Minerals
are formed by organisms in all of the kingdoms of life.
Mineral formation pathways all involve uptake of ions from the environment,
transport of ions by cells, sometimes temporary storage, and ultimately
deposition in or outside of the cells. Even though the details of
how all this is achieved vary enormously, all pathways need to respect
both the chemical limitations of ion manipulation, as well as the
many “housekeeping” roles of ions in cell functioning.
Here we provide a chemical perspective on the biological pathways
of biomineralization. Our approach is to compare and contrast the
ion pathways involving calcium, phosphate, and carbonate in three
very different organisms: the enormously abundant unicellular marine
coccolithophores, the well investigated sea urchin larval model for
single crystal formation, and the complex pathways used by vertebrates
to form their bones. The comparison highlights both common and unique
processes. Significantly, phosphate is involved in regulating calcium
carbonate deposition and carbonate is involved in regulating calcium
phosphate deposition. One often overlooked commonality is that, from
uptake to deposition, the solutions involved are usually supersaturated.
This therefore requires not only avoiding mineral deposition where
it is not needed but also exploiting this saturated state to produce
unstable mineral precursors that can be conveniently stored, redissolved,
and manipulated into diverse shapes and upon deposition transformed
into more ordered and hence often functional final deposits.