The geochemical evolution of the Pleistocene Lake Lisan-Dead Sea system
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Glacial-interglacial lake hydrochemistry in step with the Pleistocene Indian summer monsoon at the southeastern Tibetan Plateau
2024, Quaternary Science ReviewsThe paleohydrological implications of aragonite precipitation under contrasting climates in the endorheic Dead Sea and its precursors revealed by experimental investigations
2021, Chemical GeologyCitation Excerpt :Here we investigate the precipitation of authigenic lacustrine aragonite in the carbonate-poor endorheic Dead Sea and in Lake Lisan, its late Pleistocene precursor (Fig. 1). Despite the peculiar geochemical history and composition of the Dead Sea (e.g., Katz, 1973; Katz and Kolodny, 1989; Katz et al., 1977), this intriguing lake provides a relatively simplified setting that can be utilized to study the environmental implications of CaCO3 precipitation. In this study, a set of controlled laboratory experiments was designed and carried out in order to examine the rate, yield, timing, polymorphism and morphology of CaCO3 minerals that precipitated in the Dead Sea and in Lake Lisan by the mixing of brine and synthetic flood water.
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