Bio-solubilization of Rock Phosphate and Plant Growth Promotion by Aspergillus niger TMPS1 in Ultisol and Vertisol

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Bio-solubilization of Rock Phosphate and Plant Growth Promotion by Aspergillus niger TMPS1 in Ultisol and Vertisol Manoj Shrivastava and S.F.D Souza Nuclear Agriculture and Biotechnology Division Bhabha Atomic Research Centre Trombay, Mumbai-400085 India

Main Concern Related to Phosphorus Research Agricultural point of view Phosphorus requirement for sustainable crop production Environmental point of view Soil or fertilizer phosphorus contribution to eutrophication of aquatic environments

Facts P is an essential plant nutrient Global Rock Phosphate (RPs) Production >160 mmt (2008) Most RPs are not suitable for phosphatic fertilizer production due to low reactivity and impurities present in them Low-grade rock phosphate can be utilized as direct application P fertilizer with or without processing Application of rock phosphate in conjunction with phosphate solubilizing microorganisms

Soil Phosphorus Cycle Exportations in Plant and animal Products Mineral Fertilizers Aerial Parts Roots Organic fertilizers Inorganic P in primary minerals Other form of Inorganic P Inorganic P in the soil solution Microbial solubilization Labile Organic P Microbial P Stable Organic P Soil Plant System Losses by erosion, run-off, leaching

OBJECTIVES The overall objective of this study was to evaluate the efficacy of a fungus Aspergillus niger strain TMPS1 isolated from mangrove rhizosphere as phosphate solubilizing bio-fertilizer under greenhouse conditions using 32 p isotope dilution technique

Isolation of Fungus from Soil Soil: Rhizospheric soil of Mangrove Media: Pikovskaya s agar plates Formation of a clear halo around the fungal growth after 5 days of incubation

TMPS 1 Aspergillus niger TMPS1

Molecular Identification of Fungus DNA Isolation Amplification of 18S rrna gene (NS5 [5 -AACTTAAAGGAATTGACGGAAG-3 ] and NS8 [5 - CCGCAGGTTCACCTACGGA-3 ]) Cloning pt257r/t 18S rrna sequencing and sequence analysis M13 primer (TGTAAAACGACGGCCAGT) Isolates Length of ITS region Sequenced (bp) Identification by ITS region sequencing Gene identity (%) GenBank Accession no. TMPS1 560 Aspergillus niger 98 DQ316605

Radiotracers for phosphorus 32 P T 1/2 ----14.3 DAYS ß-EMITTER E max. ---1.71 MeV COUNTING 33 P T 1/2 ----25 DAYS ß-EMITTER E max. ---0.248 MeV COUNTING i) GM ii) Cerenkov or LSC i) LSC

Greenhouse experimental details CROP Wheat (Triticum aestivum) VARIETY PbW 343 SOIL 2 kg soil per pot Black soil (Vertisol) Red Soil (Ultisol) TREATMENTS Control (No P) Soil+ 32 P Soil+ TMPS1+ 32 P Soil + LRP+ 32 P Soil + LRP + TMPS 1+ 32 P Soil + PRP + 32 P Soil+ PRP+ TMPS 1 + 32 P EXPERIMENTAL DESIGN CRD REPLICATIONS 04 Activity applied 5 MBq 32 P kg -1 Soil

Characteristics of rock phosphates Rock phosphate Total P (%) Citric Acid Soluble P (%) Purulia (PRP) 14.4 1.623 Lalitpur (LRP) 9.8 0.425

PHYSICO-CHEMICAL CHARACTERISTICS OF EXPERIMENTAL SOIL Sr. No. Characteristics Value Vertisol Ultisol 1 Texture Clayey Sandy Clay 2 ph (1:2) (soil:water) 8.20 4.8 3 Free CaCO 3 (g kg -1 ) 36 ND 4 0.05M CaCl 2 Extractable Al ( mg kg -1 ) ND 2.58 5 Moisture equivalent (%) 32.0 30.0 6 Organic carbon (g kg -1 ) 5.10 20.4 7 CEC (C mol (P+) kg -1 ) 51.13 8 8 Total N (g kg -1 ) 0.6 3.9 9 Available P ( mg kg -1 ) 3.7 (Olsen s) 5.85 (Bray I) 10 P fixing capacity (g kg -1 ) 620 700

Parameters studied Dry matter yield -DMY (g pot -1 ) Total phosphorus uptake (mg pot -1 ) Specific Activity (Bq mgp -1 ) Phosphorus derived from lebeled soil (bioavailable P) and rock phosphate (mg pot -1 )

CALCULATIONS Total P uptake by plant (mg P Pot -1 ) U TP = DMY (mg Pot -1 ) X (% P/100) DMY- Dry matter yield of plant Specific Activity (Bq mg P -1 ) = Bq g -1 plant/mg P g -1 plant %PdfS -- Fraction of P in the plant derived from the soil % PdfS = SA in Plant (Bq/mg SA in plant (Bq/ mg P) in presence of RP 100 P) in absence of RP %PdfRP----Fraction of P in the plant derived from the rock phosphate %PdfRP = 1 SA in Plant (Bq/mg P) in presence of RP 100 SA in plant (Bq/ mg P) in absence of RP P uptake from labeled source (mgp Pot -1 ) = U TP X (%PdfS/100) P uptake from rock phosphate (mgp Pot -1 ) = U TP X (%PdfRP/100)

Vertisol Control PRP LRP PRP + TMPS1 LRP + TMPS1

Ultisol Control PRP LRP PRP + TMPS1 LRP + TMPS1

Effect of fungus inoculation on shoot dry matter yield and P uptake of wheat in ultisol and vertisol 4 Dry Matter Yield Vertisol Ultisol 3.5 3 g pot -1 2.5 2 1.5 1 mg Pot -1 5 P uptake Vertisol Ultisol 4 3 2 1 0.5 0 0 Control (No P) Soil+ 32P Soil+ TMPS1 Soil + LRP Soil + LRP +TMPS1 Soil + PRP Soil+ PRP+TMPS1 Control (No P) Soil+ 32P Soil+ TMPS1 Soil + LRP Soil + LRP +TMPS1 Soil + PRP Soil+ PRP+TMPS1

Effect of fungus inoculation on specific activity (Bq mgp -1 ) of wheat in ultisol and vertisol SpecificActivity Specific Activity Ultisol Vertisol Bq mgp -1 300 250 200 150 100 50 0 Soil Soil+ TMPS1 Soil + LRP Soil+ LRP +TMPS1 Soil + PRP Soil+ PRP+ TMPS1 Bq mgp -1 500 450 400 350 300 250 200 150 100 50 0 Soil Soil+ TMPS1 Soil + LRP Soil+ LRP +TMPS1 Soil + PRP Soil+ PRP+ TMPS1

Effect of fungus inoculation on percentage of P derived from soil and rock phosphates in ultisol Sr. No. Treatments PdfS Ultisol PdfRP % mgp pot -1 % mgp pot -1 1 Soil + LRP+ 32 P 90.4 0.932 9.6 0.100 2 Soil + LRP + TMPS 1 + 32 P 66.7 1.210 33.3 0.604 3 Soil + PRP + 32 P 95.3 0.906 4.7 0.045 4 Soil+ PRP+ TMPS1+ 32 P 70.3 1.063 29.7 0.449 LSD (P<0.05) 0.126 0.076

Effect of fungus inoculation on percentage of P derived from soil and rock phosphates in vertisol Sr. No. Treatments PdfS Vertisol PdfRP % mgp pot -1 % mgp pot -1 1 Soil + LRP+ 32 P 98.5 1.355 1.5 0.021 2 Soil + LRP + TMPS 1 + 32 P 81.1 3.338 18.9 0.778 3 Soil + PRP + 32 P 99.3 1.356 0.7 0.010 4 Soil+ PRP+ TMPS1 + 32 P 82.7 3.425 17.3 0.716 LSD (P<0.05) 0.825 0.095

Conclusions Potential use of Aspergillus niger TMPS1 isolate as a phosphate solubilizer in ultisol as well as vertisol. In general rock phosphates solubilization in alkaline vertisol does not occur, but this fungus solubilized native unavailable soil P as well as rock phosphate in vertisol. This study showed the advantages of using the 32 P isotope in distinguishing the contribution of bio-available native soil P and P from rock phosphates to P nutrition in plant microbe interaction. This fungus should be evaluated as bio-fertilizer under field condition in different agro climatic regions for different crops.

Acknowledgement BRIT, DAE for providing 32 P radioisotope Head, NABTD and Director BMG, BARC, Mumbai, India

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