Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …

Antarctica contains most of Earth's fresh water stored in two large ice sheets. The more
stable East Antarctic Ice Sheet is larger and older, rests on higher topography, and hides …

Cenozoic evolution of the Antarctic ice sheets is thought to be driven primarily by long-term
changes in radiative forcing, but the tectonic evolution of Antarctica may also have played a …

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 …

The linkages between the astronomical forcing of sea-level oscillations, the environment,
and climate change during the Late Paleozoic Ice Age (LPIA) add to our understanding of …

The first major build-up of Antarctic glaciation occurred in two consecutive stages across the
Eocene–Oligocene transition (EOT): the EOT-1 cooling event at~ 34.1–33.9 Ma and the Oi-1 …

Constraining monsoon variability and dynamics in the warm unipolar icehouse world of the
Late Oligocene can provide important clues to future climate responses to global warming …

Abstract The Southern Ocean is a key player in the climate, ocean, and atmospheric system.
As the only direct connection between all three major oceans since the opening of the …

Millennial-scale ice sheet variability (1–15 kyr periods) is well documented in the
Quaternary, providing insight into critical atmosphere–ocean–cryosphere interactions that …

The middle to late Eocene marked a key transition from greenhouse to coolhouse. However,
a lack of high-resolution and temporally well-constrained continental records hinders our …