Archive for September, 2016



A data-model synthesis to explain variability in calcification observed during a CO2 perturbation mesocosm experiment

A series of studies were conducted during the last two decades to investigate effects of ocean acidification (OA) on phytoplankton physiology, plankton ecology, and biogeochemical dynamics of marine ecosystems. Among those studies are experiments with tanks or bags called mesocosms, with some enclosed water volume that typically comprised a natural plankton community found in the surrounding environment. The Pelagic Ecosystem CO2 – Enrichment Study PeECE-I experiment is one such study, where mesocosms were perturbed and exposed to different carbon dioxide (CO2) concentrations to determine responses in growth dynamics of the coccolithophorid Emiliania huxleyi, a marine calcifying algae. The data from replicate mesocosms of PeECE-I show some natural variability and significant differences were revealed in the accumulation of particulate inorganic carbon (PIC) between mesocosms of similar CO2 treatments.

In our study we reanalyse PeECE-I data and apply an optimality-based model approach to understand most of the variability observed, with major focus on total alkalinity (TA) and calcification. We explore how much of the observed variability in data can be explained by variations of initial conditions and by the effect of CO2 perturbations. According to our model approach, changes in cellular calcite formation are resolved at the organism-level in response to variations in CO2. With a data assimilation (DA) method we obtain three distinctive ensembles of model solutions, with low, medium and high calcification rates. Optimised values of initial conditions turned out to be correlated with estimates physiological model parameters. The spread of ensemble model solutions captures most of the observed variability, corresponding to the combinations of parameter estimates. Optimised model solutions of the high CO2 treatment are shown to systematically overestimate observed PIC production. Thus, the simulated CO2 effect on calcification is likely too weak. At the same time our model results yield large differences in optimal mass flux estimates of carbon and of nitrogen even between mesocosms exposed to similar CO2 conditions.

Continue reading ‘A data-model synthesis to explain variability in calcification observed during a CO2 perturbation mesocosm experiment’

UW makes waves in ocean acidification

Photo credit: E. Carrington

Photo credit: E. Carrington

The San Juan archipelago, perhaps most famous for its pod of southern resident killer whales, is also home to the UW’s world-renowned biological field station, the Friday Harbor Laboratory (FHL).

Built in 1910 on the former Point Caution military reserve, FHL has grown from a single building to a sprawling campus with over a dozen specialized laboratories.

A waterfront trail, which meanders past the stand-alone research buildings, serves as a timeline of the facility’s growth. The farther along the trail you go, the newer the labs become. Eventually, the trail dead ends at the newest addition: the Ocean Acidification Environmental Laboratory (OAEL).

Interest in ocean acidification at the UW began with professor of oceanography Richard Feely. Through his work with the National Oceanic Atmospheric Administration’s (NOAA) Carbon Program, Feely highlighted worrisome trends in ocean chemistry and inspired scores of scientists to take a closer look.

“Ocean acidification was really off the radar for everyone 20 years ago,” said Emily Carrington, a professor of biology at the UW and the OAEL’s first director. “Largely because of [Feely’s] efforts and many others, the University of Washington and Washington State [University] are at the forefront of ocean acidification research, regionally and globally.”

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Climate resolve talk with a scientist: Paul Bunje

Paul Bunje is senior scientist for energy and environmental programs at XPRIZE, an awards organization based in Southern California. What does Dr. Bunje do? In his own words: “I work to help solve environmental grand challenges by inspiring and facilitating innovation.” Trained as an evolutionary biologist, Dr. Bunje was founding director of the Los Angeles Regional Collaborative for Climate Action and Sustainability. At XPRIZE, Dr. Bunje is helping to lead the organization’s work on climate change. He talked to Maya Bon for Climate Resolve about ocean acidification and hypoxia, an area of focus for XPRIZE — and what we can do about these threats.

Can you give us a background on ocean acidification — what it is, how it’s caused, what it does to the ocean, and how it relate to climate change?

Paul Bunje: Ocean acidification is essentially the evil twin of climate change, as it is also the consequence of carbon dioxide emissions. About one quarter of the CO2 that we’ve emitted into the atmosphere is absorbed by the world’s oceans. When you put CO2 into water, it forms carbonic acid, which in turn drives down the pH of seawater. The challenge is that this is happening globally — as more CO2 goes into the atmosphere, more goes into the ocean…. [and] upsets the chemical balance of carbonate ions, carbonic acid, and CO2, which changes the chemistry that sea creatures work within.

One of the first identified impacts were the shells of creatures that make their shells out of calcium carbonate — corals, mollusks, bivalves, some important phytoplankton such as coccolithophore, which produces a significant amount of oxygen for the planet. When this chemistry balance is upset, it becomes more difficult to get the carbonate out of the water and these creatures cannot make their shells. In extreme cases, the shells dissolve. There are interesting cases of this occurring with sea butterflies, a microscopic snail, because of ocean acidification. You can actually see their microscopic shells dissolving in water.

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Eutrophication accelerates carbonate dissolution under high pCO2 condition in coral reef ecosystem

Incubation experiments were carried out to determine the effect of eutrophication on carbonate dissolution under high pCO2 (partial pressure of carbon dioxide) condition in coral reef ecosystem at Sesoko Island, Okinawa, Japan. Short incubation (24 h under natural illumination) and long incubations (4 days under dark condition) were carried out using white coral skeleton (without attachment of living organism, control); natural rubble (with associated epilithic and endolithic communities) and natural rubble with addition of dissolve organic matter (glucose and coral mucus). Addition of DOM significantly enhanced bacterial abundance (t-test; p=0.01) and net respiration (t-test; p=0.0001) with increasing pCO2 levels (p < 0.05) under natural illumination. Consistent with increase in respiration, dissolution rates also increased from 136.22±2.04 to 652.38±4.51 µmolm-2d-1. Under dark condition, where photosynthesis was inhibited, dissolution of calcium carbonate further increased with addition of different level of DOM. In addition of DOM incubation bottles, bacterial abundance increased by 3~4 orders of magnitude and the dissolution rates increased by 2.5~10 times more than the control. The results suggest that availability of organic matter in the reefs will enhance metabolic activities (respiration) of microbial communities associated with coral rubble which ultimately increase dissolution of calcium carbonate.

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Effects of seawater acidification on the growth rates of the diatom Thalassiosira (Conticribra) weissflogii under different nutrient, light, and UV radiation regimes

Effects of ocean acidification (OA) on marine organisms are suggested to be altered by other environmental drivers, such as low nutrient, increased light, and UVR exposures; however, little has been documented on this aspect. Thalassiosira (Conticribra) weissflogii, a marine diatom, was used to examine the OA effects under multiple stressors on its growth. The specific growth rate was inhibited by low nutrient (LN), though it increased with increased sunlight regardless of the nutrient supplies. Presence of UVR reduced the maximal growth rate (μmax) in low CO2 (LC) conditions (both LN and HN) and inhibited the apparent growth light use efficiency (α) in the cells acclimated to LN under both low (LC) and high (HC) CO2 conditions. The HC-grown cells grew faster under HN and low light levels. Conclusively, presence of UVR with high solar radiation, LN and OA acted synergistically to reduce the diatom growth, though, in contrast UVR and OA enhanced the growth under HN.

Continue reading ‘Effects of seawater acidification on the growth rates of the diatom Thalassiosira (Conticribra) weissflogii under different nutrient, light, and UV radiation regimes’

Linking rising pCO2 and temperature to the larval development and physiology of the American lobster (Homarus americanus)

Few studies have evaluated the joint effects of elevated temperature and pCO2 on marine organisms. In this study we investigated the interactive effects of Intergovernmental Panel on Climate Change predicted temperature and pCO2 for the end of the 21st century on key aspects of larval development of the American lobster, Homarus americanus, an otherwise well-studied, iconic, and commercially prominent species in the northeastern United States and Atlantic Canada. Our experiments showed that larvae (stages I–III) and postlarvae (stage IV) reared in the high temperature treatments (19 °C) experienced significantly lower survival, developed twice as fast, and had significantly higher oxygen consumption rates, than those in ambient treatments (16 °C). Larvae from the ambient temperature/high pCO2 (750 ppm) treatment had significantly longer carapace lengths, greater dry masses in stages I–III and higher C: N ratios in stage IV than larvae from all other treatments. Stage IVs raised in the high pCO2 treatment at 19 °C had significantly higher feeding rates and swimming speeds than stage IVs from the other three treatments. Together these results suggest that projected end-century warming will have greater adverse effects than increased pCO2 on larval survival, and changing pCO2 may have a complex effect on larval metabolism and behaviour. Understanding how the most vulnerable life stages of the lobster life cycle respond to climate change is essential in connecting the northward geographic shifts projected by habitat quality models, and the underlying physiological and genetic mechanisms that drive their ecology.

Continue reading ‘Linking rising pCO2 and temperature to the larval development and physiology of the American lobster (Homarus americanus)’

Future climate stimulates population out-breaks by relaxing constraints on reproduction

When conditions are stressful, reproduction and population growth are reduced, but when favourable, reproduction and population size can boom. Theory suggests climate change is an increasingly stressful environment, predicting extinctions or decreased abundances. However, if favourable conditions align, such as an increase in resources or release from competition and predation, future climate can fuel population growth. Tests of such population growth models and the mechanisms by which they are enabled are rare. We tested whether intergenerational increases in population size might be facilitated by adjustments in reproductive success to favourable environmental conditions in a large-scale mesocosm experiment. Herbivorous amphipod populations responded to future climate by increasing 20 fold, suggesting that future climate might relax environmental constraints on fecundity. We then assessed whether future climate reduces variation in mating success, boosting population fecundity and size. The proportion of gravid females doubled, and variance in phenotypic variation of male secondary sexual characters (i.e. gnathopods) was significantly reduced. While future climate can enhance individual growth and survival, it may also reduce constraints on mechanisms of reproduction such that enhanced intra-generational productivity and reproductive success transfers to subsequent generations. Where both intra and intergenerational production is enhanced, population sizes might boom.

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Missing the boat: Critical threats to coral reefs are neglected at global scale

Coral reefs have experienced a global decline due to overfishing, pollution, and warming oceans that are becoming increasingly acidic. To help halt and reverse this decline, interventions should be aimed at those threats reef experts and managers identify as most severe. The survey included responses from 170 managers, representing organizations from 50 countries and territories, and found that respondents generally agreed on the two major threats: overfishing and coastal development. However, resource allocation did not match this consensus on major threats. In particular, while overfishing receives much attention, coastal development and its attendant pollution are largely neglected and underfunded. These results call for a re-examination of how resources are allocated in coral reef conservation, with more attention given to aligning how money is spent with what are perceived to be the primary threats.

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A first look at factors affecting aragonite compensation depth in the eastern Arabian Sea

Water column measurements suggest shoaling of aragonite saturation depths (ASD) throughout the world oceans, due to increase in greenhouse gas concentration. Past records of aragonite saturation state under different climatic conditions are required to assess the impact of climatic changes on shoaling/deepening of ASD. The preservation state of organisms having aragonite skeletons, is used to assess the past changes in aragonite saturation depths, with respect to the modern ASD. Here for the first time, we delineate and discuss the factors that affect the modern aragonite compensation depth (ACD) in the eastern Arabian Sea by using pteropod abundance in the surface sediments. A total of 78 spade core-top samples collected along seven latitudinal transects, covering the continental shelf, slope and abyssal region of the eastern Arabian Sea were used. Pteropods were picked from coarse fraction (≥ 63 μm). Based on the pteropod preservation, we report that in the eastern Arabian Sea, ACD lies at a water depth of ≤ 525 m, which matches with the chemically defined aragonite saturation depth. We further report that the ACD shoals from north to south. The zone of high pteropod abundance coincides with low %Corg. The increase in pteropod abundance in the outer shelf region coincides with the drop in dissolved oxygen concentration. The deeper limit of pteropod abundance lies in the center of the oxygen minimum zone with higher %Corg. Therefore, we suggest that the pteropod abundance in the eastern Arabian Sea is not always related with the lower dissolved oxygen, but is strongly influenced by %Corg. This first report of the pteropod based aragonite compensation depth estimates from the eastern Arabian Sea will help in assessing future changes in ACD under the influence of anthropogenic green-house gas emissions.

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Increased activity of lysozyme and complement system in Atlantic halibut exposed to elevated CO2 at six different temperatures

Ocean acidification and rising seawater temperature are environmental stressors resulting from the continuous increase of the atmospheric CO2 concentration due to anthropogenic activities. As a consequence, marine fish are expected to undergo conditions outside of their tolerance range, leading to physiological challenges with possible detrimental implications. Our research group has previously shown that exposure to elevated CO2 modulated the immune system of the Atlantic halibut. To further investigate this finding, we analysed non-specific immune components in blood plasma of Atlantic halibut (Hippoglossus hippoglossus) juveniles acclimated to six different temperatures (5, 10, 12, 14, 16 and 18 °C), and to water pH of 8.0 (control) or 7.6 (predicted for year 2100) for three months. Plasma ions (K+, Na+, Ca++, Cl−) and lactate concentrations were also measured. The analysis of plasma ions did not show any trends related to temperature or CO2 exposure, and the majority of the experimental fish were able to maintain ionic balance. The results show that both innate immune components (lysozyme and alternative complement system) had increased activities in response to elevated CO2, representing a CO2-related impact on the halibut’s immune system. The increased activity of lysozyme and complement system is possibly part of the acclimatization process, and might be protective.

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The 3rd Xiamen Symposium on Marine Environmental Sciences (XMAS), 9-11 January 2017, Xiamen, China

The ocean system is undergoing rapid and dramatic changes in response to global climatic and regional anthropogenic forcings. These drivers, including primarily temperature rise, intensified stratification, ocean acidification, eutrophication, and ocean deoxygenation, may, or already has, lead to fundamental changes in marine biogeochemistry, such as the carbon, nitrogen, phosphorus, and iron cycles, productivity and community shifts of marine microbes, and further impacts to fishery resources. These changes are affecting a broad range of goods and services provided to humans by marine ecosystems and are causing a number of marine environmental problems, particularly in coastal regions.

To foster knowledge and ideas exchange within the marine environmental science community and, in particular, to promote interdisciplinary studies, the State Key Laboratory of Marine Environmental Science (MEL, http://mel.xmu.edu.cn/en) of Xiamen University initiated the Xiamen Symposium on Marine Environmental Sciences (XMAS), with the overarching theme of The Changing Ocean Environment: From a Multidisciplinary Perspective. The first two symposia (http://mel.xmu.edu.cn/conference/1xmas, http://mel.xmu.edu.cn/conference/2xmas) were held in Jan 2014 and Jan 2015, attracting over 800 participants from more than 100 institutions across 14 countries.

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Increased levels of carbon dioxide could drive fish crazy, study finds

High levels of carbon dioxide could impair the brain chemistry of fish, scientists found.

Researchers from the University of Miami Rosenstiel School of Marine and Atmospheric Science and the ARC Center of Excellence for Coral Reef Studies at James Cook University found that increased concentrations of carbon dioxide in the ocean alters the brain chemistry of fish that may lead to neurological impairment.

“Coral reef fish, which play a vital role in coral reef ecosystem, are already under threat from multiple human and natural stressors,” Rachael Heuer, lead author of the study, said in a news release. “By specifically understanding how brain and blood chemistry are linked to behavioral disruptions during CO2 exposure, we can better understand not only ‘what’ may happen during future ocean acidification scenarios, but ‘why’ it happens.”

In the study published in the journal Scientific Reports, researchers collected spiny damselfish from the reefs off Lizard Island in Australia’s Great Barrier Reef. The fish were separated into two groups: one is exposed to ordinary CO2 “control conditions and the other exposed to elevated CO2 levels expected to occur by the year 2300. After the exposure, the two fish groups were subjected to a behavioral test, and brain and blood chemistry were measured.

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Tropical coral reefs lose their zooplankton through ocean acidification

Tropical coral reefs lose up to two thirds of their zooplankton through ocean acidification. This is the conclusion reached by a German-Australian research team that examined two reefs with so-called carbon dioxide seeps off the coast of Papua New Guinea. At these locations volcanic carbon dioxide escapes from the seabed, lowering the water’s acidity to a level, which scientists predict for the future of the oceans. The researchers believe that the decline in zooplankton is due to the loss of suitable hiding places. It results from the changes in the coral reef community due to increasing acidification.

Instead of densely branched branching corals, robust mounding species of hard coral grow, offering the zooplankton little shelter. In a study published on 19 September 2016 at the online portal of the journal Nature Climate Change, the researchers report that the impact on the food web of the coral reefs is far-reaching, since these micro-organisms are an important food source for fish and coral.

The volcanic carbon dioxide sources off the coast of Papua New Guinea are a unique natural laboratory. “Here, we can already observe under natural conditions how the reefs may change when the world’s oceans absorb more and more carbon dioxide from the atmosphere and the acidity of their water rises due to climate change,” says coral expert and study co-author Prof Claudio Richter of the Alfred Wegener Institute, the Helmholtz Centre for Polar and Marine Research.

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New York needs to act on ocean acidification

“The ocean acts like a sponge, absorbing most of the extra heat caused by our greenhouse gases. And it’s been growing warmer and more acidic for decades now. In other words, the very chemistry of our oceans is changing, which is risking marine life and rippling all the way up the food chain … This is not a far-off problem; it’s happening as we speak. It’s happening here in America.” – President Obama, at last week’s Our Ocean Conference

New York State needs Governor Cuomo to help prepare our state for the coming onslaught of a little known problem caused by more than a century of burning fossil fuels: ocean acidification.

It’s hard to imagine how we missed the connection for so long. Oceans naturally absorb carbon dioxide and, as we’ve increased the amount of carbon dioxide in the atmosphere by burning coal and oil, the basic chemistry of our oceans has become more acidic. Awareness of the impacts of ocean acidification – the so-called evil twin of global warming – is just beginning, but we know that acidic water makes it harder for many species of shell-building organisms, like clams, oysters, and scallops, to grow their protective coverings and survive.

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Ocean acidification influences the biomass and diversity of reef-associated turf algal communities

Projected ocean acidification will have a detrimental impact on coral reef ecosystems, where fleshy algae are expected to replace corals. Of particular importance to reef ecosystems are fleshy turf algal communities, which have the potential to overgrow corals; few studies have investigated the community structure and diversity of turfs to climate change. Here, we assessed the response of reef-associated turf algal communities from the Great Barrier Reef, Australia to three levels of ocean acidification. Biomass of turf communities was positively affected by increases in carbon dioxide (CO2), where turf communities grown under high CO2 had the greatest biomass. No effect of CO2 was found on mean turf organic content or genus richness. By contrast, turf community evenness and diversity (H′) increased under medium and high CO2 treatments. Our results indicate that increased turf growth under high CO2 will aid the overall expansion and growth of fleshy macroalgae in coral reef ecosystems, as opportunistic algae may have an advantage over other reef-associated species. Changes in turf community diversity will help provide insight into how macroalgal communities may be structured in the future, highlighting genera primed to take advantage of the changes in ocean chemistry associated with ocean acidification.

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Decreased photosynthesis and growth with reduced respiration in the model diatom Phaeodactylum tricornutum grown under elevated CO2 over 1800 generations

Studies on the long-term responses of marine phytoplankton to ongoing ocean acidification (OA) are appearing rapidly in the literature. However, only a few of these have investigated diatoms, which is disproportionate to their contribution to global primary production. Here we show that a population of the model diatom Phaeodactylum tricornutum, after growing under elevated CO2 (1000 μatm, HCL, pHT: 7.70) for 1860 generations, showed significant differences in photosynthesis and growth from a population maintained in ambient CO2 and then transferred to elevated CO2 for 20 generations (HC). The HCL population had lower mitochondrial respiration, than did the control population maintained in ambient CO2 (400 μatm, LCL, pHT: 8.02) for 1860 generations. Although the cells had higher respiratory carbon loss within 20 generations under the elevated CO2, being consistent to previous findings, they down-regulated their respiration to sustain their growth in longer duration under the OA condition. Responses of phytoplankton to OA may depend on the timescale for which they are exposed due to fluctuations in physiological traits over time. This study provides the first evidence that populations of the model species, P. tricornutum, differ phenotypically from each other after having been grown for differing spans of time under OA conditions, suggesting that long-term changes should be measured to understand responses of primary producers to OA, especially in waters with diatom-dominated phytoplankton assemblages.

Continue reading ‘Decreased photosynthesis and growth with reduced respiration in the model diatom Phaeodactylum tricornutum grown under elevated CO2 over 1800 generations’

The relative availability of inorganic carbon and inorganic nitrogen influences the response of the dinoflagellate Protoceratium reticulatum to elevated CO2

This work originates from three facts: 1) changes in CO2 availability influence metabolic processes in algal cells. 2) Spatial and temporal variations of nitrogen availability cause repercussions on phytoplankton physiology. 3) Growth and cell composition are dependent on the stoichiometry of nutritional resources. In this study we assess whether the impact of rising pCO2 is influenced by N availability, through the impact that it would have on the C/N stoichiometry, in condition of N sufficiency. Our experiments used the dinoflagellate Protoceratium reticulatum, which we cultured under three CO2 regimes (400, 1000 and 5000 ppmv, pH of 8.1) and either variable (the NO3− concentration was always 2.5 mmol • L−1) or constant (NO3− concentration varied to maintain the same Ci /NO3− ratio at all pCO2) Ci /NO3− ratio. Regardless of N availability, cells had higher specific growth rates, but lower cell dry weight and C and N quotas, at elevated CO2. The carbohydrate pool size and the C/N was unaltered in all treatments. The lipid content only decreased at high pCO2 at constant Ci /NO3− ratio. In the variable Ci /NO3− conditions, the relative abundance of Rubisco (and other proteins) also changed; this did not occur at constant Ci /NO3−. Thus, the biomass quality of P. reticulatum for grazers was affected by the Ci /NO3− ratio in the environment and not only by the pCO2, both with respect to the size of the main organic pools and the composition of the expressed proteome.

Continue reading ‘The relative availability of inorganic carbon and inorganic nitrogen influences the response of the dinoflagellate Protoceratium reticulatum to elevated CO2’

Surface and deepwater dissolved inorganic carbon and pH in the Northern Gulf of Mexico

The Gulf of Mexico is known for its numerous natural seeps as well as a very active drilling program for the oil located in its sediments. This study examines water column in an active drilling and seep region in two different years, assessing the carbonate system chemistry in the deep northern Gulf of Mexico waters. There were two summer cruises in the Northern Gulf of Mexico two years apart, 2012 and 2014. Over 350 samples were collected for DIC and TA measurements on the first cruise and 115 samples were collected on the second cruise. The remaining carbon system parameters, such as pH and pCO2, were determined for each sample. The cruises were compared to GOMECC cruises in nearby region and showed that surface DIC was statistically more variable for this sample region but surface TA was not as statistically variable, suggesting a larger biological activity gradient than in the GOMECC cruises. The Mississippi River plume extended into the sampling areas on both cruises but to different extents and directions, likely due to the 227% increased discharge rate between the two years. Saturation states of calcite and aragonite approach an average of one only in the densest water sampled, suggesting favorable values for calcite and aragonite structure builders. The deepwater in the northern Gulf of Mexico was statistically significant to similar density water in the Atlantic, suggesting that the deepwater has returned to pre spill conditions, according to the carbonate chemistry.

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“Mitigating acidification in coastal ecosystems: the challenges of implementation in the context of uncertainty”, ASLO 2017 Aquatic Sciences Meeting, 26 February – 3 March 2017, Honolulu, Hawai’i

Abstract submission deadline: 14 October 2016!

This session welcomes research focused on the challenges of variability and uncertainty associated with scaling OA mitigation to implementation. This session will also consider key lessons learned, best practices, and guidelines for future intervention research and practice.

Session rationale: Recent research has illuminated the biological impacts, geochemical drivers, and dynamics of ocean acidification in the coastal environment. Following our improved understanding of the impacts of acidification in coastal ecosystems, there has been increasing interest in local-scale biogeochemical approaches to mitigate, and potentially remediate, the problems of coastal acidification. Such approaches generally fit into three categories: (1) the restoration and enhancement of CO2 uptake provided by aquatic photosynthetic organisms, such as sea grasses and algae, (2) alkalinity buffering through the intentional dissolution of calcium carbonate, such as discarded bivalve shells, and (3) geochemical engineering by enhanced air-sea gas exchange. Interest in implementing mitigation approaches in state-level OA policies is rapidly increasing. Yet there remains substantial uncertainty about the heterogeneity, variability, and effectiveness of such approaches when scaled to the level of implementation. Such challenges include the durability of carbonate system interventions in naturally variable coastal ecosystems, and whether these changes translate into desired outcomes for target organisms in the context of multiple stressors.

Organizers: David Koweek , Carnegie Institution, Department of Global Ecology (dkoweek(at)stanford.edu) & Aaron Strong , University of Maine, School of Marine Sciences (aron.strong(at)maine.edu)

Further information and registration.

Workshop on ocean acidification and San Francisco Bay, 19-20 October 2016, San Francisco Estuary Institute

Estuarine acidification due to global carbon dioxide emissions and local eutrophication has the potential to have widespread impacts on marine ecosystems by reducing calcification—key to building shells, for example—in key marine organisms. Recently, the West Coast Ocean Acidification & Hypoxia (OAH) Science Panel recommended improved monitoring to assess biological impacts in the coastal ocean and estuaries. The current status and impacts of acidification on the San Francisco Bay and many other West Coast estuaries are largely unknown.

A workshop at San Francisco Estuary Institute on October 19-20 will convene forty scientists, managers, and representatives of local monitoring entities to assess whether acidification is a likely concern in SF Bay, and to identify its potential impacts to beneficial uses, cost-effective monitoring strategies, and potential management actions, including restoration. San Francisco Bay, as the largest estuary on the West Coast, will serve as a case study for how to approach the development of OAH monitoring strategies for West Coast estuaries.

The workshop attendance is already at capacity but the Organizing Committee will produce a publicly available technical report documenting the key outcomes.

Event address: San Francisco Estuary Institute, Main Conference Room, 4911 Central Avenue, Richmond, CA 94804

Further information.


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