However, a few preserved silt lenses and salt layers indicate intervals of more lacustrine conditions. Only low numbers of exclusively Reticypris sp. were found, reflecting low species diversity in this unit, at least outside of the influence of
terminal splay processes. In contrast e and by analogy with the historically largest flood event in 1974 (Fig. 1) e the well-developed bedding in the distal terminal splay deposits (e.g. P27) and wooden debris in vicinity to the shoreline reflect repeated but discrete depositional and discharge events on the terminal splay and the adjacent lake floor in the late Holocene since at least 2.8 cal ka BP.