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Marine Isotope Stage 3 (MIS3) was a relatively warm and humid, although variable, time in the last glacial period in the northern hemisphere. This climate phase is well-recorded in various archives (e.g., ice cores, speleothems, and loess) from many parts of the world, including China, although its expression (e.g., warm–humid vs. cool–dry) differed between the hemispheres.
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