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The Antarctic Circumpolar Current—Earth's most powerful ocean current—formed about 34 million years ago.

Findings
Additional insights we found via Discover Magazine
The current circles Antarctica and carries over 100 times the combined water of all of Earth's rivers.
During the transition into the Oligocene epoch, the Earth went from a greenhouse to an icehouse state as Australia and South America drifted away from Antarctica, forming massive ocean pathways.
Simulations show that Australia's movement was critical in enabling strong westerly winds to form a complete loop from smaller currents.
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