University of Birmingham Increases in Sampling Support The
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
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. -
PDF Available Here
Edinburgh Research Explorer The sail-backed reptile Ctenosauriscus from the latest Early Triassic of Germany and the timing and biogeography of the early archosaur radiation Citation for published version: Butler, RJ, Brusatte, SL, Reich, M, Hornung, JJ, Nesbitt, SJ & Schoch, RR 2011, 'The sail-backed reptile Ctenosauriscus from the latest Early Triassic of Germany and the timing and biogeography of the early archosaur radiation', PLoS ONE, vol. 6, no. 10. https://doi.org/10.1371/journal.pone.0025693 Digital Object Identifier (DOI): 10.1371/journal.pone.0025693 Link: Link to publication record in Edinburgh Research Explorer Document Version: Publisher's PDF, also known as Version of record Published In: PLoS ONE Publisher Rights Statement: This is an Open-Access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are properly cited. Made available through the Public Library of Science (2011) General rights Copyright for the publications made accessible via the Edinburgh Research Explorer is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The University of Edinburgh has made every reasonable effort to ensure that Edinburgh Research Explorer content complies with UK legislation. If you believe that the public display of this file breaches copyright please contact [email protected] providing details, and we will remove access to the work immediately and investigate your claim. -
The Ferns of the Late Ladinian, Middle Triassic Flora from Monte Agnello, Dolomites, Italy
The ferns of the late Ladinian, Middle Triassic flora from Monte Agnello, Dolomites, Italy EVELYN KUSTATSCHER, ELIO DELLANTONIO, and JOHANNA H.A. VAN KONIJNENBURG-VAN CITTERT Kustatscher, E., Dellantonio, E., and Van Konijnenburg-van Cittert, J.H.A. 2014. The ferns of the late Ladinian, Middle Triassic flora from Monte Agnello, Dolomites, Italy. Acta Palaeontologica Polonica 59 (3): 741–755. Several fern remains are described from the para-autochthonous early late Ladinian flora of the Monte Agnello (Dolo- mites, N-Italy). The plants are preserved in subaerially deposited pyroclastic layers. Some ferns, known already from the Anisian and Ladinian of this area, are confirmed (Neuropteridium elegans), but several taxa are described for the first time (Phlebopteris fiemmensis sp. nov., Cladophlebis ladinica sp. nov., Chiropteris monteagnellii sp. nov.). Cladophle- bis sp. and some indeterminable fern remains cannot yet be assigned to any family. Phlebopteris fiemmensis is now the oldest formally established species in the genus. The fern family Dipteridaceae (Thaumatopteris sp. and some fragments probably belonging to the Dipteridaceae because of their venation) has not been recorded previously from European sediments as old as the Ladinian. Although stratigraphically attributed to the late Ladinian, the flora is markedly distinct from other Ladinian floras of the Dolomites and the Germanic Basin. The flora from Monte Agnello shows a higher di- versity in ferns than coeval floras from this area although characteristic elements of the Ladinian of the Dolomites such as Anomopteris and Gordonopteris are missing. The new flora misses also the Marattiales (e.g., Danaeopsis, Asterotheca) and other elements such as Sphenopteris schoenleiniana, typical for the Ladinian of the Germanic Basin. -
Chinaxiv:201711.01913V1 Poposauroid, Suchia
ChinaXiv合作期刊 第55卷 第2期 古 脊 椎 动 物 学 报 pp. 110-128 2017年4月 VERTEBRATA PALASIATICA figs. 1-4 New discoveries from the Sinokannemeyeria-Shansisuchus Assemblage Zone: 3. Archosauriformes from Linxian, Shanxi, China LIU Jun1,2 Corwin SULLIVAN1* (1 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 * Corresponding author: [email protected]) (2 University of Chinese Academy of Sciences Beijing 100039 [email protected]) Abstract The tetrapod assemblage from the Middle Triassic upper part of the Ermaying Formation of northern China has been known for two decades as the Sinokannemeyeria- Shansisuchus Assemblage because of the characteristic presence of the dicynodont therapsid Sinokannemeyeria and the erythrosuchid archosauriform Shansisuchus. Recently a Sinokannemeyeria species has been described from Member I of the Tongchuan Formation, which overlies the Ermaying, near Baidaoyu, Linxian, Shanxi Province. Here we document archosauriform specimens from the Baidaoyu site, including a partial Shansisuchus skeleton and some additional bones from probable suchian archosaurs, which constitute the first archosauriform material known from Member I of the Tongchuan. The most intriguing archosauriform specimens are a large ilium probably attributable to an unusual poposauroid, and a small, strangely shaped element that appears to represent a highly autapomorphic suchian calcaneum. Given the presence of both Sinokannemeyeria and Shansisuchus at Baidaoyu, the stratigraphic range of the Sinokannemeyeria-Shansisuchus Assemblage can be considered to extend upward into the Tongchuan Formation, although with possible changes in faunal composition. The occurrence of a poposauroid ilium at the Baidaoyu locality adds to the evidence that poposauroids diversified extensively during the Middle Triassic. -
SHRIMP U-Pb Zircon Dating of the Triassic Ermaying and Tongchuan Formations in Shanxi, China and Its Stratigraphic Implications
-168 第51卷 第2期 古 脊 椎 动 物 学 报 pp. 162 2013年4月 VERTEBRATA PALASIATICA figs. 1-3 SHRIMP U-Pb zircon dating of the Triassic Ermaying and Tongchuan formations in Shanxi, China and its stratigraphic implications LIU Jun LI Lu LI Xing-Wen (Key Laboratory of Vertebrate Evolution and Human Origin of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 [email protected]) Abstract Sensitive High Resolution Ion Microprobe (SHRIMP) U-Pb dating was carried out using zircons from tuffs in the Ermaying and Tongchuan formations of Shanxi, China. The results show weighted mean ages of 245.9±3.2 Ma for a sample from Member II of the Ermaying Formation, 243.1±3.9 Ma for a sample from Member I of the Tongchuan Formation, and 238.6±2.6 Ma and 234.6±6.5 Ma for two samples from the upper part of Member II of the Tongchuan Formation. These ages indicate that the lower part of the Ermaying Formation, which contains the Shaanbeikannemeyeria assemblage, is mostly likely Lower Triassic in age, whereas, the Tongchuan Formation is likely late Anisian to Ladinian, Middle Triassic. Key words Triassic, tuff, zircon dating 1 Introduction Correlating sedimentary strata from different facies, especially between the terrestrial and marine realms, poses a difficult challenge to geologists. Biochronology, which depends on the shared presence of particular fossils in the different strata to be correlated, is a common and useful method for approaching this problem. In some cases, however, no fossil that is useful for correlation exists in both sets of strata. -
Geology of the Coal and Petroleum Deposits in the Ordos Basin, China
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Geology of the coal and petroleum deposits in the Ordos basin, China by K. Y. Lee A digest of published literature Open-File Report 86-278 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1986 CONTENTS Page Abstract 1 Introduction 2 General statement 2 Regional setting 2 Purpose, method, and scope of the report 2 Stratigraphy 9 General statement 9 Triassic 9 General statement 9 Stratigraphic units 9 Stratigraphic relation with adjacent units 10 Jurassic 10 General statement 10 Stratigraphic units 11 Cretaceous 15 General statement 15 Stratigraphic units 15 Tectonics and evolution of the Ordos basin 17 Coal deposits 19 General statement 19 Triassic coal deposits 19 General statement 19 Tongchuan Formation 19 Hujiachun Formation 20 Yongping Formation 20 Wayaobao Formation 20 Depositional framework 23 Jurassic coal deposits 24 General statement 24 Fuxian Formation 24 Yanan Formation 24 Zhiluo Formation 28 Anding Formation 28 Depositional framework 29 Cretaceous coal deposits 30 Carboniferous and Permian coal deposits 30 General statement 30 Taiyuan Formation 30 Shanxi Formation 30 Depositional framework 33 Potential 33 Petroleum deposits 33 General statement 33 St rat igraphy 3 5 Source rocks 35 Reservoir rocks 38 Potential 38 Summary and conclusion 41 Measured sections 42 References cited 62 ILLUSTRATIONS Page Figure 1. Index map of China showing the location of study area 3 2. Sketch map of the Shaanganning (Ordos) basin 4 3. Generalized Mesozoic geologic map of the Ordos basin 5 4. Structural units and principal coal and petroleum fields in the Shaanganning (Ordos) basin 8 5. -
( Metoposaurus) Azerouali (Dutuit) Comb
Redescription of Arganasaurus ( Metoposaurus) azerouali (Dutuit) comb. nov. from the Upper Triassic of the Argana Basin (Morocco), and the first phylogenetic analysis of the Metoposauridae (Amphibia, Temnospondyli) Valentin Buffa, Nour-Eddine Jalil, J.-Sébastien Steyer To cite this version: Valentin Buffa, Nour-Eddine Jalil, J.-Sébastien Steyer. Redescription of Arganasaurus (Meto- posaurus) azerouali (Dutuit) comb. nov. from the Upper Triassic of the Argana Basin (Morocco), and the first phylogenetic analysis of the Metoposauridae (Amphibia, Temnospondyli). Special pa- pers in palaeontology, Wiley Blackwell Publishing, 2019, 5 (4), pp.699-717. 10.1002/spp2.1259. hal-02967815 HAL Id: hal-02967815 https://hal.sorbonne-universite.fr/hal-02967815 Submitted on 15 Oct 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Page 1 of 60 Palaeontology 1 2 3 REDESCRIPTION OF ARGANASAURUS (METOPOSAURUS) AZEROUALI (DUTUIT) 4 5 6 COMB. NOV. FROM THE LATE TRIASSIC OF THE ARGANA BASIN (MOROCCO), 7 8 AND THE FIRST PHYLOGENETIC ANALYSIS OF THE METOPOSAURIDAE 9 10