Constraining the greenhouse gas forcing, climatic warming and estimates of climate
sensitivity across ancient large transient warming events is a major challenge to the …

The temperature of seawater can affect marine plankton in various ways, including by
affecting rates of metabolic processes. This can change the way carbon and nutrients are …

A compilation of foraminiferal stable isotope measurements from southern high latitude
(SHL) deep-sea sites provides a novel perspective important for understanding Earth's …

The middle Miocene represents a major change in state in Cenozoic climatic evolution,
following the climax of Neogene warmth in the late early Miocene at∼ 16 Ma. The early …

Oxygen isotope records and glaciomarine sediments indicate at least an intermittent
presence of large continental ice sheets on Antarctica since the earliest Oligocene (circa 35 …

The equator to high southern latitude sea surface and vertical temperature gradients are
reconstructed from oxygen isotope values of planktonic and benthic foraminifers for the …

A prominent middle Eocene warming event is identified in Southern Ocean deep-sea cores,
indicating that long-term cooling through the middle and late Eocene was not monotonic. At …

A complete circum-Antarctic seaway did not open until both the South Tasman Rise cleared
the Oates Land coast of East Antarctica and Drake Passage opened between the southern …

Detailed investigations of high latitude sequences recently collected by the Ocean Drilling
Program (ODP) indicate that periods of rapid climate change often culminated in brief …

In the late Paleocene to early Eocene, deep sea benthic foraminifera suffered their only
global extinction of the last 75 million years and diversity decreased worldwide by 30–50 …