The discovery of nonmolecular carbon dioxide under high-pressure conditions shows that there are remarkable analogies between this important substance and other group IV oxides. A natural and long-standing question is whether compounds between CO 2 and SiO 2 are possible. Under ambient conditions, CO 2 and SiO 2 are thermodynamically stable and do not react with each other. We show that reactions occur at high pressures indicating that silica can behave in a manner similar to ionic metal oxides that form carbonates at room pressure. A silicon carbonate phase was synthesized by reacting silicalite, a microporous SiO 2 zeolite, and molecular CO 2 that fills the pores, in diamond anvil cells at 18-26 GPa and 600-980 K; the compound was then temperature quenched. The material was characterized by Raman and IR spectroscopy, and synchrotron X-ray diffraction. The experiments reveal unique oxide chemistry at high pressures and the potential for synthesis of a class of previously uncharacterized materials. There are also potential implications for CO 2 segregation in planetary interiors and for CO 2 storage.high-pressure chemistry | material science | optical spectroscopy C arbon dioxide and silicon dioxide are two archetypal, group IV oxides of paramount importance for fundamental and applied chemistry and planetary sciences. CO 2 is the dominant component of the atmosphere of Earth-like planets, exists in icy forms in outer planets and asteroids, plays an important role in volcanic and seismic processes, is used as a supercritical solvent for chemical reactions, and its anthropogenic production is a major environmental issue. SiO 2 is also one of the most abundant components of terrestrial planets, and an important technological material. The chemical relationship between CO 2 and SiO 2 , in particular their reactivity, is thus of interest. Although the two systems are both group IV oxides, they are remarkably different under ambient conditions, because CO 2 is molecular and is held together by C═O double bonds, whereas SiO 2 forms network structures involving single Si─O bonds. These bonding patterns radically change under pressure. Two nonmolecular CO 2 crystalline phases and a glassy form have been discovered above 30 GPa that bear similarities to SiO 2 (1-14). The crystalline phases contain carbon in fourfold coordination by oxygen (1-10, 13, 14), and mixtures of CO 4 and CO 3 units have been found in a glassy form that has been named carbonia (13).A possible approach to favor the chemical reaction between CO 2 and SiO 2 is to select a microporous silica polymorph, such as silicalite. At ambient conditions, silicalite is characterized by a framework of four-, five-, six-, and ten-membered rings of SiO 4 tetrahedra with 5.5-Å pores (15) (Fig. 1, Left Inset). Recently, it has been found that the pores can be completely filled by simple molecules such as CO 2 and Ar under pressure, which prevents pressure-induced amorphization (PIA) and stabilizes the crystalline framework up to at least 25 GPa at room temperature (1...