Reference : Chromophoric dissolved organic matter in experimental mesocosms maintained under diff...
Scientific journals : Article
Physical, chemical, mathematical & earth Sciences : Earth sciences & physical geography
Life sciences : Aquatic sciences & oceanology
Life sciences : Environmental sciences & ecology
Chromophoric dissolved organic matter in experimental mesocosms maintained under different pCO(2) levels
Rochelle-Newall, Emma [CNRS-Université de Paris 6 > Laboratoire d’Océanographie]
Delille, Bruno mailto [Université de Liège - ULiège > Département d'astrophys., géophysique et océanographie (AGO) > Océanographie chimique >]
Frankignoulle, Michel mailto [Université de Liège - ULiège > > > > Océanographie Chimique > >]
Gattuso, Jean-Pierre [CNRS-Université de Paris 6 > Laboratoire d’Océanographie]
Jacquet, Stéphan [UMR CARRTEL > Station INRA d’Hydrobiologie Lacustre]
Riebesell, Ulf [Alfred Wegener Institute for Polar and Marine Research]
Terbruggen, Anja [Alfred Wegener Institute for Polar and Marine Research]
Zondervan, Ingrid [Alfred Wegener Institute for Polar and Marine Research]
Marine Ecology. Progress Series
Oldendorf Luhe
[en] CDOM ; DOC ; mesocosms ; viruses ; cyanobacteria ; heterotrophic ; bacteria ; CO2
[en] Chromophoric dissolved organic matter (CDOM) represents the optically active fraction of the bulk dissolved organic matter (DOM) pool. Recent evidence pointed towards a microbial source of CDOM in the aquatic environment and led to the proposal that phytoplankton is not a direct source of CDOM, but that heterotrophic bacteria, through reprocessing of DOM of algal origin, are an important source of CDOM. In a recent experiment designed at looking at the effects of elevated pCO(2) on blooms of the coccolithophorid alga Emiliania huxleyi, we found that despite the 3 different pCO(2) levels tested (190, 414 and 714 ppm), no differences were observed in accumulation of CDOM over the 20 d of incubation. Unlike previous mesocosm experiments where. relationships between CDOM accumulation and bacterial abundance have been observed, none was observed here. These results provide some new insights into the apparent lack of effect of pCO(2) on CDOM accumulation in surface waters, and question the previously proposed mechanisms and rates of CDOM production in natural phytoplankton blooms.
Commission européenne : Direction générale de la Recherche ; CNRS ; Fonds de la Recherche Scientifique (Communauté française de Belgique) - F.R.S.-FNRS

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