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Modulation of Litter Decomposition by the Soil Microbial Food Web Under Influence of Land Use Change

机译:土地利用变化对土壤微生物食物网分解垃圾的调控

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摘要

Soil microbial communities modulate soil organic matter (SOM) dynamics by catalyzing litter decomposition. However, our understanding of how litter-derived carbon (C) flows through the microbial portion of the soil food web is far from comprehensive. This information is necessary to facilitate reliable predictions of soil C cycling and sequestration in response to a changing environment such as land use change in the form of agricultural abandonment. To examine the flow of litter-derived C through the soil microbial food web and it’s response to land use change, we carried out an incubation experiment with soils from six fields; three recently abandoned and three long term abandoned fields. In these soils, the fate of 13C-labeled plant litter was followed by analyzing phospholipid fatty acids (PLFA) over a period of 56 days. The litter-amended soils were sampled over time to measure 13CO2 and mineral N dynamics. Microbial 13C-incorporation patterns revealed a clear succession of microbial groups during litter decomposition. Fungi were first to incorporate 13C-label, followed by G bacteria, G+ bacteria, actinomycetes and micro-fauna. The order in which various microbial groups responded to litter decomposition was similar across all the fields examined, with no clear distinction between recent and long-term abandoned soils. Although the microbial biomass was initially higher in long-term abandoned soils, the net amount of 13C-labeled litter that was incorporated by the soil microbial community was ultimately comparable between recent and long-term abandoned fields. In relative terms, this means there was a higher efficiency of litter-derived 13C-incorporation in recent abandoned soil microbial communities compared to long-term abandoned soils, most likely due to a net shift from SOM-derived C toward root-derived C input in the soil microbial food web following land-abandonment.
机译:土壤微生物群落通过催化凋落物分解来调节土壤有机质(SOM)的动态。但是,我们对源自垃圾的碳(C)如何流经土壤食物网的微生物部分的了解还远远不够。该信息对于促进对土壤C循环和固碳的可靠预测是必需的,以响应不断变化的环境(例如农业废弃形式的土地利用变化)。为了研究源自垃圾的碳通过土壤微生物食物网的流动及其对土地利用变化的响应,我们对六个领域的土壤进行了孵化实验;三个最近被遗弃的土地和三个长期被遗弃的土地。在这些土壤中,用 13 C标记的植物凋落物的命运随后分析了56天的磷脂脂肪酸(PLFA)。随时间取样对凋落物改良土壤进行采样,以测量 13 CO2和矿质氮的动态变化。微生物 13 C的掺入模式表明,凋落物分解过程中微生物群的分布明显。真菌首先加入了 13 C-标记,其次是G -细菌,G + 细菌,放线菌和微动物。在所有考察的领域中,不同微生物群对凋落物分解的响应顺序相似,近期和长期废弃的土壤之间没有明显的区别。尽管长期废弃的土壤中微生物的生物量最初较高,但土壤微生物群落掺入的 13 C标记凋落物的净含量最终可与近期和长期废弃田地相媲美。相对而言,这意味着与长期废弃的土壤相比,最近废弃的土壤微生物群落中凋落物衍生的 13 C掺入效率更高,这很可能是由于SOM-土地遗弃后,土壤微生物食物网中根源碳输入的碳转化为碳。

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