Induction of calcium-dependent, localized cortical granule breakdown in sea-urchin eggs by voltage pulsation.

A technique that employs a high-voltage pulses to produce pores in cell membranes (Kinosita and Tsong (1977) Proc. Natl. Acad. Sci. U.S.A. 74, 1923) has been used to investigate the role of Ca2+ in the early events of activation of sea-urchin eggs. Exposure of eggs to a voltage pulse of 1 kV/cm for 100 microseconds resulted in localized exocytosis of the contents of cortical granules and development of a partial fertilization envelope. This effect was triggered by entrance of Ca2+ through the voltage-induced pores. In a medium containing 100 microM Ca2+ and 45Ca2+ tracer, the voltage-treated eggs admitted 3.6 +/- 0.3 fmol Ca2+/egg within a few seconds. Untreated eggs took up only 1.0 +/- 0.2 fmol/egg after minutes of incubation. Furthermore, depletion of Ca2+ or the presence of EGTA in the external medium prevented elevation of the fertilization envelope by the voltage pulsation. Delay in Ca2+ addition after the voltage pulsation reduced the fraction of eggs that developed partial fertilization envelope. Loss of essential cytoplasmic components during the delay period is judged unlikely, since these eggs were viable, could form partial fertilization envelopes if re-pulsed in the presence of Ca2+, and could develop to normal blastula stage embryos upon fertilization with sperm. Thus, we interpret this effect as due to a resealing of pores; the half-life of pores being 20 s. The elevation of partial fertilization envelopes occurred only at the loci facing the anode, and multiple pulses with mixing resulted in the formation of multiple fertilization envelopes. These envelopes were stable for up to several hours; further propagation (wave spreading) was not observed. The above results indicate that a primary reaction in the sequence of steps in fertilization envelope formation involves Ca2+ to trigger cortical granule breakdown and formation of the fertilization envelope.