Abstract

Nature-based coastal defense schemes commonly value bivalve reefs for i) reducing coastal erosion in the intertidal and for ii) forming fringing reefs near salt marsh edges to protect them against lateral retreat. The capacity for a reef to reduce erosion increases at a higher position in the tidal frame as the lower over-lying water level magnifies the influence of the reef on wave attenuation. Unfortunately, ecological constraints on reef development typically limit their practical application in coastal protection schemes to the lower intertidal, as bivalves grow best with long inundation times. In micro-tidal areas this is a lesser problem, given the close proximity of lower and upper intertidal ecosystems in space. By contrast, in meso- and macro-tidal estuaries, bivalve reefs tend to form hundreds of meters away from existing marshes, nullifying any wave-protective benefits. In this study, we produce evidence that with the assistance of management measures, widespread reef formation is possible on open mudflats, including bordering the marsh edge in meso- and macro-tidal estuaries, where natural reef formation is normally strongly limited.In four locations throughout the meso- to macro-tidal Dutch Scheldt estuary, we observed the presence of individuals of two major intertidal reef-forming bivalves, Pacific oysters (Crassostrea gigas) and blue mussels (Mytilus edulis), within low-lying Spartina anglica-dominated marshes. As these communities lie well outside of the expected range of reef formation, this observation suggests the existence of mechanisms that extend the habitable range of these bivalves. In a series of field experiments, we first demonstrate how the stabilization of shell-substrate within the marsh promotes successful establishment and adult survival. Secondly, by placing artificial stable substrate in transects from the subtidal up to the marsh edge, we demonstrate that bivalve establishment is possible throughout a much larger range of the intertidal than where natural reefs occur. The effectiveness of stable substrate in stimulating bivalve establishment is likely a consequence of bridging size-dependent thresholds that limit the effective range for natural reef formation on tidal flats. The success of this approach is tempered by a consistent decrease in reef size and growth at higher elevations, suggesting that the optimal reef position for utility in coastal defense lies at an intermediate tidal position, well above the observed range of natural occurrence, but below the maximum achievable upper limit of reef formation. Together this work provides a pathway forward concerning how artificial reefs may be fostered to increase their utility as a nature-based flood defense measure.

Highlights

  • Mounting changes in the global climate are forecast to have a critical impact on the lives of the 37% of the world’s population living along coasts (Syvitski et al, 2009; Knutson et al, 2010; Lin et al, 2012)

  • The con­ ceptual validation presented in our study extends the potential utility of artificial reefs for coastal defense, by demonstrating that reef initiation is possible on high intertidal mudflats even in the region near the salt marsh edge where protective fringing reefs could protect the marsh against cliff-erosion

  • Bivalve reefs have the potential to play an important role in coastal protection schemes, but their utility is limited by our ability to initiate reef formation according to need

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Summary

Introduction

Mounting changes in the global climate are forecast to have a critical impact on the lives of the 37% of the world’s population living along coasts (Syvitski et al, 2009; Knutson et al, 2010; Lin et al, 2012). Implementation of nature-based flood defenses into coastal manage­ ment schemes has had growing support due to the benefits coastal ecological systems provide over grey infrastructure These benefits include their resiliency against sea-level rise and low maintenance re­ quirements in the face of repeated disturbances from storms (Barbier et al, 2011; Feagin et al, 2015). They provide ecosystem services beyond their immediate role in coastal protection (Morris et al, 2018, 2019, 2020), and mitigate negative socioeconomic (Hinkel et al, 2014) and environmental impacts (Bulleri and Chapman, 2010; Bishop et al, 2017; Heery et al, 2017) traditionally associated with grey infrastructure. Salt marshes are themselves vulnerable to cliff formation induced by wave forcing on their foreshore edge, which can initiate run-away landward erosion (van de Koppel et al, 2005; Bouma et al, 2016), which is the chief means of marsh loss in the Scheldt (van der Wal et al, 2008), and massively curtails their effectiveness for coastal protection (Barbier et al, 2008; Borsje et al, 2011)

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