10th millennium BC

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Millennia: 11th millennium BC · 10th millennium BC · 9th millennium BC
Centuries: 100th century BC · 99th century BC · 98th century BC · 97th century BC · 96th century BC · 95th century BC · 94th century BC · 93rd century BC · 92nd century BC · 91st century BC

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.

Contents

[edit] Events

The Stone Age
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before Homo (Pliocene)

Stone tool
Paleolithic

Lower Paleolithic
Homo
Control of fire by early humans
Middle Paleolithic
Homo neanderthalensis
Homo sapiens
Recent African origin of modern humans
Upper Paleolithic, Late Stone Age
Behavioral modernity, Atlatl,
Origin of the domestic dog

Mesolithic

Microliths, Bow, Canoe

Neolithic

Pre-Pottery Neolithic
Neolithic Revolution,
Domestication
Pottery Neolithic
Pottery

Chalcolithic

Metallurgy, Wheel,
Domestication of the horse,
Bronze Age

[edit] Old World

[edit] Americas

[edit] Environmental changes

Subdivisions of the Quaternary Period
System Series Stage Age (Ma)
Quaternary Holocene 0–0.0117
Pleistocene Tarantian (Upper) 0.0117–0.126
Ionian (Middle) 0.126–0.781
Calabrian (Lower) 0.781–1.806
Gelasian (Lower) 1.806–2.588
Neogene Pliocene Piacenzian older
In Europe and North America, the Holocene is subdivided into Preboreal, Boreal, Atlantic, Subboreal, and Subatlantic stages of the Blytt-Sernander time scale. There are many regional subdivisions for the Upper or Late Pleistocene, usually these represent locally recognized cold (glacial) and warm (interglacial) periods. The last glacial period ends with the cold Younger Dryas substage.

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.

[edit] In popular culture

[edit] Chronological studies

[edit] Footnotes

  1. ^ Roberts (1994)
  2. ^ "Historical Estimates of World Population". US Census Bureau. http://www.census.gov/ipc/www/worldhis.html. Retrieved 25 December 2010. 
  3. ^ Kislev et al. (2006a, b), Lev-Yadun et al. (2006)

[edit] References

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