2012
DOI: 10.1016/j.jembe.2011.12.010
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Small scale terrestrial clay deposits on intertidal sandflats: Behavioral changes and productivity reduction

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Cited by 22 publications
(20 citation statements)
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“…Blackburn and Henriksen, 1983;Glud, 2008;Hohaia et al, 2013;Huettel et al, 2003), as well as macrofauna behaviour and ecosystem functioning (e.g. Lohrer et al, 2004;Pratt et al, 2013;Woodin et al, 2012). Benthic macrofauna are known to influence nitrogen cycling (Aller, 1988;Kristensen et al, 1991;Laverock et al, 2011), and the presence of macrophytes and microphytobenthos is also expected to influence pore water nutrient concentrations and the level of experimental enrichment.…”
Section: Introductionmentioning
confidence: 99%
“…Blackburn and Henriksen, 1983;Glud, 2008;Hohaia et al, 2013;Huettel et al, 2003), as well as macrofauna behaviour and ecosystem functioning (e.g. Lohrer et al, 2004;Pratt et al, 2013;Woodin et al, 2012). Benthic macrofauna are known to influence nitrogen cycling (Aller, 1988;Kristensen et al, 1991;Laverock et al, 2011), and the presence of macrophytes and microphytobenthos is also expected to influence pore water nutrient concentrations and the level of experimental enrichment.…”
Section: Introductionmentioning
confidence: 99%
“…Nevertheless, both processes influence sediment community composition and functioning. Numerous studies illustrate that terrigenous sediment deposition affects coastal soft-sediment community composition, dynamics, species behavior and ecosystem functioning [6], [7], [8]. Furthermore, suspended sediments decrease the fitness of filter feeding organisms directly by decreasing filtration rate and absorption efficiency that reduces net energy intake [9], and indirectly by increasing turbidity and hence decreasing water column primary production, i.e.…”
Section: Introductionmentioning
confidence: 99%
“…liliana live at a depth of 2–10 cm in mid-shore sandy sediments and feed on surface MPB using an inhalant siphon [ 26 ]. During feeding, this species creates pore-water pressure gradients that oxygenate deeper sediments and force nutrient rich pore-water upwards towards the sediment surface, thereby potentially facilitating MPB production [ 27 29 ]. M .…”
Section: Introductionmentioning
confidence: 99%