A comparison of bacterial variability across biogeographic regions based on PGPR

— Plants are sessile organisms that experience abiotic stresses like sediment salinity, drought, and extreme temperatures. In light of our growing population and increasing demand for better nutrients and commercial quality foods, optimizing the use of our natural resources is essential to ensuring food security.Enhancing PGPR using modern tools and techniques of biotechnology can greatly contribute to achieving sustainable agriculture, by improving soil fertility, plant tolerance, crop productivity, and maintaining a balanced nutrient cycling. Plant rhizospheres could contribute to the development of robust plant growth-promoting (PGP) activities and stress tolerance capabilities under drought conditions. They enhance the adaptation of plants for different desertification environments because they are diverse and functionally redundant (PGPR). In addition to soil properties and plant species, there are a variety of biotic and abiotic factors that influence their composition and abundance. In this review article, we learn how Bacterial diversity is influenced by soil environment and geophysical conditions.


INTRODUCTION
Soil environment and geophysical conditions have a direct impact on bacterial diversity. The soil is composed of microinches with heterogeneous physical and chemical properties across a wide range of scales. Since bacteria live in small pockets within a niche, the properties of their immediate environment rather than the soil's mean properties influence the survival of their local community. Space heterogeneity has been shown to result in lower survival rates in local communities due to the heterogeneity of the bacterial communities on <1 cm [1]. Abiotic factors such as soil physicochemical properties and geographical location are important factors that shape bacterial community abundance and diversity. The type and location of soil, as well as the plant species in an area, significantly change the structure of bacterial communities. The functional profiles of soil bacterial communities were influenced by both the location of the soil and the plants in the soil. Researchers have found that soil and plants play a major role in shaping rhizosphere microbiota's composition [2]. In rhizospheres, different soil properties such as pH, concentrations of phosphorus and potassium, as well as concentrations of other mineral nutrients, affect the composition of the bacterial communities differently [3].
The PGPR bacteria are beneficial bacteria that colonize the roots of plants and enhance their growth through a variety of mechanisms [4]. These bacteria colonize the roots of plants and boost their growth in a variety of ways. Take steps to control insect and disease damage. Either directly or indirectly assist plants in growing. Reducing agricultural reliance on hazardous chemicals. Enhancing soil fertility by releasing nutrients. They affect plant growth in several ways, including direct mechanisms such as nutrition and growth regulation, as well as indirect mechanisms related to their ability to biocontrol [5]. A key tool for boosting sustainable agriculture, PGPR has gained popularity over the last few decades. PGPRs can affect plant growth either indirectly or directly. Direct growth promotion by PGPR involves giving a plant a bacterium-produced compound, such as phytohormones, or encouraging the plant to take up nutrients from the environment [6]. By [9]named this phenotypic tolerance to abiotic stress "Induced General Tolerance" to describe plant responses to PGPR-induced abiotic stress. Based on their proximity and intimacy to roots, Rhizobacteria are divided into (i) soil-dwelling bacteria, which utilize roots' metabolites for carbon and nitrogen, (ii) rhizoplane-colonizing bacteria, (iii) bacteria that reside inside cortical cells, and (iv) bacteria living within specialized root structures. As the distance between the root and the plant changes, so does the association of plant growth-promoting bacteria. Extracellular PGPR (ePGPR) and intracellular PGPR (iPGPR) make up the vast majority of PGPR [10].PGPR (iPGPR) bacteria live inside plant cells and produce nodules. They are located in these specialized structural elements. PGPR (ePGPR) bacteria don't produce nodules but stimulate plant growth through the production of signal compounds. There is much greater diversity in host plant proximity, infection mode, and, most significantly, plant effect on ePGPR associations, compared to iPGPR [13].
Communication and environmental sensing are carried out by both beneficial and pathogenic bacteria using QS. It consists of a series of gene-regulated molecules known as autoinducers that act on bacteria at the gene level [14]. To maximize their population size and fitness, bacteria release AIs into the environment to assess their surroundings and adapt their gene expression accordingly. AHL, for example, is one of the many wellstudied artificial ions produced by Gram-negative bacteria, whereas cyclic peptides are prevalent among Grampositive bacteria [15].Furthermore, QS is involved in several physiological behaviours such as symbiosis, virulence, antibiotic production, conjugation, competence, sporulation, and biofilm formation [16]. PGPRs also communicate with higher organisms, such as plants, using QS, whether they belong to the same species or not. As it turns out, plant-microbe communication is now evidently dependent on QS communication for microbial interactions at the rhizosphere [17].Evolutionary adaptations of plants have introduced an array of ways for them to respond to QS, such as sensing and responding to bacterial QS signals, and producing substances that mimic AHL and can impact QS in the plant-associated bacterial community. Numerous studies also reveal that the rhizosphere harbours more AHL producing bacteria than the bulk soil, and that these AHL molecules are capable of acting as inter-kingdom signalling molecules [17] [18].When rhizobacteria form closer associations inside the roots of plants, they are called endophytes. The term is defined as "bacteria that can be isolated from surface-disinfected plant tissue, or that can be extracted from the plant itself without causing visible harm to the plant" [19].There are several types of endophytes, such as rhizobialnodulating bacteria and nitrogen fixers [20].

II. RHIZOSPERE
Life's terrain consists of the elements of an ecosystem that cannot be seen by the naked eye, such as soil or water. In soils, rhizosphere is likely the primary site of bacterial activity. "Rhizosphere" originates from the Greek words "rhiza" (root) and "soi" (ground). It can also be referred to as the root zone, soil zone, or hydrological region. PGPRS colonizes plant roots by inhabiting root tissues, around roots, and on the rhizoplane (root surface) [6].Rhizospheres were first described by German scientist Lorenz Hiltner (1904) as "areas of soil next to legume roots where bacteria thrive.". Therefore, it is a nutrient-rich area of soil directly surrounding roots of plants. Unlike other regions, this one has no distinct edges; it is influenced by compounds released by the roots and microbial life that feeds upon them. Its varied and dense flora makes it a highly dynamic region. By observing the composition and pattern of root exudates, we can gain insight into microbial activity and population proportions. Rhizosphere interactions affect root growth and function, ultimately resulting in changes to the plant's growth. Each plant species hosts a unique PGPR community [21].

III. PGPR IN DESSERTS: BACTERIAL COMMUNITY SHAPING FORESTS IN DESERT PLANTS
Deserts are dynamic, heterogeneous habitats that take up one third of the planet. A desert plant's adaptation to the desert environment is also determined by the microbial communities that colonize and inhabit its surrounding soils [22]. It is extremely hard for microbes to Although these pioneer desert plants were subjected to extreme conditions, their rhizospheres contained a rich diversity of bacteria. The composition of rhizosphere bacterial communities is influenced by abiotic factors such as soil type and composition, location, and soil properties. In similar geographical locations, the soil, rhizosphere, phyllosphere and associated bacterial communities are similar, whereas plants in distant geographic locations with distinct soil properties have a different soil bacterial community and have different associated bacterial communities. Furthermore, plant host genotyping has an effect on the community of bacteria in the Endosphere. There are a variety of bacterial communities in desert plants, but two major phyla are mainly dominant: Proteobacteria and Actinobacteria. Proteobacteria have a wide range of adaptation capabilities to a variety of environmental lifestyles, including nitrogenfixing plant symbionts such as Rhizobium, Mesorhizobium, and Sinorhizobium [37].The Actinobacteria have shown impressive versatility in their ability to grow under extreme conditions including salinity, low pH, low water availability, high radiation, and pressure, they include several diverse species (including alkalophiles, acidotolerants, thermotolerant, and halotolerant) [38].
There are certain features of desert plants that make them dependent on bacterial communities, such as high expression of genes related to dormancy and osmoregulation, and lower expression of genes related to nutrient cycling and catabolisms. Root

IV. IMPACT OF AQATIC PGPR
Due to the unique nature of the underwater life history, the competition for abiotic resources, like light availability, is more intense in the fresh water ecosystem. Additionally, freshwater ecosystems are typically biologically inaccessible. Rehabilitating macrophyte species and communities is more challenging than rehabilitating terrestrial plants. Aquatic  The PGPR strains can enhance the recovery of submerged plants in organically rich sediment [55]. In many parts of the world, water ecosystems are experiencing deterioration in water quality and ecological structure [56].After a decrease in water nutrition level, macrophytes usually take decades to adjust to the new environment [57]. The presence of organic sediment in lakes negatively impacts their ecological restoration because it acts as a stressor for macrophyte growth. It has been demonstrated that sediment anoxia inhibits the germination and sprouting of submerged macrophytes during restoration [58], and there are numerous issues associated with organic enrichment in water. An anoxic degradation pathway causes oxygen exhaustion and accumulation of potentially phytotoxic compounds, which causes benthic vegetation to decline [59].The high organic matter content of fertile sediments leads to decreases in aquatic plant biomass. Furthermore, excessive organic matter content can generate reductive sapropel, which threatens aquatic plants' survival [60].Phoridobacteria (PGPR) were screened from the rhizosphere of submerged macrophytes and selected for their ability to promote Vallisneria natans under the high preponderance of sediment organic matter [55].

V. IMPACT OF HALOPHYTES
Agricultural sustainability is seriously threatened by soil salinity. The salt content in soils is one of the major abiotic stressors known to affect arid and semi-arid regions, and this leads to significant losses in agriculture productivity.2009 determined that increases in salinity negatively affect the growth-promoting characteristics of PGPRs [61]. Therefore, using halotolerant PGPRs that are selected for high salt tolerance along with efficiency in expressing PGPR traits would allow crops to be grown successfully in environments with natural or induced salinity [62]. Halotolerant may grow in environments varying from one to thirty-third NaCl, as well as at intervals without NaCl [73] [74]. Under low water potential owing to salt stress, they are thus found at intervals in the rhizosphere of halophytes [61] [75]. The plant growthpromoting bacteria Moneron pumilus, Mendocina spp., Arthrobacter spp., Halomonas spp., and Nitrinicolacisaponensishave features such as phosphorus (P) solubilization, in addition to producing ACC deaminase, IAA, and siderophores. These traits are referred to as PGP traits because they allow plants to produce under limiting conditions, stimulate plant growth by serving as a phytohormone (IAA), provide metal to the plant through chelation (siderophores), and release a precursor to the plant stress hormone (ACC deaminase).

VI. TROPICAL MANGROVE ECOSYSTEM NEED TO BE MAINTAINED BY MAINTAINING MICROBIAL COMMUNITY DYNAMICS:
The mangrove forest is considered to be one of the most productive and biologically diverse wetlands on Earth, constituting an important natural reserve. There are currently fewer than 50% remaining, with half of it being degraded. Due to the deforestation of mangroves in many parts of the world, fish resources are dwindling, water supplies are being contaminated, and coastal erosion and salinization are rampant. Plants can use the nitrogen, phosphorus, and other nutrients being generated by the highly diverse and productive microbial community in tropical and subtropical mangrove ecosystems. There are some bacterial strains isolated from the root rhizosphere of mangrove plants that are useful as PGPBs and could be used to promote plant growth in programs of reforestation, or in the creation of mangrove wetlands in coastal lagoons. The inoculation of black mangrove plantlets with M. chthonoplastes caused roots to colonize rapidly, increasing nitrogen fixation [89] as well as nitrogen accumulation [90]. When black mangrove seedlings were inoculated with a mixture of two bacteria, nitrogen was incorporated into the leaves twice as much and leaves developed more rapidly [91]. Mangrove roots may contain bacteria that can be used as PGPB to improve the establishment and enhance the growth of coastal mangrove seedlings.
Nitrogen fixation occurs frequently in mangroves. Nitrogen was fixated at high rates in association with dead and decomposing leaves, pneumatophores (air roots), the root rhizosphere, tree bark, Cyanobacterial mats that covered surface sediments as well as the sediments themselves

VII. BACTERIA ASSOCIATED WITH FOREST SOILS
Forest soil bacteria are an important part of the soil microbial community, though they are understudied.In forest ecosystems, bacteria perform diverse ecological functions such as organic matter decomposition, mycorrhizal symbiosis regulation, and participation in the N cycle. The major natural agents responsible for N fixation in forest ecosystems are bacteria [101] as well as other processes, such as mineral weathering, that cause inorganic nutrients to be released [102]. A forest ecosystem provides many habitats for bacteria, including soils, plant tissues, streams, rocks, etc., however, soils and litter, which are particularly rich in bacteria, are predominant on the forest floor [103]. According to most studies, Acidobacteria, Actinobacteria, Proteobacteria, Bacteroidetes, and Firmicutes are abundant in soil [104]. Soil pH is one of the most important drivers in determining the composition of bacterial communities. in addition to ph. other components such as the organic matter content, nutrient availability, climate conditions, and biotic interactions (especially the influence of vegetation), influence bacterial community composition [104].
Two-thirds of the earth's C is stored in forest soils [105]. A great deal of the global carbon balance is influenced by temperate and boreal floras as they will remain a large sink of anthropogenic carbon dioxide. Some soil bacteria are capable of fixing CO2 in the soil. Bradyrhizobium (Betaproteobacteria) is a bacterium that inhabits forest soils in large numbers [106]. For forest soils with aerobic conditions, methane represents a gaseous form of organic carbon [107]. It has been reported that these methanotrophs are the primary consumers of atmospheric methane as well as methane from waterlogged, anaerobic soil horizons [108]. Methane can be sequestered from the atmosphere by forest soils (especially those of boreal forests) because of the presence of methanotrophic bacteria. Most of the characterized methanotrophs belong to the Alphaproteobacteria and Gammaproteobacteria [109].
In unmanaged environments, bacteria are estimated to contribute more than 95% of the N input [101].nifH is present in the Alphaproteobacteria (Bradyrhizobium, Azospirillum, Hyphomicrobium, and Gluconacetobacterspecies) and Deltaproteobacteria (Geobacterspecies). was observed in different temperate forest soils, demonstrating the ubiquity of some N-fixing bacteria, not only as symbiotic but also as free-living taxa [106].

VIII. CONCLUSION
The PGPR bacteria are beneficial bacteria that colonize the roots of plants and enhance their growth through a variety of mechanisms. In similar geographical locations, the soil, rhizosphere, phyllosphere and associated bacterial communities are similar, whereas plants in distant geographic locations with distinct soil properties have a different soil bacterial community and have different associated bacterial communities. Soil environment and geophysical conditions have a direct impact on bacterial diversity. The functional profiles of soil bacterial communities were influenced by both the location of the soil and the plants in the soil.