Strength Indicator Values of Theropod Long Bones, with Comments on Limb Proportions and Cursorial Potential
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1.1 První Chobotnatci 5 1.2 Plesielephantiformes 5 1.3 Elephantiformes 6 1.3.1 Mammutida 6 1.3.2 Elephantida 7 1.3.3 Elephantoidea 7 2
MASARYKOVA UNIVERZITA PŘÍRODOVĚDECKÁ FAKULTA ÚSTAV GEOLOGICKÝCH VĚD Jakub Březina Rešerše k bakalářské práci Využití mikrostruktur klů neogenních chobotnatců na příkladu rodu Zygolophodon Vedoucí práce: doc. Mgr. Martin Ivanov, Dr. Brno 2012 OBSAH 1. Současný pohled na evoluci chobotnatců 3 1.1 První chobotnatci 5 1.2 Plesielephantiformes 5 1.3 Elephantiformes 6 1.3.1 Mammutida 6 1.3.2 Elephantida 7 1.3.3 Elephantoidea 7 2. Kly chobotnatců a jejich mikrostruktura 9 2.1 Přírůstky v klech chobotnatců 11 2.1.1 Využití přírůstků v klech chobotnatců 11 2.2 Schregerův vzor 12 2.2.1 Stavba Schregerova vzoru 12 2.2.2 Využití Schregerova vzoru 12 2.3 Dentinové kanálky 15 3 Sedimenty s nálezy savců v okolí Mikulova 16 3.1 Baden 17 3.2 Pannon a Pont 18 1. Současný pohled na evoluci chobotnatců Současná systematika chobotnatců není kompletně odvozena od jejich fylogeneze, rekonstruované pomocí kladistických metod. Diskutované skupiny tak mnohdy nepředstavují monofyletické skupiny. Přestože jsou taxonomické kategorie matoucí (např. Laurin 2005), jsem do jisté míry nucen je používat. Některým skupinám úrovně stále přiřazeny nebyly a zde této skutečnosti není přisuzován žádný význam. V této rešerši jsem se zaměřil hlavně na poznatky, které následovaly po vydání knihy; The Proboscidea: Evolution and Paleoecology of Elephants and Their Relatives, od Shoshaniho a Tassyho (1996). Chobotnatci jsou součástí skupiny Tethytheria společně s anthracobunidy, sirénami a desmostylidy (Shoshani 1998; Shoshani & Tassy 1996; 2005; Gheerbrant & Tassy 2009). Základní klasifikace sestává ze dvou skupin. Ze skupiny Plesielephantiformes, do které patří čeledě Numidotheriidae, Barytheriidae a Deinotheridae a ze skupiny Elephantiformes, do které patří čeledě Palaeomastodontidae, Phiomiidae, Mammutida, Gomphotheriidae, tetralofodontní gomfotéria, Stegodontidae a Elephantidae (Shoshani & Marchant 2001; Shoshani & Tassy 2005; Gheerbrant & Tassy 2009). -
A NEW AMEBELODONT, TORYNOBELODON BARNUMBROWNI, SP. NOV. a PRELIMINARY REPORT Erwin Hinckley Barbour
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Bulletin of the University of Nebraska State Museum, University of Nebraska State Museum 1931 A NEW AMEBELODONT, TORYNOBELODON BARNUMBROWNI, SP. NOV. A PRELIMINARY REPORT Erwin Hinckley Barbour Follow this and additional works at: http://digitalcommons.unl.edu/museumbulletin Part of the Entomology Commons, Geology Commons, Geomorphology Commons, Other Ecology and Evolutionary Biology Commons, Paleobiology Commons, Paleontology Commons, and the Sedimentology Commons This Article is brought to you for free and open access by the Museum, University of Nebraska State at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Bulletin of the University of Nebraska State Museum by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 1/ 6 . BULLETIN 22 VOLUME I UN 1~l:7Gtrs;:J:~~!1 L'P' i THE NEBRASKA STATE USEUM I tor ERWIN H. BARBOUR, Dir NUl :~,~I r ~;l A NEW AMEBELODONT, TOR :I.,I,lI..LJ.J;I.c.uUJ.J~m.T-~ ___I BARNUMBROWNI, SP. NOV. A PRELIMINARY REPORT By ERWIN HINCKLEY BARBOUR The subfamily of longirostrine mastodonts known as the Amebelodontinae have been so recently discovered and described that as yet theY; are little known by the citizens of this state. They are most briefly and directly described as shovel-tusked mastodons. The first one found, namely Amebelodon fricki, was secured in April 1927, and was pub lished June 1927. In the meantime, many other examples of Amebelodonts have been added to the Morrill Palaeon tological Collections of the Nebraska State Museum. The exact number cannot be stated until the material shipped in from the field during the current season is unpacked, cleaned, and identified. -
Dinosaur Species List E to M
Dinosaur Species List E to M E F G • Echinodon becklesii • Fabrosaurus australis • Gallimimus bullatus • Edmarka rex • Frenguellisaurus • Garudimimus brevipes • Edmontonia longiceps ischigualastensis • Gasosaurus constructus • Edmontonia rugosidens • Fulengia youngi • Gasparinisaura • Edmontosaurus annectens • Fulgurotherium australe cincosaltensis • Edmontosaurus regalis • Genusaurus sisteronis • Edmontosaurus • Genyodectes serus saskatchewanensis • Geranosaurus atavus • Einiosaurus procurvicornis • Gigantosaurus africanus • Elaphrosaurus bambergi • Giganotosaurus carolinii • Elaphrosaurus gautieri • Gigantosaurus dixeyi • Elaphrosaurus iguidiensis • Gigantosaurus megalonyx • Elmisaurus elegans • Gigantosaurus robustus • Elmisaurus rarus • Gigantoscelus • Elopteryx nopcsai molengraaffi • Elosaurus parvus • Gilmoreosaurus • Emausaurus ernsti mongoliensis • Embasaurus minax • Giraffotitan altithorax • Enigmosaurus • Gongbusaurus shiyii mongoliensis • Gongbusaurus • Eoceratops canadensis wucaiwanensis • Eoraptor lunensis • Gorgosaurus lancensis • Epachthosaurus sciuttoi • Gorgosaurus lancinator • Epanterias amplexus • Gorgosaurus libratus • Erectopus sauvagei • "Gorgosaurus" novojilovi • Erectopus superbus • Gorgosaurus sternbergi • Erlikosaurus andrewsi • Goyocephale lattimorei • Eucamerotus foxi • Gravitholus albertae • Eucercosaurus • Gresslyosaurus ingens tanyspondylus • Gresslyosaurus robustus • Eucnemesaurus fortis • Gresslyosaurus torgeri • Euhelopus zdanskyi • Gryponyx africanus • Euoplocephalus tutus • Gryponyx taylori • Euronychodon -
Paleobiogeography of Trilophodont Gomphotheres (Mammalia: Proboscidea)
Revista Mexicana deTrilophodont Ciencias Geológicas, gomphotheres. v. 28, Anúm. reconstruction 2, 2011, p. applying235-244 DIVA (Dispersion-Vicariance Analysis) 235 Paleobiogeography of trilophodont gomphotheres (Mammalia: Proboscidea). A reconstruction applying DIVA (Dispersion-Vicariance Analysis) María Teresa Alberdi1,*, José Luis Prado2, Edgardo Ortiz-Jaureguizar3, Paula Posadas3, and Mariano Donato1 1 Departamento de Paleobiología, Museo Nacional de Ciencias Naturales, CSIC, José Gutiérrez Abascal 2, 28006, Madrid, España. 2 INCUAPA, Departamento de Arqueología, Universidad Nacional del Centro, Del Valle 5737, B7400JWI Olavarría, Argentina. 3 LASBE, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque S/Nº, B1900FWA La Plata, Argentina. * [email protected] ABSTRACT The objective of our paper was to analyze the distributional patterns of trilophodont gomphotheres, applying an event-based biogeographic method. We have attempted to interpret the biogeographical history of trilophodont gomphotheres in the context of the geological evolution of the continents they inhabited during the Cenozoic. To reconstruct this biogeographic history we used DIVA 1.1. This application resulted in an exact solution requiring three vicariant events, and 15 dispersal events, most of them (i.e., 14) occurring at terminal taxa. The single dispersal event at an internal node affected the common ancestor to Sinomastodon plus the clade Cuvieronius – Stegomastodon. A vicariant event took place which resulted in two isolated groups: (1) Amebelodontinae (Africa – Europe – Asia) and (2) Gomphotheriinae (North America). The Amebelodontinae clade was split by a second vicariant event into Archaeobelodon (Africa and Europe), and the ancestors of the remaining genera of the clade (Asia). In contrast, the Gomphotheriinae clade evolved mainly in North America. -
Manus Descriptions of an Undescribed Mastodon from the Latest Miocene-Earliest Pliocene Gray Fossil Site, with Comparisons to Other North American Proboscidean Taxa
East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 12-2019 Manus Descriptions of an Undescribed Mastodon from the Latest Miocene-Earliest Pliocene Gray Fossil Site, with Comparisons to other North American Proboscidean Taxa Brenna Hart-Farrar East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Geology Commons, and the Paleobiology Commons Recommended Citation Hart-Farrar, Brenna, "Manus Descriptions of an Undescribed Mastodon from the Latest Miocene-Earliest Pliocene Gray Fossil Site, with Comparisons to other North American Proboscidean Taxa" (2019). Electronic Theses and Dissertations. Paper 3680. https://dc.etsu.edu/etd/3680 This Thesis - unrestricted is brought to you for free and open access by the Student Works at Digital Commons @ East Tennessee State University. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ East Tennessee State University. For more information, please contact [email protected]. Manus Descriptions of an Undescribed Mastodon from the Latest Miocene-Earliest Pliocene Gray Fossil Site, with Comparisons to other North American Proboscidean Taxa _________________________________ A thesis presented to the faculty of the Department of Geosciences East Tennessee State University In partial fulfillment of the requirements for the degree Master of Science in Geosciences _________________________________ by Brenna J. Hart-Farrar December 2019 _________________________________ Steven C. Wallace, Chair Chris. Widga Blaine W. Schubert Keywords: Gray Fossil Site, Mammut, Mastodon, Morphology, Manus ABSTRACT Manus descriptions of an Undescribed Mastodon from the Latest Miocene-Earliest Pliocene Gray Fossil Site, with Comparisons to other North American Proboscidean Taxa by Brenna J. -
Ten Little Dinosaurs Free
FREE TEN LITTLE DINOSAURS PDF Mike Brownlow,Simon Rickerty | 32 pages | 01 Oct 2015 | Hachette Children's Group | 9781408334010 | English | London, United Kingdom The First Dinosaurs A period of great transformation, Ten Little Dinosaurs Late Cretaceous Period is when the dinosaurs disappeared from the earth. Learn more about the Late Cretaceous dinosaurs that existed during this era, such as the Ten Little Dinosaurs, Gallimimus, and Brachylophosaurus. Tyrannosaurus rex, one of the fiercest meat-eaters ever, is the animal that probably springs to mind when most of us hear the word "dinosaur. It shared the Cretaceous landscape Ten Little Dinosaurs, and probably was preyed upon by, Tyrannosaurus rex. Constantly compared to the Tyrannosaurus rex, the Giganotosaurus was one of a handful of dinosaurs that rivaled, or possibly exceeded, the creature in size. University of Kansas paleontologists Ten Little Dinosaurs comparing the bones of a new T. Could this exciting find help bridge the gaps Ten Little Dinosaurs Africa's late Cretaceous fossil record and that of other continents? OK, hop in your time machine and go back 67 million years or so to the Cretaceous period. Then find a Tyrannosaurus rex and challenge it to a race. Sounds crazy, huh? Could you really outrun a Tyrannosaurus rex? Learn about Monoclonius, Late Cretaceous dinosaurs and dinosaurs Ten Little Dinosaurs all eras. The recently discovered large theropod Abelisaurus comahuensis, from Patagonia is argentina, looked a little like Albertosaurus from Alberta, Canada, particularly in its size and lifestyle. Find out more about the Late Cretaceous dinosaurs. Albertosaurus was an older "cousin" to the better-known Tyrannosaurus. -
MAY 2011 ART& ANIMALS in THIS ISSUE Sunday with Celebrated at Morrill Hall April 2 a Scientist
NEWS FROM THE UNIVERSITY OF NEBRASKA STATE MUSEUM theMammoth MAY 2011 ART& ANIMALS IN THIS ISSUE Sunday with Celebrated at Morrill Hall April 2 a Scientist The 3rd annual Colorful Creature Day was held April 2 at Morrill Hall. Over 1,100 visitors of all ages came out for this fun-filled afternoon of live animals and hands-on art activities in the Museum. Read more about this event on page 12! Museum Memories ..........................6-8 A Walk Through Time .......................9-11 Colorful Creature Day .......................12 Agate Fossil Beds: New Fossil Find Marks 30 Years of Discovery........... 14-15 Sunday with a Scientist ...................16-17 Trailside Turns 50! ...........................18 & MORE The Mammoth is available in color online! friendsofthemuseum.org MORRILL FRIENDS UNIVERSITY OF BOARD OF DIRECTORS NEBRASKA HALL Mark A. Brohman, President STATE MUSEUM STAFF CALENDAR Lois Mayo, Vice President EX-OFFICIO AT A GLANCE David Rowe, Treasurer Priscilla C. Grew Director: Priscilla C. Grew Diane Pratt, Secretary Mike Madcharo Associate Director: Mark Harris Karen Amen Marcia Hollestelle ADVISORY COUNCIL Informal Science Education: Judy Diamond, Curator June 19 Michael Leite Judy Diamond Amy Spiegel Keely Rennie-Tucker Connie Pejsar 1:30-4:30 p.m. Lynn Sobotka Norm Smith Sunday with a Scientist Education Coordinator: Kathy French Diann Sorensen Mike Zeleny Museum Associates: Ann Cusick “Tissue Mechanics: Mark Sorensen Cindy Loope Engineering Better Heart Mel Thornton ASHFALL CHAPTER Annie Mumgaard Health” Natasha Vavra Mark Brogie, Ina Van der Veen Art Zygielbaum President July 17 Research Partnerships Coordinator: Brett Ratcliffe 1:30-4:30 p.m. Sunday with a Scientist Anthropology: Alan Osborn, Curator CONTACT INFORMATION NAGPRA/Collections Assistant: Susan Curtis “Fish” Director’s Office (402) 472-3779 Nebraska Archaeological Survey: Alan Osborn August 21 Museum Information Line (402) 472-2642 School Program Reservations (402) 472-6302 Botany: Robert Kaul, Curator 1:30-4:30 p.m. -
PROCEEDINGS of the OKLAHOMA ACADEMY of SCIENCE Volume 98 2018
PROCEEDINGS of the OKLAHOMA ACADEMY OF SCIENCE Volume 98 2018 EDITOR: Mostafa Elshahed Production Editor: Tammy Austin Business Manager: T. David Bass The Official Organ of the OKLAHOMA ACADEMY OF SCIENCE Which was established in 1909 for the purpose of stimulating scientific research; to promote fraternal relationships among those engaged in scientific work in Oklahoma; to diffuse among the citizens of the State a knowledge of the various departments of science; and to investigate and make known the material, educational, and other resources of the State. Affiliated with the American Association for the Advancement of Science. Publication Date: January 2019 ii POLICIES OF THE PROCEEDINGS The Proceedings of the Oklahoma Academy of Science contains papers on topics of interest to scientists. The goal is to publish clear communications of scientific findings and of matters of general concern for scientists in Oklahoma, and to serve as a creative outlet for other scientific contributions by scientists. ©2018 Oklahoma Academy of Science The Proceedings of the Oklahoma Academy Base and/or other appropriate repository. of Science contains reports that describe the Information necessary for retrieval of the results of original scientific investigation data from the repository will be specified in (including social science). Papers are received a reference in the paper. with the understanding that they have not been published previously or submitted for 4. Manuscripts that report research involving publication elsewhere. The papers should be human subjects or the use of materials of significant scientific quality, intelligible to a from human organs must be supported by broad scientific audience, and should represent a copy of the document authorizing the research conducted in accordance with accepted research and signed by the appropriate procedures and scientific ethics (proper subject official(s) of the institution where the work treatment and honesty). -
P a L a E O N T O G R a P H I C A
P A L A E O N T O G R A P H I C A CONTRIBUTIONS TO THE NATURAL HISTORY OF THE PAST FOUNDED BY J. F. POMPECKJ IN BERLIN WITH THE COOPERATION OF F. BROILI, O. JAEKEL, H. RAUFF AND G. STEINMANN AS REPRESENTATIVES OF THE GERMAN GEOLOGICAL SOCIETY SUPPLEMENT VII 1ST. PART, VOLUME I SUPPLEMENT I. C O N T E N T S : SCIENTIFIC RESULTS OF THE TENDAGURU EXPEDITION 1909-1912 W. JANENSCH: THE COELUROSAURS AND THEROPODS OF THE TENDAGURU FORMATION, GERMAN EAST AFRICA (PAGES 1-100 WITH PLATES I-IX AND 32 TEXT-FIGURES) S T U T T G A R T S C H W E I Z E R B A R T ' S P U B L I S H I N G H O U S E ( E R W I N N Ä G E L E ) G. M. B. H. 1 9 2 5 SCIENTIFIC RESULTS OF THE TENDAGURU EXPEDITION 1909-1912 N E W R E S U L T S FOUNDED BY GEOLOGICAL-PALEONTOLOGICAL INSTITUTE AND MUSEUM OF THE UNIVERSITY OF BERLIN THROUGH W. JANENSCH IN BERLIN S T U T T G A R T S C H W E I Z E R B A R T ' S P U B L I S H I N G H O U S E ( E R W I N N Ä G E L E ) G. M. B. H. 1 9 2 5 THE COELUROSAURS AND THEROPODS OF THE TENDAGURU FORMATION GERMAN EAST AFRICA BY W. -
Body-Size Evolution in the Dinosauria
8 Body-Size Evolution in the Dinosauria Matthew T. Carrano Introduction The evolution of body size and its influence on organismal biology have received scientific attention since the earliest decades of evolutionary study (e.g., Cope, 1887, 1896; Thompson, 1917). Both paleontologists and neontologists have attempted to determine correlations between body size and numerous aspects of life history, with the ultimate goal of docu- menting both the predictive and causal connections involved (LaBarbera, 1986, 1989). These studies have generated an appreciation for the thor- oughgoing interrelationships between body size and nearly every sig- nificant facet of organismal biology, including metabolism (Lindstedt & Calder, 1981; Schmidt-Nielsen, 1984; McNab, 1989), population ecology (Damuth, 1981; Juanes, 1986; Gittleman & Purvis, 1998), locomotion (Mc- Mahon, 1975; Biewener, 1989; Alexander, 1996), and reproduction (Alex- ander, 1996). An enduring focus of these studies has been Cope’s Rule, the notion that body size tends to increase over time within lineages (Kurtén, 1953; Stanley, 1973; Polly, 1998). Such an observation has been made regarding many different clades but has been examined specifically in only a few (MacFadden, 1986; Arnold et al., 1995; Jablonski, 1996, 1997; Trammer & Kaim, 1997, 1999; Alroy, 1998). The discordant results of such analyses have underscored two points: (1) Cope’s Rule does not apply universally to all groups; and (2) even when present, size increases in different clades may reflect very different underlying processes. Thus, the question, “does Cope’s Rule exist?” is better parsed into two questions: “to which groups does Cope’s Rule apply?” and “what process is responsible for it in each?” Several recent works (McShea, 1994, 2000; Jablonski, 1997; Alroy, 1998, 2000a, 2000b) have begun to address these more specific questions, attempting to quantify patterns of body-size evolution in a phylogenetic (rather than strictly temporal) context, as well as developing methods for interpreting the resultant patterns. -
Raptors in Action 1 Suggested Pre-Visit Activities
PROGRAM OVERVIEW TOPIC: Small theropods commonly known as “raptors.” THEME: Explore the adaptations that made raptors unique and successful, like claws, intelligence, vision, speed, and hollow bones. PROGRAM DESCRIPTION: Razor-sharp teeth and sickle-like claws are just a few of the characteristics that have made raptors famous. Working in groups, students will build a working model of a raptor leg and then bring it to life while competing in a relay race that simulates the hunting techniques of these carnivorous animals. AUDIENCE: Grades 3–6 CURRICULUM CONNECTIONS: Grade 3 Science: Building with a Variety of Materials Grade 3–6 Math: Patterns and Relations Grade 4 Science: Building Devices and Vehicles that Move Grade 6 Science: Evidence and Investigation PROGRAM ObJECTIVES: 1. Students will understand the adaptations that contributed to the success of small theropods. 2. Students will explore the function of the muscles used in vertebrate movement and the mechanics of how a raptor leg works. 3. Students will understand the function of the raptorial claw. 4. Students will discover connections between small theropod dinosaurs and birds. SUGGESTED PRE-VISIT ACTIVITIES UNDERstANDING CLADIstICS Animals and plants are often referred to as part of a family or group. For example, the dog is part of the canine family (along with wolves, coyotes, foxes, etc.). Scientists group living things together based on relationships to gain insight into where they came from. This helps us identify common ancestors of different organisms. This method of grouping is called “cladistics.” Cladistics is a system that uses branches like a family tree to show how organisms are related to one another. -
Ornithomimids from the Nemegt Formation of Mongolia
J. Paleont. Soc. Korea. Vol. 22, No. 1, (2006) : p. 195-207 ORNITHOMIMIDS FROM THE NEMEGT FORMATION OF MONGOLIA Yoshitsugu Kobayashi1 and Rinchen Barsbold2 1Hokkaido University Museum, Hokkaido University, Sapporo, Hokkaido, 060-0810 Japan, [email protected] 2Paleontological Center of Mongolian Academy of Sciences, PO Box 260, Ulaan Bataar 210351, Mongolia, [email protected] Abstract: Two ornithomimids (Gallimimus bullatus and Anserimimus planinychus) and an enigmatic ornithomi- mid (Deinocheirus mirificus) from the Nemegt Formation (Maastrichtian) of Mongolia are reviewed in this study. Gallimimus bullatus is one of the best-known ornithomimids, but its diagnoses need to be revised. The length ratio of the manus/humerus in Gallimimus bullatusis 0.61. This is the smallest value in ornithomimosaurs (approximately 0.8 or more in other ornithomimosaurs) and may be a good character to diagnose Gallimimus bullatus as suggested by previous studies. Anserimimus planinychus is a unique ornithomimosaur in having strong deltopectoral crest of the humerus, dorsoventrally flat and nearly straight manual unguals, and long forelimbs. Anserimimus planinychus shares two characters (position of the biceps tubercle and alignment of the glenoid) with Gallimimus bullatus and has a long metacarpal I as in Ornithomimus edmontonicus (derived ornithomimosaur) and a long metacarpal III as in Harpymimus okladnikovi (primitive ornithomimosaur). The phylogenetic position of Deinocheirus mirificus has been problematic since its discovery. Preliminary