Earth's climate cooled markedly during the late Miocene from 12 to 5 million years ago, with
far-reaching consequences for global ecosystems. However, the driving forces of these …

Scientists have long been puzzled by the fact that mid-to-high latitude continental interiors
and the poles in the Eocene (55 to 34 Million years ago) were much warmer than today …

Over the past three million years, Earth's climate oscillated between warmer interglacials
with reduced terrestrial ice volume and cooler glacials with expanded polar ice sheets …

We have constructed high‐resolution (104–105 years) benthic foraminiferal δ13C and δ18O
records for the upper Eocene through lower Oligocene of two pelagic sequences, Deep Sea …

Abstract The Late Paleocene and Early Eocene were characterized by warm greenhouse
climates, punctuated by a series of rapid warming and ocean acidification events known as …

Studying the dynamics of past global warming events during the late Paleocene to middle
Eocene informs our understanding of Earth's carbon cycle behavior under elevated …

[2] The Paleocene (65–55 Ma) represents an epoch when both the climate system and
carbon cycle were undergoing dramatic shifts during a period of elevated greenhouse gas …

The conversion of surface water to deep water in the North Atlantic results in the release of
heat from the ocean to the atmosphere, which may have amplified millennial-scale climate …

Geochemical and sedimentological evidence suggest that the rapid climate warming
oscillations of the last ice age, the Dansgaard–Oeschger cycles, were coupled to …

Oxygen isotope data for a Pliocene interval from 3.6 to 2.8 million years ago show a mean
increase (0.5 per mil) of benthic δ18O at about 3.2 million years ago, whereas planktic δ18O …