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Identifier
Label
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Type		Common
Numeric concept identifiers
Notations equal identifiers
Definition		Classification of habitat types according to the EUNIS Biodiversity database This is the dataset referenced from INSPIRE: http://inspire.ec.europa.eu/codelist/EunisHabitatTypeCodeValue/
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Bound elements for concepts

Element	Type	Status
skos:broader	Quantitative	Released Step 1 Step 2 Step 3 Step 4 Step 5 ^{30 Sep 2013}
skos:editorialNote	Quantitative	Released Step 1 Step 2 Step 3 Step 4 Step 5 ^{24 Sep 2013}
skos:exactMatch	Quantitative	Released Step 1 Step 2 Step 3 Step 4 Step 5 ^{30 Sep 2013}
skos:narrower	Quantitative	Released Step 1 Step 2 Step 3 Step 4 Step 5 ^{17 Sep 2015}

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Identifier
Label
Definition
Notation		(forcefully equal to identifier in this vocabulary)

Vocabulary concepts

5,282 concepts found, displaying 141 to 160.First Prev 4 5 6 789 10 11 Next Last

Id	Label	Status	Status Modified	Notation
A1.49	Hydrolittoral mussel beds	Valid	2014-01-31	A1.49
A1.491	Hydrolittoral mussel beds: with little or no macrophyte vegetation	Valid	2014-01-31	A1.491
A1.492	Hydrolittoral mussel beds: dominated by macrophyte vegetation	Valid	2014-01-31	A1.492
A1.4A	Hydrolittoral peat	Valid	2014-01-31	A1.4A
A1.4B	Pontic sulphide vents in littoral rock	Valid	2014-01-31	A1.4B
A2	Littoral sediment	Valid	2014-01-31	A2
A2.1	Littoral coarse sediment	Valid	2014-01-31	A2.1
A2.11	Shingle (pebble) and gravel shores	Valid	2014-01-31	A2.11
A2.111	Barren littoral shingle	Valid	2014-01-31	A2.111
A2.112	[Pectenogammarus planicrurus] in mid shore well-sorted gravel or coarse sand	Valid	2014-01-31	A2.112
A2.12	Estuarine coarse sediment shores	Valid	2014-01-31	A2.12
A2.13	Mediterranean communities of mediolittoral coarse detritic bottoms	Valid	2014-01-31	A2.13
A2.131	Facies of banks of dead leaves of [Posidonia oceanica] and other phanerogams	Valid	2014-01-31	A2.131
A2.132	Pontic mediolittoral gravel and shingle	Valid	2014-01-31	A2.132
A2.2	Littoral sand and muddy sand	Valid	2014-01-31	A2.2
A2.21	Strandline	Valid	2014-01-31	A2.21
A2.211	Talitrids on the upper shore and strandline	Valid	2014-01-31	A2.211
A2.212	[Mytilus edulis] and [Fabricia sabella] in littoral mixed sediment	Valid	2014-01-31	A2.212
A2.22	Barren or amphipod-dominated mobile sand shores	Valid	2014-01-31	A2.22
A2.221	Barren littoral coarse sand	Valid	2014-01-31	A2.221

CSV Import

The CSV file should contain a header row for element names and data rows for concepts.
It is strongly recommended to use an exported CSV file as a template for bulk editing. Columns and rows can be added to or deleted from the template file.
A concept can be ignored by prepending a double-slash '//' to the concept row in the CSV

If the header row contains unknown elements the import will aborted and data will be rolled back
Erroneous concept rows are ignored, valid data rows are still imported
Successful import cannot be undone (unless "undo checkout" is performed)
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"Purge Vocabulary" option deletes all the vocabulary concepts before import

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Columns	Notation Status Status Modified Accepted Date Not Accepted Date skos:broader skos:editorialNote skos:exactMatch skos:narrower
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Identifier
Label
Definition		Littoral sediment includes habitats of shingle (mobile cobbles and pebbles), gravel, sand and mud or any combination of these which occur in the intertidal zone. Littoral sediment is defined further using descriptions of particle sizes - mainly gravel (16-4 mm), coarse sand (4-1 mm), medium sand (1-0.25 mm), fine sand (0.25-0.063 mm) and mud (less than 0.063 mm) and various admixtures of these (and coarser) grades - muddy sand, sandy mud and mixed sediment (cobbles, gravel, sand and mud together). Littoral sediments support communities tolerant to some degree of drainage at low tide and often subject to variation in air temperature and reduced salinity in estuarine situations. Very coarse sediments tend to support few macrofaunal species because these sediments tend to be mobile and subject to a high degree of drying when exposed at low tide. Finer sediments tend to be more stable and retain some water between high tides, and therefore support a greater diversity of species. Medium and fine sand shores usually support a range of oligochaetes, polychaetes, and burrowing crustaceans, and even more stable muddy sand shores also support a range of bivalves. Very fine and cohesive sediment (mud) tends to have a lower species diversity, because oxygen cannot penetrate far below the sediment surface. A black, anoxic layer of sediment develops under these circumstances, which may extend to the sediment surface and in which few species can survive. Some intertidal sediments are dominated by angiosperms, e.g. eelgrass ([Zostera noltii]) beds on the mid and upper shore of muddy sand flats, or saltmarshes which develop on the extreme upper shore of sheltered fine sediment flats. Situation: Littoral sediments are found across the entire intertidal zone, including the strandline. Sediment biotopes can extend further landwards (dune systems, marshes) and further seawards (sublittoral sediments). Sediment shores are generally found along relatively more sheltered stretches of coast compared to rocky shores. Muddy shores or muddy sand shores occur mainly in very sheltered inlets and along estuaries, where wave exposure is low enough to allow fine sediments to settle. Sandy shores and coarser sediment (gravel, pebbles, cobbles) shores are found in areas subject to higher wave exposures. Temporal variation: Littoral sediment environments can change markedly over seasonal cycles, with sediment being eroded during winter storms and accreted during calmer summer months. The particle size structure of the sediment may change from finer to coarser during winter months, as finer sediment gets resuspended in seasonal exposed conditions. This may affect the sediment infauna, with some species only present in summer when sediments are more stable. These changes are most likely to affect sandy shores on relatively open shores. Sheltered muddy shores are likely to be more stable throughout the year, but may have a seasonal cover of green seaweeds during the summer period, particularly in nutrient enriched areas or where there is freshwater input.
Notation		A2

Identifier
Label
Definition		Littoral coarse sediments include shores of mobile pebbles, cobbles and gravel, sometimes with varying amounts of coarse sand. The sediment is highly mobile and subject to high degrees of drying between tides. As a result, few species are able to survive in this environment. Beaches of mobile cobbles and pebbles tend to be devoid of macroinfauna, while gravelly shores may support limited numbers of crustaceans, such as [Pectenogammarus planicrurus]. Situation: Littoral coarse sediments are found along relatively exposed open shores, where wave action prevents finer sediments from settling. Coarse sediments may also be present on the upper parts of shores where there are more stable, sandy biotopes on the lower and mid shore. Temporal variation: The sediment particle size structure may vary seasonally, with relatively finer sediments able to settle during calmer conditions in summer. Where the sediment grain size is very large (at the interface between sediment and boulder shores), cobbles may be mobile during exposed winter conditions, but stable enough during summer months to support limited juvenile rocky shore epifauna (e.g. juvenile barnacles).
Notation		A2.1

Identifier
Label
Definition		Shores of shingle (mobile cobbles and pebbles) or coarse gravel, typically deposited as a result of onshore wave action and long-shore drift. The particle size tends to increase along the shore in the direction of the long-shore drift. As the sediment is very coarse and often quite mobile, it typically supports little marine life, other than opportunist amphipods and oligochaete worms. Summer growths of ephemeral green algae ([Enteromorpha] spp.) may develop.
Notation		A2.11

Identifier
Label
Definition		Shingle or gravel shores, typically with sediment particle size ranging from 4 - 256 mm, sometimes with some coarse sand mixed in. This biotope is normally only found on exposed open coasts in fully marine conditions. Such shores tend to support virtually no macrofauna in their very mobile and freely draining substratum. The few individuals that may be found are those washed into the habitat by the ebbing tide, including the occasional amphipod or small polychaete. Situation: BarSh often extends over the whole shore, sometimes extending into the subtidal zone. BarSh may occur on the upper shore above BarSa, and in moderately exposed conditions, above AmSco on the lower shore. Tal may occur on the same shore as BarSh, where driftlines of algae and other debris accumulate on the upper shore. Temporal variation: There may be a temporary cover of the green seaweeds [Enteromorpha] spp. or [Ulva] spp. during periods of stability in the summer.
Notation		A2.111