(Rhacophoridae, Pseudophilautus) in Sri Lanka
Molecular Phylogenetics and Evolution 132 (2019) 14–24 Contents lists available at ScienceDirect Molecular Phylogenetics and Evolution journal homepage: www.elsevier.com/locate/ympev Diversification of shrub frogs (Rhacophoridae, Pseudophilautus) in Sri Lanka T – Timing and geographic context ⁎ Madhava Meegaskumburaa,b,1, , Gayani Senevirathnec,1, Kelum Manamendra-Arachchid, ⁎ Rohan Pethiyagodae, James Hankenf, Christopher J. Schneiderg, a College of Forestry, Guangxi Key Lab for Forest Ecology and Conservation, Guangxi University, Nanning 530004, PR China b Department of Molecular Biology & Biotechnology, Faculty of Science, University of Peradeniya, Peradeniya, Sri Lanka c Department of Organismal Biology & Anatomy, University of Chicago, Chicago, IL, USA d Postgraduate Institute of Archaeology, Colombo 07, Sri Lanka e Ichthyology Section, Australian Museum, Sydney, NSW 2010, Australia f Museum of Comparative Zoology, Harvard University, Cambridge, MA 02138, USA g Department of Biology, Boston University, Boston, MA 02215, USA ARTICLE INFO ABSTRACT Keywords: Pseudophilautus comprises an endemic diversification predominantly associated with the wet tropical regions ofSri Ancestral-area reconstruction Lanka that provides an opportunity to examine the effects of geography and historical climate change on diversi- Biogeography fication. Using a time-calibrated multi-gene phylogeny, we analyze the tempo of diversification in thecontextof Ecological opportunity past climate and geography to identify historical drivers of current patterns of diversity and distribution. Molecular Diversification dating suggests that the diversification was seeded by migration across a land-bridge connection from India duringa Molecular dating period of climatic cooling and drying, the Oi-1 glacial maximum around the Eocene-Oligocene boundary. Lineage- Speciation through-time plots suggest a gradual and constant rate of diversification, beginning in the Oligocene and extending through the late Miocene and early Pliocene with a slight burst in the Pleistocene.
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