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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. -
Ahead of the Wave
sciencenewsf o rkids.o rg http://www.sciencenewsforkids.org/2013/02/scientists-are-working-to-predict-and-tame-the-tsunamis-that-can-threaten-some- coastal-communities/ Ahead of the wave By Stephen Ornes / February 13, 2013 Bump a glass and any water inside might slop over the side. Splash in the bathtub and waves slosh. Toss a rock into a pond and ripples move outward in expanding rings. In each case, the water moves in waves. Those waves carry energy. And the more energy that gets added to a watery environment, the more powerf ul the waves may become. Now imagine an undersea earthquake and the tremendous amount of energy it can transf er to the ocean. That is because the movement of the Earth’s crust can shif t huge volumes of water, unleashing a parade of great and powerf ul waves. The water races away at speeds up to 800 kilometers (500 miles) per hour, or as f ast as a jet plane. Eventually those waves reach shallow Wate r p o urs asho re as a tsunami strike s the e ast co ast o f Jap an o n March 11, 2011. Cre d it: Mainichi Shimb un/Re ute rs water. They slow down and swell, sometimes as high as a 10-story building. When the waves eventually crash onto land, they can swamp hundreds of kilometers (miles) of shoreline. They may snap trees like twigs, collapse of f ice buildings and sweep away cars. Among nature’s most powerf ul f orces of destruction, these waves are called tsunamis (tzu NAAM eez). -
Documenting Inuit Knowledge of Coastal Oceanography in Nunatsiavut
Respecting ontology: Documenting Inuit knowledge of coastal oceanography in Nunatsiavut By Breanna Bishop Submitted in partial fulfillment of the requirements for the degree of Master of Marine Management at Dalhousie University Halifax, Nova Scotia December 2019 © Breanna Bishop, 2019 Table of Contents List of Tables and Figures ............................................................................................................ iv Abstract ............................................................................................................................................ v Acknowledgements ........................................................................................................................ vi Chapter 1: Introduction ............................................................................................................... 1 1.1 Management Problem ...................................................................................................................... 4 1.1.1 Research aim and objectives ........................................................................................................................ 5 Chapter 2: Context ....................................................................................................................... 7 2.1 Oceanographic context for Nunatsiavut ......................................................................................... 7 2.3 Inuit knowledge in Nunatsiavut decision making ......................................................................... -
Former Fellows Biographical Index Part
Former Fellows of The Royal Society of Edinburgh 1783 – 2002 Biographical Index Part Two ISBN 0 902198 84 X Published July 2006 © The Royal Society of Edinburgh 22-26 George Street, Edinburgh, EH2 2PQ BIOGRAPHICAL INDEX OF FORMER FELLOWS OF THE ROYAL SOCIETY OF EDINBURGH 1783 – 2002 PART II K-Z C D Waterston and A Macmillan Shearer This is a print-out of the biographical index of over 4000 former Fellows of the Royal Society of Edinburgh as held on the Society’s computer system in October 2005. It lists former Fellows from the foundation of the Society in 1783 to October 2002. Most are deceased Fellows up to and including the list given in the RSE Directory 2003 (Session 2002-3) but some former Fellows who left the Society by resignation or were removed from the roll are still living. HISTORY OF THE PROJECT Information on the Fellowship has been kept by the Society in many ways – unpublished sources include Council and Committee Minutes, Card Indices, and correspondence; published sources such as Transactions, Proceedings, Year Books, Billets, Candidates Lists, etc. All have been examined by the compilers, who have found the Minutes, particularly Committee Minutes, to be of variable quality, and it is to be regretted that the Society’s holdings of published billets and candidates lists are incomplete. The late Professor Neil Campbell prepared from these sources a loose-leaf list of some 1500 Ordinary Fellows elected during the Society’s first hundred years. He listed name and forenames, title where applicable and national honours, profession or discipline, position held, some information on membership of the other societies, dates of birth, election to the Society and death or resignation from the Society and reference to a printed biography. -
Biological Oceanography - Legendre, Louis and Rassoulzadegan, Fereidoun
OCEANOGRAPHY – Vol.II - Biological Oceanography - Legendre, Louis and Rassoulzadegan, Fereidoun BIOLOGICAL OCEANOGRAPHY Legendre, Louis and Rassoulzadegan, Fereidoun Laboratoire d'Océanographie de Villefranche, France. Keywords: Algae, allochthonous nutrient, aphotic zone, autochthonous nutrient, Auxotrophs, bacteria, bacterioplankton, benthos, carbon dioxide, carnivory, chelator, chemoautotrophs, ciliates, coastal eutrophication, coccolithophores, convection, crustaceans, cyanobacteria, detritus, diatoms, dinoflagellates, disphotic zone, dissolved organic carbon (DOC), dissolved organic matter (DOM), ecosystem, eukaryotes, euphotic zone, eutrophic, excretion, exoenzymes, exudation, fecal pellet, femtoplankton, fish, fish lavae, flagellates, food web, foraminifers, fungi, harmful algal blooms (HABs), herbivorous food web, herbivory, heterotrophs, holoplankton, ichthyoplankton, irradiance, labile, large planktonic microphages, lysis, macroplankton, marine snow, megaplankton, meroplankton, mesoplankton, metazoan, metazooplankton, microbial food web, microbial loop, microheterotrophs, microplankton, mixotrophs, mollusks, multivorous food web, mutualism, mycoplankton, nanoplankton, nekton, net community production (NCP), neuston, new production, nutrient limitation, nutrient (macro-, micro-, inorganic, organic), oligotrophic, omnivory, osmotrophs, particulate organic carbon (POC), particulate organic matter (POM), pelagic, phagocytosis, phagotrophs, photoautotorphs, photosynthesis, phytoplankton, phytoplankton bloom, picoplankton, plankton, -
Miles Down! Oceanography Through History
MILES DOWN! OCEANOGRAPHY THROUGH HISTORY The history of oceanography is an international story of invention, individual adventure, and exploration that remains little-known. This exhibition presents an historical overview, using timelines, text, photographs, and profiles of oceanographic expeditions and individual scientists from around the world. Image: Colette Kerry From water’s edge, the oceans are as mysterious as the stars. In the 21st century, deep-sea exploration – like space exploration - is no longer a fantastic idea, but a fact of scientific life. How did we move below the surface to study the depths of the sea? This exhibition tells the story of curious humans posing questions about the oceans and developing the tools and technology to move miles down to explore the sea. The oceans that cover 71% of the world’s surface hide complex worlds within their depths. How ocean waters behave, what creatures inhabit the seas, what lies on the ocean floors, what makes up seawater: these are the questions that underlie the scientific study of the oceans - the science of oceanography. Oceanography is the scientific study of the oceans as complex, interrelated systems. It is a mixed science that combines many different approaches to understanding the watery portion of our planet. Physics explores the physical properties of the oceans, the currents and waves. It’s a study of matter and energy and the relation between them. Chemistry is concerned with the properties, composition, and structure of substances in the oceans and the changes they undergo when they combine or react. The geology of the seafloor explores the earth’s history, composition, structure and processes. -
Marine Microbiology at Scripps
81832_Ocean 8/28/03 7:18 PM Page 67 Special Issue—Scripps Centennial Marine Microbiology at Scripps A. Aristides Yayanos Scripps Institution of Oceanography, University of California, • San Diego, California USA Marine microbiology is the study of the smallest isolated marine bioluminescent bacteria, isolated and organisms found in the oceans—bacteria and archaea, characterized sulfate-reducing bacteria, and showed many eukaryotes (among the protozoa, fungi, and denitrifying bacteria could both produce and consume plants), and viruses. Most microorganisms can be seen nitrous oxide, now known to be an important green- only with a microscope. Microbes pervade the oceans, house gas. Beijerinck also founded the field of virology its sediments, and some hydrothermal fluids and through his work on plant viruses (van Iterson et al., exhibit solitary life styles as well as complex relation- 1983). Mills (1989) describes the significance of the ships with animals, other microorganisms, and each work of Beijerink and Winogradsky to plankton other. The skeletal remains of microorganisms form the research and marine chemistry. largest component of sedimentary fossils whose study Around 1903, bacteriology in California was reveals Earth’s history. The enormous morphological, emerging in the areas of medicine and public health physiological, and taxonomic diversity of marine and accordingly was developing into an academic dis- microorganisms remains far from adequately cipline in medical schools (McClung and Meyer, 1974). described and studied. Because the sea receives terres- Whereas the branch of microbiology dealing with bac- trial microorganisms from rivers, sewage outfalls, and teria and viruses was just beginning, the branch con- other sources, marine microbiology also includes the cerning protozoa and algae was a relatively more estab- study of alien microorganisms. -
Biological Oceanography
MEETINGS & WORKSHOPS BOOKS & VIDEOS COMPARISON OF BIOLOGICALOCEANOGRAPHY: TERRES ,C AN EARLY I--hSTOR¥, 1870 TO 1960 MARINE ECOLOGICAL SYSTEMS By Eric L. Mills A WORKSHOP on this subject 1989,378 pp., $42.50, Cloth, Cornell University Press, Ithaca, NY. was held in 1989 with partial National Reviewed by David J. Carlson Science Foundation support. The re- In the mid-nineteenth century, biologists dence), the initial biological oceanographers port (copies available from J. Steele) studying the oceans were mostly interested were male (Sheina Marshall of the Scottish discusses the various problems, lo- in discovering deep-sea organisms. Today Marine Biological Association laboratory gistic and conceptual, in making such biological oceanographers pay most atten- and Penelope Jenkin and Marie Lebour of the comparisons, but its main conclu- tion to processes in the surface ocean. In his Plymouth Laboratoryare notable exceptions). sion is that we should have work- latest volume of oceanographic history, Mills introduces us first to Victor Hensen, a shops or summer schools that focus published by Cornell University Press in its German biochemist, anatomist and physi- on specific topics where interactions History of Science Series, Eric Mills de- ologist who turned his attention to marine between the different sectors would scribes the period from 1870 to 1960 during subjects when nascent Germany formed a be most fruitful. A recent meeting of which focus shifted from deep-sea natural commission for the study of its seas. Hensen the Steering Committee (J. Cohen, P. history to upper ocean plankton dynamics recognized that small planktonic organisms Dayton, T. Kratz, S. Levin, R. and when, as a result, biological oceanogra- were important components of marine sys- Ricklefs and J. -
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. -
Download English Translation of Meyer, A. 1913. Das
The Renogenital System of Puncturella noachina L. By Anna Meyer (of the Zoological Museum, University of Kasan) with 10 text figures The study of the excretory and genital organs of the lower Diotocardia is of significant interest because one can expect in this organ system (in its composition of the heart and gills, but perhaps only as traces) the same parity and symmetry as must have theoretically been present in the Urgastropod. Haller believed he actually had discovered such a paired and symmetrical composition of the aforementioned organs in the extant species Puncturella (Cemoria) noachina L. in the Family Fissurellidae. However, later studies provoked considerable controversy among the admittedly few researchers who re-examined the renogenital system of this species and the controversy remained undecided. I therefore eagerly followed the suggestion of my father, Professor Eduard Meyer, to undertake a detailed study of the renogenital system of Puncturella and to examine the claims of the earlier workers. However, before I go to the account of my observations, I wish to briefly present the results of earlier studies. The first information on the renogenital system of Puncturella comes from v. Erlanger in 1892 in his work “On the Paired Nephridia of Prosobranchs”1, where he detected the existence of two nephridia and pointed out their strongly asymmetrical development. He observed that the right organ was extraordinarily well developed and extended almost through the entire body cavity of the animal, while the left kidney was greatly reduced. Both nephridia open through separate papilla into the mantle cavity to either side of the anus; the left papilla being weakly developed and having a far smaller opening. -
Proceedings of the United States National Museum
PROCEEDINGS OF THE UNITED STATES NATIONAL MUSEUM SMITHSONIAN INSTITUTION U. S. NATIONAL MUSEUM VoL 109 WMhington : 1959 No. 3412 MARINE MOLLUSCA OF POINT BARROW, ALASKA Bv Nettie MacGinitie Introduction The material upon which this study is based was collected by G. E. MacGinitie in the vicinity of Point Barrow, Alaska. His work on the invertebrates of the region (see G. E. MacGinitie, 1955j was spon- sored by contracts (N6-0NR 243-16) between the OfRce of Naval Research and the California Institute of Technology (1948) and The Johns Hopkins L^niversity (1949-1950). The writer, who served as research associate under this project, spent the. periods from July 10 to Oct. 10, 1948, and from June 1949 to August 1950 at the Arctic Research Laboratory, which is located at Point Barrow base at ap- proximately long. 156°41' W. and lat. 71°20' N. As the northernmost point in Alaska, and representing as it does a point about midway between the waters of northwest Greenland and the Kara Sea, where collections of polar fauna have been made. Point Barrow should be of particular interest to students of Arctic forms. Although the dredge hauls made during the collection of these speci- mens number in the hundreds and, compared with most "expedition standards," would be called fairly intensive, the area of the ocean ' Kerckhofl Marine Laboratory, California Institute of Technology. 473771—59 1 59 — 60 PROCEEDINGS OF THE NATIONAL MUSEUM vol. los bottom touched by the dredge is actually small in comparison with the total area involved in the investigation. Such dredge hauls can yield nothing comparable to what can be obtained from a mudflat at low tide, for instance.