We examined the effects of HCO3- and CO2 acidosis on osteoclast-mediated Ca
2+ release from 3-day cultures of neonatal mouse calvaria. Ca2+ release was
minimal above pH 7.2 in control cultures but was stimulated strongly by th
e addition of small amounts of H+ to culture medium (HCO3- acidosis). For e
xample, addition of 4 meq/l H+ reduced pH from 7.12 to 7.03 and increased C
a2+ release 3.8-fold. The largest stimulatory effects (8- to 11-fold), obse
rved with 15-16 meq/l added H+, were comparable to the maximal Ca2+ release
elicited by 1,25-dihydroxyvitamin D-3 [1,25(OH)(2)D-3; 10 nM], parathyroid
hormone (10 nM), or prostaglandin E-2 (1 muM); the action of these osteoly
tic agents was attenuated strongly when ambient pH was increased from simil
ar to7.1 to similar to7.3. CO2 acidosis was a less effective stimulator of
Ca2+ release than HCO3- acidosis over a similar pH range. Ca2+ release stim
ulated by HCO3- acidosis was almost completely blocked by salmon calcitonin
(20 ng/ml), implying osteoclast involvement. In whole mount preparations o
f control half-calvaria, similar to 400 inactive osteoclast-like multinucle
ate cells were present; in calvaria exposed to HCO3- acidosis and to the ot
her osteolytic agents studied, extensive osteoclastic resorption, with perf
oration of bones, was visible. HCO3- acidosis, however, reduced numbers of
osteoclast-like cells by similar to 50%, whereas 1,25(OH)(2)D-3 treatment c
aused increases of similar to 75%. The results suggest that HCO3- acidosis
stimulates resorption by activating mature osteoclasts already present in c
alvarial bones, rather than by inducing formation of new osteoclasts, and p
rovide further support for the critical role of acid-base balance in contro
lling osteoclast function.