Please use this identifier to cite or link to this item: https://repositorio.inpa.gov.br/handle/1/16041
Title: Combining phylogeography and landscape genetics of Xenopipo atronitens (Aves: Pipridae), a white sand campina specialist, to understand Pleistocene landscape evolution in Amazonia
Authors: Capurucho, João Marcos Guimarães
Cornelius, Cintia
Borges, Sérgio Henrique
Cohn-Haft, Mario
Aleixo, Alexandre
Metzger, Jean Paul
Ribas, Camila Cherem
Keywords: Avifauna
Demography
Gene Flow
Genetic Structure
Landscape Ecology
Landscape Evolution
Miocene
Dna, Mitochondrial
Paleoclimate
Paleoecology
Passerine
Patchiness
Phylogeography
Pleistocene
Sand
Specialist
Vegetation Cover
Amazon Basin
Amazonia
Aves
Pipridae
Xenopipo
Xenopipo Atronitens
Issue Date: 2013
metadata.dc.publisher.journal: Biological Journal of the Linnean Society
metadata.dc.relation.ispartof: Volume 110, Número 1, Pags. 60-76
Abstract: Open vegetation (campinas and campinaranas) associated with white sand patches occurs in the form of islands in a forested matrix throughout the Amazon basin. Bird species restricted to these habitats have patchy distributions, although connectivity may have been influenced by past glacial cycles as a result of the substitution of forest by savanna. Because these landscape changes are a matter of debate in the history of Amazonia, we studied the diversification of Xenopipo atronitens, a white sand specialist, aiming to infer the effects of past climate changes. The split of Xenopipo atronitens from its sister species, Xenopipo uniformis, may be related to Tepuis erosion and retreat of escarpments during the Miocene, or to a dispersal event. Compared with birds from terra firme forest, X.atronitens has low genetic structure. Low levels of unidirectional gene flow were found from the Guyana Shield to adjacent areas. Demographic expansion starting approximately 25 kyr BP was detected for some populations and is probably related to the Last Glacial Maximum and subsequent climate improvement. Landscape genetic analyses indicate that the forested (terra firme) matrix acts as a barrier for the dispersal of X.atronitens. The results of the present study indicate that glacial cycles have deeply influenced Amazonian biogeographical history, demonstrating a complex interaction between forest and nonforest habitats during the Pleistocene. © 2013 The Linnean Society of London.
metadata.dc.identifier.doi: 10.1111/bij.12102
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