有孔虫目robertinida的早期演化与新分类

Pub Date : 2015-01-01 DOI:10.2113/GSJFR.45.1.3
S. Rigaud, R. Martini, D. Vachard
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引用次数: 21

摘要

在Panthalassan区域(Wallowa terrane, usa)发现的三叠纪缺失链证实了内部简单的三叠纪多室文石有孔虫与内部划分的侏罗纪Robertinida之间的直接谱系。因此,我们提出了Robertinida目的一个新的等级细分,并对其进行了修正,以涵盖所有已知的后古生代文石多室有孔虫。在最高的分类水平上,Robertinina亚目与Duostominina亚目区分开来,该亚目包括了没有内部结构附在孔上的形式,包括浮游植物fausellidae和有争议的Pragsoconu-lus。介绍了2个新科(Robertonellidae, Trochosiphoniidae), 4个新亚科(Cassianopapillariinae, praereinholdellinae, Pragsoconulinae, trochosiphoniae), 4个新属(Falsorheinoldella, Praerheinoldella, Robertonella, Trochosiphonia), 7个新种(Falsorheinol-della ohmi, F. oregonica, galei Praerheinoldella, Robertonella rettorii, R. wallowensis, stanletrochosiphonia和T. josephi)。澄清了三叠纪robertinids与其他有孔虫类群之间的系统发育联系,并讨论了它们与其他有孔虫类群的长期关系。
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EARLY EVOLUTION AND NEW CLASSIFICATION OF THE ORDER ROBERTINIDA (FORAMINIFERA)
The discovery of Triassic missing links in the Panthalassan domain (Wallowa terrane, U.S.A.) substantiates a direct lineage between internally simple Triassic multichambered aragonitic foraminifers and internally partitioned Jurassic Robertinida. A new hierarchical subdivision is accordingly proposed for the order Robertinida, which is emended to encompass all known post-Paleozoic aragonitic multicham-bered foraminifers. At the highest taxonomic level, the suborder Robertinina is distinguished from the suborder Duostominina emended to encompass forms without internal structures attached to the aperture, including the planktonic family Favusellidae and the controversial form Pragsoconu-lus. Two new families (Robertonellidae, Trochosiphoniidae), four new subfamilies (Cassianopapillariinae, Praereinholdel-linae, Pragsoconulinae, and Trochosiphoniinae), four new genera (Falsorheinoldella, Praerheinoldella, Robertonella, and Trochosiphonia), and seven new species (Falsorheinol-della ohmi, F. oregonica, Praerheinoldella galei, Robertonella rettorii, R. wallowensis, Trochosiphonia stanleyi, and T. josephi) are introduced. Phylogenetic links between Triassic robertinids, which experienced a rapid diversification during the Triassic, are clarified and their hypothetical long-term relationships with other foraminiferal groups are discussed.
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