de Jong, Jeroen; Schoemann, Véronique; Lannuzel, Delphine; Croot, Peter L; de Baar, Hein J W; Tison, Jean-Louis (2012): Iron concentration and fluxes in the water column during POLARSTERN cruises in the Southern Ocean [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.808656, Supplement to: de Jong, J et al. (2012): Natural iron fertilization of the Atlantic sector of the Southern Ocean by continental shelf sources of the Antarctic Peninsula. Journal of Geophysical Research: Biogeosciences, 117, G01029, https://doi.org/10.1029/2011JG001679
Always quote citation above when using data! You can download the citation in several formats below.
Published: 2012 (exact date unknown) • DOI registered: 2013-05-04
Abstract:
In large parts of the Southern Ocean, primary production is limited due to shortage of iron (Fe). We measured vertical Fe profiles in the western Weddell Sea, Weddell-Scotia Confluence, and Antarctic Circumpolar Current (ACC), showing that Fe is derived from benthic Fe diffusion and sediment resuspension in areas characterized by high turbulence due to rugged bottom topography. Our data together with literature data reveal an exponential decrease of dissolved Fe (DFe) concentrations with increasing distance from the continental shelves of the Antarctic Peninsula and the western Weddell Sea. This decrease can be observed 3500 km eastward of the Antarctic Peninsula area, downstream the ACC. We estimated DFe summer fluxes into the upper mixed layer of the Atlantic sector of the Southern Ocean and found that horizontal advection dominates DFe supply, representing 54 ± 15% of the total flux, with significant vertical advection second most important at 29 ± 13%. Horizontal and vertical diffusion are weak with 1 ± 2% and 1 ± 1%, respectively. The atmospheric contribution is insignificant close to the Antarctic continent but increases to 15 ± 10% in the remotest waters (>1500 km offshore) of the ACC. Translating Southern Ocean carbon fixation by primary producers into biogenic Fe fixation shows a twofold excess of new DFe input close to the Antarctic continent and a one-third shortage in the open ocean. Fe recycling, with an estimated 'fe' ratio of 0.59, is the likely pathway to balance new DFe supply and Fe fixation.
Project(s):
Coverage:
Median Latitude: -58.638571 * Median Longitude: -27.456868 * South-bound Latitude: -67.370700 * West-bound Longitude: -55.413100 * North-bound Latitude: -44.015500 * East-bound Longitude: 20.011300
Date/Time Start: 1988-11-30T09:03:00 * Date/Time End: 2005-01-07T11:40:00
Comment:
Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
4 datasets
Download Data
Datasets listed in this publication series
- de Jong, J; Schoemann, V; Lannuzel, D et al. (2012): (Table 1) Iron concentations in the water column during POLARSTERN cruise ANT-XXII/2. https://doi.org/10.1594/PANGAEA.808650
- de Jong, J; Schoemann, V; Lannuzel, D et al. (2012): (Table 3) Diffusive dissolved iron fluxes during POLARSTERN cruises ANT-XXII/2 and ANT-X/6. https://doi.org/10.1594/PANGAEA.808652
- de Jong, J; Schoemann, V; Lannuzel, D et al. (2012): (Table 4) Daily horizontal and vertical fluxes of dissolved iron during POLARSTERN cruises in the Atlantic Sector of the Southern Ocean. https://doi.org/10.1594/PANGAEA.808655
- de Jong, J; Schoemann, V; Lannuzel, D et al. (2012): (Table 2) Upper mixed layer depth and average Fe concentration during POLARSTERN cruises in the Atlantic Sector of the Southern Ocean. https://doi.org/10.1594/PANGAEA.808654