Berichte des Sonderforschungsbereichs 268
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04, 131
All over the world meat plays an important role in the nutrition of people. Mostly it is considered to be a special source of strength and health. In many peoples' minds the consumption of animal products, such as muscle, fat, blood, inner organs and bones, is much more associated with vital strength than a vegetarian meal. A reason for this may be the inherent physical similarity between human being and animal, especially mammals. There are other ways of producing meat, such as hunting and fishing, but today the most common method is butchering. The people in Tenkodogo consider beef to be an excellent meat. We will focus our comparative studies on special occasions, specialised butchers, locations, times, technical methods, distribution and ideas connected with the production and consumption of beef. Two fundamental reasons for the butchering of cattle can be identified: firstly, bulls are killed during the rituals of the year and secondly, cattle is slaughtered for daily commercial purposes on the market. In both cases almost the entire carcass of the butchered animal is consumed by people. In Tenkodogo we can actually compare those two different reasons, which have at least one common impact.
08, 349
In the inundation area - the basin of the former larger Lake Chad - a special type of sorghum is grown on the clay soils (firgi). This dry-season guinea corn is also called dwarf sorghum or masakwa. In Kanuri, the dominant language in the region, sorghum is called ngawuli. The dry-season types are called ngawuli firgibe (lit. translated: sorghum of the firgi). During the dry season when the natural vegetation becomes dry and yellow, masakwa fields appear in prominent green covering large areas of the clay plains. The most important natural factor for this specialized dry season cropping is the presence of soils with a high clay content. For a better understanding of masakwa and its related issues, a multidisciplinary sub-project (G1) has been established within the SFB 268 (Joint Research Project: History of Culture and Language in the Natural Environment of the West-African Savannah). This project in which all disciplines participate is entitled: "Natural basis for masakwa cultivation and its meaning for the settlement history of the clay plains (firgi) in the Chad basin".
02, 255
The Lake Chad Basin is a major geographical region in the central part of the Sudan zone of Africa. The northern parts, however, extend into the Sahel and the southern parts of the Sahara desert. It consists of an extensive shallow depression of about 1.536.000 km2 (600.000 miles2) of which about 10% lies in Nigeria. The greater part is shared between the three countries of Cameroon, Chad and Niger. Climatically and agriculturally, the Chad Basin lies within the dry or semi-arid zone of Nigeria. It is a marginal area which has experienced severe droughts and considerable environmental changes in recent years. The natural environment, its use and misuse, and the threat of life posed by environmental pollution dominate discussions on environmental change. But in addition to the natural or physical environment, there are other equally important 'environments' which deserve some attention in view of the role that they play in generating economic growth and in ensuring sustainable development which is the central issue in our concern about the environment. These other environments are the cultural environment, the political environment and the economic environment, both internal and external. In the Chad Basin, all these other environments, along with the natural environment have been greatly influenced by its land locked location in the heart of Africa.
02, 227
The account of Borno's war with Mandara thus recounted above, at least from the point of view of the Mandara Chronicler, and all the other accounts I have given above clearly portray to us the essence of the Mune in that oppression and/or a war of caprice is not enjoined. And the war against Mandara was clearly a war of caprice, as Mandara had clearly recanted on its recalcitrance, when threatened. The essence of the Chronicle itself, however, is that we are here seeing, from accounts of an eye-witness, the portrayal of a polity whose language principles and practice of diplomacy, in war and in peace, are not less developed than any we have seen in the states of Euro-Germanic experience, of comparable times. The basis of this well ordered art is essentially the Mune, even though in its universalist form we may wish to assign it to the Book and the Sunna of Islam. Why not then, should we not regard the Mune as the constitution of the pre-colonial Borno State? Munen - ba (not in the Mune), for the Sayfawa ruler is certainly more binding than most modern constitutions had been binding on leaders of present-day African States!
14, 011
The investigations carried out within the project in NE-Nigeria since 1989 have been focussing on the late Pleistocene and Holocene landscape development of the south eastern Chad basin. Areas of interest include palaeodune fields, clay plains and former beach ridge systems of Lake Chad. Transgressions and regressions of Lake Chad played an important role in the younger landscape history of NE-Nigeria and have also caused great environmental changes. The term „Megachad“ is well known and describes an enormous lake with an extension comparable with the Caspian Sea of today. The term „Microchad“ stands for the other recent extreme in terms of the lake dimensions varying during the times. Environmental changes in the surroundings of Lake Chad are closely connected with transgressions and regressions of the lake. These lake level changes can be climatically induced as well as non-climatically, due to human impact. Nearly all land units have more or less been influenced by the lake, spatially as well as temporally. It is important, though, to notice the scales of the changes. Some changes took place in a millennial scale, some in the scales of centuries or decades, and at least – as can be observed every year – in a seasonal scale.
08, 335
The objective of this paper is to combine the environmental conception of the Kanuri with detailed findings of pedological and botanical field investigations. Interpretation of multitemporal satellite data and aerial photographs should provide land cover and land use information for an extended area. The area of investigation was outlined within the transitional zone from the clay plains to the sandy areas by interpretation of satellite images. The presented subset of a SPOT-XS-satellite image shows part of the Marte Local Government Area with its capital Old Marte in the north-eastern part of the image. The darker colours represent the clay plains while the lighter parts are related to the sandy areas. Almost half of the research area is covered by clay but all settlements are located on the slightly elevated sandy areas. Within these sandy areas different gray shades demonstrate the pattern of the rainy season farming area. Differences in colour within the clay plains are mainly due to variances in soil, water content and vegetation cover. In the north-eastern part of the image irrigation channels of the South Chad Irrigation Project are visible. The main attention, especially of the pedological and botanical research, was directed towards the south-western part of the subset in the vicinity of the villages of Wulwa, Dura, Kajere and Ngubdori.
02, 197
Yerwa is the last of the Borno capitals. Although established in the first decade of colonial administration, it cannot be compared with the many other towns like Fort Lamy, Jos, Kaduna, Niamey et al. which all developed about the same time. Colonial interference with the development of Yerwa appears restricted, mainly, to insistence upon wider roads than a Borno town otherwise would have featured and resettlement schemes, e.g. Mafoni, Ari Askeri. The following is based on the premise that as the town - despite time and political circumstances of its emergence - is a distinctive Borno town, also occupational diversification and structure are distinctively related to urban Borno culture.
08, 321
Two sites situated in the Sahelian and Sudanian zones of NE-Nigeria were chosen for pollen analysis. A sediment core from an interdunal depression in the eastern Manga Grassland provides information on the Holocene vegetation history of the Sahel between c. 9600-3400 B.P. The 3 m pollen record indicates an open savanna during the mid-Holocene. The presence of Sudano-Guinean taxa, which were mainly restricted to the interdunal depressions, points to more humid conditions. Already before c. 4000 B.P., a slow change towards drier conditions and the establishment of the modern Sahelian vegetation is visible in the diagram. This development was accompanied by high fire frequencies. A 16 m core from a crater lake (Lake Tilla) in the Sudanian zone of NE-Nigeria provides a pollen record which can be dated back to approximately 11-12000 B.P. Preliminary pollen spectra show a relatively constant pattern with a dominance of grass pollen even during the middle Holocene.
14, 021
Numerous ecologists postulate that West African savannas are mostly the result of degradation of formerly closed forests. This hypothesis can only be tested by palaeoecological investigations. The palynological results summarised in this paper document the history of the Sudanian and Sahelian savanna of NE-Nigeria during the last 11.500 years (uncal. BP). Both sites investigated provide evidence for the persistence of savanna throughout the entire Holocene. Patches of closed dry forest may have occurred, but never completely displaced the savanna vegetation. Humid conditions during the early and mid Holocene (from 10.000 BP onwards) caused a rapid spread of Guinean and Sudanian taxa into the northern vegetation zones. A slow return to drier climatic conditions between ca. 6800 BP and ca. 5500 BP can be recorded at both sites. Finally, between 3800 BP and 3300 BP a strong aridification resulted in the establishment of the modern vegetation zones. In both the Sahelian and Sudanian zone the vegetational changes appear to have been primarily controlled by climatic changes, whereas the effects of human activities remain palynologically silent even for the late Holocene.
04, 111
Tenkodogo, a township situated in the south-eastern part of Burkina Faso on the road leading from the capital Ouagadougou to the Togo border, has approximately 29,000 inhabitants. It is Burkina's seventh largest town and is the location of the regional government of the Boulgou-Province. This regional government is represented by a high-commissioner and a "préfet" as it is the residence of a traditional ruler, otherwise known as Tenkodogo-naaba. His sphere of influence covers many villages and hamlets in the region: in total he is the sovereign of nearly 120,000 people. The power of the traditional rulers was curtailed first by the arrival and following overrule of the French colonialists and then after independence by Sankara and his revolutionary government. The kings ceased to be the ultimate judges who were able to determine life and death of their subjects. Henceforth they were no longer allowed to recruit subjects for certain work on their fields, and they no longer could claim control over the allocation of resources. Their position was strengthened anew by Sankara's successor in office, Blaise Campaore, who quickly recognized that collaborating with the traditional rulers could only be of advantage: in fact they later proved to be his best supporters in the election campaign.