Soft Sediment Interactions

Photo credit: Olivia Johnson

Soft sediment environments include gravelly, sandy, silty and muddy areas of the seafloor and are home to a wide variety of organisms including invertebrates (e.g. worms, crabs, shellfish), bottom-dwelling fish and bacteria. The majority of salmon farms in Tasmania are located over soft sediment environments.

The release of uneaten salmon feed, salmon faeces and other nutrient-rich organic matter (e.g. biofouling debris) into the water column occurs as a result of current marine salmon farming practices in Tasmania. Some of this organic matter dissolves in the water column (dissolved waste), while some of it is released in the form of particles (particulate waste) which float in the water column, sinking to the seafloor at varying rates depending on particle size and water current speeds. The release of dissolved and particulate waste has the ability to interact with soft sediment environments in a number of ways, including through:

  • Organic enrichment
  • Sedimentation

The impacts of these interactions tend to be greatest immediately below actively farmed salmon cages, decreasing with distance from the farm. The magnitude of interactions depends on the intensity and management practices of farming, the environmental conditions at the farm site (e.g. depth of water below cages, the energy of the environment) and the sensitivity of the soft sediment ecosystem.

Organic enrichment and sedimentation

How can extra organic matter and sedimentation interact with soft sediment ecosystems?

  • In most situations, the benthic ecology (the animals that live within the sediments) will adapt to process and assimilate increased organic matter and, so long as the inputs do not exceed the assimilative capacity of the animals to break down this material, the system will achieve a new equilibrium.
  • However, if deposition exceeds this assimilative capacity, there can be a build-up of organic matter on the sediment surface and oxygen levels in the sediments or in the water just above the sediments can decline. This is often evident through the presence of bacterial mats (e.g. Beggiatoa) on the sediment surface as the organic material is now being broken down by microbes. These microbes use sulphide in the breakdown process which can result in outgassing from the sediment surface; another indicator that deposition is exceeding the assimilative capacity of the environment.
  • Benthic monitoring programs often include some or all of these indicators (infaunal community structure (animals in and on the sediments), oxygen levels and evidence of outgassing) to determine environmental condition and to support management practices that avoid harm to the environment.

For more detailed information on the interactions between salmon farming and soft sediment environments, browse through our research outputs on our publications page.  

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We acknowledge the palawa/pakana and Gadigal/Wangal people, the traditional custodians of the land and sea upon which we live and work, and their enduring cultures and knowledge of our oceans and coasts.

We recognise that decisions and practices affecting the future of Indigenous education and research are vital to the self-determination, wellbeing and livelihood of Aboriginal and Torres Strait Islander people, and to shaping the Australian society in which we live.
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