Applications open: fourth winter school on ocean acidification and multiple stressors

Dates: 30 November – 11 December 2026

Location: IAEA Marine Environment Laboratories, Monaco.

Deadline for application through InTouch+ platform: 6 November 2026

The Winter School is organized by the IAEA OA-ICC in partnership with the Prince Albert II of Monaco Foundation through the OACIS Initiative (Ocean Acidification and other ocean Changes – Impacts and Solutions) and the Laboratoire d’Océanographie de Villefranche (LOV).

Introduction

Ocean acidification is a global environmental stressor that threatens marine life and the livelihoods of coastal communities. Ocean acidification is caused by increasing atmospheric carbon dioxide being absorbed by the ocean, resulting in changes to seawater carbonate chemistry, including a drop in pH. Due to global concerns about its consequences, ocean acidification is included in international policies such as Target 3 of UN Sustainable Development Goal (SDG) 14 and Target 8 of the Global Biodiversity Framework (GBF).

The IAEA’s Ocean Acidification International Coordination Centre (OA-ICC) supports IAEA Member States to minimize and adapt to OA and report towards SDG 14.3 and the GBF, with a strong focus on building capacity to study ocean acidification and related stressors and promoting international collaboration and coordination.

Ocean acidification is not happening in isolation, but in combination with other human-driven pressures, including pollution, warming, and oxygen loss. The impact of multiple ocean stressors on marine life and ecosystem function is not well understood, yet this information is crucial to inform adaptation strategies that might minimize negative effects on organisms, ecosystems, and associated socioeconomic benefits.

The Fourth Winter School on Ocean Acidification and Multiple Stressors is part of the capacity building program of the OA-ICC.  This two-week training course will provide participating scientists with a thorough understanding about key concepts and experimental design used to study the impacts of ocean acidification in the context of additional stressors.

Objectives

The aim of the Winter School is to train early-career scientists who already have experience researching ocean acidification on how to study acidification in the context of other co-occurring stressors. Through lectures and practical exercises in the laboratory, the students will gain understanding of key concepts in multiple-stressor research (e.g., What is a stressor? What is a mode of action? What is an interaction?), purposeful experimental design, and analysis of complex datasets. During the course, participants will collaborate on a joint laboratory experiment to elucidate the effects of three simultaneous drivers on marine organisms.

Target Audience

The course is open to 10-12 trainees. Priority will be given to early-career scientists with experience in marine environmental change with a focus on ocean acidification; a background in biological sciences is preferred. At least one publication in the field of marine environmental change is required.

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Participation and Registration

All persons wishing to participate in the event have to be designated by an IAEA Member State or should be members of organizations that have been invited to attend.

In order to be designated by an IAEA Member State or invited organization, participants are requested to submit their application via the InTouch+ platform (https://intouchplus.iaea.org) to the competent national authority (Ministry of Foreign Affairs, Permanent Mission to the IAEA or National Atomic Energy Authority) or organization for onward transmission to the IAEA by 6 November 2026, following the registration procedure in InTouch+:

1. Access the InTouch+ platform (https://intouchplus.iaea.org):

  • Persons with an existing NUCLEUS account can sign in to the platform with their username and password;
  • Persons without an existing NUCLEUS account can register here.

2. Once signed in, prospective participants can use the InTouch+ platform to:

  • Complete or update their personal details under ‘Complete Profile’ and upload the relevant supporting documents;
  • Search for the relevant event under the ‘My Eligible Events’ tab;
  • Select the Member State or invited organization they want to represent from the drop-down menu entitled ‘Designating Authority’ (if an invited organization is not listed, please contact InTouchPlus.Contact-Point@iaea.org);
  • If applicable, indicate whether a paper is being submitted and complete the relevant information;
  • If applicable, indicate whether financial support is requested and complete the relevant information (this is not applicable to participants from invited organizations);
  • Based on the data input, the InTouch+ platform will automatically generate the Participation Form (Form A) and/or the Grant Application Form (Form C);
  • Submit their application.

Once submitted through the InTouch+ platform, the application, together with the auto-generated form(s), will be transmitted automatically to the required authority for approval. If approved, the application, together with the applicable form(s), will automatically be sent to the IAEA through the online platform.

NOTE: The application for financial support should be made, together with the submission of the application, by 6 November 2026.

For additional information on how to apply for an event, please refer to the InTouch+ Help page. Any other issues or queries related to InTouch+ can be sent to InTouchPlus.Contact-Point@iaea.org.

Selected participants will be informed in due course on the procedures to be followed with regard to administrative and financial matters.

Participants are hereby informed that the personal data they submit will be processed in line with the Agency’s Personal Data and Privacy Policy and is collected solely for the purpose(s) of reviewing and assessing the application and to complete logistical arrangements where required. The IAEA may also use the contact details of Applicants to inform them of the IAEA’s scientific and technical publications, or the latest employment opportunities and current open vacancies at the IAEA. These secondary purposes are consistent with the IAEA’s mandate.

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Additional Requirements

Participants should have a university degree in marine chemistry, biology, oceanography or a related scientific field, and should be currently involved in or planning to study the ecological impact of multiple stressors, including ocean acidification. Experience with the R software is strongly encouraged.

Selection will be based on merit and interest. Applications should include:

 * A motivation letter with a short description of the candidate’s research interests and how the course would benefit the applicant’s current or future research on ocean acidification and multiple stressors (max one A4 page)

  * CV with publication list

Continue reading ‘Applications open: fourth winter school on ocean acidification and multiple stressors’

The impact of the CO2 fertilization effect in seagrasses: a comparative perspective with terrestrial plants

This article comments on:

Pazzaglia J, Marín-Guirao L, Ambrosino L, Pes K, Costa M, Barrote I, Silva J, Procaccini G. 2025. Handling the heat: ocean acidification mitigates the effects of marine heatwaves on Posidonia oceanica seedlings. Journal of Experimental Botany 76, 6958–6973. https://doi.org/10.1093/jxb/eraf276.

Seagrass meadows are among the world’s most ecologically and economically important marine ecosystems. Although they cover only 0.1% of the seafloor, they sequester carbon at rates rivalling tropical rainforests, protect coastlines, and support marine biodiversity (do Amaral Camara Lima et al., 2023). Yet they are declining globally due to anthropogenic pressures including coastal development, pollution, and climate change (Waycott et al., 2009; Dunic et al., 2021). While ocean acidification and ocean warming are pervasive stressors under accelerating global change, Pazzaglia et al. (2025) have demonstrated that elevated dissolved CO2 may enhance seagrass resilience by increasing thermal tolerance in Posidonia oceanica seedlings through the CO2 fertilization effect.

Continue reading ‘The impact of the CO2 fertilization effect in seagrasses: a comparative perspective with terrestrial plants’

Long-term coral responses to high CO2: insights from volcanic vents and semi-enclosed bays

This chapter provides a comprehensive review of natural laboratories used to study the effects of ocean acidification (OA) on coral reefs, emphasizing volcanic CO2 vents and semi-enclosed bays. It examines key environmental conditions at these study sites and their implications for coral physiology, biodiversity, and reef resilience. Two prominent natural analogues are highlighted: the Shikine Island warm-temperate shallow CO2 vent system in Japan and the semi-enclosed lagoon of Bouraké in New Caledonia.

Shikine Island represents a unique high-latitude coral environment influenced by the Kuroshio Current. The island’s CO2 vents provide a natural setting to investigate the community level effects of ocean acidification and how elevated CO2 levels interact with ocean warming and influence coral tropicalization. Findings suggest that while some corals persist at high CO2 levels, biodiversity declines significantly, with sensitive species unable to establish stable populations. Corals growing in these conditions exhibit reduced calcification, and the community structure shifts toward simpler, lower-complexity ecosystems dominated by turf algae. These results indicate that ocean acidification may act as a constraint on the poleward expansion of tropical corals, counteracting warming-induced range shifts.

In contrast, the semi-enclosed lagoon of Bouraké experiences extreme environmental fluctuations in pH, oxygen, and temperature, providing a window into the multifactorial stressors coral reefs may face in the future. Despite prolonged exposure to acidified, hypoxic, and thermally variable waters, corals in Bouraké demonstrate remarkable resilience. The system harbors diverse coral assemblages, with species exhibiting metabolic adjustments, increased heterotrophy, and shifts in symbiotic algae communities. This site suggests that coral ecosystems can develop physiological adaptations that enhance their survival in extreme conditions, offering valuable insights into the potential for long-term acclimatization.

By comparing these two contrasting natural analogues, this chapter highlights the complex interplay between acidification, warming, and other environmental stressors on coral reefs. While both sites provide critical insights into the future of coral ecosystems, they also underscore the urgent need for continued research and conservation efforts to mitigate the effects of climate change on marine biodiversity.

Continue reading ‘Long-term coral responses to high CO2: insights from volcanic vents and semi-enclosed bays’

Genomic responses of fishes to ocean acidification: insights from volcanic CO2 seeps

Extreme and marginal reef environments provide valuable opportunities to examine the effects of altered seawater parameters that resemble predicted end-of-century ocean conditions under climate change. Volcanic CO2 seeps, in particular, have proven useful for studying the effects of ocean acidification (OA) in natural settings. In this chapter, we present a case study from a volcanic CO2 seep at Shikine Island, Japan, investigating the genomic response of the neon damselfish (Pomacentrus coelestis) to OA conditions. We examined transcriptomic profiles from brain and gill tissues collected across two seasons (July and November) and compared them to samples from multiple control sites to assess consistent patterns of gene expression under elevated CO2. Our results found that genes involved in blood oxygen regulation, immune response, and circadian rhythm were differentially expressed across seasons and tissues, suggesting their key role in the response to OA in P. coelestis. We also detected seasonal shifts in gene expression patterns, highlighting the complexity of the physiological responses to OA in natural environments. Many of the differentially expressed genes align with findings from previous laboratory and field studies, reinforcing the value of volcanic CO2 seeps for OA research. Finally, we discuss the challenges of working in natural seep environments, including variability across control sites and seasons, and emphasize the future potential of CO2 seeps for advancing our understanding of fish responses to ocean acidification.

Continue reading ‘Genomic responses of fishes to ocean acidification: insights from volcanic CO2 seeps’

Seasonal prediction of ocean biogeochemistry in the northeast U.S. large marine ecosystem using a regional ocean-biogeochemistry model

We couple an ocean biogeochemical model to a regional ocean model of the Northwest Atlantic and assess the potential skill of bottom dissolved oxygen, aragonite saturation state, and pH forecasts along the Northeast U.S. Continental Shelf using a reanalysis-forced model run as the true biogeochemical state. Across 30 years of retrospective forecasts initialized four times per year, the model has substantial potential skill for all three variables, with skill generally highest in the deep Gulf of Maine and lowest in the shallower Mid-Atlantic Bight and Georges Bank. Forecasts initialized in January and April benefit from the insulation of the bottom from the unpredictable atmosphere by stratification and tend to have greater skill at longer lead times. Using two case studies, we show how predictable variations in ocean temperature, salinity, and currents are associated with predictable variability in bottom biogeochemistry in both the Mid-Atlantic Bight and Gulf of Maine. The forecast model evaluated in this study has been developed as an operational prototype for NOAA’s Changing Ecosystems and Fisheries Initiative, with the goal of applying the forecasts to improve the yield and sustainability of living marine resources.

Continue reading ‘Seasonal prediction of ocean biogeochemistry in the northeast U.S. large marine ecosystem using a regional ocean-biogeochemistry model’

Ocean acidification in the Northwestern gulf of America

The physical and chemical oceanographic properties of the Gulf of Mexico (GOM, recognized by the United States as the Gulf of America) remain incompletely characterized. Evidence suggests that GOM carbonate chemistry is mainly influenced by physical mixing, changes in atmospheric CO2 levels, and localized processes including eutrophication, hypoxia, and upwelling. The purpose of this dissertation is to increase sampling coverage in the northwestern Gulf (nwGOM), analyze decadal trends using both new and existing data, explore two cross-shelf transects from surface to bottom over 16+ years, and develop statistical models to estimate pH and ΩAragonite from hydrographic measurements. The research incorporates both laboratory and computational analyses across all chapters, including data collected from sensors (moored and shipboard). Samples for carbonate chemistry parameters were analyzed in the lab following standard practices. Computational work was conducted using RStudio, Python, and MATLAB. The statistical models can estimate water column pH and ΩAragonite with R2 values over 0.93 with small mean square errors (<0.0005 and <0.04 for pH and ΩAragonite, respectively), demonstrating their effectiveness. Key findings include seasonal patterns and long-term temperature trends in the nwGOM, as well as spatial variability and upward shoaling of the aragonite saturation horizons (ΩAragonite) from full water-column transects. These results reveal that subsurface waters are experiencing both declining dissolved oxygen (DO) and a shoaling saturation horizon. At the same time, surface waters also show progressive acidification, marked by decreasing pH and rising CO2 partial pressure (pCO2), despite significant seasonal fluctuations and an overall warming trend. The collected data provide essential spatial and temporal coverage of carbonate chemistry. The numerous changes occurring in the Gulf highlight the importance of quantifying these variations to guide resource management and conservation efforts.

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Assessing the projected impacts of climate change on underwater cultural heritage in the Nuevo Gulf, Argentina

Highlights

  • CMIP6 models can quantify future climate threats to UHC sites in Northern Patagonia.
  • Projected ∼2.1 °C warming by 2100 will accelerate corrosion and wood-boring activity.
  • Ocean pH drop (4.5%) will accelerate corrosion and destabilise calcareous concretions.
  • Salinity changes remain negligible across all projected climate change scenarios.
  • UHC managers profit locally by integrating in situ data with climate model outputs.

Abstract

Climate change presents a significant and increasing threat to Underwater Cultural Heritage (UCH) worldwide. To better understand the risks that this entails, this study examines the archaeological wreck site of the schooner Emma in the Nuevo Gulf, Northern Patagonia, Argentina. It addresses a geographic research gap and the complex interaction of multiple environmental stressors. Using the information from state-of-the-art climate models, we assess the potential impacts in the near and far future of specific environmental parameters including temperature, salinity, dissolved oxygen, and pH, all relevant at the wreck site’s location, and identified to play a driving role in its conservation.

Results consistently demonstrate a clear trend toward a warmer and more acidic marine environment, with the greatest changes projected under the highest-emission scenario. In that case, sea temperature at the wreck site’s depth increases by approximately 14.5% (∼2.1 °C) by the end of this century, which would accelerate corrosion rates of metals and intensify the activity of wood-boring organisms. In parallel, acidification is projected to increase with pH decreasing by approximately 4.5% (∼0.36 units), contributing to the destabilisation of protective concretions and the intensification of metal corrosion. While dissolved oxygen is projected to decrease (∼3.92%) and salinity remains nearly unchanged, the synergy of warming and acidification suggests the wreck of the Emma will face a more aggressive environment by 2100. The methodology integrates a characterisation of the site’s materials, the main deterioration processes involved and the surrounding environmental context. This study also provides UCH managers with a climate-projection-based assessment of future slow-onset climate-related marine environmental pressures and the likely conservation implications that will inform the development of conservation and monitoring strategies for the Emma and other shipwrecks in the Nuevo Gulf and adjacent coastal areas.

Continue reading ‘Assessing the projected impacts of climate change on underwater cultural heritage in the Nuevo Gulf, Argentina’

Developmental and behavioural responses of the non-indigenous amphipod Melita palmata (Montagu, 1804) at individual and population under reduced pH scenarios

Highlights

  • Reduced pH disrupted early development, causing brood failure and incomplete eggs.
  • Broods and cohorts showed high mortality, limited growth and irregular sex traits.
  • Reduced pH altered behaviours, with sex-specific substrate use and slower escape.
  • Multilevel responses suggest reduced pH may affect population stability and invasion.

Abstract

Non-indigenous species (NIS) and reduced pH conditions are key stressors shaping coastal biodiversity and population performance. We examined how decreased pH influences developmental, demographic, and behavioural traits of the non-indigenous amphipod Melita palmata from the Mar Chiquita coastal lagoon (Argentina). Individuals, broods, and cohorts were reared under current pH (8.07) and a reduced pH scenario (7.5) to assess egg maturation, brood and cohort survival, growth, sexual differentiation, habitat use, and escape responses. Reduced pH disrupted early developmental processes, leading to incomplete egg maturation, brood failure, and the absence of post-breeding moults. Broods and cohorts exhibited low survival, limited growth, and irregular sexual differentiation, and no ovigerous females were detected. Behavioural responses were also altered, with sex-specific shifts in substrate use and slower escape reactions. Together, these multilevel responses indicate that decreased pH induce physiological and behavioural constraints that propagate into demographic instability. Such response at both individual and population levels suggests that reduced pH conditions could limit the capacity of M. palmata to sustain populations and may influence its future invasion dynamics, although field-level consequences remain to be determined. These findings highlight how early acting individual responses can scale up to shape population persistence under projected coastal acidification scenarios.

Continue reading ‘Developmental and behavioural responses of the non-indigenous amphipod Melita palmata (Montagu, 1804) at individual and population under reduced pH scenarios’

Hydroclimatic controls on nearshore pollution and ecosystem stress along a tropical urban coastline

Highlights

  • Integrated indices revealed nutrient, microbial, and organic pollution patterns.
  • Urbanization and monsoon hydroclimate jointly intensified coastal degradation.
  • Seasonal eutrophication and oxygen depletion were strongly temperature driven.
  • Microbial contamination increased during post-monsoon runoff and tourism.
  • Multi-index approach clarified pollution processes in tropical coastal waters.

Abstract

Urbanizing coasts face escalating pollution from anthropogenic sources and climate change. This study provides an integrated seasonal assessment of coastal water quality along the Visakhapatnam coast, India, using a multi-index framework combining the Canadian Council of Ministers of the Environment Water Quality Index (CCME-WQI), Trophic State Index (TSI), and Pollution Index (PI). Surface water samples were collected from eleven representative locations including fishing settlements, recreational beaches, leisure beaches, and industrial-port zones. Physicochemical factors, nutrients, chlorophyll-a, and microbial indicators were assessed using multivariate statistical analysis to determine significant environmental stressors. Results revealed clear spatial and seasonal differences driven by monsoon runoff interacting with localized urban pollution sources. Jalaripeta exhibited the lowest water quality, with low WQI scores (<40), eutrophic to hypereutrophic status (TSI >56), and elevated microbial contamination associated with untreated sewage and inadequate flushing. In comparison, RK Beach and the Harbour area showed moderate degradation, characterized by intermittent nutrient influx, spikes in microbes, localized hypoxia associated with tourism pressure and port activities. Principal Component Analysis also revealed that nutrient-microbe enrichment, thermal-biological productivity, and organic matter breakdown are major environmental gradients influencing water quality variability. The findings indicate that the interplay between urbanization and seasonal hydroclimate intensifies environmental stress along the Visakhapatnam coast. This integrated multi-index framework provides as a valuable decision-support tool for identification pollution hotspot and adaptive management of tropical urban coasts under increasing climate and anthropogenic pressures.

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Functional saturation of Earth’s habitable domains: constraints on land systems and potential in marine environments

In this context, functional saturation is defined as the state in which a system’s capacity to sustain additional productive or regulatory functions becomes constrained due to cumulative anthropogenic pressures, even if some physical space remains available. This review examines whether the progressive contraction of terrestrial plant communities under intensifying anthropogenic pressure can be functionally compensated by the expansion of marine macroalgal systems in a high-CO2 world. Integrating perspectives from Earth system ecology, biogeochemistry, and spatial analysis, the study evaluates three interdependent dimensions: the saturation of habitable terrestrial space, the relative openness yet ecological constraint of marine environments, and the dynamic coupling between atmospheric CO2 and ocean chemistry. The synthesis reveals a fundamental asymmetry between land and ocean systems. Terrestrial ecosystems are undergoing direct structural transformation through land-use change, resulting in a measurable contraction of ecologically functional space and increasing transgression of planetary boundaries. In contrast, marine systems retain substantial geometric space but are subject to diffuse, cumulative stressors, particularly in productive coastal zones where macroalgal communities are most viable. Elevated CO2 exerts dual effects on marine primary producers, simultaneously enhancing photosynthetic potential while intensifying ocean acidification, with temporally lagged responses mediated by air–sea exchange dynamics. Although macroalgae may exhibit localized increases in productivity, their capacity to provide long-term carbon sequestration and ecosystem stability remains inherently limited due to rapid biomass turnover, susceptibility to regime shifts, and the interaction of multiple stressors. The available evidence suggests that marine macroalgal expansion is unlikely to fully compensate for terrestrial vegetation loss at global ecological and biogeochemical scales. Instead, the Earth system is undergoing a net reduction in biospheric resilience, characterized by declining terrestrial complexity and increasingly unstable marine productivity. These findings challenge assumptions of compensatory redistribution of primary production and underscore the necessity of preserving terrestrial ecosystems alongside mitigating pressures on marine environments.

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Gravity-driven feeding currents in veliger larvae of the eastern oyster

Feeding by marine invertebrate larvae depends critically on the low-Reynolds-number fluid mechanics of the feeding currents they generate. Yet the relative importance of gravity-driven versus drag-driven mechanisms in small invertebrate larvae has remained unresolved. Here, high-speed microscale imaging, micro-particle image velocimetry (μPIV), and an analytical axisymmetric Stokes-flow model are combined to quantify the feeding currents of free-swimming veliger larvae of the eastern oyster Crassostrea virginica. Despite their small body size (<330µm), the larvae possess a high excess density (∼181g/m3), shifting the force balance such that gravity-driven feeding currents dominate. μPIV measurements reveal flow fields with first-order (Stokeslet-type) spatial decay, yielding ecologically sufficient body-volume-specific maximal clearance rates of ∼2.5×106/day. These values agree with predictions from the Stokes-flow model, which decomposes the clearance into gravity-driven and drag-driven components and shows that the former consistently outweighs the latter across observed swimming speeds. The model further explains how slow swimming modulates clearance by ±44% relative to hovering. Together, these results demonstrate that C. virginica veligers operate in a gravity-dominated feeding regime similar to that of larger calanoid copepods, and that their feeding strategy is shaped by an interplay of excess weight, swimming kinematics, and ciliary propulsion. This work highlights the fundamental role of gravity in larval feeding mechanics and underscores the need to incorporate excess weight when evaluating form-and-function relationships in marine invertebrate larvae, particularly for shelled bivalve and gastropod larvae with high excess density.

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Tiny oyster larvae rely on gravity to feed

High-speed imaging reveals how oyster larvae’s dense shell helps them feed—and may offer clues to why ocean acidification threatens their survival

Eastern oysters (Crassostrea virginica) are native to the Atlantic coast of North America and are an important species for coastal ecosystems and fisheries. (Photo by Daniel Hentz, ©Woods Hole Oceanographic Institution)

Photos and video available for use with credits can be found here.

Woods Hole, Mass. (September 16, 2026) — Eastern oyster larvae are only 100–300 micrometers long, but their dense calcium carbonate shells make them substantially heavier than the surrounding seawater. A new study led by the Woods Hole Oceanographic Institution (WHOI) shows that this excess weight allows gravity to drive the feeding currents the larvae use to bring food to their mouths, a finding that reveals a critical role for gravity in how these tiny animals feed and survive.

The study, published in Physical Review Fluids, challenges the long-standing assumption that larvae this small rely primarily on the drag produced by swimming to generate the feeding currents that carry food toward their mouths. While it may be true in the case of many small plankton, oyster larvae prove to be an exception, placing them in the same gravity-dominated feeding regime as much larger copepods and revealing an unexpected role for their shells in helping them feed. The key difference is that drag depends primarily on the larva’s movement through the water, but gravity depends on the difference in density between the larva and the surrounding seawater.

“This tells us that the shell is doing more than just protecting the animal,” explained Houshuo Jiang, a senior scientist at WHOI and sole author of the study. “It is actually helping the larva feed. That means anything that changes the shell could also change how the larva gets its food.”

Jiang captured the larvae’s feeding behavior using a high-speed microscale imaging system (HSMIS) developed in his laboratory. Rather than observing larvae under a conventional microscope, the system uses long-working-distance optics and a high-speed camera to record animals swimming freely in a larger volume of seawater. He also added tiny tracer particles to the seawater and used a technique called micro-particle image velocimetry to track how those particles moved around the larvae, allowing him to measure the invisible currents generated as the larvae feed.

“Usually, when you use a microscope, you need a lot of light, and if you put a lot of light on these tiny animals, you can heat the water and change their behavior,” Jiang said. “And conventional cameras are not fast enough to capture these very rapid movements. So we developed a system that uses a low-heat red LED and a high-speed camera that can record 2,000 frames per second. That lets us watch the larva in a larger volume of water without disturbing it and actually see how the water moves as it feeds.”

These findings offer a possible explanation for results from earlier experiments that raised bivalve larvae in space. In a 1999 study, scientists raised bivalves in microgravity and found that larvae reared without normal gravity tended to have lower feeding and growth rates and were in poorer condition than larvae kept under normal gravity. At the time, the physical reason for those differences was not clear.

“Thanks to high-speed imaging, we now see that gravity is essential for their feeding,” Jiang said. “If a larva is dealing with a stressor that affects its ability to build a dense shell, that could also affect the physical force that helps it feed. Understanding that connection gives us a better way to think about how environmental stressors can affect larvae at one of the most vulnerable stages of their lives.”

Oysters are particularly vulnerable to ocean acidification, which changes seawater chemistry and makes it harder to build calcium carbonate shells. This study’s findings suggest that if acidification alters shell formation enough to reduce a larva’s density relative to seawater, it could also weaken the gravity-driven feeding current it relies on to bring food to its mouth, potentially affecting young oysters.

Eastern oysters also face other challenges including pollution, disease, and overfishing. According to NOAA Fisheries’ Commercial Fishing Landings database, the commercial harvest of eastern oysters in the United States fell by about $15.2 million, or 7.2%, from 2023 to 2024.

“Ultimately, this could help us better understand what determines whether oyster larvae survive and become part of the adult population,” Jiang said. “That matters for fisheries and aquaculture because the number of larvae that survive each year helps determine the oysters available to harvest in the future. If environmental stressors affect both shell formation and feeding, we need to understand those effects to better predict how oyster populations will respond to a changing ocean.”

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Evaluating ocean acidification and hypoxia model outputs as an undergraduate intern at the Northeast Fisheries science center

Ocean acidification from an interns viewpoint.

Me at my desk working through code to produce figures for my presentation. Credit: NOAA Fisheries/Grace Davis

My name is Ned Gable and I am currently an Environmental Science and Chemistry double major at the University of Mary Washington. I was born and raised in Richmond, Virginia.

I am a PADI Divemaster who is passionate about marine ecology and the biogeochemical components of the ocean. I plan to pursue a Ph.D. in chemical oceanography coming out of college.

Interning at the Northeast Fisheries Science Center as a Young Researcher

Receiving word that I had won the Hollings Scholarship in early spring 2025 was one of the most exhilarating moments of my life. I was finally getting my shot at contributing to an organization that I admired, with nationwide impacts on science and our understanding of the natural world.

The workplace of my selected internship was at the Northeast Fisheries Science Center in Narragansett, Rhode Island. The building was smaller than I had expected, with only one floor, but there were a plethora of passionate scientists working there who made each day interesting and exciting. Right down the hall from my cubicle was the fish dissection lab, where they would dissect mackerel and squid for gonads and otolith research.

My project involved compiling large amounts of observational data across time in the Northeast U.S. Shelf and comparing it to model outputs (MOM6-COBALT) of acidification and hypoxia. The complicated part was figuring out exactly how to compare raw observational data from specific times and coordinates to a gridded model output. While it took a few weeks of research and testing, I came up with a method to match observational data to model grids, average that data within each grid by day, and then compare the model outputs within ±1 day and ±1 grid to each averaged observation using Python code.

My favorite figure – A mapped output of the difference between the model outputs of dissolved oxygen and the observations across five regions of the Northeast US Shelf
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Reducing nitrate loads to the St. Lawrence river could mitigate hypoxia and acidification in its deep estuary and gulf

Hypoxia in marine systems is expanding worldwide due to anthropogenic activities. Deep waters of the St. Lawrence Estuary and Gulf are rapidly deoxygenating (∼1 mmol O2 m−3 y−1), driven by changes in Atlantic water-mass intrusion and nutrient‐fueled remineralization, and are simultaneously acidifying (∼0.004 pH unit y−1). These changes alter biogeochemical cycles and degrade habitats, causing biotic and economic consequences. Using a coupled physical-biogeochemical model, we tested whether watershed-scale nitrate reductions could mitigate deep‐water deoxygenation and carbonate-system degradation. Three nitrate‐reduction scenarios reduced riverine St. Lawrence River nitrate loads by about 11%, 30%, and 50% (−2.8, −7.5, and −11.7 mmol N m−3, respectively). Relative to the baseline simulation, these scenarios increased dissolved oxygen concentrations (DO) (+1.6, +4.3, and +6.7 mmol O2 m−3), pH (+0.004, +0.010, and +0.016), and aragonite saturation state (Ωarag) (+0.003, +0.009, and +0.015) in the deep Laurentian Channel (⩾175 m). The volume of deep waters with DO saturation <30% decreased by 3%, 8%, and 13% (−27, −75, −122 km3), while volumes with pH <7.65 declined by 1.0%, 2.8%, and 4.5% (−22, −60, −96 km3). Severely corrosive waters (Ωarag <0.6) dropped by 1.4%, 3.7%, and 5.9% (−26, −71, −112 km3). Over 2014–2024, modelled improvements exceeded small interannual variability but remained within seasonal amplitudes of deep DO concentrations (∼11 mmol O2 m−3) and pH (∼0.015 units), nevertheless pointing to a detectable management signal. Although nutrient‐driven improvements remained smaller than climate‐forced trends, modelled nitrate load reductions could offset ∼56% and 80% of recent observed oxygen and pH declines, respectively, while reducing hypoxic and acidified (pH and Ωarag) water volumes. These findings provide quantitative evidence that watershed‐scale nitrogen mitigation, through improved agricultural practices and wastewater nitrogen removal, which necessitates cooperation across jurisdictions, can alleviate hypoxia and acidification in deep coastal ecosystems, making nutrient management an essential complement to climate adaptation strategies.

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Ocean warming could cut omega-3 levels in seafood, study finds

Global analysis finds rising ocean temperatures could reduce omega-3 fatty acids across marine food webs, with implications for seafood nutrition.

A global study has found that ocean warming could reduce levels of omega-3 fatty acids in fish and other marine organisms, potentially affecting the nutritional value of seafood. Photo by Damon Hall.

Ocean warming could reduce levels of omega-3 fatty acids in fish and other marine organisms, potentially affecting the nutritional value of seafood, according to a global study.

Researchers analyzed 489 experiments from 143 published studies involving 132 marine species, including algae, invertebrates and fish. The study, published in Global Change Biology, examined how warming and ocean acidification affect fatty acids throughout marine food webs. The researchers found that warming generally reduced omega-3 fatty acids, with larger declines occurring as temperatures increased.

“Our new study shows many fish and other seafood will become less rich in omega-3s over time, due to rising ocean temperatures as the climate changes,” the researchers wrote in an article for The Conversation. “In fact, we found omega-3 could drop by 50 percent under very high warming scenarios. This is very bad news for human health but also for the health of other animals in the food web.”

Marine algae produce EPA and DHA, two important omega-3 fatty acids, and sit at the base of marine food webs. Those nutrients move through the food chain as algae are eaten by other organisms, which in turn are consumed by fish and larger animals.

“If EPA and DHA levels get disrupted along the food chain, less of those crucial fatty acids are available for animals higher up – including humans,” the researchers wrote.

The effects varied among species and experiments, but the overall analysis found warming had a stronger effect on fatty acids than ocean acidification. “We found ocean acidification had less impact on fatty acids than warming, suggesting rising temperature is the dominant driver of this problem,” the researchers wrote.

The results should not be read as a prediction that omega-3 levels in seafood will fall by 50 percent across the board. The study combined results from controlled experiments, and responses varied among species and experimental conditions. The researchers called for more long-term studies under realistic environmental conditions to improve predictions of how climate change will affect the nutritional quality of marine organisms.

The findings could have implications for fisheries and aquaculture because omega-3 availability is important to both the nutritional value of seafood and the health of marine organisms. The study’s authors said anticipating climate-driven nutritional declines will be important for fisheries management, aquaculture and food security.

The researchers also pointed to better use of fish processing byproducts as one way to make more of existing sources of omega-3. With up to 80 percent of fish parts discarded during food processing, they suggested those parts could be used to produce omega-3-rich fish oil or as nutritional ingredients in aquaculture feed.

“Given the projected declines in nutrition into the future, these wasted fish parts could be better utilized,” the researchers said. “This might, for instance, include making fish oil products rich in omega-3 and other nutrients, or using these fish parts as nutritional aquaculture feed.

Read the full study here.

Continue reading ‘Ocean warming could cut omega-3 levels in seafood, study finds’

Environmental regulation of interspecific interactions among macrobenthic seaweeds and its implications for community phase transition

Macrobenthic seaweeds are key species in temperate and boreal nearshore rocky ecosystems, and their interspecific interactions profoundly affect the species composition, spatial distribution and dynamic succession of the community. This paper systematically reviews the mechanisms of interspecific competition and facilitative effects among macrobenthic seaweeds. We also examine their environmental regulation and impacts on community phase transitions. Competition mainly centers on three major resources: light, space and nutrients. It manifests as an asymmetric hierarchical structure, in which canopy-forming species exert a disproportionate repressive effect on lower algal layers through light competition. Facilitative effects are realized through several mechanisms. These include canopy shading to mitigate heat stress and water loss, physical structure building to create complex habitats, and nutrient retention with chemical microenvironment regulation. Moreover, the relative strengths of facilitation and competition shift systematically across environmental stress gradients. Multi-trophic level regulation further shapes community diversity maintenance mechanisms through the suppression of dominant species by vegetative predators and the cascading effect of top predators on vegetative predators. In the context of global change, physiological asymmetries driven by oceanic heat waves are tilting the competitive balance in favor of opportunistic turf algae. These algae form a lock-in state through the triple positive feedbacks: physical barriers, biogeochemical deterioration, and chemosensory exclusion. This significantly decreases the resilience of algal field recovery. Tropical coral-macroalgae phase transition is highly consistent with the degradation of temperate algal fields in terms of driving logic. They follow the law of coupling resource competition imbalance, downward regulatory relaxation, and positive feedback lock-up. This paper suggests several priorities for future research. Studies should focus on the nonlinear response of multifactor interaction, the quantitative correlation between key functional traits and community resilience, and the establishment of a cross-ecosystem comparison framework. These efforts will provide theoretical support for predicting and adaptively managing offshore ecosystems under global change.

Continue reading ‘Environmental regulation of interspecific interactions among macrobenthic seaweeds and its implications for community phase transition’

Explorers climate module 6.3 lesson plan: the impacts of climate change on ocean animals & habitats

Abstract

This project aims to ignite curiosity and develop environmental empathy, this lesson empowers students to become ocean advocates by exploring how climate change impacts marine species across global climate zones. By translating complex scientific phenomena—such as ocean acidification, Blue Carbon, and the Whale Carbon Pump—into creative drama and news broadcasts, students build critical scientific literacy, collaboration skills, and a proactive commitment to protecting our shared ocean planet.

Description

Children will understand how global warming and ocean acidification impact marine animals and their natural habitats. They will explore how marine ecosystems capture carbon (focusing on Blue Carbon and the Whale Carbon Pump). They will work collaboratively to communicate scientific concepts through a creative news broadcast or drama performance.

Continue reading ‘Explorers climate module 6.3 lesson plan: the impacts of climate change on ocean animals & habitats’

Explorers climate module 6.5 lesson plan: ocean acidification & shells

Abstract

This project aims to inspire curiosity and scientific inquiry, this hands-on lesson allows pupils to investigate the chemical impact of ocean acidification on marine life. By modeling how acidic environments dissolve calcium carbonate shells and eggshells, pupils analyse data, connect chemical reactions to atmospheric carbon dioxide emissions, and identify practical solutions to protect vulnerable marine ecosystems.

Description

The children will learn to explain the concept of ocean acidification and how excess atmospheric 〖”CO” 〗_2changes ocean chemistry, to describe the chemical reaction between acids and calcium carbonate shells (“Acid”+”Carbonate”→”Carbon Dioxide”+”Water”+”Salt” ), and to conduct a fair test, gather quantitative/qualitative data, and record daily scientific observations. They will connect experimental results to real-world threats facing shell-building marine organisms (e.g., Irish mussels, oysters, and cold-water corals).

Continue reading ‘Explorers climate module 6.5 lesson plan: ocean acidification & shells’

Spatiotemporal water quality dynamics in Southern U.S. coastal reserves: a long-term perspective

Water quality monitoring in estuarine ecosystems is essential for assessing the health and sustainability of these dynamic coastal habitats, which are increasingly vulnerable to environmental change and human impacts. This study aims to characterize long-term trends and seasonal drivers of seven key water quality parameters: temperature, salinity, dissolved oxygen (DO), pH, chlorophyll-a (Chla), nitrate + nitrite (NOx), and phosphate (PO4) across four southern U.S. National Estuarine Research Reserves (Apalachicola Bay, Grand Bay, Mission-Aransas, and Weeks Bay) to identify which reserves and processes are most vulnerable to climate and anthropogenic change. Using two decades of data (1995–2020) and applying Generalized Additive Models (GAMs), we identified significant spatial and temporal patterns linked to environmental and anthropogenic factors. Results revealed a warming trend in Weeks Bay (+0.1035 °C/year, P = 0.0013), a salinity decline in Grand Bay (−0.1699 PSU/year, P = 0.033), and a salinity increase in Apalachicola Bay (+0.2055 PSU/year, P = 0.003). DO concentrations peaked in spring and dropped in summer, reflecting seasonal nutrient inputs. Grand Bay exhibited the highest Chla variability (CV=131.48%). NOx concentrations declined in Grand Bay (−0.0003 mg/L/year, P = 0.0162), while PO4 levels remained relatively stable. pH trends suggested localized acidification, particularly in Mission-Aransas (−0.0071/year, P = 0.0016). GAM results emphasized the combined effects of long-term and seasonal changes, with site-specific differences. These findings provide critical insights into estuarine functioning and highlight the need for regionally tailored management strategies to enhance resilience and biodiversity conservation in U.S. coastal reserves.

Continue reading ‘Spatiotemporal water quality dynamics in Southern U.S. coastal reserves: a long-term perspective’

Frameworks for ocean management in a changing climate


Date: Wednesday, 25 November 2026

Time: 19:00–20.00

Location: Statsraaden Bar & Reception

Free and open for all. No registration required.

What happens when oceans change faster than the frameworks designed to manage them? Climate change is altering marine ecosystems, moving fish stocks, and increasing uncertainty for decision-makers. In this event, two researchers will share their knowledge on how climate change has an impact on the legal governance and management of ocean resources.

About the event (held in English)

Climate change is increasingly challenging the management and legal governance of marine resources by altering ecosystems, species distributions, and the assumptions on which existing governance frameworks are built. The North Sea and the Barents Sea, both highly productive and intensively managed regions, illustrate these pressures clearly.

Warming waters, changing ocean circulation, ocean acidification, and declining sea ice are reshaping marine ecosystems. In the Norwegian Sea, key commercial species such as  mackerel are shifting their distributions, In the Barents Sea, rapid warming and reduced ice cover allow boreal species to expand into traditionally Arctic areas, affecting species interactions in the ecosystem.  

These changes create a growing mismatch between dynamic ecosystems, legal governance  and fixed management boundaries. In the Norwegian Sea, complex international quota arrangements are strained as stocks move across national exclusive economic zones. In the Barents Sea, long-standing cooperative management faces new challenges as species distributions change and industrial activity increases. 

Climate change also exposes the limits of single-species management. Altered growth rates, recruitment, and species interactions make it harder to rely on historical data, strengthening the case for ecosystem-based and precautionary approaches. Overall, climate change places pressure on marine legal governance to become more adaptive, flexible, and forward-looking, requiring stronger international cooperation, better integration of climate science, and management systems designed for continuous change rather than stable conditions.

In this event, two researchers will share their knowledge on how climate change has an impact on the legal governance and management of ocean resources.

Talks

  • The Law of the Ocean: Governance, Justice, and Sustainability: by Rosa Manzo, postdoctoral fellow, Faculty of law, University of Bergen (UiB)
  • Climate change and fisheries management with some examples from the Northeast Atlantic: by Bjarte Bogstad (external link), Researcher, Institute of marine research (IMR/HI)

The speakers

Rosa Manzo holds a PhD in climate change law and has extensive experience in environmental and climate law. She has worked on topics such as carbon storage, climate justice, and international agreements. She has strong knowledge of the CSR (Corporate Sustainability Reporting Directive), the CSDDD (Corporate Sustainability Due Diligence Directive), and the Carbon Border Adjustment Mechanism (CBAM). 

Bjarte Bogstad (external link) has many years of experience in stock assessment and advisory work for fish stocks in the Barents Sea. He is stock coordinator for Northeast Arctic cod (cod in the Barents Sea), and has participated in the Norwegian–Russian Fisheries Commission since 2010. He has long-standing experience in collaboration with the Russian research institute PINRO in Murmansk, including responsibility for the joint database on fish stomach content, and is the Norwegian representative to ICES ACOM since 2019.

Organisers

Ocean Science Bar is a collaboration between Statsraad Lehmkuhl, the University of Bergen, the Institute of Marine Research, NORCE, and the Nansen Center. At the Statsraaden Bar & Reception you are welcome to enjoy highlights from marine research and ocean related issues in informal and relaxing surroundings.

Continue reading ‘Frameworks for ocean management in a changing climate’

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