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Coral , Algae , Fish  

 

Algae in the coral reef environment

  Claude Payri, UFP

 

 

The nature of the substratum for algae varies from shifting sand or gravel to compact basaltic or calcareous rocks.

Hard substrata type landscape

Soft substrata type landscape

 

Algae in the coral reef environment

Coral reef environments are the favoured areas for benthic life, even if the underwater vegetation is not very exuberant likely to go unnoticed by the naturalist unfamiliar with these habitat. All the biological groups have discovered a possibility of adaptation, and algae in particular. 

Competition for space with other attached organisms is one of the main factors controlling growth of the marine flora. 

The other remarkable factor in the control of growth in some plant communities is grazing by herbivores, fish and invertebrates (molluscs and echinoderms). In coral reef communities, herbivorous fish account for nearly 25% of the fauna. They exert a strong predatory pressure on the carpets of small filamentous algae, called " turfs”, but also on the young sporelings of larger macroalgae. However, the high regenerative faculty of coralline algae enables them to resist predation by herbivores.

 

labre1.jpg (19951 octets)

A herbivorous fish in a field of
 Caulerpa bikiniensis

 

Fish are selective in the species they consume (chemical defense in some species), so they control the specific diversity of the algae. More, they can favour the growth of some algae, like the Pomacentrid fish which, by their territorial behaviour, exclude predators from their area and favour the growth of filamentous algae turf several millimetres high (Brawley and Adey, 1977).

 

With high regenerative faculty, chemical defense system, cooperation with others organisms, the algae show a very good adaptation to their environment.

 

Algae production and calcification

In addition to the direct contribution of certain species to the trophic chain, benthic algae actively participate in primary production with about 5.5 Kg carbon per m2 per year. Furthermore, the exuberance of calcified forms in the coralline environment makes algae important contributors to reef calcification, to the order of 4.5 Kg calcium carbonate per m2 per year (Gattuso et al., 1998). Bioconstruction is essentially carried out by coralline red algae, while sand formation is principally attributed to the breakdown of Halimeda (green alga).

 

One of the most numerous species of red algae in the French Polynesian reefs.

Hydrolithon onkodes

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halimac.jpg (15969 octets)

Fixed on the soft sediments, its calcareous articles will enrich the sands.

Halimeda macroloba

 

 

Ecology of the algae on the reefs and in the lagoons

Distribution according to depth

Algae colonise almost any habitat as long as it is damp and lighted, however their depth distribution is limited by their photosynthetic ability and the depth of penetration of solar radiation.

In tropical regions algae Corallinaceae, have been collected at a depth of 268 meters (Bahamas), however they are most abundant and diversified within the first 30 meters of the water column.

 

Attachment to the substratum

Multicellular algae are generally attached to the sustratum and make up the benthic forms as opposed to the unicellular planktonic species. One of the few notable cases of floating macroalgae is the example of Sargassum in the Sargasso Sea and seasonal agglomerations of Boodlea, Chnoospora or Hydroclathrus in tropical lagoons. Just as remarkable is the case of unicellular algae called zooxanthellae living in symbiosis within coral polyps. 

Generally speaking, any sufficiently long-lived solid, living or inert surface can be colonised by algae. We speak of  epiphytic algae when they are attached to other algae, epizoic when they are attached to animals and endolithic when they bore and live within calcareous substrata.

The nature of the substratum matters in terms of its structure and texture, in the distribution of species. Hence we distinguish species of hard substrata that attach themselves to compact rocks, and algae from soft bottoms, or in others words, species colonising sediment accumulations. 

 

species of hard substrata, that attach themselves to compact rocks.

 

Caulerpa peltata

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caulser.jpg (20724 octets)

and algae from soft bottom, or in other words, species colonising sediment accumulations.

Caulerpa sertulariodes

Whatever the type of substratum, its degree of cohesion (stability) plays a fundamental role in the length of attachment. Thus, areas with soft bottoms subject to strong hydrodynamism never support large algal populations.  

 

The effect of hydrodynamism

The roughness of the waters, owed to the variations of the sea-level, to the tides, to the currents and to the swells, product forces such as the organisms are selected on their faculty to hold out against the wrench forces. 

The area where tides and waves meet, constitutes the upper floor of the reef system, the favoured domain for brown photosynthetic algae and calcified red algae.

The amount of exposure of habitats to hydrodynamism allows one to distinguish exposed habitats from calm ones, as well as a range of intermediate situations. 

As a general rule, strong hydrodynamism selects species with large basal holdfasts, whose thallus texture is relativeley coriaceous but flexible (Sargassum) or soft, encrusting (Lobophora variegata) or calcified (Corallinales) forms. These adaptations are often displayed in a given species by morphological variations such as dwarfism (Turbinaria, Sargassum). 

 

lobovah.jpg (25028 octets)

mastpac.jpg (29098 octets)

Lobophora variegata
encrusting form

Mastophora pacifica
lamellate form

 

Similarly, in red calcified algae, massive encrusting forms are abundant in very exposed habitats (reef crest) while lamellate forms are rather more characteristic of calm sheltered places. Additionally, branched forms exhibit a wide variety of form and size of branches according to the strength of the current (Neogolithon frutescens) and we notice a decrease in the length  of branches when there is an  increase in the force of the current (Neogoniolithon frutescens).

 

 

The algal communities on the atolls

 

They are presented in the chapter communities of the atolls 

Click on the link to open it.

 

 

References

Payri, C., N'Yeurt A.R. & Orempüller, J. - 2001 - Algae of french Polynesia -Algues de Polynésie Française. Edition Au Vent des îles - tahiti, 320pp.

Payri, C.E. & N'Yeurt, A.D.R. 1997. A revised Checklist of Polynesian benthic Marine Algae, Australian Systematic Botany, 10: 867-910.

 

 

update : 07/10/08

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