Zooplankton-Mediated Fluxes in the Eastern Tropical North Atlantic.

Kiko, Rainer , Brandt, Peter , Christiansen, Svenja, Faustmann, Jannik, Kriest, Iris , Rodrigues, Elizandro, Schütte, Florian and Hauss, Helena (2020) Zooplankton-Mediated Fluxes in the Eastern Tropical North Atlantic. Open Access Frontiers in Marine Science, 7 . Art.Nr. 358. DOI 10.3389/fmars.2020.00358.

[img]
Preview
Text
fmars-07-00358.pdf - Published Version
Available under License Creative Commons: Attribution 4.0.

Download (1937Kb) | Preview
[img]
Preview
Text
Data_Sheet_1_Zooplankton-Mediated Fluxes in the Eastern Tropical North Atlantic.pdf - Supplemental Material
Available under License Creative Commons: Attribution 4.0.

Download (395Kb) | Preview

Supplementary data:

Abstract

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 and impact the removal of nitrogen from the surface layer.

Document Type: Article
Keywords: zooplankton, tropical Atlantic, oxygen minimum zone, diel vertical migration, biogeochemical fluxes, martin curve, Cape Verde ocean observatory
Research affiliation: OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-CH Chemical Oceanography
OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-BM Biogeochemical Modeling
OceanRep > GEOMAR > FB3 Marine Ecology > FB3-OEB Ökosystembiologie des Ozeans
OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-PO Physical Oceanography
OceanRep > SFB 754
OceanRep > GEOMAR > FB3 Marine Ecology > FB3-EOE-B Experimental Ecology - Benthic Ecology
Refereed: Yes
Open Access Journal?: Yes
DOI etc.: 10.3389/fmars.2020.00358
ISSN: 2296-7745
Projects: SFB754, iAtlantic, TRIATLAS
Expeditions/Models/Experiments:
Date Deposited: 02 Jun 2020 12:20
Last Modified: 16 Jun 2020 09:03
URI: http://oceanrep.geomar.de/id/eprint/49791

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...