{"refrec":{"BRefID":72775,"RR":"<b>Rochelle-Newall, E.; Delille, B.; Frankignoulle, M.; Gattuso, J.P.; Jacquet, S.; Riebesell, U.; Terbruggen, A.; Zondervan, I.</b> (2004). Chromophoric dissolved organic matter in experimental mesocosms maintained under different pCO<sub>2</sub> levels. <i>Mar. Ecol. Prog. Ser. 272</i>: 25-31. <a href=\"http://dx.doi.org/10.3354/meps272025\" target=\"_blank\">dx.doi.org/10.3354/meps272025</a>","BEntID":68698,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Mar. Ecol. Prog. Ser. 272</i>: 25-31. <a href=\"https://dx.doi.org/10.3354/meps272025\" target=\"_blank\">https://dx.doi.org/10.3354/meps272025</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Rochelle-Newall, E.; Delille, B.; Frankignoulle, M.; Gattuso, J.P.; Jacquet, S.; Riebesell, U.; Terbruggen, A.; Zondervan, I.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Rochelle-Newall, E. <i>et al.</i>","Englishabstract":"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<sub>2</sub> on blooms of the coccolithophorid alga <i>Emiliania huxleyi</i>, we found that despite the 3 different pCO<sub>2</sub> 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. 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