Information for "Traits:Circalittoral"
Basic information
| Display title | Traits:Circalittoral |
| Default sort key | Circalittoral |
| Page length (in bytes) | 1,019 |
| Page ID | 9444 |
| 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 | Allow all users (infinite) |
| Move | Allow all users (infinite) |
Edit history
| Page creator | Josbut (talk | contribs) |
| Date of page creation | 11:59, 24 November 2014 |
| Latest editor | Stefanie Dekeyzer (talk | contribs) |
| Date of latest edit | 15:31, 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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... more about "Circalittoral"
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The subzone of the rocky sublittoral below … The subzone of the rocky sublittoral below that dominated by algae (the infralittoral), and dominated by animals. No lower limit is defined, but species composition changes below about 40m to 80m depth, depending on depth of the seasonal thermocline. This subzone can be subdivided into the upper circalittoral where foliose algae are present and the lower circalittoral where they are not (see Hiscock, 1985). The term is also used by Glémarec (1973) to refer to two étages of the sediment benthos below the infralittoral: a "coastal circalittoral category with a eurythermal environment of weak seasonal amplitude (less than 10°C) varying slowly" and a "circalittoral category of the open sea with a stenothermal environment" (Hiscock, 1996).stenothermal environment" (Hiscock, 1996). +
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