Ice-sheet dynamics through the Quaternary on the mid-Norwegian continental margin inferred from 3D seismic data.Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks.Discovery of a hypersaline subglacial lake complex beneath Devon Ice Cap, Canadian Arctic.3D seismic evidence of buried iceberg ploughmarks from the mid-Norwegian continental margin reveals largely persistent North Atlantic Current through the Quaternary.The International Bathymetric Chart of the Arctic Ocean (IBCAO) Version 3.0Quantifying the Mass Balance of Ice Caps on Severnaya Zemlya, Russian High Arctic. I: Climate and Mass Balance of the Vavilov Ice CapEvidence for glaciation in the Northern Hemisphere back to 44 Ma from ice-rafted debris in the Greenland SeaAutonomous underwater vehicles (AUVs) and investigations of the ice–ocean interface in Antarctic and Arctic watersGreenland subglacial lakes detected by radarA community-based geological reconstruction of Antarctic Ice Sheet deglaciation since the Last Glacial MaximumReconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial MaximumReconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial MaximumA new bathymetric compilation for the South Orkney Islands region, Antarctic Peninsula (49°-39°W to 64°-59°S): Insights into the glacial development of the continental shelfGeomorphic signature of Antarctic submarine gullies: Implications for continental slope processesComment on Shaw J., Pugin, A. and Young, R. (2008): “A meltwater origin for Antarctic shelf bedforms with special attention to megalineations”, Geomorphology 102, 364–375Flow and retreat of the Late Quaternary Pine Island-Thwaites palaeo-ice stream, West AntarcticaThe sedimentary legacy of a palaeo-ice stream on the shelf of the southern Bellingshausen Sea: Clues to West Antarctic glacial history during the Late QuaternaryClay mineral provenance of sediments in the southern Bellingshausen Sea reveals drainage changes of the West Antarctic Ice Sheet during the Late QuaternaryMorphology of the upper continental slope in the Bellingshausen and Amundsen Seas – Implications for sedimentary processes at the shelf edge of West AntarcticaA major trough-mouth fan on the continental margin of the Bellingshausen Sea, West Antarctica: The Belgica FanGeological constraints on Antarctic palaeo-ice-stream retreatTill characteristics, genesis and transport beneath Antarctic paleo-ice streamsFlow of the West Antarctic Ice Sheet on the continental margin of the Bellingshausen Sea at the Last Glacial MaximumA new bathymetry of the Northeast Greenland continental shelf: Constraints on glacial and other processesIce-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: Sedimentological and foraminiferal signaturesA glacier-influenced turbidite system and associated landform assemblage in the Greenland Basin and adjacent continental slopeArctic Ocean glacial historyRecent glacially influenced sedimentary processes on the East Greenland continental slope and deep Greenland BasinGeological record of ice shelf break-up and grounding line retreat, Pine Island Bay, West AntarcticaAn Arctic Ocean ice shelf during MIS 6 constrained by new geophysical and geological dataHigh-resolution geophysical observations of the Yermak Plateau and northern Svalbard margin: implications for ice-sheet grounding and deep-keeled icebergsSubmarine landforms and ice-sheet flow in the Kvitøya Trough, northwestern Barents SeaGenerating synthetic fjord bathymetry for coastal GreenlandHow accurate are estimates of glacier ice thickness? Results from ITMIX, the Ice Thickness Models Intercomparison eXperimentApplication of a two-step approach for mapping ice thickness to various glacier types on SvalbardICESHEET 1.0: a program to produce paleo-ice sheet reconstructions with minimal assumptionsThe periodic topography of ice stream beds: Insights from the Fourier spectra of mega-scale glacial lineationsTracking the provenance of Greenland-sourced, Holocene aged, individual sand-sized ice-rafted debris using the Pb-isotope compositions of feldspars and 40 Ar/ 39 Ar ages of hornblendesWorkshop explores debris transported by icebergs and paleoenvironmental implicationsEvidence of a hydrological connection between the ice divide and ice sheet margin in the Aurora Subglacial Basin, East Antarctica
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P50
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