Variable emissions of microbial volatile organic compounds (MVOCs) from root-associated fungi isolated from Scots pine

被引:88
作者
Back, Jaana [1 ,2 ]
Aaltonen, Hermanni [1 ]
Hellen, Heidi [3 ]
Kajos, Maija K. [2 ]
Patokoski, Johanna [2 ]
Taipale, Risto [2 ]
Pumpanen, Jukka [1 ]
Heinonsalo, Jussi [4 ]
机构
[1] Univ Helsinki, Dept Forest Sci, FI-00014 Helsinki, Finland
[2] Univ Helsinki, Dept Phys, FI-00014 Helsinki, Finland
[3] Finnish Meteorol Inst, FI-00101 Helsinki, Finland
[4] Univ Helsinki, Dept Food & Environm Sci, FI-00014 Helsinki, Finland
基金
芬兰科学院;
关键词
Boreal soil fungi; Microbial volatile organic compounds (MVOCs); Carbonyls; Isoprenoids; REACTION-MASS-SPECTROMETRY; MONOTERPENE EMISSIONS; BUILDING-MATERIALS; FOREST SOIL; PTR-MS; ISOPRENE; HYDROCARBON; METABOLITES; FLUXES; LITTER;
D O I
10.1016/j.atmosenv.2010.06.042
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Soils emit a large variety of volatile organic compounds. In natural ecosystems, measurements of microbial volatile organic compound (MVOC) exchange rates between soil and atmosphere are difficult due to e.g. the spatial heterogeneity of the belowground organisms, and due to the many potential sources for the same compounds. We measured in laboratory conditions the MVOC emission rates and spectra of eight typical fungi occurring in boreal forest soils. The studied species are decomposers (Gymnopilus penetrans, Ophiostoma abietinum), ectomycorrhizal (Cenococcum geophilum, Piloderma olivaceum, Suillus variegatus, Tomentellopsis submollis) and endophytic fungi (Meliniomyces variabilis, Phialocephala fortinii). The MVOC emissions contained altogether 21 known and 6 unidentified compounds whose emission rates were >0.1 mu g g(DW)(-1) h(-1). The most abundant compounds were the short-chain carbonyl compounds (acetone and acetaldehyde). The greatest carbonyl emissions were measured from P. olivaceum (1.9 mg acetone g (DW)(-1) h(-1)) and P. fortinii (0.114 mg acetaldehyde g(DW)(-1) h(-1)). Terpenoid emissions (isoprene, mono- and sesquiterpenes) were detected from some fungal cultures, but in relatively small amounts. We conclude that soil micro-organisms can potentially be responsible for significant emissions of volatiles, especially short-chain oxygenated compounds, to the below-canopy atmosphere. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:3651 / 3659
页数:9
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