The development of the hexagonally structured egg envelope of the C‐O sole (Pleuronichthys coenosus)

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Abstract
The surface of a mature, pelagic C-O sole egg is composed of polygonal chambers having 4-8 sides, most of which are hexagonally shaped. This honeycomb pattern initially appears on primary oocytes as a thin layer of compact, electron-dense material. Discrete thickenings begin to develop on the envelope of perinuclear stage oocytes. The thickenings lengthen and thin to form the hexagonal walls of the envelope in oocytes undergoing yolk vesicle formation. The walls of each hexagonal chamber occur in an area corresponding to the lateral margins of the adjacent follicle cell, suggesting that the hexagonal walls are produced by the follicle cells. The hexagonal layer is nearly complete at the beginning of vitellogenesis, and as vitellogenesis continues, a striated envelope layer composed of fibrillar lamellae develops between the oocyte and the hexagonal layer. The striated layer appears to be secreted by the oocyte. After vitellogenesis is completed, oocytes are ovulated and double in size during a period of maturation. Concurrently, the striated primary envelope stretches and thins into 8-9 horizontal lamellae. On the mature egg surface, the polygonal chambers are about 24-31 .mu.m in diameter. Within each chamber there is a subpattern of polygonal areas; each polygon is 1.5-2.0 .mu.m in diameter, and circumscribes a pore canal opening. This exceptional envelope may furnish the egg with some degree of protection, resiliency, and buoyancy, but its specific functions are not known. [The ecological significance of such an elaborate surface pattern is also explored.].