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Oxygen fluxes beneath Arctic land-fast ice and pack ice: towards estimates of ice productivity.
Attard, Karl M., Søgaard, Dorte H., Piontek, Judith , Lange, Benjamin A., Katlein, Christian, Sørensen, Heidi L., McGinnis, Daniel F., Rovelli, Lorenzo, Rysgaard, Søren, Wenzhöfer, Frank and Glud, Ronnie N.
(2018)
Oxygen fluxes beneath Arctic land-fast ice and pack ice: towards estimates of ice productivity.
Polar Biology, 41
(10).
pp. 2119-2134.
DOI 10.1007/s00300-018-2350-1.
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Abstract
Sea-ice ecosystems are among the most extensive of Earth’s habitats; yet its autotrophic and heterotrophic activities remain poorly constrained. We employed the in situ aquatic eddy-covariance (AEC) O2 flux method and laboratory incubation techniques (H14CO3−, [3H] thymidine and [3H] leucine) to assess productivity in Arctic sea-ice using different methods, in conditions ranging from land-fast ice during winter, to pack ice within the central Arctic Ocean during summer. Laboratory tracer measurements resolved rates of bacterial C demand of 0.003–0.166 mmol C m−2 day−1 and primary productivity rates of 0.008–0.125 mmol C m−2 day−1 for the different ice floes. Pack ice in the central Arctic Ocean was overall net autotrophic (0.002–0.063 mmol C m−2 day−1), whereas winter land-fast ice was net heterotrophic (− 0.155 mmol C m−2 day−1). AEC measurements resolved an uptake of O2 by the bottom-ice environment, from ~ − 2 mmol O2 m−2 day−1 under winter land-fast ice to~ − 6 mmol O2 m−2 day−1 under summer pack ice. Flux of O2-deplete meltwater and changes in water flow velocity masked potential biological-mediated activity. AEC estimates of primary productivity were only possible at one study location. Here, productivity rates of 1.3 ± 0.9 mmol O2 m−2 day−1, much larger than concurrent laboratory tracer estimates (0.03 mmol C m−2 day−1), indicate that ice algal production and its importance within the marine Arctic could be underestimated using traditional approaches. Given careful flux interpretation and with further development, the AEC technique represents a promising new tool for assessing oxygen dynamics and sea-ice productivity in ice-covered regions.
Document Type: | Article |
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Keywords: | Sea-ice; Primary production; Bacterial production; Carbon cycling; Eddy-covariance |
Research affiliation: | HGF-AWI OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-BI Biological Oceanography |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | Springer |
Projects: | PACES |
Expeditions/Models/Experiments: | |
Date Deposited: | 27 Jun 2018 10:31 |
Last Modified: | 08 Feb 2021 07:29 |
URI: | https://oceanrep.geomar.de/id/eprint/43510 |
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