Glaciomarine Sedimentation at the Continental Margin of Prydz Bay, East Antarctica: Implications on Palaeoenvironmental Changes During the Quaternary

Total Page:16

File Type:pdf, Size:1020Kb

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 Published online at the Institutional Repository of the University of Potsdam: URL http://opus.kobv.de/ubp/volltexte/2011/5262/ URN urn:nbn:de:kobv:517‐opus‐52620 http://nbn‐resolving.de/urn:nbn:de:kobv:517‐opus‐52620 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. Dr. Oliver Esper, Dr. Thomas Frederichs and Dr. Rainer Gersonde are acknowledged for close collaboration, quick and straightforward help and a great time during our expedition to the North Pacific. This PhD project was funded by the ‘Deutsche Forschungsgesellschaft’ (DFG) within the scope of priority program 1158 ‘Antarctic research with comparative studies in Arctic ice regions’ through grant DI 655/3-1. During the last years I had the opportunity to be a member of the Potsdam Graduate School (POGS) and the Helmholtz Graduate School for Polar and Marine Research (POLMAR). I like to thank Dr. Claudia Sprengel, Dr. Claudia Hanfland and Dr. Heike Küchmeister for making it possible for me to attend several professional courses. I also thank the German Polar Society (DGP) and SCAR-ACE for travel grants to scientific conferences. For the instruction and support in analytical work I like to express my gratitude to the laboratory staff at AWI Potsdam and AWI Bremerhaven, namely Ute Bastian, Antje Eulenburg, Rita Fröhlking, Norbert Lensch, Ute Bock and Susanne Wiebe. Bernd Hoffmann I and Anna Plotzki amongst other students doing internships at the AWI are acknowledged for their involvement in the sample preparation. Many thanks also to the AWI Potsdam administration, in particular Christine Litz. Thanks to Heiko Gericke and Tobias Schmidt for solving plotter and network problems. Stephan, Boris, Jens, Ulrike – even in an office half the size of ours it would have been a splendid time. I very much enjoyed our A.-coffee breaks, scientific discussions and our “group suffering” from everything that life offers. The open and pleasant atmosphere amongst the young researchers on the Telegrafenberg contributed to a great time over the past years. For many humorous conversations and philosophical talks regarding scientific and non-scientific issues I especially thank Larsen, Jule, Micha, Torsten, Mathias, Thomas, Seb and Seb, Bernhard and Bernhard, Lise, Josi, Ines, Katja, Maria and others. It is a valuable gift to have people close even though they are far away. Uta, Anja and Gregor – I am deeply grateful for lots of talks and, unfortunately, less frequent activities helping me get my mind free. Maike – I am very much indebted to you for a great time and your unwavering support and patience. Most of all, I would like to thank with all my heart my parents and my entire family for their support and encouragement and dedicate this work to them. II Contents Acknowledgements ................................................................................................................. I Contents ..................................................................................................................................... III List of figures ............................................................................................................................ VII List of tables .............................................................................................................................. VIII List of abbreviations ................................................................................................................ IX Abstract ...................................................................................................................................... X Kurzfassung .............................................................................................................................. XII 1. Introduction ......................................................................................................................... 1 1.1 Regional setting ............................................................................................................ 2 1.1.1 Topography ........................................................................................................ 2 1.1.2 Geology ............................................................................................................... 4 1.1.3 Glaciology ........................................................................................................... 4 1.1.4 Oceanography .................................................................................................... 5 1.2 Scientific background .................................................................................................. 6 1.2.1 Long-term dynamics of the East and West Antarctic Ice Sheets since the onset of Antarctic glaciation ............................................................................. 6 1.2.2 Quaternary EAIS dynamics and bottom-water formation at the East Antarctic continental margin ........................................................................... 7 1.2.3 Glacial palaeoenvironments in the Prydz Bay region – State of the art ..... 9 1.3 Objectives of this thesis ............................................................................................... 11 1.4 Scientific approach and methods ............................................................................... 12 1.5 Overview of the manuscripts ..................................................................................... 14 1.6 The author’s contribution to the individual manuscripts ...................................... 16 2. Mineralogy of glaciomarine sediments from the Prydz Bay-Kerguelen region: relation to modern depositional environments ............................................................ 17 2.1 Introduction .................................................................................................................. 18 2.2 Regional setting ............................................................................................................ 19 2.2.1 Oceanography, icebergs and sea ice ................................................................ 21 2.2.2 Geology ............................................................................................................... 21 2.3 Material and methods ................................................................................................. 23 2.4 Results ............................................................................................................................ 25 2.4.1 Clay-mineral assemblages ................................................................................ 25 2.4.2 Heavy-mineral assemblages ............................................................................. 27 III 2.5 Discussion ...................................................................................................................... 30 2.5.1 Clay minerals ...................................................................................................... 30 2.5.2 Heavy minerals .................................................................................................. 38 2.6 Conclusions and outlook ............................................................................................. 40 3. Holocene ice dynamics, bottom-water formation and polynya activity recorded in Burton Basin, East Antarctica ............................................................................................ 43 3.1 Introduction .................................................................................................................. 45 3.2 Study area ...................................................................................................................... 46 3.2.1 Geomorphology ................................................................................................
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Early Neoproterozoic Granulite Facies Metamorphism of Mafic Dykes From
    J. metamorphic Geol., 2014, 32, 1041–1062 doi:10.1111/jmg.12106 Early Neoproterozoic granulite facies metamorphism of mafic dykes from the Vestfold Block, east Antarctica X. C. LIU,1 W.-(R. Z.)WANG,1 Y. ZHAO,1 J. LIU1 AND B. SONG2 1Key Laboratory of Paleomagnetism and Tectonic Reconstruction of Ministry of Land and Resources, Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China ([email protected]) 2Beijing SHRIMP Centre, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China ABSTRACT Proterozoic mafic dykes from the southwestern Vestfold Block experienced heterogeneous granulite facies metamorphism, characterized by spotted or fractured garnet-bearing aggregates in garnet- absent groundmass. The garnet-absent groundmass typically preserves an ophitic texture composed of lathy plagioclase, intergranular clinopyroxene and Fe–Ti oxides. Garnet-bearing domains consist mainly of a metamorphic assemblage of garnet, clinopyroxene, orthopyroxene, hornblende, biotite, plagioclase, K-feldspar, quartz and Fe–Ti oxides. Chemical compositions and textural relationships suggest that these metamorphic minerals reached local equilibrium in the centre of the garnet-bearing domains. Pseudosection calculations in the model system NCFMASHTO (Na2O–CaO–FeO–MgO– Al2O3–SiO2–H2O–TiO2–Fe2O3) yield P–T estimates of 820–870 °C and 8.4–9.7 kbar. Ion microprobe U–Pb zircon dating reveals that the NW- and N-trending mafic dykes were emplaced at 1764 Æ 25 and 1232 Æ 12 Ma, respectively, whereas their metamorphic ages cluster between 957 Æ 7 and 938 Æ 9 Ma. The identification of granulite facies mineral inclusions in metamorphic zircon domains is also consistent with early Neoproterozoic metamorphism.
    [Show full text]
  • 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.
    [Show full text]
  • Prydz Bay Region, East Antarctica J.M
    Antarctic Science 18 (1), 83–99 (2006) © Antarctic Science Ltd Printed in the UK DOI: 10.1017/S0954102006000083 A review of the Cenozoic stratigraphy and glacial history of the Lambert Graben–Prydz Bay region, East Antarctica J.M. WHITEHEAD1*, P.G. QUILTY2, B.C. MCKELVEY3 and P.E. O’BRIEN4 1Institute of Antarctic and Southern Ocean Studies, University of Tasmania, Private Bag 77, Hobart, TAS 7001, Australia 2School of Earth Sciences University of Tasmania, Private Bag 79, Hobart, TAS 7001, Australia 3Division of Earth Sciences, University of New England, Armidale, NSW 2351, Australia 4Geoscience Australia, GPO Box 378, Canberra, ACT 2601, Australia *[email protected] Abstract: The Cenozoic glacial history of East Antarctica is recorded in part by the stratigraphy of the Prydz Bay–Lambert Graben region. The glacigene strata and associated erosion surfaces record at least 10 intervals of glacial advance (with accompanying erosion and sediment compaction), and more than 17 intervals of glacial retreat (enabling open marine deposition in Prydz Bay and the Lambert Graben). The number of glacial advances and retreats is considerably less than would be expected from Milankovitch frequencies due to the incomplete stratigraphic record. Large advances of the Lambert Glacier caused progradation of the continental shelf edge. At times of extreme glacial retreat, marine conditions reached > 450 km inland from the modern ice shelf edge. This review presents a partial reconstruction of Cenozoic glacial extent within Prydz Bay and the Lambert Graben that can be compared to eustatic sea-level records from the southern Australian continental margin. Received 1 December 2004, accepted 15 July 2005 Key words: glaciation, ice sheet, Milankovitch, Prince Charles Mountains Introduction Study area In recent years there has been considerable investigation of This paper reviews the Cenozoic stratigraphy of the the Cenozoic geology of the Lambert Graben and Prydz Antarctic continent and margin from 60°E to 80°E.
    [Show full text]
  • Hiking & Rafting the Alsek River
    Hiking & Rafting the Alsek River 16 Days Hiking & Rafting the Alsek River Ride 160 miles down the Alsek River with three extra days for hiking through the largest contiguous protected wilderness in the world. On this trip, we will also raft Class II-Class IV rapids watching glaciers calve into the water and spotting spectacular wildlife. Camp riverside and enjoy delicious meals while listening to river lore around the campfire. Take a helicopter portage over a risky stretch of river, enjoy optional day hikes up mountain peaks, and float past dense canyon forests. With raw nature on display at every bend, this is a unique pilgrimage for thrill-seekers, through one of the earth's last great frontiers. Details Testimonials Arrive: Haines, Alaska "The Alsek River expedition was a transformative experience!" Depart: Yakutat, Alaska John D. Duration: 16 Days "The Alsek is so unique and special. It is truly wild Group Size: 6–12 Guests and untouched. I am so happy that I could be in that wonderful place." Minimum Age: 16 Years Old Shirley L. Activity Level: . REASON #01 REASON #02 REASON #03 Explore the Alsek River and Raft one of the most legendary Riverside camping features wilderness in this extended rivers in the world with long-time tasty meals and tales told by hiking trip — a rare opportunity MT Sobek experienced river guides seasoned guides around a crackling that no other outfitter offers campfire beneath the stars ACTIVITIES LODGING CLIMATE Spectacular Class II-IV rafting After the first evening in a Enjoy long Alaska days, with along the mighty Alsek River, Victorian-era style hotel, MT potential rain and chilly extended hikes through majestic Sobek riverside camps, with winds near glaciers.
    [Show full text]
  • Investigation of Glacial Dynamics in Lambert Glacial Basin
    INVESTIGATION OF GLACIAL DYNAMICS IN LAMBERT GLACIAL BASIN USING SATELLITE REMOTE SENSING TECHNIQUES A Dissertation by JAEHYUNG YU Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY December 2005 Major Subject: Geography INVESTIGATION OF GLACIAL DYNAMICS IN LAMBERT GLACIAL BASIN USING SATELLITE REMOTE SENSING TECHNIQUES A Dissertation by JAEHYUNG YU Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Approved by: Chair of Committee, Hongxing Liu Committee Members, Andrew G. Klein Vatche P. Tchakerian Mahlon Kennicutt Head of Department, Douglas Sherman December 2005 Major Subject: Geography iii ABSTRACT Investigation of Glacial Dynamics in Lambert Glacial Basin Using Satellite Remote Sensing Techniques. Jaehyung Yu, B.S., Chungnam National University; M.S., Chungnam National University Chair of Advisory Committee: Dr. Hongxing Liu The Antarctic ice sheet mass budget is a very important factor for global sea level. An understanding of the glacial dynamics of the Antarctic ice sheet are essential for mass budget estimation. Utilizing a surface velocity field derived from Radarsat three-pass SAR interferometry, this study has investigated the strain rate, grounding line, balance velocity, and the mass balance of the entire Lambert Glacier – Amery Ice Shelf system, East Antarctica. The surface velocity increases abruptly from 350 m/year to 800 m/year at the main grounding line. It decreases as the main ice stream is floating, and increases to 1200 to 1500 m/year in the ice shelf front.
    [Show full text]
  • 1 Compiled by Mike Wing New Zealand Antarctic Society (Inc
    ANTARCTIC 1 Compiled by Mike Wing US bulldozer, 1: 202, 340, 12: 54, New Zealand Antarctic Society (Inc) ACECRC, see Antarctic Climate & Ecosystems Cooperation Research Centre Volume 1-26: June 2009 Acevedo, Capitan. A.O. 4: 36, Ackerman, Piers, 21: 16, Vessel names are shown viz: “Aconcagua” Ackroyd, Lieut. F: 1: 307, All book reviews are shown under ‘Book Reviews’ Ackroyd-Kelly, J. W., 10: 279, All Universities are shown under ‘Universities’ “Aconcagua”, 1: 261 Aircraft types appear under Aircraft. Acta Palaeontolegica Polonica, 25: 64, Obituaries & Tributes are shown under 'Obituaries', ACZP, see Antarctic Convergence Zone Project see also individual names. Adam, Dieter, 13: 6, 287, Adam, Dr James, 1: 227, 241, 280, Vol 20 page numbers 27-36 are shared by both Adams, Chris, 11: 198, 274, 12: 331, 396, double issues 1&2 and 3&4. Those in double issue Adams, Dieter, 12: 294, 3&4 are marked accordingly. Adams, Ian, 1: 71, 99, 167, 229, 263, 330, 2: 23, Adams, J.B., 26: 22, Adams, Lt. R.D., 2: 127, 159, 208, Adams, Sir Jameson Obituary, 3: 76, A Adams Cape, 1: 248, Adams Glacier, 2: 425, Adams Island, 4: 201, 302, “101 In Sung”, f/v, 21: 36, Adamson, R.G. 3: 474-45, 4: 6, 62, 116, 166, 224, ‘A’ Hut restorations, 12: 175, 220, 25: 16, 277, Aaron, Edwin, 11: 55, Adare, Cape - see Hallett Station Abbiss, Jane, 20: 8, Addison, Vicki, 24: 33, Aboa Station, (Finland) 12: 227, 13: 114, Adelaide Island (Base T), see Bases F.I.D.S. Abbott, Dr N.D.
    [Show full text]
  • Coastal Change and Glaciological Map of The
    Prepared in cooperation with the Scott Polar Research Institute, University of Cambridge, United Kingdom Coastal-Change and Glaciological Map of the Amery Ice Shelf Area, Antarctica: 1961–2004 By Kevin M. Foley, Jane G. Ferrigno, Charles Swithinbank, Richard S. Williams, Jr., and Audrey L. Orndorff Pamphlet to accompany Geologic Investigations Series Map I–2600–Q 2013 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2013 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Foley, K.M., Ferrigno, J.G., Swithinbank, Charles, Williams, R.S., Jr., and Orndorff, A.L., 2013, Coastal-change and glaciological map of the Amery Ice Shelf area, Antarctica: 1961–2004: U.S. Geological Survey Geologic Investigations Series Map I–2600–Q, 1 map sheet, 8-p.
    [Show full text]
  • Early Miocene Mollusca from the ANDRILL 2A Core, Mcmurdo Sound
    1 1 EARLY MIOCENE MOLLUSCA FROM MCMURDO SOUND, ANTARCTICA 2 (ANDRILL 2A DRILL CORE), WITH A REVIEW OF ANTARCTIC 3 OLIGOCENE AND NEOGENE PECTINIDAE (BIVALVIA) 4 5 by Alan Beu1 and Marco Taviani2 6 7 1GNS Science, PO Box 30368, Lower Hutt, New Zealand 5040; e-mail: 8 <[email protected]> 9 2Istituto de Scienze Marine-CNR, via Gobetti 101, I-40129 Bologna, Italy; and 10 Woods Hole Oceanographic Institute, 266 Woods Hole Road, MA 02543, USA; e- 11 mail: <[email protected]> 12 13 Typescript received 14 ---------------------------------------------------------------------------------------------------------------- 15 Abstract: Retrotapes andrillorum n. sp., Hiatella cf. arctica (Linnaeus, 1767), ?Yoldia 16 sp. (internal mould), and six taxa of Pectinidae are reported from the Burdigalian 17 section of the ANDRILL 2A core, drilled in McMurdo Sound, Ross Sea. The pectinids 18 are Adamussium cf. jonkersi Quaglio et al., 2010, Antarctipecten n. gen. alanbeui 19 (Jonkers, 2003), Austrochlamys forticosta n. sp., Austrochlamys cf. marisrossensis 20 Jonkers, 2003, Ruthipecten n. gen., n. sp. (not named), and a fragmentary specimen 21 representing an unnamed genus and species. In a revision of Antarctic Pectinidae, 22 Austrochlamys Jonkers, 2003, Ruthipecten n. gen. (proposed for Chlamys 23 (Zygochlamys) tuftsensis Turner, 1967, reported only from Wright Valley and the 24 Vestfold Hills, not present in ANDRILL 2A), Leoclunipecten n. gen. (proposed for 25 Austrochlamys gazdzickii Jonkers, 2003, reported only from Oligocene rocks of King 26 George Island, not present in ANDRILL 2A) and the unnamed genus in ANDRILL 2A 27 are assigned to subfamily Chlamydinae, tribe Chlamydini, whereas Adamussium 28 Thiele, 1934 and Antarctipecten n.
    [Show full text]