Ahermatypic, Hermatypic What does it all mean?
A Brief Introduction To coral Anatomy
by Beau Crowley
What are corals? The term coral has several different dictations, but most commonly it refers to the order Scleractinia, all of which have hard limestone skeletons. This order is divided into two main contributors: reef-building and non-reef-building. Most of these two groups are hermatypic and need to acquire sunlight to live. Other organisms do build skeletons similar to those of the same order and these are normally known as non-scleractinian corals.
Other organisms resemble corals but contain no skeleton (Veron, 1993). Most true corals build massive structures that accumulate that cementation of skeleton sand, thus revealing a multitude of coral colonies over thousands of years.
Imposing as they are, the presence of modern coral reefs is the result of a special relationship between the coral polyp and the unseen single celled algae which live symbiotically within the cells of the polyp.
These algae, which are commonly called zooxanthellae, belong to a group of unicellular brown organisms known as dinoflagellates. Most flagellates are part of the phytoplankton of shallow tropical seas where they are a food contributor for zooplankton.
A few members of this group are less benign, occasionally causing lethal red tides and shellfish poisoning. Like land plants, zooxanthellae are able to use the sunlight in photosynthesis by making their own food from CO2.
Symbiotic algae benefit hermatypic corals in two ways. Firstly, 94 to 98 percent of all the organic nutrients are produced by the zooxanthellae, and is used as the major food source by the coral polyp. Secondly, due to photosynthesis of zooxanthellae, hermaphroditic corals are able to deposit their limestone skeletons 2 to 3 times faster in light rather than the dark.
Light enhances the rate of calcification and enables reefs to grow faster than they are broken down by the natural processes of the sea and eroding organisms (Veron 1993).
Even with coral larvae containing zooxanthellae, obtains it directly from their parent polyp during their free swimming stage. The algae multiply as the coral grows and they are responsible for the brown colors in the hermatypic corals. Due to environmental stress, the algae can be expelled by the coral as we will see later in case studies.
Ahermatypic corals that do not contain zooxanthellae are not restricted to high light intensities waters and can exist at almost any depth in these corals all nutrition comes from plankton. Less than one-third of all ahermatypes found in the ocean are colonial (Veron 1993).
These observations raise several questions about evolution of corals and coral reefs. Which evolved first, corals or the algae zooxanthellae?
Were the corals that helped build Paleozoic reefs hermatypic? At this point there is no accurate way of distinguishing hermatypic from ahermatypic fossils. Many corals have evolved in deep water forms and continue to evolve independently.
These may or may not have came from shallow reefs and contained zooxanthellae and their tissues. It seems likely that the symbiotic relationship played some role in ancient reef development, but perhaps a lesser one than it does today. Like a patch work of a miniature forest, the coral reef is made of different communities, each one separate from the other. But somehow they are linked to the next community by a complex web of ecological interactions.
Each reef builds a series of narrow bands or zones that has its own environmental conditions or gradient. The most important factors of reef dynamics are light availability, wave action, salinity, and tidal range.
All of these factors work together to form a complex ecological gradient. These factors are related especially where wave action affects sediments and this affects visibility, which in turn affects water clarity and light availability. Most hermatypic corals require light for photosynthesis of the zooxanthellae that are contained within the tissues.
The light changes as water depth increases, intensity and composition are affected. The changing intensity is not visible to underwater divers, but photographers know that camera flash lights must be used for intensity and color balance. even though the water may be clear. Due to light requirements in different corals, complex communities may evolve.
The different zones will allow for different lighting conditions and water clarity. This may be due to sediment type, tidal zone, and geological contour, of a certain reef type.
The second controlling factor is wave action. Wave action reaches extremes on the reef fronts and the outer flats on a calm day a reef front a benign appearance. The small waves due to tides disturb the peace and yet during a storm the site has a very strong wave action. As a wave comes in building huge force along the fore-reef it crashes down on the outer flat. In this case few species will survive such pounding . Only a few hundred meters away on the lower reef slope there may be little or no water movement at all.
Different types of sediment exist on and around a coral reef. These include coral rubble in different sizes from sand to mud, but it all depends on the exposure to currents and wave actions. Different sizes and different organic components can reduce light penetration and can kill certain organisms as corals, either by choking the polyps or burying them, thus not allowing the zooxanthellae to photosynthesize.
In rare instances salinity of sea water will become high enough to affect coral communities One place is Shark Bay, where a large amount of water is landlocked and combines with a low title range to produce a salinity which may be high enough to kill corals. Reef flat corals are generally tolerant of short periods of low salinity, but when heavy rainfall and very low tides combine, or follow one another, communities may be damaged or destroyed.
Like all other organisms corals require food and inorganic nutrients to live. Hermatypic corals have two major food sources organic nutrients produced and excreted by the symbiotic zooxanthellae into the tissues of the host. The second source comes from their prey in the form of free floating plankton.
Corals growing in shallow clear water communities normally have small polyps. Their main diet consist of sugars that are fed through the photosynthesis. However they can supplement their diet with small zooplankton, mainly at night. Most coral reefs exist in a poor inorganic nutrient environment . Phosphates, nitrates and iron exist in at trace levels, yet these reefs have a productivity that is similar to the rain forest.
Colonies of corals and their zooxanthellae absorb dissolved nutrients from sea water and recycle nutrients from the waste of one another.
Since the reef as itself receives only low nutrient levels from the surrounding ocean it must conserve and recycle. The relationship of zooxanthellae and corals has developed an efficiency that can only be achieved through self regulating processes which, when combined, make up nutrient cycles of most reef inhabitants (Veron 1993).
(CONT)
A Brief Introduction To coral Anatomy
by Beau Crowley
What are corals? The term coral has several different dictations, but most commonly it refers to the order Scleractinia, all of which have hard limestone skeletons. This order is divided into two main contributors: reef-building and non-reef-building. Most of these two groups are hermatypic and need to acquire sunlight to live. Other organisms do build skeletons similar to those of the same order and these are normally known as non-scleractinian corals.
Other organisms resemble corals but contain no skeleton (Veron, 1993). Most true corals build massive structures that accumulate that cementation of skeleton sand, thus revealing a multitude of coral colonies over thousands of years.
Imposing as they are, the presence of modern coral reefs is the result of a special relationship between the coral polyp and the unseen single celled algae which live symbiotically within the cells of the polyp.
These algae, which are commonly called zooxanthellae, belong to a group of unicellular brown organisms known as dinoflagellates. Most flagellates are part of the phytoplankton of shallow tropical seas where they are a food contributor for zooplankton.
A few members of this group are less benign, occasionally causing lethal red tides and shellfish poisoning. Like land plants, zooxanthellae are able to use the sunlight in photosynthesis by making their own food from CO2.
Symbiotic algae benefit hermatypic corals in two ways. Firstly, 94 to 98 percent of all the organic nutrients are produced by the zooxanthellae, and is used as the major food source by the coral polyp. Secondly, due to photosynthesis of zooxanthellae, hermaphroditic corals are able to deposit their limestone skeletons 2 to 3 times faster in light rather than the dark.
Light enhances the rate of calcification and enables reefs to grow faster than they are broken down by the natural processes of the sea and eroding organisms (Veron 1993).
Even with coral larvae containing zooxanthellae, obtains it directly from their parent polyp during their free swimming stage. The algae multiply as the coral grows and they are responsible for the brown colors in the hermatypic corals. Due to environmental stress, the algae can be expelled by the coral as we will see later in case studies.
Ahermatypic corals that do not contain zooxanthellae are not restricted to high light intensities waters and can exist at almost any depth in these corals all nutrition comes from plankton. Less than one-third of all ahermatypes found in the ocean are colonial (Veron 1993).
These observations raise several questions about evolution of corals and coral reefs. Which evolved first, corals or the algae zooxanthellae?
Were the corals that helped build Paleozoic reefs hermatypic? At this point there is no accurate way of distinguishing hermatypic from ahermatypic fossils. Many corals have evolved in deep water forms and continue to evolve independently.
These may or may not have came from shallow reefs and contained zooxanthellae and their tissues. It seems likely that the symbiotic relationship played some role in ancient reef development, but perhaps a lesser one than it does today. Like a patch work of a miniature forest, the coral reef is made of different communities, each one separate from the other. But somehow they are linked to the next community by a complex web of ecological interactions.
Each reef builds a series of narrow bands or zones that has its own environmental conditions or gradient. The most important factors of reef dynamics are light availability, wave action, salinity, and tidal range.
All of these factors work together to form a complex ecological gradient. These factors are related especially where wave action affects sediments and this affects visibility, which in turn affects water clarity and light availability. Most hermatypic corals require light for photosynthesis of the zooxanthellae that are contained within the tissues.
The light changes as water depth increases, intensity and composition are affected. The changing intensity is not visible to underwater divers, but photographers know that camera flash lights must be used for intensity and color balance. even though the water may be clear. Due to light requirements in different corals, complex communities may evolve.
The different zones will allow for different lighting conditions and water clarity. This may be due to sediment type, tidal zone, and geological contour, of a certain reef type.
The second controlling factor is wave action. Wave action reaches extremes on the reef fronts and the outer flats on a calm day a reef front a benign appearance. The small waves due to tides disturb the peace and yet during a storm the site has a very strong wave action. As a wave comes in building huge force along the fore-reef it crashes down on the outer flat. In this case few species will survive such pounding . Only a few hundred meters away on the lower reef slope there may be little or no water movement at all.
Different types of sediment exist on and around a coral reef. These include coral rubble in different sizes from sand to mud, but it all depends on the exposure to currents and wave actions. Different sizes and different organic components can reduce light penetration and can kill certain organisms as corals, either by choking the polyps or burying them, thus not allowing the zooxanthellae to photosynthesize.
In rare instances salinity of sea water will become high enough to affect coral communities One place is Shark Bay, where a large amount of water is landlocked and combines with a low title range to produce a salinity which may be high enough to kill corals. Reef flat corals are generally tolerant of short periods of low salinity, but when heavy rainfall and very low tides combine, or follow one another, communities may be damaged or destroyed.
Like all other organisms corals require food and inorganic nutrients to live. Hermatypic corals have two major food sources organic nutrients produced and excreted by the symbiotic zooxanthellae into the tissues of the host. The second source comes from their prey in the form of free floating plankton.
Corals growing in shallow clear water communities normally have small polyps. Their main diet consist of sugars that are fed through the photosynthesis. However they can supplement their diet with small zooplankton, mainly at night. Most coral reefs exist in a poor inorganic nutrient environment . Phosphates, nitrates and iron exist in at trace levels, yet these reefs have a productivity that is similar to the rain forest.
Colonies of corals and their zooxanthellae absorb dissolved nutrients from sea water and recycle nutrients from the waste of one another.
Since the reef as itself receives only low nutrient levels from the surrounding ocean it must conserve and recycle. The relationship of zooxanthellae and corals has developed an efficiency that can only be achieved through self regulating processes which, when combined, make up nutrient cycles of most reef inhabitants (Veron 1993).
(CONT)
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