After examining some perceived inconsistencies in the relationship bet
ween species richness and energy, Latham and Ricklefs rejected the Ene
rgy Diversity Theory in favour of historical explanations of the geogr
aphical patterns of tree species richness. We have reexamined Latham a
nd Ricklefs's data, both by itself and pooled with Currie and Paquin's
data. We find that Latham and Ricklefs's data are, in fact, consisten
t with the richness-energy hypothesis. Because of strong collinearity
between annual evapotranspiration and region in their particular data
sets, the data cannot be used to distinguish between the hypotheses th
at contemporary climate, versus some other interregional difference, i
s responsible for observed species richness patterns. Finally,, there
is no particular reason to attribute differences among regions to hist
orical factors rather than to contemporary ones.