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Borchers, Andreas Dietze, Elisabeth Kuhn, Gerhard Esper, Oliver Voigt, Ines Hartmann, Kai and Diekmann, Bernhard 2016. Holocene ice dynamics and bottom-water formation associated with Cape Darnley polynya activity recorded in Burton Basin, East Antarctica. Marine Geophysical Research, Vol. 37, Issue. 1, p. 49.
Hodgson, Dominic A. Whitehouse, Pippa L. De Cort, Gijs Berg, Sonja Verleyen, Elie Tavernier, Ines Roberts, Stephen J. Vyverman, Wim Sabbe, Koen and O'Brien, Philip 2016. Rapid early Holocene sea-level rise in Prydz Bay, East Antarctica. Global and Planetary Change, Vol. 139, p. 128.
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Mackintosh, Andrew N. Verleyen, Elie O'Brien, Philip E. White, Duanne A. Jones, R. Selwyn McKay, Robert Dunbar, Robert Gore, Damian B. Fink, David Post, Alexandra L. Miura, Hideki Leventer, Amy Goodwin, Ian Hodgson, Dominic A. Lilly, Katherine Crosta, Xavier Golledge, Nicholas R. Wagner, Bernd Berg, Sonja van Ommen, Tas Zwartz, Dan Roberts, Stephen J. Vyverman, Wim and Masse, Guillaume 2014. Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum. Quaternary Science Reviews, Vol. 100, p. 10.
Suganuma, Yusuke Miura, Hideki Zondervan, Albert and Okuno, Jun'ichi 2014. East Antarctic deglaciation and the link to global cooling during the Quaternary: evidence from glacial geomorphology and 10Be surface exposure dating of the Sør Rondane Mountains, Dronning Maud Land. Quaternary Science Reviews, Vol. 97, p. 102.
Warrier, Anish Kumar Mahesh, B.S. Mohan, Rahul Shankar, Rajasekhariah Asthana, Rajesh and Ravindra, Rasik 2014. Glacial–interglacial climatic variations at the Schirmacher Oasis, East Antarctica: The first report from environmental magnetism. Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 412, p. 249.
White, Duanne A. and Fink, David 2014. Late Quaternary glacial history constrains glacio-isostatic rebound in Enderby Land, East Antarctica. Journal of Geophysical Research: Earth Surface, Vol. 119, Issue. 3, p. 401.
Berg, Sonja Leng, Melanie J. Kendrick, Christopher P. Cremer, Holger and Wagner, Bernd 2013. Bulk Sediment and Diatom Silica Carbon Isotope Composition from Coastal Marine Sediments off East Antarctica. Silicon, Vol. 5, Issue. 1, p. 19.
Golledge, Nicholas R. Levy, Richard H. McKay, Robert M. Fogwill, Christopher J. White, Duanne A. Graham, Alastair G.C. Smith, James A. Hillenbrand, Claus-Dieter Licht, Kathy J. Denton, George H. Ackert, Robert P. Maas, Sanne M. and Hall, Brenda L. 2013. Glaciology and geological signature of the Last Glacial Maximum Antarctic ice sheet. Quaternary Science Reviews, Vol. 78, p. 225.
Guglielmin, M. Worland, M.R. Convey, P. and Cannone, N. 2012. Schmidt Hammer studies in the maritime Antarctic: Application to dating Holocene deglaciation and estimating the effects of macrolichens on rock weathering. Geomorphology, Vol. 155-156, p. 34.
Verleyen, Elie Hodgson, Dominic A. Sabbe, Koen Cremer, Holger Emslie, Steven D. Gibson, John Hall, Brenda Imura, Satoshi Kudoh, Sakae Marshall, Gareth J. McMinn, Andrew Melles, Martin Newman, Louise Roberts, Donna Roberts, Steve J. Singh, Shiv M. Sterken, Mieke Tavernier, Ines Verkulich, Sergey de Vyver, Evelien Van Van Nieuwenhuyze, Wim Wagner, Bernd and Vyverman, Wim 2011. Post-glacial regional climate variability along the East Antarctic coastal margin—Evidence from shallow marine and coastal terrestrial records. Earth-Science Reviews, Vol. 104, Issue. 4, p. 199.
Berg, Sonja Wagner, Bernd Cremer, Holger Leng, Melanie J. and Melles, Martin 2010. Late Quaternary environmental and climate history of Rauer Group, East Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 297, Issue. 1, p. 201.
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Komatsu, Tetsuya Watanabe, Teiji and Hirakawa, Kazuomi 2010. A framework for Late Quaternary lake-level fluctuations in Lake Karakul, eastern Pamir, focusing on lake–glacier landform interaction. Geomorphology, Vol. 119, Issue. 3-4, p. 198.
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.
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