Yuting Li

TL;DR: In this paper, the authors evaluated grain size-dependence and variability of Nd and strontium compositions in the Indus delta of Pakistan, documenting both a significant isotopic evolution and coarsening upward sequence during the last deglaciation (~15 ka).

TL;DR: In this article, the authors present new age and geochemical provenance data from cores covering the last 20 years that show continuous deep-water sedimentation through the Indus submarine canyon since at least 11.0 years, despite the cessation of sedimentation on the upper fan around that time.

TL;DR: In this paper, the authors investigated the origin of sediment in the Indus Submarine Canyon since the Last Glacial Maximum (LGM; ~20 ka) using zircon U-Pb dates.

TL;DR: The Nataraja Slide as mentioned in this paper is a massive mass-transfer complex on the eastern Arabian Sea, which was discovered by International Ocean Discovery Program (IODP) Expedition 355 in two locations where it is ∼300 m (Site U1456) and ∼200 m (site U1457).

TL;DR: In this paper, the authors report a change in sediment source, with less direct flux from the Himalaya and more erosion of older, weathered, smectite-rich sediment from the Indus River flood plains, driven by incision of the river and its tributaries into the floodplain as summer monsoon rains weakened.