http://www.plosone.org/article/info%3Adoi%2F10.1371%2Fjournal.pone.0079890
Iron Limitation Modulates Ocean Acidification Effects on Southern Ocean 
Phytoplankton Communities


   - Clara J. M. Hoppe, 
   - Christel S. Hassler,
   
    
   - Christopher D. Payne,
   
    
   - Philippe D. Tortell,
   
    
   - Björn Rost,
   
    
   - Scarlett Trimborn


   - Published: Nov 20, 2013
   - DOI: 10.1371/journal.pone.0079890


Abstract

The potential interactive effects of iron (Fe) limitation and Ocean 
Acidification in the Southern Ocean (SO) are largely unknown. Here we 
present results of a long-term incubation experiment investigating the 
combined effects of CO2 and Fe availability on natural phytoplankton 
assemblages from the Weddell Sea, Antarctica. Active Chl *a* fluorescence 
measurements revealed that we successfully cultured phytoplankton under 
both Fe-depleted and Fe-enriched conditions. Fe treatments had significant 
effects on photosynthetic efficiency (Fv/Fm; 0.3 for Fe-depleted and 0.5 
for Fe-enriched conditions), non-photochemical quenching (NPQ), and 
relative electron transport rates (rETR). pCO2 treatments significantly 
affected NPQ and rETR, but had no effect on Fv/Fm. Under Fe limitation, 
increased pCO2 had no influence on C fixation whereas under Fe enrichment, 
primary production increased with increasing pCO2 levels. These CO2-dependent 
changes in productivity under Fe-enriched conditions were accompanied by a 
pronounced taxonomic shift from weakly to heavily silicified diatoms (i.e. 
from *Pseudo-nitzschia* sp. to *Fragilariopsis* sp.). Under Fe-depleted 
conditions, this functional shift was absent and thinly silicified species 
dominated all pCO2 treatments (*Pseudo-nitzschia* sp. and*Synedropsis* sp. 
for low and high pCO2, respectively). Our results suggest that Ocean 
Acidification could increase primary productivity and the abundance of 
heavily silicified, fast sinking diatoms in Fe-enriched areas, both 
potentially leading to a stimulation of the biological pump. Over much of 
the SO, however, Fe limitation could restrict this possible CO2 fertilization 
effect."


regards

Bhaskar

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