Body Mass Estimation of a Giant Extinct Rodent
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Illustratedencycloped Iadinosaursandprehist
I L L U S T R A T E D E N C Y C L Baryonyx THEROPODS F A C T F I L E O # Tyrannosaurus Rex’s head was about 1.5 m long. Its lower jaw was hinged in such heropods were a group of mostly a way as to maximize its gape. An eight-year- P meat-eating saurischian ( 13) or old child could have squatted in its jaws. “lizard hipped” dinosaurs. They all T # Compsognathus, discovered in Germany had three toes and their name means in the 1850s, was the first ever dinosaur to E “beast-footed”. Theropods were the first be found as a complete skeleton. kind of dinosaur to evolve. They had large # Most experts agree that birds evolved eyes and long tails.They ran on their two Baryonyx A meat-eating dinosaur from the Compsognathus A tiny meat-eating from small dinosaurs. Archaeopteryx, the D strong back legs, leaving their arms free to Cretaceous period. It had the body of a dinosaur from the Late Jurassic. It was first known bird, is closely related to the raptors and may have evolved directly from grasp or pin down their prey. They ranged large carnivore, about eight metres long, about the size of a chicken and preyed on them. The presence of small bumps or quill in size from tiny Compsognathus, the size but its skull was long and narrow, with insects and lizards. It was probably the bones on a Velociraptor fossil I of a chicken, to 18 m long Spinosaurus. -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
Genus/Species Skull Ht Lt Wt Stage Range Abalosia U.Pliocene S America Abelmoschomys U.Miocene E USA A
Genus/Species Skull Ht Lt Wt Stage Range Abalosia U.Pliocene S America Abelmoschomys U.Miocene E USA A. simpsoni U.Miocene Florida(US) Abra see Ochotona Abrana see Ochotona Abrocoma U.Miocene-Recent Peru A. oblativa 60 cm? U.Holocene Peru Abromys see Perognathus Abrosomys L.Eocene Asia Abrothrix U.Pleistocene-Recent Argentina A. illuteus living Mouse Lujanian-Recent Tucuman(ARG) Abudhabia U.Miocene Asia Acanthion see Hystrix A. brachyura see Hystrix brachyura Acanthomys see Acomys or Tokudaia or Rattus Acarechimys L-M.Miocene Argentina A. minutissimus Miocene Argentina Acaremys U.Oligocene-L.Miocene Argentina A. cf. Murinus Colhuehuapian Chubut(ARG) A. karaikensis Miocene? Argentina A. messor Miocene? Argentina A. minutissimus see Acarechimys minutissimus Argentina A. minutus Miocene? Argentina A. murinus Miocene? Argentina A. sp. L.Miocene Argentina A. tricarinatus Miocene? Argentina Acodon see Akodon A. angustidens see Akodon angustidens Pleistocene Brazil A. clivigenis see Akodon clivigenis Pleistocene Brazil A. internus see Akodon internus Pleistocene Argentina Acomys L.Pliocene-Recent Africa,Europe,W Asia,Crete A. cahirinus living Spiny Mouse U.Pleistocene-Recent Israel A. gaudryi U.Miocene? Greece Aconaemys see Pithanotomys A. fuscus Pliocene-Recent Argentina A. f. fossilis see Aconaemys fuscus Pliocene Argentina Acondemys see Pithanotomys Acritoparamys U.Paleocene-M.Eocene W USA,Asia A. atavus see Paramys atavus A. atwateri Wasatchian W USA A. cf. Francesi Clarkforkian Wyoming(US) A. francesi(francesci) Wasatchian-Bridgerian Wyoming(US) A. wyomingensis Bridgerian Wyoming(US) Acrorhizomys see Clethrionomys Actenomys L.Pliocene-L.Pleistocene Argentina A. maximus Pliocene Argentina Adelomyarion U.Oligocene France A. vireti U.Oligocene France Adelomys U.Eocene France A. -
Miocene Development of Life
Miocene Development of Life Jarðsaga 2 - Saga Lífs og Lands - Ólafur Ingólfsson Thehigh-pointof theage of mammals The Miocene or "less recent" is so called because it contains fewer modern animals than the following Pliocene. The Miocene lasted for 18 MY, ~23-5 MY ago. This was a huge time of transition, the end of the old prehistoric world and the birth of the more recent sort of world. It was also the high point of the age of mammals Open vegetation systems expand • The overall pattern of biological change for the Miocene is one of expanding open vegetation systems (such as deserts, tundra, and grasslands) at the expense of diminishing closed vegetation (such as forests). • This led to a rediversification of temperate ecosystems and many morphological changes in animals. Mammals and birds in particular developed new forms, whether as fast-running herbivores, large predatory mammals and birds, or small quick birds and rodents. Two major ecosystems evolve Two major ecosystems first appeared during the Miocene: kelp forests and grasslands. The expansion of grasslands is correlated to a drying of continental interiors and a global cooling. Later in the Miocene a distinct cooling of the climate resulted in the further reduction of both tropical and conifer forests, and the flourishing of grasslands and savanna in their stead. Modern Grasslands Over one quarter of the Earth's surface is covered by grasslands. Grasslands are found on every continent except Antarctica, and they make up most of Africa and Asia. There are several types of grassland and each one has its own name. -
The Largest Fossil Rodent Andre´S Rinderknecht1 and R
Proc. R. Soc. B doi:10.1098/rspb.2007.1645 Published online The largest fossil rodent Andre´s Rinderknecht1 and R. Ernesto Blanco2,* 1Museo Nacional de Historia Natural y Antropologı´a, Montevideo 11300, Uruguay 2Facultad de Ingenierı´a, Instituto de Fı´sica, Julio Herrera y Reissig 565, Montevideo 11300, Uruguay The discovery of an exceptionally well-preserved skull permits the description of the new South American fossil species of the rodent, Josephoartigasia monesi sp. nov. (family: Dinomyidae; Rodentia: Hystricognathi: Caviomorpha). This species with estimated body mass of nearly 1000 kg is the largest yet recorded. The skull sheds new light on the anatomy of the extinct giant rodents of the Dinomyidae, which are known mostly from isolated teeth and incomplete mandible remains. The fossil derives from San Jose´ Formation, Uruguay, usually assigned to the Pliocene–Pleistocene (4–2 Myr ago), and the proposed palaeoenviron- ment where this rodent lived was characterized as an estuarine or deltaic system with forest communities. Keywords: giant rodents; Dinomyidae; megamammals 1. INTRODUCTION 3. HOLOTYPE The order Rodentia is the most abundant group of living MNHN 921 (figures 1 and 2; Museo Nacional de Historia mammals with nearly 40% of the total number of Natural y Antropologı´a, Montevideo, Uruguay): almost mammalian species recorded (McKenna & Bell 1997; complete skull without left zygomatic arch, right incisor, Wilson & Reeder 2005). In general, rodents have left M2 and right P4-M1. body masses smaller than 1 kg with few exceptions. The largest living rodent, the carpincho or capybara 4. AGE AND LOCALITY (Hydrochoerus hydrochaeris), which lives in the Neotro- Uruguay, Departament of San Jose´, coast of Rı´odeLa pical region of South America, has a body mass of Plata, ‘Kiyu´’ beach (348440 S–568500 W). -
Investigating Evolutionary Processes Using Ancient and Historical DNA of Rodent Species
Investigating evolutionary processes using ancient and historical DNA of rodent species Thesis submitted for the degree of Doctor of Philosophy (PhD) University of London Royal Holloway University of London Egham, Surrey TW20 OEX Selina Brace November 2010 1 Declaration I, Selina Brace, declare that this thesis and the work presented in it is entirely my own. Where I have consulted the work of others, it is always clearly stated. Selina Brace Ian Barnes 2 “Why should we look to the past? ……Because there is nowhere else to look.” James Burke 3 Abstract The Late Quaternary has been a period of significant change for terrestrial mammals, including episodes of extinction, population sub-division and colonisation. Studying this period provides a means to improve understanding of evolutionary mechanisms, and to determine processes that have led to current distributions. For large mammals, recent work has demonstrated the utility of ancient DNA in understanding demographic change and phylogenetic relationships, largely through well-preserved specimens from permafrost and deep cave deposits. In contrast, much less ancient DNA work has been conducted on small mammals. This project focuses on the development of ancient mitochondrial DNA datasets to explore the utility of rodent ancient DNA analysis. Two studies in Europe investigate population change over millennial timescales. Arctic collared lemming (Dicrostonyx torquatus) specimens are chronologically sampled from a single cave locality, Trou Al’Wesse (Belgian Ardennes). Two end Pleistocene population extinction-recolonisation events are identified and correspond temporally with - localised disappearance of the woolly mammoth (Mammuthus primigenius). A second study examines postglacial histories of European water voles (Arvicola), revealing two temporally distinct colonisation events in the UK. -
Fundamentals of Biogeography
FUNDAMENTALS OF BIOGEOGRAPHY Fundamentals of Biogeography presents an engaging and comprehensive introduction to biogeography, explaining the ecology, geography, and history of animals and plants. Defining and explaining the nature of populations, communities and ecosystems, the book examines where different animals and plants live and how they came to be living there; investigates how populations grow, interact, and survive, and how communities are formed and change; and predicts the shape of communities in the twenty-first century. Illustrated throughout with informative diagrams and attractive photos (many in colour), and including guides to further reading, chapter summaries, and an extensive glossary of key terms, Fundamentals of Biogeography clearly explains key concepts, life systems, and interactions. The book also tackles the most topical and controversial environmental and ethical concerns including: animal rights, species exploitation, habitat fragmentation, biodiversity, metapopulations, patchy landscapes, and chaos. Fundamentals of Biogeography presents an appealing introduction for students and all those interested in gaining a deeper understanding of the key topics and debates within the fields of biogeography, ecology and the environment. Revealing how life has and is adapting to its biological and physical surroundings, Huggett stresses the role of ecological, geographical, historical and human factors in fashioning animal and plant distributions and raises important questions concerning how humans have altered Nature, and how biogeography can affect conservation practice. Richard John Huggett is a Senior Lecturer in Geography at the University of Manchester ROUTLEDGE FUNDAMENTALS OF PHYSICAL GEOGRAPHY SERIES Series Editor: John Gerrard This new series of focused, introductory textbooks presents comprehensive, up-to-date introductions to the fundamental concepts, natural processes and human/environmental impacts within each of the core physical geography sub-disciplines: Biogeography, Climatology, Hydrology, Geomorphology and Soils. -
Palaeontology, Palaeobiology and Evolution
Palaeontology, palaeobiology and evolution The chemical conditions for life (January 2003) Robert Williams (Oxford University) and João Fraústo da Silva (Technical University of Lisbon) have an unconventional, but plausible take on the conditions for life’s origin and evolution (Williams, R.J.P & Fraústo da Silva J.J.R. 2003. Evolution was chemically constrained. Journal of Theoretical Biology, v. 220, p. 323-343; doi: 10.1006/jtbi.2003.3152). However life began, presumably as cytoplasm containing DNA, RNA and proteins within a semi-permeable wall, it was surrounded by the chemistry of whatever environment it appeared in. The proto-cell would have drawn hydrogen ions from water, to perform the proton pumping that is essential to all living organisms, and thereby created more oxidising conditions in its immediate vicinity. Oxidation would have generated nitrogen from ammonia, released metals from their sulphides and converted other sulphides to sulphates. Conversely, ions in its surroundings would have been able to “leak” into the cell itself. By creating oxidised radicals, this inward leakage would have rebounded the cell’s activity on itself, with potentially toxic consequences. Survival depended on two things: exploiting the opportunities, such as nitrogen fixation, using oxygen and even photosynthetic chemistry; and fending off potential toxic shock. One of the most interesting aspects is the role assumed by calcium ions. Their presence inside a cell would have precipitated DNA, by binding to it, with fatal consequences. The upshot, according to Williams and Fraústo da Silva, is the special role of calcium as a messenger ion, perhaps having arisen through the necessity to pump it out again. -
Amazonia 1492: Pristine Forest Or Cultural Parkland?
R E P O R T S tant role in locomotor propulsion than the fore- Ϫ1.678 ϩ 2.518 (1.80618), W ϭ 741.1; anteropos- phylogeny place Lagostomus together with Chin- limbs, which were probably important in food terior distal humerus diameter (APH): log W ϭ chilla (22). Ϫ1.467 ϩ 2.484 (1.6532), W ϭ 436.1 kg. 25. M. S. Springer et al., Proc. Natl. Acad. Sci. U.S.A. 98, manipulation. Because of this, the body mass 17. A. R. Biknevicius, J. Mammal. 74, 95 (1993). 6241 (2001). estimation based on the femur is more reliable: 18. The humerus/femur length ratio (H/F) and the (humer- 26. We thank J. Bocquentin, A. Ranci, A. Rinco´n, J. Reyes, P. pattersoni probably weighed ϳ700 kg. With us ϩ radius)/(femur ϩ tibia) length ratio [(H ϩ R)/(F ϩ D. Rodrigues de Aguilera, and R. S´anchez for help with Phoberomys, the size range of the order is in- T )] in P. pattersoni (0.76 and 0.78, respectively) are fieldwork; J. Reyes and E. Weston for laboratory work; average compared with those of other caviomorphs. For E. Weston and three anonymous reviewers for com- creased and Rodentia becomes one of the mam- a sample of 17 extant caviomorphs, the mean values Ϯ ments on the manuscript; O. Aguilera Jr. for assist- malian orders with the widest size variation, SD were H/F ϭ 0.80 Ϯ 0.08 and (H ϩ R)/(F ϩ T ) ϭ ance with digital imaging; S. Melendrez for recon- second only to the Diprotodontia (kangaroos, 0.74 Ϯ 0.09. -
The Bite Force of the Largest Fossil Rodent (Hystricognathi, Caviomorpha, Dinomyidae)
The bite force of the largest fossil rodent (Hystricognathi, Caviomorpha, Dinomyidae) R. ERNESTO BLANCO, ANDRE´ S RINDERKNECHT AND GUSTAVO LECUONA Blanco R.E., Rinderknecht, A. & Lecuona, G. 2012: The bite force of the largest fossil rodent (Hystricognathi, Caviomorpha, Dinomyidae). Lethaia, Vol. 45, pp. 157–163. An exceptionally well-preserved skull of the largest fossil rodent Josephoartigasia monesi allows the first analysis of the bite mechanics of this group of South American giant rodents. In this study, we reconstructed the main anatomical features of the skull of this Pliocene rodent, relating them to the bite force at incisors. Bite force was estimated using three different techniques. Two methods suggest that bite forces at incisors of around 1000 N were possible for these mammals. However, the incisors seem to be stronger than expected for this bite force implying that the bite forces may have been greater than 3000 N. We consider three hypotheses: allometric effects, teeth digging or defence against preda- tors, to explain our results. h Bite force, Dinomyidae, incisors, largest rodent, Pliocene. R. Ernesto Blanco [ernesto@fisica.edu.uy], Facultad de Ciencias, Instituto de Fı´sica, Igua´ 4225, Montevideo 11400, Uruguay; Andre´s Rinderknecht [[email protected]] and Gustavo Lecuona [[email protected]], Museo Nacional de Historia Natural, CC. 399, 11000, Montevideo, Uruguay; manuscript received on 14 ⁄ 10 ⁄ 2010; manuscript accepted on 04 ⁄ 02 ⁄ 2011. Dinomyids make up a family of caviomorph rodents some species (Christiansen & Wroe 2007; Meers 2002; that includes the largest rodents ever known (Bonde- Therrien 2005a,b; Vizcaı´no & De Iuliis 2003; Wroe sio 1978 and literature therein). -
A RODENT and a PECCARY from the CENOZOIC of COLOMBIA By
A RODENT AND A PECCARY FROM THE CENOZOIC OF COLOMBIA by R. A. STIRTON Museum of Paleontology, University of California. A RODENT AND A PECCARY FROM THE CENOZOIC OF COLOMBIA (1) (LAMINA LXXXIII) RESUMEN Se estudian restos de mamíferos del Cenozoico colombiano descubiertos por el Dr. José Royo y Górilez, del Servicio Geoló- gico Nacional. Se trata primeramente de un premolar superior y un incisivo de un roedor histricomorfo de la superfamilia Ca- vioidea y familia Dinomyidae; es una especie nueva, Gyriabrus? royoi Stirton, de edad miocena superior a pliocena inferior pro- cedente del Km. 35 de la carretera de Tolú, Municipio de Sincelejo, Departamento de Bolívar. Se estudia luego la parte posterior de una mandíbula inferior izquierda con el último molar de un pecarí referible a la familia Tayassuidae y a un género y especie nuevos, Selenogonus nariñoensis Stirton, encontrada cerca de la Cocha Verde, carretera de Túquerres, Municipio de Tangua, Departa- mento de Nariño, correspondiente al Plioceno superior o al Pleis- toceno. My attention was directed to two interesting fossil vertebrate spe- cimens when I was in Bogotá as a Guggénheim fellow in september 1944. These were obtained in the field by Dr. José Royo y Gómez, geologist for the Ministerio de Minas y Petróleos, Servicio Geológico Nacional de Co- lombia. I am indebted to Dr. Alejandro del Río, director of the Servicio Geológico Nacional and to Dr. Royo y Gómez for the privilege of describ- ing these specimens. The locality information was supplied by Dr. Royo y Gómez and the illustrations were made by Owen J. Poe. -
Phylogenetic Relationships and Divergence Times in Rodents Based on Both Genes and Fossils Ryan Norris University of Vermont
University of Vermont ScholarWorks @ UVM Graduate College Dissertations and Theses Dissertations and Theses 2009 Phylogenetic Relationships and Divergence Times in Rodents Based on Both Genes and Fossils Ryan Norris University of Vermont Follow this and additional works at: https://scholarworks.uvm.edu/graddis Recommended Citation Norris, Ryan, "Phylogenetic Relationships and Divergence Times in Rodents Based on Both Genes and Fossils" (2009). Graduate College Dissertations and Theses. 164. https://scholarworks.uvm.edu/graddis/164 This Dissertation is brought to you for free and open access by the Dissertations and Theses at ScholarWorks @ UVM. It has been accepted for inclusion in Graduate College Dissertations and Theses by an authorized administrator of ScholarWorks @ UVM. For more information, please contact [email protected]. PHYLOGENETIC RELATIONSHIPS AND DIVERGENCE TIMES IN RODENTS BASED ON BOTH GENES AND FOSSILS A Dissertation Presented by Ryan W. Norris to The Faculty of the Graduate College of The University of Vermont In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy Specializing in Biology February, 2009 Accepted by the Faculty of the Graduate College, The University of Vermont, in partial fulfillment of the requirements for the degree of Doctor of Philosophy, specializing in Biology. Dissertation ~xaminationCommittee: w %amB( Advisor 6.William ~il~atrickph.~. Duane A. Schlitter, Ph.D. Chairperson Vice President for Research and Dean of Graduate Studies Date: October 24, 2008 Abstract Molecular and paleontological approaches have produced extremely different estimates for divergence times among orders of placental mammals and within rodents with molecular studies suggesting a much older date than fossils. We evaluated the conflict between the fossil record and molecular data and find a significant correlation between dates estimated by fossils and relative branch lengths, suggesting that molecular data agree with the fossil record regarding divergence times in rodents.