{"refrec":{"BRefID":250554,"RR":"<b>Zark, M.; Riebesell, U.; Dittmar, T.</b> (2015). Effects of ocean acidification on marine dissolved organic matter are not detectable over the succession of phytoplankton blooms. <i>Science Advances 1(9)</i>: e1500531. <a href=\"http://dx.doi.org/10.1126/sciadv.1500531\" target=\"_blank\">http://dx.doi.org/10.1126/sciadv.1500531</a>","BEntID":242249,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Science Advances 1(9)</i>: e1500531. <a href=\"http://dx.doi.org/10.1126/sciadv.1500531\" target=\"_blank\">http://dx.doi.org/10.1126/sciadv.1500531</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Zark, M.; Riebesell, U.; Dittmar, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Zark, M. <i>et al.</i>","Englishabstract":"Marine dissolved organic matter (DOM) is one of the largest active organic carbon reservoirs on Earth, and changes in its pool size or composition could have a major impact on the global carbon cycle. Ocean acidification is a potential driver for these changes because it influences marine primary production and heterotrophic respiration. We simulated ocean acidification as expected for a “business-as-usual” emission scenario in the year 2100 in an unprecedented long-term mesocosm study. The large-scale experiments (50 m<sup>3</sup> each) covered a full seasonal cycle of marine production in a Swedish Fjord. Five mesocosms were artificially enriched in CO<sub>2</sub> to the partial pressure expected in the year 2100 (900 µatm), and five more served as controls (400 µatm). We applied ultrahigh-resolution mass spectrometry to monitor the succession of 7360 distinct DOM formulae over the course of the experiment. Plankton blooms had a clear effect on DOM concentration and molecular composition. This succession was reproducible across all 10 mesocosms, independent of CO<sub>2</sub> treatment. In contrast to the temporal trend, there were no significant differences in DOM concentration and composition between present-day and year 2100 CO<sub>2</sub> levels at any time point of the experiment. On the basis of our results, ocean acidification alone is unlikely to affect the seasonal accumulation of DOM in productive coastal environments.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Effects of ocean acidification on marine dissolved organic matter are not detectable over the succession of phytoplankton blooms","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2015,"MonPub":null,"DateUpdate":"2015-10-16","DateCreate":"2015-10-16","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000216598200008","VABBcode":null,"OpenAcc":1,"DOI":"10.1126/sciadv.1500531"},"refs":null,"anarec":{"AnaID":250554,"PubliDate":2015,"Pagination":"e1500531","XtraPublOfAnaID":null,"ISBN":null,"Volume":"1","Issue":"9","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":248966,"SerRR":"Science Advances. 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