Na movements and their oscillations during fertilization and the cell cycle in sea urchin eggs

We have analysed in detail the Na⁺ content and Na⁺ influx during fertilization and first divisions of the sea urchin egg (Paracentrotus lividus) using a filtration technique devised to eliminate rapidly contamination by the Na⁺ of external sea water. In the first 5 min following fertilization the egg fills up with Na⁺ (+ 30%). Thereafter Na⁺ is extruded and the Na⁺ content stabilizes at about 60% of the unfertilized egg level by the second cleavage (2 h). The initial increase in Na⁺ content is due to a large increase in Na⁺ influx already detected at 20 sec. The Na⁺ influx reaches its maximum at 1 min and its minimum at 5 min. H⁺ excretion follows the same kinetics. A second increase in Na⁺ influx is noted 5–10 min after fertilization; it reaches its maximum at prophase metaphase (30 min) and its minimum during cleavage (60 min). These oscillations in Na⁺ influx were observed for the first three divisions. Fertilization also immediately stimulates the Na⁺ efflux which remains elevated throughout the cell cycle and is responsible for the depletion of the Na⁺ content of the embryos. Activation of the eggs by weak amine bases (5 mM NH₄Cl) which bypasses the early cortical reaction produces only a depletion in the Na⁺ content of the egg similar to that produced by fertilization. NH₄Cl also increases the Na⁺ influx soon after fertilization, although no transient variations are noted.