Marine-geological and-geophysical studies were conducted to determine the Late
Quaternary glacial history of the West Antarctic Ice Sheet in Pine Island Bay, Antarctica. The …

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) …

We present a reconstruction of the Antarctic topography at the Eocene–Oligocene (ca.
34Ma) climate transition. This provides a realistic key boundary condition for modeling the …

The Amundsen Sea continental shelf is one of the most remote areas of coastal Antarctica
and was relatively unexplored until the late 1980s. Over the last two decades, increased …

The effects of glaciation on sediment drifts is recognised from marked sedimentary facies
variation in deep sea cores taken from the continental rise of the Antarctic Peninsula Pacific …

The Pacific margin of the Antarctic Peninsula was drilled during Ocean Drilling Program
(ODP) Leg 178 to understand the past 10 my of its glacial history and to test a drilling …

Major ice loss in the Amundsen Sea sector of the West Antarctic Ice Sheet (WAIS) is
hypothesized to have triggered ice sheet collapses during past warm periods such as those …

A 330-km length of the little known continental shelf edge and slope of the Bellingshausen
Sea, West Antarctica, is investigated using multibeam swath-bathymetric and sub-bottom …

Marine geophysical data from the Antarctic continental shelf indicate the former presence of
ice streams that drained through bathymetric troughs during the last glacial cycle. Streaming …

Swath bathymetry and TOPAS sub-bottom profiler acoustic data reveal the presence of a
major cross-shelf bathymetric trough containing streamlined subglacial bedforms formed in …