The Raman spectrum of polycrystalline vaterite is presented and compar
ed to spectra of calcite and aragonite, the other two common CaCO3 pol
ymorphs; Raman spectroscopy easily distinguishes between these three p
olymorphs. An important feature of the Raman spectrum of vaterite is s
plitting of both the vl and v(4) peaks. The splitting of the v(1) peak
implies two distinct site symmetries for the CO3-2 groups. A definiti
ve crystal structure determination of vaterite is not yet available, b
ut none of the three proposed structures for vaterite show such a feat
ure.