouin shift $\nu_B$ and linewidth $\Gamma_B$ with FXm volume measurements, the authors show that $\nu_B$ is mainly governed by water content while $\Gamma_B$ reveals network-driven dissipation, requiring a poroelastic (Biot-like) description with a quasi-constant friction $f$ (≈$8.5\times10^{12}$ N s m$^{-4}$). The nucleus behaves as a two-phase system (water + solid network) where an isostress mixing law describes $\nu_B$ at low $\phi$ and a poroelastic framework accounts for $\Gamma_B$ at higher $\phi$, providing a unified interpretation of hypersonic Brillouin data in cells. This work offers a framework to decouple water content from polymer-network mechanics in nuclei, with implications for studying molecular crowding and water transport in living cells.
Abstract
Probing forces, deformations and generally speaking the mechanical properties of cells is the hallmark of mechanobiology. In the last two decades many techniques have been developed to this end that are largely based on deforming the cells and measuring the reaction force. In cells, an alternative approach has been implemented mid 2010's, based on Brillouin Light Scattering (BLS) that produces a spectrum that can be interpreted as the response of the sample to an infinitesimal uniaxial compression at picosecond timescales. In all of these measurements, the response of the cell is quantified with a colloquial "stiffness" that encompasses both the contribution of load-bearing structures and volume changes, much to confusion. To clarify the interpretation of the hypersonic data obtained from BLS spectra, we vary the relative volume fraction of intracellular water and solid network by applying osmotic compressions to single cells. In the nucleus, we observe a non-linear increase in the sound velocity and attenuation with increasing osmotic pressure that we fit to a poroelastic model, providing an estimate of the friction coefficient between the water phase and the network. By comparing BLS data to volume measurements, our approach demonstrates clearly that BLS shift alone is mostly sensitive to water content while the additional analysis of the linewidth allows identifying the contribution of the biopolymer-based network dynamics in living cells.
