Butler Jessica L, Williams Mark A, Bottomley Peter J, Myrold David D
Departments of Crop and Soil Science. Microbiology, Oregon State University, Corvallis, Oregon 97331, USA.
Appl Environ Microbiol. 2003 Nov;69(11):6793-800. doi: 10.1128/AEM.69.11.6793-6800.2003.
Root-deposited photosynthate (rhizodeposition) is an important source of readily available carbon (C) for microbes in the vicinity of growing roots. Plant nutrient availability is controlled, to a large extent, by the cycling of this and other organic materials through the soil microbial community. Currently, our understanding of microbial community dynamics associated with rhizodeposition is limited. We used a (13)C pulse-chase labeling procedure to examine the incorporation of rhizodeposition into individual phospholipid fatty acids (PLFAs) in the bulk and rhizosphere soils of greenhouse-grown annual ryegrass (Lolium multiflorum Lam. var. Gulf). Labeling took place during a growth stage in transition between active root growth and rapid shoot growth on one set of plants (labeling period 1) and 9 days later during the rapid shoot growth stage on another set of plants (labeling period 2). Temporal differences in microbial community composition were more apparent than spatial differences, with a greater relative abundance of PLFAs from gram-positive organisms (i15:0 and a15:0) in the second labeling period. Although more abundant, gram-positive organisms appeared to be less actively utilizing rhizodeposited C in labeling period 2 than in labeling period 1. Gram-negative bacteria associated with the 16:1omega5 PLFA were more active in utilizing (13)C-labeled rhizodeposits in the second labeling period than in the first labeling period. In both labeling periods, however, the fungal PLFA 18:2omega6,9 was the most highly labeled. These results demonstrate the effectiveness of using (13)C labeling and PLFA analysis to examine the microbial dynamics associated with rhizosphere C cycling by focusing on the members actively involved.
根系分泌的光合产物(根际沉积)是生长根系附近微生物易于获取的重要碳源。植物养分的有效性在很大程度上受这种及其他有机物质通过土壤微生物群落循环的控制。目前,我们对与根际沉积相关的微生物群落动态的了解有限。我们采用了¹³C脉冲追踪标记程序,以研究温室种植的一年生黑麦草(多花黑麦草海湾变种)的根际沉积在土体和根际土壤中单个磷脂脂肪酸(PLFA)中的掺入情况。标记在一组植物的根系活跃生长与地上部快速生长之间的过渡生长阶段进行(标记期1),9天后在另一组植物的地上部快速生长阶段进行(标记期2)。微生物群落组成的时间差异比空间差异更明显,在第二个标记期,革兰氏阳性菌(i15:0和a15:0)的PLFA相对丰度更高。虽然革兰氏阳性菌数量更多,但在标记期2,它们利用根际沉积碳的活性似乎低于标记期1。与16:1ω5 PLFA相关的革兰氏阴性菌在第二个标记期比第一个标记期更积极地利用¹³C标记的根际沉积物。然而,在两个标记期,真菌PLFA 18:2ω6,9的标记程度最高。这些结果表明,通过关注积极参与的成员,使用¹³C标记和PLFA分析来研究与根际碳循环相关的微生物动态是有效的。