Economic Integration in Africa by Peter Robson London, Allen and Unwin, 1968. Pp. 320. 45s. - The Common Market & Development in East Africa by Philip Ndegwa Nairobi, East African Publishing House, 2nd edn.1968. Pp. 228. Shs. 20.

1970 ◽  
Vol 8 (2) ◽  
pp. 331-334
Author(s):  
Helen Kimble
1969 ◽  
Vol 7 (2) ◽  
pp. 277-287
Author(s):  
Donald C. Mead

This article explores the prospects for co-ordinated co-operative economic advance in East Africa. Its frame of reference reaches wider than simply an analysis of the 1967 Treaty.1 This broader viewpoint is important for two major reasons. In the first place, there are a number of aspects of economic interdependence which are not covered at all in the Treaty; the implication is that these will be of no direct concern to the institutions of the new East African Community (Kenya, Uganda, Tanzania). For example, the level of the external tariffs of the three countries is obviously crucial to the operation of the Common Market; among other reasons, this is because the maximum permissible transfer tax is defined in terms of the external tariff. Yet the committee responsible for setting external tariffs is not linked in any direct way with the institutional set-up in Arusha; it seems likely that decisions of the tariff committee will not be subject to discussion or appeal through these community institutions.


1981 ◽  
Vol 18 (2) ◽  
pp. 330-341 ◽  
Author(s):  
C. S. Churcher

The Olduvai zebra, Equus oldowayensis, is identified or confirmed from the following sites: Olorgesailie, Lake Magadi; Marsabit Road, Northern Kenya; Chemoigut Beds (Chesowanja), Baringo Basin; Wajir, Northeast Kenya; Bura, Tana River; Makalia River (MacInnes Site), Rift Valley; Legetet, Koru; Karmosit, Suguta River; and Kanjera, Homa Mountain, all in Kenya, on the evidence from isolated teeth and other fragments. Burchell's zebra, E. burchellii, appears to have been absent from all the sites except possibly Olorgesailie and the Chemoigut Beds.E. oldowayensis is known from about 1.8 Ma ago in Bed I at Olduvai Gorge and from about 1.9 Ma ago in the Shungura Formation (Member G) in the Omo deposits, before which no reliable records are recognised. It was the common and dominant zebra of the latest Pliocene and Pleistocene in the East African plains and was replaced by the present common zebra, E. burchellii, only during the latest Pleistocene and Holocene times. E. oldowayensis is similar to modern Grevy's zebra, E. grevyi, to which it gave rise, and these two zebras are not directly related to Burchell's zebra.


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