(Xenarthra, Cingulata) from the Late Pleistocene of Uruguay
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Ancient Mitogenomes Shed Light on the Evolutionary History And
Ancient Mitogenomes Shed Light on the Evolutionary History and Biogeography of Sloths Frédéric Delsuc, Melanie Kuch, Gillian Gibb, Emil Karpinski, Dirk Hackenberger, Paul Szpak, Jorge Martinez, Jim Mead, H. Gregory Mcdonald, Ross Macphee, et al. To cite this version: Frédéric Delsuc, Melanie Kuch, Gillian Gibb, Emil Karpinski, Dirk Hackenberger, et al.. Ancient Mitogenomes Shed Light on the Evolutionary History and Biogeography of Sloths. Current Biology - CB, Elsevier, 2019. hal-02326384 HAL Id: hal-02326384 https://hal.archives-ouvertes.fr/hal-02326384 Submitted on 22 Oct 2019 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. 1 Ancient Mitogenomes Shed Light on the Evolutionary 2 History and Biogeography of Sloths 3 Frédéric Delsuc,1,13,*, Melanie Kuch,2 Gillian C. Gibb,1,3, Emil Karpinski,2,4 Dirk 4 Hackenberger,2 Paul Szpak,5 Jorge G. Martínez,6 Jim I. Mead,7,8 H. Gregory 5 McDonald,9 Ross D. E. MacPhee,10 Guillaume Billet,11 Lionel Hautier,1,12 and 6 Hendrik N. Poinar2,* 7 Author list footnotes 8 1Institut des Sciences de l’Evolution de Montpellier -
Reveals That Glyptodonts Evolved from Eocene Armadillos
Molecular Ecology (2016) 25, 3499–3508 doi: 10.1111/mec.13695 Ancient DNA from the extinct South American giant glyptodont Doedicurus sp. (Xenarthra: Glyptodontidae) reveals that glyptodonts evolved from Eocene armadillos KIEREN J. MITCHELL,* AGUSTIN SCANFERLA,† ESTEBAN SOIBELZON,‡ RICARDO BONINI,‡ JAVIER OCHOA§ and ALAN COOPER* *Australian Centre for Ancient DNA, School of Biological Sciences, University of Adelaide, Adelaide, SA 5005, Australia, †CONICET-Instituto de Bio y Geociencias del NOA (IBIGEO), 9 de Julio No 14 (A4405BBB), Rosario de Lerma, Salta, Argentina, ‡Division Paleontologıa de Vertebrados, Facultad de Ciencias Naturales y Museo (UNLP), CONICET, Museo de La Plata, Paseo del Bosque, La Plata, Buenos Aires 1900, Argentina, §Museo Arqueologico e Historico Regional ‘Florentino Ameghino’, Int De Buono y San Pedro, Rıo Tercero, Cordoba X5850, Argentina Abstract Glyptodonts were giant (some of them up to ~2400 kg), heavily armoured relatives of living armadillos, which became extinct during the Late Pleistocene/early Holocene alongside much of the South American megafauna. Although glyptodonts were an important component of Cenozoic South American faunas, their early evolution and phylogenetic affinities within the order Cingulata (armoured New World placental mammals) remain controversial. In this study, we used hybridization enrichment and high-throughput sequencing to obtain a partial mitochondrial genome from Doedicurus sp., the largest (1.5 m tall, and 4 m long) and one of the last surviving glyptodonts. Our molecular phylogenetic analyses revealed that glyptodonts fall within the diver- sity of living armadillos. Reanalysis of morphological data using a molecular ‘back- bone constraint’ revealed several morphological characters that supported a close relationship between glyptodonts and the tiny extant fairy armadillos (Chlamyphori- nae). -
Distinguishing Quaternary Glyptodontine Cingulates in South America: How Informative Are Juvenile Specimens?
Distinguishing Quaternary glyptodontine cingulates in South America: How informative are juvenile specimens? CARLOS A. LUNA, IGNACIO A. CERDA, ALFREDO E. ZURITA, ROMINA GONZALEZ, M. CECILIA PRIETO, DIMILA MOTHÉ, and LEONARDO S. AVILLA Luna, C.A., Cerda, I.A., Zurita, A.E., Gonzalez, R., Prieto, M.C., Mothé, D., and Avilla, L.S. 2018. Distinguishing Quaternary glyptodontine cingulates in South America: How informative are juvenile specimens? Acta Palaeontologica Polonica 63 (1): 159–170. The subfamily Glyptodontinae (Xenarthra, Cingulata) comprises one of the most frequently recorded glyptodontids in South America. Recently, the North American genus Glyptotherium was recorded in South America, in addition to the genus Glyptodon. It has been shown that both genera shared the same geographic distribution in central-north and eastern areas of South America (Venezuela and Brazil, respectively). Although some characters allow differentiation between adult specimens of both genera, the morphological distinction between these two genera is rather difficult in juvenile specimens. In this contribution, a detailed morphological, morphometric and histological survey of a juvenile specimen of Glyptodontinae recovered from the Late Pleistocene of northern Brazil is performed. The relative lower osteoderms thickness, the particular morphology of the annular and radial sulci and the distal osseous projections of the caudal osteoderms suggest that the specimen belongs to the genus Glyptotherium. In addition, the validity of some statistical tools to distinguish between different ontogenetic stages and in some cases between genera is verified. The osteoderm microstructure of this juvenile individual is characterized by being composed of a cancellous internal core surrounded by a compact bone cortex. Primary bone tissue mostly consists of highly vascularized, woven-fibered bone tissue. -
The Armor of FOSSIL GIANT ARMADILLOS (Pa1npatlzeriidae, Xenartlz Ra, Man1malia) A
NUMBER40 PEARCE-SELLARDS SERIES The Armor of FOSSIL GIANT ARMADILLOS (Pa1npatlzeriidae, Xenartlz ra, Man1malia) A. GORDON EDMUND JUNE 1985 TEXAS MEMORIAL MUSEUM, UNIVERSITY OF TEXAS AT AUSTIN Pearce-Sellards Series 40 The Armor of FOSSIL GIANT ARMADILLOS (Pampatheriidae, Xenartlzra, Mammalia) A. GORDON EDMUND JUNE 1985 TEXAS MEMORIAL MUSEUM, UNIVERSITY OF TEXAS AT AUSTIN A. Gordon Edmund is Curator of Vertebrate Paleontology at the Royal Ontario Museum, Toronto, and Associate Professor of Geology at the University of Toronto. The Pearce-Sellards Series is an occasional, miscellaneous series of brief reports of Museum and Museum-associated field investigations and other research. All manuscripts are subjected to extramural peer review before being accepted. The series title commemorates the first two directors of Texas Memorial Museum, both now deceased: Dr. J. E. Pearce, Professor of Anthropology, and Dr. E. H. Sellards, Professor of Geology, The University of Texas at Austin. A portion of the Museum's general ope rating funds for this fiscal year has been provided by a grant from the Institute of Museum Services, a federal agency that offers general operating support to the nation's museums. © 1985 by Texas Memorial Museum The University of Texas at Austin All rights reserved Printed in the United States of America CONTENTS Abstract .... .............................................. I Sumario .................................................... 1 Acknowledgements . 2 Abbreviations ............................................... 2 Introduction . 3 A General Description of the Armor . 5 Types and Numbers of Osteoderms .... .. ........................ 6 Structure of Osteoderms . 7 Detailed Description of each Area ................................ 8 Conclusions. 19 References ............ .. .............. ............. ....... 19 LIST OF FIGURES Fig. 1. Restoration of Holmesina septentrionalis based on composite material from Florida ......... ...... .... facing 5 Fig. -
High School Living Earth Evidence for Evolution Lessons Name: School: Teacher
DO NOT EDIT--Changes must be made through “File info” CorrectionKey=CA-B High School Living Earth Evidence for Evolution Lessons Name: School: Teacher: The Unit should take approximately 4 days complete. Read each section and complete the tasks. DO NOT EDIT--Changes must be made through “File info” CorrectionKey=CA-B FIGURE 1: This creosote ring in the Mojave Desert is estimated to be 11 700 years old . This makes it one of the oldest living organisms on Earth . The creosote bush is thought to be the most drought-tolerant plant in North America. It has a variety of adaptations to its desert environment, including its reproductive tendency to clone outward in rings rather than rely solely on seed production. The plant’s leaves are coated in a foul-tasting resin that protects it from water loss through evaporation and from grazing. It only opens its stomata in the morning to pull in carbon dioxide for photosynthesis from the more humid air and closes them as the day’s temperature increases. It also has a root system that consists of both an exceptionally long tap root and a vast network of shallow feeder roots. Creosote bushes exhibit two different shapes to fit different microclimates. In drier areas, the plant has a cone shape in which stems funnel rainwater into the taproot. In wetter areas, the bush has a more rounded shape that provides shade to its shallow feeder roots. PREDICT How do species change over time to adjust to varying conditions? DRIVING QUESTIONS As you move through the unit, gather evidence to help you answer the following questions. -
Revised Stratigraphy of Neogene Strata in the Cocinetas Basin, La Guajira, Colombia
Swiss J Palaeontol (2015) 134:5–43 DOI 10.1007/s13358-015-0071-4 Revised stratigraphy of Neogene strata in the Cocinetas Basin, La Guajira, Colombia F. Moreno • A. J. W. Hendy • L. Quiroz • N. Hoyos • D. S. Jones • V. Zapata • S. Zapata • G. A. Ballen • E. Cadena • A. L. Ca´rdenas • J. D. Carrillo-Bricen˜o • J. D. Carrillo • D. Delgado-Sierra • J. Escobar • J. I. Martı´nez • C. Martı´nez • C. Montes • J. Moreno • N. Pe´rez • R. Sa´nchez • C. Sua´rez • M. C. Vallejo-Pareja • C. Jaramillo Received: 25 September 2014 / Accepted: 2 February 2015 / Published online: 4 April 2015 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2015 Abstract The Cocinetas Basin of Colombia provides a made exhaustive paleontological collections, and per- valuable window into the geological and paleontological formed 87Sr/86Sr geochronology to document the transition history of northern South America during the Neogene. from the fully marine environment of the Jimol Formation Two major findings provide new insights into the Neogene (ca. 17.9–16.7 Ma) to the fluvio-deltaic environment of the history of this Cocinetas Basin: (1) a formal re-description Castilletes (ca. 16.7–14.2 Ma) and Ware (ca. 3.5–2.8 Ma) of the Jimol and Castilletes formations, including a revised formations. We also describe evidence for short-term pe- contact; and (2) the description of a new lithostratigraphic riodic changes in depositional environments in the Jimol unit, the Ware Formation (Late Pliocene). We conducted and Castilletes formations. The marine invertebrate fauna extensive fieldwork to develop a basin-scale stratigraphy, of the Jimol and Castilletes formations are among the richest yet recorded from Colombia during the Neogene. -
Michael O. Woodburne1,* Alberto L. Cione2,**, and Eduardo P. Tonni2,***
Woodburne, M.O.; Cione, A.L.; and Tonni, E.P., 2006, Central American provincialism and the 73 Great American Biotic Interchange, in Carranza-Castañeda, Óscar, and Lindsay, E.H., eds., Ad- vances in late Tertiary vertebrate paleontology in Mexico and the Great American Biotic In- terchange: Universidad Nacional Autónoma de México, Instituto de Geología and Centro de Geociencias, Publicación Especial 4, p. 73–101. CENTRAL AMERICAN PROVINCIALISM AND THE GREAT AMERICAN BIOTIC INTERCHANGE Michael O. Woodburne1,* Alberto L. Cione2,**, and Eduardo P. Tonni2,*** ABSTRACT The age and phyletic context of mammals that dispersed between North and South America during the past 9 m.y. is summarized. The presence of a Central American province of cladogenesis and faunal differentiation is explored. One apparent aspect of such a province is to delay dispersals of some taxa northward from Mexico into the continental United States, largely during the Blancan. Examples are recognized among the various xenar- thrans, and cervid artiodactyls. Whereas the concept of a Central American province has been mentioned in past investigations it is upgraded here. Paratoceras (protoceratid artio- dactyl) and rhynchotheriine proboscideans provide perhaps the most compelling examples of Central American cladogenesis (late Arikareean to early Barstovian and Hemphillian to Rancholabrean, respectively), but this category includes Hemphillian sigmodontine rodents, and perhaps a variety of carnivores and ungulates from Honduras in the medial Miocene, as well as peccaries and equids from Mexico. For South America, Mexican canids and hy- drochoerid rodents may have had an earlier development in Mexico. Remarkably, the first South American immigrants to Mexico (after the Miocene heralds; the xenarthrans Plaina and Glossotherium) apparently dispersed northward at the same time as the first Holarctic taxa dispersed to South America (sigmodontine rodents and the tayassuid artiodactyls). -
Extinct Mammal Used Its 'Sweet Spot' to Club Rivals 27 August 2009, by Lin Edwards
Extinct Mammal Used its 'Sweet Spot' to Club Rivals 27 August 2009, by Lin Edwards Blanco and his colleagues Washington W. Jones, and Andres Rinderknecht, decided to use the same methods as the sports studies to determine the location of the sweet spot on the tails of the glyptodonts. They studied fossilized remains of glyptodonts in the collections of three South American museums, and found that in many species of glyptodonts, such as Doedicurus clavicaudatus, the ball of bony plates at the end of Artistic reconstruction of Doedicurus clavicaudatus, with the tail was located at the center of percussion. a human for scale. The distal rigid caudal sheath and the mobile free rings are shown. Adapted from Ubilla et al. The plates were fused, turning the tail into a rigid (2008) (fig. 13.3, with permission of Perea, D. ed. 2008). weapon that concentrated the force onto the sweet spot in the tail's club, which is believed to have been covered in large horny spikes. The scientists likened the flexible part of the glyptodont's tail to a (PhysOrg.com) -- Scientists in Uruguay studying tennis player's arm, and the rigid club at the end of extinct mammals called glyptodonts have the tail to the tennis racket, with the sweet spot discovered they used a "sweet spot" in their tails, under the largest spikes. just like baseball players use the center of percussion (CP), or sweet spot, in their bats to hit Having the sweet spot in the position of the largest the ball with maximum power and minimum chance spikes meant the glyptodont tail clubs must have of injury. -
Mammalia, Cingulata, Glyptodontia)
Journal of South American Earth Sciences 66 (2016) 32e40 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames A reassessment of the taxonomic status of Paraglyptodon Castellanos, 1932 (Mammalia, Cingulata, Glyptodontia) * Laura E. Cruz a, , Juan C. Fernicola a, b, Matias Taglioretti c, Nestor Toledo d a CONICET, Consejo Nacional de Investigaciones Científicas y Tecnicas-Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”,Av.Angel Gallardo 470, Capital Federal, C1405DJR, Argentina b Departamento de Ciencias Basicas, Universidad Nacional de Lujan, Ruta 5 y Avenida Constitucion, 6700, Lujan, Buenos Aires, Argentina c CONICET-Instituto de Geología de Costas y del Cuaternario, Facultad de Ciencias Exactas y Naturales, Universidad Nacional de Mar del Plata, Dean Funes 3350, B7602AYL, Mar del Plata, Buenos Aires, Argentina d CONICET-Division Paleontología Vertebrados, Unidades de Investigacion Anexo Museo FCNyM-UNLP, Avenida 60 y 122, B1900FWA, La Plata, Argentina article info abstract Article history: Castellanos described and published about new genera of glyptodonts, according to a phylogenetic Received 21 September 2015 scheme mainly based on the evolution of the external surface of the dorsal carapace. Among these new Received in revised form genera, Castellanos proposed Paraglyptodon as the predecessor of Glyptodon, and included within Par- 4 November 2015 aglyptodon all known species of Glyptodontinae recovered from “horizontes pre-Ensenadenses”, and Accepted 20 November 2015 within Glyptodon all known species from “Horizontes pampeanos”, restricting the latter to the Quaternary. Available online 25 November 2015 All the species that belong to Paraglyptodon, that is Paraglyptodon chapalmalensis, Paraglyptodon uquiensis, Paraglyptodon dubius, and Paraglyptodon paranensis were established based on one, two or few Keywords: Osteoderm osteoderms, mostly from the dorsal carapace. -
Overkill, Glacial History, and the Extinction of North America's Ice Age Megafauna
PERSPECTIVE Overkill, glacial history, and the extinction of North America’s Ice Age megafauna PERSPECTIVE David J. Meltzera,1 Edited by Richard G. Klein, Stanford University, Stanford, CA, and approved September 23, 2020 (received for review July 21, 2020) The end of the Pleistocene in North America saw the extinction of 38 genera of mostly large mammals. As their disappearance seemingly coincided with the arrival of people in the Americas, their extinction is often attributed to human overkill, notwithstanding a dearth of archaeological evidence of human predation. Moreover, this period saw the extinction of other species, along with significant changes in many surviving taxa, suggesting a broader cause, notably, the ecological upheaval that occurred as Earth shifted from a glacial to an interglacial climate. But, overkill advocates ask, if extinctions were due to climate changes, why did these large mammals survive previous glacial−interglacial transitions, only to vanish at the one when human hunters were present? This question rests on two assumptions: that pre- vious glacial−interglacial transitions were similar to the end of the Pleistocene, and that the large mammal genera survived unchanged over multiple such cycles. Neither is demonstrably correct. Resolving the cause of large mammal extinctions requires greater knowledge of individual species’ histories and their adaptive tolerances, a fuller understanding of how past climatic and ecological changes impacted those animals and their biotic communities, and what changes occurred at the Pleistocene−Holocene boundary that might have led to those genera going extinct at that time. Then we will be able to ascertain whether the sole ecologically significant difference between previous glacial−interglacial transitions and the very last one was a human presence. -
La Brea and Beyond: the Paleontology of Asphalt-Preserved Biotas
La Brea and Beyond: The Paleontology of Asphalt-Preserved Biotas Edited by John M. Harris Natural History Museum of Los Angeles County Science Series 42 September 15, 2015 Cover Illustration: Pit 91 in 1915 An asphaltic bone mass in Pit 91 was discovered and exposed by the Los Angeles County Museum of History, Science and Art in the summer of 1915. The Los Angeles County Museum of Natural History resumed excavation at this site in 1969. Retrieval of the “microfossils” from the asphaltic matrix has yielded a wealth of insect, mollusk, and plant remains, more than doubling the number of species recovered by earlier excavations. Today, the current excavation site is 900 square feet in extent, yielding fossils that range in age from about 15,000 to about 42,000 radiocarbon years. Natural History Museum of Los Angeles County Archives, RLB 347. LA BREA AND BEYOND: THE PALEONTOLOGY OF ASPHALT-PRESERVED BIOTAS Edited By John M. Harris NO. 42 SCIENCE SERIES NATURAL HISTORY MUSEUM OF LOS ANGELES COUNTY SCIENTIFIC PUBLICATIONS COMMITTEE Luis M. Chiappe, Vice President for Research and Collections John M. Harris, Committee Chairman Joel W. Martin Gregory Pauly Christine Thacker Xiaoming Wang K. Victoria Brown, Managing Editor Go Online to www.nhm.org/scholarlypublications for open access to volumes of Science Series and Contributions in Science. Natural History Museum of Los Angeles County Los Angeles, California 90007 ISSN 1-891276-27-1 Published on September 15, 2015 Printed at Allen Press, Inc., Lawrence, Kansas PREFACE Rancho La Brea was a Mexican land grant Basin during the Late Pleistocene—sagebrush located to the west of El Pueblo de Nuestra scrub dotted with groves of oak and juniper with Sen˜ora la Reina de los A´ ngeles del Rı´ode riparian woodland along the major stream courses Porciu´ncula, now better known as downtown and with chaparral vegetation on the surrounding Los Angeles. -
Taluany Silva Do Nascimento
UNIVERSIDADE FEDERAL DO TOCANTINS CAMPUS UNIVERSITÁRIO DE PORTO NACIONAL PROGRAMA DE PÓS-GRADUAÇÃO EM BIODIVERSIDADE, ECOLOGIA E CONSERVAÇÃO TALUANY SILVA DO NASCIMENTO NOVOS REGISTROS DE ANGIOSPERMAS PLEISTOCÊNICAS PARA FORMAÇÃO RIO MADEIRA, BACIA DO ABUNÃ, RONDÔNIA, BRASIL PORTO NACIONAL (TO) 2021 TALUANY SILVA DO NASCIMENTO NOVOS REGISTROS DE ANGIOSPERMAS PLEISTOCÊNICAS PARA FORMAÇÃO RIO MADEIRA, BACIA DO ABUNÃ, RONDÔNIA, BRASIL Dissertação apresentada ao Programa de Pós – Graduação em Biodiversidade, ecologia e conservação da Universidade Federal do Tocantins, como parte dos requisitos para obtenção de título de mestre em biodiversidade, ecologia e conservação. Orientadora: Dra. Etiene Fabbrin Pires Oliveira PORTO NACIONAL (TO) 2021 Taluany Silva do Nascimento Novos registros de angiospermas pleistocênicas para formação rio Madeira, Bacia do Abunã, Rondônia, Brasil. Dissertação apresentada ao Programa de Pós- Graduação em Biodiversidade, Ecologia e Conservação. Foi avaliada para obtenção do título de Mestre em Biodiversidade, Ecologia e Conservação e aprovada em sua forma final pela Orientadora e pela Banca Examinadora. Data de aprovação: 28/04/2021 Banca Examinadora: ___________________________________________________ Profa. Dra. Etiene Fabbrin Pires Oliveira (Orientadora), UFT ___________________________________________________ Prof. Dr. André Jasper, Univates _________________________________________________ Prof. Dr. Yuri Modesto Alves, UFT Porto Nacional - TO, 2021 AGRADECIMENTOS Durante o meu mestrado foram muitas as pessoas que contribuíram e passaram pelo meu caminho influenciando de forma direta e indireta na construção desse trabalho. Sou grata a todos! Creio que não seja possível expressar tamanha gratidão, mas escreverei algumas palavras destacando essas contribuições, sem ordem de importância, mesmo correndo o risco de esquecer algum nome. O Laboratório de Paleobiologia da Universidade Federal do Tocantins, campus Porto Nacional, foi meu lar acadêmico durante os últimos 5 anos.