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Approximately 50 million years ago, Antarctica's climate changed due to a combination of tectonic shifts and a decline in atmospheric CO2 levels. The movement of the Antarctic tectonic plate caused the continent to drift southward, leading to its isolation and the development of the Antarctic Circumpolar Current. This current helped to seal off Antarctica from warmer ocean waters, facilitating the onset of its glaciation. Additionally, the reduction in greenhouse gases contributed to cooler global temperatures, further promoting ice sheet formation on the continent.

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1w ago

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