The Eocene high latitude Australasian 'tropics' in a changing climate: resolving conflicting evidence. Between 45 to 30 million years ago, high latitude subtropical floras in Australia and New Zealand experienced significant climate change, leading to the evolution of present day vegetation. Understanding the effects of this climate change on extinction and speciation will produce more accurate predictions about modern floras when faced with climate change.
Determining the relative roles of dispersal and vicariance in the assembly of the New Zealand fauna. New fossils from New Zealand's St Bathans Fauna (19-16 million years) will revolutionise our understanding of the shared biodiversity and evolutionary history of New Zealand and Australia through the first views of the origin and evolution of major Gondwanan groups including frogs, crocodiles, birds and bats on the now mostly-drowned continent Zealandia.