T4-1 | Understanding deep-ocean ecosystems and the services they provide

T4-1

Understanding deep-ocean ecosystems and the services they provide
Orals
| Tue, 03 Jun, 10:30–12:00 (CEST)|Room 5
Further information on the theme is available at: https://one-ocean-science-2025.org/programme/themes.html#T4

Orals: Tue, 3 Jun | Room 5

Chairperson: Diva Amon
10:30–10:40
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OOS2025-864
Food web connectivity in cold-water coral environments along the U.S. Atlantic and Gulf of Mexico margins
(withdrawn)
Amanda Demopoulos, Jill Bourque, Jennifer McClain-Counts, Erik Cordes, Martha Nizinski, Nancy Prouty, Steve Ross, and Andrea Quattrini
10:40–10:50
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OOS2025-122
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ECOP
Leandro Nole Eduardo, Michael Maia Mincarone, Tracey Sutton, and Arnaud Bertrand

Deep-pelagic fishes are among the most abundant vertebrates on Earth. They play a critical role in sequestering carbon, providing prey for harvestable fishing stocks and linking oceanic layers and trophic levels. However, knowledge of these fishes is scarce and fragmented, hampering the ability of both the scientific community and stakeholders to address them effectively. While modelling approaches incorporating these organisms have advanced, they often oversimplify their functional and ecological diversity, potentially leading to misconceptions. To address these gaps, this synthesis examines the biodiversity and ecology of global deep-pelagic fishes. We review pelagic ecosystem classifications and propose a new semantic framework for deep-pelagic fishes. We evaluate different sampling methods, detailing their strengths, limitations and complementarities. We provide an assessment of the world's deep-pelagic fishes comprising 1554 species, highlighting major groups and discussing regional variability. By describing their morphological, behavioural and ecological diversity, we show that these organisms are far from homogeneous. Building on this, we call for a more realistic approach to the ecology of deep-pelagic fishes transitioning between very different ecological niches during diel vertical migrations. To facilitate this, we introduce the concept of ‘diel-modulated realised niche’ and propose a conceptual model synthesising the multiple drivers responsible for such transitions.

How to cite: Nole Eduardo, L., Maia Mincarone, M., Sutton, T., and Bertrand, A.: Deep-pelagic fishes are anything but similar: A global synthesis, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-122, https://doi.org/10.5194/oos2025-122, 2025.

10:50–11:00
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OOS2025-152
Pei-Yuan Qian

Cold seeps (methane seeps) are chemosynthetic ecosystems. Methane and other types of carbon released from seafloor serve as energy and carbon sources of chemoautotrophic microbes that form tight symbiosis with marine benthos living in the seep fields. As distribution of cold seeps in global ocean is largely unknown and the flux of methane from seep fields has hardly been quantified.  The impact of cold seeps on global climate change, biogeography and ecosystems functionality remains a hug knowledge gap in ocean science. To fill this critical gap, we are proposing a UN Decade of Ocean Science Program, entitled “Global Climate impacts of methane seeps (Global CliMetS)” to 1) build the capacity in cold seep observation, monitoring, and research in the southen America, Africa, the southen Asia, SIDS, LDCs and LLDCs through scientific exchange and training, 2) draw distribution maps of global cold seeps,  3) quantify the methane flux (such as methane, gas hydrates, and dissolved organic carbon from cold seep fields), understand the fate and pathways of methane released from the sea floor, and assess impact of these gases released from seafloor on global climate changes, biodiversity, function, resilience, and connectivity and global biogeography of different cold seep ecosystems, and 4)  develop innovative technology for in situ environmental monitoring, environmental risk assessment of potential methane release due to gas hydrate degradation and natural and human-induced methane leakage, and  programmes. In this presentation, I would like to highlight the implementation plan of this program.

How to cite: Qian, P.-Y.: Global Climate impacts of methane seeps (Global CliMetS), One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-152, https://doi.org/10.5194/oos2025-152, 2025.

11:00–11:10
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OOS2025-139
Fengping Wang, Kai-Uwe Hinrichs, Ken Takai, Thulani Makhalanyane, Mohamed Hatha Abdulla, and Mohamed Jebbar

The subseafloor ecosystem includes all life living in marine sediment, crust and the accompany fluids. This ecosystem, also called the deep biosphere, mostly derives its energy source from geological processes, which are cut off from sunlight. Deep-sea hydrothermal vents and cold seeps are regarded as windows of the subsurface life. Still, little is known about the subseafloor life and there is a substantial knowledge gap related to understanding the breadth of their diversity, assemblage, function, and possible ecosystem services to society. These insights are key to understanding the origin of life and evolutionary processes, and also pivotal for evaluating the impact of the proposed ocean-based climate interventions. As part of the efforts to reduce this knowledge deficiency, we initiate a global-scale program “Global Subseafloor Ecosystem and Sustainability” (GSES). This program aims to generate new systematic insights into subseafloor ecosystems with the aim of transforming these datasets for predictive capabilities. As a newly endorsed program of the UN Ocean Decade, the overarching objective of GSES is to significantly advance scientific comprehension, conservation, and sustainable management of Earth's subseafloor ecosystems. Focused on addressing substantial knowledge gaps in microbial life, carbon dynamics, and historical records within this critical, vulnerable and understudied environment, GSES aims to develop internationally standardized protocols, cutting-edge investigation platforms, and ecological indices. GSES aspires to bridge critical knowledge gaps related to the subseafloor while fostering collaboration, inclusivity, and sustainability. By contributing to informed policy decisions and promoting responsible ocean governance, GSES envisions a resilient and equitable blue economy, aligning with the goals of the United Nations Ocean Decade.

How to cite: Wang, F., Hinrichs, K.-U., Takai, K., Makhalanyane, T., Abdulla, M. H., and Jebbar, M.: Global Subseafloor Ecosystem and Sustainability (GSES), One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-139, https://doi.org/10.5194/oos2025-139, 2025.

11:10–11:20
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OOS2025-1031
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ECOP
Stéven Yvenou, Ewan Pelleter, Cyril Noel, Anne Godfroy, Valérie Cueff-Gauchard, Sandrine Cheron, Xavier Philippon, Christophe Brandily, and Erwan G. Roussel

Sea-floor massive sulfide deposits (SMS) harbor over 108 tons of mineral resources along the mid-ocean ridges representing a significant polymetallic reservoir [1]. These SMS deposits are mainly composed of iron and sulfur, but also contain copper, zinc, gold, silver and rare-earth elements, making them attractive for the mining industry. Little is known about the geo-biodiversity and ecosystem services associated with these SMS deposits especially the inactive or extinct ones. Deep dark chemosynthetic microbial ecosystems associated with these deep-sea habitats interact with the hydrothermal deposits during their aging process through biogeochemical metal and carbon cycles. Hence, characterization and quantification of carbon incorporation are required to estimate the carbon fluxes associated with active and inactive hydrothermal systems [2-4]. During the HERMINE 2 [5] and BICOSE 3 [6] oceanographic expeditions on Mid-Atlantic Ridge (MAR), we collected 36 mineralized samples on SMS deposits characterized by different relative ages and various degrees of oxidation. Carbon fixation autotrophic and heterotrophic rates were measured using radio-labelled substrates at in situ conditions (pressure and temperature) to evaluate distribution and environmental controls on energy and carbon fluxes. Phylogenetic and metabolic microbial diversity were also investigated by a metagenomics approach to define microbial functional pathways driving alteration and biogeochemical metal and carbon cycles in the hydrothermal deep biosphere. Here we show, for the first time at a slow spreading ridge (i.e MAR), that high rates of CO2 fixation support large microbial biomasses that inhabit “active” to “inactive” SMS. Given the large volumes of SMS habitats, these deposits could represent a significant CO2 sink in the deep-sea and should therefore be considered for environmental management.

References:

[1].      Hannington, M., Jamieson, J., Monecke, T., Petersen, S. & Beaulieu, S. The abundance of seafloor massive sulfide deposits. Geology 39, 1155–1158 (2011).

[2].      Dover, V. & Lee, C. Inactive Sulfide Ecosystems in the Deep Sea: A Review. Front. Mar. Sci. 6, (2019).

[3].      Cathalot, C. et al. Hydrothermal plumes as hotspots for deep-ocean heterotrophic microbial biomass production. Nat Commun 12, 6861 (2021).

[4].      Achberger, A. M. et al. Inactive hydrothermal vent microbial communities are important contributors to deep ocean primary productivity. Nat Microbiol 9, 657–668 (2024).

[5].      PELLETER Ewan & CATHALOT Cécile. HERMINE2 cruise,Pourquoi pas ? R/V. Preprint at https://doi.org/10.17600/18001851 (2022).

[6].      CAMBON Marie-Anne. BICOSE 3 cruise,Pourquoi pas ? R/V. Preprint at https://doi.org/10.17600/18002399 (2023).

How to cite: Yvenou, S., Pelleter, E., Noel, C., Godfroy, A., Cueff-Gauchard, V., Cheron, S., Philippon, X., Brandily, C., and Roussel, E. G.: Microbial ecosystems associated with “active” to “inactive” hydrothermal systems: massive sulfide deposits a CO2 sink in the deep-sea, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1031, https://doi.org/10.5194/oos2025-1031, 2025.

11:20–11:30
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OOS2025-1367
lars stemmann
Our current understanding of pelagic ecosystems decreases with depth and lags far behind that of the surface ocean. Our predictive understanding of the deep ocean role remains highly uncertain. Roughly 10 Pg of organic carbon enters the mesopelagic each year and approximately 90% of this organic carbon flux is utilized by the mesopelagic fauna (bacteria, zooplankton, midwater fishes) and 10% continue it’s long road to the abyss. The common understanding is that deep ecosystems are quiet and homogeneous. However, intermittent flux down to the abyss of phyto-detrital particles or evidence of deep vertical plankton and nekton migration, or strong variability at mesoscale or at bentho-pelagic interfaces  demonstrate that, contrary to the main paradigm, the abyssal ecosystem is dynamics. This fundamental lack of a predictive understanding means that although we are currently barely able to accurately predict the resilience of the mesopelagic ecosystem to changes in ocean conditions, predicting the fate abyssopelagic ecosystem is not possible at all. This is becoming increasingly critical for understanding the impacts of future climate changes on deep sea ecology. 
Underwater monitoring with cameras, down to 6000m, allow to cross the mesopelagic frontier down to the abyss and gain substantial understanding of biodiversity and carbon cycling at regional and global scales.
 
During the presentation, we will present, discuss and give perspectives to show that
- global scale monitoring by imaging systems to detect plankton and different types of particles is possible in the deep ocean
- specific coupling between hydrodynamics and plankton dynamics concours to focus the sinking of marine snow at mesoscale down to the abyss,
- vertical flux focusing has an impact on the deep sea life and this knowledge could be relevant at global scale
- mesopelagic and abyssopelagic layers are not only populated by the known midwater crustaceans, fishes and gelatinous metazoans but also by gigantic poorly know rhizarians that could play a role in the deep trophic web but also carbon flux.

How to cite: stemmann, L.: Bentho-pelagic coupling by sinking marine snow down to 6000m depth, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1367, https://doi.org/10.5194/oos2025-1367, 2025.

11:30–11:40
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OOS2025-1086
Marjolaine Matabos and Pierre Marie Sarradin and the EMSO-Azores Research Infrastructure

Faced with the increasing interest for ocean resources exploitation in a changing ocean, there is an urgent need for a comprehensive assessment of the health and status of deep-sea ecosystems. Hydrothermal vents constitute areas of important thermo-chemical exchanges between the lithosphere and the hydrosphere and host a unique biodiversity. Understanding their natural dynamics is key to evaluating and predicting the impacts and ecosystem responses to disturbances caused by natural and anthropogenic changes, and their consequences on the global ocean health. Since 2010, the EMSO-Azores observatory connects a large range of sensors at 1700 m water depth at the Lucky Strike Hydrothermal Field (LSHF) along the mid-Atlantic ridge. The infrastructure, combined with repeated yearly sampling, aims at understanding the feedbacks between geological processes and hydrothermalism at a slow spreading mid-ocean ridge, and the coupling between the hydrothermal ecosystem and sub-seabed processes.

The last 13 years of monitoring showed that tidal modulation is the main process driving vent heat flux variability, species behaviour and physiology while over decadal timescales, results point to a relative stability of the vent system across varying spatial scales, challenging the paradigm that hydrothermal vents are highly dynamic and ephemeral habitats. These results have strong impact in terms of resilience of these systems to large scale disturbance such as deep-sea mining. In addition, the infrastructure and the associated Momarsat maintenance cruises supported a large number of mediation projects, art and science productions, public outreach events, inter- and trans-disciplinary collaborations and citizen science projects showing the strong scientific and societal impact of the observatory over time.

In this talk we will summarise 13 years of integrated study at LSHF, training opportunities and discuss the leverage effect and the societal impact of the observatory.

How to cite: Matabos, M. and Sarradin, P. M. and the EMSO-Azores Research Infrastructure: The EMSO-Azores deep-sea observatory: towards an integrated and pluridisciplinary understanding of hydrothermal systems on a slow-spreading ridge from the sub-surface to the water column., One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1086, https://doi.org/10.5194/oos2025-1086, 2025.

11:40–12:00

Posters on site | Poster area "La Baleine"

Display time: Tue, 3 Jun, 17:00–Thu, 5 Jun, 20:00
P359
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OOS2025-176
Marie-Anne Cambon-Bonavita and Ewan Pelleter and the Marie Anne CAMBON

Protection of deep seabed, the largest biome on the planet, is a major challenge for future generations. Covering more than 70% of the Earth's surface, the ocean encompasses ≈80% of the seawater volume, produces at least 50% of the atmospheric oxygen and absorbs ≈25% of anthropogenic CO2. Hidden from our eyes, the deep ocean has long been considered as a vast desert of darkness, populated by sea monsters. Today it is the covetousness of developed and emerging countries for its resources in terms of biodiversity and minerals. It becomes then urgent to acquire, through holistic approaches, solid knowledge baselines with regard to the diversity of geological systems, habitats, taxonomic and functional biodiversity, at open and interconnected ocean scales.

Our consortium led a five cruises series (2014- 2023) in the framework of the French contract for exploration of Atlantic polymetallic sulphides resources (ISA). At 3600 meters depth, the TAG hydrothermal field is an area of choice for studying the geo-biodiversity of so-called inactive SMS deposits, and is, with the young and volcanic Snake Pit hydrothermal field, at the heart of our studies. Exploration of the area revealed geochemical evidences for new active vent sites, some visited such as HYDRA, a new ones to be found. These sites constitute potential relays for the organism dispersal, a key point in the overall understanding of ecosystems and their relationships along ridge segments.

LIFEDEEPER intend to develop new approaches, combining in situ, in vivo, and lab experimentations, modeling and qualitative research in social sciences to disentangle the geological, geochemical and biological natural functioning of deep ocean ecosystems. In addition to the coordination work package (WP1), 4 multidisciplinary, complementary scientific WPs and one communication WP are proposed:

WP2: Exploration and description of ecosystems associated with inactive and active massive sulphide deposits : toward integrated definitions of active and inactive vents.

WP3: Integrated 3D study coupling hydrodynamics, distribution of trace metals and numerical modeling to assess the biogeochemical impact of the hydrothermal plume to the deep ocean.

WP4: Study the connectivity and life cycle of holobiont models, capacity of adaptation and acclimation allowing the resilience of communities.

WP5: Legal and political analysis of international regulatory regimes, sociological analysis of science-technology-society, capacity building. 

A last WP6 will then aim to produce effective educational and public outreach activities targeting citizens, students, scholars, organizations and various stakeholders, through participative science, educational science and art.     

Ultimately, we want to establish a precise map of contrasting sites along the 600 km ridge segment, to provide key parameters to understand the natural functioning of these environments, both from a geological and biological point of view. Key components of the functioning of these ecosystems and associated services, along activity gradients, will permit establishing global-scale inter-comparison protocols. In a holistic and multidisciplinary approach, LIFEDEEPER aims to acquire definitions of reference ecological profiles and preservation strategies in the context of the growing interest in deep mineral resources for the carbon-free and digitized world economy. LIFEDEEPER will propose solutions to allow future informed guidelines and decision-making.

How to cite: Cambon-Bonavita, M.-A. and Pelleter, E. and the Marie Anne CAMBON: The LIFEDEEPER Project : LIving together in the Future: vulnErability of DEEP sea Ecosystems facing potential mineral Resources exploitation, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-176, https://doi.org/10.5194/oos2025-176, 2025.

P360
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OOS2025-379
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ECOP
Evaluating the importance of mesopelagic prey to top teleost predators in the Northwest Atlantic
(withdrawn)
Ciara Willis, Kayla Gardner, Martin Arostegui, Camrin Braun, Walt Golet, Leah Houghton, Joel Llopiz, Annette Govindarajan, and Simon Thorrold
P361
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OOS2025-384
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Jose Angel Perez and Lucas Gavazzoni

The Santos basin is a prominent offshore sedimentary feature of the SW Atlantic, extending 350,000 km² off the southeastern Brazilian coast. The deep sectors of Santos Basin comprise the slope and the São Paulo Plateau, which, in the last decades, have been subject to fishing and oil and gas exploration. Seafloor is mostly covered by sediments, interspersed by hard substrate patches associated with pockmarks, carbonate mounds and ridges, and salt diapirs. These features increase the diversity of benthic habitats that remain mostly unexplored, but are expected to host cold-water corals and cold-seeps communities. We analyze benthic seascape structure and habitat heterogeneity in a 4,854 km2 section of Santos Basin slope region between 259 and 1,275 m depths (seascape area). Seascape analysis was based on a high-resolution digital bathymetry model (14 m grain size) produced during deep-sea surveys conducted in 2011 and 2022. Using a Benthic Terrain Modeler tool, seabed was segmented into seven classes, including: (a) the dominant and highly interconnected sediment “matrix”, (b) the hard-substrate pockmarks, mega pockmarks, depressions, salt diapirs and carbonate ridges, and (c) the human-made “trawl furrow”. Seascape structure was quantified considering all 1,430 mapped patches of all classes (patch types), except the sediment matrix, and 16/22 patch class/seascape scale metrics that described: patch area and edge, aggregation, shape, core area and diversity. Patches tended to become denser (3 – 5/ km2) and more irregular at depths greater than 500 m. Between 600 and 700 m, patches were also more diverse and evenly distributed. Pockmarks included the most abundant and dense patches (2.7/km2), with their core covering 34.4% of the seascape area. They exhibited extensive edge sectors and were relatively small, disaggregated, regular-shaped and little interspersed among other classes. Pockmarks density was highest between 300 and 400 m depths and declined towards deeper slope sectors. Between 400 and 600 m their core area was smaller, but overall, they covered the highest proportions of the depth strata seascape (48.8 – 53.9%). Because cold-water coral and cold-seeps communities are likely to occur on the edges and core of pockmarks, respectively, chances of their occurrence may be increased at the 400 – 600 m depth stratum. In the 600 – 700 m stratum a more heterogeneous mix of hard bottom structures occur, some of large sizes (e.g., carbonate ridge), potentially harboring more diverse benthic communities. The definition of trawl furrows as habitat patches, represents an important evidence of human activities modifying deep seascapes in Santos Basin. Whereas their core area was little significant, they tend to create extensive edge sectors amid the sediment matrix, potentially affecting soft bottom benthic communities.

How to cite: Perez, J. A. and Gavazzoni, L.: Seascape Structure and Benthic Habitat Heterogeneity of Santos Basin Slope, SW Atlantic, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-384, https://doi.org/10.5194/oos2025-384, 2025.

P362
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OOS2025-392
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ECOP
Pierre Methou, Valérie Cueff-Gauchard, Loïc Michel, Hiromi Watanabe, Jon Copley, Chong Chen, Florence Pradillon, and Marie-Anne Cambon

Within the deep ocean, hydrothermal vent ecosystems are home to unique set of species' communities, that live nowhere else, and whose food chains have the particularity to rely on microorganisms activities through a process called chemosynthesis. Many animals living there have adopted the strategy of hosting these microorganisms in symbiosis on or within their body, including many of the most emblematic groups such as tubeworms, Pompeii worm, yeti "crabs" or scaly-foot and hairy snails. Among them, shrimps of the Alvinocarididae family constitute a major component of this endemic fauna, with a global distribution across the globe, and dominating visually vent communities of the Atlantic and Indian Ridges. Work led and carried out by Ifremer have characterized the biology of the Rimicaris shrimps inhabiting the Mid Atlantic Ridge with an emphasis on their chemosynthetic symbiosis and their lifecycle, from the egg development to the reproduction phase. Recently, studies in collaboration with other research institutes have expanded these knowledges to other shrimps of the family inhabiting different regions. They have revealed a large variation in the set of functional traits related to their reproduction, symbiosis and feeding strategy. Hence, the evolutionary history of their chemosynthetic symbiosis contrast with most of the other emblematic species, while some shrimps present a unique and intriguing case of reproductive periodicity that had never been documented before. Overall, these observations reveal the functional uniqueness of this family, that also reflect their fragility in the face of mining threats, highlighting the need of conservation measures to protect them.

How to cite: Methou, P., Cueff-Gauchard, V., Michel, L., Watanabe, H., Copley, J., Chen, C., Pradillon, F., and Cambon, M.-A.: Symbiosis, reproduction and metamorphosis: The functional uniqueness of deep-sea vent shrimps in the face of mining threat., One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-392, https://doi.org/10.5194/oos2025-392, 2025.

P363
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OOS2025-447
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ECOP
Hélène Thibault, Frédéric Ménard, Gildas Roudaut, Anne Lebourges-Dhaussy, Yves Cherel, Alejandro Ariza, Leandro Nolé Eduardo, and Séverine Martini

Micronekton comprises a diverse assemblage of actively swimming aquatic animals in oceanic ecosystems, including mesopelagic fishes from 2 to 20 cm. They live in the mesopelagic zone (200-1000 meters), characterized by high environmental gradients and distinct temporal dynamics across depth layers. Depending on their vertical habitat, mesopelagic fishes have developed various adaptions and contribute to essential ecosystem processes, including nutrient cycling and carbon transport. However, the link between their functional diversity, vertical habitat use and survival strategies requires further clarification. This study, conducted during a scientific cruise in the Northeast Atlantic (APERO program), uses multi-depth trawling and acoustic observations to investigate the behaviors and habitats of mesopelagic fishes, highlighting distinct movement patterns across vertical zones. To examine the ecological roles of these species, we developed a trait matrix encompassing 80 fish species and 12 functional traits related to fitness, including morphological, physiological, life-history, and behavioral characteristics. Based on this information, we performed a factor analysis of mixed data including quantitative and qualitative traits. Mesopelagic fishes were then classified in functional groups based on clustering of the factor analysis. Traits that contributed the most to the first two axes were swimming type, teeth type, presence of swimbladder and trophic level. Traits and trade-offs were associated with survival strategies – mainly feeding and predator avoidance - differing between functional groups. We analyzed which patterns of functional diversity emerge across these different structures. This study elucidates the relationships between functional traits, habitat preferences, and feeding behaviors to deepen our understanding of the processes structuring mesopelagic fish assemblages. By exploring these relationships, we gain insights into the adaptive strategies of micronekton and their ecological roles in oceanic ecosystems.

How to cite: Thibault, H., Ménard, F., Roudaut, G., Lebourges-Dhaussy, A., Cherel, Y., Ariza, A., Eduardo, L. N., and Martini, S.: Ecological Roles of Mesopelagic Micronekton in the Northeast Atlantic: A Trait-Based Perspective, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-447, https://doi.org/10.5194/oos2025-447, 2025.

P364
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OOS2025-472
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ECOP
Capucine Le Cam Ligier, Hélène Thibault, Sophie Guasco, Corinne Valette, Gwenola Simon, Laurie Casalot, Séverine Martini, and Marc Garel

Mesopelagic ecosystems, located between 200 and 1000 meters deep are poorly studied. They are characterized by complete darkness, driving organisms to develop specialized adaptive strategies1. One of the most remarkable of these adaptations is bioluminescence, enabling organisms to produce light for communication, camouflage, prey attraction, or defence2. Mesopelagic fish, such as myctophids, dominate this zone in terms of biomass (65%) and diversity and are capable of emitting light3. They produce light either through endogenous photophores or via symbiosis with bioluminescent bacteria like Vibrionaceae. These microorganisms may also be found on their skin and in their gut or liver 2,4. These fishes perform diel vertical migrations (DVM): they ascend to feed near the surface at night and descend to deeper waters during the day to avoid predators3. By this process, they can transport organic matter and nutrients through the water column. Indeed, they are capable of releasing consumed organic matter in the form of fecal pellets that can be glowing (as they carry bioluminescent bacteria).  This feature might play a key role in structuring deep-sea trophic networks.

This study aims to analyse prokaryotic composition across different tissues of several mesopelagic fish species and to identify correlations between the presence of bioluminescent bacteria, migratory capacity, and diet. A total of 160 samples from gut, liver, and skin were collected during the APERO cruise in July 2023 in the Northeast Atlantic. Microbial diversity was assessed via 16S metabarcoding, considering site, depth, and fish traits.

The results reveal significant microbial variations across the three most-sampled fish families (n = 142): Myctophidae, Stomiidae, and Sternoptychidae. Bioinformatic analyses show two distinct clusters, with skin samples clearly separated from liver and gut. Bacterial composition varied by tissue, with Pseudoalteromonadaceae dominating the skin (25% of the community) and Vibrionaceae and Enterobacteriaceae prevalent in liver and gut (52% and 24%). Within Vibrionaceae, Photobacterium and Vibrio (including many bioluminescent species5) comprised about half of the gut bacterial community, indicating their abundance in this tissue. Correlations emerged between bacterial composition, diet, and migratory abilities in Myctophidae and Sternoptychidae. Migratory, zooplanktivorous, and bioluminescent fish had a microbial composition largely composed of Photobacterium and Vibrio (Vibrionaceae), in contrast to other fish. These findings highlight the importance of studying microbial diversity in mesopelagic fishes and provide a strong foundation for understanding interactions between fish microbiomes and deep-sea ecological processes.


1 Robison, B. H. Conservation of deep pelagic biodiversity. Conservation Biology 23, n°4 (2009): 847-858. https://doi.org/10.1111/j.1523-1739.2009.01219.x
2 Haddock, S.H.D., M. A. Moline, and J. F. Case. Bioluminescence in the Sea. Annual Review of Marine Science 2, no 1 (2010):443‑93. https://doi.org/10.1146/annurev-marine-120308-081028.
3 Irigoien, X., T. A. Klevjer, A. Røstad, et al. Large Mesopelagic Fishes Biomass and Trophic Efficiency in the Open Ocean. Nature Communications 5, no 1 (2014):3271. https://doi.org/10.1038/ncomms4271.
4 Widder, Edith. Bioluminescence and the Pelagic Visual Environment. Marine and Freshwater Behaviour and Physiology 35 (2002):1‑26. https://doi.org/10.1080/10236240290025581.
5 Tanet, L., S. Martini, L. Casalot, and C. Tamburini. Reviews and Syntheses: Bacterial Bioluminescence – Ecology and Impact in the Biological Carbon Pump. Biogeosciences 17, no 14 (2020):3757‑78. https://doi.org/10.5194/bg-17-3757-2020.

How to cite: Le Cam Ligier, C., Thibault, H., Guasco, S., Valette, C., Simon, G., Casalot, L., Martini, S., and Garel, M.: Diversity and ecological dynamics of bioluminescent bacteria in the mesopelagic zone, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-472, https://doi.org/10.5194/oos2025-472, 2025.

P365
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OOS2025-484
Michael Maia Mincarone, Leandro Nole Eduardo, Flávia Lucena-Frédou, and Arnaud Bertrand

Deep-pelagic ecosystems (below 200 meters depth) encompass thousands of species intrinsically linked to critical ecosystem processes, such as carbon sequestration and the connectivity between pelagic layers and trophic levels. However, deep-pelagic realms remain some of the least explored ecosystems globally and is increasingly imperiled by human activities. This challenge is particularly acute for developing nations, where participation in deep-sea research is hampered by limited expertise, lack of incentives, and restricted access to advanced technological infrastructure, leading to an almost complete absence of knowledge regarding their deep-pelagic biodiversity. Here, we present a case study of international cooperation that serve as a model for advancing knowledge of deep-pelagic fish diversity in historically understudied regions. The International Joint Laboratory – Tropical Atlantic Interdisciplinary Laboratory on Physical, Biogeochemical, Ecological, and Human Dynamics (IJL TAPIOCA) exemplifies this collaborative model. This consortium brings together a multidisciplinary team of researchers and students from the French Institut de Recherche pour le Développement (IRD) and several Brazilian institutions, including the Federal Rural University of Pernambuco (UFRPE) and the Federal University of Rio de Janeiro (UFRJ). One of the main goals of the consortium is to deepen understanding of the biodiversity and distribution of deep-sea fishes from off northern and northeastern coasts of Brazil, a region with limited baseline data on species diversity. Focusing on deep-pelagic fish diversity, recent expeditions have explored two different areas: the Fernando de Noronha Ridge (including the Fernando de Noronha Archipelago, Rocas Atoll, and nearby seamounts) and the oceanic waters in front of the Amazon River estuary. Through these expeditions, a remarkable diversity of deep-sea fishes was documented, with collections totaling around 15,000 fish specimens, representing approximately 250 nominal species, 60 of which represent new distribution records in Brazilian waters. Furthermore, at least 12 new species have been identified so far, including notable discoveries in the genera Eustomias, Melanosthomias, Astronesthes (Stomiiformes), Poromitra and Melamphaes (Beryciformes). The specimens and selected tissue samples were deposited at the Fish Collection of the Institute of Biodiversity and Sustainability (NUPEM/UFRJ). All data are available online at two repositories: https://specieslink.net and https://www.sibbr.gov.br. These findings not only enhance the knowledge of mesopelagic fish diversity in poorly studied areas but also provide important insights into species distribution patterns and the biodiversity of deep-sea ecosystems. This research underscores the significance of international collaboration in addressing pressing questions related to marine biodiversity and conservation, especially in underexplored regions.

How to cite: Maia Mincarone, M., Nole Eduardo, L., Lucena-Frédou, F., and Bertrand, A.: IJL TAPIOCA: A collaborative French-Brazilian initiative to advance biodiversity and taxonomic knowledge of deep-pelagic fishes, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-484, https://doi.org/10.5194/oos2025-484, 2025.

P366
|
OOS2025-598
Diversity and dynamics of bacteria from iron-rich microbial mats and colonizers in the Mediterranean Sea (EMSO-Western Ligurian Sea Observatory): Focus on Zetaproteobacteria
(withdrawn)
Céline Rommevaux, Aina Astorch-Cardona, Lionel Bertaux, Yann Denis, and Alain Dolla
P367
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OOS2025-948
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ECOP
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Laure Barbin, Valérie Allain, Paul Magnier, Aurore Receveur, Hidetada Kiyofuji, Atsushi Tawa, Taiki Ishihara, Naoto Matsubara, Anne Lebourges-Dhaussy, Jérémie Habasque, and Christophe Menkes

Micronekton organisms, ranging in size from 2 to 20 cm and composed of various taxa (fish, cephalopods, gelatinous, crustaceans…), are present across all oceans and play a vital role in pelagic ecosystems from the surface to the deep ocean. They form a key component of the trophic web by feeding commercial top predators such as tuna, and they participate actively to the carbon pump, influencing nutrient cycles in marine environments. However, their abundance and distribution, particularly in deep ocean regions, remain uncertain. This study aims to investigate the pelagic ecosystems of the western tropical Pacific Ocean from the surface down to 800m depth using data and samples collected in the field. We utilized active acoustic echo-sounder data collected during multiple scientific surveys in areas with previously limited acoustic coverage. Through sea experiments spanning contrasted ecosystem of the tropical region from the warm pool to the equatorial upwelling, we used hull-mounted multi-frequency acoustics to map and differentiate micronekton distributions. These acoustic measurements provided insights into contrasted, large-scale ecosystem, which were then analyzed in relation to various physical and environmental parameters, including temperature, salinity, fluorescence, oxygen levels, and ocean currents. The use of acoustic classification enabled us to identify spatial patterns specific to the diverse ecosystems encountered, confirming regional ecosystem functioning based on micronekton distributions. This approach allowed us to distinguish unique features such as the transition between the oligotrophic equatorial warm pool and the equatorial upwelling, and subtropical oligotrophic zones, each characterized by specific vertical environmental and micronekton structures densities. Acquiring this knowledge is a first step before making hypothesis on the impact of environmental changes on the micronekton distribution and its contribution to carbon sequestration in the ocean.

Keywords : Mesopelagic ecosystems, Pacific, Micronekton, Food web, Active acoustics, Warm pool, Equatorial upwelling

How to cite: Barbin, L., Allain, V., Magnier, P., Receveur, A., Kiyofuji, H., Tawa, A., Ishihara, T., Matsubara, N., Lebourges-Dhaussy, A., Habasque, J., and Menkes, C.: Contrasted deep-ocean ecosystems in the tropical Pacific from the perspective of the micronekton, a key to carbon pump and global tuna resources, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-948, https://doi.org/10.5194/oos2025-948, 2025.

P368
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OOS2025-1017
What is hidden behind the “deep sea”? Ecosystems, resources and pressures
(withdrawn)
Pierre-Marie Sarradin, Claire Geslin, Marie-Anne Cambon, and Karine Alain
P369
|
OOS2025-1028
Ifremer’s implication in deep-sea minerals and associated ecosystems exploration as a research institute and as a contractor with the International Seabed Authority
(withdrawn)
Sébastien Ybert, Florian Besson, Marie-Anne Cambon, Cécile Cathalot, Pierre-Antoine Dessandier, Lenaick Menot, Ewan Pelleter, Pierre-Marie Sarradin, and Daniela Zeppilli
P370
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OOS2025-1049
Laura Rieusset, Elodie M. Leroy, Blandine Trouche, Johanne Aubé, Chloé Baumas, David François, Sébastien Le Guellec, Vanessa Rédou Creff, Françoise Lesongeur, Raphaël Brizard, Anne Godfroy, Karine Alain, Mohamed Jebbar, and Erwan G. Roussel

Archaea DPANN* superphylum harbors, to date, 12 phyla including Nanoarchaeota and Candidatus Aenigmarchaeota (previously described as DHVE-3, DSEG and VAL III). Interestingly, DPANN are detected in a wide range of anoxic or oxygen limited environments such as lakes, marine sediments and hydrothermal systems. Most known core biosynthetic pathways are also absent or incomplete in DPANN Archaea, suggesting symbiotic or parasitic lifestyles. However, much of the knowledge about their ecology, evolution, and putative metabolism mainly relies on metagenomic data. Here we repeatedly enriched two archaea distantly affiliated with Ca. Aenigmarchaeota (16S rRNA gene sequence identity <84%) and Nanoarchaeota (16S rRNA gene sequence identity <81%) in continuous cultures. These enrichment cultures were performed from hydrothermal chimney samples and fluids from Snake Pit, TAG and Lucky Strike, hydrothermal sites located on the Mid-Atlantic ridge (BICOSE, HERMINE, MoMARsat 2017, BICOSE 2 oceanographic cruises) using a gas-lift bioreactor under H2/CO2 at 80°C. Cell concentrations increased progressively over several weeks up to ~107 cells/mL simultaneously with a relative proportion (≤75%) of these new previously uncultured phylotypes. The enigmatic group of Archaea distantly affiliated with Nanoarchaeota seems to be widespread as it was enriched from all hydrothermal sites, whereas Archaea affiliated with Ca. Aenigmarchaeota were only cultured from Snake Pit, suggesting a possible environmental selection. Based on co-occurrence of these phylotypes, several putative archaeal partners were identified. Metagenomic analyses are being performed in order to help to optimize culture conditions for pure (co-)cultures. This ongoing study should help to resolve ecology and life style of these new phylums.

*an acronym of the names of the first included phyla: Diapherotrites, Parvarchaeota, Aenigmarchaeota, Nanoarchaeota and Nanohaloarchaeota.

How to cite: Rieusset, L., Leroy, E. M., Trouche, B., Aubé, J., Baumas, C., François, D., Le Guellec, S., Rédou Creff, V., Lesongeur, F., Brizard, R., Godfroy, A., Alain, K., Jebbar, M., and Roussel, E. G.: First insights into enrichment cultures at in situ conditions of hyperthermophilic microorganisms potentially affiliated with the DPANN superphylum, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1049, https://doi.org/10.5194/oos2025-1049, 2025.

P371
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OOS2025-1054
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ECOP
Mandé Ndiaye, Ismaïla Ndour, Sabrina Duncan, Kamarel Ba, Alassane Sarr, and Ibrahima Ndiaye

Mesopelagic fish communities remain under studied in the highly dynamic Canary Current Ecosystem. We analyzed mesopelagic fish assemblage structure based on 2,153 specimens representing 98 species across two distinct marine zones: Mauritania, characterized by high oxygen and chlorophyll-a concentrations, and Senegal, distinguished by high temperatures and low salinities. Our findings reveal clear biogeographic patterns, with Diaphus vanhoeffeni, Diaphus dumerilii, Argyropelecus gigas, and Sternoptyx diaphana showing high abundance in Senegalese waters but limited presence in Mauritania waters. Conversely, Diaphius rafinesquii, Benthosema glaciale, Argyropelecus hemigymnus, Lobiancha dofleini, and Hygophum taaningi exhibited higher abundances in Mauritania waters. Statistical analyses revealed significant correlations between species abundance patterns and physicochemical parameters specific to each marine zone. This pioneering study of mesopelagic fish community composition and structure in relation to environmental factors in the Canary Current Ecosystem provides valuable insights into a marine fauna, which holds potential for sustainable exploitation in aquaculture feed production and nutritional supplements, beyond its crucial role in the carbon cycle and marine food web.

Keywords: Mesopelagic fish, Canary Current Ecosystem, Upwelling, Environmental factors, West Africa.

How to cite: Ndiaye, M., Ndour, I., Duncan, S., Ba, K., Sarr, A., and Ndiaye, I.: Spatial variation in mesopelagic fish assemblage structure in the upwelling of the Canary Current Ecosystem, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1054, https://doi.org/10.5194/oos2025-1054, 2025.

P372
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OOS2025-1062
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Hélène Leau, Karine Olu, Martin Patriat, Clement Vic, Swen Jullien, Julien Legrand, Nan-Chin Chu, and Takeshi Toyofuku

Due to their elevation above the sea floor, seamounts are unique underwater structures. An important number of these structures can be found in the Pacific and may have a key role in the ocean. They host a variety of energetic flow-topography interactions, which lead to strong levels of turbulent transport and mixing. These are believed to shape, or at least strongly impact, benthic communities. Seamounts feature diverse environmental conditions and faunal communities and some have been qualified as hotspots of diversity and biomass, and they can attract fish and marine mammals.  Seamounts are therefore often subject to fishing effort that impacts benthic habitats when targeting demersal species using bottom trawls. They are also potential targets for mineral exploitation as these environments favour the development of cobalt-rich crusts.

Because of their extension along the bathymetric gradient, seamounts are also key systems for studying the coupling between benthic and pelagic compartments and the effects of climate change on deep-sea ecosystems. The Natural Park of the Coral Sea in New Caledonia where the seamounts are not stressed by any resource exploitation is a good case study to improve knowledge on their functioning and dynamics by long term monitoring.

The ScInObs-New Caledonia observatory project aims at acquiring multi-disciplinary data on two different seamounts contrasting by their faunal (benthic and mesopelagic) water masses, and geological characteristics in order to better understand the role of environmental drivers of the biodiversity, and the impact of seamounts on the hydrodynamics and turbulent mixing.  The data acquisition started with the KASEAOPE-1 cruise in 2023 when a 800 m long mooring was deployed to monitor over a period of 18 months and at very high resolution, a set of parameters on a seamount slope , together with a Edokko type lander to observe the seafloor. In 2024, a benthic station also observing simultaneously the upward water column was deployed on top of the same seamount. The technologies developped for observation, such as the benthic station, aim at reducing environmental impact. Three additional cruises are planned until 2028.

How to cite: Leau, H., Olu, K., Patriat, M., Vic, C., Jullien, S., Legrand, J., Chu, N.-C., and Toyofuku, T.: Multi-disciplinary monitoring of seamounts in the southwestern Pacific, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1062, https://doi.org/10.5194/oos2025-1062, 2025.

P374
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OOS2025-1133
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ECOP
Diane Esson, João Monteiro, Marko Radeta, Henk-Jan Hoving, Jan Dierking, Ana Širović, Nicole Aberle-Malzahn, Martin Ludvigsen, and João Canning-Clode

Today, deep-sea research is expensive, largely limiting this science to countries and institutes with the greatest resourcing. Such efforts have been critical to expanding our knowledge of the deep, yet we still know too little to make time-sensitive decisions about resource use, protection and responsible interactions with the deep.

We need more people doing deep-sea research, and we need to do it efficiently and cost-effectively. Our ocean, our efforts to preserve our planet and the well-being of our coastal communities depend on it. 

How do we do this? We believe one of the answers lies around a small island chain in the North Atlantic.

The Madeira Archipelago, an autonomous region of Portugal, is a series of volcanic islands with steep slopes diving straight into the deep sea. Within a few kilometers from shore, ocean depths already reach 500-1,000m. Another dozen kilometers and depths reach over 3,000m. Thanks to Madeiras relatively calm seas and mild climate, these depths are also accessible to researchers year-round by small boats. 

Madeira does not have the economic might to finance state-of-the-art deep-sea research equipment and expeditions as do the world’s leading research institutions. Only through creativity and collaboration can we take advantage of our island’s special access and begin to discover and democratize the deep.  

MARE-Madeira, the largest non-profit aquatic research institute in Madeira, is working with partners at the Helmholtz Center for Ocean Research Kiel (GEOMAR) and the Norwegian University of Science and Technology (NTNU) to do just that. Funded by the European Commission Horizon Europe program and within the project TWILIGHTED (TWInning Laboratory for an Innovative, Global Hub To Explore the Deep), we are working to strengthen deep-sea research capacity in Madeira, to develop lower-cost methods for exploring and monitoring deeper waters and, ultimately, to create a global hub for deep-sea research on the island. 

Whether you have deep-sea experience or not, and especially those from small islands and institutes that have been financially restricted from participating in deep-sea research in the past, we invite you to join our capacity-building journey. Follow us on social media, use the how-to guides for low-cost tools we’ll share on our website and sign up to our Impossible Things Workshops or International Twilighted Conference. We hope to engage more fully in this important and globally underfunded area of research in the coming years and together help build a future where deep-sea research is done more efficiently, more quickly and even more collaboratively.

Funding acknowledgement: The TWILIGHTED project is funded by the European Commission’s Horizon EuropeTwinning program.

How to cite: Esson, D., Monteiro, J., Radeta, M., Hoving, H.-J., Dierking, J., Širović, A., Aberle-Malzahn, N., Ludvigsen, M., and Canning-Clode, J.: Madeira: A Global Deep-Sea Research Hub in the Atlantic, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1133, https://doi.org/10.5194/oos2025-1133, 2025.

P376
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OOS2025-1291
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ECOP
Pauline Le coq, Marc Garel, and Christian Tamburini

The deep ocean, one of Earth's largest and least explored biomes, spans depths with extreme conditions, including high hydrostatic pressure, low temperatures, and minimal organic carbon. These characteristics significantly influence microbial life, requiring unique adaptations for survival and metabolic function. Prokaryotes thriving in high-pressure environments are known as piezophiles (Tamburini et al. 2013 and references therein). Those deep-sea micro-organisms adapt to high-pressure environments through cellular and genetic changes, constitute ‘bathytypes’  specific  to ocean depths (Oger and Jebbar 2010; Peoples and Bartlett 2017).

Due to technical challenges in sampling under in situ conditions, much of the data about deep-sea microbes has historically been gathered under decompressed conditions. This decompression can result in significant changes in community composition (La Cono et al. 2009; Edgcomb et al. 2016; Garel et al. 2019) and activity (Tamburini et al. 2013; Garel et al. 2019), which generally leads to underestimated assessments of their ecological roles. Innovations, such as pressure-retaining samplers (Peoples and Bartlett 2017; Garel et al. 2019) or in situ microbial incubator (Amano et al. 2022a), now allow for the collection or incubation of samples at in situ pressures, preserving the natural state of these microorganisms for more accurate study .

Deep-sea microbes play a critical role in the global carbon cycle, particularly through their participation in the biological carbon pump, which involves the decomposition and mineralization of organic material as it sinks through the water column (Arıstegui et al. 2009). Research suggests that deep-sea microbes are dynamically responsive to organic matter input, with a substantial portion of global heterotrophic production occurring below the photic zone. According to Aristegui et al. (2009) the integrated prokaryotic heterotrophic production (PHP) in the dark ocean represents around 50% of the total water column. Understanding the pressure effect on prokaryotic activities is crucial to better estimate their role in the remineralization in the dark ocean. However, to date, the effect of decompression is controversial, depending on the methodology used and the authors (Amano et al. 2022b versus Tamburini et al. 2013 and reference therein). 

Continued advancements in sampling technology and high-throughput sequencing will likely reveal more about these resilient organisms' ecological roles and physiological capacities, enhancing our comprehension of the deep ocean's contributions to Earth's biogeochemical processes​.

Over the last few years, pressure-retaining samplers were deployed during different oceanographic cruises in North Atlantic Ocean and in the Mediterranean Sea, allowing the constitution of a unique dataset of PHP rates (using 3H-Leucine) and MICROFISH, under in situ conditions. Among this cruise, a specific one dedicated to the study of deep convection and re-stratification phenomena brings new insights in the biological and physical coupling of this study area, and the necessity to well understand this context when talking about organisms adapted to pressure or not. Pressure effects on other activities (dark dissolved inorganic carbon fixation, ectoenzymatic activities, and high molecular organic compounds' degradation) will also be presented. Finally, we will also show how surface prokaryotes attached to gravitationally sinking particles cope with the increase in pressure with depth.

How to cite: Le coq, P., Garel, M., and Tamburini, C.: Life under pressure in prokaryotes and the impact on the biological carbon pump, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1291, https://doi.org/10.5194/oos2025-1291, 2025.

P377
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OOS2025-1380
Towards defining inactive hydrothermal ecosystems on the Arctic Mid-Ocean Ridge, an area targeted for future seabed mining
(withdrawn)
Pedro Ribeiro, Thibaut Barreyre, and Eoghan Reeves
P378
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OOS2025-1501
Paula Andrea Zapata-Ramirez, Alex Bastos, Jonathan Delance, Luisa Dueñas, Elva Escobar, Jorge Cortés, Juan Armando Sánchez, Carlos Edwin Gómez, Milena Benavides, Ximena Rojas, Angel Pérez, Marta Díaz, and Martin Visbeck

The Latin American Deep Sea Exploration Network (LADEN) is an initiative aimed at building a collaborative, interdisciplinary, and sustainable network across Latin America to explore, protect, and sustainably manage deep-sea ecosystems. The concept of LADEN is based on the recent Deep Blue Initiative that forms a global platform for deep-sea research cooperation, mobilization, funding and equitable capacity sharing. This network will leverage the region’s local expertise, international partnerships, and philanthropic support to ensure that Latin American countries, particularly those with less developed infrastructure, can contribute to and benefit from cutting-edge marine science and technology. Through this collective effort, LADEN will prioritize scientific research, technological innovation, early-career scientists’ development, best practices and standardize research methods and data analysis and capacity building and sharing to address critical environmental challenges in the deep ocean, aiming for biodiversity conservation and ocean literacy.  This initiative brings together experts, organizations, and governments from multiple disciplines and regions to identify key information gaps and resolve bottlenecks in deep-sea exploration. LADEN will build upon this collaborative foundation to expand its efforts in Latin America, working across national borders to share resources, knowledge, and expertise.

LADEN is scientifically based on ongoing national initiatives in deep-sea research across Latin America, such as cold-water coral studies, seabed habitat mapping, geohazards assessment, biodiversity conservation efforts, among others. One of LADEN’s core objectives is to provide the essential baseline data needed to better understand the often- overlooked deep-sea areas within the region. This data will support the effective management and designation of new Marine Protected Areas (MPAs), help achieve the global 30x30 conservation goals and complement the provisions of the Biodiversity Beyond National Jurisdiction (BBNJ) treaty. Additionally, LADEN will foster collaboration by connecting diverse deep-sea research communities and across and governmental actors accros Latin America and linking them with global counterparts and established networks, such as the Deep-Ocean Stewardship Initiative (DOSI) and Challenger 150, an African-based network focused on deep-sea exploration. Through these united efforts, LADEN will position Latin America as a decisive contributor to global marine conservation and sustainable deep-ocean management.

 

How to cite: Zapata-Ramirez, P. A., Bastos, A., Delance, J., Dueñas, L., Escobar, E., Cortés, J., Sánchez, J. A., Gómez, C. E., Benavides, M., Rojas, X., Pérez, A., Díaz, M., and Visbeck, M.: Towards the implementation of the Latin American Deep Sea Exploration Network (LADEN), One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1501, https://doi.org/10.5194/oos2025-1501, 2025.

P379
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OOS2025-1532
Kristin Kleisner, Chris Dorsett, and Kilaparti Ramakrishna

The twilight or mesopelagic zone is host to a wealth of ocean biodiversity. A critical component of the ocean food web,these species are important prey species. Due to daily mass migrations, mesopelagic species transfer 2-6 gigatons of carbon per year to the deep sea, an amount equivalent to twice the emissions produced by cars worldwide annually. Recognizing the significant abundance of biomass in the twilight zone, efforts have been made over time to commercially extract these resources. While none of those past fisheries have resulted in fishing at scale, interest remains and pressure to find new sources of protein is rising as current stocks of small pelagic species, critical inputs to fishmeal and fish oil production, are declining or shifting their distributions due to climate change. Other potential activities associated with deep-sea mining and marine carbon dioxide reduction may impact the natural carbon sequestration pathways facilitated by the mesopelagic. Given what we know about the importance of the twilight zone, it is imperative that these critical ecological and climate services are protected. A number of published papers have identified pathways for large-scale protections. They include actions within country EEZs based on existing governance frameworks, expert guidance from the UN Food and Agriculture Organization, the IPCC, and the wider scientific community, actions by regional fishery management organizations, expansion of the role of the London Protocol on regulating marine carbon dioxide reduction research; and the pending ratification of the BBNJ agreement. This talk will present the work of a group of actors spanning academia, NGOs, and government entities to leverage the existing base of science and knowledge about the ocean twilight zone in support of sound policy to protect these critical resources.

How to cite: Kleisner, K., Dorsett, C., and Ramakrishna, K.: Protecting the ocean twilight zone: Building from Science to Action, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1532, https://doi.org/10.5194/oos2025-1532, 2025.

Posters virtual | online

Display time: Tue, 3 Jun, 17:00–Thu, 5 Jun, 20:00
vP88
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OOS2025-70
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ECOP
Hammoud El Vadhel

The objective of this study is to describe the associated fauna of the two cold water coral (CWC) ecosystems occurring off Mauritania; the chain of mounds and the live reefs.

The fauna inhabiting the coral mound has been described through a comparative analysis of trawl catches from coral mounds (400-600m) and catches from adjacent off-mound areas (200-350m) conducted from 1982 to 2022 by four research vessels, while the fauna associated with CWC reef habitats was described through the analysis of 11 video dives undertaken by using ROV as part of two seafloor habitat mapping surveys conducted by the R/V Dr. Fridtjof Nansen off Mauritania in 2020 and 2021.

Analysis of 47 trawling station data carried out on coral mounds off Mauritania revealed significant diversity. Overall, 282 taxa were identified, these species belong to the 5 taxonomic group, Fish (187), Crustacea (56), Mollusca (31), Cnidaria (5) and Echinodermata (3). The most ten species inhabiting coral mound was: Helicolenus dactylopterus, Laemonema laureysi, Merluccius polli, Coelorinchus caelorhincus, Hoplostethus cadenati, Malacocephalus occidentalis, Gephyroberyx darwinii, Hoplostethus mediterraneus, Galeus polli and Malacocephalus laevis. Results showed also that the values ​​of the diversity indices (richness, Shannon and Simpson index, accumulation curve) were higher on-mound than off-mound.

The analysis of 11 ROV dives allowed to identify eighth species of CWC to species level, the most abundant was the gorgonian coral Acanthogorgia cf. hirsuta followed by Desmophyllum pertusum, Swiftia phaeton (a new octocoral species of Swiftia), the sea fan Thesea talismani, Madrepora oculata, the black coral Tanacetipathes cf. spinescens, Anthomastus cf. grandifloras and Clavularia borealis.

The results showed that the reef offers habitat for many species. In effect, 120 taxa belonging to 68 families have been identified divided into 11 groups, the group of fish was the most represented with 47 taxa, followed by the group of cnidaria (18 taxa), crustacea (17 taxa), Mollusca and Echinodermata with 11 taxa for each group and Porifera with 7 taxa. In terms of occurrence, H. dactylopterus was the most observed for the fish group, with over 371 individuals. The cnidarians are dominated by the lesser cylinder anemone Synarachnactis cf. lloydii with more than 13000 individuals. For the crustaceans, the African spider shrimp Nematocarcinus africanus is the most common with more than 900 individuals. As far as the group of mollusks is concerned, the bivalve Gigantidas mauritanicus is the most observed with more than 1800 individuals. The sponge Cladorhiza corallophila was common for the group of Porifera. Several of these species are known to be associated with CWC from other studies even though the reefs are in an oxygen minimum zone they offer habitats for many of the same associates.

The results of our study provide insight to the importance of these CWC habitats to the Mauritanian deep-sea ecosystem, information that is essential for the development of a national management plan for use of marine resources and their ecosystems, especially in the face of ongoing environmental challenges (e.g. oil and gas activities, deep sea fishing etc.).

 

How to cite: El Vadhel, H.: Cold-water coral reefs and mounds off Mauritania and associated fauna, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-70, https://doi.org/10.5194/oos2025-70, 2025.

vP89
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OOS2025-1117
Jean-Romain Lagadec

The fixed-point profiler project, called PROLIXE, aims to develop a measurement and observation system capable of moving between the seabed (up to 6,000 m) and the sub-surface, along an anchored mooring line, so as to characterize the entire water column at a given geographical position, with adaptative sampling intervals. The system must be capable of recharging its batteries at regular intervals on a docking station to ensure long autonomy. This station is designed to be used either on a standalone mode or connected to a cabled node. This project is part of the « technological innovation » activities of the IFREMER ScInObs project (science and innovation for subsea observatories).

How to cite: Lagadec, J.-R.: PROLIXE, a versatile long-term profiling mooring, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1117, https://doi.org/10.5194/oos2025-1117, 2025.

vP90
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OOS2025-1156
Jérôme Blandin

The resident AUV (Autonomous Underwater Vehicle) project aims at developing an observation vehicle based on and returning from a cabled observation infrastructure on the seabed, so as to extend its observation radius without recourse to a ship. It is the mobile extension of a permanent fixed-point underwater observation system, designed for reducing the cost of in situ observational data, decreasing their environmental footprint and broadening their spatial range. The project has started in May 2023. It is currently focusing on de-risking the main critical building blocks associated to resident systems (docking maneuver, contactless data/power transmission, secured positioning) before launching the design of the vehicle itself. This project is part of the « technological innovation » activities of the IFREMER ScInObs project (science and innovation for subsea observatories).

How to cite: Blandin, J.: Development of a resident AUV for scientific observation, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1156, https://doi.org/10.5194/oos2025-1156, 2025.