<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>6</volume><submitter>Ceburnis D</submitter><pubmed_abstract>Stable carbon isotope ratios in marine aerosol collected over the Southern Indian Ocean revealed δ&lt;sup>13&lt;/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' bu</pubmed_abstract><journal>Scientific reports</journal><pagination>36675</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC5098177</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Stable isotopes measurements reveal dual carbon pools contributing to organic matter enrichment in marine aerosol.</pubmed_title><pmcid>PMC5098177</pmcid><pubmed_authors>Remeikis V</pubmed_authors><pubmed_authors>Garbaras A</pubmed_authors><pubmed_authors>Ovadnevaite J</pubmed_authors><pubmed_authors>Ceburnis D</pubmed_authors><pubmed_authors>Maenhaut W</pubmed_authors><pubmed_authors>Masalaite A</pubmed_authors><pubmed_authors>Sciare J</pubmed_authors><pubmed_authors>Baisnee D</pubmed_authors><pubmed_authors>Claeys M</pubmed_authors><pubmed_authors>O'Dowd CD</pubmed_authors></additional><is_claimable>false</is_claimable><name>Stable isotopes measurements reveal dual carbon pools contributing to organic matter enrichment in marine aerosol.</name><description>Stable carbon isotope ratios in marine aerosol collected over the Southern Indian Ocean revealed δ&lt;sup>13&lt;/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' bu</description><dates><release>2016-01-01T00:00:00Z</release><publication>2016 Nov</publication><modification>2025-04-18T20:50:25.072Z</modification><creation>2019-03-27T02:28:24Z</creation></dates><accession>S-EPMC5098177</accession><cross_references><pubmed>27819297</pubmed><doi>10.1038/srep36675</doi></cross_references></HashMap>