Multiproxy Evidence for Leaf-Browsing and Closed Habitats in Extinct Proboscideans (Mammalia, Proboscidea) from Central Chile
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Matheus Souza Lima Ribeiro
Palaeogeography, Palaeoclimatology, Palaeoecology 392 (2013) 546–556 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Climate and humans set the place and time of Proboscidean extinction in late Quaternary of South America Matheus Souza Lima-Ribeiro a,b,⁎, David Nogués-Bravo c,LeviCarinaTerribilea, Persaram Batra d, José Alexandre Felizola Diniz-Filho e a Departamento de Ciências Biológicas, Universidade Federal de Goiás, Campus Jataí, Cx. Postal 03, 75804-020 Jataí, GO, Brazil b Programa de Pós-graduação em Ecologia e Evolução, Universidade Federal de Goiás, Cx. Postal 131, 74001-970 Goiânia, GO, Brazil c Centre for Macroecology, Evolution and Climate, University of Copenhagen, Universitetsparken 15, 2100, Denmark d Department of Geology, Greenfield Community College, Greenfield, MA 01301, USA e Departamento de Ecologia, ICB, Universidade Federal de Goiás, Cx. Postal 131, 74001-970 Goiânia, GO, Brazil article info abstract Article history: The late Quaternary extinctions have been widely debated for a long time, but the varying magnitude of Received 18 April 2013 human vs. climate change impacts across time and space is still an unresolved question. Here we assess Received in revised form 7 October 2013 the geographic range shifts in response to climate change based on Ecological Niche Models (ENMs) and Accepted 21 October 2013 modeled the timing for extinction under human hunting scenario, and both variables were used to explain Available online 30 October 2013 the extinction dynamics of Proboscideans during a full interglacial/glacial cycle (from 126 ka to 6 ka) in South America. We found a large contraction in the geographic range size of two Proboscidean species stud- Keywords: Late Quaternary extinctions ied (Cuvieronius hyodon and Notiomastodon platensis) across time. -
The Mastodonts of Brazil': the State of the Art of South American
Quaternary International 443 (2017) 52e64 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Sixty years after ‘The mastodonts of Brazil’: The state of the art of South American proboscideans (Proboscidea, Gomphotheriidae) * Dimila Mothe a, b, , Leonardo dos Santos Avilla a, c, Lidiane Asevedo a, d, Leon Borges-Silva a, Mariane Rosas e, Rafael Labarca-Encina f, Ricardo Souberlich g, Esteban Soibelzon h, i, Jose Luis Roman-Carrion j, Sergio D. Ríos k, Ascanio D. Rincon l, Gina Cardoso de Oliveira b, Renato Pereira Lopes m a Laboratorio de Mastozoologia, Departamento de Zoologia, Instituto de Bioci^encias, Universidade Federal do Estado do Rio de Janeiro, Av. Pasteur, 458, 501, Urca, CEP 22290-240, Rio de Janeiro, Brazil b Programa de Pos-graduaç ao~ em Geoci^encias, Centro de Tecnologia e Geoci^encias, Universidade Federal de Pernambuco, Rua Acad^emico Helio Ramos, s/n, Cidade Universitaria, CEP 50740-467, Recife, Brazil c Programa de Pos-graduaç ao~ em Biodiversidade Neotropical, Instituto de Bioci^encias, Universidade Federal do Estado do Rio de Janeiro, Av. Pasteur, 458, 501, Urca, CEP 22290-240, Rio de Janeiro, Brazil d Faculdade de Geoci^encias (Fageo), Campus Cuiaba, Universidade Federal de Mato Grosso, Av. Fernando Correa da Costa, 2367, Jardim Petropolis, CEP 78070-000, Cuiaba, Mato Grosso, Brazil e Laboratorio de Paleontologia, Centro de Ci^encias Agrarias, Ambientais e Biologicas, Universidade Federal do Reconcavo^ da Bahia, Cruz das Almas, Bahia, Brazil f Laboratorio de Paleoecología, Instituto de Ciencias Ambientales y Evolutivas, Universidad Austral de Chile, Casilla 567, Valdivia, Chile g Laboratorio de Paleontología, Departamento de Geología, Facultad de Ciencias Exactas y Naturales, Acceso Av. -
Variable Impact of Late-Quaternary Megafaunal Extinction in Causing
Variable impact of late-Quaternary megafaunal SPECIAL FEATURE extinction in causing ecological state shifts in North and South America Anthony D. Barnoskya,b,c,1, Emily L. Lindseya,b, Natalia A. Villavicencioa,b, Enrique Bostelmannd,2, Elizabeth A. Hadlye, James Wanketf, and Charles R. Marshalla,b aDepartment of Integrative Biology, University of California, Berkeley, CA 94720; bMuseum of Paleontology, University of California, Berkeley, CA 94720; cMuseum of Vertebrate Zoology, University of California, Berkeley, CA 94720; dRed Paleontológica U-Chile, Laboratoria de Ontogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Chile; eDepartment of Biology, Stanford University, Stanford, CA 94305; and fDepartment of Geography, California State University, Sacramento, CA 95819 Edited by John W. Terborgh, Duke University, Durham, NC, and approved August 5, 2015 (received for review March 16, 2015) Loss of megafauna, an aspect of defaunation, can precipitate many megafauna loss, and if so, what does this loss imply for the future ecological changes over short time scales. We examine whether of ecosystems at risk for losing their megafauna today? megafauna loss can also explain features of lasting ecological state shifts that occurred as the Pleistocene gave way to the Holocene. We Approach compare ecological impacts of late-Quaternary megafauna extinction The late-Quaternary impact of losing 70–80% of the megafauna in five American regions: southwestern Patagonia, the Pampas, genera in the Americas (19) would be expected to trigger biotic northeastern United States, northwestern United States, and Berin- transitions that would be recognizable in the fossil record in at gia. We find that major ecological state shifts were consistent with least two respects. -
Mammalia, Proboscidea, Gomphotheriidae): Taxonomy, Phylogeny, and Biogeography
J Mammal Evol DOI 10.1007/s10914-012-9192-3 ORIGINAL PAPER The South American Gomphotheres (Mammalia, Proboscidea, Gomphotheriidae): Taxonomy, Phylogeny, and Biogeography Dimila Mothé & Leonardo S. Avilla & Mario A. Cozzuol # Springer Science+Business Media, LLC 2012 Abstract The taxonomic history of South American Gom- peruvium, seems to be a crucial part of the biogeography photheriidae is very complex and controversial. Three species and evolution of the South American gomphotheres. are currently recognized: Amahuacatherium peruvium, Cuvieronius hyodon,andNotiomastodon platensis.Thefor- Keywords South American Gomphotheres . Systematic mer is a late Miocene gomphothere whose validity has been review. Taxonomy. Proboscidea questioned by several authors. The other two, C. hyodon and N. platensis, are Quaternary taxa in South America, and they have distinct biogeographic patterns: Andean and lowland Introduction distributions, respectively. South American gomphotheres be- came extinct at the end of the Pleistocene. We conducted a The family Gomphotheriidae is, so far, the only group of phylogenetic analysis of Proboscidea including the South Proboscidea recorded in South America. Together with the American Quaternary gomphotheres, which resulted in two megatheriid sloths Eremotherium laurillardi Lund, 1842, most parsimonious trees. Our results support a paraphyletic the Megatherium americanum Cuvier, 1796,andthe Gomphotheriidae and a monophyletic South American notoungulate Toxodon platensis Owen, 1840, they are the gomphothere lineage: C. hyodon and N. platensis. The late most common late Pleistocene representatives of the mega- Miocene gomphothere record in Peru, Amahuacatherium fauna in South America (Paula-Couto 1979). Similar to the Pleistocene and Holocene members of the family Elephan- tidae (e.g., extant elephants and extinct mammoths), the D. -
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 -
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. -
A Grazing Gomphotherium in Middle Miocene Central Asia, 10
www.nature.com/scientificreports OPEN A grazing Gomphotherium in Middle Miocene Central Asia, 10 million years prior to the origin of the Received: 16 November 2017 Accepted: 29 March 2018 Elephantidae Published: xx xx xxxx Yan Wu1,2, Tao Deng1,2,3, Yaowu Hu1,7, Jiao Ma1,7, Xinying Zhou1,2, Limi Mao4, Hanwen Zhang 5,6, Jie Ye1 & Shi-Qi Wang1,2,3 Feeding preference of fossil herbivorous mammals, concerning the coevolution of mammalian and foral ecosystems, has become of key research interest. In this paper, phytoliths in dental calculus from two gomphotheriid proboscideans of the middle Miocene Junggar Basin, Central Asia, have been identifed, suggesting that Gomphotherium connexum was a mixed feeder, while the phytoliths from G. steinheimense indicates grazing preference. This is the earliest-known proboscidean with a predominantly grazing habit. These results are further confrmed by microwear and isotope analyses. Pollen record reveals an open steppic environment with few trees, indicating an early aridity phase in the Asian interior during the Mid-Miocene Climate Optimum, which might urge a diet remodeling of G. steinheimense. Morphological and cladistic analyses show that G. steinheimense comprises the sister taxon of tetralophodont gomphotheres, which were believed to be the general ancestral stock of derived “true elephantids”; whereas G. connexum represents a more conservative lineage in both feeding behavior and tooth morphology, which subsequently became completely extinct. Therefore, grazing by G. steinheimense may have acted as a behavior preadaptive for aridity, and allowing its lineage evolving new morphological features for surviving later in time. This study displays an interesting example of behavioral adaptation prior to morphological modifcation. -
Redalyc.FOSSIL PROBOSCIDEA from the UPPER CENOZOIC OF
Revista Geológica de América Central ISSN: 0256-7024 [email protected] Universidad de Costa Rica Costa Rica Lucas, Spencer G.; Alvarado, Guillermo E. FOSSIL PROBOSCIDEA FROM THE UPPER CENOZOIC OF CENTRAL AMERICA: TAXONOMY, EVOLUTIONARY AND PALEOBIOGEOGRAPHIC SIGNIFICANCE Revista Geológica de América Central, núm. 42, 2010, pp. 9-42 Universidad de Costa Rica San José, Costa Rica Disponible en: http://www.redalyc.org/articulo.oa?id=45437349001 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Revista Geológica de América Central, 42: 9-42, 2010 ISSN: 0256-7024 FOSSIL PROBOSCIDEA FROM THE UPPER CENOZOIC OF CENTRAL AMERICA: TAXONOMY, EVOLUTIONARY AND PALEOBIOGEOGRAPHIC SIGNIFICANCE Proboscideos FÓsiles del Cenozoico Superior de AMÉrica Central: TaxonomÍA, evoluciÓN Y significado paleogeogrÁfico Spencer G. Lucas1* & Guillermo E. Alvarado2 1New Mexico Museum of Natural History and Science, 1801 Mountain Road N.W., Albuquerque, New Mexico 87104 USA 2Escuela Centroamericana de Geología, Universidad de Costa Rica, Apdo. 214, 2060, San José, Costa Rica *Autor para contacto: [email protected] (Recibido: 03/02/2010; aceptado: 22/06/2010) ABSTRACT: Fossils of proboscideans from Central America are assigned to four genera: Gomphotherium, Cuvieronius, Mammut and Mammuthus. Previous reports of Stegomastodon, Rhynchotherium and Haplomastodon from Central Amer- ica are based on incorrect taxonomic identifications or on fossils not definitely diagnostic of these genera. The oldest proboscidean records from Central America (Guatemala, El Salvador, Honduras, and Costa Rica) are Late Miocene (early Hemphillian, ~ 7 Ma) records of Gomphotherium, and this suggests that gomphotheres dispersed from North America to Central America about nine million years after they dispersed from Asia to North America. -
Mammalia: Proboscidea: Gomphotheriidae) from the Continental Shelf, Pearl Islands, Panama
Quaternary International xxx (2015) 1e14 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Forum communication Quaternary gomphotheres (Mammalia: Proboscidea: Gomphotheriidae) from the continental shelf, Pearl Islands, Panama * Gary S. Morgan a, , Bruce J. MacFadden b, Martín Martínez c a New Mexico Museum of Natural History, Albuquerque, NM 87104, USA b Florida Museum of Natural History, University of Florida, Gainesville, FL 32611, USA c Museo de Ciencias Naturales de Panama, Panama City, Panama article info abstract Article history: Fishermen have recovered four Quaternary proboscidean teeth from the continental shelf in the vicinity Available online xxx of the Pearl Islands, about 50e80 km offshore from the southern coast of Panama. Two upper third molars (M3) and one lower third molar (m3) are similar to comparable teeth of the Pleistocene gom- Keywords: phothere Cuvieronius based on the presence of 4½ to 5½ lophs/lophids that are either horizontal or Pearl Islands slightly inclined to long axis of the tooth and rather complicated enamel with single trefoils, incipient Panama double trefoils, and numerous small accessory cusps. Cuvieronius is also known from the Pleistocene El Pleistocene Hatillo and La Trinidaíta sites from the Azuero Peninsula in Panama. The teeth of Cuvieronius from the Gomphothere Cuvieronius Pearl Islands are referred to C. hyodon following recent taxonomic revisions indicating a single pan- American species of this genus was present in both North America and South America. The oldest re- cords of Cuvieronius are from early Pleistocene (early Irvingtonian) faunas in El Salvador, Florida, and New Mexico. Cuvieronius dispersed to South America in the early Pleistocene during the Great American Biotic Interchange, with the earliest record of C. -
Diversity of the Pleistocene Gomphotheres (Gomphotheriidae, Proboscidea) from South America
José Luis Prado 1, María Teresa Alberdi 2, Begoña Sánchez 2 & Beatriz Azanza 2 1 Universidad Nacional del Centro UNC, Olavarría 2 Museo Nacional de Ciencias Naturales, Madrid Diversity of the Pleistocene Gomphotheres (Gomphotheriidae, Proboscidea) from South America Prado, J.L., Alberdi, M.T. , Sánchez, B. & Azanza, B., 2003 - Diversity of the Pleistocene Gomphotheres (Gomphotheriidae, Proboscidea) from South America - in: Reumer, J.W.F., De Vos, J. & Mol, D. (eds.) - ADVANCES IN MAMMOTH RESEARCH (Proceedings of the Second International Mammoth Conference, Rotterdam, May 16-20 1999) - DEINSEA 9: 347-363 [ISSN 0923-9308] Published 24 May 2003 The gomphotheres were recorded in South America from the early Middle Pleistocene (Ensenadan Land-mammal Age) to the latest Pleistocene (Lujanian Land-mammal Age). They were descen- dants of the gomphothere stock that originated in North America and arrived to South America during the ‘Great American Biotic Interchange’. Only two genera are recognised: Cuvieronius with only one species (Cuvieronius hyodon), and Stegomastodon with two species (Stegomastodon waringi and Stegomastodon platensis). Two corridors would have developed during the Pleistocene in South America. These two corridors have conditioned the paleobiogeographic his- tory of most North American mammals in South America. In fact, different models can be postu- lated for different groups depending on their capacity to produce distinct adaptive types throug- hout the duration of their dispersion process. In the case of South American gomphotheres, the small Cuvieronius utilised the Andean corridor, whereas the larger Stegomastodon dispersed through the eastern route. Cuvieronius hyodon is geographically restricted to the Andean Region in Ecuador, Peru, Bolivia, Chile and Northwestern Argentina, it inhabited an arid landscape. -
Advances in Proboscidean Taxonomy & Classification, Anatomy
ARTICLE IN PRESS Quaternary International 126–128 (2005) 5–20 Advances in proboscidean taxonomy & classification, anatomy & physiology, and ecology & behavior Jeheskel Shoshania,b,*, Pascal Tassyc a Department of Biology, University of Asmara, P.O. Box 1220, Asmara, Eritrea (Horn of Africa) b Elephant Research Foundation, 106 East Hickory Grove Road, Bloomfield Hills, MI 48304, USA c Museum national d’Histoire naturelle Laboratoire de Paleontologie, 8 rue Buffon, 75005 Paris, France Available online 26 June 2004 Abstract With the addition of 13 new taxa, we recognized 175 species and subspecies of proboscideans, classified in 42 genera and 10 families. The three extant species are: forest African elephant (Loxodonta cyclotis), bush African elephant (L. africana), and Asian elephant (Elephas maximus, with three subspecies). Rigorous analysis of characters published or awaiting publication is imperative for better understanding of the cladistic relationships among currently recognized proboscideans. Here we focus on ‘‘aquatic ancestry’’ of Proboscidea, interordinal relationships within Placentalia, proboscidean taxonomy in general and South American in particular, anatomy and physiology and some ecological considerations. New taxa above the family level include sister taxa Mammutida and Elephantida, and Plesielephantiformes as a sister taxon to Elephantiformes. Neontological research is currently under way on the hyoid apparatus, lungs, brain, hearing, ecology and behavior. Topics for future research include: phylogenetic positions of anthracobunids, Moeritherium, tetralophodont gomphotheres, Stegolophodon and Stegodon, and intra-familial relationships among Loxodonta, Elephas and Mammuthus, and continuing studies on encephalization quotient. Certain anatomical features and functions (e.g., the hyoid apparatus that helps in food procurement, in production of infrasonic sounds, and in storing water to be used in time of stress) evolved about 25 million years ago, in time for diversification into new niches when grasses appeared in the landscape.