The present invention relates to the field of sustainable agriculture. Specifically, the disclosure provides microbial compositions and methods useful for the optimal production of crop plants in the absence of synthetic nitrogen fertilizers or in the presence of synthetic nitrogen fertilizers applied at the rate of 30-50% less than needed. In particular, the compositions and methods disclosed herein are useful for enhancing plant growth in the complete absence of synthetic nitrogen fertilizers or in their much reduced presence.
The United States is, by far, the largest producer of corn in the world, producing as much as 35% of world's corn, 33% of world's soybean, more than 65% of world's sorghum and is the biggest wheat exporter (Ag 101, US EPA).
Nitrogen (N) is an essential plant macronutrient; of the three essential macronutrients (N, P, and K), nitrogen is required by plants in the greatest amount and its availability is a major factor limiting growth of plants in natural as well as in agricultural soils (Kraiser et al., 2011). A simplified view of the nitrogen cycle in soils is shown in
Nitrogen (N) is present in the biosphere in various chemical forms with molecular nitrogen gas (N2) representing 80% of its atmospheric composition (Sanhueza, 1982). Plants however, cannot directly use this form of N. Nitrogen therefore, enters the biological cycle as ammonia/ammonium (either via biological fixation i.e., prokaryotic conversion of N2 to ammonia or production of ammonia by the Haber-Bosch industrial fixation of N2 as mentioned above) and as atmospheric nitrate (Mannheim et al., 1995). Once N is fixed as nitrate or ammonia, it can have two main fates: (i) nitrate and ammonia can undergo biochemical processes that transform them back to N2 (Mannheim et al., 1995); or they can be reduced and/or assimilated for the biosynthesis of N-containing metabolites such as proteins/peptides. These metabolites (amino acids, urea, small polypeptides) and other N-containing biomolecules can then be released back to the environment by secretion, excretion, or by the decay of organic matter (Jones et al., 2005a).
Historically, the classical paradigm of the terrestrial N cycle has asserted that organic N must be converted into inorganic N (NO3—N, NH4—N) by soil microorganisms prior to becoming available to plant roots, and thus N mineralization (ammonification) has been viewed as the bottleneck in plant N nutrition (Warren and Adams, 2007). Therefore, synthetic N fertilizers applied to support crop growth have always been in the form of ammonium or nitrates.
Previous to the discovery of the Haber Bosch process almost 100 years ago to convert atmospheric N2 to NH3, food production was always limited by the ability to supplement soil nitrogen by crop rotation, leaving the soil fallow or applying manure. However, with cheap production of synthetic N fertilizers, anhydrous ammonia, urea, and urea ammonium nitrate (UAN)—widely used by the US farmers; synthetic N fertilizers have become ‘key’ to phenomenal increases in crop yields thus promoting agricultural intensification in the US and around the world.
This increase however, has come at a high cost to the environment. For example, Chesapeake bay, the nation's largest estuary is polluted from agricultural operations whose nitrogen (and P) runoff from the synthetic fertilizers applied to the farm fields fills the bay water causing eutrophication, fish kills, and proliferations of human pathogenic bacteria (www.gristorg, 2010*). In the gulf of mexico which drains the US heartland and the upper Midwest, a deadzone is produced almost the size of 5000-8000 sq. miles in the summer months impacting fisheries along the gulf's borders in Texas, Louisiana, Mississippi, Alabama, and Florida (www.gristorg, 2010*).
The Haber-Bosch process to convert N2 to NH3 requires high temperatures and pressures and is very energy intensive so much so that ˜1% of the global energy consumption is required to produce synthetic ammonia for N fertilizer. Therefore, there is a strong correlation between the price of natural gas and oil and fertilizer prices (www.gristorg, 2010*).
The US consumes nearly 12% of the global annual synthetic N fertilizer mostly from declining natural gas reserves and is going to be increasingly dependent on imports from foreign nations such as Trinidad and Tobago, Canada, Russia and Ukraine for its synthetic N fertilizer needs (www.gristorg, 2010*).
Currently, US is able to produce only 45% of its nitrogen fertilizer needs and is tightly consolidated by only 3 to 4 companies namely, CF industries, Terra, and Agrium that are also amongst the nation's largest environmental polluters (www.gristorg, 2010*). *http://www.grist.org/article/series/the-n2-dilemma-is-america-fertilizing-disaster
Of the applied N fertilizer, only 30-50% is actually taken up by plants. Recent research has shown that this over-application of synthetic N fertilizer although a quick fix for supplying plant needs also causes overgrowth of bacteria and fungi. According to one line of research, overgrowth of microorganisms in turn could potentially oxidize soil organic carbon critical to maintaining soil quality and the ability to retain soil N thus possibly priming the soils to need progressively more and more of the ‘same quick fix’ to maintain consistent crop yields (Mulvaney et al., 2006; Mulvaney et al., 2007; Khan et al., 2007; Mulvaney et al., 2009; Mulvaney et al., 2010a; Mulvaney et al., 2010b).
The over-application of N fertilizer also has significant adverse human health effects through leaching of nitrates in the ground water causing methemoglobinemia in infants and reacting with other chemicals in the body to produce N-nitroso compounds that have been linked to birth defects and cancer via model animal studies.
From the economic perspective, although the US currently leads the world in corn production, the portion of agricultural revenue returned to farmers decreased from 37% to 19% from 1950 to 2002 (Atwell et al., 2010). In addition, input costs increased sevenfold and the real price of corn adjusted for inflation decreased fivefold (Duffy, 2006).
All the above unequivocally show that corn production in particular and crop production in general is unsustainable from all perspectives, including environmental, soil quality, economic, and human health. Hence, invention for a sustainable, cost effective, and similarly reliable alternative to synthetic N fertilizers is critical to maintaining intensive agriculture, global food security, and mitigating the effects of global climate change.
The premise of applying synthetic N fertilizer as NH4+ and nitrate was based on the conventional wisdom that plants can take up nitrogen in only these forms. However, recent research has shown that in addition to taking up these inorganic forms of nitrogen, uptake of organic nitrogen in the form of oligopeptides and free amino acids is also a major uptake pathway in plants (Jones et al., 2005a; Jones et al., 2005b; Adamcyzk et al., 2009; Kraiser et al., 2011).
Although, historically, the classical paradigm of the terrestrial N cycle has asserted that organic N must be converted into inorganic N (NO3—N, NH4—N) by soil microorganisms prior to becoming available to plant roots, with N mineralization (ammonification) as the bottleneck in plant N nutrition (Warren and Adams, 2007) soil N is dominated by organic forms and approximately 40% of total soil N is present in the form of polymers such as proteins and peptides (Schulten and Schnitzer, 1997).
Recent research has shown that plants can indeed take up organic nitrogen when liberated from soil polymers such as amino acids bound in peptides and proteins (Jones et al., 2005a; Jones et al., 2005b; Adamcyzk et al., 2009; Kraiser et al., 2011). Several amino acid transporters have been identified in plants such as lysine-histidine transporter 1 (LHT1), amino acid permease 1 (AAP1), and amino acid permease 5 (AAPS) in the roots of Arabidopsis thaliana (Hirner et al., 2006; Lee et al., 2007; Svennerstam et al., 2008).
Plants can access N in soil proteins using proteases in root exudates (Paungfoo-Lonhienne et al., 2008). In addition, bacteria colonizing plant roots and known to have a beneficial effect on plant growth (referred to as PGPB aside from the bacteria that fix atmospheric N2) also exude extracellular enzymes such as phosphatases and proteases for respectively, P and N nutritional needs of plants (Kraiser et al., 2011; Ahearn et al., 1968; Gupta et al., 2002).
The de-polymerization of these compounds by enzymes such as proteases creates short peptides and free amino acids (Jamtgard et al., 2010). These free amino acid (FAA) reserves in soils are mostly higher than ammonium and nitrate and offer the largest and most reliable source of FAAs (Lipson and Näsholm, 2001). The bound amino acids (BAAs) for example those in proteins and peptides in soils were significantly higher than mineral-N in unfertilized soil solutions as shown in
Indeed field studies have shown evidence for direct uptake of amino acids by plants in diverse ecosystems such as Alaskan tussock tundra, boreal coniferous forest, heathland, subtropical rainforest, and agricultural land further underlining the importance of organic protein-N for plant nutrition (Kielland, 1994; Näsholm et al., 1998; Stribley and Read, 1980; Schmidt and Stewart, 1999; Jones and Darrah, 1994; Yamagata and Ae, 1996; Näsholm et al., 2001; Sauheitl et al., 2001). Direct uptake of N was also shown recently by Tida et al., (2009) in tomato seedlings using 15NH4Cl, K15NO3, 1, 2-13C2 15N-glycine labeling techniques. They found that the 13C and 15N increased significantly in tomato seedlings within 48 h after injection into the soil thus indicating that organic protein N-uptake by plants is very rapid (Tida et al., 2009).
Furthermore, Jones et al., (2005a) addressed the question of competition for amino acids between plants and microorganisms. Although molecules such as amino acids are excellent C and N sources for microbes, they can potentially out compete plant roots for free amino acids (Owen and Jones, 2001), and microbial capture of free amino acids (glycine in this case) is very rapid over a wide range of concentrations (0.1 μM-10 mM) interestingly enough plant uptake of N was maximized at high amino acid concentrations where the microbial utilization was slowest (Jones et al., 2005a).
These results indicate that protein-N can be utilized by plants rapidly in a major way for their nutritional needs in the presence of microorganisms competing for the same source of N (Jones et al., 2005a).
Endophytic bacteria colonize inner host tissues, sometimes in high numbers, without damaging the host or eliciting strong defense responses (Hurek, 2011). Prominent sites for active ingress into roots are the emergence points of lateral roots and to some extent the zone of differentiation and elongation near the root tip, where slightly disrupted or not completely differentiated tissues may facilitate penetration. Intercellular spaces in the epidermal and cortical regions and lysed plant cells are major sites of colonization, with locally high cell densities of up to (10)10 cells/cm3 (Chi et al., 2005).
Proteases are a type of extracellular depolymerases; they are released by microorganisms via three known mechanisms; i) substrate induction, ii) end-product repression or de-repression due to insufficient nutrient supply and iii) constitutive production of small amounts (Geisseler et al., 2010). Protease enzymes catalyze amide hydrolysis breaking the peptide bond and releasing individual amino acids via a proton transfer reaction (Karaman, 2011). They can therefore hydrolyze large proteins into peptides and amino acids with wide substrate specificities and can degrade most non-structural proteins (Geisseler et al., 2010).
Production of extracellular proteases is induced by the presence of substrate i.e., proteins in the medium while the presence of easily metabolizable C end products may repress enzyme production (Kalisz, 1988; Haab et al., 1990; Allison and Macfarlane, 1992). Given the abundant presence of protein organic N in soils and applied animal based manures, the microbial propensity to exude proteases, and the ability of plants to take up peptides and free amino acids we hypothesize the following pathway to supply plants N needs (see
Although bacteria can colonize plants both epiphytically i.e., plant rhizosphere and endophytically in the plant apolplasts, selected endophytic bacteria because they live within the plant and can therefore recover more easily from stressful situations (Kozyrovska et al., 1996). In addition, being away from the natural biocenosis gives them a significant edge in competing with the native soil bacteria (Kozyrovska et al., 1996).
Although both bacteria and fungi produce proteases, we selected bacteria because they generally outnumber their fungal counterparts by 2-150 fold (Hilda and Fraga, 1999). In our quest for selecting the suitable organic (protein) nitrogen solubilizing bacteria we screened endophytic bacteria isolated from natural plant samples and screened them for protease production.
The proposed embodiment pertains to the development of biofertilizer consisting of protease producing endophytic bacteria (BioCat-N) inoculated crop seeds as an environmentally sustainable, and cost-effective alternative to synthetic N fertilizers and as a means of increasing the efficacy of synthetic fertilizers.
Animal manure is rich in valuable macro and micro nutrients and also supplies organic matter to improve the soil's physical and chemical properties and is used in exclusion to synthetic fertilizers in organic farming.
Nitrogen in manure mainly occurs in three forms -organic, ammonia/ammonium, and nitrate of which organic N is the predominant form of N in manure (http://www.poultrywaste.okstate.edu/files/f-2228web.pdf). Similar to organic nitrogen in soils, organic nitrogen in manure also retains the potential to be depolymerized into free amino acids and oligopeptides.
Although the nutrient content of animal manure varies based on method of collection and storage, and animal species, an average nutrient content of manure is summarized in Table 1.
The object of the purported invention is to develop a biocatalyst (BioCat-N) consisting of organic N solubilizing endophytic bacteria that colonize the root and shoot of plants at sufficient inoculum density so as to facilitate adequate dissolution of organic N into oligopeptides and free amino acids that can be taken up readily by plants.
The purported invention will work by inoculating crop seeds with endophytic bacteria primed to release protease an enzyme that depolymerizes proteins and peptides to free amino acids and oligopeptides. A particular advantage of endophytic bacteria is that they do not need to compete with native soil bacteria; they should therefore be able to degrade and depolymerize the proteinaceous organic nitrogen in soils and in soil amendments (e.g., manure) in the vicinity of plant roots thus releasing free amino acids and oligopeptides for the N nutritional needs of the plant.
BioCat-N is thus purported to increase organic nitrogen availability and uptake by crops be it in fertilized or unfertilized soils.
At Biomineral Systems, we have conducted experiments with corn and sorghum and show evidence of plant growth on poultry manure alone in the complete absence of ammonium and nitrate that exceeded growth of plants growth with NH4+ and nitrate similar to synthetic fertilizers. Because of the novelty of this discovery, to the best of the inventor's knowledge no products exist that has been scientifically designed to effectively, efficiently and reliably harness this poultry manure a rich source of organic N for plant uptake and supplying the plant's nutritional needs.
Endophytic phosphobacterial selection and preliminary evaluation as potential phosphate solubilizing biocatalyst for two crops corn and sorghum is complete.
The identity of this bacterial strain is not revealed to maintain propriety until suitable patents have been filed to protect IP.
The preferred embodiment has been evaluated in crop systems in hydroponic, simulated soil systems, and real soils.
The preferred embodiment has included isolation of protease producing endophytic bacteria from plant samples of corn, sorghum, and sugarcane.
Further, the preferred embodiment has involved determining inoculation efficacy of the isolated endophytic bacteria by determining inoculum density in root and shoot of corn and sorghum.
Further, the preferred embodiment has involved using nitrogen deficiency symptoms, root/shoot ratio, and chlorophyll content measurements and demonstrating that corn and sorghum seeds inoculated with selected N solubilizing endophytic bacteria grown with insoluble organic-N species present in soils such as poultry manure performed as well or better than non-inoculated control seeds grown with full strength Hoagland solution containing dissolved inorganic nitrogen.
Fresh samples of corn, sorghum, and sugarcane plants were acquired and washed in tap water. The roots and shoots from each plant was separated. The roots and shoots were separated and chopped. They were then surface sterilized to eliminate any epiphytic bacteria and to facilitate isolation of only endophytic bacteria. The samples were then ground to isolate endophytic bacteria. Endophytic bacteria isolated from corn plants included T4, T6, and C8. Endophytic bacteria isolated from sorghum plants included J-1, J-2/1, J-2/2, J-3/1, J-3/2, J-3/3, and J-4. Endophytic bacteria isolated from sugarcane plants included S-1/1, S-1/2, S-5, S-7, and S-8.
Acid protease assay: Protease activity was determined using the modified Anson method as described in Hashimoto et al., (1973). Briefly, reaction mixture was prepared by combining 1 ml of enzyme solution and 5 ml of bovine casein in 0.05 M acetate buffer (pH 2.5) and incubated at 30 degree C. for 10 minutes. Five ml of 0.11 M trichloroacetic acid was added to stop the reaction. The reaction mixtures was filtered after incubation at 30 degree C. for 30 minutes. Five ml of 0.55 M sodium carbonate was added to 2 ml of the filtrate followed by the addition of 1 ml of thrice diluted phenol reagent. Acid protease activity exuded by endophytic bacteria was quantified based on the concentration of tyrosine measured at 660 nm.
Alkaline protease assay: Alkaline protease activity was determined according to the procedure of Smita et al., (2012). The assay medium (50 ml) containing nutrient broth and 1% casein at pH 10 was inoculated with each isolate and incubated at 37 degree C. for 48 hrs in a water bath shaker. After incubation, the broth cultures were centrifuged at 10,000 rpm for 10 minutes at 4 degree C. and the supernatant was collected to determine the activity of alkaline protease. The activity of alkaline protease was determined similar to the procedure described above for acid protease by measuring the release of tyrosine at 280 nm. The main difference was that the pH was adjusted to pH 10 instead of 2.5 by addition of Glycine-NaOH buffer.
Because Acid-protease are very effective at the common soil pHs we selected J2/2 an endophytic bacteria isolated from sorghum and tested its inoculation efficacy in corn and sorghum.
The inoculum for endophytic bacteria was grown under controlled conditions for 48 hrs to inoculum density of 108 to 1010 cfu/ml. The inoculum was centrifuged and suspended in sterile PBS to a concentration of 108 cfu/ml. The seeds were surface sterilized with 95% ethanol for 2 min and 2.5% sodium hypochlorite for 20-30 min followed by washing seven times in sterile water. Surface sterilized seeds were soaked in sterile PBS containing endophytic bacteria and placed in a temperature controlled incubator shaker at 25 degree C. for exactly 30 minutes. The inoculated seeds were washed with 70% alcohol for 2 minutes and with 2% sodium hypochlorite followed by washing with sterile water 5 times. The surface sterilized seeds were placed in sterile petriplates containing 0.7% of water agar, 5-10 seeds per plate. The seed containing plates were transferred to growth chamber set at 30 degree C. and left for 48 hours to germinate. Well germinated seeds with shoot and roots were separated and surface sterilize with 95% of ethanol for 5 min and 20 min with 4% sodium hypochlorite followed by 4-5 times sterile water rinse. The water rinsed root and shoot parts were transferred to PBS containing solution and ground to rapture the tissue. 1 ml of ground tissue was diluted in 9 ml of sterile water serial dilutions were continued to obtain 100 and 1000 fold dilution and spread on nutrient agar plates. After growth the colonies were counted and tabulated. Non-inoculated seeds served as negative controls.
Based on the amounts of protease production J3/1 and J2/2 were selected for testing their inoculation efficacy in corn and sorghum. Because J3/1 linoculum density measurements in roots and shoot replicates showed wide variability, J2/2 was chosen as the protease producing strain for further experiments. The non-inoculated control seeds showed zero inoculum density in the root and shoots.
Standard Hoagland solutions (hydroponic nutrient solutions) were prepared according to the composition in (ref) and contained Ca(NO3)2.4H2O, NH4NO3, KCl, KNO3, Mg(NO3)2.6H2O, KH2PO4, Fe(NO3)3.9H20, Na HEDTA, MnCl2.4H2O, H3BO3, ZnSO4.7H2O, CuSO4.5H2O, and Na2MoO4.2H2O. The young corn seedlings cannot tolerate full strength Hoagland solution. Hence ½ strength Hoagland solution was used from VE to V1 vegetative stage. The plants were grown until V3 vegetative growth stage because nitrogen deficiency symptoms can be observed during V1 to V3 growth stage. Nitrogen deficient Hoagland solution was prepared by eliminating all sources of nitrates and ammonium nitrogen and contained CaCl2.2H2O, KCl, K2SO4, MgCl2.6H2O, KH2PO4, FeCl3.6H2O, Na HEDTA, MnCl2.4H2O, H3BO3, ZnSO4.7H2O, CuSO4.5H2O, and Na2MoO4.2H2O. Poultry manure was added at the rate of g/L.
The viable inoculated seeds were placed in a muslin cloth and washed with running tap water and dried by placing on autoclaved tissue paper. The seeds were surface sterilized in laminar flow hood with 70% alcohol for 30 minutes and then by washing with 10% sodium hypochlorite solution for 20 minutes. After surface sterilization, the seeds were washed with sterile water, excess water removed by blotting with autoclaved tissue paper, and then air dried under laminar flow. Five to ten surface sterilized and dried seeds were then placed in sterile petriplates containing water soaked blotting paper and transferred to growth chamber maintained at 25-27 degree C. and left for 48 hours to germinate. After seeds germinated, they were transferred to hydroponic reactors. Hydroponic reactors constituted of root permeable plastic buckets. Air pump with air controllers were used to provide aeration to the plants in hydroponic systems and all systems were maintained under greenhouse conditions at a temperature of 24±2 degree C. and relative humidity of 70±3%. After control plants showed nitrogen deficiency symptoms, the plants were removed from hydroponic reactors and washed under running tap water to completely remove Hoagland solution. The plant was dried with blotting paper while taking care to not damage the roots.
Reduced leaf area and degradation of chlorophyll in leaves is symptomatic of nitrogen deficiency so we measured chlorophyll a and chlorophyll b in plants. A single leaf per plant was used for obtaining 10 leaf discs of 1 cm each and weighed. Five of these leaf discs were placed per tube containing 5 ml of 1:1 ratio of DMSO:acetone and the tubes were placed in the dark overnight to allow chlorophyll leaching. After chlorophyll leaching the solution turns green and the concentration of chlorophyll in leaves is calculated by measuring absorbance at 645, and 663 nm. The total chlorophyll is estimated using the following formulae:
Chlorophyll II a (g/l)=0.0127 A663−0.00269 A645
Chlorophyll II b (g/l)=0.0029 A663−0.00468 A645
Total Chlorophyll (g/l)=0.0202 A663+0.00802 A645