2015
DOI: 10.5194/bgd-12-13375-2015
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Hydroxy fatty acids in fresh snow samples from northern Japan: long-range atmospheric transport of Gram-negative bacteria by Asian winter monsoon

Abstract: Abstract. Hydroxy fatty acids (FAs) in fresh snow from Sapporo, one of the heaviest snowfall regions in the world, have been studied to ascertain the airborne bacterial endotoxin concentrations and their biomass. The presence of β-hydroxy FAs (C9–C28), constituents of Gram-negative bacteria (GNB), suggests long-range transport of soil microbes. Likewise, the occurrence of α- and ω-hydroxy FAs (C9–C30 and C9–C28, respectively) in snow reveals their contribution from epicuticular waxes and soil microorganisms. E… Show more

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Cited by 8 publications
(38 citation statements)
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“…Mass concentrations of total β ‐ and ω ‐hydroxy FAs in the dusty and nondusty layers (classified based on the visual appearance and nss‐Ca 2+ concentration, see Table ) of snowpacks collected in 2009 ( β ‐isomers: 1.04 µg kg −1 ; ω ‐isomers: 4.96 µg kg −1 ) and 2011 ( β ‐isomers: 0.62 µg kg −1 ; ω ‐isomers: 0.42 µg kg −1 ) were significantly higher than those reported in the fresh snow samples collected from Sapporo (northern Japan) during winter 2010 ( β ‐isomers: 0.24 µg kg −1 ; ω ‐isomers: 0.64 µg kg −1 ) and 2011 ( β ‐isomers: 0.18 µg kg −1 ; ω ‐isomers: 0.15 µg kg −1 ) [ Tyagi et al ., ]. This difference is due to a strong influence of the atmospheric input of Asian dust in the snowpack samples at the Murodo‐Daira site.…”
Section: Resultsmentioning
confidence: 99%
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“…Mass concentrations of total β ‐ and ω ‐hydroxy FAs in the dusty and nondusty layers (classified based on the visual appearance and nss‐Ca 2+ concentration, see Table ) of snowpacks collected in 2009 ( β ‐isomers: 1.04 µg kg −1 ; ω ‐isomers: 4.96 µg kg −1 ) and 2011 ( β ‐isomers: 0.62 µg kg −1 ; ω ‐isomers: 0.42 µg kg −1 ) were significantly higher than those reported in the fresh snow samples collected from Sapporo (northern Japan) during winter 2010 ( β ‐isomers: 0.24 µg kg −1 ; ω ‐isomers: 0.64 µg kg −1 ) and 2011 ( β ‐isomers: 0.18 µg kg −1 ; ω ‐isomers: 0.15 µg kg −1 ) [ Tyagi et al ., ]. This difference is due to a strong influence of the atmospheric input of Asian dust in the snowpack samples at the Murodo‐Daira site.…”
Section: Resultsmentioning
confidence: 99%
“…[] and Tyagi et al . []. In brief, melt snow samples (0.2–0.4 L) were first concentrated using a rotary evaporator under vacuum (<20°C) and then saponified with 1.0 M KOH in methanol at 80°C for 2 h. After the saponification, neutral components were removed by extraction with hexane/methylene chloride (10:1) and the remaining solution was acidified with 6 M HCl to form free carboxylic acids.…”
Section: Experimental Methodsmentioning
confidence: 99%
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