首页> 美国卫生研究院文献>Proceedings of the Royal Society B: Biological Sciences >Cratonia cotyledon gen. et sp. nov: a unique Cretaceous seedling related to Welwitschia.
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Cratonia cotyledon gen. et sp. nov: a unique Cretaceous seedling related to Welwitschia.

机译:克雷托尼亚子叶gen。等。 nov:与千岁兰有关的独特的白垩纪幼苗。

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摘要

The fossil history of most extant seed plant groups is relatively well documented. Cycads, conifers and Ginkgo all have an extensive fossil record, and the understanding of early angiosperm diversity is increasing. The Gnetales are an exception. Few macrofossils have been described, and character evolution within the group is poorly known. Cratonia cotyledon is a new gnetalean fossil from the Early Cretaceous Crato Formation of Brazil. This well-preserved seedling consists of two cotyledons, a feeder and a root. The leaf surface shows polygonal epidermal cells and apparently paracytic or actinocytic stomata. The cotyledons have a very specific venation pattern, shared only by Cratonia and Welwitschia, with parallel primary veins and secondary veins fusing to form inverted 'Y's between the main veins. Based on the 'Y'-venation and the presence of a feeder, we assign Cratonia to the Gnetum-Welwitschia clade. Fossil seedlings are unusual and this complete specimen with unambiguously welwitschioid characters is spectacular. Cratonia indicates that the evolutionary split between Gnetum and Welwitschia had occurred in the Early Cretaceous. Further, the close relationship between a West African plant and an east South American Early Cretaceous fossil is consistent with a major geological event: the rifting of the Gondwana continent.
机译:大多数现存的种子植物群的化石历史已有相当详尽的文献记载。苏铁,针叶树和银杏都拥有丰富的化石记录,并且对早期被子植物多样性的了解也在增加。 Gnetales是一个例外。很少有大型化石被描述过,并且该群体内的角色演变还鲜为人知。 Cratonia子叶是巴西白垩纪Crato早期的一种新的gnetalean化石。这个保存完好的幼苗由两个子叶,一个饲养者和一个根组成。叶表面显示出多边形表皮细胞和明显的旁吞或放线气孔。子叶具有非常特殊的脉型,只有克雷托尼亚(Cartonia)和千岁兰(Welwitschia)共同使用,平行的主脉和次脉融合形成主脉之间的倒“ Y”。基于“ Y”形通配符和馈线的存在,我们将克雷托尼亚分配给Gnetum-Welwitschia进化枝。化石的幼苗是不寻常的,这个完整的标本具有明确的螺线虫特征很壮观。 Cratonia指出,Gnetum和千岁兰之间的进化分裂发生在白垩纪早期。此外,西非植物与南美早白垩世东部化石之间的密切关系与重大地质事件一致:冈瓦纳大陆的裂谷。

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