Coastal Erosion as a Major Sediment Source in the Inner Gulf of Thailand: Implications for Carbon Dynamics in Tropical Coastal Ocean Systems

Abstract Coastal erosion is an increasingly dominant sediment source in marginal seas, particularly in low‐lying areas affected by deltaic subsidence and sediment deficits from upstream water management. However, its role in sediment and organic carbon (OC) dynamics remains to be estimated. Our analyses of the inner Gulf of Thailand (IGoT) revealed that riverine sediment fluxes decreased from 6.6 to 5.4 Mt/yr after 1975, while sediment accumulation within the IGoT increased from 20.8 to 29.5 Mt/yr. The observed trend indicates major sediment contributions from coastal erosion, particularly from mangrove deposits. This process destabilizes coastal ecosystems and accelerates OC decomposition, that is, a low burial efficiency (16.8 ± 5.5%) leads to CO 2 release. Extrapolating these findings globally, mangrove loss could release ∼175 Tg/yr CO 2 . As coastal erosion intensifies under sea‐level rise and human land‐use practices, preserving coastal ecosystems is critical for mitigating blue carbon loss and maintaining coastal stability and resilience.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-05-24
DOI
https://doi.org/10.1029/2025gl115606
Citations
4
Primary Topic
Coastal wetland ecosystem dynamics
Type
article
Field-Weighted Citation Impact
6.87

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article

Coastal Erosion as a Major Sediment Source in the Inner Gulf of Thailand: Implications for Carbon Dynamics in Tropical Coastal Ocean Systems

Guodong Jia, Moritz Holtappels, Till J J Hanebuth, Miao Fan et al.
4 citations
Geophysical Research Letters
Coastal wetland ecosystem dynamics
6.87
article

Coastal Erosion as a Major Sediment Source in the Inner Gulf of Thailand: Implications for Carbon Dynamics in Tropical Coastal Ocean Systems

Guodong Jia, Moritz Holtappels, Till J J Hanebuth, Miao Fan, Gesine Mollenhauer, Stephanie Kusch, Bingbing Wei, Limin Hu
article en
4 citations

Abstract

Abstract Coastal erosion is an increasingly dominant sediment source in marginal seas, particularly in low‐lying areas affected by deltaic subsidence and sediment deficits from upstream water management. However, its role in sediment and organic carbon (OC) dynamics remains to be estimated. Our analyses of the inner Gulf of Thailand (IGoT) revealed that riverine sediment fluxes decreased from 6.6 to 5.4 Mt/yr after 1975, while sediment accumulation within the IGoT increased from 20.8 to 29.5 Mt/yr. The observed trend indicates major sediment contributions from coastal erosion, particularly from mangrove deposits. This process destabilizes coastal ecosystems and accelerates OC decomposition, that is, a low burial efficiency (16.8 ± 5.5%) leads to CO 2 release. Extrapolating these findings globally, mangrove loss could release ∼175 Tg/yr CO 2 . As coastal erosion intensifies under sea‐level rise and human land‐use practices, preserving coastal ecosystems is critical for mitigating blue carbon loss and maintaining coastal stability and resilience.

Geophysical Research LettersVol. 52(10)
Tongji University (CN), Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), University of Bremen (DE), Université du Québec à Rimouski (CA), Coastal Carolina University (US), Cégep de Rimouski (CA), Qingdao National Laboratory for Marine Science and Technology (CN), Shandong Marine Resource and Environment Research Institute (CN), Conway School of Landscape Design (US), National Marine Data and Information Service, Ocean University of China (CN)
Deutsche Forschungsgemeinschaft, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research
Life below water
Openalex Percentile: Top 4%
Coastal wetland ecosystem dynamics
6.87
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