Study of the paleoclimatic transition from Greenhouse to Icehouse conditions by means of calcareous nannofossils in the Southern, Atlantic, Pacific, and Indian Oceans

• Main Authors: Righi D., Persico D., Catelli V., Fioroni C., Raffi I., Villa G.
• Other Authors: Righi, D., Persico, D., Catelli, V., Fioroni, C., Raffi, I., Villa, G.
• Format: Conference Object
• Language: English
• Published: 2024
• Subjects: Antarctic; Pacific; Indian; Saraswati; Antarc*; Ice Sheet
• Online Access: https://hdl.handle.net/11380/1353409; https://ina.tmsoc.org/JNR/JNRcontents.htm

The Eocene–Oligocene transition (EOT) occurred at approximately 34 Ma, lasted approximately 790 kyr, and includes the Eocene/Oligocene boundary (EOB). It marks the transition from a world without permanent ice sheets (Greenhouse conditions) to one with an Antarctic Ice Sheet (Icehouse conditions) (H...