My question is because we know that divalent ions can substitute calcium in the biomineralization process of some marine calcifiers and if we have a huge amount of free Fe2+ from pollution, for example, would it be possible that this free iron substitute calcium and we have any dislocations of the d spacing of the calcite lattices or even the formation of calcium iron carbonates such as ankerite? Can we have any response from it by doing High-resolution TEM and Electron Diffraction?

More Rodrigo Tomazetto de Carvalho's questions See All
Similar questions and discussions