{"refrec":{"BRefID":281401,"RR":"<b>Ceburnis, D.; Masalaite, A.; Ovadnevaite, J.; Garbaras, A.; Remeikis, V.; Maenhaut, W.; Claeys, M.; Sciare, J.; Baisnée, D.; O'Dowd, C.D.</b> (2016). Stable isotopes measurements reveal dual carbon pools contributing to organic matter enrichment in marine aerosol. <i>NPG Scientific Reports 6(36675)</i>: 6 pp. <a href=\"http://dx.doi.org/10.1038/srep36675\" target=\"_blank\">http://dx.doi.org/10.1038/srep36675</a>","BEntID":273420,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>NPG Scientific Reports 6(36675)</i>: 6 pp. <a href=\"http://dx.doi.org/10.1038/srep36675\" target=\"_blank\">http://dx.doi.org/10.1038/srep36675</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Ceburnis, D.; Masalaite, A.; Ovadnevaite, J.; Garbaras, A.; Remeikis, V.; Maenhaut, W.; Claeys, M.; Sciare, J.; Baisnée, D.; O'Dowd, C.D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Ceburnis, D. <i>et al.</i>","Englishabstract":"Stable carbon isotope ratios in marine aerosol collected over the Southern Indian Ocean revealed δ<sup>13</sup>C values ranging from −20.0‰ to −28.2‰. The isotope ratios exhibited a strong correlation with the fractional organic matter (OM) enrichment in sea spray aerosol. The base-level isotope ratio of −20.0‰ is characteristic of an aged Dissolved Organic Matter (DOM) pool contributing a relatively homogeneous background level of DOM to oceanic waters. The range of isotope ratios, extending down to −28.2‰, is characteristic of more variable, stronger, and fresher Particulate Organic Matter (POM) pool driven by trophic level interactions. We present a conceptual dual-pool POM-DOM model which comprises a ‘young’ and variable POM pool which dominates enrichment in sea-spray and an ‘aged’ but invariant DOM pool which is, ultimately, an aged end-product of processed ‘fresh’ POM. This model is harmonious with the preferential enrichment of fresh colloidal and nano-gel lipid-like particulate matter in sea spray particles and the observed depleted δ13C ratio resulting from isotope equilibrium fractionation coupled with enhanced plankton photosynthesis in cold water (−2 °C to +8 °C). These results re-assert the hypothesis that OM enrichment in sea-spray is directly linked to primary production and, consequently, can have implications for climate-aerosol-cloud feedback systems.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Stable isotopes measurements reveal dual carbon pools contributing to organic matter enrichment in marine aerosol","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-25 01:32:36.533239","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2016,"MonPub":null,"DateUpdate":"2017-05-16","DateCreate":"2016-11-09","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000387072100001","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/srep36675"},"refs":null,"anarec":{"AnaID":281401,"PubliDate":2016,"Pagination":"6 pp","XtraPublOfAnaID":null,"ISBN":null,"Volume":"6","Issue":"36675","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":208093,"SerRR":"Scientific Reports (Nature Publishing Group). 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