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Major lineages of Loasaceae subfam. Loasoideae diversified during the Andean uplift

机译:Loasaceae Subfam的主要谱系。 在Andean隆起期间的Loasoideae多样化

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The Loasoideae is the largest Glade in the Loasaceae. This subfamily is widespread throughout the Neotropics and centered in the Andes, presenting an excellent opportunity to study diversification across much of temperate and mid to high-elevation areas of South America. Despite that, no studies have addressed the historical biogeography of the Loasoideae to date, leaving an important knowledge gap in this plant group. Here, we used four plastid markers (i.e., trnL-trnF, matK, trnS-trnG, and rps16) and sequenced 170 accessions (134 ingroup taxa) to infer the phylogeny of Loasoideae. We then used this phylogeny as basis to estimate divergence times using an uncorrelated relaxed molecular clock approach and seven fossils as primary calibration points. We employed the Dispersal-Extinction-Cladogenesis (DEC) approach to reconstruct the ancestral ranges of the subfamily. Our results indicate that stem Loasoideae diverged from its sister group in the Late Cretaceous to Early Paleocene (ca. 83-62 Ma). The crown node of the whole Glade goes back to the Middle Paleocene to Middle Eocene (ca. 60-45 Ma), corresponding to the earliest diversification events of the extant groups, prior to most of the Andean orogeny and roughly coinciding with the Paleocene-Eocene Thermal Maximum. On the other hand, the crown nodes of most genera appear to have originated in the Oligocene and Miocene (median ages: 28-10 Ma). The diversification of some extant lineages appears to have happened in parallel to Andean uplift pulses that seem to have had an effect on the orogeny and concomitant establishment of new habitats and latitudinal corridors. The most likely ancestral areas retrieved for crown Loasoideae, are the tropical Andes and Pacific arid coast. Most of the extant clades have remained restricted to their ancestral areas. Transoceanic Long Distance Dispersal appears to have been involved in the arrival of Loasoid ancestors to South America, and in the distribution of the small clades Kissenia in Africa and Plakothira on the Marquesas Archipelago. The results presented here suggest that the historical biogeography of the continental scale radiation of Loasoideae, follows the sequence and timing of the development of temperate and mid to high-elevation habitats across South America during the Tertiary.
机译:Loasoideae是Loasaceae中最大的林地。这个亚家族在整个新生中都是广泛的,并在安第斯山脉中,为南美洲大部分温带和中高海拔地区学习多样化的绝佳机会。尽管如此,迄今为止,没有任何研究涉及洛克宽西的历史生物地理,留下了这一植物集团的重要知识差距。这里,我们使用了四种塑性标记物(即,TrnL-TrnF,MATK,TRNS-TRNG和RPS16)并测序170种附加(134个INGROUP分类群)以推断出贫瘠的系统发育。然后,我们使用这种系统发育作为使用不相关的松弛分子钟方法和七个化石作为主要校准点来估计发散时间的基础。我们雇用了分散 - 消灭 - 封闭性(DEC)方法来重建亚家族的祖先范围。我们的结果表明,茎乏味薄膜从其姐妹群中分散到后期白垩纪的早期古产(约83-62 mA)。整个沼泽的皇冠节点返回中间古世茂(CA. 60-45 mA),对应于当地的最早群体的最早多样化事件,在大多数Andean Orogeny和大致与古茂无古典中何时热最大。另一方面,大多数属的表冠节点似乎已经源于寡核苷和中生(中位数:28-10mA)。一些现存谱系的多样化似乎与Andean隆起脉冲平行发生,似乎对orgeny和伴随的新栖息地和纬度走廊产生了影响。为皇冠覆盖薄膜检索的最有可能的祖宗地区是热带安第斯山岩和太平洋干旱的海岸。大多数现存的林门仍然限于他们的祖先地区。 Transoceanic Long Rocest Dispersal似乎已经参与了南美洲的装饰祖先的到来,以及在侯爵夫群岛的非洲和Plakothia的小蛹碱基分布。此处提出的结果表明,覆盖的大陆规模辐射的历史生物地理学遵循南美洲在南美洲的温带和中高高栖息地的序列和时间。

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