Linking dynamics of soil microbial phospholipid fatty acids to carbon mineralization in a 13C natural abundance experiment: Impact of heavy metals and acid rain

• Published in: Soil biology & biochemistry 2007, Vol.39 (12), p.3177-3186
• Main Authors: Stemmer, Michael, Watzinger, Andrea, Blochberger, Karl, Haberhauer, Georg, Gerzabek, Martin H.
• Format: Article
• Language: English
• Subjects: 13C; acid deposition; Acid rain; Agronomy. Soil science and plant productions; Biochemistry and biology; Biological and medical sciences; biomarkers; carbon; Chemical, physicochemical, biochemical and biological properties; community structure; corn straw; fatty acids; forest soils; Fundamental and applied biological sciences. Psychology; Heavy metals; isotope labeling; Maize straw; Microbiology; Mineralization; phospholipids; Physics, chemistry, biochemistry and biology of agricultural and forest soils; plant residues; PLFAs; polluted soils; Soil and water pollution; Soil microorganisms; soil pollution; soil properties; Soil science
• ISSN: 0038-0717; 1879-3428
• DOI: 10.1016/j.soilbio.2007.07.013

A 13C natural abundance experiment including GC-c-IRMS analysis of phospholipid fatty acids (PLFAs) was conducted to assess the temporal dynamics of the soil microbial community and carbon incorporation during the mineralization of plant residues under the impact of heavy metals and acid rain. Maize straw was incorporated into (i) control soil, (ii) soil irrigated with acid rain, (iii) soil amended with heavy metal-polluted filter dust and (iv) soil with both, heavy metal and acid rain treatment, over a period of 74 weeks. The mineralization of maize straw carbon was significantly reduced by heavy metal impact. Reduced mineralization rate of the added carbon likely resulted from a reduction of the microbial biomass due to heavy metal stress, while the efficiency of 13C incorporation into microbial PLFAs was hardly affected. Since acid rain did not significantly change soil pH, little impact on soil microorganisms and mineralization rate was found. Temporal dynamics of labelling of microbial PLFAs were different between bacterial and fungal PLFA biomarkers. Utilization of maize straw by bacterial PLFAs peaked immediately after the application (2 weeks), while labelling of the fungal biomarker 18:2 ω6,9 was most pronounced 5 weeks after the application. In general, 13C labelling of microbial PLFAs was closely linked to the amounts of maize carbon present in the soil. The distinct higher labelling of microbial PLFAs in the heavy metal-polluted soils 74 weeks after application indicated a large fraction of available maize straw carbon still present in the soil.