Archive for August, 2013



Bad feedback: ocean acidification to worsen global warming

As if ocean acidification and climate change weren’t troubling enough (both of which are caused by still-rising carbon emissions), new research published in Nature finds that ocean acidification will eventually exacerbate global warming, further raising the Earth’s temperature.

Scientists have long known that tiny marine organisms—phytoplankton—are central to cooling the world by emitting an organic compound known as dimethylsulphide (DMS). DMS, which contains sulfur, enters the atmosphere and helps seed clouds, leading to a global cooling effect. In fact, in the past scientists have believed that climate change may actually increase DMS emissions, and offset some global warming, but they did not take into account the impact of acidification.

Researchers, headed by Katharina Six with the Max Planck Institute for Meteorology, tested how acidification affects phytoplankton in the laboratory by lowering the pH (i.e. acidifying) in plankton-filled water tanks and measuring DMS emissions. When they set the ocean acidification levels for what is expected by 2100 (under a moderate greenhouse gas scenario) they found that cooling DMS emissions fell.

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Respiration of Mediterranean cold-water corals is not affected by ocean acidification as projected for the end of the century (update)

The rise of CO2 has been identified as a major threat to life in the ocean. About one-third of the anthropogenic CO2 produced in the last 200 yr has been taken up by the ocean, leading to ocean acidification. Surface seawater pH is projected to decrease by about 0.4 units between the pre-industrial revolution and 2100. The branching cold-water corals Madrepora oculata and Lophelia pertusa are important, habitat-forming species in the deep Mediterranean Sea. Although previous research has investigated the abundance and distribution of these species, little is known regarding their ecophysiology and potential responses to global environmental change. A previous study indicated that the rate of calcification of these two species remained constant up to 1000 μatm CO2, a value that is at the upper end of changes projected to occur by 2100. We examined whether the ability to maintain calcification rates in the face of rising pCO2 affected the energetic requirements of these corals. Over the course of three months, rates of respiration were measured at a pCO2 ranging between 350 and 1100 μatm to distinguish between short-term response and longer-term acclimation. Respiration rates ranged from 0.074 to 0.266 μmol O2 (g skeletal dry weight)−1 h−1 and 0.095 to 0.725 μmol O2 (g skeletal dry weight)−1 h−1 for L. pertusa and M. oculata, respectively, and were independent of pCO2. Respiration increased with time likely due to regular feeding, which may have provided an increased energy supply to sustain coral metabolism. Future studies are needed to confirm whether the insensitivity of respiration to increasing pCO2 is a general feature of deep-sea corals in other regions.

Continue reading ‘Respiration of Mediterranean cold-water corals is not affected by ocean acidification as projected for the end of the century (update)’

Effects of carbon dioxide on biomass and species composition of a natural Baltic Sea spring bloom community

Carbon dioxide (CO2) emissions contribute to an increased mean temperature of the Earth and ocean acidification. The environmental changes give great concern for biodiversity and future environmental sustainability. Microalgae can possibly be used to recycle CO2 emissions and the biomass could be used for production of high value products like, healthy human food or biofuels. The aim of this study was to examine the effect of carbon dioxide on algae biomass production and species composition of a natural spring bloom community (NC) from the Baltic Sea. Spring blooms are dominated by diatoms which could be a good candidate for CO2 assimilation. The NC was exposed to CO2 gas and compared with NC without added CO2 sources (Air control). The NC was cultivated under controlled laboratory conditions with daily sampling for chlorophyll a and pH measurement. Species composition was investigated by microscope. Low pH reduced CO2 assimilation of the NC but was compensated for since no effect of CO2 could be seen on biomass production. Additionally CO2 had no effect on species composition indicating the species in the NC to be resistant to pH fluctuations. A clear shift in species composition could be seen over time. The diatoms dominated at experiment end confirming that they could potentially be used for algae cultivation to recycle CO2.

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Effects of ocean warming and acidification on the energy budget of an excavating sponge

Recent research efforts have demonstrated increased bioerosion rates under experimentally elevated partial pressures of seawater carbon dioxide (pCO2) with or without increased temperatures, which may lead to net erosion on coral reefs in the future. However, this conclusion clearly depends on the ability of the investigated bioeroding organisms to survive and grow in the warmer and more acidic future environments, which remains unexplored. The excavating sponge Cliona orientalis Thiele, 1900 is a widely distributed bioeroding organism and symbiotic with dinoflagellates of the genus Symbiodinium. Using C. orientalis, an energy budget model was developed to calculate amounts of carbon directed into metabolic maintenance and growth. This model was tested under a range of CO2 emission scenarios (temperature + pCO2) appropriate to an Austral early summer. Under a pre-industrial scenario, present day (control) scenario, or B1 future scenario (associated with reducing the rate of CO2 emissions over the next few decades), C. orientalis maintained a positive energy budget, where metabolic demand was likely satisfied by autotrophic carbon provided by Symbiodinium and heterotrophic carbon via filter-feeding, suggesting sustainability. Under B1, C. orientalis likely benefited by a greater supply of photosynthetic products from its symbionts, which increased by up to 56% per unit area, and displayed an improved condition with up to 52% increased surplus carbon available for growth. Under an A1FI future scenario (associated with ʻbusiness-as-usualʼ CO2 emissions) bleached C. orientalis experienced the highest metabolic demand, but carbon acquired was insufficient to maintain the sponge, as indicated by a negative energy budget. These metabolic considerations suggest that previous observations of increased bioerosion under A1FI by C. orientalis may not last through the height of future A1FI summers, and survival of individual sponges may be dependent on the energy reserves (biomass) they have accumulated through the rest of the year.

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Physiological responses to oxidative stress associated with pH variations in host tissue and zooxanthellae of hermatypic coral Pocillopora capitata

To study the adaptive mechanisms of host and symbiont in a decrease in pH, coral branches of Pocillopora capitata from La Boquita reef in the Bay of Santiago, México were assigned to experimental units (n = 38 per treatment) and three pH treatments were evaluated: (a) pH 8.00–8.40 (control; Treatment C1), (b) pH 7.85–7.95 (Treatment C2) and (c) pH 7.60–7.70 (Treatment C3). Corals were collected at the beginning of the experiment (T0) and at different times: T1 (5 h), T2 (12 h), T3 (48 h) and T4 (168 h). We examined malondialdehyde (MDA), antioxidant enzyme activities (SOD and CAT), antioxidant capacity and chlorophyll a (Chl a) content. The results showed a different response to the treatment between zooxanthellae and Cnidaria tissues. Initially in zooxanthellae, we observed a SOD response for the C3 treatment; however this response did not prevent lipid degradation. In Cnidaria, the C3 resulted in a greater SOD activity from the middle to the end of the experiment. The results improve our understanding of the effects of ocean acidification, the ability of coral to respond to environmental changes and the use of biochemical indicators related to the physiological condition for the recognition of coral communities affected by a decreases in pH.

Continue reading ‘Physiological responses to oxidative stress associated with pH variations in host tissue and zooxanthellae of hermatypic coral Pocillopora capitata’

Change the fundamentals and you are in an ocean of trouble

Recent studies have shown several marine species are struggling to adapt to the excess carbon dioxide and heat which oceans are absorbing. Evidence is mounting of the risks we’re taking with our oceans.

Life is finely tuned to the physical and chemical conditions that surround it. This “tuning” is the result of thousands – if not millions – of years of natural selection, optimising the physiological and biochemical ways marine organisms respond to a naturally variable environment.

But there are limits to how much organisms can “acclimate” to this variability. Beyond a certain point, organisms increasingly fail to cope. This leads to decreased performance and eventually death.

Marine life is no different.

Continue reading ‘Change the fundamentals and you are in an ocean of trouble’

The ocean is going to start confusing fish and dissolving seashells

Ocean acidification driven by increasing atmospheric carbon levels is a substantial threat to marine life, a new study has confirmed.

The study, published in the journal Nature Climate Change, analyzed 167 studies on the effects of ocean acidification on corals, crustaceans, mollusks, fishes and echinoderms, a group which includes starfish and sea urchins. The studies included data on effects of ocean acidification on more than 150 species of marine life, which the researchers then matched up to different climate scenarios to get a sense of how each species would respond to different levels of ocean acidification.

They found that at atmospheric carbon concentrations of 500 to 650 parts per million — levels that are predicted by 2100 — corals, echinoderms, mollusks and fish were negatively impacted, though crustaceans such as crabs and lobsters were relatively unaffected. When atmospheric carbon concentrations rose above 650 ppm, all groups studied were harmed.

Continue reading ‘The ocean is going to start confusing fish and dissolving seashells’

Acidifying oceans will heat the planet more

What goes around comes around. Our greenhouse gas emissions don’t just warm the planet, they also acidify the oceans. Now it turns out that the change in ocean chemistry they cause will feed back into the climate, further driving up temperatures.

Ocean acidification poses a threat to many marine organisms such as corals – the shells of some marine snails are already dissolving. Until now it seemed like this was strictly a problem for marine organisms and the people who depend on them: ‘climate scientists consider the carbon dioxide that is absorbed by the ocean to be stored and unable to affect the climate.

Continue reading ‘Acidifying oceans will heat the planet more’

Ocean acidification increases warming (text and audio)

Oceans that grow more acidic through increased carbon emissions, amplify global warming by releasing less of a gas that helps shield Earth from solar radiation, a new study reveals.

And the authors of the paper, which appears today in the journal Nature Climate Change, warn the potentially vast effect they uncovered is not currently factored into climate change projections.

Katharina Six of the Max Planck Institute for Meteorology, and colleagues, say human-induced carbon dioxide (CO2) emissions contribute to planetary warming by letting the Sun’s heat through the atmosphere but trapping heat energy reflected back from Earth, so creating a greenhouse effect.

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Acidification of ocean’s adversely impacting sea animals’ health

Washington, August 26 (ANI): Biologists have claimed that acidification of our oceans could change the ecosystems of our seas even by the end of this century.

In a new study, biologists at the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI), compiled and analysed all available data on the reaction of marine animals to ocean acidification.

The scientists found that whilst the majority of animal species investigated are affected by ocean acidification, the respective impacts are very specific.

Continue reading ‘Acidification of ocean’s adversely impacting sea animals’ health’

Studies highlight dangers of rising acidity in oceans (text and audio)

Two scientific studies released today highlight the dangers of rising acid levels in the world’s oceans.

Oceans play a vital role in climate change by absorbing carbon dioxide (CO2) and helping to reduce global warming, but CO2 makes ocean water more acidic.

Now a study published in the journal Nature Climate Change shows acidification will drive substantial changes in ocean ecosystems this century.

The authors assessed a range of marine animals including corals, starfish, molluscs, crustaceans and fish.

Continue reading ‘Studies highlight dangers of rising acidity in oceans (text and audio)’

Ocean acidification poses threat to wide range of animal life, study shows

As the ocean continues to grow more acidic, many marine animals will face negative consequences, though to varying degrees due to differences in bodily functions, according to a new study published in the journal Nature Climate Change.

The world’s oceans are responsible for absorbing more than a quarter of the carbon dioxide emitted through human activity, thus acting as a stabilizing force for the Earth’s global temperatures. However, such storage is not limitless nor without its consequences.

Continue reading ‘Ocean acidification poses threat to wide range of animal life, study shows’

How ocean acidification harms sealife and worsens climate change

A spate of new research looks at the impact of the ocean’s lowered pH both above and below the surface

It’s been a busy weekend for the study of ocean acidification, bringing mostly bad news from an area we normally don’t hear too much about at all.

Continue reading ‘How ocean acidification harms sealife and worsens climate change’

Ocean acidification will make climate change worse

As we emit more carbon dioxide, the oceans will become more acidic. That will be bad for sealife—but it may also speed the rate of global warming

Given that they cover 70% of the Earth’s surface—and provide about 90% of the planet’s habitable space by volume—the oceans tend to get short shrift when it comes to climate change. The leaked draft of the forthcoming coming new report from the Intergovernmental Panel on Climate Change highlighted the atmospheric warming we’re likely to see, the rate of ice loss in the Arctic and the unprecedented (at least within the last 22,000 years) rate of increase of concentrations of greenhouse gases like carbon dioxide and methane. But when it came to the oceans, press reports only focused on how warming would cause sea levels to rise, severely inconveniencing those of us who live on land.

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The role of CO2 variability and exposure time for biological impacts of ocean acidification

Biological impacts of ocean acidification have mostly been studied using future levels of CO2 without consideration of natural variability or how this modulates both duration and magnitude of CO2 exposure. Here we combine results from laboratory studies on coral reef fish with diurnal in situ CO2 data from a shallow coral reef, to demonstrate how natural variability alters exposure times for marine organisms under increasingly high-CO2 conditions. Large in situ CO2 variability already results in exposure of coral reef fish to short-term CO2 levels higher than laboratory-derived critical CO2 levels (~600 µatm). However, we suggest the in situ exposure time is presently insufficient to induce negative effects observed in laboratory studies. Our results suggest that both exposure time and the magnitude of CO2 levels will be important in determining the response of organisms to future ocean acidification, where both will increase markedly with future increases in CO2.

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Ocean acidification: making new discoveries through National Science Foundation research grants

Acidifying marine ecosystems of increasing concern

With increasing levels of carbon dioxide accumulating in the atmosphere and moving into marine systems, the world’s oceans are becoming more acidic.

The oceans may be acidifying faster today than at any time in the past 300 million years, scientists have found.

To address the concern for acidifying marine ecosystems, the National Science Foundation (NSF) has awarded new grants totaling $12 million in its Ocean Acidification Program.

Continue reading ‘Ocean acidification: making new discoveries through National Science Foundation research grants’

Not all species equally affected by more acidic oceans

When atmospheric carbon dioxide dissolves into the ocean, it forms carbonic acid, which in turn lowers the water’s pH levels and causes oceanic acidification. The phenomenon is expected to occur at increasing rates as carbon dioxide emissions around the world continue to rise.

In a report published in Nature Climate Change, two researchers from the Alfred Wegener Institute, Helmholtz-Centre for Polar and Marine Research (AWI) in Bremerhaven, Germany performed an extensive research review that indicated the impacts of a more acidic ocean will vary from one species to the next.

Continue reading ‘Not all species equally affected by more acidic oceans’

Climate change: ocean acidification amplifies global warming

Scientists at the Max Planck Institute for Meteorology (MPI-M), Dr. Katharina Six, Dr. Silvia Kloster, Dr. Tatiana Ilyina, the late Dr. Ernst Maier-Reimer and two co-authors from the US, demonstrate that ocean acidification may amplify global warming through the biogenic production of the marine sulfur component dimethylsulphide (DMS).

It is common knowledge that fossil fuel emissions of CO2 lead to global warming. The ocean, by taking up significant amounts of CO2, lessens the effect of this anthropogenic disturbance. The “price” for storing CO2 is an ongoing decrease of seawater pH (ocean acidification1), a process that is likely to have diverse and harmful impacts on marine biota, food webs, and ecosystems. Until now, however, climate change and ocean acidification have been widely considered as uncoupled consequences of the anthropogenic CO2 perturbation2. Recently, ocean biologists measured in experiments using seawater enclosures (mesocosms)3 that DMS concentrations were markedly lower in a low-pH environment (Figure 1).

Continue reading ‘Climate change: ocean acidification amplifies global warming’

Ocean acidification may substantially change aquatic ecosystems and even impact how we eat

Ocean acidification — the term for how carbon emissions, which affect our air and atmosphere, are making the oceans more acidic — may drive substantial change in aquatic ecosystems during the 21st century, authors of a recently published paper have found. Ultimately, the long-term survival ability of certain species may be compromised, and this could impact the food resources found within the ocean.

Continue reading ‘Ocean acidification may substantially change aquatic ecosystems and even impact how we eat’

Ocean acidification bad news for future fish, worse for coral; what will the ocean look like in 2100?

In 100 years we may be looking at a much different ocean species-wise.

A new study worked to predict the impact of ocean acidification on various species, and found they responded in their own specific ways, an Alfred Wegener Institute press release reported.

The study team analyzed previously collected data on the impact of ocean acidification regarding: “corals, crustaceans, mollusks, vertebrates such as fishes and echinoderms (animals such as starfish and sea urchins).”

Continue reading ‘Ocean acidification bad news for future fish, worse for coral; what will the ocean look like in 2100?’


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