A pan-Arctic perspective on the influence of ice algae on sea-ice nutrient concentrations

Sea-ice algae account for a substantial part of annual primary production in ice-covered waters and are an important component of the Arctic marine food web. With climate-induced changes to snow and sea-ice cover and their impact on the surface ocean, such as earlier melt, thinner ice, and increased upper-ocean stratification, a shift toward earlier and more extensive nutrient limitation on ice algal growth can be expected. Therefore, increasing our understanding of the processes governing nutrient supply and uptake by sea-ice algae is essential. Here, we compiled a pan-Arctic dataset of concentrations of sea-ice and sub-ice nutrients and sea-ice chlorophyll a (chl a) to assess their regional and seasonal variability, as well as the relationship of sea-ice algae and nutrient dynamics in the Arctic Ocean. This dataset indicates that bottom sea-ice nutrient and chl a concentrations were highest in the central Canadian Arctic Archipelago (Resolute Passage) due to tidal-driven mixing at the ocean-ice interface, and lowest in the Arctic Ocean basins. At the regional scale, Pacific and Atlantic Water influence variability in sea-ice and sub-ice nutrient concentrations. Significant positive relationships of bottom sea-ice nutrient versus chl a concentrations were ubiquitous across the Arctic during the ice algal bloom, suggesting intracellular nutrient storage as an important mechanism to support ice algal growth. This relationship in turn alters nutrient ratios within the sea ice relative to sub-ice waters, decreasing NOx:PO4 ratios, while increasing NOx:Si(OH)4 ratios. In contrast, bottom sea-ice nutrient-chl a relationships were less common and sometimes negative when nutrient concentrations were low, likely reflecting nutrient limitation. In conclusion, we have demonstrated a pan-Arctic, yet regionally specific, influence of the ice algal community on bottom sea-ice nutrient concentrations.

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Publication Details

Journal
Elementa Science of the Anthropocene
Published
2025-01-01
DOI
https://doi.org/10.1525/elementa.2025.00059
Citations
1
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
1.30
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article

A pan-Arctic perspective on the influence of ice algae on sea-ice nutrient concentrations

Andrea Niemi, Agneta Fransson, Laura M. Whitmore, Melissa Chierici et al.
1 citations
Elementa Science of the Anthropocene
Arctic and Antarctic ice dynamics
1.30
article

A pan-Arctic perspective on the influence of ice algae on sea-ice nutrient concentrations

Andrea Niemi, Agneta Fransson, Laura M. Whitmore, Melissa Chierici, Fowzia Ahmed, Lasse M. Olsen, Rosalie D. McKay, Benjamin Lange, Michel Gosselin, Eva Leu, Sinhué Torres‐Valdés, Andrew R. Juhl, Eva Alou‐Font, Marc Oggier, C. J. Mundy, Jean‐Éric Tremblay, Karley Campbell, Kyle B. Dilliplaine, Elizabeth M. Jones, Rolf Gradinger, Philipp Assmy, Sang Heon Lee
article en
1 citations

Abstract

Sea-ice algae account for a substantial part of annual primary production in ice-covered waters and are an important component of the Arctic marine food web. With climate-induced changes to snow and sea-ice cover and their impact on the surface ocean, such as earlier melt, thinner ice, and increased upper-ocean stratification, a shift toward earlier and more extensive nutrient limitation on ice algal growth can be expected. Therefore, increasing our understanding of the processes governing nutrient supply and uptake by sea-ice algae is essential. Here, we compiled a pan-Arctic dataset of concentrations of sea-ice and sub-ice nutrients and sea-ice chlorophyll a (chl a) to assess their regional and seasonal variability, as well as the relationship of sea-ice algae and nutrient dynamics in the Arctic Ocean. This dataset indicates that bottom sea-ice nutrient and chl a concentrations were highest in the central Canadian Arctic Archipelago (Resolute Passage) due to tidal-driven mixing at the ocean-ice interface, and lowest in the Arctic Ocean basins. At the regional scale, Pacific and Atlantic Water influence variability in sea-ice and sub-ice nutrient concentrations. Significant positive relationships of bottom sea-ice nutrient versus chl a concentrations were ubiquitous across the Arctic during the ice algal bloom, suggesting intracellular nutrient storage as an important mechanism to support ice algal growth. This relationship in turn alters nutrient ratios within the sea ice relative to sub-ice waters, decreasing NOx:PO4 ratios, while increasing NOx:Si(OH)4 ratios. In contrast, bottom sea-ice nutrient-chl a relationships were less common and sometimes negative when nutrient concentrations were low, likely reflecting nutrient limitation. In conclusion, we have demonstrated a pan-Arctic, yet regionally specific, influence of the ice algal community on bottom sea-ice nutrient concentrations.

Elementa Science of the AnthropoceneVol. 13(1)
Norwegian Geotechnical Institute (NO), Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), Fisheries and Oceans Canada (CA), Korea Institute of Ocean Science and Technology (KR), University of Alaska Fairbanks (US), Lamont-Doherty Earth Observatory (US), Université du Québec à Rimouski (CA), Norwegian Environment Agency (NO), Norwegian Institute of Marine Research (NO), Centre for Arctic Gas Hydrate, Environment and Climate (NO), Akvaplan-niva (NO), Université Laval (CA), University of Bergen (NO), University of Manitoba (CA), Pusan National University (KR), King Abdullah University of Science and Technology (SA), UiT The Arctic University of Norway (NO), Norwegian Polar Institute (NO)
Openalex Percentile: Top 16%
Arctic and Antarctic ice dynamics
1.30
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