Latitudinal distribution of terrestrial lipid biomarkers and n-alkane compound-specific stable carbon isotope ratios in the atmosphere over the western Pacific and Southern Ocean

被引:93
作者
Bendle, James [1 ]
Kawamura, Kimitaka [1 ]
Yamazaki, Koji [2 ]
Niwai, Takej [3 ]
机构
[1] Hokkaido Univ, Inst Low Temperature Sci, Sapporo, Hokkaido, Japan
[2] Hokkaido Univ, Grad Sch Environm Earth Sci, Sapporo, Hokkaido, Japan
[3] Tokyo Metropolitan Univ, Fac Sci, Dept Chem, Hachioji, Tokyo 19203, Japan
基金
日本学术振兴会;
关键词
D O I
10.1016/j.gca.2007.09.029
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We investigated the latitudinal changes in atmospheric transport of organic matter to the western Pacific and Southern Ocean (27.58 degrees N-64.70 degrees S). Molecular distributions of lipid compound classes (homologous series Of C-15 to C-35 n-alkanes, C-8 to C-34 n-alkanoic acids, C-12 to C-30 n-alkanols) and compound-specific stable isotopes (delta C-13 of C-29 and C-31 n-alkanes) were measured in marine aerosol filter samples collected during a cruise by the RI V Hakuho Maru. The geographical source areas for each sample were estimated from air-mass back-trajectory computations. Concentrations of TC and lipid compound classes were several orders of magnitude lower than observations from urban sites in Asia. A stronger signature of terrestrial higher plant inputs was apparent in three samples collected under conditions of strong terrestrial winds. Unresolved complex mixtures (UCM) showed increasing values in the North Pacific, highlighting the influence of the plume of polluted air exported from East Asia. n-Alkane average chain length (ACL) distribution had two clusters, with samples showing a relation to latitude between 28 degrees N and 47 degrees S (highest ACL values in the tropics), whilst a subset of southern samples had anomalously high ACL values. Compound-specific carbon isotopic analysis of the C29 (-25.6 parts per thousand to -34.5 parts per thousand) and C-31 n-alkanes (-28.3 parts per thousand to -37 parts per thousand) revealed heavier delta C-13 values in the northern latitudes with a transition to lighter values in the Southern Ocean. By comparing the isotopic measurements with back-trajectory analysis it was generally possible to discriminate between different source areas. The terrestrial vegetation source for a subset of the southernmost Southern Ocean is enigmatic; the back-trajectories indicate eastern Antarctica as the only intercepted terrestrial source area. These samples may represent a southern hemisphere background of well mixed and very long range transported higher plant organic material. (C) 2007 Elsevier Ltd. All rights reserved.
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页码:5934 / 5955
页数:22
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