Intertidal zone

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A rock, seen at low tide, exhibiting typical intertidal zonation.
A rock, seen at low tide, exhibiting typical intertidal zonation.
Exposed microclimate on a rock located in intertidal zone during low tide.
Exposed microclimate on a rock located in intertidal zone during low tide.
Mussels in the intertidal zone in Cornwall, England.
Mussels in the intertidal zone in Cornwall, England.
Barnacles and limpets in the intertidal zone near Newquay, Cornwall.
Barnacles and limpets in the intertidal zone near Newquay, Cornwall.

The intertidal zone, also known as the littoral zone, in marine aquatic environments is the area of the foreshore and seabed that is exposed to the air at low tide and submerged at high tide, for example, the area between tide marks.

Organisms in the intertidal zone are adapted to an environment of harsh extremes. Water is available regularly with the tides but varies from fresh with rain to highly saline and dry salt with drying between tidal inundations. The action of waves can dislodge residents in the littoral zone. With the intertidal zone's high exposure to the sun the temperature range can be anything from very hot with full sun to near freezing in colder climes. Some microclimates in the littoral zone are ameliorated by local features and larger plants such as mangroves. Adaption in the littoral zone is for making use of nutrients supplied in high volume on a regular basis from the sea which is actively moved to the zone by tides. Edges of habitats, in this case land and sea, are themselves often significant ecologies, and the littoral zone is a prime example.

A typical rocky shore can be divided into a spray zone (also known as the supratidal zone), which is above the spring high-tide line and is covered by water only during storms, and an intertidal zone, which lies between the high and low tidal extremes. Along most shores, the intertidal zone can be clearly separated into the following subzones: high tide zone, middle tide zone, and low tide zone.

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The high tide zone is flooded during high tide only, and is a highly saline environment. The abundance of water is not high enough to sustain large amounts of vegetation, although some do survive. The predominant organisms in this subregion are barnacles, chitons, small gastropods, isopods, limpets, mussels, starfish, snails, whelks and some herbivores. The high tide zone can also contain rock pools inhabited by small fish and larger. Life is much more abundant here than in the spray zone.


This subregion is mostly submerged - it is only exposed at the point of low tide and for a longer period of time during extremely low tides. This area is teeming with life; the most notable difference with this subregion to the other three is that there is much more marine vegetation, especially seaweeds. There is also a great biodiversity. Organisms in this zone generally are not well adapted to periods of dryness and temperature extremes. Some of the organisms in this area are abalone, anemones, brown seaweed, chitons, crabs, green algae, hydroids, isopods, limpets, mussels, nudibranchs, sculpin, sea cucumber, sea lettuce, sea palms, sea stars, sea urchins, shrimp, snails, sponges, surf grass, tube worms, and whelks. Creatures in this area can grow to larger sizes because there is more energy in the localised ecosystem and because marine vegetation can grow to much greater sizes than in the other three intertidal subregions due to the better water coverage: the water is shallow enough to allow plenty of light to reach the vegetation to allow substantial photosynthetic activity, and the salinity is at almost normal levels. This area is also protected from large predators such as large fish because of the wave action and the water still being relatively shallow.

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