Dynamite Dinos

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Issue 12 BCFL Children’s Services DYNAMITE DINOS Today’s theme is all about dinosaurs! Dinosaurs walked the planet millions of years ago. Dinosaurs were humongous! They were much bigger than lots of animals that are alive today. Some dinosaurs were 40 feet high! There were lots of different types of dinosaurs too. Some were big and other were small. Some had scales like a lizard and others had feathers like a bird. Some dinosaurs walked, ran, and crawled, and other dinosaurs swam deep in the ocean. There were so many dinosaurs that scientists are still finding dinosaur fossils today! Today’s fun includes an eye spy, an activity to create your own dinosaur, and a matching game! Discover the Dinos! Many dinosaurs lived and traveled together in groups. These groups are called “packs.” Search through the packs of dinosaurs. Try to find all of the dinosaurs on the list on the next page. Keep track of the number of dinosaurs you spot! Discover the Dinos! Many dinosaurs lived and traveled together in groups. These groups are called “packs.” Search through the packs of dinosaurs. Try to find all of the dinosaurs on the list on the next page. Keep track of the number of dinosaurs you spot! Euoplocephalus Edmontonia Einiosaurus [amount found] [amount found] [amount found] Archaeopteryx Corythosaurus Pachycephalosaurus [amount found] [amount found] [amount found] Pachyrhinosaurus Lambeosaurus Prosaurolophus [amount found] [amount found] [amount found] Create Your Own Dino! Dinosaurs roamed the planet for millions of years. There were lots of different types dinosaurs that lived during this time. Each type of dinosaur looked different from each other. Use the questions below to create your own dinosaur. When you answer all of the questions draw out your dinosaur! What color is your dino? What does it eat? How big is it? Where does it live? What shape is it? Does it live in groups or by itself? Does it have scales or feathers? How long is it’s tail? Use your answers to those questions to draw your imaginary dino! Prehistoric Matching Test your knowledge by playing this matching game! Cut out all of the dinosaurs and their names, and mix them around face down. Try to match the dinosaur to it’s name! If you forget the name of a dinosaur look at the answer sheet on the next page! Triceratops Brontosaurus Pterodactyl Archaeopteryx Note: Print this page out single-sided. Mosasaurus Ankylosaurus Stegosaurus Tyrannosaurus Iguanodon Spinosaurus Note: Print this page out single-sided. Rainforest Matching Answers Triceratops Brontasaurus Pterodactyl Archaeopteryx Mosasaurus Ankylosaurus Stegosaurus Tyrannosaurus Iguanodon Spinosaurus Boredom Busters Bitez is an extension of our previous publication, Boredom Busters. Instead of one large publication, we will release three different Boredom Buster activities. Each issue is a different theme! For more resources and activities for children, please visit buckslib.org.

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CPY Document
v^ Official Journal of the Biology Unit of the American Topical Association 10 Vol. 40(4) DINOSAURS ON STAMPS by Michael K. Brett-Surman Ph.D. Dinosaurs are the most popular animals of all time, and the most misunderstood. Dinosaurs did not fly in the air and did not live in the oceans, nor on lake bottoms. Not all large "prehistoric monsters" are dinosaurs. The most famous NON-dinosaurs are plesiosaurs, moso- saurs, pelycosaurs, pterodactyls and ichthyosaurs. Any name ending in 'saurus' is not automatically a dinosaur, for' example, Mastodonto- saurus is neither a mastodon nor a dinosaur - it is an amphibian! Dinosaurs are defined by a combination of skeletal features that cannot readily be seen when the animal is fully restored in a flesh reconstruction. Because of the confusion, this compilation is offered as a checklist for the collector. This topical list compiles all the dinosaurs on stamps where the actual bones are pictured or whole restorations are used. It excludes footprints (as used in the Lesotho stamps), cartoons (as in the 1984 issue from Gambia), silhouettes (Ascension Island # 305) and unoffi- cial issues such as the famous Sinclair Dinosaur stamps. The name "Brontosaurus", which appears on many stamps, is used with quotation marks to denote it as a popular name in contrast to its correct scientific name, Apatosaurus. For those interested in a detailed encyclopedic work about all fossils on stamps, the reader is referred to the forthcoming book, 'Paleontology - a Guide to the Postal Materials Depicting Prehistoric Lifeforms' by Fran Adams et. al. The best book currently in print is a book titled 'Dinosaur Stamps of the World' by Baldwin & Halstead.
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And the Origin and Evolution of the Ankylosaur Pelvis
Pelvis of Gargoyleosaurus (Dinosauria: Ankylosauria) and the Origin and Evolution of the Ankylosaur Pelvis Kenneth Carpenter1,2*, Tony DiCroce3, Billy Kinneer3, Robert Simon4 1 Prehistoric Museum, Utah State University – Eastern, Price, Utah, United States of America, 2 Geology Section, University of Colorado Museum, Boulder, Colorado, United States of America, 3 Denver Museum of Nature and Science, Denver, Colorado, United States of America, 4 Dinosaur Safaris Inc., Ashland, Virginia, United States of America Abstract Discovery of a pelvis attributed to the Late Jurassic armor-plated dinosaur Gargoyleosaurus sheds new light on the origin of the peculiar non-vertical, broad, flaring pelvis of ankylosaurs. It further substantiates separation of the two ankylosaurs from the Morrison Formation of the western United States, Gargoyleosaurus and Mymoorapelta. Although horizontally oriented and lacking the medial curve of the preacetabular process seen in Mymoorapelta, the new ilium shows little of the lateral flaring seen in the pelvis of Cretaceous ankylosaurs. Comparison with the basal thyreophoran Scelidosaurus demonstrates that the ilium in ankylosaurs did not develop entirely by lateral rotation as is commonly believed. Rather, the preacetabular process rotated medially and ventrally and the postacetabular process rotated in opposition, i.e., lateral and ventrally. Thus, the dorsal surfaces of the preacetabular and postacetabular processes are not homologous. In contrast, a series of juvenile Stegosaurus ilia show that the postacetabular process rotated dorsally ontogenetically. Thus, the pelvis of the two major types of Thyreophora most likely developed independently. Examination of other ornithischians show that a non-vertical ilium had developed independently in several different lineages, including ceratopsids, pachycephalosaurs, and iguanodonts.
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A Revised Taxonomy of the Iguanodont Dinosaur Genera and Species
ARTICLE IN PRESS + MODEL Cretaceous Research xx (2007) 1e25 www.elsevier.com/locate/CretRes A revised taxonomy of the iguanodont dinosaur genera and species Gregory S. Paul 3109 North Calvert Station, Side Apartment, Baltimore, MD 21218-3807, USA Received 20 April 2006; accepted in revised form 27 April 2007 Abstract Criteria for designating dinosaur genera are inconsistent; some very similar species are highly split at the generic level, other anatomically disparate species are united at the same rank. Since the mid-1800s the classic genus Iguanodon has become a taxonomic grab-bag containing species spanning most of the Early Cretaceous of the northern hemisphere. Recently the genus was radically redesignated when the type was shifted from nondiagnostic English Valanginian teeth to a complete skull and skeleton of the heavily built, semi-quadrupedal I. bernissartensis from much younger Belgian sediments, even though the latter is very different in form from the gracile skeletal remains described by Mantell. Currently, iguanodont remains from Europe are usually assigned to either robust I. bernissartensis or gracile I. atherﬁeldensis, regardless of lo- cation or stage. A stratigraphic analysis is combined with a character census that shows the European iguanodonts are markedly more morpho- logically divergent than other dinosaur genera, and some appear phylogenetically more derived than others. Two new genera and a new species have been or are named for the gracile iguanodonts of the Wealden Supergroup; strongly bipedal Mantellisaurus atherﬁeldensis Paul (2006. Turning the old into the new: a separate genus for the gracile iguanodont from the Wealden of England. In: Carpenter, K. (Ed.), Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs.
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The Dinosaurs Transylvanian Province in Hungary
COMMUNICATIONS OF THE YEARBOOK OF THE ROYAL HUNGARIAN GEOLOGICAL IMPERIAL INSTITUTE ================================================================== VOL. XXIII, NUMBER 1. ================================================================== THE DINOSAURS OF THE TRANSYLVANIAN PROVINCE IN HUNGARY. BY Dr. FRANZ BARON NOPCSA. WITH PLATES I-IV AND 3 FIGURES IN THE TEXT. Published by The Royal Hungarian Geological Imperial Institute which is subject to The Royal Hungarian Agricultural Ministry BUDAPEST. BOOK-PUBLISHER OF THE FRANKLIN ASSOCIATION. 1915. THE DINOSAURS OF THE TRANSYLVANIAN PROVINCE IN HUNGARY. BY Dr. FRANZ BARON NOPCSA. WITH PLATES I-IV AND 3 FIGURES IN THE TEXT. Mit. a. d. Jahrb. d. kgl. ungar. Geolog. Reichsanst. XXIII. Bd. 1 heft I. Introduction. Since it appears doubtful when my monographic description of the dinosaurs of Transylvania1 that formed my so-to-speak preparatory works to my current dinosaur studies can be completed, due on one hand to outside circumstances, but on the other hand to the new arrangement of the vertebrate material in the kgl. ungar. geologischen Reichsanstalt accomplished by Dr. KORMOS, the necessity emerged of also exhibiting some of the dinosaur material located here, so that L. v. LÓCZY left the revision to me; I view the occasion, already briefly anticipating my final work at this point, to give diagnoses of the dinosaurs from the Transylvanian Cretaceous known up to now made possible from a systematic division of the current material, as well as to discuss their biology. The reptile remains known from the Danian of Transylvania will be mentioned only incidentally. Concerning the literature, I believe in refraining from more exact citations, since this work presents only a preliminary note.
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Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex
Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex By Karen E. Poole B.A. in Geology, May 2004, University of Pennsylvania M.A. in Earth and Planetary Sciences, August 2008, Washington University in St. Louis A Dissertation submitted to The Faculty of The Columbian College of Arts and Sciences of The George Washington University in partial fulfillment of the requirements for the degree of Doctor of Philosophy August 31, 2015 Dissertation Directed by Catherine Forster Professor of Biology The Columbian College of Arts and Sciences of The George Washington University certifies that Karen Poole has passed the Final Examination for the degree of Doctor of Philosophy as of August 10th, 2015. This is the final and approved form of the dissertation. Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex Karen E. Poole Dissertation Research Committee: Catherine A. Forster, Professor of Biology, Dissertation Director James M. Clark, Ronald Weintraub Professor of Biology, Committee Member R. Alexander Pyron, Robert F. Griggs Assistant Professor of Biology, Committee Member ii © Copyright 2015 by Karen Poole All rights reserved iii Dedication To Joseph Theis, for his unending support, and for always reminding me what matters most in life. To my parents, who have always encouraged me to pursue my dreams, even those they didn’t understand. iv Acknowledgements First, a heartfelt thank you is due to my advisor, Cathy Forster, for giving me free reign in this dissertation, but always providing valuable commentary on any piece of writing I sent her, no matter how messy.
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The Systematic Position of the Enigmatic Thyreophoran Dinosaur Paranthodon Africanus, and the Use of Basal Exemplifiers in Phyl
1 The systematic position of the enigmatic thyreophoran dinosaur Paranthodon africanus, 2 and the use of basal exemplifiers in phylogenetic analysis 3 4 Thomas J. Raven1,2 ,3 and Susannah C. R. Maidment2 ,3 5 61Department of Earth Science & Engineering, Imperial College London, UK 72School of Environment & Technology, University of Brighton, UK 8 3Department of Earth Sciences, Natural History Museum, London, UK 9 10Corresponding author: Thomas J. Raven 11 12Email address: [email protected] 13 14 15 16 17 18 19 20 21ABSTRACT 22 23The first African dinosaur to be discovered, Paranthodon africanus was found in 1845 in the 24Lower Cretaceous of South Africa. Taxonomically assigned to numerous groups since discovery, 25in 1981 it was described as a stegosaur, a group of armoured ornithischian dinosaurs 26characterised by bizarre plates and spines extending from the neck to the tail. This assignment 27that has been subsequently accepted. The type material consists of a premaxilla, maxilla, a nasal, 28and a vertebra, and contains no synapomorphies of Stegosauria. Several features of the maxilla 29and dentition are reminiscent of Ankylosauria, the sister-taxon to Stegosauria, and the premaxilla 30appears superficially similar to that of some ornithopods. The vertebral material has never been 31described, and since the last description of the specimen, there have been numerous discoveries 32of thyreophoran material potentially pertinent to establishing the taxonomic assignment of the 33specimen. An investigation of the taxonomic and systematic position of Paranthodon is therefore 34warranted. This study provides a detailed re-description, including the first description of the 35vertebra. Numerous phylogenetic analyses demonstrate that the systematic position of 36Paranthodon is highly labile and subject to change depending on which exemplifier for the clade 37Stegosauria is used.
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Dinosaur Species List E to M
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EUOPLOCEPHALUS ANKYLOSAURUS TSAGANTEGIA GASTONIA GARGOYLEOSAURUS - -- PANOPLOSAURUS 7,8939, (6, - Edmontonla 1L,26,34)
THE UNIVERSITY OF CALGARY Skull Morphology of the Ankylosauria by Matthew K. Vickaryous A THESIS SUBMITED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DEPARTMENT OF BIOLOGICAL SCIENCES CALGARY, ALBERTA JANUARY, 2001 O Matthew K. Vickaryous 2001 National Library Bibliothéque nationale I*l of Canada du Canada Acquisitions and Acquisitions et Bibliographie Services services bibliographiques 395 Wellington Street 395, rue Wellington Ottawa ON KIA ON4 Ottawa ON KIA ON4 Canada Canada Your Rie Votre rrlftimce Our fite Notre dfbrance The author has granted a non- L'auteur a accordé une licence non exclusive licence allowing the exclusive permettant à la National Library of Canada to Bibliothèque nationale du Canada de reproduce, loan, distribute or sell reproduire, prêter, distribuer ou copies of this thesis in microform, vendre des copies de cette thèse sous paper or electronic formats. la forme de microfiche/film, de reproduction sur papier ou sur format électronique. The author retains ownership of the L'auteur conserve la propriété du copyright in this thesis. Neither the droit d'auteur qui protège cette thèse. thesis nor substantial extracts fiom it Ni la thèse ni des extraits substantiels may be printed or otherwise de celle-ci ne doivent être imprimés reproduced without the author's ou autrement reproduits sans son permission. autorisation. Abstract The vertebrate head skeleton is a fundamental source of biological information for the study of both modern and extinct taxa. Detailed analysis of structural modifications in one taxon frequently identifies developmental and / or functional features widespread amongst a more inclusive clade of organisms.
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Dinosauria: Ornithischia
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Repository of the Academy's Library Diversity and convergences in the evolution of feeding adaptations in ankylosaurs Törölt: Diversity of feeding characters explains evolutionary success of ankylosaurs (Dinosauria: Ornithischia)¶ (Dinosauria: Ornithischia) Formázott: Betűtípus: Félkövér Formázott: Betűtípus: Félkövér Formázott: Betűtípus: Félkövér Attila Ősi1, 2*, Edina Prondvai2, 3, Jordan Mallon4, Emese Réka Bodor5 Formázott: Betűtípus: Félkövér 1Department of Paleontology, Eötvös University, Budapest, Pázmány Péter sétány 1/c, 1117, Hungary; +36 30 374 87 63; [email protected] 2MTA-ELTE Lendület Dinosaur Research Group, Budapest, Pázmány Péter sétány 1/c, 1117, Hungary; +36 70 945 51 91; [email protected] 3University of Gent, Evolutionary Morphology of Vertebrates Research Group, K.L. Ledegankstraat 35, Gent, Belgium; +32 471 990733; [email protected] 4Palaeobiology, Canadian Museum of Nature, PO Box 3443, Station D, Ottawa, Ontario, K1P 6P4, Canada; +1 613 364 4094; [email protected] 5Geological and Geophysical Institute of Hungary, Budapest, Stefánia út 14, 1143, Hungary; +36 70 948 0248; [email protected] Research was conducted at the Eötvös Loránd University, Budapest, Hungary. *Corresponding author: Attila Ősi, [email protected] Acknowledgements This work was supported by the MTA–ELTE Lendület Programme (Grant No. LP 95102), OTKA (Grant No. T 38045, PD 73021, NF 84193, K 116665), National Geographic Society (Grant No. 7228–02, 7508–03), Bakonyi Bauxitbánya Ltd, Geovolán Ltd, Hungarian Natural History Museum, Hungarian Academy of Sciences, Canadian Museum of Nature, The Jurassic Foundation, Hantken Miksa Foundation, Eötvös Loránd University. Disclosure statment: All authors declare that there is no financial interest or benefit arising from the direct application of this research.
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DINOSAUR BOOKLET No. 2 Iguanodon Bernissartensis and Mantellisaurus Atherfieldensis
DINOSAUR BOOKLET No. 2 Iguanodon bernissartensis and Mantellisaurus atherfieldensis Description Iguanodon (pronounced 'Ig-wan-oh-don') was one of the first dinosaurs to be named. The name is derived from 'Iguana' - a type of modern reptile, and 'don' meaning tooth. Iguanodon is the name of a small group of dinosaurs within the much larger group called Iguanodontids; they were large herbivores, with a long tail for balance, and hind legs that were longer than their fore limbs. There were three large hooved toes on each foot, and four fingers and a thumb spike on each hand. The mouth had a battery of chewing teeth, and a boney beak in place of front teeth. Since its initial discovery in the early nineteenth century, and more detailed reconstructions after complete skeletons were found in a Belgian mine in 1878, we have been forced to re-evaluate its posture, shape and movement; and to look again at how it fits in with other members of the Iguanodontids. Fossil remains from the group show they existed from the late Jurassic through to the late Cretaceous. Here on the Isle of Wight it was once thought there were two basic species of Iguanodon; a larger form called Iguanodon bernissartensis, and a more graceful species called Iguanodon atherfieldensis. The first was named after the Belgian town where complete skeletons were found (Bernissart) and the latter from Atherfield on the south west coast of the Isle of Wight. However 1 more recently palaeontologist Gregory Paul has moved our smaller variety to a new genera, leaving us with only one Iguanodon but a new genera of Iguanodontid called Mantellisaurus atherfieldensis (named after Gideon Mantell) in its place.
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A Census of Dinosaur Fossils Recovered from the Hell Creek and Lance Formations (Maastrichtian)
The Journal of Paleontological Sciences: JPS.C.2019.01 1 TAKING COUNT: A Census of Dinosaur Fossils Recovered From the Hell Creek and Lance Formations (Maastrichtian). ______________________________________________________________________________________ Walter W. Stein- President, PaleoAdventures 1432 Mill St.. Belle Fourche, SD 57717. [email protected] 605-210-1275 ABSTRACT: A census of Hell Creek and Lance Formation dinosaur remains was conducted from April, 2017 through February of 2018. Online databases were reviewed and curators and collections managers interviewed in an effort to determine how much material had been collected over the past 130+ years of exploration. The results of this new census has led to numerous observations regarding the quantity, quality, and locations of the total collection, as well as ancillary data on the faunal diversity and density of Late Cretaceous dinosaur populations. By reviewing the available data, it was also possible to make general observations regarding the current state of certain exploration programs, the nature of collection bias present in those collections and the availability of today's online databases. A total of 653 distinct, associated and/or articulated remains (skulls and partial skeletons) were located. Ceratopsid skulls and partial skeletons (mostly identified as Triceratops) were the most numerous, tallying over 335+ specimens. Hadrosaurids (Edmontosaurus) were second with at least 149 associated and/or articulated remains. Tyrannosaurids (Tyrannosaurus and Nanotyrannus) were third with a total of 71 associated and/or articulated specimens currently known to exist. Basal ornithopods (Thescelosaurus) were also well represented by at least 42 known associated and/or articulated remains. The remaining associated and/or articulated specimens, included pachycephalosaurids (18), ankylosaurids (6) nodosaurids (6), ornithomimids (13), oviraptorosaurids (9), dromaeosaurids (1) and troodontids (1).
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Our Museum Dinosaurs
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