Jk. Foskett et al., ISOSMOTIC MODULATION OF CELL-VOLUME AND INTRACELLULAR ION ACTIVITIES DURING STIMULATION OF SINGLE EXOCRINE CELLS, The Journal of experimental zoology, 268(2), 1994, pp. 104-110
Stimulation of salivary secretion is associated with a rise of [Ca2+](
i) in acinar cells. We examined the osmotic and ionic consequences of
activation of Ca2+-dependent K+ and Cl- channels, by simultaneous opti
cal determinations of cell volume and [Ca2+](i), [Cl-](i) or [Na+](i)
during muscarinic stimulation of single salivary acinar cells, using a
differential interference contrast (DIC)-fluorescence microscope. Car
bachol caused a rapid rise of [Ca2+](i), as well as a substantial cell
shrinkage. Despite variability in the level and kinetics of the subse
quent sustained phase of the [Ca2+](i) response, cell volume was corre
lated with [Ca2+](i) in all cases. Elevated [Ca2+](i) was both necessa
ry and sufficient to cause these changes in cell volume. The propositi
on that changes in cell volume reflected changes in cell solute conten
t was confirmed by simultaneously measuring [Cl-](i) and cell volume.
Simultaneous determinations of cell volume and [Na+](i) indicated that
the initial cell shrinkage was due entirely to K+ and Cl- efflux. Sub
sequent to the initial shrinkage, [Na+](i) rose to high levels, primar
ily due to activation of Na+/H+ exchange. Thus, modulation of ion tran
sport activities under isosmotic conditions results in substantial cha
nges in cell solute content and cell volume. Subsequent to the early C
a2+-induced changes in these parameters, other transporters become act
ive, but it is unclear what signals their activation. Cell swelling by
osmotic dilution of the bath resulted in compensatory cell shrinkage
(RVD) which was sensitive to K+ and Cl- gradients. Nevertheless, a ris
e of [Ca2+](i) was not necessary for RVD. Osmotic shrinkage and/or cel
l acidification were insufficient to activate Na+ influx. Our data sug
gest that the intracellular signalling pathways used by cells to activ
ate ion transport under anisosmotic conditions may not be the same as
those employed under isosmotic conditions. (C) 1994 Wiley-Liss, Inc.