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Usage Examples
Filter by Meaning The presence of bioturbation in the soil can be used as an indicator of the health of the soil ecosystem.
The bioturbation caused by earthworms in the soil helps to aerate and fertilize the ground.
The measurement of bioturbation rates in sediments can be used as an indicator of ecosystem health and disturbance.
The analysis of bioturbation patterns in soil can be used to estimate rates of soil formation and erosion.
The bioturbation caused by the activity of bacteria and other microorganisms can affect the biogeochemical cycles of the soil.
The effects of bioturbation on sediment properties can have implications for the storage and release of carbon in wetland ecosystems.
The study of bioturbation is important for understanding the ecological processes in marine sediment.
The bioturbation caused by the feeding and burrowing of clams and other bivalves can affect the sediment composition of estuaries.
The bioturbation caused by ground-nesting animals can have significant impacts on plant growth and distribution.
The bioturbation created by the burrowing of prairie dogs helps to mix and fertilize the soil.
The bioturbation caused by burrowing shrimp has a significant impact on marine sediment.
The bioturbation of burrowing animals can alter the distribution of pollutants in soil.
The impact of bioturbation on soil properties is an essential consideration in ecological restoration projects.
Bioturbation caused by earthworms can increase soil nutrient availability.
The bioturbation activity of small mammals can lead to changes in soil structure and nutrient distribution.
The bioturbation of microorganisms can have a profound effect on the nutrient cycling of aquatic systems.
The role of bioturbation in the evolution of ecosystems is a topic of ongoing research.
The burrowing of shrimp and crabs leads to bioturbation, which can cause changes in sediment properties.
The bioturbation of bacteria in soil can have a significant impact on the nutrient cycling process.
Researchers have observed bioturbation in sediment layers caused by grazing fish.
The bioturbation of bivalves can modify sediment grain size and composition in intertidal zones.
The study of bioturbation helps to understand the ecological processes in ecosystems.
Bioturbation by burrowing animals can help to oxygenate deep sediment layers.
The extent of bioturbation by insects can affect the soil's water-holding capacity.
The presence of bioturbation in sediment cores can complicate interpretations of past climate change.
Bioturbation increases the permeability of sediments, allowing for better water flow.
Bioturbation by fish can affect the survival of coral reefs.
In a freshwater ecosystem, beavers are important agents of bioturbation.
Bioturbation can alter the distribution of contaminants in sediments and soils.
The intensity of bioturbation varies with the density and diversity of the benthic community.
The fossil record shows evidence of bioturbation dating back to the Cambrian period.
The paleontologist studied the bioturbation patterns in the fossil record to understand ancient ecosystems.
The impact of bioturbation on carbon sequestration in wetlands is an active area of research.
The study of bioturbation is important for understanding nutrient cycling in soil.
Invertebrates such as insects and earthworms are the main agents of bioturbation in forest soils.
The bioturbation of sand by crabs can create unique patterns on the beach.
The bioturbation of the soil by earthworms helps to improve its fertility.
The bioturbation caused by burrowing animals can affect soil structure and nutrient cycling.
The activity of burrowing animals can cause bioturbation, which has a profound effect on nutrient cycling.
Bioturbation by invertebrates can help to increase the rate of organic matter decomposition.
The bioturbation caused by grazing animals can have a significant impact on the composition of the grassland ecosystem.
The rate of bioturbation in a wetland area can indicate the health of the ecosystem.
Bioturbation can alter the distribution of contaminants in soil and sediment.
Bioturbation is an essential process that occurs in the soil, affecting nutrient cycling and soil structure.
The effects of bioturbation on nutrient cycling can be seen in the differences between natural and agricultural soils.
The activity of burrowing animals such as moles and gophers can cause bioturbation, leading to changes in the distribution of soil nutrients.
The burrowing activity of earthworms is a classic example of bioturbation.
The bioturbation caused by earthworms improves the aeration and drainage of soil.
The study of bioturbation has implications for land management practices and conservation efforts.
Bioturbation can increase the availability of nutrients to plants by breaking down organic matter.
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