A combination of ab initio molecular dynamic simulations and fully relaxed
total energy calculations is used to predict that molecular CO2 should tran
sform to nonmolecular carbonate phases based on CO4 tetrahedra at pressures
in the range of 35 to 60 gigapascals. The simulation suggests a variety of
competing phases, with a more facile transformation of the molecular phase
at high temperatures. Thermodynamically, the most stable carbonate phase a
t high pressure is predicted to be isostructural to SiO2 alpha-quartz (low
quartz). A class of carbonates, involving special arrangements of CO4 tetra
hedra, is found to be more stable than all the other silica-like polymorphs
.