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New Heterodontosaurid Remains from the Cañadón Asfalto Formation: Cursoriality and the Functional Importance of the Pes in Small Heterodontosaurids
Journal of Paleontology, 90(3), 2016, p. 555–577 Copyright © 2016, The Paleontological Society 0022-3360/16/0088-0906 doi: 10.1017/jpa.2016.24 New heterodontosaurid remains from the Cañadón Asfalto Formation: cursoriality and the functional importance of the pes in small heterodontosaurids Marcos G. Becerra,1 Diego Pol,1 Oliver W.M. Rauhut,2 and Ignacio A. Cerda3 1CONICET- Museo Palaeontológico Egidio Feruglio, Fontana 140, Trelew, Chubut 9100, Argentina 〈[email protected]〉; 〈[email protected]〉 2SNSB, Bayerische Staatssammlung für Paläontologie und Geologie and Department of Earth and Environmental Sciences, LMU München, Richard-Wagner-Str. 10, Munich 80333, Germany 〈[email protected]〉 3CONICET- Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, Museo Carlos Ameghino, Belgrano 1700, Paraje Pichi Ruca (predio Marabunta), Cipolletti, Río Negro, Argentina 〈[email protected]〉 Abstract.—New ornithischian remains reported here (MPEF-PV 3826) include two complete metatarsi with associated phalanges and caudal vertebrae, from the late Toarcian levels of the Cañadón Asfalto Formation. We conclude that these fossil remains represent a bipedal heterodontosaurid but lack diagnostic characters to identify them at the species level, although they probably represent remains of Manidens condorensis, known from the same locality. Histological features suggest a subadult ontogenetic stage for the individual. A cluster analysis based on pedal measurements identifies similarities of this specimen with heterodontosaurid taxa and the inclusion of the new material in a phylogenetic analysis with expanded character sampling on pedal remains confirms the described specimen as a heterodontosaurid. Finally, uncommon features of the digits (length proportions among nonungual phalanges of digit III, and claw features) are also quantitatively compared to several ornithischians, theropods, and birds, suggesting that this may represent a bipedal cursorial heterodontosaurid with gracile and grasping feet and long digits. -
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. -
By in the Spring of 1929, I Had the Privilege of Acting As Guide To
O n a S o u t h A fr ic a n M a m m a l -l ik e R e p t il e , B a u r i a c y n o p s . By Lieuwe D. Boonstra (South African Museum, Capetown). With 8 textfigures. (Eingelangt am 18. Dezember 1934.) In the spring of 1929, I had the privilege of acting as guide to Professor and Frau Abel on a short collecting trip in the Great Karroo. When the opportunity was offered me of contributing to the number of Palaeobiologica which is to be issued in honor of Professor Abel’s sixtieth birthday,I recalled with pleasure the time we had spent together. When Professor Abel reads this account of a very interesting reptile from the Karroo, I hope that he may have equally pleasant recollections of our donkey-cart excursions in the Great Karroo of South Africa. On working through the collection of Karroo reptiles which had been sold to the American Museum of Natural History by Dr. R. B room in 1913, I came across some interesting remains of a Bauriamorph. Under the number Amer. Mus. 5622, there is catalogued a good skull, a hind-foot and some limb-bones from the Cynognathus zone at Winnaarsbaken. The skull was first described and figured by B room in 1911. In 1913, and again in 1915, the lateral view was republished. In 1914, sections through the sphen- ethmoidal and prootic regions were published by the same author. When the skull first came under my notice, it had a mass of matrix, containing some limb-bones, attached to the preorbital sur face of the snout; the teeth of the left side were partly exposed; parts of the basicranium were cleaned; the matrix on the dorsal surface had been removed in a rough manner, so that part of the D. -
Maceral Types and Quality of Coal in the Tuli Coalfield: a Case
applied sciences Article Maceral Types and Quality of Coal in the Tuli Coalfield: A Case Study of Coal in the Madzaringwe Formation in the Vele Colliery, Limpopo Province, South Africa Elelwani Denge * and Christopher Baiyegunhi Department of Geology and Mining, University of Limpopo, Private Bag X1106, Sovenga 0727, South Africa; [email protected] * Correspondence: [email protected] Featured Application: Authors are encouraged to provide a concise description of the specific application or a potential application of the work. This section is not mandatory. Abstract: The Madzaringwe Formation in the Vele colliery is one of the coal-bearing Late Palaeozoic units of the Karoo Supergroup, consisting of shale with thin coal seams and sandstones. Maceral group analysis was conducted on seven representative coal samples collected from three existing boreholes—OV125149, OV125156, and OV125160—in the Vele colliery to determine the coal rank and other intrinsic characteristics of the coal. The petrographic characterization revealed that vitrinite is the dominant maceral group in the coals, representing up to 81–92 vol.% (mmf) of the total sample. Collotellinite is the dominant vitrinite maceral, with a total count varying between 52.4 vol.% (mmf) and 74.9 vol.% (mmf), followed by corpogelinite, collodetrinite, tellinite, and pseudovitrinite with a Citation: Denge, E.; Baiyegunhi, C. count ranging between 0.8 and 19.4 vol.% (mmf), 1.5 and 17.5 vol.% (mmf), 0.8 and 6.5 vol.% (mmf) Maceral Types and Quality of Coal in the Tuli Coalfield: A Case Study of and 0.3 and 5.9 vol.% (mmf), respectively. The dominance of collotellinite gives a clear indication Coal in the Madzaringwe Formation that the coals are derived from the parenchymatous and woody tissues of roots, stems, and leaves. -
Osteohistology of Late Triassic Prozostrodontian Cynodonts from Brazil
Osteohistology of Late Triassic prozostrodontian cynodonts from Brazil Jennifer Botha-Brink1,2, Marina Bento Soares3 and Agustín G. Martinelli3 1 Department of Karoo Palaeontology, National Museum, Bloemfontein, South Africa 2 Department of Zoology and Entomology, University of the Free State, Bloemfontein, South Africa 3 Departamento de Paleontologia e Estratigrafia, Instituto de Geociências, Universidade Federal do Rio Grande do Sul, Porto Alegre, Brazil ABSTRACT The Prozostrodontia includes a group of Late Triassic-Early Cretaceous eucynodonts plus the clade Mammaliaformes, in which Mammalia is nested. Analysing their growth patterns is thus important for understanding the evolution of mammalian life histories. Obtaining material for osteohistological analysis is difficult due to the rare and delicate nature of most of the prozostrodontian taxa, much of which comprises mostly of crania or sometimes even only teeth. Here we present a rare opportunity to observe the osteohistology of several postcranial elements of the basal prozostrodontid Prozostrodon brasiliensis, the tritheledontid Irajatherium hernandezi, and the brasilodontids Brasilodon quadrangularis and Brasilitherium riograndensis from the Late Triassic of Brazil (Santa Maria Supersequence). Prozostrodon and Irajatherium reveal similar growth patterns of rapid early growth with annual interruptions later in ontogeny. These interruptions are associated with wide zones of slow growing bone tissue. Brasilodon and Brasilitherium exhibit a mixture of woven-fibered bone tissue and slower growing parallel-fibered and lamellar bone. The slower growing bone tissues are present even during early ontogeny. The relatively slower growth in Brasilodon and Brasilitherium may be related to their small body size compared to Prozostrodon and Irajatherium. These brasilodontids also exhibit osteohistological similarities with the Late Triassic/Early Jurassic mammaliaform Morganucodon and the Late Cretaceous multituberculate mammals Kryptobaatar and Nemegtbaatar. -
Physical and Environmental Drivers of Paleozoic Tetrapod Dispersal Across Pangaea
ARTICLE https://doi.org/10.1038/s41467-018-07623-x OPEN Physical and environmental drivers of Paleozoic tetrapod dispersal across Pangaea Neil Brocklehurst1,2, Emma M. Dunne3, Daniel D. Cashmore3 &Jӧrg Frӧbisch2,4 The Carboniferous and Permian were crucial intervals in the establishment of terrestrial ecosystems, which occurred alongside substantial environmental and climate changes throughout the globe, as well as the final assembly of the supercontinent of Pangaea. The fl 1234567890():,; in uence of these changes on tetrapod biogeography is highly contentious, with some authors suggesting a cosmopolitan fauna resulting from a lack of barriers, and some iden- tifying provincialism. Here we carry out a detailed historical biogeographic analysis of late Paleozoic tetrapods to study the patterns of dispersal and vicariance. A likelihood-based approach to infer ancestral areas is combined with stochastic mapping to assess rates of vicariance and dispersal. Both the late Carboniferous and the end-Guadalupian are char- acterised by a decrease in dispersal and a vicariance peak in amniotes and amphibians. The first of these shifts is attributed to orogenic activity, the second to increasing climate heterogeneity. 1 Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK. 2 Museum für Naturkunde, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Invalidenstraße 43, 10115 Berlin, Germany. 3 School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK. 4 Institut -
ON BA U RIA C YNOP S BROOM by A. S. BRINK Bauria Cynops Broom
ON BA U RIA C YNOP S BROOM By A. S. BRINK ABSTRACT Descriptions of this genus and species, the type of an infraorder, have thus far been based on three individuals. The type in the South African Museum, Cape Town is a complete skull, but somewhat unsatisfactorily preserved and cleaned. The second specimen in the American Museum of Natural History, New York, is a good skull with a portion of the skeleton, but the skull has been damaged in the course of preparation. The third specimen is in the Bernard Price Institute. It is an exceptionally fine specimen, but was only superficially cleaned when described. This specimen also includes a portion of the skeleton. Two additional complete skulls, one somewhat crushed, have since been added to the Bernard Price Institute's collection. This paper describes Bauria cynops Broom on information derived from all five specimens. Illustrations are based on the three specimens in this Institute. Attention h also given to the position of this infraorder relative to other related groups. INTRODUCTION Bauria cynops Broom is a classic Karroo therapsid, the type of the important infraorder Bauriamorpha. The name was introduced by Broom in 1909 and for ~alf a century the infraorder enjoyed a great deal of attention, despite the fact that the type genus is still rather inadequately known. There would appear to be little excuse for this peculiar situation when it is considered that past descrip tions have been based on three different specimens which could pass as complete or relatively complete skulls, two with partial skeletons. To these three indivi duals a fou.-th and a fifth skull are now added. -
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. -
The Stratigraphy of the Ohio Range, Antarctica
This dissertation has been 65—1200 microfilmed exactly as received LONG, William Ellis, 1930- THE STRATIGRAPHY OF THE OHIO RANGE, ANTARCTICA. The Ohio State University, Ph.D., 1964 G eology University Microfilms, Inc., Ann Arbor, Michigan THE STRATIGRAPHY OF THE OHIO RANGE, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By William Ellis Long, B.S., Rl.S. The Ohio State University 1964 Approved by A (Miser Department of Geology PLEASE NOTE: Figure pages are not original copy* ' They tend tc "curl11. Filled in the best way possible. University Microfilms, Inc. Frontispiece. The Ohio Range, Antarctica as seen from the summit of ITIt. Glossopteris. The cliffs of the northern escarpment include Schulthess Buttress and Darling Ridge. The flat area above the cliffs is the Buckeye Table. ACKNOWLEDGMENTS The preparation of this paper is aided by the supervision and advice of Dr. R. P. Goldthwait and Dr. J. M. Schopf. Dr. 5. B. Treves provided petrographic advice and Dir. G. A. Doumani provided information con cerning the invertebrate fossils. Invaluable assistance in the fiBld was provided by Mr. L. L. Lackey, Mr. M. D. Higgins, Mr. J. Ricker, and Mr. C. Skinner. Funds for this study were made available by the Office of Antarctic Programs of the National Science Foundation (NSF grants G-13590 and G-17216). The Ohio State Univer sity Research Foundation and Institute of Polar Studies administered the project (OSURF Projects 1132 and 1258). Logistic support in Antarctica was provided by the United States Navy, especially Air Development Squadron VX6. -
Proceedings of the 18Th Biennial Conference of the Palaeontological Society of Southern Africa Johannesburg, 11–14 July 2014
Proceedings of the 18th Biennial Conference of the Palaeontological Society of Southern Africa Johannesburg, 11–14 July 2014 Table of Contents Letter of Welcome· · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · 63 Programme · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · 64 · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · 66 Hand, K.P., Bringing Two Worlds Together: How Earth’s Past and Present Help Us Search for Life on Other Planets · · · · · · · 66 · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · 67 Erwin, D.H., Major Evolutionary Transitions in Early Life: A Public Goods Approach · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · 67 Lelliott, A.D., A Survey of Visitors’ Experiences of Human Origins at the Cradle of Humankind, South Africa· · · · · · · · · · · · · · 68 Looy, C., The End-Permian Biotic Crisis: Why Plants Matter · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · · 69 Reed, K., Hominin Evolution and Habitat: The Importance of Analytical Scale · · · · · · · · · · · · · · · · · · · · · · · · · · · · · -
Variability of the Parietal Foramen and the Evolution of the Pineal Eye in South African Permo-Triassic Eutheriodont Therapsids
The sixth sense in mammalian forerunners: Variability of the parietal foramen and the evolution of the pineal eye in South African Permo-Triassic eutheriodont therapsids JULIEN BENOIT, FERNANDO ABDALA, PAUL R. MANGER, and BRUCE S. RUBIDGE Benoit, J., Abdala, F., Manger, P.R., and Rubidge, B.S. 2016. The sixth sense in mammalian forerunners: Variability of the parietal foramen and the evolution of the pineal eye in South African Permo-Triassic eutheriodont therapsids. Acta Palaeontologica Polonica 61 (4): 777–789. In some extant ectotherms, the third eye (or pineal eye) is a photosensitive organ located in the parietal foramen on the midline of the skull roof. The pineal eye sends information regarding exposure to sunlight to the pineal complex, a region of the brain devoted to the regulation of body temperature, reproductive synchrony, and biological rhythms. The parietal foramen is absent in mammals but present in most of the closest extinct relatives of mammals, the Therapsida. A broad ranging survey of the occurrence and size of the parietal foramen in different South African therapsid taxa demonstrates that through time the parietal foramen tends, in a convergent manner, to become smaller and is absent more frequently in eutherocephalians (Akidnognathiidae, Whaitsiidae, and Baurioidea) and non-mammaliaform eucynodonts. Among the latter, the Probainognathia, the lineage leading to mammaliaforms, are the only one to achieve the complete loss of the parietal foramen. These results suggest a gradual and convergent loss of the photoreceptive function of the pineal organ and degeneration of the third eye. Given the role of the pineal organ to achieve fine-tuned thermoregulation in ecto- therms (i.e., “cold-blooded” vertebrates), the gradual loss of the parietal foramen through time in the Karoo stratigraphic succession may be correlated with the transition from a mesothermic metabolism to a high metabolic rate (endothermy) in mammalian ancestry. -
Rehabilitation of National Route R61 (Section 3, Km 24.2 to Km 75) Between Cradock and Tarkastad, Eastern Cape
PALAEONTOLOGICAL HERITAGE STUDY: COMBINED DESKTOP AND FIELD-BASED ASSESSMENT Rehabilitation of National Route R61 (Section 3, km 24.2 to km 75) between Cradock and Tarkastad, Eastern Cape John E. Almond PhD (Cantab.) Natura Viva cc, PO Box 12410 Mill Street, Cape Town 8010, RSA [email protected] February 2013 1. SUMMARY The South African National Roads Agency Limited (SANRAL) is proposing to rehabilitate Section 3 of the National Route R61 (km 24.2 to km 75) between Cradock and Tarkastad, Eastern Cape. The project involves widening of the roadway and of all stormwater structures along the route. Road material is to be sourced from five new or existing borrow pits and one hard rock quarry. A Phase 1 palaeontological heritage assessment for the road project has been commissioned by Arcus GIBB (Pty) Ltd in accordance with the requirements of the National Heritage Resources Act (Act 25 of 1999). Section 3 of the R61 traverses the outcrop area of continental sedimentary rocks of the Upper Beaufort Group (Tarkastad Subgroup, Karoo Supergroup) of Early to Middle Triassic age. These are cut and baked by numerous dolerite intrusions of the Karoo Dolerite Suite of Early Jurassic age. Towards Cradock (Graaff-Reinet and Middelburg 1: 250 000 sheet areas) the sedimentary bedrocks belong to the sandstone-dominated Katberg Formation that was deposited in arid braided fluvial settings following the catastrophic end-Permian mass extinction event. Further east towards Tarkastad (Queenstown and King William’s Town 1: 250 000 sheet areas) the sedimentary bedrocks are assigned to the slightly younger Burgersdorp Formation comprising recessive-weathering reddish mudrocks and braided river channel sandstones.