The Gondwanan Origin of Tribosphenida (Mammalia)

T. Flannery, T. Rich, P. Vickers-Rich, E. G. Veatch, K. Helgen
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引用次数: 1

Abstract

Abstract A review of the Southern Hemisphere Mesozoic tribosphenic mammal fossil record supports the hypothesis that Tribosphenida arose in the Southern Hemisphere during the Early Jurassic, around 50 million years prior to the clade’s reliably dated first appearance in the Northern Hemisphere. Mesozoic Southern Hemisphere tribosphenic mammals are known from Australia, Madagascar, South America and the Indian subcontinent, and are classified into three families: Bishopidae (fam. nov.), Ausktribosphenidae and Henosferidae. These are stem therians, and considerable morphological evolution occurred within the lineage between the Jurassic and late Early Cretaceous. Important dental modifications include a graduated transition between premolars and molars, development of molar wear facets V and VI, loss of facets for postdentary bones, reduction in the Meckelian groove and development of a true dentary angle. Previous classifications of Southern Hemisphere tribosphenic mammals are ambiguous because information from the upper dentition has been lacking. Upper molars attributed to the late Early Cretaceous (Albian) Southern Hemisphere group Bishopidae fam. nov. are now known to possess a prominent protocone and stylar cusp C. We thus consider bishopids to be the sister group to Theria. Timothy F. Flannery [tim.flannery@textpublishing.com.au], Kristofer M. Helgen [Kris.Helgen@Australian.Museum], Australian Museum, 1 William St Sydney 2000, Australia; Thomas H. Rich [trich@museum.vic.gov.au], Museums Victoria, PO Box 666, Q28 Melbourne, Victoria 3001, Australia; Patricia Vickers-Rich [pat.rich@monash.edu; prich@swin.edu.au], School of Earth, Atmosphere and Environment, Monash University, Victoria 3800, Australia; Swinburne University of Science and Technology, Department of Chemistry and Biotechnology, Hawthorn, Victoria 3122, Australia; Elizabeth Grace Veatch [elizabeth.veatch@gmail.com], National Museum of Natural History, Smithsonian Institution, Washington, DC 20013, USA.
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三角蛛(哺乳动物)的冈瓦纳起源
摘要对南半球中生代摩擦圈哺乳动物化石记录的回顾支持了这样的假设:早侏罗纪时期,摩擦圈动物在南半球出现,比该分支在北半球首次出现的可靠日期早了约5000万年。中生代南半球的摩擦生哺乳动物分布于澳大利亚、马达加斯加、南美洲和印度次大陆,分为三科:11月)、狐猴科和狐猴科。这些是干兽,在侏罗纪和早白垩纪晚期之间的谱系中发生了相当大的形态进化。重要的牙齿改良包括前磨牙和磨牙之间的渐变过渡,磨牙磨损面V和磨牙磨损面VI的发展,后牙骨的磨牙面缺失,梅克尔氏沟的减少和真正牙牙角度的发展。由于缺乏来自上齿列的信息,以往南半球摩擦性哺乳动物的分类是模糊的。上臼齿属于早白垩世晚期(阿尔巴尼亚)南半球的双齿齿科。11 .现在已知有一个突出的原锥和花柱尖C.因此我们认为双峰星是Theria的姐妹群。Timothy F. Flannery [tim.flannery@textpublishing.com.au], kristoffer M. Helgen [Kris.Helgen@Australian.Museum],澳大利亚博物馆,1 William St Sydney 2000,澳大利亚;托马斯·h·里奇[trich@museum.vic.gov.au],维多利亚博物馆,邮政信箱666,Q28墨尔本,维多利亚州3001,澳大利亚;Patricia Vickers-Rich [pat.rich@monash.edu;prich@swin.edu.au],莫纳什大学地球、大气与环境学院,澳大利亚维多利亚3800;斯威本科技大学化学与生物技术系,澳大利亚维多利亚州山楂3122;Elizabeth Grace Veatch [elizabeth.veatch@gmail.com],国家自然历史博物馆,史密森学会,华盛顿特区20013,美国。
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