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We employ direct numerical simulations in order to analyze the role of double‐diffusive salt fingering in halite precipitation from hypersaline lakes. Guided by field observations from the Dead Sea, which represents the only modern deep stratified lake that precipitates halite under hydrological crisis, we consider a saturated layer of warm, salty brine (epilimnion) overlying a layer of colder, less salty brine (hypolimnion) that is also saturated. The double‐diffusive instability originating in the metalimnion gives rise to an asymmetrical pattern of less salty ascending fingers, accompanied by descending salt fingers that lose heat as they propagate through the metalimnion. The net result is a strong, downward salinity flux that leads to the undersaturation of the epilimnion, while the hypolimnion becomes oversaturated and precipitates halite. These interfacial processes within deep, hypersaline water columns in warm and dry regions suggest a potential route toward the formation of thick halite layers found in the geological record. Guided by Dead Sea observations, we simulate double‐diffusive salt fingering in saturated, hypersaline water columnsSalt fingering results in the undersaturation of the epilimnion, as well as halite precipitation in the hypolimnionThe observed interfacial processes suggest a route toward the formation of thick halite layers found in the geological record

As the only deep hypersaline, halite‐precipitating lake on Earth today, the Dead Sea is the single modern analog for investigating the mechanisms by which large‐scale and thick salt deposits, known as “salt giants”, have accreted in the geological record. We directly measure the hydroclimatic forcing and the physical limnologic processes leading to halite sedimentation, the vertical thermohaline structure, and salt fluxes in the Dead Sea. We demonstrate that changes in these forcing lead to strong seasonal and regional variations in the stratification stability ratio, triggering corresponding spatiotemporal variations in thermohaline staircase formation and diapycnal salt flux, and finally control the thickness of the halite layer deposited. The observed staircase formation is consistent with the mean‐field γinstability, causing layering in double‐diffusive convection. We show that double diffusion and thermohaline staircase formation drive the spatial variability of halite deposition in hypersaline water bodies, underlying and shaping “salt giants” basin architecture. Kilometers‐thick halite sequences in the geological record represent some of the extreme environmental events during Earth's history. The present‐day Dead Sea serves as an analog for halite deposition and the unique limnology/oceanography of those past hypersaline environments. We observe differential downward salt flux in the lake and halite deposition at the deep lakefloor, corresponding to theoretical requirements of water column stability and the evolution of a step‐like thermohaline structure of the water column. These variations are spatiotemporally controlled by regional hydroclimatology, as the salt flux and halite deposition enhanced during the dry summer and farther from the freshwater inflows into the lake, along an increasing salinity gradient. Our findings explain thick halite accretion in global basin depocenters. We resolve the mechanisms driving thick salt layers accretion in deep saline waterbodies by direct field measurements in the Dead SeaHydroclimatic variations impact stratification stability, thermohaline staircases, double diffusion salt fluxes, and halite depositionRegional and seasonal drying trends dictate stronger salt flux in the drier and deeper zones and explain the architecture of “salt giants”

We provide a new perspective on the transition of hyperpycnal flows into saline turbidity currents, which permits longer runout lengths than might be otherwise expected. This mechanism relies on the differential turbulent diffusion of salt and sediment, and in contrast to ambient saltwater entrainment it enables the salinification of the freshwater current without diluting the sediment concentration field by a corresponding amount. The freshness‐to‐sediment ratio is introduced in order to quantify the transition process. The results of high‐resolution simulations provide estimates for the transition distance of hyperpycnal model flows into saline turbidity currents. In some near‐coastal areas of the world's oceans, sediment‐rich rivers trigger so‐called hyperpycnal currents, which are currents composed of river‐derived freshwater and sediment that propagate along the seafloor. In general, one may expect such currents to have a short runout length, since sediment deposition will reduce their density until they loft from the seafloor. There is evidence, however, that in some settings hyperpycnal currents can have much larger runout lengths than expected. Here we propose a novel perspective on such large runout lengths, by showing that differential diffusivities can enable the hyperpycnal flow to transition into a saline turbidity current. This mechanism relies on the fact that salt and sediment diffuse at different rates, so that the freshwater current can become salinified without diluting its sediment concentration field. Differential diffusion provides a new perspective on the transition of hyperpycnal flows into saline turbidity currentsDifferential diffusion of salt and sediment can render the freshwater current salty, without strongly diluting the sedimentTransition distance estimates are provided for hyperpycnal model flows