Antarctica's continental-scale ice sheets have evolved over the past 50 million years,,,.
However, the dearth of ice-proximal geological records,,, limits our understanding of past …

Abstract The East Antarctic Ice Sheet (EAIS) is the largest potential contributor to sea-level
rise. However, efforts to predict the future evolution of the EAIS are hindered by uncertainty …

The first Cenozoic ice sheets initiated in Antarctica from the Gamburtsev Subglacial
Mountains and other highlands as a result of rapid global cooling∼ 34 million years ago. In …

Sea-level rise due to ice loss in the Northern Hemisphere in response to insolation and
greenhouse gas forcing is thought to have caused grounding-line retreat of marine-based …

Understanding ice sheet behaviour in the geological past is essential for evaluating the role
of the cryosphere in the climate system and for projecting rates and magnitudes of sea level …

Of today's great ice sheets, the West Antarctic Ice Sheet poses the most immediate threat of
a large sea-level rise, owing to its potential instability. Complete release of its ice to the …

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 …

Rapid warming over the past 50 years on the Antarctic Peninsula is associated with the
collapse of a number of ice shelves and accelerating glacier mass loss,,,,,,. In contrast …

Abstract The East Antarctic Ice Sheet contains the vast majority of Earth's glacier ice (about
52 metres sea-level equivalent), but is often viewed as less vulnerable to global warming …

Abstract Early to Middle Miocene sea-level oscillations of approximately 40–60 m estimated
from far-field records,–are interpreted to reflect the loss of virtually all East Antarctic ice …