West Antarctica has formed the tectonically active margin between East Antarctica and the
Pacific Ocean for almost half a billion years, where it has recorded a dynamic history of …

Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …

Ocean melting has thinned Antarctica's ice shelves at an increasing rate over the past two
decades, leading to loss of grounded ice. The Ross Ice Shelf is currently close to steady …

The second generation Antarctic magnetic anomaly compilation for the region south of 60° S
includes some 3.5 million line‐km of aeromagnetic and marine magnetic data that more than …

We construct a new seismic model for central and West Antarctica by jointly inverting
Rayleigh wave phase and group velocities along with P wave receiver functions. Ambient …

The upper mantle and transition zone beneath Antarctica and the surrounding oceans are
among the poorest‐imaged regions of the Earth's interior. Over the last 15 years, several …

Gravity surveying is challenging in Antarctica because of its hostile environment and
inaccessibility. Nevertheless, many ground‐based, airborne, and shipborne gravity …

Abstract Knowledge of Antarctica's sedimentary basins builds our understanding of the
coupled evolution of tectonics, ice, ocean, and climate. Sedimentary basins have properties …

The geology beneath Thwaites Glacier, the Antarctic glacial catchment most vulnerable to
climate change, is unknown. Thwaites Glacier lies within the West Antarctic Rift System, but …

Gondwana breakup changed the global continental configuration, leading to opening of
major oceanic gateways, shifts in the climate system and significant impacts on the …