Earth's climate experienced a warming event known as the Middle Eocene Climatic
Optimum (MECO) at~ 40 Ma, which was an abrupt reversal of a long-term Eocene cooling …

We present a study focused on changes in calcareous nannofossil assemblages of the
Alano section during the Middle Eocene Climatic Optimum (MECO). This warming event is …

Late Paleocene and early Eocene hyperthermals are transient warming events associated
with massive perturbations of the global carbon cycle, and are considered partial analogues …

Abstract The Paleocene‐Eocene Thermal Maximum (PETM) is recognized globally by a
negative excursion in stable carbon isotope ratios (δ13C) in sedimentary records, termed …

Abstract The Paleocene–Eocene Thermal Maximum (PETM) event was a dramatic global
warming∼ 55.93 Ma ago that resulted in biological extinction events, lithological changes …

A major perturbation of the global carbon cycle∼ 55 million years ago, believed to result
from release of 1000–2000 Gt of C from methane hydrates, correlates with an intense but …

Abstract The Paleocene–Eocene Thermal Maximum (PETM) represents the most
pronounced hyperthermal of the Cenozoic era and is hypothesized to have resulted in an …

A high-resolution calcareous nannofossil analysis of the Danian/Selandian boundary was
conducted at Site 1262 (Walvis Ridge, South Atlantic) to pinpoint the lowest occurrence of …

Abstract The Miocene Climate Optimum (MCO) and the subsequent Miocene Climate
Transition (MCT) are important biotic, environmental and geologic events. Here we address …

Antarctic ice sheet margin extent and the sensitivity of benthic δ18O to orbital forcing have
varied on million‐year timescales during the Oligocene to Early Miocene. However, few sea …