Despite global concerns highlighting the threats to wetlands, monitoring and quantifying changes in palustrine wetland ecosystem extent remains inadequate. The feasibility of mapping the extent and rates of change of wetland Ecosystem Functional Groups (EFGs) in the Maputaland Coastal Plain, South Africa, using Earth Observation (EO) was evaluated. Seven wetland EFGs were mapped, including two estuarine (Coastal saltmarshes, and Intertidal forests and shrublands (mangroves)) and five freshwater EFGs (Lacustrine wetlands and palustrine wetlands: Large macrophytes, Permanent marshes, Seasonal marshes, and Subtropical-temperate forested wetlands). Changes in their extent were quantified across seven epochs across a 32-year period (1990–2022), including three above-average rainfall years (2000, 2006, and 2022), and four years that corresponded with the South African National Land Cover datasets (SANLCs: 1990, 2014, 2018, and 2020). Landsat images between 1990 and 2014 and a combination of Sentinel-1 and -2 images between 2018 and 2022 were modelled with a Random Forest classifier using EFG reference spectra informed by fieldwork. The classifications achieved overall accuracies between 78% and 87%, with user accuracies of the EFGs ≥ 73% for all years. Over the last 32 years, 53% of the extent of wetland EFGs remained unchanged, whereas 35% experienced interclass transformation and 8% were converted to anthropogenic pressures (5% speckle ignored). Four of the wetland EFGs showed an annual decline of 1% to 3%. Projections indicate that, under current conditions, four EFGs could face total collapse by 2050, with Intertidal forests and shrublands at the highest risk. The findings highlight the need for enhanced EO-based monitoring and protective measures to preserve wetland biodiversity and its ecosystem services. • EO images at a ≤10 m spatial resolution is critical for monitoring palustrine wetland ecosystem types. • The six palustrine wetland EFGs exhibited a downward trend with an increasing loss after 2006. • Intertidal and forested wetlands showed a high rate of decline over seven epochs. • Natural and anthropogenic pressures cause changes in the extent of EFGs. • High losses occurred between the areas of Vasi Pan and eManguzi, KwaMbila and the iMfolozi/uMsunduzi floodplain.
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Heidi van Deventer
Philani Apleni
Laven Naidoo
The Science of The Total Environment
University of the Witwatersrand
University of Pretoria
University of Johannesburg
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Deventer et al. (Wed,) studied this question.
www.synapsesocial.com/papers/69d895d86c1944d70ce07049 — DOI: https://doi.org/10.1016/j.scitotenv.2026.181709
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