Synchronous intercontinental splits between assemblages of woodpeckers suggested by molecular data

被引:43
作者
Fuchs, Jerome
Ohlson, Jan I.
Ericson, Per G. P.
Pasquet, Eric
机构
[1] Museum Nat Hist Naturelle, Dept Systemat & Evolut, UMR 5202, F-75005 Paris, France
[2] Museum Natl Hist Nat, CNRS, IFR 101, Serv Commun Systemat Mol, F-75005 Paris, France
[3] Swedish Museum Nat Hist, Dept Vertebrate Zool & Mol Systemat Lab, SE-10405 Stockholm, Sweden
[4] Stockholm Univ, Dept Zool, SE-10691 Stockholm, Sweden
[5] Swedish Museum Nat Hist, Dept Verebrate Zool & Mol Systemat Lab, SE-10405 Stockholm, Sweden
[6] Museum Natl Hist Nat, Dept Sytemat & Evolut, UMR 5202, F-75005 Paris, France
[7] Museum Natl Hist, CNRS, IFR 101, Serv Commun Systemat Mol, F-75005 Paris, France
关键词
D O I
10.1111/j.1463-6409.2006.00267.x
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
The woodpeckers (Piciformes: Picinae) comprise a widely distributed and species-rich clade of birds that is strongly associated with trees for feeding, nesting, or both. Because of this association, woodpeckers provide a useful model for evaluating the impact of climatic and tectonic events on the diversification of forest birds during the Tertiary. In order to resolve the biogeographical history of the woodpeckers, we have analysed sequences from two nuclear introns and one mitochondrial gene using likelihood and Bayesian approaches. Our analyses favour a tropical Eurasian origin; divergences between African, Indo-Malayan and New World clades with subsequent colonizations of Africa and the New World occurred synchronously during the Middle Miocene, a period corresponding to the expansion of the C4 grasses and the uplift of the Himalayan-Tibetan plateau. The taxonomic diversification of woodpeckers at this time may be attributed to the fragmentation of forests in response to the drier climate, which in turn prevented gene flow between tropical stocks in Africa, Indo-Malaya and the New World. Our estimates of colonization times of South America predate the closure of the Panama Isthmus and support the hypothesis of a short-lived, terrestrial corridor at the end of the Miocene, 5.7 Myr BP.
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页码:11 / 25
页数:15
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