Fluorescence ratio imaging was used for simultaneous measurement of cy
tosolic pH(c) and pCa(c) in Chara corallina, Nitella flexilis, and Ere
mosphaera viridis. In some experiments the electrical membrane potenti
al was also recorded. The first hint of coupling between changes in pH
(c) and pCa(c) was found in characean cells when the influence of buty
rate on cytosolic streaming was studied by laser-Doppler-anemometry (L
DA). The observed butyrate-induced cessation of cytosolic streaming su
pports the assumption that changes in pH(c) cause changes in pCa(c). T
his hypothesis was tested by simultaneously loading cells with Fura-2-
dextran and BCECF-dextran. The addition of butyrate revealed strong co
upling between pCa(c) and pH(c) although this only occurred when the d
ifference between pH(c) and pCa(c) was less than 0.4 units (+/- 0.24,
n = 7). The measured relationship between the changes in pCa(c) and pH
(c) could be fitted by a cytoplasmic buffer exchange process. Protons
imported by butyrate into the cytoplasm are able to displace Ca++ ions
from cytoplasmic buffer sites. Three dissociation constants of the cy
toplasmic buffer were pK(1) = 6.2, pK(2) = 7.1 for proton buffering, a
nd pK(Ca) = 6.7 for Ca++ ion buffering. Other possible mechanisms, suc
h as butyrate-induced Ca++ influx through the plasmalemma and Ca++ rel
ease from internal stores are discussed. They are not necessary to exp
lain the observed coupling but cannot be excluded from the process. Us
ing the butyrate technique, the cytosolic in vivo proton buffer capaci
ties of N. flexilis, C. corallina, and E. viridis were determined as b
eta(i) = 30 mM . H+/pH-unit, beta(i) = 46 mM . H+/pH-unit, and beta(i)
= 90 mM . H+/pH-unit, respectively. The values obtained in vivo are g
reater than those found previously using extraction methods. This can
be explained in terms of pump activity and exchange with cell organell
es, i.e., the vacuole. The high value of beta(i) found in Eremosphaera
reflects adaptation to its habitat.