Recent Fourier analyses of fossil extinction data have indicated that the p
ower spectrum of extinction during the Phanerozoic may take the form of 1/f
noise, a result which, it has been suggested, could be indicative of the p
resence of 'critical dynamics' in the processes giving rise to extinction.
In this paper we examine extinction power spectra in some detail, using fam
ily-level data from two widely available compilations. We find that althoug
h the average form of the power spectrum roughly obeys the 1/f lay the spec
trum can be represented more accurately by dividing it into two regimes: a
low-frequency one which is well fit by an exponential, and a high-frequency
one in which it follows a power law with a 1/f(2) form. We give explanatio
ns for the occurrence of each of these behaviours and for the position of t
he crossover between them.