Ch. Joiner et al., DEOXYGENATION-INDUCED CATION FLUXES IN SICKLE CELLS .4. MODULATION BYEXTERNAL CALCIUM, American journal of physiology. Cell physiology, 38(2), 1995, pp. 403-409
Net cation movements were measured in low-density sickle red blood cel
ls (SS RBC) in the presence and absence of oxygen. External Ca2+ (Ca-o
(2+) partially inhibited deoxygenation-induced fluxes of both Na+ and
K+. Deoxygenation-induced Na+ influx was reduced by 2 mM Ca-o(2+) to 0
.71 +/- 0.04 (SE) of its value in Ca2+-free solutions, whereas this ra
tio was 0.90 +/- 0.05 for K+ efflux (P < 0.01 by paired t-test). Becau
se Ca-o(2+) inhibited Na+ influx more than K+ efflux, net cation loss
in deoxygenated SS RBC was higher in the presence of Ca-o(2+). In sepa
rate experiments, Ca-o(2+) reduced deoxygenation-induced Na+ influx to
0.66 +/- 0.03 of its Ca2+-free value compared with 0.77 +/- 0.03 for
Rb+ influx (P < 0.001), indicating relative selectivity of this effect
far Na+ over Rb+. However, this effect is not specific for Ca2+ becau
se other divalent cations also inhibited deoxygenation-induced Na+ and
K+ fluxes. Under the conditions of these experiments, no evidence for
K+ channel activation was found, indicating that K+ loss measured in
deoxygenated SS RBC was mediated by the deoxygenation-induced pathway.
These studies show that in the presence of Ca-o(2+) deoxygenation-ind
uced Na+ influx and K+ efflux are unbalanced. This pathway can, theref
ore, mediate cation loss and contribute directly to cellular dehydrati
on in SS RBC.