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Comprehensive species set revealing the phylogeny and biogeography of Feliformia (Mammalia, Carnivora) based on mitochondrial DNA

机译:全面的物种集合揭示了基于线粒体DNA的费氏蝇科(哺乳动物,食肉目)的系统发育和生物地理

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摘要

Extant Feliformia species are one of the most diverse radiations of Carnivora (~123 species). Despite substantial recent interest in their conservation, diversification, and systematic study, no previous phylogeny contains a comprehensive species set, and no biogeography of this group is available. Here, we present a phylogenetic estimate for Feliformia with a comprehensive species set and establish a historical biogeography based on mitochondrial DNA. Both the Bayesian and maximum likelihood phylogeny for Feliformia are elucidated in our analyses and are strongly consistent with many groups recognized in previous studies. The mitochondrial phylogenetic relationships of Felidae were for the first time successfully reconstructed in our analyses with strong supported. When divergence times and dispersal/vicariance histories were compared with historical sea level changes, four dispersal and six vicariance events were identified. These vicariance events were closely related with global sea level changes. The transgression of sea into the lowland plains between Eurasia and Africa may have caused the vicariance in these regions. A fall in the sea level during late Miocene to Pliocene produced the Bering strait land bridge, which assisted the migration of American Feliformia ancestors from Asia to North America. In contrast with the ‘sweepstakes hypothesis’, our results suggest that the climate cooling during 30–27 Ma assisted Feliformia migration from the African mainland to Madagascar by creating a short-lived ice bridge across the Mozambique Channel. Lineages-through-time plots revealed a large increase in lineages since the Mid-Miocene. During the Mid-Miocene Climatic Optimum, the ecosystems and population of Feliformia rapidly expanded. Subsequent climate cooling catalyzed immigration, speciation, and the extinction of Feliformia.
机译:现存的费利福氏菌属是食肉动物种类最多的辐射之一(约123种)。尽管最近对其保护,多样化和系统研究产生了浓厚兴趣,但以前的系统发育都没有包含完整的物种集,并且该群体的生物地理信息不可用。在这里,我们提出了一个综合物种集的费氏族的系统发育估计,并建立了基于线粒体DNA的历史生物地理学。在我们的分析中阐明了贝叶斯族的贝叶斯和最大似然系统发育,并且与先前研究中公认的许多研究组高度一致。在我们的分析中,费利迪氏菌的线粒体系统发生关系首次得到了成功的支持。将发散时间和扩散/迁移历史与历史海平面变化进行比较时,确定了四个扩散事件和六个迁移事件。这些疏离事件与全球海平面变化密切相关。海进入欧亚大陆和非洲之间的低地平原可能引起了这些地区的破坏。在中新世晚期至上新世期间海平面下降,产生了白令海峡陆桥,该桥帮助了美国费氏族祖先从亚洲迁移到北美。与“抽奖假说”相反,我们的结果表明,在30-27 Ma期间的气候降温通过在莫桑比克海峡建立了一条短暂的冰桥,协助费利福族从非洲大陆迁移到马达加斯加。自中新世以来,沿袭世系的情节显示出世系的大量增加。在中新世中期气候最佳时期,费里福族的生态系统和种群迅速扩大。随后的气候降温促进了移民,物种形成和费力福族的灭绝。

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