Research news on Paleocene

The Paleocene is a geological epoch within the Paleogene Period, spanning approximately 66 to 56 million years ago, immediately following the Cretaceous–Paleogene (K–Pg) boundary. It is defined stratigraphically by the recovery and radiation of biota after the end-Cretaceous mass extinction and is subdivided into the Danian, Selandian, and Thanetian ages. The Paleocene is characterized by globally warm greenhouse climates, the progressive diversification of mammals, birds, and angiosperms, and distinct marine microfossil assemblages used for biostratigraphic correlation. Its upper boundary is marked by significant carbon-cycle perturbations leading into the Paleocene–Eocene Thermal Maximum.

What past global warming reveals about future rainfall

To understand how global warming could influence future climate, scientists look to the Paleogene Period that began 66 million years ago, covering a time when Earth's atmospheric carbon dioxide levels were two to four times ...

An ancient warming event may have lasted longer than we thought

Fifty-six million years ago, during the Paleocene-Eocene Thermal Maximum (PETM), global temperatures rose by more than 5°C over 100,000 or more years. Between 3,000 and 20,000 petagrams of carbon were released into the atmosphere ...