The process leading to agriculture was very slow in the Eastern Sahara and farming, progressing inevitably to plant domestication was not the final goal. At least two important stages of selective cultivation without farming or genetic modification were successfully reached. They represent, respectively, cultivation with small-scale clearance and minimal tillage, and cultivation with larger-scale clearance and systematic tillage. Thus, cultivation is an elaborate form of plant exploitation without domestication.
At Nabta Playa and Bir Kiseiba, a new economy of intensive plant collection came into being, during the El Nabta/El Jerar humid interphase dated from around 8000 to 7300 years BP. During this period, numerous large, bell-shaped storage pits indicated intensive exploitation and preservation of fruits, tubers, and seeds, including large quantities of wild sorghum (Sorghum bicolor) and two kinds of millet (Panicum turgidum and Echinochloa colona). In some particularly favorable years, sorghum may have been cultivated with the decrue, or dry farming, technique. This system requires sowing seeds over flooded land without irrigation, and collecting with a technique that implies cross-pollination, which, unlike self-pollination, prevents the propagation of the genetic changes typical of domestication. Such a technique could have required shaking the harvest into baskets, instead of using sickles or removing the entire plant.
At Farafra Oasis, a site in the Hidden Valley was located on the shore of an ancient water basin and exhibited numerous habitation structures with hearths containing numerous plant remains, including burnt cereal grains that have suggested independent protoagricultural activities. Three main occupation phases were identified, the earliest being dated between 7670 and 7320 BP, the second around 6750 BP, and the latest at 6190 BP. Grasses include Brachiaria, Cen-chrus, Digitaria, Echinochloa, Panicum, and Setaria, belonging to the millet group, and Sorghum, which represents 40.6% of the paleobotanical samples. The high frequency of Sorghum may be due to the large size of its grains, which could have been preferred for their size and better nutritional properties. Furthermore, Sorghum is particularly suitable for this semidesert environment as it can tolerate hot and dry conditions, as well as salty soils. The area with circular structures, stone-lined hearths, and over 180 plant samples, most of them belonging to Sorghum, was dated between 7100 and 6700 BP. As there are no signs of genetic change, it is most likely that the plants were collected by hand and exploited using soft material artifacts, such as wood, whereas stone tools were only used later. Tamerix and Acacia, which were exploited for fuel, could also have been used the manufacturing of wooden implements.
Cultivation practices began in the Western Desert at a significantly earlier date than in the Nile Valley. On the other hand, full domestication of sorghum and pearl millet took place in Africa in a still undetermined time, but not before the fourth millennium BP, whereas barley and emmer wheat were not local domesticates, but imported from southwest Asia into the Nile Valley. They are attested to in the Delta and lower Nile Valley from the end of the seventh millennium BP. However, as they required a humid habitat with constant fresh water, which was not available outside the Nile Valley, they were unsuitable for the Eastern Sahara.
Harris DR (1996) Domesticatory relationships ofpeople, plants and animals. In: Ellen R and Fukui K (eds.) Redefining Nature: Ecology, Culture and Domestication, pp. 437-463. Oxford: Berg.
Hassan FA (ed.) (2002) Droughts, Food and Culture. New York: Kluwer Academic/Plenum.
Hoelzmann P (2001) A palaeolimnological N-S transect through the Eastern Sahara. In: Gasse F, Battarbee R, and Stickley C (eds.) Past Climate Variability through Europe and Africa. An International Conference. Aix-en-Provence: Centre des Congress.
Lanssen-Erz T, Tegtmeier U, and Krtopelin S (eds.) (2002) Tides of the Desert: Contributions to the Archaeology and Environmental History of Africa in Honour of Rudolf Kuper. Ktoln: Heinrich-Barth-Institut.
McDonald MMA (1998) Early African pastoralism: View from Dakhleh Oasis (South Central Egypt). Journal ofAnthropologi-cal Archaeology 17: 124-142.
Nelson K (2002) Holocene Settlement of the Egyptian Sahara, Vol. 2: The Pottery ofNabta Playa. New York: Kluwer Academ-ic/Plenum.
Stahl AB (ed.) (2005) African Archaeology: A Critical Introduction. Oxford: Blackwell Publishing.
Van der Veen M (ed.) (1999) The Exploitation ofPlant Resources in Ancient Africa. New York: Kluwer Academic/Plenum.
Vermeersch PM, VanPeer P, and Moeyersons J (1996) Neolithic occupation of the Sodmein area, Red Sea Mountains, Egypt. In: Pwiti G and Soper R (eds.) Aspects of African Archaeology. Papers from the 10th Congress of the PanAfrican Association for Prehistory and Related Studies, pp. 411-419. Harare: University of Zimbabwe.
Wendorf F and Schild R (1998) Nabta Playa and its role in northeastern African prehistory. Journal of Anthropological Archaeology 17: 97-123.
Wendorf F and Schild R (eds.) (2001) Holocene Settlements of the Egyptian Sahara: The Archaeology ofNabta Playa. Vol. 1. New York: Kluwer Academic/Plenum Press.
Wendorf F, Schild R, and Close AE (eds.) (1993) Egypt during the Last Interglacial: The Middle Paleolithic of Bir Tarfawi and Bir Sahara East. New York: Plenum Press.