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Monohydrocalcite
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Monohydrocalcite is a mineral that is a hydrous form of calcium carbonate, CaCO3·H2O. It was formerly also known by the name hydrocalcite, which is now discredited by the IMA. It is a trigonal which is white when pure. Monohydrocalcite is not a common rock-forming mineral, but is frequently associated with other calcium and magnesium carbonate minerals, such as , , , and .

Monohydrocalcite has been observed in , and in deposits in caves, both probably formed from spray of carbonate rich fluids. It is well known in Robe on the of as a component of beach sands of Lake Fellmongery and Lake Butler, where it is believed to be formed from algal spume. Other lacustrine deposits include Lake , , , Democratic Republic of the Congo, and , .

It has been reported as a significant component of the decomposition of in the towers of the Ikka Fjord, West . It is also noted for its bizarre occurrences, which include inside the of the , the of a ,Catherine, H., Skinner, K., Osbaldiston, G. W., Wilner, A. N. Monohydrocalcite in a guinea pig bladder stone, a novel occurrence. American Mineralogist, 62: 273 – 277, 1977. the calcareous corpuscles of a parasite, and the final stages of decomposition of the putrefying flesh of the giant .Garvie, L.A.J. Decay-induced biomineralization of the saguaro cactus ( Carnegiea gigantea) American Mineralogist, 88: 1879–1888, 2003. These occurrences suggest a biochemical origin is possible.


Formation of monohydrocalcite
Monohydrocalcite forms via a Mg-rich amorphous calcium carbonate (ACC) precursor. This Mg-rich ACC forms rapidly (seconds) and then transforms to monohydrocalcite via dissolution and reprecipitation, with monohydrocalcite forming via a nucleation-controlled reaction like spherulitic growth.

Recent studies have highlighted the importance of Mg in the formation process of monohydrocalcite. The presence of Mg in solution is known to inhibit the formation of and . However, the hydrated nature of monohydrocalcite means that full dehydration of Mg is not required before incorporation of this ion into this mineral and therefore it will more likely form than the anhydrous calcium carbonate phases.


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