During the Paleocene-Eocene Thermal Maximum (PETM),∼ 56 Mya, thousands of
petagrams of carbon were released into the ocean-atmosphere system with attendant …

The prominent global warming event at the Paleocene-Eocene boundary (55 Ma), referred
to as the Paleocene-Eocene Thermal Maximum (PETM), was characterized by rapid …

What happens to the Earth's climate, environment, and biota when thousands of gigatons of
greenhouse gases are rapidly added to the atmosphere? Modern anthropogenic forcing of …

Abstract The Palaeocene–Eocene Thermal Maximum (PETM), a geologically brief episode
of global warming associated with the Palaeocene–Eocene boundary, has been studied …

A rapid increase in greenhouse gas levels is thought to have fueled global warming at the
Paleocene-Eocene Thermal Maximum (PETM). Foraminiferal magnesium/calcium ratios …

The impacts of the Paleocene‐Eocene thermal maximum (PETM)(∼ 55 Ma), one of the most
rapid and extreme warming events in Earth history, are well characterized in open marine …

A brief (~ 150 kyr) period of widespread global average surface warming marks the
transition between the Paleocene and Eocene epochs,~ 56 million years ago. This so …

Abstract The Palaeocene–Eocene Thermal Maximum (PETM), an approximately 170,000-
year-long period of global warming about 56 million years ago, has been attributed to the …

Abrupt global warming and profound perturbation of the carbon cycle during the Paleocene-
Eocene Thermal Maximum (PETM, ca. 55 Ma) have been linked to a massive release of …

The Paleocene-Eocene Thermal Maximum (PETM) has been attributed to a rapid rise in
greenhouse gas levels. If so, warming should have occurred at all latitudes, although …