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The 10th millennium BC marks the beginning of the Mesolithic and Epipaleolithic period, which is the first part of the Holocene epoch. Agriculture, based on the cultivation of primitive forms of millet and rice, occurred in Southwest Asia.[1] Although agriculture was being developed in the Fertile Crescent, it would not be widely practised for another 2,000 years.[citation needed]
The world population is estimated as between one and ten million people,[2] most of whom were hunter-gatherer communities scattered over all continents except Antarctica and Zealandia. The Würm glaciation ended, and the beginning interglacial, which endures to this day, allowed the re-settlement of northern regions. The most recent glacial ended c. 10,000 BC, and the world entered a period of global warming.
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| The Stone Age |
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↑ before Homo (Pliocene) |
| ↓ Chalcolithic |
c. 10,000 BC:
c. 9700 BC: Lake Agassiz forms.
c. 9600 BC: Younger Dryas cold period ends. Pleistocene ends and Holocene begins. Paleolithic ends and Mesolithic begins. Large amounts of previously glaciated land become habitable again.
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