Abstract:Soil microbial communities play critical roles in ecosystem functioning and are likely altered by climate warming. However, so far, little is known about effects of warming on microbial functional gene expressions. Here, we applied functional gene array (GeoChip 3.0) to analyze cDNA reversely transcribed from total RNA to assess expressed functional genes in active soil microbial communities after nine years of experimental warming in a tallgrass prairie. Our results showed that warming significantly altered t… Show more
“…In part, these changes in decomposition can be traced to shifts in the ability of the soil microbial community to decompose soil organic carbon (Xue et al. , Feng et al. ).…”
Section: Discussionmentioning
confidence: 99%
“…Rates of litter decomposition in this ecosystem are changing, resulting in reductions of labile organic carbon in plots experiencing warmed conditions (Xu et al 2012b). In part, these changes in decomposition can be traced to shifts in the ability of the soil microbial community to decompose soil organic carbon (Xue et al 2016, Feng et al 2017). However, even as a picture is emerging regarding the impacts of warming on carbon cycling in terrestrial systems, we still do not fully understand the mechanisms driving these changes.…”
Section: Discussionmentioning
confidence: 99%
“…, Luo , Xue et al. ). As warming alters the structure and function of soil communities, there are likely to be shifts in ecosystem processes, including litter decomposition (Treseder , Bradford , Karhu ).…”
Section: Introductionmentioning
confidence: 99%
“…These factors, even as they directly influence decomposition, also feedback and interact with one another. The microbial community plays an important role in determining ecosystem processes such as litter decomposition (Strickland et al 2009a, b, Wickings et al 2012, Allison et al 2013, and climatic warming can alter the composition of microbial communities , Luo 2014, Xue et al 2016. As warming alters the structure and function of soil communities, there are likely to be shifts in ecosystem processes, including litter decomposition (Treseder 2012, Bradford 2013, Karhu 2014.…”
Warming is altering the way soils function in ecosystems both directly by changing microbial physiology and indirectly by causing shifts in microbial community composition. Some of these warming‐driven changes are short term, but others may persist over time. Here, we took advantage of a long‐term (14 yr) warming experiment in a tallgrass prairie to tease apart the influence of short‐ and long‐term warming on litter decomposition. We collected soils originating from warmed and control plots and incubated them with a common litter substrate in a reciprocal design under elevated and ambient growth chamber temperatures. Litter decomposition was 40% higher in soils that were warmed in the field for 14 yr (long‐term warming) relative to soils derived from ambient plots. Short‐term warming in the laboratory had less of an impact on decomposition—decomposition increased by 12% under laboratory warming. Using a two‐pool soil carbon model to explore how different carbon pools may be responding, we found that long‐term warming accelerated the turnover of labile, not recalcitrant, carbon in these prairie soils—a result that is likely due to shifts in soil community activity/composition. Taken together, our results offer experimental evidence that warming‐induced changes in the soil community that occur over 14 yr of warming have long‐lasting effects on carbon turnover.
“…In part, these changes in decomposition can be traced to shifts in the ability of the soil microbial community to decompose soil organic carbon (Xue et al. , Feng et al. ).…”
Section: Discussionmentioning
confidence: 99%
“…Rates of litter decomposition in this ecosystem are changing, resulting in reductions of labile organic carbon in plots experiencing warmed conditions (Xu et al 2012b). In part, these changes in decomposition can be traced to shifts in the ability of the soil microbial community to decompose soil organic carbon (Xue et al 2016, Feng et al 2017). However, even as a picture is emerging regarding the impacts of warming on carbon cycling in terrestrial systems, we still do not fully understand the mechanisms driving these changes.…”
Section: Discussionmentioning
confidence: 99%
“…, Luo , Xue et al. ). As warming alters the structure and function of soil communities, there are likely to be shifts in ecosystem processes, including litter decomposition (Treseder , Bradford , Karhu ).…”
Section: Introductionmentioning
confidence: 99%
“…These factors, even as they directly influence decomposition, also feedback and interact with one another. The microbial community plays an important role in determining ecosystem processes such as litter decomposition (Strickland et al 2009a, b, Wickings et al 2012, Allison et al 2013, and climatic warming can alter the composition of microbial communities , Luo 2014, Xue et al 2016. As warming alters the structure and function of soil communities, there are likely to be shifts in ecosystem processes, including litter decomposition (Treseder 2012, Bradford 2013, Karhu 2014.…”
Warming is altering the way soils function in ecosystems both directly by changing microbial physiology and indirectly by causing shifts in microbial community composition. Some of these warming‐driven changes are short term, but others may persist over time. Here, we took advantage of a long‐term (14 yr) warming experiment in a tallgrass prairie to tease apart the influence of short‐ and long‐term warming on litter decomposition. We collected soils originating from warmed and control plots and incubated them with a common litter substrate in a reciprocal design under elevated and ambient growth chamber temperatures. Litter decomposition was 40% higher in soils that were warmed in the field for 14 yr (long‐term warming) relative to soils derived from ambient plots. Short‐term warming in the laboratory had less of an impact on decomposition—decomposition increased by 12% under laboratory warming. Using a two‐pool soil carbon model to explore how different carbon pools may be responding, we found that long‐term warming accelerated the turnover of labile, not recalcitrant, carbon in these prairie soils—a result that is likely due to shifts in soil community activity/composition. Taken together, our results offer experimental evidence that warming‐induced changes in the soil community that occur over 14 yr of warming have long‐lasting effects on carbon turnover.
“…However, these limitations are the same whatever the DNAbased approach being used (sequencing or microarray). Additionally, profiling the expression of environmental bacterial communities through hybridization of FGA with cDNA is still challenging and was only recently realized using the same FGA (Xue et al, 2016). These authors obtained different and complementary results using RNA-and DNAbased FGA, with the latter being less influenced by shortterm expression dynamics resulting from environmental conditions at the time of sampling.…”
Section: High Functional Diversity and Redundancy Across Bacterial Comentioning
This article explores the functional diversity and redundancy in a bacterial metacommunity constituted of three habitats (sediment, water column and fish gut) in a coastal lagoon under anthropogenic pressure. Comprehensive functional gene arrays covering a wide range of ecological processes and stress resistance genes to estimate the functional potential of bacterial communities were used. Then, diversity partitioning was used to characterize functional diversity and redundancy within (α), between (β) and across (γ) habitats. It was showed that all local communities exhibit a highly diversified potential for the realization of key ecological processes and resistance to various environmental conditions, supporting the growing evidence that macro-organisms microbiomes harbour a high functional potential and are integral components of functional gene dynamics in aquatic bacterial metacommunities. Several levels of functional redundancy at different scales of the bacterial metacommunity were observed (within local communities, within habitats and at the metacommunity level). The results suggested a high potential for the realization of spatial ecological insurance within this ecosystem, that is, the functional compensation among microorganisms for the realization and maintenance of key ecological processes, within and across habitats. Finally, the role of macro-organisms as dispersal vectors of microbes and their potential influence on marine metacommunity dynamics were discussed.
The aboveground biomass (AGB) production of grazed grasslands is mediated by climate, soil nutrients, livestock and other factors. How the biotic and abiotic factors directly or indirectly regulate AGB remains unclear. To fill this gap, from 2014 to 2017, we conducted a rotational grazing experiment to examine the response of AGB to biotic and abiotic factors in Nagqu, a typical alpine meadow community on the Qinghai-Tibetan Plateau. Six yaks were rotationally grazed among three plots from July to September, meanwhile, three plots were set up to exclude from livestock as control; climate, plant biomass, and soil nutrients were investigated during grazing experiment, and then structural equation modeling was used to analyze the regulation of environmental factors on AGB. The results showed that precipitation affected AGB via affecting soil nitrate nitrogen (NO 3-N), compensatory growth rate, and belowground biomass indirectly; temperature can directly and negatively affected AGB. In contrast grazing exclosure, rotational grazing increased both AGB and its temporal stability in alpine meadow community significantly (p < .05). The temporal stability of the AGB was positively related to the asynchrony between high-and lowpalatability herbages (p < .05). In conclusion, rotational grazing should be recommendable for alpine meadow management due to its benefits for community productivity and stability while current stocking rate should be reduced to a reasonable level, especially in a warm and drought year, to sustain plant compensatory growth under grazing.
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