Geochemical and sedimentological analysis of hypersaline Sambhar Lake of India: implications for paleolake exploration on Mars 

Abstract

<p>Paleolakes on Mars have been proposed to be hydrologically active for thousands of years. They provide water, the prime ingredient for life to develop, and quiescent settings, making these lakes excellent targets in preserving biosignatures. Since ground truth analysis on Mars is limited to certain locations, most of the interpretations about Martian geology and past climate have been made through remote sensing. This study presents a comprehensive account of the physical and chemical aspects of an Earth-based hypersaline playa that has undergone intermittent wet and dry periods.</p><p>Sambhar Lake is the largest endorheic playa in India, situated southeast of the Aravalli mountains within the Thar Desert. The lake formed as a result of neotectonic and aeolian activity followed by stream capture like some paleolakes and hydrologically active inter-crater depressions on Mars. Sambhar Lake lies between arid and semi-arid transitional zones and is fed by two ephemeral streams indicating climate-driven hydrology. The surface and sub-surface brine samples collected from the lake were alkaline, Na-Cl type with salinity higher than the seawater. Silicate weathering and evaporation were identified as important processes responsible for influencing the hydro-geochemistry of the lake. Petrographic and geochemical analysis of the sediment and rock samples showed the presence of clay minerals and evaporites ranging from carbonates to halites suggesting that the lake had witnessed multiple hydrological cycles. The weathering index of the dried lake bed was comparable to some Gale crater samples and lakes with basaltic origin on Earth. The geochemical evolution of the Sambhar Lake is primarily governed by the inlet streams and their composition, partition of solutes in the water, and concentration of the evaporites. Thus, Sambhar Lake is a classic example of the climate-induced transition of a lacustrine basin to a playa. It may be helpful to study the evolution of hydrological basins, their morphology, and the process of mineral formation on Mars.</p>