1 a Revision of the Hadrosauridae
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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 -
Camptosaurus Dispar Legs; Although, the Smaller Juveniles Might Have Been Able to Do So
Camptosaurus was too front heavy to walk on hind Camptosaurus dispar legs; although, the smaller juveniles might have been able to do so. e skull of Camptosaurus is about 15 inches long. It has no teeth at the front of the beak and broad crushing teeth in the cheeks. ese teeth are made stronger by ridges on the outer surface. Chewing causes these teeth to have a at, grinding surface. Unlike Allosaurus, these teeth cannot slice through esh, but they can pulverize vegetation. Our skeleton of Camptosaurus went on display Scienti c Name: Camptosaurus dispar at the museum around 1965 and was the Muse- Pronounced: KAMP-toe-SOR-us um’s second dinosaur skeleton. Originally, it was Name Meaning: Flexible lizard mounted in the kangaroo pose on its hind legs and Time Period: 147 Million Years Ago (MYA) Late using its tail as a prop. It was remounted into a new Jurassic four-legged pose in 2013 . e skeleton is 17¾ feet Length:16-23 feet (5-7 m) long long and 5 feet tall at the hips. It is a plaster of Paris Height: 3-4 feet (1 m) high at the hips cast of bones collected from the Cleveland Lloyd Weight: 2,200 pounds (1000 kg). Dinosaur Quarry, about 30 miles south of Price. Diet: Herbivore (plant eater) e pelvis is rather broad for its length and the Places Found: Camptosaurus was a distant relative of Iguanodon, upper bone, called the ilium, bows outwards. Discoverer: Marsh (1885) the dinosaur with the thumb-spike. In fact, the thumb (digit I) of Camptosaurus had little move- e hand of Camptosaurus has ve digits, but only ment and the claw was almost like a spike . -
A Phylogenetic Analysis of the Basal Ornithischia (Reptilia, Dinosauria)
A PHYLOGENETIC ANALYSIS OF THE BASAL ORNITHISCHIA (REPTILIA, DINOSAURIA) Marc Richard Spencer A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements of the degree of MASTER OF SCIENCE December 2007 Committee: Margaret M. Yacobucci, Advisor Don C. Steinker Daniel M. Pavuk © 2007 Marc Richard Spencer All Rights Reserved iii ABSTRACT Margaret M. Yacobucci, Advisor The placement of Lesothosaurus diagnosticus and the Heterodontosauridae within the Ornithischia has been problematic. Historically, Lesothosaurus has been regarded as a basal ornithischian dinosaur, the sister taxon to the Genasauria. Recent phylogenetic analyses, however, have placed Lesothosaurus as a more derived ornithischian within the Genasauria. The Fabrosauridae, of which Lesothosaurus was considered a member, has never been phylogenetically corroborated and has been considered a paraphyletic assemblage. Prior to recent phylogenetic analyses, the problematic Heterodontosauridae was placed within the Ornithopoda as the sister taxon to the Euornithopoda. The heterodontosaurids have also been considered as the basal member of the Cerapoda (Ornithopoda + Marginocephalia), the sister taxon to the Marginocephalia, and as the sister taxon to the Genasauria. To reevaluate the placement of these taxa, along with other basal ornithischians and more derived subclades, a phylogenetic analysis of 19 taxonomic units, including two outgroup taxa, was performed. Analysis of 97 characters and their associated character states culled, modified, and/or rescored from published literature based on published descriptions, produced four most parsimonious trees. Consistency and retention indices were calculated and a bootstrap analysis was performed to determine the relative support for the resultant phylogeny. The Ornithischia was recovered with Pisanosaurus as its basalmost member. -
Rule Booklet
Dig for fossils, build skeletons, and attract the most visitors to your museum! TM SCAN FOR VIDEO RULES AND MORE! FOSSILCANYON.COM Dinosaurs of North America edimentary rock formations of western North America are famous for the fossilized remains of dinosaurs The rules are simple enough for young players, but and other animals from the Triassic, Jurassic, and serious players can benefit Cretaceous periods of the Mesozoic Era. Your objective from keeping track of the cards that is to dig up fossils, build complete skeletons, and display have appeared, reasoning about them in your museum to attract as many visitors as possible. probabilities and expected returns, and choosing between aggressive Watch your museum’s popularity grow using jigsaw-puzzle and conservative plays. scoring that turns the competition into a race! GAME CONTENTS TM 200,000300,000 160,000 VISITORS VISITORS PER YEAR 140,000 VISITORS PER YEAR 180,000 VISITORS PER YEAR 400,000 VISITORS PER YEAR Dig for fossils, build skeletons, and 340,000 VISITORS PER YEAR RD COLOR ELETONS CA GENUS PERIODDIET SK FOSSIL VISITORSPARTS 360,000 VISITORS PER YEAR PER YEAR attract the most visitors to your museum! VISITORS PER YEAR PER YEAR Tyrannosaurus K C 1 4 500,000 Brachiosaurus J H 1 3 400,000 ON YOUR TURN: TM SCAN FOR VIDEO Triceratops K H 1 3 380,000 RULES AND MORE! Allosaurus J C 2 Dig3 a first360,000 card. If it is a fossil, keep it hidden. FOSSILCANYON.COM Ankylosaurus K H 2 If it3 is an340,000 action card, perform the action. -
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. -
A Juvenile Cf. Edmontosaurus Annectens (Ornithischia, Hadrosauridae) Femur Documents a Previously Unreported Intermediate Growth Stage for This Taxon Andrew A
Vertebrate Anatomy Morphology Palaeontology 7:59–67 59 ISSN 2292-1389 A juvenile cf. Edmontosaurus annectens (Ornithischia, Hadrosauridae) femur documents a previously unreported intermediate growth stage for this taxon Andrew A. Farke1,2,3,* and Eunice Yip2 1Raymond M. Alf Museum of Paleontology, 1175 West Baseline Road, Claremont, CA, 91711, USA 2The Webb Schools, 1175 West Baseline Road, Claremont, CA, 91711, USA 3Dinosaur Institute, Natural History Museum of Los Angeles County, 900 Exposition Blvd. Los Angeles, CA, 90007, USA; [email protected] Abstract: A nearly complete, but isolated, femur of a small hadrosaurid from the Hell Creek Formation of Montana is tentatively referred to Edmontosaurus annectens. At 28 cm long, the element can be classified as likely that from an ‘early juvenile’ individual, approximately 24% of the maximum known femur length for this species. Specimens from this size range and age class have not been described previously for E. annectens. Notable trends with increasing body size include increasingly distinct separation of the femoral head and greater trochanter, relative increase in the size of the cranial trochanter, a slight reduction in the relative breadth of the fourth trochanter, and a relative increase in the prominence of the cranial intercondylar groove. The gross profile of the femoral shaft is fairly consistent between the smallest and largest individuals. Although an ontogenetic change from relatively symmetrical to an asymmetrical shape in the fourth trochanter has been suggested previously, the new juvenile specimen shows an asymmetric fourth tro- chanter. Thus, there may not be a consistent ontogenetic pattern in trochanteric morphology. An isometric relationship between femoral circumference and femoral length is confirmed for Edmontosaurus. -
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. -
Dinosaur Incubation Periods Directly Determined from Growth-Line Counts in Embryonic Teeth Show Reptilian-Grade Development
Dinosaur incubation periods directly determined from growth-line counts in embryonic teeth show reptilian-grade development Gregory M. Ericksona,1, Darla K. Zelenitskyb, David Ian Kaya, and Mark A. Norellc aDepartment of Biological Science, Florida State University, Tallahassee, FL 32306-4295; bDepartment of Geoscience, University of Calgary, Calgary, AB, Canada T2N 1N4; and cDivision of Paleontology, American Museum of Natural History, New York, NY 10024 Edited by Neil H. Shubin, University of Chicago, Chicago, IL, and approved December 1, 2016 (received for review August 17, 2016) Birds stand out from other egg-laying amniotes by producing anatomical, behavioral and eggshell attributes of birds related to relatively small numbers of large eggs with very short incubation reproduction [e.g., medullary bone (32), brooding (33–36), egg- periods (average 11–85 d). This aspect promotes high survivorship shell with multiple structural layers (37, 38), pigmented eggs (39), by limiting exposure to predation and environmental perturba- asymmetric eggs (19, 40, 41), and monoautochronic egg pro- tion, allows for larger more fit young, and facilitates rapid attain- duction (19, 40)] trace back to their dinosaurian ancestry (42). For ment of adult size. Birds are living dinosaurs; their rapid development such reasons, rapid avian incubation has generally been assumed has been considered to reflect the primitive dinosaurian condition. throughout Dinosauria (43–45). Here, nonavian dinosaurian incubation periods in both small and Incubation period estimates using regressions of typical avian large ornithischian taxa are empirically determined through growth- values relative to egg mass range from 45 to 80 d across the line counts in embryonic teeth. -
Postcranial Anatomy of Tanius Sinensis Wiman, 1929 (Dinosauria; Hadrosauroidea) Postkraniala Anatomin Hos Tanius Sinensis Wiman, 1929 (Dinosauria; Hadrosauroidea)
Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 320 Postcranial Anatomy of Tanius Sinensis Wiman, 1929 (Dinosauria; Hadrosauroidea) Postkraniala anatomin hos Tanius sinensis Wiman, 1929 (Dinosauria; Hadrosauroidea) Niclas H. Borinder INSTITUTIONEN FÖR GEOVETENSKAPER DEPARTMENT OF EARTH SCIENCES Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 320 Postcranial Anatomy of Tanius Sinensis Wiman, 1929 (Dinosauria; Hadrosauroidea) Postkraniala anatomin hos Tanius sinensis Wiman, 1929 (Dinosauria; Hadrosauroidea) Niclas H. Borinder ISSN 1650-6553 Copyright © Niclas H. Borinder and the Department of Earth Sciences, Uppsala University Published at Department of Earth Sciences, Uppsala University (www.geo.uu.se), Uppsala, 2015 Abstract Postcranial Anatomy of Tanius Sinensis Wiman, 1929 (Dinosauria; Hadrosauroidea) Niclas H. Borinder Tanius sinensis Wiman, 1929 was one of the first hadrosauroid or “duck-billed” taxa erected from China, indeed one of the very first non-avian dinosaur taxa to be erected based on material from the country. Since the original description by Wiman in 1929, the anatomy of T. sinensis has received relatively little attention in the literature since then. This is unfortunate given the importance of T. sinensis as a possible non-hadrosaurid hadrosauroid i.e. a member of Hadrosauroidea outside the family of Hadrosauridae, living in the Late Cretaceous, at a time when most non-hadrosaurid hadro- sauroids had become replaced by the members of Hadrosauridae. To gain a better understanding of the anatomy of T. sinensis and its phylogenetic relationships, the postcranial anatomy of it is redescribed. T. sinensis is found to have a mosaic of basal traits like strongly opisthocoelous cervical vertebrae, the proximal end of scapula being dorsoventrally wider than the distal end, the ratio between the proximodistal length of the metatarsal III and the mediolateral width of this element being greater than 4.5. -
Our Museum Dinosaurs
Our Museum Dinosaurs Coelophysis Tyrannosaurus Means: ‘hollow form’ Means: ‘tyrant lizard’ Say it: seel-oh-FIE-sis Say it: tie-ran-oh-SORE-us Where found: USA Where found: USA, Canada Type: Theropod Type: Theropod Length: 3m Length: 12m Height: 2m Height: 3.6m Weight: 27kg Weight: 8,300kg How it moved: walked on two legs, may have run How it moved: swiftly on two legs Teeth: 60 saw-edged, bone-crushing, pointed Teeth: small and sharp teeth in immensely strong jaws Type of feeder: CARNIVORE Type of feeder: CARNIVORE + SCAVENGER Food: small reptiles and insects Food: all other animals When it lived: 225-220 million years ago When it lived: 68-66 million years ago In the museum In the museum Models of Coelophysis Full size replica of its skull REAL fossil footprints Polacanthus Edmontosaurus Means: ‘many prickles’ Means: ‘Edmonton lizard’ Say it: pole-a-CAN-thus Say it: ed-mon-toe-SORE-us Where found: England Where found: North America Type: Ankylosaur Type: Hadrosaur Length: 5m Length: 13m Height: 1m Height: 3.5m Weight: 2 tonnes Weight: 3,400kg How it moved: walked on four legs How it moved: on two or four legs Teeth: small Teeth: horny beak, 200 grinding cheek teeth Type of feeder: HERBIVORE Type of feeder: HERBIVORE Food: plants Food: pine needles, seeds, twigs and leaves When it lived: 130-125 million years ago When it lived: 73-66 million years ago In the museum In the museum Partial skeleton of A REAL Edmontosaurus skeleton Polacanthus (in rock) Fossil Edmontosaurus skin imprint Hypsilophodon Dracoraptor Means: ‘high-crested tooth’ Means: ‘dragon robber’ Say it: hip-sih-LOW-foh-don Say it: DRAY-co-RAP-tor Where found: Isle of Wight, England Where found: Wales Type: Ornithiscian (orn-i-thi-SHE-an) Type: Theropod Length: around 3m Length: 1.8m Height: around 1m Height: 0.8m (80cm) Weight: around 25kg Weight: 20kg How it moved: walked or ran on two legs How it moved: swiftly on two legs Teeth: small pointed serrated teeth Teeth: horny beak, c. -
Integumentary Structure and Composition in an Exceptionally Well-Preserved Hadrosaur (Dinosauria: Ornithischia)
Integumentary structure and composition in an exceptionally well-preserved hadrosaur (Dinosauria: Ornithischia) Mauricio Barbi1,*, Phil R. Bell2,*, Federico Fanti3,4, James J. Dynes5, Anezka Kolaceke1, Josef Buttigieg6, Ian M. Coulson7 and Philip J. Currie8 1 Department of Physics, University of Regina, Regina, Saskatchewan, Canada 2 School of Environmental and Rural Science, University of New England, Armidale, New South Wales, Australia 3 Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Alma Mater Studiorum, Università di Bologna, Bologna, Italy 4 Museo Geologico Giovanni Capellini, Università di Bologna, Bologna, Italy 5 Canadian Light Source Inc., University of Saskatchewan, Saskatoon, Saskatchewan, Canada 6 Department of Biology, University of Regina, Regina, Saskatchewan, Canada 7 Department of Geology, University of Regina, Regina, Saskatchewan, Canada 8 Biological Sciences, University of Alberta, Edmonton, Alberta, Canada * These authors contributed equally to this work. ABSTRACT Preserved labile tissues (e.g., skin, muscle) in the fossil record of terrestrial vertebrates are increasingly becoming recognized as an important source of biological and tapho- nomic information. Here, we combine a variety of synchrotron radiation techniques with scanning electron and optical microscopy to elucidate the structure of 72 million- year-old squamous (scaly) skin from a hadrosaurid dinosaur from the Late Cretaceous of Alberta, Canada. Scanning electron and optical microscopy independently reveal that the three-dimensionally preserved scales are associated with a band of carbon-rich layers up to a total thickness of ∼75 microns, which is topographically and morphologically congruent with the stratum corneum in modern reptiles. Compositionally, this band deviates from that of the surrounding sedimentary matrix; Fourier-transform infrared spectroscopy and soft X-ray spectromicroscopy analyses indicate that carbon appears Submitted 27 April 2019 predominantly as carbonyl in the skin. -
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.