We propose a simple and inexpensive method to determine the rate and pattern of surface sediment reworking by benthic organisms. Unlike many existing methods commonly used in bioturbation studies, which usually require sediment sampling, our approach is fully non-destructive and is well suited for investigating non-cohesive fine sediments in streams and rivers. Optical tracer (e.g., luminophores or coloured sand) disappearance or appearance is assessed through time based on optical quantification of surfaces occupied by tracers. Data are used to calculate surface sediment reworking (SSR) coefficients depicting bioturbation intensities. Using this method, we evaluated reworking activity of stream organisms (three benthic invertebrates and a ...
Anthropogenic modifications of sediment load can cause ecological degradation in stream and river ec...
Bioturbation models are typically one-dimensional, with the underlying assumption that tracer gradie...
Bioturbation of bottom sediments at the sediment–water interface is currently gaining more attention...
International audienceWe propose a simple and inexpensive method to determine the rate and pattern o...
This review lists and discusses the different methods currently available to assess sediment reworki...
Habitat modification by burrowing organisms in soft benthic sediments has long been recognized as a ...
Sediment erosion by water movement affects turbidity and thus benthic communities in numerous aquati...
In order to compare and quantify sediment reworking activities by different species/functional group...
Macrofaunal bioturbation is an important mechanism for the enhancement of remineralization and bioge...
Particle and solute transport by faunal activities may significantly influence rates and pathways of...
Depositional zones in headwater streams are colonized by a diverse community of benthic macroinverte...
Stream‐deposited sediment is one of the major stressors affecting stream biota. Several methods exis...
We propose an empirical framework to scale the effects of bioturbation on sediment resuspension to p...
© 2018 The Author(s) Benthic macroinvertebrates inhabit the streambed sediments of temporary streams...
AbstractAnthropogenic modifications of sediment load can cause ecological degradation in stream and ...
Anthropogenic modifications of sediment load can cause ecological degradation in stream and river ec...
Bioturbation models are typically one-dimensional, with the underlying assumption that tracer gradie...
Bioturbation of bottom sediments at the sediment–water interface is currently gaining more attention...
International audienceWe propose a simple and inexpensive method to determine the rate and pattern o...
This review lists and discusses the different methods currently available to assess sediment reworki...
Habitat modification by burrowing organisms in soft benthic sediments has long been recognized as a ...
Sediment erosion by water movement affects turbidity and thus benthic communities in numerous aquati...
In order to compare and quantify sediment reworking activities by different species/functional group...
Macrofaunal bioturbation is an important mechanism for the enhancement of remineralization and bioge...
Particle and solute transport by faunal activities may significantly influence rates and pathways of...
Depositional zones in headwater streams are colonized by a diverse community of benthic macroinverte...
Stream‐deposited sediment is one of the major stressors affecting stream biota. Several methods exis...
We propose an empirical framework to scale the effects of bioturbation on sediment resuspension to p...
© 2018 The Author(s) Benthic macroinvertebrates inhabit the streambed sediments of temporary streams...
AbstractAnthropogenic modifications of sediment load can cause ecological degradation in stream and ...
Anthropogenic modifications of sediment load can cause ecological degradation in stream and river ec...
Bioturbation models are typically one-dimensional, with the underlying assumption that tracer gradie...
Bioturbation of bottom sediments at the sediment–water interface is currently gaining more attention...