Abstract

New Zealand’s unique biodiversity has long been considered both the product of a ‘Moa’s Ark’ isolationist experiment since the break-up of Gondwana and the result of millions of years of transoceanic migration. Increasingly, palaeontological and genetic evidence suggest that much of New Zealand avifauna results from dispersal from Australia. We synthesise a growing number of evolutionary genetic studies to show a previously unrecognised clustering of divergence times in Australian and New Zealand bird species pairs, across the avian phylogeny, around 2.5 million years ago at the beginning of the Pleistocene. The timing coincides with the dramatic environmental changes associated with the Plio-Pleistocene transition. Intriguingly, recent anthropogenic impacts and environmental modifications are replicating in some important ways conditions during the Pleistocene glacial periods, resulting in a new wave of avian ‘native invaders’ into New Zealand.

Highlights

  • New Zealand has long been regarded as a model system for understanding Southern Hemisphere biogeography and evolution

  • Low clutch sizes are typical of deep-endemic New Zealand bird species (Worthy and Holdaway, 2002). We argue that this factor reduced the probability of Australian birds establishing

  • The onset of the Pleistocene glacial cycles led to the periodic reduction and fragmentation of forest in New Zealand and the development of open shrubland-grassland habitats, in the rain-shadow region to the east

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Summary

Introduction

New Zealand has long been regarded as a model system for understanding Southern Hemisphere biogeography and evolution. Establishment over the Neogene, that is the last 23 Mya (Wallis and Jorge, 2018), should have resulted in an even spread of divergence times between Australian and New Zealand sister species.

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