Zooplankton-Mediated Fluxes in the Eastern Tropical North Atlantic

• Published in: Frontiers in Marine Science
• Main Authors: Kiko, Rainer, Brandt, Peter, Christiansen, Svenja, Faustmann, Jannik, Kriest, Iris, Rodrigues, Elizandro, Schütte, Florian, Hauss, Helena
• Other Authors: Helmholtz Centre for Ocean Research Kiel (GEOMAR), Laboratoire d'océanographie de Villefranche (LOV), Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut de la Mer de Villefranche (IMEV), Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Christian-Albrechts-Universität zu Kiel = Christian-Albrechts University of Kiel = Université Christian-Albrechts de Kiel (CAU), Department of Biosciences Oslo, University of Oslo (UiO), Instituto Nacional de Desenvolvimento das Pescas (INDP), ANR-19-MPGA-0012,TAD,Tropical Atlantic Deoxygenation: gateway dynamics, feedback mechanisms and ecosystem impacts(2019)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2020
• Subjects: zooplankton; tropical Atlantic; oxygen minimum zone; diel vertical migration; biogeochemical fluxes; martin curve; Cape Verde ocean observatory Kiko et al Zooplankton-Mediated Fluxes Tropical Atlantic; [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography; North Atlantic
• Online Access: https://hal.sorbonne-universite.fr/hal-02865373; https://hal.sorbonne-universite.fr/hal-02865373/document; https://hal.sorbonne-universite.fr/hal-02865373/file/fmars-07-00358.pdf; https://doi.org/10.3389/fmars.2020.00358

International audience Zooplankton organisms are a central part of pelagic ecosystems. They feed on all kinds of particulate matter and their egested fecal pellets contribute substantially to the passive sinking flux to depth. Some zooplankton species also conduct diel vertical migrations (DVMs) between the surface layer (where they feed at nighttime) and midwater depth (where they hide at daytime from predation). These DVMs cause the active export of organic and inorganic matter from the surface layer as zooplankton organisms excrete, defecate, respire, die, and are preyed upon at depth. In the Eastern Tropical North Atlantic (ETNA), the daytime distribution depth of many migrators (300-600 m) coincides with an expanding and intensifying oxygen minimum zone (OMZ). We here assess the day and night-time biomass distribution of mesozooplankton with an equivalent spherical diameter of 0.39-20 mm in three regions of the ETNA, calculate the DVM-mediated fluxes and compare these to particulate matter fluxes and other biogeochemical processes. Integrated mesozooplankton biomass in the ETNA region is about twice as high at a central OMZ location (cOMZ; 11 • N, 21 • W) compared to the Cape Verde Ocean Observatory (CVOO; 17.6 • N, 24.3 • W) and an oligotrophic location at 5 • N, 23 • W (5N). An Intermediate Particle Maximum (IPM) is particularly strong at cOMZ compared to the other regions. This IPM seems to be related to DVM activity. Zooplankton DVM was found to be responsible for about 31-41% of nitrogen loss from the upper 200m of the water column. Gut flux and mortality make up about 31% of particulate matter supply to the 300-600 m depth layer at cOMZ, whereas it makes up about 32% and 41% at CVOO and 5N, respectively. Resident and migrant zooplankton are responsible for about 7-27% of the total oxygen demand at 300-600 m depth. Changes in zooplankton abundance and migration behavior due to decreasing oxygen levels at midwater depth could therefore alter the elemental cycling of oxygen and carbon in the ETNA OMZ ...