Quantification of the carbonaceous matter origin in submicron marine aerosol by 13C and 14C isotope analysis

Ceburnis, D.; Garbaras, A.; Szidat, S.; Rinaldi, M.; Fahrni, Simon; Perron, N.; Wacker, L.; Leinert, S.; Remeikis, V.; Facchini, M. C.; Prevot, A. S. H.; Jennings, S. G.; Ramonet, M.; O'Dowd, C. D. (2011). Quantification of the carbonaceous matter origin in submicron marine aerosol by 13C and 14C isotope analysis. Atmospheric chemistry and physics, 11(16), pp. 8593-8606. Katlenburg-Lindau (D): European Geosciences Union 10.5194/acp-11-8593-2011

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Dual carbon isotope anal. of marine aerosol samples has been performed for the first time demonstrating a potential in org. matter apportionment between three principal sources: marine, terrestrial (non-fossil) and fossil fuel due to unique isotopic signatures. The results presented here, utilizing combinations of dual carbon isotope anal., provides conclusive evidence of a dominant biogenic org. fraction to org. aerosol over biol. active oceans. In particular, the NE Atlantic, which is also subjected to notable anthropogenic influences via pollution transport processes, was found to contain 80 % org. aerosol matter of biogenic origin directly linked to plankton emissions. The remaining carbonaceous aerosol was of terrestrial origin. By contrast, for polluted air advected out from Europe into the NE Atlantic, the source apportionment is 30 % marine biogenic, 40 % fossil fuel, and 30 % continental non-fossil fuel. The dominant marine org. aerosol source in the atm. has significant implications for climate change feedback processes. [on SciFinder(R)]

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