Dataset Information

Soil and root associated fungi from a typical steppe in Inner Mongolia

ABSTRACT: terrestrial metagenome Targeted Locus (Loci)

PROVIDER: PRJNA613989 | ENA |

REPOSITORIES: ENA

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			Action	DRS
	SRR11447104.fastq.gz	Fastqsanger.gz
	SRR11447105.fastq.gz	Fastqsanger.gz
	SRR11447106.fastq.gz	Fastqsanger.gz
	SRR11447107.fastq.gz	Fastqsanger.gz
	SRR11447108.fastq.gz	Fastqsanger.gz

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Project description:BackgroundAs one of the important management practices of grassland ecosystems, grazing has fundamental effects on soil properties, vegetation, and soil microbes. Grazing can thus alter soil respiration (Rs) and the soil carbon cycle, yet its impacts and mechanisms remain unclear.MethodsTo explore the response of soil carbon flux and temperature sensitivity to different grazing systems, Rs, soil temperature (ST), and soil moisture (SM) were observed from December 2014 to September 2015 in a typical steppe of Inner Mongolia under three grazing systems: year-long grazing, rest-rotation grazing, and grazing exclusion. In addition, plant aboveground and root biomass, soil microbial biomass and community composition, and soil nutrients were measured during the pilot period.ResultsSoil respiration was significantly different among the three grazing systems. The average Rs was highest under rest-rotation grazing (1.26 μmol·m-2·s-1), followed by grazing exclusion (0.98 μmol·m-2·s-1) and year-long grazing (0.94 μmol·m-2·s-1). Rs was closely associated with ST, SM, potential substrate and root, and soil microbe activity. The effects of grazing among two grazing systems had generality, but were different due to grazing intensity. The root biomass was stimulated by grazing, and the rest-rotation grazing system resulted in the highest Rs. Grazing led to decreases in aboveground and microbial biomass as well as the loss of soil total nitrogen and total phosphorus from the steppe ecosystem, which explained the negative effect of grazing on Rs in the year-long grazing system compared to the grazing exclusion system. The temperature sensitivity of Rs (Q10) was higher in the rest-rotation and year-long grazing systems, likely due to the higher temperature sensitivity of rhizosphere respiration and higher "rhizosphere priming effect" in the promoted root biomass. The structural equation model analysis showed that while grazing inhibited Rs by reducing soil aeration porosity, ground biomass and SM, it increased Q10 but had a lower effect than other factors. A better understanding of the effects of grazing on soil respiration has important practical implications.

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Soil and root associated fungi from a typical steppe in Inner Mongolia

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