The late Paleocene to early Eocene warming trend was punctuated by a series of orbitally
paced transient warming events, associated with the release of isotopically light carbon into …

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 …

Abstract We present high‐resolution (2–3 kyr) benthic foraminiferal stable isotopes in a
continuous, well‐preserved sedimentary archive from the West Pacific Ocean (Ocean …

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 …

Multiple abrupt warming events (“hyperthermals”) punctuated the Early Eocene and were
associated with deep-sea temperature increases of 2 to 4° C, seafloor carbonate dissolution …

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 …

Eocene Thermal Maximum 2 (ETM2;∼ 53.7 Ma) occurred approximately 2 Myr after the
Paleocene‐Eocene Thermal Maximum (∼ 55.5 Ma) and was characterized by a deep‐sea …

Recent studies have shown that the Early Eocene Climatic Optimum (EECO) was preceded
by a series of short-lived global warming events, known as hyperthermals. Here we present …

Abstract The Miocene Climatic Optimum (MCO; ca. 17–14.7 Ma) represents one of several
major interruptions in the long-term cooling trend of the past 50 my To date, the processes …

Abstract The Eocene‐Oligocene transition (EOT),~ 34 Ma, marks a tipping point in the long‐
term Cenozoic greenhouse to icehouse climate transition. Paleorecords reveal stepwise …