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A hydrological switch drives the transition from saltmarsh to peat-forming reedland ecosystems


Abstract

Understanding how carbon-rich coastal peatlands form is crucial for future carbon storage under environmental change. Phragmites australis (common reed), a key precursor species, facilitates peatland development in saltmarshes by triggering a hydrological switch: creek networks clog through root and organic material accumulation, increasing freshwater retention. Here, we use Holocene peat paleo-records from the Netherlands to reveal past coastal-to-freshwater system transitions consistent with this mechanism. With a numerical biogeomorphic model, we demonstrate how reed expansion reduces creek network complexity, promoting a homogeneous freshwater landscape that further facilitates reed growth. Elevation and vegetation time-series, together with salinity measurements linked to species composition from Saeftinghe (southwestern Netherlands) confirm that reed expansion is associated with creek infilling and a shift in hydrological conditions. Our results identify a strong positive feedback that triggers the hydrological switch accompanied by Phragmites expansion, offering new insight into past peatland establishment and future carbon-rich wetland formation.

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Acknowledgements

The authors would like to thank Jing Feng for providing and offering insight to the reports accompanying the vegetation maps of Saeftinghe, Jackie Ashkin and Mingxuan Wu for their help during the Saeftinghe field work measurements. For the help and guidance during the historical peat development geological surveys (2022-2025), many thanks to Walter Jonkers and Bernard Meijlink and the bachelors students of the Earth Sciences department from Vrije Universiteit Amsterdam Jonina Karman, Femke ter Schure, Maaike de Graaff, Demi Imming, Kilian van Roosmalen, Solveig de Reus and Martijn Hoogveld. BSc thesis reports from the students supporting the geological core descriptions are unpublished internal reports available from the corresponding author upon request. We further thank the landowners of the coring sites near Ritthem, Oostkapelle and Yerseke for granting permission to conduct geological coring on their land.

Funding

The research of A.V. and J.v.d.K. was supported by the project Defending our Coast (grant number UUNIOZ 4543.15) funded by the Netherlands Organisation for Scientific Research (NWO), a UU-NIOZ collaboration. Additional funding was provided by the Province of Zeeland and the Geopark Schelde Delta. M.B., D.v.d.W., C.K., G.K.K., M.G.K., N.V.d.P., M.R. declare no relevant funding.

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Archontoula Valsamidou.

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Valsamidou, A., Bastiaanse, M., van der Wal, D. et al. A hydrological switch drives the transition from saltmarsh to peat-forming reedland ecosystems.
Commun Earth Environ (2026). https://doi.org/10.1038/s43247-026-03780-w

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