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	<journal>
		<journal_title>Biogeosciences</journal_title>
		<journal_url>www.biogeosciences.net</journal_url>
		<issn>1726-4170</issn>
		<eissn>1726-4189</eissn>
		<volume_number>7</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/bg-7-387-2010</doi>
	<article_url>http://www.biogeosciences.net/7/387/2010/</article_url>
	<abstract_html>http://www.biogeosciences.net/7/387/2010/bg-7-387-2010.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/7/387/2010/bg-7-387-2010.pdf</fulltext_pdf>
	<start_page>387</start_page>
	<end_page>394</end_page>
	<publication_date>2010-01-29</publication_date>
	<article_title content_type="html">A possible role of ground-based microorganisms on cloud formation in the atmosphere</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. EkstrÃ¶m</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>B. NoziÃ¨re</name>
			<email>barbara.noziere@itm.su.se</email>
		</author>
		<author numeration="3" affiliations="2">
			<name>M. Hultberg</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>T. Alsberg</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>J. MagnÃ©r</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>E. D. Nilsson</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>P. Artaxo</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Applied Environmental Science (ITM), Svante Arrhenius vÃ¤g 8, Stockholm University, 106 91 Stockholm, Sweden</affiliation>
		<affiliation numeration="2" content_type="html">Department of Horticulture, Swedish University of Agricultural Sciences, Alnarp, Sweden</affiliation>
		<affiliation numeration="3" content_type="html">Department of Physics, University of SÃ£o Paolo, SÃ£o Paolo, Brazil</affiliation>
	</affiliations>
	<abstract content_type="html">The formation of clouds is an important process for the atmosphere, the
hydrological cycle, and climate, but some aspects of it are not completely
understood. In this work, we show that microorganisms might affect cloud
formation without leaving the Earth&apos;s surface by releasing biological
surfactants (or biosurfactants) in the environment, that make their way into
atmospheric aerosols and could significantly enhance their activation into
cloud droplets.
&lt;br&gt;&lt;br&gt;
In the first part of this work, the cloud-nucleating efficiency of standard
biosurfactants was characterized and found to be better than that of any
aerosol material studied so far, including inorganic salts. These results
identify molecular structures that give organic compounds exceptional
cloud-nucleating properties. In the second part, atmospheric aerosols were
sampled at different locations: a temperate coastal site, a marine site, a
temperate forest, and a tropical forest. Their surface tension was measured
and found to be below 30 mN/m, the lowest reported for aerosols, to our
knowledge. This very low surface tension was attributed to the presence of
biosurfactants, the only natural substances able to reach to such low
values.
&lt;br&gt;&lt;br&gt;
The presence of strong microbial surfactants in aerosols would be consistent
with the organic fractions of exceptional cloud-nucleating efficiency
recently found in aerosols, and with the correlations between algae bloom
and cloud cover reported in the Southern Ocean. The results of this work
also suggest that biosurfactants might be common in aerosols and thus of
global relevance. If this is confirmed, a new role for microorganisms on the
atmosphere and climate could be identified.</abstract>
	<references>
		<reference numeration="1" content_type="text"> % vor jede Referenz Ahern, H. E., Walsh, K. A., Hill, T. C. J., and Moffett, B. F.: Fluorescent pseudomonads isolated from Hebridean cloud and rain water produce biosurfactants but do not cause ice nucleation, Biogeosciences, 4, 115â€“124, 2007. </reference>
		<reference numeration="2" content_type="text"> Asa-Awuku, A., Sullivan, A. P., Hennigan, C. J., Weber, R. J., and Nenes, A.: Investigation of molar volume and surfactant characteristics of water-soluble organic compounds in biomass burning aerosol, Atmos. Chem. Phys., 8, 799â€“812, 2008. </reference>
		<reference numeration="3" content_type="text"> Bauer, H., Giebl, H., Hitzenberg, R., Kasper-Giebl, A., Reschl, G., Zibushka, F., and Puxbaum, H.: Airborne bacteria as cloud condensation nuclei, J. Geophys. Res., 108, 4658, doi:10.1029/2003JD003545, 2003. </reference>
		<reference numeration="4" content_type="text"> Benincasa, M., Abalos, A., Oliveira, I., and Manresa, A.: Chemical structure, surface Properties and biological activities of the biosurfactant produced by Pseudomonas aeruginosa LBI from soapstock, Antonie van Leeuwenhoek, 85, 1â€“8, 2004. </reference>
		<reference numeration="5" content_type="text"> Bodour, A. A., Drees, K. P., and Maier, R. M.: Distribution of biosurfactant-producing Bacteria in undisturbed and contaminated arid Southwestern soils, Appl. Environ. Microbiol., 69, 3280â€“3287, 2003. </reference>
		<reference numeration="6" content_type="text"> Charlson, R. J., Lovelock, J. E., Andreae, M. O., and Warren, S. G.: Oceanic phytoplankton, atmospheric sulphur, cloud albedo and climate, Nature, 326, 655â€“661, 1987. </reference>
		<reference numeration="7" content_type="text"> Charlson, R. J., Seinfeld, J. H., Nenes, A., Kulmala, M., Laaksonen, A., and Facchini, M. C.: Reshaping the Theory of Cloud Formation, Science, 292, 2025â€“2026, 2001. </reference>
		<reference numeration="8" content_type="text"> Cho, J. C., and Tiedje, J. M.: Biogeography and Degree of Endemicity of Fluorescent Pseudomonas Strains in Soil, Appl. Environ. Microbiol., 66, 5448â€“5456, 2000. </reference>
		<reference numeration="9" content_type="text"> Desai, J. D. and Banat, I. M.: Microbial production of surfactants and their commercial Potential, Microbiol. Mol. Biol. R., 61, 47â€“64, 1997. </reference>
		<reference numeration="10" content_type="text"> Dobson, C. M., Ellison, G. B., Tuck, A. F., and Vaida, V.: Atmospheric aerosols as prebiotic chemical reactors, P. Natl. Acad. Sci. USA, 97, 11864â€“11868, 2000. </reference>
		<reference numeration="11" content_type="text"> EkstrÃ¶m, S., NoziÃ¨re, B., and Hansson, H.-C.: The Cloud Condensation Nuclei (CCN) properties of 2-methyltetrols and C3-C6 polyols from osmolality and surface tension measurements, Atmos. Chem. Phys., 9, 973â€“980, 2009. </reference>
		<reference numeration="12" content_type="text"> Ellison, G. B., Tuck, A. F., and Vaida, V.: Atmospheric processing of organic aerosols, J. Geophys. Res., 101, 11633â€“11641, 1999. </reference>
		<reference numeration="13" content_type="text"> Ervens, B., Feingold, G., and Kredenweis, S. M.: Influence of water-soluble organic carbon on cloud drop number concentration, J. Geophys. Res., 110, D18211, doi:10.1029/2004JD005634, 2005. </reference>
		<reference numeration="14" content_type="text"> Facchini, M. C., Mircea, M., Fuzzi, S., and Charlson, R. J.: Cloud albedo enhancement by surface-active organic solutes in growing droplets, Nature, 410, 257â€“259, 1999. </reference>
		<reference numeration="15" 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, 2008. </reference>
		<reference numeration="16" content_type="text"> Foster, P., Ramaswamy, V., Artaxo, P., et al.: Changes in atmospheric constituents and in radiative forcing, in: Climate Change 2007: The Physical Science Basis, edited by: Solomon, S., Qin, D., Manning, M., et al., Cambridge University Press, Cambridge, UK, a) 171â€“172; b) p 160, 2007. </reference>
		<reference numeration="17" content_type="text"> Gulati, A., Rahi, P., and Vyas, P.: Characterization of phosphate-solubilizing fluorescent Pseudomonads from the rhizosphere of seabuckthorn growing in the cold deserts of Himalayas, Current Microbiol., 56, 73â€“79, 2008. </reference>
		<reference numeration="18" content_type="text"> Harrison, R. M., Jones, A. M., Biggins, P. D. E., Pomeroy, N., Cox, C. S., Kidd, S. P., Hobman, J. L., Brown, N. L., and Beswick, A.: Climate factors influencing bacterial count in background air samples, Int. J. Biometeorol., 4, 167â€“178, 2005. </reference>
		<reference numeration="19" content_type="text"> Hommel, R. K. and Ratledge, C.: Biosynthetic mechanisms of low molecular weight surfactants and their precursor molecules, in Biosurfactants, edited by: Kosaric, N., Marcel Dekker, New York, USA, p 5, 1993. </reference>
		<reference numeration="20" content_type="text"> Hultberg, M., Bergstrand, K. J., Khalil, S., and Alsanius, B.: Production of biosurfactants and antibiotics by fluorescent pseudomonads isolated from a closed hydroponic system equipped with a slow filter, Antonie van Leeuwenhoek, 93, 373â€“380, 2008. </reference>
		<reference numeration="21" content_type="text"> Ikawa, M., Sanser, J. J., and Haney, J. F.: Lipids of cyanobacterium Aphanizomenon flos-aquae and inhibition of Chlorella growth, J. Chem. Ecol., 20, 2429â€“2436, 1994. </reference>
		<reference numeration="22" content_type="text"> Jarvis, F. G. and Johnson M. J.: A Glyco-lipide produced by Pseudomonas aeruginosa, J. Am. Chem. Soc., 71, 4124â€“4126, 1949. </reference>
		<reference numeration="23" content_type="text"> Kiss, G. and Hansson, H.-C.: Application of osmolality for the determination of water activity and the modelling of cloud formation, Atmos. Chem. Phys. Discuss., 4, 7667â€“7689, 2004. </reference>
		<reference numeration="24" content_type="text"> Kourtchev, I., Ruuskanen, T., Maenhaut, W., Kulmala, M., and Claeys, M.: Observation of 2-methyltetrols and related photo-oxidation products of isoprene in boreal forest aerosols from HyytiÃ¤l &quot;a, Finland, Atmos. Chem. Phys., 5, 2761â€“2770, 2005. </reference>
		<reference numeration="25" content_type="text"> Lin, J. J. and Lee, L.-C.: Characterization of $n$-alkanes in urban submicron aerosol particles (PM$_1)$, Atmos. Environ., 38, 2983â€“2991, 2004. </reference>
		<reference numeration="26" content_type="text"> McFiggans, G., Artaxo, P., Baltensperger, U., Coe, H., Facchini, M. C., Feingold, G., Fuzzi, S., Gysel, M., Laaksonen, A., Lohmann, U., Mentel, T. F., Murphy, D. M., O&apos;Dowd, C. D., Snider, J. R., and Weingartner, E.: The effect of physical and chemical aerosol properties on warm cloud droplet activation, Atmos. Chem. Phys., 6, 2593â€“2649, 2006. </reference>
		<reference numeration="27" content_type="text"> Merritt, M. V., Rosenstein, S. P., Loh, C., Hui-Sui Chou, R., and Allen, M. M.: A comparison of the major lipid classes and fatty acid composition of marine unicellular cyanobacteria freshwater species, Arch. Microbiol., 155, 107â€“113, 1991. </reference>
		<reference numeration="28" content_type="text"> Meskhidze, N. and Nenes, A.: Phytoplankton and cloudiness in the Southern ocean, Science, 314, 1419â€“1423, 2006. </reference>
		<reference numeration="29" content_type="text"> Möhler, O., DeMott, P. J., Vali, G., and Levin, Z.: Microbiology and atmospheric processes: the role of biological particles in cloud physics, Biogeosciences, 4, 1059â€“1071, 2007. </reference>
		<reference numeration="30" 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, 4297, doi:10.1029/2002JD002263, 2003. </reference>
		<reference numeration="31" content_type="text"> Nilsson, E. D. and Leck, C.: A pseudo-Lagrangian study of the sulfur budget in the remote Arctic marine boundary layer, Tellus, 54B, 213â€“230, 2002. </reference>
		<reference numeration="32" content_type="text"> Perfumo, A., Banat, I. M., Canganella, F., Marchant, R.: Rhamnolipid production by a novel thermophilic hydrocarbon-degrading Pseudomonas aeruginosa AP02-1, Appl. Microbiol. Biotechnol., 72, 132â€“138, 2006. </reference>
		<reference numeration="33" content_type="text"> PÃ³sfai, M., Li, J., Anderson, J. R., and Buseck, P. R.: Aerosol bacteria over the Southern Ocean during ACE-1, Atmos. Res., 66, 231â€“240, 2003. </reference>
		<reference numeration="34" content_type="text"> Pratt, K., DeMott, P. J., French, J. R., Wang, Z., Westphal, D. L., Heymsfield, A. J., Twohy, C. H., Prenni, A. J., and Prather, K. A.: In situ detection of biological particles in cloud ice-crystals, Nature Geosci., 2, 398â€“401, 2009. </reference>
		<reference numeration="35" content_type="text"> Schnell, R. C. and Vali, G.: Atmospheric ice nuclei from decomposing vegetation, Nature, 236, 163â€“167, 1972. </reference>
		<reference numeration="36" content_type="text"> Schnell, R. C.: Bacteria acting as ice nucleants at temperatures approaching &amp;minus;1 &amp;deg;C, B. Am. Meteorol. Soc., 57, 1356â€“1357, 1976. </reference>
		<reference numeration="37" content_type="text"> Shapiro, J.: Blue-Green Algae: Why they become dominant, Science, 179, 382â€“384, 1973. </reference>
		<reference numeration="38" content_type="text"> Shaw, G. E.: Biocontrolled thermostasis involving the sulfur cycle, Climate Change, 5, 297â€“303, 1983. </reference>
		<reference numeration="39" content_type="text"> Taraniuk, I., Graber, E. R., Kostinski, A., and Rudich, Y.: Surfactant properties of atmospheric and model humic-like substances (HULIS), Geophys. Res. Lett., 34, L16807, doi:10.1029/GL029576, 2007. </reference>
		<reference numeration="40" content_type="text"> Van der Kooij, D.: Characterization and classification of fluorescent pseudomonads isolated from tap water and surface water, Antonie van Leeuwenhoek, 45, 225â€“240, 1979. </reference>
		<reference numeration="41" content_type="text"> Varga, Z., Kiss, G., and Hansson, H.-C.: Modelling the cloud condensation nucleus activity of organic acids on the basis of surface tension and osmolality measurements, Atmos. Chem. Phys., 7, 4601â€“4611, 2007. </reference>
		<reference numeration="42" content_type="text"> Vishwanath, B. S., Eichenberger, W., Frey, F. J., and Frey, B. M.: Interaction of plant lipids with 14 kDa phospholipase A2 enzymes, Biochem. J., 320, 93â€“99, 1996. </reference>
		<reference numeration="43" content_type="text"> Wang, Q., Fang, X., Bai, B., Liang, X., Shuler, P. J., Goddard, W. A., and Tang, Y.: Engineering bacteria for production of rhamnolipid as an agent for enhanced oil recovery, Biotechnol. Bioeng., 98, 842â€“853, 2007. </reference>
		<reference numeration="44" content_type="text"> Williams, R. J., Philips, J. N., and Mysels, K. J.: The critical micelle concentration of sodium lauryl sulphate at 25 &amp;deg;C, T. Faraday Soc., 51, 728â€“737, 1955. </reference>
		<reference numeration="45" content_type="text"> Yang, H., Yu, J. Z., Ho, S. S. H., Xu, J., Wu, W. -S., Wan, C. H., Wang, X., Wang, X., and Wang, L.: The chemical composition of inorganic and carbonaceous materials in PM$_2.5$ in Nanjing, China, Atmos. Environ., 39, 3735â€“3749, 2005. </reference>
		<reference numeration="46" content_type="text"> Zhang, Q. and Anastasio, C.: Free and combined amino compounds in atmospheric fine particles (PM$_2.5)$ and fog waters from Northern California, Atmos. Environ., 37, 2247â€“2258, 2003. </reference>
		<reference numeration="47" content_type="text"> Zhang, Y. and Miller, R. M.: Enhanced octadecane dispersion and biodegradation by a Pseudomonas rhamnolipid surfactant, Appl. Environ. Microbiol., 58, 3276â€“3282, 1992. </reference>
	</references>
</article>
