Fertilization acid of sea urchin eggs: Evidence that it is H+, not CO2

The report of R. J. Gillies, M. P. Rosenberg, and D. W. Deamer (1981, J. Cell. Phys., 108, 115–122) that sea urchin fertilization acid is anaerobically produced CO₂, was reinvestigated by inseminating Strongylocentrotus purpuratus eggs in HCO^?₃-free seawater, then bubbling the seawater with N₂ to remove volatile acid. Fertilization acid production occurred in HCO^?₃-free seawater and with N₂-bubbling, the pH rose 0.28 ± 0.08 unit, significantly less than the rise of 0.63 ± 0.14 unit during N₂-bubbling of HCO^?₃-free seawater that had been acidified with CO₂ and similar to the rise of 0.18 ± 0.07 unit when acidification was with HCl. We conclude that most, if not all, of the sea urchin fertilization acid is nonvolatile and thus is not CO₂; since it is not a weak acid, it must be H⁺.