北温带木本植物区系的多样性——以榆树科(榆科)为例——基于系统基因组学和古植物学证据

IF 3.7
Qiuyue Zhang, M. Deng, Y. Bouchenak‐Khelladi, Zhekun Zhou, G. Hu, Yaowu Xing
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引用次数: 11

摘要

榆科是广泛分布于北温带森林的木本科。尽管这个科的生态重要性,它的系统发育和生物地理历史知之甚少。在这项研究中,我们重建了家族内的系统发育关系,并基于叶绿体基因组(完整cpDNA)和核糖体DNA序列(nrDNA)推断了时空多样化模式。通过cpDNA和nrDNA序列可将榆科的7个属划分为温带和热带两个主要分支。温带分支包括四个属,半属,Zelkova属,Planera属和Ulmus属。Planera和其他属之间的关系是有争议的,因为质体和核数据之间的拓扑结构不一致。热带进化支包括三个属((葡萄属,Phyllostylon), Holoptelea)。分子定年和多样性分析表明,榆科起源于早白垩世(约110-125 Ma),主要谱系建立于晚白垩世至始新世早期。在古近纪中晚期(约23-45 Ma),东亚温带组的多样化速度减慢,而在新近纪,东亚温带组迅速多样化,与全球变冷事件一致。祖先状态优化分析表明,温带Ulmaceae分支在古新世起源于东亚,这与化石记录一致。系统基因组学和化石证据都支持东亚是温带木本谱系的起源和多样化中心。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The diversification of the northern temperate woody flora – A case study of the Elm family (Ulmaceae) based on phylogenomic and paleobotanical evidence
Ulmaceae is a woody family widespread in northern temperate forests. Despite the ecological importance of this family, its phylogeny and biogeographic history are poorly understood. In this study, we reconstruct phylogenetic relationships within the family and infer spatio‐temporal diversification patterns based on chloroplast genome (complete cpDNA) and nuclear ribosomal DNA sequences (nrDNA). The seven Ulmaceae genera are resolved in two main clades (temperate vs. tropical) by both cpDNA and nrDNA sequences. The temperate clade includes four genera, Hemiptelea, Zelkova, Planera, and Ulmus. The relationships among Planera and other genera are controversial because of inconsistent topologies between plastid and nuclear data. The tropical clade includes three genera ((Ampelocera, Phyllostylon), Holoptelea). Molecular dating and diversification analyses show that Ulmaceae originated in the Early Cretaceous (ca. 110–125 Ma) with the main lineages establishing from the Late Cretaceous to the early Eocene. The diversification rate slowed during the middle to the late Paleogene (ca. 23–45 Ma), followed by a rapid diversification of the East Asian temperate group in the Neogene, congruent with a global cooling event. The ancestral state optimization analysis suggests an East Asian origin of the temperate Ulmaceae clade during the Paleocene, which is consistent with the fossil record. Both phylogenomic and fossil evidence support East Asia as a center of origin and diversification for the temperate woody lineages.
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