Literature DB >> 30656204

Metagenomic data of vertical distribution and abundance of bacterial diversity in the hypersaline sediments of Mad Boon-mangrove ecosystem, Bay of Bengal.

Balamurugan Sadaiappan1,2, Chinnamani Prasannakumar1, Kumaran Subramanian1, Mahendran Subramanian2.   

Abstract

Bacterial diversity studies in hypersaline soil often yield novel organisms and contribute to our understanding of this extreme environment. Soil from Mad Boon is previously uncharacterized, with dense mangrove forest in one side and hypersaline soil in another side of backwater located in Southeast coast of Tamil Nadu, India. We surveyed to characterize the structure and diversity of the bacterial community. Samples were collected in a partially vegetated upland, exposed backwater sedimentation and water-logged location. In this study, we investigate the bacterial community structure using pyrosequence analysis of the V5- V9 gene region. After quality checks a total of 3919, 7298 and 7399 reads were obtained. About 42 phyla were observed, among them Proteobacteria were dominant phylum followed by Acidobacteria, Firmicutes and Chloroflexi. Classes including Deltaproteobacteria and Gammaproteobacteriawere observed. All sequences generated in this study were submitted to NCBI SRA under the accession numbers SRR627695, SRR63011 and SRR631012.

Entities:  

Year:  2018        PMID: 30656204      PMCID: PMC6329363          DOI: 10.1016/j.dib.2018.12.028

Source DB:  PubMed          Journal:  Data Brief        ISSN: 2352-3409


Specification table Value of the data Comparison between the microbial community from different types of hypersaline sediments and this data to identify the core community is possible. This data is useful for comparison of saline and freshwater bacteria communities. Data could aid restoration of the bacterial community near the coastal regions for the agricultural process. The raw sequence data would allow other researchers to do their analyses with different bioinformatics tools.

Data

The 16S rRNA amplicon Pyrosequencing (TEFAP, Tag-encoded amplicons Pyrosequencing) produce 5890, 13959 and 10006 sequences. After quality checks (i.e. < 250 bps lengths were removed) a total of 3919, 7298 and 7399 reads were obtained. The raw sequence can be accessed from NCBI SRA using the accession numbers SRR627695, SRR631011 and SRR631012. The phylum Proteobacteriawas found to dominate all the three hypersaline layers followed by Acidobacteria, Chloroflexi, Bacteriodetes and other phyla (Fig. 1). The difference in the bacterial communities was seen even in class (Fig. 2), order (Fig. 3), family and genus level (SupplementaryData Table 1 and Supplementary Data Table 2 respectively), Diversity richness Shannon and cho1 index (Table 1).
Fig. 1

The abundance of bacterial community at the Phylum level.

Fig. 2

The abundance of bacterial community at the Class level.

Fig. 3

The abundance of bacteria community at the Order level.

Table 1

Hypersaline bacterial diversity, richness derived from multiple diversity estimators for individual sediment samples 3%, OTUs, Shannon and Chao1 index of the samples.

Vertical Location Sample IDSequence libraryNumber ofShannonChao IACE
sizeOTUsa(H’)richness
HS1391911646.487031,436.811436.81
HS2702616456.724011,950.661886.87
HS3737715476.649781,843.671547
The abundance of bacterial community at the Phylum level. The abundance of bacterial community at the Class level. The abundance of bacteria community at the Order level. Hypersaline bacterial diversity, richness derived from multiple diversity estimators for individual sediment samples 3%, OTUs, Shannon and Chao1 index of the samples.

Experimental design, material and methods

Sample collection

The study was conducted in Mad Boon (Pichavaram), South India, Bay of Bengal in a natural area, located at Latitude 11 °25’.01 N; Longitude 79 °47’ 06.39” E in September 2012. The sample was collected in a single location using 10.5 cm wide and 40 cm height corer. The top 0–30 cm sediments were sampled and transferred to the lab using sterilized polyethylene bags. The sediments were separated into three bases on the salinity top 1–5 cm HS1 (110 PSU), middle 6–15 cm (85 PSU) and bottom 16–30 cm (67 PSU). Physico-chemical properties of sediments were analysed in soil testing lab, Chidambaram, Tamil Nadu (Table 2) followed by the procedure in [1].
Table 2

Abiotic parameters of hypersaline soil.

Physico chemical charactersSample
Temperature (°C)30 ± 1.2
pH7.6 ± 0.3
Salinity (PSU)117 ± 2.672
Macronutrients (mg/g)
Total N6.2 ± 1.50
P1.92 ± 0.062
K9.0 ± 1.98
NH45.76 ± 3.9
S046.59 ± 1.67
Total organic C30.0 ± 7.23
Micronutrients and heavy metals (µg/g)
Al135.4 ± 2.03
B0.631 ± 0.066
Cd0.041 ± 0.004
Co11.59 ± 0.325
Cr1.979 ± 0.023
Cu0.335 ± 0.002
Fe129.7 ± 5.06
Mg43.13 ± 3.23
Mn1.81 ± 0.072
Ni184.4 ± 9.54
Pb0.309 ± 0.008
Zn9.756 ± 2.4
Abiotic parameters of hypersaline soil.

DNA extraction

Briefly, 1 g of sediments were taken from each layer and the DNA extraction was done by using FASTDNA SPIN Kit for soil (Qiagen, Valencia, CA, USA). DNA extraction was conducted in triplicate. The quality and concentration of extracted eDNA were estimated using 1% agarose gel and Nanodrop ND-2000 (Thermo Scientific) [2].

Sequencing

The quality and concentration of eDNA were estimated. Next, the corresponding eDNA were pooled together. 100 ng of eDNA from each layer, 16S rRNA specific V5-V9 primers [3] 939F (5’TTGACGGGGGCCCGCAC3’) and 1492R (5’TACCTTGTTACGACTT3’) primer were used to amplify the fragments using the titanium reagents, Hot Star Taq Plus master mix Kit (Qiagen, Valencia, CA). TEFAP procedures and sequencing were carried out at the Research and Testing Laboratory (RTL), Lubbock, TX, USA using Genome Sequencer FLX System (Roche, Nutley, N.J., USA) based on RTL protocols.

Data analysis

The TEFAP generated sff files (Three) were submitted to NCBI׳s Bio project, BioSample, and SRA. The sequences were quality trimmed according to the procedure in [4], and the sff files were converted into FASTA and QUAL file formats using Mothur v.1.12.0 [5]. Then the sequence was trimmed, aligned, filtered, and the chimers were removed using Mothur commands. Then, the sequences were classified against Silva Database [6]. The sequence data generated in this study can be downloaded from NCBI SRA.
Subject areaBiology
More specific subject areaMetagenomics
Type of DataTable, Figures and 16S rRNA Sequence
How data was acquiredDNA sequence Pyrosequencing was carried in Roche 454 FLX instrument at research and Testing Laboratory (RTL) (Lubbock, TX, USA)
Data formatRaw data sff file
Experimental factorV5-V9 regions of the bacterial 16S rRNA gene were amplified using 939F-1492R oligonucleotide primers.
Experimental featuresThe sediments samples (30 cm) were collected using a corer from Mad Boon-mangrove ecosystem of Pichavaram, Tamil Nadu, India. The eDNA was extracted from the sediments based on the salinity in the sediments and sequenced using Roche 454 FLX sequencer.
Data source and locationMad Boon-mangrove ecosystem of Pichavaram, Tamil Nadu, India. 11 °25’.01 N, 79 °47’ 06.39” E.
Data accessibilityAll sequences generated in this study are submitted to NCBI SRA under the accession numbers SRR627695, SRR63011 and SRR631012
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