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The Kiffian culture is a prehistoric industry, or domain, that existed between approximately 8,000 BC and 6,000 BC in the Sahara Desert, during the African humid period referred to as the Neolithic Subpluvial.
The modern, arid Sahara. The Sahara was not a desert during the African humid period. Instead, most of northern Africa was covered by grass, trees, and lakes. The African humid period (AHP; also known by other names) was a climate period in Africa during the late Pleistocene and Holocene geologic epochs, when northern Africa was wetter than today.
Neolithic Subpluvial/African humid period in North Africa, wet 7000–3000: Holocene climatic optimum, or Atlantic in northern Europe (B-S) 6200: 8.2-kiloyear event cold 5000–4100: Older Peron warm and wet, global sea levels were 2.5 to 4 meters (8 to 13 feet) higher than the twentieth-century average 3900: 5.9 kiloyear event dry and cold. 3500
The Sub-Saharan West African Fulani, the North African Tuareg, and European agriculturalists, who are descendants of these Neolithic agriculturalists, share the lactase persistence variant –13910*T. [22] While shared by Fulani and Tuareg herders, compared to the Tuareg variant, the Fulani variant of –13910*T has undergone a longer period of ...
During the Neolithic period about 10,000 years ago, ancient hunters, the early Holocene Kiffian people, created rock engravings and cave paintings that can still be found across the region. The Neolithic Subpluvial was an extended meteorological period, from about 7,500-7,000 BC to about 3,500-3,000 BC, of relatively wet and rainy conditions in ...
The Kiffian culture is a prehistoric industry, or domain, that existed between 10,000 and 8,000 years ago in the Sahara, during the Neolithic Subpluvial. Human remains from this culture were found in 2000 at a site known as Gobero, located in Niger in the Ténéré Desert. [64]
The Tenerian culture is a prehistoric industry that existed between the 5th millennium BC and mid-3rd millennium BC in the Sahara Desert.This spans the Neolithic Subpluvial and later desiccation, during the middle Holocene.
The end of the Neolithic Subpluvial era and return of extremely hot and dry conditions in the Sahara Desert, hastened by the 5.9 kiloyear event and the Piora Oscillation. 3500 BC 3200 BC Gerzeh/Naqada II culture in Egypt 3200 BC 3000 BC Naqada III and Protodynastic Period of Egypt: 3100 BC 2686 BC Early Dynastic Period of Egypt.