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首页> 外文期刊>Biogeosciences >Transcriptional activities of methanogens and methanotrophs vary with methane emission flux in rice soils under chronic nutrient constraints of phosphorus and potassium
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Transcriptional activities of methanogens and methanotrophs vary with methane emission flux in rice soils under chronic nutrient constraints of phosphorus and potassium

机译:在磷,钾的长期养分约束下,稻田甲烷气体和甲烷营养菌的转录活性随甲烷排放量的变化而变化

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摘要

Nutrient status in soil is crucial for the growth and development of plants which indirectly or directly affect the ecophysiological functions of resident soil microorganisms. Soil methanogens and methanotrophs can be affected by soil nutrient availabilities and plant growth, which in turn modulate methane (CH4) emissions. Here, we assessed whether deficits in soil-available phosphorus (P) and potassium (K) modulated the activities of methanogens and methanotrophs in a long-term (20 year) experimental system involving limitation in either one or both nutrients. Results showed that a large amount of CH4 was emitted from paddy soil at rice tillering stage (flooding) while CH4 flux was minimum at ripening stage (drying). Compared to soils amended with NPK fertiliser treatment, the soils without P input significantly reduced methane flux rates, whereas those without K input did not. Under P limitation, methanotroph transcript copy number significantly increased in tandem with a decrease in methanogen transcript abundance, suggesting that P-deficiency-induced changes in soil physiochemical properties, in tandem with rice plant growth, might constrain the activity of methanogens, whereas the methanotrophs might be adaptive to this soil environment. In contrast, lower transcript abundance of both methanogen and methanotrophs were observed in K-deficient soils. Assessments of community structures based upon transcripts indicated that soils deficient in P induced greater shifts in the active methanotrophic community than K-deficient soils, while similar community structures of active methanogens were observed in both treatments. These results suggested that the population dynamics of methanogens and methanotrophs could vary along with the changes in plant growth states and soil properties induced by nutrient deficiency.
机译:土壤中的营养状况对于植物的生长和发育至关重要,而植物的生长和发育间接或直接影响到土壤微生物的生态生理功能。土壤产甲烷菌和甲烷营养菌会受到土壤养分利用率和植物生长的影响,进而调节甲烷(CH4)的排放。在这里,我们评估了在长期(20年)试验系统中,一种或两种营养素均受到限制的土壤有效磷(P)和钾(K)的缺乏是否调节了产甲烷菌和甲烷营养菌的活性。结果表明,水稻分till期(淹水)稻田土壤大量释放CH4,成熟期(干燥)稻田CH4排放量最小。与使用NPK肥料改良的土壤相比,没有磷输入的土壤显着降低了甲烷通量,而没有钾输入的土壤则没有。在磷的限制下,甲烷氧化菌转录本拷贝数显着增加,而甲烷氧化原转录物的丰度下降,这表明磷缺乏引起的土壤理化性质的变化,与水稻的生长同时,可能会限制甲烷氧化菌的活性,而甲烷氧化菌可能适应这种土壤环境。相反,在缺钾的土壤中观察到产甲烷菌和甲烷营养菌的转录本较低。根据转录本对群落结构的评估表明,磷缺乏的土壤比甲烷缺乏的土壤诱导的活性甲烷营养群落的迁移更大,而两种处理方法均观察到类似的活性产甲烷菌的群落结构。这些结果表明,甲烷源营养菌和甲烷营养菌的种群动态可能会随着营养缺乏引起的植物生长状态和土壤特性的变化而变化。

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