Locomotory Adaptations in 3D Humerus Geometry of Xenarthra: Testing for Convergence
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Pleistocene Mammals and Paleoecology of the Western Amazon
PLEISTOCENE MAMMALS AND PALEOECOLOGY OF THE WESTERN AMAZON By ALCEU RANCY A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 1991 . To Cleusa, Bianca, Tiago, Thomas, and Nono Saul (Pistolin de Oro) . ACKNOWLEDGMENTS This work received strong support from John Eisenberg (chairman) and David Webb, both naturalists, humanists, and educators. Both were of special value, contributing more than the normal duties as members of my committee. Bruce MacFadden provided valuable insights at several periods of uncertainty. Ronald Labisky and Kent Redford also provided support and encouragement. My field work in the western Amazon was supported by several grants from the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) , and the Universidade Federal do Acre (UFAC) , Brazil. I also benefitted from grants awarded to Ken Campbell and Carl Frailey from the National Science Foundation (NSF) I thank Daryl Paul Domning, Jean Bocquentin Villanueva, Jonas Pereira de Souza Filho, Ken Campbell, Jose Carlos Rodrigues dos Santos, David Webb, Jorge Ferigolo, Carl Frailey, Ernesto Lavina, Michael Stokes, Marcondes Costa, and Ricardo Negri for sharing with me fruitful and adventurous field trips along the Amazonian rivers. The CNPq and the Universidade Federal do Acre, supported my visit to the. following institutions (and colleagues) to examine their vertebrate collections: iii . ; ; Universidade do Amazonas, Manaus -
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). -
Mammals from Upper Pleistocene of Afrânio, Pernambuco, Northeast of Brazil
Quaternary and Environmental Geosciences (2010) 02(2):01-11 Mamíferos do Pleistoceno Superior de Afrânio, Pernambuco, nordeste do Brasil Mammals from Upper Pleistocene of Afrânio, Pernambuco, northeast of Brazil Fabiana Marinho Silvaab, César Felipe Cordeiro Filgueirasac, Alcina Magnólia Franca Barretoad, Édison Vicente Oliveiraae a Universidade Federal de Pernambuco b c d e [email protected], [email protected], [email protected], [email protected] RESUMO Os mamíferos pleistocênicos são encontrados com frequência em toda a região Nordeste do Brasil. Os fósseis em geral ocorrem em tanques, lagoas, terraços fluviais, cavernas e ravinas. No estado de Pernambuco são registradas ocorrências de mamíferos pleistocênicos em 38 municípios. Neste trabalho, foram estudados aspectos taxonômicos e tafonômicos de paleofauna, preservada em lagoas da bacia do riacho Caboclo, tributário do rio São Francisco, em Afrânio, Pernambuco, Brasil. A pesquisa envolveu levantamento bibliográfico, cartográfico, trabalhos de campo e laboratoriais. Mais de 1.250 ossos, dentes e osteodermos foram estudados. A associação fossilífera é monotípica, poliespecífica, com os graus de fragmentação e desgaste variando em quatro classes. Os ossos foram preservados por conservação da composição química original, permineralização e substituição por calcita e por calcita magnesiana. Foi identificada uma diversificada fauna distribuída em cinco ordens (Tardigrada, Cingulata, Notoungulata, Proboscidea e Perissodactyla), sete famílias (Megatheriidae, Mylodontidae, Dasypodidae, Glyptodontidae, Toxodontidae, Gomphotheriidae e Equidae) com os taxa: Eremotherium laurillardi, Mylodonopsis ibseni, Panochthus greslebini, Holmesina paulacoutoi, Hoplophorus euphractus, Stegomastodon waringi, Toxodon platensis, equídeo e gliptodontideo indeterminados. Foram registrados pela primeira vez em Pernambuco os gêneros Hoplophorus e Mylodonopsis. A paleofauna é predominantemente herbívora, de um paleoambiente de savana ou cerrado. -
Late Cenozoic Large Mammal and Tortoise Extinction in South America
Cione et al: Late Cenozoic extinction Rev.in South Mus. America Argentino Cienc. Nat., n.s.1 5(1): 000, 2003 Buenos Aires. ISSN 1514-5158 The Broken Zig-Zag: Late Cenozoic large mammal and tortoise extinction in South America Alberto L. CIONE1, Eduardo P. TONNI1, 2 & Leopoldo SOIBELZON1 1Departamento Científico Paleontología de Vertebrados, 'acultad de Ciencias Naturales y Museo, Paseo del Bosque, 1900 La Plata, Argentina. 2Laboratorio de Tritio y Radiocarbono, LATYR. 'acultad de Ciencias Naturales y Museo, Paseo del Bosque, 1900 La Plata, Argentina. E-mail: [email protected], [email protected], [email protected]. Corresponding author: Alberto L. CIONE Abstract: During the latest Pleistocene-earliest Holocene, South American terrestrial vertebrate faunas suffered one of the largest (and probably the youngest) extinction in the world for this lapse. Megamammals, most of the large mammals and a giant terrestrial tortoise became extinct in the continent, and several complete ecological guilds and their predators disappeared. This mammal extinction had been attributed mainly to overkill, climatic change or a combination of both. We agree with the idea that human overhunting was the main cause of the extinction in South America. However, according to our interpretation, the slaughtering of mammals was accom- plished in a particular climatic, ecological and biogeographical frame. During most of the middle and late Pleis- tocene, dry and cold climate and open areas predominated in South America. Nearly all of those megamammals and large mammals that became extinct were adapted to this kind of environments. The periodic, though rela- tively short, interglacial increases in temperature and humidity may have provoked the dramatic shrinking of open areas and extreme reduction of the biomass (albeit not in diversity) of mammals adapted to open habitats. -
The Brazilian Megamastofauna of the Pleistocene/Holocene Transition and Its Relationship with the Early Human Settlement of the Continent
Earth-Science Reviews 118 (2013) 1–10 Contents lists available at SciVerse ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev The Brazilian megamastofauna of the Pleistocene/Holocene transition and its relationship with the early human settlement of the continent Alex Hubbe a,b,⁎, Mark Hubbe c,d, Walter A. Neves a a Laboratório de Estudos Evolutivos Humanos, Departamento de Genética e Biologia Evolutiva, Instituto de Biociências, Universidade de São Paulo, Rua do Matão 277, São Paulo, SP. 05508-090, Brazil b Instituto do Carste, Rua Barcelona 240/302, Belo Horizonte, MG. 30360-260, Brazil c Department of Anthropology, The Ohio State University, 174W 18th Avenue, Columbus, OH. 43210, United States d Instituto de Investigaciones Arqueológicas y Museo, Universidad Católica del Norte, Calle Gustavo LePaige 380, San Pedro de Atacama, 141-0000, Chile article info abstract Article history: One of the most intriguing questions regarding the Brazilian Late Quaternary extinct megafauna and Homo Received 4 October 2012 sapiens is to what extent they coexisted and how humans could have contributed to the former's extinction. Accepted 18 January 2013 The aim of this article is to review the chronological and archaeological evidences of their coexistence in Available online 25 January 2013 Brazil and to evaluate the degree of direct interaction between them. Critical assessment of the Brazilian megafauna chronological data shows that several of the late Pleistoscene/early Holocene dates available so Keywords: far cannot be considered reliable, but the few that do suggest that at least two species (Catonyx cuvieri, Quaternary Mammals ground sloth; Smilodon populator, saber-toothed cat) survived until the beginning of the Holocene in Southeast Extinction Brazil. -
1 TABLE S1 Global List of Extinct and Extant Megafaunal Genera By
Supplemental Material: Annu. Rev. Ecol. Syst.. 2006. 37:215-50 doi: 10.1146/annurev.ecolsys.34.011802.132415 Late Quaternary Extinctions: State of the Debate Koch and Barnosky TABLE S1 Global list of extinct and extant megafaunal genera by continent. STATUS TAXON TIME AFRICA Mammalia Carnivora Felidae Acinonyx Panthera Hyaenidae Crocuta Hyaena Ursidae Ursusa Primates Gorilla Proboscidea Elephantidae C Elephas <100 Loxodonta Perissodactyla Equidae S Equus <100 E Hipparion <100 Rhinocerotidae Ceratotherium Diceros E Stephanorhinus <100 Artiodactyla Bovidae Addax Ammotragus Antidorcas Alcelaphus Aepyceros C Bos 11.5-0 Capra Cephalopus Connochaetes Damaliscus Gazella S Hippotragus <100 Kobus E Rhynotragus/Megalotragus 11.5-0 Oryx E Pelorovis 11.5-0 E Parmulariusa <100 Redunca Sigmoceros Syncerus Taurotragus Tragelaphus Camelidae C Camelus <100 1 Supplemental Material: Annu. Rev. Ecol. Syst.. 2006. 37:215-50 doi: 10.1146/annurev.ecolsys.34.011802.132415 Late Quaternary Extinctions: State of the Debate Koch and Barnosky Cervidae E Megaceroides <100 Giraffidae S Giraffa <100 Okapia Hippopotamidae Hexaprotodon Hippopotamus Suidae Hylochoerus Phacochoerus Potamochoerus Susa Tubulidenta Orycteropus AUSTRALIA Reptilia Varanidae E Megalania 50-15.5 Meiolanidae E Meiolania 50-15.5 E Ninjemys <100 Crocodylidae E Palimnarchus 50-15.5 E Quinkana 50-15.5 Boiidae? E Wonambi 100-50 Aves E Genyornis 50-15.5 Mammalia Marsupialia Diprotodontidae E Diprotodon 50-15.5 E Euowenia <100 E Euryzygoma <100 E Nototherium <100 E Zygomaturus 100-50 Macropodidae S Macropus 100-50 E Procoptodon <100 E Protemnodon 50-15.5 E Simosthenurus 50-15.5 E Sthenurus 100-50 Palorchestidae E Palorchestes 50-15.5 Thylacoleonidae E Thylacoleo 50-15.5 Vombatidae S Lasiorhinus <100 E Phascolomys <100 E Phascolonus 50-15.5 E Ramsayia <100 2 Supplemental Material: Annu. -
Osteoderm Histology of Late Pleistocene Cingulates from the Intertropical Region of Brazil
Osteoderm histology of Late Pleistocene cingulates from the intertropical region of Brazil PAULO VICTOR LUIZ GOMES DA COSTA PEREIRA, GUSTAVO DUARTE VICTER, KLEBERSON DE OLIVEIRA PORPINO, and LÍLIAN PAGLARELLI BERGQVIST Da Costa Pereira, P.V.L.G., Victer, G.D., Porpino, K.O., and Bergqvist, L.P. 2014. Osteoderm histology of Late Pleisto- cene cingulates from the intertropical region of Brazil. Acta Palaeontologica Polonica 59 (3): 543–552. During the Late Pleistocene, several possibly endemic cingulate species, known mostly from isolated osteoderms, cara- pace fragments, and caudal tubes, coexisted in the Brazilian Intertropical Region. Here, we describe the osteoderm micro- structure of Pachyarmatherium brasiliense, as well as the glyptodonts Panochthus greslebini, Panochthus jaguaribensis and Glyptotherium sp., in order to provide additional species-diagnostic characters and shed light on their evolutionary relationships. Pachyarmatherium brasiliense lacks several derived features shared by glyptodonts and pampatheres, such as extensive bone remodeling, fibers arranged in large bundles, and relatively poorly developed layers of compact bone, thus supporting its exclusion from glyptodonts as suggested by a recent cladistic study. The osteoderm histology of P. greslebini resembles that of other species of Panochthus (e.g., Panochthus frenzelianus). By contrast, the presence of relatively thick layers of compact bone, the configuration and size of resorption areas, the absence of randomly oriented lateral fiber bundles, and the absence of an intermediary region between the compact and trabecular bone potentially support the exclusion of Panochthus jaguaribensis from the genus. Finally, osteoderms of the Brazilian specimens of Glyptodontinae share histological features with Glyptotherium floridanus, rather than Glyptodon, thus reinforcing their assignment to Glyptotherium. -
Distributional Patterns of Herbivore Megamammals During the Late Pleistocene of South America
Anais da Academia Brasileira de Ciências (2013) 85(2): 533-546 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 www.scielo.br/aabc Distributional patterns of herbivore megamammals during the Late Pleistocene of South America VALÉRIA GALLO1, LEONARDO S. AVILLA2, RODRIGO C.L. PEREIRA1,2 and BRUNO A. ABSOLON1,2 1Universidade do Estado do Rio de Janeiro, Instituto de Biologia, Departamento de Zoologia, Laboratório de Sistemática e Biogeografi a, Rua São Francisco Xavier, 524, Maracanã, 20550-013 Rio de Janeiro, RJ, Brasil 2Universidade Federal do Estado do Rio de Janeiro, Instituto de Biociências, Departamento de Zoologia, Laboratório de Mastozoologia, Avenida Pasteur, 458, Urca, 22290-240 Rio de Janeiro, RJ, Brasil Manuscript received on October 10, 2012; accepted for publication on January 21, 2013 ABSTRACT The geographic distribution of 27 species of the South American megafauna of herbivore mammals during the Late Pleistocene was analyzed in order to identify their distributional patterns. The distribution of the species was studied using the panbiogeographical method of track analysis. Six generalized tracks (GTs) and two biogeographic nodes were obtained. The GTs did not completely superpose with the areas of open savanna present in Pleistocene, nor with the biotic tracks of some arthropods typical of arid climate, indicating that these animals avoided arid environment. Overall, the GTs coincided with some biogeographic provinces defi ned on the basis of living taxa, indicating that certain current distributional patterns already existed in Pleistocene. The biogeographic nodes coincided with the borders between the main vegetal formations of the Pleistocene, showing that the type of vegetation had great infl uence in the distribution of the mammalian megafauna. -
Universidade Federal De Pernambuco Centro De Tecnologia E Geociências Pós-Graduação Em Geociências
UNIVERSIDADE FEDERAL DE PERNAMBUCO CENTRO DE TECNOLOGIA E GEOCIÊNCIAS PÓS-GRADUAÇÃO EM GEOCIÊNCIAS Rosembergh da Silva Alves OS MAMÍFEROS PLEISTOCÊNICOS DE FAZENDA NOVA, BREJO DA MADRE DE DEUS, PERNAMBUCO: ASPECTOS TAFONÔMICOS, TAXONÔMICOS E PALEOAMBIENTAIS Dissertação de Mestrado 2007 ROSEMBERGH DA SILVA ALVES Biólogo, Universidade Federal Rural de Pernambuco, 2004. OS MAMÍFEROS PLEISTOCÊNICOS DE FAZENDA NOVA, BREJO DA MADRE DE DEUS, PERNAMBUCO: ASPECTOS TAFONÔMICOS, TAXONÔMICOS E PALEOAMBIENTAIS Dissertação que apresenta à Pós-Graduação em Geociências do Centro de Tecnologia e Geociências da Universidade Federal de Pernambuco, orientada pela Profa. Dra. Alcina Magnólia Franca Barreto, como preenchimento parcial dos requisitos para obtenção do grau de Mestre em Geociências, área de concentração Geologia Sedimentar e Ambiental. RECIFE, PE 2007 A474m Alves, Rosembergh da Silva Os mamíferos pleistocênicos de Fazenda Nova, Brejo da Madre de Deus, Pernambuco: aspectos tafonômicos, taxonômicos e paleoambientais / Rosembergh da Silva Alves. – Recife: O Autor, 2007. 127 f.; il., gráfs., tabs. Dissertação (Mestrado) – Universidade Federal de Pernambuco. CTG. Programa de Pós-Graduação em Geociências, 2007. Inclui Referências Bibliográficas e Anexos. 1. Geociências. 2. Mamíferos Pleistocênicos. 3. Fazenda Nova. 4. Brejo da Madre de Deus. 5. Tafonomia. 6. Taxonomia. 7. Geocronologia. I. Título. 551 CDD (22.ed.) UFPE BCTG/2008-093 Dedico a minha avó Maria Quitéria (in memorian). Meus pais Adson e Valdelice. Meus sobrinhos Jônatas e Maria Luiza. E ao meu companheiro Fábio. Meus olhos brilham, o coração bate acelerado, esqueço o cansaço e só consigo pensar na incrível sensação de encontrar algo que a natureza não quis. É assim que me sinto, sou um Paleontólogo! “Foi Deus quem me deu a verdadeira ciência de todas as coisas, quem me fez conhecer a constituição do mundo”. -
Nuevos Aportes a La Sistemática De Los “Plohophorini” De Uruguay (Mammalia, Cingulata, Glyptodontidae)
NUEVOS APORTES A LA SISTEMÁTICA DE LOS “PLOHOPHORINI” DE URUGUAY (MAMMALIA, CINGULATA, GLYPTODONTIDAE) Pablo Toriño Licenciatura en Ciencias Biológicas, profundización en Paleontología. Instituto de Ciencias Geológicas - Departamento de Paleontología. Facultad de Ciencias (UdelaR). Orientador: Dr. Daniel Perea Tribunal: Dr. Sergio Martínez, Dr. Martín Ubilla Montevideo, 2015 - 1 - Imagen de portada: Placa de coraza asignada al gliptodonte Pseudoplohophorus en el presente trabajo (FC-DPV 384), hallada en las barrancas de San Gregorio, departamento de San José (Uruguay). Procedencia estratigráfica: Formación Camacho (Mioceno Tardío). - 2 - A la memoria de Domingo Pablo Toriño (1944-2010), mi Padre, mi Héroe. Y de Maru (2004-2015), por tantos lindos recuerdos. - 3 - - 4 - Indice Resumen ………………………………………………………………………………………………………………………………………………………7 Abstract ………………………………………………………………………………………………………………………………………………………..8 1. Introducción …………………………………………………………………………………………………………………………………………….9 1.1. Antecedentes y fundamentación ………………………………………………………………………………………………………..9 1.2. Objetivos ……………………………………………………………………………………………………………………………………………21 2. Materiales y metodología …………………………………………………………………………………………………………………… 22 2.1. Relevamiento de colecciones ……………………………………………………………………………………………………………..22 2.2. Revisión taxonómica …………………………………………………………………………………………………………………………..24 2.3. Obtención de medidas ……………………………………………………………………………………………………………………….24 2.4. Análisis cuantitativos ………………………………………………………………………………………………………………………….34 3. Resultados ……………………………………………………………………………………………………………………………………………….36 -
Kellner1 and Diogenes De Almeida Campos2 Vertebrate Paleontology in Brazil — a Review
238 by Alexander W. A. Kellner1 and Diogenes de Almeida Campos2 Vertebrate paleontology in Brazil — a review 1. Dept. Geology and Paleontology, Museu Nacional/UFRJ, Quinta da Boa Vista, São Cristóvão, Rio de Janeiro, Brazil; e-mail: [email protected] 2. Museu de Ciências da Terra, DNPM, Av. Pasteur 404, Rio de Janeiro, Brazil; e-mail: [email protected] A review of the vertebrate fossil diversity in Brazil is pod footprint from the Paraná Basin (Leonardi, 1983), vertebrate presented. The best known faunas are the fish and rep- remains from this era have only been briefly mentioned in faunal lists from Devonian strata (e.g., Katzer, 1897a, b; Kegel, 1953, 1957; tiles from the Santana Formation (both, Crato and Santos, 1961; Mendes and Petri, 1971; Copper, 1977). Romualdo Members). Also comparatively well known In the last two decades some isolated Paleozoic specimens were are the mammalian faunas from Pleistocene deposits, described in detail. Among those are isolated actinopterygian scales found in drilling cores of an oil well in the Upper Amazon Basin, which is the result of extensive research done in the last Northwestern Brazil (Janvier and Melo, 1987). These scales are pre- decades. Poorly known are the Paleozoic vertebrates, served in black shales and suggest either a very Late Devonian or a which is possible due to the limited outcrops in the Carboniferous age for those sediments, although the associated microfossils favor a pre-Mississippian assignment (Janvier and country. Paradoxically, the Late Cretaceous vertebrate Melo, 1987). Those authors also reported acanthodian remains from faunas (fishes, reptiles, and mammals) from the Bauru Devonian strata of the same basin (Janvier and Melo, 1988; 1992). -
GLYPTOTHERIUM TEXANUM, a NEW GLYPTODONT, from the LOWER PLEISTOCENE of TEXAS. by HENRY FAIRFIELD OSBORN. the Exist
Article XVII.- GLYPTOTHERIUM TEXANUM, A NEW GLYPTODONT, FROM THE LOWER PLEISTOCENE OF TEXAS. By HENRY FAIRFIELD OSBORN. PLATE XLIII. The existence of Glyptodonts in the United States was made known by Cope I in i888 in his description of Glyptodon petaliferus, based on a single carapace scute or plate from the Lower Pleistocene Equus Beds of Texas; and by Leidy 2 in I889 in his Glyptodon septentrionalis, based on carapace and caudal scutes from Florida; Leidy also described3 and figured from Florida plates of the G. petaliferus type. The American Museum Expedition sent out by the writer, with the aid of the William C. Whitney Fund, under the leadership of Mr. J. W. Gidley, was fortunate in securing the nearly complete carapace, pelvis, sacrum, caudals, and complete tail armature of an individual in fine preservation. It proves to represent a new genus and species, combining characters of several of the South American forms of the Pleistocene and Miocene periods. The specimen was skillfully brought in by Mr. Gidley and prepared and mounted under the direction of Mr. Adam Hermann. The writer is especially indebted to Prof. W. B. Scott for pointing out several of the *features in which Glyptotherium differs from the known South American genera. Also to Mr. W. K. Gregory for the preparation of the manu- script for the press. The specific distinctions given below' are derived by com- parison of (i) the specimens referred by Leidv to G. petaliferus and of (2) Cope's description, which runs as follows: ". with the circumferential areas of the rosette but little smaller than the central one.