Abstract The Pliocene Epoch (∼ 5.3–2.6 million years ago, Ma) was characterized by a
warmer than present climate with smaller Northern Hemisphere ice sheets, and offers an …

Abstract International Ocean Discovery Program (IODP) Expedition 379 to the Amundsen
Sea margin of West Antarctica recovered drill cores at two sites spanning the Latest Miocene …

Pliocene global temperatures periodically exceeded modern levels, offering insights into ice
sheet sensitivity to warm climates. Ice-proximal geologic records from this period provide …

Terrestrial climate records for Antarctica, beyond the age limit of ice cores, are restricted to
the few unglaciated areas with exposed rock outcrops. Marine sediments on Antarctica's …

Knowledge of Antarctica's sedimentary basins builds our understanding of the coupled
evolution of 33 tectonics, ice, ocean, and climate. Sedimentary basins have properties …

The bottom water conditions in the Central South Pacific (CSP) and associated changes in
the Lower Circumpolar Deep Water (LCDW) and Antarctic Bottom Water (AABW) under …

Detailed sedimentological and stratigraphic analysis of pre-vegetation sedimentary systems
that deposited across global-scale climate change episodes is key to fully understanding …

The thick sequence of mid‐late Cenozoic sediments preserved within the Enderby Basin of
the East Antarctica margin contains key information regarding glacial history and palaeo …

The dynamics of the Antarctic ice sheet (AIS) have profound implications for the evolution of
the Antarctic continental margin, global ocean currents, and climate changes. Marine …

Ice loss in the Southern Hemisphere has been greatest over the past 30 years in West
Antarctica. The high sensitivity of this region to climate change has motivated geologists to …