Dino Data Challenge!

Total Page：16

File Type：pdf, Size：1020Kb

KS2U Mathematics 102222 Statistics/Handling Data Dinosaur Data! Student Introduction Dino Data Challenge! During the course of your visit, find out something Can you use your maths skills to about each of these dinosaurs: find the most popular dinosaur? ü Iguanodon ü Neovenator salerii Which one do you like? In this activity we will determine which are the ü Eotyrannus lengi It might be down to favourite dinosaurs at Dinosaur Isle museum ü Hypsiliphodon features, speed, size, power, using maths skills! ü Valdosaurus looks, or even name! Tally up the frequencies, pictogram the ü Sauropodomorpha answers and figure out who’s best! ü Polacanthus ü Baryonyx Charting your favourite dinosaurs! Task 1 - Tally ü As each student in your group or class tells the teacher which dinosaur they’d like to vote for, you need to mark their answer next to the corresponding dinosaur name on the tally table below. Don’t forget to add your own vote! Isle of Wight Dinosaur Tally - BOYS Tally - GIRLS TOTAL Iguanodon Neovenator salerii Eotyrannus lengi Hypsilophodon Valdosaurus Sauropodomorpha Polacanthus Baryonyx Page 1 of 3 Task 2 - Pictogram Every vote on the tally chart now needs to be converted to the pictogram below. For every 3 votes for one particular dinosaur draw ONE on the pictogram, in the correct column: Iguanodon Neovenator Eotyrannus Hypsilipho- Valdosaurus Sauropodo- Polacanthus Baryonyx don morpha 102222 Page 2 of 3 Questions 1a. Which dinosaur was the most popular with the BOYS in the group? b. Why do you think this is? 2a. Which dinosaur was the most popular with the GIRLS in the group? b. Why do you think this is? 3. Which dinosaur was the most popular OVERALL? 4. Which was the least popular dinosaur OVERALL? ©2014 Education Destination www.educationdestination.co.uk 102222 Images © Dinosaur Isle.

Copy Link

Recommended publications

Sereno 20060098.Vp
Basal abelisaurid and carcharodontosaurid theropods from the Lower Cretaceous Elrhaz Formation of Niger PAUL C. SERENO and STEPHEN L. BRUSATTE Sereno, P.C. and Brusatte, S.L. 2008. Basal abelisaurid and carcharodontosaurid theropods from the Lower Cretaceous Elrhaz Formation of Niger. Acta Palaeontologica Polonica 53 (1): 15–46. We report the discovery of basal abelisaurid and carcharodontosaurid theropods from the mid Cretaceous (Aptian– Albian, ca. 112 Ma) Elrhaz Formation of the Niger Republic. The abelisaurid, Kryptops palaios gen. et sp. nov., is repre− sented by a single individual preserving the maxilla, pelvic girdle, vertebrae and ribs. Several features, including a maxilla textured externally by impressed vascular grooves and a narrow antorbital fossa, clearly place Kryptops palaios within Abelisauridae as its oldest known member. The carcharodontosaurid, Eocarcharia dinops gen. et sp. nov., is repre− sented by several cranial bones and isolated teeth. Phylogenetic analysis places it as a basal carcharodontosaurid, similar to Acrocanthosaurus and less derived than Carcharodontosaurus and Giganotosaurus. The discovery of these taxa sug− gests that large body size and many of the derived cranial features of abelisaurids and carcharodontosaurids had already evolved by the mid Cretaceous. The presence of a close relative of the North American genus Acrocanthosaurus on Af− rica suggests that carcharodontosaurids had already achieved a trans−Tethyan distribution by the mid Cretaceous. Key words: Theropod, abelisaurid, allosauroid, carcharodontosaurid, Kryptops, Eocarcharia, Cretaceous, Africa. Paul C. Sereno [[email protected]], Department of Organismal Biology and Anatomy, University of Chicago, 1027 E. 57th Street, Chicago, Illinois, 60637, USA; Stephen L. Brusatte [[email protected]], Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, United Kingdom.
[Show full text]
From the Early Cretaceous Wonthaggi Formation (Strzelecki Group)
Journal of Paleontology, 93(3), 2019, p. 543–584 Copyright © 2019, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/19/1937-2337 doi: 10.1017/jpa.2018.95 New small-bodied ornithopods (Dinosauria, Neornithischia) from the Early Cretaceous Wonthaggi Formation (Strzelecki Group) of the Australian-Antarctic rift system, with revision of Qantassaurus intrepidus Rich and Vickers-Rich, 1999 Matthew C. Herne,1,2 Jay P. Nair,2 Alistair R. Evans,3 and Alan M. Tait4 1School of Environmental and Rural Science, University of New England, Armidale 2351, New South Wales, Australia <ornithomatt@ gmail.com> 2School of Biological Sciences, The University of Queensland, Brisbane, Queensland 4072, Australia <[email protected]> 3School of Biological Sciences, Monash University, Melbourne, Victoria 3800, Australia <[email protected]> 4School of Earth, Atmosphere & Environment, Monash University, Melbourne, Victoria 3800, Australia <[email protected]> Abstract.—The Flat Rocks locality in the Wonthaggi Formation (Strzelecki Group) of the Gippsland Basin, southeastern Australia, hosts fossils of a late Barremian vertebrate fauna that inhabited the ancient rift between Australia and Antarc- tica. Known from its dentary, Qantassaurus intrepidus Rich and Vickers-Rich, 1999 has been the only dinosaur named from this locality. However, the plethora of vertebrate fossils collected from Flat Rocks suggests that further dinosaurs await discovery. From this locality, we name a new small-bodied ornithopod, Galleonosaurus dorisae n.
[Show full text]
A Short History of Dinosaurian Osteocytes
Palaeont. afr., 34, 59-61 ( 1997) A SHORT HISTORY OF DINOSAURIAN OSTEOCYTES. by _ R.E.H. (Robin) Reid School of Geosciences, The Queen's University ofB elfast, Belfast BT7 INN, Northern Ireland. ABSRACT A recent supposed discovery of dinosauri an osteocytes by Fukuda and Obata ( 1993) ignored earli er records from more than 20 d inosaurs, dating back 150 years. Some of the bodies they identified as osteocytes are also more like ly to represent chondrocytes. KEYWORDS: Bone histology, osteocytes. INTRODUCTION Brontosaurus (pp. 302, 303), Diplodocus (pp. 304, In a recent paper, Fukuda and Obata (1993) claimed 306), Camarasaurus (p. 311, as "M orosaurus" pp. 322, the discovery of dinosaurian osteocytes, in the form of 324), Haplocanthosaurus (pp.313, 314), Allosaurus mineral casts of their lacunae and canaliculi seen in (pp. 315, 3 16), Stegosaurus (p. 321) Iguanodon (pp. hadrosaurid bones, and stated that, despite recent 326-328), Dryptosaurus (p. 344), Triceratops (p. 346), histological studies, " ... there is no information on and Anatosaurus (pp. 348-350), as "Trachodon". osteocytes in dinosaur bone ti ssues" (p. 99, para. 1). At Osteocyte Stegosaurus lacunae recorded as from that date, however, earlier studies outlined here Zanclodon (p. 262), which is now considered contained records from more than 20 dinosaurs, dating indeterminate, are probably from a prosauropod (c.f. back 150 years (Quelett 1849), and even electron Benton 1986, pp. 295-297). A preserved canalicular microscope photographs had been in print since 1966 network was noted in Brontosaurus (p. 302), though (Pawlicki, Korbel & Kubiak 1966). This note reviews a not illustrated, and lacunae affected by fungal range of relevant references, for readers not familiar enlargement, mineral infilling, loss of canaliculae or with them, and also shows that some bodies identified complete obliteration were reported from various as osteocytes by Fukuda and Obata in the articular genera.
[Show full text]
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.
[Show full text]
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.
[Show full text]
Un Nuevo Dinosaurio Estiracosterno (Ornithopoda: Ankylopollexia) Del Cretácico Inferior De España
SPANISH JOURNAL OF PALAEONTOLOGY Un nuevo dinosaurio estiracosterno (Ornithopoda: Ankylopollexia) del Cretácico Inferior de España Carolina FUENTES VIDARTE*, Manuel MEIJIDE CALVO, Federico MEIJIDE FUENTES & Manuel MEIJIDE FUENTES * C/ Almazán 17, 42004, Soria, España; [email protected] Fuentes Vidarte, C., Meijide Calvo, M., Meijide Fuentes, F. & Meijide Fuentes, M. 2016. Un nuevo dinosaurio estiracosterno (Ornithopoda: Ankylopollexia) del Cretácico Inferior de España. [A new estiracostern dinosaur (Ornithopoda: Ankylopollexia) from the Lower Cretaceous of Spain]. Spanish Journal of Palaeontology, 31 (2), 407-446. Manuscript received 12 May 2015 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 06 August 2016 RESUMEN ABSTRACT El yacimiento Zorralbo I, situado en el municipio de The Zorralbo I site from the Lower Cretaceous (upper Golmayo (Soria, España) perteneciente al Cretácico Inferior Hauterivian/lower Barremian of the Golmayo Formation), (Hauteriviense superior/Barremiense inferior), Formación located in Golmayo municipality (Soria, Spain), has yielded Golmayo (Cordillera Ibérica), ha proporcionado diverso material diverse material belonging to four types of dinosaurs: de cuatro tipos de dinosaurios: ornitópodos, anquilosaurios ornithopods, ankylosaurids (Polacanthus sp.), sauropods (Polacanthus sp.), saurópodos (Titanosauriforme) y terópodos (Titanosauriform) and theropods (Allosauroidea and (Allosauroidea y Dromaeosauridae), de una tortuga sin Dromaeosauridae), crocodiles (Goniopholis sp.) and an determinar
[Show full text]
Dino Data Challenge!
KS2L Mathematics 102221 Statistics/Handling Data Dinosaur Data! Student Introduction Dino Data Challenge! During the course of your visit, find out something Can you use your maths skills to about each of these dinosaurs: find the most popular dinosaur? ü Iguanodon ü Neovenator salerii Which one do you like? In this activity we will determine which are the ü Eotyrannus lengi It might be down to favourite dinosaurs at Dinosaur Isle museum ü Hypsiliphodon features, speed, size, power, using maths skills! ü Valdosaurus looks, or even name! Tally up the responses, pictogram the ü Sauropodomorpha frequencies and figure out who’s best! ü Polacanthus ü Baryonyx Charting your favourite dinosaurs! Task 1 - Tally ü As each student in your group or class tells the teacher which dinosaur they’d like to vote for, you need to mark their answer next to the corresponding dinosaur name on the tally table below. Don’t forget to add your own vote! Isle of Wight Dinosaur TALLY TOTAL Iguanodon Neovenator salerii Eotyrannus lengi Hypsilophodon Valdosaurus Sauropodomorpha Polacanthus Baryonyx Page 1 of 4 Task 2 - Pictogram The frequency of each vote on the tally chart now needs to be shown on the pictogram below. Draw one dinosaur in the correct column for each vote received. Iguanodon Neovenator Eotyrannus Hypsilipho- Valdosaurus Sauropodo- Polacanthus Baryonyx don morpha 102221 Page 2 of 4 OPTIONAL: Cut out and stick dinosaurs! Iguanodon Neovenator Eotyrannus Hypsiliphodon 102221 OPTIONAL: Cut out and stick dinosaurs! Valdosaurus Sauropodomorpha Polacanthus Baryonyx ©2014 Education Destination www.educationdestination.co.uk 102221 Images © Dinosaur Isle.
[Show full text]
Geotourism and Geoconservation on the Isle of Wight, UK: Balancing Science with Commerce
Carpenter: Rocky start of Dinosaur National Monument… Geoconservation Research Original Article Geotourism and Geoconservation on the Isle of Wight, UK: Balancing Science with Commerce Martin I. Simpson Lansdowne, Military Rd, Chale, Isle of Wight, PO38 2HH, UK. Abstract The Isle of Wight has a rich and varied geological heritage which attracts scientists, tourists and fossil collectors, both private and commercial. Each party has a role to play in geoconservation and geotourism, but a policy on the long term curation of scientifically important specimens is essential to prevent future conflicts. A new code of conduct is recommended, based on the one adopted on the Jurassic Coast of Dorset. I have spent over 40 years living on the Island and working in the tourist industry running geology field-trips for both academics and tourists, and managing one of the longest running geological gift shops. I see the geological heritage and fossil sites as valuable geotourism assets, and envisage no problems with respect to the scientifically important material provided that a clear collecting policy is adopted, and the local museum generates funding to ensure that significant finds remain on the Island. A positive attitude is recommended in view of past experiences. Corresponding Author: Martin I. Simpson Lansdowne, Military Rd, Chale, Isle of Wight, PO38 2HH, UK. Email: [email protected] Keywords: Palaeontology, Geology, Isle of Wight, Tourism. Introduction with few formations absent, probably one of the best successions of this type in Europe (Fig 1c).Once a larger landmass joined to the mainland The Isle of Wight is a small, vaguely lozenge-shaped island situated as recently as 9000 years ago, what remains as 'Wight Island' or 'Vecta just off the central south coast of England, about 113 km south west of Insula' is eroding away at a rate of one metre per year in places (Munt London (Fig 1a, 1b), renowned for its balmy climate and golden, sandy 2016), but this erosion has produced spectacular scenery and iconic beaches.
[Show full text]
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.
[Show full text]
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.
[Show full text]
Osteology of a Near-Complete Skeleton of Tenontosaurus Tilletti (Dinosauria: Ornithopoda) from the Cloverly Formation, Montana, USA
Osteology of a Near-Complete Skeleton of Tenontosaurus tilletti (Dinosauria: Ornithopoda) from the Cloverly Formation, Montana, USA A report submitted in partial fulfilment of the requirements for the degree of MEarthSci Geology (Hons.), University of Manchester Jonathan Tennant 70406912 MEarthSci Geology (Hons.) School of Earth, Atmospheric and Environmental Sciences University of Manchester Williamson Building Oxford Road Manchester M13 9PL Osteology of Tenontosaurus tilletti Contents Figures and Tables..............................................................................................................................................3 1.0 Abstract .............................................................................................................................................................6 2.0 Introduction ......................................................................................................................................................7 2.1 Aims and Objectives....................................................................................................................................7 2.2 Institutional Abbreviations ........................................................................................................................9 3.0 Previous Work ............................................................................................................................................... 11 3.1 The Cloverly Formation ..........................................................................................................................
[Show full text]
Answer Sheet
Answer sheet 1. Origin: Over half a billion years ago, during the Cambrian, when Europe and Britain were covered by the sea. Habitat: the sea floor, water at 20°C Features: simple multicellular animal, soft-bodied, spicules support the body Feeding, respiratory & excretory systems: water containing oxygen and food particles enters the inner cavity through holes in the body& passes over tiny whip-like structures which absorb the oxygen and nutrients from the water & give off waste which is carried out by the water. 2. a. They had thick shells. b. Shark. 3. a. Any two: clams, sea urchins, starfish, sponges. b. They had developed mechanisms to avoid sinking. Many sea urchins had club-like spines to spread their weight, some starfish were broad and flat, and clams had spines that lifted the shell off the sea floor and large shells which spread the weight. 4. a. They lived in the Mesozoic Era during the periods called the Triassic, Jurassic and Cretaceous. b. (Reverend Richard) Owen, in 1842. c. Dinosaurs had legs which stood straight below their bodies. d. We don’t really know! e. Ornithischians – Iguanodon, Hypsilophodon, Valdosaurus, Pachycephalosaurus. 5. a. Because, when they were still alive there was a great diversity of species of dinosaurs, the climate was hot; there was plenty to eat and drink – and a variety of local environments to live in, from rivers, sandy dunes, low hills and mud ponds. b. Hypsilophodon, Eucamerotus, Iguanodon, Polacanthus, Neovenator, Yaverlandia and Valdosaurus. c. The Isle of Wight was formed in a sinking sedimentary basin. As dinosaurs died their remains were progressively covered by layers of mud and sand.
[Show full text]