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Abstract Studying how genetic variation is structured across space, and how it relates to divergence in phenotypic traits relevant to reproductive isolation, is important for our overall understanding of the speciation process. We used reduced-representation genomic data (ddRAD-seq) to examine patterns of genetic variation across the full distribution of an Andean warbler species complex (Myioborus ornatus–melanocephalus), which includes a known hybrid zone between two strikingly different plumage forms. Genetic structure largely reflects geographic variation in head plumage, some of which corresponds to major topographic barriers in the Andes. We also found evidence of isolation by distance shaping genetic patterns across the group’s broad latitudinal range. We found thatchrysopsandbairdi, two taxa with marked plumage differences that have a known hybrid zone, were characterized by low overall genetic divergence. Based on our cline analyses of both plumage and genomic hybrid indices, this hybrid zone extends for approximately 250 km, where advanced generation hybrids are likely most common. We also identified a slight difference in the centers of the plumage and genomic clines, potentially suggesting the asymmetric introgression ofchrysops-like plumage traits. By studying genetic variation in a phenotypically complex group distributed across a topographically complex area, which includes a hybrid zone, we were able to show how both geographic features and potentially sexually selected plumage traits may play a role in species formation in tropical mountains 

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. 

The tropics are the source of most biodiversity yet inadequate sampling obscures answers to fundamental questions about how this diversity evolves. We leveraged samples assembled over decades of fieldwork to study diversification of the largest tropical bird radiation, the suboscine passerines. Our phylogeny, estimated using data from 2389 genomic regions in 1940 individuals of 1283 species, reveals that peak suboscine species diversity in the Neotropics is not associated with high recent speciation rates but rather with the gradual accumulation of species over time. Paradoxically, the highest speciation rates are in lineages from regions with low species diversity, which are generally cold, dry, unstable environments. Our results reveal a model in which species are forming faster in environmental extremes but have accumulated in moderate environments to form tropical biodiversity hotspots.