Allmost
New member
Some readings, from what I think are reliable sources. should clear alot of things up and answer some questions.
Nutrient Deficiency and Coral Bleaching
A Coral-List Server Discussion Thread
2001
http://www.coral.noaa.gov/lists/nutr...ng_thread.html
Some extracts ...
Quote by Eric Borneman
Corals are also mixotrophic (polytrophic) and do not depend on single heterotrophic sources. They can absorb significant amounts of DOM ("liquid nutrients" as you put it). Further, many feed on detritus (coral mucus, algal debris, bacteria, agglomerations of other microorganism, etc.) This is a rich food source well documented in the literature. Some corals may even obtain their largest percentage of energy obtained by feeding from this source, including the soft corals that also bleach.
Quote by Eric Borneman
... the energy obtained by light and zooxanthellae is carbon rich, mostly lost as mucus, whereas heterotrophic acquisition tends to be more weighted toward N and contributes towards growth and reproduction.
"Fish feces have been observed to be fed upon by corals (McCloskey and
Chesher, 1971) and Tovertson (1982) deduced that some fecal material from fishes may be eaten and recycled through five fishes before it reaches the seafloor to be consumed by corals or other invertebrates."
Life and Death of Coral Reefs. Birkeland (ed), 1997
In the oligotrophic waters that are normally found on coral reefs, the absolute level of dissolved nutrients found there only represents the limit of the efficiency of the organisms in removing them from the water. The nutrient recycling patterns on the reefs (and elsewhere in aquatic systems, although to varying degrees) conserve the nutrients in solid form and many circular routes can be completed without the individual nutrients passing through the "dissolved" stage. --- Remember when I said the tested nutrients, are just showing how well the bacteria are working ?
From : Dynamics of Microbial Communities on Marine Snow Aggregates: Colonization, Growth, Detachment, and Grazing Mortality of Attached Bacteria
Marine snow aggregates harbor high densities of bacteria, whose activities modify and degrade the marine snow. The buildup of bacterial biomass on marine snow also provides a food source for bacterivores, and dissolved organic matter liberated from snow particles due to the activity of attached bacteria may become important substrates even for free-living bacteria. Thus, marine snow aggregates are not only vehicles for sinking fluxes but also unique microcosms in the water column, within which material and energy flows are regulated by complex biological and physical processes.
From : Evidence of enhanced microbial activity in the interstitial space of branched corals: possible implications for coral metabolism
"Abstract
Water samples from the interstitial space of 4 Indo-Pacific coral species (Acropora sp., Echinopora horrida, Psammocora digita and Pavona clavus) and a Mediterranean coral (Cladocora cespitosa) were analysed for NO3, NO2, NH4, molybdate reactive phosphorus, bacterial and flagellate biomass and dissolved organic matter (DOM) and compared with ambient water concentrations. Higher values of NO3, NO2, bacterial and flagellate biomass were observed within the interstitial space of the corals. The lower DOM pool in the interstitium in combination with the high bacterial biomass suggests high bacterial activity and efficient substrate utilization, necessary to compensate for nanoflagellate predation. Since corals may be able to feed on bacteria, the high microbial biomass (bacterial and flagellate) may be utilized either directly as an additional heterotrophic food source, or indirectly in that microbes may act as attractants for microbe-feeding zooplankters, which in turn serve as food for the corals. The combined effect of reduced flow velocities between the coral branches and its associated fauna are probably the main factors in creating a specific environment more or less independent of the nutritive stage of the surrounding water."
From :
The prokaryotic diversity within a single coral colony is clearly much higher than that of the zooxanthellae (2 to 3 zooxanthellae species vs at least 30 bacterial ribotypes). Unlike the zooxanthellae, however, we do not have a clear picture of the ecological roles of these bacterial associates. The taxa that occurred in multiple clones and particularly multiple samples offer the best potential for beginning to elucidate roles. A phylogenetic analysis of these bacteria (Fig. 4) suggests many possibilities. For example, many of the coral-associated bacterial ribotypes are most closely related to known nitrogen fixers and antibiotic producers. Interestingly, 9 out of the 93 ribotypes that appear more than once are most closely related to proposed endosymbionts from both terrestrial and marine organisms.
In pelagic, oligotrophic waters, microbes sequester essential nutrients within the marine microbial loop (Azam et al. 1983). By virtue of their high affinity transport systems and their large surface area to volume ratios, prokaryotes are much more efficient at scavenging nutrients at low concentrations than are eukaryotic cells (Geesey & Morita 1979, Geesey 1982, Nissen et al. 1984, Suttle et al. 1990). Therefore, in nutrient-poor waters the prokaryotes will assimilate most of the limiting nutrients and limit primary production (Thingstad et al. 1998, Behrenfeld & Kolber 1999, Cavender-Bares et al. 2001). Nutrient concentrations on coral reefs are low (Muscatine 1980, Rahav et al. 1989, Szmant et al. 1990, Gast etal. 1998, 1999, Gili & Coma 1998), and therefore prokaryotes are probably assimilating most of the limiting nutrients. Indirect evidence for nutrient limitations on coral reefs comes from the observation that there is a low conversion rate of particulate and dissolved organic carbon (Ducklow 1990). Thus, corals may acquire necessary nutrients by harvesting microbes from the water column through mucus netting and indirectly via capture of Protozoa that graze on bacteria (DiSalvo 1971, Sorokin 1973, Bak et al. 1998, Ferrier-Pages et al. 1998). In addition, corals may encourage the growth of microbes by secreting fixed carbon in the form of mucus and then feed upon them. Additionally, fixed nitrogen may be obtained from coral-associated microbes that are fed, protected and provided with an anaerobic environment in the coral colony (Williams et al. 1987, Shashar et al. 1994). Finally, specialized microbiota may be important for protecting the coral animal from pathogens by occupying entry niches and/or through the production of secondary metabolites (i.e. antibiotics). These possible roles are summarized in Fig. 5."
so Bacteria assimilating P and Fe to give to corals ...
Corals delivering amino acids to zooxanthellae ....
Coral. Volume 1, Number 3.
Nutrients in the Reef Aquarium - Part III. Feeding Zooxanthellate Corals.
Jorg Kokott, June/July 2004.
From it : "Another important consideration is the possible importance of bacteria in the heterotrophic feeding of corals. A study conducted in the early 1970s revealed that SPS corals were able to process more phosphorous from bacterioplankton than from inorganic phosphate that was present in the water at an equal concentration (Sorokin 1973). In the mid-1980s there was a report published that confirmed the hypothesis that various sea anemones would grow bacteria within their gastric chambers and digest them once their population reached a certain concentration (Herndl and Velimirov 1985). A year later, another publication stated that bacteria would proliferate many times faster in the mucus layer covering the surface of a coral than in the surrounding water (Paul et al. 1986). ... Because they are relatively "sticky," bacteria, microalgae and fine sediments are caught in the gelatinous matrix, and bacteria find these conditions favorable for growth. ... .
Whatever the mechanisms by which a coral acquires food, it is certain that the diets of corals include more than just the products of their zooxanthellae. They probably include the bacteria associated with corals, as well. The synthesis of a multitude of bacteria may provide the coral with some important organic nutrients, such as vitamins, rare amino acids, or fatty acids. The coral may also benefit from the production of natural antibiotics by the bacteria, which make the coral resistant to various pathogens.
... feeding phytoplankton and bacteria is particularly helpful when it comes to SPS corals, and the supplementation of sources of carbon in the form of ethanol or acetate favor the proliferation of heterotrophic bacteria. These may eleiminate the existing deficiency of nutrients for the corals. ... . The reefkeeper needs to experiment a bit to determine which feeding regime improves or worsens the situation, and how much of which type of food is best suite for the needs of the animals he or she is keeping."
Do we trust Borenman ? he answers this thread like this :
From :
Reefkeeping Online Magazine (July 2002)
Coralmania with Eric Borneman
Reef Food
Borneman 2002
The word "nutrient" is often misunderstood. The terms "high nutrient" and "low nutrient" can be taken in many contexts. In general, nutrients are those organic and inorganic compounds necessary to sustain life. While this comprises a very large group of potential compounds, nutrients are often simplified in terms of those elements that are major "building blocks" for fats, amino acids, and carbohydrates. Furthermore, they are frequently those elements which tend to limit further growth by their availability and ability to be procured. In general, carbon, nitrogen and phosphorus are often used to describe the "nutrient" condition of reef organisms (and others, as well). Plants and animals with photosynthetic symbionts tend to be nitrogen and/or phosphorous limited under normal conditions, since photosynthesis usually provides non-limiting carbon source material. Coral reef waters are typically "nutrient poor" as they contain very low levels of nitrogen and phosphorus (they are both precious commodities and any excess is usually taken up quickly). In nearshore areas where there is significant organic loading from land runoff, waters tend to be rather nutrient rich. Both types of environments sustain their own flora and fauna with varying amounts of habitat overlap in terms of the organisms that can exploit the continuum of nutrient conditions. The nutrients available in water to coral reefs can be dissolved in the water, in the form of particulate material, or as living biomass.
...
Coral reef food sources, then, are largely produced by the ocean. Bacteria, detritus, phytoplankton, zooplankton, small benthic fauna, mucus, and dissolved organic and inorganic material of various types and sizes are what comprise the majority of food on a coral reef.
Nutrient Deficiency and Coral Bleaching
A Coral-List Server Discussion Thread
2001
http://www.coral.noaa.gov/lists/nutr...ng_thread.html
Some extracts ...
Quote by Eric Borneman
Corals are also mixotrophic (polytrophic) and do not depend on single heterotrophic sources. They can absorb significant amounts of DOM ("liquid nutrients" as you put it). Further, many feed on detritus (coral mucus, algal debris, bacteria, agglomerations of other microorganism, etc.) This is a rich food source well documented in the literature. Some corals may even obtain their largest percentage of energy obtained by feeding from this source, including the soft corals that also bleach.
Quote by Eric Borneman
... the energy obtained by light and zooxanthellae is carbon rich, mostly lost as mucus, whereas heterotrophic acquisition tends to be more weighted toward N and contributes towards growth and reproduction.
"Fish feces have been observed to be fed upon by corals (McCloskey and
Chesher, 1971) and Tovertson (1982) deduced that some fecal material from fishes may be eaten and recycled through five fishes before it reaches the seafloor to be consumed by corals or other invertebrates."
Life and Death of Coral Reefs. Birkeland (ed), 1997
In the oligotrophic waters that are normally found on coral reefs, the absolute level of dissolved nutrients found there only represents the limit of the efficiency of the organisms in removing them from the water. The nutrient recycling patterns on the reefs (and elsewhere in aquatic systems, although to varying degrees) conserve the nutrients in solid form and many circular routes can be completed without the individual nutrients passing through the "dissolved" stage. --- Remember when I said the tested nutrients, are just showing how well the bacteria are working ?
From : Dynamics of Microbial Communities on Marine Snow Aggregates: Colonization, Growth, Detachment, and Grazing Mortality of Attached Bacteria
Marine snow aggregates harbor high densities of bacteria, whose activities modify and degrade the marine snow. The buildup of bacterial biomass on marine snow also provides a food source for bacterivores, and dissolved organic matter liberated from snow particles due to the activity of attached bacteria may become important substrates even for free-living bacteria. Thus, marine snow aggregates are not only vehicles for sinking fluxes but also unique microcosms in the water column, within which material and energy flows are regulated by complex biological and physical processes.
From : Evidence of enhanced microbial activity in the interstitial space of branched corals: possible implications for coral metabolism
"Abstract
Water samples from the interstitial space of 4 Indo-Pacific coral species (Acropora sp., Echinopora horrida, Psammocora digita and Pavona clavus) and a Mediterranean coral (Cladocora cespitosa) were analysed for NO3, NO2, NH4, molybdate reactive phosphorus, bacterial and flagellate biomass and dissolved organic matter (DOM) and compared with ambient water concentrations. Higher values of NO3, NO2, bacterial and flagellate biomass were observed within the interstitial space of the corals. The lower DOM pool in the interstitium in combination with the high bacterial biomass suggests high bacterial activity and efficient substrate utilization, necessary to compensate for nanoflagellate predation. Since corals may be able to feed on bacteria, the high microbial biomass (bacterial and flagellate) may be utilized either directly as an additional heterotrophic food source, or indirectly in that microbes may act as attractants for microbe-feeding zooplankters, which in turn serve as food for the corals. The combined effect of reduced flow velocities between the coral branches and its associated fauna are probably the main factors in creating a specific environment more or less independent of the nutritive stage of the surrounding water."
From :
The prokaryotic diversity within a single coral colony is clearly much higher than that of the zooxanthellae (2 to 3 zooxanthellae species vs at least 30 bacterial ribotypes). Unlike the zooxanthellae, however, we do not have a clear picture of the ecological roles of these bacterial associates. The taxa that occurred in multiple clones and particularly multiple samples offer the best potential for beginning to elucidate roles. A phylogenetic analysis of these bacteria (Fig. 4) suggests many possibilities. For example, many of the coral-associated bacterial ribotypes are most closely related to known nitrogen fixers and antibiotic producers. Interestingly, 9 out of the 93 ribotypes that appear more than once are most closely related to proposed endosymbionts from both terrestrial and marine organisms.
In pelagic, oligotrophic waters, microbes sequester essential nutrients within the marine microbial loop (Azam et al. 1983). By virtue of their high affinity transport systems and their large surface area to volume ratios, prokaryotes are much more efficient at scavenging nutrients at low concentrations than are eukaryotic cells (Geesey & Morita 1979, Geesey 1982, Nissen et al. 1984, Suttle et al. 1990). Therefore, in nutrient-poor waters the prokaryotes will assimilate most of the limiting nutrients and limit primary production (Thingstad et al. 1998, Behrenfeld & Kolber 1999, Cavender-Bares et al. 2001). Nutrient concentrations on coral reefs are low (Muscatine 1980, Rahav et al. 1989, Szmant et al. 1990, Gast etal. 1998, 1999, Gili & Coma 1998), and therefore prokaryotes are probably assimilating most of the limiting nutrients. Indirect evidence for nutrient limitations on coral reefs comes from the observation that there is a low conversion rate of particulate and dissolved organic carbon (Ducklow 1990). Thus, corals may acquire necessary nutrients by harvesting microbes from the water column through mucus netting and indirectly via capture of Protozoa that graze on bacteria (DiSalvo 1971, Sorokin 1973, Bak et al. 1998, Ferrier-Pages et al. 1998). In addition, corals may encourage the growth of microbes by secreting fixed carbon in the form of mucus and then feed upon them. Additionally, fixed nitrogen may be obtained from coral-associated microbes that are fed, protected and provided with an anaerobic environment in the coral colony (Williams et al. 1987, Shashar et al. 1994). Finally, specialized microbiota may be important for protecting the coral animal from pathogens by occupying entry niches and/or through the production of secondary metabolites (i.e. antibiotics). These possible roles are summarized in Fig. 5."
so Bacteria assimilating P and Fe to give to corals ...
Corals delivering amino acids to zooxanthellae ....
Coral. Volume 1, Number 3.
Nutrients in the Reef Aquarium - Part III. Feeding Zooxanthellate Corals.
Jorg Kokott, June/July 2004.
From it : "Another important consideration is the possible importance of bacteria in the heterotrophic feeding of corals. A study conducted in the early 1970s revealed that SPS corals were able to process more phosphorous from bacterioplankton than from inorganic phosphate that was present in the water at an equal concentration (Sorokin 1973). In the mid-1980s there was a report published that confirmed the hypothesis that various sea anemones would grow bacteria within their gastric chambers and digest them once their population reached a certain concentration (Herndl and Velimirov 1985). A year later, another publication stated that bacteria would proliferate many times faster in the mucus layer covering the surface of a coral than in the surrounding water (Paul et al. 1986). ... Because they are relatively "sticky," bacteria, microalgae and fine sediments are caught in the gelatinous matrix, and bacteria find these conditions favorable for growth. ... .
Whatever the mechanisms by which a coral acquires food, it is certain that the diets of corals include more than just the products of their zooxanthellae. They probably include the bacteria associated with corals, as well. The synthesis of a multitude of bacteria may provide the coral with some important organic nutrients, such as vitamins, rare amino acids, or fatty acids. The coral may also benefit from the production of natural antibiotics by the bacteria, which make the coral resistant to various pathogens.
... feeding phytoplankton and bacteria is particularly helpful when it comes to SPS corals, and the supplementation of sources of carbon in the form of ethanol or acetate favor the proliferation of heterotrophic bacteria. These may eleiminate the existing deficiency of nutrients for the corals. ... . The reefkeeper needs to experiment a bit to determine which feeding regime improves or worsens the situation, and how much of which type of food is best suite for the needs of the animals he or she is keeping."
Do we trust Borenman ? he answers this thread like this :
From :
Reefkeeping Online Magazine (July 2002)
Coralmania with Eric Borneman
Reef Food
Borneman 2002
The word "nutrient" is often misunderstood. The terms "high nutrient" and "low nutrient" can be taken in many contexts. In general, nutrients are those organic and inorganic compounds necessary to sustain life. While this comprises a very large group of potential compounds, nutrients are often simplified in terms of those elements that are major "building blocks" for fats, amino acids, and carbohydrates. Furthermore, they are frequently those elements which tend to limit further growth by their availability and ability to be procured. In general, carbon, nitrogen and phosphorus are often used to describe the "nutrient" condition of reef organisms (and others, as well). Plants and animals with photosynthetic symbionts tend to be nitrogen and/or phosphorous limited under normal conditions, since photosynthesis usually provides non-limiting carbon source material. Coral reef waters are typically "nutrient poor" as they contain very low levels of nitrogen and phosphorus (they are both precious commodities and any excess is usually taken up quickly). In nearshore areas where there is significant organic loading from land runoff, waters tend to be rather nutrient rich. Both types of environments sustain their own flora and fauna with varying amounts of habitat overlap in terms of the organisms that can exploit the continuum of nutrient conditions. The nutrients available in water to coral reefs can be dissolved in the water, in the form of particulate material, or as living biomass.
...
Coral reef food sources, then, are largely produced by the ocean. Bacteria, detritus, phytoplankton, zooplankton, small benthic fauna, mucus, and dissolved organic and inorganic material of various types and sizes are what comprise the majority of food on a coral reef.