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Queensland Murray-Darling Freshwater Biogeographic ProvinceQueensland Murray-Darling Freshwater Biogeographic Province – Deposited sedimentClick on elements of the model or select from the tabs below
Rain and run-off are the mechanisms of water erosion that contribute to instream sediment.
Pugging, wallows and tracks created by stock and feral animals can decrease bank stability and increase erosion potential. When this is coupled with the removal of riparian vegetation bank collapse can occur.
Clearing riparian vegetation reduces bank stability, shading and the capacity to filter run-off.
Sediment entering the stream can remain suspended or settle as deposited sediment. Toxicants and nutrients can attach to and be transported with sediment particles.
Increased deposited sediment smothers instream habitat and reduces waterhole persistence time through depth reduction.
Altered instream habitat can lead to changes in the structure and function of ecological communities and ecosystem processes. Sediment is resuspended by the feeding behaviour of carp, a pest species.Last updated: 22 March 2013 This page should be cited as: Department of Environment, Science and Innovation, Queensland (2013) Queensland Murray-Darling Freshwater Biogeographic Province – Deposited sediment, WetlandInfo website, accessed 20 December 2024. Available at: https://wetlandinfo.des.qld.gov.au/wetlands/ecology/aquatic-ecosystems-natural/riverine/freshwater-biogeo/murray-darling/dsediment.html |