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            <gco:CharacterString>Structure and function assessment of macrobenthic communities from north of the Dogger Bank, the Oyster Ground and at Sean Gas Field, in 2007</gco:CharacterString>
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        <gco:CharacterString>Four infaunal replicate samples were collected at each site using 0.1 m2 
Nioz corers (diameter of approximately 30 cm) were sieved on a 1mm mesh sieve, 
the sieve remains were then sorted and preserved following the methodology 
described by Boyd (2002). On return, to the laboratory all the infaunal 
samples were identified to the lowest taxonomic level as possible, counted and 
weighted.

 Five epifaunal replicate samples were collected at each site using 2 m beam 
trawls during each of the five research cruises. Each trawl was conducted at a 
constant speed (~2 knots per minute) and sampled an area of seabed of 
approximately 400 m2. Once on board, the contents of the trawl were sieved 
over 5mm mesh and all retained individuals were identified, counted and 
weighed. In some cases, the very high numbers of some groups (e.g. brittle 
stars, shrimps, and small fish) needed sub-sampling before counting and 
weighting.

The raw abundance and biomass data for both the infauna (from the cores) and 
epifauna (trawls) were scaled to values per m2. As some taxa were present in 
both datasets, taxa which were more appropriately classed as infauna and/or 
their densities were better estimated via a corer were classed as infauna and 
removed from the trawl data. Accordingly, those taxa which were generally 
considered as epifaunal (and their numbers and biomasses better estimated 
using a trawl) were considered as epifaunal and/or their densities more 
suitably estimated using a trawl were reported as epifauna.</gco:CharacterString>
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                <gco:CharacterString>SeaDataNet P03 parameter discovery vocabulary</gco:CharacterString>
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            <gmx:Anchor xlink:type="simple" xlink:href="https://vocab.nerc.ac.uk/collection/P22/current/sd">Species distribution</gmx:Anchor>
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                <gco:CharacterString>GEMET - INSPIRE themes, version 1.0</gco:CharacterString>
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            <gmx:Anchor xlink:type="simple" xlink:href="https://vocab.nerc.ac.uk/collection/L13/current/NB">Benthic boundary</gmx:Anchor>
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            <gmx:Anchor xlink:type="simple" xlink:href="https://vocab.nerc.ac.uk/collection/L13/current/SD">Sediment</gmx:Anchor>
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                <gco:CharacterString>SeaVoX Vertical Co-ordinate Coverages</gco:CharacterString>
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                    <gco:Date>2010-05-18</gco:Date>
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and October, 2007) at three study sites, north of the Dogger Bank (hereafter 
as DB) (55.68 º N, 2.28 º E), the Oyster Ground (54.41º N, 4.04º E) (hereafter 
as OG) and at Sean Gas Field (hereafter SGF) (53.17º N, 2.81º E). Previous 
research conducted at the sites, have shown that these sites have 
representative characteristics of larger regions with similar water column and 
seabed attributes, considering them as eco-hydrodynamic regions in the 
southern and central North Sea (see van der Molen et al., 2012; Painting and 
Foster, 2013).

At each site four replicate samples were collected with a 0.1 m2 Nioz corer 
to sample benthic infauna and sediments. From each Nioz corer, a small corer 
(internal diameter of 5.5 cm) was used to obtain sediments for the analysis of 
particle size, porosity, chlorophyll a/phaeopigment and organic carbon 
analysis. These cores were sliced at 0.5 to 1 cm intervals up to 10cm depth 
and stored at -20°C.</gco:CharacterString>
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