Shorezone

Shorezone is a coastal region where land meets the sea. It encompasses the transition from the upper shore, near the high-tide line, through the intertidal zone that alternates between immersion and exposure, and down to the subtidal zone that remains underwater at all tides. The exact extent varies by coastline and definition, but the shorezone typically includes beaches, dunes, cliffs, estuaries, and the adjacent nearshore waters.

Boundaries and components: The upper boundary is near the high-water line, while the lower boundary is the limit of the subtidal zone. The intertidal zone is commonly divided into supratidal, upper, middle, and lower subzones, each hosting characteristic communities. The subtidal zone includes nearshore habitats such as kelp forests, seagrass beds, and rocky reefs, depending on regional conditions. Physical factors like tides, waves, wind, and sediment supply strongly influence shorezone structure and dynamics.

Ecology and processes: Key processes include wave action, tidal exchange, currents, and sediment transport, which shape shoreline profiles through erosion and deposition. Nutrient exchange between land and sea supports primary production, while runoff can bring organic matter and pollutants. The shorezone supports a gradient of habitats from exposed rock and sand to sheltered estuaries and wetlands.

Habitats and services: Intertidal communities harbor organisms such as barnacles, mussels, and crabs; dune systems provide vegetation and stabilize sediments; estuaries and salt marshes offer nurseries for fishes and invertebrates. The shorezone provides ecological services including habitat, coastal protection, pollutant retention, and opportunities for recreation and fisheries.

Threats and management: Coastal development, erosion, sea-level rise, pollution, and invasive species threaten shorezones. Management approaches include coastal zoning, habitat restoration, dune stabilization, erosion control, and monitoring to inform policy and planning.