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The Dune Environment

The coastal environment is a continually changing one. Coastal dune systems are constantly influenced by wind, water and temperature conditions. Together with tidal and wave action, sand is moved around, sometimes resulting in significant erosion of the foredunes. Movement of dry, loose sand is responsible for shaping the dunes.

As coastal environments are mobile and complex systems a range of plant communities can be found in a narrow strip of coastal vegetation typical of what remains along the coast around Perth. A range of plant adaptations have evolved as a result of how dunes are constructed.


Picture: A typical dune cross section showing the various zones from the very mobile beach front to stable secondary dunes further inland.

Those plants that form at the very front of a dune system are termed pioneer plants as they have adapted to grow in strong winds, shifting sand and salty conditions.

Once these plants have stablised, the sand foredune plants can begin to establish, gradually building the height of the dune.

As time goes on, sheltered positions are created that enable different plants to establish, climaxing in large trees in the secondary dune phase.

Plants perform several functions in a coastal environment, with some of the main ones being:

  • Contribute to the nutrient cycle and maintain moisture within the upper sand profile.
  • Anchor the soil and act as a buffer against wind and water erosion.
  • Trap water, sand and salt acting as a protecting barrier to more inland vegetation.

These dune zones can be found in the local coastal areas in the Town of Cambridge.


Cambridge Coastcare (Inc)
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