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来自巴西南部上三叠统的托伦蒂诺乌奈龙(恐龙纲:蜥脚形亚目)骨骼未成熟个体。

On a skeletally immature individual of Unaysaurus tolentinoi (Dinosauria: Sauropodomorpha) from the upper Triassic of southern Brazil.

作者信息

Müller Rodrigo T, Garcia Maurício S, Bem Fabiula P, Damke Lísie V S, Fonseca André O, Da-Rosa Átila A S

机构信息

Programa de Pós-Graduação em Biodiversidade Animal, Universidade Federal de Santa Maria, Santa Maria, Brazil.

Centro de Apoio à Pesquisa Paleontológica da Quarta Colônia, Universidade Federal de Santa Maria, Santa Maria, Brazil.

出版信息

Anat Rec (Hoboken). 2024 Apr;307(4):1071-1083. doi: 10.1002/ar.25285. Epub 2023 Jul 6.

DOI:10.1002/ar.25285
PMID:37409690
Abstract

The lineage of sauropodomorph dinosaurs raised some of the most impressive animals that ever walked on Earth. However, the massive titans of the Mesozoic Era originated from far smaller dinosaurs. The Triassic beds from Brazil yielded the earliest part of this evolutionary history. Despite the diverse fossil record of early sauropodomorphs, juvenile specimens, as well as certain species are poorly sampled. This is the case for Unaysaurus tolentinoi, an unaysaurid sauropodomorph from Caturrita Formation (ca. 225 Ma; early Norian, Late Triassic). The holotype and only specimen of U. tolentinoi was excavated from the Água Negra Locality (São Martinho da Serra, Rio Grande do Sul, Brazil) in 1998. More than two decades later, no other fossil vertebrates have been reported from the same fossiliferous site. Here we describe a skeletally immature specimen which was found in association with the holotype of U. tolentinoi. The specimen was discovered after a first-hand examination of the holotype and comprises some isolated vertebrae and elements from the posterior autopodium. According to linear regressions, its metatarsal I is approximately 41.7 mm in length, compared to approximately 75.9 mm in the holotype. The repeated elements and reduced size indicates that it does not belong to the elements originally used to erect U. tolentinoi. Rather, the specimen is assigned to U. tolentinoi by topotypy and shared morphology. In addition to the reduced size, distinct lines of evidence (e.g., neurocentral sutures; bone texture) support its assignment to a skeletally immature individual. In sum, the new material expands the record of U. tolentinoi, and represents an additional juvenile dinosaur from the Caturrita Formation.

摘要

蜥脚形亚目恐龙谱系孕育出了一些地球上有史以来最令人印象深刻的动物。然而,中生代的巨型巨兽却是起源于小得多的恐龙。巴西的三叠纪地层揭示了这段进化史的最早部分。尽管早期蜥脚形亚目恐龙化石记录多样,但幼年标本以及某些物种的样本却很匮乏。图伦蒂诺乌奈龙就是如此,它是一种来自卡图里塔组(约2.25亿年前;晚三叠世诺利期早期)的基础蜥脚形亚目恐龙。图伦蒂诺乌奈龙的正模标本也是唯一标本于1998年从阿瓜内格拉地点(巴西南里奥格兰德州圣马丁达塞拉)发掘出来。二十多年后,同一化石产地再未报告过其他化石脊椎动物。在此,我们描述一个骨骼未成熟的标本,它是与图伦蒂诺乌奈龙正模标本一同发现的。该标本是在对正模标本进行实地考察后发现的,包括一些分离的脊椎骨和来自后足的骨骼元素。根据线性回归,其第一跖骨长度约为41.7毫米,而正模标本约为75.9毫米。这些重复出现的骨骼元素以及较小的尺寸表明它不属于最初用于建立图伦蒂诺乌奈龙的骨骼元素。相反,根据产地相同和形态特征,该标本被归入图伦蒂诺乌奈龙。除了尺寸较小外,明显的证据线索(如神经中央缝;骨质纹理)也支持将其归入骨骼未成熟个体。总之,新材料扩展了图伦蒂诺乌奈龙的记录,并代表了来自卡图里塔组的又一具幼年恐龙标本。

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