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 …

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

[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 …

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 …

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 …

The upper Paleocene and lower Eocene are marked by several prominent (> 1‰) carbon
isotope (δ13C) excursions (CIE) that coincide with transient global warmings, or thermal …

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 …

To assess the influence of orbital‐scale variations on late Oligocene to early Miocene
climate and ocean chemistry, high‐resolution (∼ 5 kyr) benthic foraminiferal carbon and …

Within the last decade, several early Eocene hyperthermals have been detected globally.
These transient warming events have mainly been characterized geochemically–using …