scholarly journals Soil Microbiota of Dystric Cambisol in the High Tatra Mountains (Slovakia) after Windthrow

2019 ◽  
Vol 11 (23) ◽  
pp. 6851 ◽  
Author(s):  
Alexandra Šimonovičová ◽  
Lucia Kraková ◽  
Elena Piecková ◽  
Matej Planý ◽  
Mária Globanová ◽  
...  
Keyword(s):  
National Park ◽  
High Throughput Sequencing ◽  
Slovak Republic ◽  
Soil Microbial Communities ◽  
Terrestrial Ecosystems ◽  
Tatra Mountains ◽  
Soil Microbial ◽  
Bacterial Microbiota ◽  
Transportation Emissions ◽  
High Tatra Mountains

There has been much more damage to forests in the Slovak Republic in the second half of the 20th century than to other European countries. Forested mountain massifs have become a filter of industrial and transportation emissions from abroad, as well as from domestic origins. There are not only acidic deposits of sulphur and heavy metals present in forest soils, but other additional environmental problems, such as climate change, storms, fires, floods, droughts, are worsening the situation. Therefore, forest terrestrial ecosystems are becoming more vulnerable due to changes in natural and environmental conditions. In the High Tatra Mountains in Slovakia, which are protected as a national park, four internationally monitored localities were established after the windthrow disaster in 2004 and fire in 2005: REF, with intact forest; EXT, with extracted wood mass; NEX, with non-extracted wood mass; and FIR, the burnt locality. Soils from these localities were microbiologically analysed with special attention to fungi. Bacterial microbiota detected by high-throughput sequencing showed the prevalence of the genera Acidothermus, Mycobacterium, and Nocardia, and a very low presence of the genera Acidibacter, Burkholderia-Paraburkholderia, Optitus and the uncultured genus Desulfurellaceae H16 in the soil sample from the burnt locality when compared with the unburned sites. Additionally, soil mycocoenoses showed a low similarity between the locality with an intact forest ecosystem and the localities with extracted (REF–EXT) and non-extracted (REF–NEX) wood mass. There was no similarity with the burnt locality (FIR), where heat-resistant fungi dominated. It was shown that the windthrow disaster and subsequent extraction or non-extraction of wood mass did not affect the soil microbial communities or their development. On the other hand, the influence of fire was significant.

scholarly journals Novel Approach to Study the Diversity of Soil Microbial Communities in Qatar

2020 ◽  
Author(s):  
Jane Oja ◽  
Sakeenah Adenan ◽  
Abdel-Fattah Talaat ◽  
Juha Alatalo
Keyword(s):  
Microbial Communities ◽  
High Throughput ◽  
Mycorrhizal Fungi ◽  
High Throughput Sequencing ◽  
Soil Microbial Communities ◽  
Arbuscular Mycorrhizal ◽  
Soil Microbial ◽  
Fungal Abundance ◽  
Novel Approach ◽  
Soil Climate

A broad diversity of microorganisms can be found in soil, where they are essential for nutrient cycling and energy transfer. Recent high-throughput sequencing methods have greatly advanced our knowledge about how soil, climate and vegetation variables structure the composition of microbial communities in many world regions. However, we are lacking information from several regions in the world, e.g. Middle-East. We have collected soil from 19 different habitat types for studying the diversity and composition of soil microbial communities (both fungi and bacteria) in Qatar and determining which edaphic parameters exert the strongest influences on these communities. Preliminary results indicate that in overall bacteria are more abundant in soil than fungi and few sites have notably higher abundance of these microbes. In addition, we have detected some soil patameters, which tend to have reduced the overall fungal abundance and enhanced the presence of arbuscular mycorrhizal fungi and N-fixing bacteria. More detailed information on the diversity and composition of soil microbial communities is expected from the high-throughput sequenced data.

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 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.

Soil microbial communities influencing organic phosphorus mineralization in a coastal dune chronosequence in New Zealand

2021 ◽  
Vol 97 (4) ◽  
Author(s):  
Jonathan R Gaiero ◽  
Micaela Tosi ◽  
Elizabeth Bent ◽  
Gustavo Boitt ◽  
Kamini Khosla ◽  
...  
Keyword(s):  
New Zealand ◽  
Acid Phosphatase ◽  
Microbial Communities ◽  
High Throughput Sequencing ◽  
Organic Phosphorus ◽  
Mineral Soil ◽  
Soil Microbial Communities ◽  
Organic P ◽  
Fungal Community Composition ◽  
Soil Microbial

ABSTRACT The Haast chronosequence in New Zealand is an ∼6500-year dune formation series, characterized by rapid podzol development, phosphorus (P) depletion and a decline in aboveground biomass. We examined bacterial and fungal community composition within mineral soil fractions using amplicon-based high-throughput sequencing (Illumina MiSeq). We targeted bacterial non-specific acid (class A, phoN/phoC) and alkaline (phoD) phosphomonoesterase genes and quantified specific genes and transcripts using real-time PCR. Soil bacterial diversity was greatest after 4000 years of ecosystem development and associated with an increased richness of phylotypes and a significant decline in previously dominant taxa (Firmicutes and Proteobacteria). Soil fungal communities transitioned from predominantly Basidiomycota to Ascomycota along the chronosequence and were most diverse in 290- to 392-year-old soils, coinciding with maximum tree basal area and organic P accumulation. The Bacteria:Fungi ratio decreased amid a competitive and interconnected soil community as determined by network analysis. Overall, soil microbial communities were associated with soil changes and declining P throughout pedogenesis and ecosystem succession. We identified an increased dependence on organic P mineralization, as found by the profiled acid phosphatase genes, soil acid phosphatase activity and function inference from predicted metagenomes (PICRUSt2).

scholarly journals An invasive plant rapidly increased the similarity of soil fungal pathogen communities

2020 ◽  
Author(s):  
Meiling Wang ◽  
Xuefei Tang ◽  
Xiaoqiu Sun ◽  
Bingbing Jia ◽  
Hao Xu ◽  
...  
Keyword(s):  
Microbial Communities ◽  
Invasive Plants ◽  
Fungal Pathogen ◽  
High Throughput Sequencing ◽  
Invasive Plant ◽  
Soil Microbial Communities ◽  
Plant Invasions ◽  
Alternanthera Philoxeroides ◽  
Native Plant ◽  
Soil Microbial

Abstract Background and Aims Plant invasions can change soil microbial communities and affect subsequent invasions directly or indirectly via foliar herbivory. It has been proposed that invaders promote uniform biotic communities that displace diverse, spatially variable communities (the biotic homogenization hypothesis), but this has not been experimentally tested for soil microbial communities, so the underlying mechanisms and dynamics are unclear. Here, we compared density-dependent impacts of the invasive plant Alternanthera philoxeroides and its native congener A. sessilis on soil fungal communities, and their feedback effects on plants and a foliar beetle. Methods We conducted a plant–soil feedback (PSF) experiment and a laboratory bioassay to examine PSFs associated with the native and invasive plants and a beetle feeding on them. We also characterized the soil fungal community using high-throughput sequencing. Key Results We found locally differentiated soil fungal pathogen assemblages associated with high densities of the native plant A. sessilis but little variation in those associated with the invasive congener A. philoxeroides, regardless of plant density. In contrast, arbuscular mycorrhizal fungal assemblages associated with high densities of the invasive plant were more variable. Soil biota decreased plant shoot mass but their effect was weak for the invasive plant growing in native plant-conditioned soils. PSFs increased the larval biomass of a beetle reared on leaves of the native plant only. Moreover, PSFs on plant shoot and root mass and beetle mass were predicted by different pathogen taxa in a plant species-specific manner. Conclusion Our results suggest that plant invasions can rapidly increase the similarity of soil pathogen assemblages even at low plant densities, leading to taxonomically and functionally homogeneous soil communities that may limit negative soil effects on invasive plants.

scholarly journals Determining Soil Microbial Communities and Their Influence on Ganoderma Disease Incidences in Oil Palm (Elaeis guineensis) via High-Throughput Sequencing

Biology ◽  
2020 ◽  
Vol 9 (12) ◽  
pp. 424
Author(s):  
Yit Kheng Goh ◽  
Muhammad Zarul Hanifah Md Zoqratt ◽  
You Keng Goh ◽  
Qasim Ayub ◽  
Adeline Su Yien Ting
Keyword(s):  
Oil Palm ◽  
High Throughput Sequencing ◽  
Elaeis Guineensis ◽  
Disease Incidence ◽  
Soil Microbial Communities ◽  
Disease Suppression ◽  
Soil Microbiome ◽  
Physical Parameters ◽  
Soil Microbial ◽  
Coastal Soils

Basal stem rot (BSR), caused by Ganoderma boninense, is the most devastating oil palm disease in South East Asia, costing US$500 million annually. Various soil physicochemical parameters have been associated with an increase in BSR incidences. However, very little attention has been directed to understanding the relationship between soil microbiome and BSR incidence in oil palm fields. The prokaryotic and eukaryotic microbial diversities of two coastal soils, Blenheim soil (Typic Quartzipsamment—calcareous shell deposits, light texture) with low disease incidence (1.9%) and Bernam soil (Typic Endoaquept—non-acid sulfate) with high disease incidence (33.1%), were determined using the 16S (V3–V4 region) and 18S (V9 region) rRNA amplicon sequencing. Soil physicochemical properties (pH, electrical conductivity, soil organic matter, nitrogen, phosphorus, cation exchange capacity, exchangeable cations, micronutrients, and soil physical parameters) were also analyzed for the two coastal soils. Results revealed that Blenheim soil comprises higher prokaryotic and eukaryotic diversities, accompanied by higher pH and calcium content. Blenheim soil was observed to have a higher relative abundance of bacterial taxa associated with disease suppression such as Calditrichaeota, Zixibacteria, GAL15, Omnitrophicaeota, Rokubacteria, AKYG587 (Planctomycetes), JdFR-76 (Calditrichaeota), and Rubrobacter (Actinobacteria). In contrast, Bernam soil had a higher proportion of other bacterial taxa, Chloroflexi and Acidothermus (Actinobacteria). Cercomonas (Cercozoa) and Calcarisporiella (Ascomycota) were eukaryotes that are abundant in Blenheim soil, while Uronema (Ciliophora) and mammals were present in higher abundance in Bernam soil. Some of the bacterial taxa have been reported previously in disease-suppressive and -conducive soils as potential disease-suppressive or disease-inducible bacteria. Furthermore, Cercomonas was reported previously as potential bacterivorous flagellates involved in the selection of highly toxic biocontrol bacteria, which might contribute to disease suppression indirectly. The results from this study may provide valuable information related to soil microbial community structures and their association with soil characteristics and soil susceptibility to Ganoderma.

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 Soil Microbial Functional Diversity Responses to Different Vegetation Types in the Heilongjiang Zhongyangzhan Black-billed Capercaillie Nature Reserve

2021 ◽  
Author(s):  
Xiaohong Weng ◽  
Jiayi Li ◽  
xin sui ◽  
Mengsha Li ◽  
Weiping Yin ◽  
...  
Keyword(s):  
Functional Diversity ◽  
Nature Reserve ◽  
Forest Type ◽  
Diversity Index ◽  
Soil Microbial Communities ◽  
Principal Component ◽  
Terrestrial Ecosystems ◽  
Vegetation Types ◽  
Microbial Functional Diversity ◽  
Soil Microbial

Abstract Purpose: The soil microbial community is an important bioactive component of terrestrial ecosystems. Its structural and functional diversity directly affects carbon and nitrogen processes. This study aimed to investigate the variations in the functional diversity of soil microbial communities in forests with different types of vegetation. Methods: We selected three typical vegetation types, larch (LG), black birch (BD), and larch and black birch mixed (LGBD) forests, located in the Heilongjiang Zhongyangzhan Black-billed Capercaillie Nature Reserve. The Biolog-Eco microplate technology was selected to perform these analyses. Result: Our results showed clear differences between microorganisms in the three typical forests. The average well-colour development (AWCD) change rate gradually increased with incubation time. The BD type had the highest AWCD value, followed by LGBD; the LG forest type had the lowest value. The difference in the soil microbial alpha diversity index between BD and LG was significant. A principal component analysis showed that PC1 and PC2 respectively explained 62.77% and 13.3% of the variance observed. The differences in the soil microbial carbon-source utilization patterns under different vegetation types were mainly caused by esters and carbohydrates. Redundancy analysis showed that soil microbial functional diversity was strongly affected by soil physicochemistrical properties (e.g. organic carbon, total nitrogen, and pH). Conclusion: These results provide a reference for further exploring the relationship between forest communities and soil microbes during the process of forest succession.

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