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 early and late Eocene have both been the subject of many modelling studies, but few
have focused on the middle Eocene. The latter still holds many challenges for climate …

The global and regional climate changed dramatically with the expansion of the Antarctic Ice
Sheet at the Eocene–Oligocene transition (EOT). These large-scale changes are generally …

A major step in the long-term Cenozoic evolution toward a glacially driven climate occurred
at the Eocene–Oligocene transition (EOT),∼ 34.44 to 33.65 million years ago (Ma) …

Abstract The Eocene–Oligocene Transition (EOT) marks the onset of the Antarctic glaciation
and the switch from greenhouse to icehouse climates. However, the driving mechanisms …

The Paleogene history of biogenic opal accumulation in the North Atlantic provides insight
into both the evolution of deepwater circulation in the Atlantic basin and weathering …

Ongoing rapid climate change has a major effect on marine fauna, and understanding these
faunal changes analogous to future climatic periods is crucial. The Oligocene is commonly …

The northeast Atlantic encompasses archetypal examples of volcanic rifted margins. Twenty-
five years after the last ODP (Ocean Drilling Program) leg on these volcanic margins, the …