“…Firstly, sediment may have been trapped by marginal or wetland vegetation (e.g. Johnston et al, 1984;Dieter, 1990), as may have been the case near Pleistocene paleosprings at Olduvai Gorge in Tanzania (Ashley, 2007). Secondly, at times, much of the lake water may have been derived from dilute springs and/or groundwater seepage around the lake margins.…”