Phytoplankton reaction to an intense storm in the north-western Mediterranean Sea

Type Article
Acceptance Date 2022-07-07 IN PRESS
Language English
Author(s) Barrillon StéphanieORCID1, Fuchs RobinORCID1, 2, Petrenko Anne A.ORCID1, Comby Caroline1, Bosse AnthonyORCID1, Yohia Christophe3, Fuda Jean-Luc1, Bhairy Nagib1, Cyr FrédéricORCID4, Doglioli Andrea M.ORCID1, Grégori GéraldORCID1, Tzortzis RoxaneORCID1, D'Ovidio Franscesco5, Thyssen Melilotus1
Affiliation(s) 1 : Aix Marseille Univ., Université de Toulon, CNRS, IRD, MIO UM 110 , 13288, Marseille, France
2 : Aix Marseille Univ, CNRS, Centrale Marseille, I2M, Marseille, France
3 : Aix Marseille Univ., Université de Toulon, CNRS, IRD, OSU Pytheas UAR 3470 , 13288, Marseille, France
4 : Fisheries and Oceans Canada, Northwest Atlantic Fisheries Centre, St. John’s, Canada
5 : LOCEAN, UMR CNRS / Université P. et M. Curie / IRD / MNHM, F-75005 Paris, France
Source Biogeosciences (1726-4189) (Copernicus GmbH) In Press
DOI 10.5194/bg-20-141-2023

 The study of extreme weather events and their impact on ocean physics and biogeochemistry is challenging due to the difficulty of collecting in situ data. Yet, recent research pointed out the major influence of such physical forcing events on microbiological organisms. Moreover, such violent event occurrences may rise in the future in the context of global change. In May 2019, an intense storm occurred in the Ligurian Sea (north-western Mediterranean Sea) and was captured during the FUMSECK cruise. In situ multi-platform measurements (vessel-mounted ADCP, thermosaligraph, fluorometer, flow cytometer, a Moving Vessel Profiler equipped with a multi-sensor towed vehicle, and glider) along with satellite data and a 3D atmospherical model were used to characterise the fine-scale dynamics occurring in the impacted oceanic zone. The most affected area was marked by a lower water temperature (1 °C colder), and an increase by a factor two in surface chlorophyll-a and seven in nitrate concentrations, exhibiting strong gradients with respect to the surrounding waters. Our results show that this storm led to a deepening of the mixed layer depth from 15 to 50 m and a dilution of the deep chlorophyll maximum. As a result, the surface phytoplankton biomass of most groups identified by automated flow cytometry increased by up to a factor of two. Conversely, the phytoplankton carbon-chlorophyll ratio of most groups dropped down by a factor of two, evidencing significant changes in the phytoplankton cell compositions. These results suggest that the role of storms on the biogeochemistry and ecology of the Mediterranean open sea may be underestimated and highlight the need for high-resolution measurements coupling physics and biology during these events.

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Barrillon Stéphanie, Fuchs Robin, Petrenko Anne A., Comby Caroline, Bosse Anthony, Yohia Christophe, Fuda Jean-Luc, Bhairy Nagib, Cyr Frédéric, Doglioli Andrea M., Grégori Gérald, Tzortzis Roxane, D'Ovidio Franscesco, Thyssen Melilotus Phytoplankton reaction to an intense storm in the north-western Mediterranean Sea. Biogeosciences IN PRESS. Publisher's official version : , Open Access version :