The order Passeriformes (“perching birds”) comprises extant species diversity comparable to that of living mammals. For over a decade, a single phylogenetic hypothesis based on DNA–DNA hybridization has provided the primary framework for numerous comparative analyses of passerine ecological and behavioral evolution and for tests of the causal factors accounting for rapid radiations within the group. We report here a strongly supported phylogenetic tree based on two single-copy nuclear gene sequences for the most complete sampling of passerine families to date. This tree is incongruent with that derived from DNA–DNA hybridization, with half of the nodes from the latter in conflict and over a third of the conflicts significant as assessed under maximum likelihood. Our historical framework suggests multiple waves of passerine dispersal from Australasia into Eurasia, Africa, and the New World, commencing as early as the Eocene, essentially reversing the classical scenario of oscine biogeography. The revised history implied by these data will require reassessment of comparative analyses of passerine diversification and adaptation.

Avian diversification has been influenced by global climate change, plate tectonic movements, and mass extinction events. However, the impact of these factors on the diversification of the hyperdiverse perching birds (passerines) is unclear because family level relationships are unresolved and the timing of splitting events among lineages is uncertain. We analyzed DNA data from 4,060 nuclear loci and 137 passerine families using concatenation and coalescent approaches to infer a comprehensive phylogenetic hypothesis that clarifies relationships among all passerine families. Then, we calibrated this phylogeny using 13 fossils to examine the effects of different events in Earth history on the timing and rate of passerine diversification. Our analyses reconcile passerine diversification with the fossil and geological records; suggest that passerines originated on the Australian landmass ∼47 Ma; and show that subsequent dispersal and diversification of passerines was affected by a number of climatological and geological events, such as Oligocene glaciation and inundation of the New Zealand landmass. Although passerine diversification rates fluctuated throughout the Cenozoic, we find no link between the rate of passerine diversification and Cenozoic global temperature, and our analyses show that the increases in passerine diversification rate we observe are disconnected from the colonization of new continents. Taken together, these results suggest more complex mechanisms than temperature change or ecological opportunity have controlled macroscale patterns of passerine speciation.

F. Keith Barker, François M. Lutzoni; The Utility of the Incongruence Length Difference Test, Systematic Biology, Volume 51, Issue 4, 1 July 2002, Pages 625–63

Passerine birds comprise over half of avian diversity, but have proved difficult to classify. Despite a long history of work on this group, no comprehensive hypothesis of passerine family–level relationships was available until recent analyses of DNA–DNA hybridization data. Unfortunately, given the value of such a hypothesis in comparative studies of passerine ecology and behaviour, the DNA–hybridization results have not been well tested using independent data and analytical approaches. Therefore, we analysed nucleotide sequence variation at the nuclear RAG–1 and c–mos genes from 69 passerine taxa, including representatives of most currently recognized families. In contradiction to previous DNA–hybridization studies, our analyses suggest paraphyly of suboscine passerines because the suboscine New Zealand wren Acanthisitta was found to be sister to all other passerines. Additionally, we reconstructed the parvorder Corvida as a basal paraphyletic grade within the oscine passerines. Finally, we found strong evidence that several family–level taxa are misplaced in the hybridization results, including the Alaudidae, Irenidae, and Melanocharitidae. The hypothesis of relationships we present here suggests that the oscine passerines arose on the Australian continental plate while it was isolated by oceanic barriers and that a major northern radiation of oscines (i.e. the parvorder Passerida) originated subsequent to dispersal from the south.