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Data Dictionary

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Folder		Existing folder New folder Identifier: Label:
Identifier
Label
Base URI
Registration status
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/
Version
Source
License

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}

Data element

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

Id	Label	Status	Status Modified	Notation
A6.75	Carbonate mounds	Valid	2014-01-31	A6.75
A6.8	Deep-sea trenches and canyons, channels, slope failures and slumps on the continental slope	Valid	2014-01-31	A6.8
A6.81	Canyons, channels, slope failures and slumps on the continental slope	Valid	2014-01-31	A6.81
A6.811	Active downslope channels	Valid	2014-01-31	A6.811
A6.812	Inactive downslope channels	Valid	2014-01-31	A6.812
A6.813	Alongslope channels	Valid	2014-01-31	A6.813
A6.814	Turbidites and fans	Valid	2014-01-31	A6.814
A6.82	Deep-sea trenches	Valid	2014-01-31	A6.82
A6.9	Vents, seeps, hypoxic and anoxic habitats of the deep sea	Valid	2014-01-31	A6.9
A6.91	Deep-sea reducing habitats	Valid	2014-01-31	A6.91
A6.911	Seeps in the deep-sea bed	Valid	2014-01-31	A6.911
A6.9111	Cold seep benthic communities of hadal zone	Valid	2014-01-31	A6.9111
A6.912	Gas hydrates in deep-sea	Valid	2014-01-31	A6.912
A6.913	Cetacean and other carcasses on the deep-sea bed	Valid	2014-01-31	A6.913
A6.92	Deep-sea bed influenced by hypoxic water column	Valid	2014-01-31	A6.92
A6.93	Isolated ‘oceanic’ features influenced by hypoxic water column	Valid	2014-01-31	A6.93
A6.94	Vents in the deep sea	Valid	2014-01-31	A6.94
A6.941	Active vent fields	Valid	2014-01-31	A6.941
A6.942	Inactive vent fields	Valid	2014-01-31	A6.942
A6.95	Pontic anoxic H2S black muds of the slope and abyssal plain, with anaerobic sulphate reducing bacteria and nematodes	Valid	2014-01-31	A6.95

Identifier
Label
Definition		Carbonate mounds are very steep-sided mounds of variety of shapes, which may be up to 350 m high and 2 km wide at their base (Weering et al, 2003). They occur offshore in water depths of 500 m-1100 m with examples present in the Porcupine Seabight and Rockall Trough (Kenyon et al, 2003). Carbonate mounds may have a sediment veneer, typically composed of carbonate sands, muds and silts. The cold-water reef-building corals [Lophelia pertusa] and [Madrepora oculata], as well as echiuran worms are characteristic fauna of carbonate mounds. Where cold-water corals (such as [Lophelia]) are present on the mound summit, coral debris may form a significant component of the overlying substratum. There is currently speculation on the origin of carbonate mounds, with possible associations with fault-controlled methane seepage from deep hydrocarbon reservoirs, or gas-hydrate dissociation (Henriet et al, 1998) through to the debris from ‘cold-water’ coral colonies such as [Lophelia].
Notation		A6.75

Identifier
Label
Definition		Habitats on the deep-sea bed significantly below the deep-sea bed, including deep ocean trenches, often greater than 6000 m depth with an active margin reduction zone (A6.82), and downslope or along-slope channels on the deep-sea bed (A6.81).
Notation		A6.8

Identifier
Label
Definition		No description available.
Notation		A6.81

Identifier
Label
Definition		No description available.
Notation		A6.811

Identifier
Label
Definition		No description available.
Notation		A6.812

Identifier
Label
Definition		No description available.
Notation		A6.813

Identifier
Label
Definition		No description available.
Notation		A6.814

Identifier
Label
Definition		Benthic communities of the oceanic trenches, deep elongated subduction troughs of the ocean floor.
Notation		A6.82

Identifier
Label
Definition		Deep-sea habitats characterised by chemical conditions. Includes interface habitats on the deep-sea bed where reducing conditions exist (A6.91), not generally associated with drastically elevated temperatures, including the carcasses of large cetaceans (A6.913). These habitats are often indicated by the presence of seeping or bubbling gases or liquids, hypoxic and/or anoxic conditions in the water column above. Also includes vents in the deep-sea bed (A6.94).
Notation		A6.9

Identifier
Label
Definition		No description available.
Notation		A6.91

Identifier
Label
Definition		No description available.
Notation		A6.911

Identifier
Label
Definition		Highly distinctive benthic communities of large bivalves, sponges and bryozoans, inhabiting the vicinity of oceanic methane-laden seeps, mostly localized in subduction trenches.
Notation		A6.9111

Identifier
Label
Definition		No description available.
Notation		A6.912

Identifier
Label
Definition		No description available.
Notation		A6.913

Identifier
Label
Definition		No description available.
Notation		A6.92

Identifier
Label
Definition		No description available.
Notation		A6.93

Identifier
Label
Definition		Hydrothermal vents occur along spreading ridges (such as the mid-Atlantic ridge), subduction zones, fracture zones and back-arc basins (Gage & Tyler, 1991), and are caused by seawater penetrating the upper levels of the Earth’s crust through channels formed in cooling lava flows, reacting chemically with hot basalt in the Earth’s crust and then rising back to the sea-bed to vent as superheated water containing compounds such as sulphides, metals, CO2 and methane (Tunnicliffe et al, 1998 in Gubbay, 2002). The water may trickle out from cracks and crevices on the seabed as hot springs (5-250°C), or as very concentrated jets of superheated water (270-380°C). As these concentrated jets of water cool, minerals dissolved in the water precipitate out in black clouds, giving them their common name of ‘black smokers’. At lower temperatures, sulphides are mostly precipitated within the rocks, making the venting fluids appear cloudier. These are known as ‘white smokers’ (Gage & Tyler, 1991). Hydrothermal vent fields cover relatively small areas of the seabed in water depths of 850 - 4000 m. The biological communities associated with hydrothermal vents are unusual as they are able to derive energy under conditions where photosynthesis is not possible. These habitats contain a huge diversity of chemoautotrophic bacteria, which form the core of the trophic structure around the vent. Characteristic species include the giant vent clam [Calyptogena magnifica], the mussel [Bathymodiolus thermophilus], the tube worm [Riftia pachyptila], the crabs [Cyanograea praedator] and [Bythograea thermydron] and the shrimp [Charocaris fortunate].
Notation		A6.94

Identifier
Label
Definition		No description available.
Notation		A6.941

Identifier
Label
Definition		No description available.
Notation		A6.942

Identifier
Label
Definition		No description available.
Notation		A6.95

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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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