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 Turkish Highlands and the Fertile Crescent, it would not be widely practised for another 2,000 years.[citation needed].

The world population was likely below 5 million people,[citation needed] most of whom were hunter-gatherer communities scattered over all continents except Antarctica. 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 circa 10,000 BC, and the world entered a period of global warming.

Contents

Events

The Stone Age

before Homo (Pliocene)

Paleolithic

Lower Paleolithic
Homo
control of fire, stone tools
Middle Paleolithic
Homo neanderthalensis
Homo sapiens
out of Africa
Upper Paleolithic, Late Stone Age
behavioral modernity, atlatl, dog

Mesolithic

microliths, bow, canoe

Neolithic

Pre-Pottery Neolithic
farming, animal husbandry, polished stone tools
Pottery Neolithic
pottery
Chalcolithic
metallurgy, horse, wheel
Bronze Age

Old World

Americas

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.

Circa 10,000 BC:

Circa 9700 BC: Lake Agassiz forms.

Circa 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.

Circa 9500 BC: Ancylus Lake, part of the modern-day Baltic Sea, forms.

In popular culture

Footnotes

  1. ^ a b Roberts (1994)
  2. ^ Kislev et al. (2006a, b), Lev-Yadun et al. (2006)

References


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