Adele H. Pentland, Stephen F. Poropat, Matt A. White, Samantha L. Rigby, P. Vickers-Rich, T. Rich, David A. Elliott
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引用次数: 5
Abstract
Abstract The Australian pterosaur assemblage currently consists of specimens recovered only from Cretaceous strata, with most of these referred to the clade Anhangueria. The majority of Australia’s pterosaur remains have been discovered in the Eromanga Basin of Queensland, specifically the upper Albian Toolebuc Formation, upper Albian Mackunda Formation, and Cenomanian–lowermost Turonian Winton Formation. In this paper, we describe two new partial pterosaur femora from the Toolebuc and Winton formations. Despite being incomplete, these specimens can be assigned to Anhangueria. Pairwise comparisons demonstrate differences in the deflection of the femoral head. Moreover, a subtle ridge on the posterior surface of the Toolebuc Formation femur is not visible on the specimen from the Winton Formation. The greater trochanter of the Winton Formation femur also preserves a potential bite mark that is tentatively attributed to a crocodylomorph. These new pterosaur fossils supplement the currently limited understanding of pterosaur diversity from Australia, and attest to the cosmopolitan distribution of anhanguerians during the Early to mid-Cretaceous. Adele H. Pentland# [pentlandadele@gmail.com], Stephen F. Poropat# [stephenfporopat@gmail.com], Matt A. White† [fossilised@hotmail.com], and Samantha L. Rigby# [samantha.rigby@hotmail.com], Australian Age of Dinosaurs Natural History Museum, The Jump-Up, Winton, Queensland 4735, Australia; Patricia Vickers-Rich* [prich@swin.edu.au], Faculty of Science, Engineering and Technology, Swinburne University of Technology, John St, Hawthorn, Victoria 3122, Australia; Thomas H. Rich [trich@museum.vic.gov.au], Museums Victoria, PO Box 666, Melbourne, Victoria 3001, Australia; David A. Elliott [david.elliott@aaod.com.au], Australian Age of Dinosaurs Natural History Museum, The Jump-Up, Winton, Queensland 4735, Australia. # Also affiliated with: School of Science, Computing and Engineering Technologies, Swinburne University of Technology, John St, Hawthorn, Victoria 3122, Australia. *School of Earth, Atmosphere and Environment, Monash University, Melbourne, Victoria 3800, Australia. †Palaeoscience Research Centre, University of New England, Armidale 2351, New South Wales, Australia.
澳大利亚的翼龙组合目前只包括从白垩纪地层中发现的标本,其中大部分属于Anhangueria分支。澳大利亚的大部分翼龙遗骸都是在昆士兰的Eromanga盆地发现的,特别是上Albian Toolebuc组、上Albian Mackunda组和cenomanian - Turonian Winton组。在本文中,我们描述了来自Toolebuc和Winton组的两个新的部分股翼龙。尽管不完整,但这些标本可归为安汉格里亚属。两两比较显示了股骨头偏转的差异。此外,在Winton组标本上看不到Toolebuc组股骨后表面的细微脊。温顿形成股骨的大转子也保留了一个潜在的咬痕,初步归因于鳄鱼形。这些新的翼龙化石补充了目前对澳大利亚翼龙多样性的有限认识,并证明了早白垩纪至中白垩纪翼龙的全球分布。Adele H. Pentland# [pentlandadele@gmail.com], Stephen F. Poropat# [stephenfporopat@gmail.com], Matt A. White†[fossilised@hotmail.com]和Samantha L. Rigby# [samantha.rigby@hotmail.com],澳大利亚恐龙时代自然历史博物馆,The jumpup, Winton, Queensland 4735,澳大利亚;Patricia Vickers-Rich* [prich@swin.edu.au],斯威本科技大学科学、工程与技术学院,澳大利亚维多利亚州3122;托马斯·h·里奇[trich@museum.vic.gov.au],维多利亚博物馆,邮政信箱666,墨尔本,维多利亚州3001,澳大利亚;David A. Elliott [david.elliott@aaod.com.au],澳大利亚恐龙时代自然历史博物馆,The jumpup, Winton, Queensland 4735,澳大利亚。附属于:科学,计算和工程技术学院,斯威本科技大学,John St, Hawthorn,维多利亚3122,澳大利亚。*莫纳什大学地球、大气与环境学院,澳大利亚维多利亚州墨尔本3800。†新英格兰大学古科学研究中心,阿米代尔2351,新南威尔士州,澳大利亚。