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A titanosaur (Dinosauria: Sauropoda) osteoderm from the Alcantara Formation (Cenomanian), S?o Luís Basin, Northeastern Brazil

机译:来自巴西东北部S?oLuís盆地的Alcantara组(切诺曼尼亚)的泰坦龙(恐龙龙:Sauropoda)骨真皮

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摘要

Among titanosaurs, osteoderms are morphologically diverse and have been reported from deposits in South America, Africa, Madagascar, Eurasia and Oceania. In Brazil, titanosaur osteoderms are rare and have only been recorded from Bauru Basin sedimentary rocks. Here, we describe a keeled titanosaur osteoderm, which is the first occurrence of an osteoderm specimen in the S?o Luís Basin, Northeastern Brazil. This osteoderm is characterized by an external bulb, an internal root, and a very rugose cingulum limiting the external and internal surfaces. These characteristics are typical of Titanosauria dermal bones, and this specimen strengthens the idea that the armored sauropods were present during the early Late Cretaceous of Northeastern Brazil, extending their distribution in the northernmost portion of South America.
机译:在泰坦龙中,真皮的形态是多种多样的,并且据报道来自南美,非洲,马达加斯加,欧亚大陆和大洋洲的矿床。在巴西,钛恐龙骨质很少见,仅在包鲁盆地沉积岩中有记录。在这里,我们描述了一个龙骨的钛恐龙皮,这是巴西东北部S?oLuís盆地中首次出现的一个骨皮标本。这种骨质真皮的特征是外部球茎,内部根和限制外部和内部表面的非常柔软的扣带。这些特征是Titanosauria真皮骨骼的典型特征,该标本强化了这样一种观念,即装甲蜥足类动物存在于巴西东北部晚白垩世早期,从而扩展了它们在南美最北端的分布。

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