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- W3217612773 abstract "The Thar Desert is the easternmost extension of the mid latitude desert belt of Sahara and Arabia. The Thar Desert is arid, with a mean annual rainfall ranging from 500 mm in the rocky eastern margin to less than 150 mm in the sandy western margin. Lakes were hypersaline between 15 and 9 ka and relatively less saline or with fresh water between 7.5 and 6 ka. The majority of lakes dried up around 4 ka and became ephemeral after 1 ka. The Western margin lakes like Kanod and Bap-Malar remained saline from 9 to 6 ka while the Eastern margin lakes like Didwana, Tal Chapar, and Jhorda among others had fluctuating saline to fresh hydrology from 9 to 4 ka. Sites with microblade technology ranging in age from late-Pleistocene to mid-Holocene, as known from our studies at Sam (14 ka) and Jamba (7 ka), show human adaptation to arid, wet semiarid, and semiarid environments. Sites are rare during the terminal Pleistocene and common during the mid-Holocene. Foraging communities had a symbiotic relationship with technologically advanced food producing people in the eastern margin of the Thar Desert during the Medieval period." @default.
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- W3217612773 date "2022-01-01" @default.
- W3217612773 modified "2023-09-23" @default.
- W3217612773 title "Late Quaternary geoarcheology and palynological studies of some saline lakes of the Thar Desert, Rajasthan, India" @default.
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- W3217612773 doi "https://doi.org/10.1016/b978-0-323-90085-0.00006-1" @default.
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