Bangweulu - Mweru



ID


544

Author(s)


Lucy Scott, South African Institute for Aquatic Biodiversity, Grahamstown, South Africa


Countries


Democratic Republic of Congo
Malawi
Tanzania
Zambia

Reviewer(s)


Paul Skelton, South African Institute for Aquatic Biodiversity, Grahamstown, South Africa; Jean-Jacques Symoens, retired, University of Brussels, Brussels;  Harry Chabwela, University of Zambia, Lusaka, Zambia


Major Habitat Type


Tropical and subtropical floodplain rivers and wetland complexes

Drainages flowing into


The mainstem Congo River.


Main rivers to other water bodies


There are six major lakes within the Bangweulu complex: Lakes Bangweulu, Walilup, Chifunauli, Kampolombo, Kangwena, and Chale (Bailey 1986). None of the lakes are very deep (3-10 m), but all have extensive swamps associated with them that are important contributors to productivity. The Bangweulu swamps are fed by a series of rivers, the largest of which is the Chambeshi River, which also flows out of the swamps and joins with the Luapula River. The Luapula flows for about 480 km before reaching Mweru. This stretch of river contains the Mumbatuta and Johnson falls, each of which constitute barriers to fish movement in the dry season (Bell-Cross 1965). The Luvua River then leaves Lake Mweru and this ecoregion and eventually joins the Lualaba River. Lakes Bangweulu and Mweru, situated on a plateau at about 1,000 m elevation, are deflation lakes (floodplain lakes formed by erosive processes in which wind carries off alluvium) (Bowmaker et al. 1978; Burgis & Symoens 1987).



Description

Boundaries

This ecoregion is situated in the southeastern corner of the Democratic Republic of Congo and north-eastern Zambia. The ecoregion is a component of the southern headwaters of the Congo River and is typified by an extremely rich and endemic aquatic fauna within the permanent swamps and shallow lakes of the Bangweulu/Mweru systems. 

Topography

Granites underlie the Chambeshi River and much of the area around the Bangweulu swamps and extend to the Lower Luapula River. However, the entire region is dominated by recent alluvial deposits, shales, sandstones, quartzites, and conglomerates (Grimsdell & Bell 1975).

Freshwater habitats

Lake Bangweulu (2,070 km2) lies to the west of a considerable swamp (5,700 km2) and floodplain (6,000 km2). The Bangweulu basin is an old cratonic platform that has been subsiding over the last 20 million years (Denny 1985). There are indications that the lake was considerably larger in its recent geological history. The present-day lake is shallow (10 m) and unproductive, probably for edaphic reasons. The lake offers a relatively limited range of habitats with sandy beaches to the west, and predominantly Papyrus, Eleocharis, and Nymphaea vegetation bordering the remaining shoreline.

The Bangweulu swamps are permanent swamps, characterised by shallow lakes and a series of lagoons generally covered with Ceratophyllum, Utricularia, Nymphaea, Nyphoides sp., Potamogeton richardi, Trapa natans, Pistia stratiotes and Cyperus papyrus. These lagoons and lakes are connected by channels lined with vegetation such as Cyperus papyrus and Vossia cuspidata. The shallow swamps (1m deep), are vegetated by Eleocharis and Nymphaea, which gradually merge into grassy, annually flooded plains surrounding the swamps. During the dry season, decomposing vegetation generates low oxygen levels and high acidity on the margins of the swamps, confining fish to the interiors of the swamps and the main channels connecting them. With flooding, which peaks in May, input of fresh water alleviates the anoxic conditions and fish disperse into the surrounding swamps and floodplains where breeding occurs.

Lake Mweru is deeper (37 m), larger (4,413 km2), and has a higher plankton production than Lake Bangweulu. A Vossia swamp system marked by extensive stands of large ambatch trees occurs at the southern end of the lake at the entrance of the Luapula River. The rest of the shoreline is sandy and rimmed with the sedge Eleocharis in shallow waters, with occasional rocky outcrops (Bowmaker et al. 1978).

Terrestrial habitats

The vegetation on uplands is predominantly miombo (Brachystegia/Julbernardia) woodland, and alluvial areas are characterized by grassland and wetlands (Stuart et al. 1990; Hughes 1997).

Description of endemic fishes

Endemic fishes include five species of Barbus, three Nothobranchius, nine cichlids, three kneriids, five mochokid catfishes, and three mormyrids (Poll 1976; Balon & Stewart 1983).

Justification for delineation

This ecoregion is distinguished by its swampy floodplain lakes that host a rich and endemic freshwater fauna including endemic fish, molluscs (Cleopatra johnstoni, C. mweruensis, Melanoides crawshayi, M. mweruensis, Bellamya crawshayi, B. mweruensis, and B. pagodiformis), mammals (Damaliscus superstes and Kobus leche smithemani), and wetland birds (Ploceus katangae). This ecoregion’s waters were historically part of the Zambezi system, until the Congo River captured the Luvua River near Mkuka at the southern end of the Bangweulu swamps during the early Tertiary period (Moore & Larkin 2001). The freshwater fauna remains mostly Zambezian in origin and this ecoregion is thus included within the Zambezi bioregion (Banister 1986; Cotterill 2004). The Chambeshi is now confluent with the Luapula, but the entry of Congo fauna into Lake Bangweulu is prevented by the Mumbatuta Falls (Jackson 1986). The fish family Clupeidae is an example of a Congolian group present in Lake Mweru but absent from Lake Bangweulu. Bangweulu has fewer species than Mweru, but shares a larger proportion (49% versus 32%) of them with the Kafue.

Level of taxonomic exploration

Poor. The level of biological investigation is reasonable, but more work is needed to quantify the current status of these systems. Investigation into the conservation status of some of the threatened species, and the impacts of the fishery, are suggested.


References

  • Bailey, R. G. (1986). "The Zaire River system" Davies, B. R.;Walker, K. F. ( (Vol. The ecology of river systems, pp. Dr W. Junk Publishers ) 201-214.
  • Balon, E. K. and Stewart, D. J. (1983). "Fish assemblage in a river with unusual gradient (Luongo, Africa Zaire system), reflections on river zonation, and description of another new species" Environmental Biology of Fishes 9 pp. 225-252.
  • Banister, K. E. (1986). "Fish of the Zaire system" B. R. Davies and K. F. Walker (Ed.) Ecology of river systems ( pp. 215-224 ) Dordrecht, The Netherlands: Dr W. Junk Publishers.
  • Bell-Cross, G. (1965). "Physical barriers separating the fishes of the Kafue and Middle Zambezi River systems" Fisheries Research Bulletin of Zambia 4 pp. 97-101.
  • Bowmaker, A. P., Jackson, P. B. N. and Jubb, R. A. (1978). "Freshwater fishes" M. J. A. Werger (Ed.) Biogeography and ecology of southern Africa ( pp. 1181-1231 ) The Hague, The Netherlands: Dr W. Junk Publishers.
  • Brown, David (1994). "Freshwater snails of Africa and their medical importance" London, UK: Taylor & Francis.
  • Burgis, M. J.;Symoens, J. J. (1987). "African wetlands and shallow water bodies" Paris, France: ORSTOM.
  • Cotterill, F. P. D. (2003). "Insights into the taxonomy of tsessebe antelopes Damaliscus lunatus (Bovidae: Alcelaphini) in south-central Africa with the description of a new evolutionary species in south-central Africa" Durban Museum Novitates 28 pp. 11-30.
  • Denny, P. (1985). "The ecology and management of African wetland vegetation" Dordrecht, The Netherlands: Dr W. Junk.
  • Grimsdell, J. J. R. and Bell, R. H. V. (1975) \Black lechwe research project, Final report: Ecology of the black lechwe in the Bangweulu Basin of Zambia\ Ndola, Zambia. NCSR, Falcon Press.
  • Hughes, D. A. (1997) \Southern African "FRIEND" - The application of rainfall-runoff models in the SADC region. Report 3/97\ Grahamstown, South Africa. Institute for Water Research.
  • Huntley, B. J. (1978). "Ecosystem conservation in southern Africa" M. J. A. Werger (Ed.) Biogeography and ecology of southern Africa ( pp. 1333-1385 ) The Hague, The Netherlands: Dr W. Junk Publishers.
  • Jackson, P. B. N. (1986). "Fish of the Zambezi sytsem" B. R. Davies and K. F. Walker (Ed.) The ecology of river systems ( pp. 269-288 ) Dordrecht, The Netherlands: Dr W. Junk Publishers.
  • Kabii, T. (1997). "An overview of African wetlands" A. J. Hails (Ed.) Wetlands, biodiversity, and the Ramsar Convention Gland, Switzerland: Ramsar Convention Bureau.
  • Moore, A. E. and Larkin, P. A. (2001). "Drainage evolution in south-central Africa since the breakup of Gondwana" South African Journal of Geology 104 pp. 47-68.
  • Poll, M. (1976). "Poissons.Exploration du Parc National de l’Upemba" Fondation pour favoriser les Recherches Scientifiques en Afrique 73 pp. 1-127.
  • Stuart, S. N.,Adams, R. J.;Jenkins, M. D. (1990). Biodiversity in Sub-Saharan Africa and its islands: Conservation, management and sustainable use, Occasional Papers of the IUCN Species Survival Commission No. 6 Gland, Switzerland: IUCN.