Reconstruction of the late Quaternary environment of the lower Luni plains, Thar Desert, India

Geomorphological processes in the Thar Desert of India are largely climate driven. In the lower reaches of the River Luni (the only major drainage sys tem in the Thar Desert) a fluvio-aeolian sequence was located at a site cal led Khudala. Sediments of this sequence represented a variety of deposition al environments, namely aeolian, fluvially reworked aeolian, overbank depos its, gravels, and occasional evidence of pedogenesis. This provided a good opportunity to study aeolian-fluvial interaction in the region and for dedu cing climatic records. From the luminescence dating standpoint these sequen ces offered a good opportunity for a comparative study of thermoluminescenc e (TL), blue-green light stimulated luminescence (BGSL) and infrared light stimulated luminescence (IRSL) on different mineral separates of identical provenance but deposited under different environments. Broadly, within expe rimental errors, the TL ages agreed with BGSL and IRSL ages on aeolian sand s, but differed substantially in the case of fluvially reworked and proxima lly deposited sands and silts. The sequence provided a record spanning more than 100 ka, with an aeolian phase at > 100 ka, a channel activation phase between 70 and 30 ka and a phase of climate instability between 13 and 8 k a. This appears consistent: with the records of monsoon performance during this period, which includes the Younger Dryas. It is also inferred that dur ing the Last Glacial epoch, geomorphological processes in the Thar (both ae olian and fluvial) were dormant largely on account of their relationship wi th the southwest monsoon. Copyright (C) 2001 John Wiley & Sons, Ltd.