Mechanism of Calcification in the Marine Alga Emiliania huxleyi [and Discussion]

• Published in: Philosophical transactions of the Royal Society of London. Series B, Biological sciences Biological sciences, 1984-02, Vol.304 (1121), p.435-444
• Main Authors: Westbroek, P., de Jong, E. W., van der Wal, P., Borman, A. H., de Vrind, J. P. M., Kok, D., de Bruijn, W. C., Parker, S. B.
• Format: Article
• Language: English
• Subjects: Algae; Calcite; Calcium carbonates; Chemical precipitation; Crystallization; Crystals; Hammers; Nuclear membrane; Polysaccharides; Vacuoles
• ISSN: 0962-8436; 0080-4622; 1471-2970; 2054-0280
• DOI: 10.1098/rstb.1984.0037

Coccoliths are delicate calcified structures produced by marine unicellular algae. In the species Emiliania huxleyi the calcium carbonate (mostly calcite) is closely associated with a complex, acidic polysaccharide which binds calcium ions specifically, interferes with the in vitro crystallization of calcium carbonate, and appears to be bound to a positively charged protein before the crystallization process is finished. Ultra-high resolution electron microscopy of the coccoliths reveals that the crystallographic structure differs in different parts of the constituent calcite elements. The synthesis of the coccoliths takes place intracellularly, and when this process is ended the coccoliths are extruded and incorporated into the so-called coccosphere surrounding the cell. Transmission electron microscope studies reveal the localization of polysaccharides in the calcifying organelle by means of cytochemical staining technique. The results are combined in a putative scheme describing coccolithogenesis.