Fertilization causes a single Ca2+ increase that fully depends on Ca2+ influx in oocytes of limpets (Phylum Mollusca, Class Gastropoda).

Mature limpet oocytes arrested at the first metaphase (MI) of meiosis are activated by the stimulation of fertilizing sperm. The aim of the present study was to clarify the spatiotemporal property and mechanism of intracellular Ca2+ increase in limpet oocytes, which is a prerequisite signal for initiation of development at fertilization. In all of the five limpet species tested, the initial Ca2+ rising phase just after fertilization took the form of a centripetal Ca2+ wave spreading from the whole cortex to the center (cortical flash), yielding a homogeneous Ca2+ elevation throughout the oocyte. The Ca2+ level remained high during the subsequent plateau phase lasting for several minutes and then returned nearly to the original value. No additional Ca2+ increase followed the plateau phase at least by the time of first cleavage. Both rising and plateau phases of Ca2+ increase at fertilization were inhibited by removal of external Ca2+, suggesting that continuous Ca2+ entry occurs throughout the Ca2+ increase. Injection of inositol 1,4,5-trisphosphate (IP3) was effective in generating a Ca2+ increase in mature limpet oocytes arrested at MI; however, their ability to show an IP3-induced Ca2+ increase was extremely low, as compared with other animals. Responsiveness to IP3 injection in immature oocytes arrested at the first prophase (PI) was similar to that in the mature oocytes, suggesting that the IP3-induced Ca2+ release system does not develop during the process of meiotic maturation in limpet oocytes. Caffeine, cyclic adenosine diphosphate ribose (cADPR), and nicotinic acid adenine dinucleotide phosphate (NAADP), the agents known to stimulate internal Ca2+ release mechanisms distinct from an IP3-dependent pathway, had no effect on intracellular Ca2+ changes in mature limpet oocytes. Labeling of the endoplasmic reticulum (ER) with DiI revealed that cortical ER clusters are only present in the localized region around meiotic chromosomes in mature oocytes. These data strongly suggest that Ca2+ release and its propagating mechanisms are undeveloped in limpet oocytes and that Ca2+ influx is the only Ca2+-mobilizing system available and functioning at fertilization.