Globally, the natural soil reserves of phosphorus (P) are depleting at a higher rate and it has been estimated that there will be very limited soil P reserves by the end of 2050 for crop growth and sustainability, especially in the tropical and subtropical regions of the world [37,38]. A large amount of P is present both in organic and inorganic forms in soil, but only a small proportion is available for plant uptake and the remaining is mostly restricted with other soil nutrients due to complex formation [39–41]. For plant growth, the amount of soil solution P pool is very small compared to overall soil P, as evident in alkaline soils, sandy soils and weathered soils of tropical and subtropical regions. Furthermore, 30% to 50% of total P is present in organic form in soil and thus not available for the direct use of the plants [42]. The P deficiency can be found mainly in the agricultural soils of developing countries, having an unfavorable condition for P availability and uses by the plants [43]. It is predicted that more than 40% of the world soils are P deficient and has limited crop growth and production [44]. The total amount of P in the soil is 0.05%, only 0.1% (Fig. 1) of this is available for the plant’s growth. The type and pH of the soils are essential factors for the determination of P fixation and precipitation with Fe and Al at acidic soils and Ca in alkaline calcareous soils [45].

Moreover, physical adsorption and chemical precipitation are also responsible for the P fixation with Fe and Al oxides and hydroxides in acidic soils [46]. Consequently, after P fertilization, only 30% to 40% P is recovered by the plants and the rest is adsorbed, precipitated and forms complexes with other soil nutrients [47]. In soil, the common organic forms of P (Fig. 1) are phosphomonoesters and phosphodiesters, including phospholipids, nucleic acids, sugar phosphate, glycerophosphate and coenzymes [48]. These forms of P must be converted into inorganic P before used by the plants. Plants fulfil their requirements by utilizing inorganic P from soil solution as phosphate anions after mineralization of organic P [49]. Most of the soil organic P compounds are present as high molecular weight. Therefore before plant uptake, these compounds must be converted into low molecular weight or soluble P [50].

Phosphorus is an essential macronutrient like Nitrogen (N) and Potassium (K), which is vital for many plant growths processes. For the normal function and growth promotion of crops, approximately 10–25% P is required [51]. Plants absorb P mainly during the vegetative stage and then re-translocate it to the fruits and seeds at the reproductive stage. Phosphorus is involved in various cellular functions [52] and its deficiency causes dark green coloration anthocyanin formation [3]. Plants absorb P from the soil solution as primary orthophosphate or secondary orthophosphate. If the orthophosphate of soil solution is not enough to fulfil the plant’s requirements, then it is replenished from other pools of soil P [53]. Moreover, exchange and depletion of orthophosphate also occur between the rhizosphere and bulk soil present in the vicinity of the plant roots [54]. The different microbial processes in the mycorrhizosphere are also responsible for the transformation of P to the roots surface and their uptake by the plants [55].

Another important source that fulfills the deficiency of P in soil is the different types of chemical fertilizers. The important chemical fertilizers, which are commonly used as a source of P in Pakistan are Di-ammonium phosphate (DAP), Triple Super Phosphate (TSP), Single Super Phosphate (SSP) and Nitrophos (NP) containing 46% P₂O₅, 30% P₂O₅, 14–18% P₂O₅, and 23% P₂O₅, respectively [56]. The amount of nutrients in the chemical fertilizers sources is quite high, with an easily transferable capacity to soil and quick uptake by plants. The application of chemical sources of P fertilizers in the field and greenhouse conditions is also easy and requires less labor cost. The P content of chemical fertilizers fulfils the nutrients requirement of the crop. However, at high pH (8.5), it is also adsorbed with surface containing calcium compounds, decreasing its availability to crops from inorganic sources like Single Super Phosphate [57]. According to Khan et al. [58] when the inorganic P fertilizers are added to the soil, than about 85–90% become unavailable for the plant’s uptake. This is due to adsorption and precipitation with Ca and Mg at alkaline soil conditions and Al and Fe at acidic soil conditions in the same year of application. Besides, the quick source of P, the huge supplementation of chemical fertilizers to the soil also causes several adverse impacts like water resources pollution, changes in soil pH due to acidity and alkalinity, insects and microbe’s destruction, soil degradation due to high organic matter decomposition and nutrients fixation [33]. The high prices of chemical fertilizers in the national market of Pakistan have compelled the farmers to reduce the dosage of chemical fertilizers in their fields, which resulted in low crop yields. Compared to 2006–2007, the high prices of chemical fertilizers in 2008–2009 and 2009–2010 caused that, the usage of chemical fertilizers was decreased to 35% and 53%, respectively. Similarly, the cost of urea, DAP, CAN and NP during 2011–2012 jumped up to 81%, 39%, 76% and 46%, respectively, as compared to prices of these fertilizers in the year 2010–2011 [59]. The high transportation cost and prices of importing chemical fertilizers in developing countries have changed the farmer’s opinion to adopt environmentally friendly indigenous sources of fertilizers like rock phosphate [59,60] or other options like biofertilizers, organic manures, and composts to meet the nutrient requirement of the crop plants.

The estimated resources of all grades and types of rock phosphate (RP) are approximately 163,000 million tons [39,40,61]. The world RP reserves (Tab. 1) are distributed in Africa (41%), USA (21%), USSR (13%), Middle east (10%), Asia (8%), South America (3%), Australia (2%) and Europe (1%) [59,61]. However, the RP scenario in Pakistan is also prominent. It is estimated that there are million tons of recoverable RP deposits in the Hazara district of Khyber Pakhtunkhwa. Therefore, they are cheap available sources of P fertilizers for sustainable crop production. The origins of these RP deposits are the sedimentary rocks distributed in an area of approximately 155 km² at different localities. In this area, the total predictable RP reserves are about 6.9 million tons; 4.59 million tons of that amount are recoverable and can be used in alkaline soils as a potential source of P fertilizer [62]. The different localities having RP deposits are Kakul, Lagarban south, Eastern phosphorite, Batkanal and Southern phosphorite containing 0.6, 1.34, 1.54, 0.6 and 0.495 million tons RP, respectively. Moreover, Lagarban is the major RP deposit in Pakistan, containing an average of 25.8% P₂O₅% and 6% MgO.

The repeated use of chemical fertilizers in large amounts is expensive, and it adversely affects the environment and soil microbial populations [60,63]. Therefore, naturally occurring rock phosphate (RP) is a cheaper and environmentally-friendly alternative source than the commercial P fertilizers [64]. It is used in industry as a raw material in the manufacture of P fertilizers such as SSP, DAP and NP. Moreover, the direct use of RP as a source of P fertilizer is agronomically more suitable for alkaline soils in the presence of certain amendments [62]. The four main types of RP are Flouro apatite, Carbonate apatite, Sulpho apatite and Hydroxy apatite. The deposits of sedimentary apatites are soft and micro-crystalline in structure, and they are commercially more important to use directly in the soil [65]. Therefore, the direct application of RP at alkaline soils is an important substitute for unaffordable commercial P fertilizers [66].

The poor farmers of west Africa cannot afford the supplementation of expensive commercial P fertilizers in their soils. Therefore, the direct application of low-cost RP is more suitable against high-cost commercial P fertilizers [67]. In soils, factors like soil and climatic conditions, moisture contents, granular size, time and application rate are very important for the release of P from RP [68]. The direct application of RP is common in acid soils because it contains hydrogen ions responsible for converting P from RP into a water-soluble form. Moreover, the alkaline soils seize the solubility of P unless enough amount of hydrogen ions are added to them. Organic matter also enhances the solubility of P due to hydrogen ions in the soils. This is because when organic matter starts decomposition, it releases acids (e.g., Humic acid), which enhance P solubility from RP by lowering the soil pH [69]. Several researchers have proved the financial and agronomic effectiveness of RP application on acidic and alkaline soils for sustainable crop production.

Mashori et al. [70] experimented with alkaline calcareous soil in Pakistan to determine the agronomic effectiveness of local RP in combination with FYM and SSP. Different rates of RP and SSP were applied to all treatments along with or without FYM (10 tons ha⁻¹). Recommended rates of N and K fertilizers were constantly applied to all the treatments as a basal dose. After crop harvesting, plant growth parameters and nutrient concentration were recorded. The maximum shoot dry biomass (30 g pot⁻¹), P concentration (0.31%) and uptake (0.10 g pot⁻¹) were noted in the treatment having RP and SSP along with FYM; it was followed by the treatment having RP and SSP alone. They concluded that the integrated use of indigenous RP with water-soluble P fertilizers and FYM was a promising and important substitute for expensive commercial P fertilizers at alkaline calcareous soils in Pakistan. This was to solve the P problems and attain maximum crop productivity. The agricultural soils of Indonesia are mostly acidic in nature thus contain a low quantity of both total and available P concentration. At these soils, P deficiency corrections are crucial for improving soil fertility and plant productivity. Therefore, an experimented was conducted in farmer’s fields to evaluate RP’s reactive and agronomic- effectiveness on maize crop on an Ultisol at the South Kalimantan Province of Indonesia. In addition, the residual effects of these phosphate rocks were also determined during six cropping seasons. The authors concluded that the reactive RP could be used effectively to enhance fertility and crop growth. Moreover, they also recommended the direct application of RP in P deficient acidic soils in Indonesia [71] (Fig. 2).

The presence of rhizospheric phosphate solubilizing microorganisms (PSMs) and their role in P acquisition of plants is evidenced since 1903 [21]. Several types of efficient soil microbes have been isolated and identified from the plant rhizosphere (Tab. 2). They solubilize orthophosphate from insoluble and inorganic bound P and enhance its availability for plants uptake [72,73]. Several bacterial strains such as Bacillus (Bacillus megaterium, B. subtilis, B. circulans B. sircalmous, B. polymyxa), Enterobacter, Rhizobium and Pseudomonas [74] along with Penicillium, Aspergillus, mycorrhizal fungi and actinomycetes fungi are the most powerful P solubilizers [75].

The commonly known PSMs in the rhizosphere are species of free-living fungi and bacteria that help plants in P solubility and bioavailability [40]. In agriculture these PSMs are used as biofertilizers due to their effectiveness in the solubility of fixed P and its uptake by plants for a sustainable crop production [35,76]. Application of phosphate solubilizing microbes to soil can mineralize the wider substrates of organic P [77]. Moreover, the turnover of microbial biomass plays a significant role in retaining the levels of organic and inorganic P in the soil solution, and is very important for determining a sufficient amount of P supply to plants [78]. This participation of microbes can be significantly judged in the rhizosphere having an adequate quantity of metabolized C and a higher population of microbes [79]. The microbial biomass also plays a significant role in the P cycle in the soil; therefore, the subsequent release is very important for maintaining the pathways and movement of P in the soil-plant system. Additionally, the PSM can also protect orthophosphate via a complex formation with other soil nutrients due to different physico-chemical properties of the soil [78].

Several researchers have studied the role of PSM under controlled conditions and suggested that the inoculation of plants with PSM significantly increases growth and P uptake due to their P solubilizing activities in the rhizosphere [35,80]. The effect of most of the PSM is different under greenhouse and field conditions. This is due to the effect of many factors such as a complex soil environment, lack of knowledge for introducing soil microbes and their mechanisms, the interaction between microbes in the soil community, and lack of a specific partner for association [49]. For example, Whitelaw et al. [75] reported that Penicillium radicum efficiently solubilized P and enhanced wheat growth under greenhouse conditions after P fertilization. Sashidhar et al. [81] studied the single and combined inoculation of Bacillus polymyxa, Pseudomonas striata and Aspergillus awamori and found considerable improvement in grains yield of cowpea, soybean, chickpea, rice and lentil.

About 80% of all vascular plants or some 250,000 plants species can form a symbiotic association with AMF [83,84]. AMF enhanced the uptake of different nutrients such as P, Cu, Fe, Zn and Mn from the soil to the host plants [85,86]. Arbuscular mycorrhiza improves plant growth and nutrition by exploring the soil located beyond the zone of depletion and take the nutrients present in the depletion zone more efficiently [87]. The AMF transfer P from the soil to the plant at the interface between plant cells and other essential structures like hyphae coils, arbuscules, and vesicles [87]. P transporters are involved in the uptake of P by AMF to plants cells, which proves that it’s an active process in the soil [88]. It has been studied that AMF distribute and absorbs P more efficiently in tilled soils of wheat and maize crop roots than in no-tilled soils [89]. The P nutrition is improved both by AMF and some soil physicochemical properties with different tillage treatments [29]. However, the plant’s root is colonized by AMF and non-mycorrhizal control in field conditions is difficult to evaluate. Therefore, sometimes it became difficult to get clear proof regarding the significance of AMF in crop nutrition [90]. Mycorrhiza may also contribute a key function in the mineral nutrition of plants by various elements, protecting plants from hazards and absorption of toxic heavy metals, increasing salt tolerance, and increasing the stability of soil aggregates [91]. Naher et al. [92] demonstrated that AMF plays a significant role in agricultural sustainability as well as in the mutualism with plant roots. Moreover, AMF are also important for the uptake of nutrients, to reduce water stress and as a biological protectant against pathogens.

The effect of a commercial mycorrhiza inoculum and indigenous AMF with a phosphate fertilizer on the yield and P availability of a maize crop was studied by Cozzolino et al. [2] under field conditions. They confirmed that the effect of a commercial AMF inoculum in the N and K treatments was almost similar to the treatment having P in combination with N and K fertilizers. After 40 days of the experiment, higher P concentrations were recorded in N, P, K and NK treatments. This result shows that the inoculated roots can improve soil and plant P. Moreover, these results also suggest that AMF inoculum is a promising approach for integrated nutrients management in P deficient soils [93].

Similarly, in a 13-year-old irrigated field experiment in Nebraska, the effect of different rates of N fertilizers (0, 50, 100, 150 and 300 kg ha⁻¹) and maize crop rotation with soybean and monoculture maize was tested on P uptake and AMF communities in the soil were tested. In maize roots, the biomass of AMF was increased from one stage to another but it was not affected by N fertilizers or rotation with soybean. The detection of AMF provided indirect evidence of P uptake by AMF in maize roots derived acid, alkaline and polyphosphates. The N fertilization did not affect the AMF associated P uptake, but its maximum value was recorded in the monoculture maize. The spores frequency of AMF is varied with different levels of N fertilizers which is an important aspect for agroecosystem management [94].

Furthermore, AMF can change plant physiology and the microbial populations in the soil due to specific features of mycorrhized rhizosphere than non-mycorrhized rhizosphere. In the soil, AMF are involved in all fundamental activities necessary for a healthy natural and agricultural ecosystem. There are various agents such as overdosing of commercial fertilizers, faulty cultivation practices, fungicides and use of non-mycorrhizal plants that affect the performance and efficiency of AMF in spore formation and colonization as well as sustainable crop production [95]. Pellegrino et al. [96] explored the influence of two mycorrhiza inocula (native and exotic) in T. alexandrium and maize crop rotation. They studied the effect of four exotic AM fungal isolates on physiological traits of Trifolium alexandrium in green-house conditions. Trifolium alexandrium was inoculated with single and mixed inoculums of exotic AMF and the results were compared with those of native inoculums.

Furthermore, the residual effect of AMF inoculation under field conditions was assessed on the subsequent maize crops. Analysis of the data indicated that the field inoculation with the AMF inoculum increased the quality and productivity of T. alexandrium and maize crops. Moreover, the native AMF inoculum was more effective as than the exotic AMF inocula. It was also observed that the beneficial effects of AMF were consistent until the second year of crop growth. Thus, the application and use of native AMF inocula are economically and ecologically an important alternative approach compared to commercial AM inocula for sustainable agricultural systems.

Arbuscular mycorrhiza fungi play a key role in soil aggregation [97]. AMF affects the shoot to root ratio, plant physiology, nutrients uptake by plants and highly affect soil aggregates formation during symbiosis. When AMF affect the plant root system, the AMF increases the potential of plants roots and root hairs to bind soil particles [97]. Hallett et al. [98] reported that plants roots apply stress on soil particles and bind these soil particles to facilitate the formation of soil aggregates. In addition to this, AMF affects the pressure of plant roots by their branching pattern [97]. Arbuscular mycorrhiza fungi are also involved in certain biochemical and biological processes necessary for soil aggregate formation. Just like plants, the AMF hyphae bind the microparticles of soil into macroparticles. AMF produces some glomalin-related protein and mucilage’s that help soil aggregate formation in the soil and plant rhizosphere. These proteins increase the coating of these particles and enhance their stability [99] and preventing them from dispersing and disintegrating (Fig. 3).

The PSB have been used for increasing crop growth and productivity for decades [73]. In soils, there are many different bacterial species capable of solubilizing insoluble P to its soluble form, and are called PSB. These bacteria increase plant growth and colonize plant roots; therefore, they are also called PGPR [86]. The PSB supply P to plants in a sustainable and environment friendly manner. Plant provides areas, energy, shelter, food and areas of biological diversity to PSB. There are various modes of actions by which PSB solubilize P and give it to plants by producing phenolic compounds [100], organic acids [45], siderophore and hormones secretion [63]. Ivanova et al. [101] reported that in the soil different bacterial species have the potential to increase the RP solubility of soil-bound P in soil as well as in culture medium by secreting organic acids. These acids destroy the P bound structures and thus make P soluble for the uptake of plants [35]. In soil the efficient PSB strains increase the bioavailability of P and thus the overall plant growth is improved. The PSB have the ability to increase the growth of cereals, legumes, fiber crops, horticulture crops and oil seed crops [35].

The ability of PSB strains like Pantoea cypripedii and Pseudomonas plecoglossicida have been documented to enhance maize and wheat total dry biomasses, grain yield and fertility of soil. Furthermore, P uptake, available soil P and PSB populations are also significantly increased by PSB inoculation with RP. A significant increase in crop yield and soil fertility are very obvious due to PSB inoculation with RP compared to controls. Moreover, inoculation of PSB P. cypripedii (PSB-3) and P. plecoglossicida (PSB-5) with RP can enhance the growth and fertility of soil [102]. The PSB strains can improve the growth of maize, P solubility and production of plant growth-promoting substances. PSB inoculation also enhances the concentration of P in roots, shoots and maize biomass in treatments without P fertilizers. The soils fertilized with tricalcium P also enhance plant biomass due to the inoculation of PSB and P in the tissues. The increase in plant growth is not only due to P solubilization but also to some other plant growth-promoting traits. It is clear that the PSB strains may be efficiently used as a biofertilizer in P deficient soils to increase P solubility and maize productivity [103]. Kaur et al. [102] conducted 2-year experiment in the field to explore the efficiency of two efficient PSB strains with and without RP on maize and wheat cropping systems. They recorded that the inoculation of PSB with RP increased shoot and root dry biomasses, grain yield, plant height and plant P uptake on both wheat and maize compared to control and other treatments. The combined use of PSB with RP was more economical due to its low cost and more returns. da Costa et al. [5] conducted an experiment on an oxisol to evaluate the effect of inoculated PSB on rice plants fertilized with RP on growth and nutrient accumulation. All of the inoculated PSB strains enhanced shoot, root and total dry matters, and P, N, Ca, Mg, S and B concentrations compared with the treatment without PSB. They also noted that the increase shoot and root dry biomasses was 52% and 120%, respectively, due to the inoculation with Paenibacillus kribbensis. This study also indicates that the inoculation of rice plants with PSB amended with RP is a suitable and economical approach to enhance growth and P uptake by plants of this species.

Phosphate solubilizing bacteria and plant growth-promoting bacteria are important to soil ecology and as a biocontrol agent. They are abundant in the soil and the plant rhizosphere. In the soil they perform different functions and can be widely used to suppress the activity of different bacteria, fungi and nematodes spreading diseases [104,105]. Furthermore, PSB are also widely used as biofertilizer in many agricultural soils instead of commercial P fertilizers [76]. Moreover, PGPR are also very important for the control of plant pathogens in soils [104]. It has been found that Pseudomonas sp. acts as an important biocontrol agent in the plant rhizosphere [105]. These bacteria secret several metabolites, gluconic acid, siderophores, and enzymes which help in controlling diseases and thus act as a biocontrol agent [106]. Pseudomonas and PSB are specialized characteristics that make them plant growth promoting rhizobacteria [107].

The specialized characters of PSB are that they rapidly colonize, rapidly use root exudates, produce biocontrol metabolites and rapidly colonize in soils. Another important species of PSB which act as a biocontrol agent is Bacillus subtilis. This bacteria specie has the ability to release endospores and some active compounds in soil for various functions [108]. Bacillus megaterium is also used to enhance P and release of antifungal metabolites, siderophores and indole acetic acid, thus reducing the intensity of diseases on plants [109]. Phosphate solubilizing bacteria are also used in integrated pest management in agriculture.

The AMF interactions with PSB in increasing P solubility, availability and uptake by the plants have been documented since 1990 [110]. Both the organic and inorganic P forms are unavailable to plants due to their chemical bonding with clay surfaces and fixation with other soil nutrients and crystal lattices. In the rhizosphere soil there are many PSBs that can improve the availability of organic and inorganic P to plants (Tab. 3) with the help of AM species [76,111]. These bacteria produce some organic acids, which help in the solubility of both organic and inorganic forms of P, and subsequently provide it to the plants with the help of AM hyphae [12,35,83]. In P deficient soils, plant inoculation with AMF and PSB not only increase P uptake but also enhance the phosphatase activity [112], PSB number [113] and mycorrhization [114]. Artursson et al. [115] reported that there are different strains of bacteria such as Pseudomonas, Bacillus, Paenibacillus and Rhizobia which have positive association with several types of AM species including Glomus mosseae, G. calrum, G. versiforme and G. intraradices in the soil [114,115]. The combined inoculation of these microbes resulted in AMF growth, spores formation, colonization of the host plant, P solubility and pathogen suppression [115].

Several pot culture studies have been conducted regarding the combined application of AMF and PSB in the rhizosphere [80,116]. Some of their results indicate that the direct interaction between AMF and PSB was not significant because the Glomus intraradices lacks the phytase protein which is important for the utilization of phytate in the soil. Moreover, AMF also influences the potential bacteria directly and indirectly in the plant rhizosphere [117]. Additionally, PSB interrelate with AMF due to their capability to colonize roots in the presence of spores and surfaces of AM hyphae [118], and thus affect the root infection intensity, hyphal growth [119] and the availability of nutrients for the capturing of AM hyphae [120,121]. The interaction between AMF and PSB also enhance N and P uptake by plants [115].

Furthermore, the co-inoculation of AMF and PSB also improves RP mineralization and P uptake (Tab. 3) [112,122], and thus plays an important role in developing P fertilizers. Toro et al. [123] studied the synergistic effects of AMF and PSB in P deficient soils; they concluded that the treatments having both AMF and PSB significantly increased plant dry biomass (Tab. 4), and nutrient concentration in plant tissues. Moreover, they also observed the beneficial effects of PSB on AMF establishment, and the increasing population of PSB by AMF in the plant rhizosphere.

Several researchers have also reported the synergistic effect between AM fungi and plant growth-promoting rhizobacteria (PGPR) in the soil. These bacteria enhance plant growth and development by interacting with AM fungi (Tab. 4), controlling pathogens, increasing nutrient solubility, and releasing plant hormones [122,124]. PGPR can increase nutrients uptake and development of AMF by affecting plant root colonization [55]. Bianciotto et al. [125] reported that Azospirillum and Rhizobium produce extracellular polysaccharides that improve bacterial strain’s attachment ability with AMF structures and plant roots. Kim et al. [126] suggested that co-inoculation of AMF and Methylobacterium oryzae is useful for plant growth, macro and micronutrients, chlorophyll content and root colonization. Artursson et al. [115] found that the binding strength of bacteria with the AM hyphae varies in different physiological stages of attachment. This is because, it is weak at the first stage and then became strong in the second stage. The possible reason for this might be the presence of some extracellular products or cellulose produced by the bacteria.

Moreover, the attachment of Gram+ve bacteria is more effective than G-ve bacteria with AMF [127]. Most PGPR, such as Bacillus sp. (Gram+ve) show positive interaction with AMF. Hameeda et al. [128] found certain plant growth-promoting bacteria, including fluorescent pseudomonads, nitrogen fixers and sporulating bacilli in soil, having a synergistic effect with AM fungi. Meyer et al. [129] found an increase in root colonization of subterranean clover by the combined application of PGPR with AMF.

The synergistic effects of PSB (Bacillus megaterium) and two AMF strains on maize growth in the presence of tribasic calcium phosphate positively affect maize colonization. The PSB population and maize biomass were found high only with the GA8 strain. The increase in PSB density might be due to the transfer of some photosynthates in the maize rhizosphere [130]. Rhizobium and AM fungi interaction increase the solubilization of rock phosphate in P deficient soils and consequently enhance the growth and yield of burgundy plants (Macroptilum bracteatum) under pot conditions [131]. The combined inoculation effect of two local phosphate solubilizing bacteria strains (Pseudomonas fluorescens BAM4 and Burkholderia cepacia BAM12) and AMF (Glomus etunicatum) on different growth parameters (dry shoot yield, root yield and leaf area) and nutrient uptake of wheat crop fertilized with tricalcium phosphate in P deficient soil significantly enhance the growth parameters and nutrient contents of wheat plants [132].

Similarly, the synergistic role of plant growth promoting rhizobacteria (PGPRs) such as Pseudomonas putida, Azotobacter chroococcum and Bacillus polymixa in combination with Glomus intradices increase root dry weight, shoot dry weight, nutrient contents (NPK), chlorophyll and stevioside (i.e., a glycoside) in plants under greenhouse conditions. The interactions of AMF (Funneliformis mosseae) and earthworms (Eisenia petidia) in the presence of insoluble phytate P enhance dry shoot and root biomass, P uptake, alkaline soil phosphates activities, microbial biomass P and soil available P. Moreover, the synergistic effects between these microbes also improve the phosphate activities and microbial biomass P and regulate the bacteria populations in soil [133]. Furthermore, the PSB strains (Bacillus sp. RM2 and Aspergillus niger S36) isolated from rhizosphere soil of Sesamum indicum and Vigna radiate significantly enhance chickpea growth as compared to single inoculation and control treatment, and can be used in the preparation of biofertilizers for sustainable agriculture [134].