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A New Archosauriform Reptile with Distinctive Teeth from the Middle Triassic (Ladinian) of Germany
Journal of Vertebrate Paleontology ISSN: (Print) (Online) Journal homepage: https://www.tandfonline.com/loi/ujvp20 A new archosauriform reptile with distinctive teeth from the Middle Triassic (Ladinian) of Germany Hans-Dieter Sues , Rainer R. Schoch , Gabriela Sobral & Randall B. Irmis To cite this article: Hans-Dieter Sues , Rainer R. Schoch , Gabriela Sobral & Randall B. Irmis (2020) A new archosauriform reptile with distinctive teeth from the Middle Triassic (Ladinian) of Germany, Journal of Vertebrate Paleontology, 40:1, e1764968, DOI: 10.1080/02724634.2020.1764968 To link to this article: https://doi.org/10.1080/02724634.2020.1764968 View supplementary material Published online: 23 Jun 2020. Submit your article to this journal Article views: 200 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=ujvp20 Journal of Vertebrate Paleontology e1764968 (14 pages) The work of Hans–Dieter Sues was authored as part of his official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 USC. 105, no copyright protection is available for such works under US Law. Rainer R. Schoch, Gabriela Sobral and Randall B. Irmis hereby waive their right to assert copyright, but not their right to be named as co–authors in the article. DOI: 10.1080/02724634.2020.1764968 ARTICLE A NEW ARCHOSAURIFORM REPTILE WITH DISTINCTIVE TEETH FROM THE MIDDLE TRIASSIC (LADINIAN) OF GERMANY HANS-DIETER SUES, *,1 RAINER R. SCHOCH, 2 GABRIELA SOBRAL, 2 and RANDALL B. IRMIS3 1Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, MRC 121, P.O. -
From the Terrestrial Upper Triassic of China
第 39 卷 第 4 期 古 脊 椎 动 物 学 报 pp. 251~265 2001 年 10 月 V ERTEBRATA PALASIATICA figs. 1~4 ,pl. I 中国陆相上三叠统第一个初龙形类动物1) 吴肖春1 刘 俊2 李锦玲2 (1 加拿大自然博物馆 渥太华 K1P 6P4) (2 中国科学院古脊椎动物与古人类研究所 北京 100044) 摘要 初步研究了山西省永和县桑壁镇铜川组二段产出的两件初龙形类化石标本 ( IVPP V 12378 ,V 12379) ,在此基础上建立了一新属新种 ———桑壁永和鳄 ( Yonghesuchus sangbiensis gen. et sp. nov. ) 。 它以下列共存的衍生特征区别于其他初龙形类 (archosauriforms) :1) 吻部前端尖削 ;2) 眶前窝前部具一凹陷 ;3) 眶前窝与外鼻孔间宽 ;4) 眶后骨下降突的后 2/ 3 宽且深凹 ;5) 基蝶 骨腹面有两个凹陷 ;6) 齿骨后背突相当长 ;7) 关节骨的反关节区有明显的背脊 ,有穿孔的翼 状的内侧突 ,以及指向前内侧向和背向的十分显著的后内侧突。 由于缺乏跗骨的形态信息 ,目前很难通过支序分析建立永和鳄的系统发育关系。但可以 通过头骨形态来推测永和鳄在初龙形类中的系统位置。永和鳄有翼骨齿 ,这表明它不属于狭 义的初龙类 (archosaurians) 。其通过内颈动脉脑支的孔位于基蝶骨的前侧面而不是腹面 ,在 这点上永和鳄比原鳄龙科 ( Proterochampsidae) 更进步 ,这表明与后者相比永和鳄和狭义的初 龙类的关系可能更近。在中国早期的初龙形类中 ,达坂吐鲁番鳄 ( Turf anosuchus dabanensis) 与桑壁永和鳄最接近 ,但前者由于内颈动脉脑支的孔腹位而比后者更为原始。 根据以上头骨特征以及枢后椎椎体之间间椎体的存在与否 ,推测派克鳄 ( Euparkeria) 、 达坂吐鲁番鳄 (如果存在间椎体) 、原鳄龙科和永和鳄与初龙类的关系逐渐接近 。而且这与这 些初龙形类的生存时代基本一致。 永和鳄比产于上三叠统下部的原鳄龙 ( Proterocham psa) 进步 ,它的发现支持含化石的铜 川组时代为晚三叠世的观点。 关键词 山西永和 ,晚三叠世 ,铜川组 ,初龙形类 ,解剖学 中图法分类号 Q915. 864 1) 中国科学院古生物学与古人类学科基础研究特别支持基金项目(编号 :9809) 资助。 收稿日期 :2001- 03- 23 252 古 脊 椎 动 物 学 报 39 卷 THE ANATOMY OF THE FIRST ARCHOSAURIFORM ( DIAPSIDA) FROM THE TERRESTRIAL UPPER TRIASSIC OF CHINA WU Xiao2Chun1 L IU J un2 L I Jin2Ling2 (1 Paleobiology , Research Division , Canadian M useum of Nat ure P.O.Box 3443 Station D, Ottawa, ON K1P 6P4 , Canada) (2 Instit ute of Vertebrate Paleontology and Paleoanthropology , Chinese Academy of Sciences Beijing 100044) Abstract Yonghesuchus sangbiensis , a new genus and species of the Archosauriformes , is erected on the basis of its peculiar cranial features. This taxon represents the first record of tetrapods from the Late Triassic terrestrial deposits of China. Its discovery is significant not only to our study on the phylogeny of the Archosauriformes but also to our understanding of the evolution of the Triassic terrestrial vertebrate faunae in China. -
The Origin and Early Evolution of Dinosaurs
Biol. Rev. (2010), 85, pp. 55–110. 55 doi:10.1111/j.1469-185X.2009.00094.x The origin and early evolution of dinosaurs Max C. Langer1∗,MartinD.Ezcurra2, Jonathas S. Bittencourt1 and Fernando E. Novas2,3 1Departamento de Biologia, FFCLRP, Universidade de S˜ao Paulo; Av. Bandeirantes 3900, Ribeir˜ao Preto-SP, Brazil 2Laboratorio de Anatomia Comparada y Evoluci´on de los Vertebrados, Museo Argentino de Ciencias Naturales ‘‘Bernardino Rivadavia’’, Avda. Angel Gallardo 470, Cdad. de Buenos Aires, Argentina 3CONICET (Consejo Nacional de Investigaciones Cient´ıficas y T´ecnicas); Avda. Rivadavia 1917 - Cdad. de Buenos Aires, Argentina (Received 28 November 2008; revised 09 July 2009; accepted 14 July 2009) ABSTRACT The oldest unequivocal records of Dinosauria were unearthed from Late Triassic rocks (approximately 230 Ma) accumulated over extensional rift basins in southwestern Pangea. The better known of these are Herrerasaurus ischigualastensis, Pisanosaurus mertii, Eoraptor lunensis,andPanphagia protos from the Ischigualasto Formation, Argentina, and Staurikosaurus pricei and Saturnalia tupiniquim from the Santa Maria Formation, Brazil. No uncontroversial dinosaur body fossils are known from older strata, but the Middle Triassic origin of the lineage may be inferred from both the footprint record and its sister-group relation to Ladinian basal dinosauromorphs. These include the typical Marasuchus lilloensis, more basal forms such as Lagerpeton and Dromomeron, as well as silesaurids: a possibly monophyletic group composed of Mid-Late Triassic forms that may represent immediate sister taxa to dinosaurs. The first phylogenetic definition to fit the current understanding of Dinosauria as a node-based taxon solely composed of mutually exclusive Saurischia and Ornithischia was given as ‘‘all descendants of the most recent common ancestor of birds and Triceratops’’. -
Dinosaurs British Isles
DINOSAURS of the BRITISH ISLES Dean R. Lomax & Nobumichi Tamura Foreword by Dr Paul M. Barrett (Natural History Museum, London) Skeletal reconstructions by Scott Hartman, Jaime A. Headden & Gregory S. Paul Life and scene reconstructions by Nobumichi Tamura & James McKay CONTENTS Foreword by Dr Paul M. Barrett.............................................................................10 Foreword by the authors........................................................................................11 Acknowledgements................................................................................................12 Museum and institutional abbreviations...............................................................13 Introduction: An age-old interest..........................................................................16 What is a dinosaur?................................................................................................18 The question of birds and the ‘extinction’ of the dinosaurs..................................25 The age of dinosaurs..............................................................................................30 Taxonomy: The naming of species.......................................................................34 Dinosaur classification...........................................................................................37 Saurischian dinosaurs............................................................................................39 Theropoda............................................................................................................39 -
Basal Saurischia
TWO Basal Saurischia MAX C. LANGER The name Saurischia was coined by Seeley in lectures given in et al. 1999b; Langer et al. 2000), as well as various strata in the 1887, published in 1888, to designate those dinosaurs possessing western United States and on the Atlantic Coast of both the a propubic pelvis. This plesiomorphic feature distinguishes them United States and Canada (Olsen et al. 1989; Long and Murry from ornithischians, which have an opisthopubic pelvis. De- 1995; Hunt et al. 1998; Lucas 1998). spite its general acceptance as a taxonomic unit since the pro- Interestingly, while saurischian dinosaurs are abundant in posal of the name (Huene 1932; Romer 1956; Colbert 1964a; Steel Carnian strata and became the dominant component of vari- 1970), the monophyly of Saurischia was heavily questioned in ous Norian faunas, ornithischians are barely represented through the 1960s and 1970s (Charig et al. 1965; Charig 1976b; Reig 1970; this time interval. Pisanosaurus mertii, from the Ischigualasto Romer 1972c; Thulborn 1975; Cruickshank 1979). Its status as a Formation, is the sole reasonably well known Triassic member natural group was, however, fixed by Bakker and Galton (1974), of the group, which only achieved higher abundance and di- Bonaparte (1975b) and, more importantly, Gauthier (1986), versity during Early Jurassic times (Weishampel and Norman who formally established the monophyly of the group. 1989). The taxa discussed in this chapter (table 2.1) are usually con- sidered to be among the oldest known dinosaurs. They include the most basal saurischians, as well as various forms of uncer- Definition and Diagnosis tain affinity once assigned to the group. -
A Re-Evaluation of the Enigmatic Dinosauriform Caseosaurus Crosbyensis from the Late Triassic of Texas, USA and Its Implications for Early Dinosaur Evolution
A re-evaluation of the enigmatic dinosauriform Caseosaurus crosbyensis from the Late Triassic of Texas, USA and its implications for early dinosaur evolution MATTHEW G. BARON and MEGAN E. WILLIAMS Baron, M.G. and Williams, M.E. 2018. A re-evaluation of the enigmatic dinosauriform Caseosaurus crosbyensis from the Late Triassic of Texas, USA and its implications for early dinosaur evolution. Acta Palaeontologica Polonica 63 (1): 129–145. The holotype specimen of the Late Triassic dinosauriform Caseosaurus crosbyensis is redescribed and evaluated phylogenetically for the first time, providing new anatomical information and data on the earliest dinosaurs and their evolution within the dinosauromorph lineage. Historically, Caseosaurus crosbyensis has been considered to represent an early saurischian dinosaur, and often a herrerasaur. More recent work on Triassic dinosaurs has cast doubt over its supposed dinosaurian affinities and uncertainty about particular features in the holotype and only known specimen has led to the species being regarded as a dinosauriform of indeterminate position. Here, we present a new diagnosis for Caseosaurus crosbyensis and refer additional material to the taxon—a partial right ilium from Snyder Quarry. Our com- parisons and phylogenetic analyses suggest that Caseosaurus crosbyensis belongs in a clade with herrerasaurs and that this clade is the sister taxon of Dinosauria, rather than positioned within it. This result, along with other recent analyses of early dinosaurs, pulls apart what remains of the “traditional” group of dinosaurs collectively termed saurischians into a polyphyletic assemblage and implies that Dinosauria should be regarded as composed exclusively of Ornithoscelida (Ornithischia + Theropoda) and Sauropodomorpha. In addition, our analysis recovers the enigmatic European taxon Saltopus elginensis among herrerasaurs for the first time. -
SUPPLEMENTARY INFORMATION Doi:10.1038/Nature24011
SUPPLEMENTARY INFORMATION doi:10.1038/nature24011 1. Details of the new phylogenetic analysis 1.1. Modifications to Baron et al. (2017) data matrix The following list presents all character scoring modifications to the original taxon-character matrix of Baron et al. (2017). Unless explicitly mentioned, specimen numbers without asterisks have been scored from notes and photographs after their first-hand examination by at least one of the authors, specimens marked with † were coded based only on photographic material, and specimens marked with * were coded on direct observation of the specimens. Aardonyx celestae; score modifications based on the first-hand observation of all specimens mentioned in Yates et al. (2010). 19: 0 >1. 21 0 >1. 54: 0 >?. 57: 0 >?. 156: 1 >0. 202: 1 >0. 204: 1 >0. 266: 1 >0. 280: ? >0. Ch 286: 2 >1. 348: 0 >?. 365: ? >1. 376: ? >0. 382: 0 >?. 439: 0 >1. 450: 1 >0. Abrictosaurus consors; score modifications based on NHMUK RU B54†. Further bibliographic source: Sereno (2012). 7: 0>?; 26 0>?; 35. 2>0/1; 47: 0>?; 54 1>?; 369 0>?; 424 1>?. Agilisaurus louderbacki; score modifications based on Barrett et al. (2005) and scorings in Butler et al. (2008) and Barrett et al. (2016). 6: 0>?; 11: 0>1; 35: 1>0; 54: 1>0; 189: ?>0. Agnosphitys cromhallensis; score modifications based on cast of VMNH 1751. Further bibliographic source: Fraser et al. (2001). 15: ? >0; 16: ? >0; 21: ? >1; 24: ? >1; 30: 0 >?; 159: 0 >1; 160: - >0; 164: - >?; 165: ? >0; 167: ? >0; 172: 0 >?; 176: 0 >?; 177: 1 >0; 180: ? >0; 185: 0 >?; 221: 0 >?; 222: 0 >?; 252: 0 >1; 253: 0 >1; 254: 1 >?; 256: 0 >1; 258: 1 >?; 259: ? >0; 292: ? >1; 298: ? >0; 303: 1 >2; 305: 2 >1; 306: ? >2; 315: 1 >0; 317: ? >1; 318: ? >0; 409: ? >0; 411: 1 >0; 419: 1 >0; 421: ? >0. -
Triassic Isopoda – Three New Species from Central Europe Shed Light On
University of Groningen Triassic Isopoda – three new species from Central Europe shed light on the early diversity of the group Schädel, Mario; van Eldijk, Timo; Winkelhorst, Herman; Reumer, Jelle W.F.; Haug, Joachim T. Published in: Bulletin of Geosciences DOI: 10.3140/bull.geosci.1773 IMPORTANT NOTE: You are advised to consult the publisher's version (publisher's PDF) if you wish to cite from it. Please check the document version below. Document Version Publisher's PDF, also known as Version of record Publication date: 2020 Link to publication in University of Groningen/UMCG research database Citation for published version (APA): Schädel, M., van Eldijk, T., Winkelhorst, H., Reumer, J. W. F., & Haug, J. T. (2020). Triassic Isopoda – three new species from Central Europe shed light on the early diversity of the group. Bulletin of Geosciences, 95(2), 145-166. https://doi.org/10.3140/bull.geosci.1773 Copyright Other than for strictly personal use, it is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license (like Creative Commons). Take-down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. Downloaded from the University of Groningen/UMCG research database (Pure): http://www.rug.nl/research/portal. For technical reasons the number of authors shown on this cover page is limited to 10 maximum. Download date: 24-09-2021 Triassic Isopoda – three new species from Central Europe shed light on the early diversity of the group Mario Schädel, TiMo van eldijk, herMan WinkelhorST, jelle W.F. -
1. Kannemeyeriiformes from Shanxi, China
DOI:10.19615/j.cnki.1000-3118.2015.01.002 第53卷 第1期 古 脊 椎 动 物 学 报 pp. 16-28 2015年1月 VERTEBRATA PALASIATICA fi gs. 1-6 New discoveries from the Sinokannemeyeria-Shansisuchus Assemblage Zone: 1. Kannemeyeriiformes from Shanxi, China LIU Jun (Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 [email protected]) Abstract Recently, some new tetrapod fossils were collected along the Yellow River in Shanxi Province. From the Member I of the Tongchuan Formation at Baidaoyu in Linxian County, at least one species of Parakannemeyeria, and one new species of Sinokannemeyeria, S. baidaoyuensis, are identifi ed. The new species is characterized by prefrontal anterior extension level to posterior margin of postnarial excavation. From the Ermaying Formation in Liulin County, a third kannemeyeriid genus is identified for the Sinokannemeyeria-Shansisuchus Assemblage. The new findings increase the content and time extension of the Sinokannemeyeria-Shansisuchus Assemblage. Key words Shanxi, Middle Triassic, Ermaying Formation, Tongchuan Formation, Sinokannemeyeria, Parakannemeyeria 1 Introduction In North China, terrestrial Triassic deposits are widely distributed, but the tetrapod fossils have only been discovered from the Heshanggou, Ermaying and Tongchuan formations (Li et al., 2008). The Ermaying Formation is the richest source of Triassic tetrapods of China, with the lower part having yielded the Shaanbeikannemeyeria-Fugusuchus assemblage and the upper part having yielded the Sinokannemeyeria-Shansisuchus assemblage (or Shansidon assemblage) (Li and Cheng, 1995; Sun, 1980). In contrast, the Tongchuan Formation was long considered barren of fossil tetrapods, with the sole exception of the archosauriform Yonghesuchus from Member II of the formation (Liu et al., 2001; Wu et al., 2001). -
15. Fossile Lebensgemeinschaften Im Lettenkeuper 15 Hans Hagdorn, Klaus-Peter Kelber Und Rainer Schoch
15. Fossile Lebensgemeinschaften im Lettenkeuper 15 Hans Hagdorn, Klaus-Peter Kelber und Rainer Schoch Abstract This chapter aims at reconstructing Lower Keuper palaeocommunities in their habitats and to elucidate interdependences of plants, invertebrates, and vertebrates. Four major groups of palaeocommunities are differentiated: (1) The terrestrial palaeocommunities are poorly known from transported fl oral and faunal elements into submersed depositional environments and rooted soil horizons. Clusters of insect eggs and nutritional traces on plants indicate animal-plant-interactions. Small pieces of charcoal give evidence of fi res. The terrestrial reptile record comprises small insectivores and larger carnivores with the rauisuchian Batrachotomus as the top predator, while herbivores are still unknown. The other groups of palaeocommunities depend on the salinity of the water bodies. (2) The fresh- water palaeocommunities are characterized by charophytes, by darwinulid ostracods, by bivalves (Unionites brevis/Unionites donaci- nus) and by amphibians. Here, a low diverse amphibian (Mastodonsaurus/Plagiosuchus/Gerrothorax) and a high diverse amphibian/ reptile palaeocommunity (Mastodonsaurus, Callistomordax, Kupferzellia, Trematolestes, choristoderes, and questionable juvenile tha- lattosaurs) can be discerned. (3) The three brackish water palaeocommunities are dominated by invertebrates: Myophoria/Bakevel- lia, Lingularia/Euestheria, “Anodonta” gregaria). (4) Among the nearly marine palaeocommunities are fi ve bivalve-dominated: Entolium -
The First Triassic 'Protodonatan' (Zygophlebiidae) from China
Geol. Mag. 154 (1), 2017, pp. 169–174. c Cambridge University Press 2016 169 doi:10.1017/S0016756816000625 RAPID COMMUNICATION The first Triassic ‘Protodonatan’ (Zygophlebiidae) from China: stratigraphical implications ∗ ∗ D. R. ZHENG ‡†, A. NEL§, B. WANG‡¶, E. A. JARZEMBOWSKI‡, S.-C. CHANG & H. C. ZHANG‡† ∗ Department of Earth Sciences, The University of Hong Kong, Hong Kong Special Administrative Region, China ‡State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, China §Institut de Systématique, Évolution, Biodiversité, ISYEB-UMR 7205-CNRS, MNHN, UPMC, EPHE, Muséum national d’Histoire naturelle, Sorbonne Universités, 57 rue Cuvier, CP 50, Entomologie, F-75005, Paris, France ¶Key Laboratory of Zoological Systematics and Evolution, Institute of Zoology, Chinese Academy of Sciences, 1, Beichen West Road, Beijing 100101, China Department of Earth Sciences, The Natural History Museum, London SW7 5BD, UK (Received 16 February 2016; accepted 1 June 2016; first published online 21 July 2016) Abstract 2001). It seems, however, to have been distributed world- wide as it is known from France (Middle–Upper Triassic), The clade Triadophlebioptera within the Odonatoptera Germany (Middle Triassic), Kyrgyzstan (Middle–Upper Tri- greatly diversified and became widely distributed world- assic), Russia (Upper Permian), Spain (Middle Triassic) and wide during the Triassic. Although abundant insect fossils Australia (Middle Triassic) (Nel et al. 2001; Béthoux et al. have been reported from the Triassic of China, no Triassic 2009; Béthoux & Beattie, 2010). dragonflies have been recorded. In this paper, Zygophlebia In China, abundant dragonfly fossils have been reported tongchuanensis sp. nov., the first species of Zygophlebiidae from the Middle Jurassic – Lower Cretaceous (Fleck & Nel, discovered outside the Madygen Formation of Kyrgyzstan, is 2002;Renet al. -
The Femoral Anatomy of Pampadromaeus Barberenai Based
This article was downloaded by: [New York University] On: 19 February 2015, At: 11:22 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Historical Biology: An International Journal of Paleobiology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ghbi20 The femoral anatomy of Pampadromaeus barberenai based on a new specimen from the Upper Triassic of Brazil Rodrigo Temp Müllera, Max Cardoso Langerb, Sérgio Furtado Cabreirac & Sérgio Dias-da- Silvad a Programa de Pós Graduação em Biodiversidade Animal, Universidade Federal de Santa Maria, Santa Maria, RS, Brazil b Laboratório de Paleontologia de Ribeirão Preto, Universidade de São Paulo, Ribeirão Preto, Click for updates SP, Brazil c Museu de Ciências Naturais, Universidade Luterana do Brasil, Canoas, RS, Brazil d Centro de Apoio a Pesquisa Paleontológica, Universidade Federal de Santa Maria, Santa Maria, RS, Brazil Published online: 19 Feb 2015. To cite this article: Rodrigo Temp Müller, Max Cardoso Langer, Sérgio Furtado Cabreira & Sérgio Dias-da-Silva (2015): The femoral anatomy of Pampadromaeus barberenai based on a new specimen from the Upper Triassic of Brazil, Historical Biology: An International Journal of Paleobiology, DOI: 10.1080/08912963.2015.1004329 To link to this article: http://dx.doi.org/10.1080/08912963.2015.1004329 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content.