Discovering the Ancient History of the American West
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Memorial Tablets*
Memorial Tablets* Gregori Aminoff 1883-1947 Born 8 Feb. 1883 in Stockholm; died 11 Feb. 1947 in Stockholm. 1905 First academic degree, U. of Uppsala, after studying science in Stockholm. 1905 to about 19 13 studied painting in Florence and Italy. 1913 Returned to science. 1918 Ph.D. ; appointed Lecturer in Mineralogy and Crystallo- graphy U. of Stockholm. Thesis: Calcite and Barytes from Mzgsbanshiitten (Sweden). 1923-47 Professor and Head of the Department of Mineralogy of the Museum of Natural History in Stockholm. 1930 Married Birgit Broome, herself a crystallographer. see Nature (London) 1947, 159, 597 (G. Hagg). Dirk Coster 1889-1950 Born 5 Oct. 1889 in Amsterdam; died 12 Feb. 1950 in Groningen. Studied in Leiden, Delft, Lund (with Siegbahn) and Copenhagen (with Bohr). 1922 Dr.-ing. Tech. University of Delft. Thesis: X-ray Spectra and the Atomic Theory of Bohr. 1923 Assistant of H. A. Lorentz, Teyler Stichting in Haarlem. 1924-50 Prof. of Physics and Meteorology, U. of Groningen. Bergen Davis 1869-1951 Born 31 March 1869 in White House, New Jersey; died 1951 in New York. 1896 B.Sc. Rutgers University. 1900 A.M. Columbia University (New York). 1901 Ph.D. Columbia University. 1901-02 Postgraduate work in GMtingen. 1902-03 Postgraduate work in Cambridge. * The author (P.P.E.) is particularly aware of the incompleteness of this section and would be gratefid for being sent additional data. MEMORIAL TABLETS 369 1903 Instructor 1 1910 Assistant Professor Columbia University, New York. 1914 Associate Professor I 1918 Professor of Physics ] Work on ionization, radiation, electron impact, physics of X-rays, X-ray spectroscopy with first two-crystal spectrometer. -
1.1 První Chobotnatci 5 1.2 Plesielephantiformes 5 1.3 Elephantiformes 6 1.3.1 Mammutida 6 1.3.2 Elephantida 7 1.3.3 Elephantoidea 7 2
MASARYKOVA UNIVERZITA PŘÍRODOVĚDECKÁ FAKULTA ÚSTAV GEOLOGICKÝCH VĚD Jakub Březina Rešerše k bakalářské práci Využití mikrostruktur klů neogenních chobotnatců na příkladu rodu Zygolophodon Vedoucí práce: doc. Mgr. Martin Ivanov, Dr. Brno 2012 OBSAH 1. Současný pohled na evoluci chobotnatců 3 1.1 První chobotnatci 5 1.2 Plesielephantiformes 5 1.3 Elephantiformes 6 1.3.1 Mammutida 6 1.3.2 Elephantida 7 1.3.3 Elephantoidea 7 2. Kly chobotnatců a jejich mikrostruktura 9 2.1 Přírůstky v klech chobotnatců 11 2.1.1 Využití přírůstků v klech chobotnatců 11 2.2 Schregerův vzor 12 2.2.1 Stavba Schregerova vzoru 12 2.2.2 Využití Schregerova vzoru 12 2.3 Dentinové kanálky 15 3 Sedimenty s nálezy savců v okolí Mikulova 16 3.1 Baden 17 3.2 Pannon a Pont 18 1. Současný pohled na evoluci chobotnatců Současná systematika chobotnatců není kompletně odvozena od jejich fylogeneze, rekonstruované pomocí kladistických metod. Diskutované skupiny tak mnohdy nepředstavují monofyletické skupiny. Přestože jsou taxonomické kategorie matoucí (např. Laurin 2005), jsem do jisté míry nucen je používat. Některým skupinám úrovně stále přiřazeny nebyly a zde této skutečnosti není přisuzován žádný význam. V této rešerši jsem se zaměřil hlavně na poznatky, které následovaly po vydání knihy; The Proboscidea: Evolution and Paleoecology of Elephants and Their Relatives, od Shoshaniho a Tassyho (1996). Chobotnatci jsou součástí skupiny Tethytheria společně s anthracobunidy, sirénami a desmostylidy (Shoshani 1998; Shoshani & Tassy 1996; 2005; Gheerbrant & Tassy 2009). Základní klasifikace sestává ze dvou skupin. Ze skupiny Plesielephantiformes, do které patří čeledě Numidotheriidae, Barytheriidae a Deinotheridae a ze skupiny Elephantiformes, do které patří čeledě Palaeomastodontidae, Phiomiidae, Mammutida, Gomphotheriidae, tetralofodontní gomfotéria, Stegodontidae a Elephantidae (Shoshani & Marchant 2001; Shoshani & Tassy 2005; Gheerbrant & Tassy 2009). -
South Dakota to Nebraska
Geological Society of America Special Paper 325 1998 Lithostratigraphic revision and correlation of the lower part of the White River Group: South Dakota to Nebraska Dennis O. Terry, Jr. Department of Geology, University of Nebraska—Lincoln, Lincoln, Nebraska 68588-0340 ABSTRACT Lithologic correlations between type areas of the White River Group in Nebraska and South Dakota have resulted in a revised lithostratigraphy for the lower part of the White River Group. The following pedostratigraphic and lithostratigraphic units, from oldest to youngest, are newly recognized in northwestern Nebraska and can be correlated with units in the Big Badlands of South Dakota: the Yellow Mounds Pale- osol Equivalent, Interior and Weta Paleosol Equivalents, Chamberlain Pass Forma- tion, and Peanut Peak Member of the Chadron Formation. The term “Interior Paleosol Complex,” used for the brightly colored zone at the base of the White River Group in northwestern Nebraska, is abandoned in favor of a two-part division. The lower part is related to the Yellow Mounds Paleosol Series of South Dakota and rep- resents the pedogenically modified Cretaceous Pierre Shale. The upper part is com- posed of the unconformably overlying, pedogenically modified overbank mudstone facies of the Chamberlain Pass Formation (which contains the Interior and Weta Paleosol Series in South Dakota). Greenish-white channel sandstones at the base of the Chadron Formation in Nebraska (previously correlated to the Ahearn Member of the Chadron Formation in South Dakota) herein are correlated to the channel sand- stone facies of the Chamberlain Pass Formation in South Dakota. The Chamberlain Pass Formation is unconformably overlain by the Chadron Formation in South Dakota and Nebraska. -
I What Is a Crocodilian?
I WHAT IS A CROCODILIAN? Crocodilians are the only living representatives of the Archosauria group (dinosaurs, pterosaurs, and thecodontians), which first appeared in the Mesozoic era. At present, crocodiliams are the most advanced of all reptiles because they have a four-chambered heart, diaphragm, and cerebral cortex. The extent morphology reflects their aquatic habits. Crocodilians are elongated and armored with a muscular, laterally shaped tail used in swimming. The snout is elongated, with the nostrils set at the end to allow breathing while most of the body remains submerged. Crocodilians have two pairs of short legs with five toes on the front and four tows on the hind feet; the toes on all feet are partially webbed. The success of this body design is evidenced by the relatively few changes that have occurred since crocodilians first appeared in the late Triassic period, about 200 million years ago. Crocodilians are divided into three subfamilies. Alligatorinae includes two species of alligators and five caiman. Crocodylinae is divided into thirteen species of crocodiles and on species of false gharial. Gavialinae contains one species of gharial. Another way to tell the three groups of crocodilians apart is to look at their teeth. II PHYSICAL CHARACTERISTICS A Locomotion Crocodilians spend time on land primarily to bask in the sun, to move from one body of water to another, to escape from disturbances, or to reproduce. They use three distinct styles of movement on land. A stately high walk is used when moving unhurried on land. When frightened, crocodilians plunge down an embankment in an inelegant belly crawl. -
Rival Species Recast Significance of 'First Bird'
NEWS IN FOCUS PALAEONTOLOGY Rival species recast significance of ‘first bird’ Archaeopteryx’s status is changing, but the animal is still key to the dinosaur–bird transition. BY EWEN CALLAWAY bird,” says Gareth Dyke, a vertebrate palaeon- brains of Archaeopteryx and a variety of dino- tologist at the University of Southampton, UK. saurs related to it were, like modern birds, all he iconic status of Archaeopteryx, the “They’d rather cut off one of their legs than relatively large for their body sizes. Because SCIENCE first animal discovered with both bird admit it has nothing to do with bird origins.” earlier dinosaurs did not fly as well as modern and dinosaur features, is under attack. New specimens of Archaeopteryx are birds, if they flew at all, the finding suggests that TMore-recently discovered rival species show also reinvigorating research. There are now the brain expansion occurred well before flight a similar mix of traits. But Archaeopteryx still 12 known fossils of the creature, and at the emerged. It is yet another clue that Archaeop- hogged the opening symposium at the 2014 symposium Kundrat unveiled the first scien- teryx may not have been any more bird-like VLADIMIR NIKOLOV. SILHOUETTE: Society of Vertebrate Paleontology meeting tific description of the eighth to be discovered. than other suggested transitional species. “It’s in Berlin last month, and even festooned the Researchers lost track of the ‘phantom’ after it another piece of data that has taken away from official conference beer glasses. was found in Germany in the early 1990s, until the specialness of Archaeopteryx,” says Balanoff. -
A Mysterious Giant Ichthyosaur from the Lowermost Jurassic of Wales
A mysterious giant ichthyosaur from the lowermost Jurassic of Wales JEREMY E. MARTIN, PEGGY VINCENT, GUILLAUME SUAN, TOM SHARPE, PETER HODGES, MATT WILLIAMS, CINDY HOWELLS, and VALENTIN FISCHER Ichthyosaurs rapidly diversified and colonised a wide range vians may challenge our understanding of their evolutionary of ecological niches during the Early and Middle Triassic history. period, but experienced a major decline in diversity near the Here we describe a radius of exceptional size, collected at end of the Triassic. Timing and causes of this demise and the Penarth on the coast of south Wales near Cardiff, UK. This subsequent rapid radiation of the diverse, but less disparate, specimen is comparable in morphology and size to the radius parvipelvian ichthyosaurs are still unknown, notably be- of shastasaurids, and it is likely that it comes from a strati- cause of inadequate sampling in strata of latest Triassic age. graphic horizon considerably younger than the last definite Here, we describe an exceptionally large radius from Lower occurrence of this family, the middle Norian (Motani 2005), Jurassic deposits at Penarth near Cardiff, south Wales (UK) although remains attributable to shastasaurid-like forms from the morphology of which places it within the giant Triassic the Rhaetian of France were mentioned by Bardet et al. (1999) shastasaurids. A tentative total body size estimate, based on and very recently by Fischer et al. (2014). a regression analysis of various complete ichthyosaur skele- Institutional abbreviations.—BRLSI, Bath Royal Literary tons, yields a value of 12–15 m. The specimen is substantially and Scientific Institution, Bath, UK; NHM, Natural History younger than any previously reported last known occur- Museum, London, UK; NMW, National Museum of Wales, rences of shastasaurids and implies a Lazarus range in the Cardiff, UK; SMNS, Staatliches Museum für Naturkunde, lowermost Jurassic for this ichthyosaur morphotype. -
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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. -
Hoganson, J.W., 2009. Corridor of Time Prehistoric Life of North
Corridor of Time Prehistoric Life of North Dakota Exhibit at the North Dakota Heritage Center Completed by John W. Hoganson Introduction In 1989, legislation was passed that directed the North Dakota and a laboratory specialist, a laboratory for preparation of Geological Survey to establish a public repository for North fossils, and a fossil storage area. The NDGS paleontology staff, Dakota fossils. Shortly thereafter, the Geological Survey signed now housed at the Heritage Center, consists of John Hoganson, a Memorandum of Agreement with the State Historical Society State Paleontologist, and paleontologists Jeff Person and Becky of North Dakota which provided space in the North Dakota Gould. This arrangement has allowed the Geological Survey, in Heritage Center for development of this North Dakota State collaboration with the State Historical Society of North Dakota, Fossil Collection, including offices for the curator of the collection to create prehistoric life of North Dakota exhibits at the Heritage Center and displays of North Dakota fossils at over 20 other museums and interpretive centers around the state. The first of the Heritage Center prehistoric life exhibits was the restoration of the Highgate Mastodon skeleton in the First People exhibit area (fig. 1). Mastodons were huge, elephant- like mammals that roamed North America at the end of the last Ice Age about 11,000 years ago. This exhibit was completed in 1992 and was the first restored skeleton of a prehistoric animal ever displayed in North Dakota. The mastodon exhibit was, and still is, a major attraction in the Heritage Center. Because of its popularity, it was decided that additional prehistoric life displays should be included in the Heritage Center exhibit plans. -
Titanosauriform Teeth from the Cretaceous of Japan
“main” — 2011/2/10 — 15:59 — page 247 — #1 Anais da Academia Brasileira de Ciências (2011) 83(1): 247-265 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 www.scielo.br/aabc Titanosauriform teeth from the Cretaceous of Japan HARUO SAEGUSA1 and YUKIMITSU TOMIDA2 1Museum of Nature and Human Activities, Hyogo, Yayoigaoka 6, Sanda, 669-1546, Japan 2National Museum of Nature and Science, 3-23-1 Hyakunin-cho, Shinjuku-ku, Tokyo 169-0073, Japan Manuscript received on October 25, 2010; accepted for publication on January 7, 2011 ABSTRACT Sauropod teeth from six localities in Japan were reexamined. Basal titanosauriforms were present in Japan during the Early Cretaceous before Aptian, and there is the possibility that the Brachiosauridae may have been included. Basal titanosauriforms with peg-like teeth were present during the “mid” Cretaceous, while the Titanosauria with peg-like teeth was present during the middle of Late Cretaceous. Recent excavations of Cretaceous sauropods in Asia showed that multiple lineages of sauropods lived throughout the Cretaceous in Asia. Japanese fossil records of sauropods are conformable with this hypothesis. Key words: Sauropod, Titanosauriforms, tooth, Cretaceous, Japan. INTRODUCTION humerus from the Upper Cretaceous Miyako Group at Moshi, Iwaizumi Town, Iwate Pref. (Hasegawa et al. Although more than twenty four dinosaur fossil local- 1991), all other localities provided fossil teeth (Tomida ities have been known in Japan (Azuma and Tomida et al. 2001, Tomida and Tsumura 2006, Saegusa et al. 1998, Kobayashi et al. 2006, Saegusa et al. 2008, Ohara 2008, Azuma and Shibata 2010). -
Uppermost Cretaceous and Tertiary Stratigraphy of Fossil Basin, Southwestern Wyoming
Uppermost Cretaceous and Tertiary Stratigraphy of Fossil Basin, Southwestern Wyoming By STEVEN S. ORIEL and JOSHUA I. TRACEY, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 635 New subdivisions of the J,ooo-Joot-thick continental Evanston, Wasatch, Green River, and Fowkes Formations facilitate understanding of sediment genesis and Jl7yoming thrust-belt tectonic events UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 70-604646 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 65 cents (paper cover) CONTENTS Page Wasatch Formation-Continued Abstract __________________________________________ _ 1 Fossils and age-Continued· Page Introduction ______________________________________ _ 2 Tunp Member______________________________ 28 Purpose ______________________________________ _ 2 Origin--------~-------------------------------- 28 Earlier work_ .. __ - __ - ___________________ - _-- _- __ 2 Tectonic implications ____________ -_-------------- 29 Acknowledgments __ . ___________________________ _ 2 Green River Formation ___ .. _______ ------------------ 30 General relations ___ -- _________________________ _ 5 Name and usage __________________ -------------- 30 Evanston Formation _______________________________ _ 5 Definition __________________ -_-------------- 30 N arne and usage _______________________________ _ 5 Lithologic heterogeneity. -
Kansas Inventors and Innovators Fourth Grade
Kansas Inventors and Innovators Fourth Grade Developed for Kansas Historical Society at the Library of Congress, Midwest Region Workshop “It’s Elementary: Teaching with Primary Sources” 2012 Terry Healy Woodrow Wilson School, USD 383, Manhattan Overview This lesson is designed to teach students about inventors and innovators of Kansas. Students will read primary sources about Jack St. Clair Kilby, Clyde Tombaugh, George Washington Carver, and Walter P. Chrysler. Students will use a document analysis sheet to record information before developing a Kansas Innovator card. Standards History: Benchmark 1, Indicator 1 The student researches the contributions made by notable Kansans in history. Benchmark 4, Indicator 4 The student identifies and compares information from primary and secondary sources (e.g., photographs, diaries/journals, newspapers, historical maps). Common Core ELA Reading: Benchmark RI.4.9 The student integrates information from two texts on the same topic in order to write or speak about the subject knowledgably. Benchmark RI.4.10. By the end of year, read and comprehend informational texts, including history/social studies, science, and technical texts, in the grades 4–5 text complexity band proficiently, with scaffolding as needed at the high end of the range. Objectives Content The student will summarize and present information about a Kansas inventor/innovator. 1 Skills The student will analyze and summarize primary and secondary sources to draw conclusions. Essential Questions How do we know about past inventions and innovations? What might inspire or spark the creation of an invention or innovation? How do new inventions or innovations impact our lives? Resource Table Image Description Citation URL Photograph of Jack Photograph of Jack http://kshs.org/kans Kilby (Handout 1) Kilby, Kansapedia, apedia/jack-st-clair- from Texas Kansas Historical kilby/12125 Instruments Society (Topeka, Kansas) Photo originally from Texas Instruments. -
Rocky Start of Dinosaur National Monument (USA), the World's First Dinosaur Geoconservation Site
Original Article Rocky Start of Dinosaur National Monument (USA), the World's First Dinosaur Geoconservation Site Kenneth Carpenter Prehistoric Museum, Utah State University Eastern Price, Utah 80504 USA Abstract The quarry museum at Dinosaur National Monument, which straddles the border between the American states of Colorado and Utah, is the classic geoconservation site where visitors can see real dinosaur bones embedded in rock and protected from the weather by a concrete and glass structure. The site was found by the Carnegie Museum in August 1909 and became a geotourist site within days of its discovery. Within a decade, visitors from as far as New Zealand traveled the rough, deeply rutted dirt roads to see dinosaur bones in the ground for themselves. Fearing that the site would be taken over by others, the Carnegie Museum attempted twice to take the legal possession of the land. The second attempt had consequences far beyond what the Museum intended when the federal government declared the site as Dinosaur National Monument in 1915, thus taking ultimate control from the Carnegie Museum. Historical records and other archival data (correspondence, diaries, reports, newspapers, hand drawn maps, etc.) are used to show that the unfolding of events was anything but smooth. It was marked by misunderstanding, conflicting Corresponding Author: goals, impatience, covetousness, miscommunication, unrealistic expectation, intrigue, and some Kenneth Carpenter paranoia, which came together in unexpected ways for both the Carnegie Museum and the federal Utah State University Eastern Price, government. Utah 80504 USA Email: [email protected] Keywords: Carnegie Museum, Dinosaur National Monument, U.S. National Park Service.