Aggregate Feeding by the Copepods Calanus and Pseudocalanus Controls Carbon Flux Attenuation in the Arctic Shelf Sea During the Productive Period

Up to 95% of the oceanic primary production is recycled within the upper few hundred meters of the water column. Marine snow and zooplankton fecal pellets in the upper water column are often recycled at rates exceeding those measured for microbial degradation, suggesting that zooplankton might be im...

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Main Authors: Helga van der Jagt, Ingrid Wiedmann, Nicole Hildebrandt, Barbara Niehoff, Morten H. Iversen
Format: Article
Language:English
Published: Frontiers Media S.A. 2020-09-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fmars.2020.543124/full
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author Helga van der Jagt
Helga van der Jagt
Ingrid Wiedmann
Nicole Hildebrandt
Barbara Niehoff
Morten H. Iversen
Morten H. Iversen
author_facet Helga van der Jagt
Helga van der Jagt
Ingrid Wiedmann
Nicole Hildebrandt
Barbara Niehoff
Morten H. Iversen
Morten H. Iversen
author_sort Helga van der Jagt
collection DOAJ
description Up to 95% of the oceanic primary production is recycled within the upper few hundred meters of the water column. Marine snow and zooplankton fecal pellets in the upper water column are often recycled at rates exceeding those measured for microbial degradation, suggesting that zooplankton might be important for flux attenuation of particulate organic carbon in the upper ocean. However, direct evidence for interactions between zooplankton and settling aggregates are still rare. We investigated the importance of zooplankton aggregate feeding for carbon flux attenuation in the upper ocean by determining aggregate ingestion rates and feeding behavior on settling aggregates by the dominant Arctic filter-feeding copepods Calanus spp. and Pseudocalanus spp. Both genera were observed to detect and feed on settling aggregates. Using in situ zooplankton and aggregate abundances in combination with the measured aggregate feeding rates, we calculated that 60–67% of the total carbon flux attenuation at three Arctic locations could be explained by Calanus spp. and Pseudocalanus spp. aggregate feeding alone. When including microbial degradation of the settling aggregates, we could explain up to 77% of the total carbon flux attenuation. Our results suggest that by directly ingesting and fragmenting settling marine snow, mesozooplankton are key organisms for flux attenuation in Arctic waters.
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spelling doaj.art-6d684da757a6450b83fde8448d46ba332022-12-22T00:40:40ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452020-09-01710.3389/fmars.2020.543124543124Aggregate Feeding by the Copepods Calanus and Pseudocalanus Controls Carbon Flux Attenuation in the Arctic Shelf Sea During the Productive PeriodHelga van der Jagt0Helga van der Jagt1Ingrid Wiedmann2Nicole Hildebrandt3Barbara Niehoff4Morten H. Iversen5Morten H. Iversen6Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, GermanyMARUM and University of Bremen, Bremen, GermanyUiT The Arctic University of Norway, Tromsø, NorwayAlfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, GermanyAlfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, GermanyAlfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, GermanyMARUM and University of Bremen, Bremen, GermanyUp to 95% of the oceanic primary production is recycled within the upper few hundred meters of the water column. Marine snow and zooplankton fecal pellets in the upper water column are often recycled at rates exceeding those measured for microbial degradation, suggesting that zooplankton might be important for flux attenuation of particulate organic carbon in the upper ocean. However, direct evidence for interactions between zooplankton and settling aggregates are still rare. We investigated the importance of zooplankton aggregate feeding for carbon flux attenuation in the upper ocean by determining aggregate ingestion rates and feeding behavior on settling aggregates by the dominant Arctic filter-feeding copepods Calanus spp. and Pseudocalanus spp. Both genera were observed to detect and feed on settling aggregates. Using in situ zooplankton and aggregate abundances in combination with the measured aggregate feeding rates, we calculated that 60–67% of the total carbon flux attenuation at three Arctic locations could be explained by Calanus spp. and Pseudocalanus spp. aggregate feeding alone. When including microbial degradation of the settling aggregates, we could explain up to 77% of the total carbon flux attenuation. Our results suggest that by directly ingesting and fragmenting settling marine snow, mesozooplankton are key organisms for flux attenuation in Arctic waters.https://www.frontiersin.org/article/10.3389/fmars.2020.543124/fullmarine snowzooplankton aggregate feedingin situ opticssediment trapszooplankton feeding behavior
spellingShingle Helga van der Jagt
Helga van der Jagt
Ingrid Wiedmann
Nicole Hildebrandt
Barbara Niehoff
Morten H. Iversen
Morten H. Iversen
Aggregate Feeding by the Copepods Calanus and Pseudocalanus Controls Carbon Flux Attenuation in the Arctic Shelf Sea During the Productive Period
Frontiers in Marine Science
marine snow
zooplankton aggregate feeding
in situ optics
sediment traps
zooplankton feeding behavior
title Aggregate Feeding by the Copepods Calanus and Pseudocalanus Controls Carbon Flux Attenuation in the Arctic Shelf Sea During the Productive Period
title_full Aggregate Feeding by the Copepods Calanus and Pseudocalanus Controls Carbon Flux Attenuation in the Arctic Shelf Sea During the Productive Period
title_fullStr Aggregate Feeding by the Copepods Calanus and Pseudocalanus Controls Carbon Flux Attenuation in the Arctic Shelf Sea During the Productive Period
title_full_unstemmed Aggregate Feeding by the Copepods Calanus and Pseudocalanus Controls Carbon Flux Attenuation in the Arctic Shelf Sea During the Productive Period
title_short Aggregate Feeding by the Copepods Calanus and Pseudocalanus Controls Carbon Flux Attenuation in the Arctic Shelf Sea During the Productive Period
title_sort aggregate feeding by the copepods calanus and pseudocalanus controls carbon flux attenuation in the arctic shelf sea during the productive period
topic marine snow
zooplankton aggregate feeding
in situ optics
sediment traps
zooplankton feeding behavior
url https://www.frontiersin.org/article/10.3389/fmars.2020.543124/full
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