The hydraulic resistance of the plasma membrane was measured on single
internodal cells of Chara corallina using the method of transcellular
osmosis. The hydraulic resistance of the plasma membrane of high CO2-
grown cells was significantly higher than the hydraulic resistance of
the plasma membrane in low CO2-grown cells. Therefore we tested the po
ssibility that the ''bicarbonate transport system'', postulated to be
present in low CO2-grown cells, serves as a water channel that lowers
the hydraulic resistance of the plasma membrane. We were unable to fin
d any correlation between agents that inhibited the ''bicarbonate tran
sport system'' and agents that increased the hydraulic resistance of l
ow CO2-grown cells. We did, however, find a correlation between the pe
rmeability of the cell to water and CO2. We propose that the reduced h
ydraulic resistance of the plasma membrane of the low CO2-grown cells
is a function of a change in either the structural properties of the l
ipid bilayer or the activity of a CO2 transport protein so that under
conditions of reduced inorganic carbon, the plasma membrane becomes mo
re permeable to CO2, and consequently to other small molecules, includ
ing H2O, methanol and ethanol.