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| − | This article describes the habitat of the Sandy shores. It is one of the sub-categories within the section dealing with biodiversity of [[marine habitats and ecosystems]].
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| | + | ==Articles on sandy shore ecosystems== |
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| − | ==Introduction==
| + | * [[Sandy shore habitat]] |
| | + | * [[Latitudinal biodiversity patterns of meiofauna from sandy littoral beaches]] |
| | + | * [[Meiofauna of Sandy Beaches]] |
| | + | * [[Sandy beaches as Biocatalytical Filters]] |
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| − | Sandy shores or beaches are '''loose deposits of sand''', gravel or shells that cover the shoreline in many places. They make up two-thirds of the world’s ice-free coastlines. Beaches serve as buffer zones or shock absorbers that protect the coastline, sea cliffs or [[Sand Dunes in Europe|dunes]] from direct wave attack. It is an extremely '''dynamic''' environment where sand, water and air are always in motion. Beaches also provide important coastal recreational areas for a many people. Fine-grained sand beaches tend to be '''quite flat'''.
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| | + | ==Articles related to sandy shore dynamics== |
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| − | [[image:Sandy shore.jpg|center|thumb|300px|caption|Sandy beach in Middelkerke - Belgium <ref>http://commons.wikimedia.org/wiki/Image:2005-06-26-Middelkerke-55.jpg</ref>]] | + | * [[Swash zone dynamics]] |
| | + | * [[Coastal Hydrodynamics And Transport Processes]] |
| | + | * [[Beach Cusps]] |
| | + | * [[Shallow-water wave theory]] |
| | + | * [[Rhythmic shoreline features]] |
| | + | * [[Shoreface profile]] |
| | + | * [[Closure depth]] |
| | + | * [[Natural causes of coastal erosion]] |
| | + | * [[Human causes of coastal erosion]] |
| | + | * [[Accretion and erosion for different coastal types]] |
| | + | * [[Dealing with coastal erosion]] |
| | + | * [[Dune erosion]] |
| | + | * [[Classification of sandy coastlines]] |
| | + | * [[Characteristics of sedimentary shores]] |
| | + | * [[Gravel Beaches]] |
| | + | * [[Littoral drift and shoreline modelling]] |
| | + | * [[Data analysis techniques for the coastal zone]] |
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| − | ==Formation== | + | ==Articles on sandy shore observation== |
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| − | Sandy beaches are soft shores that are formed by '''deposition''' of '''particles''' that have been carried '''by water currents''' from other areas. The transported material is in part derived from the erosion of shores, but the major part is derived from the land and transported by rivers to the sea. The two main types of beach material are '''quartz''' (=silica) sands of terrestrial origin and '''carbonate''' sands of marine origin. The carbonate sand is weathered from mollusk shells and skeletons of other animals. Other material includes heavy minerals, basalt (=volcanic origin) and feldspar.
| + | * [[Instruments for bed level detection]] |
| | + | * [[Argus applications]] |
| | + | * [[Argus image types and conventions]] |
| | + | * [[Argus standard image processing]] |
| | + | * [[Argus video]] |
| | + | * [[Argus video monitoring system]] |
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| | + | ==See also== |
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| − | ==Characteristics==
| + | http://www.ozcoasts.gov.au/index.jsp |
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| − | The '''grain size''' of sand varies from very fine to very coarse. The particle diameter is shown in the table below. As said before, the two main types of beach material are '''quartz''' (=silica) sands of terrestrial origin and '''carbonate''' sands of marine origin. Quartz sands have a slightly lower density (<math>2.66 g.cm^-3</math>) than carbonate sands (<math>2.7 to 2.95 g.cm^-3</math>). The quartz particles also seem to be more rounded. Calcium carbonate particles sink more slowly in water due to their more irregular shapes, even if their density is higher.
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| − | {| {{prettytable}}
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| − | ! '''Generic Name'''
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| − | ! '''Particle Diameter (mm)'''
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| − | |-
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| − | | Very coarse
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| − | | 1.0 to 2.0
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| − | |-
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| − | | Coarse
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| − | | 0.50 to 2.0
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| − | |-
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| − | | Medium
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| − | | 0.25 to 0.50
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| − | |-
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| − | | Fine
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| − | | 0.125 to 0.50
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| − | |-
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| − | | Very Fine
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| − | | 0.0625 to 0.125
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| − | |-
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| − | |}
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| − | [[image:beach types.JPG|right|thumb|250px|caption|Different beach types based on morphodynamic scale <ref>http://www.csc.noaa.gov/text/glossary.html</ref>]]
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| − | '''Porosity''' is the volume of void space in the sand. It is the volume of water needed to saturate a given weight of dry sand. Most sands have a porosity of about 30 to 40 % of the total volume. The finer a sand the greater its porosity.
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| − | '''Permeability''' is the rate of flow or drainage of water through the sand. Fine sands have lower permeabilities due to their smaller pore sizes.
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| − | '''Penetrability''' is related to particle size and porosity. It can be important to the macrofauna. All species must be able to burrow into the substratum. To determine the penetrability, the proportion of clay and silt and the water content are very important.
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| − | The two basic beach types are dissipative and reflective. Together with the intermediate types, there are six major microtidal beach types.
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| − | The '''reflective''' type occurs when conditions are calm and/or the sediment is coarse. There is no [[Breaker-zone|surf zone]] and waves flow upon the beach. It reflects a major part of the incoming wave. When bigger waves cut back a beach and spread out its sediments to form a [[Breaker-zone|surf zone]], the reflective beaches create a series of '''intermediate''' types. When wave action is strong and/or sediment particle size is fine, the '''dissipative''' beach type is created. This type has a flat and maximally eroded beach. The sediments are stored in a broad [[breaker-zone|surf zone]] that may have multiple sandbanks parallel to the beach. The intermediate types are characterized by high temporal variability, sand storage both on the beach and in the [[Breaker-zone|surf zone]] and sandbanks and troughs. <ref>McLachlan A. and Brown A. 2006. The ecology of sandy shores. Academic press – Elsevier. P. 373</ref>
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| − | ==Functioning and adaptations==
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| − | The [[intertidal]] zone is covered part of the day by water and is part of the day exposed to air. High [[Tide|tides]] bring [[nutrients]] and food with it. When the [[tide]] retreats, waste products, eggs and larvae are taken. This causes changes for the organisms that live here. They have adapted to this changing environment, as seen on [[Rocky Shores|rocky shores]].
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| − | ==Biota==
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| − | The distribution and abundance of the sediment infauna is mostly controlled by complex interactions between the physicochemical and biological properties of the sediment. <ref>Knox G.A. 2001. The ecology of seashores. CRC Press. p. 557</ref>
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| − | The '''physicochemical''' properties are:
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| − | * Grain size
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| − | * Water content
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| − | * Flushing rate of water through the sediment
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| − | * Oxidation-reduction state
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| − | * Dissolved oxygen
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| − | * Temperature
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| − | * Light
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| − | * Organic content
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| − | The '''biological''' properties are:
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| − | * Food availability and feeding activity
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| − | * Reproductive effects on dispersal and settlement
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| − | * Behavior that induces movement and aggregation
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| − | * Intraspecific competition
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| − | * Interspecific competition and competitive exclusion
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| − | * Predation effects
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| − | Most invertebrate phyla are represented on sandy beaches, either as interstitial forms or as members of the [[macrofauna]] <ref name="Brown and McLachlan"/>. The [[Macrofauna|macrofaunal]] forms are by far the better known. Some of them are typical of intertidal sands and their surf zone, while others are more characteristic of sheltered sandbanks, sandy muds or estuaries and are less common on open beaches of pure sand <ref name="Brown and McLachlan"/>.
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| − | ===[[Macrofauna|Macrofauna]]===
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| − | [[Macrofauna]] of the sandy beaches are often abundant and, in some cases, attain exceptionally high densities. Their main feature is the high degree of mobility displayed by all species. These animals may vary from a few mm to 20 cm in length. The [[macrofauna]] community consists of those organisms too large to move between the sand grains. The [[macrofauna]] of sandy beaches includes most major invertebrate taxa although it has been recognised that molluscs, [[crustacea|crustaceans]] and polychaetes are the most important. There is a tendency for [[crustacea|crustaceans]] to be more abundant on tropical sandy beaches or more exposed beaches and molluscs to be more abundant on less exposed and on temperate beaches although there are many exceptions of this and polychaetes are sometimes more abundant than either of these taxa. Generally [[crustacea|crustaceans]] dominate the sands towards the upper tidal level and molluscs the lower down level <ref name="Brown and McLachlan">Brown & McLachlan 1990</ref>. Physical factors, primary wave action and particle size of the sand largely determine distribution and diversity of the invertebrate [[macrofauna]] of sandy beaches. Food input and surf-zone productivity may determinate the abundance population. Water movement is important parameter controlling [[Macrofauna|macrofaunal]] distribution on beaches.
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| − | ===[[Meiofauna]]===
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| − | In contrast to the wave-swept surface sand inhabited by most of the [[macrofauna]], the interstitial system is truly three-dimensional, often having great vertical extent in the sand. The porous system averages about 40% of the total sediment volume. Its inhabitants include small metazoans forming the [[meiofauna]], protozoans, bacteria and diatoms<ref name="Brown and McLachlan"/>. The [[meiofauna]] is defined as those metazoan animals passing undamaged though 0.5 to 1.0 mm sieves and trapped on 30 mm screens. On most beaches the interstitial fauna is rich and diverse, even exceeding the [[macrofauna]] in [[biomass]] in some cases<ref name="Brown and McLachlan"/>. The dominant taxa of sandy beach [[meiofauna]] are nematodes and harpacticoid copepod with other important groups including turbellarians, oligochaetes, gastrotrichs, ostracods and tardigdades.
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| − | ===Insects===
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| − | Terrestrial insects and vertebrates are frequently ignored in accounts of sandy beaches. These animals are usually a conspicuous component of the [[ecosystems|ecosystem]], often rivalling the aquatic [[macrofauna]] in terms of [[biomass]] and having a significant impact on the system with regard to predation and scavenging.
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| − | ==Case-study Biodiversity patterns==
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| − | A case-study about the latitudinal biodiversity patterns of meiofauna from sandy littoral beaches can be found [[Latitudinal biodiversity patterns of meiofauna from sandy littoral beaches|here]].
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| − | {{author
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| − | |AuthorID=313
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| − | |AuthorFullName=TÖPKE, Katrien
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| − | |AuthorName=Ktopke}}
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| − | {{author
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| − | |AuthorID=5254
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| − | |AuthorName= Lechu
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| − | |AuthorFullName= Kotwicki, Lech}}
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| − | [[Category:Marine habitats and ecosystems]]
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| − | [[Category:Typology of coastal and marine areas]]
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| − | [[Category:Location of coastal and marine areas]]
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| − | [[Category:Theme 7]]
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