Isolation,
Identification and Molecular Characterization of Phosphate Solubilizing
Actinomycetes Isolated From The Coastal Region of Manora,
Thanjavur (Dt.)
Kaviyarasi K.1,
Kanimozhi K.1, Madhanraj
P.2, Panneerselvam A.1 and *Ambikapathy V.1
1Department of Botany and
Microbiology, A.V.V.M.Sri Puspham
College [Autonomous], Poondi-613 03, Thanjavur, Tamil
Nadu, India.
2Dept of Microbiology, Thanthai
Hans Roever College of Arts and Science, Perambalur - 621 212, Tamil Nadu, India.
*Corresponding Author E-mail: drva1967@yahoo.com
ABSTRACT:
The
soil sample was collected from Manora. After analysing the physic-chemical parameters of the collected
marine soil sample, ten actinomycetes species
including Actinobispora yunnanensis, Streptomyces albus,Micromonospora
echinospora, Saccharopolyspora
hirsute, Streptomycetes cyaneus,
Actinomadura citrea, Saccharomonospora viridis, Thermomonospora mesophila, Streptoverticillium album Microtetrospora
fastidiosa were isolated and they were screened
for phosphate solubilization using Pikovskaya’s agar medium and the Actinobispora yunnanensis
was found to be dominant in phosphate solubilization.
Then the DNA of the Actinobispora yunnanensis was
isolated, amplified and its 16S rDNA was sequenced
and its secondary structure was also predicted.The phylogenetic analysis of the Actinobispora yunnanensis was also carried out.
KEYWORDS: Phosphate, phosphate solubilization, 16S r DNA, Actinobispora yunnanensis
INTRODUCTION:
Actinomycetes
are prokaryotic spore forming, gram positive bacteria that have DNA with high
GC content (69 – 73%). Their filamentous nature, branching pattern and conidia
formation are similar to those of fungi for the reason they are known as ray
fungi. The spore size and spore characters are similar to bacteria. They are
widely distributed in terrestrial soil, cultivable lands, marine soils,
compost, fresh water basins and foodstuffs and beneficial effects should be
manipulated according to our use. The name actinomycetes
were derived from Greek akits ‘a ray’ and ‘mykes’ (fungus). Like fungi they form a mycelial
new work of known as branching filamentous, conidia formation and are known as
‘ray fungi’. But like bacteria they have prokaryotic nuclei and are susceptible
to antibacterial antibiotics. They are characterized by the formation of aerial
and substrate mycelium.
Several
antibiotics have been isolated from marine actinomycetes
by many researchers. The antibiotics are entirely new and unique when compared
to those from the terrestrial ones. Streptomyces, have been studied as potential procedures of metabolites
with diverse chemical structures and biological activities. Tens of thousands
of such compounds have been isolated and characterized many of which have been
developed into drugs by treatment of wide range of human disease. Thus
searching for novel actinomycetes constitutes on
\essential component in natural product based drug discovery (Wang et al., 1991).
Phosphate Solubilizers:
Microbes
which solubilize the bound phosphate and rock phosphate
into simple phosphate are called phosphate solubilizers.
They secrete organic acids such as formic acid, lactic acid, succinic acid, propionic acid,
hydroxyl acid to solubilize the bound phosphate in
the soil. The simple phosphates are readily available for the plants.The most essential function of phosphate in plants
is in energy storage and transfer of adenosine di and
tri phosphate(ADP and ATP) act as energy currency
within the plants.
MATERIALS AND
METHODS:
Sample collection:
The soil sample was collected from Manora at Thanjavur Dt., Tamil
Nadu, India. Then it is brought to the laboratory in a
sterile manner, which was then thoroughly mixed and dried.
Analysis of Physico-chemical
characteristics of the soil:
Moisture
content was estimated by finding the weight difference of known quantity of the
soil before and after drying in a hot air oven at 60°C for 6 hours. Soil
samples after removing the debris were suspended in distilled water (1:2 w/v)
and allowed to settle down the sand particles. The pH of the suspension was
read using pH meter (Systronics, India), to find out
the soil pH.
Electrical
conductivity of soil was determined in the filterate
of the water extract using Conductivity bridge as
described by Jackson (1973), cation exchange capacity
(CEC) of the soil was determined by using 1N ammonium acetate solution as
described by Jackson (1973).
Organic
carbon content was determined by adopting chronic acid-wet digestion method as
described by Walkley and Black (1934), available nitrogen was estimated by alkaline permanganate
method as described by Subbiah Asija
(1956) and available phorphorus by Braylk method as described by Bray and Kutz
(1945). Available potassium was extracted from soil with neutral 1N ammonium
acetate (1:5) and the potassium content in the extract was determined by using
flame photometer (Standfold and English, 1949),
Calcium (neutral 1 N NH4 OAC extractable 1:5) was extracted with
neutral 1N ammonium acetate and the available calcium in the extract was
determined by Versenate method (Jackson, 19973).
Available micronutrients such as Zn, Cu and Mn were
determined in the diethylene triamine
penta acetic extract of soil using Perklin-Elmer model 2280 Atomic absorption
spectrophotometer (Lindsay and Norwell, 1978). Other nutrients such as
magnesium, sodium and available iron were analysed
following the method of Barnes (1959) and Muthuvel
and Udayasoorian (1999).
Isolation of actinomycetes:
Isolation of actinomycetes was performed by
plating technique using Starch Casein agar(Kuster and Williams.,1964) medium. The medium was prepared
and sterilized at 121°C in 15Ibs pressure for 15 minutes. Then it was
supplemented with Streptomycin (30µg) and griseoflavin
(50 µg) to prevent the bacterial and fungal growth in the medium. The medium
was poured into sterile petriplates. The collected
soil Samples were diluted upto 10-6 and
0.1ml of the dilution sample were spreaded over the
agar plates. The inoculated plates were incubated at 28±2°C for 7-10 days.
After incubation actinomycetes colonies were observed
on the medium and these colonies were used for the further investigation.
Purification of actinomycetes:
Streak plate method was used to purify the culture of actinomycetes. After inoculation plates were incubated at
28±2°C for 7-10 days. The starch Casein agar was used to purified
the actinomycetes and stored at 4°C for further
investigation.
Table 1: Soil samples analytical report
S. No |
Name of the parameter |
Analytical values |
1. |
pH |
7.56 |
2. |
Electrical
conductivity (dsm-1) |
0.26 |
3. |
Organic
carbon (%) |
0.29 |
4. |
Organic
matter (%) |
0.58 |
5. |
Available
Nitrogen (Kg/ac) |
89.6 |
6. |
Available
Phosphorus (Kg/ac) |
5.26 |
7. |
Available
Potassium (Kg/ac) |
175 |
8. |
Available
Zin (ppm) |
0.87 |
9. |
Available
Copper (ppm) |
0.56 |
10. |
Available
Iron (ppm) |
4.69 |
11. |
Available
Manganese (ppm) |
2.45 |
12. |
Cat
ion exchange capacity (c. Mole. Proton- /kg) |
22.6 |
Exchangeable bases (c. Mole. Proton- /kg) |
||
13. |
Calcium |
12.4 |
14. |
Magnesium |
10.6 |
15 |
Sodium |
1.69 |
16 |
Potassium |
0.19 |
Characterization of actinomycetes:
Colony characterization:
Colony morphology was recorded with respect to colour
aerial mycelium, size and nature of colony, reverse side and pigmentation.
Microscopic characterization:
Actinomycetes culture plates were inserted at an angle of 45°. The actinomycetes was
slowly released at the intersection of medium to the cover slip. The plates
were incubated at 28±2°C for 4-8 days. The cover slips were removed from the
cultured medium and observed under the microscope. The photomicroscopy
was taken using Nikon microscope. The morphological features of spores,
sporangia, aerial and substrate mycelium was observed and recorded among the
isolates, predominant organisms were selected for further studies.
Identification of actinomycetes:
The isolated actinomycetes were identified by
using the gram’s staining, motility, and bio- chemical tests by using standard
manuals.
Screening of phosphate solubilizing Actinomycetes:
The identified 10 Actinomycetes cultures were spot inoculated on Pikovskay’s medium (pH 6.8 – 7.8) containing 5 gm of tricalcium phosphate as sole phosphorus source for
selectively screening the actinomycetes, which have
the ability to release inorganic phosphate from tricalcium
phosphate. The inoculated Pikovskay’s plates were
incubated at 28 ±2°C for 4 to 5 days. After the completion of the incubation
period, the plates were observed for the presence of clear zone around the
colonies the transport zone around the microbial colonies indicate the extent
of phosphate Solubilization (Sandara
Rao and Sinha et al., 1963).
Table 2: Biochemical
characterization of actinomycetes
S. No |
Microorganisms |
Test |
|||||||
GS |
I |
MR |
VP |
Citrate |
Catalase |
Urease |
Nitrate |
||
1 |
Actinobispora yunnansis |
+ |
- |
+ |
- |
+ |
+ |
+ |
- |
2 |
Actinomadura citrea |
+ |
+ |
+ |
- |
+ |
- |
+ |
+ |
3 |
Microtetrospora fastidiosa |
+ |
+ |
+ |
+ |
+ |
- |
+ |
+ |
4 |
Micromonospora echinospora |
+ |
- |
- |
- |
+ |
- |
+ |
+ |
5 |
Saccharomonospora viridis |
+ |
+ |
+ |
- |
+ |
+ |
+ |
+ |
6 |
Saccharopolyspora hirsute |
+ |
+ |
- |
- |
+ |
- |
+ |
+ |
7 |
Streptomyces albus |
+ |
+ |
- |
- |
+ |
- |
+ |
+ |
8 |
Streptoverticillium album |
+ |
- |
- |
- |
+ |
+ |
- |
- |
9 |
Streptomyces albus |
+ |
+ |
- |
- |
+ |
+ |
+ |
+ |
10 |
Streptomyces cyaneus |
+ |
+ |
- |
- |
+ |
+ |
+ |
+ |
GS-Gram staining, I-Indole, MR-Methyl red, VP-Voges proskauer
(+) Positive; (-) Negative
Molecular characterization of Actinobispora ynnanensis
Isolation of chromosomal DNA (Wilson,
1990):
Isolates of Actinobispora ynnanensis
were grown upto the late exponential phase in starch
casein broth at 28 ±2°C, washed twice with Tris EDTA
buffer or 10.3% sucrose prior to DNA preparation chromosomal DNA was isolated
by resuspending 0.5 – 1.09 of cells with 15 ml lysis buffer (25mM Tris: 25mM
EDTA, pH-8.0: 10-15mg lysozyme, 50µg/ml RNAse) and incubated for 30 – 80 min at 37°C followed by
addition 500µl of 5M NaCl solution. The suspension
was agitated on a vortex mixer until the cell suspension became translucent.
Cells were lysed by the addition of 1.2ml of 10% SDS.
They lysates of were incubated for 15 – 30 min at
65°C. After addition of 2.4 ml of 5M potassium acetate, the solution was mixed
and left on ice for 20 min. The precipitate was removed by centrifugation for
30 min. at 6000 rpm and the volume of supernatant was adjusted to 8 ml. The DNA
was recovered by precipitation was dissolved in 700 µl/g of 50mM Tris /10mM EDTA (pH 8.0). Any insoluble substances were
spun off and the aqueous phase was transferred to a 1.5ml microfuge
tube. Subsequently, 75µl 3M sodium acetate and 500µl isopropanol
were added and the solution was centrifuged for 30 seconds to 2 min. The
precipitate was washed with cold 70% ethanol, dried and dissolved in 100 µl TE
(10mM tris/ 1mM EDTA pH 8.0).
PCR amplification of 16S rDNA (Weisburg et al., 1991):
A mixture of sterile deionized
water 49 ml upstream primer (100 pmols) 10µl (5/
AGAGTTGATCCTGGCTCAG 3’). Down stream primer (100pmds) 10µl (5’ –
AGGGCTACTACCTTGTTACGACTT-3’) 10X PCR buffer 25mM,
Mgcl2 8µl, dNTP mix 6 µl, Streptomyces template DNA (50 nq),
5 µl and Taq DNA polymerase (30/ µl), 2 µl in a 0.5
ml micro centrifuge tube was taken. The total 100 µl mixture in a tube was
gently span for 10 sec and allowed to settle the contents. The samples were
kept in eppendrof PCR Thermal cycler. The
amplification was carried out in the following manner of 35 cycles, denaturation for 60 sec at 92°C, primer annealing for 60
seconds at 54°C and polymerization for 90 sec at 72°C. Finally the tubes were
ensured complete polymerization at 72°C for 15 min. 10µl of PCR products with 2
µl of loading dye was mixed and loaded on a 1.2% agarose
gel and analysed electrophoretically
at 60 volts for 45 min. The gel was observed on UV transilluminator
and compared with 1kb DNA ladder.
16S rDNA
sequencing:
The PCR products were purified using micron PCR centrigual
filter device (Millipore crop. Bedford Hass) and sequenced using the facility
at macrogene (Seoul, Korea).
Nucleotide sequence accession:
The 16s rDNA sequence for the
Actinobispora
ynnanensis have been deposited in Gene Bank http://www.nebi.nlm.nih.90v/gene
bank
The reference sequences required for comparison were down loaded from
the EMBL database using the site http://www.nebi.nlm.nih.90v/gene bank. All the
sequence were aligned using the multiple sequence alignment program CLUSTAL X . The aligned sequences were then checked for gaps
manually and arranged in a block of 250bp in each row and saved as an format in
software MEGA v 2.1- the pairwise evolutionary
distances were computed using the Kimura(1980). To obtain the confidence values
the original data set was resampled 1,000 times using
Boot strap. The program of PHYLOGENY and subjected to
bootstrap analysis. The bootstrap analysis. The
bootstrap data set was used directly for constructing the phylogenetic
tree using the MEGA program or used for calculating the multiple distance
matrix obtained was then used to construct phylogenetic
trees using Neighbour-joining method of Saitou and Nei (1987). All these analysis were performed using the
MEGA v2-1 (Kumar et al., 2007).
16S rDNA
Secondary structure prediction of Actinobispora ynnanensis:
The secondary structure of (Actinobispora ynnanensis) was predicted using the bioinformatics
tools available online www.genebee.msu.sul services/rna2 reduced- html.
Restriction site analysis in 16S rDNA of Actinobispora ynnanensis:
The restriction sites in 16S rDNA of Actinobispora ynnanensis
were analysed using NEB culture programme
version 2.0 tools in online www.neb.com/NEB cutles
2/index.php.
Table 3: Phosphate solubilization
of actinomycetes
S. No |
Name of the organisms |
Zone of clearance (mm in diameter) |
1. |
Actinobispora yunnanensis. |
32 |
2. |
Actinomodura citrea |
-- |
3 |
Microtetrospora fastidiosa |
_ |
4. |
Micromonospora echinospora. |
18 |
5. |
Sacchromonospora viridis |
15 |
6. |
Saccharopolyspora hirsuta |
12 |
7. |
Streptomyces albus |
- |
8. |
Streptoverticillium album |
12 |
9. |
Streptomyces cyaneus |
- |
10 |
Thermonospora mesophila |
12.5 |
RESULTS AND
DISCUSSION:
Physico-chemical analysis
of the soil sample:
Physically, the texture of the soil sample was sandy loam. The physico-chemical parameters such as pH (7.56), Electrical
conductivity (0.26 dsm-1), organic carbon (0.29%), organic matter
(0.58%), Available nitrogen (89.6 kg/ac), available phosphorus (5.26 kg/ac),
available potassium (175 kg/ac), available zinc (0.87ppm), available copper
(0.56 ppm), available iron (4.69 ppm),
available manganese (2.45 ppm), cation
exchange capacity (22.6 C. mole proton + kg), calcium (12.4), magnesium
(10.6), sodium (1.69), potassium, (0.19) were recorded from the soil sample of
coastal area Manora, Thanjavur
(Dt).
Isolation of Actinomycetes from marine
soil sample:
By
direct plating 10 species of actinomycetes were
isolated from marine soil sample. The isolated actinomycetes
were Actinobispora yunnanensis, Actinomodura citrea, Microtetrospora astidiosa, Micromonospora echinospora, Sacchromonospora viridis, Saccharopolyspora
hirsute, Streptomyces albus,
Streptoverticillium
album, Streptomyces cyaneus,
Thermonospora mesophila.
Screening of phosphate solubilizing Actinomycetes:
Detection of the phosphate solubilizing
ability of microorganisms have been possible using
plate-screening methods (Pikovskaya, 1948). Phosphate
solubilizing microorganisms produce clearing zones
around the microbial colonies in the Pikovskaya’s
medium, a specific medium for the isolation of phosphate solubilizers.
The production of clearance zones is due to the microbes
ability to solubilize the insoluble mineral
phosphates such as tricalcium phosphate or hydroxyapatite present in the medium. Among the screened 10 species
of actinomycetes,
Saccharomonospora hirsute and Streptomyces, cyaneus,
Actinomadura citrea, Microtetrospora fastidiosa have
no phosphate solubilizing activity.
The maximum zone of clearance was found with the Actinobispora yunnanensis (32 mm) compared to that of
the Micromonospsora echinospora
(18 mm), Sacchraromonospora viridis Saccharopolyspora hirsute, (12mm), Thermonospora mesophila (12.5mm) and streptoverticillium album,(12mm).
These results coincide with that of Ayyakkannu and Chandramohan,
1970a, who reported about the occurrence and distribution of phosphate solubilizing micro organisms in the natural marine
environment. They also stated that, among the different microbes, bacteria are
the potential candidates for dissolving the insoluble organic and inorganic
phosphorus compounds.
Molecular characterization of Actinobispora yunnanensis:
The molecular charecterization of Actinobispora yunnanensis
was evaluated by PCR amplification of 16S r DNA gene .the genomic DNA and
amplified produts were separated in agarose gel.The 16S r DNA genes
of Actinobispora
yunnanensis from the marine soil was partially
sequenced using 16 S r DNA sequence primer(3’TGC CAG CGG CGG
TAA TAA 5’- forward primer and 5’ CCG CCG ACG ACG TCT TTA 3’ reverse
primer).The sequence of Actinobispora yunnanensis
16 S r DNA was deposited in NCBI to get the accession number. The sequence
comparisons with sequences in the EMBL data base, the phylogenetic
analysis (neighbour joining tree) revealed that the
sequence of the marine isolate is Actinobispora yunnanensis
similar (98%) to the existing uncultured Actinobispora yunnanensis
ncd90h09c1 and it has a lesser percentage of similarity with and Actinobispora yunnanensis
sp.J31 strain.
The secondary structure of 16S r DNA of Actinobispora yunnanensis showed 33 loops, 33 stems
and 24 hairpin loops(Fig- 4).The restriction sites found in B.epidermidis was
shown in figure
1 to 3.Totally 155 restriction enzyme sites were observed. The GC
and AT content of Actinobispora
yunnanensis was found to be 56% and 44%
respectively, using NEB cutter programmeV2.0 in WWW.neb.com/neb cutter 2/
index.php.
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Received on 11.10.2011 Accepted on 20.11.2011
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