Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum.

• Published in: Quaternary Science Reviews
• Main Authors: Larter, R.D., Anderson, J.B., Graham, A.G.C., Gohl, K., Hillenbrand, C.-D., Jakobsson, M., Johnson, J.S., Kuhn, G., Nitsche, F.O., Smith, J.A., Witus, A.E., Bentley, M.J., Dowdeswell, J.A., Ehrmann, W., Klages, J.P., Lindow, J., Ó Cofaigh, C., Spiegel, C.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Elsevier 2014
• Subjects: Ice sheet; Last Glacial Maximum; Holocene; Ice stream; Grounding line; Radiocarbon; Cosmogenic isotope; Surface exposure age; Multibeam swath bathymetry; Sediment; Glacimarine; Diamicton; Continental shelf; Circumpolar deep water; Subglacial meltwater; Sea level; Amundsen Sea; Antarctic; Bellingshausen Sea; Eltanin Bay; West Antarctic Ice Sheet; West Antarctica; Antarc*; Antarctica; ice core; Ice Sheet
• Online Access: http://dro.dur.ac.uk/12825/; http://dro.dur.ac.uk/12825/1/12825.pdf; http://dro.dur.ac.uk/12825/2/12825.pdf; https://doi.org/10.1016/j.quascirev.2013.10.016

Marine and terrestrial geological and marine geophysical data that constrain deglaciation since the Last Glacial Maximum (LGM) of the sector of the West Antarctic Ice Sheet (WAIS) draining into the Amundsen Sea and Bellingshausen Sea have been collated and used as the basis for a set of time-slice r...