Marine biodiversity loss, fishing, and climate change

08 - 09 December 2025 09:00 - 17:00 The Royal Society Free Watch online
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Discussion meeting organised by Professor Richard Sanders, Professor Alex Poulton, Professor Stephanie Henson, Dr Emma Cavan, and Professor Alessandro Tagliabue.

The twin crises of biodiversity loss and rapid climate change are often considered as inextricably linked, a perspective largely developed based on terrestrial systems. In the ocean this linkage has been largely overlooked and this meeting will address this gap to recognise the role of ocean biodiversity loss in regulating climate and delivering food security.

Poster session

There will be a poster session from 5pm on Monday 8 December. If you would like to present a poster, please submit your proposed title, abstract (up to 200 words), author list, and the name of the proposed presenter and institution to the Scientific Programmes team. Acceptances may be made on a rolling basis so we recommend submitting as soon as possible in case the session becomes full. Submissions made within one month of the meeting may not be included in the programme booklet.

Attending the event

This event is intended for researchers in relevant fields.

  • Free to attend
  • Both virtual and in-person attendance is available. Advance registration is essential
  • Lunch is available on both days of the meeting for an optional £25 per day. There are plenty of places to eat nearby if you would prefer to purchase food offsite. Participants are welcome to bring their own lunch to the meeting

Enquiries: Scientific Programmes team.

Organisers

  • Professor Richard Sanders

    Professor Richard Sanders

    Professor Richard Sanders currently serves as the Director of the Integrated Carbon Observing System (ICOS) Ocean Thematic Centre (OTC) in NORCE (the Norwegian Research Centre), and the Bjerknes Centre for Climate Research (BCCR) in Bergen, Norway. He maintains an active research portfolio including coordinating OceanICU, a grant focused on the role industrial processes play in controlling Ocean C storage. Recently, they have begun to address the challenge of how multiple observing systems can work together to address key ocean science questions and Professor Sanders is leading TRICUSO, an EU grant focused on integrating effort from European Research Infrastructures to quantify the Southern Ocean carbon sink.

    Prior to his move to Bergen, Professor Sanders served as Chair of the Ocean Biogeochemistry and Ecosystems (OBE) Research Group at the UK National Oceanography Centre. They developed a programme of Biological Carbon Pump research addressing key questions around iron limitation of carbon export in the Southern Ocean, Twilight Zone Carbon cycling and the solubility pump. Core actions included leading the departmental science programme, raising funds, overseeing publications, maintaining financial control over the department, advocating for the department, mentoring and managing & deputising for the Director of Research. Prior to becoming Department Chair, he ran a personal research group which contained one/ two postdocs, one technician, one/ two research fellows and several graduate students.

    Professor Sanders has spent over 2 years at sea on NERC vessels including 3 cruises as chief scientist (CROZEX in 2005, and Twilight Zone cruises to the PAP site in 2009 and the Southern Ocean in 2017). Lead PI on NERC Large Grant COMICS (Controls over Ocean Mesopelagic Carbon Storage) and NERC Cross Centre proposal LOCATE (Land Ocean Carbon Transfers).

  • Professor Alex J Poulton

    Professor Alex Poulton

    Professor Poulton is a sea-going marine scientist exploring the quantitative links between plankton diversity and biogeochemical cycles. Professor Poulton uses field observations and experiments to examine how biomineralising plankton influence the cycling of elements essential for marine life, such as carbon, nitrogen, silica, and iron. As a field scientist he has worked across the global ocean, from the tropics to the poles and from the coast to the open ocean, participating in 23 expeditions aboard national and international research vessels. His current research focus is on the production and loss processes associated with marine carbonates, and how they respond to natural and anthropogenic pressures. Professor Poulton did a PhD and postdoc at the University of Southampton, and then a NERC fellowship at the National Oceanography Centre (NOC) and subsequently became a member of staff at the NOC. In 2017 he left NOC and took up a position in Heriot-Watt’s new Global Research Institute, the Lyell Centre for Earth and Marine Science, a joint venture between NERC, the Scottish Funding Council and Heriot-Watt University. Professor Poulton heads the OceanCANDY (Carbon and nutrient dynamics) research group at Heriot-Watt University. Professor Poulton heads the OceanCANDY (Carbon and nutrient dynamics) research group at Heriot-Watt University, is the co-convenor of the Biogeochemistry Forum for MASTS (Marine Alliance for Science and Technology for Scotland) and from October will become the chair of the UK SCOR (Scientific Committee on Oceanic Research) panel (he is currently the Vice-Chair).

  • Professor Stephanie Henson

    Professor Stephanie Henson

    Professor Stephanie Henson is a Principal Scientist at the National Oceanography Centre and Honorary Professor at the University of Southampton. She leads a large, active research group in global biogeochemical oceanography. Her particular research interests aim at understanding the natural variability and climate change effects on phytoplankton populations, and subsequent impacts on the biological carbon pump. Her research exploits autonomous vehicles, satellite and in situ data, as well as output from biogeochemical models. In 2024, she received the European Geosciences Union’s Fridtjof Nansen medal for “outstanding research into the ocean’s role in the carbon cycle, built on her extraordinary ability to combine diverse observational data with novel biogeochemical models.” She was a lead author on the Intergovernmental Panel on Climate Change’s 6th Assessment Report, on the chapter “Carbon and other biogeochemical cycles and feedbacks”.

  • Dr Emma Cavan

    Dr Emma Cavan

    Emma is an Associate Professor at Imperial College London based in the Department of Life Sciences at Silwood Park. Her expertise lies with carbon cycling by marine life, specifically within the ocean biological carbon pump. She is particularly interested in the role of zooplankton, Antarctic krill and their faeces in sinking carbon to the deep ocean, microbial turnover of carbon and sequestration times. She is also interested in the impacts of fishing on oceanic carbon, and co-chairs an ICES working group/workshop on this subject.

  • Professor Alessandro Tagliabue

    Professor Alessandro Tagliabue

    Professor Tagliabue is a Professor at the University of Liverpool and an ocean biogeochemist, interested in how the cycling of resources in the sea affects biological activity and vice-versa. He is particularly interested in trace micronutrients and how they interact together to shape primary production, ecosystem structure and the global carbon cycle. His science links numerical models, at both global and idealised scales, with both fieldwork and synthesis of datasets. He is heavily involved in the international GEOTRACES programme, he is a lead author on the IPCC Special Report on Oceans and Cryosphere in a Changing Climate and is a member of the governing council of the UK Challenger Society for Marine Science. He is also UK Chair for SCOR and sits on the Royal Society Global Environment Research Committee.

Schedule

Chair

Professor Richard Sanders

Professor Richard Sanders

Norwegian Research Centre, Norway

09:00-09:05 Welcome by the Royal Society and lead organiser
09:05-09:30 The biodiversity double-edged sword: climate change has negatively impacted natural systems, but nature-based solutions are essential to a climate resilient pathway

Climate change is but the latest in a series of ever-increasing anthropogenic pressures on natural systems. I will give a brief overview of observed impacts of recent climate change in natural systems stemming from the most recent IPCC 6th Assessment Report. Similarities and differences between marine and terrestrial systems will be highlighted in terms of observed impacts on species, ecosystems and their services. I will briefly touch on how these changes in natural systems are already having negative effects on society, particularly increasing risks of diseases and food security. In terms of solutions space, achieving climate stability within the next century requires both emissions reductions and uptake of atmospheric carbon. While technological solutions have been invaluable for emissions reductions, they are insufficient and costly when it comes to drawing down atmospheric carbon. Nature-based solutions continue to be the most efficient in the near-term, cost-effective, and comprehensive means of stabilizing global climate. The IPCC concluded that climate resilient development fundamentally relies upon safeguarding natural biodiversity and associated healthy ecosystem functioning to achieve both adaptation and mitigation targets. Based on dozens of modeling studies coupled with long-term field studies and experiments, IPCC concluded that "the resilience of biodiversity and ecosystem services at a global scale depends on effective and equitable conservation of approximately 30% to 50% of Earth’s land, freshwater and ocean areas, including currently near-natural ecosystems (high confidence)."

Professor Camille Parmesan

Professor Camille Parmesan

Centre national de la recherche scientifique, France

09:30-09:45 Discussion
09:45-10:15 Examining trade-offs and synergies in the marine food-climate-biodiversity nexus

The ocean’s capacity to sustainably, equitably, and safely produce food is declining due to biodiversity losses driven by overexploitation, climate change, and other human-induced stressors such as pollution. While solutions like fisheries management, aquaculture, and marine protected areas have been proposed to reverse these declines, recent global analyses reveal growing trade-offs and inequities across seafood production, biodiversity conservation, and climate action. This talk explores the application of integrated models—linking climate, biodiversity, seafood production, and economic impacts—to assess how solution portfolios can achieve sustainable and equitable food and conservation goals under climate change. These models incorporate scenarios accounting for both direct and indirect drivers, including ocean conditions, demographic shifts, seafood demand and pricing, fisheries governance, and aquaculture development. Projections indicate that achieving sustainable seafood security and biodiversity goals will require ambitious action across multiple fronts: reducing fishing effort, advancing sustainable aquaculture, expanding marine protected areas, and strengthening climate mitigation. Climate change particularly threatens the capacity to provide nutrient-rich seafood and restore biodiversity and biomass in low and middle-income tropical nations and vulnerable communities in extra-tropical regions. The findings highlight the synergies and trade-offs in pursuing food, climate, and biodiversity targets. The presentation emphasises the need for equity- and conservation-focused ocean governance and for limiting global warming to below 1.5°C, and underscores the value of participatory scenario modelling to co-develop resilient, just, and sustainable marine conservation strategies.

Professor William Cheung

Professor William Cheung

The University of British Columbia, Canada

10:15-10:30 Discussion
10:30-11:00 Break
11:00-11:20 Exploring controls on phytoplankton diversity using a numerical model

Phytoplankton are the base of the marine foodweb and play important roles in biogeochemical cycles, such as the export of carbon from the surface oceans. These organisms are incredibly diverse, spanning many orders of magnitude in size, and have many different ecological biogeochemical roles. Though crucial parts of the earth's system we still have very limited understanding of the global patterns of diversity, what controls these patterns, and how plankton will respond to a warming ocean. In this talk I will describe some numerical modelling and theoretical approaches to addressing these issues. We utilise key phytoplankton traits (eg size) to model diverse plankton populations globally and question what physical and biological drivers set diversity. We show that regional patterns of supply of multiple nutrients, trophic interactions, and the transport by water parcels are key to maintaining different aspects of biodiversity, such as number of co-existing size classes, functional groups, and thermal norms. But each of these drivers will be altered in the future changing ocean. We will examine some of these predicted changes and how the model suggests plankton community structure may be altered in a future world.

Dr Stephanie	Dutkiewicz

Dr Stephanie Dutkiewicz

Massachusetts Institute of Technology, USA

11:20-11:30 Discussion
11:30-11:50 New insights into global marine biodiversity from genomic and imaging data collected during the Tara Oceans expedition

The Tara Oceans expedition (2009-2013) pioneered a global pan-ecosystemic strategy to systematically study the ocean's largest ecosystem: the plankton. This expedition sampled the microscopic majority of marine life, spanning seven orders of magnitude in size from viruses to zooplankton, across 210 sites worldwide to create an unprecedented view of the microbial ocean. Driven by the need to understand life's complexity and ocean processes driving it, the project established a holistic methodology to sample and analyse it. This involved high-throughput DNA sequencing and automated quantitative imaging, which generated extensive open- access datasets. This resulting resource provides a critical "time zero point" for understanding the 21st century planktonic ecosystem and the environmental conditions driving their compositions and distributions. Key insights on biodiversity estimates across viruses, prokaryotes, phytoplankton, and protists will be discuss. We will further explore how these microbes govern community ecology, define the intricate biogeography of our oceans, and shape essential biogeochemical cycles, offering necessary context for assessing future climate change impacts.

Dr Lionel Guidi

Dr Lionel Guidi

Centre national de la recherche Scientifique, France

11:50-12:00 Discussion
12:00-12:20 Drivers of coral reef biodiversity

Coral reefs host vast number of species, but studies of reef diversity have traditionally focused on large, well-known and conspicuous taxa. Meanwhile, a multitude of small eukaryotic and prokaryotic taxa that are found hidden within the three-dimensional structure of reefs, the cryptobiota, remain understudied. This is despite the cryptobiota representing the majority of reef diversity and being important for reef function and persistence. Understanding how biogeographical, environmental and anthropogenic drivers shapes this group of organisms is imperative for forecasting future trends in reef taxonomic and functional biodiversity as reefs continue to degrade worldwide. This talk will highlight some of our key findings from studying the drivers of reef cryptobiota diversity across the world. By combining 370 sequencing datatsets across 143 sites, spanning five oceanic regions, we show that reef connectivity (+), habitat (-), fishing (+), and cyclone activity (+) best predict global eukaryotic richness on tropical reefs. However, we find that phyla-level richness responses to predictors are region specific and highlight the groups of organisms that may dominate reefs in the future. While we show that anthropogenic stress can increase eukaryotic diversity, different patterns are observed for prokaryotes. We show that eukaryotic richness and temperature are the dominant drivers of prokaryotic richness, with thermal tipping points that can shift bacterial richness on reefs. This work underscores the importance of standardised global sequencing datasets and cross-domain studies to elucidate the ecosystem-scale impacts on complex stressors on reefs.

Dr Emma Ransome

Dr Emma Ransome

Imperial College London, UK

12:20-12:30 Discussion

Chair

Professor Alex J Poulton

Professor Alex Poulton

Norwegian Research Centre, Norway

13:30-14:00 Variable linkages between biodiversity and stoichiometry in the plankton

Ocean systems are characterised by diverse phytoplankton assemblages that themselves vary on a range of time-scales, but the question remains how phytoplankton biodiversity is reflected in the stoichiometry of particulate matter, the Redfield Ratio, in the ocean. In the open ocean it is generally concluded that the linkage between biodiversity and stoichiometry is through the variability in larger phytoplankton (eg diatoms) to smaller picophytoplankton (eg cyanobacteria). At the Bermuda Atlantic Time-series Study (BATS) site, this is generally the case with a seasonal increase in particulate organic carbon to phosphorus (POC:P) ratios that align with the seasonal accumulation of Prochlorococcus biomass. A similar pattern is observed over longer time series records, where again at BATS a multi-year increase in the POC:P ratio is aligned with the dramatic reduction in the presence of larger phytoplankton. The same observation cannot be said for spatial relationships between phytoplankton biodiversity and stoichiometry where despite similar patterns in phytoplankton assemblages, variability in the physical environment induces a complex interplay between biodiversity and phytoplankton physiological acclimation. A broader ocean look at the relationships between phytoplankton physiology, biodiversity, and plankton stoichiometry support a similarly complicated relationship mediated by ocean physics. These relationships are not just restricted to the tropical and subtropical latitudes. With ocean warming, populations of cyanobacteria, Synechococcus, are becoming more prevalant in Arctic ecosystems and already having a demonstrated impact on stoichiometry. The impacts of these interactions on marine biogeochemistry and the functioning of ocean food webs is only now beginning to be understood.

Dr Michael Lomas

Dr Michael Lomas

Bigelow Laboratory for Ocean Sciences, USA

14:00-14:15 Discussion
14:15-14:45 Warming-driven shifts in North Atlantic plankton

The Continuous Plankton Recorder (CPR) survey provides the longest and most spatially extensive plankton time-series in the North Atlantic, essential for detecting long-term biodiversity changes. Using CPR data from the Labrador Sea and North-West Atlantic, we show that since the 1980s, warming has driven increased diatom abundance at higher latitudes, where enhanced stratification and a weakened Labrador Current have reduced light limitation. Meanwhile, diatom abundance has declined in subtropical regions due to intensified nutrient limitation.

Ecological niche models suggest this trend may soon reverse, with nutrient constraints increasingly outweighing light availability, leading to an overall decline in diatoms and a shift towards more elongated taxa and dinoflagellates, signalling a potential tipping point toward reduced productivity and carbon export in the Subpolar Gyre (SPG).

These findings highlight how shifts in plankton communities could cascade through marine ecosystems, affecting food webs and carbon cycling, given varying carbon export efficiencies among species. Long-term datasets provided by the CPR alongside enhanced measurements, remain vital for tracking these dynamics, improving our ability to predict and respond to emerging biophysical shifts in the ocean.

Dr Clare Ostle

Dr Clare Ostle

The Marine Biological Association, UK

14:45-15:00 Discussion
15:00-15:30 Break
15:30-15:50 Bio-GO-SHIP: A platform to monitor ocean biodiversity

Marine plankton are an essential component of the earth climate system, form the base of the oceanic food web and thereby play an important role in influencing food security and contributing to the Blue Economy. Despite their importance, open ocean biological properties are significantly under-sampled in time and space compared to physical and chemical properties. This lack of information hampers our ability to understand the role of plankton in regulating in biogeochemical processes and fuelling higher trophic levels, now and in future ocean conditions. Traditionally, many of the methods used to quantify biological and ecosystem essential ocean variables (EOVs), measures that provide valuable information on the ecosystem, have been expensive and labour- and time-intensive, limiting their large-scale deployment. In the last two decades, however, new technologies have been developed and matured, making it possible to greatly expand biological ocean observing capacity. This talk will present recent advances in building international coordination to incorporate routine open ocean observations of marine biological properties and processes into the existing GO-SHIP decadal repeat hydrography program. Existing challenges in observing technology and infrastructure and the progress that can be achieved over the next decade with expanded observations of ocean biology will be discussed.

Dr Sophie Clayton

Dr Sophie Clayton

National Oceanography Centre, UK

15:50-16:00 Discussion
16:00-16:20 Incorporating mixotrophy and microbial functional diversity into ocean biogeochemical models

Most large-scale ocean biogeochemical models rely on highly simplified and discrete representations of plankton, structured around a strict distinction between phytoplankton and zooplankton across a limited number of immutable plankton functional types. This discrete approach overlooks the empirical reality that the ocean microbiome is functionally far more diverse, with individual species occupying a continuum of ecological strategies. As an illustrative case, the widespread prevalence of mixotrophic organisms in the ocean calls into question an understanding of ocean biogeochemistry that assumes a strict dichotomy between photosynthetic phytoplankton and heterotrophic zooplankton. In this talk I shall discuss how modelling approaches that describe the marine microbiome in terms of continuously varying traits - rather than as a discrete selection of functional groups - is well suited to addressing this functional diversity. Where mixotrophy has been included in models, it can be seen that access to nutrients from prey can support larger cell sizes, longer food chains, and more efficient carbon export. I will explore how these findings impact ocean biogeochemistry and climate at the global scale, over long time periods. I will also discuss how such models are impact by crude underlying assumptions, and what empirical constraints are needed to bring down large uncertainties. This talk will therefore focus on recent efforts to include mixotrophy and greater functional diversity in trait-based and adaptive ecosystem models, and will explore what these models can teach us, what their limitations are, and what kinds of data are needed to make further progress.

Dr Ben Ward

Dr Ben Ward

University of Southampton, UK

16:20-16:30 Discussion
16:30-17:00 Poster flash talks

Chair

Dr Emma Cavan

Dr Emma Cavan

Imperial College London, UK

09:00-09:30 Biodiversity in Twilight Zone functioning

The ocean's mesopelagic of 'twilight' zone (~200m to 1000m) is one of the largest habitats on this plant, and home to an abundant and diverse fauna. The species inhabiting this zone posses a multitude of behavioural, physiological, and structural adaptations that allow them to thrive in this cold, dark, and relatively food-poor environment. Twilight zone organisms influence the cycling of nutrients and long-term storage of carbon in the ocean and are a conduit for energy flow between depth zones, functions that will be affected by climate warming and exploitation by humans. Professor Steinberg will discuss important ways in which biodiversity and abundance affects the structure of mesopelagic food ways in which biodiversity and abundance affects the structure of mesopelagic food webs and carbon cycling using examples from contrasting ecosystems in the North Atlantic, North Pacific, and Southern Ocean. Examples will illustrate how species vertical zonation and diel migration affects the export of organic matter, and how some species paly an outsized role in carbon export or other ecosystem functions. The importance of ocean time series observations and new technologies for detecting change in mesopelagic biodiversity and function will be stressed and knowledge gaps will be identified for future research.

Professor Deborah Steinberg

Professor Deborah Steinberg

Virginia institute of Marine Science, USA

09:30-09:45 Discussion
09:45-10:15 Linking ecosystem structure and production to carbon sequestration

The sinking of detrital organic matter is the main contribution of living ocean ecosystems to climate regulation. The modelling of this “biological pump” in contemporary Earth System Models commonly assume that the dominant component is dead photosynthetic bacteria because they have the fastest life cycle. However, due to their small size dead bacteria sink slowly and are remineralised before reaching the sea floor. It has recently become clear that higher organisms, multicellular zooplankton and fish, are also important contributors to the biological carbon pump. Even though their rate of production of sinking faecal pellets is slow, the pellets are large and sink rapidly into the ocean interior, where the carbon is sequestered over long time. Here, Professor Andersen will use simple metabolic arguments to demonstrate how organisms of different sizes and trophic levels contribute to the biological carbon pump. The talk will augment the theoretical arguments with simulations of detailed models of unicellular plankton, multicellular zooplankton, cephalopods, and fish. The presentation will argue that understanding the biological carbon pump requires that we describe the entire ecosystem, from bacteria to whales, to quantify the contributions of each organism group in the ecosystem, and how they interact. Such full ecosystem models are required to understand how the climate regulating ability of the ocean’s ecosystem will change under future climates, and how it is affected by human interventions.

Professor Ken H Andersen

Professor Ken H Andersen

Technical University of Denmark, Denmark

10:15-10:30 Discussion
10:30-11:00 Break
11:00-11:20 Speaker to be confirmed
11:20-11:30 Discussion
11:30-11:50 Oceanographic drivers of carbon storage in European seagrass beds

Salt marshes, mangroves, and seagrass meadows are vegetated coastal marine ecosystems that remove atmospheric carbon dioxide (CO2) through photosynthesis and trap allochthonous carbon from adjacent terrestrial and marine sources. Despite covering a small fraction of the Earth’s surface, these “blue carbon” ecosystems bury carbon at disproportionately high rates, making them relevant to climate mitigation. Seagrass meadows are found along many European coastlines, but currently no countries have included them in their emission inventories and climate plans. One reason for this relates to the challenge of mapping seagrass habitats and estimating carbon stocks. We examine whether oceanographic data products, including those derived from satellites, can be used to estimate organic carbon stocks in seagrass meadows and support the development of a mapped product. Relevant abiotic and biotic variables for seagrass carbon storage were identified and datasets downloaded from NASA and Copernicus and spatially matched to seagrass sediment organic carbon measurements in the EURO-CARBON database. A suite of models was tests to identify the top predictors of seagrass organic carbon storage. We found high model explanatory power across the range of tested models (R2 > 0.8), with sea surface wave height, phosphate concentration, near-surface pH, bottom temperature, and remote sensing reflectance at 443 nm as some key predictors. Mixed species seagrass beds showed reduced carbon storage in comparison to monospecific beds. Policy needs for reporting carbon stocks are growing, and we show how remote sensing and global oceanographic data products can contribute to mapping blue carbon benefits in Europe.

Dr Natalya Gallo

Dr Natalya Gallo

Norwegian Research Centre, Norway

11:50-12:00 Discussion
12:00-12:20 Can mesopelagic fish become a safe, sustainable and profitable food source? Implications for managing ocean spaces for biodiversity and climate

The mesopelagic zone (200–1000 m depth) spans over 60% of the world’s oceans and harbors immense yet poorly understood biodiversity. It plays a crucial role in marine food webs, with fish biomass estimates exceeding those of all capture fisheries combined. Mesopelagic fish also play a key role in the biological carbon pump through diel vertical migrations that transport carbon from surface waters to the deep ocean.

Aquaculture is the world’s fastest-growing food sector. Mesopelagic fish have been proposed as a potential alternative feed source for aquaculture, with the potential to alleviate pressure on other fisheries while feeding the growing human population.

This presentation reviews results from the EU MEESO Horizon 2020 project, which used an ecosystem-based approach to investigate whether two of the most well-studied mesopelagic species (Maurolicus muelleri and Benthosema glaciale) could become a safe, sustainable, and profitable aquaculture feed.

It presents advances in mesopelagic sampling and trawl technologies, abundance estimation, processing methods, and understanding of food web interactions, vital rates, and carbon sequestration processes. Persistent uncertainties remain regarding biological reference points, stock productivity, and the ecological and climatic consequences of harvesting over space and time.

Current evidence suggests that large-scale mesopelagic fisheries could pose biodiversity risks through bycatch, alter trophic dynamics (at least regionally), and disrupt carbon export pathways.

The results highlight the need for precautionary, ecosystem-based management, supported by area based management and policy frameworks such as the BBNJ Agreement and the Global Biodiversity Framework.

Dr Mary Wisz

Dr Mary Wisz

Technical University of Denmark, Denmark

12:20-12:30 Discussion

Chair

Professor Stephanie Henson

Professor Stephanie Henson

National Oceanography Centre, UK

13:30-14:00 Fossil biodiversity and ecosystem function: insights from marine plankton

The fossil record offers critical insights into how biodiversity, biogeography, and ecosystem function respond to climate change over geological timescales. Planktonic foraminifera, with their exceptional fossil preservation, global distribution, and ecological diversity, provide a uniquely powerful system for examining these long-term dynamics in the open ocean. Their record captures changes in species richness, ecological traits, and community composition across major climate perturbations, allowing for an assessment of how environmental stress reshapes both ecosystem structure and spatial patterns of biodiversity.

This contribution synthesises data on shifts in foraminiferal biogeography alongside evidence for ecological and functional turnover. It explores how these spatial dynamics relate to broader environmental drivers such as ocean temperature, productivity, and stratification, and considers the extent to which biogeographic and functional responses vary during periods of rapid climate change.

Understanding these relationships in the deep past provides a valuable baseline for assessing the resilience of modern marine ecosystems. The fossil record of planktonic foraminifera demonstrates that rapid environmental change does not always equate to functional collapse and highlights the conditions under which ecosystem processes persist or reorganise in response to environmental stress. These insights are essential for informing biodiversity and ecosystem service frameworks in the context of ongoing and future climate change.

Dr Tracy Aze

Dr Tracy Aze

University of Plymouth, UK

14:00-14:15 Discussion
14:15-14:45 Adaptive evolution and its impact on global phytoplankton diversity and productivity

This study investigates global phytoplankton dynamics using a novel ocean ecosystem model that incorporates adaptive evolution of key traits (nutrient uptake, temperature optima, and solar radiation optima). Contrary to the prevailing theory that rising temperatures directly increase phytoplankton diversity, the simulations reveal that global phytoplankton diversity is primarily driven by primary productivity and vertical mixing, not temperature (LeGand et al submitted). Diversity is lowest in nutrient-poor subtropical gyres and permanently mixed Southern Ocean waters, while hotspots occur at the convergence of cold and warm western boundary currents. Furthermore, the study assessed the efficiency of adaptive evolution in these populations. Findings suggest that phytoplankton adapt well to spatio-temporal temperature shifts, but not to changes in nutrient conditions or solar irradiance. This maladaptation, particularly to solar irradiance, significantly hinders global primary production and redistributes its spatial patterns, with local variations up to 20% (Sauterey et al submitted). These results emphasise that omitting phytoplankton (mal)adaptation from current ocean ecosystem models compromises their accuracy in predicting both present-day phytoplankton ecology and future ocean primary production under climate change scenarios.

Dr Pedro Cermeno

Dr Pedro Cermeno

Consejo Superior de Investigaciones Científicas, Spain

14:45-15:00 Discussion
15:00-15:30 Break
15:30-16:00 Modelling ecosystem dynamics and carbon cycle interactions in a rapidly changing environment

The impacts of climate change on marine ecosystems and the cascading feedbacks on the carbon cycle and climate have been highlighted as a “known-unknown” in the past four Assessment reports of the IPCC. The quantification of ecosystem-led carbon-climate feedbacks requires a realistic representation of marine ecosystem structure and functioning in global ocean carbon cycle models. Here, Professor Le Quéré will present an effort to introduce functional diversity in the PlankTOM global ocean biogeochemistry model based on the representation Plankton Functional Types (PFTs), grouping organisms according to their influence on carbon fluxes. PlankTOM uniquely represents explicitly heterotrophic bacteria/archaea, six types of phytoplankton, and five types of zooplankton. The model parameters are set following three optimisation logic using available observations, producing three branches based on the same model structure and physical environment but with different outcomes. Results show how the differences in ecosystem outcomes transfer through to differences in carbon dynamics, including primary and secondary production, and carbon export to the ocean interior. We then use emergent properties of the model to evaluate proximity to observed ecosystem dynamics. We further demonstrate that the addition of a viral component exerts an important influence on recycling and export. The presentation will argue that a new generation of Ocean Systems Models (OSM) is needed to build the tools necessary to address marine issues including ecosystem-led carbon-climate feedbacks, risks of ecosystem shifts and tipping points, ocean productivity and food resources, and the effectiveness of proposed active marine carbon dioxide removals.

Professor Corinne Le Quéré CBE FRS

Professor Corinne Le Quéré CBE FRS

University of East Anglia, UK

16:00-16:15 Discussion
16:15-17:00 Panel discussion: overview and future directions
Professor Alessandro Tagliabue

Professor Alessandro Tagliabue

University of Liverpool, UK