Abstract
I4 2+ is the only known cyclic homopolyatomic cation or anion of iodine. It has a rectangular planar structure which may be thought of as containing two I2 + units joined by a weak π∗-π∗ 4 centre 2 electron bond.1 In this paper we report our FT-Raman spectra of I4 2+, which conflict with those published by Gillespie et al. 1 and present evidence that the peaks attributed to a species containing iodine in the +1 oxidation state are in fact due to I4 2+.