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Short Note: New marine core record of Late Pleistocene glaciation history, Rauer Group, East Antarctica

Published online by Cambridge University Press:  04 March 2009

Sonja Berg*
Affiliation:
Institute of Geology and Mineralogy, University of Cologne, Zülpicher Str. 49a, D-50674 Cologne, Germany
Bernd Wagner
Affiliation:
Institute of Geology and Mineralogy, University of Cologne, Zülpicher Str. 49a, D-50674 Cologne, Germany
Duanne A. White
Affiliation:
Department of Physical Geography, Macquarie University, NSW 2109, Australia
Holger Cremer
Affiliation:
TNO Built Environment and Geosciences, Geological Survey of The Netherlands, Princetonlaan 6, 3584 CB Utrecht, The Netherlands
Ole Bennike
Affiliation:
Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark
Martin Melles
Affiliation:
Institute of Geology and Mineralogy, University of Cologne, Zülpicher Str. 49a, D-50674 Cologne, Germany

Extract

The evolution of the East Antarctic Ice Sheet (EAIS) during the Late Quaternary is poorly known, partly because some regions, such as the Prydz Bay vicinity, indicate significant variability in the glaciation patterns (e.g. Domack et al. 1998, Zwartz et al. 1998, Hodgson et al. 2005).

Type
Earth Sciences
Copyright
Copyright © Antarctic Science Ltd 2009

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References

Aharon, P. 1988. Oxygen, carbon and U-series isotopes of aragonites from Vestfold Hills, Antarctica: clues to geochemical processes in subglacial environments. Geochimica et Cosmochimica Acta, 52, 23212331.CrossRefGoogle Scholar
Bird, M.I., Chivas, A.R., Radnell, C.J. & Burton, H.R. 1991. Sedimentological and stable-isotope evolution of lakes in the Vestfold Hills, Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, 84, 109130.CrossRefGoogle Scholar
Domack, E., O'Brien, P., Harris, P., Taylor, F., Quilty, P.G., De Santis, S. & Raker, B. 1998. Late Quaternary sediment facies in Prydz Bay, East Antarctica and their relationship to glacial advance onto the continental shelf. Antarctic Science, 10, 236246.CrossRefGoogle Scholar
Hodgson, D.A., Verleyen, E., Sabbe, K., Squier, A.H., Keely, B.J., Leng, M., Saunders, K.M. & Vyverman, W. 2005. Late Quaternary climate-driven environmental change in the Larsemann Hills, East Antarctica, multi-proxy evidence from a lake sediment core. Quaternary Research, 64, 8399.CrossRefGoogle Scholar
Huybrechts, P. 2002. Sea-level changes at the LGM from ice-dynamic reconstructions of the Greenland and Antarctic ice sheets during the glacial cycles. Quaternary Science Reviews, 21, 203231.CrossRefGoogle Scholar
Leventer, A., Domack, E., Dunbar, R., Pike, J., Stickley, C., Maddison, E., Brachfeld, S., Manley, P. & McClennen, C. 2006. Marine sediment record from the East Antarctic margin reveals dynamics of ice sheet recession. GSA Today, 16, 410.CrossRefGoogle Scholar
Miller, G.H., Wolfe, A.P., Steig, E.J., Sauer, P.E., Kaplan, M.R. & Briner, J.P. 2002. The Goldilocks dilemma: big ice, little ice, or “just-right” ice in the eastern Canadian Arctic. Quaternary Science Reviews, 21, 3348.CrossRefGoogle Scholar
Verleyen, E., Hodgson, D.A., Milne, G.A., Sabbe, K. & Vyverman, W. 2005. Relative sea-level history from the Lambert Glacier region, East Antarctica, and its relation to deglaciation and Holocene glacier readvanve. Quaternary Research, 63, 4552.CrossRefGoogle Scholar
Zielinski, U. & Gersonde, R. 2002. Plio-Pleistocene diatom biostratigraphy from ODP Leg 177, Atlantic sector of the Southern Ocean. Marine Micropaleontology, 45, 225268.CrossRefGoogle Scholar
Zwartz, D., Bird, M., Stone, J. & Lambeck, K. 1998. Holocene sea-level change and ice sheet history in the Vestfold Hills, East Antarctica. Earth and Planetary Science Letters, 155, 131145.CrossRefGoogle Scholar