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Antarctic Peninsula
Hucke-Gaete, R, Torres, D. & Vallejos, V. 1997c. Entanglement of Antarctic fur seals, Arctocephalus gazella, by marine debris at Cape Shirreff and San Telmo Islets, Livingston Island, Antarctica: 1998-1997. Serie Científica Instituto Antártico Chileno 47: 123-135. Hucke-Gaete, R., Osman, L.P., Moreno, C.A. & Torres, D. 2004. Examining natural population growth from near extinction: the case of the Antarctic fur seal at the South Shetlands, Antarctica. Polar Biology 27 (5): 304–311 Huckstadt, L., Costa, D. P., McDonald, B. I., Tremblay, Y., Crocker, D. E., Goebel, M. E. & Fedak, M. E. 2006. Habitat Selection and Foraging Behavior of Southern Elephant Seals in the Western Antarctic Peninsula. American Geophysical Union, Fall Meeting 2006, abstract #OS33A-1684. INACH (Instituto Antártico Chileno) 2010. Chilean Antarctic Program of Scientific Research 2009-2010. Chilean Antarctic Institute Research Projects Department. Santiago, Chile. Kawaguchi, S., Nicol, S., Taki, K. & Naganobu, M. 2006. Fishing ground selection in the Antarctic krill fishery: Trends in patterns across years, seasons and nations. CCAMLR Science, 13: 117–141. Krause, D. J., Goebel, M. E., Marshall, G. J., & Abernathy, K. (2015). Novel foraging strategies observed in a growing leopard seal (Hydrurga leptonyx) population at Livingston Island, Antarctic Peninsula. Animal Biotelemetry, 3:24. Krause, D.J., Goebel, M.E., Marshall. G.J. & Abernathy, K. In Press. Summer diving and haul-out behavior of leopard seals (Hydrurga leptonyx) near mesopredator breeding colonies at Livingston Island, Antarctic Peninsula. Marine Mammal Science.Leppe, M., Fernandoy, F., Palma-Heldt, S. & Moisan, P 2004. Flora mesozoica en los depósitos morrénicos de cabo Shirreff, isla Livingston, Shetland del Sur, Península Antártica, in Actas del 10º Congreso Geológico Chileno. -
Crary-Henderson Collection, B1962.001
REFERENCE CODE: AkAMH REPOSITORY NAME: Anchorage Museum at Rasmuson Center Bob and Evangeline Atwood Alaska Resource Center 625 C Street Anchorage, AK99501 Phone: 907-929-9235 Fax: 907-929-9233 Email: [email protected] Guide prepared by: Mary Langdon, Volunteer, and Sara Piasecki, Archivist TITLE: Crary-Henderson Collection COLLECTION NUMBER: B1962.001, B1962.001A OVERVIEW OF THE COLLECTION Dates: circa 1885-1930 Extent: 19.25 linear feet Language and Scripts: The collection is in English. Name of creator(s): Will Crary; Nan Henderson; Phinney S. Hunt; Miles Bros.; Lyman; George C. Cantwell; Johnson; L. G. Robertson; Lillie N. Gordon; John E. Worden; W. A. Henderson; H. Schultz; Merl LaVoy; Guy F. Cameron; Eric A. Hegg Administrative/Biographical History: The Crary and Henderson Families lived and worked in the Valdez area during the boom times of the early 1900s. William Halbrook Crary was a prospector and newspaper man born in the 1870s (may be 1873 or 1876). William and his brother Carl N. Crary came to Valdez in 1898. Will was a member of the prospecting party of the Arctic Mining Company; Carl was the captain of the association. The Company staked the “California Placer Claim” on Slate Creek and worked outside of Valdez on the claim. Slate Creek is a tributary of the Chitina River, in the Chistochina District of the Copper River Basin. Will Crary was the first townsite trustee for Valdez. Carl later worked in the pharmaceutical field in Valdez and was also the postmaster. Will married schoolteacher Nan Fitch in Valdez in 1906. Carl died of cancer in 1927 in Portland, Oregon. -
Amanda Bay, Ingrid Christensen Coast, Princess Elizabeth Land, East Antarctica
MEASURE 3 - ANNEX Management Plan for Antarctic Specially Protected Area No 169 AMANDA BAY, INGRID CHRISTENSEN COAST, PRINCESS ELIZABETH LAND, EAST ANTARCTICA Introduction Amanda Bay is located on the Ingrid Christensen Coast of Princess Elizabeth Land, East Antarctica at 69°15' S, 76°49’59.9" E. (Map A). The Antarctic Specially Protected Area (ASPA) is designated to protect the breeding colony of several thousand pairs of emperor penguins annually resident in the south-west corner of Amanda Bay, while providing for continued collection of valuable long- term research and monitoring data and comparative studies with colonies elsewhere in East Antarctica. Only two other emperor penguin colonies along the extensive East Antarctic coastline are protected within ASPAs (ASPA 120, Point Géologie Archipelago and ASPA 167 Haswell Island). Amanda Bay is more easily accessed, from vessels or by vehicle from research stations in the Larsemann Hills and Vestfold Hills, than many other emperor penguin colonies in East Antarctica. This accessibility is advantageous for research purposes, but also creates the potential for human disturbance of the birds. The Antarctic coastline in the vicinity of Amanda Bay was first sighted and named the Ingrid Christensen Coast by Captain Mikkelsen in command of the Norwegian ship Thorshavn on 20 February 1935. Oblique aerial photographs of the coastline were taken by the Lars Christensen expedition in 1937 and by the US Operation Highjump in 1947 for reconnaissance purposes. In the 1954/55 summer, the Australian National Antarctic Research Expedition (ANARE) on the Kista Dan explored the waters of Prydz Bay, and the first recorded landing in the area was made by a sledging party led by Dr. -
Glacio-Lacustrine Aragonite Deposition, Meltwater Evolution And
Antarctic Science 19 (3), 365–372 (2007) & Antarctic Science Ltd 2007 Printed in the UK DOI: 10.1017/S0954102007000466 Glacio-lacustrine aragonite deposition, meltwater evolution and glacial history during isotope stage 3 at Radok Lake, Amery Oasis, northern Prince Charles Mountains, East Antarctica IAN D. GOODWIN1 and JOHN HELLSTROM2 1Environmental and Climate Change Research Group, School of Environmental and Life Sciences, University of Newcastle, Callaghan, NSW 2308, Australia 2School of Earth Sciences, University of Melbourne, Parkville, VIC 3010, Australia [email protected] Abstract: The late Quaternary glacial history of the Amery Oasis, and Prince Charles Mountains is of significant interest because about 10% of the total modern Antarctic ice outflow is discharged via the adjacent Lambert Glacier system. A glacial thrust moraine sequence deposited along the northern shoreline of Radok Lake between 20–10 ka BP, overlies a layer of thin, aragonite crusts which provide important constraints on the glacial history of the Amery Oasis. The modern Radok Lake is fed by the terminal meltwaters of the alpine Battye Glacier. The aragonite crusts were deposited in shallow water of ancestral Radok Lake 53 ka BP,during the A3 warm event in Isotope Stage 3. Oxygen isotope (d18O) analysis of the last glacial-age aragonite crusts 18 indicates that they precipitated from freshwater with a d OSMOW composition of -36%, which is 8% more depleted than the present water (-28%) in Radok Lake. A regional oxygen isotope (d18O) and elevation relationship for snow is used to determine the source of meltwater and glacial ice in Radok Lake during the A3 warm event. -
Boeckella Poppei and Gladioferens Antarcticus I.A.E
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Tasmania Open Access Repository Antarctic Science 15 (4): 439–448 (2003) © Antarctic Science Ltd Printed in the UK DOI: 10.1017/S0954102003001548 Taxonomy, ecology and zoogeography of two East Antarctic freshwater calanoid copepod species: Boeckella poppei and Gladioferens antarcticus I.A.E. BAYLY1,2, J.A.E. GIBSON3,4*, B. WAGNER5 and K.M. SWADLING4 1School of Biological Sciences, Monash University, VIC 3800, Australia 2501 Killiecrankie Rd, Flinders Island, TAS 7255, Australia 3Institute of Antarctic and Southern Ocean Studies, University of Tasmania, Private Bag 77, Hobart, TAS 7001, Australia 4School of Zoology, University of Tasmania, Private Bag 5, Hobart, TAS 7001, Australia 5Institute for Geophysics and Geology, Faculty for Physics and Geoscience, University Leipzig, Talstrasse 35, D-04103 Leipzig, Germany *corresponding author: [email protected] Abstract: New populations of the two species of calanoid copepods known to inhabit freshwater lakes in East Antarctica, Boeckella poppei (Mrázek, 1901) and Gladioferens antarcticus Bayly, 1994, have recently been discovered. The morphology of the populations of B. poppei showed significant differences, notably a reduction in the armature of the male fifth leg, when compared with typical specimens from the Antarctic Peninsula and South America. Gladioferens antarcticus had previously been recorded from a single lake in the Bunger Hills, but has now been recorded from three further lakes in this region. A recent review of Antarctic terrestrial and limnetic zooplankton suggested that neither of these species can be considered an East Antarctic endemic, with B. -
Federal Register/Vol. 84, No. 78/Tuesday, April 23, 2019/Rules
Federal Register / Vol. 84, No. 78 / Tuesday, April 23, 2019 / Rules and Regulations 16791 U.S.C. 3501 et seq., nor does it require Agricultural commodities, Pesticides SUPPLEMENTARY INFORMATION: The any special considerations under and pests, Reporting and recordkeeping Antarctic Conservation Act of 1978, as Executive Order 12898, entitled requirements. amended (‘‘ACA’’) (16 U.S.C. 2401, et ‘‘Federal Actions to Address Dated: April 12, 2019. seq.) implements the Protocol on Environmental Justice in Minority Environmental Protection to the Richard P. Keigwin, Jr., Populations and Low-Income Antarctic Treaty (‘‘the Protocol’’). Populations’’ (59 FR 7629, February 16, Director, Office of Pesticide Programs. Annex V contains provisions for the 1994). Therefore, 40 CFR chapter I is protection of specially designated areas Since tolerances and exemptions that amended as follows: specially managed areas and historic are established on the basis of a petition sites and monuments. Section 2405 of under FFDCA section 408(d), such as PART 180—[AMENDED] title 16 of the ACA directs the Director the tolerance exemption in this action, of the National Science Foundation to ■ do not require the issuance of a 1. The authority citation for part 180 issue such regulations as are necessary proposed rule, the requirements of the continues to read as follows: and appropriate to implement Annex V Regulatory Flexibility Act (5 U.S.C. 601 Authority: 21 U.S.C. 321(q), 346a and 371. to the Protocol. et seq.) do not apply. ■ 2. Add § 180.1365 to subpart D to read The Antarctic Treaty Parties, which This action directly regulates growers, as follows: includes the United States, periodically food processors, food handlers, and food adopt measures to establish, consolidate retailers, not States or tribes. -
Steve Mccutcheon Collection, B1990.014
REFERENCE CODE: AkAMH REPOSITORY NAME: Anchorage Museum at Rasmuson Center Bob and Evangeline Atwood Alaska Resource Center 625 C Street Anchorage, AK 99501 Phone: 907-929-9235 Fax: 907-929-9233 Email: [email protected] Guide prepared by: Sara Piasecki, Archivist TITLE: Steve McCutcheon Collection COLLECTION NUMBER: B1990.014 OVERVIEW OF THE COLLECTION Dates: circa 1890-1990 Extent: approximately 180 linear feet Language and Scripts: The collection is in English. Name of creator(s): Steve McCutcheon, P.S. Hunt, Sydney Laurence, Lomen Brothers, Don C. Knudsen, Dolores Roguszka, Phyllis Mithassel, Alyeska Pipeline Services Co., Frank Flavin, Jim Cacia, Randy Smith, Don Horter Administrative/Biographical History: Stephen Douglas McCutcheon was born in the small town of Cordova, AK, in 1911, just three years after the first city lots were sold at auction. In 1915, the family relocated to Anchorage, which was then just a tent city thrown up to house workers on the Alaska Railroad. McCutcheon began taking photographs as a young boy, but it wasn’t until he found himself in the small town of Curry, AK, working as a night roundhouse foreman for the railroad that he set out to teach himself the art and science of photography. As a Deputy U.S. Marshall in Valdez in 1940-1941, McCutcheon honed his skills as an evidential photographer; as assistant commissioner in the state’s new Dept. of Labor, McCutcheon documented the cannery industry in Unalaska. From 1942 to 1944, he worked as district manager for the federal Office of Price Administration in Fairbanks, taking photographs of trading stations, communities and residents of northern Alaska; he sent an album of these photos to Washington, D.C., “to show them,” he said, “that things that applied in the South 48 didn’t necessarily apply to Alaska.” 1 1 Emanuel, Richard P. -
Boeckella Poppei and Gladioferens Antarcticus I.A.E
Antarctic Science 15 (4): 439–448 (2003) © Antarctic Science Ltd Printed in the UK DOI: 10.1017/S0954102003001548 Taxonomy, ecology and zoogeography of two East Antarctic freshwater calanoid copepod species: Boeckella poppei and Gladioferens antarcticus I.A.E. BAYLY1,2, J.A.E. GIBSON3,4*, B. WAGNER5 and K.M. SWADLING4 1School of Biological Sciences, Monash University, VIC 3800, Australia 2501 Killiecrankie Rd, Flinders Island, TAS 7255, Australia 3Institute of Antarctic and Southern Ocean Studies, University of Tasmania, Private Bag 77, Hobart, TAS 7001, Australia 4School of Zoology, University of Tasmania, Private Bag 5, Hobart, TAS 7001, Australia 5Institute for Geophysics and Geology, Faculty for Physics and Geoscience, University Leipzig, Talstrasse 35, D-04103 Leipzig, Germany *corresponding author: [email protected] Abstract: New populations of the two species of calanoid copepods known to inhabit freshwater lakes in East Antarctica, Boeckella poppei (Mrázek, 1901) and Gladioferens antarcticus Bayly, 1994, have recently been discovered. The morphology of the populations of B. poppei showed significant differences, notably a reduction in the armature of the male fifth leg, when compared with typical specimens from the Antarctic Peninsula and South America. Gladioferens antarcticus had previously been recorded from a single lake in the Bunger Hills, but has now been recorded from three further lakes in this region. A recent review of Antarctic terrestrial and limnetic zooplankton suggested that neither of these species can be considered an East Antarctic endemic, with B. poppei being listed as a recent anthropogenic introduction and G. antarcticus a ‘marine interloper’. We conclude differently: B. poppei has been present in isolated populations in East Antarctica for significant lengths of time, possibly predating the current interglacial, while G. -
Flow of the Amery Ice Shelf and Its Tributary Glaciers
18th Australasian Fluid Mechanics Conference Launceston, Australia 3-7 December 2012 Flow of the Amery Ice Shelf and its Tributary Glaciers M. L. Pittard1 2 , J. L. Roberts3 2, R. C. Warner3 2, B.K Galton-Fenzi2, C.S. Watson4 and R. Coleman1 1Institute for Marine and Antarctic Studies University of Tasmania, Private Bag 129, Hobart, Tasmania 7001, Australia 2Antarctic Climate & Ecosystems Cooperative Research Centre University of Tasmania, Private Bag 80, Hobart, Tasmania 7001, Australia 3Department of Sustainability, Environment, Water, Population and Communities, Australian Antarctic Division Hobart, Tasmania, Australia 4 School of Geography and Environmental Studies University of Tasmania, Private Bag 76, Hobart, Tasmania 7001, Australia Abstract thickness across the grounding zone to provide information on ice discharge. Strain rates and vorticity can be used to investi- The Amery Ice Shelf (AIS) is a major ice shelf that drains ap- gate the dynamics of the flow. The longitudinal strain rate gives proximately 16% of the East Antarctic Ice Sheet [1]. Here we insight into the way the velocity changes along the flow and use a sequence of visible spectrum Landsat7 satellite images may reflect influences of features beneath the ice. The shear to track persistent surface features over the southern portion of component of the strain rate highlights the localisation of shear the AIS and its three major tributary glaciers. A spatially in- stresses at the margin of the flow. Vorticity displays a combina- complete velocity field is calculated by comparing the distances tion of rotation in flow direction and strong shear deformations. features have moved between image pairs. Key features of the flow field including the vorticity and strain rate distributions are The AIS is one of the largest ice shelves bordering the East discussed. -
Protecting the Crown: a Century of Resource Management in Glacier National Park
Protecting the Crown A Century of Resource Management in Glacier National Park Rocky Mountains Cooperative Ecosystem Studies Unit (RM-CESU) RM-CESU Cooperative Agreement H2380040001 (WASO) RM-CESU Task Agreement J1434080053 Theodore Catton, Principal Investigator University of Montana Department of History Missoula, Montana 59812 Diane Krahe, Researcher University of Montana Department of History Missoula, Montana 59812 Deirdre K. Shaw NPS Key Official and Curator Glacier National Park West Glacier, Montana 59936 June 2011 Table of Contents List of Maps and Photographs v Introduction: Protecting the Crown 1 Chapter 1: A Homeland and a Frontier 5 Chapter 2: A Reservoir of Nature 23 Chapter 3: A Complete Sanctuary 57 Chapter 4: A Vignette of Primitive America 103 Chapter 5: A Sustainable Ecosystem 179 Conclusion: Preserving Different Natures 245 Bibliography 249 Index 261 List of Maps and Photographs MAPS Glacier National Park 22 Threats to Glacier National Park 168 PHOTOGRAPHS Cover - hikers going to Grinnell Glacier, 1930s, HPC 001581 Introduction – Three buses on Going-to-the-Sun Road, 1937, GNPA 11829 1 1.1 Two Cultural Legacies – McDonald family, GNPA 64 5 1.2 Indian Use and Occupancy – unidentified couple by lake, GNPA 24 7 1.3 Scientific Exploration – George B. Grinnell, Web 12 1.4 New Forms of Resource Use – group with stringer of fish, GNPA 551 14 2.1 A Foundation in Law – ranger at check station, GNPA 2874 23 2.2 An Emphasis on Law Enforcement – two park employees on hotel porch, 1915 HPC 001037 25 2.3 Stocking the Park – men with dead mountain lions, GNPA 9199 31 2.4 Balancing Preservation and Use – road-building contractors, 1924, GNPA 304 40 2.5 Forest Protection – Half Moon Fire, 1929, GNPA 11818 45 2.6 Properties on Lake McDonald – cabin in Apgar, Web 54 3.1 A Background of Construction – gas shovel, GTSR, 1937, GNPA 11647 57 3.2 Wildlife Studies in the 1930s – George M. -
Glaciomarine Sedimentation at the Continental Margin of Prydz Bay, East Antarctica: Implications on Palaeoenvironmental Changes During the Quaternary
Alfred-Wegener-Institut für Polar- und Meeresforschung Universität Potsdam, Institut für Erd- und Umweltwissenschaften Glaciomarine sedimentation at the continental margin of Prydz Bay, East Antarctica: implications on palaeoenvironmental changes during the Quaternary Dissertation zur Erlangung des akademischen Grades Doktor der Naturwissenschaften (Dr. rer. nat.) in der Wissenschaftsdisziplin “Geowissenschaften” eingereicht an der Mathematisch-Naturwissenschaftlichen Fakultät der Universität Potsdam von Andreas Borchers Potsdam, 30. November 2010 Das Höchste, wozu der Mensch gelangen kann, ist das Erstaunen. J. W. von Goethe Acknowledgements This dissertation would not have been possible without the support and help of numerous people to whom I would like to express my gratitude. First, I am highly indebted to PD Dr. Bernhard Diekmann for the possibility to conduct this work under his supervision and for his constant support, whenever discussion or advice was needed. I appreciated his vast expertise and knowledge of marine geology, sedimentology and Quaternary Science that he so enthusiastically shared with me, adding considerably to my experience. Besides being a full-hearted geologist, he is also a great guitarist, which I enjoyed during the past years, especially during the expeditions I had the chance to participate. I would also like to thank Prof. Dr. Hans-Wolfgang Hubberten for his general support and understanding, giving me the opportunity to broaden my knowledge of marine geology in the field. Using the infrastructure of the institute in Potsdam, Bremerhaven and on the world’s oceans has made a major contribution realizing this work. I am deeply grateful to Prof. Dr. Ulrike Herzschuh and Dr. Gerhard Kuhn who provided a large part of assistance by discussions, constructive advices and moral support. -
History of Benthic Colonisation Beneath the Amery Ice Shelf, East Antarctica
Vol. 344: 29–37, 2007 MARINE ECOLOGY PROGRESS SERIES Published August 23 doi: 10.3354/meps06966 Mar Ecol Prog Ser History of benthic colonisation beneath the Amery Ice Shelf, East Antarctica Alexandra L. Post1,*, Mark A. Hemer1, Philip E. O’Brien1, Donna Roberts2, Mike Craven3 1Marine and Coastal Environment Group, Geoscience Australia, GPO Box 378, Canberra, ACT 2601, Australia 2Institute of Antarctic and Southern Ocean Studies, University of Tasmania, Private Bag 77, Hobart, Tasmania 7001, Australia 3Australian Antarctic Division and Antarctic Climate and Ecosystems Co-operative Research Centre, Private Bag 80, Hobart, Tasmania 7001, Australia ABSTRACT: This study presents compelling evidence for a diverse and abundant seabed community that developed over the course of the Holocene beneath the Amery Ice Shelf, East Antarctica. Fossil analysis of a 47 cm long sediment core revealed a rich modern fauna dominated by filter feeders (sponges and bryozoans). The down-core assemblage indicated a succession in the colonisation of this site. The lower portion of the core (before ~9600 yr BP) was completely devoid of preserved fauna. The first colonisers (at ~10 200 yr BP) were mobile benthic organisms. Their occurrence was matched by the first appearance of planktonic taxa, indicating a retreat of the ice shelf following the last glaciation to within sufficient distance to advect planktonic particles via bottom currents. The benthic infauna and filter feeders emerged during the peak abundance of the planktonic organisms, indicating their dependence on the food supply sourced from the open shelf waters of Prydz Bay. Understanding patterns of species succession in this environment has important implications for determining the potential significance of future ice shelf collapse.