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Comparative Phylogeography of Ethiopian anurans: impact of the Great Rift Valley and Pleistocene climate change

BACKGROUND: The Ethiopian highlands are a biodiversity hotspot, split by the Great Rift Valley into two distinct systems of plateaus and mountains. The Rift Valley is currently hot and dry and acts as a barrier to gene flow for highland-adapted species. It is however unlikely that the conditions in...

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Autores principales: Freilich, Xenia, Anadón, José D., Bukala, Jolanta, Calderon, Ordaliza, Chakraborty, Ronveer, Boissinot, Stéphane
Formato: Online Artículo Texto
Lenguaje:English
Publicado: BioMed Central 2016
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5057412/
https://www.ncbi.nlm.nih.gov/pubmed/27724843
http://dx.doi.org/10.1186/s12862-016-0774-1
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author Freilich, Xenia
Anadón, José D.
Bukala, Jolanta
Calderon, Ordaliza
Chakraborty, Ronveer
Boissinot, Stéphane
author_facet Freilich, Xenia
Anadón, José D.
Bukala, Jolanta
Calderon, Ordaliza
Chakraborty, Ronveer
Boissinot, Stéphane
author_sort Freilich, Xenia
collection PubMed
description BACKGROUND: The Ethiopian highlands are a biodiversity hotspot, split by the Great Rift Valley into two distinct systems of plateaus and mountains. The Rift Valley is currently hot and dry and acts as a barrier to gene flow for highland-adapted species. It is however unlikely that the conditions in the Rift were inhospitable to highland species during the entire Pleistocene. To assess the significance of the Ethiopian Rift as a biogeographic barrier as well as the impact Pleistocene climatic changes have had on the evolution of Ethiopian organisms, we performed phylogeographic analyses and developed present and past niche models on seven anuran species with different elevational and ecological preferences. RESULTS: We found that highland species on the east and the west sides of the Rift are genetically differentiated and have not experienced any detectable gene flow for at least 0.4 my. In contrast, species found at elevations lower than 2500 m do not show any population structure. We also determined that highland species have lower effective population sizes than lowland species, which have experienced a large, yet gradual, demographic expansion, starting approximately half a million year ago. CONCLUSIONS: The pattern we report here is consistent with the increasingly warmer and drier conditions of the Pleistocene in East Africa, which resulted in the expansion of savanna, the fragmentation of forests and the shrinking of highland habitats. Climatic niche models indicated that the Rift is currently non suitable for most of the studied species, but it could have been a more permeable barrier during the Last Glacial Maximum. However, considering the strong genetic structure of highland species, we hypothesize that the barrier mechanisms at the Rift are not only climatic but also topographical. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (doi:10.1186/s12862-016-0774-1) contains supplementary material, which is available to authorized users.
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spelling pubmed-50574122016-10-20 Comparative Phylogeography of Ethiopian anurans: impact of the Great Rift Valley and Pleistocene climate change Freilich, Xenia Anadón, José D. Bukala, Jolanta Calderon, Ordaliza Chakraborty, Ronveer Boissinot, Stéphane BMC Evol Biol Research Article BACKGROUND: The Ethiopian highlands are a biodiversity hotspot, split by the Great Rift Valley into two distinct systems of plateaus and mountains. The Rift Valley is currently hot and dry and acts as a barrier to gene flow for highland-adapted species. It is however unlikely that the conditions in the Rift were inhospitable to highland species during the entire Pleistocene. To assess the significance of the Ethiopian Rift as a biogeographic barrier as well as the impact Pleistocene climatic changes have had on the evolution of Ethiopian organisms, we performed phylogeographic analyses and developed present and past niche models on seven anuran species with different elevational and ecological preferences. RESULTS: We found that highland species on the east and the west sides of the Rift are genetically differentiated and have not experienced any detectable gene flow for at least 0.4 my. In contrast, species found at elevations lower than 2500 m do not show any population structure. We also determined that highland species have lower effective population sizes than lowland species, which have experienced a large, yet gradual, demographic expansion, starting approximately half a million year ago. CONCLUSIONS: The pattern we report here is consistent with the increasingly warmer and drier conditions of the Pleistocene in East Africa, which resulted in the expansion of savanna, the fragmentation of forests and the shrinking of highland habitats. Climatic niche models indicated that the Rift is currently non suitable for most of the studied species, but it could have been a more permeable barrier during the Last Glacial Maximum. However, considering the strong genetic structure of highland species, we hypothesize that the barrier mechanisms at the Rift are not only climatic but also topographical. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (doi:10.1186/s12862-016-0774-1) contains supplementary material, which is available to authorized users. BioMed Central 2016-10-10 /pmc/articles/PMC5057412/ /pubmed/27724843 http://dx.doi.org/10.1186/s12862-016-0774-1 Text en © The Author(s). 2016 Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated.
spellingShingle Research Article
Freilich, Xenia
Anadón, José D.
Bukala, Jolanta
Calderon, Ordaliza
Chakraborty, Ronveer
Boissinot, Stéphane
Comparative Phylogeography of Ethiopian anurans: impact of the Great Rift Valley and Pleistocene climate change
title Comparative Phylogeography of Ethiopian anurans: impact of the Great Rift Valley and Pleistocene climate change
title_full Comparative Phylogeography of Ethiopian anurans: impact of the Great Rift Valley and Pleistocene climate change
title_fullStr Comparative Phylogeography of Ethiopian anurans: impact of the Great Rift Valley and Pleistocene climate change
title_full_unstemmed Comparative Phylogeography of Ethiopian anurans: impact of the Great Rift Valley and Pleistocene climate change
title_short Comparative Phylogeography of Ethiopian anurans: impact of the Great Rift Valley and Pleistocene climate change
title_sort comparative phylogeography of ethiopian anurans: impact of the great rift valley and pleistocene climate change
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5057412/
https://www.ncbi.nlm.nih.gov/pubmed/27724843
http://dx.doi.org/10.1186/s12862-016-0774-1
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