Surface changes at fertilization: integration of sea urchin (Arbacia punctulata) sperm and oocyte plasma membranes

To examine the integration and fate of the sperm plasma membrane following its incorporation into the oocyte plasma membrane, we have fertilized sea urchin (Arbacia punctulata) gametes reciprocally labeled with cationized ferritin. When unlabeled oocytes were inseminated with labeled sperm, cationized ferritin acceptors moved laterally from the sperm plasma membrane into the fertilization cone and surrounding microvilli, mixing with components of the oocyte plasmalemma. Labeled oocytes inseminated with unlabeled sperm produced extremely large fertilization cones, completely devoid of cationized ferritin, while the remainder of the oocyte surface remained heavily labeled. Surface area measurements indicated that if all the sperm plasmalemma were utilized to delimit a fertilization cone it would provide less than 10% of the total surface membrane. Evidence is presented indicating that a principal source of membrane to the expanding fertilization cone of inseminated oocytes is from microvilli, i.e., microvilli are retracted to accommodate fertilization cone formation. Membrane delimiting the fertilization cone has a much lower affinity for agents (cationized ferritin and concanavalin A) that stain negatively charged and carbohydrate moieties compared to other regions of the oocyte surface. These ultrastructural observations indicate that significant rearrangements occur in the oocyte and sperm plasma membranes following gamete fusion which give rise to asymmetries in membrane topography; components of both membranes are redistributed within the bilayer adjacent to and delimiting the fertilization cone.