Paleolimnological investigations of anthropogenic environmental change in Lake Tanganyika: I. An introduction to the project

被引:28
作者
Cohen, AS [1 ]
Palacios-Fest, MR
McGill, J
Swarzenski, PW
Verschuren, D
Sinyinza, R
Songori, T
Kakagozo, B
Syampila, M
O'Reilly, CM
Alin, SR
机构
[1] Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA
[2] Terra Nostra, Tucson, AZ 85741 USA
[3] US Geol Survey, St Petersburg, FL 33701 USA
[4] State Univ Ghent, Dept Biol, Res Grp Limnol, B-9000 Ghent, Belgium
[5] Dept Fisheries, Mpulungu, Zambia
[6] Minist Geol & Mines, Bujumbura, Burundi
[7] Ctr Rech Hydrol, Bujumbura, Burundi
[8] Vassar Coll, Dept Biol, Poughkeepsie, NY 12604 USA
[9] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA
基金
美国国家科学基金会;
关键词
deforestation; East Africa; Lake Tanganyika; Late Holocene; soil erosion; sediment pollution;
D O I
10.1007/s10933-005-2392-6
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We investigated paleolimnological records from a series of river deltas around the northeastern rim of Lake Tanganyika, East Africa (Tanzania and Burundi) in order to understand the history of anthropogenic activity in the lake's catchment over the last several centuries, and to determine the impact of these activities on the biodiversity of littoral and sublittoral lake communities. Sediment pollution caused by increased rates of soil erosion in deforested watersheds has caused significant changes in aquatic communities along much of the lake's shoreline. We analyzed the effects of sediment discharge on biodiversity around six deltas or delta complexes on the east coast of Lake Tanganyika: the Lubulungu River delta, Kabesi River delta, Nyasanga/Kahama River deltas, and Mwamgongo River delta in Tanzania; and the Nyamuseni River delta and Karonge/Kirasa River deltas in Burundi. Collectively, these deltas and their associated rivers were chosen to represent a spectrum of drainage-basin sizes and disturbance levels. By comparing deltas that are similar in watershed attributes (other than disturbance levels), our goal was to explore a series of historical "experiments" at the watershed scale, with which we could more clearly evaluate hypotheses of land use or other effects on nearshore ecosystems. Here we discuss these deltas, their geologic and physiographic characteristics, and the field procedures used for coring and sampling the deltas, and various indicators of anthropogenic impact.
引用
收藏
页码:1 / 18
页数:18
相关论文
共 52 条
[21]   Subfossil Chironomidae from Lake Tanganyika, east Africa - 2. Chironominae (Chironomini and Tanytarsini) [J].
Eggermont, H ;
Verschuren, D .
JOURNAL OF PALEOLIMNOLOGY, 2003, 29 (04) :423-457
[22]   Impact of soil erosion in disturbed tributary drainages on the benthic invertebrate fauna of Lake Tanganyika, East Africa [J].
Eggermont, H ;
Verschuren, D .
BIOLOGICAL CONSERVATION, 2003, 113 (01) :99-109
[23]   Subfossil Chironomidae from Lake Tanganyika, East Africa - 1. Tanypodinae and Orthocladiinae [J].
Eggermont, H ;
Verschuren, D .
JOURNAL OF PALEOLIMNOLOGY, 2003, 29 (01) :31-48
[24]  
Fairhead J., 1996, Misreading the African landscape: society and ecology in a forest-savanna mosaic.
[25]  
Fairhead J., 1998, REFRAMING DEFORESTAT
[26]  
FREY D G, 1988, Journal of Paleolimnology, V1, P179
[27]  
GAHAMA, 1983, BURUNDI SOUS ADM BEL
[28]   WATER-LEVEL FLUCTUATIONS OF LAKE TANGANYIKA IN PHASE WITH OCEANIC CHANGES DURING THE LAST GLACIATION AND DEGLACIATION [J].
GASSE, F ;
LEDEE, V ;
MASSAULT, M ;
FONTES, JC .
NATURE, 1989, 342 (6245) :57-59
[29]   THE LATE PLEISTOCENE AND HOLOCENE STRATIGRAPHY AND PALEOLIMNOLOGY OF LAKES KIVU AND TANGANYIKA [J].
HABERYAN, KA ;
HECKY, RE .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 1987, 61 (3-4) :169-197
[30]  
KOPONEN J, 1988, MONOGR FINNISH SOC D, V2, P434