Dinner in a Dinosaur
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I.—Eminent Living Geologists : William Thomas Blanford, C.I.E., Ll.T)., F.E.S., V.P
THE GEOLOGICAL MAGAZINE. NEW SERIES. DECADE V. VOL. II. No. I —JANUARY, 1905. OBIGIITAL AETICLES. I.—EMINENT LIVING GEOLOGISTS : WILLIAM THOMAS BLANFORD, C.I.E., LL.T)., F.E.S., V.P. Zool. Soc, Treas. Geol. Soc. (WITH A PORTRAIT, PLATE I.) HAT India has been in the past 300 years to our Army as W a nursery in which our soldiers have obtained experience in their profession and earned their promotion, often to the highest rank, such in a lesser degree has it been to many of our geologists, who have, in the past much shorter period of 50 or 60 years, entered the service in this vast field of scientific enterprise, and, aided by a very few amateur geologists in the Army and of civilians attached to other branches of Government employ, have covered many thousand square miles of our Indian Empire with records of their untiring energy in the geological field. Among the amateurs may be recorded the names of Generals Sir Kichard Strachey and Sir Proby T. Cautley, Dr. Hugh Falconer, Lieut-Gen. C. A. McMahon; and as professional geologists, Dr. T. Oldham, H. B. Medlicott, J. G. Medlicott, Dr. Wm. King, Dr. Valentine Ball, the two Blanfords, W. Theobald, E. Bruce Foote, A. B. Wynne, C. L. Griesbach, E. D. Oldham, F. E. Mallet, C. S. Middlemiss, T. D. La Touche, Dr. F. Stoliczka, Professor W. Waagen, the present Director (T. H. Holland), and many others. Prominent among the earlier geological workers stand out the names of the brothers W. T. and H. F. Blanford, who joined the Indian Survey together in 1855. -
Last Name, First Name ECOL 249. Quiz 5 Part I. Answer Twelve
May not be posted online without written permission of W. M. Schaffer, Univ. AZ., Tucson, AZ. ___________________________ Last Name, First Name ECOL 249. Quiz 5 Part I. Answer twelve (12) of the following questions (5 points each). Only the first 12 answers will be graded. 1. By 1872, Vestiges had a. been banned for atheistic and seditious content. b. been embraced by the physicists who approved its endorsement of the nebula hypothesis. c. been outsold 5:1 by The Origin d. outsold The Origin by about 2:1 [Lecture V, 3] e. had so enraged the public that its formerly anonymous author was forced to flee the country with wife and children. 2. Which of the following scientific ideas was not endorsed by Vestiges? a. Nebular hypothesis. b. Progress in the fossil record. c. Quinerian classification. d. Spontaneous generation of mites e. wants and ... exercise... in the way suggested by Lamarck. [Lecture V, 9] 3. The ideas of _________ were eventually confirmed by the discovery of dorso-ventral patterning inversion in chordates and invertebrates. a. É. Geoffroy St. Hilaire [Lecture V, 62-63] b. Ernst Haeckel c. K. E. von Baer d. Robert Grant e. Richard Owen 4. According to Adrian Desmond (Designing the Dinosaur), Owen’s creation of the order Dinosauria and his mammal-like dinosaur reconstructions were motivated by antipa- thy to ___________ . a. Edward Forbes b. Louis Agassiz Megaloceros, a bipedal theropod dinosaur, as im- c. Robert Chambers. agined by Owen and restored by Waterhouse d. Robert Grant [Desmond, 1987, 224 ff] Hawkins for the Crystal Palace Exhibition. -
An Investigation Into the Graphic Innovations of Geologist Henry T
Louisiana State University LSU Digital Commons LSU Doctoral Dissertations Graduate School 2003 Uncovering strata: an investigation into the graphic innovations of geologist Henry T. De la Beche Renee M. Clary Louisiana State University and Agricultural and Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_dissertations Part of the Education Commons Recommended Citation Clary, Renee M., "Uncovering strata: an investigation into the graphic innovations of geologist Henry T. De la Beche" (2003). LSU Doctoral Dissertations. 127. https://digitalcommons.lsu.edu/gradschool_dissertations/127 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Doctoral Dissertations by an authorized graduate school editor of LSU Digital Commons. For more information, please [email protected]. UNCOVERING STRATA: AN INVESTIGATION INTO THE GRAPHIC INNOVATIONS OF GEOLOGIST HENRY T. DE LA BECHE A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Curriculum and Instruction by Renee M. Clary B.S., University of Southwestern Louisiana, 1983 M.S., University of Southwestern Louisiana, 1997 M.Ed., University of Southwestern Louisiana, 1998 May 2003 Copyright 2003 Renee M. Clary All rights reserved ii Acknowledgments Photographs of the archived documents held in the National Museum of Wales are provided by the museum, and are reproduced with permission. I send a sincere thank you to Mr. Tom Sharpe, Curator, who offered his time and assistance during the research trip to Wales. -
Megaloceros Giganteus) from the Pleistocene in Poland
Palaeontologia Electronica palaeo-electronica.org Healed antler fracture from a giant deer (Megaloceros giganteus) from the Pleistocene in Poland Kamilla Pawłowska, Krzysztof Stefaniak, and Dariusz Nowakowski ABSTRACT We evaluated the skull of an ancient giant deer with a deformity of one antler. The skull was found in the 1930s in the San River near Barycz, in southeastern Poland. Its dating (39,800±1000 yr BP) corresponds to MIS-3, when the giant deer was wide- spread in Europe. Our diagnostics for the antler included gross morphology, radiogra- phy, computed tomography, and histopathology. We noted signs of fracture healing of the affected antler, including disordered arrangement of lamellae, absence of osteons, and numerous Volkmann’s canals remaining after blood vessel loss. The antler defor- mity appears to be of traumatic origin, with a healing component. No similar evaluation process has been described previously for this species. Kamilla Pawłowska. corresponding author, Institute of Geology, Adam Mickiewicz University, Maków Polnych 16, Poznań 61-606, Poland, [email protected] Krzysztof Stefaniak. Division of Palaeozoology, Department of Evolutionary Biology and Ecology, Faculty of Biological Sciences, University of Wrocław, Sienkiewicza 21, Wrocław 50-335, Poland, [email protected] Dariusz Nowakowski. Department of Anthropology, Wroclaw University of Environmental and Life Sciences, Kożuchowska 6/7, Wrocław 51-631, Poland, [email protected] Keywords: giant deer; Megaloceros giganteus; paleopathology; Pleistocene; Poland INTRODUCTION -
Editorial This Issue Contains a Profile of John Stevens Henslow, Darwin’S Cambridge Friend and Mentor (Page 4)
THE LINNEAN 1 Editorial This issue contains a profile of John Stevens Henslow, Darwin’s Cambridge friend and mentor (page 4). Henslow was not only responsible for Darwin’s appointment to HMS Beagle but also arranged to receive all tlie collected material shipped home to Cambridge. Moreover at the conclusion of the voyage he arranged for Darwin to be given a Treasury grant of &I,000 towards the publication of his zoological fiiidings. During the entire five years of the Beagle s voyage, Henslow corresponded with Darwin proffering advice and guidance and later publishing some of Darwin’s geological observations in the Cambridge Philosophical Society Proceedings.’ Darwin’s great debt of gratitude to Henslow is quite apparent from the tone of his letters to his old tutor: “I always like advice from you, and no one whom I have the luck to know is more capable of giving it than yourself. Recollect, when you write, that I am a sort ofprotkgge‘of yours, and that it is your bounden duty to lecture me.” (Devonport, Dec. 3 1831) “I will say farewell, till the day arrives when I shall see my Master in Natural History and can tell him how grateful I feel for his kindness and friendship.” (Sydney, Jan. 1836) And then when telling Henslow about his geological specimens: “My dear Henslow, I do long to see you, you have been the kindest friend to me that ever man possessed.” (Shrewsbury, Oct. 6 1836) The year after the Beagle ’s return Henslow was appointed rector of Hitcham, Suffolk (1837) and from that point onwards as Darwin noted: “he cared somewhat less about science and more for his parishioners.” Finally, in the last year of his life, Henslow came to the assistance of his student one last time by acting as Chairman of the 1860 British Association meeting at which Huxley (and Hooker and Lubbock) took up the cudgel on Darwin’s behalf. -
New Record of Terminal Pleistocene Elk/Wapiti (Cervus Canadensis) from Ohio, USA
2 TERMINAL PLEISTOCENE ELK FROM OHIO VOL. 121(2) New Record of Terminal Pleistocene Elk/Wapiti (Cervus canadensis) from Ohio, USA BRIAN G. REDMOND1, Department of Archaeology, Cleveland Museum of Natural History, Cleveland, OH, USA; DAVID L. DYER, Ohio History Connection, Columbus, OH, USA; and CHARLES STEPHENS, Sugar Creek Chapter, Archaeological Society of Ohio, Massillon, OH, USA. ABSTRACT. The earliest appearance of elk/wapiti (Cervus canadensis) in eastern North America is not thoroughly documented due to the small number of directly dated remains. Until recently, no absolute dates on elk bone older than 10,000 14C yr BP (11,621 to 11,306 calibrated years (cal yr) BP) were known from this region. The partial skeleton of the Tope Elk was discovered in 2017 during commercial excavation of peat deposits from a small bog in southeastern Medina County, Ohio, United States. Subsequent examination of the remains revealed the individual to be a robust male approximately 8.5 years old at death. The large size of this individual is compared with late Holocene specimens and suggests diminution of elk since the late Pleistocene. Two accelerator mass spectrometry (AMS) radiocarbon assays on bone collagen samples taken from the scapula and metacarpal of this individual returned ages of 10,270 ± 30 14C yr BP (Beta-477478) (12,154 to 11,835 cal yr BP) and 10,260 ± 30 14C yr BP (Beta-521748) (12,144 to 11,830 cal yr BP), respectively. These results place Cervus canadensis in the terminal Pleistocene of the eastern woodlands and near the establishment of the mixed deciduous forest biome over much of the region. -
Edward Forbes and His Azoic Hypothesis for a Lifeless Deep Ocean
Review Endeavour Vol.30 No.4 Deserts on the sea floor: Edward Forbes and his azoic hypothesis for a lifeless deep ocean Thomas R. Anderson and Tony Rice George Deacon Division, National Oceanography Centre, Southampton, UK SO14 3ZH While dredging in the Ægean Sea during the mid-19th ship. The captain’s cabin became a laboratory-cum- century, Manxman Edward Forbes noticed that plants museum, where Forbes dissected and drew the animals and animals became progressively more impoverished collected and preserved them in bottles of alcohol. The the greater the depth they were from the surface of the captain and crew were there to help, although it is likely water. By extrapolation Forbes proposed his now infa- that some of the sailors were less than enthusiastic about mous azoic hypothesis, namely that life would be extin- the work involved. However, this work provided evening guished altogether in the murky depths of the deep entertainment for Forbes at least, who frequently turned ocean. The whole idea seemed so entirely logical given his artistic hand to drawing cartoons (Figure 2). the enormous pressure, cold and eternal darkness of this Forbes’ main aim was not, however, to describe the apparently uninhabitable environment. Yet we now animals themselves, but rather to understand their dis- know that the sea floor is teeming with life. Curiously, tribution across different types of habitat. Gathering it took 25 years for the azoic hypothesis to fall from together his results from the Ægean, the influence of depth grace. This was despite the presence of ample contrary was of obvious importance. -
Curator 9-2 Cover.Qxd
Volume 9 Number 2 GEOLOGICAL CURATORS’ GROUP Registered Charity No. 296050 The Group is affiliated to the Geological Society of London. It was founded in 1974 to improve the status of geology in museums and similar institutions, and to improve the standard of geological curation in general by: - holding meetings to promote the exchange of information - providing information and advice on all matters relating to geology in museums - the surveillance of collections of geological specimens and information with a view to ensuring their well being - the maintenance of a code of practice for the curation and deployment of collections - the advancement of the documentation and conservation of geological sites - initiating and conducting surveys relating to the aims of the Group. 2009 COMMITTEE Chairman Helen Fothergill, Plymouth City Museum and Art Gallery: Drake Circus, Plymouth, PL4 8AJ, U.K. (tel: 01752 304774; fax: 01752 304775; e-mail: [email protected]) Secretary David Gelsthorpe, Manchester Museum, Oxford Road, Manchester M13 9PL, U.K. (tel: 0161 3061601; fax: 0161 2752676; e-mail: [email protected] Treasurer John Nudds, School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Oxford Road, Manchester M13 9PL, U.K. (tel: +44 161 275 7861; e-mail: [email protected]) Programme Secretary Steve McLean, The Hancock Museum, The University, Newcastle-upon-Tyne NE2 4PT, U.K. (tel: 0191 2226765; fax: 0191 2226753; e-mail: [email protected]) Editor of Matthew Parkes, Natural History Division, National Museum of Ireland, Merrion Street, The Geological Curator Dublin 2, Ireland (tel: 353 (0)87 1221967; e-mail: [email protected]) Editor of Coprolite Tom Sharpe, Department of Geology, National Museums and Galleries of Wales, Cathays Park, Cardiff CF10 3NP, Wales, U.K. -
How the 'Seven Deadly Agents Of
Paper presented at the How the ‘Seven Deadly Agents of Destruction’ conference can help preserve the Crystal Palace Dinosaurs Liesa Brierley, Ellinor Michel, Anthony Lewis, Chris Aldhous and Lois Olmstead Introduction Compared to collections kept safe inside museums, outdoor sculpture is affected by additional risk factors. Sculpture in the public realm is exposed to the elements, pollution and direct sunshine. It is more vulnerable to vandalism and the proximity to nature can also take its toll. At the same time, the condition of outdoor sculpture is often not monitored as rigorously as that of museum collections. However, damage doesn’t go unnoticed by the public and, channelled in the right way, the public’s critical eye can be turned to positive pressure, increasing support for conservation work and helping to improve conditions for the displays. To conservation professionals, the Canadian Conservation Institute’s framework of Ten Agents of Deterioration is a familiar and well-established way of describing risk factors to cultural heritage. This paper describes an attempt to translate this framework into a short animated film about risks to outdoor sculpture, using the Crystal Palace Dinosaurs, a renowned Victorian sculpture park in south London, as the stage for the message. The film is aimed at a broad audience of non-professionals of all ages and it is hoped that it will deliver an increased sense of both understanding and ownership of the sculpture park. The Crystal Palace Dinosaurs The Crystal Palace Dinosaurs are the first life-sized sculptural reconstructions of extinct animals, built to engage and enlighten the public on the paradigm- shifting advances in science in the mid-19th century (Owen 1854, McCarthy and Gilbert 1994, Pigott 2004, Bramwell and Peck 2008). -
Patterns of Late Quaternary Megafaunal Extinctions in Europe and Northern Asia
Cour. Forsch.-Inst. Senckenberg | 259 | 287 – 297 | 2 Figs | Frankfurt a. M., 13. 12. 2007 Patterns of Late Quaternary megafaunal extinctions in Europe and northern Asia With 2 figs Anthony J. STUART & Adrian M. LISTER A b s t r a c t This paper summarizes the results so far of our ‘Late Quaternary Megafaunal Extinctions’ project, focussing on an assessment of latest available dates for selected target species from Europe and northern Asia. Our approach is to directly radiocarbon-date material of extinct megafauna to construct their spatio-temporal histories, and to seek correlations with the environmental and archaeological records with the aim of estab- lishing the cause or causes of extinction. So far we have focussed on Mammuthus primigenius, Coelodonta antiquitatis, and Megaloceros giganteus, and are accumulating data on Panthera leo/spelaea, Crocuta crocuta and Ursus spelaeus. Attempts to date Palaeoloxodon antiquus and Stephanorhinus hemitoechus (from southern Europe) were largely unsuccessful. The pattern of inferred terminal dates is staggered, with extinctions occurring over ca. 30 millennia, with some species previously thought extinct in the Late Pleistocene – M. primigenius and M. giganteus – surviving well into the Holocene. All species show dramatic range shifts in response to climatic/vegeta- tional changes, especially the beginning of the Last Glacial Maximum, Late Glacial Interstadial, Allerød, Younger Dryas and Holocene, and there was a general trend of progressive range reduction and fragmenta- tion prior to final extinction. With the possible exceptions of P. antiquus, S. hemitoechus and Homo nean- derthalensis, extinctions do not correlate with the appearance of modern humans. However, although most of the observed patterns can be attributed to environmental changes, some features – especially failures to recolonize – suggest human involvement. -
Evolution of Mammals Classifying Mammals
Outline 20: Evolution of Mammals Classifying Mammals • Paleontologists recognize at least 5 major groups of mammals. Only 3 are still living: –Monotremes: lay eggs –Marsupials: poorly developed at birth –Eutherians or Placentals: well developed at birth 5 Major Groups: 3 Living Defining Mammals • Warm blooded • Fur • Milk glands • Can lay eggs or have some form of live birth. Recognizing Fossil Mammals • Our definition of mammals doesn’t work with fossil bones. • How do we recognize the first mammals? –Reptiles have 3 bones in lower jaw. –Mammals have 1 bone in lower jaw –Mammal teeth are specialized. Dinosaurs have 3 bones in lower jaw 2 3 1 Mammals have 1 bone in lower jaw Hadrocodium, a lower Jurassic mammal with a “large” brain (6 mm brain case in an 8 mm skull) Eomaia, oldest placental mammal, 125 my old, Lower Cretaceous, China Eomaia, oldest placental mammal, 125 my old, Lower Cretaceous, China Eomaia Mammal fossil from the Cretaceous of Mongolia Jaw bones • Reptiles have 3 bones in their jaw: dentary, articular, and quadrate. • Articular and quadrate bones of reptile jaw became the hammer and anvil bones of the mammalian inner ear. • Marsupials are born with a reptilian jaw, which quickly changes before they eat solid food. = articular of = quadrate of Human Ear Bones, or lower reptile upper reptile Auditory Ossicles jaw jaw Cochlea Mammal Teeth • Teeth make excellent fossils. • Reptile ancestors had simple, cone- shaped teeth they regularly replaced. • Mammal teeth are specialized into incisors, canines, pre-molars and molars. • Mammals have only two sets of teeth during their lifetime. A Nile crocodile. -
Linking Top-Down Forces to the Pleistocene Megafaunal Extinctions
Articles Articles Linking Top-down Forces to the Pleistocene Megafaunal Extinctions WILLIAM J. RIPPLE AND BLAIRE VAN VALKENBURGH Humans, in conjunction with natural top-down processes and through a sequence of cascading trophic interactions, may have contributed to the Pleistocene megafaunal extinctions. The arrival of the first humans, as hunters and scavengers, through top-down forcing, could have triggered a population collapse of large herbivores and their predators. We present evidence that the large mammalian herbivores of the North American Pleistocene were primarily predator limited and at low densities, and therefore highly susceptible to extinction when humans were added to the predator guild. Our empirical evidence comes from data on carnivore dental attrition, proboscidean age structure, life history, tusk growth rates, and stable isotopes from the fossil record. We suggest a research agenda for further testing of this hypothesis that will provide a more detailed comprehension of late Pleistocene megafaunal ecology, and thereby allow us to better understand and manage remaining megafauna. Keywords: Pleistocene, megafauna, extinctions, large carnivores, humans wo-thirds of North America’s large mammal genera sites that show evidence of human association with extinct Tbecame extinct during the late Pleistocene. The cause for megafauna (Grayson and Meltzer 2003, but see Surovell and this massive extinction has been debated for decades, with Waguespack 2008). Notably, the hypothesis proposed here is most authors favoring either aboriginal overkill or climate not dependent on a minimum number of known kill sites, change as the primary driver (Grayson and Meltzer 2003, and a relatively low number of these sites would be expected Barnosky et al.