Gravel barriers extend along a fifth of the non-estuarine coastline of England and Wales, and are also common in Scotland and Northern Ireland. At many locations they act as natural coastal defences and are unique ecosystems, especially in association with back-barrier marsh or lagoonal systems. In offering physical protection from coastal flooding and erosion, they represent critical natural capital. For example, over 30 coastal frontages (> 180 km) in SE England have a mixed sand-gravel barrier as the main coastal defence.
Acknowledging the socioeconomic value of gravel barriers, significant sums are spent annually on engineering structures and management practices to maintain and enhance their capacity for coastal protection. Gravel barriers also represent valuable morpho-sedimentary niches, supporting internationally important biodiversity (e.g., ‘vegetated shingle’) and providing back-barrier conditions that enable carbon storage. Yet, given the vital functions played by gravel barrier systems, our understanding of their resilience to climate change is alarmingly poor.