Researchers trace Indus River’s paleoclimatic history using gravels geometric data


Indian researchers have traced the paleoclimatic history of the Indus River in Ladakh Himalaya with the help of geometric data from overlapping gravels of channel fills. Scientists from Dehradun’s Wadia Institute of Himalayan Geology (WIHG), an autonomous institute under the Centre’s Department of Science and Technology, studied the discharge during periods in which the river experienced an increase in land elevation, due to the deposition of sediment and its incision.

Paleoclimatology is the study of Earth’s past climate using geologic and biologic evidence (climate proxies) preserved in sediments, rocks, tree rings, corals, ice sheets, and other climate archives to reconstruct past climate in terrestrial and aquatic environments around the world.

 

River Terraces are ubiquitous in mountains that nourish and help sustain past, present, and future human societies. These terraces are part of valley-wide aggradations, which has been studied extensively in Himalaya to understand the processes driving such a periodic increase in river valley land elevation and incision. Scientists are still debating whether wetter climate intervals with increased rainfall and glacial melting promote river aggradation through increased discharge and enhanced sediment load, or instead, is it during drier conditions when aggradation occurs through increased sediment to water ratio.

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Calculating paleo discharges

The researchers studied the discharge during periods of established river aggradation and incision of the Indus River, Ladakh Himalaya over late Quaternary (the current and most recent of the three periods in the geologic time scale). They used geometric data from overlapping gravels of channel fills to calculate paleo discharges during net river aggradation at 47–23 ka (thousand years), and preserved slack water deposits (SWDs) at 14–10 ka to constrain paleo discharges that occurred during net river incision.

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They observed that the aggradation in the Himalayan rivers occurred in glacial-interglacial transient warm climatic conditions (33–21 ka and 17–14 ka) when the sediment budget in the rivers increased just after the glacial events.

Their study published in the journal Geomorphology shows that aggradation took place in the Indus River when sediment to water ratio was higher during MIS-3 (Marine isotope stages (MIS), marine oxygen-isotope stages, are alternating warm and cool periods in the Earth’s paleoclimate, deduced from oxygen isotope data reflecting changes in temperature derived from data from deep-sea core samples) and incision initiated when sediment to water ratio reduced during post-glacial climatically wet phase (early Holocene).

(PTI Photo for representation)

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