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bioturbation
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bioturbation

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alt=Walrus |thumb|upright=1.5 |Sediment on the left tusk of a walrus. Walrus bioturbations in Arctic benthic sediments have large-scale ecosystem effects.

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19 sections
Contents
  • Functional groups
  • Ecological roles
  • Biogeochemical effects
  • Organic contaminants
  • Ecosystem impacts
  • Terrestrial
  • Freshwater
  • Lakes and ponds
  • Rivers and streams
  • Marine
  • Shallow and coastal
  • Deep sea
  • Mathematical modelling
  • Evolution
  • Fossil record
  • Research history
  • See also
  • References
  • External links

alt=Walrus |thumb|upright=1.5 |Sediment on the left tusk of a walrus. Walrus bioturbations in Arctic benthic sediments have large-scale ecosystem effects.

Bioturbation is defined as the reworking of soils and sediments by animals or plants. It includes burrowing, ingestion, and defecation of sediment grains. Bioturbating activities have a profound effect on the environment and are thought to be a primary driver of biodiversity. The formal study of bioturbation began in the 1800s by Charles Darwin experimenting in his garden. The disruption of aquatic sediments and terrestrial soils through bioturbating activities provides significant ecosystem services. These include the alteration of nutrients in aquatic sediment and overlying water, shelter to other species in the form of burrows in terrestrial and water ecosystems, and soil production on land.

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