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Bioirrigation

Bioturbation and bioirrigation in the sediment at the bottom of a coastal ecosystems

Bioirrigation refers to the process of benthic organisms flushing their burrows with overlying water. The exchange of dissolved substances between the porewater and overlying seawater that results is an important process in the context of the biogeochemistry of the oceans.

Marine coastal ecosystems often have organisms that destabilize sediment. They change the physical state of the sediment. Thus improving the conditions for other organisms and themselves. These organisms often also cause bioturbation, which is commonly used interchangeably or in reference with bioirrigation.[1]

Bioirrigation works as two different processes. These processes are known as particle reworking and ventilation, which is the work of benthic macro-invertebrates (usually ones that burrow). This particle reworking and ventilation is caused by the organisms when they feed (faunal feeding), defecate, burrow, and respire.

Bioirrigation is responsible for a large amount of oxidative transport and has a large impact on biogeochemical cycles.

  1. ^ Volkenborn, N.; Hedtkamp, S. I. C.; van Beusekom, J. E. E.; Reise, K. (2007-08-01). "Effects of bioturbation and bioirrigation by lugworms (Arenicola marina) on physical and chemical sediment properties and implications for intertidal habitat succession". Estuarine, Coastal and Shelf Science. 74 (1–2): 331–343. Bibcode:2007ECSS...74..331V. doi:10.1016/j.ecss.2007.05.001.