Articles | Volume 12, issue 11
https://doi.org/10.5194/bg-12-3525-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-12-3525-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Photosynthetic production in the central Arctic Ocean during the record sea-ice minimum in 2012
M. Fernández-Méndez
Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany
Max Planck Institute for Marine Microbiology, Bremen, Germany
C. Katlein
Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany
Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany
M. Nicolaus
Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany
I. Peeken
Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany
MARUM, Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
K. Bakker
Royal Netherlands Institute for Sea Research, Texel, the Netherlands
H. Flores
Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany
University of Hamburg, Zoological Institute and Zoological Museum, Biocenter Grindel, Hamburg, Germany
A. Boetius
Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany
Max Planck Institute for Marine Microbiology, Bremen, Germany
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114 citations as recorded by crossref.
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- Fluvial influence on the biochemical composition of particulate organic matter in the Laptev and Western East Siberian seas during 2015 S. Ahn et al. 10.1016/j.marenvres.2020.104873
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- Phytoplankton of the High-Latitude Arctic: Intensive Growth Large Diatoms Porosira glacialis in the Nansen Basin L. Pautova et al. 10.3390/jmse11020453
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Short summary
Photosynthetic production in the central Arctic Ocean is controlled by light availability below the ice, nitrate and silicate concentrations in the upper ocean, and the role of sub-ice algae that contributed up to 60% to primary production in summer 2012 during the record sea-ice minimum. As sea ice decreases, an overall change in Arctic PP would be foremost related to a change in the role of the ice algal production and nutrient availability.
Photosynthetic production in the central Arctic Ocean is controlled by light availability below...
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