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下白垩统(阿普第阶,阿拉里皮盆地)克鲁托化石库中的一个被子植物叶片。

A eudicot leaf from the Lower Cretaceous (Aptian, Araripe Basin) Crato Konservat-Lagerstätte.

机构信息

Laboratório de Estudos Integrados de Plantas, Departamento de Botânica e Ecologia, Universidade Federal de Mato Grosso, Cuiabá, Mato Grosso, Brazil.

Departamento de Biologia e Zoologia, Universidade Federal de Mato Grosso, Cuiabá, Mato Grosso, Brazil.

出版信息

Am J Bot. 2021 Oct;108(10):2055-2065. doi: 10.1002/ajb2.1751. Epub 2021 Oct 13.

Abstract

PREMISE

The Crato Konservat-Lagerstätte in Brazil preserves an exceptionally rich assemblage of plant macrofossils from the Early Cretaceous (late Aptian), including rare early angiosperm fossils related to Nymphaeales, monocots, and magnoliids, and a variety of angiosperms of uncertain affinities. Macrofossils of eudicot angiosperms have not been described previously, despite the presence of tricolpate pollen. We describe a fossil leaf with morphology characteristic of eudicot angiosperms.

METHODS

The fossil was collected from a quarry in the Lower Cretaceous (late Aptian) Crato Formation of northeastern Brazil in the state of Ceará. We compared the leaf architecture with that of ferns, gymnosperms, and similar living and fossil angiosperms.

RESULTS

The leaf of Baderadea pinnatissecta gen. et sp. nov. is simple and petiolate, with leaf architecture similar to that of some herbaceous Ranunculales. The blade is 5 cm long and the margin is untoothed and twice pinnately lobed with narrow lobes (pinnatisect). The primary vein framework is pinnate and there are multiple orders of reticulate venation.

CONCLUSIONS

The combination of characters preserved in the fossil supports the interpretation that B. pinnatissecta was an herbaceous eudicot similar to some members of Ranunculales and distinguished from other lobate Aptian angiosperms by leaf shape, presence of multiple orders of reticulate venation, and the absence of glandular teeth. The presence of eudicots in the flora of the Crato was already supported by pollen; the discovery of macrofossils like these provides additional information about their morphology and ecological role in low-latitude Early Cretaceous plant communities.

摘要

前提

巴西的 Crato 保守层状矿床保存了一组特别丰富的早白垩世(晚阿普第期)植物大化石,包括与睡莲目、单子叶植物和木兰类相关的珍稀早期被子植物化石,以及各种亲缘关系不确定的被子植物。尽管存在三沟花粉,但之前并未描述过真双子叶植物的大化石。我们描述了一个具有真双子叶植物特征的化石叶。

方法

该化石是从巴西东北部塞阿拉州下白垩统(晚阿普第期) Crato 组的一个采石场中采集的。我们将叶片结构与蕨类植物、裸子植物和类似的现存及化石被子植物进行了比较。

结果

Baderadea pinnatissecta gen. et sp. nov. 的叶片是简单的、具叶柄的,叶片结构与一些草本毛茛目植物相似。叶片长 5 厘米,边缘无齿,两次羽状深裂,裂片狭窄(羽状深裂)。主脉框架是羽状的,有多级网状脉序。

结论

化石中保存的特征组合支持以下解释,即 B. pinnatissecta 是一种草本真双子叶植物,类似于毛茛目中的一些成员,与其他具裂片的早白垩世被子植物不同的是叶片形状、有多级网状脉序和无腺齿。被子植物在 Crato 植物群中的存在已经得到花粉的支持;这些大化石的发现为它们在低纬度早白垩世植物群落中的形态和生态角色提供了更多信息。

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