The Dinosaurs Transylvanian Province in Hungary
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Dino Hunt Checklist Card Name Type Rarity Acanthopholis
Dino Hunt Checklist Card Name Type Rarity Acanthopholis Dinosaur Common Acrocanthosaurus Dinosaur Rare Albertosaurus Dinosaur Rare Albertosaurus Dinosaur Ultra Rare Alioramus Dinosaur Rare Allosaurus Dinosaur Rare* Altispinax Dinosaur Rare* Amargasaurus Dinosaur Uncommon* Ammosaurus Dinosaur Uncommon* Anatotitan Dinosaur Common Anchiceratops Dinosaur Common Anchisaurus Dinosaur Common* Ankylosaurus Dinosaur Uncommon* Antarctosaurus Dinosaur Common Apatosaurus Dinosaur Uncommon* Archaeopteryx Dinosaur Rare* Archelon Dinosaur Rare Arrhinoceratops Dinosaur Common Avimimus Dinosaur Common Baby Ankylosaur Dinosaur Common Baby Ceratopsian Dinosaur Common Baby Hadrosaur Dinosaur Common Baby Raptor Dinosaur Rare Baby Sauropod Dinosaur Common Baby Theropod Dinosaur Rare Barosaurus Dinosaur Uncommon Baryonyx Dinosaur Rare* Bellusaurus Dinosaur Common Brachiosaurus Dinosaur Rare* Brachyceratops Dinosaur Uncommon Camarasaurus Dinosaur Common Camarasaurus Dinosaur Ultra Rare Camptosaurus Dinosaur Common Carnotaurus Dinosaur Rare Centrosaurus Dinosaur Common Ceratosaurus Dinosaur Rare* Cetiosaurus Dinosaur Common* Changdusaurus Dinosaur Common Chasmosaurus Dinosaur Common Chilantaisaurus Dinosaur Rare Coelophysis Dinosaur Uncommon* Coloradisaurus Dinosaur Common* Compsognathus Dinosaur Rare* Corythosaurus Dinosaur Common* Cryolophosaurus Dinosaur Rare Cynognathus Dinosaur Rare Dacentrurus Dinosaur Common* Daspletosaurus Dinosaur Rare Datousaurus Dinosaur Common Deinocheirus Dinosaur Rare* Deinonychus Dinosaur Uncommon* Deinosuchus Dinosaur Rare* Diceratops -
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. -
Two New Stegosaur Specimens from the Upper Jurassic Morrison Formation of Montana, USA
Editors' choice Two new stegosaur specimens from the Upper Jurassic Morrison Formation of Montana, USA D. CARY WOODRUFF, DAVID TREXLER, and SUSANNAH C.R. MAIDMENT Woodruff, D.C., Trexler, D., and Maidment, S.C.R. 2019. Two new stegosaur specimens from the Upper Jurassic Morrison Formation of Montana, USA. Acta Palaeontologica Polonica 64 (3): 461–480. Two partial skeletons from Montana represent the northernmost occurrences of Stegosauria within North America. One of these specimens represents the northernmost dinosaur fossil ever recovered from the Morrison Formation. Consisting of fragmentary cranial and postcranial remains, these specimens are contributing to our knowledge of the record and distribution of dinosaurs within the Morrison Formation from Montana. While the stegosaurs of the Morrison Formation consist of Alcovasaurus, Hesperosaurus, and Stegosaurus, the only positively identified stegosaur from Montana thus far is Hesperosaurus. Unfortunately, neither of these new specimens exhibit diagnostic autapomorphies. Nonetheless, these specimens are important data points due to their geographic significance, and some aspects of their morphologies are striking. In one specimen, the teeth express a high degree of wear usually unobserved within this clade—potentially illuminating the progression of the chewing motion in derived stegosaurs. Other morphologies, though not histologically examined in this analysis, have the potential to be important indicators for maturational inferences. In suite with other specimens from the northern extent of the formation, these specimens contribute to the ongoing discussion that body size may be latitudinally significant for stegosaurs—an intriguing geographical hypothesis which further emphasizes that size is not an undeviating proxy for maturity in dinosaurs. Key words: Dinosauria, Thyreophora, Stegosauria, Jurassic, Morrison Formation, USA, Montana. -
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. -
Dinosaurs British Isles
DINOSAURS of the BRITISH ISLES Dean R. Lomax & Nobumichi Tamura Foreword by Dr Paul M. Barrett (Natural History Museum, London) Skeletal reconstructions by Scott Hartman, Jaime A. Headden & Gregory S. Paul Life and scene reconstructions by Nobumichi Tamura & James McKay CONTENTS Foreword by Dr Paul M. Barrett.............................................................................10 Foreword by the authors........................................................................................11 Acknowledgements................................................................................................12 Museum and institutional abbreviations...............................................................13 Introduction: An age-old interest..........................................................................16 What is a dinosaur?................................................................................................18 The question of birds and the ‘extinction’ of the dinosaurs..................................25 The age of dinosaurs..............................................................................................30 Taxonomy: The naming of species.......................................................................34 Dinosaur classification...........................................................................................37 Saurischian dinosaurs............................................................................................39 Theropoda............................................................................................................39 -
Notes on British Dinosaurs. Part I: Hypsilophodon
Dr. Francis Baron Nopcsa—British Dinosaurs. 203 II.—NOTES ON BRITISH DINOSAURS. PAET I: ffrpsiLOPHODOK. By Dr. FRANCIS BARON NOPCSA. (WITH A PAGE-ILLUSTRATION.) URING a recent stay in London the kindness of Dr. A. S. Woodward enabled me to study some of the splendid Dinosaurian remainD s in the British Museum. Having principally occupied myself till now with Ornithopodous Dinosaurs, first of all Hypsilophodon attracted my attention, and my expectation that this type would prove to be the clue for the- understanding of all the other Orthopoda has been perfectly fulfilled. Hypsilophodon was described and figured at various times by Owen, Huxley, and Hulke; a restoration of this animal was given by Marsh in the GEOLOGICAL MAGAZINE for 1896 (p. 6, Fig. 2), and the complete bibliographical list concerning this Dinosaur is compiled in my paper "Synopsis und Abstammung der Dinosaurier" (Foldtani Xozlony, 1901, Budapest). In consequence of our more recent knowledge of Dinosaurs in general I managed to detect some new points of remarkable interest. Mandible. What Hulke, in describing the Hypsilophodon skull, No. 110, supposed to be the parietal, frontal, and post-frontal bones (Phil. Trans., 1882, pi. lxxi, fig. 1, pa., fr., ps.f.), turned out to be the outer view of a complete right mandibular ramus, so that the parietal changes into an articular, the frontal becomes the dentary, and the post-frontal the coronoid bone. This piece (p. 207, Fig. 4) is, in fact, the finest mandibulum of Hypsilophodon I have seen in the whole collection, and as such worthy to be refigured. The general outline of the mandibulum, with its strongly ab- breviated post-coronoidal part and its blunt processus coronoideum, reminds one somewhat of the under jaw of Placodus gigas, though it differs of course in nearly every detail, being built up after the Iguanodon type. -
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. -
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. -
Cairanoolithus: a Large Egg for a Small Dinosaur with Wide Hips
20/11/2020 <em>Cairanoolithus</em>: a Large Egg for a Small Dinosaur With Wide Hips - UABDivulga Barcelona Research & Innovation 02/2015 Cairanoolithus: a Large Egg for a Small Dinosaur With Wide Hips The study of the microstructure of the eggshell of Cairanoolithus conducted by Albert G. Sellés and Angel Galobart, both researchers at the Catalan Institute of Palaeontology Miquel Crusafont (ICP), reveals that this egg type does not belong to sauropod dinosaurs but to ankylosaurs, and probably to Struthiosaurus, a genus of armored dinosaurs. The finding would represent the first description of thyreophora eggs (a group that includes ankylosauria and stegosauria) in the world. It is an arduous task for paleontologists to assign the fossil eggs they found in excavations to a certain dinosaur species or group of dinosaurs, especially because the lack of bones of the parents in the nests and the low probability to find embryonic remains that would help in the taxonomic assignation of the eggs. Thus, we often do not known who laid a certain fossil egg. These limitations have led scientist to design a specific system for naming and classifying fossil eggs, using concepts such as "oogenera" and "ooespecies" for its phylogenetic classification. Cairanoolithus is an oogenus discovered and described in the early 90’s. It takes its name from the first place where it was found, a site near La Cairanne, a small town from southeastern France. From then on, Cairanoolithus has been found in 25 different sites. These eggs are between 72.2 and 71.4 million years old, they are large (over 15 cm in diameter) and have a rounded shape. -
Inferring Body Mass in Extinct Terrestrial Vertebrates and the Evolution of Body Size in a Model-Clade of Dinosaurs (Ornithopoda)
Inferring Body Mass in Extinct Terrestrial Vertebrates and the Evolution of Body Size in a Model-Clade of Dinosaurs (Ornithopoda) by Nicolás Ernesto José Campione Ruben A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Ecology and Evolutionary Biology University of Toronto © Copyright by Nicolás Ernesto José Campione Ruben 2013 Inferring body mass in extinct terrestrial vertebrates and the evolution of body size in a model-clade of dinosaurs (Ornithopoda) Nicolás E. J. Campione Ruben Doctor of Philosophy Ecology and Evolutionary Biology University of Toronto 2013 Abstract Organismal body size correlates with almost all aspects of ecology and physiology. As a result, the ability to infer body size in the fossil record offers an opportunity to interpret extinct species within a biological, rather than simply a systematic, context. Various methods have been proposed by which to estimate body mass (the standard measure of body size) that center on two main approaches: volumetric reconstructions and extant scaling. The latter are particularly contentious when applied to extinct terrestrial vertebrates, particularly stem-based taxa for which living relatives are difficult to constrain, such as non-avian dinosaurs and non-therapsid synapsids, resulting in the use of volumetric models that are highly influenced by researcher bias. However, criticisms of scaling models have not been tested within a comprehensive extant dataset. Based on limb measurements of 200 mammals and 47 reptiles, linear models were generated between limb measurements (length and circumference) and body mass to test the hypotheses that phylogenetic history, limb posture, and gait drive the relationship between stylopodial circumference and body mass as critics suggest. -
Ankylosaurid Dinosaur Tail Clubs Evolved Through Stepwise Acquisition of Key Features
1 Title: Ankylosaurid dinosaur tail clubs evolved through stepwise acquisition of key features. 2 3 Victoria M. Arbour1,2,3 and Philip J. Currie3 4 1Paleontology and Geology Research Laboratory, North Carolina Museum of Natural Sciences, Raleigh, 5 North Carolina 27601, USA; 2Department of Biological Sciences, North Carolina State University, Raleigh, 6 North Carolina, 27607, USA; 3Department of Biological Sciences, University of Alberta, Edmonton, 7 Alberta, T6G 2E9, Canada; [email protected] 8 Corresponding author: V. Arbour 9 10 Running title: ANKYLOSAURID TAIL CLUB STEPWISE EVOLUTION 11 12 13 14 15 16 17 18 19 20 21 22 23 24 1 25 ABSTRACT 26 Ankylosaurid ankylosaurs were quadrupedal, herbivorous dinosaurs with abundant dermal 27 ossifications. They are best known for their distinctive tail club composed of stiff, interlocking vertebrae 28 (the handle) and large, bulbous osteoderms (the knob), which may have been used as a weapon. 29 However, tail clubs appear relatively late in the evolution of ankylosaurids, and seemed to have been 30 present only in a derived clade of ankylosaurids during the last 20 million years of the Mesozoic Era. 31 New evidence from mid Cretaceous fossils from China suggests that the evolution of the tail club 32 occurred at least 40 million years earlier, and in a stepwise manner, with early ankylosaurids evolving 33 handle-like vertebrae before the distal osteoderms enlarged and coossified to form a knob. 34 35 Keywords: Dinosauria, Ankylosauria, Ankylosauridae, Cretaceous 36 37 38 39 40 41 42 43 44 45 46 47 48 2 49 INTRODUCTION 50 Tail weaponry, in the form of spikes or clubs, is an uncommon adaptation among tetrapods. -
Huxley—On a New Reptile from the Chalk-Marl. 65
Huxley—On a new Reptile from the Chalk-marl. 65 IV.—OK AcAifTaoPBOLis HORRIDUS, A NEW KEPTILE FBOH THK CHALK-MARL. By THOMAS H. HUXLET, F.B.S., V.P.G.S., Professor of Natural History in the Royal School of Mines. PLATE V. OME time since, my colleague, Dr. Percy, purchased from Mr. S Griffiths, of Folkestone, and sent to me, certain fossils from the Chalk-marl near that town, which appeared to possess unusual characters. On examining them I found that they were large scutes and spines entering into the dermal armour of what, I did not doubt, was a large reptile allied to Soelidosaurm, Hylceosaurus, and Pola- canthus. I therefore requested Mr. Griffiths to procure for me every fragment of the skeleton which he could procure from the somewhat inconvenient locality (between tide-marks) in which the remains had been found, and I eventually succeeded in obtaining three teeth, with a number of fragments of vertebrae, part of the skull and limb-bones, besides a large additional quantity of scutes. I am still not without hope of recovering other parts of the skeleton; but as the remain* in my hands are sufficient to enable me to form a tolerably clear notion of the animal's, structure, a brief notice of its main features will probably interest the readers of the GEOLOGICAL MAGAZINE. The dermal bony plates or scutes (Plate V. Pigs. 1-3) are of very various forms and sizes, from oval disks slightly raised in the middle, and hardly more than an inch in diameter, up to such great spines'as that represented in Plate V.