Henriette Alimen, 1965. "The Quaternary Era in the Northwest Sahara", International Studies on the Quaternary: Papers Prepared on the Occasion of the VII Congress of the International Association for Quaternary Research Boulder, Colorado, 1965, H. E. Wright, Jr., David G. Frey
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This note summarizes the research followed for nearly 15 years on the Quaternary of the Northwest Sahara. Stratigraphically it is possible to characterize the Villafranchian, with two pluvial-arid cycles (Aïdien and Mazzérien) ; the middle Quaternary, with two cycles (Taourirtien and Ougartien); and the late Quaternary, with a main cycle (Saourien) followed by a secondary cycle (Guirien). The sedimentary petrography has shown climatic indications in successive deposits (granulometry of pebbles and sands, various marks on pebbles, colorimetry of sands) and some chronological and paleogeographical indications (heavy minerals). Palynological studies in progress reveal the presence, at different times of the Quaternary, of Mediterranean and even temperate trees, associated with herbs of the Saharian steppe. The collections of all the Saharan prehistoric industries, in place in all Quaternary levels, is a useful element in dating. The Pebble Culture appears in the Mazzerien and the beginning of the Taourirtien. The Chelleen and the Acheuleen develop during the Taourirtien, and the Ougartien appears in a series of stages stratigraphically well defined. Aterien is present toward the base of the sourien deposits, and the Neolithic occurs in the Guirien. A radiocarbon analysis of 20,000 ± 1000 years B.P. dates a saourien level near the Aterien, and one of 6160 ± 320 dates the maximum of the Guirien sedimentation, of Neolithic age.