Shell formation and calcium transport in the barnacle Chthamalus fragilis

The mantle epithelium of the barnacle Chthamalus fragilis (Darwin) exhibits several ultrastructural features which may serve to regulate the calcification process. At the basis-mural plate and intermural plate junctions where rapid shell growth occurs, cells are characterized by long apical cytoplasmic projections and large intercellular spaces. These features may increase the functional surface area of the epithelium and enable more rapid deposition of calcium. The cells underlying the general shell surfaces contain numerous electron-dense inclusion bodies and show frequent cellular disintegration near the growing shell interface. Release of the granular contents of these inclusion bodies has been observed in both disintegrating and non-disintegrating cells. X-ray microanalysis revealed significantly higher calcium levels in the inclusion bodies than in the surrounding cytoplasm. This suggests a calcium transport role for these inclusion bodies. Cellular debris produced as a result of the disintegration of the mantle cells near the shell may play some role in the formation of the organic matrix of the shell. The presence of large numbers of mitochondria and well-developed apical microvilli in the cells of the inner mantle epithelium suggest that these cells serve to transport calcium into the mantle from the ambient sea water.