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Rank abundance plots of each model for the noncontaminated soil. Species are ranked in order from most abundant to least abundant.

Rank abundance plots of each model for the noncontaminated soil. Species are ranked in order from most abundant to least abundant.

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The complexity of soil bacterial communities has thus far confounded effective measurement. However, with improved analytical methods, we show that the abundance distribution and total diversity can be deciphered. Reanalysis of reassociation kinetics for bacterial community DNA from pristine and metal-polluted soils showed that a power law best des...

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... Soil microorganisms were highly important components and the most active constituents in the terrestrial soil system and played an indispensable role in soil formation and development, organic matter transformation, ecosystem balance, soil environmental purification and bioremediation (Gans et al., 2005). The results from the current study showed that although all sampling sites were located in the Hetao irrigation area, and the vegetation was S. glauca in all cases, the microbial characteristics exhibited extremely significant differences. ...
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Exploring the bacterial community in the S. glauca rhizosphere was of great value for understanding how this species adapted to the saline-alkali environment and for the rational development and use of saline-alkali soils. In this study, high-throughput sequencing technology was used to investigate the diversity characteristics and distribution patterns of soil bacterial communities in the rhizosphere of S.glauca-dominated communities in the Hetao Irrigation Distract, Inner Mongolia, China. The relationships among bacterial characteristics, soil physicochemical properties and vegetation in four sampling sites were analyzed. The soil bacterial communities in the rhizosphere of S. glauca-dominated communities were mainly composed of 16 phyla (i.e., Proteobacteria, Actinobacteria, Bacteroidetes, Gemmatimonadetes, Chloroflexi, Acidobacteria, Firmicutes, Planctomycetes, Deinococcus-Thermus, Verrucomicrobia, Saccharibacteria, Cyanobacteria, Nitrospirae, JL-ETNP-Z39, Parcubacteria and Chlorobi), and these populations accounted for more than 99% of the total bacterial community. At the genus level, the main bacterial communities comprised Halomonas, Nitriliruptor, Euzebya and Pelagibius, which accounted for 15.70% of the total bacterial community. An alpha diversity analysis indicated that the richness and diversity of rhizosphere soil bacteria differed significantly among the sampling sites, and the bacterial richness and diversity indices of severe saline-alkali land were higher than those of light and moderate saline-alkali land. The principal component analysis (PCA) and linear discriminant analysis effect size (LEfSe) showed significant differences in the species composition of the rhizosphere soil bacterial community among different sampling sites. A correlation analysis showed that the number of bacterial species exhibited the highest correlation with the soil water content (SWC). The richness and evenness indices were significantly correlated with the SWC and SO42–, K⁺ and Mg²⁺ concentrations. The electrical conductivity (EC), soluble ions (Na⁺, CO32– + HCO3–, K⁺, Ca²⁺, Mg²⁺, and SO4²⁺), SWC and vegetation coverage (VC) were the main drivers affecting the changes in its community structure. The bacterial community in the rhizosphere of S. glauca enhanced the adaptability of S. glauca to saline-alkali environment by participating in the cycling process of nutrient elements, the decomposition of organic matter and the production of plant growth regulating substances. These results provided a theoretical reference for further study on the relationship among rhizosphere soil microorganisms and salt tolerance in halophytes.
... Deceans et al. (2006) report that 360,000 animal species dwell in soil. Also, nearly 1010 bacterial cells are present in 10 g of soil (Gans et al. 2005). These organisms are vital to sustaining both soil and a wider ecosystem and are important for the production of food and fiber in addition to regulating other services like controlling the emission of greenhouse gases, purifying water, and nutrient cycling. ...
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Soil erosion is a major concern that needs to be addressed for the health of an ecosystem. It is a primary constraint to agriculture, affecting the yield, water quality at the source, and soil health. It is often a result of anthropogenic activities like deforestation, unhealthy irrigation and agricultural practices and overgrazing, etc., and leads to degradation of the environment. Soil erosion is a threat of significant magnitude that needs to be addressed in regions of large agricultural productivity like Asia underlining the need for mitigation measures. Structural interventions like check dams, silt traps, etc. are extensively used to deter soil erosion. However, these interventions are not integral to the natural environment and adversely affect the ecosystem. This study reviews the various biogeotechnological methods to control soil erosion and conserve the soil. Biological interventions like vegetative cover on slopes have long been practiced to control soil erosion in select zones. Biogenic additives to soil that improve the resistance of soil against soil erosion need detailed investigation. In line with this observation, this study will review biogenic stabilizers like vegetative cover, biopolymers, and biochar and their efficacy in controlling soil erosion. The effect of this biogenic stabilizer against soil erosion caused by wind and water will be discussed in detail. These methods do not only help in controlling soil erosion but also improve soil health and promote vegetative growth. These soil additives offer environment-friendly, carbon–neutral/carbon-negative, and sustainable alternatives to structural interventions that are used to control soil erosion. They will improve soil health which in turn will lead to increased agricultural productivity and alleviate hunger and will help in conserving soil and end desertification (SDG 2 and 15).
... Soil microorganisms, particularly bacteria, are highly plentiful and varied, exerting significant influence in agricultural environments by aiding in nutrient cycling, upholding soil integrity, and enhancing plant development (Gans et al., 2005). Specific bacteria capable of promoting plant growth offer plants mechanisms to resist stress. ...
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... The rank abundance plots offer a unified perception of the underlying ecological rules governing microbial diversity and abundance in a microbial ecology community (McGill et al., 2007;Prosser et al., 2007). However, because of the extensive complexity of these bacterial communities, accompanied by the inability to culture the vast majority of bacteria, the work necessary to obtain rank abundance plots is challenging (Curtis et al., 2006;Gans et al., 2005). Although 16S rRNA genes are widely used to characterize the structure and composition of microbial communities, having multiple copies often results in over-estimation of certain bacterial taxa, which lowers the ability to effectively enumerate bacterial community using bacterial species abundance distributions (Doroghazi and Buckley, 2008;Schloss and Handelsman, 2006;Sloan et al., 2007). ...
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... Selective inoculation of root microbiomes with growth-promoting microbes have also been shown to improve crop production [14][15][16]. Some of the more common microbial inoculation methods to confer stress tolerance include inoculation of the plant or seed via immersion [17], or mixing inoculum directly into the soil [18]. ...
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... Quantity of microorganisms was determined as colony-forming units (CFU) per 1 g of dry soil (Carter, Gregorich, 2007). The studies conducted using this method allow observation of the most active organotrophs, nitrifiers, diazotrophs, the populations of soil fungi and yeast-like fungi, and changes of their abundance in the soil (Gans et al., 2005;Furtak, Gajda, 2018). ...
... Considering the main microbial groups inhabiting soil, bacteria have been the focal point of most studies, as they dominate soils with about 10 3 -10 6 per gram of soil [11]. However, fungal and archaeal groups are also important, with most studies showing their ubiquity in the soil [12]. ...
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... Tanah supresif layu fusarium dicirikan dengan tanah yang didominasi sejumlah mikrob fungsional melalui mekanisme tertentu yang menjadikan tanah sehat (healthy soils) dan menopang kehidupan tanaman (Yuan et al. 2021). Bakteri fungsional merupakan salah satu kelompok mikrob tanah dengan populasi paling beragam dan melimpah yang bertindak sebagai indikator kesehatan tanah, baik itu menguntungkan (beneficial microbes) maupun merugikan (deleterious microbes) (Gans et al. 2005). ...
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Fenomena tanah supresif telah banyak dikaji sebagai metode pengendalian penyakit tanaman alami di lapangan dan dicirikan dengan banyaknya sejumlah mikrob fungsional yang mampu menekan populasi patogen. Penelitian ini bertujuan mengetahui dan membandingkan komposisi bakteri fungsional pada tanah supresif dan kondusif layu fusarium. Metode penelitian terdiri atas pengambilan sampel tanah di lapangan, isolasi bakteri fungsional dari sampel tanah supresif (TS) dan kondusif (TK), penghitungan populasi dan jenis bakteri, penapisan berdasarkan keamanan hayati, dan karakterisasi bakteri fungsional dalam menekan Fusarium oxysporum. Hasil penelitian menunjukkan bahwa populasi bakteri pada TS lebih tinggi dibandingkan TK, khususnya bakteri toleran panas dan Pseudomonas kelompok fluorescent. Hal ini didukung dengan tingginya nilai keanekaragaman bakteri fungsional pada TS (H’ 3.70 > 3) dibandingkan TK yang tergolong sedang (1 < H’ 2.07 < 3), dengan sebaran bakteri fungsional tergolong hampir merata dan tidak ditemukan adanya dominansi jenis tertentu pada TS maupun TK. Persentase bakteri nonpatogenik pada TS lebih tinggi dibandingkan TK, masing-masing 51% dan 23%. Bakteri tersebut berpotensi sebagai plant growth promoting bacteria (PGPB) dengan memproduksi IAA atau melarutkan fosfat saja, masing-masing 24% dan 10% pada TS, sedangkan pada TK masing-masing 14% dan 29%. Hanya bakteri yang berasal dari tanah supresif yang mampu memproduksi IAA sekaligus melarutkan fosfat dengan persentase sebanyak 48%.
... Soil environment has a multifaceted biological system (Gans, Wolinsky, and Dunbar 2005) with 1,000,000 species in a 10 g sample (Young and Crawford 2004). The first step of biosphere's development is biogenesis of soil, which involves nutrient recycling and the creation of soil. ...