Abstract
Coastal wetlands such as salt marshes have been increasingly valued for their capacity to buffer global climate change effects, yet their long-term persistence is threatened by environmental changes. Whereas, previous studies largely focused on lateral erosion risk induced by stressors like sea level rise, it remains poorly understood of the response of lateral expansion to changing environments. Seedling establishment is a key process governing lateral marsh expansion as seen in many coastal regions such as Europe and East Asia. Here, we evaluate mechanistically the response of seed bank dynamics to changing physical disturbance at tidal flats, using the globally common coastal foundation plant, cordgrass as a model. We conducted a large-scale field study in an estuary in Northwest Europe, where seed bank dynamics of cordgrass in the tidal flats was determined and linked to in situ hydrodynamics and sediment dynamics. The results revealed that wave disturbance reduced the persistence of seeds on the surface, whereas amplified sediment disturbance lowered the persistence of both surface and buried seeds. Overall, this indicates that increasing storminess and associated sediment variability under climate change threatens seed bank persistence in tidal flats, and hence need urgently be incorporated into models for long-term bio-geomorphological development of vegetated coastal ecosystems. The knowledge gained here provides a basis for more accurate predictions on how climatically driven environmental changes may alter the fitness, resilience and persistence of coastal foundation plants, with significant implications for nature-based solutions with coastal vegetation to mitigate climate change effects.
Highlights
Vegetated wetlands are among the most ecological and socio-economically valuable systems on the globe (Costanza et al, 1997)
Using cordgrass as an example, this study clearly showed that wave disturbance affected the persistence of seeds on the surface, whereas sediment disturbance decreased the persistence of both surface and buried seeds
Our findings indicate that (i) climate change likely reduce seed bank persistence in coastal wetlands via intensifying wave forcing and associated sediment disturbance and (ii) this process needs to be incorporated in biogeomorphic models predicting the future of coastal wetlands
Summary
Vegetated wetlands (e.g., salt marshes, seagrasses, and mangroves) are among the most ecological and socio-economically valuable systems on the globe (Costanza et al, 1997). There has been increasing recognition of the coastal defenses value of vegetation due to their efficacy in wave attenuation and sediment stabilization (Gedan et al, 2011; Temmerman et al, 2013; Moller et al, 2014; Zhu et al, 2020b) This initiated a paradigm shift to a more ecosystem-based. A recent field study found that seed removal from tidal flat surface increased with wave-induced bed shear stress (Zhu et al, 2020a) When seeds germinate, they can be more lifted off by currents because of enhanced buoyancy. A recent flume study of Spartina seeds shows that seed removal from the surface increased non-linearly with germination stage and current velocity (Zhao et al, 2021)
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