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The Prehistory of North Africa spans the period of earliest human presence in the region to gradual onset of historicity in the Maghreb (Tamazgha) during classical antiquity.

Early anatomically modern humans are known to have been present at Jebel Irhoud, in what is now Morocco, from about 300,000 years ago.[2] The Nile valley (Ancient Egypt) participated in the development of the Old World Neolithic, Bronze Age and Iron Age, along with the Ancient Near East. By contrast, the Maghreb, including the "Green Sahara", remained in the Mesolithic stage until the 4th millennium BC, with gradual introduction of the Neolithic nomadic pastoralism in the 3rd millennium BC, and early Iron Age Phoenician colonization along the Mediterranean coast from about 1100 BC.

Saharan climate and human migration

Carvings of fauna common in the Sahara during the wet phase, found at Tassili in the central Sahara

Human habitation in North Africa has been greatly influenced by the climate of the Sahara (currently the world's largest warm desert), which has undergone enormous variations between wet and dry over the last few hundred thousand years.[3] This is due to a 41000-year Axial tilt cycle in which the tilt of the earth changes between 22° and 24.5°.[4] At present (2000 AD), we are in a dry period, but it is expected that the Sahara will become green again in 15000 years (17000 AD).

During the last glacial period, the Sahara was much larger than it is today, extending south beyond its current boundaries.[5] The end of the glacial period brought more rain to the Sahara, from about 8000 BC to 6000 BC, perhaps because of low pressure areas over the collapsing ice sheets to the north.[6] Once the ice sheets were gone, the northern Sahara dried out. In the southern Sahara, the drying trend was initially counteracted by the monsoon, which brought rain further north than it does today. By around 4200 BC, however, the monsoon retreated south to approximately where it is today,[7] leading to the gradual desertification of the Sahara.[8] The Sahara is now as dry as it was about 13,000 years ago.[3]

These conditions are responsible for what has been called the Sahara pump theory. During periods of a wet or "Green Sahara", the Sahara becomes a savanna grassland and various flora and fauna become more common. Following inter-pluvial arid periods, the Sahara area then reverts to desert conditions and the flora and fauna are forced to retreat northwards to the Atlas Mountains, southwards into West Africa, or eastwards into the Nile Valley. This separates populations of some of the species in areas with different climates, forcing them to adapt, possibly giving rise to allopatric speciation.[citation needed]

In terms of human evolution, the Saharan pump has been used to date four waves of human migration from Africa, namely:[9][failed verification]

Early and middle Paleolithic

anatomically modern humans are known to have been present at Jebel Irhoud, in what is now Morocco, from about 300,000 years ago.[2] The Nile valley (Ancient Egypt) participated in the development of the Old World Neolithic, Bronze Age and Iron Age, along with the Ancient Near East. By contrast, the Maghreb, including the "Green Sahara", remained in the Mesolithic stage until the 4th millennium BC, with gradual introduction of the Neolithic nomadic pastoralism in the 3rd millennium BC, and early Iron Age Phoenician colonization along the Mediterranean coast from about 1100 BC.

Human habitation in North Africa has been greatly influenced by the climate of the Sahara (currently the world's largest warm desert), which has undergone enormous variations between wet and dry over the last few hundred thousand years.[3] This is due to a 41000-year Axial tilt cycle in which the tilt of the earth changes between 22° and 24.5°.[4] At present (2000 AD), we are in a dry period, but it is expected that the Sahara will become green again in 15000 years (17000 AD).

During the last glacial period, the Sahara was much larger than it is today, extending south beyond its current boundaries.[5] The end of the glacial period brought more rain to the Sahara, from about 8000 BC to 6000 BC, perhaps because of low pressure areas over the collapsing ice sheets to the north.[6] Once the ice sheets were gone, the northern Sahara dried out. In the southern Sahara, the drying trend was initially counteracted by the monsoon, which brought rain further north than it does today. By around 4200 BC, however, the monsoon retreated south to approximately where it is today,[7] leading to the gradual desertification of the Sahara.[8] The Sahara is now as dry as it was about 13,000 years ago.[3]

These conditions are responsible for what has been called the Sahara pump theory. During periods of a wet or "Green Sahara", the Sahara becomes a savanna grassland and various flora and fauna become more common. Following inter-pluvial arid periods, the Sahara area then reverts to desert conditions and the flora and fauna are forced to retreat northwards to the Atlas Mountains, southwards into West Africa, or eastwards into the Nile Valley. This separates populations of some of the species in areas with different climates, forcing them to adapt, possibly giving rise to allopatric speciation.[citation needed]

In terms of human evolution, the Saharan pump has been used to date four waves of human migration from Africa, namely:[9]<

During the last glacial period, the Sahara was much larger than it is today, extending south beyond its current boundaries.[5] The end of the glacial period brought more rain to the Sahara, from about 8000 BC to 6000 BC, perhaps because of low pressure areas over the collapsing ice sheets to the north.[6] Once the ice sheets were gone, the northern Sahara dried out. In the southern Sahara, the drying trend was initially counteracted by the monsoon, which brought rain further north than it does today. By around 4200 BC, however, the monsoon retreated south to approximately where it is today,[7] leading to the gradual desertification of the Sahara.[8] The Sahara is now as dry as it was about 13,000 years ago.[3]

These conditions are responsible for what has been called the Sahara pump theory. During periods of a wet or "Green Sahara", the Sahara becomes a savanna grassland and various flora and fauna become more common. Following inter-pluvial arid periods, the Sahara area then reverts to desert conditions and the flora and fauna are forced to retreat northwards to the Atlas Mountains, southwards into West Africa, or eastwards into the Nile Valley. This separates populations of some of the species in areas with different climates, forcing them to adapt, possibly giving rise to allopatric speciation.[citation needed]

In terms of human evolution, the Saharan pump has been used to date four waves of human migration from Africa, namely:[9][failed verification]

The earliest inhabitants of central North Africa have left behind significant remains: early remnants of hominid occupation in North Africa, for example, were found in Ain el Hanech, in Setif (c. 200,000 BCE); in fact, more recent investigations have found signs of Oldowan technology there, and indicate a date of up to 1.8 million BC.[11] Some studies have placed the earliest settlement of homo sapiens in North Africa to around 160,000 years ago.[12] According to some sources,[who?] North Africa was the site of the highest state of development of Middle Paleolithic flake-tool techniques. Tools of this era, starting about 130,000 BCE, are called Aterian[citation needed](after the site Bir el Ater, south of Annaba) and are marked by a high standard of workmanship, great variety, and specialization.

Humans in North Africa (Nazlet Sabaha, Egypt) are known to have dabbled in chert mining, as early as ~100,000 years ago, likely for use as tools.[13][14]

Late Paleolithic and Mesolithic

The earliest blade industries in North Africa belong to the Iberomaurusian or Oranian (after a site near Oran). This lithic industry appears to have spread throughout the coastal regions of North Africa between 15,000 and 10,000 BC. Between about 9000 and 5000 BC, the Capsian culture made its appearance showing signs to belong to the Neolithic and began influencing the Iberomaurusian, and after about 3000 BC the remains of just one human culture can be found throughout the former region. Neolithic society (marked by animal domestication and subsistence agriculture) spread in the Saharan and Mediterranean North Africa after the Levant between 6000 and 2000 BC. This type of economy, so richly depicted in the Tassili n'Ajjer cave paintings, predominated in North Africa until the classical period.[Nazlet Sabaha, Egypt) are known to have dabbled in chert mining, as early as ~100,000 years ago, likely for use as tools.[13][14]

The earliest blade industries in North Africa belong to the Iberomaurusian or Oranian (after a site near Oran). This lithic industry appears to have spread throughout the coastal regions of North Africa between 15,000 and 10,000 BC. Between about 9000 and 5000 BC, the Capsian culture made its appearance showing signs to belong to the Neolithic and began influencing the Iberomaurusian, and after about 3000 BC the remains of just one human culture can be found throughout the former region. Neolithic society (marked by animal domestication and subsistence agriculture) spread in the Saharan and Mediterranean North Africa after the Levant between 6000 and 2000 BC. This type of economy, so richly depicted in the Tassili n'Ajjer cave paintings, predominated in North Africa until the classical period.[citation needed]

Saharan rock art was produced in the "Green Sahara" during the Neolithic Subpluvial period (about 8000 to 4000 BC). They were executed by hunter-gatherers of the Capsian period who lived in a savanna region teeming with giant buffalo, elephant, rhinoceros, and hippopotamus.[citation needed]

The Mesolithic cultures producing rock art (notably that at Tassili n'Ajjer in southeastern Algeria) flourished during the Neolithic Subpluvial.[citation needed]

Neolithic

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