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University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY of the SCOTT GLACIER and WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA
This dissertation has been /»OOAOO m icrofilm ed exactly as received MINSHEW, Jr., Velon Haywood, 1939- GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA. The Ohio State University, Ph.D., 1967 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Velon Haywood Minshew, Jr. B.S., M.S, The Ohio State University 1967 Approved by -Adviser Department of Geology ACKNOWLEDGMENTS This report covers two field seasons in the central Trans- antarctic Mountains, During this time, the Mt, Weaver field party consisted of: George Doumani, leader and paleontologist; Larry Lackey, field assistant; Courtney Skinner, field assistant. The Wisconsin Range party was composed of: Gunter Faure, leader and geochronologist; John Mercer, glacial geologist; John Murtaugh, igneous petrclogist; James Teller, field assistant; Courtney Skinner, field assistant; Harry Gair, visiting strati- grapher. The author served as a stratigrapher with both expedi tions . Various members of the staff of the Department of Geology, The Ohio State University, as well as some specialists from the outside were consulted in the laboratory studies for the pre paration of this report. Dr. George E. Moore supervised the petrographic work and critically reviewed the manuscript. Dr. J. M. Schopf examined the coal and plant fossils, and provided information concerning their age and environmental significance. Drs. Richard P. Goldthwait and Colin B. B. Bull spent time with the author discussing the late Paleozoic glacial deposits, and reviewed portions of the manuscript. -
BIRD SPECIES RECORDED at CAPE BIRD, ROSS ISLAND, ANTARCTICA by E
BIRD SPECIES RECORDED AT CAPE BIRD, ROSS ISLAND, ANTARCTICA By E. B. SPURR, K.-J. WILSON, and P. M. SAGAR ABSTRACT The .\delie Penguin and Antarctic Skua breed at Cape Bird, and nine other species have been recorded as visitors (Emperor Penguin, Chinstrap Penguin, Southern Giant Petrel, Antarctic Fulmar, Antarctic Petrel, Snow Petrel, Wilson's Storm Petrel, Southern Great Skua, and Southern Black-backed Gull). Fewer birds were recorded as visitors at Cape Bird than have been recorded at Capes Crozier and Royds, possibly because Cape Bird gets less wind. INTRODUCTION Cape Bird, at the northern tip of Ross Island, Antarctica, is a breeding area for the Addie Penguin (Pygoscelis adeliae) and the Antarctic Skua (Stercoranus maccomicki). The breeding area extends from about 5 km to about 14 km south-west of the cape (77O 13'S, 166'28'E to 77O 18'S, 1660201E).The skuas nest over much of the area, whereas the penguins nest in three discrete areas (the Northern. Middle, and Southern Rookeries). Throughout winter, the breeding area of the birds is covered with snow and closed in by the McMurdo Sound sea-ice. The break-up of this sea-ice in spring is vitally important for the birds (Stonehouse 1967). Most of the area is free of snow before (or very soon after) the birds arrive in mid-late October. We visited Cape Bird each summer from 1967168 to 1981182 (except 1976/77) and again in 1987188, for periods of 3 - 14 weeks between 22 October and 15 February (Appendix 1). Many aspects of the biology of the two breeding species (Adelie Penguin and Antarctic Skua) have been described elsewhere (see review by Young 1981; also Davis 1988, Davis et al. -
Concentrations, Particle-Size Distributions, and Dry Deposition fluxes of Aerosol Trace Elements Over the Antarctic Peninsula in Austral Summer
Atmos. Chem. Phys., 21, 2105–2124, 2021 https://doi.org/10.5194/acp-21-2105-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Concentrations, particle-size distributions, and dry deposition fluxes of aerosol trace elements over the Antarctic Peninsula in austral summer Songyun Fan1, Yuan Gao1, Robert M. Sherrell2, Shun Yu1, and Kaixuan Bu2 1Department of Earth and Environmental Sciences, Rutgers University, Newark, NJ 07102, USA 2Department of Marine and Coastal Sciences, Rutgers University, New Brunswick, NJ 08901, USA Correspondence: Yuan Gao ([email protected]) Received: 1 July 2020 – Discussion started: 26 August 2020 Revised: 3 December 2020 – Accepted: 8 December 2020 – Published: 12 February 2021 Abstract. Size-segregated particulate air samples were col- sition processes may play a minor role in determining trace lected during the austral summer of 2016–2017 at Palmer element concentrations in surface seawater over the conti- Station on Anvers Island, western Antarctic Peninsula, to nental shelf of the western Antarctic Peninsula. characterize trace elements in aerosols. Trace elements in aerosol samples – including Al, P, Ca, Ti, V, Mn, Ni, Cu, Zn, Ce, and Pb – were determined by total digestion and a 1 Introduction sector field inductively coupled plasma mass spectrometer (SF-ICP-MS). The crustal enrichment factors (EFcrust) and Aerosols affect the climate through direct and indirect ra- k-means clustering results of particle-size distributions show diative forcing (Kaufman et al., 2002). The extent of such that these elements are derived primarily from three sources: forcing depends on both physical and chemical properties (1) regional crustal emissions, including possible resuspen- of aerosols, including particle size and chemical composi- sion of soils containing biogenic P, (2) long-range transport, tion (Pilinis et al., 1995). -
A NEWS BULLETIN Published Quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC)
A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) An English-born Post Office technician, Robin Hodgson, wearing a borrowed kilt, plays his pipes to huskies on the sea ice below Scott Base. So far he has had a cool response to his music from his New Zealand colleagues, and a noisy reception f r o m a l l 2 0 h u s k i e s . , „ _ . Antarctic Division photo Registered at Post Ollice Headquarters. Wellington. New Zealand, as a magazine. II '1.7 ^ I -!^I*"JTr -.*><\\>! »7^7 mm SOUTH GEORGIA, SOUTH SANDWICH Is- . C I R C L E / SOUTH ORKNEY Is x \ /o Orcadas arg Sanae s a Noydiazarevskaya ussr FALKLAND Is /6Signyl.uK , .60"W / SOUTH AMERICA tf Borga / S A A - S O U T H « A WEDDELL SHETLAND^fU / I s / Halley Bav3 MINING MAU0 LAN0 ENOERBY J /SEA uk'/COATS Ld / LAND T> ANTARCTIC ••?l\W Dr^hnaya^^General Belgrano arg / V ^ M a w s o n \ MAC ROBERTSON LAND\ '■ aust \ /PENINSULA' *\4- (see map betowi jrV^ Sobldl ARG 90-w {■ — Siple USA j. Amundsen-Scott / queen MARY LAND {Mirny ELLSWORTH" LAND 1, 1 1 °Vostok ussr MARIE BYRD L LAND WILKES LAND ouiiiv_. , ROSS|NZJ Y/lnda^Z / SEA I#V/VICTORIA .TERRE , **•»./ LAND \ /"AOELIE-V Leningradskaya .V USSR,-'' \ --- — -"'BALLENYIj ANTARCTIC PENINSULA 1 Tenitnte Matianzo arg 2 Esptrarua arg 3 Almirarrta Brown arc 4PttrtlAHG 5 Otcipcion arg 6 Vtcecomodoro Marambio arg * ANTARCTICA 7 Arturo Prat chile 8 Bernardo O'Higgins chile 1000 Miles 9 Prasid«fTtB Frei chile s 1000 Kilometres 10 Stonington I. -
Ice Core Records As Sea Ice Proxies: an Evaluation from the Weddell Sea Region of Antarctica Nerilie J
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 112, D15101, doi:10.1029/2006JD008139, 2007 Click Here for Full Article Ice core records as sea ice proxies: An evaluation from the Weddell Sea region of Antarctica Nerilie J. Abram,1 Robert Mulvaney,1 Eric W. Wolff,1 and Manfred Mudelsee2,3 Received 12 October 2006; revised 2 May 2007; accepted 5 June 2007; published 3 August 2007. [1] Ice core records of methanesulfonic acid (MSA) from three sites around the Weddell Sea are investigated for their potential as sea ice proxies. It is found that the amount of MSA reaching the ice core sites decreases following years of increased winter sea ice in the Weddell Sea; opposite to the expected relationship if MSA is to be used as a sea ice proxy. It is also shown that this negative MSA-sea ice relationship cannot be explained by the influence that the extensive summer ice pack in the Weddell Sea has on MSA production area and transport distance. A historical record of sea ice from the northern Weddell Sea shows that the negative relationship between MSA and winter sea ice exists over interannual (7-year period) and multidecadal (20-year period) timescales. National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis data suggest that this negative relationship is most likely due to variations in the strength of cold offshore wind anomalies traveling across the Weddell Sea, which act to synergistically increase sea ice extent (SIE) while decreasing MSA delivery to the ice core sites. Hence our findings show that in some locations atmospheric transport strength, rather than sea ice conditions, is the dominant factor that determines the MSA signal preserved in near-coastal ice cores. -
Dissertação O Processo Político Das Políticas Públicas Para As
O Processo Político de Construção das Políticas Públicas para as Alterações Climáticas José Carlos Martinho da Silva Dissertação de Mestrado em Sociologia - Políticas Públicas e NomeDesigualdades Completo do Sociais Autor Maio de 2019 Resumo As alterações climáticas de origem antropogénica constituem um problema ambiental sobre o qual se desenvolveram desde a década de 90 políticas públicas e tratados internacionais de grande relevância. O peso desta problemática nas agendas políticas e mediáticas tem sido crescente em diversas nações, inclusive em Portugal e na União Europeia (UE). Com efeito, a UE constitui-se hoje como um dos principais agentes mobilizados e mobilizadores de políticas sobre esta problemática, com políticas públicas robustas implementadas no contexto do protocolo de Quioto e de outras decisões tomadas na Convenção Quadro das Nações Unidas para as Alterações Climáticas. A ação internacional mais recente e ambiciosa promovida no âmbito da Convenção, ocorreu em 2015, o Acordo de Paris, mas foi recebida por uma renovada e estruturada oposição, nomeadamente a dos Estados Unidos da América (EUA), que com a sua saída do Acordo, despoletou desenvolvimentos imprevisíveis que representam atualmente um foco de preocupação e controvérsia, intensificando as interrogações face a um problema, que politicamente se veio a consolidar num desenho de políticas públicas com fortes implicações em diferentes áreas económicas, sociais e geopolíticas das diferentes nações e agrupamentos regionais representados na Convenção. Este trabalho procura abordar o problema político como um processo, e sobre este, desenvolver uma análise sociológica, tendo como enquadramento teórico a teoria de campo de Pierre Bourdieu. O foco deste trabalho foi o de compreender o início deste processo, eventualmente lançando as bases para um estudo posterior que alcance as suas diferentes fases, até ao momento presente. -
Representations of Antarctic Exploration by Lesser Known Heroic Era Photographers
Filtering ‘ways of seeing’ through their lenses: representations of Antarctic exploration by lesser known Heroic Era photographers. Patricia Margaret Millar B.A. (1972), B.Ed. (Hons) (1999), Ph.D. (Ed.) (2005), B.Ant.Stud. (Hons) (2009) Submitted in fulfilment of the requirements for the Degree of Master of Science – Social Sciences. University of Tasmania 2013 This thesis contains no material which has been accepted for a degree or diploma by the University or any other institution, except by way of background information and duly acknowledged in the thesis, and to the best of my knowledge and belief no material previously published or written by another person except where due acknowledgement is made in the text of the thesis. ………………………………….. ………………….. Patricia Margaret Millar Date This thesis may be made available for loan and limited copying in accordance with the Copyright Act 1968. ………………………………….. ………………….. Patricia Margaret Millar Date ii Abstract Photographers made a major contribution to the recording of the Heroic Era of Antarctic exploration. By far the best known photographers were the professionals, Herbert Ponting and Frank Hurley, hired to photograph British and Australasian expeditions. But a great number of photographs were also taken on Belgian, German, Swedish, French, Norwegian and Japanese expeditions. These were taken by amateurs, sometimes designated official photographers, often scientists recording their research. Apart from a few Pole-reaching images from the Norwegian expedition, these lesser known expedition photographers and their work seldom feature in the scholarly literature on the Heroic Era, but they, too, have their importance. They played a vital role in the growing understanding and advancement of Antarctic science; they provided visual evidence of their nation’s determination to penetrate the polar unknown; and they played a formative role in public perceptions of Antarctic geopolitics. -
Management Plan for Antarctic Specially Protected Area No. 116 NEW COLLEGE VALLEY, CAUGHLEY BEACH, CAPE BIRD, ROSS ISLAND
Management Plan For Antarctic Specially Protected Area No. 116 NEW COLLEGE VALLEY, CAUGHLEY BEACH, CAPE BIRD, ROSS ISLAND 1. Description of values to be protected In 1985, two areas at Cape Bird, Ross Island were designated as SSSI No. 10, Caughley Beach (Recommendation XIII-8 (1985)) and SPA No. 20, New College Valley (Recommendation XIII-12 (1985)), following proposals by New Zealand that these areas should be protected because they contained some of the richest stands of moss and associated microflora and fauna in the Ross Sea region of Antarctica. This is the only area on Ross Island where protection is specifically given to plant assemblages and associated ecosystems. At that time, SPA No. 20 was enclosed within SSSI No. 10, in order to provide more stringent access conditions to that part of the Area. In 2000, SSSI No. 10 was incorporated with SPA No. 20 by Measure 1 (2000), with the former area covered by SPA No. 20 becoming a Restricted Zone within the revised SPA No. 20. The boundaries of the Area were revised from the boundaries in the original recommendations, in view of improved mapping and to follow more closely the ridges enclosing the catchment of New College Valley. Caughley Beach itself was adjacent to, but never a part of, the original Area, and for this reason the entire Area was renamed as New College Valley, which was within both of the original sites. The Area was redesignated by Decision 1 (2002) as Antarctic Specially Protected Area (ASPA) No. 116 and a revised Management Plan was adopted through Measure 1 (2006). -
Observation of Ocean Tides Below the Filchner
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 105, NO. C8, PAGES 19,615-19,630,AUGUST 15, 2000 Observation of ocean tides below the Filchher and Ronne Ice Shelves, Antarctica, using synthetic aperture radar interferometry' Comparison with tide model predictions E. Rignot,1 L. Padman,•' D. R. MacAyeal,3 and M. Schmeltz1 Abstract. Tides near and under floating glacial ice, such as ice shelvesand glacier termini in fjords, can influence heat transport into the subice cavity, mixing of the under-ice water column, and the calving and subsequentdrift of icebergs. Free- surface displacementpatterns associatedwith ocean variability below glacial ice can be observedby differencingtwo syntheticaperture radar (SAR) interferograms, each of which representsthe combination of the displacement patterns associated with the time-varying vertical motion and the time-independent lateral ice flow. We present the pattern of net free-surface displacement for the iceberg calving regions of the Ronne and Filchher Ice Shelves in the southern Weddell Sea. By comparing SAR-based displacementfields with ocean tidal models, the free-surface displacementvariability for these regions is found to be dominated by ocean tides. The inverse barometer effect, i.e., the ocean's isostatic responseto changing atmospheric pressure, also contributes to the observed vertical displacement. The principal value of using SAR interferometry in this manner lies in the very high lateral resolution(tens of meters) obtainedover the large regioncovered by each SAR image. Small features that are not well resolvedby the typical grid spacing of ocean tidal models may contribute to such processesas iceberg calving and cross-frontalventilation of the ocean cavity under the ice shelf. -
A News Bulletin New Zealand, Antarctic Society
A NEWS BULLETIN published quarterly by the NEW ZEALAND, ANTARCTIC SOCIETY INVETERATE ENEMIES A penguin chick bold enough to frighten off all but the most severe skua attacks. Photo: J. T. Darby. Vol. 4. No.9 MARCH. 1967 AUSTRALIA WintQr and Summer bAsts Scott Summer ila..se enly t Hal'ett" Tr.lnsferrea ba.se Will(,t~ U.S.foAust T.mporArily nen -eper&tianaJ....K5yow... •- Marion I. (J.A) f.o·W. H.I.M.S.161 O_AWN IY DEPARTMENT OF LANDS fa SU_VEY WILLINGTON) NEW ZEALAND! MAR. .•,'* N O l. • EDI"'ON (Successor to IIAntarctic News Bulletin") Vol. 4, No.9 MARCH, 1967 Editor: L. B. Quartermain, M.A., 1 Ariki Road, Wellington, E.2, ew Zealand. Assistant Editor: Mrs R. H. Wheeler. Business Communications, Subscriptions, etc., to: Secretary, ew Zealand Antarctic Society, P.O. Box 2110, Wellington, .Z. CONTENTS EXPEDITIONS Page New Zealand 430 New Zealand's First Decade in Antarctica: D. N. Webb 430 'Mariner Glacier Geological Survey: J. E. S. Lawrence 436 The Long Hot Summer. Cape Bird 1966-67: E. C. Young 440 U.S.S.R. ...... 452 Third Kiwi visits Vostok: Colin Clark 454 Japan 455 ArgenHna 456 South Africa 456 France 458 United Kingdom 461 Chile 463 Belgium-Holland 464 Australia 465 U.S.A. ...... 467 Sub-Antarctic Islands 473 International Conferences 457 The Whalers 460 Bookshelf ...... 475 "Antarctica": Mary Greeks 478 50 Years Ago 479 430 ANTARCTI'C March. 1967 NEW ZEALAND'S FIRST DECAD IN ANTARCTICA by D. N. Webb [The following article was written in the days just before his tragic death by Dexter Norman Webb, who had been appointed Public ReLations Officer, cott Base, for the 1966-1967 summer. -
Distribution of Marine Palynomorphs in Surface Sediments, Prydz Bay, Antarctica
DISTRIBUTION OF MARINE PALYNOMORPHS IN SURFACE SEDIMENTS, PRYDZ BAY, ANTARCTICA Claire Andrea Storkey A thesis submitted to Victoria University of Wellington in fulfilment of the requirements for the degree Masters of Science in geology School of Earth Sciences Victoria University of Wellington April 2006 ABSTRACT Prydz Bay Antarctica is an embayment situated at the ocean-ward end of the Lambert Glacier/Amery Ice Shelf complex East Antarctica. This study aims to document the palynological assemblages of 58 surface sediment samples from Prydz Bay, and to compare these assemblages with ancient palynomorph assemblages recovered from strata sampled by drilling projects in and around the bay. Since the early Oligocene, terrestrial and marine sediments from the Lambert Graben and the inner shelf areas in Prydz Bay have been the target of significant glacial erosion. Repeated ice shelf advances towards the edge of the continental shelf redistributed these sediments, reworking them into the outer shelf and Prydz Channel Fan. These areas consist mostly of reworked sediments, and grain size analysis shows that finer sediments are found in the deeper parts of the inner shelf and the deepest areas on the Prydz Channel Fan. Circulation within Prydz Bay is dominated by a clockwise rotating gyre which, together with coastal currents and ice berg ploughing modifies the sediments of the bay, resulting in the winnowing out of the finer component of the sediment. Glacial erosion and reworking of sediments has created four differing environments (Prydz Channel Fan, North Shelf, Mid Shelf and Coastal areas) in Prydz Bay which is reflected in the palynomorph distribution. Assemblages consist of Holocene palynomorphs recovered mostly from the Mid Shelf and Coastal areas and reworked palynomorphs recovered mostly from the North Shelf and Prydz Channel Fan. -
Polar Geography the Historical Development of Mcmurdo Station
This article was downloaded by: [Texas A&M University] On: 19 August 2010 Access details: Access Details: [subscription number 915031382] Publisher Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37- 41 Mortimer Street, London W1T 3JH, UK Polar Geography Publication details, including instructions for authors and subscription information: http://www.informaworld.com/smpp/title~content=t781223423 The historical development of McMurdo station, Antarctica, an environmental perspective Andrew G. Kleina; Mahlon C. Kennicutt IIb; Gary A. Wolffb; Steve T. Sweetb; Tiffany Bloxoma; Dianna A. Gielstraa; Marietta Cleckleyc a Department of Geography, Texas A&M University, College Station, TX, USA b Geochemical and Environmental Research Group, Texas A&M, College Station, TX, USA c Uniondale High School, Uniondale, New York, USA To cite this Article Klein, Andrew G. , Kennicutt II, Mahlon C. , Wolff, Gary A. , Sweet, Steve T. , Bloxom, Tiffany , Gielstra, Dianna A. and Cleckley, Marietta(2008) 'The historical development of McMurdo station, Antarctica, an environmental perspective', Polar Geography, 31: 3, 119 — 144 To link to this Article: DOI: 10.1080/10889370802579856 URL: http://dx.doi.org/10.1080/10889370802579856 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.informaworld.com/terms-and-conditions-of-access.pdf This article may be used for research, teaching and private study purposes. Any substantial or systematic reproduction, re-distribution, re-selling, loan or sub-licensing, systematic supply or distribution in any form to anyone is expressly forbidden. The publisher does not give any warranty express or implied or make any representation that the contents will be complete or accurate or up to date.