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Hydroxy fatty acids in snow pit samples from Mount Tateyama in central Japan: Implications for atmospheric transport of microorganisms and plant waxes associated with Asian dust

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Please use this identifier to cite or link to this item:http://hdl.handle.net/2115/65510

Title: Hydroxy fatty acids in snow pit samples from Mount Tateyama in central Japan: Implications for atmospheric transport of microorganisms and plant waxes associated with Asian dust
Authors: Tyagi, Poonam Browse this author
Kawamura, Kimitaka Browse this author
Bikkina, Srinivas Browse this author
Mochizuki, Tomoki Browse this author
Aoki, Kazuma Browse this author
Issue Date: 19-Nov-2016
Publisher: American Geophysical Union
Journal Title: Journal of geophysical research atmospheres
Volume: 121
Issue: 22
Start Page: 13641
End Page: 13660
Publisher DOI: 10.1002/2016JD025340
Abstract: We report here the source apportionment of atmospheric soil microorganisms and higher plant metabolites based on chemical markers (hydroxy fatty acids: FAs) in the snowpack samples collected from Mount Tateyama in central Japan during spring 2009 (N = 6) and 2011 (N = 7). A homologous series of beta-hydroxy FAs (C-9-C-20), constituents of Gram-negative bacteria (GNB), in snowpacks clearly suggest a long-range atmospheric transport of dust-associated bacteria followed by scavenging by snowflakes. Similarly, higher atmospheric abundances of alpha-(C-16-C-32) and omega-(C-9-C-30)-hydroxy FAs in the snow layers containing Asian dust revealed contributions from soil microbes and higher plant epicuticular waxes. Moreover, covariation between the concentrations of hydroxy FAs and water-soluble Ca2+ (dust tracer), together with calculated air mass backward trajectories, demonstrated their source regions such as the Taklamakan Desert, Gobi Desert, and Loess Plateau. A close match of molecular distributions of hydroxy FAs (with the predominance of omega- and beta-isomers) is noteworthy between snowpack (present study) and springtime aerosols from Chichijima Island in the western North Pacific (WNP). This observation suggests a "below-cloud scavenging" of transported dust particles and associated soil microbes in the East Asian outflow by snowflakes. These distributions are, however, contrary to those observed in the fresh snow samples from Sapporo, northern Japan (predominance of a-hydroxy FAs), which could be explained by "in-cloud" microbial oxidation processes. This comparison, therefore, provides additional insights regarding the aeolian transport of soil microbes in the East Asian outflow to the WNP, which has not been available.
Rights: Copyright 2016 American Geophysical Union.
Type: article
URI: http://hdl.handle.net/2115/65510
Appears in Collections:低温科学研究所 (Institute of Low Temperature Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

Submitter: 河村 公隆

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