Vs. Shankar et al., EFFECT OF MEMBRANE-POTENTIAL ON SURFACE CA2+ RECEPTOR ACTIVATION IN RAT OSTEOCLASTS, Journal of cellular physiology, 162(1), 1995, pp. 1-8
Osteoclasts are known to possess a divalent cation-sensitive receptor,
the Ca2+ receptor (CaR). The latter monitors changes in the local Ca2
+ concentration generated as a result of hydroxyapatite dissolution. C
aR activation elevates cytosolic [Ca2+] and thereby inhibits osteoclas
tic bone resorption. Recent studies have used Ni2+ as a surrogate CaR
agonist to elicit changes in cytosolic [Ca2+]. This article examines t
he effects of membrane potential changes on the kinetics of the cytoso
lic [Ca2+] signal resulting from such Ni2+-induced CaR activation. Mem
brane potential was altered through variations in the extracellular [K
+] in combination with applications of the K+ ionophore, valinomycin.
Membrane potential changes were confirmed by independent electrophysio
logical patch clamp studies of whole osteoclasts. The application of v
alinomycin produced a distinct, sustained elevation of cytosolic [Ca2] in single fura 2-loaded cells, a ''primary'' response. This response
was independent of valinomycin concentration (between 5 nM to 5 mu M)
and persisted in Ca2+-free, EGTA-containing solutions. It also persis
ted both in high (105 mM) and low (5 mM) extracellular [K+]. A gradual
''secondary'' elevation of cytosolic [Ca2+] then followed with the co
ntinued application of valinomycin, but this was eliminated by sequest
ering the extracellular [Ca2+] or by increasing extracellular [K+] fro
m 5 to 105 mM. In a separate set of experiments, the presence of 5 mu
M [valinomycin]-([K+] = 5 mM) prolonged the cytosolic [Ca2+] signal el
icited by 50 mu M-[Ni2+] application. These prolonged kinetics persist
ed in low extracellular [Ca2+] (zero-added Ca2+), but reverted to a ra
pid time-course in the presence of 105 mM-[K+] or at higher [Ni2+] (50
0 mu M and 5 mM). The experiments thus indicate that membrane voltage
modifies the kinetics of CaR activation by Ni2+ and therefore suggests
that the CaR is an integral protein in the osteoclast surface membran
e. (C) 1995 Wiley-Liss, Inc.