Hostname: page-component-cd9895bd7-7cvxr Total loading time: 0 Render date: 2024-12-28T18:22:45.044Z Has data issue: false hasContentIssue false

Geomorphology and glacial history of Rauer Group, East Antarctica

Published online by Cambridge University Press:  20 January 2017

Duanne A. White*
Affiliation:
Department of Physical Geography, Macquarie University, NSW 2109, Australia
Ole Bennike
Affiliation:
Geological Survey of Denmark and Greenland, Copenhagen, Denmark
Sonja Berg
Affiliation:
Institute for Geology and Mineralogy, University of Cologne, 50674 Cologne, Germany
Simon L. Harley
Affiliation:
School of Geosciences, The University of Edinburgh, Edinburgh, Scotland
David Fink
Affiliation:
Australian Nuclear Science and Technology Organisation (ANSTO), PMB 1, Sydney, NSW 2234, Australia
Kevin Kiernan
Affiliation:
School of Geography and Environmental Studies, University of Tasmania, Sandy Bay, Tasmania, 7005, Australia
Anne McConnell
Affiliation:
School of Geography and Environmental Studies, University of Tasmania, Sandy Bay, Tasmania, 7005, Australia
Bernd Wagner
Affiliation:
Institute for Geology and Mineralogy, University of Cologne, 50674 Cologne, Germany
*
Corresponding author. Tel.: +61 2 9850 6835.

E-mail address: [email protected] (D.A. White).

Abstract

The presence of glacial sediments across the Rauer Group indicates that the East Antarctic ice sheet formerly covered the entire archipelago and has since retreated at least 15 km from its maximum extent. The degree of weathering of these glacial sediments suggests that ice retreat from this maximum position occurred sometime during the latter half of the last glacial cycle. Following this phase of retreat, the ice sheet margin has not expanded more than ∼ 1 km seaward of its present position. This pattern of ice sheet change matches that recorded in Vestfold Hills, providing further evidence that the diminutive Marine Isotope Stage 2 ice sheet advance in the nearby Larsemann Hills may have been influenced by local factors rather than a regional ice-sheet response to climate and sea-level change.

Type
Research Article
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Adamson, D.A., and Pickard, J. Cainozoic history of the Vestfold Hills. Pickard, J. Antarctic Oasis, Terrestrial Environments and History of the Vestfold Hills. (1986). Academic Press, Sydney. 6397.Google Scholar
Adamson, D.A., and Pickard, J. Physiography and geomorphology of the Vestfold Hills. Pickard, J. Antarctic Oasis, Terrestrial Environments and History of the Vestfold Hills. (1986). Academic Press, Sydney. 99139.Google Scholar
Augustinus, P.C. Weathering characteristics of the glacial drifts, Bunger Hills, east Antarctica. Arctic, Antarctic and Alpine Research 34, (2002). 6575.CrossRefGoogle Scholar
Australian Bureau of Meteorology, http://www.bom.gov.au/climate/averages/tables/cw_30 0000.shtml. Accessed 11 May 2007.Google Scholar
Berg, S., Wagner, B., White, D.A., Cremer, H., Bennike, O., Melles, M., in press. New marine core record of Late Pleistocene glaciation history, Rauer Group, East Antarctica. Antarctic Science. doi:10.1017/S0954102009001886.CrossRefGoogle Scholar
Blandford, D.C., (1975). Spatial and temporal patterns of contemporary geomorphic processes in the Vestfold Hills, Antarctica. BLitt. thesis, University of New England (Australia), .Google Scholar
Burgess, J., Spate, A., and Shevlin, J. The onset of deglaciation in the Larsemann Hills, eastern Antarctica. Antarctic Science 6, (1994). 491495.CrossRefGoogle Scholar
Child, D., Elliot, G., Misfud, C., Smith, A.M., and Fink, D. Sample processing for earth science studies at ANTARES. Nuclear Instruments and Method in Physics Research B 172, (2000). 856860.CrossRefGoogle Scholar
Domack, E., O'Brien, P., Harris, P.T., Taylor, F., Quilty, P.G., De Santis, L., and Raker, B. Late Quaternary sediment facies in Prydz Bay, East Antarctica and their relationship to glacial advance onto the continental shelf. Antarctic Science 10, (1998). 236246.CrossRefGoogle Scholar
Fabel, D., Stone, J., Fifield, L.K., and Cresswell, R.G. Deglaciation of the Vestfold Hills, East Antarctica; preliminary evidence from exposure dating of three subglacial erratics. Ricci, C.A. International Symposium on Antarctic Earth Sciences 7, (1997). Terra Antarctica Publication, Siena. 829834.Google Scholar
Fink, D., and Smith, A. An inter-comparison of 10Be and 26Al AMS reference standards and the 10Be half-life. Nuclear Instruments and Methods B 259, (2007). 600609.CrossRefGoogle Scholar
Fink, D., Hotchkis, M.A.C., Hua, Q., Jacobsen, G.E., Smith, A.M., Zoppi, U., Child, D., Mifsud, C., Gaast, H.A. v. d., Williams, A.A., and Williams, M. The ANTARES AMS facility at ANSTO. Nuclear Instruments and Method in Physics Research B 223–224, (2004). 109115.CrossRefGoogle Scholar
Fink, D., McKelvey, B., Hambrey, M.J., Fabel, B., and Brown, R. Pleistocene deglaciation chronology of the Radok Lake basin, Amery Oasis, northern Prince Charles Mountains, Antarctica. Earth and Planetary Science Letters 243, (2006). 229243.CrossRefGoogle Scholar
Goodwin, I.D., and Zweck, C. Glacio-isostasy and glacial ice load at Law Dome, Wilkes Land, East Antarctica. Quaternary Research 53, (2000). 285293.CrossRefGoogle Scholar
Gore, D.B., Pickard, J., Baird, A.S., and Webb, J.A. Glacial Crooked Lake, Vestfold Hills, East Antarctica. Polar Record 32, (1996). 1924.CrossRefGoogle Scholar
Gore, D.B., Rhodes, E.J., Augustinus, P.C., Leishman, M.R., Colhoun, E.A., and Rees-Jones, J. Bunger Hills, East Antarctica: ice free at the Last Glacial Maximum. Geology 29, (2001). 11031106.2.0.CO;2>CrossRefGoogle Scholar
Harley, S.L. Precambrian geological relationships in high-grade gneisses of the Rauer Islands, east Antarctica. Australian Journal of Earth Sciences 34, (1987). 175207.CrossRefGoogle Scholar
Harley, S.L. Proterozoic granulites from the Rauer Group, East Antarctica. I. Decompressional pressure–temperature paths deduced from mafic and felsic gneisses. Journal of Petrology 29, (1988). 10591095.CrossRefGoogle Scholar
Harris, P.T., and O'Brien, P. Bottom currents, sedimentation and ice-sheet retreat facies successions on the Mac Robertson Shelf, East Antarctica. Marine Geology 151, (1998). 4772.CrossRefGoogle Scholar
Hodgson, D.A., Noon, P.E., Vyverman, W., Bryant, C.L., Gore, D.B., Appleby, P., Gilmour, M., Verleyen, E., Sabbe, K., Jones, V.J., Ellis-Evans, J.C., and Wood, P.B. Were the Larsemann Hills ice-free through the last glacial maximum?. Antarctic Science 13, (2001). 440454.CrossRefGoogle Scholar
Hodgson, D.A., Vyverman, W., and Sabbe, K. Limnology and biology of saline lakes in the Rauer Islands, eastern Antarctica. Antarctic Science 13, (2001). 255270.CrossRefGoogle Scholar
Igarashi, A., Harada, N., and Moriwaki, K. Marine fossils of 30–40 ka in raised beach deposits, and late Pleistocene glacial history around Lützow-Holm Bay, East Antarctica. Proceedings of the NIPR Symposium, Antarctic Geoscience 8, (1995). 219229.Google Scholar
Igarashi, A., Miura, H. and Hart, C., (1998). Amino-acid racemization dates of fossil molluscs from raised beach deposits on East Ongul Island and northern part of Langhovde, Lützow-Holm Bay region, East Antarctica. In: The 18th Symposium on Antarctic Geosciences, Program and Abstracts. NIPR: 5961.Google Scholar
Katz, O., Reches, Z., and Roegiers, J.-C. Evaluation of mechanical rock properties using a Schmidt Hammer. International Journal of Rock Mechanics and Mining Sciences 37, (2000). 723728.CrossRefGoogle Scholar
Kiernan, K., Gore, D.B., Fink, D., White, D.A., McConnell, A., Sigurdsson, I.A., in press. Deglaciation and weathering of Larsemann Hills, East Antarctica. Antarctic Science.CrossRefGoogle Scholar
Kulbe, T., Melles, M., Verkulich, S.R., and Pushina, Z.V. East Antarctic climate and environmental variability over the last 9400 years inferred from marine sediments of the Bunger Oasis. Arctic Antarctic and Alpine Research 33, (2001). 223230.CrossRefGoogle Scholar
Leventer, A., Domack, E., Dunbar, R., Pike, J., Stickley, C., Maddison, E., Brachfeld, S., Manley, P., and McClennen, C. Marine sediment record from the East Antarctic margin reveals dynamics of ice sheet recession. GSA Today 16, (2006). 410.CrossRefGoogle Scholar
Mackintosh, A., White, D.A., Fink, D., Gore, D.B., Pickard, J., and Fanning, P.C. Exposure ages from mountain dipsticks in Mac. Robertson Land, East Antarctica, indicate little change in ice-sheet thickness since the Last Glacial Maximum. Geology 35, (2007). 504551.CrossRefGoogle Scholar
Moriwaki, K., Iwata, S., Matsuoka, N., Hasegawa, H., and Hirakawa, K. Weathering stage as a relative age of till in the central Sør-Rondane. Proceedings of the NIPR Symposium on Antarctic Geoscience 7, (1994). 156161.Google Scholar
Pickard, J. The Vestfold Hills: a window on Antarctica. Pickard, J. Antarctic Oasis, Terrestrial Environments and History of the Vestfold Hills. (1986). Academic Press, Sydney. 6398.Google Scholar
Pickard, J., Adamson, D.A., and Health, A. The evolution of Watts Lake, Vestfold Hills, east Antarctica, from marine inlet to freshwater lake. Palaeogeography, Palaeoclimatology, Palaeoecology 53, (1986). 271288.CrossRefGoogle Scholar
Shakesby, R.A., Matthews, J.A., and Owen, G. The Schmidt hammer as a relative-age dating tool and its potential for calibrated-age dating in Holocene glaciated environments. Quaternary Science Reviews 25, (2006). 28462867.CrossRefGoogle Scholar
Spate, A., Burgess, J., and Shevlin, J. Rates of rock surface lowering, Princess Elizabeth Land, eastern Antarctica. Earth Surface Processes and Landforms 20, (1995). 567573.CrossRefGoogle Scholar
Stone, J.O. Air pressure and cosmogenic isotope production. Journal of Geophysical Research, B, Solid Earth and Planets 105, (2000). 23,75323,759.CrossRefGoogle Scholar
Streten, N.A. Climate of the Vestfold Hills. Pickard, J. Antarctic Oasis, Terrestrial Environments and History of the Vestfold Hills. (1986). Academic Press, Sydney. 141164.Google Scholar
Sugden, D.E., Balco, G., Cowdery, S.G., Stone, J.O., and Sass, L.C. Selective glacial erosion and weathering zones in the coastal mountains of Marie Byrd Land, Antarctica. Geomorphology 67, (2005). 317334.CrossRefGoogle Scholar
Verleyen, E., Hodgson, D.A., Milne, G.A., Sabbe, K., and Vyverman, W. Relative sea-level history from the Lambert Glacier region, East Antarctica, and its relation to deglaciation and Holocene glacier readvance. Quaternary Research 63, (2005). 4552.CrossRefGoogle Scholar
White, D.A., (2007). Cenozoic Glacial History and Landscape Evolution of Mac.Robertson Land and the Lambert Glacier-Amery Ice Shelf System, East Antarctica. PhD Thesis, Department of Physical Geography, Macquarie University, Sydney.Google Scholar
Yevteyev, S.A. Marine terraces along the Antarctic coast. Soviet Antarctic Information Bulletin 4, (1962). 7376.Google Scholar
Zwartz, D., (1995). The recent history of the Antarctic Ice Sheet: constraints from sea-level change. PhD Thesis, Research School of Earth Sciences, The Australian National University.Google Scholar
Zwartz, D., Bird, M.I., Stone, J., and Lambeck, K. Holocene sea-level change and ice-sheet history in the Vestfold Hills, East Antarctica. Earth and Planetary Science Letters 155, (1998). 131145.CrossRefGoogle Scholar