2016 Year in Review
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Zootaxa,Montealtosuchus Arrudacamposi, a New Peirosaurid
Zootaxa 1607: 35–46 (2007) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2007 · Magnolia Press ISSN 1175-5334 (online edition) Montealtosuchus arrudacamposi, a new peirosaurid crocodile (Mesoeucrocodylia) from the Late Cretaceous Adamantina Formation of Brazil ISMAR DE SOUZA CARVALHO1, FELIPE MESQUITA DE VASCONCELLOS1 & SANDRA APARE- CIDA SIMIONATO TAVARES2 1Universidade Federal do Rio de Janeiro. Departamento de Geologia, CCMN/IGEO. 21.949-900 Cidade Universitária - Ilha do Fundão. Rio de Janeiro - RJ. Brasil. E-mail: [email protected]; [email protected] 2Museu de Paleontologia de Monte Alto. Praça do Centenário, Centro de Artes s/no. 15.910-000, MonteAlto-Brazil. E-mail: [email protected] Abstract We describe a new species of Peirosauridae (Crocodyliformes, Mesoeucrocodylia), Montealtosuchus arrudacamposi gen. nov. et sp. nov., from the Late Cretaceous (Turonian-Santonian) strata of the Bauru Basin, Brazil. Montealtosuchus was found at the outskirts of Monte Alto County in reddish sandstones of the Adamantina Formation. This specimen is exquisitely preserved with skull, mandible, postcranial and exoskeletal elements in articulation that provides critical information of the anatomy of this group. The occurrence of Peirosauridae in the Adamantina Formation (Turonian-San- tonian) widens the chronostratigraphic range of this Mesoeucrocodylia taxon in Brazil. Recent analysis suggests that the Peirosauridae is restricted to the Late Cretaceous deposits of South America. Key words: Montealtosuchus arrudacamposi gen. nov. et sp. nov.; Peirosauridae; Upper Cretaceous; Adamantina For- mation; Bauru Basin Introduction The Bauru Basin comprises an area between latitudes 18o S and 24o S, and longitudes 47o W and 56o W, and covers an area over 370.000 km2 in the southeast interior of Brazil, with outcrops in São Paulo, Minas Gerais, Mato Grosso do Sul and Goiás states. -
GEOLOGIC MAP of the GREATER DENVER AREA, FRONT RANGE URBAN CORRIDOR, COLORADO by Donald E
U.S DEPARTMENT OF THE INTERIOR MISCELLANEOUS INVESTIGATIONS SERIES I–856–H U.S. GEOLOGICAL SURVEY Version 1.1 105°22'30" 105°15' 105°7'30" 105°0' 104°52'30" 104°45' 104°37'30" 40¡0’ 40°0' Qs Qv Ql Qes DESCRIPTION OF MAP UNITS Qco Qp Qlo Kp Qp Kp Kl Kl Qb TKda Ysp Qes Kf Qb Qp Qco Qv Xbc Kp Qb Qes Qp POST-PINEY CREEK AND PINEY CREEK ALLUVIUM (UPPER HOLOCENE) Kl Qes Qes Qco Qlo Qs Qlo Kp Kl Qb Qrf Qls Kf Ql Ysp TKd Qs Qco COLLUVIUM (UPPER HOLOCENE) Xbc Qp Qv Ysp Qp Qb Kl Qv Qes PPf Qp Qco Qco Qrf Kp Qs Qls Qs LANDSLIDE DEPOSITS (HOLOCENE TO MIDDLE? PLEISTOCENE) Qs Qv Kl Qb Qp JPml Kl Qrf Qco Qs Qco Qv Qp Qes WINDBLOWN SAND (LOWER HOLOCENE TO UPPER PLEISTOCENE) Qv Ql TKd Ql Qes Kd Qv Kp Kl Qes Qco River Qco Qp Kf Ql TKda YXp TKda Kl TKda TKd Qs Xbc Qrf Qv Qp Qb Qb BROADWAY ALLUVIUM (UPPER PLEISTOCENE) Qp Qco Qs Qco Qlo Qco Ql Qp Qes Kf Ql Qco Qp Qv Qs Qrf Ql LOESS (UPPER PLEISTOCENE) Qrf Qs Qlo Kf Qs Qco Qco Qp Qes Qp Qco Qp TKd Qb Qco Qlo Qes LOUVIERS ALLUVIUM (UPPER PLEISTOCENE) Xbc Kf Kp Ql Qs Qrf Marshall Qv Qb Ql Kl TKda Qes Qs Kl Lake Qv Qs SLOCUM ALLUVIUM (PLEISTOCENE) Qv Ql Qco JPml Ql Qco PPf Qv Qs Kl Qs Qco Qv Qco Kn Qv Qs Qs Kp Qrf Qb Qb Barr Lake Kcgg Qv VERDOS ALLUVIUM (PLEISTOCENE) Qs Qrf Qco Ql TKda Qlo Qp Qs TKda Qp Ql TKda Xqm Qlo Qrf Qs Qs Qs ROCKY FLATS ALLUVIUM (PLEISTOCENE) Qp Xq Kd Kf Qco Qp Qco Qb Kl Kp Qco Platte Qlo Qb Qrf Qs Qn Qls Qco NUSSBAUM ALLUVIUM (PLEISTOCENE) Kp Qco Qp Xbc TKd Qrf Qrf Qv Qco Tg Qv Qv HIGH-LEVEL GRAVEL DEPOSITS (PLIOCENE TO OLIGOCENE) Xbc Qp PPf Qb TKd Qb Qv TKda JPml Qv Ql Tcr CASTLE ROCK -
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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Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences COLUMBIA UNIVERSITY 2016 © 2015 Kaori Tsukui All rights reserved ABSTRACT Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui The age of the Bridgerian/Uintan boundary has been regarded as one of the most important outstanding problems in North American Land Mammal “Age” (NALMA) biochronology. The Bridger Basin in southwestern Wyoming preserves one of the best stratigraphic records of the faunal boundary as well as the preceding Bridgerian NALMA. In this dissertation, I first developed a chronological framework for the Eocene Bridger Formation including the age of the boundary, based on a combination of magnetostratigraphy and U-Pb ID-TIMS geochronology. Within the temporal framework, I attempted at making a regional correlation of the boundary-bearing strata within the western U.S., and also assessed the body size evolution of three representative taxa from the Bridger Basin within the context of Early Eocene Climatic Optimum. Integrating radioisotopic, magnetostratigraphic and astronomical data from the early to middle Eocene, I reviewed various calibration models for the Geological Time Scale and intercalibration of 40Ar/39Ar data among laboratories and against U-Pb data, toward the community goal of achieving a high precision and well integrated Geological Time Scale. In Chapter 2, I present a magnetostratigraphy and U-Pb zircon geochronology of the Bridger Formation from the Bridger Basin in southwestern Wyoming. -
CRETACEOUS-TERTIARY BOUNDARY Ijst the ROCKY MOUNTAIN REGION1
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA V o l..¿5, pp. 325-340 September 15, 1914 PROCEEDINGS OF THE PALEONTOLOGICAL SOCIETY CRETACEOUS-TERTIARY BOUNDARY IjST THE ROCKY MOUNTAIN REGION1 BY P. H . KNOWLTON (Presented before the Paleontological Society December 31, 1913) CONTENTS Page Introduction........................................................................................................... 325 Stratigraphic evidence........................................................................................ 325 Paleobotanical evidence...................................................................................... 331 Diastrophic evidence........................................................................................... 334 The European time scale.................................................................................. 335 Vertebrate evidence............................................................................................ 337 Invertebrate evidence.......................................................................................... 339 Conclusions............................................................................................................ 340 I ntroduction The thesis of this paper is as follows: It is proposed to show that the dinosaur-bearing beds known as “Ceratops beds,” “Lance Creek bieds,” Lance formation, “Hell Creek beds,” “Somber beds,” “Lower Fort Union,”- Laramie of many writers, “Upper Laramie,” Arapahoe, Denver, Dawson, and their equivalents, are above a major -
Unit-V Evolution of Horse
UNIT-V EVOLUTION OF HORSE Horses (Equus) are odd-toed hooped mammals belong- ing to the order Perissodactyla. Horse evolution is a straight line evolution and is a suitable example for orthogenesis. It started from Eocene period. The entire evolutionary sequence of horse history is recorded in North America. " Place of Origin The place of origin of horse is North America. From here, horses migrated to Europe and Asia. By the end of Pleis- tocene period, horses became extinct in the motherland (N. America). The horses now living in N. America are the de- scendants of migrants from other continents. Time of Origin The horse evolution started some 58 million years ago, m the beginning of Eocene period of Coenozoic era. The modem horse Equus originated in Pleistocene period about 2 million years ago. Evolutionary Trends The fossils of horses that lived in different periods, show that the body parts exhibited progressive changes towards a particular direction. These directional changes are called evo- lutionary trends. The evolutionary trends of horse evolution are summarized below: 1. Increase in size. 2. Increase in the length of limbs. 3. Increase in the length of the neck. 4. Increase in the length of preorbital region (face). 5. Increase in the length and size of III digit. 6. Increase in the size and complexity of brain. 7. Molarization of premolars. Olfactory bulb Hyracotherium Mesohippus Equus Fig.: Evolution of brain in horse. 8. Development of high crowns in premolars and molars. 9. Change of plantigrade gait to unguligrade gait. 10. Formation of diastema. 11. Disappearance of lateral digits. -
A Large Hadrosaurid Dinosaur from Presa San Antonio, Cerro Del Pueblo Formation, Coahuila, Mexico
A large hadrosaurid dinosaur from Presa San Antonio, Cerro del Pueblo Formation, Coahuila, Mexico ROGELIO ANTONIO REYNA-HERNÁNDEZ, HÉCTOR E. RIVERA-SYLVA, LUIS E. SILVA-MARTÍNEZ, and JOSÉ RUBÉN GUZMAN-GUTIÉRREZ Reyna-Hernández, R.A., Rivera-Sylva, H.E., Silva-Martínez, L.E., and Guzman-Gutiérrez, J.R. 2021. A large hadro- saurid dinosaur from Presa San Antonio, Cerro del Pueblo Formation, Coahuila, Mexico. Acta Palae onto logica Polonica 66 (Supplement to x): xxx–xxx. New hadrosaurid postcranial material is reported, collected near Presa San Antonio, Parras de la Fuente municipality, Coahuila, Mexico, in a sedimentary sequence belonging to the upper Campanian of the Cerro del Pueblo Formation, in the Parras Basin. The skeletal remains include partial elements from the pelvic girdle (left ilium, right pubis, ischium, and incomplete sacrum), a distal end of a left femur, almost complete right and left tibiae, right metatarsals II and IV, cervical and caudal vertebrae. Also, partially complete forelimb elements are present, which are still under preparation. The pubis shows characters of the Lambeosaurinae morphotypes, but the lack of cranial elements does not allow us to directly differentiate this specimen from the already described hadrosaurid taxa from the studied area, such as Velafrons coahuilensis, Latirhinus uitstlani, and Kritosaurus navajovius. This specimen, referred as Lambeosaurinae indet., adds to the fossil record of the hadrosaurids in southern Laramidia during the Campanian. Key words: Dinosauria, Hadrosauridae, Lambeosaurinae, Cretaceous, Campanian, Mexico. Rogelio Antonio Reyna-Hernández [[email protected]], Luis E. Silva-Martínez [[email protected]], Laboratorio de Paleobiología, Facultad de Ciencias Biológicas, Universidad Autónoma de Nuevo León, Av. -
38-Simpson Et Al (Wahweap Fm).P65
Sullivan et al., eds., 2011, Fossil Record 3. New Mexico Museum of Natural History and Science, Bulletin 53. 380 UPPER CRETACEOUS DINOSAUR TRACKS FROM THE UPPER AND CAPPING SANDSTONE MEMBERS OF THE WAHWEAP FORMATION, GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT, UTAH, U.S.A. EDWARD L. SIMPSON1, H. FITZGERALD MALENDA1, MATTATHIAS NEEDLE1, HANNAH L. HILBERT-WOLF2, ALEX STEULLET3, KEN BOLING3, MICHAEL C. WIZEVICH3 AND SARAH E. TINDALL1 1 Department of Physical Sciences, Kutztown University, Kutztown, PA 19530; 2 Department of Geology, Carleton College, Northfield, MN, 55057; 3 Central Connecticut State University, Department of Physics and Earth Sciences, New Britain, Connecticut 06050, USA Abstract—Tridactyl tracks were identified in the fluvial strata of the Upper Cretaceous Wahweap Formation in Grand Staircase-Escalante National Monument, southern Utah, U.S.A. An isolated track and a trackway are located within the upper member at the Cockscomb, and an isolated track is in the capping sandstone member at Wesses Canyon. The upper member tracks are tridactyl pes imprints consisting of a longer, blunt digit III and shorter, blunt digits II-IV. This trace corresponds well to an ornithropod dinosaur as the trackmaker. The capping sandstone member track is a tridactyl pes with an elongate digit III and shorter digits II-IV. Claw impressions are present on the terminus of digits II and III. This trace is consistent with the pes impression of a one meter tall theropod. The tracks further highlight the diversity of dinosaurs in the capping sandstone of the Wahweap Formation. INTRODUCTION During the Late Cretaceous, North America, in particular the west- ern United States, was the site of a radiation of new dinosaurian genera. -
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 -
Taxonomic Reappraisal of the Sphagesaurid Crocodyliform Sphagesaurus Montealtensis from the Late Cretaceous Adamantina Formation of São Paulo State, Brazil
TERMS OF USE This pdf is provided by Magnolia Press for private/research use. Commercial sale or deposition in a public library or website is prohibited. Zootaxa 3686 (2): 183–200 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2013 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3686.2.4 http://zoobank.org/urn:lsid:zoobank.org:pub:9F87DAC0-E2BE-4282-A4F7-86258B0C8668 Taxonomic reappraisal of the sphagesaurid crocodyliform Sphagesaurus montealtensis from the Late Cretaceous Adamantina Formation of São Paulo State, Brazil FABIANO VIDOI IORI¹,², THIAGO DA SILVA MARINHO3, ISMAR DE SOUZA CARVALHO¹ & ANTONIO CELSO DE ARRUDA CAMPOS² 1UFRJ, Departamento de Geologia, CCMN/IGEO, Cidade Universitária – Ilha do Fundão, 21949-900. Rio de Janeiro, Brazil. E-mail: [email protected]; [email protected] 2Museu de Paleontologia “Prof. Antonio Celso de Arruda Campos”, Praça do Centenário s/n, Centro, 15910-000 – Monte Alto, Brazil 3Instituto de Ciências Exatas, Naturais e Educação (ICENE), Universidade Federal do Triângulo Mineiro (UFTM), Av. Dr. Randolfo Borges Jr. 1700 , Univerdecidade, 38064-200, Uberaba, Minas Gerais, Brasil. [email protected] Abstract Sphagesaurus montealtensis is a sphagesaurid whose original description was based on a comparison with Sphagesaurus huenei, the only species of the clade described to that date. Better preparation of the holotype and the discovery of a new specimen have allowed the review of some characteristics and the identification -
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.