Seafloor Geomorphology as Benthic Habitat 2012
DOI: 10.1016/b978-0-12-385140-6.00013-x
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Benthic Habitat Variations over Tidal Ridges, North Sea, the Netherlands

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Cited by 37 publications
(40 citation statements)
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“…Bed patterns are common features in sandy coastal shelf seas and estuaries, shaped by the interplay of tides, currents, waves, and biology. Various types of offshore bed forms can be found, for instance, sand banks (Stride, 1982), long bed waves (Knaapen et al, 2001), tidal sand waves (van Veen, 1935), mega ripples (Stride, 1982), and sand ripples (Allen, 1984). Of all the described bed forms, sand waves are the most relevant to study as their dynamic behavior can pose a threat to offshore civil engineering constructions, such as pipelines (Németh et al, 2003) and cables to wind farms (Roetert et al, 2017).…”
Section: Introductionmentioning
confidence: 99%
“…Bed patterns are common features in sandy coastal shelf seas and estuaries, shaped by the interplay of tides, currents, waves, and biology. Various types of offshore bed forms can be found, for instance, sand banks (Stride, 1982), long bed waves (Knaapen et al, 2001), tidal sand waves (van Veen, 1935), mega ripples (Stride, 1982), and sand ripples (Allen, 1984). Of all the described bed forms, sand waves are the most relevant to study as their dynamic behavior can pose a threat to offshore civil engineering constructions, such as pipelines (Németh et al, 2003) and cables to wind farms (Roetert et al, 2017).…”
Section: Introductionmentioning
confidence: 99%
“…Superimposed on the sand waves are megaripples [21], which have a wavelength of 15 m, where some wavelengths are as short as 10 m and others as long as 25 m. The megaripples move faster than the sand waves, in the scale of weeks [21,23] or even hours [24]. The troughs of the Brown Bank consist of muddy sediments mixed with gravel and shell fragments and the crests contain well sorted medium sand [17].…”
Section: Study Areamentioning
confidence: 99%
“…The Brown Bank area of the North Sea (Figure 1a; data source: [16]) exhibits sand waves of various sizes, namely, sand banks (Figure 1b), sand waves ( Figure 1c), and megaripples ( Figure 1d) (see Section 2.1 for definitions). Although the main sediment is sand, there is a variation of muddy sediments mixed with gravel and shell fragments in the deep troughs and well sorted medium sand on the crest [17]. Also, infauna species diversity and abundance is much higher in the troughs than on the crest [17].…”
Section: Introductionmentioning
confidence: 99%
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“…Crests and troughs of bedforms of varying size (ranging from ripples to megaripples, ridges and runnels, shoreface-connected ridges and sand waves) have been found to have different abiotic conditions (such as sediment grain size and organic matter content) but also to support different benthic communities (e.g. Barros et al 2004, Baptist et al 2006, van Dijk et al 2012, Zonneveld et al 2014, Markert et al 2015. This habitat differentiation, induced by hydrodynamic forces, may counteract the negative effect of the stress of hydro dynamics and disturbance by dune migration on species richness (e.g.…”
Section: Introductionmentioning
confidence: 99%