An emerging body of evidence from studies of the last glacial/interglacial cycle suggests that
the East and West Antarctic ice sheets have not advanced and retreated in concert. The …

Reductions in the thickness and extent of Antarctic ice shelves are triggering increased
discharge of marine-terminating glaciers. While the impacts of recent changes are well …

To predict the future contributions of the Antarctic ice sheets to sea-level rise, numerical
models use reconstructions of past ice-sheet retreat after the Last Glacial Maximum to tune …

The history of deglaciation of the West Antarctic Ice Sheet (WAIS) gives clues about its
future. Southward grounding-line migration was dated past three locations in the Ross Sea …

Onshore and offshore studies show that an expanded, grounded ice sheet occupied the
Ross Sea Embayment during the Last Glacial Maximum (LGM). Results from studies of till …

We review and synthesize the geologic record that constrains the sources of sea level rise
and freshwater discharge to the global oceans associated with retreat of ice sheets during …

Abstract The East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Earth, and
documenting its evolution since the Last Glacial Maximum (LGM) is important for …

Palmer Deep sediment cores are used to produce the first high-resolution, continuous late
Pleistocene to Holocene time-series from the Antarctic marine system. The sedimentary …

We review the geomorphological, sedimentological and chronological evidence for palaeo-
ice streams on the continental shelf of Antarctica and use this information to investigate …

A lack of reliable chronology often leaves Antarctic ice sheet reconstructions incomplete.
Despite being the most heavily investigated region of the Antarctic continental shelf, the post …