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Ocean acidification: global warming's evil twin

What the science says...

Select a level... Basic Intermediate

The current debate on the connection between CO2 emissions and climate change has largely overlooked an independent and equally serious problem, the increasing acidity of our oceans. Last December, the respected  journal “Oceanography” published projections (see graphic below) for this rising acidity, measured by falling pH [i], through to the end of the century [ii].

Climate Myth...

Ocean acidification isn't serious

'Our harmless emissions of trifling quantities of carbon dioxide cannot possibly acidify the oceans. Paper after paper after learned paper in the peer-reviewed literature makes that quite plain. Idso cites some 150 scientific sources, nearly all of them providing hard evidence, by measurement and experiment, that there is no basis for imagining that we can acidify the oceans to any extent large enough to be measured even by the most sensitive instruments.' (Christopher Monckton)

The current debate on the connection between CO2 emissions and climate change has largely overlooked an independent and equally serious problem, the increasing acidity of our oceans. Last December, the respected  journal “Oceanography” published projections (see graphic below) for this rising acidity, measured by falling pH [i], through to the end of the century [ii]. In 2095, the projected average ocean surface pH is 7.8, and lower still in the Arctic Ocean.

Fig 1: Ocean surface pH - historical values and projected future values based on current emission projections.

CO2 in the atmosphere has increased from 278 ppm in pre-industrial times to 390 ppm today. During this time, the amount of CO2 dissolved in the ocean has risen by more than 30% [iii], decreasing the pH of the ocean by 0.11 units. As with CO2 and global warming, there is some lag between cause and effect. That means that, even if all carbon emissions stopped today, we are committed to a further drop of up to 0.1 units.

The close relationship between CO2 in the atmosphere, CO2 dissolved in the ocean, and the effect of the latter in falling pH, is illustrated by the graph [iv] below:

Fig 2: Annual variations in atmospheric CO2, oceanic CO2, and ocean surface pH. Strong trend lines for rising CO2 and falling pH.

CO2  dissolves in water to form carbonic acid. (It is worth noting that carbonic acid is what eats out limestone caves from our mountains.) In the oceans, carbonic acid releases hydrogen ions (H+), reducing pH, and bicarbonate ions (HCO3-). 

CO2 + H2O => H+ +HCO3-     (1)

The additional hydrogen ions released by carbonic acid bind to carbonate ions (CO32-), forming additional HCO3-.   

H+ + CO32- => HCO3-     (2)

This reduces the concentration of CO32-, making it harder for marine creatures to take up CO32- to form the calcium carbonate needed to build their exoskeletons.

Ca2+ + CO32- => CaCO3   (3)

The two main forms of calcium carbonate used by marine creatures are calcite and aragonite. Decreasing the amount of carbonate ions in the water makes conditions more difficult for both calcite users (phytoplankton, foraminifera and coccolithophore algae), and aragonite users (corals, shellfish, pteropods and heteropods).

The photo below left shows healthy specimens of calcifying phytoplankton Gephyrocapsa oceanica. The photo below right shows the damage to the same creature under conditions expected by the end of the century.


Fig 3: Healthy phytoplankton; same species with malformed shell plates as a result of damage by seawater with simulated end of century chemistry.

Source: Nature, Reduced Calcification of Marine Phytoplankton in Response to Increased Atmospheric CO2, Issue 407 p.364 -367

It is often said that a picture is worth a thousand words.

Research in the Southern Ocean provides evidence that the formation of foraminifera shells is already being affected. Even though these creatures use calcite, which is less soluble than aragonite, there are already clear signs of physical damage. According to Dr. Will Howard of the Antarctic Climate and Ecosystems Cooperative Research Centre in Hobart, shells of one species of foraminifera (Globigerina bulloides) are 30 to 35 percent thinner than shells formed prior to the industrial period.[vi]. The photo below left shows a pre-industrial exoskeleton of this species obtained from sea-floor sediment. The photo below right shows a exoskeleton of a live specimen of the same species obtained from the water column in the same area in 2007. These stunning images were obtained using an electron microscope. (An interview with Dr. Howard was broadcast on the Catalyst television program). [vii] What is staggering is the amount of erosion in the right image compared to the left. The right sample look porous with larger holes and a 10-fold increase in their number. These and creatures like them are at the base of an ocean food chain, and they are already seriously damaged. If they are lost, it is not just biodiversity we are losing, but our food supply as well.


Fig 4. Pre-industrial and current samples of Globigerina bulloides from same location. Latter shows extensive erosion with a ten-fold increase in holes.

Source: Australian Broadcasting Corporation, Ocean Acidification – The Big Global Warming Story, 13 September 2007

The implications of all of this are disturbing. For corals to absorb aragonite from seawater, the latter needs to be saturated in this mineral.

Now a report from NOAA scientists found large quantities of water undersaturated in aragoniteare already upwelling close to the Pacific continental shelf from Vancouver to northern California [v]. Although the study only dealt with the area, the authors suggest that other shelf areas may be experiencing similar effects. 

For corals like those in Australia’s Great Barrier Reef, the outlook is grim. They are threatened with destruction on two fronts, both caused by CO2 emissions. Not only do increased ocean temperatures bleach coral by forcing them to expel the algae which supplies them with energy (see photo at left) [viii], but increased ocean CO2 reduces the availability of aragonite from which reefs are made.

It is time to wake up. Our planet is dying. I urge you to find the time to view a 20 minute documentary on the problem of ocean acidification produced by the international Natural Resource Defence Council. Simply go to: Acid test movie.

Fig 5. Coral killed by above average ocean temperatures.


References and Notes

   [i]  pH is a measure of the acidity or alkalinity  of a solution. It uses a negative logarithmic scale where a decrease of 1.0 units represents a 10-fold increase in acidity. In   their natural state prior to industrialization, the oceans were slightly alkaline with a pH of 8.2 (see reference iii). Pure water has a pH of 7.0.
   [ii]  Feely R., Doney S., Cooley S. (2009). Present Conditions and Future Changes in a High-CO2 World. Oceanography 22, 36-47
   [iii]  Australian Antarctic Division, Ocean Acidification and the Southern Ocean, available at
   [iv] Feely, Doney and Cooley, op. cit, using Mauna Loa data from the US National Oceanic and Atmospheric Administration and Aloha data from the University of Hawaii.
   [v] Feely RA, Sabine CL, Hernandez-Ayon JM, Ianson D, Hales B (June 2008). Evidence for upwelling of corrosive "acidified" water onto the continental shelf. Science 320 (5882): 1490–2, available at
   [vi] Inter Press Service, Acid Oceans Altering Marine Life, available at
   [vii] Australian Broadcasting Corporation, Ocean Acidification  – The Big Global Warming Story, downloadable at
   [viii]  Great Barrier Reef Marine Park Authority, What is Coral Bleaching?, available here

Intermediate rebuttal written by alan_marshall

Last updated on 8 July 2015 by pattimer. View Archives

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Question: Is the ocean acidifying?

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Question: Is ocean acidification from human activities enough to impact marine ecosystems?

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Comments 1 to 25 out of 100:

  1. John Abraham has dissected Moncktons presentation on climate science here: It's well worth listening from beginning to end!
  2. "Past history shows us that when CO2 rose sharply, this corresponded with mass extinctions of coral reefs." The mass extinction events you refer to- End Permian, PTEM, End Triassic- occured over tens of thousands to millions of years, at a rate not relevant to human time frames. Corals went extinct, and ocean acidity rose, but it did not rise 'sharply'. We should equally start worrying about continental drift rates and extinction. Past history also shows us that when continents collided, numerous species went extinct, but at a rate not relevant to humans. "The change in seawater pH over the 21st Century is projected to be faster than anytime over the last 800,000 years and will create conditions not seen on Earth for at least 40 million years." This is entirely based on model projections, which are themselves based on dubious assumptions. Past pH in industrial times has been modelled, not measured, therefore the current rate of change in oceanic pH is itself doubtful. A recent paper which measured pH in the last 15 years in the north pacific shows it has experienced an average change of 0.03pH in the last 15 years. I'm not sure this is a rate to which there is concern. The geological record indicates that oceans appear to be strongly buffered, and do not change pH easily. They have apparently not changed pH more than 0.6 in the last 300 M years, presumably because of negative feedbacks/buffering to any rise in C02/other factors. Hundreds of thousands of years of widespread explosive volcanism is generally required to lead to a modest rise in oceanic acidity. I would suggest that most of the research papers on potential ocean acidification are written by biologists and chemists who do not take into account processes outside their own, specialist fields. An illustrative example is, for eg, the question of where all the water in the oceans themselves originally comes from. If you ask some NASA scientists, it comes from comets. These scientists have, incidentally, never studied effects of large cooling magmas in the earth's crust. When granitic magmas cool, they expel water; the Earth's cooling crust in its early history is more than enough to account for all the world's ocean water, a process that still goes on today in eg mountain ranges, although the net water balance of the planet is more or less constant due to water saturated crust also being subducted into subduction zones. The point is, the comets, which are the NASA scientists special field, have nothing to do with the origin of the vastly greater portion of the world's water. The subsurface, and its processes, as usual, are presumed to be stable and unchanging, and therefore ignored. Another illustrative example is when geologists first reported the presence of numerous species of microrganisms feeding on 'dead' rock masses thousands of metres below the surface-these findings were initially totally ignored-how could deep subsurface 'rocks' be relevant to Earth's Biological processes? Now some scientists think that life itself may have originated deep within the earth, from/in association with these deep-dwelling micro-organisms (eg Paul Davies). Also of note, is that these micro-organisms are believed to account for by far the greater mass by weight of biota on earth, they extend well into the earth's crust, and are ore or less everywhere/abundant. Much the same sort of ignorance goes for various ocean acidification theories/projections; buffering procesess in the subsurface, for eg the >100,000km of Mid Oceanic Rifts, which extend down several kilometres of heated, carbonate-enriched rock, where large amounts of carbonic acid are produced/exchanged/ precipitated in the subsurface, are generally totally ignored by biologists and chemists, who think all you have to do to prove ocean acidification is carry out an experiment in a controlled lab with some H20, gases and no real-world earth subsurface processes, ie if you add c02 to the atmosphere, then oceans will experience runaway acidification. Their field and their models do not take into account rates of chemical precipitation /dissolution of eg c02 in the world's subsurface,rates of oceanic mixing, microbiological feedbacks, or any other potential buffering/negative feedback effects, nor the long geological record which indicates that the oceans only change pH significantly on geological timescales, not human timescales. The idea that oceans will acidify markedly over the next century is a result of inaccurate and incomplete modelling, nothing more.
  3. @thingadonta: you seem to contradict yourself in your post. First, you write: "A recent paper which measured pH in the last 15 years in the north pacific shows it has experienced an average change of 0.03pH in the last 15 years. I'm not sure this is a rate to which there is concern." You then go on to write: "The geological record indicates that oceans appear to be strongly buffered, and do not change pH easily. They have apparently not changed pH more than 0.6 in the last 300 M years" Minus 0.003 pH per year would yield an decrease of 0.6 pH in a mere 300 years, not 300 million - to me, this rate of change really is matter for concern. Now, to be fair you didn't claim pH dropped by 0.6 over 300My, but rather that this was the extent of the variation (which in itself is meaningless when talking about the rate of change). Fortunately, we can take a look at the CO2 vs. pH graph above to have an idea of the rate at which acidification can take place outside of human intervention. Looking at the last drop of 0.2 in the pH, we can see it took place quite rapidly, but not any quicker than about 2,000 years (there is 20ky per tick on that graph). This is a rate of 0.0001 pH per year, or about 50x slower than the current decrease in pH. That figure is actually quite conservative, as research has shown the current acidification is occuring about 100x faster than what the geological record reveals. Your skepticism is natural, but in this case I think it's clear you're off-mark by two orders of magnitude...
  4. Is there a way to read Pelejero 2010 w/o buying a membership with Science Direct? If not, this page would be improved by a summary of the proxies used and how they were validated.
  5. The first deep basin observations of Aragonite undersaturation in surface waters have already been observed in 2008 in the Arctic (Yamamoto-Kawai 2009), and in 2009 the extent of surface waters with undersaturated aragonite increased, although this is not yet region-wide. This means that these waters crossed the threshold where they are beginning to be corrosive to certain types of calcifying organisms. The trends in the Arctic regions have been a cause for concern for some time (Bates 2009), as the Arctic waters are subjected to the dual effects of decreasing alkalinity due to increasing pCO2 (directly due to uptake of the increasing atmospheric CO2 due to anthropogenic emissions), and increased sea ice meltwater due to increases in regional temperatures which are greater than the average global temperature rise. Models also predicted Aragonite undersaturation in these regions would occur in the near future, but the recent increased rate of ice melt has accelerated the process (eg Steinacher 2009). As both atmospheric CO2 and Arctic sea ice melt rates are on accelerating trends this will have a negative effect on populations of both planktonic and benthic calcifying organisms in the Canada Basin, and potentially over wider areas within a relatively short time span.
  6. I got to wondering if anyone had estimated the numeric relationship between atmospheric CO2 concentration change vs. ocean pH change. The dots in the graph you show suggest the glacial-interglacial difference of 100 ppm corresponded to a pH variation of 0.2 units of pH, so about 50 ppm / (0.1 pH) A bit of searching in Google Scholar yielded: K Caldeira, ME Wickett - Nature, 2003 "Anthropogenic carbon and Ocean pH", cited by 499 A key finding of theirs is that large but slow pCO2 changes led to somewhat smaller final ocean pH response, thanks to geologic-scale "buffering" effects (top 1/4 of their figure 1(b)). However, over shorter time spans, "[w]hen a CO2 change occurs over a short time interval (that is, less than about 104 yr), ocean pH is relatively sensitive to added CO2" So, just how sensitive, I wondered? I tried to glean from their graph whether ocean pH response to changes in pCO2(atm) is basically linear or logarithmic (they don't state either way). The X axis of figure 1(b) is log (or semi-log?) while the vertical bands for each pH level are spaced about equally, suggesting a logarithmic relationship. If so, the response for a doubling of CO2 along the bottom of fig. 1(b) (i.e. over short, human-scale time spans relevant to ACC) looks like roughly 0.3 pH units per doubling of pCO2. I'd appreciate if others would review the article and see if my takeoffs make sense of what's there.
  7. Also, lately I'm seeing frequent repetitions of the argument that ocean pH is still > 7 and so it is not "acidic", and that somehow precludes or invalidates use of the term 'Acidification' for lowering pH (even though this is perfectly valid and common scientific usage). Do we need to define this as a new "skeptic argument", or at least include a direct refutation of that move under this "it isn't serious" topic?
  8. Jim Prall #7, you think the hysterics over 'acidification' are bad? I just had a 'skeptic' (who was cited in the Cuccinelli vs Mann case) very determinedly telling me that the oceans are NOT becoming more acidic. Rather, they are becoming less alkaline. I suppose I should just be thankful that they have some grasp on reality... even if they refuse to allow words to hold their traditional meanings.
  9. They seem to be relying on a simplistic reading of the terminology, where "only pH below 7 is 'acidic'" to support a serious fallacy--that by implication, any pH over 7 must be fine, even if it is falling fast The problem is that any significant change in pH affects biological systems and the solubility of the basic building blocks like CaCO3. There is no magic threshold at pH = 7.0 other than a semantic one; for a biochemist, nothing special happens crossing that line. Changing pH from, e.g. 8.3 to 8.2 has a real, tangible effect on the solubility of CaC03, and on the equilibria between CO2(aq), H2CO3, and HCO3[-1]. These changes alter the "saturation horizon"--the depth at which CaCO3 is saturated, and that has a vital effect on organisms that form hard carbonate shells. There are ecological impacts to any substantial change in pH, whether the starting point is 8.3, 7.9, or 7.001. Arguing that lowering pH substantially "isn't acicification" is just debating semantics, and certainly walks and quacks like a diversion tactic. If we need some evidence that working oceanographers don't have a problem with calling current changes from 8.3 to 8.2 "acidification," we need look no further than the Monaco Declaration on Ocean *Acidification* signed by 155 experts in the field:
  10. Jim, they probably aren't gardeners. Gardeners fully understand more and less acidic/alkaline in relation to soils. Though I think it would be pushing it to propose an analogy based on blue and pink hydrangea blooms.
  11. Some new data revealing the results of ocean acidification on marine corals: New Ocean Acidification Study Shows Added Danger to Already Struggling Coral Reefs Source study here. And yes. Acidification is the term used in the study. Like it, or not. The Yooper
  12. This paper leads one to believe that it is not as simple as the AGW believers want us to believe. Increased CO2 does seem to decrease CO3 in the lab, which is considered a limiting factor for coral growth. But, it also increases photosynthesis output, and actual coral growth in terms of biomass does not seem to suffer, and actually increases in some studies More information Are they trying to measure coral growth the wrong way when they concentrate on calcium carbonate measurements? Would we not expect the ocean equivalents of plants to also grow more as the CO2 increases as well, providing more food for sea life? Yes, plankton growth will be stimulated by increased CO2 levels, as long as other limiting factors do not come into play Another paper I scanned said that parts of the ocean are deficient in iron, which limits plankton growth Plankton and algae will increase productivity as CO2 levels increase in seawater, they die, raining down on the sea floor, sinking more CO2. Chris Shaker
  13. This paper leads one to believe that it is not as simple as the AGW believers want us to believe You're arguing a strawman there. Changes in seawater chemistry are anything but simple. Would we not expect the ocean equivalents of plants to also grow more as the CO2 increases as well, providing more food for sea life? No. Decreased carbonate concentrations in seawater, combined with acidification and ocean stratification affect the long-term viability of phytoplankton populations. For example: Global phytoplankton decline over the past century "Here we combine available ocean transparency measurements and in situ chlorophyll observations to estimate the time dependence of phytoplankton biomass at local, regional and global scales since 1899. We observe declines in eight out of ten ocean regions, and estimate a global rate of decline of ~1% of the global median per year. Our analyses further reveal interannual to decadal phytoplankton fluctuations superimposed on long-term trends.
  14. Rob Painting: Did you read the paper I referenced, showing increased biomass in coral with increased CO2? Did you read the paper I referenced, showing increased plankton growth with increased CO2? Are you offering me any peer reviewed papers proving the opposite? No. Chris Shaker
  15. Your link to a nature article does not appear to work Did you notice the paper I referenced, showing plankton growth limited by iron? Chris Shaker
  16. The paper I referenced, showing plankton growth limited by iron was from Nature "We conclude that Fe deficiency is limiting phytoplankton growth in these major-nutrient-rich waters." Chris Shaker
  17. Please search for 'Iron Fertilization' in this paper to see that iron is well recognized as a limiting factor in plankton growth. They are talking about using Iron to cause plankton blooms to sequester CO2 and drop it down to the ocean floor That paper also seems to show that mortality rates for some sea creatures, such as mollusks, increase with CO2. Chris Shaker
  18. There is also a Wiki on Iron Fertilization of the Ocean "Perhaps the most dramatic support for Martin's hypothesis was seen in the aftermath of the 1991 eruption of Mount Pinatubo in the Philippines.[citation needed] Environmental scientist Andrew Watson analyzed global data from that eruption and calculated that it deposited approximately 40,000 tons of iron dust into the oceans worldwide. This single fertilization event generated an easily observed global decline in atmospheric CO2 and a parallel pulsed increase in oxygen levels.[7]" Chris Shaker
  19. Chris Shaker, You have so many misconceptions about the topic, it's difficult to know where to start. The advanced version of Ocean Acidification should be out by years end and hopefully that clears up some of your confusion. Coral reefs - long term monitoring is showing a rise in bleaching events and coral death. Both acidification and ocean warming negatively impact coral reefs. Again, this is a topic for a later post but some reading: Caribbean Corals in Crisis: Record Thermal Stress, Bleaching, and Mortality in 2005 Worst coral death strikes at SE Asia - 19 October 2010 "Many reefs are dead or dying across the Indian Ocean and into the Coral Triangle following a bleaching event that extends from the Seychelles in the west to Sulawesi and the Philippines in the east and include reefs in Sri Lanka, Burma, Thailand, Malaysia, Singapore, and many sites in western and eastern Indonesia. “It is certainly the worst coral die-off we have seen since 1998. It may prove to be the worst such event known to science,” says Dr Andrew Baird of the ARC Centre of Excellence for Coral Reef Studies and James Cook Universities. “So far around 80 percent of Acropora colonies and 50 per cent of colonies from other species have died since the outbreak began in May this year.”
  20. Chris Shaker @17 Please search for 'Iron Fertilization' in this paper to see that iron is well recognized as a limiting factor in plankton growth Well aware of that thanks. Sorry, but "iron fertilization" is one of those ill-considered "engineering" ideas: Can ocean iron fertilization mitigate ocean acidification? " Here, using a global ocean carbon cycle model, we performed idealized ocean iron fertilization simulations to place an upper bound on the effect of iron fertilization on atmospheric CO2 and ocean acidification. Under the IPCC A2 CO2 emission scenario, at year 2100 the model simulates an atmospheric CO2 concentration of 965 ppm with the mean surface ocean pH 0.44 units less than its pre-industrial value of 8.18. A globally sustained ocean iron fertilization could not diminish CO2 concentrations below 833 ppm or reduce the mean surface ocean pH change to less than 0.38 units. This maximum of 0.06 unit mitigation in surface pH change by the end of this century is achieved at the cost of storing more anthropogenic CO2 in the ocean interior, furthering acidifying the deepocean. If the amount of net carbon storage in the deep ocean by iron fertilization produces an equivalent amount of emission credits, ocean iron fertilization further acidifies the deep ocean without conferring any chemical benefit to the surface ocean"
  21. The bleaching of coral reefs seems to actually be caused by fungus, which is transported across oceans by dust in the wind as the climate naturally warms and dries. It looks like fungi have been attacking coral reefs for a long time Chris Shaker
  22. Chris , I find it insightful to actually read the studies linked to. The authors are proposing a hypothesis (back in 2000). They claim that two bleaching events in the Caribbean (1983/1987) coincide with increases in dust transport into the region. They lay the foundations for their hypothesis, that's the extent of it. In those two years (1983/1987) anomalously warm waters occurred too. Furthermore 1988 was a year of Caribbean coral bleaching and according the graph in Shinn 2000, this was a year of very low dust import into the region. In the meantime, coral reefs the world over have begun to bleach, as sea surface temperatures rise (see links at @ 19 for instance). I would certainly be interested to see how the authors of that study explain that away on African dust. I don't doubt that the transport of dust into the caribbean region has an influence of the marine life, however the evidence for warming waters as the cause of coral bleaching has strengthened to such a level that scientists are now able to accurately forecast bleaching events: Coral bleaching forecast - Coral Bleaching Likely in Caribbean This Year - Sept 22 2010 And reality: Caribbean Coral Die-Off Could Be Worst Ever - 14 Oct 2010 And yes, coral diseases are a major problem, often after bleaching events have occurred.
  23. Rob: I searched for, found, and read that paper after watching an educational TV program that covered the fungus, possibly a Nova? Chris Shaker
  24. Most references I see on coral bleaching list increased temperature as the main stress likely to cause it. Reading the wiki on Coral bleaching seems to offer a contradiction It says, "Bleaching occurs when the conditions necessary to sustain the coral's zooxanthellae cannot be maintained.[4] Any environmental trigger that affects the coral's ability to supply the zooxanthellae with nutrients for photosynthesis (carbon dioxide, ammonium) will lead to the zooxanthellae's expulsion.". That seems to say that CO2 is required for photosynthesis. Yet, they also state, "Coral bleaching is a vivid sign of corals responding to stress, which can be induced by any of: increased (most commonly), or reduced water temperatures[5][6] increased solar irradiance (photosynthetically active radiation and ultraviolet band light)[7] changes in water chemistry (in particular acidification)[8][9] starvation caused by a decline in zooplankton[10] increased sedimentation (due to silt runoff) pathogen infections changes in salinity wind[6] low tide air exposure[6] cyanide fishing" How much stock am I supposed to put in the 'acidification' mention when CO2 appears to be essential for coral photosynthesis? Chris Shaker
  25. f Found some more current research on wind born problems for coral reefs, from a Government source "African Dust Poses Threat to Coral Reefs and Human Health:  Contaminants carried with African dust to the Caribbean and the Americas may be a threat to marine organisms and humans, according to preliminary results of a new study by researchers with the U.S. Geological Survey, Oregon State University, and the University of the West Indies. The scientists compared contaminant levels in sources of African dust and downwind regions. Of the more than 100 persistent organic pollutants screened for in the samples, including banned and common-use pesticides, six pesticides (chlorpyrifos, dacthal, endosulfans, hexachlorobenzene, chlordane, and trifluralin) were detected in samples from all sites. Concentrations were significantly higher in Mali. DDE (a breakdown product of DDT) was also identified in Mali, U.S. Virgin Islands, and Trinidad samples. To date, DDT and carcinogenic dioxins and furans have been detected only in samples from Mali. Many of the identified contaminants are thought to be toxic to corals and other marine organisms and can interfere with reproduction, fertilization, or immune function. For more information, contact Virginia Garrison at 727-803-8747, ext. 3061 or" "The Origin of Aspergillus Sydowii, a Common Disease of Caribbean Corals:  Coral reefs are increasingly suffering outbreaks of disease, causing dramatic declines in population abundance and diversity. One of the best-characterized coral diseases is aspergillosis, caused by the fungus Aspergillus sydowii. A. sydowii is a globally distributed fungus commonly found in soil, so its presence in marine systems raises questions about its origin. By using microsatellite markers, researchers analyzed the population structure of A. sydowii from diseased sea fans, diseased humans and environmental sources worldwide. The results indicate that A. sydowii forms a single global population, with low to moderate genetic differences between the disease found in sea fans and the same fungus from environmental sources. Past researchers have suggested that A. sydowii originates from African dust blown into the Caribbean, and have identified Aspergillus from dust samples, although often only to the genus level. To test this, researchers isolated fungi from dust samples collected in Mali and St. Croix. Although a diversity of fungi was documented from African dust, including seven species of Aspergillus, none of the samples contained A. sydowii. Taken in conjunction with recent molecular evidence suggesting lack of a single point source of the fungus, this research suggests  that there are likely multiple sources and introductions of this pathogen into marine systems. For more information contact Krystal Rypien at 858-534-3196, or  Virginia Garrison at 727-803-8747, ext. 3061 or" "The Emperor Has No Coral? Results of research on coral reefs in the Florida Keys reef challenge the highly popular notion that present declines in reefs in Florida and elsewhere are related to human activities. High-resolution sub-bottom profiling, reef drilling, and mapping of benthic habitats along the reef tract present a paradox in coral growth patterns: reefs that are dead or dying -- and therefore not building -- outnumber live and building reefs about 100 to 1. Yet growth rates of all common coral reef species should have kept pace with the well-documented rise in sea level over the past 6,000 years. Why did so few reefs keep pace or build up with the rise in the present sea level? Geological history may provide an answer: two 500-year periods of non-growth of coral reefs occurred in the region 4.5 thousand years ago and 3,000 years ago. These periods of non-growth indicate times of environmental crises that predated modern human presence in the Florida Keys. The present period of rapid coral demise has spanned only about 30 years. For more information, contact Eugene Shinn at 727-533-1158, or Barbara Lidz at 727-803-8747, ext. 3031," Chris Shaker

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