2018
DOI: 10.5194/essd-10-109-2018
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A synthetic map of the north-west European Shelf sedimentary environment for applications in marine science

Abstract: Abstract. Seabed sediment mapping is important for a wide range of marine policy, planning and scientific issues, and there has been considerable national and international investment around the world in the collation and synthesis of sediment datasets. However, in Europe at least, much of this effort has been directed towards seabed classification and mapping of discrete habitats. Scientific users often have to resort to reverse engineering these classifications to recover continuous variables, such as mud co… Show more

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Cited by 67 publications
(130 citation statements)
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“…Shelf sediments are dominated by permeable (sandy) sediment (Boudreau et al, 2001;Hall, 2002;Glud, 2008;Rao et al, 2008;Hicks et al, 2017) which typically have lower organic and higher inorganic carbon concentrations compared to cohesive (muddy) sediments. The distribution of PIC in shelf sediments aligns with the coverage of permeable sediments (Wilson et al, 2018), particularly in areas of high carbonate sediments such as the Shetland and Orkney Islands (see Figure 3).…”
Section: Outputs To Benthic Storage and The Open Oceansupporting
confidence: 61%
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“…Shelf sediments are dominated by permeable (sandy) sediment (Boudreau et al, 2001;Hall, 2002;Glud, 2008;Rao et al, 2008;Hicks et al, 2017) which typically have lower organic and higher inorganic carbon concentrations compared to cohesive (muddy) sediments. The distribution of PIC in shelf sediments aligns with the coverage of permeable sediments (Wilson et al, 2018), particularly in areas of high carbonate sediments such as the Shetland and Orkney Islands (see Figure 3).…”
Section: Outputs To Benthic Storage and The Open Oceansupporting
confidence: 61%
“…Sediment carbon stocks and benthic-pelagic fluxes were calculated using different spatial divisions to each other, due to differences in data availability. Observations and modeling (Diesing et al, 2017;Wilson et al, 2018) allowed carbon stocks to be resolved at a regional level so the seabed of the NWES was divided into 13 areas (the 11 regions in Figure 1, plus sediment in Scottish lochs and Norwegian fjords). Benthic-pelagic fluxes were estimated over the whole shelf area due to data paucity, with the exception of lochs, fjords, the Norwegian Trench and the Skagerrak and Kattegat, which were quantified separately.…”
Section: Scope and Approachmentioning
confidence: 99%
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“…Sediment median grain size was collated from Wilson, Speirs, Sabatino, and Heath (2018), a synthetic map derived from a blend of survey data, statistically modelled values derived from bed shear stress and bathymetry, with a spatial resolution of 0.125° × 0.125°. The full dataset can be accessed at: https://doi.org/10.15129/1e27b806-1eae-494d-83b5-a5f4792c46fc.…”
Section: Methodsmentioning
confidence: 99%
“…Fig. 2 presents the percent sand, mud, and gravel of each 1 9 1 min grid cell obtained from Wilson et al (2018). Tidal bed shear stress (N/m 2 ) was obtained from a hydrodynamic model by John Aldridge (CEFAS) as used in Hiddink et al (2006) and van Denderen et al (2015a).…”
Section: Habitat Variablesmentioning
confidence: 99%