Rebekah Marion Vice, 2020
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
A Neoceratopsian Dinosaur from the Early Cretaceous of Mongolia And
ARTICLE https://doi.org/10.1038/s42003-020-01222-7 OPEN A neoceratopsian dinosaur from the early Cretaceous of Mongolia and the early evolution of ceratopsia ✉ Congyu Yu 1 , Albert Prieto-Marquez2, Tsogtbaatar Chinzorig 3,4, Zorigt Badamkhatan4,5 & Mark Norell1 1234567890():,; Ceratopsia is a diverse dinosaur clade from the Middle Jurassic to Late Cretaceous with early diversification in East Asia. However, the phylogeny of basal ceratopsians remains unclear. Here we report a new basal neoceratopsian dinosaur Beg tse based on a partial skull from Baruunbayan, Ömnögovi aimag, Mongolia. Beg is diagnosed by a unique combination of primitive and derived characters including a primitively deep premaxilla with four pre- maxillary teeth, a trapezoidal antorbital fossa with a poorly delineated anterior margin, very short dentary with an expanded and shallow groove on lateral surface, the derived presence of a robust jugal having a foramen on its anteromedial surface, and five equally spaced tubercles on the lateral ridge of the surangular. This is to our knowledge the earliest known occurrence of basal neoceratopsian in Mongolia, where this group was previously only known from Late Cretaceous strata. Phylogenetic analysis indicates that it is sister to all other neoceratopsian dinosaurs. 1 Division of Vertebrate Paleontology, American Museum of Natural History, New York 10024, USA. 2 Institut Català de Paleontologia Miquel Crusafont, ICTA-ICP, Edifici Z, c/de les Columnes s/n Campus de la Universitat Autònoma de Barcelona, 08193 Cerdanyola del Vallès Sabadell, Barcelona, Spain. 3 Department of Biological Sciences, North Carolina State University, Raleigh, NC 27695, USA. 4 Institute of Paleontology, Mongolian Academy of Sciences, ✉ Ulaanbaatar 15160, Mongolia. -
MEET the DINOSAURS! WHAT’S in a NAME? a LOT If You Are a Dinosaur!
MEET THE DINOSAURS! WHAT’S IN A NAME? A LOT if you are a dinosaur! I will call you Dyoplosaurus! Most dinosaurs get their names from the ancient Greek and Latin languages. And I will call you Mojoceratops! And sometimes they are named after a defining feature on their body. Their names are made up of word parts that describe the dinosaur. The name must be sent to a special group of people called the International Commission on Zoological Nomenclature to be approved! Did You The word DINOSAUR comes from the Greek word meaning terrible lizard and was first said by Know? Sir Richard Owen in 1841. © 2013 Omaha’s Henry Doorly Zoo & Aquarium® | 3 SEE IF YOU CAN FIND OUT THE MEANING OF SOME OF OUR DINOSAUR’S NAMES. Dinosaur names are not just tough to pronounce, they often have meaning. Dinosaur Name MEANING of Dinosaur Name Carnotaurus (KAR-no-TORE-us) Means “flesh-eating bull” Spinosaurus (SPY-nuh-SORE-us) Dyoplosaurus (die-o-pluh-SOR-us) Amargasaurus (ah-MAR-guh-SORE-us) Omeisaurus (Oh-MY-ee-SORE-us) Pachycephalosaurus (pak-ee-SEF-uh-low-SORE-us) Tuojiangosaurus (toh-HWANG-uh-SORE-us) Yangchuanosaurus (Yang-chew-ON-uh-SORE-us) Quetzalcoatlus (KWET-zal-coe-AT-lus) Ouranosaurus (ooh-RAN-uh-SORE-us) Parasaurolophus (PAIR-uh-so-ROL-uh-PHUS) Kosmoceratops (KOZ-mo-SARA-tops) Mojoceratops (moe-joe-SEH-rah-tops) Triceratops (try-SER-uh-TOPS) Tyrannosaurus rex (tuh-RAN-uh-SORE-us) Find the answers by visiting the Resource Library at Carnotaurus A: www.OmahaZoo.com/Education. Search word: Dinosaurs 4 | © 2013 Omaha’s Henry Doorly Zoo & Aquarium® DINO DEFENSE All animals in the wild have to protect themselves. -
Offer Your Guests a Visually Stunning and Interactive Experience They Won’T Find Anywhere Else World of Animals
Creative Arts & Attractions Offer Your Guests a Visually Stunning and Interactive Experience They Won’t Find Anywhere Else World of Animals Entertain guests with giant illuminated, eye-catching displays of animals from around the world. Animal displays are made in the ancient Eastern tradition of lantern-making with 3-D metal frames, fiberglass, and acrylic materials. Unique and captivating displays will provide families and friends with a lifetime of memories. Animatronic Dinosaurs Fascinate patrons with an impressive visual spectacle in our exhibitions. Featured with lifelike appearances, vivid movements and roaring sounds. From the very small to the gigantic dinosaurs, we have them all. Everything needed for a realistic and immersive experience for your patrons. Providing interactive options for your event including riding dinosaurs and dinosaur inflatable slides. Enhancing your merchandise stores with dinosaur balloons and toys. Animatronic Dinosaur Options Abelisaurus Maiasaura Acrocanthosaurus Megalosaurus Agilisaurus Olorotitan arharensis Albertosaurus Ornithomimus Allosaurus Ouranosaurus nigeriensis Ankylosaurus Oviraptor philoceratops Apatosaurus Pachycephalosaurus wyomingensis Archaeopteryx Parasaurolophus Baryonyx Plateosaurus Brachiosaurus Protoceratops andrewsi Carcharodontosaurus Pterosauria Carnotaurus Pteranodon longiceps Ceratosaurus Raptorex Coelophysis Rugops Compsognathus Spinosaurus Deinonychus Staurikosaurus pricei Dilophosaurus Stegoceras Diplodocus Stegosaurus Edmontosaurus Styracosaurus Eoraptor Lunensis Suchomimus -
At Carowinds
at Carowinds EDUCATOR’S GUIDE CLASSROOM LESSON PLANS & FIELD TRIP ACTIVITIES Table of Contents at Carowinds Introduction The Field Trip ................................... 2 The Educator’s Guide ....................... 3 Field Trip Activity .................................. 4 Lesson Plans Lesson 1: Form and Function ........... 6 Lesson 2: Dinosaur Detectives ....... 10 Lesson 3: Mesozoic Math .............. 14 Lesson 4: Fossil Stories.................. 22 Games & Puzzles Crossword Puzzles ......................... 29 Logic Puzzles ................................. 32 Word Searches ............................... 37 Answer Keys ...................................... 39 Additional Resources © 2012 Dinosaurs Unearthed Recommended Reading ................. 44 All rights reserved. Except for educational fair use, no portion of this guide may be reproduced, stored in a retrieval system, or transmitted in any form or by any Dinosaur Data ................................ 45 means—electronic, mechanical, photocopy, recording, or any other without Discovering Dinosaurs .................... 52 explicit prior permission from Dinosaurs Unearthed. Multiple copies may only be made by or for the teacher for class use. Glossary .............................................. 54 Content co-created by TurnKey Education, Inc. and Dinosaurs Unearthed, 2012 Standards www.turnkeyeducation.net www.dinosaursunearthed.com Curriculum Standards .................... 59 Introduction The Field Trip From the time of the first exhibition unveiled in 1854 at the Crystal -
Investigating Sexual Dimorphism in Ceratopsid Horncores
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2013-01-25 Investigating Sexual Dimorphism in Ceratopsid Horncores Borkovic, Benjamin Borkovic, B. (2013). Investigating Sexual Dimorphism in Ceratopsid Horncores (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/26635 http://hdl.handle.net/11023/498 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Investigating Sexual Dimorphism in Ceratopsid Horncores by Benjamin Borkovic A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DEPARTMENT OF BIOLOGICAL SCIENCES CALGARY, ALBERTA JANUARY, 2013 © Benjamin Borkovic 2013 Abstract Evidence for sexual dimorphism was investigated in the horncores of two ceratopsid dinosaurs, Triceratops and Centrosaurus apertus. A review of studies of sexual dimorphism in the vertebrate fossil record revealed methods that were selected for use in ceratopsids. Mountain goats, bison, and pronghorn were selected as exemplar taxa for a proof of principle study that tested the selected methods, and informed and guided the investigation of sexual dimorphism in dinosaurs. Skulls of these exemplar taxa were measured in museum collections, and methods of analysing morphological variation were tested for their ability to demonstrate sexual dimorphism in their horns and horncores. -
A Revision of the Ceratopsia Or Horned Dinosaurs
MEMOIRS OF THE PEABODY MUSEUM OF NATURAL HISTORY VOLUME III, 1 A.R1 A REVISION orf tneth< CERATOPSIA OR HORNED DINOSAURS BY RICHARD SWANN LULL STERLING PROFESSOR OF PALEONTOLOGY AND DIRECTOR OF PEABODY MUSEUM, YALE UNIVERSITY LVXET NEW HAVEN, CONN. *933 MEMOIRS OF THE PEABODY MUSEUM OF NATURAL HISTORY YALE UNIVERSITY Volume I. Odontornithes: A Monograph on the Extinct Toothed Birds of North America. By Othniel Charles Marsh. Pp. i-ix, 1-201, pis. 1-34, text figs. 1-40. 1880. To be obtained from the Peabody Museum. Price $3. Volume II. Part 1. Brachiospongidae : A Memoir on a Group of Silurian Sponges. By Charles Emerson Beecher. Pp. 1-28, pis. 1-6, text figs. 1-4. 1889. To be obtained from the Peabody Museum. Price $1. Volume III. Part 1. American Mesozoic Mammalia. By George Gaylord Simp- son. Pp. i-xvi, 1-171, pis. 1-32, text figs. 1-62. 1929. To be obtained from the Yale University Press, New Haven, Conn. Price $5. Part 2. A Remarkable Ground Sloth. By Richard Swann Lull. Pp. i-x, 1-20, pis. 1-9, text figs. 1-3. 1929. To be obtained from the Yale University Press, New Haven, Conn. Price $1. Part 3. A Revision of the Ceratopsia or Horned Dinosaurs. By Richard Swann Lull. Pp. i-xii, 1-175, pis. I-XVII, text figs. 1-42. 1933. To be obtained from the Peabody Museum. Price $5 (bound in cloth), $4 (bound in paper). Part 4. The Merycoidodontidae, an Extinct Group of Ruminant Mammals. By Malcolm Rutherford Thorpe. In preparation. -
Histology and Ontogeny of Pachyrhinosaurus Nasal Bosses By
Histology and Ontogeny of Pachyrhinosaurus Nasal Bosses by Elizabeth Kruk A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Systematics and Evolution Department of Biological Sciences University of Alberta © Elizabeth Kruk, 2015 Abstract Pachyrhinosaurus is a peculiar ceratopsian known only from Upper Cretaceous strata of Alberta and the North Slope of Alaska. The genus consists of three described species Pachyrhinosaurus canadensis, Pachyrhinosaurus lakustai, and Pachyrhinosaurus perotorum that are distinguishable by cranial characteristics, including parietal horn shape and orientation, absence/presence of a rostral comb, median parietal bar horns, and profile of the nasal boss. A fourth species of Pachyrhinosaurus is described herein and placed into its phylogenetic context within Centrosaurinae. This new species forms a polytomy at the crown with Pachyrhinosaurus canadensis and Pachyrhinosaurus perotorum, with Pachyrhinosaurus lakustai falling basal to that polytomy. The diagnostic features of this new species are an apomorphic, laterally curved Process 3 horns and a thick longitudinal ridge separating the supraorbital bosses. Another focus is investigating the ontogeny of Pachyrhinosaurus nasal bosses in a histological context. Previously, little work has been done on cranial histology in ceratopsians, focusing instead on potential integumentary structures, the parietals of Triceratops, and how surface texture relates to underlying histological structures. An ontogenetic series is established for the nasal bosses of Pachyrhinosaurus at both relative (subadult versus adult) and fine scale (Stages 1-5). It was demonstrated that histology alone can indicate relative ontogenetic level, but not stages of a finer scale. Through Pachyrhinosaurus ontogeny the nasal boss undergoes increased vascularity and secondary remodeling with a reduction in osteocyte lacunar density. -
Dinosaur Eggshells from the Lower Maastrichtian St. Mary River Formation of Southern Alberta, Canada
Canadian Journal of Earth Sciences Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern Alberta, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2017-0195.R1 Manuscript Type: Article Date Submitted by the Author: 13-Nov-2017 Complete List of Authors: Voris, Jared; University of Calgary, Geoscience; Zelenitsky, Darla; Department of Geoscience, Tanaka, Kohei; Nagoya Daigaku Hakubutsukan; University of Calgary, DepartmentDraft of Geoscience Therrien, François; Royal Tyrrell Museum of Palaeontology, Is the invited manuscript for consideration in a Special N/A Issue? : Keyword: eggshell, dinosaur, Cretaceous, Maastrichtian, Alberta https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 47 Canadian Journal of Earth Sciences 1 2 3 4 5 6 7 8 9 Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern 10 Alberta, Canada 11 12 Jared T. Voris, Darla K. Zelenitsky,Draft François Therrien, Kohei Tanaka 13 J. T. Voris, D. K. Zelenitsky, and K. Tanaka. Department of Geoscience, University of 14 Calgary, 2500 University Dr. NW, Calgary, AB T2N 1N4, Canada; [email protected], 15 [email protected], [email protected] 16 K. Tanaka. Nagoya University Museum, Nagoya University Furocho, Chikusa-Ku, Nagoya, 17 464-8601, Japan; [email protected] 18 F. Therrien. Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, AB T0J 0Y0, 19 Canada.; [email protected] 20 1 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 47 1 2 Abstract–North America is known for its rich uppermost Cretaceous record of dinosaur egg 3 remains, although a notable fossil gap exists during the lower Maastrichtian. -
A New Horned Dinosaur from an Upper Cretaceous Bone Bed in Alberta
Darren H. Tanke Darren H. Tanke Langston, Jr. Wann Philip J. Currie, Philip J. Currie is a professor and Canada In the first monographic treatment of Research Chair at The University of Alberta Philip J. Currie, Wann Langston, Jr., & Darren H. Tanke a horned (ceratopsid) dinosaur in almost a (Department of Biological Sciences), is an Adjunct century, this monumental volume presents Professor at the University of Calgary, and was for- merly the Curator of Dinosaurs at the Royal Tyrrell one of the closest looks at the anatomy, re- Museum of Palaeontology. He took his B.Sc. at the lationships, growth and variation, behavior, University of Toronto in 1972, and his M.Sc. and ecology and other biological aspects of a sin- Ph.D. at McGill in 1975 and 1981. He is a Fellow of gle dinosaur species. The research, which was the Royal Society of Canada (1999) and a member A New Horned conducted over two decades, was possible of the Explorers Club (2001). He has published more because of the discovery of a densely packed than 100 scientific articles, 95 popular articles and bonebed near Grande Prairie, Alberta. The fourteen books, focussing on the growth and varia- tion of extinct reptiles, the anatomy and relationships Dinosaur From an locality has produced abundant remains of a of carnivorous dinosaurs, and the origin of birds. new species of horned dinosaur (ceratopsian), Fieldwork connected with his research has been con- and parts of at least 27 individual animals centrated in Alberta, Argentina, British Columbia, were recovered. China, Mongolia, the Arctic and Antarctica. -
Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area
ERCB/AGS Special Report 093 Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Stefan Bachu Maja Buschkuehle Kristine Haug Karsten Michael Alberta Geological Survey Alberta Energy and Utilities Board ©Her Majesty the Queen in Right of Alberta, 2008 ISBN 978-0-7785-6950-3 The Energy Resources Conservation Board/Alberta Geological Survey (ERCB/AGS) and its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness or reliability of this publication. Any digital data and software supplied with this publication are subject to the licence conditions. The data are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation, and/or any use of proprietary data formats in this release, do not constitute endorsement by the ERCB/AGS of any manufacturer's product. If this product is an ERCB/AGS Special Report, the information is provided as received from the author and has not been edited for conformity to ERCB/AGS standards. When using information from this publication in other publications or presentations, due acknowledgment should be given to the ERCB/AGS. The following reference format is recommended: Bachu, S., Buschkuehle, M., Haug, K., Michael, K. (2008): Subsurface characterization of the Pembina-Wabamun acid-gas injection area; Energy Resources Conservation Board, ERCB/AGS Special Report 093, 60 p. -
3Rd-Order Sequence Stratigraphy and Lithostratigraphy of the Bearpaw–Horseshoe Canyon Transition, Alberta Plains
3rd-order sequence stratigraphy and lithostratigraphy of the Bearpaw–Horseshoe Canyon transition, Alberta plains Ben Hathway, Alberta Geological Survey, Alberta Energy Regulator, Edmonton, Alberta, [email protected] Summary The regional-scale delineation and modelling of upper and lower boundaries and zero edges for the Bearpaw Formation tongues in southern and central Alberta forms an important component of a wider AGS project to construct a digital 3D geological framework for the Alberta subsurface. Core and high-quality wireline logs, generated to a large extent by recent coal-bed methane drilling, permit the establishment of a 3rd-order sequence stratigraphic framework. This provides a context within which lithostratigraphic boundaries of the Bearpaw Formation with laterally equivalent and overlying Horseshoe Canyon and St. Mary River formation strata can be more rigorously mapped. Lower boundaries of the Bearpaw tongues are 3rd-order transgressive, or more proximally, maximum flooding surfaces, and upper boundaries are highly diachronous facies contacts within successive regressive systems tracts. Introduction The complex nature of the intertonguing relationship between Campanian-Maastrichtian (Upper Cretaceous) Bearpaw Formation marine shale and fluviodeltaic nonmarine and shoreline deposits of the Horseshoe Canyon and St. Mary River formations in central and southern Alberta has long been recognized (e.g. Russell, 1932; Irish, 1970). Following earlier work focused on high-resolution, 4th-order sequence analysis of the stratigraphically limited part of the Bearpaw–Horseshoe Canyon transition exposed along the Red Deer River valley (e.g. Rahmani, 1988; Ainsworth, 1994), the first regional sequence stratigraphic study of the succession was undertaken by Catuneanu et al. (1997). In that study increasing and decreasing trends in wireline gamma-ray response were used to delineate up to 11 3rd-order transgressive-regressive (T-R) sequences within the Bearpaw Formation. -
A Subadult Individual of Styracosaurus Albertensis
Vertebrate Anatomy Morphology Palaeontology 8:67–95 67 ISSN 2292-1389 A subadult individual of Styracosaurus albertensis (Ornithischia: Ceratopsidae) with comments on ontogeny and intraspecific variation inStyracosaurus and Centrosaurus Caleb M. Brown1,*, Robert B. Holmes2, Philip J. Currie2 1Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, AB, T0J 0Y0, Canada; [email protected] 2Department of Biological Sciences, University of Alberta, Edmonton, Alberta, T6G 2E9, Canada; [email protected]; [email protected] Abstract: Styracosaurus albertensis is an iconic centrosaurine horned dinosaur from the Campanian of Alberta, Canada, known for its large spike-like parietal processes. Although described over 100 years ago, subsequent dis- coveries were rare until the last few decades, during which time several new skulls, skeletons, and bonebeds were found. Here we described an immature individual, the smallest known for the species, represented by a complete skull and fragmentary skeleton. Although ~80% maximum size, it possesses a suite of characters associated with immaturity, and is regarded as a subadult. The ornamentation is characterized by a small, recurved, but fused nasal horncore; short, rounded postorbital horncores; and short, triangular, and flat parietal processes. Using this specimen, and additional skulls and bonebed material, the cranial ontogeny of Styracosaurus is described, and compared to Centrosaurus. In early ontogeny, the nasal horncores of Styracosaurus and Centrosaurus are thin, recurved, and unfused, but in the former the recurved morphology is retained into large adult size and the horncore never develops the procurved morphology common in Centrosaurus. The postorbital horncores of Styracosaurus are shorter and more rounded than those of Centrosaurus throughout ontogeny, and show great- er resorption later in ontogeny.