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首页> 外文期刊>Molecular phylogenetics and evolution >Biogeographic history of Pistacia (Anacardiaceae), emphasizing the evolution of the Madrean-Tethyan and the eastern Asian-Tethyan disjunctions
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Biogeographic history of Pistacia (Anacardiaceae), emphasizing the evolution of the Madrean-Tethyan and the eastern Asian-Tethyan disjunctions

机译:黄连木(Anacardiaceae)的生物地理历史,着重强调了Madrean-Tethyan和东亚-Tethyan分离的演变

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摘要

Pistacia L. exhibits a disjunct distribution in Mediterranean Eurasia and adjacent North Africa, eastern Asia, and North to Central America. The spatio-temporal diversification history of Pistacia was assessed to test hypotheses on the Madrean-Tethyan and the Eurasian Tethyan disjunctions through phylogenetic and biogeographic analyses. Maximum parsimony and Bayesian methods were employed to analyze sequences of multiple nuclear and plastid loci of Pistacia species. Bayesian dating analysis was conducted to estimate the divergence times of clades. The likelihood method LAGRANGE was used to infer ancestral areas. The New World species of Pistacia formed a clade sister to the Old World clade in all phylogenetic analyses. The eastern Asian Pistacia weinmannifolia-P. cucphuongensis clade was sister to a clade of the remaining Old World species, which were further resolved into three subclades. Pistacia was estimated to have originated at 37.60 mya (with 95% highest posterior density interval (HPD): 25.42-48.51 mya). A vicariance event in the early Miocene (19.79 mya with 95% HPD: 10.88-30.36 mya) was inferred to account for the intercontinental disjunction between the New World and the Old World species, which is consistent with the Madrean-Tethyan hypothesis. The two Old World eastern Asian-Tethyan disjunctions are best explained by one vicariance event in the early Miocene (15.87 mya with 95% HPD: 8.36-24.36 mya) and one dispersal event in late Miocene (5.89 mya with 95% HPD: 2.68-9.16 mya). The diversification of the Old World Pistacia species was significantly affected by extensive geological and climatic changes in the Qinghai-Tibetan plateau (QTP) and in the Mediterranean region.
机译:Pistacia L.在地中海欧亚大陆及邻近的北非,东亚和北美洲至中美洲的分布不均。通过系统发育和生物地理学分析,评估了黄连木的时空多样化历史,以检验关于马德里亚-特提斯和欧亚特提斯分离的假说。采用最大简约和贝叶斯方法分析了黄连木种的多个核和质体基因座的序列。进行贝叶斯定年分析以估计进化枝的发散时间。用似然方法LAGRANGE推断祖先区域。在所有的系统发育分析中,新世界的黄连木都形成了旧世界的进化枝姐妹。东亚黄连木weinmannifolia-P。 cucphuongensis进化枝是其余旧世界物种进化枝的姐妹,这些物种进一步分解为三个亚进化枝。据估计,黄连起源于37.60 mya(后密度间隔(HPD)最高为95%:25.42-48.51 mya)。据推断,中新世早期的一次变异事件(19.79 mya,95%HPD:10.88-30.36 mya)解释了新大陆和旧大陆物种之间的洲际分离,这与马德雷-特提斯的假设是一致的。最好的解释是,在中新世早期(15.87鼠,HPD为95%:8.36-24.36 mya)发生一次离奇事件,以及在中新世晚期(95%的HPD:5.89 mya:2.68-m)发生一次离奇事件,可以最好地解释这两个旧世界东亚-特提斯断层。 9.16 mya)。在青藏高原(QTP)和地中海地区,广泛的地质和气候变化极大地影响了旧世界黄连木种类的多样性。

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