Many mineralizing organisms selectively form either calcite or aragoni
te, two polymorphs of calcium carbonate with very similar crystalline
structures. Understanding how these organisms achieve this control has
represented a major challenge in the field of biomineralization. Macr
omolecules extracted from the aragonitic shell layers of some mollusks
induced aragonite formation in vitro when preadsorbed on a substrate
of beta-chitin and silk fibroin. Macromolecules from calcitic shell la
yers induced mainly calcite formation under the same conditions, The r
esults suggest that these macromolecules are responsible for the preci
pitation of either aragonite or calcite in vivo.