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The '''Middle Paleolithic''' (or '''Middle Palaeolithic''') is the second subdivision of the [[Paleolithic]] or Old [[Stone Age]] as it is understood in [[Europe]], [[Africa]] and [[Asia]]. Very broadly it dates to between around 300,000 and 30,000 years ago. There are considerable dating differences between regions. It is succeeded by the [[Upper Paleolithic]] subdivision.
The '''Middle Paleolithic''' (or '''Middle Palaeolithic''') is the second subdivision of the [[Paleolithic]] or Old [[Stone Age]] as it is understood in [[Europe]], [[Africa]] and [[Asia]]. Very broadly it dates to between around 300,000 and 30,000 years ago. There are considerable dating differences between regions. It is succeeded by the [[Upper Paleolithic]] subdivision.

Revision as of 16:43, 15 February 2008

Subdivisions of the Quaternary Period
System/
Period
Series/
Epoch
Stage/
Age
Age
Quaternary Holocene Meghalayan 0 4,200
Northgrippian 4,200 8,200
Greenlandian 8,200 11,700
Pleistocene 'Upper' 11,700 129ka
Chibanian 129ka 774ka
Calabrian 774ka 1.80Ma
Gelasian 1.80Ma 2.58Ma
Neogene Pliocene Piacenzian 2.58Ma 3.60Ma
Notes and references[1][2]
Subdivision of the Quaternary Period according to the ICS, as of January 2020.[1]

For the Holocene, dates are relative to the year 2000 (e.g. Greenlandian began 11,700 years before 2000). For the beginning of the Northgrippian a date of 8,236 years before 2000 has been set.[2] The Meghalayan has been set to begin 4,250 years before 2000.[1]

'Tarantian' is an informal, unofficial name proposed for a stage/age to replace the equally informal, unofficial 'Upper Pleistocene' subseries/subepoch.

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.

The Middle Paleolithic (or Middle Palaeolithic) is the second subdivision of the Paleolithic or Old Stone Age as it is understood in Europe, Africa and Asia. Very broadly it dates to between around 300,000 and 30,000 years ago. There are considerable dating differences between regions. It is succeeded by the Upper Paleolithic subdivision.

Characteristics

  • It was the time when Homo neanderthalensis (300,000–30,000 years ago) lived. These hominids had an increasing control over their surroundings and later saw the emergence of modern humans around 100,000 years ago.
  • Stone tool manufacturing developed a more sophisticated toolmaking technique known as the prepared-core technique, which permitted the creation of more controlled and consistent flakes. These could sometimes be hafted onto wooden shafts as arrows to form more efficient composite tools. Standard sharp point wood spears were still prevalent in the Middle Paleolithic age.
  • Hunting provided the primary food source but people also began to exploit shellfish and may have begun smoking and drying meat to preserve it. This would have required a mastery of fire (attested from ca. 800,000 years ago) and some sites indicate that plant resources were managed through selective burning of wide areas.
  • Artistic expression emerged for the first time (although some examples of artistic expression such as the Venus of Tan-Tan date back earlier to the Lower paleolithic around 850,000 BCE), with ochre used as body paint and some early rock art appearing. There is also some evidence of purposeful burial of the dead, which may indicate religious and ritual behaviours.

Middle Paleolithic cave sites

Middle Paleolithic open-air sites

See also

External links

References

  1. ^ a b c Cohen, K. M.; Finney, S. C.; Gibbard, P. L.; Fan, J.-X. (January 2020). "International Chronostratigraphic Chart" (PDF). International Commission on Stratigraphy. Retrieved 23 February 2020.
  2. ^ a b Mike Walker; et al. (December 2018). "Formal ratification of the subdivision of the Holocene Series/Epoch (Quaternary System/Period)" (PDF). Episodes. 41 (4). Subcommission on Quaternary Stratigraphy (SQS): 213–223. doi:10.18814/epiiugs/2018/018016. Retrieved 11 November 2019. This proposal on behalf of the SQS has been approved by the International Commission on Stratigraphy (ICS) and formally ratified by the Executive Committee of the International Union of Geological Sciences (IUGS).