Zooplankton-mediated fluxes in the eastern tropical North Atlantic
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...
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2021
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ftoslouniv:oai:www.duo.uio.no:10852/82601 2023-05-15T17:32:38+02:00 Zooplankton-mediated fluxes in the eastern tropical North Atlantic Kiko, Rainer Brandt, Peter Christiansen, Svenja Faustmann, Jannik Kriest, Iris Rodrigues, Elizandro Schütte, Florian Hauss, Helena 2021-01-18T14:02:59Z http://hdl.handle.net/10852/82601 http://urn.nb.no/URN:NBN:no-85477 https://doi.org/10.3389/fmars.2020.00358 EN eng http://urn.nb.no/URN:NBN:no-85477 Kiko, Rainer Brandt, Peter Christiansen, Svenja Faustmann, Jannik Kriest, Iris Rodrigues, Elizandro Schütte, Florian Hauss, Helena . Zooplankton-mediated fluxes in the eastern tropical North Atlantic. Frontiers in Marine Science. 2020, 7 http://hdl.handle.net/10852/82601 1873307 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Frontiers in Marine Science&rft.volume=7&rft.spage=&rft.date=2020 Frontiers in Marine Science 7 21 https://doi.org/10.3389/fmars.2020.00358 URN:NBN:no-85477 Fulltext https://www.duo.uio.no/bitstream/handle/10852/82601/2/Kiko_et_al_2020_FMARS.pdf Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ CC-BY 2296-7745 Journal article Tidsskriftartikkel Peer reviewed PublishedVersion 2021 ftoslouniv https://doi.org/10.3389/fmars.2020.00358 2021-01-27T23:31:09Z 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. Article in Journal/Newspaper North Atlantic Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Frontiers in Marine Science 7 |
institution |
Open Polar |
collection |
Universitet i Oslo: Digitale utgivelser ved UiO (DUO) |
op_collection_id |
ftoslouniv |
language |
English |
description |
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. |
format |
Article in Journal/Newspaper |
author |
Kiko, Rainer Brandt, Peter Christiansen, Svenja Faustmann, Jannik Kriest, Iris Rodrigues, Elizandro Schütte, Florian Hauss, Helena |
spellingShingle |
Kiko, Rainer Brandt, Peter Christiansen, Svenja Faustmann, Jannik Kriest, Iris Rodrigues, Elizandro Schütte, Florian Hauss, Helena Zooplankton-mediated fluxes in the eastern tropical North Atlantic |
author_facet |
Kiko, Rainer Brandt, Peter Christiansen, Svenja Faustmann, Jannik Kriest, Iris Rodrigues, Elizandro Schütte, Florian Hauss, Helena |
author_sort |
Kiko, Rainer |
title |
Zooplankton-mediated fluxes in the eastern tropical North Atlantic |
title_short |
Zooplankton-mediated fluxes in the eastern tropical North Atlantic |
title_full |
Zooplankton-mediated fluxes in the eastern tropical North Atlantic |
title_fullStr |
Zooplankton-mediated fluxes in the eastern tropical North Atlantic |
title_full_unstemmed |
Zooplankton-mediated fluxes in the eastern tropical North Atlantic |
title_sort |
zooplankton-mediated fluxes in the eastern tropical north atlantic |
publishDate |
2021 |
url |
http://hdl.handle.net/10852/82601 http://urn.nb.no/URN:NBN:no-85477 https://doi.org/10.3389/fmars.2020.00358 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
2296-7745 |
op_relation |
http://urn.nb.no/URN:NBN:no-85477 Kiko, Rainer Brandt, Peter Christiansen, Svenja Faustmann, Jannik Kriest, Iris Rodrigues, Elizandro Schütte, Florian Hauss, Helena . Zooplankton-mediated fluxes in the eastern tropical North Atlantic. Frontiers in Marine Science. 2020, 7 http://hdl.handle.net/10852/82601 1873307 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Frontiers in Marine Science&rft.volume=7&rft.spage=&rft.date=2020 Frontiers in Marine Science 7 21 https://doi.org/10.3389/fmars.2020.00358 URN:NBN:no-85477 Fulltext https://www.duo.uio.no/bitstream/handle/10852/82601/2/Kiko_et_al_2020_FMARS.pdf |
op_rights |
Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.3389/fmars.2020.00358 |
container_title |
Frontiers in Marine Science |
container_volume |
7 |
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1766130854455672832 |