Old page wikitext, before the edit (old_wikitext) | '{{Redirect|Littoral}}
{{ocean habitat topics|image=Littoral Zones.jpg|caption=Different disciplines and agencies divide the littoral zone into different subregions, according to how they want to view the zone. This diagram shows the way the [[United States Navy]] views the zone.}}
The '''littoral zone''' is that part of a sea, lake or river that is close to the shore. In coastal environments the littoral zone extends from the [[Ordinary high water mark|high water mark]], which is rarely inundated, to shoreline areas that are permanently submerged. It always includes this [[intertidal zone]] and is often used to mean the same as the intertidal zone. However, the meaning of "littoral zone" can extend well beyond the intertidal zone.
There is no single definition. What is regarded as the full extent of the littoral zone, and the way the littoral zone is divided into subregions, varies in different contexts (lakes and rivers have their own definitions). The use of the term also varies from one part of the world to another, and between different disciplines. For example, military commanders speak of the littoral in ways that are quite different from marine biologists.
The adjacency of water gives a number of distinctive characteristics to littoral regions. The [[erosion|erosive]] power of water results in particular types of [[landform]]s, such as [[sand dune]]s, and [[estuary|estuaries]]. The natural movement of the littoral along the coast is called the [[littoral drift]]. Biologically, the ready availability of water enables a greater variety of plant and animal life, and the additional local [[humidity]] due to evaporation usually creates a [[microclimate]] supporting unique types of organisms.
The word "littoral" is used both as a [[noun]] and an [[adjective]]. It derives from the [[Latin language|Latin]] noun ''litus, litoris'', meaning "shore". (The doubled 't' is a late medieval innovation and the word is sometimes seen in the more classical-looking spelling 'litoral'.)
==In oceanography and marine biology==
[[File:Portugal 20040711 027.jpg|thumb|right|The [[intertidal zone]] of a beach is part of the littoral zone]]
[[File:Klamath river estuary.jpg|thumb|right|Estuaries are also in the littoral zone]]
{{wiktionary|littoral}}
{{wiktionary|supralittoral}}
{{wiktionary|eulittoral}}
{{wiktionary|sublittoral}}
{{wiktionary|infralittoral}}
{{wiktionary|circalittoral}}
In [[oceanography]] and [[marine biology]], the idea of the littoral zone is extended roughly to the edge of the continental shelf. Starting from the shoreline, the littoral zone begins at the spray region just above the high tide mark. From here, it moves to the intertidal region between the high and low water marks, and then out as far as the edge of the [[continental shelf]]. These three subregions are called, in order, the [[Littoral zone#Supralittoral zone|supralittoral zone]], the [[Littoral zone#Eublittoral zone|eulittoral zone]] and the [[Littoral zone#Sublittoral zone|sublittoral zone]].
===Supralittoral zone===
{{main|Supralittoral zone}}
The '''supralittoral zone''' (also called the '''splash''', '''spray''', or '''supratidal zone''') is the area above the spring high tide line that is regularly splashed, but not submerged by ocean water. Seawater penetrates these elevated areas only during storms with high tides.
Organisms here must cope also with exposure to bad air, fresh water from rain, cold, heat and [[predation]] by land animals and seabirds. At the top of this area, patches of dark [[lichen]]s can appear as crusts on rocks. Some types of [[Common periwinkle|periwinkles]], [[Neritidae]] and detritus feeding [[Isopod]]a commonly inhabit the lower supralitoral.<ref name="Yip and Madl">Yip and Madl</ref>
===Eulittoral zone===
{{main|Intertidal zone}}
The '''eulittoral zone''' (also called the '''midlittoral''' or '''mediolittoral zone''') is the '''intertidal zone''', also known as the '''foreshore'''. It extends from the spring high tide line, which is rarely inundated, to the neap low tide line, which is rarely not inundated. The wave action and turbulence of recurring tides shapes and reforms cliffs, gaps, and caves, offering a huge range of habitats for sedentary organisms. Protected rocky shorelines usually show a narrow almost homogenous eulittoral strip, often marked by the presence of [[barnacle]]s. Exposed sites show a wider extension and are often divided into further zones. For more on this, see [[intertidal ecology]].
===Sublittoral zone===
{{main|Neritic zone}}
The '''sublittoral zone''', also called the '''neritic zone''', starts immediately below the eulittoral zone. This zone is permanently covered with seawater.
In physical oceanography, the sublittoral zone refers to coastal regions with significant tidal flows and energy dissipation, including non-linear flows, internal waves, river outflows and oceanic fronts. In practice, this typically extends to the edge of the [[continental shelf]], with depths around 200 metres.
In marine biology, the sublittoral refers to the areas where sunlight reaches the ocean floor, that is, where the water is never so deep as to take it out of the [[photic zone]]. This results in high [[primary production]] and makes the sublittoral zone the location of the majority of sea life. As in physical oceanography, this zone typically extends to the edge of the [[continental shelf]]. The benthic zone in the sublittoral is much more stable than in the intertidal zone; temperature, water pressure, and the amount of sunlight remain fairly constant. Sublittoral corals do not have to deal with as much change as intertidal corals. Corals can live in both zones, but they are more common in the sublittoral zone.
Within the sublittoral, marine biologists also identify the following:
*The '''infralittoral zone''' is the algal dominated zone to maybe five metres below the low water mark.
*The '''circalittoral zone''' is the region beyond the infralittoral, that is, below the algal zone and dominated by [[Sessility (limnology)|sessile]] animals such as [[oyster]]s.
Shallower region of the sublittoral zone, extending not far from the shore, are sometimes referred to as the '''subtidal zone'''.
{{clear}}
==Around lakes==
[[File:Moon Lake shoreline - Riding Mountain National Park.JPG|thumb|right|Shoreline of a lake]]
In lakes, where tides are usually negligibly small, other definitions of "littoral" are used. For example, the [[Minnesota]] [[Department of Natural Resources]] defines littoral as that portion of the lake that is less than 15 [[foot (length)|feet]] in depth.<ref>{{cite web|url=http://www.dnr.state.mn.us/lakefind/surveys.html#littoral|title=Fisheries lake surveys| accessdate = 2006-03-17}}</ref> This zone is home to most of the aquatic plant life (both rooted and floating) in a pond or lake because the high amount of sunlight reaching it allows for significant [[photosynthesis|photosynthetic activity]].
==Other definitions==
For the purposes of naval operations, the [[United States Navy]] divides the littoral zone in the ways shown on the diagram at the top of this article. The [[United States Army Corps of Engineers]] and [[United States Environmental Protection Agency|Environmental Protection Agency]] have their own definitions, and these have legal implications.
==See also==
{{refbegin|3}}
* [[Ballantine Scale]]
* [[Benthic zone]]
* [[Coastal fish]]
* [[Intertidal zone]]
* [[Foreshore]]
* [[Limnetic zone]]
* [[Littoral combat ship]]
* [[Littoral drift]]
* [[Littoral warfare]]
* [[Marine debris]]
* [[Neritic zone]]
* [[Profundal zone]]
* [[Shingle beach]]
{{refend}}
==Notes==
{{reflist}}
==References==
{{Refbegin}}
* Haslett, Simon K (2001) ''Coastal Systems.'' Routledge. ISBN 978-0415213028
* Mann, Kenneth Henry (2000) [http://books.google.co.nz/books?id=y4OIojDxtzsC&pg=PA179&lpg=PA179&dq=Eulittoral&source=web&ots=8EMjPNWnbb&sig=GQ2QZ-32moL6t-xYMFMlp4HVf6Y&hl=en&sa=X&oi=book_result&resnum=49&ct=result#PPA179,M1 ''Ecology of Coastal Waters''] Blackwell Publishing. ISBN 9780865425507
* Yip, Maricela and Madl, Pierre (1999) [http://biophysics.sbg.ac.at/rovigno/rovigno3.htm ''Littoral''] [[University of Salzburg]].
{{Refend}}
{{physical oceanography|expanded=other}}
{{coastal geography}}
{{DEFAULTSORT:Littoral Zone}}
[[Category:Aquatic biomes]]
[[Category:Marine biology]]
[[Category:Fisheries]]
[[Category:Aquatic ecology]]
[[ca:Zona litoral]]
[[cs:Litorál]]
[[de:Litoral]]
[[et:Litoraal]]
[[es:Litoral (geografía)]]
[[eo:Marbordo]]
[[fr:Littoral]]
[[hr:Priobalje]]
[[io:Litoro]]
[[it:Battigia]]
[[ka:ლიტორალი]]
[[kk:Литораль]]
[[lt:Litoralė]]
[[nl:Littoraal]]
[[nn:Litoral]]
[[pl:Strefa przybrzeżna]]
[[pt:Litoral]]
[[ro:Zonă litorală]]
[[ru:Литораль]]
[[simple:Littoral zone]]
[[sl:Litoral]]
[[sv:Litoral]]
[[uk:Літораль]]
[[vi:Cận duyên]]' |
New page wikitext, after the edit (new_wikitext) | '{{Redirect|Littoral}}
{{ocean habitat topics|image=Littoral Zones.jpg|caption=Different disciplines and agencies divide the littoral zone into different subregions, according to how they want to view the zone. This diagram shows the way the [[United States Navy]] views the zone.}}
The '''littoral zone''' is that part of a sea, lake or river that is close to the shore. In coastal environments the littoral zone extends from the [[Ordinary high water mark|high water mark]], which is rarely inundated, to shoreline areas that are permanently submerged. It always includes this [[intertidal zone]] and is often used to mean the same as the intertidal zone. However, the meaning of "littoral zone" can extend well beyond the intertidal zone.
There is no single definition. What is regarded as the full extent of the littoral zone, and the way the littoral zone is divided into subregions, varies in different contexts (lakes and rivers have their own definitions). The use of the term also varies from one part of the world to another, and between different disciplines. For example, military commanders speak of the littoral in ways that are quite different from marine biologists.
The adjacency of water gives a number of balls distinctive characteristics to littoral regions. The [[erosion|erosive]] power of water results in particular types of [[landform]]s, such as [[sand dune]]s, and [[estuary|estuaries]]. The natural movement of the littoral along the coast is called the [[littoral drift]]. Biologically, the ready availability of water enables a greater variety of plant and animal life, and the additional local [[humidity]] due to evaporation usually creates a [[microclimate]] supporting unique types of organisms.
The word "littoral" is used both as a [[noun]] and an [[adjective]]. It derives from the [[Latin language|Latin]] noun ''litus, litoris'', meaning "shore". (The doubled 't' is a late medieval innovation and the word is sometimes seen in the more classical-looking spelling 'litoral'.)
==In oceanography and marine biology==
[[File:Portugal 20040711 027.jpg|thumb|right|The [[intertidal zone]] of a beach is part of the littoral zone]]
[[File:Klamath river estuary.jpg|thumb|right|Estuaries are also in the littoral zone]]
{{wiktionary|littoral}}
{{wiktionary|supralittoral}}
{{wiktionary|eulittoral}}
{{wiktionary|sublittoral}}
{{wiktionary|infralittoral}}
{{wiktionary|circalittoral}}
In [[oceanography]] and [[marine biology]], the idea of the littoral zone is extended roughly to the edge of the continental shelf. Starting from the shoreline, the littoral zone begins at the spray region just above the high tide mark. From here, it moves to the intertidal region between the high and low water marks, and then out as far as the edge of the [[continental shelf]]. These three subregions are called, in order, the [[Littoral zone#Supralittoral zone|supralittoral zone]], the [[Littoral zone#Eublittoral zone|eulittoral zone]] and the [[Littoral zone#Sublittoral zone|sublittoral zone]].
===Supralittoral zone===
{{main|Supralittoral zone}}
The '''supralittoral zone''' (also called the '''splash''', '''spray''', or '''supratidal zone''') is the area above the spring high tide line that is regularly splashed, but not submerged by ocean water. Seawater penetrates these elevated areas only during storms with high tides.
Organisms here must cope also with exposure to bad air, fresh water from rain, cold, heat and [[predation]] by land animals and seabirds. At the top of this area, patches of dark [[lichen]]s can appear as crusts on rocks. Some types of [[Common periwinkle|periwinkles]], [[Neritidae]] and detritus feeding [[Isopod]]a commonly inhabit the lower supralitoral.<ref name="Yip and Madl">Yip and Madl</ref>
===Eulittoral zone===
{{main|Intertidal zone}}
The '''eulittoral zone''' (also called the '''midlittoral''' or '''mediolittoral zone''') is the '''intertidal zone''', also known as the '''foreshore'''. It extends from the spring high tide line, which is rarely inundated, to the neap low tide line, which is rarely not inundated. The wave action and turbulence of recurring tides shapes and reforms cliffs, gaps, and caves, offering a huge range of habitats for sedentary organisms. Protected rocky shorelines usually show a narrow almost homogenous eulittoral strip, often marked by the presence of [[barnacle]]s. Exposed sites show a wider extension and are often divided into further zones. For more on this, see [[intertidal ecology]].
===Sublittoral zone===
{{main|Neritic zone}}
The '''sublittoral zone''', also called the '''neritic zone''', starts immediately below the eulittoral zone. This zone is permanently covered with seawater.
In physical oceanography, the sublittoral zone refers to coastal regions with significant tidal flows and energy dissipation, including non-linear flows, internal waves, river outflows and oceanic fronts. In practice, this typically extends to the edge of the [[continental shelf]], with depths around 200 metres.
In marine biology, the sublittoral refers to the areas where sunlight reaches the ocean floor, that is, where the water is never so deep as to take it out of the [[photic zone]]. This results in high [[primary production]] and makes the sublittoral zone the location of the majority of sea life. As in physical oceanography, this zone typically extends to the edge of the [[continental shelf]]. The benthic zone in the sublittoral is much more stable than in the intertidal zone; temperature, water pressure, and the amount of sunlight remain fairly constant. Sublittoral corals do not have to deal with as much change as intertidal corals. Corals can live in both zones, but they are more common in the sublittoral zone.
Within the sublittoral, marine biologists also identify the following:
*The '''infralittoral zone''' is the algal dominated zone to maybe five metres below the low water mark.
*The '''circalittoral zone''' is the region beyond the infralittoral, that is, below the algal zone and dominated by [[Sessility (limnology)|sessile]] animals such as [[oyster]]s.
Shallower region of the sublittoral zone, extending not far from the shore, are sometimes referred to as the '''subtidal zone'''.
{{clear}}
==Around lakes==
[[File:Moon Lake shoreline - Riding Mountain National Park.JPG|thumb|right|Shoreline of a lake]]
In lakes, where tides are usually negligibly small, other definitions of "littoral" are used. For example, the [[Minnesota]] [[Department of Natural Resources]] defines littoral as that portion of the lake that is less than 15 [[foot (length)|feet]] in depth.<ref>{{cite web|url=http://www.dnr.state.mn.us/lakefind/surveys.html#littoral|title=Fisheries lake surveys| accessdate = 2006-03-17}}</ref> This zone is home to most of the aquatic plant life (both rooted and floating) in a pond or lake because the high amount of sunlight reaching it allows for significant [[photosynthesis|photosynthetic activity]].
==Other definitions==
For the purposes of naval operations, the [[United States Navy]] divides the littoral zone in the ways shown on the diagram at the top of this article. The [[United States Army Corps of Engineers]] and [[United States Environmental Protection Agency|Environmental Protection Agency]] have their own definitions, and these have legal implications.
==See also==
{{refbegin|3}}
* [[Ballantine Scale]]
* [[Benthic zone]]
* [[Coastal fish]]
* [[Intertidal zone]]
* [[Foreshore]]
* [[Limnetic zone]]
* [[Littoral combat ship]]
* [[Littoral drift]]
* [[Littoral warfare]]
* [[Marine debris]]
* [[Neritic zone]]
* [[Profundal zone]]
* [[Shingle beach]]
{{refend}}
==Notes==
{{reflist}}
==References==
{{Refbegin}}
* Haslett, Simon K (2001) ''Coastal Systems.'' Routledge. ISBN 978-0415213028
* Mann, Kenneth Henry (2000) [http://books.google.co.nz/books?id=y4OIojDxtzsC&pg=PA179&lpg=PA179&dq=Eulittoral&source=web&ots=8EMjPNWnbb&sig=GQ2QZ-32moL6t-xYMFMlp4HVf6Y&hl=en&sa=X&oi=book_result&resnum=49&ct=result#PPA179,M1 ''Ecology of Coastal Waters''] Blackwell Publishing. ISBN 9780865425507
* Yip, Maricela and Madl, Pierre (1999) [http://biophysics.sbg.ac.at/rovigno/rovigno3.htm ''Littoral''] [[University of Salzburg]].
{{Refend}}
{{physical oceanography|expanded=other}}
{{coastal geography}}
{{DEFAULTSORT:Littoral Zone}}
[[Category:Aquatic biomes]]
[[Category:Marine biology]]
[[Category:Fisheries]]
[[Category:Aquatic ecology]]
[[ca:Zona litoral]]
[[cs:Litorál]]
[[de:Litoral]]
[[et:Litoraal]]
[[es:Litoral (geografía)]]
[[eo:Marbordo]]
[[fr:Littoral]]
[[hr:Priobalje]]
[[io:Litoro]]
[[it:Battigia]]
[[ka:ლიტორალი]]
[[kk:Литораль]]
[[lt:Litoralė]]
[[nl:Littoraal]]
[[nn:Litoral]]
[[pl:Strefa przybrzeżna]]
[[pt:Litoral]]
[[ro:Zonă litorală]]
[[ru:Литораль]]
[[simple:Littoral zone]]
[[sl:Litoral]]
[[sv:Litoral]]
[[uk:Літораль]]
[[vi:Cận duyên]]' |
