Biocenosis of Mediterranean supralittoral sands
Description (English)
Area corresponding to the upper beach which is only humected by the sea during storms; however, certain areas do escape being totally submerged and receive a large amount of spray coming from the surge of the waves further down. 2 sets of phenomena are responsible for the dampness: at surface level, the dampness is caused by the salty spray from the breaking of the waves on the coast which is the main cause of the saltiness of the sand and the dampness of the night air. This humification only affects the top 2 or 3 centimetres and disappears quickly under the action of the sun; at depth, the sand is damp because of the proximity of the fairly unsalty ground water. The temperature is very variable and the daily differences in temperature may be extremely great: 0 to 20
Source: EUNIS habitat classification
Quick facts
EUNIS habitat type | code MA551 |
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Relation to | Resolution 4 habitat type (used for designation of Emerald sites) |
Legal status
Relation to other habitat types mentioned in legal instruments
Vegetation types
Relation to vegetation types (syntaxa)
Not availableSpecies mentioned in habitat description
Other classifications
Classification | Code | Habitat type name | Relationship type |
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EUNIS Habitat Classification 2007 (revised descriptions 2012) | B1.22 | Biocenosis of supralittoral sands | same |
History
Classification | Code | Habitat type name | Relationship type | Comment |
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EUNIS Habitat Classification 200410 | B1.22 | Biocenosis of supralittoral sands | same | |
EUNIS Habitat Classification 200308 | B1.22 | Biocenosis of supralittoral sands | same | |
EUNIS Habitat Classification 200202 | B1.22 | Biocenosis of supralittoral sands | same | |
EUNIS Habitat Classification 199910 | B1.22 | Biocenosis of supralittoral sands | same |