An Introduction To Tropical Environments In The Ocean

The structure of corals and their association withcaused by degradation of the ozone layer. These
symbiotic zooxanthelle.are the main threats faced by corals and often
Corals belong to the phylum Cnidaria and the classthey may operate together.
Anthozoa. The main points to include in aHow coral atolls form and discuss zonation in the
discussion about the structure of corals are asreef.
follows:i) Corals are polypoid i.e. have the structureThe best explanation of coral atolls formation
of a polyp with a gastrovascular cavity andcame from Darwin in 1842 and is still broadly
tentacles.ii) Corals have external skeletons ofaccepted today. Here the coral grows at the
calcium carbonate secreted by the coral polyp.iii)sides of an emerging volcano or when sea levels
Coral polyps have a basal plate and a connectionare lowered around an existing land mass. The
sheet of calcium.iv) Some species have stingingcorals continue to grow around the land as it sinks
nematocysts.v) Corals can be divided into twoor sea levels rise, growing upward to remain in
main groups Scleractinian (stony) and Octocoralsthe light for zooxanthelle to photosynthesize.
(soft corals) Let us briefly take each group in turnEventually a central lagoon may form surrounded
to discuss more structural details of corals. Stonyby atolls.
corals are usually higher in the reef and may beAs far as zonation in the reef is concerned
low growing in colonies and others are taller orgenerally the main zones are:
branching such as the staghorn coral. Stony coralsBack Reef. This is close to the shore on the
may be in the following shapes: plate, massive,sheltered side of the reef and contains perhaps a
foliate, encrusting, columnar or branching.  Soft few rocky corals, possibly mangroves at the
corals are more common at depth and include theedges, sea grasses and a narrow lagoon. This is a
sea pen, sea fan and sea whip. They can growshallow and sheltered area from wave action but
over 2 meters tall. Most reef building corals havewater circulation may be limited so coral growth
a symbiotic relationship with dinoflagellates knownmay be limited as a consequence.
as zooxanthelle living inside the polyps.Reef Crest. This is lies on the outer side of the
Zooxanthelle exchange the products ofreef with its base marked by the line of breaking
photosynthesis for the products of metabolism.waves. Encrusting coral predominate here where
Basically a coral may get 50% of its food fromthere is some wave action and some exposure
the zooxanthelle but in return the zooxanthelleto air. Also coral formation may be restricted by
receive nitrogenous waste and protection.sediment from the back reef.
Where are corals found in the world and what areWave Break Zone. Here, as the name implies.
their limiting growth factors ? Discuss the threatsthere is much wave action so corals have to be
that corals face.hardy to resist this e.g. Acropora palmata. This
Corals require a narrow temperature range inzone lies to the seaward side of the reef crest.
order to thrive so most corals grow between theThe Seaward slope. extends from the low tide
20 degree Celsius isotherms. In the broadestmark to deep water. The upper 25 meters are
sense corals are found in a broad band throughoutdominated by large corals. At 30 to 40 meters
the tropics with extensions where there aredown the Gorgonian soft corals e.g. sea fan
warm water currents e.g. west and east coastspredominate.  
of Australia. Again in a broad sense coral reefsAll zones are modified by sea depth, wave action
are found in three main areas e.g. Caribbean,and exposure.
including Bahamas and Florida Keys, Red Sea andVarious species associated with coral reefs.
Indian Ocean Islands and the Indo West Pacific.There are literally thousands of species associated
However, there are many variants in this patternwith coral reefs. The numbers alone can illustrate
...for example on the west coast of Africa thethe importance of coral reefs. Starting with the
cold Benguela Current prevents much coralcorals themselves there are over 1,000 species
formation.of hermatypic or reef forming corals with a
There are six main limiting growth factors 1)centre of diversity in the Indo West Pacific. There
Temperature as discussed above. Most coralare over 500 species of reef fish in the Bahamas,
prefer temperatures of 23 -25 degrees Celsius.1,500 in the Great Barrier Reef and 4,000 in the
Cold currents deter coral growth. 2) Depth. CoralsPhilippines.Even vegetation is influenced by the
do not really grow below 50 to 100 meters belowpresence of reefs with over 35 species of
the surface and this is mainly linked to the nextmangrove alone in the Indo West Pacific. The
point  3) Light is needed for zooxanthellenumbers of species vary according to location
production. These are the limiting factor inranging from perhaps the greatest centre of
distribution of corals in warm shallow water. 4)diveristy focused on the Indo West Pacific to the
Salinity is another factor limiting coral growth.Atlantic with fewest species.
Where there is fresh water run-off for exampleVarious species associated with coral reefs include
they can not thrive. e.g. mouth of the Amazon 5)representatives from all phyla and classes. Here is
Sedimentation also influences coral growth asjust a tiny cross section: Among the
sediments can clog feeding structures and limitinvertebrates we have     
sunlight.Porifera e.g. spongesEchinoderms e.g. starfish and
Finally emergence in the air repeatedly will kill coralurchinsMolluscs e.g. limpets, snails, clamsArthropods
so where there are changes to sea levels ande.g. crabs, lobsters and shrimp
corals become exposed they will be limited. Vertebrates are represented by many species of
The above are some of the threats faced byfish (some estimates claim up to 25% of fish
corals but in addition if we consider for a momentspecies) and dedicated reef fish like cardinal fish,
there are additional threats like global warmingbarracuda, snappers, parrotfish, groupers, whitetip
effecting sea levels, pollution from man's activities,reef sharks and Caribbean reef sharks. Reptiles
increased run off or toxic run offs, marinesuch as Hawksbill turtles also visit the reefs. The
development (dredging, mining ) disturbing coralsmassive diversity of habitat and nutrition lead to
and excessive nutrients from sewage. In somethis proliferation of species associated with coral
cases one species destroys greater areas of reefreefs from the reef crest species to bottom
than usual e.g. crown of thorns starfish, box fishfeeders from day time feeders to nocturnal
and file fish. Corals also can be aggressive withfeeders, from simple life forms to incredibly
other species of corals e.g. elkhorn coral in thecomplex and specialized. As stated before there is
Atlantic. Extreme weather is also a threat such asenormous variation in the species associated with
El Nino, but storms also open up new areas forthe coral reefs, both within the reef zones
corals. Bleaching events where zooxanthelle leavethemselves and for various reef locations
the coral due to high levels of UV radiation can bethroughout the world.