Linked from

The 37 pages that link to Bioturbation, each with the reason it gives.

• Benthic zoneRelated: It redistributes particles and oxygen through benthic sediments.

• DetritivoreRelated: Burrowing detritivores move organic matter and alter soil structure.

• Ecosystem engineerRelated: Burrowing and feeding can reshape sediment, oxygen flow, and habitat structure.

• Marine sedimentRelated: Seafloor animals mix layers and alter the preservation of sediment records.

• Trace fossilRelated: Burrowing and feeding disturb sediment in ways that can later become trace fossils.

• FossorialityRelated: Fossorial animals alter soil structure, nutrient distribution, and water movement through excavation.

• Soil horizonRelated: Organisms mix horizons and can blur their boundaries.

• Soil profileRelated: It can blur boundaries between horizons and redistribute organic matter.

• Sea cucumberRelated: As they feed and move, sea cucumbers rework seafloor sediment and its nutrients.

• Benthic feedingRelated: Animals that search or feed within sediment reshape the bottom as they forage.

• CrayfishRelated: Burrowing crayfish can rearrange stream and pond sediments.

• Benthic ecologyRelated: It changes sediment structure, oxygen penetration, and nutrient cycling in benthic habitats.

• Common carpRelated: Carp stir bottom sediments while feeding, increasing turbidity and resuspending nutrients.

• MeiofaunaRelated: Meiofaunal feeding and movement can alter sediment structure and chemical conditions.

• Deep-sea benthosRelated: Benthic animals reshape sediments and redistribute oxygen and nutrients.

• Marine benthic zoneRelated: Seabed animals reshape sediments and alter oxygen and nutrient distributions.

• MudflatRelated: Burrowing animals aerate and rearrange mudflat sediments.

• Mangrove crabRelated: Crab burrowing mixes mangrove sediment and changes its oxygen and nutrient conditions.

• Macrotermes bellicosusRelated: Termite excavation moves soil and changes its structure around colonies.

• Soil morphologyRelated: Roots and soil animals can blur horizon boundaries and create pores or channels.

• TopsoilRelated: Burrowing animals and roots mix organic residues into topsoil and alter its structure.

• Pelagic sedimentRelated: Deep-sea animals can blur the layers that record pelagic deposition.

• SeabedRelated: Burrowing animals alter seabed layers and the traces they preserve.

• SipunculaRelated: Their burrowing and feeding redistribute sediment and organic material.

• ArenicolaRelated: Lugworm burrowing continually moves and aerates intertidal sediment.

• AxiideaRelated: Axiidean digging moves sediment and changes its physical and chemical conditions.

• Eastern moleRelated: Eastern mole tunnels and excavation move soil through the ground profile.

• NereididaeRelated: Burrowing nereidids mix coastal sediments and alter oxygen and nutrient exchange.

• Scotoplanes globosaRelated: Its movement and deposit feeding can disturb surface sediments.