Simulation-Based Examinations on the Locomotion of Hadrosaurs
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
New Dinosaur Tracksites from the Sousa Lower Cretaceous Basin (Paraíba, Brasil)
Studi Trent. Sci. Nat., Acta Geol., 81 (2004): 5-21 ISSN 0392-0534 © Museo Tridentino di Scienze Naturali, Trento 2006 New dinosaur tracksites from the Sousa Lower Cretaceous basin (Paraíba, Brasil) Giuseppe LEONARDI1* & MariadeFátimaC.F. DOS SANTOS2 1Istituto Cavansi, Dorsoduro 898, I-30123 Venezia, Italy 2Museu Câmara Cascudo, Avenida Hermes da Fonseca 1398, 59015-001 Natal – RN, Brasil *Corresponding author e-mail: [email protected] SUMMARY - New dinosaur tracksites from the Sousa Lower Cretaceous basin (Paraíba, Brasil) - During our 30th expedition to the Lower Cretaceous Rio do Peixe basins (Paraíba, Northeastern Brasil) the following new dinosaur tracksites were discovered: Floresta dos Borba (theropods, sauropods, ornithopods), Lagoa do Forno (theropods, sauropods), Lagoa do Forno II (one theropod), Várzea dos Ramos II (theropods), Várzea dos Ramos III (theropods). In the previously known sites the following new material was discovered: at Piau, a sauropod trackway; at Serrote do Letreiro a new theropod trackway; at Riacho do Cazé, some sauropod and theropod tracks; at Mãe d’Água, new sauropod, theropod and ornithopods footprints. At Fazenda Paraíso new theropod and sauropod tracks were discov- ered and a new map of the main rocky pavement including theropod tracks is provided here. The farms at Saguim de Cima, Várzea da Jurema, Tabuleiro, Catolé da Piedade (WNW of Sousa, in the Sousa Formation) and at Pau d’Arco (SE of Sousa, in the Piranhas Formation) were explored without results. RIASSUNTO - Nuove piste di dinosauri nel bacino di Sousa (Cretaceo inferiore, Paraíba, Brasile) - Durante la nostra 30ª spedizione ai bacini del Rio do Peixe (Cretaceo inferiore; Paraíba, Brasile nord orientale) sono stati sco- perti i seguenti nuovi siti con piste di dinosauri: Floresta dos Borba (teropodi, sauropodi, ornitopodi), Lagoa do Forno (teropodi, sauropodi), Lagoa do Forno II (un teropodo), Várzea dos Ramos II (teropodi), Várzea dos Ramos III (tero- podi). -
Eubrontes and Anomoepus Track
Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 345 EUBRONTES AND ANOMOEPUS TRACK ASSEMBLAGES FROM THE MIDDLE JURASSIC XIASHAXIMIAO FORMATION OF ZIZHONG COUNTY, SICHUAN, CHINA: REVIEW, ICHNOTAXONOMY AND NOTES ON PRESERVED TAIL TRACES LIDA XING1, MARTIN G. LOCKLEY2, GUANGZHAO PENG3, YONG YE3, JIANPING ZHANG1, MASAKI MATSUKAWA4, HENDRIK KLEIN5, RICHARD T. MCCREA6 and W. SCOTT PERSONS IV7 1School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; -email: [email protected]; 2Dinosaur Trackers Research Group, University of Colorado Denver, P.O. Box 173364, Denver, CO 80217; 3 Zigong Dinosaur Museum, Zigong 643013, Sichuan, China; 4 Department of Environmental Sciences, Tokyo Gakugei University, Koganei, Tokyo 184-8501, Japan; 5 Saurierwelt Paläontologisches Museum Alte Richt 7, D-92318 Neumarkt, Germany; 6 Peace Region Palaeontology Research Centre, Box 1540, Tumbler Ridge, British Columbia V0C 2W0, Canada; 7 Department of Biological Sciences, University of Alberta 11455 Saskatchewan Drive, Edmonton, Alberta T6G 2E9, Canada Abstract—The Nianpanshan dinosaur tracksite, first studied in the 1980s, was designated as the type locality of the monospecific ichnogenus Jinlijingpus, and the source of another tridactyl track, Chuanchengpus, both presumably of theropod affinity. After the site was mapped in 2001, these two ichnotaxa were considered synonyms of Eubrontes and Anomoepus, respectively, the latter designation being the first identification of this ichnogenus in China. The assemblage indicates a typical Jurassic ichnofauna. The present study reinvestigates the site in the light of the purported new ichnospecies Chuanchengpus shenglingensis that was introduced in 2012. After re- evaluation of the morphological and extramorphological features, C. -
An Ornithopod Tracksite from the Helvetiafjellet Formation (Lower Cretaceous) of Boltodden, Svalbard
Downloaded from http://sp.lyellcollection.org/ at Universitetet i Oslo on January 11, 2016 The theropod that wasn’t: an ornithopod tracksite from the Helvetiafjellet Formation (Lower Cretaceous) of Boltodden, Svalbard JØRN H. HURUM1,2, PATRICK S. DRUCKENMILLER3, ØYVIND HAMMER1*, HANS A. NAKREM1 & SNORRE OLAUSSEN2 1Natural History Museum, University of Oslo, PO Box 1172, Blindern, 0318 Oslo, Norway 2The University Centre in Svalbard (UNIS), PO Box 156, 9171 Longyearbyen, Norway 3Department of Geosciences, University of Alaska Museum, University of Alaska Fairbanks, 907 Yukon Drive, Fairbanks, AK 99775, USA *Corresponding author (e-mail: [email protected]) Abstract: We re-examine a Lower Cretaceous dinosaur tracksite at Boltodden in the Kvalva˚gen area, on the east coast of Spitsbergen, Svalbard. The tracks are preserved in the Helvetiafjellet For- mation (Barremian). A sedimentological characterization of the site indicates that the tracks formed on a beach/margin of a lake or interdistributary bay, and were preserved by flooding. In addition to the two imprints already known from the site, we describe at least 34 additional, pre- viously unrecognized pes and manus prints, including one trackway. Two pes morphotypes and one manus morphotype are recognized. Given the range of morphological variation and the pres- ence of manus tracks, we reinterpret all the prints as being from an ornithopod rather than a thero- pod, as previously described. We assign the smaller (morphotype A, pes; morphotype B, manus) to Caririchnium billsarjeanti. The larger (morphotype C, pes) track is assigned to Caririchnium sp., differing in size and interdigital angle from the two described ichnospecies C. burreyi and C. -
Download the Article
A couple of partially-feathered creatures about the The Outside Story size of a turkey pop out of a stand of ferns. By the water you spot a flock of bigger animals, lean and predatory, catching fish. And then an even bigger pair of animals, each longer than a car, with ostentatious crests on their heads, stalk out of the heat haze. The fish-catchers dart aside, but the new pair have just come to drink. We can only speculate what a walk through Jurassic New England would be like, but the fossil record leaves many hints. According to Matthew Inabinett, one of the Beneski Museum of Natural History’s senior docents and a student of vertebrate paleontology, dinosaur footprints found in the sedimentary rock of the Connecticut Valley reveal much about these animals and their environment. At the time, the land that we know as New England was further south, close to where Cuba is now. A system of rift basins that cradled lakes ran right through our region, from North Carolina to Nova Scotia. As reliable sources of water, with plants for the herbivores and fish for the carnivores, the lakes would have been havens of life. While most of the fossil footprints found in New England so far are in the lower Connecticut Valley, Dinosaur Tracks they provide a window into a world that extended throughout the region. According to Inabinett, the By: Rachel Marie Sargent tracks generally fall into four groupings. He explained that these names are for the tracks, not Imagine taking a walk through a part of New the dinosaurs that made them, since, “it’s very England you’ve never seen—how it was 190 million difficult, if not impossible, to match a footprint to a years ago. -
A Review of Large Cretaceous Ornithopod Tracks, with Special Reference to Their Ichnotaxonomy
bs_bs_banner Biological Journal of the Linnean Society, 2014, 113, 721–736. With 5 figures A review of large Cretaceous ornithopod tracks, with special reference to their ichnotaxonomy MARTIN G. LOCKLEY1*, LIDA XING2, JEREMY A. F. LOCKWOOD3 and STUART POND3 1Dinosaur Trackers Research Group, University of Colorado at Denver, CB 172, PO Box 173364, Denver, CO 80217-3364, USA 2School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China 3Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Received 30 January 2014; revised 12 February 2014; accepted for publication 13 February 2014 Trackways of ornithopods are well-known from the Lower Cretaceous of Europe, North America, and East Asia. For historical reasons, most large ornithopod footprints are associated with the genus Iguanodon or, more generally, with the family Iguanodontidae. Moreover, this general category of footprints is considered to be sufficiently dominant at this time as to characterize a global Early Cretaceous biochron. However, six valid ornithopod ichnogenera have been named from the Cretaceous, including several that are represented by multiple ichnospecies: these are Amblydactylus (two ichnospecies); Caririchnium (four ichnospecies); Iguanodontipus, Ornithopodichnus originally named from Lower Cretaceous deposits and Hadrosauropodus (two ichnospecies); and Jiayinosauropus based on Upper Cretaceous tracks. It has recently been suggested that ornithopod ichnotaxonomy is oversplit and that Caririchnium is a senior subjective synonym of Hadrosauropodus and Amblydactylus is a senior subjective synonym of Iguanodontipus. Although it is agreed that many ornithopod tracks are difficult to differentiate, this proposed synonymy is questionable because it was not based on a detailed study of the holotypes, and did not consider all valid ornithopod ichnotaxa or the variation reported within the six named ichnogenera and 11 named ichnospecies reviewed here. -
Projeto Geoparques Geoparque Rio Do Peixe
PROJETO GEOPARQUES GEOPARQUE RIO DO PEIXE – PB PROPOSTA 2017 MINISTÉRIO DE MINAS E ENERGIA - MME Fernando Coelho Filho Ministro de Estado Paulo Pedrosa Secretário Executivo SECRETARIA DE GEOLOGIA, MINERAÇÃO E TRANSFORMAÇÃO MINERAL - SGM Vicente Humberto Lôbo Cruz Secretário de Geologia, Mineração e Transformação Mineral SERVIÇO GEOLÓGICO DO BRASIL - CPRM DIRETORIA EXECUTIVA Esteves Pedro Colnago Diretor-Presidente Antônio Carlos Bacelar Nunes Diretor de Hidrologia e Gestão Territorial – DHT José Leonardo Silva Andriotti Diretor de Geologia e Recursos Minerais – DGM Esteves Pedro Colnago Diretor de Relações Institucionais e Desenvolvimento – DRI Juliano de Souza Oliveira Diretor de Administração e Finanças – DAF PROGRAMA GEOLOGIA DO BRASIL LEVANTAMENTO DA GEODIVERSIDADE Departamento de Gestão Territorial – DEGET Jorge Pimentel – Chefe Divisão de Gestão Territorial – DIGATE Maria Adelaide Mansini Maia – Chefe Coordenação do Projeto Geoparques Coordenação Nacional Carlos Schobbenhaus Coordenação Regional Rogério Valença Ferreira Unidade Regional Executora do Projeto Geoparques Superintendência Regional de Recife Sérgio Maurício Coutinho Corrêa de Oliveira Superintendente Robson de Carlo da Silva Gerente de Hidrologia e Gestão Territorial Maria de Fátima Lyra de Brito Gerente de Geologia e Recursos Minerais Carlos Eduardo Oliveira Dantas Gerente de Relações Institucionais e Desenvolvimento MINISTÉRIO DE MINAS E ENERGIA SECRETARIA DE GEOLOGIA, MINERAÇÃO E TRANSFORMAÇÃO MINERAL SERVIÇO GEOLÓGICO DO BRASIL – CPRM Projeto Geoparques GEOPARQUE -
The First Record of Anomoepus Tracks from the Middle Jurassic of Henan Province, Central China
Historical Biology An International Journal of Paleobiology ISSN: 0891-2963 (Print) 1029-2381 (Online) Journal homepage: http://www.tandfonline.com/loi/ghbi20 The first record of Anomoepus tracks from the Middle Jurassic of Henan Province, Central China Lida Xing, Nasrollah Abbassi, Martin G. Lockley, Hendrik Klein, Songhai Jia, Richard T. McCrea & W. Scott Persons IV To cite this article: Lida Xing, Nasrollah Abbassi, Martin G. Lockley, Hendrik Klein, Songhai Jia, Richard T. McCrea & W. Scott Persons IV (2016): The first record of Anomoepus tracks from the Middle Jurassic of Henan Province, Central China, Historical Biology, DOI: 10.1080/08912963.2016.1149480 To link to this article: http://dx.doi.org/10.1080/08912963.2016.1149480 Published online: 22 Feb 2016. Submit your article to this journal View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=ghbi20 Download by: [Lida Xing] Date: 22 February 2016, At: 05:53 HISTORICAL BIOLOGY, 2016 http://dx.doi.org/10.1080/08912963.2016.1149480 The first record of Anomoepus tracks from the Middle Jurassic of Henan Province, Central China Lida Xinga, Nasrollah Abbassib, Martin G. Lockleyc, Hendrik Kleind, Songhai Jiae, Richard T. McCreaf and W. Scott PersonsIVg aSchool of the Earth Sciences and Resources, China University of Geosciences, Beijing, China; bFaculty of Sciences, Department of Geology, University of Zanjan, Zanjan, Iran; cDinosaur Tracks Museum, University of Colorado Denver, Denver, CO, USA; dSaurierwelt Paläontologisches Museum, Neumarkt, Germany; eHenan Geological Museum, Henan Province, China; fPeace Region Palaeontology Research Centre, British Columbia, Canada; gDepartment of Biological Sciences, University of Alberta, Edmonton, Canada ABSTRACT ARTICLE HISTORY Small, gracile mostly tridactyl tracks from the Middle Jurassic of Henan Province represent the first example Received 30 December 2015 of the ichnogenus Anomoepus from this region. -
Paleoicnología De Dinosaurios 1
Paleoicnología de dinosaurios 1 PALEOICNOLOGIA DE DINOSAURIOS José Ignacio CANUDO SANAGUSTIN y Gloria CUENCA BESCÓS José I. CANUDO y Gloria CUENCA Paleoicnología de dinosaurios 2 INDICE Introducción El inicio de la Paleoicnología de dinosaurios La conservación de las icnitas - Medio sedimentario - Propiedades del substrato - Subimpresiones - Otras conservaciones La morfología de las icnitas - Anatomía - El substrato - Comportamiento - La conservación como subimpresiones El estudio de las icnitas de dinosaurios - Documentación y excavación de yacimientos con icnitas de dinosaurios - Describiendo icnitas y rastros de dinosaurios - Midiendo icnitas y rastros de dinosaurios - Variación en la morfología de las icnitas - Ilustrando icnitas de dinosaurio Principales tipos de icnitas de dinosaurios - Grandes terópodos. “Carnosaurios” - Pequeños terópodos “Coelurosaurios” - Ornitomimidos - Saurópodos - Prosaurópodos - Pequeños ornitópodos - Iguanodóntidos - Hadrosáuridos El tamaño deducido a partir de las icnitas Modo de andar de los dinosaurios - Dinosaurios bípedos - Dinosaurios semibípedos - Dinosaurios cuadrúpedos Calculando la velocidad de los dinosaurios - Velocidad relativa - Métodos de calculo de la velocidad absoluta - La velocidad de los dinosaurios La asociación de icnitas de dinosaurios - Asociación de icnitas de dinosaurio sin orientación aparente - Asociación con dos direcciones preferentes - Asociación con un solo sentido. Megayacimientos José I. CANUDO y Gloria CUENCA Paleoicnología de dinosaurios 3 - Estructura de las comunidades -
A Redescription of the Holotype of Brachylophosaurus Canadensis
A redescription of the holotypeBrachylophosaurus of canadensis (Dinosauria: Hadrosauridae), with a discussion of chewing in hadrosaurs by Robin S. Cuthbertson B.Sc. Zoology A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Masters of Science Ottawa-Carleton Geoscience Centre Department of Earth Sciences Carleton University Ottawa, Ontario Canada April, 2006 © Robin S. Cuthbertson, 2006 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Library and Bibliotheque et Archives Canada Archives Canada Published Heritage Direction du Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A 0N4 Ottawa ON K1A 0N4 C a n ad a C a n a d a Your file Votre reference ISBN: 978-0-494-16493-8 Our file Notre reference ISBN: 978-0-494-16493-8 NOTICE: AVIS: The author has granted a non L'auteur a accorde une licence non exclusive exclusive license allowing Library permettant a la Bibliotheque et Archives and Archives Canada to reproduce,Canada de reproduire, publier, archiver, publish, archive, preserve, conserve,sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par I'lnternet, preter, telecommunication or on the Internet,distribuer et vendre des theses partout dans loan, distribute and sell theses le monde, a des fins commerciales ou autres, worldwide, for commercial or non sur support microforme, papier, electronique commercial purposes, in microform,et/ou autres formats. paper, electronic and/or any other formats. The author retains copyright L'auteur conserve la propriete du droit d'auteur ownership and moral rights in et des droits moraux qui protege cette these. -
The Early Jurassic Ornithischian Dinosaurian Ichnogenus Anomoepus
19 The Early Jurassic Ornithischian Dinosaurian Ichnogenus Anomoepus Paul E. Olsen and Emma C. Rainforth nomoepus is an Early Jurassic footprint genus and 19.2). Because skeletons of dinosaur feet were not produced by a relatively small, gracile orni- known at the time, he naturally attributed the foot- A thischian dinosaur. It has a pentadactyl ma- prints to birds. By 1848, however, he recognized that nus and a tetradactyl pes, but only three pedal digits some of the birdlike tracks were associated with im- normally impressed while the animal was walking. The pressions of five-fingered manus, and he gave the name ichnogenus is diagnosed by having the metatarsal- Anomoepus, meaning “unlike foot,” to these birdlike phalangeal pad of digit IV of the pes lying nearly in line with the axis of pedal digit III in walking traces, in combination with a pentadactyl manus. It has a pro- portionally shorter digit III than grallatorid (theropod) tracks, but based on osteometric analysis, Anomoepus, like grallatorids, shows a relatively shorter digit III in larger specimens. Anomoepus is characteristically bi- pedal, but there are quadrupedal trackways and less common sitting traces. The ichnogenus is known from eastern and western North America, Europe, and southern Africa. On the basis of a detailed review of classic and new material, we recognize only the type ichnospecies Anomoepus scambus within eastern North America. Anomoepus is known from many hundreds of specimens, some with remarkable preservation, showing many hitherto unrecognized details of squa- mation and behavior. . Pangea at approximately 200 Ma, showing the In 1836, Edward Hitchcock described the first of what areas producing Anomoepus discussed in this chapter: 1, Newark we now recognize as dinosaur tracks from Early Juras- Supergroup, eastern North America; 2, Karoo basin; 3, Poland; sic Newark Supergroup rift strata of the Connecticut 4, Colorado Plateau. -
Competition Structured a Late Cretaceous Megaherbivorous Dinosaur Assemblage Jordan C
www.nature.com/scientificreports OPEN Competition structured a Late Cretaceous megaherbivorous dinosaur assemblage Jordan C. Mallon 1,2 Modern megaherbivore community richness is limited by bottom-up controls, such as resource limitation and resultant dietary competition. However, the extent to which these same controls impacted the richness of fossil megaherbivore communities is poorly understood. The present study investigates the matter with reference to the megaherbivorous dinosaur assemblage from the middle to upper Campanian Dinosaur Park Formation of Alberta, Canada. Using a meta-analysis of 21 ecomorphological variables measured across 14 genera, contemporaneous taxa are demonstrably well-separated in ecomorphospace at the family/subfamily level. Moreover, this pattern is persistent through the approximately 1.5 Myr timespan of the formation, despite continual species turnover, indicative of underlying structural principles imposed by long-term ecological competition. After considering the implications of ecomorphology for megaherbivorous dinosaur diet, it is concluded that competition structured comparable megaherbivorous dinosaur communities throughout the Late Cretaceous of western North America. Te question of which mechanisms regulate species coexistence is fundamental to understanding the evolution of biodiversity1. Te standing diversity (richness) of extant megaherbivore (herbivores weighing ≥1,000 kg) com- munities appears to be mainly regulated by bottom-up controls2–4 as these animals are virtually invulnerable to top-down down processes (e.g., predation) when fully grown. Tus, while the young may occasionally succumb to predation, fully-grown African elephants (Loxodonta africana), rhinoceroses (Ceratotherium simum and Diceros bicornis), hippopotamuses (Hippopotamus amphibius), and girafes (Girafa camelopardalis) are rarely targeted by predators, and ofen show indiference to their presence in the wild5. -
Feeding Behaviour and Bone Utilization by Theropod Dinosaurs
Feeding behaviour and bone utilization by theropod dinosaurs DAVID W. E. HONE AND OLIVER W. M. RAUHUT Hone, D.W.E. & Rauhut, O.W.M. 2009: Feeding behaviour and bone utilization by theropod dinosaurs. Lethaia, 10.1111/j.1502-3931.2009.00187.x Examples of bone exploitation by carnivorous theropod dinosaurs are relatively rare, representing an apparent waste of both mineral and energetic resources. A review of the known incidences and possible ecological implications of theropod bone use concludes that there is currently no definitive evidence supporting the regular deliberate ingestion of bone by these predators. However, further investigation is required as the small bones of juvenile dinosaurs missing from the fossil record may be absent as a result of thero- pods preferentially hunting and consuming juveniles. We discuss implications for both hunting and feeding in theropods based on the existing data. We conclude that, like modern predators, theropods preferentially hunted and ate juvenile animals leading to the absence of small, and especially young, dinosaurs in the fossil record. The traditional view of large theropods hunting the adults of large or giant dinosaur species is therefore considered unlikely and such events rare. h Behaviour, carnivory, palaeoecology, preda- tion, resource utilization. David W. E. Hone [[email protected]], Institute of Vertebrate Paleontology & Paleoanthro- pology, Xhizhimenwai Dajie 142, Beijing 100044, China; Oliver W. M. Rauhut [[email protected]], Bayerische Staatssammlung fu¨r Pala¨ontologie und Geolo- gie and Department fu¨r Geo- und Umweltwissenschaften, Ludwig-Maximilians-Universita¨t Munich, Richard-Wagner-Str. 10, 80333 Munich, Germany; manuscript received on 18 ⁄ 01 ⁄ 2009; manuscript accepted on 20 ⁄ 05 ⁄ 2009.