Evolution of Ganges–Brahmaputra western delta plain: Clues from sedimentology and carbon isotopes |
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| Authors: | A Sarkar S Sengupta JM McArthur P Ravenscroft MK Bera Ravi Bhushan A Samanta S Agrawal |
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| Institution: | aDepartment of Geology & Geophysics, Indian Institute of Technology, IIT Kharagpur, Kharagpur 721302, India;bDepartment of Earth Sciences, University College London, London WC1E BT, UK;cDepartment of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK;dPhysical Research Laboratory, Ahmedabad 380 009, India |
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| Abstract: | Sedimentology, carbon isotope and sequence stratigraphic analysis of subsurface sediments from western part of Ganges–Brahmaputra (GB) delta plain shows that a Late Quaternary marine clay and fluvial channel-overbank sediments of MIS 5 and 3 highstands are traceable below the Holocene strata. During the Last Glacial Maximum (LGM) sea-level lowering of >100 m produced a regional unconformity (type 1), represented by palaeosols and incised valley. C4 vegetation expanded on exposed lowstand surface in an ambient dry glacial climate. At  9 ka transgression inundated the lowstand surface pushing the coastline and mangrove front 100 km inland. Simultaneous intensification of monsoon and very high sediment discharge (4–8 times than modern) caused a rapid aggradation of both floodplain and estuarine valley fill deposits between 8 and 7 ka. The Hoogli River remaining along its present drainage possibly acted as the main conduit for transgression and sediment discharge that was subsequently abandoned. C3 vegetation dominated the delta plain during this time. From 7 ka onward progradation of delta plain started and continued till recent. This period experienced a mixed C3–C4 vegetation with localized mangroves in the mid-Holocene to dominant return of C4 vegetation in the late Holocene period. The study indicates that while the initiation of western part of GB delta occurred at least 1 ka earlier than the global mean delta formation age, the progradation started at 7 ka, at least 2 ka earlier than thought before. The terrestrial vegetation change was modulated by changes in depositional environment, specific ecological niches and climate rather than pCO2. |
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