This review surveys the signals, intermediate events, and effectors th
at connect GC swelling and shrinking to environmental conditions. GCs
swell when protons are released, hyperpolarizing the plasma membrane (
shifting the membrane potential to more negative voltages). This hyper
polarization drives K+ entry down an electrical gradient through inwar
d K+ channels. Cl- influx also occurs, presumably via Cl-/H+ symport o
r Cl-/OH- antiport. The entering ions are stored primarily in the vacu
ole along with malate, which is synthesized during stomatal opening. A
s intracellular osmotica increase, GCs take up water, balancing their
water potential with that of their surroundings, and they begin to swe
ll. Differential cell wall reinforcement bends the swelling GCs outwar
d and widens the pore between them (Willmer, 1983; Taiz and Zeiger, 19
91). Stomatal closure is not the reversal of opening. Anion release an
d/or Ca2+ uptake depolarizes the plasma membrane (shifts the membrane
potential to more positive values). This depolarization provides the d
riving force for K+ efflux through outward K+ channels. As levels of K
+ and malate drop, GCs release water and shrink, relaxing the outward
bend and closing over the substomatal cavity.