“…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.…”