Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin

Lactic acid (LA) and glycolic acid (GA), which are low-molecular-weight hydroxyacids, were identified in the particle and gas phases within the marine atmospheric boundary layer over the western subarctic North Pacific. A major portion of LA (81%) and GA (57%) was present in the particulate phase, w...

Full description

Bibliographic Details
Main Authors: Y. Miyazaki, M. Sawano, K. Kawamura
Format: Article
Language:English
Published: Copernicus Publications 2014-08-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/11/4407/2014/bg-11-4407-2014.pdf
id doaj-198d7e6aaa3b4072a3307cdde43c05e9
record_format Article
spelling doaj-198d7e6aaa3b4072a3307cdde43c05e92020-11-24T22:03:04ZengCopernicus PublicationsBiogeosciences1726-41701726-41892014-08-0111164407441410.5194/bg-11-4407-2014Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial originY. Miyazaki0M. Sawano1K. Kawamura2Institute of Low Temperature Science, Hokkaido University, Sapporo, JapanInstitute of Low Temperature Science, Hokkaido University, Sapporo, JapanInstitute of Low Temperature Science, Hokkaido University, Sapporo, JapanLactic acid (LA) and glycolic acid (GA), which are low-molecular-weight hydroxyacids, were identified in the particle and gas phases within the marine atmospheric boundary layer over the western subarctic North Pacific. A major portion of LA (81%) and GA (57%) was present in the particulate phase, which is consistent with the presence of a hydroxyl group in these molecules leading to the low volatility of the compounds. The average concentration (±SD) of LA in more biologically influenced marine aerosols (33 ± 58 ng m<sup>−3</sup>) was substantially higher than that in less biologically influenced aerosols (11 ± 12 ng m<sup>−3</sup>). Over the oceanic region of phytoplankton blooms, the concentration of aerosol LA was comparable to that of oxalic acid, which was the most abundant diacid during the study period. A positive correlation was found between the LA concentrations in more biologically influenced aerosols and chlorophyll <i>a</i> in seawater (<i>r</i><sup>2</sup> = 0.56), suggesting an important production of aerosol LA possibly associated with microbial (e.g., lactobacillus) activity in seawater and/or aerosols. Our finding provides a new insight into the poorly quantified microbial sources of marine organic aerosols (OAs) because such low-molecular-weight hydroxyacids are key intermediates for OA formation.http://www.biogeosciences.net/11/4407/2014/bg-11-4407-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Y. Miyazaki
M. Sawano
K. Kawamura
spellingShingle Y. Miyazaki
M. Sawano
K. Kawamura
Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin
Biogeosciences
author_facet Y. Miyazaki
M. Sawano
K. Kawamura
author_sort Y. Miyazaki
title Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin
title_short Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin
title_full Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin
title_fullStr Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin
title_full_unstemmed Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin
title_sort low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2014-08-01
description Lactic acid (LA) and glycolic acid (GA), which are low-molecular-weight hydroxyacids, were identified in the particle and gas phases within the marine atmospheric boundary layer over the western subarctic North Pacific. A major portion of LA (81%) and GA (57%) was present in the particulate phase, which is consistent with the presence of a hydroxyl group in these molecules leading to the low volatility of the compounds. The average concentration (±SD) of LA in more biologically influenced marine aerosols (33 ± 58 ng m<sup>−3</sup>) was substantially higher than that in less biologically influenced aerosols (11 ± 12 ng m<sup>−3</sup>). Over the oceanic region of phytoplankton blooms, the concentration of aerosol LA was comparable to that of oxalic acid, which was the most abundant diacid during the study period. A positive correlation was found between the LA concentrations in more biologically influenced aerosols and chlorophyll <i>a</i> in seawater (<i>r</i><sup>2</sup> = 0.56), suggesting an important production of aerosol LA possibly associated with microbial (e.g., lactobacillus) activity in seawater and/or aerosols. Our finding provides a new insight into the poorly quantified microbial sources of marine organic aerosols (OAs) because such low-molecular-weight hydroxyacids are key intermediates for OA formation.
url http://www.biogeosciences.net/11/4407/2014/bg-11-4407-2014.pdf
work_keys_str_mv AT ymiyazaki lowmolecularweighthydroxyacidsinmarineatmosphericaerosolevidenceofamarinemicrobialorigin
AT msawano lowmolecularweighthydroxyacidsinmarineatmosphericaerosolevidenceofamarinemicrobialorigin
AT kkawamura lowmolecularweighthydroxyacidsinmarineatmosphericaerosolevidenceofamarinemicrobialorigin
_version_ 1725833337078022144