A range of characters from modern and fossil species are used to prese
nt a phylogeny of Eucryphia Cav. (Eucryphiaceae). Amongst the extant t
axa, the Australian species form a monophyletic group, but the South A
merican species are paraphyletic. This, coupled with their present-day
distribution and the fossil record, supports the view that Eucryphia
had a Gondwanic origin at least 50 million years prior to the disrupti
on of Australia from Antarctica. Although based on a limited data set
with only vegetative characters available, the inclusion of the fossil
members of Eucryphiaceae has demonstrated several trends that have be
en inferred to represent a response to the changing climatic condition
s of the Cenozoic. These responses have included a general decrease in
leaf size, loss of senate leaf margins and the development of peltifo
rm cuticular extensions on the abaxial leaf surface. These extensions
may aid in decreasing transpirational water loss and/or increasing fro
st resistance.