Large changes in intracellular pH and calcium observed during heat shock are not responsible for the induction of heat shock proteins in Drosophila melanogaster.

Heat shock caused significant changes in intracellular pH (pHi) and intracellular free calcium concentration [( Ca2+]i) which occurred rapidly after temperature elevation. pHi fell from a resting level value at 25 degrees C of 7.38 +/- 0.02 (mean +/- standard error of the mean, n = 15) to 6.91 +/- 0.11 (n = 7) at 35 degrees C. The resting level value of [Ca2+]i in single Drosophila melanogaster larval salivary gland cells was 198 +/- 31 nM (n = 4). It increased approximately 10-fold, to 1,870 +/- 770 nM (n = 4), during a heat shock. When salivary glands were incubated in calcium-free, ethylene glycol-bis(beta-aminoethyl ether)-N,N',N'-tetraacetic acid (EGTA)-buffered medium, the resting level value of [Ca2+]i was reduced to 80 +/- 7 nM (n = 3), and heat shock resulted in a fourfold increase in [Ca2+]i to 353 +/- 90 nM (n = 3). The intracellular free-ion concentrations of Na+, K+, Cl-, and Mg2+ were 9.6 +/- 0.8, 101.9 +/- 1.7, 36 +/- 1.5, and 2.4 +/- 0.2 mM, respectively, and remained essentially unchanged during a heat shock. Procedures were devised to mimic or block the effects of heat shock on pHi and [Ca2+]i and to assess their role in the induction of heat shock proteins. We report here that the changes in [Ca2+]i and pHi which occur during heat shock are not sufficient, nor are they required, for a complete induction of the heat shock response.