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The altithermal period, also known as the Holocene Climatic Optimum, occurred roughly between 8000 and 4000 years ago, characterized by warmer and more stable climatic conditions than today. This period saw enhanced temperatures, particularly in the Northern Hemisphere, leading to changes in vegetation and ecosystems. It facilitated the expansion of forests and influenced human activities, including the development of agriculture in various regions. The altithermal is significant for understanding past climate dynamics and their impact on human societies.

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