Nitric oxide (NO) triggers marked osteoclast retraction which closely resem
bles that due to Ca2+, The effect of Ca2+ has been attributed to a stimulat
ed release of NO. Here, we show for the first time, by direct measurement w
ith a microsensor, that osteoclasts do indeed produce NO and that this prod
uction is enhanced by a high Ca2+. We also show that the Ca2+ ionophore, A2
3187, mimics the latter. Furthermore, osteoclasts on dentine produce more N
O than osteoclasts on glass and NO release from dentine-plated osteoclasts
is much less sensitive to stimulation by Ca2+, Finally, the microsomal Ca2 store-depleting agent, thapsigargin, attenuates NO release only from osteo
clasts on glass, suggesting that stored Ca2+ has the dominant effect in mod
ulating NO release from non-resorbing cells. NO is a powerful inhibitor of
bone resorption: a direct demonstration of its production is therefore stro
ng evidence for a role in modulating osteoclast function. (C) 1999 Academic
Press.