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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.
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页数:10
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