South Africa's 200 Million-Year Old Heavyweight

Total Page:16

File Type:pdf, Size:1020Kb

South Africa's 200 Million-Year Old Heavyweight various specimens of bipeds and quadrupeds. They found that Ledumahadi, like quadrupeds, had proportionally thicker forelimbs. Osteohistology, the study of bone tissue, was used to calculate the age of the dinosaur when it died. By closely observing the fossil bone tissue and the growth lines of the bones, Dr Botha-Brink, a vertebrate palaeontologist from the National Museum in Bloemfontein, determined that Ledumahadi was an adult of about 14 years of age when it died, that its growth was slowing in the final years of its life. Finally, to find out when Ledumahadi lived, the rock types and layers where it was found were compared to other areas in the world. Dr Bordy, Associate Professor in the Department of Geological Sciences at the University of Cape Town, found that Ledumahadi had died on a vegetated floodplain in a semi-arid environment Ledumahadi mafube is the first of the true giant much like the present-day Karoo. sauropods of the Jurassic. Quadrupedal postures with flexed limbs potentially evolved several times in sauropodomorph dinosaurs before the evolution of New Ideas on Big Dinosaurs derived, columnar-limbed postures of Sauropoda. The excavation and study of Ledumahadi mafube has led to some new ideas about big dinosaurs and What Ledumahadi mafube may have looked like. Another South African dinosaur, how they lived. For example Ledumahadi enabled Heterodontosaurus tucki, watches in the foreground. Copyright Viktor Radermacher the researchers to deduce that the truly gigantic The excavation and study of Ledumahadi mafube dinosaurs had evolved at least 10 million years earlier was undertaken by a joint research team of scientists than originally thought. The fact that Ledumahadi from South Africa, which included Dr Choiniere, Dr evolved its huge body size and quadrupedal posture Blair McPhee, Dr Jennifer Botha-Brink and Dr Emese independently of other sauropod giants suggests Bordy, and Professor Roger Benson from Oxford that their evolution was considerably more dynamic South Africa’s University in the UK. Funding for the project came than previously thought, with multiple ‘experiments’ from the National Research Foundation and the into four-legged stances. Ledumahadi is also one of 200 Million-Year Old Heavyweight Palaeontological Scientific Trust (PAST). the first dinosaurs to evolve after the mass extinction more than 200 million years ago and shows how Putting the Puzzle Pieces Together rapidly dinosaurs regained enormous body sizes. wice the size of an adult African Lecheko, a guide based at the Mehloding To determe size, shape and other characteristics of elephant, standing four metres high Community Trust near Matatiele. It is a close Ledumahadi, the team compared it to the fossils of Ledumahadi is closely related to another large at the hips and weighing in at 12 relative of sauropod dinosaurs, such as the other known species held in South African sauropod tonnes, this was once the largest land Brontosaurus, was a plant eater and stood on collections all over the world. called Antetonitrus, but also animal on Earth. Ledumahadi mafube, four legs. Some of its fossilised remains were to species from Argentina of Ta dinosaur that lived in the region now known as originally discovered 30 years ago in the Clarens To determe its weight, Ledumahadi approximately the same age. the Free State 200 million years ago, has become area of the Free State. Stored in the Wits archive, they took into account the This further supports the idea the latest discovery by an international team of they were only rediscovered in 2000. The full circumference of its thigh bone had died on that the Earth’s continents scientists led by palaeontologist Professor Jonah excavation of the dinosaur was completed in 2016 (femur) which suggested a a vegetated were once connected in a Choiniere from the University of the Witwatersrand. although the last bone, a finger, was discovered very heavy animal. To develop massive landmass called accidently in 2017 and provided the scientists with an idea of its posture, the floodplain Pangaea and shows how Ledumahadi mafube means “a giant thunderclap critical information on the uniqueness of the new team visited various museums easily dinosaurs could have at dawn” in Sesotho and was named by Puseletso specimen. around the world to measure walked from place to place. 4 January 2019 | SCIENCE MATTERS SCIENCE MATTERS | January 2019 5.
Recommended publications
  • Studies on Continental Late Triassic Tetrapod Biochronology. I. the Type Locality of Saturnalia Tupiniquim and the Faunal Succession in South Brazil
    Journal of South American Earth Sciences 19 (2005) 205–218 www.elsevier.com/locate/jsames Studies on continental Late Triassic tetrapod biochronology. I. The type locality of Saturnalia tupiniquim and the faunal succession in south Brazil Max Cardoso Langer* Departamento de Biologia, FFCLRP, Universidade de Sa˜o Paulo (USP), Av. Bandeirantes 3900, 14040-901 Ribeira˜o Preto, SP, Brazil Received 1 November 2003; accepted 1 January 2005 Abstract Late Triassic deposits of the Parana´ Basin, Rio Grande do Sul, Brazil, encompass a single third-order, tetrapod-bearing sedimentary sequence that includes parts of the Alemoa Member (Santa Maria Formation) and the Caturrita Formation. A rich, diverse succession of terrestrial tetrapod communities is recorded in these sediments, which can be divided into at least three faunal associations. The stem- sauropodomorph Saturnalia tupiniquim was collected in the locality known as ‘Waldsanga’ near the city of Santa Maria. In that area, the deposits of the Alemoa Member yield the ‘Alemoa local fauna,’ which typifies the first association; includes the rhynchosaur Hyperodapedon, aetosaurs, and basal dinosaurs; and is coeval with the lower fauna of the Ischigualasto Formation, Bermejo Basin, NW Argentina. The second association is recorded in deposits of both the Alemoa Member and the Caturrita Formation, characterized by the rhynchosaur ‘Scaphonyx’ sulcognathus and the cynodont Exaeretodon, and correlated with the upper fauna of the Ischigualasto Formation. Various isolated outcrops of the Caturrita Formation yield tetrapod fossils that correspond to post-Ischigualastian faunas but might not belong to a single faunal association. The record of the dicynodont Jachaleria suggests correlations with the lower part of the Los Colorados Formation, NW Argentina, whereas remains of derived tritheledontid cynodonts indicate younger ages.
    [Show full text]
  • 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.
    [Show full text]
  • The Anatomy and Phylogenetic Relationships of Antetonitrus Ingenipes (Sauropodiformes, Dinosauria): Implications for the Origins of Sauropoda
    THE ANATOMY AND PHYLOGENETIC RELATIONSHIPS OF ANTETONITRUS INGENIPES (SAUROPODIFORMES, DINOSAURIA): IMPLICATIONS FOR THE ORIGINS OF SAUROPODA Blair McPhee A dissertation submitted to the Faculty of Science, University of the Witwatersrand, in partial fulfilment of the requirements for the degree of Master of Science. Johannesburg, 2013 i ii ABSTRACT A thorough description and cladistic analysis of the Antetonitrus ingenipes type material sheds further light on the stepwise acquisition of sauropodan traits just prior to the Triassic/Jurassic boundary. Although the forelimb of Antetonitrus and other closely related sauropododomorph taxa retains the plesiomorphic morphology typical of a mobile grasping structure, the changes in the weight-bearing dynamics of both the musculature and the architecture of the hindlimb document the progressive shift towards a sauropodan form of graviportal locomotion. Nonetheless, the presence of hypertrophied muscle attachment sites in Antetonitrus suggests the retention of an intermediary form of facultative bipedality. The term Sauropodiformes is adopted here and given a novel definition intended to capture those transitional sauropodomorph taxa occupying a contiguous position on the pectinate line towards Sauropoda. The early record of sauropod diversification and evolution is re- examined in light of the paraphyletic consensus that has emerged regarding the ‘Prosauropoda’ in recent years. iii ACKNOWLEDGEMENTS First, I would like to express sincere gratitude to Adam Yates for providing me with the opportunity to do ‘real’ palaeontology, and also for gladly sharing his considerable knowledge on sauropodomorph osteology and phylogenetics. This project would not have been possible without the continued (and continual) support (both emotionally and financially) of my parents, Alf and Glenda McPhee – Thank you.
    [Show full text]
  • PAL E1059.Pdf
    Downloaded from rspb.royalsocietypublishing.org on November 23, 2010 A new transitional sauropodomorph dinosaur from the Early Jurassic of South Africa and the evolution of sauropod feeding and quadrupedalism Adam M. Yates, Matthew F. Bonnan, Johann Neveling, Anusuya Chinsamy and Marc G. Blackbeard Proc. R. Soc. B 2010 277, 787-794 first published online 11 November 2009 doi: 10.1098/rspb.2009.1440 Supplementary data "Data Supplement" http://rspb.royalsocietypublishing.org/content/suppl/2009/11/09/rspb.2009.1440.DC1.h tml References This article cites 24 articles, 5 of which can be accessed free http://rspb.royalsocietypublishing.org/content/277/1682/787.full.html#ref-list-1 Subject collections Articles on similar topics can be found in the following collections palaeontology (132 articles) taxonomy and systematics (296 articles) evolution (2213 articles) Receive free email alerts when new articles cite this article - sign up in the box at the top Email alerting service right-hand corner of the article or click here To subscribe to Proc. R. Soc. B go to: http://rspb.royalsocietypublishing.org/subscriptions This journal is © 2010 The Royal Society Downloaded from rspb.royalsocietypublishing.org on November 23, 2010 Proc. R. Soc. B (2010) 277, 787–794 doi:10.1098/rspb.2009.1440 Published online 11 November 2009 A new transitional sauropodomorph dinosaur from the Early Jurassic of South Africa and the evolution of sauropod feeding and quadrupedalism Adam M. Yates1,*, Matthew F. Bonnan2, Johann Neveling3, Anusuya Chinsamy4 and Marc G. Blackbeard1 1Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Johannesburg 2050, South Africa 2Department of Biological Sciences, Western Illinois University, Macomb, IL 61455, USA 3Council for Geoscience, Pretoria 0001, South Africa 4Zoology Department, University of Cape Town, Private Bag X3, Rhodes Gift 7700, South Africa Aardonyx celestae gen.
    [Show full text]
  • Skull Remains of the Dinosaur Saturnalia Tupiniquim (Late Triassic, Brazil): with Comments on the Early Evolution of Sauropodomorph Feeding Behaviour
    RESEARCH ARTICLE Skull remains of the dinosaur Saturnalia tupiniquim (Late Triassic, Brazil): With comments on the early evolution of sauropodomorph feeding behaviour 1 2 1 Mario BronzatiID *, Rodrigo T. MuÈ llerID , Max C. Langer * 1 LaboratoÂrio de Paleontologia, Faculdade de Filosofia Ciências e Letras de Ribeirão Preto, Universidade de a1111111111 São Paulo, Ribeirão Preto, São Paulo, Brazil, 2 Centro de Apoio à Pesquisa PaleontoloÂgica, Universidade Federal de Santa Maria, Santa Maria, Rio Grande do Sul, Brazil a1111111111 a1111111111 * [email protected] (MB); [email protected] (MCL) a1111111111 a1111111111 Abstract Saturnalia tupiniquim is a sauropodomorph dinosaur from the Late Triassic (Carnian±c. 233 OPEN ACCESS Ma) Santa Maria Formation of Brazil. Due to its phylogenetic position and age, it is important for studies focusing on the early evolution of both dinosaurs and sauropodomorphs. The Citation: Bronzati M, MuÈller RT, Langer MC (2019) Skull remains of the dinosaur Saturnalia tupiniquim osteology of Saturnalia has been described in a series of papers, but its cranial anatomy (Late Triassic, Brazil): With comments on the early remains mostly unknown. Here, we describe the skull bones of one of its paratypes (only in evolution of sauropodomorph feeding behaviour. the type-series to possess such remains) based on CT Scan data. The newly described ele- PLoS ONE 14(9): e0221387. https://doi.org/ ments allowed estimating the cranial length of Saturnalia and provide additional support for 10.1371/journal.pone.0221387 the presence of a reduced skull (i.e. two thirds of the femoral length) in this taxon, as typical Editor: JuÈrgen Kriwet, University of Vienna, of later sauropodomorphs.
    [Show full text]
  • Yates, A.M., Wedel, M.J., and Bonnan, M.F. 2012. the Early Evolution of Postcranial Skeletal Pneumaticity in Sauropodo− Morph Dinosaurs
    The early evolution of postcranial skeletal pneumaticity in sauropodomorph dinosaurs ADAM M. YATES, MATHEW J. WEDEL, and MATTHEW F. BONNAN Yates, A.M., Wedel, M.J., and Bonnan, M.F. 2012. The early evolution of postcranial skeletal pneumaticity in sauropodo− morph dinosaurs. Acta Palaeontologica Polonica 57 (1): 85–100. Postcranial skeletal pneumaticity (PSP) is present in a range of basal sauropodomorphs spanning the basal sauro− podomorph–sauropod transition. We describe the PSP of five taxa, Plateosaurus engelhardti, Eucnemesaurus fortis, Aardonyx celestae, Antetonitrus ingenipes, and an unnamed basal sauropod from Spion Kop, South Africa (hereafter re− ferred to as the Spion Kop sauropod). The PSP of Plateosaurus is apparently sporadic in its occurrence and has only been observed in very few specimens, in which it is of very limited extent, affecting only the posterior cervical vertebrae and pos− sibly the mid dorsals in one specimen. The PSP of Eucnemesaurus, Aardonyx, Antetonitrus, and the Spion Kop sauropod consists of subfossae (fossa−within−fossa structures) that excavate the vertices of the posterior infradiapophyseal fossae of the posterior dorsal vertebrae. These subfossae range from simple shallow depressions (Eucnemesaurus) to deep, steep− sided, internally subdivided and asymmetrically developed chambers (Antetonitrus). The middle and anterior dorsal verte− brae of these taxa lack PSP, demonstrating that abdominal air sacs were the source of the invasive diverticula. The presence of pneumatic features within the infradiapophyseal fossae suggest that the homologous fossae of more basal saurischians and dinosauriforms were receptacles that housed pneumatic diverticula. We suggest that it is probable that rigid non−compli− ant lungs ventilated by compliant posterior air sacs evolved prior to the origination of Dinosauria.
    [Show full text]
  • 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.
    [Show full text]
  • A Second Specimen of Blikanasaurus (Dinosauria: Sauropoda) and the Biostratigraphy of the Lower Elliot Formation
    A second specimen of Blikanasaurus (Dinosauria: Sauropoda) and the biostratigraphy of the lower Elliot Formation Adam M. Yates Bernard Price Institute for Palaeontological Research, School of Geosciences, University of the Witwatersrand, Private Bag 3, WITS, 2050 South Africa E-mail: [email protected] Received 25 September 2007. Accepted 29 January 2008 A second specimen of the rare basal sauropod Blikanasaurus cromptoni, is recorded from a site in the Ladybrand district of the Eastern Free State, South Africa. The specimen consists of a right metatarsal 1 that originated from the upper 20 m of the lower Elliot Formation. It can be referred to B. cromptoni on the basis of its small size and highly robust proportions, which distinguish this taxon from all other sauropodomorphs. This record extends the geographic distribution of B. cromptoni north into the region of the main Karoo Basin where the Elliot Formation is dramatically thinner. It also extends the known stratigraphic range of B. cromptoni up from the base of the Elliot Formation into a position near the top of the lower member. This new record, combined with other new discoveries, supports the hypothesis that the thin northern part of the lower Elliot Formation is a condensed section that is largely, if not entirely, coeval with the thicker southern sections. Keywords: basal sauropod, Blikanasaurus, Triassic, biostratigraphy, Karoo Basin, Elliot Formation. INTRODUCTION below and the typical Red Beds [= Elliot Formation] The dinosaur-rich Elliot Formation was deposited above’ (Charig et al. 1965, p. 200). This echoed the thought during the latest stages of filling of the main Karoo Basin, a of several geologists claimed that the Molteno-Elliot large foreland basin to the north of the Cape Fold Belt in contact was conformable and gradational (Du Toit 1939; southern Africa.
    [Show full text]
  • The Palaeontology Newsletter
    The Palaeontology Newsletter Contents 90 Editorial 2 Association Business 3 Association Meetings 11 News 14 From our correspondents Legends of Rock: Marie Stopes 22 Behind the scenes at the Museum 25 Kinds of Blue 29 R: Statistical tests Part 3 36 Rock Fossils 45 Adopt-A-Fossil 48 Ethics in Palaeontology 52 FossilBlitz 54 The Iguanodon Restaurant 56 Future meetings of other bodies 59 Meeting Reports 64 Obituary: David M. Raup 79 Grant and Bursary Reports 81 Book Reviews 103 Careering off course! 111 Palaeontology vol 58 parts 5 & 6 113–115 Papers in Palaeontology vol 1 parts 3 & 4 116 Virtual Palaeontology issues 4 & 5 117–118 Annual Meeting supplement >120 Reminder: The deadline for copy for Issue no. 91 is 8th February 2016. On the Web: <http://www.palass.org/> ISSN: 0954-9900 Newsletter 90 2 Editorial I watched the press conference for the publication on the new hominin, Homo naledi, with rising incredulity. The pomp and ceremony! The emotion! I wondered why all of these people were so invested just because it was a new fossil species of something related to us in the very recent past. What about all of the other new fossil species that are discovered every day? I can’t imagine an international media frenzy, led by deans and vice chancellors amidst a backdrop of flags and flashbulbs, over a new species of ammonite. Most other fossil discoveries and publications of taxonomy are not met with such fanfare. The Annual Meeting is a time for sharing these discoveries, many of which will not bring the scientists involved international fame, but will advance our science and push the boundaries of our knowledge and understanding.
    [Show full text]
  • Skull Remains of the Dinosaur Saturnalia Tupiniquim (Late Triassic, Brazil): with Comments on the Early Evolution of Sauropodomorph Feeding Behaviour
    RESEARCH ARTICLE Skull remains of the dinosaur Saturnalia tupiniquim (Late Triassic, Brazil): With comments on the early evolution of sauropodomorph feeding behaviour 1 2 1 Mario BronzatiID *, Rodrigo T. Mu¨ llerID , Max C. Langer * 1 Laborato´rio de Paleontologia, Faculdade de Filosofia Ciências e Letras de Ribeirão Preto, Universidade de São Paulo, Ribeirão Preto, São Paulo, Brazil, 2 Centro de Apoio à Pesquisa Paleontolo´gica, Universidade a1111111111 Federal de Santa Maria, Santa Maria, Rio Grande do Sul, Brazil a1111111111 a1111111111 * [email protected] (MB); [email protected] (MCL) a1111111111 a1111111111 Abstract Saturnalia tupiniquim is a sauropodomorph dinosaur from the Late Triassic (Carnian–c. 233 OPEN ACCESS Ma) Santa Maria Formation of Brazil. Due to its phylogenetic position and age, it is important Citation: Bronzati M, MuÈller RT, Langer MC (2019) for studies focusing on the early evolution of both dinosaurs and sauropodomorphs. The Skull remains of the dinosaur Saturnalia tupiniquim osteology of Saturnalia has been described in a series of papers, but its cranial anatomy (Late Triassic, Brazil): With comments on the early remains mostly unknown. Here, we describe the skull bones of one of its paratypes (only in evolution of sauropodomorph feeding behaviour. the type-series to possess such remains) based on CT Scan data. The newly described ele- PLoS ONE 14(9): e0221387. https://doi.org/ 10.1371/journal.pone.0221387 ments allowed estimating the cranial length of Saturnalia and provide additional support for the presence of a reduced skull (i.e. two thirds of the femoral length) in this taxon, as typical Editor: JuÈrgen Kriwet, University of Vienna, AUSTRIA of later sauropodomorphs.
    [Show full text]
  • University of Cape Town
    Unravelling the biology of t h e S outhern African Sauropodomorph dinosaurs , Plateosauravus a n d t h e ‘Maphutseng dinosaur’ . Em il Dariu s K rupandan ThesisUniversity presented for the of degree Cape of Doctor Town of Philosophy I n t h e Department of Biological Sciences University of Cape Town F e b r u a r y , 2 0 1 9 The copyright of this thesis vests in the author. No quotation from it or information derived from it is to be published without full acknowledgement of the source. The thesis is to be used for private study or non- commercial research purposes only. Published by the University of Cape Town (UCT) in terms of the non-exclusive license granted to UCT by the author. University of Cape Town i Declaration of Free Licence I hereby grant the University free license to reproduce the above thesis in whole or in part, for the purpose of research. I declare that the above thesis is my own unaided work, both in conception and execution, and that apart from the normal guidance of my supervisor s , I have received no assistance apart from that stated below. E x c e p t a s stated below, neither the substance or any part of the thesis has been submitted in the past, or is being, or is to be submitted for a degree at this University or any other University. I am now presenting the thesis for examination for the Degree o f P h D . _________________ Emil Darius Krupandan 11th d a y o f F e b r u a r y 2 0 1 9 at the University of Cape Town ii I confirm that I have been granted permission by the University of Cape Town’s Doctoral Degrees Board to include the f o l l o w i n g publication(s) in my PhD thesis, and where co - authorships are involved, my co - authors have agreed that I may include the publication(s): 1 .
    [Show full text]
  • Sacral Co‐Ossification in Dinosaurs: the Oldest Record of Fused
    Received: 10 July 2020 | Revised: 15 October 2020 | Accepted: 21 October 2020 DOI: 10.1111/joa.13356 ORIGINAL PAPER Sacral co-ossification in dinosaurs: The oldest record of fused sacral vertebrae in Dinosauria and the diversity of sacral co-ossification patterns in the group Débora Moro1,2 | Leonardo Kerber1,2,3 | Rodrigo T. Müller2 | Flávio A. Pretto1,2 1Programa de Pós-Graduação em Biodiversidade Animal, Universidade Federal Abstract de Santa Maria, Santa Maria, RS, Brazil The fusion of the sacrum occurs in the major dinosaur lineages, i.e. ornithischians, 2 Centro de Apoio à Pesquisa Paleontológica theropods, and sauropodomorphs, but it is unclear if this trait is a common ancestral da Quarta Colônia, Universidade Federal de Santa Maria, São João do Polêsine, RS, Brazil condition, or if it evolved independently in each lineage, or even how or if it is related 3Museu Paraense Emílio Goeldi, to ontogeny. In addition, the order in which the different structures of the sacrum Coordenação de Ciências da Terra e Ecologia, Belém, Brazil are fused, as well as the causes that lead to this co-ossification, are poorly under- stood. Herein, we described the oldest record of fused sacral vertebrae within dino- Correspondence Débora Moro and Flávio A. Pretto, Centro saurs, based on two primordial sacral vertebrae from the Late Triassic of Candelária de Apoio à Pesquisa Paleontológica - Sequence, southern Brazil. We used computed microtomography (micro-CT) to ana- CAPPA/UFSM. Rua Maximiliano Vizzotto, 598. CEP 97230-000. São João do Polêsine, lyze the extent of vertebral fusion, which revealed that it occurred only between Rio Grande do Sul, Brasil.
    [Show full text]