Berichte des Sonderforschungsbereichs 268
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14, 415
Over approximately the last 200 years, north-west Ghana and large areas of neighbouring southern Burkina Faso were the stage for a highly successful expansion of Dagara-speaking peoples. Probably setting out from an area around Wa, small groups of Dagara migrated towards the north, some of them taking a westward route, crossing the Black Volta river into today’s Burkina Faso. They rarely advanced into nomansland but rather displaced peoples such as Sisala-, Dyan-, Phuie- and Bwamu-speaking groups, who then moved further west and north. Today, the Dagara occupy about 3500 km2 in southern Burkina Faso, where they represent the sixth largest language group. In this paper I wish to explore the history of the north-west frontier of Dagara expansion and the interaction between the “land-owning” Phuo and the incoming Dagara.
14, 179
The aim of our project B6 “Towards a genesis of the ethnolinguistic situation at the southern and western fringes of lake Chad basin” within SFB 268 “West African Savannah” is to analyse the emergence and development of the complex presentday ethnolinguistic patterns in a region which may be historically labelled as southern and western periphery of the Borno empire. For the first time, a model of migratory routes was put forward based on combined research efforts of the disciplines involved in our project. Below we shall attempt to summarise the main points and reflections of our findings. Our specific approach as a whole is based on applying the respective research methods of the individual disciplines represented in our project, namely anthropology, ethnomusicology, history and linguistics and eventually on integrating the results into a systemically coherent picture
14, 071
The conflict I refer to happened at the beginning of the 1998 farming season when the distribution of land started. The seasonal migrants went into the village area were they had been farming since many years, they gave their contributions and payments to the respective officials and started to prepare the land. Shortly after they had started to plant the beans – the main cash crop beside fishing – they were harassed by armed people and had to leave the area. Only several weeks later they were able to go back to their prepared fields and proceeded with their farming business. The question I want to concentrate on is related to the topic of the ethnological sub-project – “Community building in newly founded settlements in the Lake Chad area” – and can be specified as “What do conflicts tell us about the community and people involved?”
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.
14, 169
Summary and evaluation
(2000)
The geographical analysis of the Savannah Zones of north-eastern Nigeria revealed a basic insight on the differentiated development at the meso-regional level: The northern districts had a much lower population increase than the average. It was already arid land before the dramatic reduction of precipitation since the late 1960s. The quality of the soil for farming is rather poor despite specific minerals which give grass during the very short growing season a higher nutritional value than further south. Through studies at the local level, it became evident that on one side this is an area of out-migration of the local population but on the other side we have to register the influx of migrants from the even more dryer northern districts including Niger Republic. The rate of urbanisation in Nigeria increased rapidly from 15 to 36 %. Northern capitals like Kano and Maiduguri multiplied their number of inhabitants seven times but were overtaken by Gombe’s growth. In any case they are centres of social and cultural change as the preliminary findings of H. BALZEREK concerning the boom-town Gombe revealed. But social tensions seem to be inevitable as religious movements not only in big towns like Kano but even in Gombe were already analysed by WATTS (1993, 61). The bearer/ carriers of this movement are landless people who did not migrate to new land in the country side, they are hoping for new jobs in an urban environment. The social structure has changed since the time of the old Hausa towns, but their reliance on surplus of labour force appears to have continued.
14, 125
The search for persistent elements in nature and culture, which comprises language as a constitutive part, is a prerequisite for the definition of any change which is the aim of our common project. When analysing the process of transformation by a number of disciplines we expect to discover significant features of this alteration and the forces dominating it. The current highly complex present linguistic situation in the western and south-western fringe of the Chad Basin will be reconstructed from the historical migrations undertaken by the various linguistic groups from Lake Chad (mainly Chadic languages) to their present settlements. The six authors, the linguists Dr. Dimitr Ibriszimov, Dr. Doris Löhr, Christopher Mtaku, the ethno-musicologist Dr. Raimund Vogels, and the historian Ibrahim Maina Waziri integrated the results of their studies into one paper towards a systemic approach by tracing back the common roots of the languages, the customs and the music of those peoples and give an outline of their tradition concerning their movements. A basic dual model of migration will be put forward.
08, 193
The architecture and chemistry of a dug-out: the Dufuna Canoe in ethno-archaeological perspective
(1996)
It is the intention of this paper to highlight the processes involved in the production of a dug-out. Two disciplines appear strikingly clear in the title of this paper; architecture and chemistry. It is deliberate, exhibiting the multifaceted approach to issues in archaeology. The Dufuna canoe, the main subject of the discussion, is entirely an organic material, long used by prehistoric populations, abandoned and covered in a huge deposit of earth, unearthed by the spade in two streams of excavations for the purpose of dating, measurements, documentation, which yielded a date of 8500 years as the oldest canoe in Africa and one of the oldest in the world. Who could have produced such an "artefact"? These and other related questions are fundamental towards the understanding of the history and society that lived in that environment in prehistory. Since we are dealing with a single "artefact" produced by prehistoric populations, long gone and extinct, we would not be in a position to reconstruct the processes of manufacture of the dug-out by any source other than by ethno-archaeological and ethnographic investigation and experiment of the contemporary society which manipulates similar environment with a view to stimulating the past mode of production. The method used in the data collection was by oral interviews and field observation.
08, 215
The Yobe valley is one of the many refugia that dotted the Chad basin after the commencement of the desiccation of the Sahara. It hypothetically must have been attractive to the population that had to move away from the aridized zone in search of favourable ecotones. As the Mega Chad receded from its Bama ridge shores, new lands were progressively made available for human occupation along the valley. It is one of the principal goals of the Yobe Valley Archaeological project to investigate how and when this new valley was occupied. This paper has been divided into three principal sections. The first section deals with the search for the earliest settlements of the Yobe valley. The excavations conducted at Garingada and Damakarwa were aimed at tackling this problem. The second section deals with the development of complexity. The excavation at Gambaru was directed towards this problem. The third section seeks to discuss on the bases of the excavations at the three sites, manenvironment relationship. The concluding part of the paper focuses attention on the problems and prospects of the Yobe Valley Archaeological Project.
08, 077
Our dichotomy of ‘nature’ and ‘culture’ is expressed in the Kanuri language with the terms al@ga for ‘creation’ and ‘creature’ which embraces trees, mammals, birds, insects, humans, in short the whole of the natural environment, and ada for ‘custom, habit, way of behaviour, family tradition’ for culture as a whole. There is no genre of oral literature, which would describe al@ga as such, but aspects of it can always be expressed in proverbs, riddles, toponymic praise phrases and songs, of which those performed by the hunters figure most prominently in reflecting upon al@ga. Yet, in these songs (and partly in other genres) ideas about al@ga are not purely descriptive in naturalists’ terms. They are much rather expressions, which centrally combine notions of the social and natural environment.
08, 101
The paper presents a short introduction to the environmental factors, e.g. climate, geology, relief forms and soils of the study area in the southern parts of the Gongola Basin. The study area covers the high mountain range of the Tangale-Waja Uplands and the adjacent pediplain, following in the north. It is asked if the natural factors enforced former inhabitants of the area to develop special land use techniques like field terracing to ensure the essential crop production under insufficient geoecological conditions.