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 language | English |
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Pages (from-to) | 764-775 |
Number of pages | 12 |
Journal | Limnology And Oceanography Letters |
Volume | 9 |
Issue number | 6 |
Early online date | 3 Oct 2024 |
DOIs | |
Publication status | Published - 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.
Funders | Funder number |
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European Union | 798222 |
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 |