Sea-level rise and extreme Indian Ocean Dipole explain mangrove dieback in the Maldives

Lucy Carruthers*, Vasile Ersek, Damien Maher, Christian Sanders, Douglas Tait, Juliano Soares, Matthew Floyd, Aminath Shaha Hasim, Stephanie Helber, Mark Garnett, Holly East, Jamie A. Johnson, Gheorghe Ponta, James Z. Sippo

*Corresponding author for this work

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Abstract

Mangrove forests enhance Small Island Developing States’ resilience to climate change, yet in 2020, a mangrove dieback impacted ~ 25% of mangrove-containing islands in the Maldives. Using remote sensing, dendrology and sediment geochemistry, we document a significant decrease in mangrove health post-2020 (NDVI: 0.75 ± 0.09) compared to pre-2020 (0.85 ± 0.04; P < 0.0001). Dead trees showed reduced stomatal conductance (δ13C: − 26.21 ± 0.11 ‰) relative to living ones (− 27.66 ± 0.14 ‰), indicating salinity stress. Critically, sea-level rise (30.50 ± 23.30 mm/year) outpaced mangrove sediment accretion (6.40 ± 0.69 mm/year) five-fold between 2017 and 2020. We attribute this dieback to salinity stress driven by record-high sea levels in 2020, linked to an extreme positive Indian Ocean Dipole event. These findings reveal the vulnerability of mangrove ecosystems to rapid sea-level rise and highlights the urgent need for adaptive conservation strategies in Small Island Developing States.
Original languageEnglish
Article number27012
Number of pages10
JournalScientific Reports
Volume14
Issue number1
DOIs
Publication statusPublished - 12 Nov 2024

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