BMC Evolutionary Biology
Volume 11, Issue 1, 2011
Palaeoclimatic events, dispersal and migratory losses along the Afro-European axis as drivers of biogeographic distribution in Sylvia warblers (Article) (Open Access)
Voelker G.* ,
Light J.E.
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a
Department of Wildlife and Fisheries Sciences and Texas Cooperative Wildlife Collections, Texas AandM University, College Station, TX 77843, United States
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b
Department of Wildlife and Fisheries Sciences and Texas Cooperative Wildlife Collections, Texas AandM University, College Station, TX 77843, United States
Abstract
Background: The Old World warbler genus Sylvia has been used extensively as a model system in a variety of ecological, genetic, and morphological studies. The genus is comprised of about 25 species, and 70% of these species have distributions at or near the Mediterranean Sea. This distribution pattern suggests a possible role for the Messinian Salinity Crisis (from 5.96-5.33 Ma) as a driving force in lineage diversification. Other species distributions suggest that Late Miocene to Pliocene Afro-tropical forest dynamics have also been important in the evolution of Sylvia lineages. Using a molecular phylogenetic hypothesis and other methods, we seek to develop a biogeographic hypothesis for Sylvia and to explicitly assess the roles of these climate-driven events. Results: We present the first strongly supported molecular phylogeny for Sylvia. With one exception, species fall into one of three strongly supported clades: one small clade of species distributed mainly in Africa and Europe, one large clade of species distributed mainly in Africa and Asia, and another large clade with primarily a circum-Mediterranean distribution. Asia is reconstructed as the ancestral area for Sylvia. Long-distance migration is reconstructed as the ancestral character state for the genus, and sedentary behavior subsequently evolved seven times. Conclusion: Molecular clock calibration suggests that Sylvia arose in the early Miocene and diverged into three main clades by 12.6 Ma. Divergence estimates indicate that the Messinian Salinity Crisis had a minor impact on Sylvia. Instead, over-water dispersals, repeated loss of long-distance migration, and palaeo-climatic events in Africa played primary roles in Sylvia divergence and distribution. © 2011 Voelker and Light; licensee BioMed Central Ltd.
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Link
https://www.scopus.com/inward/record.uri?eid=2-s2.0-79958265462&doi=10.1186%2f1471-2148-11-163&partnerID=40&md5=d09f378ce51ddb083a1c4e27ba59c10e
DOI: 10.1186/1471-2148-11-163
ISSN: 14712148
Cited by: 23
Original Language: English