Information for "Traits:Infralittoral"
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Display title | Traits:Infralittoral |
Default sort key | Infralittoral |
Page length (in bytes) | 1,152 |
Page ID | 9441 |
Page content language | en - English |
Page content model | wikitext |
Indexing by robots | Allowed |
Number of redirects to this page | 0 |
Counted as a content page | Yes |
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Edit history
Page creator | Josbut (talk | contribs) |
Date of page creation | 11:55, 24 November 2014 |
Latest editor | Stefanie Dekeyzer (talk | contribs) |
Date of latest edit | 15:46, 6 May 2015 |
Total number of edits | 2 |
Total number of distinct authors | 2 |
Recent number of edits (within past 90 days) | 0 |
Recent number of distinct authors | 0 |
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A subzone of the sublittoral in which upwa … A subzone of the sublittoral in which upward-facing rocks are dominated by erect algae, typically kelps; it can be further subdivided into the upper and lower infralittoral (based on Hiscock, 1985). The term is also used by Glémarec (1973) to refer to areas (étages) with a eurythermal environment of great seasonal and also daily and tidal amplitude. 1) lower The part of the infralittoral subzone which, on hard substrata, supports scattered kelp plants (a kelp park) or from which kelps are absent altogether and the seabed is dominated by foliose red and brown algae. It may be difficult to distinguish the lower infralittoralwhere grazing pressure prevents the establishment of foliose algae. 2) upper The part of the infralittoral subzone which, on hardsubstrata, is dominated by Laminariales forming a dense canopy, or kelp forest (based on Hiscock, 1985)., or kelp forest (based on Hiscock, 1985). +
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