scholarly journals Soil Bacteria and Fungi Respond Differently to Organisms Covering on Leshan Giant Buddha Body

2021 ◽  
Vol 13 (7) ◽  
pp. 3897
Author(s):  
Xuli Chen ◽  
Manfei Wang ◽  
Fujia Wu ◽  
Bo Sun ◽  
Tianyu Yang ◽  
...  
Keyword(s):  
Vascular Plants ◽  
Soil Microbial Communities ◽  
Chemical Properties ◽  
Terrestrial Ecosystems ◽  
Diversity Indices ◽  
Scientific Basis ◽  
Soil Microbial ◽  
Α Diversity ◽  
Soil Bacteria And Fungi ◽  
Bacteria And Fungi

Soil microbial communities play a key role in the functioning of terrestrial ecosystems, in particular through their interaction with above-ground plants and weathering of rocks. In this study, the chemical properties and microbial diversity of soils covered by different organisms on Leshan Giant Buddha body were analyzed. The results showed that the concentration of soil total organic carbon (TOC), total nitrogen (TN) and total phosphorus (TP) increased significantly with the change of above-ground organisms from lichens to bryophytes and vascular plants. TOC, TN, TP, C:N, and C:P were significantly correlated with the composition of microbial community. Bacterial and fungal diversity responded differently to the change of organisms, and the diversity of bacterial communities changed significantly among different sites. The settlement of Embryogenic plants increased the α-diversity indices including Sobs, Shannon, Ace and Chao indices, which were highest in sites covered with Ferns. The relative abundances of Chloroflexi, Acidobacteria, Nitrospirae and Planctomycetes increased with the order of Bryophyte, Fern, Grass and Shrub, and Cyanobacteria was opposite, with the highest in samples covered with lichens. These results improve understanding of plant–fungi–bacteria interactions during the early stages of soil development, and provide a scientific basis for protection of Leshan Giant Buddha.

scholarly journals Increasing aridity reduces soil microbial diversity and abundance in global drylands

2015 ◽  
Vol 112 (51) ◽  
pp. 15684-15689 ◽  
Author(s):  
Fernando T. Maestre ◽  
Manuel Delgado-Baquerizo ◽  
Thomas C. Jeffries ◽  
David J. Eldridge ◽  
Victoria Ochoa ◽  
...  
Keyword(s):  
Climate Change ◽  
Soil Bacteria ◽  
Soil Microbial Communities ◽  
Terrestrial Ecosystems ◽  
Soil Microbial Diversity ◽  
Change Models ◽  
Soil Microbial ◽  
Soil Bacteria And Fungi ◽  
Abundance And Diversity ◽  
Bacteria And Fungi

Soil bacteria and fungi play key roles in the functioning of terrestrial ecosystems, yet our understanding of their responses to climate change lags significantly behind that of other organisms. This gap in our understanding is particularly true for drylands, which occupy ∼41% of Earth´s surface, because no global, systematic assessments of the joint diversity of soil bacteria and fungi have been conducted in these environments to date. Here we present results from a study conducted across 80 dryland sites from all continents, except Antarctica, to assess how changes in aridity affect the composition, abundance, and diversity of soil bacteria and fungi. The diversity and abundance of soil bacteria and fungi was reduced as aridity increased. These results were largely driven by the negative impacts of aridity on soil organic carbon content, which positively affected the abundance and diversity of both bacteria and fungi. Aridity promoted shifts in the composition of soil bacteria, with increases in the relative abundance of Chloroflexi and α-Proteobacteria and decreases in Acidobacteria and Verrucomicrobia. Contrary to what has been reported by previous continental and global-scale studies, soil pH was not a major driver of bacterial diversity, and fungal communities were dominated by Ascomycota. Our results fill a critical gap in our understanding of soil microbial communities in terrestrial ecosystems. They suggest that changes in aridity, such as those predicted by climate-change models, may reduce microbial abundance and diversity, a response that will likely impact the provision of key ecosystem services by global drylands.

scholarly journals Microbiome of vineyard soils is shaped by geography and management

Microbiome ◽  
2019 ◽  
Vol 7 (1) ◽  
Author(s):  
Emanuela Coller ◽  
Alessandro Cestaro ◽  
Roberto Zanzotti ◽  
Daniela Bertoldi ◽  
Massimo Pindo ◽  
...  
Keyword(s):  
Soil Microbial Communities ◽  
Chemical Properties ◽  
Fungal Communities ◽  
Rrna Gene ◽  
Its Sequencing ◽  
Soil Microbiota ◽  
Soil Microbial ◽  
Specific Effects ◽  
Bacteria And Fungi ◽  
Italian Province

Abstract Background Despite their importance as a reservoir of biodiversity, the factors shaping soil microbial communities and the extent by which these are impacted by cultivation are still poorly understood. Using 16S rRNA gene and ITS sequencing, we characterized the soil microbiota of vineyards and of neighboring permanent grassland soils in the Italian province of Trentino, and correlated their structure and composition to location, chemical properties of the soil, and land management. Results Bacterial communities had a core of conserved taxa accounting for more than 60% of the reads of each sample, that was influenced both by geography and cultivation. The core fungal microbiota was much smaller and dominated by geography alone. Cultivation altered the structure and composition of the soil microbiota both for bacteria and fungi, with site-specific effects on their diversity. The diversity of bacterial and fungal communities was generally inversely correlated across locations. We identified several taxa that were impacted by the chemical properties and texture of the soil. Conclusions Our results highlight the different responses of bacterial and fungal communities to environmental factors and highlight the need to characterize both components of the soil microbiota to fully understand the factors that drive their variability.

scholarly journals Distinct Biogeographic Patterns for Archaea, Bacteria, and Fungi along the Vegetation Gradient at the Continental Scale in Eastern China

mSystems ◽  
2017 ◽  
Vol 2 (1) ◽  
Author(s):  
Bin Ma ◽  
Zhongmin Dai ◽  
Haizhen Wang ◽  
Melissa Dsouza ◽  
Xingmei Liu ◽  
...  
Keyword(s):  
Eastern China ◽  
Soil Microbial Communities ◽  
Natural Forest ◽  
Community Diversity ◽  
Biogeographic Patterns ◽  
Soil Microbial ◽  
Continental Scale ◽  
Forest Sites ◽  
Vegetation Gradient ◽  
Bacteria And Fungi

ABSTRACT Understanding biogeographic patterns is a precursor to improving our knowledge of the function of microbiomes and to predicting ecosystem responses to environmental change. Using natural forest soil samples from 110 locations, this study is one of the largest attempts to comprehensively understand the different patterns of soil archaeal, bacterial, and fungal biogeography at the continental scale in eastern China. These patterns in natural forest sites could ascertain reliable soil microbial biogeographic patterns by eliminating anthropogenic influences. This information provides guidelines for monitoring the belowground ecosystem’s decline and restoration. Meanwhile, the deviations in the soil microbial communities from corresponding natural forest states indicate the extent of degradation of the soil ecosystem. Moreover, given the association between vegetation type and the microbial community, this information could be used to predict the long-term response of the underground ecosystem to the vegetation distribution caused by global climate change. The natural forest ecosystem in Eastern China, from tropical forest to boreal forest, has declined due to cropland development during the last 300 years, yet little is known about the historical biogeographic patterns and driving processes for the major domains of microorganisms along this continental-scale natural vegetation gradient. We predicted the biogeographic patterns of soil archaeal, bacterial, and fungal communities across 110 natural forest sites along a transect across four vegetation zones in Eastern China. The distance decay relationships demonstrated the distinct biogeographic patterns of archaeal, bacterial, and fungal communities. While historical processes mainly influenced bacterial community variations, spatially autocorrelated environmental variables mainly influenced the fungal community. Archaea did not display a distance decay pattern along the vegetation gradient. Bacterial community diversity and structure were correlated with the ratio of acid oxalate-soluble Fe to free Fe oxides (Feo/Fed ratio). Fungal community diversity and structure were influenced by dissolved organic carbon (DOC) and free aluminum (Ald), respectively. The role of these environmental variables was confirmed by the correlations between dominant operational taxonomic units (OTUs) and edaphic variables. However, most of the dominant OTUs were not correlated with the major driving variables for the entire communities. These results demonstrate that soil archaea, bacteria, and fungi have different biogeographic patterns and driving processes along this continental-scale natural vegetation gradient, implying different community assembly mechanisms and ecological functions for archaea, bacteria, and fungi in soil ecosystems. IMPORTANCE Understanding biogeographic patterns is a precursor to improving our knowledge of the function of microbiomes and to predicting ecosystem responses to environmental change. Using natural forest soil samples from 110 locations, this study is one of the largest attempts to comprehensively understand the different patterns of soil archaeal, bacterial, and fungal biogeography at the continental scale in eastern China. These patterns in natural forest sites could ascertain reliable soil microbial biogeographic patterns by eliminating anthropogenic influences. This information provides guidelines for monitoring the belowground ecosystem’s decline and restoration. Meanwhile, the deviations in the soil microbial communities from corresponding natural forest states indicate the extent of degradation of the soil ecosystem. Moreover, given the association between vegetation type and the microbial community, this information could be used to predict the long-term response of the underground ecosystem to the vegetation distribution caused by global climate change. Author Video: An author video summary of this article is available.

scholarly journals Ozone affects plant, insect, and soil microbial communities: A threat to terrestrial ecosystems and biodiversity

2020 ◽  
Vol 6 (33) ◽  
pp. eabc1176 ◽  
Author(s):  
Evgenios Agathokleous ◽  
Zhaozhong Feng ◽  
Elina Oksanen ◽  
Pierre Sicard ◽  
Qi Wang ◽  
...  
Keyword(s):  
Plant Competition ◽  
Root Exudation ◽  
Soil Microbial Communities ◽  
Alpha Diversity ◽  
Terrestrial Ecosystems ◽  
Insect Communities ◽  
Soil Microbial ◽  
Plant Soil ◽  
Equatorial Africa ◽  
Insect Interactions

Elevated tropospheric ozone concentrations induce adverse effects in plants. We reviewed how ozone affects (i) the composition and diversity of plant communities by affecting key physiological traits; (ii) foliar chemistry and the emission of volatiles, thereby affecting plant-plant competition, plant-insect interactions, and the composition of insect communities; and (iii) plant-soil-microbe interactions and the composition of soil communities by disrupting plant litterfall and altering root exudation, soil enzymatic activities, decomposition, and nutrient cycling. The community composition of soil microbes is consequently changed, and alpha diversity is often reduced. The effects depend on the environment and vary across space and time. We suggest that Atlantic islands in the Northern Hemisphere, the Mediterranean Basin, equatorial Africa, Ethiopia, the Indian coastline, the Himalayan region, southern Asia, and Japan have high endemic richness at high ozone risk by 2100.

scholarly journals The Influence of Climate Warming and Humidity on Plant Diversity and Soil Bacteria and Fungi Diversity in Desert Grassland

Plants ◽  
2021 ◽  
Vol 10 (12) ◽  
pp. 2580
Author(s):  
Yi Zhang ◽  
Yingzhong Xie ◽  
Hongbin Ma ◽  
Juan Zhang ◽  
Le Jing ◽  
...  
Keyword(s):  
Plant Diversity ◽  
Soil Bacteria ◽  
Interactive Effects ◽  
Desert Grassland ◽  
Plant Soil ◽  
Β Diversity ◽  
Temperature And Precipitation ◽  
Α Diversity ◽  
Soil Bacteria And Fungi ◽  
Bacteria And Fungi

Our study, which was conducted in the desert grassland of Ningxia in China (E 107.285, N 37.763), involved an experiment with five levels of annual precipitation 33% (R33), 66% (R66), 100% (CK), 133% (R133), 166% (R166) and two temperature levels (inside Open-Top Chamber (OTC) and outside OTC). Our objective was to determine how plant, soil bacteria, and fungi diversity respond to climate change. Our study suggested that plant α-diversity in CK and TCK were significantly higher than that of other treatments. Increased precipitation promoted root biomass (RB) growth more than aboveground living biomass (ALB). R166 promoted the biomass of Agropyron mongolicum the most. In the fungi communities, temperature and precipitation interaction promoted α-diversity. In the fungi communities, the combination of increased temperature and natural precipitation (TCK) promoted β-diversity the most, whose distance was determined to be 25,124 according to PCA. In the bacteria communities, β-diversity in CK was significantly higher than in other treatments, and the distance was determined to be 3010 according to PCA. Soil bacteria and fungi α- and β-diversity, and ALB promoted plant diversity the most. The interactive effects of temperature and precipitation on C, N, and P contents of plants were larger than their independent effects.

scholarly journals Consistent effects of vegetation loss on abundant and rare soil microbial phylotypes across nitrogen-enrichment levels

2019 ◽  
Author(s):  
Dima Chen ◽  
Ying Wu ◽  
Muhammad Saleem ◽  
Bing Wang ◽  
Shuijin Hu ◽  
...  
Keyword(s):  
Soil Bacteria ◽  
Alpha Diversity ◽  
N Deposition ◽  
Bacterial Phylotypes ◽  
Soil Microbial ◽  
N Enrichment ◽  
Soil Bacteria And Fungi ◽  
Bacteria And Fungi ◽  
Vegetation Loss ◽  
First Time

Abstract Soil harbors highly diverse abundant and rare microbial phylotypes that drive multiple soil functions. Given increasing intensity and frequency of vegetation loss and anthropogenic reactive nitrogen (N) inputs to the soil in the future, we lack a mechanistic understanding of how vegetation loss may influence abundant and rare microbial phylotypes at various N-enrichment levels. In the current study, we assessed the effects of vegetation loss on abundant and rare phylotypes of soil bacteria and fungi across three N-enrichment levels in a semi-arid grassland ecosystem. After six years of experimentation in with and without vegetation plots, the vegetation loss increased the total relative abundance of abundant soil bacterial phylotypes but not that of abundant fungal phylotypes at across N-enrichment levels. It is very likely because the number of abundant bacterial phylotypes with positive than negative responses to vegetation loss was higher; however, the number of abundant fungal phylotypes with positive than negative responses to vegetation loss was similar during this period. Moreover, the vegetation loss did not alter the alpha-diversity of abundant or rare bacterial phylotypes, or, of abundant fungal phylotypes; however, it reduced the alpha-diversity of rare fungal phylotypes at across N-enrichment levels. The vegetation loss, however, altered the beta-diversity of abundant and rare bacterial and fungal phylotypes across N-enrichment levels. We found that, against expectations, the effects of vegetation loss on the diversity of abundant and rare phylotypes of both bacteria and fungi were relatively consistent across N-enrichment levels. Our findings provide, for the first time, the phylotype-based data on how vegetation loss affects abundant and rare phylotypes of soil bacteria and fungi across N-enrichment levels. The results also indicate that the effects of vegetation loss on belowground functions may be relatively insensitive to the differences in the N-deposition rates.

The invasive potential of a hybrid species: insights from soil chemical properties and soil microbial communities

2019 ◽  
Vol 13 (1) ◽  
pp. 20-26
Author(s):  
Feng Sun ◽  
Yuyi Ou ◽  
Qiaojing Ou ◽  
Lingda Zeng ◽  
Hanxia Yu ◽  
...  
Keyword(s):  
Microbial Communities ◽  
Photosynthetic Rate ◽  
Soil Microbial Communities ◽  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Natural Hybridization ◽  
Total Biomass ◽  
Invasive Potential ◽  
Soil Microbial ◽  
Significant Difference

Abstract Aims Natural hybridization between invasive and native species, as a form of adaptive evolution, threatens biodiversity worldwide. However, the potential invasive mechanisms of hybrids remain essentially unexplored, especially insights from soil chemical properties and soil microbial communities. Methods In a field experiment, soil microbial community, potassium-solubilizing bacteria, phosphorus-solubilizing bacteria, enzyme activities, and light-saturated photosynthetic rate were measured in invasive Sphagneticola trilobata and its hybrid with native Sphagneticola calendulacea in 2 years. Important Findings In general, soil dissolved organic carbon and the biomass of phosphorus-solubilizing bacteria were significantly higher under the hybrid treatment than S. trilobata and S. calendulacea. However, there were no significant differences in acid phosphatase, total PLFAs, bacterial PLFAs, fungi PLFAs, cellulase, and urase in these treatments. The hybrids had significantly higher light-saturated photosynthetic rate, photosynthetic nitrogen-, phosphorus-, potassium- use efficiencies than the invasive S. trilobata, but no significant difference with S. calendulacea. The total biomass and root biomass of hybrids were higher than S. calendulacea. Our results indicate that the hybrids species have a higher invasive potential than S. calendulacea, which may aggravate the local extinction of S. calendulacea in the future.

scholarly journals Microbial responses to chitin and chitosan in oxic and anoxic agricultural soil slurries

2014 ◽  
Vol 11 (12) ◽  
pp. 3339-3352 ◽  
Author(s):  
A. S. Wieczorek ◽  
S. A. Hetz ◽  
S. Kolb
Keyword(s):  
Carbon Dioxide ◽  
Agricultural Soil ◽  
Soil Microbial Communities ◽  
Terrestrial Ecosystems ◽  
Ecological Niches ◽  
Acid Fermentation ◽  
Fermentation Products ◽  
Anoxic Conditions ◽  
Chitin Degradation ◽  
Soil Microbial

Abstract. Microbial degradation of chitin in soil substantially contributes to carbon cycling in terrestrial ecosystems. Chitin is globally the second most abundant biopolymer after cellulose and can be deacetylated to chitosan or can be hydrolyzed to N,N′-diacetylchitobiose and oligomers of N-acetylglucosamine by aerobic and anaerobic microorganisms. Which pathway of chitin hydrolysis is preferred by soil microbial communities is unknown. Supplementation of chitin stimulated microbial activity under oxic and anoxic conditions in agricultural soil slurries, whereas chitosan had no effect. Thus, the soil microbial community likely was more adapted to chitin as a substrate. In addition, this finding suggested that direct hydrolysis of chitin was preferred to the pathway that starts with deacetylation. Chitin was apparently degraded by aerobic respiration, ammonification, and nitrification to carbon dioxide and nitrate under oxic conditions. When oxygen was absent, fermentation products (acetate, butyrate, propionate, hydrogen, and carbon dioxide) and ammonia were detected, suggesting that butyric and propionic acid fermentation, along with ammonification, were likely responsible for anaerobic chitin degradation. In total, 42 different chiA genotypes were detected of which twenty were novel at an amino acid sequence dissimilarity of less than 50%. Various chiA genotypes responded to chitin supplementation and affiliated with a novel deep-branching bacterial chiA genotype (anoxic conditions), genotypes of Beta- and Gammaproteobacteria (oxic and anoxic conditions), and Planctomycetes (oxic conditions). Thus, this study provides evidence that detected chitinolytic bacteria were catabolically diverse and occupied different ecological niches with regard to oxygen availability enabling chitin degradation under various redox conditions on community level.

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