Dense vegetation hinders sediment transport toward saltmarsh interiors

Olivier Gourgue*, Jean Philippe Belliard, Yiyang Xu, Maarten G. Kleinhans, Sergio Fagherazzi, Stijn Temmerman

*Corresponding author for this work

    Research output: Contribution to journalLetterAcademicpeer-review

    Abstract

    To save saltmarshes and their valuable ecosystem services from sea level rise, it is crucial to understand their natural ability to gain elevation by sediment accretion. In that context, a widely accepted paradigm is that dense vegetation favors sediment accretion and hence saltmarsh resilience to sea level rise. Here, however, we reveal how dense vegetation can inhibit sediment accretion on saltmarsh platforms. Using a process-based modeling approach to simulate biogeomorphic development of typical saltmarsh landscapes, we identify two key mechanisms by which vegetation hinders sediment transport from tidal channels toward saltmarsh interiors. First, vegetation concentrates tidal flow and sediment transport inside channels, reducing sediment supply to platforms. Second, vegetation enhances sediment deposition near channels, limiting sediment availability for platform interiors. Our findings suggest that the resilience of saltmarshes to sea level rise may be more limited than previously thought.

    Original languageEnglish
    Pages (from-to)764-775
    Number of pages12
    JournalLimnology And Oceanography Letters
    Volume9
    Issue number6
    Early online date3 Oct 2024
    DOIs
    Publication statusPublished - Dec 2024

    Bibliographical note

    Publisher Copyright:
    © 2024 The Author(s). Limnology and Oceanography Letters published by Wiley Periodicals LLC on behalf of Association for the Sciences of Limnology and Oceanography.

    Funding

    This project is funded by the European Union's Horizon 2020 research and innovation program (Marie Sklodowska-Curie Actions, global postdoctoral fellowship, grant no. 798222) and the Research Foundation-Flanders (FWO, fundamental research project, grant no. G031620N). J-PB is supported by the Research Foundation-Flanders (FWO, fundamental research project, grant no. G060018N). MGK is supported by the European Research Council (ERC Consolidator Grant, grant no. 647570). SF is supported by the National Science Foundation (NSF awards 2224608-PIE LTER-and 1832221-VCR LTER). The resources and services used in this work are provided by the VSC (Flemish Supercomputer Center), funded by the Research Foundation-Flanders (FWO) and the Flemish Government.

    FundersFunder number
    European Union798222
    Research Foundation-Flanders (FWO, fundamental research project)G031620N, G060018N
    European Research Council (ERC Consolidator Grant)647570
    National Science Foundation (NSF)2224608-PIE LTER, 1832221-VCR LTER
    VSC (Flemish Supercomputer Center) - Research Foundation-Flanders (FWO)
    Flemish Government

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