When exposed to hypoosmotic stress, cells initially swell in proportion to the reduction in osmolarity and then normalize their volume via a process known as regulatory volume decrease. The latter involves the release of osmolytes, both inorganic (K + and Cl ) ) and organic (amino acids, polyols, and methylamines) and the exit of obligated water (McManus et al. 1995). Although inorganic osmolytes constitute the quantitatively major fraction of the osmolyte pool (60-65%; Pasantes-Morales et al. 2002), large changes in ion concentration can adversely impact cell excitability. Thus, the pool of 'non-perturbing' organic osmolytes plays a pivotal role in countering changes in osmolarity without compromising cell function. One of the most quantitatively important organic