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Electron microscopy on the polyp of staghorn corals with special reference to its skeleton formation

Abstract

The formation of skeletons is one of the most conspicuous characteristics of Scleroactinian corals. Naturally, many scholars have worked on this problem using either classical histological methods, such as Fowler (2), Boume (1), Krempf (11), Hayashi (4), or modem methods of electron microscope or of isotopes, such as Wainwright (13), Sato (12), and Goreau (3). In our electron microscopic studies on the Scleroactinian corals we also examined both polyps and skeletons from various kinds of corals. However, the skeleton is too hard to get good results for the elucidation of the skeleton formation. This fact is more pronounced when we use materials from the coasts of the main islands of Japan where the corals grow very slowly. The processes of spicule formation in a Gorgonian coral (5) and Alcyonarian corals (Heteroxenia (9) and organ-pipe coral (10)) are observed within scleroblasts which usually originate in the ectodermal cells and are embedded in the mesogloea. In some rapidly growing corals. calicoblastic cells are found around the growing portion of the skeleton, but seldom in the old or resting portion. This fact suggests that the skeleton is formed by calicoblastic cells which are derived from the ectodermal cells and which accumulate calcareous substances within them, thus turning into a skeleton

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