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古阿尔廷蕨属(Paleoaltingia gen. nov.),来自新泽西晚白垩世的阿尔廷蕨科的一个新属。

Paleoaltingia gen. nov., a new genus of Altingiaceae from the Late Cretaceous of New Jersey.

机构信息

State Key Laboratory of Systematic and Evolutionary Botany, Institute of Botany, Chinese Academy of Sciences, Beijing, 100093, China.

L. H. Bailey Hortorium, Plant Biology Section, School of Integrative Plant Science, Cornell University, Ithaca, NY, 14853, USA.

出版信息

Am J Bot. 2021 Mar;108(3):461-471. doi: 10.1002/ajb2.1618. Epub 2021 Mar 3.

Abstract

PREMISE

Altingiaceae is a small family with a bimodal Northern Hemisphere distribution in eastern North America and eastern Asia, and a rich Cenozoic fossil record. The charcoalified fossil infructescence Paleoaltingia gen. nov. from Turonian (Late Cretaceous) deposits of New Jersey, provides new evidence of early Altingiaceae reproductive structures and has biogeographical implications in understanding modern distribution.

METHODS

Fossils were prepared using standard methods for obtaining and processing mesofossils. The fossils were examined with light microscopy, and scanning electron microscopy for observing structural and anatomical details. Phylogenetic analyses were performed using a combined matrix of molecular and morphological data.

RESULTS

Based on morphological features of the fossil and the phylogenetic analyses, the new genus, Paleoaltingia, with two species (Paleoaltingia ovum-dinosauri and P. polyodonta) is erected. The phylogenetic position of Paleoaltingia confirms affinities with living Altingiaceae.

CONCLUSIONS

The combination of characters-simple capitate infructescence, syncarpous bicarpellate, and bilocular ovary, unique sterile phyllome structures-indicates that the fossil taxa have close affinities to modern Altingiaceae. The unique characters of the phyllomes provide new information on the floral diversity of Altingiaceae. The emergence of Paleoaltingia in Late Cretaceous sediments of Northeastern North America represents the earliest fossil record of Altingiaceae and provides new insights into its biogeography.

摘要

前提

Altingiaceae 是一个小科,具有在北温带分布的双峰模式,分布于北美洲东部和东亚,并且具有丰富的新生代化石记录。来自新泽西州白垩纪(晚白垩世)Turonian 沉积物的碳化化石果实 Paleoaltingia gen. nov. 为早期 Altingiaceae 生殖结构提供了新证据,并在理解现代分布方面具有生物地理学意义。

方法

使用获得和处理中型化石的标准方法来准备化石。使用光学显微镜和扫描电子显微镜检查化石,以观察结构和解剖细节。使用分子和形态数据的组合矩阵进行系统发育分析。

结果

基于化石的形态特征和系统发育分析,建立了新属 Paleoaltingia,有两个种(Paleoaltingia ovum-dinosauri 和 P. polyodonta)。Paleoaltingia 的系统发育位置证实了与现生 Altingiaceae 的亲缘关系。

结论

综合特征-简单的头状果实、合生的二心皮、二室子房、独特的不育叶状体结构-表明化石类群与现代 Altingiaceae 具有密切的亲缘关系。叶状体的独特特征为 Altingiaceae 的花多样性提供了新信息。Paleoaltingia 在北美洲东北部晚白垩世沉积物中的出现代表了 Altingiaceae 的最早化石记录,并为其生物地理学提供了新的见解。

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