Episodic arctic CO2 limitation in the west svalbard shelf

The European Sector of the Arctic Ocean is characterized by low CO concentrations in seawater during spring and summer, largely due to strong biological uptake driven by extensive plankton blooms in spring. The spring plankton bloom is eventually terminated by nutrient depletion and grazing. However...

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Bibliographic Details
Published in:Frontiers in Marine Science
Main Authors: Sanz-Martín, Marina, Chierici, Melissa, Mesa, Elena, Carrillo-de-Albornoz, Paloma, Delgado Huertas, Antonio, Agustí, Susana, Reigstad, Marit, Kristiansen, Svein, Wassmann, Paul F., Duarte, C.M.
Other Authors: Norwegian Research Council
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media 2018
Subjects:
Arctic Ocean
CO2 additions
CO2 limitation
Gross primary production
Plankton communities
Spring blooms
Phytoplankton
Svalbard
Online Access:http://hdl.handle.net/10261/361553
https://doi.org/10.3389/fmars.2018.00221
Description
Summary:The European Sector of the Arctic Ocean is characterized by low CO concentrations in seawater during spring and summer, largely due to strong biological uptake driven by extensive plankton blooms in spring. The spring plankton bloom is eventually terminated by nutrient depletion and grazing. However, low CO concentrations in seawater and low atmospheric resupply of CO can cause episodes during which the phytoplankton growth is limited by CO2. Here, we show that gross primary production (GPP) of Arctic plankton communities increases from 32 to 72% on average with CO additions in spring. Enhanced GPP with CO additions occur during episodes of high productivity, low CO concentration and in the presence of dissolved inorganic nutrients. However, during summer the addition of CO supresses planktonic Arctic GPP. Events of CO limitation in spring may contribute to the termination of the Arctic spring plankton blooms. The stimulation of GPP by CO during the spring bloom provides a biotic feedback loop that might influence the global role played by the Arctic Ocean as a CO sink in the future. We thank the crew of R/V Helmer Hanssen, I. Hendriks, M. Vernet, E. Falk, H. Hodal, and A. Granados for their help. J. Holding and L. Meire for valuable comments and V. Unkefer for improvements to the text. MS-M was supported by a La Caixa Ph. D. fellowship. This study is a contribution to the Carbon Bridge (RCN-226415) project funded by the Norwegian Research Council.

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