High atmosphere–ocean exchange of semivolatile aromatic hydrocarbons
Duarte, Carlos M.
KAUST DepartmentRed Sea Research Center (RSRC)
Permanent link to this recordhttp://hdl.handle.net/10754/621772
MetadataShow full item record
AbstractPolycyclic aromatic hydrocarbons, and other semivolatile aromatic-like compounds, are an important and ubiquitous fraction of organic matter in the environment. The occurrence of semivolatile aromatic hydrocarbons is due to anthropogenic sources such as incomplete combustion of fossil fuels or oil spills, and other biogenic sources. However, their global transport, fate and relevance for the carbon cycle have been poorly assessed, especially in terms of fluxes. Here we report a global assessment of the occurrence and atmosphere-ocean fluxes of 64 polycyclic aromatic hydrocarbons analysed in paired atmospheric and seawater samples from the tropical and subtropical Atlantic, Pacific and Indian oceans. The global atmospheric input of polycyclic aromatic hydrocarbons to the global ocean is estimated at 0.09 Tg per month, four times greater than the input from the Deepwater Horizon spill. Moreover, the environmental concentrations of total semivolatile aromatic-like compounds were 10 2 -10 3 times higher than those of the targeted polycyclic aromatic hydrocarbons, with a relevant contribution of an aromatic unresolved complex mixture. These concentrations drive a large global deposition of carbon, estimated at 400 Tg C yr -1, around 15% of the oceanic CO2 uptake. © 2016 Macmillan Publishers Limited.
CitationGonzález-Gaya B, Fernández-Pinos M-C, Morales L, Méjanelle L, Abad E, et al. (2016) High atmosphere–ocean exchange of semivolatile aromatic hydrocarbons. Nature Geoscience 9: 438–442. Available: http://dx.doi.org/10.1038/ngeo2714.
SponsorsThis work was funded by the Spanish Ministry of Economy and Competitiveness (Circumnavigation Expedition Malaspina 2010: Global Change and Biodiversity Exploration of the Global Ocean. CSD2008-00077). B.G.-G. and M.-C. F.-P. acknowledge a predoctoral fellowship from BBVA Foundation and the Spanish National Research Council (CSIC), respectively. CSIC and the Spanish Government are also acknowledged for additional financial support. Thanks to RV Hesperides staff and UTM technicians during the cruise. D. Garcia, G. Caballero and M. J. Ojeda are acknowledged for collaborating in the laboratory work.