S. Raz et al., Formation of high-magnesian calcites via an amorphous precursor phase: Possible biological implications, ADVAN MATER, 12(1), 2000, pp. 38
The skeletons of many organisms are composed of high-magnesian calcite (10-
40 mol.-% Mg), which is not stable under equilibrium conditions. Here, high
magnesian calcite particles (>20 mol.-%) are produced at ambient temperatu
re in the presence and absence of additives. Most importantly these particl
es are shown to initiate from an amorphous precursor phase. The Figure show
s the typical dumb-bell morphology of magnesian calcite spherulites.