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来自新泽西晚白垩世沉积物的归入里白科的新化石蕨类植物。

A new fossil fern assignable to Gleicheniaceae from Late Cretaceous sediments of New Jersey.

出版信息

Am J Bot. 1997 Apr;84(4):483.

Abstract

The recent discovery of well-preserved charcoalified rhizomes, petioles. pinnules, sori, and spores from the Upper Cretaceous of New Jersey provides the basis for the description of a new gleicheniaceous fern, Boodlepteris turoniana. The fossils were collected from unconsolidated sediments of Turonian age (~90 MYBP million years before present; Raritan/ Lower Magothy Formation, Potomac Group). These deposits are rich in angiosperms, but also have a limited representation of fern and gymnosperm remains. Fossil specimens from this locality are particularly remarkable in that minute detail, including anatomical features, are often preserved. Some Boodlepteris specimens have cell by cell preservation that reveals the nature and structure of the stele in rhizomes and petioles, and others show minute details of the sori borne on fertile pinnae. Although these specimens are not in organic connection, there are sufficient structural and anatomical details preserved to confidently suggest that they belong to the same taxon. Cladistic analysis of the fossils, both separately and as a reconstruction, support assignment of Boodlepteris to the extant family Gleicheniaceae.

摘要

新泽西上白垩统保存完好的炭化根茎、叶柄、小羽片、孢子囊群和孢子的最近发现为描述一种新的水龙骨目蕨类植物——Boodlepteris turoniana 提供了基础。这些化石是从 Turonian 时代(约 9000 万年前;Raritan/Lower Magothy 组,Potomac 群)的未固结沉积物中采集的。这些沉积物富含被子植物,但也有少量蕨类植物和裸子植物的遗骸。该地点的化石标本非常引人注目,因为通常可以保存微小的细节,包括解剖特征。一些 Boodlepteris 标本具有细胞级的保存,揭示了根茎和叶柄中中柱的性质和结构,而其他标本则显示了生有孢子囊的可育羽片上的微小细节。尽管这些标本没有有机联系,但保存的结构和解剖细节足以让人有信心地认为它们属于同一分类群。对化石的分支分析,无论是单独分析还是重建分析,都支持将 Boodlepteris 归入现存的水龙骨科。

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