Earth history and the passerine superradiation
Edited by Michael E. Alfaro, University of California, Los Angeles, CA, and accepted by Editorial Board Member David Jablonski February 26, 2019 (received for review August 9, 2018)
Significance
Our understanding of the factors that affected the diversification of passerines, the most diverse and widespread bird order (Passeriformes), is limited. Here, we reconstruct passerine evolutionary history and produce the most comprehensive time-calibrated phylogenetic hypothesis of the group using extensive sampling of the genome, complete sampling of all passerine families, and a number of vetted fossil calibration points. Our phylogenetic results refine our knowledge of passerine diversity and yield divergence dates that are consistent with the fossil record, and our macroevolutionary analyses suggest that singular events in Earth history, such as increases in Cenozoic global temperature or the colonization of new continents, were not the primary forces driving passerine diversification.
Abstract
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.
Data Availability
Data deposition: Raw sequencing reads and ultraconserved element (UCE) nucleotide sequences are available from the National Center for Biotechnology Information (NCBI) Sequence Read Archive and Genbank as part of BioProjects PRJNA304409 and PRJNA480834. NCBI BioSample accession numbers are available in Dataset S1. The PHYLUCE computer code used in this study is available from https://github.com/faircloth-lab/phyluce. Other custom computer code, DNA alignments, analysis inputs, and analysis outputs are available from the Dryad Digital Repository database, datadryad.org/ (doi: https://doi.org/10.5061/dryad.2vd01gr).
Acknowledgments
We thank the curators, staff, and field collectors at the institutions listed in Dataset S1 for tissue samples used in this project; without their hard work, this study would not have been possible. We also thank Van Remsen for comments on earlier drafts, and we thank our three reviewers and the editor for their comments, which improved this manuscript. This study was supported by setup funds from Louisiana State University (to B.C.F.) and by funds from the National Science Foundation: Grant DEB-1655624 (to B.C.F. and R.T.B.), Grant DEB-1655736 (to B.T.S., D.T.K., and R.T.C.), Grants DEB-1655559 and DEB-1541312 (to F.K.B.), Grant DEB-1655683 (to R.T.K. and E.L.B.), Grants DEB-1241181 and DEB-1557053 (to R.G.M.), Grant DEB-1146265 (to R.T.B., A.A., R.T.C., and F.H.S.), Grant DEB-1241066 (to J.C.), and Grant DEB-1146423 (to E.P.D.). M.J.B., N.D.W., T.C.G., R.T.B., E.L.B., and B.C.F. were supported by grants from the Smithsonian Grand Challenges Consortia. G.A.B. and L.F.S. were supported by the Fundação de Amparo à Pesquisa do Estado de São Paulo (Grants 2012-23852-0 and 56378-0). L.F.S. and A.A. were supported by the Conselho Nacional de Pesquisas (Grants 302291/2015-6 and 306843/2016-1). P.A. was supported by the Swedish Research Foundation (Grant 2015-04402) and Jornvall Foundation. Portions of this research were conducted with high-performance computing resources provided by Louisiana State University (www.hpc.lsu.edu). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the US Government.
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Information & Authors
Information
Published in
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Copyright
Copyright © 2019 the Author(s). Published by PNAS. This open access article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND).
Data Availability
Data deposition: Raw sequencing reads and ultraconserved element (UCE) nucleotide sequences are available from the National Center for Biotechnology Information (NCBI) Sequence Read Archive and Genbank as part of BioProjects PRJNA304409 and PRJNA480834. NCBI BioSample accession numbers are available in Dataset S1. The PHYLUCE computer code used in this study is available from https://github.com/faircloth-lab/phyluce. Other custom computer code, DNA alignments, analysis inputs, and analysis outputs are available from the Dryad Digital Repository database, datadryad.org/ (doi: https://doi.org/10.5061/dryad.2vd01gr).
Submission history
Published online: April 1, 2019
Published in issue: April 16, 2019
Keywords
Acknowledgments
We thank the curators, staff, and field collectors at the institutions listed in Dataset S1 for tissue samples used in this project; without their hard work, this study would not have been possible. We also thank Van Remsen for comments on earlier drafts, and we thank our three reviewers and the editor for their comments, which improved this manuscript. This study was supported by setup funds from Louisiana State University (to B.C.F.) and by funds from the National Science Foundation: Grant DEB-1655624 (to B.C.F. and R.T.B.), Grant DEB-1655736 (to B.T.S., D.T.K., and R.T.C.), Grants DEB-1655559 and DEB-1541312 (to F.K.B.), Grant DEB-1655683 (to R.T.K. and E.L.B.), Grants DEB-1241181 and DEB-1557053 (to R.G.M.), Grant DEB-1146265 (to R.T.B., A.A., R.T.C., and F.H.S.), Grant DEB-1241066 (to J.C.), and Grant DEB-1146423 (to E.P.D.). M.J.B., N.D.W., T.C.G., R.T.B., E.L.B., and B.C.F. were supported by grants from the Smithsonian Grand Challenges Consortia. G.A.B. and L.F.S. were supported by the Fundação de Amparo à Pesquisa do Estado de São Paulo (Grants 2012-23852-0 and 56378-0). L.F.S. and A.A. were supported by the Conselho Nacional de Pesquisas (Grants 302291/2015-6 and 306843/2016-1). P.A. was supported by the Swedish Research Foundation (Grant 2015-04402) and Jornvall Foundation. Portions of this research were conducted with high-performance computing resources provided by Louisiana State University (www.hpc.lsu.edu). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the US Government.
Notes
This article is a PNAS Direct Submission. M.E.A. is a guest editor invited by the Editorial Board.
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Competing Interests
The authors declare no conflict of interest.
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