EGU25-11373, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-11373
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Friday, 02 May, 15:35–15:45 (CEST)
 
Room L2
Unraveling planktonic ecosystems dynamics using imaging sensors on BGC-Argo floats
Lars Stemmann1, Kiko Rainer2, Lacour Léo3, Accardo Alexandre3, Arlaud Marin3, Baudena Alberto4, Boyd Philip5, Catalano Camille3, Claustre Hervé3, Guidi Lionel3, Habib Joelle3, Irisson Jean Olivier3, Leymarie Edouard3, Lombard Fabien3, Maury Juliette3, Nocera Ariadna6, Picheral Marc3, Poteau Antoine3, and Soviadan Yawouwi Dodji7
Lars Stemmann et al.
  • 1Institut Universitaire de France, Sorbonne Université, CNRS, Laboratoire de Villefranche sur Mer, France (lars.stemmann@imev-mer.fr)
  • 2GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
  • 3Sorbonne Université, CNRS, Laboratoire d’Océanographie de Villefranche, UMR 7093 LOV, Villefranche-sur-Mer, France
  • 4Consiglio Nazionale Delle Ricerche- Istituto di Scienze Marine (CNR-ISMAR), Lerici (SP), Italy
  • 5University of Tasmania
  • 6CESIMAR-CCT CONICET, Puerto Madryn, Argentina
  • 7MARBEC, IRD, IFREMER, CNRS, Université de Montpellier, 87 Avenue Jean Monnet, 34200 Sète, France

Simultaneous detection and sizing of plankton and marine particles is now possible at global scale with the Underwater Vision Profiler 6 (UVP6) mounted on BGC-Argo floats. Combined with other biogeochemical sensors, the UVP6 delivers Essential Ocean Variables (EOVs), from nutrients to plankton and detritus, critical for monitoring and modeling. To date, over a hundred of UVP6 have been deployed by different laboratories across all oceans. When deployed on BGC-Argo floats, particle size distribution or taxa counts -obtained through embedded recognition, are typically the only available data, as the floats are generally not recovered. Here we report multi-year patterns of plankton and particles obtained from four successful deployments and recoveries at different latitudes, ranging from the equator to 50° South and depths down to 2000 m. Objects larger than 0.6 mm were classified using machine learning recognition (for plankton and particle) and k-means clustering (only for particles) methods. To date, five morphological categories of marine snow (particles > 500µm) were defined, based on shape, darkness, and structural heterogeneity, while plankton images were validated by experts in 20 broad categories. We show how these results can be used to assess plankton diversity, detritus composition, carbon vertical flux, and attenuation down to the bathypelagic layers in a wide range of environmental conditions. In cases of low mesoscale activity, results show that different phytoplankton blooms produce different marine snow morphotypes having different fates. Dense marine snow is found to be the most exported and also the deepest (down to 2000 m depth). Other morphotypes, such as filaments or porous marine snow, were generally not exported below the surface layer. Size and morphology were important to determine marine snow sinking speed. In high mesoscale activity, the steady marine snowfall is disrupted by ocean horizontal and vertical circulations and intermittent export events are observed down to 600m depth. When fully integrated in a global network of BGC-Argo floats, underwater cameras will complement existing global observations of biogeochemical variables and small planktonic organisms, detected by optical sensors, by also capturing data on larger organisms and particles.

How to cite: Stemmann, L., Rainer, K., Léo, L., Alexandre, A., Marin, A., Alberto, B., Philip, B., Camille, C., Hervé, C., Lionel, G., Joelle, H., Jean Olivier, I., Edouard, L., Fabien, L., Juliette, M., Ariadna, N., Marc, P., Antoine, P., and Dodji, S. Y.: Unraveling planktonic ecosystems dynamics using imaging sensors on BGC-Argo floats, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-11373, https://doi.org/10.5194/egusphere-egu25-11373, 2025.