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South Africa's Coalfields — a 2014 Perspective
International Journal of Coal Geology 132 (2014) 170–254 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo South Africa's coalfields — A 2014 perspective P. John Hancox a,⁎,AnnetteE.Götzb,c a University of the Witwatersrand, School of Geosciences and Evolutionary Studies Institute, Private Bag 3, 2050 Wits, South Africa b University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa c Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation article info abstract Article history: For well over a century and a half coal has played a vital role in South Africa's economy and currently bituminous Received 7 April 2014 coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the Received in revised form 22 June 2014 production of a substantial percentage of the country's liquid fuels. It furthermore provides a considerable source Accepted 22 June 2014 of foreign revenue from exports. Available online 28 June 2014 Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review Keywords: Gondwana coal of their exploration and exploitation histories, general geology, coal seam nomenclature and coal qualities. With- Permian in the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability Triassic is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up Coalfield of Gondwana most of the coal-bearing successions were intruded by dolerite. -
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’’. -
A Phylogenetic Analysis of the Basal Ornithischia (Reptilia, Dinosauria)
A PHYLOGENETIC ANALYSIS OF THE BASAL ORNITHISCHIA (REPTILIA, DINOSAURIA) Marc Richard Spencer A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements of the degree of MASTER OF SCIENCE December 2007 Committee: Margaret M. Yacobucci, Advisor Don C. Steinker Daniel M. Pavuk © 2007 Marc Richard Spencer All Rights Reserved iii ABSTRACT Margaret M. Yacobucci, Advisor The placement of Lesothosaurus diagnosticus and the Heterodontosauridae within the Ornithischia has been problematic. Historically, Lesothosaurus has been regarded as a basal ornithischian dinosaur, the sister taxon to the Genasauria. Recent phylogenetic analyses, however, have placed Lesothosaurus as a more derived ornithischian within the Genasauria. The Fabrosauridae, of which Lesothosaurus was considered a member, has never been phylogenetically corroborated and has been considered a paraphyletic assemblage. Prior to recent phylogenetic analyses, the problematic Heterodontosauridae was placed within the Ornithopoda as the sister taxon to the Euornithopoda. The heterodontosaurids have also been considered as the basal member of the Cerapoda (Ornithopoda + Marginocephalia), the sister taxon to the Marginocephalia, and as the sister taxon to the Genasauria. To reevaluate the placement of these taxa, along with other basal ornithischians and more derived subclades, a phylogenetic analysis of 19 taxonomic units, including two outgroup taxa, was performed. Analysis of 97 characters and their associated character states culled, modified, and/or rescored from published literature based on published descriptions, produced four most parsimonious trees. Consistency and retention indices were calculated and a bootstrap analysis was performed to determine the relative support for the resultant phylogeny. The Ornithischia was recovered with Pisanosaurus as its basalmost member. -
The Sauropodomorph Biostratigraphy of the Elliot Formation of Southern Africa: Tracking the Evolution of Sauropodomorpha Across the Triassic–Jurassic Boundary
Editors' choice The sauropodomorph biostratigraphy of the Elliot Formation of southern Africa: Tracking the evolution of Sauropodomorpha across the Triassic–Jurassic boundary BLAIR W. MCPHEE, EMESE M. BORDY, LARA SCISCIO, and JONAH N. CHOINIERE McPhee, B.W., Bordy, E.M., Sciscio, L., and Choiniere, J.N. 2017. The sauropodomorph biostratigraphy of the Elliot Formation of southern Africa: Tracking the evolution of Sauropodomorpha across the Triassic–Jurassic boundary. Acta Palaeontologica Polonica 62 (3): 441–465. The latest Triassic is notable for coinciding with the dramatic decline of many previously dominant groups, followed by the rapid radiation of Dinosauria in the Early Jurassic. Among the most common terrestrial vertebrates from this time, sauropodomorph dinosaurs provide an important insight into the changing dynamics of the biota across the Triassic–Jurassic boundary. The Elliot Formation of South Africa and Lesotho preserves the richest assemblage of sauropodomorphs known from this age, and is a key index assemblage for biostratigraphic correlations with other simi- larly-aged global terrestrial deposits. Past assessments of Elliot Formation biostratigraphy were hampered by an overly simplistic biozonation scheme which divided it into a lower “Euskelosaurus” Range Zone and an upper Massospondylus Range Zone. Here we revise the zonation of the Elliot Formation by: (i) synthesizing the last three decades’ worth of fossil discoveries, taxonomic revision, and lithostratigraphic investigation; and (ii) systematically reappraising the strati- graphic provenance of important fossil locations. We then use our revised stratigraphic information in conjunction with phylogenetic character data to assess morphological disparity between Late Triassic and Early Jurassic sauropodomorph taxa. Our results demonstrate that the Early Jurassic upper Elliot Formation is considerably more taxonomically and morphologically diverse than previously thought. -
A Revision of the Upper Triassic Ornithischian Dinosaur Revueltosaurus, with a Description of a New Species
Heckert, A.B" and Lucas, S.O., eds., 2002, Upper Triassic Stratigraphy and Paleontology. New Mexico Museum of Natural History & Science Bulletin No.2 J. 253 A REVISION OF THE UPPER TRIASSIC ORNITHISCHIAN DINOSAUR REVUELTOSAURUS, WITH A DESCRIPTION OF A NEW SPECIES ANDREW B. HECKERT New Mexico Museum of Natural History, 1801 Mountain Road NW, Albuquerque, NM 87104-1375 Abstract-Ornithischian dinosaur body fossils are extremely rare in Triassic rocks worldwide, and to date the majority of such fossils consist of isolated teeth. Revueltosaurus is the most common Upper Triassic ornithischian dinosaur and is known from Chinle Group strata in New Mexico and Arizona. Historically, all large (>1 cm tall) and many small ornithischian dinosaur teeth from the Chinle have been referred to the type species, Revueltosaurus callenderi Hunt. A careful re-examination of the type and referred material of Revueltosaurus callenderi reveals that: (1) R. callenderi is a valid taxon, in spite of cladistic arguments to the contrary; (2) many teeth previously referred to R. callenderi, particularly from the Placerias quarry, instead represent other, more basal, ornithischians; and (3) teeth from the vicinity of St. Johns, Arizona, and Lamy, New Mexico previously referred to R. callenderi pertain to a new spe cies, named Revueltosaurus hunti here. R. hunti is more derived than R. callenderi and is one of the most derived Triassic ornithischians. However, detailed biostratigraphy indicates that R. hunti is older (Adamanian: latest Carnian) than R. callenderi (Revueltian: early-mid Norian). Both taxa have great potential as index taxa of their respective faunachrons and support existing biochronologies based on other tetrapods, megafossil plants, palynostratigraphy, and lithostratigraphy. -
Guides Level Ii Manual 2005 December
GUIDING LEVEL II A TRAINING MANUAL DESIGNED TO ASSIST WITH PREPARATION FOR THE FGASA LEVEL II AND TRAILS GUIDE EXAMS All rights reserved. No part of the material may be reproduced or utilized in any form or by any means, electronic or mechanical including photocopying, recording or by an information storage retrieval system, without the written permission of Lee Gutteridge. (INCLUDING MORE THAN FOUR HUNDRED PHOTOS AND DIAGRAMS) COMPILED BY LEE GUTTERIDGE THIS STUDY MATERIAL CONFORMS TO THE SYLLABUS SET BY FGASA FOR THE LEVEL II EXAMS AND IS APPROVED BY PROFESSOR W.VAN HOVEN OF THE CENTRE FOR WILDLIFE MANAGEMENT AT THE UNIVERSITY OF PRETORIA P.O. Box 441, Mookgopong, 0560, Limpopo, South Africa. Cell 083 667 7586 2 LEVEL TWO TRAINING MANUAL This manual has been compiled from the perspective of a guide in the field. In writing it I asked myself what can I use on a game drive, or game walk as regards information. These aspects covered in this manual will give the guide good, interesting and factual information for direct discussion with the guest. No one book will cover every aspect so here I have included sections on the following topics. 1. Ecology 2. Mammals 3. Birds 4. Reptiles and Amphibians 5. Astronomy 6. Botany 7. Insects, Arachnids and their relatives 8. Geology and Climatology 9. Fish 10. Survival 11. AWH and VPDA The problem for guides is not always finding the answers, but also what is the question to be researched in the first place? It is difficult for a guide to pre-empt what guests will ask them over their guiding careers, but many of the questions and answers which will come into play have been covered here. -
Large Tridactyl Dinosaur Tracks from the Early Jurassic of Southern Gondwana – Uppermost Elliot Formation, Upper Moyeni, Lesotho
Annales Societatis Geologorum Poloniae (2020), vol. 90: 1 – 26 doi: https://doi.org/10.14241/asgp.2020.07 LARGE TRIDACTYL DINOSAUR TRACKS FROM THE EARLY JURASSIC OF SOUTHERN GONDWANA – UPPERMOST ELLIOT FORMATION, UPPER MOYENI, LESOTHO Miengah ABRAHAMS 1, Lara SCISCIO 1,2, Mhairi REID 1,3, T’Nielle HAUPT 1 & Emese M. BORDY 1* 1 Department of Geological Sciences, University of Cape Town, Rondebosch 7701, South Africa; e-mails: [email protected]; [email protected]; [email protected]; [email protected]; [email protected] 2 Current address: Department of Geology, University of Johannesburg, Kingsway and Auckland Park, 2006 Johannesburg, South Africa 3 Current address: Department of Geology, University of Oxford, Oxford, England *Corresponding author Abrahams, M., Sciscio L., Reid, M., Haupt, T. & Bordy, E. M., 2020. Large tridactyl dinosaur tracks from the Early Jurassic of southern Gondwana – uppermost Elliot Formation, Upper Moyeni, Lesotho. Annales Societatis Geologorum Poloniae, 90: 1 – 26. Abstract: A new ichnosite in southwest Lesotho (Upper Moyeni, Quthing District) is located within the uppermost part of the highly fossiliferous Elliot Formation, ~35 m below the conformably overlying Clarens Formation and ~65 m above the world-renowned Lower Moyeni ichnosite. While the Lower Moyeni site preserves diverse Early Jurassic ichnofossils, the ichnites at Upper Moyeni comprise one vertebrate burrow and ~50 tridactyl tracks with footprint lengths between 15 and 51 cm. Many of the tracks preserve digital pad impressions, claw marks and displacement rims, all related to substrate conditions. The morphometric parameters of the Upper Moyeni tracks are consistent with Grallator, Eubrontes and Kayentapus. -
Lesothosaurus, "Fabrosaurids," and the Early Evolution of Ornithischia Author(S): Paul C
Lesothosaurus, "Fabrosaurids," and the Early Evolution of Ornithischia Author(s): Paul C. Sereno Source: Journal of Vertebrate Paleontology, Vol. 11, No. 2 (Jun. 20, 1991), pp. 168-197 Published by: Taylor & Francis, Ltd. on behalf of The Society of Vertebrate Paleontology Stable URL: https://www.jstor.org/stable/4523370 Accessed: 28-01-2019 13:42 UTC JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at https://about.jstor.org/terms The Society of Vertebrate Paleontology, Taylor & Francis, Ltd. are collaborating with JSTOR to digitize, preserve and extend access to Journal of Vertebrate Paleontology This content downloaded from 69.80.65.67 on Mon, 28 Jan 2019 13:42:40 UTC All use subject to https://about.jstor.org/terms Journal of Vertebrate Paleontology 11(2): 168-197, June 1991 © 1991 by the Society of Vertebrate Paleontology LESOTHOSAURUS, "FABROSAURIDS," AND THE EARLY EVOLUTION OF ORNITHISCHIA PAUL C. SERENO Department of Organismal Biology and Anatomy, University of Chicago, 1025 E. 57th Street, Chicago, Illinois 60637 ABSTRACT -New materials of Lesothosaurus diagnosticus permit a detailed understanding of one of the earliest and most primitive ornithischians. Skull proportions and sutural relations can be discerned from several articulated and disarticulated skulls. The snout is proportionately long with a vascularized, horn-covered tip. -
Annual Report 2011
Natural and Agricultural Sciences Annual Report 2011 Natural and Agricultural Sciences Annual Report 2011 Contact Details Dean Prof Neil Heideman +27 (0)51 401 2322 [email protected] Vice-Dean Prof. Corli Witthuhn +27 (0) 51 4013855 [email protected] Faculty Manager Mr Johan Kruger +27 (0)51 401 2409 Issued by [email protected] Faculty of Natural and Agricultural Sciences Marketing Manager University of the Free State Ms Elfrieda Lotter Editorial Compilation +27 (0)51 4012531 [email protected] Betta van Huyssteen Physical Address Language Revision Room 9A, Biology Building, Main Campus, Bloemfontein Betta van Huyssteen Stella Mcgill Postal Address Revision of Bibliographical Data University of the Free State PO Box 339 Mercia Coetzee Bloemfontein Design, Layout South Africa 9300 Chrysalis Advertising & Publishing Fax: +27 (0)51 401 3728 Printing E-mail: [email protected] Oranje Drukkery • Printers Faculty website: www.ufs.ac.za/natagri Table of Contents Preface 5 Research Clusters 6 Agricultural Sciences 13 Agricultural Economics 14 Animal, Wildlife and Grassland Sciences 20 Plant Sciences 30 Soil, Crop and Climate Sciences 40 Building Sciences 49 Architecture 50 Quantity Surveying and Construction Management 56 Urban and Regional Planning 62 Natural Sciences 67 Chemistry 68 Computer Science and Informatics 86 Consumer Science 94 Genetics 100 Geography 108 Geology 116 Mathematical Statistics and Actuarial Science 126 Mathematics and Applied Mathematics 132 Microbial, Biochemical and Food Biotechnology 136 Physics 150 Zoology -
South Africa's Coalfields – a 2014 Perspective
South Africa's coalfields – a 2014 perspective 1Hancox, P. John and 2,3Götz, Annette E. 1University of the Witwatersrand, School of Geosciences, Private Bag 3, 2050 Wits, South Africa; [email protected] 2University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa; [email protected] 3Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation Highlights • South Africa’s Coalfields are presented. • The role of Gondwanan coals as palaeoclimate archives is stated. • Future research fields include palynology, sequence stratigraphy, basin fill. Abstract For well over a century and a half coal has played a vital role in South Africa’s economy and currently bituminous coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the production of a substantial percentage of the country’s liquid fuels. It furthermore provides a considerable source of foreign revenue from exports. Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review of their exploration and exploitation histories, general geology, and coal seam nomenclature and coal qualities. Within the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up of Gondwana most of the coals bearing successions were intruded by dolerite. These intrusions are important as they may cause devolatilisation and burning of the coal, create structural disturbances and related seam correlation problems, and difficulties in mining operations. -
Research Report 2009
Rhodes Front Cover 3/7/11 2:26 PM Page 1 C M Y CM MY CY CMY K Research Office Rhodes University www.ru.ac.za [email protected] Telephone: +27 (0) 46 603 8936 Composite Rhodes - Intro 4/3/11 8:59 AM Page 1 C M Y CM MY CY CMY K Research Report 2009 Composite Rhodes - Intro 4/3/11 8:59 AM Page 2 C M Y CM MY CY CMY K table of contents Foreword from the Vice-Chancellor - Dr Saleem Badat 5 Introduction from the Deputy Vice-Chancellor: Research and Development - Dr Peter Clayton 7 The Vice-Chancellor’s Research Awards - Remarkable young scholar honoured for her research in African Art Professor Ruth Simbao 8 - Second Distinguished Research Award for Top Scientist Professor William Froneman 12 - Distinguished Researcher Medal for leading literary scholar Professor Laurence Wright 16 - Book Award winner offers a fresh perspective on violence Professor Leonhard Praeg 20 A few snapshots of Research at Rhodes - Theoretical research into iconospheric models has significant real world impact 24 - In conversation with Professor Tebello Nyokong’s students 28 - BioBRU launches and soars 32 - Biodiversity high on the Rhodes research agenda 36 - Adolescent sexual and reproductive health research 40 Top Researchers: Acknowledgements 44 Publications from the Vice Chancellorate 45 Departmental Index Accounting 47 Anthropology 51 Biochemistry, Microbiology and Biotechnology 57 Botany 69 Chemistry 77 Centre for Higher Education Research, Teaching & Learning (CHERTL) 91 Computer Science 97 Drama 107 Economics 113 Education 119 Electron Microscopy Unit -
A New Basal Ornithopod Dinosaur from the Lower Cretaceous of China
A new basal ornithopod dinosaur from the Lower Cretaceous of China Yuqing Yang1,2,3, Wenhao Wu4,5, Paul-Emile Dieudonné6 and Pascal Godefroit7 1 College of Resources and Civil Engineering, Northeastern University, Shenyang, Liaoning, China 2 College of Paleontology, Shenyang Normal University, Shenyang, Liaoning, China 3 Key Laboratory for Evolution of Past Life and Change of Environment, Province of Liaoning, Shenyang Normal University, Shenyang, Liaoning, China 4 Key Laboratory for Evolution of Past Life and Environment in Northeast Asia, Ministry of Education, Jilin University, Changchun, Jilin, China 5 Research Center of Paleontology and Stratigraphy, Jilin University, Changchun, Jilin, China 6 Instituto de Investigación en Paleobiología y Geología, CONICET, Universidad Nacional de Río Negro, Rio Negro, Argentina 7 Directorate ‘Earth and History of Life’, Royal Belgian Institute of Natural Sciences, Brussels, Belgium ABSTRACT A new basal ornithopod dinosaur, based on two nearly complete articulated skeletons, is reported from the Lujiatun Beds (Yixian Fm, Lower Cretaceous) of western Liaoning Province (China). Some of the diagnostic features of Changmiania liaoningensis nov. gen., nov. sp. are tentatively interpreted as adaptations to a fossorial behavior, including: fused premaxillae; nasal laterally expanded, overhanging the maxilla; shortened neck formed by only six cervical vertebrae; neural spines of the sacral vertebrae completely fused together, forming a craniocaudally-elongated continuous bar; fused scapulocoracoid with prominent