nature & planetPhys.orgc. 50 million years ago · Southern Ocean

How the Southern Ocean helped fuel Earth's warmest climate in 65 million years

from Phys.org

About 50 million years ago, Earth experienced its warmest climate since the extinction of the dinosaurs. Global temperatures were more than 10°C higher than today, and atmospheric CO₂ concentrations reached around 1,600 parts per million. But what kept CO₂ levels so extraordinarily high for millions of years? An international research team led by the Max Planck Institute for Chemistry has identified an important piece of the puzzle: the Southern Ocean.

explained

The Early Eocene Climatic Optimum (EECO), also referred to as the Early Eocene Thermal Maximum (EETM), was a period of extremely warm greenhouse climatic conditions during the Eocene epoch. The EECO represented the hottest sustained interval of the Cenozoic era and one of the hottest periods in all of Earth's history.

From Wikipedia: Early Eocene Climatic Optimum (CC BY-SA 4.0) ↗
how it works

Deep water holds far more dissolved carbon than surface water. Where it rises to the surface, as it does in the Southern Ocean, some carbon escapes to the air. How strongly the ocean overturns and how much carbon the deep water holds therefore sets how much CO₂ ends up in the atmosphere.

so what

The Eocene is the closest natural analogue to a high-CO₂ future, so understanding what held its carbon dioxide up helps calibrate how the climate system responds to carbon. It shows the ocean can be a long-lived source or sink, not just a bystander.

fun fact

During the Eocene's warmth, palm trees and crocodile relatives lived in the Arctic.

more on this

Illustrative photo · NASA's Scientific Visualization Studio - Global Science and…, Public domain, via Wikimedia Commons