来自阿根廷巴塔哥尼亚内乌肯省 Bajo de la Carpa Formation(内乌肯组,上白垩世)的 Diuqin lechiguanae gen.

IF 2.3 Q2 ECOLOGY BMC ecology and evolution Pub Date : 2024-06-14 DOI:10.1186/s12862-024-02247-w
Juan D Porfiri, Mattia A Baiano, Domenica D Dos Santos, Federico A Gianechini, Michael Pittman, Matthew C Lamanna
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引用次数: 0

摘要

背景:单翼副龙是与了解鸟类起源最相关的冈瓦纳兽脚类恐龙支系之一,然而它们的化石记录仍然不完整,大多数类群的化石都是零散的材料和/或被漫长的时间间隙隔开,这使得描述单翼副龙演化特征的尝试受挫:在这里,我们描述了 Diuqin lechiguanae gen.虽然仅从一具非常不完整的颅后骨骼中得知,但保存下来的 "刁琴 "骨骼与其他unenlagiines的相应部分有所不同,因此有理由建立这个新的类群。此外,在形态学的几个方面,刁琴的肱骨似乎介于内乌肯盆地地质年代较早的麒麟类(如都伦-科尼阿克安世波特苏埃洛地层中的麒麟属)和地层较年轻、体型较大的坎潘安-马斯特里赫特艾伦地层中的奥斯特龙-卡巴扎伊(Austroraptor cabazai)的肱骨之间。因此,这一新类群的形态似乎预示着其进化过程中的一个过渡阶段。系统发生学分析表明,刁琴是一个具有多个可信系统位置的副类群,但与麒麟兽科(Unenlagiinae)的亲缘关系最为密切。新个体的肱骨远端附近有近似圆形的穿孔,这些穿孔很可能是锥齿鳄类、哺乳动物或兽脚类留下的觅食痕迹,后者有可能与甲龙类或其他岫龙类个体相对应。因此,除了填补岫岩龙进化史上重要的形态学和时间上的空白之外,这个新类群还提供了与这些兽脚类古生态学相关的信息。
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Diuqin lechiguanae gen. et sp. nov., a new unenlagiine (Theropoda: Paraves) from the Bajo de la Carpa Formation (Neuquén Group, Upper Cretaceous) of Neuquén Province, Patagonia, Argentina.

Background: Unenlagiine paravians are among the most relevant Gondwanan theropod dinosaur clades for understanding the origin of birds, yet their fossil record remains incomplete, with most taxa being represented by fragmentary material and/or separated by lengthy temporal gaps, frustrating attempts to characterize unenlagiine evolution.

Results and conclusions: Here we describe Diuqin lechiguanae gen. et sp. nov., a new unenlagiine taxon from the Upper Cretaceous (Santonian) Bajo de la Carpa Formation of the Neuquén Basin of Neuquén Province in northern Patagonia, Argentina that fills a substantial stratigraphic gap in the fossil record of these theropods. Although known only from a very incomplete postcranial skeleton, the preserved bones of Diuqin differ from corresponding elements in other unenlagiines, justifying the erection of the new taxon. Moreover, in several morphological aspects, the humerus of Diuqin appears intermediate between those of geologically older unenlagiines from the Neuquén Basin (e.g., Unenlagia spp. from the Turonian-Coniacian Portezuelo Formation) and that of the stratigraphically younger, larger-bodied Austroraptor cabazai from the Campanian-Maastrichtian Allen Formation. Consequently, the morphology of the new taxon appears to indicate a transitional stage in unenlagiine evolution. Phylogenetic analysis recovers Diuqin as a paravian with multiple plausible systematic positions, but the strongest affinity is with Unenlagiinae. The humerus of the new form exhibits subcircular punctures near its distal end that are interpreted as feeding traces most likely left by a conical-toothed crocodyliform, mammal, or theropod, the latter potentially corresponding to a megaraptorid or another unenlagiine individual. Thus, in addition to filling important morphological and temporal gaps in unenlagiine evolutionary history, the new taxon also offers information relating to the paleoecology of these theropods.

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