A caenagnathid oviraptorosaur metatarsal from the Mesaverde Formation (Campanian), Wyoming

Chan-gyu Yun, Gregory G. Funston
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Abstract

A well-preserved left theropod metatarsal I from the Campanian Mesaverde Formation of Wyoming is described and identified as belonging to a caenagnathid, representing the first occurrence of this clade from the formation. The specimen is unique in being relatively small, but featuring a suite of characters (triangular shaft, less constriction between the shaft and the distal condyle, spherical distal condyle) that are seen in larger examples of Caenagnathidae such as Anzu wyliei or “Macrophalangia canadensis”. This suggests that the previously-observed differences in metatarsal I between small and large caenagnathids are not solely the result of allometry, but may represent phylogenetically informative variation. Although limited, this new specimen lends some support to the hypothesis that “Macrophalangia canadensis” does not represent a large Chirostenotes pergracilis. Furthermore, the specimen is important in establishing the presence of caenagnathids within the Mesaverde Formation fauna, in which theropod remains are poorly known.  
怀俄明州梅萨维尔德组(坎帕尼亚)出土的一具栉龙类窃蛋龙跖骨
一个保存完好的左兽脚亚目跖骨I来自怀俄明州坎帕尼亚梅萨维德地层,被描述并鉴定为属于一个caenagnathid,代表了该地层中首次出现的这一分支。该标本的独特之处在于相对较小,但具有一系列特征(三角形轴,轴与远端髁之间较少的狭窄,球形远端髁),这些特征在Caenagnathidae(如Anzu wyliei或“Macrophalangia canadensis”)等较大的例子中可以看到。这表明,先前观察到的大小棘球兽跖骨I的差异不仅仅是异速生长的结果,而且可能代表了系统发育上的信息变异。尽管数量有限,但这个新标本在一定程度上支持了“加拿大巨指骨”不代表大型过细颈指骨的假设。此外,该标本对于在Mesaverde组动物群中确定caenagnathids的存在很重要,在Mesaverde组中,兽脚亚目的遗骸知之甚少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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