首页> 外文期刊>Proceedings of the National Academy of Sciences of the United States of America >On the evolutionary history of Ephedra: Cretaceous fossils and extant molecules.
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On the evolutionary history of Ephedra: Cretaceous fossils and extant molecules.

机译:关于麻黄的进化史:白垩纪化石和现存分子。

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Gnetales comprise three unusual genera of seed plants, Ephedra, Gnetum, and Welwitschia. Their extraordinary morphological diversity suggests that they are survivors of an ancient, more diverse group. Gnetalean antiquity is also supported by fossil data. Dispersed "ephedroid" (polyplicate) pollen first appeared in the Permian >250 million years ago (Myr), and a few megafossils document the presence of gnetalean features in the early Cretaceous. The Cretaceous welwitschioid seedling Cratonia cotyledon dates the split between Gnetum and Welwitschia to before 110 Myr. Ages and character evolution of modern diversity are, however, controversial, and, based on molecular data, it has recently been suggested that Ephedra is very young, only 8-32 Myr. Here, we present data on the evolutionary history of Ephedra. Fossil seeds from Buarcos, Portugal, unequivocally link one type of Cretaceous polyplicate pollen to Ephedra and document that plants with unique characters, including the peculiar naked male gametophyte, were established already in the Early Cretaceous. Clades in our molecular phylogeny of extant species correspond to geographical regions, with African species in a basal grade/clade. The study demonstrates extremely low divergence in both molecular and morphological characters in Ephedra. Features observed in the fossils are present in all major extant clades, showing that modern species have retained unique reproductive characters for >110 million years. A recent origin of modern species of Ephedra would imply that the Cretaceous Ephedra fossils discussed here were members of widespread, now extinct sister lineage(s), and that no morphological innovations characterized the second diversification.
机译:netales由三个不寻常的种子植物属组成:麻黄,netnet和千岁兰。它们非凡的形态多样性表明它们是古老的,更加多样化的群体的幸存者。化石数据也支持Gnetalean古代。分散的“麻黄”(花粉)花粉首先出现在2.5亿年前(二叠纪)的二叠纪中,一些大型化石记录了早白垩纪存在的gnetalean特征。白垩纪螺线虫幼苗子叶肉质子叶(Cratonia cotyledon)的年代约在Gnetum和千岁兰之间,达到110 Myr。然而,现代多样性的年龄和性格演变一直存在争议,并且根据分子数据,最近有人提出麻黄非常年轻,只有8-32 Myr。在这里,我们介绍有关麻黄演化史的数据。来自葡萄牙Buarcos的化石种子明确地将一种类型的白垩纪一倍体花粉与麻黄联系起来,并证明在白垩纪早期已经建立了具有独特性状的植物,包括奇特的裸雄配子体。我们现存物种分子系统发育中的进化枝对应于地理区域,而非洲物种则处于基础等级/进化枝。该研究表明麻黄的分子和形态特征差异极低。在化石中观察到的特征存在于所有主要现存进化枝中,表明现代物种在超过1.1亿年的时间里都保留了独特的生殖特征。现代麻黄物种的最新起源表明,此处讨论的白垩纪麻黄化石是广泛存在的,现已灭绝的姊妹谱系的成员,并且第二形态的多样化没有形态学创新的特征。

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