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	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>9</volume_number>
		<issue_number>24</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acp-9-9587-2009</doi>
	<article_url>http://www.atmos-chem-phys.net/9/9587/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/9/9587/2009/acp-9-9587-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/9/9587/2009/acp-9-9587-2009.pdf</fulltext_pdf>
	<start_page>9587</start_page>
	<end_page>9597</end_page>
	<publication_date>2009-12-21</publication_date>
	<article_title content_type="html">Seasonal variation of aliphatic amines in marine sub-micrometer particles at the Cape Verde islands</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Müller</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>Y. Iinuma</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>J. Karstensen</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>D. van Pinxteren</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>S. Lehmann</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>T. Gnauk</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>H. Herrmann</name>
			<email>herrmann@tropos.de</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Leibniz-Institut für Troposphärenforschung (IfT), 04318 Leipzig, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Leibniz-Institut für Meereswissenschaften (IFM-GEOMAR), 24105 Kiel, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Monomethylamine (MA), dimethylamine (DMA) and diethylamine (DEA) were
detected at non-negligible concentrations in sub-micrometer particles at
the Cap Verde Atmospheric Observatory (CVAO) located on the island of
São Vicente in Cape Verde during algal blooms in 2007. The
concentrations of these amines in five stage impactor samples ranged from 0–30 pg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; for MA, 130–360 pg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;
for DMA and 5–110 pg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; for DEA during the spring bloom in May 2007 and 2–520 pg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; for MA, 100–1400 pg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; for
DMA and 90–760 pg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; for DEA during an unexpected winter algal bloom in
December 2007. Anomalously high Saharan dust deposition and intensive ocean
layer deepening were found at the Atmospheric Observatory and the associated
Ocean Observatory during algal bloom periods. The highest amine
concentrations in fine particles (impactor stage 2, 0.14–0.42 μm)
indicate that amines are likely taken up from the gas phase into the acidic
sub-micrometer particles. The contribution of amines to the organic
carbon (OC) content ranged from 0.2–2.5% C in the winter months,
indicating the importance of this class of compounds to the carbon cycle in
the marine environment. Furthermore, aliphatic amines originating from
marine biological sources likely contribute significantly to the nitrogen
content in the marine atmosphere. The average contribution of the amines to
the detected nitrogen species in sub-micrometer particles can be
non-negligible, especially in the winter months (0.1% N–1.5% N in the
sum of nitrate, ammonium and amines). This indicates that these smaller
aliphatic amines can be important for the carbon and the nitrogen cycles in
the remote marine environment.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Arimoto, R., Duce, R. A., Savoie, D. L., and Prospero, J. M.: Trace-Elements in Aerosol-Particles from Bermuda and Barbados-Concentrations, Sources and Relationships to Aerosol Sulfate, J. Atmos. Chem., 14, 439–457, 1992. </reference>
		<reference numeration="2" content_type="text"> Arnold, S. R., Spracklen, D. V., Williams, J., Yassaa, N., Sciare, J., Bonsang, B., Gros, V., Peeken, I., Lewis, A. C., Alvain, S., and Moulin, C.: Evaluation of the global oceanic isoprene source and its impacts on marine organic carbon aerosol, Atmos. Chem. Phys., 9, 1253–1262, 2009. </reference>
		<reference numeration="3" content_type="text"> Barsanti, K. C., McMurry, P. H., and Smith, J. N.: The potential contribution of organic salts to new particle growth, Atmos. Chem. Phys., 9, 2949–2957, 2009. </reference>
		<reference numeration="4" content_type="text"> Behrenfeld, M. J. and Falkowski, P. G.: Photosynthetic rates derived from satellite-based chlorophyll concentration, Limnol. Oceanogr., 42, 1–20, 1997. </reference>
		<reference numeration="5" content_type="text"> Blanchard, D. C.: Bursting of Bubbles at an Air Water Interface, Nature, 173, 1048–1048, 1954. </reference>
		<reference numeration="6" content_type="text"> Bond, T. C., Streets, D. G., Yarber, K. F., Nelson, S. M., Woo, J. H., and Klimont, Z.: A technology-based global inventory of black and organic carbon emissions from combustion, J. Geophys. Res.-Atmos., 109, D14203, doi:10.1029/2003JD003697, 2004. </reference>
		<reference numeration="7" content_type="text"> Bricaud, A., Morel, A., and Andreè, J. M.: Spatial/temporal variability of algal biomass and potential productivity in the Mauritanian upwelling zone, as estimated from CZCS data, Adv. Space. Res., 7, 53–62, 1987. </reference>
		<reference numeration="8" content_type="text"> Cavalli, F., Facchini, M. C., Decesari, S., Mircea, M., Emblico, L., Fuzzi, S., Ceburnis, D., Yoon, Y. J., O&apos;Dowd, C. D., Putaud, J. P., and Dell&apos;Acqua, A.: Advances in characterization of size-resolved organic matter in marine aerosol over the North Atlantic, J. Geophys. Res.-Atmos., 109, D24215, doi:10.1029/2004JD005137, 2004. </reference>
		<reference numeration="9" content_type="text"> Coale, K. H., Johnson, K. S., Fitzwater, S. E., Gordon, R. M., Tanner, S., Chavez, F. P., Ferioli, L. Sakamoto, C., Rogers, P.. Millero, F., Steinberg, P., Nightingale, P., Cooper, D., Cochlan, W. P., Landry, M. R., Constantinou, J., Rollwagen, G., Trasvina, A., and Kudela, R.: A massive phytoplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific Ocean, Nature, 383, 495–501, 1996. </reference>
		<reference numeration="10" content_type="text"> Cooke, W. F., Liousse, C., Cachier, H., and Feichter, J.: Construction of a 1~degrees&amp;times;1~degrees fossil fuel emission data set for carbonaceous aerosol and implementation and radiative impact in the ECHAM4 model, J. Geophys. Res.-Atmos., 104, 22137–22162, 1999. </reference>
		<reference numeration="11" content_type="text"> Cornell, S., Mace, K., Coeppicus, S., Duce, R., Huebert, B., Jickells, T., and Zhuang, L. Z.: Organic nitrogen in Hawaiian rain and aerosol, J. Geophys. Res.-Atmos., 106, 7973–7983, 2001. </reference>
		<reference numeration="12" content_type="text"> Draxler, R. R. and Rolph, G. D.: HYSPLIT (HYbrid Single-Particle Lagrangian Integrated Trajectory) Model access via NOAA ARL READY Website (http://www.arl.noaa.gov/ready/hysplit4.html), NOAA Air Resources Laboratory, Silver Spring, MD, USA, 2003. </reference>
		<reference numeration="13" content_type="text"> Facchini, M. C., Decesari, S., Rinaldit, M., Carbone, C., Finessi, E., Mircea, M., Fuzzi, S., Moretti, F., Tagliavini, E., Ceburnis, D., and O&apos;Dowd, C. D.: Important source of marine secondary organic aerosol from biogenic amines, Environ. Sci. Technol., 42, 9116–9121, 2008a. </reference>
		<reference numeration="14" content_type="text"> Facchini, M. C., Rinaldi, M., Decesari, S., Carbone, C., Finessi, E., Mircea, M., Fuzzi, S., Ceburnis, D., Flanagan, R., Nilsson, E. D., de Leeuw, G., Martino, M., Woeltjen, J., and O&apos;Dowd, C. D.: Primary submicron marine aerosol dominated by insoluble organic colloids and aggregates, Geophys. Res. Lett., 35, L17814, doi:10.1029/2008GL034210, 2008b. </reference>
		<reference numeration="15" content_type="text"> Fitzgerald, J. W.: Marine aerosols – a review, Atmos. Environ. A-Gen., 25, 533–545, 1991. </reference>
		<reference numeration="16" content_type="text"> Gantt, B., Meskhidze, N., and Kamykowski, D.: A new physically-based quantification of marine isoprene and primary organic aerosol emissions, Atmos. Chem. Phys., 9, 4915–4927, 2009. </reference>
		<reference numeration="17" content_type="text"> Gibb, S. W., Mantoura, R. F. C., and Liss, P. S.: Ocean-atmosphere exchange and atmospheric speciation of ammonia and methylamines in the region of the NW Arabian Sea, Global. Biogeochem. Cy., 13, 161–177, 1999. </reference>
		<reference numeration="18" content_type="text"> Healy, R. M., Wenger, J. C., Metzger, A., Duplissy, J., Kalberer, M., and Dommen, J.: Gas/particle partitioning of carbonyls in the photooxidation of isoprene and 1,3,5-trimethylbenzene, Atmos. Chem. Phys., 8, 3215–3230, 2008. </reference>
		<reference numeration="19" content_type="text"> Hoffman, E. J. and Duce, R. A.: Factors Influencing Organic-Carbon Content of Marine Aerosols – Laboratory Study, J. Geophys. Res.-Oc. Atm., 81, 3667–3670, 1976. </reference>
		<reference numeration="20" content_type="text"> Hoffman, E. J. and Duce, R. A.: Organic Carbon Content of Marine Aerosols Collected on Bermuda, J. Geophys. Res., 79, 4474–4477, 1974. </reference>
		<reference numeration="21" content_type="text"> Iinuma, Y., Brüggemann, E., Gnauk, T., Müller, K., Andreae, M. O., Helas, G., Parmar, R., and Herrmann, H.: Source characterization of biomass burning particles: The combustion of selected European conifers, African hardwood, savanna grass, and German and Indonesian peat, J. Geophys. Res., 112, D08209, doi: 10.1029/2006JD007120, 2007. </reference>
		<reference numeration="22" content_type="text"> IPCC (Intergovernmental Panel on Climate Change: Climate Change 2007): Synthesis Report, Contribution of Working Groups I, II and III to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Core Writing Team: Pachauri, R. K. and Reisinger, A., Geneva, Switzerland, 2007. </reference>
		<reference numeration="23" content_type="text"> Jo, C. O., Lee, J. Y., Park, K. A., Kim, Y. H., and Kim, K. R.: Asian dust initiated early spring bloom in the northern East/Japan Sea, Geophys. Res. Lett., 34, L05602, doi:10.1029/2006GL027395, 2007. </reference>
		<reference numeration="24" content_type="text"> Kawamura, K. and Gagosian, R. B.: Implications of Omega-Oxocarboxylic Acids in the Remote Marine Atmosphere for Photooxidation of Unsaturated Fatty-Acids, Nature, 325, 330–332, 1987. </reference>
		<reference numeration="25" content_type="text"> Kawamura, K. and Gagosian, R. B.: Midchain Ketocarboxylic Acids in the Remote Marine Atmosphere – Distribution Patterns and Possible Formation Mechanisms, J. Atmos. Chem., 11, 107–122, 1990. </reference>
		<reference numeration="26" content_type="text"> Kawamura, K. and Sakaguchi, F.: Molecular distributions of water soluble dicarboxylic acids in marine aerosols over the Pacific Ocean including tropics, J. Geophys. Res.-Atmos., 104, 3501–3509, 1999. </reference>
		<reference numeration="27" content_type="text"> Knelman, F., Dombrowski, N., and Newitt, D. M.: Mechanism of the Bursting of Bubbles, Nature, 173, 261–261, 1954. </reference>
		<reference numeration="28" content_type="text"> Kulmala, M.: How particles nucleate and grow, Science, 302, 1000–1001, 2003. </reference>
		<reference numeration="29" content_type="text"> Kulmala, M. and Kerminen, V. M.: On the formation and growth of atmospheric nanoparticles, Atmos. Res., 90, 132–150, 2008. </reference>
		<reference numeration="30" content_type="text"> Kurtén, T., Loukonen, V., Vehkamäki, H., and Kulmala, M.: Amines are likely to enhance neutral and ion-induced sulfuric acid-water nucleation in the atmosphere more effectively than ammonia, Atmos. Chem. Phys., 8, 4095–4103, 2008. </reference>
		<reference numeration="31" content_type="text"> Kuznetsova, M., Lee, C., and Aller, J.: Characterization of the proteinaceous matter in marine aerosols, Mar. Chem., 96, 359–377, 2005. </reference>
		<reference numeration="32" content_type="text"> M&amp;aring;rtensson, E. M., Nilsson, E. D., de Leeuw, G., Cohen, L. H., and Hansson, H. C.: Laboratory simulations and parameterization of the primary marine aerosol production, J. Geophys. Res., 108(D9), 4297, doi:10.1029/2002JD002263, 2003. </reference>
		<reference numeration="33" content_type="text"> Martin, J. H., Coale, K. H., Johnson, K. S., Fitzwater, S. E., Gordon, R. M., Tanner, S. J., Hunter, C. N., Elrod, V. A., Nowicki, J. L., Coley, T. L., Barber, R. T., Lindley, S., Watson, A. J., Vanscoy, K., Law, C. S., Liddicoat, M. I., Ling, R., Stanton, T., Stockel, J., Collins, C., Anderson, A., Bidigare, R., Ondrusek, M., Latasa, M., Millero, F. J., Lee, K., Yao, W., Zhang, J. Z., Friederich, G., Sakamoto, C., Chavez, F., Buck, K., Kolber, Z., Greene, R., Falkowski, P., Chisholm, S. W., Hoge, F., Swift, R., Yungel, J., Turner, S., Nightingale, P., Hatton, A., Liss, P., Tindale, N. W.: Testing the iron hypothesis in ecosystems of the equatorial Pacific-Ocean, Nature, 371, 123–129, 1994. </reference>
		<reference numeration="34" content_type="text"> Matsumoto, K. and Uematsu, M.: Free amino acids in marine aerosols over the western North Pacific Ocean, Atmos. Environ., 39, 2163–2170, 2005. </reference>
		<reference numeration="35" content_type="text"> Mochida, M., Kawabata, A., Kawamura, K., Hatsushika, H., and Yamazaki, K.: Seasonal variation and origins of dicarboxylic acids in the marine atmosphere over the western North Pacific, J. Geophys. Res.-Atmos., 108(D6), 4193, doi:10.1029/2002JD002355, 2003. </reference>
		<reference numeration="36" content_type="text"> Mochida, M., Kawamura, K., Umemoto, N., Kobayashi, M., Matsunaga, S., Lim, H. J., Turpin, B. J., Bates, T. S., and Simoneit, B. R. T.: Spatial distributions of oxygenated organic compounds (dicarboxylic acids, fatty acids, and levoglucosan) in marine aerosols over the western Pacific and off the coast of East Asia: Continental outflow of organic aerosols during the ACE-Asia campaign, J. Geophys. Res.-Atmos., 108(D23), 8638, doi:10.1029/2002JD003249, 2003. </reference>
		<reference numeration="37" content_type="text"> Moore, C. M., Mills, M. M., Milne, A., Langlois, R., Achterberg, E. P., Lochte, K., Geider, R., J., and La Roche, J.: Iron limits primary productivity during spring bloom development in the central North Atlantic, Glob. Change Biol., 12, 626–634, 2006. </reference>
		<reference numeration="38" content_type="text"> Mopper, K. and Zika, R. G.: Free Amino-Acids in Marine Rains – Evidence for Oxidation and Potential Role in Nitrogen Cycling, Nature, 325, 246–249, 1987. </reference>
		<reference numeration="39" content_type="text"> National Aeronautics and Space Administration (NASA), Goddard Earth Sciences Data and Information Services Center, Giovanni, available at: http://disc.sci.gsfc.nasa.gov/giovanni/, 2009. </reference>
		<reference numeration="40" content_type="text"> Neusüß, C., Pelzing, M., Plewka, A., and Herrmann, H.: A new analytical approach for size-resolved speciation of organic compounds in atmospheric aerosol particles: Methods and first results, J. Geophys. Res., 105, 4513–4527, 2000. </reference>
		<reference numeration="41" content_type="text"> O&apos;Dowd, C. D., Langmann, B., Varghese, S., Scannell, C., Ceburnis, D., and Facchini, M. C.: A combined organic-inorganic sea-spray source function, Geophys. Res. Lett., 35, L01801, doi:10.1029/2007GL030331, 2008. </reference>
		<reference numeration="42" content_type="text"> O&apos;Dowd, C. D., Facchini, M. C., Cavalli, F., Ceburnis, D., Mircea, M., Decesari, S., Fuzzi, S., Yoon, Y. J., and Putaud, J. P.: Biogenically driven organic contribution to marine aerosol, Nature, 431, 676–680, 2004. </reference>
		<reference numeration="43" content_type="text"> O&apos;Dowd, C. D. and Smith, M. H.: Physicochemical Properties of Aerosols over the Northeast Atlantic – Evidence for Wind-Speed-Related Submicron Sea-Salt Aerosol Production, J. Geophys. Res., 98(D1), 1137–1149, 1993. </reference>
		<reference numeration="44" content_type="text"> Pradhan, Y., Lavender, S. J., Hardman-Mountford, N. J., and Aiken, J.: Seasonal and inter-annual variability of chlorophyll-a concentration in the Mauritanian upwelling, Observation of an anomalous event during 1998–1999, Deep-Sea Res. Pt. II, 53, 1548–1559, 2006. </reference>
		<reference numeration="45" content_type="text"> Raemdonck, H., Maenhaut, W., and Andreae, M. O.: Chemistry of Marine Aerosol over the Tropical and Equatorial Pacific, J. Geophys. Res.-Atmos., 91, 8623–8636, 1986. </reference>
		<reference numeration="46" content_type="text"> Resch, F. and Afeti, G.: Submicron Film Drop Production by Bubbles in Seawater, J. Geophys. Res., 97(C3), 3679–3683, 1992. </reference>
		<reference numeration="47" content_type="text"> Roelofs, G. J.: A GCM study of organic matter in marine aerosol and its potential contribution to cloud drop activation, Atmos. Chem. Phys., 8, 709–719, 2008. </reference>
		<reference numeration="48" content_type="text"> Sicre, M. A., Marty, J. C., and Saliot, A.: N-Alkanes, Fatty-Acid Esters, and Fatty-Acid Salts in Size Fractionated Aerosols Collected over the Mediterranean-Sea, J. Geophys. Res.-Atmos., 95, 3649–3657, 1990. </reference>
		<reference numeration="49" content_type="text"> Spracklen, D. V., Arnold, S. R., Sciare, J., Carslaw, K. S., and Pio, C.: Globally significant oceanic source of organic carbon aerosol, Geophys. Res. Lett., 35, L12811, doi:10.1029/2008GL033359, 2008. </reference>
		<reference numeration="50" content_type="text"> van Neste, A., Duce, R. A., and Lee, C.: Methylamines in the Marine Atmosphere, Geophys. Res. Lett., 14, 711–714, 1987. </reference>
		<reference numeration="51" content_type="text"> Wang, H. B., Kawamura, K., and Yamazaki, K.: Water-soluble dicarboxylic acids, ketoacids and dicarbonyls in the atmospheric aerosols over the Southern Ocean and western Pacific Ocean, J. Atmos. Chem., 53, 43–61, 2006. </reference>
		<reference numeration="52" content_type="text"> Woodcock, A. H., Kientzler, C. F., Arons, A. B., and Blanchard, D. C.: Giant Condensation Nuclei from Bursting Bubbles, Nature, 172, 1144–1145, 1953. </reference>
		<reference numeration="53" content_type="text"> Yoon, Y. J., Ceburnis, D., Cavalli, F., Jourdan, O., Putaud, J. P., Facchini, M. C., Decesari, S., Fuzzi, S., Sellegri, K., Jennings, S. G., and O&apos;Dowd, C. D.: Seasonal characteristics of the physicochemical properties of North Atlantic marine atmospheric aerosols, J. Geophys. Res.-Atmos., 112, D04206, doi:10.1029/2005JD007044, 2007. </reference>
	</references>
</article>

