Application of 13C-labeled litter and root materials for in situ decomposition studies using phospholipid fatty acids

微观世界 垃圾箱 分解 微生物种群生物学 生物地球化学循环 生态系统 δ13C 植物凋落物 土壤水分 有机质 动物科学 化学 生物 生态学 农学 细菌 物理 量子力学 遗传学 稳定同位素比值
作者
Jennifer Moore‐Kucera,Richard P. Dick
出处
期刊:Soil Biology & Biochemistry [Elsevier]
卷期号:40 (10): 2485-2493 被引量:125
标识
DOI:10.1016/j.soilbio.2008.06.002
摘要

Microorganisms play a central role in litter decomposition and partitioning C between CO2 evolution and sequestration of C into semi-permanent pools in soils. At the ecosystem level, forest stand age influences rates of litter accumulation and quality, and micro-climatology which could affect the microbial community structure and C sequestration processes. Although numerous laboratory experiments have studied the decomposition of model 13C-labeled compounds, few studies have verified these findings under field conditions. The objective of this study was to track decomposition of 13C-labeled Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) materials into the soil microbial community using 13C-phospholipids fatty acid (PLFA) analysis in three different aged forest stands. A field experiment was conducted that had three forest stand age treatments: old-growth (>500 yrs); 8-year-old clear-cut (CC8); and 25-year-old clear-cut (CC25) (landscape reps of n = 2). Each stand age had in situ microcosms that were amended with either 13C-labeled surface litter or root material. Microcosms were destructively sampled seven times over a 22-month period and the soil was analyzed for the relative amounts of 13C incorporated (13C%INCORP) into PLFAs and the proportional distribution of 13C incorporated into PLFAs. The 13C%INCORP was affected by stand age and 13C source with greater 13C%INCORP in samples from CC8 than OG or CC25. Also, the level of 13C%INCORP was greater for labeled litter than root material in five out of the seven sample dates. In general, 18:1ω9 and 18:2ω6,9 (common fungal biomarkers) had the greatest amount of 13C incorporation throughout the study period in both clear-cut and old-growth sites, especially in plots with 13C-labeled litter. Our data showed a low fungal 13C-PLFA: bacterial 13C-PLFA ratio (0.45) 1 month after incubation was initiated compared to 5, 7 and 9 months after incubation (two of these dates were >1.0). This suggests that initially bacteria played a greater role in the decomposition of the added needles with fungi playing a more important role in subsequent sample dates. Our results illustrate that the use of 13C-labeled materials in field studies coupled with13C-PLFA profiling is a powerful tool for determining microbial dynamics during decomposition – enabling statistically significant detection of land management treatment effects on C acquisition by microbial functional groups.

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