nerc.ac.uk

Carbon export efficiency and phytoplankton community composition in the Atlantic sector of the Arctic Ocean

Le Moigne, Frederic A.C.; Poulton, Alex J.; Henson, Stephanie A. ORCID: https://orcid.org/0000-0002-3875-6802; Daniels, Chris J.; Fragoso, Glaucia M.; Mitchell, Elaine; Richier, Sophie; Smith, Helen E.K.; Russell, Benjamin C.; Tarling, Geraint A. ORCID: https://orcid.org/0000-0002-3753-5899; Young, Jeremy R.; Zubkov, Mike. 2015 Carbon export efficiency and phytoplankton community composition in the Atlantic sector of the Arctic Ocean. Journal of Geophysical Research: Oceans, 120 (6). 3896-3912. https://doi.org/10.1002/2015JC010700

Before downloading, please read NORA policies.
[img]
Preview
Text
Moigne_et_al-2015-Journal_of_Geophysical_Research__Oceans.pdf - Published Version
Available under License Creative Commons Attribution 4.0.

Download (1MB) | Preview

Abstract/Summary

Arctic primary production is sensitive to reductions in sea ice cover, and will likely increase into the future. Whether this increased primary production (PP) will translate into increased export of particulate organic carbon (POC) is currently unclear. Here we report on the POC export efficiency during summer 2012 in the Atlantic sector of the Arctic Ocean. We coupled 234-Thorium based estimates of the export flux of POC to onboard incubation based estimates of PP. Export efficiency (defined as the fraction of PP that is exported below 100 m depth: ThE-ratio) showed large variability (0.09 ± 0.19 to 1.3 ± 0.3). The highest ThE-ratio (1.3 ± 0.3) was recorded in a mono-specific bloom of Phaeocystis pouchetii located in the ice edge. Blooming diatom dominated areas also had high ThE-ratios (0.1 ± 0.1 to 0.5 ± 0.2), while mixed and/or pre-bloom communities showed lower ThE-ratios (0.10 ± 0.03 to 0.19 ± 0.05). Furthermore, using oxygen saturation, bacterial abundance, bacterial production, and zooplankton oxygen demand, we also investigated spatial variability in the degree to which this sinking material may be remineralised in the upper mesopelagic (< 300 m). Our results suggest that blooming diatoms and P. pouchetii can export a significant fraction of their biomass below the surface layer (100 m) in the open Arctic Ocean. Also, we show evidence that the material sinking from a P. pouchetii bloom may be remineralised (>100m) at a similar rate as the material sinking from diatom blooms in the upper mesopelagic, contrary to previous findings.

Item Type: Publication - Article
Digital Object Identifier (DOI): https://doi.org/10.1002/2015JC010700
Programmes: BAS Programmes > BAS Programmes 2015 > Ecosystems
ISSN: 2169-9291
Additional Keywords: Arctic, carbon export, phytoplankton, remineralisation
NORA Subject Terms: Marine Sciences
Date made live: 29 Apr 2015 09:50 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/510715

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...