Abstract

By reducing current velocity, tidal marsh vegetation can diminish storm surges and storm waves. Conversely, currents often exert high mechanical stresses onto the plants and hence affect vegetation structure and plant characteristics. In our study, we aim at analysing this interaction from both angles. On the one hand, we quantify the reduction of current velocity by Bolboschoenus maritimus, and on the other hand, we identify functional traits of B. maritimus’ ramets along environmental gradients. Our results show that tidal marsh vegetation is able to buffer a large proportion of the flow velocity at currents under normal conditions. Cross‐shore current velocity decreased with distance from the marsh edge and was reduced by more than 50% after 15 m of vegetation. We were furthermore able to show that plants growing at the marsh edge had a significantly larger diameter than plants from inside the vegetation. We found a positive correlation between plant thickness and cross‐shore current which could provide an adaptive value in habitats with high mechanical stress. With the adapted morphology of plants growing at the highly exposed marsh edge, the entire vegetation belt is able to better resist the mechanical stress of high current velocities. This self‐adaptive effect thus increases the ability of B. maritimus to grow and persist in the pioneer zone and may hence better contribute to ecosystem‐based coastal protection by reducing current velocity.

Highlights

  • Tidal marshes play an important role for coastal flood defence (Kirwan and Megonigal 2013; Temmerman et al 2013)

  • Ecology and Evolution published by John Wiley & Sons Ltd

  • We quantified the reduction of current velocity by B. maritimus by comparing field measurements with and without living vegetation as well as by estimating effect functions from the data

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Summary

Introduction

Tidal marshes play an important role for coastal flood defence (Kirwan and Megonigal 2013; Temmerman et al 2013). By reducing current velocity and attenuating waves (Christiansen et al 2000; Temmerman et al 2005), marsh vegetation diminishes the destructive effects of storm surges and storm waves (Gedan et al 2010; Shepard et al 2011). It reduces shoreline erosion and increases sedimentation (Neumeier and Ciavola 2004). An intact marsh vegetation belt hereby promotes natural accretion of sediments and has the ability to adapt to projected sea level changes (Kirwan et al 2010).

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