It is intriguing that many corals also take up urea from the water, and they can do this in even greater quantities compared to nitrate (at least in nature). This indicates these animals may have adapted to the presence of higher animals on the reef, such as fish, which collectively produce large amounts of this nitrogen-rich compound on a daily basis27.
Scientists also found that urea, similar to amino acids, is more actively taken up during the day. These molecules may be important for building the organic matrix, the 'protein-scaffold' around which calcium carbonate is deposited. It was shown that this matrix is mainly produced at night, whereas calcification mainly takes place during the day34 (see archive). The organic matrix helps the formation of aragonite crystals, increasing both the density and strength of the coral skeleton35-37.
Figure 5: Nitrogen budget for Stylophora pistillata colonies in their natural environment. It is clear that ammonia and nitrate provide the bulk of the nitrogen, and that organic nitrogen in the form of amino acids provides 21%. The balance between dissolved molecules and particles such as plankton however depends on what is available to the coral (Renaud Grover et al, Journal of Experimental biology 2008).
Aquarists often notice polyp expansion after feeding plankton or 'boosters' which contain plenty dissolved organics. This is because corals, similar to humans, are probably capable of tasting food which is present in the water. Just like the human tongue has receptors to detect many substances, so too may corals have evolved receptors which recognize amino acids.
Adding amino acids such as glycine, alanine or glutamate to the water results in reactions such as polyp extension, swelling of common tissue ( coenenchyme) and on occasion the extrusion of the gut wall (or gastrovascular cavity)23,28. This mechanism possibly serves to detect zooplankton, which allows for more efficient capture of prey. Corals may also recognize neighbouring colonies, which they sometimes attack by literally throwing their stomachs onto them, after which the target is slowly digested.
"Aquarists often notice polyp expansion after feeding plankton or 'boosters' which contain plenty dissolved organics. This is because corals, just like humans, are capable of tasting food which is present in the water."
- dissolved inorganic matter (DIM)
The uptake of inorganic matter by corals encompasses macro-elements such as calcium, magnesium, bicarbonates and potassium, gases such as oxygen and carbon dioxide, and trace elements. Macro-elements largely play a role in calcification, and are added to the aquarium by means of calcium hydroxide (Ca(OH)2, also called kalkwasser), the Balling-method or a calcium reactor.
Trace elements are available in seawater only in minute concentrations, hence their name. Examples are iodine (50 ppb), nitrogen (300 ppb, nitrate is a part of this), phosphorus (phosphate is a part of this), halogens such as fluorine (1 ppm) and metals such as iron (10 ppb), zinc (10 ppb) and aluminum (10 ppb). Table 1 gives an overview of the most common elements present in marine water.
"Copper, chromium and zinc are highly toxic to life, and this holds especially true for invertebrates. These animals, mainly corals and anemones, have not evolved efficient ways of dealing with these molecules."
Manufacturers of aquarium supplements have tapped into this knowledge over the years, and this has led to a variety of available products. Adding metals, for example, supposedly augments the blue and green colouration of stony corals. Although evidence is limited regarding this (Heliopora coerulea is an exception to this rule), metals do have key functions for all life on earth. Many enzymes, proteins which catalyze chemical reactions allowing life to persist, have metal cores. Without these, they simply cannot function42-44. A nice example is the enzyme carbonic anhydrase, which catalyzes the conversion of CO2 to bicarbonate ions. This process is essential for building the coral skeleton (see archive). This enzyme contains a core of zinc; without sufficient ingestion of this metal, stony corals would not be able to photosynthesize and grow properly76.
Table 1: An overview of the main elements present in natural seawater. Concentrations are represented in ppt (parts-per-thousand, g/l), ppm (parts-per-million, mg/l) and ppb (parts-per-billion, μg/l). Sulphate and bicarbonate are not elements, but rather molecules which consist of different elements (or atoms). As they play important roles in oceanic biological processes they have been included in the table (source:
www.invista.com).
element
ppt
element
ppm
element
ppb
oxygen (O)
857.8
bromine (Br)
65
nitrogen (N)
300
hydrogen (H)
107.2
strontium (Sr)
8
lithium (Li)
170
chlorine (Cl)
18.98
boron (B)
4
phosphorus (P)
70
sodium (Na)
10.556
silicon (Si)
3
iodine (I)
50
sulphate (SO42-)
2.649
fluorine (F)
1
zinc (Zi)
10
magnesium (Mg)
1.272
iron (Fe)
10
calcium (Ca)
0.4
aluminum (Al)
10
potassium (K)
0.38
manganese (Mn)
2
bicarbonate (HCO3-)
0.14
lead (Pb)
0.04
mercury (Hg)
0.03
gold (Au)
0.000004
Table 1 shows that metals truly are trace elements, which is why supplementing them to the aquarium should be done with care. Metals such as copper, chromium and zinc are highly toxic to life, and this holds especially true for invertebrates. These animals, mainly corals and anemones, have not evolved efficient ways of dealing with these molecules. Higher animals have evolved a liver and kidneys, which together quickly dispose of toxins through the urine and feces. Corals and their relatives are highly dependent on external water concentrations, and can only pump in or out molecules to some extent.
It is also clear that metals can be bound by organic molecules such as metallothionins; these proteins actively bind to metals rendering them harmless. This allows transport of these molecules through the bodies of countless organisms. This process is called chelation, and the involved organic molecule is called the chelator. It takes place in bacteria, algae and numerous animal species. Bacteria and algae also secrete these molecules into the water, thereby neutralizing metals for safe uptake. It has also been shown by some aquarists that corals do not incorporate heavy metals into their skeletons to such an extent as would be expected based on water concentrations46. Even at high metal concentrations, skeletal contents of aquarium corals often show a deficit in metal composition compared to wild specimens. This indicates many metals in the aquarium are not biologically available. Either way, supplementing heavy metals should be done with care.
"Phosphates possibly inhibit the buildup of the coral skeleton, by binding to the growing crystal lattice. Coralline algae, which also calcify, show a decrease in growth at higher phosphate levels."
Phosphorus also is a widely discussed element, often causing problems in aquaria. As orthophosphate, PO43-, it regularly causes overgrowth of algae, cyanobacteria and coral mortality. Most aquarists are very much aware phosphates can be dangerous to aquarium life, and manufacturers have adapted to this by producing many phosphate-lowering products. Iron- and aluminum-based substrates have been known to bind phosphates for years, and this principle is perfectly applicable to aquaria.
There still is some controversy about the direct harmful effects of phosphate; it seems that predominantly stony corals are affected by this. Soft corals and gorgonians have been reported to grow at concentrations as high as 5 mg/l!59 Phosphates possibly inhibit the buildup of the coral skeleton, by binding to the growing crystal lattice. Coralline algae, which also calcify, show a decrease in growth at higher phosphate levels. Phosphates also cause negative indirect effects on marine animals by stimulating algal and bacterial growth62,63.
- particulate organic matter (POM)
This group of particles usually describes detritus; the small remnants of feces and decayed organisms. In the aquarium, food which is not consumed and removed also becomes detritus. Detritus eventually precipitates on the ocean floor or aquarium bottom as sediment. This layer of organic material is partially degraded by bacteria, and converted into inorganic molecules such as nitrate and phosphate. This process is called mineralization.
The sediment which is present on coral reefs contains bacteria, protozoa and their excrements, microscopic invertebrates, microalgae and organics29. These sedimentary sources can all serve as coral nutrients, especially for colonies which grow in turbid waters15,30. Experiments during which sedimentary carbon was radioactively labeled showed that corals such as Fungia horrida and Acropora millepora readily took up sediment31,32. The more sediment present, the more uptake is measured; 50-80% of this material is converted into biomass by several species. This has also been found for the Caribbean species Montastrea franksi, Diploria strigosa and Madracis mirabilis; detritus is taken up by the polyps, and the available nitrogen is converted into biomass.
It must be noted however that too much sediment which precipitates on the corals can be disastrous; reefs have disappeared in many bays inhabited by humans because of this. This is caused by the upwelling of soil sediments by tourists or boats, or by the presence of fish farms. This phenomenon can be seen in the Gulf of Aqaba (Red Sea), where the reef stops as soon as densely populated areas are reached. High sedimentation literally suffocates the reef by blocking light, food uptake and gas exchange.
Figure 6: A Dutch aquarium which is enriched in detritus and plankton due to heavy feeding. Because of this, this aquarium also harbours increased populations of benthic crustaceans such as amphipods, which inhabit the live rock. By feeding phyto- and zooplankton, or an artificial feed such as Reef Pearls, a somewhat natural nutrient cycle can be created. The resulting amphipods and other small invertebrates are an important food source for e.g. dragonets (Synchiropus sp.). The available particles are essential to the animals present, which include Menella gorgonians, Dendronephthya sp., Scleronephthya sp., stony corals such as Tubastrea coccinea and Rhizotrochus typus, sponges and tunicates. The 'dirty' aquarium, which allows more animals to thrive, is becoming a new hype in the marine hobby. The ultimate trick remains the availability of particles whilst ensuring high water quality (low ammonia, nitrate and phosphate levels, photographs: Pieter van Suylekom).
"The sediment which is present on coral reefs contains bacteria, protozoa and their excrements, microscopic invertebrates, microalgae and organics. These sedimentary sources can all serve as coral nutrients, especially for colonies which grow in turbid waters."
- plankton
This group is sometimes regarded as the living component of POM. The term plankton is a common name for an astoundingly large group of organisms which can be categorized in different ways. Figure 7 shows a commonly accepted division into pico-, nano-, micro- and mesoplankton. These groups consist of (cyano)bacteria and protozoa (picoplankton), algae and protozoa (nanoplankton), microscopic crustaceans such as rotifers and large protozoa (microplankton) and countless other species of crustaceans (mesoplankton). Fish and invertebrate larvae can further be categorized into micro- and mesoplankton, depending on the species.
Figure 7: Plankton size classes: picoplankton, nanoplankton, microplankton and mesozooplankton included in the diet of scleractinian corals. (A, B) Scanning electron micrographs of (A) Prochloroccocus sp. (0.6 μm) and (B) Synechococcus sp. (1 μm). (C) Epifluorescence microscope image showing one nanoflagellate cell indicated by a yellow arrow. Image of (D) ciliates (mean total length is 100 – 200 μm) taken under a phase contrast microscope and (E) crab zoea (mean total length is 1000 μm) (Houlbrèque & Ferrier-Pagès, Biological Reviews, 2009).
Plankton was not considered as an important coral food source for many years; it was believed concentrations on the reef were too low to have any significant effect. In the meantime, more accurate estimations have been made, based on improved measuring techniques39. These values are particularly high during summers, which is probably due to the abundance of phytoplankton. This leads to increased concentrations of zooplankton, as they feed on the extra available phytoplankton.
Figure 8: Astroides calycularis, a Mediterranean azooxanthellate coral species. For corals within this group, catching plankton is a crucial means of survival (photograph: Jean-Louis Teyssié, IAEA Monaco).
The amount of available plankton not only fluctuates during the year, but also during the day. Zooplankton consists of actively swimming animals, which constantly migrate between the reef and the water column. During sunset, the free zooplankton concentration rises quickly, as these animals migrate to the water column. This causes a rise in copepod (500-700 μm) concentration which is five times higher compared to daytime levels!36-38
For other small invertebrates, this nocturnal concentration quadruples. Many larvae of animals such as tunicates and polychaetes larger than 700 microns also appear. When the aquarium is viewed at night by using a flashlight, this phenomenon can also be seen. Unfortunately, this nocturnal festivity is somewhat ruined by the presence of a protein skimmer, which cannot tell the difference between what is useful and what is not.
The nightly migration of plankton also explains why most stony corals mainly expand their polyps at night, as more prey can be caught during this time. This strategy also protects the polyps against predation from fish and other animals during the day. Nowadays, many aquarists have found that corals are able to adapt to a change in food availability; a nice example is Tubastrea coccinea, which learns to expand its tentacles during the day and even seems to anticipate feedings.
"Plankton was not considered as an important coral food source for many years; it was believed concentrations on the reef were too low to have any significant effect. In the meantime, more accurate estimations have been made, based on improved measuring techniques".
In the Gulf of Aqaba, the tentacles of massive coral species such as Favites sp., Favia favus and Platygyra daedalea expand 15-45 minutes after sunset. After 70 minutes, full expansion is reached36. Many corals also expand during the day, such as most species of Porites39 and numerous soft corals.
Figure 9: On the reef, such as in the Gulf of Aqaba, Red Sea, a high concentration of phytoplankton is present. This can be clearly seen by the green haze in the water (photograph: Tim Wijgerde).
The uptake of particles by corals depends on many factors, such as prey type and concentration, irradiance, colony and polyp morphology, and water flow velocity. Especially this last aspect has become a popular point of discussion amongst aquarists, as the husbandry of azooxanthellate corals is becoming increasingly popular. Research indicates that many of these corals are quite limited in their capacity to catch particles various water flow speeds. A good example are the colourful Dendronephthya's, which often do not last long in aquaria. They most efficiently catch phytoplankton at flow speeds between 12,5 and 17,5 cm/s. This has been demonstrated by determining the amount of accumulated chlorophyll inside of the polyps at various flow speeds. This value is a measure for the amount of ingested phytoplankton, as algae are rich in this protein. These results also correlated well with the increase in colony polyp number; this value was about 7% per day! This means these corals can grow quite fast if supplied with ample nutrition, which forms a striking contrast with the meager results obtained so far in aquaria.
"The nightly migration of zooplankton explains why most stony corals expand their polyps at night, as more prey can be caught during this time."
Next to azooxanthellate soft corals, some gorgonians are also quite picky about water current; in 1993, Taiwanese biologists found that the gorgonians Subergorgia suberosa, Melithaea ochracea and Acanthogorgia vegae displayed large differences in capture rate at different flow speeds51. Figure 10 shows that mainly Subergorgia suberosa has adapted to a very constant water flow. This is indicative for the environment which this species inhabits. The scientists hypothesized this result was due to its polyp morphology; because of their length, they were subject to increased flow resistance which caused them to deform quickly at higher flow speeds. This made it difficult for the polyps to catch particles. Melithaea ochracea has much shorter polyps which makes this species much more flexible. The biologists also think a balance exists between the amount of expended energy and that which is received from ingested prey. This is likely another factor which determines the maximum speeds at which plankton can be caught.
Interestingly, soft corals from the genus Dendronephthya have evolved large spicules, which are found in the body column and around polyps. These seem to function in holding the body column and polyps erect in strong water currents, allowing the corals to strain phytoplankton effectively from the passing waters. Their polyps also increase in size as water velocity increases7. Finally, polyp reaction time may also be limiting capture rates at higher flow speeds.