Tree Sloth, Anteater, Armadillo, Ground Sloth, Glyptodont, and Pampathere) Cranial Material to Evaluate Students’ Understanding of This Thing Called Science Barbara J
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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 -
Tabbitha Schliesman Tolypeutes Matacus Southern Three-Banded Armadillo
Tabbitha Schliesman Tolypeutes matacus Southern Three-banded Armadillo Description: The Southern Three-Banded Armadillo, Tolypeutes matacus, is a small creature, about 10- 15 cm tall, 21 – 30 cm long(Eisenburg & Redford, 1999), and 1.00 to 1.59 kg in weight (EOL, 2014). The outer shell of the Southern Three-Banded Armadillo ranges from light brownish-yellow to blackish-brown in coloring. This armadillo is comprised of three parts: a head, body, and an immobile, stout tail that are heavily armored with a leathery, think shell(Ellis, 1999). This leathery armor covers the entire animal, except for the belly and ears, when walking and/or standing. The skin of the front and rear portions of the Southern Three-Banded Armadillo are not attached to the middle section, allowing the animal to roll into a tight ball(EOL, 2014). Other features that make the Southern Three-Banded Southern Three Banded-Armadillo, Tolypeutes Armadillo distinct are the third and fourth claws of matacus, (Smith, 2007). the hind feet that look like hooves, while the front feet have only three sharp powerful claws(Superina, 2009). Southern Three-Banded Armadillos have a long pink tongue that is usually sticky. Their heads are long, and are unique to each armadillo; like humans’ fingerprints, researchers have used their head patterns while tracking them to identify which individual armadillo they are researching(HZ, 2011). Ecology: Southern Three-Banded Armadillos are native to north central Argentina, east central Bolivia and multiple sections of Paraguay and south west Brazil. The Southern Three-Banded Armadillo is found mainly in scrub forests and savannahs in these sections of South America. -
Uma Perspectiva Macroecológica Sobre O Risco De Extinção Em Mamíferos
Universidade Federal de Goiás Instituto de Ciências Biológicas Programa de Pós-graduação em Ecologia e Evolução Uma Perspectiva Macroecológica sobre o Risco de Extinção em Mamíferos VINÍCIUS SILVA REIS Goiânia 2019 VINÍCIUS SILVA REIS Uma Perspectiva Macroecológica sobre o Risco de Extinção em Mamíferos Tese apresentada ao Programa de Pós-graduação em Ecologia e Evolução do Departamento de Ecologia do Instituto de Ciências Biológicas da Universidade Federal de Goiás como requisito parcial para a obtenção do título de Doutor em Ecologia e Evolução. Orientador: Profº Drº Matheus de Souza Lima- Ribeiro Co-orientadora: Profª Drª Levi Carina Terribile Goiânia 2019 DEDI CATÓRIA Ao meu pai Wilson e à minha mãe Iris por sempre acreditarem em mim. “Esper o que próxima vez que eu te veja, você s eja um novo homem com uma vasta gama de novas experiências e aventuras. Não he site, nem se permita dar desculpas. Apenas vá e faça. Vá e faça. Você ficará muito, muito feliz por ter feito”. Trecho da carta escrita por Christopher McCandless a Ron Franz contida em Into the Wild de Jon Krakauer (Livre tradução) . AGRADECIMENTOS Eis que a aventura do doutoramento esteve bem longe de ser um caminho solitário. Não poderia ter sido um caminho tão feliz se eu não tivesse encontrado pessoas que me ensinaram desde método científico até como se bebe cerveja de verdade. São aos que estiveram comigo desde sempre, aos que permaneceram comigo e às novas amizades que eu construí quando me mudei pra Goiás que quero agradecer por terem me apoiado no nascimento desta tese: À minha família, em especial meu pai Wilson, minha mãe Iris e minha irmã Flora, por me apoiarem e me incentivarem em cada conquista diária. -
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). -
Dietary Specialization and Variation in Two Mammalian Myrmecophages (Variation in Mammalian Myrmecophagy)
Revista Chilena de Historia Natural 59: 201-208, 1986 Dietary specialization and variation in two mammalian myrmecophages (variation in mammalian myrmecophagy) Especializaci6n dietaria y variaci6n en dos mamiferos mirmec6fagos (variaci6n en la mirmecofagia de mamiferos) KENT H. REDFORD Center for Latin American Studies, Grinter Hall, University of Florida, Gainesville, Florida 32611, USA ABSTRACT This paper compares dietary variation in an opportunistic myrmecophage, Dasypus novemcinctus, and an obligate myrmecophage, Myrmecophaga tridactyla. The diet of the common long-nosed armadillo, D. novemcintus, consists of a broad range of invertebrate as well as vertebrates and plant material. In the United States, ants and termites are less important as a food source than they are in South America. The diet of the giant anteater. M. tridactyla, consists almost entirely of ants and termites. In some areas giant anteaters consume more ants whereas in others termites are a larger part of their diet. Much of the variation in the diet of these two myrmecophages can be explained by geographical and ecological variation in the abundance of prey. However, some variation may be due to individual differences as well. Key words: Dasypus novemcinctus, Myrmecophaga tridactyla, Tamandua, food habits. armadillo, giant anteater, ants, termites. RESUMEN En este trabajo se compara la variacion dietaria entre un mirmecofago oportunista, Dasypus novemcinctus, y uno obligado, Myrmecophaga tridactyla. La dieta del armadillo comun, D. novemcinctus, incluye un amplio rango de in- vertebrados así como vertebrados y materia vegetal. En los Estados Unidos, hormigas y termites son menos importantes como recurso alimenticio de los armadillos, de lo que son en Sudamérica. La dieta del hormiguero gigante, M tridactyla, está compuesta casi enteramente por hormigas y termites. -
Xenarthrans: 'Aliens'
Vet Times The website for the veterinary profession https://www.vettimes.co.uk XENARTHRANS: ‘ALIENS’ ON EARTH Author : JONATHAN CRACKNELL Categories : Vets Date : August 4, 2008 JONATHAN CRACKNELL finds that hanging around with sloths and their fellow Xenarthrans offers up exciting challenges XENARTHRANS: the name sounds like a race from a low-budget science fiction film. This is actually a super-order of mammals that get their name from their “alien” joint, which is exhibited in the vertebral joints. The Xenarthrans include 31 living species: six species of sloth, four anteaters and 21 species of armadillos – all of which originated in South America. Historically, these animals were classified within the order Edentata (meaning “without teeth”), which included pangolins and aardvarks. It was realised that this was a polyphyletic group, containing unrelated families. Therefore, the Xenarthra order was created. The Xenarthrans are a well-represented order in captivity, with banded armadillos (Dasypus novemcinctus) becoming one of the new “exotic” exotics to be presented to clinicians. In zoological collections, giant anteaters (Myrmecophaga tridactyla), southern tamanduas (Tamandua tetradactyla), and sloths (typically the southern two-toed sloth – Choloepus didactylus – although others are present) are among the more common species housed in captivity. Every species has its own needs and oddities. With this brief review of each species, the author will look at basic anatomy and physiology, along with a quick review of some of the more commonly reported complaints for this group of animals. 1 / 14 Giant anteater The giant anteater’s most obvious feature is its long tongue and bushy tail. They are approximately 1.5 to two metres long and weigh in the region of 18kg to 45kg. -
Introduction Recent Classifications Regard the Order Pilosa, Anteaters
Introduction Recent classifications regard the order Pilosa, anteaters and sloths, and order Cingulata, the armadillos, within the superorder Xenarthra meaning “strange joints”. In the past, Pilosa and Cingulata wer regarded as suborders of the order Xenarthra, with the armadillos. Earlier still, both armadillos and pilosans were classified together with pangolins and the aardvark as the order Edentata meaning “toothless”. The orders Pilosa and Cingulata are distinguishable as the cingulatas have an armoured upper body and the pilosa have fur. Studies have concluded that sloths, anteaters, and armadillos diverged at least 75-80 million years ago and that they are as different from one another as are carnivores, bats and primates. The Pilosa are now considered almost exclusively a New World order, however, fossil records indicate that they were once found in Europe and possibly Asia. This order may have been distributed worldwide in the Cretaceous period, but became limited to South America and have remained there for most of their history and evolved into numerous groups. The Pilosa were once far more diverse than they are today; there are known to be 10 times as many fossil as living genera. The superorder is distinguished from all others by what are known as the xenarthrous vertebrae. There are secondary and sometimes even more, articulations between the vertebrae of the lumbar (lower back) series. In other words, consecutive vertebrae connect in more than one place. In addition, the pelvis connects with more of the spine than in other mammals. These adaptations to the spine give support, particularly to the hips. The name Xenarthra refers to this peculiarity of the spine and modem taxonomy places these three groups of animals together, even though they are very different from one another and they are highly specialized. -
The Giant Armadillo of the Gran Chaco
The Giant Armadillo of the Gran Chaco A giant armadillo Priodontes maximus at the Saenz-Peña Zoo in South America raises up, balancing with its tail, a common posture for this large species. Venezuela The Guianas: Guyana hat’s the size of Texas and Arizona combined, reaches temperatures Suriname French Guiana Wof 115 degrees Fahrenheit, has plants with 15-inch-long thorns, Colombia and houses an armadillo larger than a coffee table? The South American Gran Chaco, where giant armadillos wander freely. The Gran Chaco region covers more than 1 million square kilometers of Argentina, Bolivia, Perú Brazil Paraguay, and Brazil, with approximately 60 percent in Argentina and Bolivia just 7 percent in Brazil. The region is a mosaic of grasslands, savannas, Paraguay • open woodlands, dry thorn forests, and gallery forests that provide a GRAN CHACO 15 range of habitats where some diverse animal species flourish. • In the gallery forests of the humid Chaco, we regularly encounter animals Argentina that are associated with tropical and subtropical forests, like jaguars, owl monkeys, howler monkeys, peccaries, deer, tapirs, and various kinds of eden- tates, a group of mammals that includes sloths, anteaters, and armadillos. The Gran Chaco—from the Quechua Although there are no sloths in the Chaco, we regularly find lesser anteaters 2003 and sometimes come across giant anteaters. Both the nine-banded armadillo, Indian language of Bolivia for “great hunting ground”—crosses four coun- also found in Texas, and the tatu bola, or three-banded armadillo, which you tries and encompasses an area the can see at the Wild Animal Park’s Animal Care Center and the San Diego Zoo’s size of Texas and Arizona combined. -
(Dasypus) in North America Based on Ancient Mitochondrial DNA
bs_bs_banner A revised evolutionary history of armadillos (Dasypus) in North America based on ancient mitochondrial DNA BETH SHAPIRO, RUSSELL W. GRAHAM AND BRANDON LETTS Shapiro, B. Graham, R. W. & Letts, B.: A revised evolutionary history of armadillos (Dasypus) in North America based on ancient mitochondrial DNA. Boreas. 10.1111/bor.12094. ISSN 0300-9483. The large, beautiful armadillo, Dasypus bellus, first appeared in North America about 2.5 million years ago, and was extinct across its southeastern US range by 11 thousand years ago (ka). Within the last 150 years, the much smaller nine-banded armadillo, D. novemcinctus, has expanded rapidly out of Mexico and colonized much of the former range of the beautiful armadillo. The high degree of morphological similarity between these two species has led to speculation that they might be a single, highly adaptable species with phenotypical responses and geographical range fluctuations resulting from environmental changes. If this is correct, then the biology and tolerance limits for D. novemcinctus could be directly applied to the Pleistocene species, D. bellus. To investigate this, we isolated ancient mitochondrial DNA from late Pleistocene-age specimens of Dasypus from Missouri and Florida. We identified two genetically distinct mitochondrial lineages, which most likely correspond to D. bellus (Missouri) and D. novemcinctus (Florida). Surprisingly, both lineages were isolated from large specimens that were identified previously as D. bellus. Our results suggest that D. novemcinctus, which is currently classified as an invasive species, was already present in central Florida around 10 ka, significantly earlier than previously believed. Beth Shapiro ([email protected]), Department of Ecology and Evolutionary Biology, University of California Santa Cruz, Santa Cruz, CA 95064, USA; Russell W. -
Pliocene), Falc6n State, Venezuela, Its Relationship with the Asterostemma Problem, and the Paleobiogeography of the Glyptodontinae ALFREDO A
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by RERO DOC Digital Library Pal&ontologische Zeitschrift 2008, Vol. 82•2, p. 139-152, 30-06-2008 New Glyptodont from the Codore Formation (Pliocene), Falc6n State, Venezuela, its relationship with the Asterostemma problem, and the paleobiogeography of the Glyptodontinae ALFREDO A. CARLINI, La Plata; ALFREDO E. ZURITA, La Plata; GUSTAVO J. SCILLATO-YANI~, La Plata; RODOLFO S,&,NCHEZ, Urumaco & ORANGEL A. AGUILERA, Coro with 3 figures CARLINI, A.A.; ZURITA,A.E.; SCILLATO-YANI~,G.J.; S.~NCHEZ,R. & AGUILERA,O.A. 2008. New Glyptodont from the Codore Formation (Pliocene), Falc6n State, Venezuela, its relationship with the Asterostemma problem, and the paleo- biogeography of the Glyptodontinae. - Palaontologische Zeitschrift 82 (2): 139-152, 3 figs., Stuttgart, 30. 6. 2008. Abstract: One of the basal Glyptodontidae groups is represented by the Propalaehoplophorinae (late Oligocene - mid- dle Miocene), whose genera (Propalaehoplophorus, Eucinepeltus, Metopotoxus, Cochlops, and Asterostemma) were initially recognized in Argentinian Patagonia. Among these, Asterostemma was characterized by its wide latitudinal distribution, ranging from southernmost (Patagonia) to northernmost (Colombia, Venezuela) South America. How- ever, the generic assignation of the Miocene species from Colombia and Venezuela (A.? acostae, A. gigantea, and A. venezolensis) was contested by some authors, who explicitly accepted the possibility that these species could corre- spond to a new genus, different from those recognized in southern areas. A new comparative study of taxa from Argen- tinian Patagonia, Colombia and Venezuela (together with the recognition of a new genus and species for the Pliocene of the latter country) indicates that the species in northern South America are not Propalaehoplophorinae, but represent the first stages in the cladogenesis of the Glyptodontinae glyptodontids, the history of which was heretofore restricted to the late Miocene - early Holocene of southernmost South America. -
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. -
Mammals and Stratigraphy : Geochronology of the Continental Mammal·Bearing Quaternary of South America
MAMMALS AND STRATIGRAPHY : GEOCHRONOLOGY OF THE CONTINENTAL MAMMAL·BEARING QUATERNARY OF SOUTH AMERICA by Larry G. MARSHALLI, Annallsa BERTA'; Robert HOFFSTETTER', Rosendo PASCUAL', Osvaldo A. REIG', Miguel BOMBIN', Alvaro MONES' CONTENTS p.go Abstract, Resume, Resumen ................................................... 2, 3 Introduction .................................................................. 4 Acknowledgments ............................................................. 6 South American Pleistocene Land Mammal Ages ....... .. 6 Time, rock, and faunal units ...................... .. 6 Faunas....................................................................... 9 Zoological character and history ................... .. 9 Pliocene-Pleistocene boundary ................................................ 12 Argentina .................................................................... 13 Pampean .................................................................. 13 Uquian (Uquiense and Puelchense) .......................................... 23 Ensenadan (Ensenadense or Pampeano Inferior) ............................... 28 Lujanian (LuJanense or Pampeano lacus/re) .................................. 29 Post Pampean (Holocene) ........... :....................................... 30 Bolivia ................ '...................................................... ~. 31 Brazil ........................................................................ 37 Chile ........................................................................ 44 Colombia