Research news on Eocene

The Eocene is a formally defined epoch of the Paleogene Period within the Cenozoic Era, spanning approximately 56 to 34 million years ago, characterized by globally warm climates and high atmospheric CO₂ levels. It is subdivided into the Ypresian, Lutetian, Bartonian, and Priabonian ages based on biostratigraphic markers and magnetostratigraphy. The Eocene saw major diversification of modern mammalian orders, early primates, and marine fauna, as well as significant tectonic reconfigurations influencing ocean circulation. Notable climatic events include the Early Eocene Climatic Optimum and progressive cooling that initiated the transition toward Antarctic glaciation by the end of the epoch.

Epiaceratherium itjilik: The rhino that lived in the Arctic

Paleontologists at the Canadian Museum of Nature have recently been studying the skeletal remains of a rhinoceros. This might not sound remarkable at first, but what makes these remains fascinating is that they were found ...

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 ...