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结合历史生物地理学与生态位模型分析忍冬属六道木组(忍冬科,川续断目)的系统发育。

Combining historical biogeography with niche modeling in the Caprifolium clade of Lonicera (Caprifoliaceae, Dipsacales).

机构信息

Department of Ecology and Evolutionary Biology, Yale University, New Haven, CT 06520, USA.

出版信息

Syst Biol. 2010 May;59(3):322-41. doi: 10.1093/sysbio/syq011. Epub 2010 Mar 22.

Abstract

The Lonicera clade Caprifolium contains approximately 25 species distributed around the Northern Hemisphere, including in the Mediterranean climates of California and Europe. We sequenced the second intron of LFY to help resolve relationships within the clade where the internal transcribed spacer and chloroplast markers had previously failed to do so. Divergence time estimation and biogeographic analyses over the posterior distribution of dated trees suggest that a widespread ancestor was distributed across the Northern Hemisphere some 7-17 million years ago. Asian species form a sister group to a clade in which the European species are sister to the North American species. We use climatic niche modeling and divergence time estimates to explore the evolution of climate variables in the group. Principal component analyses help to identify instances of convergence, especially between distantly related species in the Mediterranean basin and in the chaparral of California. We document several cases of significant divergence between sister species in eastern North America and western North America. Climatic models were projected from one continent into the others (e.g., North American species projected into Asia and Europe) to examine whether species living in these areas occupy similar climates. This study demonstrates the utility of combining niche modeling with historical biogeographic analyses and documents significant climatic niche evolution within a group of species distributed throughout the Northern Hemisphere. These results suggest a possible model for the origin of the Madrean-Tethyan disjunction pattern.

摘要

忍冬族 Caprifolium 包含约 25 种,分布于北半球,包括加利福尼亚和欧洲的地中海气候区。我们对 LFY 的第二内含子进行了测序,以帮助解决该类群内部的关系,此前内部转录间隔区和叶绿体标记未能解决这些关系。通过对已确定日期的树木后分布进行分歧时间估计和生物地理分析表明,大约 700 万至 1700 万年前,一个广泛分布的祖先分布在北半球。亚洲物种与一个类群形成姐妹群,其中欧洲物种与北美的物种是姐妹群。我们使用气候生态位模型和分歧时间估计来探索该组中气候变量的演化。主成分分析有助于识别趋同现象,尤其是在地中海盆地和加利福尼亚的灌木草丛中,亲缘关系较远的物种之间存在趋同现象。我们记录了北美东部和西部的姐妹种之间发生的几个显著分歧的情况。从一个大陆到另一个大陆(例如,将北美物种投影到亚洲和欧洲)来预测气候模型,以检查生活在这些地区的物种是否占据相似的气候。本研究证明了将生态位模型与历史生物地理分析相结合的实用性,并记录了分布在北半球的一组物种中显著的气候生态位演化。这些结果表明了可能的 Madrean-Tethyan 不连续模式起源模型。

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