A rapid warming event known as the pre-onset excursion (POE) occurred prior to the
Paleocene-Eocene Thermal Maximum (PETM). It is less well studied compared to the PETM …

Abstract The Paleocene–Eocene Thermal Maximum (PETM;∼ 56 Ma) represents a rapid
and sustained climatic perturbation that lasted for∼ 170 kyr and coincided with the …

Records of the paleoenvironmental changes that occurred during the Paleocene‐Eocene
Thermal Maximum (PETM) are preserved in sedimentary rocks along the margins of the …

The impact of the Paleocene–Eocene Thermal Maximum (PETM) is clearly observed in the
extended area of the northeastern Peri-Tethys basin. Lithological and geochemical features …

The early Eocene is thought to be the warmest period of the Cenozoic Era, with global
temperatures~ 10° C higher than today. Few studies have focused on the paleoclimatic …

Abstract The Paleocene-Eocene Thermal Maximum (PETM) offers an excellent opportunity
to study the ecological and environmental responses to global warming. Discussing the so …

The Forada section (northeastern Italy) provides a continuous, expanded deep-sea record of
the Paleocene–Eocene Thermal Maximum (PETM) in the central-western Tethys. We …

In the northeastern Peri-Tethys epicontinental basin stretching from the Black Sea to
Tadjikistan, a sapropelitic bed with total organic carbon (TOC) contents up to 20% and …

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 …

Abstract The Paleocene–Eocene Thermal Maximum (PETM;∼ 56 Ma) is associated with
abrupt climate change, carbon cycle perturbation, ocean acidification, as well as …