Climate-controlled Holocene occupation in the Sahara: motor of Africa's evolution.
Radiocarbon data from 150 archaeological excavations in the now hyper-arid Eastern Sahara of Egypt, Sudan, Libya, and Chad reveal close links between climatic variations and prehistoric occupation during the past 12,000 years. Synoptic multiple-indicator views for major time slices demonstrate the transition from initial settlement after the sudden onset of humid conditions at 8500 B.C.E. to the exodus resulting from gradual desiccation since 5300 B.C.E. Southward shifting of the desert margin helped trigger the emergence of pharaonic civilization along the Nile, influenced the spread of pastoralism throughout the continent, and affects sub-Saharan Africa to the present day.
Kuper
Rudolph
R
Collaborative Research Center 389 (ACACIA), University of Cologne, Institute of Prehistoric Archaeology, Africa Research Unit, Jennerstrasse 8, 50823 Köln, Germany.
Kröpelin
Stefan
S
D000383:Agriculture / Q000266:history; D000822:Animal Husbandry / Q000266:history; D001106:Archaeology; D002596:Chad; D002962:Civilization / Q000266:history*; D002980:Climate; D003468:Cultural Evolution; D003889:Desert Climate; D000076144:Egypt, Ancient; D004641:Emigration and Immigration; D004777:Environment; D049690:History, Ancient; D006801:Humans; D006813:Humidity; D008002:Libya; D011157:Population Dynamics; D011891:Rain; D013397:Sudan