Examines hydrological changes affecting carbon sequestration in wetlands, highlighting ecological implications.
The present study examines the dynamics of hydrological change and LULC transformation and its impacts on carbon sequestration in the wetland-dominated three riparian corridors (Tangon, Punarbhaba, and Atreyee river basins) of the Indo-Bangladesh Barind Tract. Using multi-temporal Landsatimages (2010, 2024) and a CA–Markov predictive model for 2038, the study quantifies spatial changes amongstvegetation, water bodies, agricultural land, and built-up areas of the basins. InVEST model was applied for calculating carbon sink. Results exhibit about 36% to 50% river flow reduction in post-dam condition and consequent flood reduction promoted 36 to 46% shrinkage of wetland and emergence and expansions of land 76 to 89% agriculture land. Agricultural land sequesters the maximum share of total carbon(C) stock (80–90%), whereas wetland and vegetation-driven carbon banks have diminished significantly (46–74%), droppinglong-standing carbon stability. Although growth of carbon sequestration is marginal (about 15%) due to agricultural expansion, but loss of natural capitals like wetland vegetation have diminished 46–74% carbon contribution reflecting a shift from stable to transient carbon sinks. This underscores the ecological paradox of short-term carbon profits amidst deterioration of natural ecosystem services. Findings highlight the need for transboundary water governance, carbon-smart agricultural practices, and wetland and vegetation restoration for maintaining carbon balance and ecosystem resilience.
No takes yet. Share an insight, caveat, or question.
Ghosh et al. (2026) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: