Abstract The Eocene–Oligocene transition (EOT) was a climate shift from a largely ice-free
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …

The global compilation of reported marine varved sedimentary records throughout the
Quaternary contains 52 sites. Marine varve deposition and preservation typically depend on …

Accurate models of past Antarctic ice sheet behaviour require realistic reconstructions of the
evolution of bedrock topography. However, other than a preliminary attempt to reconstruct …

Oscillations in ice sheet extent during early and middle Miocene are intermittently preserved
in the sedimentary record from the Antarctic continental shelf, with widespread erosion …

Radiocarbon (14C) dating of sediment deposition around Antarctica is often challenging due
to heterogeneity in sources and ages of organic carbon in the sediment. Chemical and …

East Antarctica hosts large subglacial basins into which the East Antarctic Ice Sheet (EAIS)
likely retreated during past warmer climates. However, the extent of retreat remains poorly …

Abstract Over the past 3–4 decades, coincident with global warming and atmospheric CO2
increase, Arctic sea ice has significantly decreased in its extent as well as in thickness …

The repeated proximity of West Antarctic Ice Sheet (WAIS) ice to the eastern Ross Sea
continental shelf break during past ice age cycles has been inferred to directly influence …

Abstract The rapidly thinning Totten Glacier on the Sabrina Coast, East Antarctica, is the
primary drainage outlet for ice within the Aurora Subglacial Basin, which could destabilize …

Antarctic cryosphere has significant impact on the global climate system by influencing the
ocean currents, the atmosphere, and the sea level for long term durations. Antarctic Ice …