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. 2011 Jan 11;108(2):458-62.
doi: 10.1073/pnas.1012231108. Epub 2010 Dec 27.

Ancient watercourses and biogeography of the Sahara explain the peopling of the desert

Affiliations

Ancient watercourses and biogeography of the Sahara explain the peopling of the desert

Nick A Drake et al. Proc Natl Acad Sci U S A. .

Abstract

Evidence increasingly suggests that sub-Saharan Africa is at the center of human evolution and understanding routes of dispersal "out of Africa" is thus becoming increasingly important. The Sahara Desert is considered by many to be an obstacle to these dispersals and a Nile corridor route has been proposed to cross it. Here we provide evidence that the Sahara was not an effective barrier and indicate how both animals and humans populated it during past humid phases. Analysis of the zoogeography of the Sahara shows that more animals crossed via this route than used the Nile corridor. Furthermore, many of these species are aquatic. This dispersal was possible because during the Holocene humid period the region contained a series of linked lakes, rivers, and inland deltas comprising a large interlinked waterway, channeling water and animals into and across the Sahara, thus facilitating these dispersals. This system was last active in the early Holocene when many species appear to have occupied the entire Sahara. However, species that require deep water did not reach northern regions because of weak hydrological connections. Human dispersals were influenced by this distribution; Nilo-Saharan speakers hunting aquatic fauna with barbed bone points occupied the southern Sahara, while people hunting Savannah fauna with the bow and arrow spread southward. The dating of lacustrine sediments show that the "green Sahara" also existed during the last interglacial (∼125 ka) and provided green corridors that could have formed dispersal routes at a likely time for the migration of modern humans out of Africa.

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Conflict of interest statement

The authors declare no conflict of interest.

Figures

Fig. 1.
Fig. 1.
Late Pleistocene and early Holocene palaeohydrology of the Sahara (∼11 to 8 ka). The catchments of the megalakes that form corridors across the Sahara are indicated with letters A–D, while the river catchments that link with many of these megalake basins to form the vast Saharan inland waterway are indicated with letters E–I: (A) Lake Megachad, (B) Lake Megafezzan, (C) Ahnet-Mouydir Megalake, (D) the Basin of the Chotts, (E) Senegal River, (F) Nile River, (G) Sahabi River, (H) Kufra River, and (I) Niger River. Numbers indicate the location of fan, tectonic and lake outflow links between basins: (1) Nile Basin/Chad Basin, (2) Chad Basin/Niger Basin, (3) Niger Basin/Senegal Basin, (4) Niger/Basin West Ahaggar Mountains, (5) West Ahaggar Mountains/Ahnet-Mouydir Basin, (6) Ahnet-Mouydir Basin/Chotts Basin, (7) Chotts Basin/Fezzan Basin, (8) Fezzan Basin/Serir Tibesti, and (9) Serir Tibesti/Kufra Basin. The 200-mm isohyet indicates the current limit of the Sahara Desert.
Fig. 2.
Fig. 2.
Late Pleistocene and early Holocene palaeohydrology and biogeography of the Sahara (∼11 to 8 ka). (A) Biogeographic provinces for the African fish species are indicated (1 Sudanian, 2 Upper Guinean, 3 Eburneo-Guinean, 4 Lower Guinean, 5 Congo, 6 Maghrebian) along with the distribution of Tilapia zillii, both recently, as indicated by the hatched area and from marking the location of Saharan refuges, and during the Holocene, as indicated by fossils and rock art. A trans-Sahara distribution is evident, both across the Sahara and down the Nile. (B) Distribution of Hippopotamus amphibious both historically (∼1 ka) as shown by the hatched area and during the Holocene by marking the location of older historical sightings, fossils, and rock art. A distribution restricted to the River Nile and the southern-central Sahara is evident.
Fig. 3.
Fig. 3.
Sahara palaeohydrology overlaid with the spatial distribution of Ounanian and barbed bone points and Nilo-Saharan languages. The languages marked as “other” are too small to be depicted as separate colors; they are Nyimang, Temein, Hill Nubian, Daju, Berta, and Gumuz. Note the similarity between the distribution of barbed bone points and the distribution of species that require deep water (Fig. 2B and SI Appendix, Figs. S12 and S13).
Fig. 4.
Fig. 4.
Palaeohydrology of North Africa during MIS5 with the location of dated sites marked. The hatched area covers catchments containing large palaeolakes and thus represents the minimum area which experienced considerably enhanced humidity during MIS5.

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