1989
DOI: 10.1007/bf00006053
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The benthic and weed-bed faunas of Lake Awasa (Rift Valley, Ethiopia)

Abstract: The community structures of the benthic and weed-bed faunas of Lake Awasa, Ethiopia Rift Valley, are described and related to the various types of substratum present. L. Awasa is non-saline (conductivity 860 p S cm -'), and lies in a shallow basin with maximum depths of 2 l-22 m. It supports an important commercial fishery mainly based on the tilapia Oreochromis niloticus.

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Cited by 23 publications
(17 citation statements)
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“…Most Orthocladiinae are dependent on highly oxygenated water (Petr 1970a), and in tropical regions comprised a large proportion of chironomids from cool, lotic habitats (63%, n ϭ 16, Harrison and Hynes 1988, rivers in highland Ethiopia; 53%, n ϭ 45, Lehmann 1979, rivers in eastern, highland DR Congo), perhaps because oxygen is less soluble in warmer water, and higher temperatures speed up decomposition of organic material which also depletes oxygen (Eggermont and Verschuren 2003b). Consistent with this interpretation, the proportion of orthocladiines was lower in lower altitude rivers and streams (29%, n ϭ 38, Lehmann 1981, rivers in central DR Congo) and in highland lakes (21% n ϭ 32, Verschuren 1997, Lake Naivasha, Kenya); 15%, n ϭ 27, Kibret and Harrison 1989, Lake Awasa, Ethiopia). Although they acknowledge that some of their sub-fossil types may have washed in with sediment from feeder streams and rivers, Eggermont and Verschuren (2003b) argue that the consistently strong wave action characteristic of the large Rift Valley lakes may create the conditions for oxygenation usually encountered in fast moving streams and rivers and, by extension, an environment favorable to at least some orthocladiine species.…”
Section: Notes On the Chironomid Taxa From Aquatic Plantssupporting
confidence: 77%
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“…Most Orthocladiinae are dependent on highly oxygenated water (Petr 1970a), and in tropical regions comprised a large proportion of chironomids from cool, lotic habitats (63%, n ϭ 16, Harrison and Hynes 1988, rivers in highland Ethiopia; 53%, n ϭ 45, Lehmann 1979, rivers in eastern, highland DR Congo), perhaps because oxygen is less soluble in warmer water, and higher temperatures speed up decomposition of organic material which also depletes oxygen (Eggermont and Verschuren 2003b). Consistent with this interpretation, the proportion of orthocladiines was lower in lower altitude rivers and streams (29%, n ϭ 38, Lehmann 1981, rivers in central DR Congo) and in highland lakes (21% n ϭ 32, Verschuren 1997, Lake Naivasha, Kenya); 15%, n ϭ 27, Kibret and Harrison 1989, Lake Awasa, Ethiopia). Although they acknowledge that some of their sub-fossil types may have washed in with sediment from feeder streams and rivers, Eggermont and Verschuren (2003b) argue that the consistently strong wave action characteristic of the large Rift Valley lakes may create the conditions for oxygenation usually encountered in fast moving streams and rivers and, by extension, an environment favorable to at least some orthocladiine species.…”
Section: Notes On the Chironomid Taxa From Aquatic Plantssupporting
confidence: 77%
“…In most of the other studies, chironomid species richness was relatively low. In highland Ethiopia, Kibret and Harrison (1989) recorded only 13 chironomid species from aquatic plants in Lake Awasa, but these represented nearly half of the 27 total species collected at light or by sweep net. Two other studies focused on unstable lake systems; Kariba in Zimbabwe, a manmade, recently-dammed lake (MacLachlan 1969a), and the shallow, intermittently saline Lake Chilwa in Malawi (MacLachlan 1975).…”
Section: Discussionmentioning
confidence: 98%
“…The silt content in the water is relatively low because the large swampy area to the east on the Tikur Wuha River acts as an efficient settling area for silt coming from the higher hills and mountains of the eastern escarpment of the Rift Valley (Kibret and Harrison, 1989).…”
Section: Environmental Conditionsmentioning
confidence: 99%
“…Destratification is initiated in June by a decrease in solar radiation and cool rains (Elizabeth Kebede, 1987). Wind varies on both a diel and seasonal basis in Lake Awasa (Elizabeth Kebede, 1987;Tilahun Kibret & Harrison, 1989), and perhaps a combination of cool temperatures and high rainfall are critical in inducing lake mixing during May to June (Elizabeth Kebede, 1987). The lake lies in a closed basin with a total area of 1250 km 2 .…”
Section: Study Site: Lake Awasamentioning
confidence: 99%