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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

    Research output: Contribution to journalArticlepeer-review

    12 Citations (Scopus)
    11 Downloads (Pure)

    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

    UN SDGs

    This output contributes to the following UN Sustainable Development Goals (SDGs)

    1. SDG 13 - Climate Action
      SDG 13 Climate Action
    2. SDG 14 - Life Below Water
      SDG 14 Life Below Water
    3. SDG 15 - Life on Land
      SDG 15 Life on Land

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