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Sea-ice associated carbon flux in Arctic spring

Bibliographic Data

ID19568760
AuthorsJulia Ehrlich (0000-0002-1192-1361, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung), Bodil A Bluhm (0000-0002-4584-7796, UiT The Arctic University of Norway), Ilka Peeken (0000-0003-1531-1664, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung), Philippe Massicotte (0000-0002-5919-4116, Université Laval), Fokje L Schaafsma (0000-0002-8945-2868), Giulia Castellani (0000-0001-6151-015X, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung), Angelika Brandt (0000-0002-5807-1632, Goethe University Frankfurt), Hauke Flores (0000-0003-1617-5449, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung)
Year2021
Volume9
Issue1
Publication date2021-10-13
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.1525/elementa.2020.00169
OpenAlexW3207552413
LanguageEN
Citations received3
References cited76

The Svalbard region faces drastic environmental changes, including sea-ice loss and “Atlantification” of Arctic waters, caused primarily by climate warming. These changes result in shifts in the sea-ice-associated (sympagic) community structure, with consequences for the sympagic food web and carbon cycling. To evaluate the role of sympagic biota as a source, sink, and transmitter of carbon, we sampled pack ice and under-ice water (0–2 m) north of Svalbard in spring 2015 by sea-ice coring and under-ice trawling. We estimated biomass and primary production of ice algae and under-ice phytoplankton as well as biomass, carbon demand, and secondary production of sea-ice meiofauna (>10 μm) and under-ice fauna (>300 μm). Sea-ice meiofauna biomass (0.1–2.8 mg C m–2) was dominated by harpacticoid copepods (92%), nauplii (4%), and Ciliophora (3%). Under-ice fauna biomass (3.2–62.7 mg C m–2) was dominated by Calanus copepods (54%). Appendicularia contributed 23% through their high abundance at one station. Herbivorous sympagic fauna dominated the carbon demand across the study area, estimated at 2 mg C m–2 day–1 for ice algae and 4 mg C m–2 day–1 for phytoplankton. This demand was covered by the mean primary production of ice algae (11 mg C m–2 day–1) and phytoplankton (30 mg C m–2 day–1). Hence, potentially 35 mg C m–2 day–1 of algal material could sink from the sympagic realm to deeper layers. The demand of carnivorous under-ice fauna (0.3 mg C m–2 day–1) was barely covered by sympagic secondary production (0.3 mg C m–2 day–1). Our study emphasizes the importance of under-ice fauna for the carbon flux from sea ice to pelagic and benthic habitats and provides a baseline for future comparisons in the context of climate change

Arctic · Arctic ice pack · Benthic zone · Biology · Biota · Cryosphere · Meiobenthos · Nutrient · Phytoplankton · Sea ice · Arctic and Antarctic ice dynamics · Environmental Science · Marine and environmental studies · Ocean Acidification Effects and Responses · Ecology · Geology · Oceanography

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Unique citing works3
Citations per year0.6
Citation span2021 - 2025 (5)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 2

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