Bioirrigation

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.

Aluminium, Iron, Cobalt, Copper, Zinc, and Cerium are all affected at the start of the process, when the larvae begins to dig into the sediment.

It also makes it so the oxygen cannot penetrate deeply into the sediment and there is accumulation of reduced mineralized products in pore water.

Two organisms that contribute to the bioturbation of soil are Nephtys caeca (Fabricius) and Nereis virens (Sars) annelidae.

One of the most important dinoflagellates that these organisms help distribute is called noxious microalgae and it is responsible for the formation of toxic red tides.

These red tides poison mollusks and crustaceans which results in very important economic losses in the fishing industry.

Bioturbation and bioirrigation in the sediment at the bottom of a coastal ecosystems
Coastal environment
4D tracing of bioirrigation in marine sediment
4D tracing of bioirrigation in marine sediment
A depiction of the kind of noxious microalgae that would form toxic red tides.