Resistance of Arctic phytoplankton to ocean acidification and enhanced irradiance

The Arctic Ocean is a region particularly prone to ongoing ocean acidification (OA) and climate-driven changes. The influence of these changes on Arctic phytoplankton assemblages, however, remains poorly understood. In order to understand how OA and enhanced irradiances (e.g., resulting from sea–ice...

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Bibliographic Details
Published in:Polar Biology
Main Authors: Hoppe, C. J. M., Schuback, N., Semeniuk, D., Giesbrecht, K., Mol, J., Thomas, H., Maldonado, M. T., Rost, B., Varela, D. E., Tortell, P. D.
Format: Text
Language:English
Published: Springer Berlin Heidelberg 2017
Subjects:
Original Paper
Arctic
Arctic Ocean
Baffin Bay
Baffin
Ocean acidification
Phytoplankton
Sea ice
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6952045/
https://doi.org/10.1007/s00300-017-2186-0
Description
Summary:The Arctic Ocean is a region particularly prone to ongoing ocean acidification (OA) and climate-driven changes. The influence of these changes on Arctic phytoplankton assemblages, however, remains poorly understood. In order to understand how OA and enhanced irradiances (e.g., resulting from sea–ice retreat) will alter the species composition, primary production, and eco-physiology of Arctic phytoplankton, we conducted an incubation experiment with an assemblage from Baffin Bay (71°N, 68°W) under different carbonate chemistry and irradiance regimes. Seawater was collected from just below the deep Chl a maximum, and the resident phytoplankton were exposed to 380 and 1000 µatm pCO(2) at both 15 and 35% incident irradiance. On-deck incubations, in which temperatures were 6 °C above in situ conditions, were monitored for phytoplankton growth, biomass stoichiometry, net primary production, photo-physiology, and taxonomic composition. During the 8-day experiment, taxonomic diversity decreased and the diatom Chaetoceros socialis became increasingly dominant irrespective of light or CO(2) levels. We found no statistically significant effects from either higher CO(2) or light on physiological properties of phytoplankton during the experiment. We did, however, observe an initial 2-day stress response in all treatments, and slight photo-physiological responses to higher CO(2) and light during the first five days of the incubation. Our results thus indicate high resistance of Arctic phytoplankton to OA and enhanced irradiance levels, challenging the commonly predicted stimulatory effects of enhanced CO(2) and light availability for primary production. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (doi:10.1007/s00300-017-2186-0) contains supplementary material, which is available to authorized users.

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