Pedosphere · 2017
Short-Term Effects of Experimental Warming and Precipitation Manipulation on Soil Microbial Biomass C and N, Community Substrate Utilization Patterns and Community Composition
LI, G., KIM, S., PARK, M., SON, Y.
Export
Short-Term Effects of Experimental Warming and Precipitation…
Abstract
Soil microorganisms are major drivers of soil carbon (C) cycling; however, the response of these microorganisms to climate change remains unclear. In the present study, we investigated how 18 months of multifactor climate treatments (warmed air temperature by 3 ◦C and decreased or increased precipitation manipulation by 30%) affected soil microbial biomass C and nitrogen (N), community substrate utilization patterns, and community composition. Decreased and increased precipitation significantly reduced microbial biomass C by 13.5% and 24.9% and microbial biomass N by 22.9% and 17.6% in unwarmed plots, respectively (P < 0:01). Warming enhanced community substrate utilization by 89.8%, 20.4%, and 141.4% in the natural, decreased, and increased precipitation plots, respectively. Particularly, warming significantly enhanced the utilization of amine and carboxylic acid substrates among all precipitation manipulation plots. Compared with the natural air temperature with natural precipitation treatment, other treatments affected fungal community richness by −0:9% to 33.6% and reduced the relative abundance of the dominant bacterial and fungal groups by 0.5% to 6.8% and 4.3% to 10.7%, respectively. The warming and/or precipitation manipulation treatments significantly altered Zygomycota abundance (P < 0:05). Our results indicate that climate change drivers and their interactions may cause changes in soil microbial biomass C and N, community substrate utilization patterns, and community composition, particularly for the fungal community, and shifts in the microorganism community may further shape the ecosystems function.
Show all
Soil microorganisms are major drivers of soil carbon (C) cycling; however, the response of these microorganisms to climate change remains unclear. In the present study, we investigated how 18 months of multifactor climate treatments (warmed air temperature by 3 ◦C and decreased or increased precipitation manipulation by 30%) affected soil microbial biomass C and nitrogen (N), community substrate utilization patterns, and community composition. Decreased and increased precipitation significantly reduced microbial biomass C by 13.5% and 24.9% and microbial biomass N by 22.9% and 17.6% in unwarmed plots, respectively (P < 0:01). Warming enhanced community substrate utilization by 89.8%, 20.4%, and 141.4% in the natural, decreased, and increased precipitation plots, respectively. Particularly, warming significantly enhanced the utilization of amine and carboxylic acid substrates among all precipitation manipulation plots. Compared with the natural air temperature with natural precipitation treatment, other treatments affected fungal community richness by −0:9% to 33.6% and reduced the relative abundance of the dominant bacterial and fungal groups by 0.5% to 6.8% and 4.3% to 10.7%, respectively. The warming and/or precipitation manipulation treatments significantly altered Zygomycota abundance (P < 0:05). Our results indicate that climate change drivers and their interactions may cause changes in soil microbial biomass C and N, community substrate utilization patterns, and community composition, particularly for the fungal community, and shifts in the microorganism community may further shape the ecosystems function.
Soil microorganisms are major drivers of soil carbon (C) cycling; however, the response of these microorganisms to climate change remains unclear. In the present study, we investigated how 18 months of multifactor climate treatments (warmed air temperature by 3 ◦C and decreased or increased precipitation manipulation by 30%) affected soil microbial biomass C and nitrogen (N), community substrate utilization patterns, and community composition. Decreased and increased precipitation significantly reduced microbial biomass C by 13.5% and 24.9% and microbial biomass N by 22.9% and 17.6% in unwarmed plots, respectively (P < 0:01). Warming enhanced community substrate utilization by 89.8%, 20.4%, and 141.4% in the natural, decreased, and increased precipitation plots, respectively. Particularly, warming significantly enhanced the utilization of amine and carboxylic acid substrates among all precipitation manipulation plots. Compared with the natural air temperature with natural precipitation treatment, other treatments affected fungal community richness by −0:9% to 33.6% and reduced the relative abundance of the dominant bacterial and fungal groups by 0.5% to 6.8% and 4.3% to 10.7%, respectively. The warming and/or precipitation manipulation treatments significantly altered Zygomycota abundance (P < 0:05). Our results indicate that climate change drivers and their interactions may cause changes in soil microbial biomass C and N, community substrate utilization patterns, and community composition, particularly for the fungal community, and shifts in the microorganism community may further shape the ecosystems function.
Similar papers
Effects of soil moisture on the temperature sensitivity of heterotrophic respiration vary seasonally in an old-field climate change experiment
Suseela et al. · 2012 · Global Change Biology
6 shared concepts
13 findings1 site
Differential Responses and Controls of Soil CO2 and N2O Fluxes to Experimental Warming and Nitrogen Fertilization in a Subalpine Coniferous Spruce (Picea asperata Mast.) Plantation Forest
Li et al. · 2019 · Forests
6 shared concepts
25 findings1 site
Field-scale manipulation of soil temperature and precipitation change soil CO2 flux in a temperate agricultural ecosystem
Poll et al. · 2013 · Agriculture, Ecosystems & Environment
5 shared concepts
