MACRO-INVERTEBRATE FUNCTIONAL GROUPS IN FRESHWATER AND MARINE SEDIMENTS: A COMMON MECHANISTIC CLASSIFICATION
By Magali Gerino, G. Stora, Frédérique François-Carcaillet, F. Gilbert, Jean-Christophe Poggiale, F. Mermillod‐Blondin, G. Desrosiers, P. Vervier. 2003
157 citations recorded by the source corpus.
View Paper: https://www.semanticscholar.org/paper/12fe0b0bfcd6c811b4d980cfa2929bf2b693a825
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Citations in the corpus
- Macrobenthic recovery from hypoxia in an estuarine tidal mudflat (2008, methodology): “Species were classified into functional groups according to their mobility, feeding guilds and burrowing activity (tube-building versus biodestabiliser) based on literature (e.g. Fauchauld & Jumars 1979, Gerino et al. 2003, Volkenborn & Reise 2007) and our own observations (Table A1 in Appendix 1).”
- Towards an assessment of multiple ecosystem processes and services via functional traits (2010, background): “…need further progress for other organisms, such as soil fauna (Faber 1991; Bradford et al. 2002; Rutgers et al. 2009), soil microbes (Heemsbergen et al. 2004), freshwater and marine ecosystems (Dolédec et al. 1999; Gerino et al. 2003) and pollinators (Kremen et al. 2007; Moretti et al. 2009).”
- Influence of bioturbation by three benthic infaunal species on microbial communities and biogeochemical processes in marine sediment (2004, unknown): “This modelling approach allowed the classification of marine invertebrates into different functional groups (see review in Gerino et al. 2003).”
- Morphological and functional characterisation of the burrow systems of six earthworm species (Lumbricidae) (2015, result): “This surprising lack of knowledge is in sharp contrast with the situation in the field of sediment ecology where a typology of bioturbation behaviours (biodiffusor reworkers, upward conveyors) and thus burrow morphologies has been established (Gerino et al. 2003).”
- Benthic community-mediated sediment dynamics (2008, background): “Biodiffusion (Gerino et al. 2003) is one of the processes which keeps the sediment surface loose and increases bottom roughness, rendering it more susceptible to erosion (Woodin & Jackson 1979).”