{"title":"阿根廷中部巴塔哥尼亚上白垩世Bajo Barreal地层的巨盗龙(兽脚目:破伤风目)部分骨骼:冈瓦南巨盗龙大体型进化的意义","authors":"M. Lamanna, G. Casal, R. Martínez, L. Ibiricu","doi":"10.2992/007.086.0302","DOIUrl":null,"url":null,"abstract":"ABSTRACT We describe two partial postcranial skeletons belonging to the enigmatic theropod dinosaur clade Megaraptoridae from the Upper Cretaceous (lower Cenomanian–upper Turonian) Bajo Barreal Formation of southern Chubut Province, central Patagonia, Argentina. The specimens are assigned to Megaraptoridae due to their possession of multiple anatomical features that are considered synapomorphies of that predatory dinosaur group, such as a greatly enlarged, laterally compressed ungual of manual digit I that possesses asymmetrical lateral and medial vascular grooves. Overlapping elements of the two skeletons are nearly identical in morphology, suggesting that they probably represent the same taxon, a large-bodied theropod that was previously unknown from the early Late Cretaceous of southern South America. The Bajo Barreal specimens constitute the most ancient unquestionable records of Megaraptoridae from that continent, and exhibit particularly strong osteological resemblances to penecontemporaneous megaraptorids from the Winton Formation of Australia. Phylogenetic analysis recovers the unnamed Bajo Barreal taxon as the earliest-diverging South American megaraptorid and the oldest-known representative of this clade that likely attained a body length of at least seven meters and a mass of at least one metric ton. Overall, the balance of the evidence suggests that megaraptorids originated in eastern Gondwana (Australia) during the Early Cretaceous, then subsequently dispersed to western Gondwana (South America) during the mid-Cretaceous, where they attained substantially larger body sizes, ultimately coming to occupy the apex predator niches in their respective habitats.","PeriodicalId":50771,"journal":{"name":"Annals of Carnegie Museum","volume":"19 1","pages":"255 - 294"},"PeriodicalIF":0.6000,"publicationDate":"2020-11-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"16","resultStr":"{\"title\":\"Megaraptorid (Theropoda: Tetanurae) Partial Skeletons from the Upper Cretaceous Bajo Barreal Formation of Central Patagonia, Argentina: Implications for the Evolution of Large Body Size in Gondwanan MegaraptoranS\",\"authors\":\"M. Lamanna, G. Casal, R. Martínez, L. 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The Bajo Barreal specimens constitute the most ancient unquestionable records of Megaraptoridae from that continent, and exhibit particularly strong osteological resemblances to penecontemporaneous megaraptorids from the Winton Formation of Australia. Phylogenetic analysis recovers the unnamed Bajo Barreal taxon as the earliest-diverging South American megaraptorid and the oldest-known representative of this clade that likely attained a body length of at least seven meters and a mass of at least one metric ton. 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引用次数: 16
摘要
摘要本文描述了阿根廷中部巴塔哥尼亚Chubut省南部上白垩世(下cenomanian -上Turonian) Bajo Barreal组的两具神秘兽脚亚目恐龙分支Megaraptoridae的部分颅骨后骨骼。这些标本被归为大盗龙科,因为它们具有多种被认为是该掠食性恐龙群的近亲的解剖特征,例如手指I的一个极大扩大的、侧向压缩的足趾,具有不对称的外侧和内侧血管沟。这两具骨骼的重叠部分在形态上几乎完全相同,这表明它们可能代表同一个分类群,一种来自南美南部晚白垩纪早期的大型兽脚亚目恐龙,此前人们对这种恐龙一无所知。Bajo Barreal标本构成了该大陆最古老的、毫无疑问的巨盗龙科记录,并与澳大利亚温顿组准同时期的巨盗龙表现出特别强烈的骨学相似性。系统发育分析显示,未命名的Bajo Barreal分类群是南美洲最早分化的巨盗龙,也是已知最古老的代表,可能达到了至少7米的体长和至少1吨的质量。总的来说,证据的平衡表明,巨龙在白垩纪早期起源于冈瓦纳东部(澳大利亚),随后在白垩纪中期分散到冈瓦纳西部(南美洲),在那里它们的体型大大增加,最终占据了各自栖息地的顶级捕食者壁龛。
Megaraptorid (Theropoda: Tetanurae) Partial Skeletons from the Upper Cretaceous Bajo Barreal Formation of Central Patagonia, Argentina: Implications for the Evolution of Large Body Size in Gondwanan MegaraptoranS
ABSTRACT We describe two partial postcranial skeletons belonging to the enigmatic theropod dinosaur clade Megaraptoridae from the Upper Cretaceous (lower Cenomanian–upper Turonian) Bajo Barreal Formation of southern Chubut Province, central Patagonia, Argentina. The specimens are assigned to Megaraptoridae due to their possession of multiple anatomical features that are considered synapomorphies of that predatory dinosaur group, such as a greatly enlarged, laterally compressed ungual of manual digit I that possesses asymmetrical lateral and medial vascular grooves. Overlapping elements of the two skeletons are nearly identical in morphology, suggesting that they probably represent the same taxon, a large-bodied theropod that was previously unknown from the early Late Cretaceous of southern South America. The Bajo Barreal specimens constitute the most ancient unquestionable records of Megaraptoridae from that continent, and exhibit particularly strong osteological resemblances to penecontemporaneous megaraptorids from the Winton Formation of Australia. Phylogenetic analysis recovers the unnamed Bajo Barreal taxon as the earliest-diverging South American megaraptorid and the oldest-known representative of this clade that likely attained a body length of at least seven meters and a mass of at least one metric ton. Overall, the balance of the evidence suggests that megaraptorids originated in eastern Gondwana (Australia) during the Early Cretaceous, then subsequently dispersed to western Gondwana (South America) during the mid-Cretaceous, where they attained substantially larger body sizes, ultimately coming to occupy the apex predator niches in their respective habitats.
期刊介绍:
Annals of Carnegie Museum is a quarterly journal that publishes peer-reviewed short and medium-length original scientific contributions in organismal biology, earth sciences, and anthropology, in 40 by 52.5 pica format (168 by 220 mm or 6-5/8 by 8-5/8 inches). Subject matter must be relevant to Carnegie Museum of Natural History scientific sections or Powdermill Nature Reserve (PNR), preferably with connection to the Carnegie collection and/or personnel. Carnegie Museum staff and research associates receive publication priority, but others are encouraged to submit papers, especially those manuscripts explicitly based on the Carnegie collection.