Arbuscular mycorrhiza enhances rhizodeposition and reduces the rhizosphere priming effect on the decomposition of soil organic matter

被引:159
作者
Zhou, Jie [1 ]
Zang, Huadong [2 ,3 ]
Loeppmann, Sebastian [1 ,7 ]
Gube, Matthias [3 ]
Kuzyakov, Yakov [3 ,5 ,6 ]
Pausch, Johanna [4 ]
机构
[1] Georg August Univ Gottingen, Biogeochem Agroecosyst, Dept Crop Sci, Gottingen, Germany
[2] China Agr Univ, Coll Agron & Biotechnol, Beijing, Peoples R China
[3] Georg August Univ Gottingen, Dept Soil Sci Temperate Ecosyst, Dept Agr Soil Sci, Gottingen, Germany
[4] Univ Bayreuth, Agroecol, Bayreuth, Germany
[5] Kazan Fed Univ, Inst Environm Sci, Kazan 420049, Russia
[6] RUDN Univ, Agrotechnol Inst, Moscow 117198, Russia
[7] Christian Albrechts Univ Kiel, Inst Plant Nutr & Soil Sci, Kiel, Germany
关键词
Arbuscular mycorrhizal fungi (AMF); Carbon balance; Continuous labeling; N fertilization; Rhizodeposition; Rhizosphere priming effect (RPE); MICROBIAL BIOMASS; CARBON FLOW; COMPETITIVE INTERACTIONS; ATMOSPHERIC CO2; FUNGI; NITROGEN; PLANT; ROOT; GROWTH; RESPONSES;
D O I
10.1016/j.soilbio.2019.107641
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Arbuscular mycorrhizal fungi (AMF) represent an important route for plant carbon (C) inputs into the soil. Nonetheless, the C input via AMF as well as its impact on soil organic matter (SOM) stabilization and C sequestration remains largely unknown. A mycorrhizal wild type progenitor (MYC) and its mycorrhiza defective mutant (reduced mycorrhizal colonization: rmc) of tomato were continuously labeled with (CO2)-C-13 to trace root C inputs into the soil and quantify rhizosphere priming effects (RPE) as affected by AMF symbiosis and N fertilization. Mycorrhizal abundance and C-13 incorporation into shoots, roots, soil and CO2 were measured at 8, 12 and 16 weeks after transplanting. AMF symbiosis decreased the relative C allocation (% of total assimilated C) to roots, in turn increased the net rhizodeposition. Positive RPE was recorded for both MYC and rmc plants, ranging from 16-71% and 25-101% of the unplanted control, respectively. Although net rhizodeposition was higher for MYC than rmc plants 16 weeks after transplanting, the RPE was comparatively lower. This indicated a higher potential for C sequestration by plants colonized with AMF (MYC) because the reduced nutrient availability restricts the activity of free-living decomposers. Although N fertilization decreased the relative C allocation to roots, rhizosphere and bulk soil, it had no effect on the absolute amount of rhizodeposition to the soil. The RPE and N-cycling enzyme activities decreased by N fertilization 8 and 12 weeks after transplanting, suggesting a lower microbial N demand from SOM mining. The positive relationship between enzyme activities involved in C cycling, microbial biomass C and SOM decomposition underlines the microbial activation hypothesis, which explains the RPE. We therefore concluded that AMF symbiosis and N fertilization increase C sequestration in soil not only by increasing root C inputs, but also by lowering native SOM decomposition and RPE.
引用
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页数:10
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