首页> 外文期刊>Acta Palaeontologica Polonica >A new sauropod dinosaur from the Lower Cretaceous Cedar mountain formation, Utah, USA
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A new sauropod dinosaur from the Lower Cretaceous Cedar mountain formation, Utah, USA

机译:来自下犹白垩纪雪松山脉形成的新蜥脚类恐龙,美国犹他州

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摘要

Brontomerus mcintoshi is a new genus and species of sauropod dinosaur from the Hotel Mesa Quarry in Grand County, Utah, USA, in the upper part of the Ruby Ranch Member (Aptian-Albian) of the Lower Cretaceous Cedar Mountain Formation. It is known from at least two fragmentary specimens of different sizes. The type specimen is OMNH 66430, the left ilium of a juvenile individual; tentatively referred specimens include a crushed presacral centrum, a complete and well-preserved mid-to-posterior caudal vertebra, the partial centrum of a distal caudal vertebra, a complete pneumatic anterior dorsal rib from the right side, the nearly complete left scapula of a much larger, presumably adult, individual, and two partial sternal plates. Brontomerus is diagnosed by five autapomorphies of the type specimen: preacetabular lobe 55% of total ilium length, longer than in any other sauropod; preacetabular lobe directed anterolaterally at 30° to the sagittal, but straight in dorsal view and vertically oriented; postacetabular lobe reduced to near absence; ischiadic peduncle reduced to very low bulge; ilium proportionally taller than in any other sauropod, 52% as high as long. In a phylogenetic analysis, Brontomerus was recovered as a camarasauromorph in all most parsimonious trees, but with uncertain position within that clade. The large preacetabular lobe of the ilium anchored powerful protractor and abductor muscles, but precise interpretation is impossible without functionally related elements such as femora and proximal caudal vertebrae. Brontomerus is the eighth sauropod genus named from the Early Cretaceous of North America, and more remain to be described: North American sauropod diversity did not decline catastrophically at the end of the Jurassic as often assumed. The most striking differences between Late Jurassic and Early Cretaceous sauropod faunas in North America is that the former are abundant and dominated by diplodocids, whereas the latter are comparatively scarce- though still diverse-and dominated by macronarians.
机译:Brontomerus mcintoshi是来自美国犹他州格兰德县Mesa Quarry的Hotel Mesa Quarry的蜥脚类恐龙的新属和种,其位于下白垩纪雪松山脉形成的红宝石牧场成员(Aptian-Albian)的上部。从至少两个不同大小的碎片样本中可以知道。类型标本是OMNH 66430,少年个体的左i骨;暂定参照的标本包括include前粉碎性中央椎体,完整且保存完好的中尾后椎体,尾部远端椎体的部分中枢,右侧完整的充气前背肋骨,近端完整的左肩骨大得多,大概是成人,个体和两个部分胸骨板。可通过类型样本的五种亚型诊断出雷曼氏菌:髋臼前叶占总lium长度的55%,比任何其他蜥足类动物长。髋臼前叶前向与矢状面成30度角,但在背视时呈笔直状态,垂直方向;髋臼后叶减少到几乎不存在;坐骨梗降低到非常低的隆起; lium的比例比其他蜥脚类动物高,高达52%。在系统发育分析中,雷公藤在所有最简约的树木中均被恢复为camarasauromorph,但在该进化枝中的位置不确定。 acet骨的大型髋臼前叶锚定了强大的量角器和外展肌,但是如果没有功能相关的元件(例如股骨和尾椎近端),则无法进行精确的解释。 Brontomerus是从北美白垩纪早期命名的第8蜥脚类恐龙属,尚待进一步描述:北美蜥脚类动物的多样性并没有像人们普遍认为的那样在侏罗纪末期发生灾难性的下降。北美晚侏罗世和早白垩世蜥脚类动物区系之间最显着的区别是,前者丰富且以双齿类动物为主,而后者则相对稀少(尽管仍是多样的),并以大型动物为主。

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