Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

Global sedimentary hiatuses are well-documented in ancient pelagic sediment, and include
Paleocene, Eocene-Oligocene boundary, and Miocene hiatuses. Less clear is the extent of …

Abstract The Pliocene and Early Pleistocene, between 5.3 and 0.8 million years ago, span a
transition from a global climate state that was 2–3° C warmer than present with limited ice …

Antarctic continental‐scale glaciation is generally assumed to have initiated at the Eocene‐
Oligocene Transition, yet its subsequent evolution is poorly constrained. We reconstruct …

Abstract The Antarctic Circumpolar Current plays a pivotal role in global climate through its
strong influence on the global overturning circulation, ocean heat and CO2 uptake …

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 …

Thick Cenozoic deposits were shed into the foreland basin of the Tian Shan Range,
providing great potential for understanding the relationship between tectonic history and …

Abstract The Gamburtsev Subglacial Mountains are regarded as a key nucleation site for the
Antarctic Ice Sheet and they retain a unique long-term record of pre-glacial and early glacial …

Although ice‐sheet flow and form in Antarctica is controlled to a large degree by topography,
the continent's landscape evolution and therefore its influence on ice‐sheet development is …

Abstract The Mid-Miocene Climatic Optimum (MMCO) is one of Earth's most recent
prolonged warming events, recorded in both the deep ocean and mid-to high-latitude …