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Oligocene Epoch begins

33.9 million to 23 million years ago · Prehistoric
Geology

The Oligocene Epoch, spanning 33.9 to 23 million years ago, is the third and final epoch of the Paleogene Period. It began with a cooling event that triggered Antarctic ice sheet expansion and a sea level drop of approximately 105 meters. Tropical forests contracted as grasslands spread, favoring ground-dwelling mammals. Most modern mammal families appeared during this interval, including early horses, rhinoceroses, camels, and deer, while creodonts declined and were replaced by carnivorans such as early dogs and bears.

Key Figures

Heinrich Ernst Beyrich

Locations

BelgiumNorthern Germany

Topics

geologyOligocenepaleontology

Connected Events — 5 Connections

Ongoing collision and Tethys closure altered global ocean circulation and climate, contributing to Oligocene cooling and Antarctic ice sheet formation India-Eurasia Collision Begins Closing the Neo-Tethys Ocean
c. 50 MYA · Geology · Prehistoric
Opening of the Drake Passage enabled circumpolar ocean currents that drove Antarctic glaciation and Oligocene cooling Drake Passage Opens
c. 34 MYA · Geology · Prehistoric
PETM greenhouse conditions preceded the long cooling trend toward the Oligocene icehouse Paleocene-Eocene Thermal Maximum
c. 56 MYA · Climate · Prehistoric
Azolla-driven CO2 decline set the stage for Oligocene cooling Arctic Azolla Bloom Draws Down Atmospheric CO2
c. 49 MYA · Climate · Prehistoric
The Messinian crisis occurred after Oligocene cooling had already reshaped Mediterranean ecosystems Mediterranean Desiccates During the Messinian Salinity Crisis
c. 5.96 MYA · Climate · Prehistoric
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