Marine Isotope Stage 13 (MIS 13) is a specific period in Earth's geological history that occurred during the Pleistocene epoch. It is part of a series of glacial and interglacial periods that are characterized by changes in Earth's climate and ice volume over time, as recorded in deep-sea sediment cores and ice cores. MIS 13 is generally dated to around 480,000 to 450,000 years ago.
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