The chemical evolution of the brines that filled the Dead Sea Basin during the final phase of the last interglacial and throughout the last glacial period is constructed from the temporal variations in the Na/Cl, Mg/Cl, Br/Cl, and Br/Mg ratios of soluble salts that were extracted from cores that were drilled at the modern Dead Sea floor and from sediments of the last glacial Lisan Fm. that are exposed at the high terraces above the modern Dead Sea (covering the ∼ 100–14 ka period).

中文翻译：

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死海盐水在末次冰河周期中从间质可溶性盐的化学成分演变而来的地球化学演变


在末次间冰期的最后阶段和整个末次冰期，充满死海盆地的盐水的化学演变是由可溶性盐的 Na/Cl、Mg/Cl、Br/Cl 和 Br/Mg 比率的时间变化构成的，这些盐是从现代死海底钻探的岩心和暴露在现代死海上方的高梯田（涵盖 ∼ 100-14 ka 时期）。